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"foliated" Definitions
  1. composed of or separable into layers
  2. ornamented with foils or a leaf design
"foliated" Antonyms

316 Sentences With "foliated"

How to use foliated in a sentence? Find typical usage patterns (collocations)/phrases/context for "foliated" and check conjugation/comparative form for "foliated". Mastering all the usages of "foliated" from sentence examples published by news publications.

Sullivan's famous foliated ornament, in terra cotta, sprouts above entrances.
In Newtonian mechanics, this object is foliated by these planes of absolute simultaneity.
Central Park and the expensive property around it are a bit like that foliated box that held the water sprite's fantasies onstage.
Foliated rock is a product of differential stress that deforms the rock in one plane, sometimes creating a plane of cleavage. For example, slate is a foliated metamorphic rock, originating from shale. Non-foliated rock does not have planar patterns of strain. Rocks that were subjected to uniform pressure from all sides, or those that lack minerals with distinctive growth habits, will not be foliated.
There are two kinds of metamorphic rocks which are foliated and non-foliated. These rocks differ in their structure, appearance, texture, and the way in which they were formed. Foliated rocks have a banded or striped appearance and can split into separate rock fragments. They are formed when unequal pressure is exerted on different sides of a rock.
The larvae of this species web leaves together on the foliated stems of its host plant.
Core rock samples done by Walfried Schwerdtner in the surrounding area, show mostly foliated Grenville Gneiss.
The foliated god is present in the so-called maize tree (Temple of the Foliated Cross, Palenque), its cobs being shaped like the deity's head. A male maize deity representing the foliated type and labeled God E is present in the three extant Maya books of undisputed authenticity Whereas the foliated maize god is a one-dimensional vegetation spirit, the tonsured maize god's functions are much more diverse. When performing ritually, the latter typically wears a netted jade skirt and a belt with a large spondylus shell covering the loins. On stelae, it is a queen rather than a king that tends to represent the tonsured maize god.
The overhang is supported by consoles and foliated ornament. Large red brick chimneys rise from the roof.
The western area is a dominance of layered quartz dioritic to dioritic, tonalitic to granitic gneiss and young foliated granitic intrusions. It shows a formation of the granitic protolith of the layered gneiss at 3.97 Ga, followed by a 3.58 Gyr old granitic intrusion, which has been foliated.
Gneiss, a foliated metamorphic rock. Quartzite, a non-foliated metamorphic rock. Foliation in geology refers to repetitive layering in metamorphic rocks.Marshak, Stephen, Essentials of Geology, W. W. Norton 3rd Ed, 2009 Each layer can be as thin as a sheet of paper, or over a meter in thickness.
Between the south chapel and the chancel is a three-bay arcade with round piers and foliated capitals.
Where both heat and pressure play a role, the mechanism is termed regional metamorphism. This is typically found in mountain-building regions. Depending on the structure, metamorphic rocks are divided into two general categories. Those that possess a texture are referred to as foliated; the remainders are termed non-foliated.
Cataclasite is a fault rock that consists of angular clasts in a finer-grained matrix. It is normally non- foliated but some varieties have been described with a well-developed planar fabric that are known as foliated cataclasites. Cataclasite grades into fault breccia as the percentage of visible clasts increases to more than 30%.
The name of the rock is then determined based on the types of minerals present. Schists are foliated rocks that are primarily composed of lamellar minerals such as micas. A gneiss has visible bands of differing lightness, with a common example being the granite gneiss. Other varieties of foliated rock include slates, phyllites, and mylonite.
The Dalgaringa Supersuite comprises sheets, dykes and veins of 2005–1985 Ma foliated and gneissic tonalite, granodiorite, quartz diorite and monzogranite, intruded by a large pluton of c. 1975 Ma mesocratic and leucocratic tonalite. The oldest, and possibly most abundant, rock type is a mesocratic, foliated to gneissic diorite to tonalite, which is typically pegmatite banded. At any given locality this rock type is intruded by several granite phases, typically in the following order: foliated biotite monzogranite and leucocratic tonalite, then biotite granodiorite and monzogranite and, finally, biotite monzogranite, syenogranite and pegmatite.
Most of the unit is composed of intercalations of differently coloured, pervasively foliated, purplish red or bluish grey varicoloured calcareous shales.
A foliated pattern appears above the granite columns. The cornice, just below the roofline, features small square-cut stone blocks called dentils. The interior has been renovated over the course of years, but it does feature an ornate cast-iron staircase behind the elevator shaft. The newel post is a short, squat column with a foliated capital.
Its forearm length is . Its ears are broad, large, and triangular. Its nose-leaf is complexly foliated with intermediate, anterior, and posterior leaflets.
Familiar examples of non- foliated metamorphic rocks include marble, soapstone, and serpentine. This branch contains quartzite—a metamorphosed form of sandstone—and hornfels.
Folded foliation in a metamorphic rock from near Geirangerfjord, Norway The layering within metamorphic rocks is called foliation (derived from the Latin word folia, meaning "leaves"), and it occurs when a rock is being shortened along one axis during recrystallization. This causes the platy or elongated crystals of minerals, such as mica and chlorite, to become rotated such that their long axes are perpendicular to the orientation of shortening. This results in a banded, or foliated rock, with the bands showing the colors of the minerals that formed them. Textures are separated into foliated and non-foliated categories.
Rocks typical of shear zones include mylonite, cataclasite, S-tectonite and L-tectonite, pseudotachylite, certain breccias and highly foliated versions of the wall rocks.
The picture to the left is a reconstruction as seen from the Temple of the Foliated Cross, although Temple XV is missing from the illustration.
Inside the church the arcade between the nave and the aisle is carried on octagonal sandstone piers. The chancel arch has detached demi-shafts with foliated caps and it springs from corbels carved with angels. Above the east window is a semicircular arch, also springing from shafts with foliated caps. At the west end is a pitch pine gallery, and the organ pipes frame the west window.
In the chancel is a slab carved with a foliated cross, a sword, and a shield. Elsewhere are wall monuments, the earliest of which is dated 1674.
Internally, each side of the church has five pointed and moulded arches which separate the aisle from the nave. The arches are supported by columns with foliated capitals.
The west porch has a four-centred outer arch and foliated spandrels. The body of the church, rebuilt in the 19th century, is in the style of c.1300.
The epipodium is prominent, fleshy, with or without cirri. Frontal lobes are present. The mantle edge is simple or reflexed and foliated. There is no slit in the front.
Calligraphy and Islamic Culture. New York: New York University Press. p. 3. . The style later developed into several varieties, including floral, foliated, plaited or interlaced, bordered, and square kufic.
The two types of fossils can be distinguished by many features, most obvious among which is the suture line: simple in Orthoceras (see image), intricately foliated in Baculites and related forms.
A metamorphic rock showing Gneissic layering. Alternate layers of minerals. Metamorphism where minerals are stretched, mashed and re-arranged in foliated textures. Feldspar and quartz are light layers with ferromagnesian minerals.
Plaque commemoriating James Mooney, 2013 This highly decorative drinking fountain stands on a triangular piece of land at the junction of Queen and Eagle Streets. The foundation and steps are square and built of porphyry (Brisbane tuff). The base is square and built of granite from Mount Alexander in Victoria. It has four corner columns on its granite base, with richly foliated capitals and raised pedestals, surmounted by four Gothic arches which support a foliated and ribbed spire.
The chancel was restored in 1914. The 13th-century chancel has a two-light east window of c. 1350, and just north of it is a foliated corbel-capital, of c. 1230.
Crystals are platy, six-sided and flattened perpendicular to the c crystal axis, and may be striated triangularly on these flattened faces. It may form rosettes, or be drusy, foliated or massive.
A piece of slate (~ 6 cm long and ~ 4 cm high) Slate is a fine-grained, foliated, homogeneous metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade regional metamorphism. It is the finest grained foliated metamorphic rock.Essentials of Geology, 3rd Ed, Stephen Marshak Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression. The foliation in slate is called "slaty cleavage".
Similar motifs made up of straight lines and right angles, such as the "Greek key", are more often called meanders. In art history, a "floriated" or "flower scroll" has flowers, often in the centre of the volutes, and a "foliated" or "leaf scroll" shows leaves in varying degrees of profusion along the stems. The Ara Pacis scrolls are foliated and sparingly floriated, whilst those in the Dome of the Rock mosaics are profusely foliated with thick leaves forming segments of the stems. As in arabesques, the "leaf" forms often spring directly from the stem without a leaf stalk in ways that few if any real plants do; these are generally derived from the ancient half-palmette motif, with the stem running along the bisected edge of the palmette.
The structure was constructed using foliated brickwork and the surface details and finish in exquisite stucco called chunnam using chunnam (shell lime) and mixed with egg white to obtain a smooth and glossy texture. The steps leading up to the hall were formerly flanked by two equestrian statues of excellent workmanship. The pillars supporting the arches are 13m tall and are again joined by foliated brickwork that carries a valance and an entablature rising up to a height of 20 m. The decoration is done, (shell lime).
Shells can have numerous ultrastructural motifs, the most common being crossed-lamellar (aragonite), prismatic (aragonite or calcite), homogeneous (aragonite), foliated (aragonite) and nacre (aragonite). Although not the most common, nacre is the most studied type of layer.
One of the adults positions themselves near the feeding site and scans the surroundings for predators to protect the group during mealtimes. They then retire at night in highly foliated areas to protect themselves from predators during slumber.
Picropharmacolite is usually found as small to microscopic pearly white botryoidal aggregates with a radiating foliated structure internally. Less commonly it occurs as silky fibrous aggregates or minute needle-like crystals, that are rectangular prisms elongated along the c axis.
Inside the church are five-bay arcades carried on cylindrical columns. The capitals are alternately ring moulded and foliated. There is an oak reredos in the chancel, and another in the south transept. The pulpit is octagonal and in stone.
Another striking trait is the black line passing down his eyebrow, through his cheek and finishing at the bottom of his jaw line. These face markings are similarly and frequently used in the late post-classic depictions of the 'foliated' Maya maize god.
The interior is designed and decorated in the Austrian Baroque style. The foyer, between the lobby and main entrance, has red marble staircases decorated in scrollwork, cartouches, and garlands. The wrought iron railing is foliated. Murals by two Hungarian artists decorate the walls.
The rays are one-dimensional curved lines.Arnold, V.I. (1974/1978), p. 250. Thus, a wave is a foliated set of moving two-dimensional surfaces. In classical physics, it is not part of the definition of a wave that it be distinctly vibratory.
Tharwa is in a different geological structural unit than the rest of Canberra, being on the Cotter Horst. The village itself is built on Tharwa Adamellite. This adamellite is coarsely foliated and contains biotite mica. It has been dated at 423 ±6 million years old.
The San Pietro is a former Roman Catholic church in Vitorchiano in the province of Viterbo, region of Lazio, Italy. The main attraction is the foliated Romanesque-style columns in the portal. The peperino stone facade is otherwise undecorated.Comune of Vitorchiano, entry on church.
Additionally, there is some late Victorian stained glass by Heaton, Butler and Bayne. There is a wall monument to Robert Sutton, 1st Baron Lexinton who died in 1668. There are also two medieval memorials, a foliated cross and an effigy of a layman (poorly preserved).
There are angle turrets with conical caps on the top storey. Variations of cable moulding in diminishing courses terminating as foliated stop decorate the corbelling. At the foot of the circular wing, in the re-entrant angle, is the entrance. There is a vaulted basement.
R. acraeus is specific to high alpine environments. It grows in stable, coarse rock fields of non-foliated schist and greywacke. The rocks have been fractured into coarse and angular rocks of different sizes and shapes. The rocks are about 10–30 cm in diameter.
The large east window has stained glass, possibly by William Wailes. The nave arcades are supported by clustered marble piers with foliated tops and moulded lancet arches. There is a two-bay gallery to the west. The chancel is flanked by two lady chapels.
The principal staircase has heavily carved foliated open panels to broad balustrade. A stone screen on the landing was added in 1850 by Francis Ruddle of Peterborough.Images of England No. 49711 National Monuments Record, English Heritage (retrieved 27 January 2008). See also Country Life XVL (p.
He was, and still is, known for using the foliated vine design, which depicts vines and blossoms carved in shallow relief with flat surfaces. There was a network of families in Windsor who dominated the woodworking trade, and John Moore was considered to be at the center.
If is a Lie group, and is a Lie subgroup, then is foliated by cosets of . When is closed in , the quotient space / is a smooth (Hausdorff) manifold turning into a fiber bundle with fiber and base /. This fiber bundle is actually principal, with structure group .
The initiai"H" for Hopkins is centered above the entrance among foliated carvings. The house also features a two-story octagonal tower and a one-story, triangular-shaped window bay. The house is rich in architectural detail and scroll-sawn details are located on the exterior.
The door surround was composed of limestone with an unusual carved limestone pediment supported with carved foliated consoles. The roof is flat. A bracketed cornice built of limestone marks the top of the original section.The granite stairs rise from the sidewalk level to the first floor.
Temple of the Foliated Cross Temple of the Cross.Miller 1999, p. 9. Bas-relief carvings in the Temple of the Cross describe the accession of K'inich Kan Balam to the throne of Palenque. Within the inner chamber of these temples bas-relief carvings are found, depicting two figures.
Mafic rocks are distributed within the entire Acasta Gneiss Complex as minor blocks such as enclaves and bands. The mafic rocks consist of massive to slightly foliated amphibolite, garnet amphibolite as well as hornblendite. Mineral composition indicates that they had experienced metamorphism between amphibolite to upper amphibolite facies.
The result is a distinct boundary of very fine grain igneous rock along the border of the country rock. The surrounding rock may be "baked" through contact metamorphism, resulting in non-foliated metamorphic rocks. Rocks that were originally limestone, quartz sandstone, and shale become marble, quartzite, and hornfels, respectively.
There is a perfect cleavage parallel to the basal plane and the mineral usually occurs in foliated masses of irregular outline. The color is steel-gray, and the luster metallic and brilliant. The mineral is very soft (H = 1.52) and marks paper. The specific gravity is 7.2 to 7.9.
On the Lizard these two types of peridotite are represented by a heavily foliated orthopyroxene (enstatite)-rich serpentinite and less foliated, less orthopyroxene rich serpentinite which is typified by the presence of amphibole (tremolite). The boundary between these two types of serpentinite can be studied at Kynance Cove, and geologically represents the boundary between shallow mantle peridotites from which material has been extracted by melting and deeper peridotite from which no material has been removed. In the area of Ogo dour at the Northern reaches of Predannack, dunite, a highly depleted peridotite derivative which consists of almost pure olivine, is found. Earlier theories, most notably the BGS publication "Lizard & the Meneage"Flett, J. S. (1947).
The Taj Mahal is entirely clad in marble. Marble is a metamorphic rock composed of recrystallized carbonate minerals, most commonly calcite or dolomite. Marble is typically not foliated, although there are exceptions. In geology, the term marble refers to metamorphosed limestone, but its use in stonemasonry more broadly encompasses unmetamorphosed limestone.
The Changchun Schist being mostly greenschist is found on the western side and forms thick beds. It is found along with smaller amounts of chert, and black schist. The rock is foliated dark green rock containing chlorite, epidote, quartz, calcite, biotite, albite and actinolite. They are derived from mafic volcanic rocks.
The chancel contains unique example of ballflowers decoration in the chancel, and with the north transept dates from 1310–30. The rood and parclose screens are also medieval. The foliated crosses on coffin lids in the south aisle are medieval with 14th century tiles. The south porch in 16th century.
The porch has a vaulted ceiling with foliated bosses. The hall is entered through a Tudor arch containing a Gothic-style glazed timber screen. The hall contains a sandstone fireplace with a Tudor arch. Its windows contain stained glass dating from the late 19th century and moved here in the 20th century.
Chloritoid is a silicate mineral of metamorphic origin. It is an iron magnesium manganese alumino-silicate hydroxide with formula . It occurs as greenish grey to black platy micaceous crystals and foliated masses. Its Mohs hardness is 6.5, unusually high for a platy mineral, and it has a specific gravity of 3.52 to 3.57.
The periphery is carinated spinose, bearing about twelve radiating more or less foliated spines upon the body whorl. This body whorl descends deeply toward the aperture. The convex base is concentrically more or less densely squamosely lirate. The outer lirae are generally prominent and subspinose, sometimes causing the periphery to appear bicarinate.
At the top of the tower is a cornice and a solid parapet. Externally on the south side, between the nave and chancel, is a multi-stepped buttress. Built into one of the walls of the tower is a coffin lid dating from the 13th century which is decorated with a foliated cross.
Where a rock has been subject to differential stress, the type of foliation that develops depends on the metamorphic grade. For instance, starting with a mudstone, the following sequence develops with increasing temperature: slate is a very fine-grained, foliated metamorphic rock, characteristic of very low grade metamorphism, while phyllite is fine-grained and found in areas of low grade metamorphism, schist is medium to coarse-grained and found in areas of medium grade metamorphism, and gneiss coarse to very coarse-grained, found in areas of high-grade metamorphism. Marble is generally not foliated, which allows its use as a material for sculpture and architecture. Another important mechanism of metamorphism is that of chemical reactions that occur between minerals without them melting.
At the 15th floor, the piers end in foliated capitals, and the tops of the windows end in elaborate arches. Between each floor are terracotta spandrels, which are recessed behind the piers. The 16th floor serves as another "transitional story" and its windows are surrounded by complex ornamentation.; A cornice runs above the 16th floor.
The formation takes the form of many small dikes and plutons intruding the Moppin Complex. These consist of gray, homogeneous, well-foliated granodiorite. Its modal composition is 57% albite-oligoclase, 27% quartz, 10% biotite, 4% muscovite, and 1% each epidote and microcline. The foliation is defined by biotite knots, up to 2.5 cm in length.
He designed the Palazzo delle Papesse and the nearby Loggia del Papa (1462–63).Encyclopedia Treccani, entry on architect. He may have contributed to the design of Santa Maria delle Nevi. Federighi is considered as the architect who reintroduced the heavily foliated carving and the antique pagan imagery into the vocabulary of Sienese Quattrocento sculpture.
Phaneritic textures are where interlocking crystals of igneous rock are visible to the unaided eye. Foliated texture is where metamorphic rock is made of layers of materials. Porphyritic texture is one in which larger pieces (phenocrysts) are embedded in a background mass made of much finer grains. Fragmental textures include clastic, bioclastic, and pyroclastic.
The monuments and text associated with Kʼinich Kan Bahlam II are: Tablets and Alfardas of the Temples of the Cross, Sun and Foliated Cross; tablets and facade of the Temple of the Inscriptions; Temple 17 Panel; Death's Head; Jonuta Panel; Temple of the Cross Stela.Skidmore 2010, p. 74.Martin & Grube 2008, pp. 168-170.
Tall brick pilasters emphasize the building's verticality. The window openings are topped by terra-cotta spandrels with sharply molded projecting vertical apexes. The spandrels also feature zigzag motifs and stylized foliated decorations. The flat roof contains a centrally placed three-story penthouse tower with a glass-topped greenhouse used for agency studies and experiments.
A third porphyritic granite is . The south east granites moved into the south east about the same time. The components here are called Fort Regent/Elizabeth Castle Granophyre, Dicq Granite, Longueville Granite, and La Roque Granite. The plutonic rocks are not foliated, showing that the orogeny was near completion at the time they formed.
The clock sits above the pedestal. There is a clock face on all four faces which are illuminated at night. Each face is surrounded by a laurel wreath and foliated carving is located in the bottom corners. A hood mould over each face creates a domed surface on which sits a large cable moulding.
The shaft continues to rises to a third basin which is simpler in design and is surmounted by a small boy figure. The final basin is located above the figure's head. The entire shaft, which tapers towards the peak, is heavily ornamented with a variety of design elements, including scrollwork, panels and foliated patterns.
The recessed main entrance, on the bell tower, is flanked by engaged stone columns topped with foliated capitals, rising to an arch echoed in the window treatments in the next two stages. A griffin flanks each side. Brick porches frame the secondary entrances on the east and west. Each elevation of the roof has two dormers with hipped roofs.
The banking chamber structure of a grid of cast iron columns, beams and connecting gothic-styled arches is frankly expressed, and all surfaces above the individually designed gold leaf foliated capitals are elaborately painted in tones of blue with gold leaf highlights. In 1987 it was voted Victoria's favorite building by readers of The Age newspaper.
The building is a white terra cotta structure designed by John Ahlschlager in 1914 for the Schulze Baking Company. The terra cotta walls were five storeys high. The building featured blue lettering, foliated cornice ornamentation, and stringcourses of rosettes. The building uses 700 windows grouped to complement the ornamentation's allusion to themes of nature and purity.
At the base of the pediment, along its central axis, is a small circular window framed by smaller columns and pediment which are framed by a foliated scroll. At the right is the huge, octagonal tower characterized by cantons at its angles and pedimented window openings. The present church and convent was renovated between 1946 and 1971.
The stems branch toward the ends and are densely foliated in toothed, wavy-edged, glandular leaves 2 to 15 centimeters long. The stems and leaves are sticky with exudate. The inflorescences contain clusters of many flower heads, each cylindrical head wrapped in long, flat glandular phyllaries. The flower heads are discoid, containing only disc florets and no ray florets.
It is historically significant mostly for its connection to Henry Dinwoodey, owner of a very successful furniture business in Utah and the broader Intermountain region. Dinwoodey was jailed as a polygamist in the 1880s. and Note this document misspells, using "Dinwoody" rather than correct "Dinwoodey". Squat Romanesque columns with foliated capitals are seen on the porch of the house.
A chandelier hangs from an ornate plaster medallion in the library ceiling. Also in the library is an Italian marble fireplace with colonnettes, paneled spandrels and finely carved friezes and cartouches. It has a cast iron fireboard ornamented with a brass crane. On the south side, the dining room has a similarly foliated band around the ceiling.
The 15th-century rood screen is of five bays. The open panels above have trefoiled ogee heads and the close panels below have cinquefoiled heads with carved foliated spandrels. The screen was formerly in a dilapidated condition and was repaired by the Rev. A. R. Pain with his own hands, after he was appointed to the living in 1845.
Higgins, M.D. (2006) Quantitative Textural Measurements in Igneous and Metamorphic Petrology. Cambridge University Press, Cambridge, UK. The most common parameter is the crystal size distribution. This creates the physical appearance or character of a rock, such as grain size, shape, arrangement, and other properties, at both the visible and microscopic scale. Crystalline textures include phaneritic, foliated, and porphyritic.
A Gneiss with large eye-shaped feldspars Augen (from German "eyes") are large, lenticular eye-shaped mineral grains or mineral aggregates visible in some foliated metamorphic rocks. In cross section they have the shape of an eye. Feldspar, quartz, and garnet are common minerals which form augen. Augen form in rocks which have undergone metamorphism and shearing.
Kahn's design for this building was influenced by McKim, Mead, and White's nearby State Savings Bank.Detroit Trust Company from Detroit1701.org, retrieved February 17, 2010 A series of windows interspersed by plaques with foliated details are set in the attic story. The building was modernized in 1964, and the front section between the columns was rebuilt.
In 1979 a Chern Symposium offered him a honorary song in tribute: > Hail to Chern! Mathematics Greatest! He made Gauss-Bonnet a household word, > Intrinsic proofs he found, Throughout the World his truths abound, Chern > classes he gave us, and Secondary Invariants, Fibre Bundles and Sheaves, > Distributions and Foliated Leaves! All Hail All Hail to CHERN.
Completed in 1920, the two-story, double-wide structure features four columns in the Ionic order. Its various design elements include Greek key, Egg-and-dart, foliated rinceau, rosettes, anthemion, and volutes. First National Bank failed in the Great Depression, and the building was taken over by Jackson State Bank. It now houses a branch of US Bank.
The southern part if the island is largely composed of Icart Gneiss. The Icart Gneiss is an augen gneiss of granitic composition containing potassium feldspar. This was formed from a granite dated at using U-Pb dating on zircon grains. A foliated Perelle quartz diorite (also called Perelle Gneiss), occurs in the centre and west of the island.
Bambusa oldhamii, known as giant timber bamboo or Oldham's bamboo, is a large species of bamboo. It is the most common and widely grown bamboo in the United States and has been introduced into cultivation around the world. It is densely foliated, growing up to tall in good conditions, and can have a diameter of up to .
Above it is an entablature with a frieze decorated with a geometric pattern of red and yellow brick. The cornice is dentilled with plain modillions and shallow panels between. The short roof parapet has limestone coping and, at a higher section over the main entrance, foliated brackets. The middle bay on the east (front) elevation projects.
St Giles' Church is laid out in a cruciform plan and has gabled transepts. The nave has a clerestory and lower aisles with five bays and gabled entrance porches. The interior has an arch-braced roof and a lierne vault at the crossing. The nave is flanked by alternately round and octagonal columns with foliated capitals.
The main entrance's rounded arch with support from thick, foliated columns is a distinct Romanesque touch, however. In recent years its age has made it a difficult building to keep warm in the wintertime. Even with the windows closed, City Hall has been drafty. The city installed Cellular Shades, and later window insulating panels, to keep it warm.
Tierra del Fuego Igneous and Metamorphic Complex is a geological basement complex known from boreholes in northern Tierra del Fuego. The complex is made up of foliated igneous rocks of Cambrian age including orthogneiss. It underlies unconformably the Jurassic Tobífera Formation. The protoliths of Cordillera Darwin Metamorphic Complex are unrelated to Tierra del Fuego Igneous and Metamorphic Complex despite present-day proximity.
The maximum reported size of this species shell is 114.9 mm. Vasum cassiforme has a large, thick and heavy shell, presenting 8 whorls. One of its most striking characteristics is its rich ornamentation, with foliated cords and spines over the body whorl and shoulder, respectively. It is colored cream or light brown externally, while the aperture may be colored purplish-brown.
Inside the church is a horseshoe-shaped gallery carried on thin cast iron columns with Ionic caps, and with a foliated balustrade. The ceiling is coffered with glazed panels in the centre. The original pipe organ was built by Gray and Davison and had two manuals. This was replaced in 1881 by a three-manual organ built by W. E. Richardson.
William Phillips (1773–1828) lists the mineral under SILEX, and describes it as follows: According to Parker Cleaveland (1780–1858) the mineral is probably a variety of Fettstein. Cleaveland defines it as follows: Webster's 1828 English Dictionary gives: :GA'BRONITE, n. A mineral, supposed to be a variety of fettstein. It occurs in masses, whose structure is more or less foliated, or sometimes compact.
It is foliated and white to cream with biotite and feldspar in large crystals.P R Williams and E B Corbett, : Geological Survey Explanatory Report Geological Atlas 1:250,000 series sheet SK55/7 Port Davey 1977 The Meredith Batholith contains biotite adamellite. It contains ten separate plutons. A contact aureole of 2.5 km thickness surrounds the batholith in the form of albite epidote hornfels.
To the north, the Isua supracrustal belt is bounded by orthogneiss. Dominant tonalitic gneisses shows a protolith age of about 3.7 billion years ago. A low strain area of several square kilometres are observed at the immediate north to the Isua Belt. Dominant phases are foliated metatonalites, in which several localities shows 3660 Ma diorite and 3655 to 3640 Ma granite and pegmatite.
From the meseta, a flight of balayong stairs led to the wide caida with its panoramic view of Balayan Bay. The hardwood floors of the upper floors, the elaborately carved and gilded foliated transoms over the double doors carved with ogee panels in the formal rooms and walls and ceilings stretched with handpainted canvas are typical of the 1850s Taal houses.
The font consists of a small octagonal bowl; its cover is inscribed with the date 1662. Also in the church is a poor box, cut from a log, and dated 1648. Only the east window contains stained glass; this dates from 1926 and is by Powells. In the south transept is a coffin lid from the 13th century, carved with a foliated cross.
Each level is articulated in a slightly different way and distinguished by belt courses that encircle the building. Round arches of polished granite, which feature rosettes and cable moldings, dominate the first story. The arches spring from carved posts with foliated motifs. Rectangular windows surrounded by contrasting trim are on the second floor, while round-arch openings are on the third floor.
An ornate oval medallion with a garland, acanthus leaves, and a shell motif tops the doorway. Rectangular, first-story windows have flat arches with projecting keystones. A colonnade that features paired Ionic columns with stylized foliated motifs and unusual tassel ornamentation dominates the three central bays of the second and third stories. Small balustrades with urn-shaped members extend between the columns.
Lepidium fremontii is a robust perennial herb producing a branching, tangled gray stem to about a meter in height. The many sprawling stems are foliated in linear leaves up to about 10 centimeters long which may have several fingerlike lobes. The plant produces thick racemes of many small flowers. Each flower has spoon-shaped white petals just a few millimeters long.
A common cornice with bead and reel molded cornice set off by a simple chair rail and dado paneling unites all areas. Decoration continues above the cornice with cyma recta moldings in egg-and-dart and Greek fret and foliated patterns below carved modillions on the cornice. Above the cornice is a triple fascia. The rooms are entered through portals with sliding doors.
The apatite is fluorapatite and the amount of CO2 varies.Härmälä 1981 Glimmerite is intensely foliated, greenish black, dark or reddish brown rock (depending on the dominating mica mineral) containing 0-15 % carbonate minerals. The oriented rocks are fine- to medium-grained and usually porphyritic. The matrix is composed of fine-grained, aphanitic phlogopite and the porphyroclasts are tabular phlogopite grains.
Phlogopite occurs as disseminated flakes, tabular crystals and lamellar or foliated aggregates. The grain size of the micas varies from only a couple of µm to several centimetres, the average size is 1–2 mm in diameter.Härmälä 1981 The phlogopite is altered into brown biotite-phlogopite in the shear zones, and in the most intensely sheared zones, into biotite and chlorite.O’Brien et al.
The design is generally Romanesque in style, including in its type of stonework and features such as a semicircular arch, vermiculated stone sills, short columns with foliated capitals, and cone-shaped roofs on its tower. With It was completed in 1901. The 1901 building is now a museum called the Wyoming Frontier Prison. Visitors can go on guided tours through the old prison.
The walls are wainscoted, and the ceiling is made of boxed beams and wood sheathing. Foliated stencilwork lines the sheathing, while the beams have a multicolored stencilwork pattern on their bottoms. The angled portions of the ceiling are also decorated with foliate stencils. Windows on the building sides have colored sections, and the buildings sole interior light source is a kerosene chandelier.
Sometimes women create foliated borders using finger-tips on the wet coating. The patterns are termed hangaiyan. Tadvalkar (2011) states that the "cow-dunging process is known as lipna in the region, whereas the floor art is referred to as likhnoo (writing), dehar (with respect to dehali, the threshold) or chowk". The background is painted with brown coloured earth (loshti).
It has three mihrabs with the central mihrab being the largest in size and projecting outwards. It has a hemispherical dome with frontal arches. There are also squinches and half domes. It is distinctly different from the Khan Jahan style mosque in its exterior decorations, particularly the east façade, which depicts four rectangular panels bordered by foliated scrolls with merlons having plant motifs.
A colonnade of trefoil arches and foliated capitals forms a screen to the platform. The same arch form being employed for both ends of the platform and for the octagonal porte-cochère to the west. The station building is above street level, with a flight of stairs leading to the platform level. Ramps to the north and south were used for carriages.
The clerestory has three three-light windows and one five-light window on each side. Along the side of the south aisle are three four-light windows. The south chapel has a four-light south window, and a five-light east window. Between the aisle and the chapel is a rood turret with a polygonal roof and a foliated finial.
The bedrock in the region surrounding Caracas is mainly metamorphic. From the coast and extending approximately inland, deeply foliated schist of the Mesozoic Tacagua Formation is exposed. Soils forming on them are fine-grained (clayey), thin (), and often colluvial. Although the A horizon of the soil is often less than thick, the bedrock is often weathered down to greater than .
The church comprises a central nave with gable roof and two aisles. The walls are of red sandstone with limestone dressing. The aisles are at either side of the nave, which is covered with a gable roof. The ridge of the roof is decorated by ornamental ironwork, partly gilt, terminated at the western gable by an ornamental cross with foliated arms.
The lodge is built in brick with stone banding and dressings on a stone plinth in 1½ storeys. It is roofed with red tiles. It has two gables, each with pargeting decorated with foliated geometric patterns. The windows have moulded stone surrounds; those on the ground floor have camber arches and on the upper floor the window arches are semicircular.
All Saints ChurchA long, cruciform church of ca1300, although the north transept has been demolished. Much restoration has been carried out on the building, most recently in 1959-60 by John Seely, Lord Mottistone. The large geometric windows cannot be relied upon and may have once been foliated. The south doorway and porch is in a good state, as is the West tower.
The facade is made of ashlar, of a similar color to the rest of the building. A doorway leads to a cellar on the wing's western facade. The ground floor contains three arched windows on the western and eastern facades, and two doorways on each side of the southern facade. The second and fourth floors contain compound arched windows, while the third floor contains foliated banding.
The rail, however, curves into the transverse section, rather than continuing perpendicular to the runs of the stair. The delicate foliated stair brackets are thereby forced to constrict and form a frieze-like pattern on the curved section. The brackets are similar to ones illustrated in Owen Biddle "The Young Carpenter's Assistant" (1810). The molded handrail is supported by plain balusters that are square in section.
The roofline features a parapet roof with a molded cornice below featuring small lion's heads. The frieze has other features of the style, such as anthemion brackets, egg-and-dart and dentil moldings. Further down the facade are found pilasters with foliated capitals. Immediately adjacent on either street are older, more Italianate buildings which housed the store's operations before the construction of the main building.
Santa Monica de Angat Parish Church was designed in Baroque architectural style. This could be verified with the existence of 18 adobe posts, along with eight windows. Windows, statued niches, and spaces between horizontal string courses, dividing the front facade into three parts, were ornamented with floral carvings. Also, foliated crestings on the raking course of the pediment were used as an added ornamentation.
Schorn and Wehr placed the different detached organ fossils in the same species based on a number of factors. Where visible, all the cone scales have bracts and are morphologically similar. The scales display impressions on the admedial surface of wing seeds that match the fossil seed dimensions. The needle arrangement is consistent on both foliated and defoliated axes, with attached needles matching isolated needles.
View of the corridor around the courtyard of the palace Upon entering into the gates of the palace, the visitor enters into present day’s huge central courtyard measuring 3,700 m² (41,979 sq ft). The courtyard is surrounded by massive circular pillars. Now it has a circular garden. A view of the interior of the palace, with an arcade of columns enriched with foliated brick arches.
The rocks that make up the feature consist of hornblende-biotite monzogranite gneiss that are medium to coarse-grained and moderately foliated containing minerals such as perthite, quartz, hornblende with accessory biotite, opaques, apatite, and zircon. The original rock that underwent medium metamorphism was granite. The estimated age of crystallisation is 702 ± 7 million years. The Cape to Cape Track passes near the lookout over the rocks.
With increasing serpentinization knot-like clusters of colourless, magnesium-rich chlorite, meshes of serpentine minerals, and felt-like aggregates of colourless amphiboles (tremolite), talc, anthophyllite and pargasite occur. In foliated serpentinites newly formed chlorite is more common. Chlorite grows in leaf- like layers paralleling the regional foliation. This process can even lead to chlorite schists observable at La Rougerie, Cussac, Lageyrat, La Boissonie and Champagnac-la-Rivière.
Akal-n-iguinawen – land of the black). The gate was called Bab al Kohl (the word kohl also meaning "black") or Bab al Qsar (palace gate) in some historical sources. The corner-pieces are embellished with floral decorations. This ornamentation is framed by three panels marked with an inscription from the Quran in Maghrebi script using foliated Kufic letters, which were also used in Al-Andalus.
The priest's door is in the north wall of the chancel chapel, as the rectory is on this side of the church, and has over it externally a curious little projecting hood. Above the chancel arch is a picturesque stone sanctus bell-turret with panelled sides surmounted by a short broach spirelet with foliated finial. The ceiled wagon roof is tiled in Cotswold stone.
The hyaline, white shell has a fusiformshape. Its length measures up to 25 mm but generally no more than 15 mm. The small protoconch is smooth and consists of little more than one whorl. The teleoconch contains 6-7 whorls bearing a very strong median keel and delicate, foliated varixes (6-9 on the body whorl) forming elongated projections at their intersection with the keel.
The main entrance is flanked by fluted floral-topped wooden pilasters that support an entablature with similarly foliated cornice. Above it a plain frieze reads "Hudson, N.Y., 12534." The entire entry is surrounded by a large arch with a decorated marble surround, featuring rosettes, an archivolt with interlocking wooden circles. It is topped by an architrave with carved guttae and a deep cornice with modillions.
Consider an -dimensional space, foliated as a product by subspaces consisting of points whose first coordinates are constant. This can be covered with a single chart. The statement is essentially that with the leaves or plaques being enumerated by . The analogy is seen directly in three dimensions, by taking and : the 2-dimensional leaves of a book are enumerated by a (1-dimensional) page number.
New York: Simon & Schuster Inc. Phyllite has fine-grained mica flakes, whereas slate has extremely fine mica flakes, and schist has large mica flakes, all mica flakes of which have achieved a preferred orientation. Among foliated metamorphic rocks, it represents a gradation in the degree of metamorphism between slate and schist. The minute crystals of graphite,Schumann, Walter, (1993) Handbook of Rocks, Minerals, & Gemstones.
It was built in Islamic style with a high, domed tower in the center, domed pavilions at the corners, minarets and multi-foliated arches in the facade. The palace is divided into two parts: the front is for males and the rear for females. The most important portion is the drawing room in the front with a fireplace, moulding and an ornamental ceiling painted with gold powder.
Within the church, the aisles are lit by Decorated Period windows. Much medieval stonework is in evidence with moulded doorways and ballflower ornaments and carved foliated bosses. The church is especially noted for its fine 15th-century tie-beam roof, supported by stone corbels with sculpted heads and carved wooden angels with outspread wings. In the nave roof, the braces feature carved figures of the apostles.
Here Jürgen Christian Findorff had built a new church for the marsh colonists in 1781–1785. Wilhelmy built new casework below the original Hauptwerk impost and rearranged the structural housing of the two manuals. The Mittelwerk, originally sited behind the Hauptwerk, was re-installed in the new lower case as a Brustwerk. In the doors in front of the Brustwerk are foliated wooden pipe dummies.
These are double- winged and filled with openwork carving of acanthus leaves and volutes. The box-shaped Oberpositiv front has four pipe-flats with wide-scaled, foliated dummy wooden pipes, and towards the choir there is another pipe flat. On the Oberpositiv flat-carved ornaments are used. The polygonal pedal tower on the crossing pier is crowned by a volute and a trumpeting angel.
Akal-n-iguinawen – land of the black). The gate was called Bab al Kohl (the word kohl also meaning "black") or Bab al Qsar (palace gate) in some historical sources. The corner-pieces are embellished with floral decorations. This ornamentation is framed by three panels marked with an inscription from the Quran in Maghrebi script using foliated Kufic letters, which were also used in Al-Andalus.
The pointed tower arch, of three chamfered orders, is blocked and flanked by semi- circular headed niches. The chancel arch is pointed, has dog-tooth moulding and is supported on short columns with foliated capitals. Similar detailing has been used by Street throughout the chancel. Throughout the church there are wagon roofs, plastered in the nave and aisles and ornately painted in the chancel and transepts.
They sit on a base with foliated designs at the centre and corner of each face. Above the first basin is a square pedestal with moulded festoons on each face. This is surmounted by an urn-like element with four small winged griffins and scrollwork at the top, which is the support for the second basin. This is also has scalloped edges and heads of gargoyles.
Some authors believe that there was an unconformity during the Brioverian succession, as there are phtanite stones in the upper parts believed to be eroded from the lower parts, but this is still inconclusive. Cadomian magmatism has been dated in the intrusions and volcanics as . Foliated quartz diorite occur at Baie de St Brieuc, at Coutances, La Hague, Guernsey, Alderney and Sark. These are only roughly dated .
Chert or flint may become a finely crystalline quartz rock; sandstones lose their clastic structure and are converted into a mosaic of small close-fitting grains of quartz in a metamorphic rock called quartzite. If the rock was originally banded or foliated (as, for example, a laminated sandstone or a foliated calc-schist) this character may not be obliterated, and a banded hornfels is the product; fossils even may have their shapes preserved, though entirely recrystallized, and in many contact-altered lavas the vesicles are still visible, though their contents have usually entered into new combinations to form minerals that were not originally present. The minute structures, however, disappear, often completely, if the thermal alteration is very profound. Thus small grains of quartz in a shale are lost or blend with the surrounding particles of clay, and the fine ground-mass of lavas is entirely reconstructed.
The base is three stories tall and clad with Fox Island granite. There are segmental arches at ground level, and a cornice runs above the second story. At West Street, there are single-width arches within the outermost bays, and double- width arches in all the other bays. The center bay consists of a double-height arched entrance flanked by red marble columns, foliated bosses with tracery, and a sign saying .
The Lady Chapel has lancet windows, foliated ornaments and a groined roof. The tomb of Charles Booth, bishop and builder of the porch, is in the sixth bay of the nave on the north side, guarded by the only ancient ironwork left in the cathedral. On the south side of the nave is the Norman font, a circular bowl large enough to allow of the immersion of children.
The Queen Anne is found in its irregular plan, wraparound porch, full-height bays, small second floor porch, and the small screened porch. The Colonial Revival is found in the Ionic fluted porch columns, and the consoles with a row of dentils located along the cornice. The house also features foliated designs on the gable ends. It remained in the Weis family into the 1930s when it was converted into apartments.
The proscenium arch, rising to above the stage floor, is decorated with alternating octagons, foliated candelabras and other foliate motifs. On either side it has fluted Corinthian pilasters and engaged columns with Adamesque carvings in the surrounding walls. It is topped by a highly detailed entablature, its cornice decorated with lions' heads, anthemion leaves, dentils and egg-and-dart molding. The frieze features steer skulls, candelabras, shields and swag.
The unit is a pink fine- to medium-grained rock with microcline megacrysts in some locations. It is subtly foliated in some locations, particularly to the south. The lithology was originally assessed as granitic with some quartz monzonite. The modal composition is 40 to 50 percent microcline-microperthite, 18 to 21 percent plagioclase (An24), 24 to 37 percent quartz, 2 to 3 percent biotite, and 1 percent muscovite.
The body of Cymbula adansonii consists of a central apex with a concentric outer crossed- foliated shell layer. Each shell has repeating layers that connect with each other and share a common center. Shells of Patellidae gastropods have various levels of finely detailed structure with multiple layers on each respective species’ shell. The number of shell layers vary from four to six and are classified in regards to the myostracum.
The ribbed vaults of the three naves – all of equal height – are supported by sturdy compound piers. The tops of the vaults reach heights of 21 metres. The tall compound piers are based on those in the cathedrals of Minden and Paderborn. The naturalistic capital ornamentation of the compound piers in the Marienkirche bears a resemblance to the foliated capitals at the Elisabethkirche in Marburg and at Minden Cathedral.
The black-breasted buzzard is usually monogamous, forming lifelong pair-bonds. The buzzard nests in trees of notable height and girth, larger and more independent from others generally available. The trees may be dead with bare exposed limbs, or live and foliated, with nests positioned in prominent forks high up in the canopies. Both parents contribute equally to nest-building and often work together in unison on the nest structure.
The niches created in the walls are of rectangular shape and have carved sculptures of gods, demi-gods and the kings. The skirting around the images are of wild aquatic animals with "foliated tails and open jaws." The wall pilasters have curved brackets, and columns on the porch provide support to an overhanging eave; arch windows occasionally carved with images are located above them. The mouldings culminate in parapets.
The main entrance has a large foliated arch supported by clusters of short columns, all in the Richardsonian Romanesque style. A very old flat- roofed addition on the back (north) side is made of matching materials, and matches the exact style. This addition houses the present-day City Council meeting room. A highlight of the interior is a fine oak staircase, which leads to each floor, and up to the tower.
On the other hand, non-foliated rocks have a more solid appearance consisting of a collection of small particles and no layers. These rocks are created when they are exposed to direct pressure. The lake also consists of various clay and plastic soils. These mechanically engineered soils are maintained and constructed with artificial enforcing, which adds a stabilization factor, and solidifies the lake so it won't break down and wear away.
The Wawa subprovince is a formerly active volcanic island chain, consisting of metamorphosed greenstone belts which are surrounded by and cut by granitic plutons and batholiths. These greenstone belts consist of felsic volcanics, felsic batholiths, felsic plutons and sediments aged from 2,700 to 2,670 million years old. The predominate rock type is a white, coarse-grained, foliated hornblende tonalite. Minerals in the tonalite are quartz, plagioclase, alkali feldspar and hornblende.
British Library Additional MS. 70513, See British Library Catalogue of Illuminated manuscripts, detailed record (with Bibliography and images).Read the Lives at the Electronic Campsey Project (Margot/University of Waterloo). A Latin Psalter which belonged to the priory, apparently produced c. 1247–1249, with superbly foliated initial letters, includes Calendar references to the East Anglian saints Seaxburga, Wihtburga and Edmund the Martyr, and has additions referring to Edmund Rich, Modwenna, etc.
The codex contains the text of the four Gospels, on 229 parchment leaves (24.2 cm by 16 cm). The leaves are not foliated. The text is written in one column per page, 24 lines per page in minuscule letters. The text is divided according to the (chapters), whose numbers are given at the left margin of the text, with their (titles) at the top or bottom of the pages.
At each corner is a column with foliated capital set in a rectangular recess, and each face has two pilasters either side of a semi-circular headed recess. The entablature consists of architrave, frieze and projecting cornice, with a panelled pediment at the centre of each face. 1902 is inscribed on the pediment of the east face. The lifelike statue stands larger-than-life at approximately in height.
Phyllite thumb Photomicrograph of thin section of phyllite (in cross polarised light) Phyllite is a type of foliated metamorphic rock created from slate that is further metamorphosed so that very fine grained white mica achieves a preferred orientation.Stephen Marshak Essentials of Geology, 3rd ed. It is primarily composed of quartz, sericite mica, and chlorite.Mottana, Annibale, Rodolfo Crespi and Giuseppe Liborio (1978) Simon & Schuster's Guide to Rocks and Minerals.
Gray succeeded Brockett in this position after the latter's death. Brockett died on 12 July 1768 after a riding accident while returning from Hinchingbrooke, near Huntingdon, to Cambridge. He was buried according to tradition at Gainford by torchlight, probably the church's last nocturnal burial. An ancient foliated cross in the porch of Gainford church, Co. Durham, is superinscribed as memorial to Lawrence Brockett, MA, BD of Trinity College, Cambridge.
Beyond to the south is a carved oak staircase with fluted and foliated balusters, a York motif, standing on steps with scrolled panelled ends. The staircase is supported by a Corinthian column and may have been moved at some point. The floor is paved with black and white marble squares. There is a panelled drawing room leading to an enormous ballroom occupying the western of the two wings added .
A medium to large, spreading tree, growing up to 20 metres, but more commonly from 5 to 10 metres depending on conditions. Canopy spread can vary between 5 and 15 metres. Trees grown in poor soil or in very dry conditions tend to be smaller (about 5 metres tall with a 5-metre canopy spread) and more sparsely foliated. Trunk form varies from specimens with single trunks to low-branching specimens with multiple trunks.
Shell layers are numbered m+3, m+2, m+1, m, m-1, and m-2, starting from the edge of the shell moving inwards to the center. The orientation of Cymbula adansonii's inner (m+1) shell layer is radial while its width is narrow. Cymbula adansonii has a cross-foliated center (m-2) shell layer composed of calcium carbonate. Cymbula adansonii has a set of radula that are not visible from its back side.
The building itself is a three-bay blue granite structure with a steep gabled nave. On the east (front) facade is a narthex with an engaged bell tower on the southern end. It is topped with a steeply pitched slate roof, with a corbeled cornice and lancet windows below. The main entrance, a pair of heavy wooden doors in the center of the narthex, is framed by recessed columns with foliated capitals.
It is very unusual to find both a merchant's mark and a coat of arms on the same monument,Davis, p.22 as the social classes of merchant and gentry were distinct. The two outer pinnacles are continued down till their bases from the extremity of the diapered band at the bottom upon which the figures stand. The centre pinnacle has a foliated capital and is continued till its base rests on the diapered band.
The Faribault County Courthouse in Blue Earth, Minnesota, United States, is listed on the National Register of Historic Places. The building was completed in December 1892 at a cost of $70,000. Materials included Kasota limestone, sand from the Blue Earth River bottoms, red brick above the rusticated sandstone ground floor, and clay tile for the roof. The arches at the entrance rest on short columns with foliated capitals, a hallmark of the Richardsonian Romanesque style.
A secondary entrance, located on the east elevation, features a limestone surround with a decorative lintel carved with a foliated motif. An original cast-iron light fixture with replacement globe extends from the lintel. The rear elevation contains an original U-shaped light court. The chimney, clad in brick and topped with a limestone cap, extends from the southeastern corner of the low-pitched hipped roof, which is covered with standing-seam metal.
But the voussoirs is similar to that at Shobdon within a sequence of zodiacal beasts. There are two coffin lids in the church with foliated crosses. The early 14th century church of St George's has a single nave and chancel with an arcade of two bays and double-chamfered arches have a date of c1320, and two bays were added c. 1333–40. The north aisle was probably built after 1300Salter, p.
Blocks are nearly always angular to sub-angular and roughly equidimensional. If the parent rock is flow-foliated lava, sedimentary material or schistose metamorphic rocks, the blocks may have a plate-like or slab-like form. In other cases, blocks derived from great depths may resemble polished water-worn pebbles and are cobbled due to fluidisation and upwards transport. Blocks can be enormous and may be transported great distances from the volcanic vent.
This is a calc-alkaline tonalitic rock. The foliation was formed at around during the Cadomian Orogeny. Rafts of metamorphosed sediments, older than the Foliated Perelle Diorite are embedded between them. The Pleinmont Formation consists of metamorphosed sediments is of unknown age, although it has been proposed that these belong to the Brioverian group that outcrop on nearby Jersey It is named after Pleinmont Point on the south west tip of the Island.
The white and gold wooden structure is placed on a column with a foliated Gothic capital. The balustrade and the rear wall is decorated with simple blind tracery. The abat-voix forms a canopy with the usual symbol of the dove and a statue of Saint Paul (?) on the top. A painting of the interior by Martin van Meytens from 1760 shows another simple, rectangular pulpit with the statue of the Madonna on the top.
Foliated-dish, white glaze, 15-16th century Daughters of the demon Mara, glazed terra cotta, 1460-1470, southern Myanmar Burmese ceramics refers to ceramic art and pottery designed or produced as a form of Burmese art. The tradition of Burmese ceramics dates back to the third millennium BCE. Pottery and ceramics were an essential part of the trade between Myanmar and its neighbours. The village of Kyaukmyaung (Sagaing) is an important traditional production centre.
General View of The Agriculture of the County of Ayr; observations on the means of its improvement; drawn up for the consideration of the Board of Agriculture, and Internal Improvements, with Beautiful Engravings. Glasgow. p. 318 The bridge's cast iron parapet is a repetition of the pointed Gothic arch design of the castle, surmounted by a battlement, and relieved in the centre with foliated pinnacles.Millar, A. H. (1885). The Castles and Mansions of Ayrshire.
However, their ability to adapt gives hope that this factor will not severely affect their population numbers. Moustached tamarin monkeys select densely foliated areas for resting and sleeping to best camouflage themselves because their small size makes them an easy target. Their main tactic is to avoid predation by attracting as little attention as possible. Their predators include eagles and other birds of prey, snakes, tayras, jaguarundis, ocelots and other wild cats.
St Andrew's is constructed in sandstone ashlar. The spire is roofed in stone slates, and the rest of the church in red tiles. Its plan consists of a five- bay nave with a porch, a south baptistry projecting at the western end, a chancel at a higher level with a vestry to its north, and a north tower. The porch is open, forming a narthex, and is supported on grey stone columns with foliated capitals.
Talc is a clay mineral, composed of hydrated magnesium silicate with the chemical formula Mg3Si4O10(OH)2. Talc in powdered form, often combined with corn starch, is used as baby powder. This mineral is used as a thickening agent and lubricant; is an ingredient in ceramics, paint, and roofing material; and is a main ingredient in many cosmetics. It occurs as foliated to fibrous masses, and in an exceptionally rare crystal form.
The Bündner schists were deposited in the two small oceanic basins (the Valais Ocean and the Piemont-Liguria Ocean) that were located south of the European continent in the Mesozoic era. They formed a kilometers thick monotonous layer of dark clays, marbles and sandy limestones. These sediments were subducted to great depths during the Alpine orogeny. The resulting metamorphism and deformation turned them into calcareous phyllites and schists, strongly foliated rocks rich in micas.
In Maya oral tradition, maize is usually personified as a woman \- like rice in Southeast Asia, or wheat in ancient Greece and Rome. The acquisition of this woman through bridal capture constitutes one of the basic Maya myths. In contrast to this, the pre-Spanish Maya aristocracy appears to have primarily conceived of maize as male. The classic period distinguished two male forms: a foliated (leafy) maize god and a tonsured one.
Although the two intrusions have the same trend and are of similar age, they are not thought to be related. In detail, three separate outcrops have been identified using a combination of radiometric data and seabed sampling. The granite is fine to medium-grained, unlike the megacrystic granite typical of the Cornubian batholith intrusions, although this may be due to the low level of sampling available. A foliated granite is locally developed as a marginal facies.
The Pace–King House, also known as the Charles Hill House, is a historic home located in Richmond, Virginia. It was built in 1860, and is a large two-story, three bay, Italianate style brick dwelling. It has a shallow hipped roof with a richly detailed bracketed cornice and four exterior end chimneys. It features a one-story, cast-iron porch, composed of a wide center arch with narrow flanking arches, all supported on slender foliated columns.
Another column can now be observed up close in the St. Peter's Treasury Museum. Other columns from this set of twelve have been lost over the course of time. If these columns really were from one of the Temples in Jerusalem, the spiral pattern may have represented the oak tree which was the first Ark of the Covenant, mentioned in Joshua 24:26. These columns have sections of twist-fluting alternating with wide bands of foliated reliefs.
The north transept has an aisle of two bays, intricate rib vaulting and small bosses. The aisle has circular piers with square abaci and delicate capitals. The south transept—formerly the separate chapel of the Knights Templar—is linked to the rest of the church by a 19th-century arch and doorway. The chapel, built at a lower level than the church, is rib-vaulted and has a series of foliated capitals in a style similar to the Corinthian.
The bedrock that comprises the shoreline and landscape that lies inland of the Nastapoka arc largely consists of Archean age rocks of the Superior craton. In areal distribution, these rocks consist of about 60% Archean granitic plutons and granitic gneiss. The granitic rocks include typically foliated granodiorites, quartz diorites, quartz monzonites, granites; related intrusive rocks; and their metamorphosed equivalents. Less common in occurrence are layered gneisses, migmatites and hybrid rocks that often form easterly trending linear belts.
This church is first documented in 998, when the Marquis of Tuscany, Ugo, donated this church the Abbey of Marturi. In 1046, it is cited as being under the Pieve di Sant’Agnese a Castellina in Chianti. The stone façade of the church is simple but decorated in foliated reliefs on the round portal. The mullioned window above the portal has a mysterious dedication to R, S, A, Ω. The apse has columns with decoration with human and animal forms.
It is densely foliated in thick green leaves which are hairless lower on the stems and velvety to hairy toward the tips of the branches. The inflorescences at the ends of the stems are dense with small, pointed leaves between which the flowers emerge. Many of the flowers are cleistogamous, meaning they self-pollinate without opening, while others open to reveal four bright pink darkly veined notched petals. The fruit is a small capsule a few millimeters long.
Gneissic rocks are usually medium- to coarse-foliated; they are largely recrystallized but do not carry large quantities of micas, chlorite or other platy minerals. Gneisses that are metamorphosed igneous rocks or their equivalent are termed granite gneisses, diorite gneisses, etc. Gneiss rocks may also be named after a characteristic component such as garnet gneiss, biotite gneiss, albite gneiss, etc. Orthogneiss designates a gneiss derived from an igneous rock, and paragneiss is one from a sedimentary rock.
On the north side of the central hall are library and parlor with high ceilings. Their plaster molding features a band with a talon motif over a cornice with an acanthus band and a broad ribbon of flowers and leaves. Below that is a frieze with meticulously detailed plaster heads of noteworthy literary figures encircled and connected by oak leaves and acorns. The doorways and windows are framed by fluted Corinthian pilasters with foliated entablatures atop.
The charnockite suite or series is a particularly widespread form of granofels. Granofels are one of the few non-foliated rocks to form under relatively high temperatures and pressures. This combination is generated only deep in the crust by tectonic forces that operate on a grand scale, so granofels is a product of regional, rather than contact, metamorphism. It is formed mostly from the granite clan of rocks, or occasionally from thoroughly reconstituted clays and shales.
At the site of a tomb chamber, slabs from the sides and end of a large purbeck marble tomb chest of the later 14th century were found, of very fine workmanship. The long sides had each formed nine panels with half pedestals and foliated canopies for mourner figures, the capitals of their columns sculpted with heads and small animals. Between the canopies were recesses for heraldic shields. This was possibly the tomb of the 2nd Earl.
Inside, nave has four-bay arcades of pointed arches chamfered in two orders. The columns have foliated capitals and are of four clustered shafts, except for the eastern bay, which is wider and is separated from the others by a round column. The nave roof trusses have tie-beams, king- posts rising to the ridge, and arch-braces rising from the tie-beams to meet the king-posts below the ridge. The chancel arch is moulded.
Also projecting from this base at the four corners of the pedestal are free standing round columns with simple Doric order bases and capitals. These support a cornice with curved pediment detail above which on the southern side is carved ornament of foliated scrolls and a central anthemion element. Surmounting the pedestal is the digger statue, which is slightly smaller than life size. The soldier stands to attention and with his head bowed his rifle reverse.
A porphyroblast is a large mineral crystal in a metamorphic rock which has grown within the finer grained matrix. Porphyroblasts are commonly euhedral crystals, but can also be partly to completely irregular in shape. The most common porphyroblasts in metapelites (metamorphosed mudstones and siltstones) are garnets and staurolites, which stand out in well-foliated metapelites (such as schists) against the platy mica matrix. A similar type of crystal is a phenocryst, a large crystal in an igneous rock.
Igneous rocks can become foliated by alignment of cumulate crystals during convection in large magma chambers, especially ultramafic intrusions, and typically plagioclase laths. Granite may form foliation due to frictional drag on viscous magma by the wall rocks. Lavas may preserve a flow foliation, or even compressed eutaxitic texture, typically in highly viscous felsic agglomerate, welded tuff and pyroclastic surge deposits. Metamorphic differentiation, typical of gneisses, is caused by chemical and compositional banding within the metamorphic rock mass.
All of this ornamentation is in turn framed by a long frieze carved with an inscription from the Quran in foliated Kufic letters. The inscription includes excerpts from the Surah al-Hijr. On either side of the decorated facade are pilasters which are sometimes thought to have supported a canopy or awning but which is believed by many scholars to have been merely a decorative transition between the decorated facade and the flanking bastions of the gate.
The site is noted for the size of its buildings as well as number and large number of glyph inscriptions. It is the site of the tomb of King Pakal, discovered in the 1950s, one of the most important Mayan discoveries of the 20th century. The largest and most complex structure is the Palace with its four-story tower. Other important structures include Temple of the Cross, Temple of the Foliated Cross and the Temple of the Sun.
The oak cover is a memorial to two members of the Hall family who fell in the First World War. Pulpit This seems to have been made for some other church where the steps would have wound round a pillar. The Caenstone body rests on serpentine shafts with foliated capitals. and three of the panels contain carved representations of preaching – Christ in the centre, and St Peter and St Paul on the left and right respectively.
Schele's "Hun-Nal-Ye" used to be popular; more recently, "Ixim" (maize grains) and "Nal" (wet ear of corn) are being considered. In a general sense, maize relates to the day Qʼan (ripe or ripeness). The appearance of the tonsured maize god is connected to the base date of the Long Count, 4 Ahau 8 Cumku. The head of the tonsured maize god serves to denote the number 1, that of the foliated maize god the number 8.
Between the window openings in each bay, there are granite panels, as well as foliated bosses at each corner of the window openings. The outermost bays contain one window each and are framed by more elaborate surrounds, while all the other bays contain two windows each. There are marble panels below the cornice, and single-story engaged columns at each corner of the building. Some of the granite lintels are spalled because they had been burned in the September 11 attacks.
It contains "panels of elaborate pierced flamboyant tracery". Also in the church are two pairs of oak stalls which were moved here from the parish church of Blackburn, which was demolished in 1820. One pair has a stall with a good poppyhead finial, and the other has two misericords, one of which has foliated carving, and the other depicts a mermaid with a mirror and has fish supporters. Some of the panelling in the church is in linenfold style with a vine-trail.
Middle Silurian Colinton Volcanics foliated dacite and tuff is under Williamsdale. A roughly north south band of these acid volcanics extends to the north along the Monaro Highway and then follows the Cooma road to Cottondale. South the volcanics also follow the Monaro Highway in a more complex band through Colinton past Michelago and at least as far south as Bredbo. To the west of Williamsdale is an outcrop of Upper Silurian Laidlaw Volcanics dark grey rhyodacitic and dacitic crystal tuff.
The five-bay arcades are carried on square columns with angled corners and have foliated capitals. The chancel is paved with Minton encaustic tiles. The marble reredos dates from 1888, and the alabaster altar rails from 1900; both were donated by the daughter of Rev John Barclay, a former vicar of the church who died in 1866. Mural tablets, some of which were moved from the old church, commemorate members of the Brooke family and previous vicars of the parish.
The bedrock of Mount Cardigan is the upper member of the Lower Devonian Littleton Formation (a light grey meta-turbidite) on its west flank (seen on lower parts of the West Ridge Trail). On the summit and to the east on the Clark Trail the bedrock is the Kinsman Granodiorite of the Early Devonian Cardigan Pluton (a foliated granitic body with large megacrysts of potassium feldspar).Lyons, J.B., Bothner, W., Moench, R., Thompson, J.B., 1997, Bedrock Geology of New Hampshire. Map Sheet.
The presence of these dense, shallow-rooted shrubs also means less water reaches the soil than areas with sparse, short grasses, subsurface flows, and deep drainage. However, their dense canopies and thick litter do reduce overland flows compared to grazed grasses. Also, much more water is evaporated from the sparse grass areas than originally calculated. Old-growth Ashe junipers are different in that they have true trunks, use less water, are slow growing and less foliated, and have very deep roots.
The cross in the churchyard probably dates from the 13th century (it has a crude crucifixus figure on one side of the head and a foliated cross on the other). The cross at Trelissick was moved from Tredrea in the parish of St Erth in the 1840s; it has a crude crucifixus figure on the front of the head but the back is defaced. It had been found in a field called "Parc an Grouse".Langdon, A. G. (1896) Old Cornish Crosses.
The largest window, which sits under a hoodmould, is in the east end of the chancel; it is a three-light lancet with prominent tracery in the curvilinear/reticulated style. The window dates from the 14th century, which may make it the same age as a small window next to the porch, which has twin lights with foliated heads set below a quatrefoil in an ogive arch. Both windows also have scrollwork drip-moulds. Most other windows are plain trefoil-headed single lancets.
Hotel Troy is a historic commercial building located at Troy, Montgomery County, North Carolina. It was built in 1908–1909, and is a three-story, seven bay by eight bay, brick building, rising above a full basement with Classical Revival style design elements. The front facade features cast iron pilasters, columns with foliated capitals and cornices. Originally built for multi- purpose use including a sanitorium, in 1925, rooms in the upper stories were modified for use as hotel rooms and baths.
The projecting central portion of the upper stories contains a classical portico with a pediment supported by four, two-story Roman Doric order columns. The frieze contains triglyphs, incised patterns commonly paired with Doric columns, which alternate with paterae, circular medallions that occupy the spaces in the frieze called metopes. The tympanum, or triangular area of the pediment, contains a single, large, centrally placed patera that is flanked with a foliated pattern. Mutule blocks, another Doric detail, line the tympanum.
Amphibolite from Cape Cod, Massachusetts Garnet bearing amphibolite from Val di Fleres, Italy Amphibolite () is a metamorphic rock that contains amphibole, especially hornblende and actinolite, as well as plagioclase. Amphibolite is a grouping of rocks composed mainly of amphibole and plagioclase feldspar, with little or no quartz. It is typically dark-colored and dense, with a weakly foliated or schistose (flaky) structure. The small flakes of black and white in the rock often give it a salt-and-pepper appearance.
The first John Bibb structure was built in Victorian Free Classical style in temple form, resulting in a single large prismatic volume with two projecting wings with a cruciform plan symmetrical about two axes. The elevations have a high piano nobile (main floor) four pediments and carved foliated decoration. The 1909 alterations were designed by Harry Chambers Kent in Federation Free Classical style. The closure of Bethel Street and the creation of the Bethel Steps to replace it enabled a larger site.
Her aim is to give visitors the chance to better see how these women from different dynasties lived and looked. A second part of her residency involved the creation of a two-part mural onsite at the Shangri La Museum of Islamic Art, Culture & Design. Based on a poem from the Palestinian poet Mahmoud Darwish, the stanza - depicted in an artists-created font of foliated and pixellated Kufic, with roots instead of vegetation - is a site-specific commentary on colonized land.
The Ivanpah orogeny was a mountain building event in the Proterozoic from 1.71 to 1.70 billion years ago, preserved in the Ivanpah Mountains and the rocks of some mountain ranges in western Arizona and eastern California. The event is closely related to the Yavapai orogeny and may have had the same underlying causes. Foliated intrusive rocks including granite-gneiss, augen gneiss as well as amphibolite and granulite-grade metamorphism on the sequence of metamorphic facies offers evidence about the extent of deformation.
All the windows are one-over-one double-hung sash with yellow terra cotta sills. The exterior brown brick skin rises up to the tenth floor in one even plane. The grouped windows of the tenth floor and penthouse on the front and side facades have a foliated terra cotta border and a tympanum with a central quatrefoil. Above each tympanum is a bearded male mask between a pair of tall, narrow panels with terra cotta medallions of a squirrel, eagle, and cherub.
There are three bays with buttresses at the gable ends and a three-light east window has a hood mould with foliated stops and continuous sill string. Pointed windows, without tracery, are located at the north-east and south-east ends. The north transept gable end has four cusped lancets beneath a rose window. The vestry projects from its east side elevation and has three cusped lancets, a door facing north and a rose window in its east gable end.
The south transept has a parallel east wing. Tomb of Thomas Bowater Vernon, of Hanbury Hall, outside the Vernon Chapel The vestry and transept house the Vernon Chapel which has a transept gable end and a central pointed doorway with nookshafts and an outer dog-tooth and an inner rosette moulding. Above is a three-light window with hood mould and foliated stops. The adjacent gable end has at its base a gabled monument to Thomas Bowater Vernon (died 1859).
The small, three-bay manor house is an unusual example of eighteenth-century architecture, distinguished by its lack of symmetry. Its square footprint is divided into four unequal- sized rooms on the main floor, and five fireplaces on three floors feed a central T-shaped chimney. While the interior was renovated in the early nineteenth century, many original features still exist. These include the triple-run walnut staircase, pine floors, chair rails, and doors, which feature both HL and foliated H hinges.
Litchfieldite (nepheline syenite gneiss) from Canaã Massif, Brazil Litchfieldite is a rare igneous rock. It is a coarse-grained, foliated variety of nepheline syenite,Le Maitre, R.W. (2002) Igneous Rocks - A Classification and Glossary of Terms, 2nd edition, Cambridge, Cambridge University Press, page 105. sometimes called nepheline syenite gneiss or gneissic nepeheline syenite.Robins, B. and Tysseland, M. (1979) Fenitization of some mafic igneous rocks in the Seiland province, northern Norway , Norsk Geologisk Tidsskrift, Volume 59 Number 1 pages 1-23, page 3.
The leather covers are imprinted with decorative lozenge shapes—"filled with foliated ornaments and a framework parallel with the edges"—and the Beaufort family's coat of arms is prominent. By the mid-16th century, it had come into the possession of the antiquarian John Stow, who added many of his own comments to the manuscript, although in the event Stow hardly used it as a source for his own monograph—the 1598 Survey of London—as he had most of his material from elsewhere.
Both contain organic components (proteins, sugars and lipids) and the organic components are characteristic of the layer, and of the species. The structures and arrangements of mollusc shells are diverse, but they share some features: the main part of the shell is a crystalline Ca carbonate (aragonite, calcite), despite some amorphous Ca carbonate occurs; and despite they react as crystals, they never show angles and facets. The examination of the inner structure of the prismatic units, nacreous tablets, foliated laths... shows irregular rounded granules.
While many of smaller lakes in southern Sweden are thought to have originated by glacial stripping of an irregular weathering mantle in the last 2.5 million years Vättern formed by tectonics as a graben 700 to 800 million years ago in the Neoproterozoic. Granitic basement rocks in the lake are deformed (foliated) by the Protogine Zone that crosses the area. The basin is partially filled by sedimentary rock of the Visingsö Group of Neoproterozoic age. This group include rocks such as conglomerate, sandstone, arkose and carbonates.
Grenada - NASA NLT Landsat 7 (Visible Color) Satellite Image Part of the volcanic chain in the Lesser Antilles arc, Grenada and its possessions generally vary in elevation from under 300 meters to over 600 meters above sea level. Grenada is more rugged and densely foliated than its outlying possessions, but other geographical conditions are more similar. Grenada's landmass rises from a narrow, coastal plain in a generally north-south trending axis of ridges and narrow valleys. Mount St. Catherine is the highest peak at 840 meters.
Two groups of pews are located to either side of a central aisle at the balcony level. The interior of the church is a large, open area with a central aisle and very narrow side aisles located between the pews and end walls. The central nave of the church soars a full three stories high, terminating at the raised altar at the east end. The east wall of the altar holds a Sacramental mosaic, beyond a high arch supported by clustered columns with foliated capitals.
The facade contains ornaments such as swags and wreaths. There are bronze spandrels with decorative friezes within the upper-story bays, and the facade of the top story under the parapet contains bronze lion heads. Foliated reliefs are located within the door and window frames at ground level, and antefixes are located above the shop windows and the Dey and Fulton Street subway entrances. The subway entrances also contained granite faces and bronze gates, and the decoration extended into the basement where the subway platform was located.
Internally, the church is unusual in having a vast and complex timber roof structure rather than the usual stone arches. In the main internal space, the roof is supported by four pairs of tall, slender cast iron columns, quatrefoil in section and with moulded collars and foliated capitals. These columns support fretwork spandrels, pierced with dagger motifs and quatrefoils which in turn support dark stained rafters decorated with a sawtooth pattern. The ceiling is painted a deep orange colour between the timbers, but was originally white.
Shrigley monument 1871, designed by Timothy Hevey. A remarkably imposing monument of brown stone, in three layers; the design has much in common with, but is rather grander than, the Rossmore Memorial of about the same date in the Diamond of Monaghan town. The base, surrounded by iron railings, originally with an elaborate lamp at each corner, is square. Upon this, an octagonal arcade of round-headed arches, carried on columns with Ruskinian foliated capitals, surrounds the central shaft which incorporates the drinking-fountain.
These columns are arranged so as not to intercept the view of the High Altar from the aisles. The columns have capitals of foliated form artistically treated so as to appear alike, but the detail of each differs materially. The columns have marble bases, which, in turn, are supported on smoothly rutted Malmsbury bluestone plinths. The columns each bear a polished brass plate at the base of the shaft, inscribed with the name of the parishioner or the parish organization who funded the cost of that column.
The Temple of the Cross Complex The Temple of the Cross Complex is a complex of temples at the Maya site of Palenque in the state of Chiapas in Mexico. It is located in the south-east corner of the site and consists of three main structures: the Temple of the Cross, Temple of the Sun, and the Temple of the Foliated Cross. The Temple of the Cross is the largest and most significant. The temple is a step pyramid containing bas-relief carvings inside.
According to accounts from the 16th century, the stone temples were covered in stucco and decorated with blue and red paint. The three main temples that comprise the Cross Complex are aligned to form a cross. The Temple of the Foliated Cross is directly across the courtyard from the Temple of the Sun, and both are adjacent to the Temple of the Cross. Temple XIV and Temple XV are two smaller temples are found between the Temple of the Sun and the Temple of the Cross.
Similar arrangement is replicated on the western doorway of the tomb leading to the open pavilion on the west. The ceiling in the dome depicts a circular gold medallion with Quranic inscriptions in Naksh characters. Foliated crenellations are seen on the outer faces of the base of the tomb. Interesting features seen on the northern and southern sides of the tomb, considered typical of the Tuglaq period layout, are the ceremonial steps provided at the ground level that connect to the larger steps leading into the reservoir.
The Church of England parish church of Saint Mary Magdalene has a 12th-century chancel and 13th-century nave. In the 14th century new Decorated Gothic windows were added to the chancel. In the 15th century a Perpendicular Gothic clerestory was added to the nave and a west tower was built. Monuments in the church include two 14th-century tomb recesses and a 14th-century slab with a foliated cross. There is a 15th-century monumental brass to Henry Freebody, who died in 1444.
The tradition identifies the makara with water, the source of all existence and fertility. In the medieval era of South India, Makara was shown as a fifth stage of development, symbolized in the form of an elephant head and body with an elaborately foliated fish tail. Most myths maintain this symbolism of this stage in the evolution of life. (Note makara in fifth row of animistic carvings in temple wall at right.) The Makara Thoranam above the door of the Garbhagriha of Chennakesava Temple at Belur.
Other exterior elements typical to the Italian Renaissance Revival style of architecture include classical features such as pediments, triglyphs, and dentils, which are interspersed with foliated and floral designs. A unique detail is the arch keystones that have carved fish-scale patterns. Perhaps the most striking exterior features of the building are the groupings of four colossal statues placed at each of the building's corners. These identical copper and bronze sculptures are called History, Agriculture, Industry, and Arts, but are popularly known as The Ladies.
Sanchis, Frank E.; American Architecture Westchester County: Colonial to Contemporary (Great Barrington, Massachusetts: North River Press, 1977.) The building reflects two distinct periods of construction; the original two-story building dates from the 1880s and is four bays in width, and built in brownstone with a curvilinear foliated Sullivanesque ornament. The 1908 remodeling of the building resulted in the creation of a new entrance bay made from brownstone, as well as the construction of two additional stories of office space faced in buff-colored brick.
The site lay in ruin for decades and lost further sculptural elements until Barnard arranged for the entrances' transfer to New York. The doorway had been the main portal of the abbey, and was probably built as the south transept door. Carvings on the elaborate white oolitic limestone doorway depict the Coronation of the Virgin and contains foliated capitals and statuettes on the outer piers; including two kings positioned in the embrasures and various kneeling angels. Carvings of angels are placed in the archivolts above the kings.
Wireless Internet service providers (WISPs) are rapidly becoming a popular broadband option for rural areas.Wireless World: Wi-Fi now in rural areas July 7, 2006 The technology's line-of-sight requirements may hamper connectivity in some areas with hilly and heavily foliated terrain. However, the Tegola project, a successful pilot in remote Scotland, demonstrates that wireless can be a viable option. The Broadband for Rural Nova Scotia initiative is the first program in North America to guarantee access to "100% of civic addresses" in a region.
A tall modernistic building is at left; a tower with a red peaked roof is at right The belfry, with six tons (5.4 tonnes) of bells inside, is 30 feet (10 m) tall. The three lancet windows on its faces are divided by molded shafts and topped by arches supported by sculpted heads. Above a decorative foliated frieze is the parapet, with arched openings, surrounding the roof. Three gargoyles, each weighing 3 tons (2.7 tonnes) and projecting out eight feet, project from the three corners.
Simple round columns with Doric order bases and capitals are found on each corner of the pedestal. Small carved field guns are mounted on the side tops of the pedestal flanking the obelisk which rises from the centre. The obelisk comprises a square planned shaft with various mouldings on its faces above which is a cornice of a cyma recta moulding with foliated carving. Surmounted on this is the obelisk, of smooth faced sandstone; a tapering column with carved shields affixed to the north and south.
Foliated dish or tray in the tixi technique with the guri or "Sword-Pommel Pattern", here using red with three thin layers of black. The polished top layer of red contrasts with the duller bottom layer. Early Ming. The style of carving into thick lacquer used later is first seen in the Southern Song (1127–1279), following the development of techniques for making very thick lacquer.Watt and Ford, 7; Rawson, 175 There is some evidence from literary sources that it had existed in the late Tang.
The two end bays have stop-chamfered corners to the ground and first floors which are rendered and painted. Engaged columns capped with foliated convex elements are located within the stop chamfers. Each end bay has a centrally located segmental arch which surrounds a rendered section containing two lancet-type windows with semi-circular heads. The first floor levels have three similarly styled windows, symmetrically placed, and the second floor levels have larger scale windows which project above the eaves line and have curved pediments.
Poppleton Fire Station, also known as Engine House #38, is a historic fire station located at Baltimore, Maryland, United States. It is a Tudor Revival style building built of brick, one large bay wide, approximately nine bays long, and two stories high with a gable roof. The front façade is a brick and limestone composition featuring a central, Tudor archway flanked by octagonal towers and crowned with crenellation. The archway features engaged colonettes with carved, foliated capitals containing firemen racing to extinguish a fire.
The southern (entrance) bay is narrower, shorter and has a very steep hipped roof; a drawing in the architects' journal Building News in 1873 showed a tall flèche on top of this roof. The door is set into an ogee-headed white-painted arch; the tympanum formed by the space between the arch and the door is decorated with carved scrolls and a shield. Around the door, columns terminate in intricate foliated capitals. A first-floor window with three lights has similar decoration above.
640 Broadway demonstrates Delemos & Cordes' competency for Neoclassic design. The Broadway facade shows a two- story base with second-story comer show windows, a limestone entrance leading to the upper floors with oval transom, a denticulated hood and paired, grouped and arched fenestration across the upper stories. Classical ornamentation, including cartouches, triglyphs, keystones, molded architraves and foliated capitals ornament the facade. The Bleecker Street facade shows the same two- story brick base, recessed fenestration, a historic wood sash and end bay at the west, similar to the Broadway facade.
Rare barium minerals, mainly silicates, can be uncovered in sanbornite deposits of eastern Fresno and Mariposa counties, California. Alforsite is found in metamorphic sanbornite quartz, which occurs within a few hundred meters of granodiorite intrusions, and foliated quartzite. Gneissic banded rocks contain the mineral, which has been shown to be associated with witherite, sanbornite, and celsian in samples (with quartz-rich and gillespite-rich bands) from Incline. In order for the witherite- sanbornite- quartz to be stable, temperatures of 500 °C to 600 °C and pressures of 1-3 kbar are required.
These strata unconformably overlie Archean strata of the Superior craton and Proterozoic Richmond Group. The unconformity between the Early Proterozoic Nastapoka Group and the underlying Archean Superior craton lies just inland of Nastapoka arc as defined by the edge of arcuate eastern coastline of Hudson Bay. The unconformity consists of undeformed stromatolite-bearing dolomites overlying either foliated Archean granodiorite or the tilted and eroded strata of the Richmond Gulf Group. A thin, conglomeratic quartz sandstone separates the dolomites from the underlying strata and forms the base of the Nastapoka Group.
The placement in Abies is based on the dorso-ventrally flattened leaves, and the circular leaf scars, which separate the organs from those of Pseudotsuga and Keteleeria. Within Abies, A. milleri shows similarities with A. kawakamii and A. chensiensis from Asia and with A. concolor and A. lasiocarpa of North America. A. milleri does not show traits which allow placement in any one of the genus Abies sections, however. The 81 specimens studied for the A. milleri description included 40 cone scales, 21 wing seeds, 10 foliated axes, and two detached needles.
The large aperture is oval in shape, with an elaborate peristome. The outer lip is flaring, thickened at a short distance from the edge and with internal denticles. The inner part of the peristome shows an appressed parietal callus continued into a foliated columellar callus, which has a raised edge overhanging the siphonal canal on large specimens, and bears indistinct ridges towards the edge. The colour pattern is very characteristic, with articulated spiral bands of light patches on the knobs and dark brown in the interspaces, alternating with medium brown uniform bands.
Tivoli Building, 2016 The Tivoli Building is a historic building at 301 West Lincolnway (301 West 16th Street) in downtown Cheyenne, Wyoming, and a part of the Downtown Cheyenne Historic District. The three-story Victorian building was built in 1892. Its design incorporates several elements typical of Queen Anne style architecture, including an oriel window, an octagonal ornamented turret, and use of foliated stone, as well as some Chateauesque and Romanesque Revival architectural elements. The hipped roof of the building and the roof of the turret were both covered with pressed metal sheets.
They show the transition from Norman architecture to the Early English Style. The piers are Norman in character with foliated capitals from which spring pointed arches. The four clerestory windows on either side of the nave are examples of Early English lancets, whilst the two long lancets of the west wall are part of the nineteenth-century restoration. The chancel, which is separated from the nave by an Early English arch, is approached by a flight of steps, necessitated by the sloping nature of the site on which the church is built.
The nacreous layer of monoplacophoran shells appears to have undergone some modification. Whilst normal nacre, and indeed part of the nacreous layer of one monoplacophoran species (Veleropilina zografi), consists of "brick-like" crystals of aragonite, in monoplacophora these bricks are more like layered sheets. The c-axis is perpendicular to the shell wall, and the a-axis parallel to the growth direction. This foliated aragonite is presumed to have evolved from the nacreous layer, with which it has historically been confused, but represents a novelty within the molluscs.
The Henry Dinwoodey House, at 411 East 100 South, Salt Lake City, Utah, is a Late Victorian house that was designed by Richard Kletting, architect of the Utah State Capitol. It was built in 1890 and was listed on the National Register of Historic Places in 1974. The house exhibits characteristics of both Queen Anne Style architecture, with its assymmetrical facade and corner turret, and Romanesque Revival style, including rough-hewn stone, squat columns, and foliated carvings. It was built as a home for Sara Kinersley, the third polygamous wife of Henry Dinwoodey, a Mormon.
Its cover dates from 1921, and is carved with various items linked to the sea. Two of the windows on the south side of the chancel contain fragments of medieval stained glass. In the south wall of the nave is a window known as the Maiden's window, which was made in 1912–13, and a window of 1931 depicting Doubting Thomas, made by Powells. Also in the church is a 13th-century coffin lid inscribed with a foliated cross, and memorial wall tablets dating from the 18th and 19th centuries.
Yorkshire House is a historic home located at Warrenton, Fauquier County, Virginia. It was built in 1938–1939, and is a two-story, 13 bay, brick dwelling in the Modern Movement style. It features a low-pitched slate roof, a horizontal emphasis, a curved corner with continuous steel windows, a large glass block window, an elliptical bay window with steel casements and a foliated, geometric, metal balustrade on the rear balcony. Also on the property are the contributing brick and- stucco garage, a banked stone pump house, and a frame storage shed (c. 1939).
Carved lid of the tomb of Kʼinich Janaab Pakal I in the Temple of the Inscriptions. The large carved stone sarcophagus lid in the Temple of Inscriptions is a unique piece of Classic Maya art. Iconographically, however, it is closely related to the large wall panels of the temples of the Cross and the Foliated Cross centered on world trees. Around the edges of the lid is a band with cosmological signs, including those for sun, moon, and star, as well as the heads of six named noblemen of varying rank.
Seigneurial chairs at a table with tin cutlery, pottery, medieval glass and earthenware in majolica, c. 1465 The chair of Maximian in the cathedral of Ravenna is believed to date from the middle of the 6th century. It is of marble, round, with a high back, and is carved in high relief with figures of saints and scenes from the Gospels—the Annunciation, the Adoration of the Magi, the flight into Egypt and the baptism of Christ. The smaller spaces are filled with carvings of animals, birds, flowers and foliated ornament.
The Gneiss is homogeneous overall, but is recognized as having four subdivisions. These are the layered gneiss member, the augen gneiss member, the streaked-augen gneiss member, and the hornblende gneiss member. Additionally, the Baltimore Gneiss outcrops into three discrete masses of uniform, well-foliated to massive granitic gneiss referred to as the Slaughterhouse Gneiss. The layered gneiss member consists of dark and light layers of gneiss bearing biotite, microcline, quartz, and plagioclase, varying from biotite schist to quartzo-feldspathic granofels interlayered on a centimeter to decimeter scale.
Metamorphism at equal to, or higher than, greenschist facies will cause solid massive sulfides to deform in a ductile fashion and to travel some distance into the country rock and along structures. Upon cessation of metamorphism, the sulfides may inherit a foliated or sheared texture, and typically develop bright, equigranular to globular aggregates of porphyroblastic pentlandite crystals known colloquially as "fish scales". Metamorphism may also alter the concentration of Ni and the Ni:Fe ratio and Ni:S ratio of the sulfides (see sulfide tenor). In this case, pentlandite may be replaced by millerite, and rarely heazlewoodite.
The gallery at the West end was not part of MacPherson's plan but added after the Cathedral opened. It has the only decorated elements in the church, with foliated pillars and pilasters, and crocketed arches. Three objects in the Saint Andrew's Cathedral symbolise the affiliation of the Church with the Anglican Communion in England and its allegiance to the worldwide See of Canterbury. The Canterbury Stone, set in a pillar by the lectern and bearing a bronze replica of the Canterbury Cross, was sent from Canterbury Cathedral in 1936.
The ceiling of the lantern was painted a deep Prussian blue with a pattern of gilded stars to represent the firmament of God. The limestone tracery of the west wall of the sanctuary, with its foliage and animals, combined with the highly carved foliated woodwork and the overhead representation of the nighttime sky was intended to echo God's creation. Above the doors on the east chancel walls are glass mosaics of the tree of life by Antonio Salviati. A third mosaic by Salviati originally hung in the tympanum above the tower's front doors.
In and around the churchyard are three items, all dating from 1877, and all listed at Grade II. The lychgate and the wall, which completely encircles the churchyard, were designed by Street, and both are constructed in sandstone ashlar. Over the lychgate is a gabled roof, with a cross on its north end. In the churchyard is a cross, also designed by Street and in sandstone ashlar. It is circular in plan and consists of a fluted shaft on a base of three steps, carrying a foliated cross under a crocketed, gabled canopy.
This chill zone may represent a chill zone which infers an intrusive origin for the ultramafic, or it may represent a zone of metasomatism and/or contamination. The orebody itself is composed of 2 to 6 metres of massive nickeliferous sulfides, usually banded and foliated pentlandite-pyrrhotite-pyrite. Dodecahedral pyrite crystals to 20 cm are formed within the massive sulfide zones. The massive zone is overlain by a matrix ore zone composed of the above sulfide assemblage and coarse jackstraw textured bladed olivine, now retrogressed to black serpentinite.
The adoption of the star configuration goes back to the star used by the Mapuches. According to O'Higgins, the star of the flag was the Star of Arauco. In Mapuche iconography, the morning star or Venus, (Mapudungun: Wünelfe or the Hispanicized Guñelve) was represented through the figure of an octagram star or a foliated cross. Although, the star which was finally adopted bore a star having five points with the design of the guñelve remaining reflected in an asterisk inserted in the center of the star, representing the combination of European and indigenous traditions.
The mountains of K2 and Broad Peak, and the area westward to the lower reaches of Sarpo Laggo glacier, consist of metamorphic rocks, known as the K2 Gneiss, and part of the Karakoram Metamorphic Complex. The K2 Gneiss consists of a mixture of orthogneiss and biotite-rich paragneiss. On the south and southeast face of K2, the orthogneiss consists of a mixture of a strongly foliated plagioclase-hornblende gneiss and a biotite- hornblende-K-feldspar orthogneiss, which has been intruded by garnet-mica leucogranitic dikes. In places, the paragneisses include clinopyroxene- hornblende-bearing psammites, garnet (grossular)-diopside marbles, and biotite-graphite phyllites.
The stone is probably connected with the Campbells of Lochow, which family, at a later date, have for supporters an armed man holding a spear, and a lady holding a missive letter; they bear as their arms a galley with oars in action for Lorn, with a boar's head for crest. On the left side, after entering by the gate, is a stone, in fairly good condition. It resembles one of those at Kilmartin. It bears, near the top, a man armed with a sword and spear, under which are two animals, their feet rolling away in interlaced foliated ornament.
Mercantile Trust and Deposit Company is a historic bank building in Baltimore, designed by the Baltimore architectural firm of Wyatt and Sperry and constructed in 1885. It has a brick-with-stone-ornamentation Romanesque Revival structure, with deeply set windows, round-arch window openings, squat columns with foliated capitals, steeply pitched broad plane roofs, and straight-topped window groups. The interior features a large banking room with a balcony, Corinthian columns and ornate wall plaster work. The Safe Deposit Company on Redwood Street in Baltimore was one of the few buildings that survived the Great Baltimore Fire of 1904.
The floor of the sanctuary and side chapels is covered with a marble mosaic pavement installed in 1927. The mosaic tiling comprises off-white tiles, set into a square grid of yellow tiles, with an ornate geometric and foliated border of black, grey and yellow tiles. The design incorporates a number of circular panels, including symbolic representations of a Pascal lamb (representing Christ), a sailing ship (representing the Star of the Sea), a Latin cross, a basket with loaves and fish (representing the Eucharist), and the monograms of the Sacred Heart and the Blessed Virgin Mary.
Temple of the Cross Layout:C-Cross, F-Foliated Cross, S-Sun The Cross Complex site is located at the bottom of the mountain Yehmal K'uk' Lakam Witz, The Great Mountain of the Descending Quetzal. Yehmal K'uk' Lakam Witz was considered a sacred mountain by the Maya because of the many natural springs that supply fresh water to Otulum River. The Otulum River was the principal water source for the city. Temple of the Sun (left), Temple XIV (center), and Temple of the Cross (right) The Cross Complex structures are built from limestone which is widely available throughout the region.
However, despite allowing writing on both sides of the leaves, they were still foliated—numbered on the leaves, like the Indian books. The idea spread quickly through the early churches, and the word Bible comes from the town where the Byzantine monks established their first scriptorium, Byblos, in modern Lebanon. The idea of numbering each side of the page—Latin pagina, "to fasten"—appeared when the text of the individual testaments of the Bible were combined and text had to be searched through more quickly. This book format became the preferred way of preserving manuscript or printed material.
The central part of the fort, identified as the archaeological zone, contains the ruins of the great Swayambhusiva temple, now seen with only the free-standing "Entrance Portals", or gates on the four sides, all being similar in design. Each gate has twin pillars with angled brackets over which lies the huge lintel; the height of this gate being . The gates have extensive intricate carvings of "lotus buds, looped garlands, mythical animals, and birds with foliated tails". They do not depict any religious symbols, said to be the reason for its preserved condition for not being destroyed by Muslim invaders.
Above these, on both floors are pairs of colonnettes with foliated caps, a frieze and a cornice. Along the top of the building is a balustraded parapet, and a pedimented attic window in the central bay of each side. In the left bay of the Lord Street face and in the central bay of the Eastbank Street face is a round-headed doorway with a moulded head, a keystone and carved spandrels. The other bays on Lord Street and the first three bays on Eastbank Street contain tall pilastered two-light windows; the last three bays on Eastbank Street have inserted shop fronts.
Quartzite, containing darker bands of phengite and chlorite, from Maurienne Valley in the French Alps Quartzite can have a grainy, glassy, sandpaper-like surface Quartzite is a hard, non-foliated metamorphic rock which was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts. Pure quartzite is usually white to grey, though quartzites often occur in various shades of pink and red due to varying amounts of hematite. Other colors, such as yellow, green, blue and orange, are due to other minerals.
The eastern entrance facade consists of a large central gabled bay adjoining a smaller gabled bay to the north and the tower to the south. Access is gained to a porch up seven stairs extending the width of the central bay, and through three segmental arches which are supported on circular granite columns with foliated capitals and resting on elongated octagonal bases. The archways are under a chevroned hood moulding resting on corbels; surmounting the central chevron is a cross. Above the porch opening is a large window of geometrical tracery, with lancets under a large circular light.
The church guidebook notes that the tower gets progressively younger as it goes up. The lower section is Early English up to the sill of the belfry windows. The belfry itself is Decorated (14th century) while the battlements and pinnacles are Perpendicular (15th to 16th century). During restoration work at least six 12th and 13th century coffin lids with foliated crosses were found on site and are now on show inside the church. The north aisle and north transept are thought to have been added later than the 13th century as burials and parts of coffin lids were found under the foundations.
Tight folds at the contact between Icart Gneiss (light) and mylonitised quartz diorite (dark), western end of Lihou Island Many of the rocks present in the south of Guernsey may also be observed on Lihou Island. At the western coast of the island, a shear zone is exposed at the contact between the Perelle Foliated Quartz Diorite and the Icart Gneiss. The younger quartz diorite is mylonitised, where field evidence suggests that it was most likely deformed synchronously with its intrusion. The contact between the two rocks is tightly folded, as are the mylonitic fabrics in the two rocks.
On the thin section and hand specimen scale a metamorphic rock may manifest a planar penetrative fabric called a foliation or a cleavage. Several foliations may be present in a rock, giving rise to a crenulation. Identifying a foliation and its orientation is the first step in analysis of foliated metamorphic rocks. Gaining information on when the foliation formed is essential to reconstructing a P-T-t (pressure, temperature, time) path for a rock, as the relationship of a foliation to porphyroblasts is diagnostic of when the foliation formed, and the P-T conditions which existed at that time.
In gneiss, the foliation is more typically represented by compositional banding due to segregation of mineral phases. Foliated rock is also known as S-tectonite in sheared rock masses. Examples include the bands in gneiss (gneissic banding), a preferred orientation of planar large mica flakes in schist (schistosity), the preferred orientation of small mica flakes in phyllite (with its planes having a silky sheen, called phylitic luster – the Greek word, phyllon, also means "leaf"), the extremely fine grained preferred orientation of clay flakes in slate (called "slaty cleavage"), and the layers of flattened, smeared, pancake-like clasts in metaconglomerate.
The upper and lower guards are curved and contain various interlaced designs, including birds, animal and human figures, and foliated patterns. The figures on the upper guard have been identified as the four symbols of the evangelists. The style of leaf used next to the figure of the eagle on the upper guard has also been identified on early tenth century embroideries from Durham, on the back of the Alfred Jewel and a number of other objects dating to this period. The pommel incorporates two outward-looking animal heads, with protruding ears and round eyes and nostrils, now fragmentary.
The arcade detail of Mortuary Central, with its pointed trefoil arches, medallions and foliated capitals, is reminiscent of the hotel at St Pancras Station by Sir George Gilbert Scott, designed in 1865 and constructed in 1868–73. There are few other station buildings, either in Australia or the United Kingdom, with this level of decorative detail. The construction of special mortuary stations is rare, with no other examples having been located. The Mortuary station became part of the rail complex at Central after the new station was constructed in 1906, although it remained physically separate from the new station buildings.
It has a perfect basal cleavage and an uneven flat fracture, and it is foliated with a two- dimensional platy form. The Mohs scale of mineral hardness is based on scratch hardness comparison, ranging from 1 to 10, a value of 10 being the hardest of minerals. The hardness of talc, the softest of minerals, defines the value of 1 on the scale. (Any mineral with a value less than 2 can be scratched by a fingernail.) When scraped on a streak plate, talc produces a white streak; though this indicator is of little importance, because most silicate minerals produce a white streak.
The meta-sedimentary rock along with the granite batholith that forms Black Mountain are remnants of what laid hidden beneath a sea and underground, that are now exposed by headward erosion that continues northward today into Arizona's Transition Zone. The highly shortened and foliated phyllite began as a mudstone which was metamorphosed to shale. The shale was then subjected to pressure-solution volume-diffusion; the rock was metamorphosed while deeply buried then subjected to heating during the emplacement of the batholith. The phyllite at the granite contact formed a weak horizon, which assisted the decollement process after the batholith was emplaced.
It includes smaller pieces of richly coloured glass, less painted details and greater prominence given to the lead lines. It is possible, though speculation only, that the west window was the last to be installed, due to the larger scale of its design, softer colouring, and more fluid, interlacing design, which is suggestive of Art Nouveau influences of the 1890s. All windows share the same borders. The west and nave windows share the small inscription lettering, and the vestry windows and the Richard Little memorial window (northern wall of the nave) share similar painted details and foliated designs.
The entrance has glass-paneled double doors, set in a recess framed by marble trim and topped by a sill with a foliated cartouche, and a half-round transom window. Windows on the ground floor are set in rectangular openings with splayed keystoned lintels; there are small windows beneath the eaves that illuminate the rooms of the half-story. The interior begins with a tiled entry area, with stairs rising around the outer walls to a large meeting room that occupies most of the upper story. The entry opens into a central rotunda, with reading rooms on either side, and stacks and librarian area to the rear.
It forms a solid solution series with the minerals enstatite and ferrosilite, being a mid-way member between the two. Pure enstatite contains no iron, while pure ferrosillite contains no magnesium; hypersthene is the name given to the mineral when a significant amount of both elements are present. Distinctly developed crystals are rare, the mineral being usually found as foliated masses embedded in the igneous rocks norite and hypersthene-andesite, of which it forms an essential constituent. The coarse-grained labradorite-hypersthene-rock (norite) of Paul's Island off the coast of Labrador has furnished the most typical material; for this reason, the mineral has been known as Labrador hornblende or paulite.
The individual mineral grains in schist, drawn out into flaky scales by heat and pressure, can be seen with the naked eye. Schist is characteristically foliated, meaning that the individual mineral grains split off easily into flakes or slabs. The word schist is derived ultimately from the Greek word σχίζειν (schízein) meaning "to split", which is a reference to the ease with which schists can be split along the plane in which the platy minerals lie. Most schists are derived from clays and muds that have passed through a series of metamorphic processes involving the production of shales, slates and phyllites as intermediate steps.
Metasomatism will change the original composition. Regional metamorphism tends to make the rock more indurated and at the same time to give it a foliated, shistose or gneissic texture, consisting of a planar arrangement of the minerals, so that platy or prismatic minerals like mica and hornblende have their longest axes arranged parallel to one another. For that reason many of these rocks split readily in one direction along mica-bearing zones (schists). In gneisses, minerals also tend to be segregated into bands; thus there are seams of quartz and of mica in a mica schist, very thin, but consisting essentially of one mineral.
The cerebellum develops in a rostro-caudal manner, with rostral regions in the midline giving rise to the vermis, and caudal regions developing into the cerebellar hemispheres. By 4 months of prenatal development, the vermis becomes fully foliated, while development of the hemispheres lags by 30–60 days. Postnatally, proliferation and organization of the cellular components of the cerebellum continues, with completion of the foliation pattern by 7 months of life and final migration, proliferation, and arborization of cerebellar neurons by 20 months. Inspection of the posterior fossa is a common feature of prenatal ultrasound and is used primarily to determine whether excess fluid or malformations of the cerebellum exist.
In the Earth's crust, anisotropy may be caused by preferentially aligned joints or microcracks, by layered bedding in sedimentary formations, or by highly foliated metamorphic rocks. Crustal anisotropy resulting from aligned cracks can be used to determine the state of stress in the crust, since in many cases, cracks are preferentially aligned with their flat faces oriented in the direction of minimum compressive stress. In active tectonic areas, such as near faults and volcanoes, anisotropy can be used to look for changes in preferred orientation of cracks that may indicate a rotation of the stress field. Both seismic P-waves and S-waves may exhibit anisotropy.
H. Cloos, D. Roeder and K. Schmidt, Stuttgart, Schweizerbart, pp. 455-76. a stack of metamorphic tectonic nappes, mainly comprising variable types of gneiss, schist, marble and amphibolite, and tectonic slices of unmetamorphosed sediments on top, separated by low-angle normal faults from the metamorphic units below. Despotiko is dominated by metamorphic rocks with foliation surfaces dipping quite uniformly towards the southwest at shallow angles. The structurally lowest parts in the north and northeast of the island consist of grey, strongly foliated, mylonitic ortho-gneiss with abundant cross-cutting pegmatite dikes that become more and more deformed and rotated parallel to the foliation towards the hanging wall.
It is found in Brunei, Cocos (Keeling) Islands, Indonesia, Malaysia, Myanmar, Singapore, and Thailand. Its natural habitat is subtropical or tropical moist lowland forests. It typically is a resident of evergreen forests with pools or streams, but also ranges into large gardens with tall, densely foliated trees, such as the Bogor Botanical Gardens found in West Java as well as wooded groves in cultivated country, both sometimes not far from human habitations. It usually ranges in elevation from sea-level to roughly but can range up to about or more at locations like Mount Gede in West Java and Mount Singgalang in West Sumatra.
The chancel arch is plain, supported on circular shafts with richly foliated capitals. The priest's door to the south is elegant; the head is a segmented arch boldly trifoliated the cusps are terminated with fleur-de-lys. In the east wall of the transept is a niche leaf with beautiful moulding of foliate design In the south-east angle of the transept is a beautiful Early English double piscina under two trefoil arches one in each wall supported on three circular shafts the central shaft being in the angle of the walls In the chancel are two ancient benches with well carved poppy heads. The font is Norman.
The heavy entablature has three bands in the architrave; a band of foliated molding under the plain frieze; and a denticulated cornice defined by a bead and reel molding and an elaborate crown molding. Around 1855 the rear portico was enclosed and is now divided by six pilasters (originally square pillars) into five bays of windows with small protruding balconies in the end bays. A two-story north wing, added around 1855, is attributed to Alexander Jackson Davis, a former partner of Ithiel Town. Although not consistent with the symmetry of the whole, it is treated sympathetically through the use of identical pilasters and entablature.
The Murrieta Hogbacks are underlain by Cretaceous granitic rocks of the Peninsular Ranges Batholith. On the north half of the hogbacks, by foliated biotite-hornblende tonalite and on the southern half by hornblende gabbro. The basalt is potassium-argon dated to 10.4 to 10.8 million years and is a remnant of a channel-filling basalt flow, overlying a thin deposit of unconsolidated gray stream gravel, indicating that the basalt had filled in a former water course.M.P. Kennedy and D.M. Morton, PRELIMINARY GEOLOGIC MAP OF THE U.S. Geological Survey Murrieta 7.5' quadrangle, 1979, RIVERSIDE COUNTY, CALIFORNIA, Version 1.0, USGS, Prepared in cooperation with the CALIFORNIA GEOLOGICAL SURVEY, 2003.
Spread over 500 sq. yards it is built in the architecture of 19th and 20th around a central courtyard it has intricate designs of wood work on the rooftops, sculptures and Hindu goddesses engraved in stone and steel, antique balconies intricate stone brackets, balconies, jharoka, red sandstone brackets, floral decorations, motifs, wooden joist flooring and lime concrete flooring, multi foliated arched gateway and arches, carved sandstone facades, large arched openings with elephants and intricate carvings on the main door, wooden doorways using traditional material including lakhori bricks and lime mortar."Haveli to speak of a history lost in time.", Times of India, 21 Dec 2015.5\.
The basic types of the former are represented by the sills of epidiorite and hornblende gneiss in Glen Muick and Glen Callater, which have been permeated by granite and pegmatite in veins and lenticles, often foliated. The later granites subsequent to the plication of the schists have a wide distribution on the Ben Macdhui and Ben Avon range, and on Lochnagar; they stretch eastwards from Ballater by Tarland to Aberdeen and north to Bennachie. Isolated masses appear at Peterhead and at Strichen. Though consisting mainly of biotite granite, these later intrusions pass by intermediate stages into diorite, as in the area between Balmoral and the head-waters of the Gairn.
Religious Patrimony The municipality has a vast religious patrimony, which includes the Mother Churches, chapels, shrines, calvaries and cruises, often associated with religious festivities and local folk stories. Bugiada e Mouriscada is a festivity where populars stage a fight between Bugios (christians) and Mourisqueiros ( non-believers) by the possession of John the Baptist, alongside other folk and everyday lives activities. Slate There's a strong presence of slate mining industry and different transformative industries associated with slate, whose industrialization began in the 19th century and matured in the 20th century. Slate was formed 350 million years ago by a metamorphosis of shale, clay and volcanic ash that results to a fine-grained foliated rock.
The arcades are supported by piers, some of which are circular, others octagonal. On the north side of the chancel is a double aumbry; on the south side is a single aumbry and a damaged piscina. In the south aisle is a recess dating from the middle of the 14th century with a crocketed canopy, a finial at the apex and pinnacles at the sides; it had possibly been an Easter Sepulchre. The monuments include a 13th-century effigy of a knight with chain mail, a sword and a shield; a grave cover carved with a foliated cross, a man's head, and hands in prayer; and two Anglo-Saxon cross shafts dating from about 800.
The pavilions with domes are in different shapes and sizes (rectangular, octagonal and hexagonal) and on the basis of inscriptions are inferred to be graves. A cluster of three hemispherical domes, a large one of diameter and two smaller ones of diameter, portray exquisite architectural features of foliated motifs on the drums with kalasa motifs on top of the domes. Each pavilion is raised on a plinth of about and is supported by square shaped wide columns with entablature which have decorative capitals that support beams with projecting canopies. Ruins of a courtyard with a rectangular plan, are seen to the west of the three pavilions which are built of double columns.
This sketch, painted on paper in black ink with light colouring, depicts two ladies sitting opposite each another, their heads being encircled by nimbi. Both are represented holding various attributes: the lady on the left, who sits on a rectangular throne supported by a row of lotus petals, holds a foliated cup and a tray with a dog seated on it. The one on the right is seated on a dog or wolf, and has four arms, the upper two supporting the sun and moon discs, the lower two arms holding a scorpion and a snake. They wear a characteristic hairstyle, surmounted by a water-drop-shaped or peach-shaped headdresses that are probably made of metal.
The pillar in the second bay has two statues, probably representing St. John and the Mother Church. The capitals in the third bay illustrate the entry of Christ into Jerusalem, Palm Sunday and Pentecost, and a knight striking down an adversary, and then walking over to a lady; possibly representing Constantine defeating paganism and then being thanked by the mother church. The southern pillar illustrates the Baptism of Christ and the devil tempting Christ, Christ washing the apostles' feet, the Last Supper and the kiss of Judas. The Southern Gallery probably dates to the 1380s or 1390s, and is built in the Gothic style, with pointed arches intersecting vaults resting on colonnettes with foliated capitals.
The front facade features finer piers, spandrels with Art Nouveau foliated decoration, a large entry arch, the lettering B & M above, topped by an unusual pierced arched pediment. Bryant & May Factory, from Church Street, Richmond Other smaller buildings were added across a small lane on the north side in 1910 and 1917 in a matching style. A large addition was made to the rear (west) of the building in 1921-22, designed by Klingender & Hamilton, in matching red brick but in a Stripped Classical style. This addition has an extra floor, with prominent signage, and a clock tower on the north side and the clock face bears the name BRYANT AND MAY in place of numbers.
Mythological beings using a variety of emblem glyphs in their titles suggests a complex early history. For instance, Kʼukʼ Bahlam I, the supposed founder of the Palenque dynasty, is called a Toktan Ajaw in the text of the Temple of the Foliated Cross. The famous structures that we know today probably represent a rebuilding effort in response to the attacks by the city of Calakmul and its client states in 599 and 611.Martin and Grube 2000: One of the main figures responsible for rebuilding Palenque and for a renaissance in the city's art and architecture is also one of the best-known Maya Ajaw, Kʼinich Janaabʼ Pakal (Pacal the Great), who ruled from 615 to 683.
The Aeronautica Lombarda AL-12P in flight The AL-12P was designed by A. Ambrosini and was a high-wing cantilever monoplane with a wood-ribbed fuselage covered with stressed molded plywood. It wing had a foliated spruce plywood spar and was covered with plywood although the ailerons were fabric covered. It also had large slotted spoilers that could be opened perpendicular above and below the wing. The pilot and co-pilot sat side by side in the nose which made from plywood-covered welded steel tubes and was hinged to allow cargo to be loaded into the fuselage, a passenger door was fitted on the right hand side of the fuselage.
The essential idea is that a Calabi-Yau manifold with complex dimension three should be foliated by "special Lagrangian" tori, which are certain types of three-dimensional minimal submanifolds of the six-dimensional Riemannian manifold underlying the Calabi-Yau structure. Given one three- dimensional Calabi-Yau manifold, one constructs its "mirror" by looking its torus foliation, dualizing each torus, and reconstructing the three- dimensional Calabi-Yau manifold, which will now have a new structure. The Strominger-Yau-Zaslow (SYZ) proposal, although not stated very precisely, is now understood to be overly optimistic. One must allow for various degenerations and singularities; even so, there is still no single precise form of the SYZ conjecture.
The ortho-gneiss is followed by up to several metres thick, prominent white, strongly foliated, mylonitic gneiss. Higher up are medium-grained, white calcite marble, followed by greenish-white gneiss and an alternation of chlorite epidote schist and thin marble layers, on top of which are found chlorite epidote gneiss and retrogressed amphibolite as well as some small serpentinite lenses. The structurally highest parts in the south and southwest of the island comprise thick white to yellowish, fine grained dolomite marble with thin layers of dark grey, carbonaceous calcite marble. This metamorphic succession is penetrated by six early Pliocene,Innocenti, F., Kolios, N., Manetti, P., Rita, F. and Villari, L. (1982) Acid and basic late neogene volcanism in central Aegean Sea: its nature and geotectonic significance.
The memorial is surrounded by a low fence, consisting of evenly spaced bollards linked by steel rods. The sandstone memorial sits on a base step with picked stone faces, margined and chiselled around. Surmounting this is a smooth faced stone step with plinth, on the faces of both of which are marble plaques with details of the opening of the statue and the names of the Allora men who took part in the war along with the names of the fallen with details of their death. The plinth supports the shaft of the memorial comprising a recessed square pier which features a wreath on the southern facing side and has a base element comprising a cyma recta moulding with foliated carving.
Architect Harry Norris incorporated many American styles into his work. He was inspired by the then popular Spanish Colonial Revival style after visits to the United States. The building is laden with Spanish/Moorish features, including blue faience tiles; foliated (leaf shaped) and rope moulded ornament, painted in gold and a foyer featuring terrazzo and inlaid stone. A Heritage Victoria database entry for Majorca House, says: "The Moorish influence in its terracotta façade places it firmly within the Melbourne tradition of exotic architecture in the late 1920s." The Majorca Building is a natural progression from Norris’s other celebrated building in this style, the Kellow Houses (Former Kellow Falkiner Showrooms) at St Kilda, South Yarra, a car showroom completed in 1928.
When a rock is contact altered by an igneous intrusion it very frequently becomes more indurated, and more coarsely crystalline. Many altered rocks of this type were formerly called hornstones, and the term hornfels is often used by geologists to signify those fine grained, compact, non-foliated products of contact metamorphism. A shale may become a dark argillaceous hornfels, full of tiny plates of brownish biotite; a marl or impure limestone may change to a grey, yellow or greenish lime-silicate-hornfels or siliceous marble, tough and splintery, with abundant augite, garnet, wollastonite and other minerals in which calcite is an important component. A diabase or andesite may become a diabase hornfels or andesite hornfels with development of new hornblende and biotite and a partial recrystallization of the original feldspar.
Compressive deformation during the Penokean orogeny reactivated the GLTZ, which followed deposition of the Marquette Range Supergroup sediments and resulted in a north-side up motion along steep brittle-ductile faults in the eastern, low-grade portion of the Marquette Trough In the western portion of the Marquette syncline, a second episode of GLTZ reactivation took place during the uplift of the post-Huronian 2,400- to 2,100-million-year-old granitic Southern Complex. The Northern and Southern complexes of the Upper Peninsula are highly migmatized and intensely foliated, with the intensity of foliation increasing toward margins. The western part of the Southern Complex shows intricate phases of folding and foliation. These Late Archean rocks form a roughly north–south belt lying south of Marquette extending to the Michigan-Wisconsin border.
Dark dikes (now foliated amphibolites) cutting light grey Lewisian gneiss of the Scourie complex, both deformed and cut by later (unfoliated) pink granite dikes Contact between a dark-colored diabase dike (about 1100 million years old)Bjørn Hageskov (1985): Constrictional deformation of the Koster dyke swarm in a ductile sinistral shear zone, Koster islands, SW Sweden. Bulletin of the Geological Society of Denmark 34(3–4): 151–97 and light-colored migmatitic paragneiss in the Kosterhavet National Park in the Koster Islands off the western coast of Sweden. Most of the Outer Hebrides of Scotland have a bedrock formed from Lewisian gneiss. In addition to the Outer Hebrides, they form basement deposits on the Scottish mainland west of the Moine Thrust and on the islands of Coll and Tiree.
Mean apatite fission-track age of 156 ± 4 Ma is interpreted to represent the time the rocks of the complex were last at temperatures of 60 °C to 100 °C. Previously, Rb-Sr and K–Ar dating of biotite from the nepheline syenite at Beemerville yielded ages of about 435 ± 20 Ma (444 Ma. using current decay constants) for the Beemerville Alkaline Complex. All of these dates are consistent with the observations that the dikes of the Beemerville Alkaline Complex crosscut folded and foliated strata of the Martinsburg Formation as young as early Late Ordovician but are not known to intrude younger rocks. Based upon emplacement models for diatremes it can be inferred that the diatreme that forms Rutan Hill is the throat of an ancient, extinct volcano.
On the opposite side of the building, between the first and second > stories, a wide bay window projects outward for some distance, its roof > forming a balcony of considerable dimensions, enclosed by rails of dark > brownstone. The features of this window are two panes of bent glass, eight > by ten feet in size, which are said to be the largest of their kind in the > country. Above the arch of the doorway four pilasters, faced with terra > cotta flower and basket work, and capped with elaborately carved brownstone > copings, extend to the height of the building, terminating at either corner > of the gable. At every suitable space on the front of the club house there > is an abundance of delicated carvings and moulding, while each of the > windows is supported on sheaves of slender columns, crowned with richly > foliated capitals.
In Gaul the Merovingian successors to Roman power employed the curule seat as an emblem of their right to dispense justice, and their Capetian successors retained the iconic seat: the "Throne of Dagobert", of cast bronze retaining traces of its former gilding, is conserved in the Bibliothèque nationale de France. The "throne of Dagobert" is first mentioned in the 12th century, already as a treasured relic, by Abbot Suger, who claims in his Administratione, "We also restored the noble throne of the glorious King Dagobert, on which, as tradition relates, the Frankish kings sat to receive the homage of their nobles after they had assumed power. We did so in recognition of its exalted function and because of the value of the work itself." Abbot Suger added bronze upper members with foliated scrolls and a back-piece.
Santa Vittoria di Serri – Nell'Olimpia della Sardegna – Storia Archeologia Viva – anno XXXVI – n. 183 maggio – giungo 2017 – Giunti Milano From 1 October 2019 the Superintendence of archeology, fine arts and landscape of Cagliari has started a new excavation campaign with consolidation and restoration works. The excavation campaigns recovered important objects which confirmed the relationships that the Nuragics had with the Etruscans, Phoenicians and Cypriots. It is worth mentioning a violin bow fibula in foliated bronze, a double silver foil disc, necklaces composed of amber and glass paste elements, vases in bronze foil of Etruscan origin and in particular a decorated cylindrical torch holder composed of three floral corollas of Phoenician origin from Cyprus dating from the late 8th - first half of the 7th century BC. The torch holder and the bronze vases have been recovered in the so-called "curia".
Geological map of the Hebridean Terrane showing distribution of rocks of the Lewisian complex Undeformed Scourie dyke cutting Lewisian Gneiss, about 1.6 km west of Scourie foliated amphibolites) cutting grey gneiss of the Scourie complex, both deformed during the Laxfordian tectonic event and cut by later (unfoliated) granite veins - road cutting on the A838 just north of Laxford Bridge The main outcrops of the Lewisian complex are on the islands of the Outer Hebrides, including Lewis, from which the complex takes its name. It is also exposed on several islands of the Inner Hebrides, small islands north of the Scottish mainland and forms a coastal strip on the mainland from near Loch Torridon in the south to Cape Wrath in the north. Its presence at seabed and beneath Paleozoic and Mesozoic sediments west of Shetland and in the Minches and Sea of the Hebrides has been confirmed from the magnetic field, by shallow boreholes and hydrocarbon exploration wells.C.Michael Hogan. 2011.
Edward Williams probably began his art career making picture frames, but he was surrounded by relatives who were well-known painters and engravers, and over the years he reinvented himself as a painter. He started by painting miniatures, and copying Baroque landscapes from the 1600s in the style of the Dutch painters Ruisdael (1628-1682) and Hobbema (1638-1709) - the former known for woodland scenes with detailed renderings of trees, particularly the leaves, and water scenes with small boats moored beneath windmills; the latter known for his densely foliated trees with stippled leaves. As Edward Williams developed his own style, he moved on to contemporary landscapes of the English countryside that, not surprisingly, hint of some of the work of his uncle George Morland. However, he became best known for moonlit scenes of boats and windmills along the Thames River, which earned him the epithet with the public of "Moonlight Williams", or simply the "moonlight painter".
A 19th-century-added arched squint is on each side of the chancel arch, each with a chamfered rebate as part of the arch. Set above each squint on the chancel side is a gable as moulding with, at its spring and point, a carved foliated detail. Within the chancel is a 14th-century piscina containing a quatrefoil shaped drain. Chancel arch with squint niches The north transept (or Priory End) windows, east and north, are 19th century but within 14th-century openings. The trussed roof is possibly 16th century with tie beam support added in the 19th. The south transept (or Hall End) east and south windows are 14th century although partly restored. The 15th-century south transept roof trussing is of hammer beam construction, with curved collar braces springing from beams which are supported by curved chamfered brackets. Running on the wall from the hammer beams to the roof line are wind braces, and to the ridge beam is roof truss framing.
The fertile Copán River valley was long a site of agriculture before the first known stone architecture was built in the region about the 9th century BC. The city was important before its refounding by a foreign elite; mentions of the predynastic history of Copán are found in later texts, but none of these predates the refounding of the city in AD 426. There is an inscription that refers to the year 321 BC, but no text explains the significance of this date.. An event at Copán is linked to another event that happened 208 days before in AD 159 at an unknown location that is also mentioned on a stela from Tikal, suggesting that it is a location somewhere in the Petén Basin, possibly the great Preclassic Maya city of El Mirador. This AD 159 date is mentioned in several texts and is linked to a figure known as "Foliated Ajaw". This same person is mentioned on the carved skull of a peccary recovered from Tomb 1, where he is said to perform an action with a stela in AD 376.
Dated from the ninth century (about 862) and erected under the reign of the sixth Aghlabid ruler Abul Ibrahim (856–863), it is made in teak wood imported from India.Minbar of the Great Mosque of Kairouan (Qantara) Among all the pulpits of the Muslim world, it is certainly the oldest example of minbar still preserved today.Mohammad Adnan Bakhit, History of humanity, Routledge, 2000, page 345 Probably made by cabinetmakers of Kairouan (some researchers also refer to Baghdad), it consists of an assembly of more than 300 finely carved wood pieces with an exceptional ornamental wealth (vegetal and geometric patterns refer to the Umayyad and Abbasid models), among which about 90 rectangular panels carved with plenty of pine cones, grape leaves, thin and flexible stems, lanceolate fruits and various geometric shapes (squares, diamonds, stars, etc.). The upper edge of the minbar ramp is adorned with a rich and graceful vegetal decoration composed of alternately arranged foliated scrolls, each one containing a spread vine-leaf and a cluster of grapes.
Federation of Old Cornwall Societies; pp. 30–32 There are two Cornish crosses in the parish of Feock: one is in the churchyard and the other at Trelissick. The cross in the churchyard probably dates from the 13th century (it has a crude crucifixus figure on one side of the head and a foliated cross on the other). The cross at Trelissick was moved from Tredrea in the parish of St Erth in the 1840s; it has a crude crucifixus figure on the front of the head but the back is defaced.Old crosses 1896, pp. 153–54 & 277–78Stone crosses; mid, p. 38 There is a fine Cornish cross in the churchyard of Gerrans.Old crosses 1896, pp. 263–64 According to Andrew Langdon (1994) this cross was not originally a churchyard cross but a wayside cross. No other ancient stone cross exists in the Roseland Peninsula; however a cross called Penpirthe Cross is shown on the parish terrier of 1613 as standing on the boundary of the parishes of Gerrans and Philleigh.Langdon A. G. (2002) Stone Crosses in Mid Cornwall; 2nd ed.

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