There's a big hill and where the festival was, there's sort of a low area with a natural bowl shape, it was very nice with the sound.
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"The fact is that most of the inhabitants are living in a very low area that is not good for human habitation," said presiding member of the Accra Metropolitan Assembly, Hon.
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And yes there they So many Bastards , Turds , Creeps , Idiots standing across from us Between them and us: long low area I would term: river Filled not with water though but Police looking nervous.
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The low area of the park is much closer to the city of Itatiaia and has many waterfalls, such as Véu da Noiva with 45 meters. The low area has also a Natural History museum. Itatiaia means "many-pointed rock" in the Tupi language.
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Due to the low area population and relatively little through traffic, the area's highways and the Gouverneur Town Court are not that busy.
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Most habitation was on the eastern end of the island, the peninsula East Head of Papa. A beached loch and a low area divide the island nearly into three separate parts.
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Ar Rakiyat is an Arabic term used to denote a low area that has been excavated, typically for a well. It was named this in reference to the well in Ar Rakiyat Fort.
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A low area between Parana Valles and Loire Vallis is believed to have once held a lake.Goldspiel, J. and S. Squyres. 2000. Groundwater sapping and valley formation on Mars. Icarus. 89: 176-192.
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Their breeding habitats are brushy areas and forest edges in eastern North America. The prairie warbler's nests are open cups, which are usually placed in a low area of a tree or shrub. Incubation period is 12 to 13 days.
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Mangroves line the shore which is backed by low-lying swamps, marshes, and salt flats. Plains then encircle much of this low area and extend inland 20 to 30 km. Major river systems with wide floodplains cut through the plains and discharge into the bay.
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This cave has six openings and located on a hill in the middle of a wet low area. The hill is 5 meters high, 50 meters wide and 75 meters long. The Franklin Marble is what makes up this cave. This cave is on private land.
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The site is built adjacent to a low area. The west and south flanks are protected by the wadi and its steep slope (see the section in Fig. 1). Walls range up to 2 m in height. Upslope, the houses have walls up to 80 cm in thickness.
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This situation was well-discussed in the FTC investigation of U-I Sugar. Before the factory opened, Oregon-Utah Sugar was merged into Utah-Idaho Sugar. Because of labor shortages and low area planted with sugar beets, the processing machinery was moved to Toppenish, Washington in October 1917.
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From the early 1900s until 1941, mail was delivered by dog sled from Dillingham. In 1941 a post office opened in Ekwok. Before 1960, most of the buildings in Ekwok were located in a low area near the river. After a flood in the early 1960s, the village was relocated to its current location.
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A view of Eden Valley, Yangsan, South Korea This is a list of valleys in South Korea. A valley is a low area between hills, often with a river running through it. Some Korean valleys are similar to one-another in terms of their geographic features, although there is also significant variation in their formations.
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The Zona Baja (low area) includes areas below 200 meters above sea level. It has a tropical climate with agriculture dedicated primarily to citrus fruits such as oranges, mandarin oranges, grapefruit, papaya and mamey. It is also noted for its cattle. It includes the municipalities of Francisco Z. Mena, Venustiano Carranza, Pantepec, Jalpan and Tenampulco.
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The Stain Hill Reservoirs in London, England with embankments occupy . They are a pair which sit high between others; Kempton Nature Reserve; riverside houses in Sunbury-on-Thames; and a low area of flood meadow to the west alongside the closing stretch of the Port Lane (or Felthamhill) Brook. Other nearby settlements are Molesey, Hampton and Hanworth.
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The low area surrounding the table mountains is Wonkén Planation Surface. The Auyán- Tepui Planation Surface forms the quartzite tepui summits. High precipitation combined with the long period of weathering has produced quartz and sandstone karst features. These include arches, towers, tower fields, dolines, collapse shafts, polje, corridors, grikes, and large cave systems extending many kilometers in length.
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The Salton Sink is the topographic low area within the Salton Trough, an active tectonic pull-apart basin.Kearey, Philip and Frederick J. Vine, Global Tectonics, Blackwell Science, 2nd ed., 1996, pp. 131–133 The Salton Trough is a result of crustal stretching and sinking by the combined actions of the San Andreas Fault and the East Pacific Rise.
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The water was carried across the bridge of Agrippa after it was first transported from the low area of the Campus Martius over the higher ground of the ridge surrounding the Pantheon basin by using the baths drainage system as well as the Stagnum (an artificial lake) and the Euripus (an artificial channel for swimming) where it was drained into the Tiber River.
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Szirma is located at the southeast corner of Miskolc and lies on a low area between river Hejő and Sajó, near the edge of The Great Plain. It is 3 km (1.8m) away from the centre, which can be easily reached by local public transport, by bus 3. Szirma is also close to the M30 Motorway and the Park Center shopping centre.
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Many streets were blocked by the fallen trees and power lines. At the White House, the winds downed one tree in the front garden, though there was no damage to the building itself. The storm surge resulted in flooding at the Washington Navy Yard. There, the marina was damaged, and some buildings and cars in low area garages were flooded.
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Uplifted strata in the center of a geological dome have higher potential erosive energy than the surrounding strata, because they are physically higher. Erosion thus acts on the uplifted area at a greater rate than on the surrounding flat-lying area, creating a low area, i.e. a basin. This area is more correctly referred to as the "Central Dome" of Tennessee.
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The Seymour River, one of three by that name in the province of British Columbia, Canada, is a river in the Central Coast region, flowing south out of the Pacific Ranges of the Coast Mountains into the head of Seymour Inlet, the largest of a maze of inland waterways within a relatively low area of the British Columbia mainland on the northwest side of the Queen Charlotte Strait region.
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The San Andres Mountains-(southern subrange of San Augustin Mountains), are separated from the Organ Mountains by San Augustin Pass, through which U.S. Highway 70 passes on its way to White Sands Missile Range, White Sands National Park and Alamogordo. The Franklin Mountains are separated from the Organ Mountains by a 10-mile wide low area known as Anthony Gap. Much of this intervening land is part of Fort Bliss.
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The Tian Shan have a number of named ranges which are often mentioned separately (all distances are approximate). Tian Shan with the ancient silk road In China the Tian Shan starts north of Kumul City (Hami) with the U-shaped Barkol Mountains, from about east of Ürümqi. Then the Bogda Shan (god mountains) run from east of Ürümqi. Then there is a low area between Ürümqi and the Turfan Depression.
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The route travels through the Jackfork Creek basin, a low area between the Jack Fork Mountains and the Big Caney Mountains. After passing through another unincorporated place, Adel, the highway cuts across the far southeast corner of Pittsburg County. SH-43 re-enters Pushmataha County southwest of the far south arm of Sardis Lake, a reservoir formed by impounding Jackfork Creek. The highway runs along the south shore of the lake.
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Halse og Harkmark (literally: Halse and Harkmark) is a combination of the names of two parishes surrounding the town of Mandal. The name Halse is the name of the site where Mandal Church is located. The name comes from the Old Norse name Halshaugar, where hals means a low area of land between two waters and haugr meaning hill or mound. The name Harkmark may be derived from an old river name.
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The horizontal tail was mounted on top of the fuselage, braced from the lower fuselage longerons on each side with a pair of parallel struts. Its plan was similar to the wing and the elevators were split, with a cut-out for the deep, broad rudder. The tailplane angle of incidence could be trimmed in flight. The low area fin was broad but unusually low; its angle of incidence could only be adjusted on the ground.
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For such low area fractions, the clusters have a finite mean size while at larger area fractions (30% or higher), a complete phase separation has been reported. The dynamics of the finite-size clusters are very rich, exhibiting either crystalline order or amorphous packing. The finite size of the clusters comes from a balance between attachment of new particles to pre-existing clusters and breakdown of large clusters into smaller ones, which has led to the term "living clusters".
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In ISW, when a photon passes through a low area of gravitational potential it is shielded from the cosmological expansion of space, making the background galaxy appear closer. Gravitational lensing, unlike all of the previous effects, distorts the apparent position, and number, of background galaxies. The RSDs measured in galaxy redshift surveys can be used as a cosmological probe in their own right, providing information on how structure formed in the Universe, and how gravity behaves on large scales.
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In addition to the amenity provided by the range of plantings along the road, the drive along Anzac Avenue provides many opportunities to enjoy vistas and views along and from the road including the vista east from Tilley Street to Redcliffe Parade towards Moreton Bay and towards the Fig tree terminating the Avenue at Redcliffe, and the vista west from Ashmole Street over the low area of Hay's Inlet and Pine Rivers towards Mount D'Aguilar, Mt Samson and Brisbane Forest Park.
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The house sits on a slightly sloping lot between Route 211 and Main Street, on the west side of Otisville near where the highway crests a low area of the Shawangunk Ridge. A neighboring parcel is included in the Register listing, for a total of including the house, three outbuildings, two objects, a ruin and a non- contributing swimming pool. It is a -story frame with a two-story wing to the rear, giving it an L-shape. The facade is three bays wide.
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The course is far less muddy and has a different route than the original course and has been well received.Fayetteville–Manlius High School Takes Girls, Boys Team Titles at 2014 Nike Cross Nationals on Nike News, Dec 6, 2014 NXN has a reputation for being extremely muddy. The course is located not only in the rainy Pacific Northwest but also in a low area and a drainage basin. It is a common sight to see runners soaked in mud at the end of NXN races.
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The anomaly will be mapped in a much greater detail to determine if it is related to the impact event. Airborne magnetic data show a strikingly circular magnetic anomaly, but for a reason not yet known it is slightly east from the gravity low area as well as the region where the shatter cones are found. It is possible that the ring was created for example by a granitic intrusion instead of the impact event. No specific anomalies have been found from radiometric or electromagnetic data.
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The Island Falls power dam spanned the main river channel at Big Eddy Falls, where there was a drop of . In addition, a number of earthen dams were built along the margin of the head pond (fore bay) to prevent overflow. About one mile (1.6 km) south, a 900-foot (275 m) concrete spillway dam known as "A-dam" was built across a low area on dry land later to be flooded. The fore bay was filled during July 1930, completely submerging the three low falls from which Island Falls gets its name.
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Together, these parameters tend to increase core thermal efficiency and improve fuel efficiency. # Some high-bypass-ratio civil turbofans use an extremely low area ratio (less than 1.01), convergent-divergent, nozzle on the bypass (or mixed exhaust) stream, to control the fan working line. The nozzle acts as if it has variable geometry. At low flight speeds the nozzle is unchoked (less than a Mach number of unity), so the exhaust gas speeds up as it approaches the throat and then slows down slightly as it reaches the divergent section.
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Calchaquí Valleys in Argentina Glacier National Park, Montana, United States Romsdalen in Western Norway is an almost vertical valley. Fljótsdalur in East Iceland, a rather flat valley Rio de Janeiro state, Brazil Baemsagol valley of Jirisan, Korea A valley is a low area between hills or mountains typically with a river running through it. In geology, a valley or dale is a depression that is longer than it is wide. The terms U-shaped and V-shaped are descriptive terms of geography to characterize the form of valleys.
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The ecoregion is a thin band of lowland terrain, long, stretching from Tomsk in the west, to the east of Krasnoyarsk in southern Siberia. On the western edge there is a north-south extension that follows the Tom River in the Kuznetsk Basin. In the middle is another extension, covering a low area along the Yenisei River and some of its tributaries; this area is known as the Minusinsk Hollow. To the west is the West Siberian broadleaf and mixed forests ecoregion, which is now mostly cultivated agricultural land.
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The Ukinrek Maars are two phreatomagmatic vents that formed on the north side of the Aleutian Range on a low area bordering the Bering Sea. The maars are 1.5 km south of Becharof Lake and 12 km northwest of Peulik Volcano. The western of the two is elliptical in shape and up to 170 m in diameter and 35 m deep. The east maar lies 600 m to the east and is circular and up to 300 m in diameter and 70 m deep. The east maar has a 49 m-high lava dome within the crater lake.
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Water loss is proportional to surface area, whereas the amount of water present is proportional to volume. Structures with a high surface area-to-volume ratio, such as thin leaves, necessarily lose water at a higher rate than structures with a low area-to- volume ratio, such as thickened stems. Spines, which are modified leaves, are present on even those cacti with true leaves, showing the evolution of spines preceded the loss of leaves. Although spines have a high surface area-to- volume ratio, at maturity they contain little or no water, being composed of fibers made up of dead cells.
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According to local tradition, Treasure Island was originally named Mindemoya, because of the distinctive shape of the island: rising at one end to a long, flat hill, with a steep drop to a short, low area at the other end. According to legend, a great chieftain or demi-god who once lived in Sault Ste. Marie, Ontario had a wife who would not give him any peace. In frustration he eventually kicked her and sent her flying, to land on her hands and knees in Lake Mindemoya, leaving her back and rump above the water, which we see today as the island.
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About the cult of the Santa Maria of the Assumption there are traces of it in numerous documents since the XII century. The veneration of the Madonna is of Greek origin and was, perhaps, introduced in Italy by monks that took refuge at the time of the iconoclastic wars. The first church dedicated to Her was situated in the lower part of the town, in the suburb "Fontana Vecchia", not far from the Basìa or Batìa, low area, and from the water spring, from which water was drawn for all necessities, till when, eventually, the water of Crini reached all the houses. Crini, in Greek means spring, source.
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In geology a sag, or trough, is a depressed, persistent, low area; the opposite of an arch, or ridge, a raised, persistent, high area. The terms sag and arch were used historically to describe very large features, for example, characterizing North America as two arches with a sag between them. Also, a sag is a former river bed which has been partially filled with debris from glaciation or other natural processes but which is still visible in the surface terrain. Sags formed by the former river beds of large rivers often become the valleys of smaller streams after a change of course by the main river.
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Ardmore is located about south of the Arbuckle Mountains, an ancient, eroded range spanning some across southern Oklahoma. The geology is highly variegated within the area, with uplifted and folded ridges visible within the shoreline of some of the lakes surrounding Ardmore. The city of Ardmore has no intracity streams or rivers, but is part of the Washita and Red River watersheds, with two tributaries, Caddo and Hickory creeks, flanking the broad, low area in which Ardmore is situated. Ardmore is also north of Lake Murray, an impoundment of the two arms of Anadarche Creek, which eventually flows into the western reaches of Lake Texoma.
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An anglers catch of Malabar trevallyThe Malabar trevally often schools, especially as juveniles in shallow bays, becoming more solitary as they age. The species is not particularly aggressive, feeding on small planktonic and pelagic crustaceans such as krill, prawns, shrimp, and mysids, as well as small squids and fishes. Geographical variation in diet is common, with fish in Malaysia taking species of polychaete worms as the preferred species. Studies on gill filtering mechanisms has shown the Malabar trevally's anatomy lies between two extremes, one which is a high filtration area characteristic of planktivorous species and the other of very low area which is associated with species which take large prey items.
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Barker and Rasmussen 1998, p. 56 Metalwork and glass beads among archaeological finds indicate that even at this period Narce was involved in long-range trade routes.Turfa 2005, p. 14 During the Villanovan Iron Age (900-700 B.C.), settlements grew up in higher areas to the north and south.Barker and Rasmussen 1998, p. 63 The latest habitation on the lower-lying part of the site dates to the 7th century B.C.Turfa 2005, p. 14 This low area was used exclusively for burials from the second half of that century onward.Turfa 2005, p. 14 At this time the center of the settlement was at Monte li Santi.
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Barbentane is located at the northernmost point of the Bouches- du-Rhône department immediately south-west of Avignon near a rocky plateau and stretching a few kilometres across a flat low area and low hills where the urban area is located. The northern border of the commune is the departmental border between Bouches-du-Rhône and Vaucluse while the western border is the departmental border with Gard. Access to the commune is by the D35 road from Rognonas in the east, which passes through the commune and the town and continues west, then south-west, to Boulbon. The D570N from Graveson in the south-east passes along the eastern border of the commune then goes east to Rognonas.
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Of the original zoological facilities in the park, the Deer Paddock, located near the present Carousel, was converted into a meadow and the deer were moved to the new Menagerie, The Wild Fowl Pond remained, located on the east side of the park in a low area now forming the northern part of the zoo. The Menagerie continued to accrue animals in the first decades of the 20th century. These were generally donated by prominent individuals and institutions and formed a varied collection of specimens both native to North America and other regions of the world. A two-story brick building was opened in the Menagerie in 1916, housing monkeys, some small mammals, and several birds.
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The station is located on the southwest corner of downtown Chappaqua, located in a low area amid hilly terrain just north of the Mount Pleasant town line. At that point the two railroad tracks run straight in a northeast-southwest heading, paralleling the Saw Mill River Parkway and the headwaters of the eponymous stream immediately to their west. Quaker Road (New York State Route 120) crosses over the tracks just north of the station, east of its interchange with the parkway. Beyond the Quaker Road bridge, a parking lot separates the road from the main commercial area of downtown around the intersection of King Street, South Greeley Avenue, and North Greeley Avenue.
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The yield of the Kraft process is only about 50%, which makes the demand of wood twice as high for the same amount of produced pulp Another benefit of the mechanical pulps is the excellent printing properties, making them very useful in newsprint and magazines. This is because of their good properties of absorbing the ink and also their high opacities and low area density. Chemimechanical pulps can give paper with high stiffness, making them suitable for paper board and as a stiff layer in paper packaging. The mechanical pulping processes have a high yield, which at the same time means that all the lignin is still present in the pulp and paper.
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Based on an assessment published in 2012 and current in 2016, the IUCN Red List has assigned Pseudomys shortridgei a classification of near threatened, of less concern than the conservations status of vulnerable. They have a low area of occupancy, less than 2000 km2, and occurrence at less than ten locations protected by conservation acts.. The population trajectory is noted as declining toward extinction, potentially elevating the concern if it continues, and was estimated to be a total of around 11000 individuals in 2012. This species is listed as threatened in the states of Victoria, South Australia, and Western Australia. The national status of P. shortridgei (EPBC act,1999) is vulnerable to extinction.
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Hermann Dischler (1867-1935): Die Baar The Baar is composed of several types of landscape. In the west is Baarschwarzwald (the Black Forest), in the center Baarhochmulde (a marshy area), in the south the Wutachland around the Wutach river, and in the east the Baaralb, a low area with buttes of the Swabian Alb like the Hohenkarpfen and the Lupfen, which is the highest point in the Baar at 977 metres. The Baar makes up the core of the Schwarzwald-Baar-Heuberg administrative region of Baden-Württemberg and contains the district Schwarzwald-Baar-Kreis (except for its northwest portion), the western part of Kreis Tuttlingen, and the southern part of Kreis Rottweil, and juts out into Kreis Breisgau-Hochschwarzwald.
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Anochetus ghilianii is a species of ant of the subfamily Ponerinae, which is native to Morocco, and it also has a not confirmed status in Gibraltar and Spain, as scientists are not sure whether its native or exotic due having a very low area where it lives in the Iberian peninsula (Only found in the province of Cadiz in Spain). The species is monogynous, the queens of this species is ergatoid, meaning that it does not have wings. However, the males from the colony do have wings. The worker numbers can vary from having between 300-250 in early months of the year to just between 10-50 in the summer, thus the colonies are not very big and they are usually 20-30cm deep.
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Its territory has an area of 11,100 km2, where the Andean physiographic character predominates, with heights above 2,000 m. The mountainous relief is the southern continuation of the Merida mountain range, which penetrates from the north in a southwesterly direction, exceeding 4,000 m in the La Negra moor. Mountain formations, El Tamá National Park, Táchira State In the extreme southwest, the Táchira depression was formed, which includes the tectonic trench through which the river of the same name runs and the entire relatively low area located between this trench and the valleys of the Lobaterita, the Torbes Medio and the Quinimarí Medio. The depression of the Torbes River separates the main range of the Mérida Range from the Tamá Range.
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Faulting here is not only responsible for the blocks but has allowed incursions of more than one stream to aid the process of block fall. At present one small stream enters at the southern end, but previous flooding such as in 1998 has opened up choked passages, allowing a large volume of water to enter Main Chamber. A huge section of the mud bank in that chamber collapsed and the flood subsiding refilled the passage. This process of opening and closing of inlets has probably been repeated many times over the centuries. The stream at the base of the chamber flows amongst fallen blocks to enter a passage of fine proportions, but the roof soon dips to where the stream enters a low area known as ‘the grovel’.
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It then forms the northern boundary of Strathmore and reaches the North Sea immediately north of Stonehaven near the ruined Chapel of St. Mary and St. Nathalan. Aeromagnetic maps of Great Britain and Northern Ireland show that the Highland Boundary Fault can be traced from Ireland to the region of Greenock. In these areas, the Highland Boundary Fault is seen to be dividing a northerly low area from a southerly high area. The fault is often considered a terrane boundary: the Midland Valley terrane lies to the south whilst the Southern Highlands or Grampian terrane lies to the north In 1970, Hall and Dagley identified the Highland Boundary Fault as coincident with a regional magnetic feature dividing a string of negative anomalies in the north from positive ones in the south.
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In the early Mesolithic period (Middle Stone Age, mid to late 8th millennium BC), the local upland was mostly pine woodland and the low area of central Berkhamsted probably a grass-sedge fen. In the 6th Millennium BC the dense deciduous forest became well established. By the Mid to late 3rd millennium BC during the Neolithic period (the New Stone Age) human activity can be seen in wood clearances; the woodland being then dominated by lime trees, with alder trees growing on the flood plain. The River Bulbourne, a chalk stream, runs through the valley for in a southeast direction, starting at Dudswell and the adjoining village of Northchurch and running through Berkhamsted, Bourne End and Boxmoor, where it merges with the River Gade at Two Waters in Apsley, near Hemel Hempstead.
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This natural dike cuts off the flow of the river to the remarkable low area in southern California known as the Salton Sink in the Coachella Valley, and the Imperial Valley. The Salton Sink and its Salton Sea are located below sea level; therefore, the descent from the river near Yuma is very much greater than the descent from Yuma to the Gulf of California. This geographical peculiarity is the result of the Colorado River Delta, formed over millions of years by over of rock and sand eroded from the Grand Canyon and other canyons along the river's course. The delta eventually split the Gulf of California in two; the northern part in present-day California, cut off from the sea, eventually evaporated, creating a "sink" more than below sea level.
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To calculate land use requirements for different kinds of energy production, it is essential to know the relevant area-specific power densities. Smil estimates that the average area-specific power densities for modern biofuels, wind, hydro and solar power production are 0.30 W/m2, 1 W/m2, 3 W/m2 and 5 W/m2, respectively (power in the form of heat for biofuels, and electricity for wind, hydro and solar). The average human power consumption on ice-free land is 0.125 W/m2 (heat and electricity combined), although rising to 20 W/m2 in urban and industrial areas. The reason for the low area-specific power density for biofuels is a combination of low yields and only partial utilization of the plant (for instance, ethanol is typically made from sugarcane's sugar content or corn's starch content, while biodiesel is often made from rapeseed and soybean's oil content).
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A saddle is the lowest area between two highlands (prominences or peaks) but has two wings which span the divide (the line between the two prominences) by crossing the divide at an angle, so is concurrently the local highpoint of the land surface which falls off in the down direction. That is, the drainage divide is a ridge along the high point of the saddle, as well as between the two peaks so defines the major reference axis. A saddle can vary from a sharp narrow gap to a broad comfortable sway-backed shallow valley so long as it is both the high point in the sloping faces descending to lower elevations and the low area between the two (or three or four.) flanking summits. Concurrently, along a different axis, it is the low point between two peaks, so is the likely 'optimal' high point in a pass if the saddle is traversed by a track, road or railway.
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