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"upthrust" Definitions
  1. (physics) the force with which a liquid or gas pushes up against an object that is floating in it
  2. (also uplift) (geology) the process or result of land being moved to a higher level by movements inside the earth

58 Sentences With "upthrust"

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

But they had left that fence line standing against the sky like a bunch of upthrust middle fingers.
The crescent lines with which their lowered arms answer their upthrust legs are terrific, like the long, slanting curve of the two legs.
The warning is in stark contrast with its previous prediction that the economy would grow in line with the "robust underlying cyclical upthrust" in the quarter.
In her 1982 painting "Crevice," slabs of upthrust rock tumbled against one another, with a pair of disembodied feet and ankles adding a ghostly human presence.
The scenery would have been enough to draw me to the cordillera, with its upthrust layers of multicolored sedimentary rock set around a crater that's encircled by rugged river canyons.
There is the "Rescue Team, Royal National Lifeboat Institution, UK," standing atop the upthrust prow of a rescue boat while a yellow copter hovers overhead, dangling a rescued man on a wire.
"After finding major support at the $1,300 per ounce mark, (gold) prices have witnessed an upthrust, and moved past the invincible $824.503,326 per ounce mark," said Sugandha Sachdeva, vice-president, metals, energy and currency research, Religare Broking Ltd.
"After finding major support at the $1,300 per ounce mark, (gold) prices have witnessed an upthrust, and moved past the invincible $1,0.13 per ounce mark," said Sugandha Sachdeva, vice-president, metals, energy and currency research, Religare Broking Ltd.
"After finding major support at the $1,300 per ounce mark, (gold) prices have witnessed an upthrust, and moved past the invincible $1,0.53 per ounce mark," said Sugandha Sachdeva, vice-president, metals, energy and currency research, Religare Broking Ltd.
The severity of the damage caused by the earthquake is attributed to severe upthrust. It is considered the deadliest earthquake to hit South Asia, surpassing the 1935 Quetta earthquake.
The summit of Stone Arthur is difficult to locate exactly amongst the upthrust rocks of Arthur's Chair. The view is excellent, particularly over Grasmere with Easedale Tarn showing across the valley.
Unsworth (2000), pp. 334-337 While the exact height of Everest's summit is subject to minor variation due to the level of snow cover and the gradual upthrust of the Himalaya, significant changes to the world altitude record are now impossible.
Sagunto Castle occupies a prominent hilltop The castle is located north of Valencia, upon a flat-topped hill.Collins 1998, p. 229. The hill is the last upthrust of the Sierra Calderona mountains, reaching an altitude of above mean sea level.Tourist Info Sagunto.
Eventually the rocks were pushed up and out of the water. Over time, the rock was upthrust and tilted to a westerly direction. The thrusting also pushed the rock from the Connecticut River Valley to its present location, just west of the Hudson River.
An even longer trench runs alongside the coast of Peru and Chile, reaching a depth of and extending for approximately . It occurs where the oceanic Nazca Plate slides under the continental South American Plate and is associated with the upthrust and volcanic activity of the Andes.
At highstand, Lake Palomas contained the islands Unión and Santa María. The islands were and , respectively. Islands were formed by the Carrizal Mountains, the Guzmán Mountains and the Las Muertos Mountains. The lake was subdivided into three basins (east, central and west) by upthrust Cretaceous mountains and Tertiary intrusives.
An explanation for the embayment's formation was put forward by Van Arsdale and Cox in 2007: movement of the earth's crust brought this region over a volcanic "hotspot" in the Earth's mantle causing an upthrust of magma which formed the Appalachian- Ouachita range. Subsequent erosion caused a deep trough that was flooded by the Gulf of Mexico and eventually filled with sediment from the Mississippi River.
A subsidiary spur branches off north-west of the summit, passing over White Pike before petering out in the Ennerdale Forest. The eastern ridge of Pillar stretches for about a mile, gradually descending before the final upthrust of Looking Stead. This subsidiary top is listed as a Nuttall in its own right. Beyond is Black Sail Pass, a pedestrian route between Wasdale and the head of Ennerdale.
The parapet walls connect the towers to the cable anchorage structures. These consist of a shaft sunk some 25 ft into sound sandstone. At the bottom of each shaft is an enlarged chamber where riveted steel beams transfer the tensile forces from the cables to upthrust in the sandstone above. At the surface there are cast iron shoulder castings which turn the cables from inclined to vertical.
Graystones summit is grassy, the highest point marked by a slight upthrust in the underlying rock. It lies within a few yards of the end of the wall rising from Widow Hause. A cairn has been erected on the western slopes of Kirk Fell. The slopes are too shallow to give any remarkable view, but the Loweswater Fells and the tops surrounding Coledale Hause can all be seen.
This was probably an idealization of the shapes of ships' hulls. Some of his sections float with the base under water and the summit above water, similar to the way that icebergs float. Archimedes' principle of buoyancy is given in the work, stated as follows: > Any body wholly or partially immersed in a fluid experiences an upthrust > equal to, but opposite in sense to, the weight of the fluid displaced.
The Lusatian Fault (), formerly Lusatian Overthrust (Lausitzer Überschiebung), is the most important geological disturbance zone between the Elbe valley and the Giant Mountains. It is a fault that separates the granite of Lusatia from the Cretaceous sandstones of North Bohemia to the south. It is assumed that there was a fault throw of several hundred metres whereby the northern block was uplifted or upthrust relative to the southern block.
Kupe's Sail is another feature of Cape Palliser - a triangular upthrust of sedimentary rock shaped like a sail. Maori history and the Kupe legend both feature Cape Palliser. Cape Palliser was named in 1770 by Captain James Cook in honour of his friend Admiral Sir Hugh Palliser of the British Royal Navy. The Cape Palliser Lighthouse is located here; it was first lit in 1897 but became automated in 1986.
Scuba divers often wear lead weights to counteract the positive buoyancy of their bodies and gear. Gases are also fluids, and so objects floating in the air may also be trimmed to be neutrally buoyant. A hot-air balloon that is neither sinking nor rising uses the lower density of hot air compared with the density of the surrounding air to produce sufficient upthrust to balance the weight of the basket and its contents.
Lake Clark National Park geologic map The park has four main physiographic regions. The upthrust granite Chigmit Mountains connect the Alaska Range to the Aleutian Range. Superimposed on these mountains and little to the east of the main range are the two stratovolcanoes, Redoubt high, and Iliamna at . Glaciers have altered the mountains, carving cirques and U-shaped valleys into the range, which end abruptly on the east at the steep coast in deep bays or in outwash flats.
The metasedimentary rocks are quartz-rich and the amphibolites represent mafic igneous intrusions. Age analyses of detrital minerals, petrology, and geochemistry all indicate that the island belongs geologically with the other islands of the Outer Banda Arc. This series of islands formed when the northern edge of the Australian continent was upthrust in collision with southeast Asia. These islands are paralleled by the Inner Banda Arc, a series of active and extinct volcanic islands, including neighboring Wetar.
A torpedo fitted with a proximity fuze can be detonated directly under the keel of a target ship. The explosion creates a gas bubble which may damage the keel or underside plating of the target. However, the most destructive part of the explosion is the upthrust of the gas bubble, which will bodily lift the hull in the water. The structure of the hull is designed to resist downward rather than upward pressure, causing severe strain in this phase of the explosion.
Like the Catskills as a whole, a dissected plateau, Tremper was formed not through the upthrust of rock layers but by the gradual erosion of stream valleys in an uplifted region about 350 mya. Its rock layers and bedrock are primarily Devonian and Silurian shale and sandstone. Bluestone is present in enough quantity that a quarry was once located on the south side of the mountain at an elevation of . Its remains are still visible today from the old road to the fire tower, which passes it.
By defining the apparent weight of an object in terms of normal forces, one can capture this effect of the stress forces. A common definition is "the force the body exerts on whatever it rests on." The apparent weight can also differ from weight when an object is "partially or completely immersed in a fluid", where there is an "upthrust" from the fluid that is working against the force of gravity. Another example is the weight of an object or person riding in an elevator.
Timor is located north of Australia, and is one of the easternmost Sunda Islands. Together with Sumba, Babar and associated smaller islands, Timor forms the southern outer archipelago of the Lesser Sunda Islands with the inner islands of Flores, Alor and Wetar to the north, and beyond them Sulawesi. Timor is the principal island of the Outer Banda Arc, which has been upthrust by collision with the Australian continent. Timor has older geology and lacks the volcanic nature of the northern Lesser Sunda Islands.
In simple terms, the principle states that the buoyancy force on an object is equal to the weight of the fluid displaced by the object, or the density of the fluid multiplied by the submerged volume times the gravitational acceleration, g. Thus, among completely submerged objects with equal masses, objects with greater volume have greater buoyancy. This is also known as upthrust. Suppose a rock's weight is measured as 10 newtons when suspended by a string in a vacuum with gravity acting upon it.
NOAA tsunami energy map An upthrust of along a wide seabed at offshore from the east coast of TōhokuNHK BS News reported 2011-04-03-02:55 JST resulted in a major tsunami that brought destruction along the Pacific coastline of Japan's northern islands. Thousands of lives were lost and entire towns were devastated. The tsunami propagated throughout the Pacific Ocean region reaching the entire Pacific coast of North and South America from Alaska to Chile. Warnings were issued and evacuations were carried out in many countries bordering the Pacific.
Like the Catskills as a whole, a dissected plateau, Halcott was formed not through the upthrust of rock layers but by the gradual erosion of stream valleys in an uplifted region about 350 mya. Its rock layers and bedrock are primarily Devonian and Silurian shale and sandstone. Later glaciation, primarily the Illinois and Wisconsin periods, shaped the slopes of the mountain, smoothing its slopes on the west when the ice was covering it and steepening the east slopes through erosion when the meltwater burst through Deep Notch.DEC, 7.
The underlying rock formation derives from the Kaapvaal Craton, formed as a precursor island roughly 2.7 billion years ago. This crustal formation became the base of the Waterberg, which was further transformed by upward extrusion of igneous rocks.William Taylor, Gerald Hinde and David Holt-Biddle, The Waterberg, Struik Publishers, Cape Ttown, South Africa (2003) These extruded rocks, containing minerals such as vanadium and platinum, are called the Bushveld Igneous Complex. The original extent of this rock upthrust involved about 250,000 square kilometers, and is sometimes called the Waterberg Supergroup.
The Eastern Mobile Belt extends from this fault zone to the north-south trending Taranaki fault zone, which is adjacent to the a large upthrust basement block that divides the Taranaki Basin from the later-formed, eastward Wanganui Basin. ;Nature The Blue whale, Southern right whale and the critically endangered Maui's dolphin are living beings in the sea in Taranaki Basin, or live near the coast of Taranaki. For the Blue whale it is a breeding ground.Rainbow Warrior confronts Taranaki oil rigs’’, Greenpeace New Zealand, October 2, 2018.
The steeply dipping, ESE-striking rocks of the Thiviers-Payzac Unit upthrust obliquely over the Upper Gneiss Unit with a right-lateral shearing component. The Upper Gneiss Unit strikes southwest- northeast and in turn overrides The Lower Gneiss Unit to the northwest, also showing a SW-NE strike. Enclosed within the micaschists are basic and ultrabasic rocks of the Roche Noire Massif (near the hamlet La Valade), mainly metagabbros and peridotites. These are some of the very few remnants of oceanic crust left behind from a now subducted ocean.
The long south east ridge of Skiddaw descends over Little Man and Jenkin Hill to the depression of Flag Pots. Beyond this is the final upthrust of Lonscale Fell before the craggy descent to the Glenderaterra Beck, The southern flanks fall gently over acres of sheep pasture in the manner of the Skiddaw range. At the base of the slope is the wooded valley of Whit Beck, separating Lonscale Fell from the east ridge of Latrigg. Here also is Lonscale, the farm which has given its name to the fell.
The Jaramillo Petrified Forest National Park is a protected area of petrified forest located in the Deseado Department, in the northeast of Santa Cruz Province, Argentina. Formerly part of the site was a natural monument, established in 1954 and known as the Petrified Forest Natural Monument, covering about . This area has remnants of a forest preserved in stone, that had been growing on the site before the upthrust of the Andes some 150 million years ago. In December 2012, further land was added and the protected area was reclassified as a national park with a total area of .
Heavier-than-air aircraft, such as airplanes, must find some way to push air or gas downwards, so that a reaction occurs (by Newton's laws of motion) to push the aircraft upwards. This dynamic movement through the air is the origin of the term aerodyne. There are two ways to produce dynamic upthrust — aerodynamic lift, and powered lift in the form of engine thrust. Aerodynamic lift involving wings is the most common, with fixed-wing aircraft being kept in the air by the forward movement of wings, and rotorcraft by spinning wing-shaped rotors sometimes called rotary wings.
Florence, the county seat, is to the northwest, while Myrtle Beach is to the east. According to the United States Census Bureau, the city has a total area of , of which , or 1.36%, is water. The city of Johnsonville is located only a few miles from The Johnsonville Impact Crater, a circular geophysical feature that has been interpreted by some scientists as an impact crater, situated at the junction of Lynches River and the Pee Dee River in South Carolina. Snows Island, at that point, is believed to be the upthrust of the center after the impact.
Map of the Maatsuyker Islands detailed map of Maatsuyker Island detailed map of de Witt Island Outline of Ile du Golfe shaped like a dolphin The Maatsuyker Islands are a group of islands and rocks located off the south coast of Tasmania, Australia. Maatsuyker Island is the southernmost island of the group and of the Australian continental shelf. There are exposed rocks further south of Maatsuyker but they do not meet the definition of "islands". Macquarie Island, far to the south, is also Australian territory but it is an upthrust piece of ocean floor in the remote Southern Ocean and is in a geological sense completely separate from the continent.
The underlying rock formation of the Palala River basin derives from the Kaapvaal craton, formed as a precursor island roughly 2.7 billion years ago. This crustal formation became the base of the Waterberg, which was further transformed by upward extrusion of igneous rocks.William Taylor, Gerald Hinde and David Holt-Biddle, The Waterberg, Struik Publishers, Cape Town, South Africa (2003) These extruded rocks, containing minerals such as vanadium and platinum, are called the Bushveld igneous complex, leading to the colourful bluff faces along much of the Palala River. The original extent of this rock upthrust involved about 250,000 square kilometers, and is sometimes called the Waterberg Supergroup.
According to the U.S. Census Bureau, the county has a total area of , of which is land and (11%) is water. Contra Costa County's physical geography is dominated by the bayside alluvial plain, the Oakland Hills-Berkeley Hills, several inland valleys, and Mount Diablo, an isolated 3,849-foot (1,173 m) upthrust peak at the north end of the Diablo Range of hills. The summit of Mount Diablo is the origin of the Mount Diablo Meridian and Base Line, on which the surveys of much of California and western Nevada are based. The Hayward Fault Zone runs through the western portion of the county, from Kensington to Richmond.
16th-century illustration of Archimedes in the bath, with Hiero's crown at bottom right The exclamation 'Eureka!' is attributed to the ancient Greek scholar Archimedes. He reportedly proclaimed "Eureka! Eureka!" after he had stepped into a bath and noticed that the water level rose, whereupon he suddenly understood that the volume of water displaced must be equal to the volume of the part of his body he had submerged. (This relation is not what is known as Archimedes' principle—that deals with the upthrust experienced by a body immersed in a fluid.) He then realized that the volume of irregular objects could be measured with precision, a previously intractable problem.
The region is cut by several major rivers, including the Oder (Odra), which defines the Silesian Lowlands in the southwest, and the Vistula (Wisla), which defines the lowland areas of east-central Poland. To the south of the lowlands are the lesser Poland uplands, a belt varying in width from 90 to 200 kilometers, formed by the gently sloping foothills of the Sudeten and Carpathian mountain ranges and the uplands that connect the ranges in southcentral Poland. The topography of this region is divided transversely into higher and lower elevations, reflecting its underlying geological structure. In the western section, the Silesia-Kraków Upthrust contains rich coal deposits.
There are a few small rivers running through Suhl: The Hasel rises at Friedberg in the south-east and runs westward through Suhl, Heinrichs, Mäbendorf, Dietzhausen and Wichtshausen. The Lauter rises on the southern slope of Großer Beerberg mountain and runs through Goldlauter, Lauter and the city centre, before it joins the Hasel behind the station. The Mühlwasser rises on the western slope of Großer Beerberg and runs southward through the northern city parts before it joins the Lauter at the northern city centre. Suhl sits on the southern edge of the Suhler Scholle, an upthrust granite complex that is streaked by numerous dikes.
Kawarau Gorge, where Roaring Meg joins the Kawarau River, in central Otago The country's fourth-longest river, the Taieri, also has both its source and outflow in Otago, rising from rough hill country and following a broad horseshoe-shaped path, north, then east, and finally southeast, before reaching the Pacific Ocean. Along its course it forms two notable geographic features – the broad high valley of the Strath-Taieri in its upper reaches, and the fertile Taieri Plains as it approaches the ocean. Travelling east from the mountains, the Central Otago drylands predominate. These are Canterbury-Otago tussock grasslands dominated by the block mountains, upthrust schist mountains.
The watershed is formed primarily by the upthrust of Ordovician (Precambrian) rocks north-east of the Ticknall–Thringstone Fault with Carboniferous measures to the south-west of the fault, including coal, clay and sandstone, which have been exploited in the 19th and 20th centuries as the Leicestershire and South Derbyshire Coalfield. Over much of the watershed, the Ordovician outcrop of Bardon Hill is prominent. Most of the Carboniferous measures of western Leicestershire are covered with red mudstones of the Triassic Mercia Mudstone Group. The outcrop of these rocks gives rise to a moderately undulating landscape characterised by mixed pasture and arable agricultural use that has developed on the neutral clay soils.
Most of the wilderness lies between the crests of two parallel mountain ranges, the San Rafael Mountains and Sierra Madre Mountains, and includes the drainages of two watercourses: the Sisquoc River and Manzana Creek. Both flow to the northwest, eventually joining together and draining into the ocean near Santa Maria. Elevations within the wilderness vary from at the confluence of Manzana Creek and the Sisquoc River on the western boundary, to over at Big Pine Mountain, the highest point in Santa Barbara County. Dividing the drainages of the Manzana and Sisquoc is a ridge known as Hurricane Deck, a rugged slab of upthrust sandstone with a trail snaking along the top.
The modern meaning of the American flag, according to Harold Holzer in 2007 and Adam Goodheart in 2011, was forged by Anderson's stand at Fort Sumter. Holzer states that New York City: :responded with a "feast of the American flag." Eyewitnesses estimated that as many as 100,000 flags quickly went on display across the city. To punctuate this feast of national colors, New York's graphic artists rushed out patriotic engravings and lithographs depicting avenging soldiers or gowned goddesses, bayonets upthrust, carrying "The Flag of Our Union" into future battles....Composers dedicated songs like "Our Countries Flag" to President Lincoln, and adorned their published sheet music with colorful images of resolute soldiers gripping the national banner.
Aerial view of the Los Medanos foothills and Mount Diablo from over Suisun Bay at Concord, California Mount Diablo is a mountain of the Diablo Range, in Contra Costa County of the eastern San Francisco Bay Area in Northern California. It is south of Clayton and northeast of Danville. It is an isolated upthrust peak of , visible from most of the San Francisco Bay Area. Mount Diablo appears from many angles to be a double pyramid and has many subsidiary peaks, the largest and closest of which is the other half of the double pyramid, North Peak, nearly as high in elevation at and about a mile northeast of the main summit.
On October 8, 2005, a major earthquake registered a moment magnitude of 7.6 in Azad Kashmir, near the city of Muzaffarabad in Pakistan. Occurring at 08:52:37 Pakistan Standard Time, it registered a moment magnitude of 7.6 The disaster destroyed 50% of the buildings in Muzaffarabad (including most of the official buildings) and is estimated to have killed up to 80,000 people in the Pakistani-controlled areas of Kashmir, alone. The severity of the damage caused by the earthquake is attributed to severe upthrust, coupled with poor construction. CMAT focused its efforts in northern Pakistan, initially in Bagh and Muzaffarabad areas sending an assessment team from Canada on October 10, consisting of search and rescue, logistics and paramedics, as well as an emergency physician.
Geoscience, 366, 19-28 The geology of the area has attracted considerable study and is fundamental to the position of the town: # the weakness in the rocks giving rise to the course of the river # the mountain pass following the river # the formation of the local marble through metamorphosis and # the subsequent development of complex local soil types allowing for a variety of vineyard terroirs On a larger scale, the Montagne Noir result from the tectonic movements of ancient plates, ultimately resulting in the upthrust of the Alps and the Pyrenees. These mountain building events are known as orogenic periods, often named after the principal mountain ranges or ancient tribal areas in which the early geological research was undertaken. The Montagne Noire result largely from what is known as the Variscan (or Hercynian) Orogeny.
The second phase, the paleotechnic (roughly 1700 to 1900), is "an upthrust into barbarism, aided by the very forces and interests which originally had been directed toward the conquest of the environment and the perfection of human nature." p.154 Inventions of the paleotechnic are made by men trying to solve specific problems rather than hunting for general scientific principles; in fact, scientific learning is devalued by men of business. The invention of coal-fired steam powered factories and the installation of capital-intensive machinery leads to a necessarily gigantic round-the-clock scale of production supported by unskilled machine tenders. Labour becomes a commodity, rather than an inalienable set of skills, the labourer who tended machines, lived in slums, and was paid starvation wages, became physically stunted and socially and spiritually stultified.
On 2 April 2007 at 07:39:56 local time (UTC+11) an earthquake with magnitude 8.1 occurred at hypocenter S8.453 E156.957, 349 kilometres (217 miles) northwest of the island's capital, Honiara and south- east of the capital of Western Province, Gizo, at a depth of 10 km (6.2 miles)."Solomon Islands earthquake and tsunami", Breaking Legal News – International, 4 March 2007 More than 44 aftershocks with magnitude 5.0 or greater occurred up until 22:00:00 UTC, Wednesday, 4 April 2007. A tsunami followed killing at least 52 people, destroying more than 900 homes and leaving thousands of people homeless."Aid reaches tsunami-hit Solomons", BBC News, 3 April 2007 Land upthrust extended the shoreline of one island, Ranongga, by up to 70 metres (230 ft) exposing many once pristine coral reefs.
John Underhill, the third co-author of the study,Odysseus Unbound, particularly Appendix 2. is Professor of Stratigraphy at the University of Edinburgh and a recognized authority on the structure and stratigraphy of sedimentary basins, and on the geology of the Ionian islands. His contributions in several areas, including investigation of the prior existence of "Strabo's Channel", and analyses of factors such as tectonic uplift, and erosion, also were crucial in authenticating Paliki. The initial geological problem posed by Bittlestone — whether sea levels in the region might once have been higher, such that the narrow isthmus now connecting Paliki to the rest of Kefalonia might once have been submerged — turned out to be exactly the opposite, the sea didn't fall but the land rose, and the periodic earthquakes that triggered this upthrust simultaneously brought down catastrophic rockfalls.
Geological map of Thuringian Forest Geologically, the Thuringian Forest is defined by a belt of strongly uplifted and deformed metamorphic and igneous rock that divides the relatively flat sedimentary plains of the Thüringer Becken (to the northeast) from similar rock formations in the valley of the Werra (to the southwest). It consists of a large fault block in hercynian orientation, which consists from sandstones and conglomerates of Rotliegend age in its western parts (Eisenach trough), followed by granites and gneisses of the Ruhlaer Kristallin formation of early paleozoic origin which were uplifted in the Rotliegend era, and the conglomerates, sandstones, and abundant volcanic rocks (rhyolites and andesites) of the Oberhof trough. Ore deposits associated with the upthrust of the range have been of significant historical importance in the development of the region, for example, the metalworking tradition in Suhl and the mining history of Ilmenau. The uplift of the horst-like fault block was part of the Saxonian tectonic processes and is understood as a long range effect of the Alpine orogeny.
The chosen site presented a number of construction challenges because the southern half was a swamp and the northern half was on the steep slope of Nobby's Headland, an upthrust of schist about 50 m high at its highest point. The challenges were met by the simple expedient of blasting the slope and dumping the rubble in the swamp, but with a consequent complete loss of topsoil that created enduring problems for many years. Construction always stayed behind the needs of the students throughout the sixties. This was for three reasons: (a) it was an entirely new school competing with established schools for resources in a state that had allowed chronic neglect of its education infrastructure and which was in far worse condition than the larger states of Victoria (Australia) and New South Wales, (b) Miami High's construction coincided precisely with the transition of the Baby Boom Generation from primary school to high school, and (c) in 1964, Queensland's primary schools ceased to teach the eighth year, which was transferred to the high schools, so that the entry year to high school became year 8.

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