query: what large plateau is in the north-eastern part of california

pos: Modoc Plateau part of the plateau, while southern watersheds either collect in basin reservoirs or flow into the large Big Sage Reservoir, which sits in the center of Modoc County. Modoc Plateau The Modoc Plateau lies in the northeast corner of California as well as parts of Oregon and Nevada. Nearly of the Modoc National Forest are on the plateau between the Medicine Lake Highlands in the west and the Warner Mountains in the east. Its landform is volcanic table land ranging from 4,000 to 6,000 feet above sea level, cut by many north-south faults. "Occasioned lakes, marshes, and sluggishly flowing streams

pos: Modoc Plateau part of the plateau, while southern watersheds either collect in basin reservoirs or flow into the large Big Sage Reservoir, which sits in the center of Modoc County. Modoc Plateau The Modoc Plateau lies in the northeast corner of California as well as parts of Oregon and Nevada. Nearly of the Modoc National Forest are on the plateau between the Medicine Lake Highlands in the west and the Warner Mountains in the east. Its landform is volcanic table land ranging from 4,000 to 6,000 feet above sea level, cut by many north-south faults. "Occasioned lakes, marshes, and sluggishly flowing streams

pos: Geography of California is centered on Mount Shasta, near the Trinity Alps. Mount Shasta is a dormant volcano, but there is some evidence that it erupted in the 18th Century. In the northeast corner of the state lies the Modoc Plateau, an expanse of lava flows that formed a million years ago and now lie at an altitude of . The plateau has many cinder cones, juniper flats, pine forests, and seasonal lakes. The plateau lies between the Cascade Range to the west and the Warner Mountains to the east. The Lost River watershed drains the north part of the plateau, while southern

neg: Geography of Tanzania Tanzania is a large plateau, which is part of the East African Plateau. The southern half of this plateau is grassland within the Eastern Miombo woodlands ecoregion, the majority of which is covered by the huge Selous National Park. Further north the plateau is arable land and includes the national capital, Dodoma. The eastern coast contains Tanzania's largest city and former capital, Dar es Salaam. Just north of this city lies the Zanzibar Archipelago, a semi-autonomous territory of Tanzania which is famous for its spices. The coast is home to areas of East African mangroves, mangrove swamps that are an

neg: Pennyroyal Plateau Pennyroyal Plateau The Pennyroyal Plateau is a large area of Kentucky that features rolling hills, caves, and karst topography in general. It is named for a wild mint that grows in the area. It is also called the "Mississippian Plateau," for the Mississippian geologic age in which it was formed. The Pennyroyal is bordered by the Pottsville Escarpment in the east. The Pottsville Escarpment is the transition zone from the central part of Kentucky to the higher and geologically younger Cumberland Plateau in the eastern part of the state. The Pennyroyal is bordered on the north by Muldraugh Hill, the

neg: Uncompahgre Plateau Uncompahgre Plateau The Uncompahgre Plateau in western Colorado is a distinctive large uplift part of the Colorado Plateau. Uncompahgre is a Ute Indian word that describes the water: "Dirty Water" or "Rocks that make Water Red". The plateau, with an average elevation of , rises from the Colorado River to Horsefly Peak . It continues on about southeast to the northwest margin of the San Juan Mountains. Its boundaries are the San Miguel and Dolores Rivers to the west, the Colorado River to the north and the Gunnison and Uncompahgre Rivers on the eastern side. Large canyons such as Big

neg: Nyika Plateau settlement on the plateau is Chelinda, the headquarters and accommodation site for the Malawian park. A large area of the Nyika Plateau, around , makes up the Nyika National Park. Owing to its protected status, endemic flora continue to flourish in this part of the plateau. The flora of the plateau include gladioli, delphiniums, lobelia, and 'red hot pokers'. The plateau is also home to around 200 species of orchids. Groves of montane forests also dot the plateau. Nyika Plateau The Nyika Plateau lies in northern Malawi, with a small portion in north eastern Zambia. Most of it lies at

neg: Coteau du Missouri Coteau du Missouri The Coteau du Missouri, or Missouri Plateau, is a large plateau that stretches along the eastern side of the valley of the Missouri River in central North Dakota and north-central South Dakota in the United States. In the Canadian provinces of Saskatchewan and Alberta this physiographic region is classified as the uplands Missouri Coteau, which is a part of the Great Plains Province or Alberta Plateau Region, which extends across the south west corner of the province of Saskatchewan as well as the south east corner of the province of Alberta. Historically, in Canada the area was

neg: Modoc County, California The Clear Lake National Wildlife Refuge and Long Bell State Game Refuge are located on the plateau as well. The Lost River watershed, which later drains into the Klamath River basin, drains the north part of the plateau, while southern watersheds either collect in basin reservoirs or flow into the large Big Sage Reservoir, which sits in the center of the county, which later flows into the Pit River. Below the rim of the Plateau is Big Valley in the extreme southwest corner of the county, and the large Warm Springs Valley that forms the bottom of the Pit River

neg: Shimōsa Plateau accounted for 27%, and tertiary 68%. Tertiary industry on the plateau consists of both the service industry serving the densely populated areas of northern Chiba Prefecture, as well as the extensive logistics network connecting the Keiyō Industrial Zone and Narita International Airport with other areas of Japan. While agriculture accounts for a small part of the overall economy on the Shimōsa Plateau, the northern and eastern area of the plateau is a large producer of vegetables for the Tokyo Metropolitan Region. The flat, eastern part of the Shimōsa Plateau continues to support rice production. Shimōsa Plateau The is a plateau

neg: Allegheny Plateau with relief of up to . The Allegheny Plateau is a physiographic section of the larger Appalachian Plateau province, which in turn is part of the larger Appalachian physiographic division. Allegheny Plateau The Allegheny Plateau , in the United States, is a large dissected plateau area in western and central New York, northern and western Pennsylvania, northern and western West Virginia, and eastern Ohio. It is divided into the unglaciated Allegheny Plateau and the glaciated Allegheny Plateau. The plateau extends southward into western West Virginia, eastern Kentucky and Tennessee where it is instead called the Cumberland Plateau. The plateau terminates

neg: North Atlantic Igneous Province North Atlantic Igneous Province The North Atlantic Igneous Province (NAIP) is a large igneous province in the North Atlantic, centered on Iceland. In the Paleogene, the province formed the Thulean Plateau, a large basaltic lava plain, which extended over at least 1.3 km in area and 6.6 km in volume. The plateau was broken up during the opening of the North Atlantic Ocean leaving remnants existing in Northern Ireland, bits of northwestern Scotland, the Faroe Islands, bits of northwestern Iceland, eastern Greenland and western Norway and many of the islands located in the north eastern portion of the North Atlantic

neg: Waikato (for the north-eastern part of Waikato region) and Taupo, on the Volcanic or Central Plateau (for the south-eastern part of the region). To the west, the region is bounded by the Tasman Sea. The coastal region is largely rough hill country, known locally as the Hakarimata Range, though it is more gently undulating in the north, closer to the mouth of the Waikato River. The coast is punctured by three large natural harbours: Raglan Harbour, Aotea Harbour, and Kawhia Harbour. The area around Raglan is noted for its volcanic black sand beaches and for its fine surfing conditions at Manu

neg: Nechako Region on Thermal oil, Canfor, Houston and Tolko Slave Lake are both getting a reciprocating grate thermal oil system. Another large company is called the Nechako Mechanical Vanderhoof Ltd. They have industrial projects in British Columbia, Alberta, Saskatchewan, and the Yukon. Nechako Mechanical Ltd. has their equipment used by other regions such as Russia, Washington, Oregon, Idaho and California. This company has 6 facilities: Fabrication Plant, Paint Shop, Machine Shop, Millwrighting Shop, their main Office, and of land. Upper Nechako lies within the expansive Nechako Plateau, part of the larger North Central Interior Plateau. The topography of the Nechako Plateau is

neg: Caribbean large igneous province Caribbean large igneous province The Caribbean large igneous province (CLIP) consists of a major flood basalt, which created this large igneous province (LIP). It is the source of the current large eastern Pacific oceanic plateau, of which the Caribbean-Colombian oceanic plateau is the tectonized remnant. The deeper levels of the plateau have been exposed on its margins at the North and South American plates. The volcanism took place between 139 and 69 million years ago, with the majority of activity appearing to lie between 95 and 88 Ma. The plateau volume has been estimated as on the order of 4

neg: Caribbean large igneous province the oldest still active hotspot on Earth. Caribbean large igneous province The Caribbean large igneous province (CLIP) consists of a major flood basalt, which created this large igneous province (LIP). It is the source of the current large eastern Pacific oceanic plateau, of which the Caribbean-Colombian oceanic plateau is the tectonized remnant. The deeper levels of the plateau have been exposed on its margins at the North and South American plates. The volcanism took place between 139 and 69 million years ago, with the majority of activity appearing to lie between 95 and 88 Ma. The plateau volume has been

neg: Central Deccan Plateau Dry Deciduous Forests Central Deccan Plateau Dry Deciduous Forests The Central Deccan Plateau dry deciduous forests southern India, containing large protected areas of natural habitat of the tiger. The Deccan Plateau is a large triangular plateau in southern India, bounded by the Western Ghats range to the west, the Eastern Ghats to the east, and the western Satpura Range to the north. The Central Deccan Plateau dry deciduous forests occupy an area of , in which the dominant natural habitat is or was woodland of "Hardwickia binata" and "Albizia amara" trees, located on the central and southern portion of the plateau. The ecoregion

neg: Irkutsk Oblast is drained by the Angara, which flows north across the province; the outflow rate is controlled by the Irkutsk Dam. The two other major dams on the Irkutsk Oblast's section of the Angara are at Bratsk and Ust-Ilimsk; both forming large reservoirs. The Lena has its source in Irkutsk Oblast as well, and flows north-east into the neighboring Sakha Republic. Irkutsk Oblast consists mostly of the hills and broad valleys of the Central Siberian Plateau and of its eastern extension, the Patom Plateau. The climate varies from warm summer continental in the south to continental-subarctic in the northern part (:

neg: North American Cordillera Columbia Mountains, and the eastern system includes the Canadian Rockies. At its midsection between San Francisco, California and Denver, Colorado, the North American Cordillera is about wide, and its physiographic provinces at this midpoint are as follows, going from west to east: the Pacific Coast Ranges, the Central Valley, the Sierra Nevada, the Basin and Range Province (forming many narrow ranges and valleys), the Colorado Plateau, and the Rocky Mountains. In the United States, another major feature of the Cordillera is the Columbia Plateau, located north of California between the Cascade Range — which is a northern extension of the

neg: Hikurangi Plateau forearc and hence earthquakes such as the 7.8 M 1931 Hawke's Bay earthquake. Hikurangi Plateau The Hikurangi Plateau is an oceanic plateau in the South Pacific Ocean east of the North Island of New Zealand. It is part of a large igneous province (LIP) together with Manihiki and Ontong Java, now located and north of Hikurangi respectively. Mount Hikurangi, in Māori mythology the first part of North Island to emerge from the ocean, gave its name to the plateau. The Hikurangi Plateau covers approximately and reaches below sea level. Hikurangi Plateau is cut by the Hikurangi Channel, a 2000 km

neg: Hikurangi Plateau Hikurangi Plateau The Hikurangi Plateau is an oceanic plateau in the South Pacific Ocean east of the North Island of New Zealand. It is part of a large igneous province (LIP) together with Manihiki and Ontong Java, now located and north of Hikurangi respectively. Mount Hikurangi, in Māori mythology the first part of North Island to emerge from the ocean, gave its name to the plateau. The Hikurangi Plateau covers approximately and reaches below sea level. Hikurangi Plateau is cut by the Hikurangi Channel, a 2000 km abyssal channel that starts at Kaikoura and runs along the Hikurangi Trench as

neg: Geography of Norway the coast, and numerous fjords. The fjords and valleys generally lie in a west–east direction in the southern part of this area, and a more northwest - southeast direction further north. The Saltfjellet mountain range is an exception, as the valleys goes in a more north–south direction from these mountains. This long area comprises many large islands, including Lofoten, Vesterålen and Senja. Far northeast: the interior and the coast east of Nordkapp (corresponding to Finnmarksvidda and eastern Finnmark) is less dominated by mountains, and is mostly below . The interior is dominated by the large Finnmarksvidda plateau. There are large,

neg: Quercus engelmannii winters prevail. The Engelmann oak has a smaller range than most California oaks, and suburban sprawl in the San Gabriel Valley has eliminated the oaks from most of the northern part of the range. The largest remaining stands of Engelmann Oaks are on the Santa Rosa Plateau, near Murrieta in Riverside County, and on Black Mountain near Ramona in San Diego County. Fossil evidence shows that Engelmann oaks once had a wider range, extending through what is now the Mojave and Sonoran deserts into eastern California and Arizona. The Engelmann oak is most closely related to the Arizona white oak

neg: Adamawa Plateau savanna, and is sparsely populated. Cattle raising is the main occupation in the area. The endangered toad "Amietophrynus djohongensis" is only known from the Adamawa Plateau in Cameroon. Adamawa Plateau The Adamawa Plateau () is a plateau region in central Africa stretching from south-eastern Nigeria through north-central Cameroon (Adamawa and North Provinces) to the Central African Republic. The plateau was named after Fulani Muslim leader Modibo Adama. The part of the plateau that lies in Nigeria is more popularly known as Gotel Mountains. The Adamawa Plateau is the source of many waterways, including the Benue River. It is important for

neg: Chota Nagpur Plateau ecoregion, encompasses the plateau. The ecoregion has an area of , covering most of Jharkhand state and adjacent portions of Odisha, West Bengal, Bihar, Chhattisgarh, Uttar Pradesh, and Madhya Pradesh. The ecoregion is drier than surrounding ones, including the Eastern Highlands moist deciduous forests that covers the Eastern Ghats and Satpura Range to the south, and the Lower Gangetic Plains moist deciduous forests in the lowlands to the east and north. The plateau is covered with a variety of various habitats of which Sal forest is predominant. The plateau is home to the Palamau Tiger Reserve and other large blocks

neg: Castlecomer Plateau Castlecomer Plateau The Castlecomer Plateau is an upland area in the North of County Kilkenny, in Ireland, extending into County Laois and County Carlow at its northern edge. The plateau is bounded on the east and south by the R448 regional road, on the west by the N77. The River Nore flows southward past the plateau's western flank, the River Barrow past its eastern flank and it is dissected by the River Dinnin, which flows through Castlecomer itself. The eastern section, which is the larger and more elevated part of the plateau is known as the "Rossmore Plateau", after the

neg: Adamawa Plateau Adamawa Plateau The Adamawa Plateau () is a plateau region in central Africa stretching from south-eastern Nigeria through north-central Cameroon (Adamawa and North Provinces) to the Central African Republic. The plateau was named after Fulani Muslim leader Modibo Adama. The part of the plateau that lies in Nigeria is more popularly known as Gotel Mountains. The Adamawa Plateau is the source of many waterways, including the Benue River. It is important for its deposits of bauxite. The average elevation is about 3,300 feet (1,000 meters), but elevations can reach as high as 8,700 feet (2,650 meters). The vegetation is mostly

neg: Late Antiquity and Medieval sites in Kosovo of the fortress are still preserved. The Novo Brdo fortress is composed by; the Upper Town and the Lower Town, built on the Novo Brdo hill. The Novo Brdo Upper Town, was erected on top of the hill, while below, toward west, the Lower Town stretches in a wide countryside territory. The fortress has access only from the eastern part, whereas from the other parts the hills are steep and inclining toward the walleye. Toward the eastern part, the terrain gradually raises what makes possible to pass to a lower hill in a plateau whereas ruins of a large medieval

neg: Springbrook, Queensland Road and from Numinbah Valley via Pine Creek Road. To the south of Springbrook is the Tweed Range, west is the Numinbah Valley and the Lamington Plateau. Both the Nimmel Range and Tamborine Mountain are to the north, as is Hinze Dam while the peak of Mount Nimmel is at the north eastern tip. The plateau is part of a biodiversity hot spot. It is part of the Scenic Rim Important Birdlife Area. Pademelons are commonly seen by visitors. Springbrook Plateau is the remains of the Tweed Volcano—now known as Mount Warning. The plateau is an undulating elevated patch that

neg: Moldavian Plateau creeks is quite conspicuous, so that the valleys have large terraces and hillocks. The Siret Passage (), ramified in the north with the Moldova Valley, and Suceava Valley cuts the main part of the plateau from the Moldavian Subcarpathians. The Prut Passage cuts the Plateau in half in the north-south direction. The Dniester Passage bounds it from the Podolian Plateau and the Pontic Plain. Its ramification Răut Passage separates the main part of the Moldavian Plateau from the Dniester Hills The Moldavian Plateau comprises several distinct regions: The climate of this plateau is transitional Temperate Continental. Overall, the altitude affects

neg: Wallaby Plateau the plateau was at or above sea level.(Sayers 2002) From the sediment rock samples collected researchers determined that a poorly sorted “ooze” comprises a large part of the seafloor sediments on the Plateau. Wallaby Plateau The Wallaby Plateau, which is also known as the Cuvier Plateau, is a large bathymetric high about west of Carnarvon, Western Australia. The Wallaby Plateau covers approximately and is in water depths of to greater than . In the west, the Wallaby Plateau is separated from the Zenith Plateau by a wide, north to northeast-trending bathymetric trough. "Wallaby Plateau" is the name used by the

neg: Campbell Plateau as a broad, weak flow. The main part of the ACC, however, passes around the Macquarie Ridge together with the SAF and then flows north along the eastern margin of the Campbell Plateau. At 55°S and 50°S the ACC turns eastward again. There is, however, a wind-driven Ekman transport of surface water across the Campbell Plateau. At the Subtropical Convergence the Southland Current rounds the South Island and flows north-east along the island's east coast. From there it entrains Subantarctic and subtropical waters across the north-western Campbell Plateau before branching over the Chatman Rise north of the plateau. Campbell Plateau

neg: Malang parts of Malang have their own characteristics so that they are well-suited for various activities. The southern part of Malang is a large enough plateau that is suitable for industry; the northern part is a fertile highland that is suitable for agriculture; the eastern part is a plateau with a less fertile soil; and the western part is a vast plateau and is now an educational area. Malang City is passed by one of the longest river in Indonesia and the second longest in Java after Bengawan Solo, Brantas River whose the source is located on the slopes of Mount

neg: Walden Ridge War Soldiers) as a signal point toward Lookout Mountain south across the Tennessee River. Being part of the Cumberland Plateau, Walden Ridge is also part of the Appalachian Plateau physiographic province. According to the USGS, variant names of Walden Ridge include Waldens Ridge, Walldenns Ridge, Wallens Ridge, Walden's Ridge, and Walden Ridge Plateau. Walden Ridge Walden Ridge (or Walden's Ridge) is a mountain ridge and escarpment located in Tennessee, in the United States. It marks the eastern edge of the Cumberland Plateau and is generally considered part of it. Walden Ridge is about long, running generally north-south. Its highest point

neg: Deccan Plateau Deccan Plateau The Deccan Plateau is a large plateau in western and southern India. It rises to in the north, and to more than in the south, forming a raised triangle within the South-pointing triangle of the Indian subcontinent's coastline. It extends over eight Indian states and encompasses a wide range of habitats, covering most of central and southern India. The plateau is located between two mountain ranges, the Western Ghats and the Eastern Ghats, each of which rises from its respective nearby coastal plain, and almost converge at the southern tip of India. It is separated from the Gangetic

neg: California Plateau University of California which have sent numerous researchers to work in Antarctica. California Plateau California Plateau () is an undulating ice-covered plateau, long and from wide, which rises to at the eastern side of Scott Glacier. The plateau reaches a maximum height of in Mount Blackburn at the southern end. The northwestern side of the plateau is marked by the steep rock cliffs of Watson Escarpment; the southeastern side grades gradually to the elevation of the interior ice. It was mapped by the United States Geological Survey from ground surveys and from U.S. Navy aerial photography, 1960–64, and named by

neg: Columbia Plateau Columbia Plateau The Columbia Plateau or Columbia Basin is a geographic region located almost entirely in Eastern Washington and north-central Oregon—with the eastern edge spilling over into Northern Idaho The area is characterized by its mostly semi-arid climate ("Bsk" under the Köppen classification)—with some areas falling under the desert ("BWk") and mediterranean ("Csa" and "Csb") classifications—resulting in a shrub-steppe environment. During late Miocene and early Pliocene times, a flood basalt engulfed about of the Pacific Northwest, forming a large igneous province. Over a period of perhaps 10 to 15 million years, lava flow after lava flow poured out, ultimately accumulating

neg: Zambia November to April). The flood dominates the natural environment and the lives, society and culture of the inhabitants and those of other smaller, floodplains throughout the country. In Eastern Zambia the plateau which extends between the Zambezi and Lake Tanganyika valleys is tilted upwards to the north, and so rises imperceptibly from about in the south to in the centre, reaching in the north near Mbala. These plateau areas of northern Zambia have been categorised by the World Wildlife Fund as a large section of the Central Zambezian Miombo woodlands ecoregion. Eastern Zambia shows great diversity. The Luangwa Valley splits

neg: East African Plateau great valley (occupied by Lake Nyasa, or Lake Malawi), the southern part of which is less distinct due to rifting and subsidence than the rest of the system. East African Plateau East African Plateau is a huge plateau in the eastern part of central Africa in Kenya, Tanzania and Uganda. Its elevation is mostly between 1000 and 1500 metres. It is subdivided into a number of zones running north and south and consisting in turn of mountain ranges, tablelands and hollows. The most striking feature is the existence of two great lines of hollows, due largely to the subsidence of

neg: Chota Nagpur Plateau The area is also referred to as Western Ranchi Plateau. It is believed to be composed of Deccan lava. It is the largest part of the Chhota Nagpur Plateau. The elevation of the plateau land in this part is about and gradually slopes down towards south-east into the hilly and undulating region of Singhbhum (earlier Singhbhum district or what is now Kolhan division). The plateau is highly dissected. Damodar River originates here and flows through a rift valley. To the north it is separated from the Hazaribagh plateau by the Damodar trough. To the west is a group of plateaux

neg: Modoc Plateau forests, and seasonal lakes. The plateau is thought to have been formed approximately 25 million years ago. Forested areas of the plateau include Ponderosa Pine ("Pinus ponderosa"), as well as other tree species such as California Buckeye ("Aesculus californica"). and Modoc Cypress ("Cupressus bakeri"). The plateau supports large herds of Mule Deer ("Odocoileus hemionus"), Rocky Mountain Elk ("Cervus canadensis"), and Pronghorn ("Antilocapra americana"). There are also several herds of wild horses on the plateau. The Clear Lake National Wildlife Refuge and Long Bell State Game Refuge are located on the plateau as well. The Lost River watershed drains the north

neg: Pothohar Plateau Pothohar Plateau The Pothohar Plateau (, ; alternatively spelled Potohar or Potwar) is a plateau in north-eastern Pakistan, forming the northern part of Punjab. It borders the western parts of Azad Kashmir and the southern part of Khyber Pakhtunkhwa. The region was once the home of the ancient Soanian culture, which is evidenced by the discovery of fossils, tools, coins, and remains of ancient archaeological sites. The major language of the region is Pothwari, while the standard Majhi dialect of Punjabi and Hindko are also spoken. Other dialects include Dhani diaelect, Shahpuri and Chacchi. Potohar is home to many different

neg: Arden Way (Sacramento, California) turns east, leaving the city of Sacramento and into the unincorporated community of Arden-Arcade. The unusually large overpass between Evergreen and Harvard Streets was to have been part of the I-80 freeway replacement of what is now the Capital City Freeway (or Business 80). Caltrans abandoned the project in the early 1980s and was turned over to Regional Transit for their light rail system. After leaving Sacramento, Arden Way immediately intersects Howe Avenue, another major thoroughfare running north-south. It continues east to intersect with other north-south major thoroughfares, including Fulton Avenue, Watt Avenue and Eastern Avenue. As Arden Way meets

neg: North American Cordillera Okanagan Highland is described as being a hilly plateau, and is located in southern British Columbia and northern Washington. The Interior Plateau also includes the Quesnel Highland, Fraser Plateau, Nechako Plateau, and McGregor Plateau. California's Central Valley is a large, flat valley that dominates the central portion of California, stretching inland and parallel to the Pacific Ocean coast. Its northern half is referred to as the Sacramento Valley, and its southern half as the San Joaquin Valley. The two halves meet at the huge Sacramento-San Joaquin River Delta of the Sacramento and San Joaquin Rivers, which along with their tributaries

neg: Kerguelen Plateau whales including sperm, minke, and humpback whales along the southern end of the Kerguelen Plateau and the northern part of the adjacent Princess Elizabeth Trough. These whales choose this location for foraging because the Southern Front of the Antarctic Circumpolar Current is steered off by the plateau — resulting in a poleward extent for the Southern Front only found near the Kerguelen Plateau. This brings shoaled, nutrient-rich Upper Circumpolar Deep Water to the surface which brings macronutrients to the surface. Ice is additionally advected north along the eastern side of the plateau. Kerguelen Plateau The Kerguelen Plateau (, ) is

neg: Allegheny Plateau Allegheny Plateau The Allegheny Plateau , in the United States, is a large dissected plateau area in western and central New York, northern and western Pennsylvania, northern and western West Virginia, and eastern Ohio. It is divided into the unglaciated Allegheny Plateau and the glaciated Allegheny Plateau. The plateau extends southward into western West Virginia, eastern Kentucky and Tennessee where it is instead called the Cumberland Plateau. The plateau terminates in the east at the Allegheny Mountains, which are the highest ridges just west of the Allegheny Front. The Front extends from central Pennsylvania through Maryland and into eastern West

neg: Jharkhand His widow, Suman Mahato, the Jharkhand Mukti Morcha candidate, won the Jamshedpur Lok Sabha by-election in September 2007 and served in parliament until 2009. Jharkhand is located in the eastern part of India and is enclosed by Bihar to the northern side, Chhattisgarh and Uttar Pradesh to the western side, Odisha to the southern part and West Bengal to the eastern part. Jharkhand envelops a geographical area of 79.70 lakh hectare. Much of Jharkhand lies on the Chota Nagpur Plateau. Many rivers pass through the Chota Nagpur plateau. They are: Damodar, North Koel, South Koel, Sankh, Brahmani and Subarnarekha rivers.

neg: California Plateau California Plateau California Plateau () is an undulating ice-covered plateau, long and from wide, which rises to at the eastern side of Scott Glacier. The plateau reaches a maximum height of in Mount Blackburn at the southern end. The northwestern side of the plateau is marked by the steep rock cliffs of Watson Escarpment; the southeastern side grades gradually to the elevation of the interior ice. It was mapped by the United States Geological Survey from ground surveys and from U.S. Navy aerial photography, 1960–64, and named by the Advisory Committee on Antarctic Names for the several branches of the

neg: Chota Nagpur Plateau Chota Nagpur Plateau The Chhota Nagpur Plateau is a plateau in eastern India, which covers much of Jharkhand state as well as adjacent parts of Odisha, West Bengal, Bihar and Chhattisgarh. The Indo-Gangetic plain lies to the north and east of the plateau, and the basin of the Mahanadi River lies to the south. The total area of the Chota Nagpur Plateau is approximately . The name "Nagpur" is probably taken from Nagavanshis, who ruled in this part of the country. "Chhota" (="small" in Hindi and Urdu) is also the name of a village in the outskirts of Ranchi, which

neg: Kaibab Plateau Kaibab Plateau The Kaibab Plateau is located in northern Arizona in the United States. The plateau, part of the larger Colorado Plateau, is bordered on the south by the Grand Canyon and reaches an elevation of 9200 feet (2817 m) above sea level. The plateau is divided between Kaibab National Forest and the "North Rim" portion of Grand Canyon National Park. Tributary canyons of the Colorado River form the plateau's eastern and western boundaries, and tiers of uplifted cliffs define the northern edges of the land form. Winter snowfall is often heavy (sometimes exceeding ), and this creates opportunities for

neg: High Desert (Oregon) for its generally high elevation, averaging about across the region. It is bordered by the eastern foothills of the Cascade Range to the west. The Blue Mountains are the geographical boundary to the north, marking the northern end of the high desert's semi-arid plateau. The southern high desert is part of North America's Basin and Range Province, which extends south through Nevada and Arizona and into Mexico. It contains large alkali lakes and tall cliffs, some with a prominence of more than . Steens Mountain, in Harney County, is the highest point within the region; its summit is above sea

neg: California Current California Current The California Current is a Pacific Ocean current that moves southward along the western coast of North America, beginning off southern British Columbia and ending off southern Baja California Peninsula. It is considered an Eastern boundary current due to the influence of the North American coastline on its course. It is also one of five major coastal currents affiliated with strong upwelling zones, the others being the Humboldt Current, the Canary Current, the Benguela Current, and the Somali Current. The California Current is part of the North Pacific Gyre, a large swirling current that occupies the northern basin

neg: Western Allegheny Plateau (ecoregion) Western Allegheny Plateau (ecoregion) The Western Allegheny Plateau is an ecoregion of the Temperate broadleaf and mixed forests Biome, located on the western Allegheny Plateau and in the Appalachia region of the Eastern United States. The Western Allegheny Plateau ecoregion is located on the western Allegheny Plateau, which is within the central region of the Appalachian Plateau. The World Wildlife Fund defines the ecoregion as being the northern part of the Appalachian mixed mesophytic forests. The Environmental Protection Agency defines it as running from west-central Pennsylvania, east-central and south Ohio, north and northwest West Virginia, and a portion of northeast

neg: Pernambuco Atlantic Ocean, 535 km northeast of Recife, has been part of Pernambuco since 1988. The rivers of the state include a number of small plateau streams flowing southward to the São Francisco River, and several large streams in the eastern part flowing eastward to the Atlantic. The former are the Moxotó, Ema, Pajeú, Terra Nova, Brigida, Boa Vista and Pontai, and are dry channels the greater part of the year. The largest of the coastal rivers are the Goiana River, which is formed by the confluence of the Tracunhaem and Capibaribe-mirim, and drains a rich agricultural region in the north-east

neg: Florești District of Independence of Moldova, part of the Soroca County (1991–2003), and in 2003 became administrative unit of Moldova. Floresti district (http://floresti.md) is located in north-eastern part of Moldova and is bordered to the north Soroca District, north-west Drochia District, Telenesti District to the south, east to Camenca District, south-east Soldanesti District and west with Singerei District. Landscape is fragmented in Nistru Plateau, and less in Balti steppe in the west. Soil consists of chernozem, cambisol, alluvial soil and arenosol. Maximum altitude is 289 m Nistru plateau. District climate is temperate-continental. The average temperature in July is 20–20.5 °C, and in

neg: North German Plain are found the oldest settlement locations in Germany (Linear Pottery culture). The north eastern part of the plain (Young Drift) is geomorphologically distinct and contains a multitude of lakes (e.g. the Mueritz lake in the Mecklenburg Lake Plateau) which are vestiges of the last ice age. The retreating glaciers left this landscape behind around 16,000 to 13,000 years ago. In comparison, the dry plains of northwestern Germany (Lower Saxony, western Schleswig-Holstein and the Bochum area of North Rhine Westphalia) are more heavily weathered and levelled (Old Drift) as the last large scale glaciations here occurred at least 130,000 years ago.

neg: Bernese Alps This makes a large difference between the south, where the lateral short valleys descend abruptly into the deep trench forming the valley of the Rhône and the north, where the Bernese Alps extends through a great part of the canton of Bern (Bernese Oberland), throwing out branches to the west into the adjoining cantons of Vaud and Fribourg. There the mountains progressively become lower and disappear into the hilly Swiss Plateau. The main chain west of Gemmi Pass consists mainly of a few large prominent summits (as the Wildhorn) slightly above , generally covered by glaciers. On the eastern part,

neg: Norwood, Tasmania Norwood, Tasmania Norwood is a suburb 3 kilometers southeast of the Launceston CBD. The minor suburb of Queechy is also included as part of Norwood. The area was opened up for development in the 1960s with considerable growth in the 1970s to 1980s and contains a mix of large, older-style family homes with patches of more modern homes, mostly in the central-eastern portion of the suburb. Norwood is located on a 60-80m high, relatively flat-topped alluvial plateau with the valley of the North Esk River to the east, the Punchbowl Reserve to the north and the Carr Villa Flora Reserve,

neg: Mid-Pacific Mountains hotspot chain, a lineament that include the Line Islands and Tuamotu archipelago, begins near the eastern part of the MPM. The formation of the MPM thus probably occurred at the Pacific-Farallon Ridge and the Easter hotspot, or where the Easter Microplate is now located. Mid-Pacific Mountains The Mid-Pacific Mountains (MPM) is a large oceanic plateau located in the central North Pacific Ocean or south of the Hawaiian–Emperor seamount chain. Of volcanic origin and Mesozoic in age, it is located on the oldest part of the Pacific Plate and rises up to (Darwin Rise) above the surrounding ocean floor and is

neg: Tibetan Plateau the Dangjin pass on the Dunhuang-Golmud road. To the west are short ranges called the Danghe, Yema, Shule, and Tulai Nanshans. The easternmost range is the Qilian Mountains. The line of mountains continues east of the plateau as the Qinling, which separates the Ordos Plateau from Sichuan. North of the mountains runs the Gansu or Hexi Corridor which was the main silk-road route from China proper to the West. The plateau is a high-altitude arid steppe interspersed with mountain ranges and large brackish lakes. Annual precipitation ranges from and falls mainly as hail. The southern and eastern edges of the

neg: House Mountain (Knox County, Tennessee) and east, the Cumberland Plateau is visible to the west, and Powell Mountain and Clinch Mountain are visible to the north and northeast. The origin of the mountain's name is unknown, though a local legend suggests early settlers thought the mountain was shaped like the roof of a house. House Mountain rises from a large plain in eastern Knox County, about southwest of the southern terminus of Clinch Mountain and immediately north of McAnnally Ridge. House, McAnnally, and Clinch are all part of the Appalachian Ridge-and-Valley Province, which consists of a series of narrow, elongate ridges stretching in a northeast-to-southwest

neg: Great Papuan Plateau Great Papuan Plateau The Great Papuan Plateau is a karst plateau in the Southern Highlands and Western Provinces of Papua New Guinea. It is bordered the upper stretches of the Kikori River and the Strickland River on the east and west, respectively, and the Karius Range, the southern edge of the highlands, including Mount Sisa, to the north, and Mount Bosavi to the south. The eastern part of the plateau, east of the Sioa River, covers about and had a sparse population of 2,100 people (1966 government census), speaking at least five different languages. The dominant ethnic groups of this

neg: Portales, New Mexico affordability, and low taxes. Clovis Man inhabited the Blackwater Draw area north of Portales until 11,000 years ago. Seminomadic non-Pueblo Southern Athabaskan groups (Apache, Navajo) occupied much of the area as early as the 13th century. In the early 18th century, the Comanche displaced the Apache, who had previously lived in this region. The Comanche commanded the area until late in the 19th century. The surrounding area of eastern New Mexico is part of what came to be known in the colonial period during Spanish rule as the "Llano Estacado", an arid and treeless plateau bounded on the north and

neg: Black Mountains (North Carolina) prominently above the surrounding lower terrain. This is particularly noticeable from the range's eastern side, which rises over 4500 feet (1375 meters) above the Catawba River Valley and Interstate 40, providing some impressive mountain scenery. The Black Mountains consist primarily of Precambrian gneiss and schists formed over a billion years ago from primordial sea sediments. The mountains themselves were formed roughly 200-400 million years ago during the Alleghenian orogeny, when the collision of two continental plates thrust what is now the Appalachian Mountains upward to form a large plateau. Weathering and minor geologic events in subsequent periods carved out the

neg: Arizona/New Mexico Mountains ecoregion Arizona/New Mexico Mountains ecoregion The Arizona/New Mexico Mountains ecoregion is a Level III ecoregion designated by the United States Environmental Protection Agency (EPA) in the U.S. states of Arizona and New Mexico. The region is a transition region from the lower elevation Sonoran Desert (81) to the southwest and Chihuahuan Desert (24) southeast; the west is bordered by the mid elevation Mojave Desert (14). The north is bordered by the east-west "Arizona/New Mexico Plateau" (22), ecoregion which is part of and is the southern region of the Colorado Plateau. The north region of the Colorado Plateau covers eastern Utah/western Colorado

neg: Mashonaland of Harare was given its own provincial status as well. Since the constitutional amendments that took effect in 1988, each is run by a governor appointed by the president. The territory is composed of a broad plateau that slopes gradually to the north and north-west. The lowest land is on its northern border, which is formed by the Zambezi River, with Zambia beyond. A small part straddles the plateau at its south-eastern edge and here the land drains into the Save River but the rest of Mashonaland is part of the Zambezi drainage basin. To the south, the Munyati River

neg: Solca the central-eastern part of Suceava County, at the foot of the eastern part of Obcina Mare Mountains, in Solca-Cacica Depression. The town is situated at the border of Suceava Plateau and the Eastern Carpathians, at an average altitude of 522 metres. Solca River crosses the town. Solca is a place known for the beauty of the natural landscape and the high quality of its air. Solca borders with the following communes: Marginea (in north-west), Arbore (in north and north-east), Poieni-Solca (in south and south-east), Cacica (in south) and Mănăstirea Humorului (in west). The town is situated at a distance of

neg: North Shore (Sydney) Shore. Cumberland County mapping from 1792 to 1894 indicate that the four local governments that stand today were derived from one: the Parish of Willoughby. From the Parish of Willoughby came the City of Willoughby and the municipalities of Mosman, Lane Cove and North Sydney. North Sydney was formerly known as St. Leonards. Most of the North Shore suburbs are part of the Hawkesbury Plateau, a large sandstone plateau overlaid by a system of ridges and gullies. The Plateau begins north of the Port Jackson and runs up until the Hawkesbury River. Thus much of the North Shore is hilly

neg: Physiographic province Physiographic province A physiographic province is a geographic region with a characteristic geomorphology, and often specific subsurface rock type or structural elements. The continents are subdivided into various physiographic provinces, each having a specific character, relief, and environment which contributes to its uniqueness. The physiographic provinces are then subdivided into smaller physiographic sections. In eastern North America, the Atlantic Coastal Plain, Piedmont, Blue Ridge Mountains, Ridge-and-Valley Appalachians, and Appalachian Plateau are specific physiographic provinces. In the Western United States of western North America: the Basin and Range Province, Cascade Range, Colorado Plateau, Rio Grande rift, Great Basin, Central Valley (California),

neg: East African Plateau East African Plateau East African Plateau is a huge plateau in the eastern part of central Africa in Kenya, Tanzania and Uganda. Its elevation is mostly between 1000 and 1500 metres. It is subdivided into a number of zones running north and south and consisting in turn of mountain ranges, tablelands and hollows. The most striking feature is the existence of two great lines of hollows, due largely to the subsidence of whole segments of the Earth's crust, the lowest parts of which are occupied by vast lakes. Towards the south the two lines converge and give place to one

neg: North Asia by Eurasian Plate, except for its eastern part which lies on North American, Amurian and Okhotsk Plate. It is divided by three major plains: the West Siberian Plain, Central Siberian Plateau and Verhoyansk-Chukotka collision zone. The Uralian orogeny in the west raised Ural Mountains, the informal boundary between Europe and Asia. Tectonic and volcanic activities are frequently occurred in the eastern part of the region as part of the Ring of Fire, evidenced by the formation of island arc such as Kuril Islands and ultra-prominent peaks such as Klyuchevskaya Sopka, Kronotsky and Koryaksky. The central part of North Asia is

neg: Scenic Rim Scenic Rim The Scenic Rim is a group of forested mountain ranges of the Great Dividing Range straddling the border between south-eastern Queensland and north-eastern New South Wales, Australia. The mountainous landscape forms a quarter circle ridge positioned roughly from south of Toowoomba around to Springbrook. Tamborine Mountain, Lever's Plateau and the Lamington Plateau are part of the rim formation. The scenic rim is considered part of the Gold Coast hinterland. Parts of the rim are well developed, crossed by highways with facilities for tourists like Cunninghams Gap, others are privately owned agricultural properties and rural villages such as Beechmont

neg: Nauen Plateau of Havelland. That said, the river country of the Havelland extends beyond the plateau to include the Havel valley and other lowland areas. The Nauen Plateau lies in the central Mark and in the extreme west of the state of Berlin. Its northern boundary is formed by a glacial meltwater valley, the Berlin Urstromtal, and by the former marshlands of the Havelland Luch, now part of the West Havelland Nature Park. North of the "luch" is the smaller ridge of "Ländchen Glien". The Plateau's eastern boundary is formed by the Berlin-Potsdam chain of Havelsee lakes, which separates the Nauen Plateau

neg: Corregidor Middleside is a small plateau that interrupts the upward slope from Bottomside to Topside, and was the location of 2-story officers' quarters, barracks for the enlisted men, a hospital, quarters for non-commissioned officers, a service club, PX, and two schoolhouses—one for the children of Filipino soldiers and the other for American children. Bottomside is the lower part of the island and is the neck that connects the tail and head of the island. South of Bottomside was "Barangay or Barrio" San José (near what was Navy Beach); on the north is what was Army Dock, with its three large piers,

neg: North Alabama Alabama are low upland, the eastern regions part of the Cumberland Plateau, marked by tablelands incised with gorges, some of them, such as Little River Canyon in DeKalb County, of considerable depth. The northern areas of Alabama contain a wide variety of industrial, manufacturing, and high-tech corporations with both large and small operations. Each of the three economic centers in the region (Huntsville, Decatur, and Florence) have a distinct type of economic base. The Huntsville area is mostly dominated by high-tech industries and federal operations such as Boeing and NASA. The Decatur area, in the central part of the region,

neg: Baugh Fell over a mile from the summit. There are five small lakes or tarns, called the East Tarns, grouped together on the eastern part of the plateau just to the north of the summit of Tarn Rigg Hill. The West Tarn, meanwhile, lies at the north-western end of the summit plateau at , and is difficult to find on the almost flat top because it nestles in a slight hollow, even though it can be seen from the trig point. It may be located from the latter by following the western rim of the plateau, overlooking Sedbergh, until two cairns point

neg: Kenn Reef 500 km to the southwest. Kenn Reef is part of a submerged continental block, called the Kenn Plateau. The Kenn Plateau lies off the north eastern Australian coast and is a region characterised by a series of prominent, bathymetric troughs and marginal plateaux. And is submerged by 1000 m to over 3000 m of water. The Kenn Plateau, covers around 100,000 km², an area larger than the Tasmanian landmass. Various islands and reefs, whose origin is thought to be related to the Tasmantid Seamount Chain, lie along the western margin of the Kenn Plateau and include the well known Kenn

neg: China Flat (Santa Monica Mountains) China Flat (Santa Monica Mountains) China Flat is a plateau in the north−central Simi Hills, in Ventura County, Southern California. The plateau sits at a elevation and is situated just below Simi Peak, which is the highest point in the Simi Hills. The plateau averages around in elevation. It features native oak woodlands and chaparral habitats, with large sandstone outcroppings. It is protected within Cheeseboro Canyon / Palo Comado Canyon Open Space park of the Santa Monica Mountains National Recreation Area. The area is located between the cities of Oak Park, Thousand Oaks and Simi Valley. Trails reach China Flat

neg: Central U.S. hardwood forests Central U.S. hardwood forests The central U.S. hardwood forests comprise a temperate broadleaf and mixed forests ecoregion in the Eastern United States, as defined by the World Wildlife Fund. It has one of the most diverse herbaceous plant floras of ecoregions in North America. This is a large region, mainly of rolling plain except for the Ozark plateau and other smaller areas of plateau and basin in Kentucky and Tennessee. The region contains the large system of sandstone caves in Mammoth Cave National Park. The region was designated by the World Wide Fund for Nature (WWF) and is a fraction

neg: Dobrogea Plateau Dobrogea Plateau The Dobrogea Plateau (Romanian: "Podişul Dobrogei") is a plateau in Eastern Romania located in the Dobruja region, surrounded to the north and west by the Danube and to the east by the Danube Delta and the Black Sea. Its average altitude is around 200–300 metres, higher in the northern part. The highest point is the Ţuţuiatu/Greci Peak in the Măcin Mountains, at a height of 467 m. The climate is slightly warmer and more arid than in the rest of Romania and as such, its flora and flora contains some Mediterranean species. The Casimcea River and Taița River

neg: Phu Kradueng can be heard in the area of the mountain. Phu Kradueng seen from above is heart-shaped. It has a relatively flat plain on its top, sloping slightly to the north. The summit, in the southwestern part of the plateau, is inconspicuous. The western, southern, and eastern edges of the mountain have a fairly regular shape and are formed by abrupt sandstone cliffs, while the northwestern corner is deeply indented, containing a number of streams and seasonal waterfalls. Geologically, Phu Kradueng is formed by Jurassic and Cretaceous sandstone. Large parts of the mountain are covered in mixed evergreen forest. At the

neg: China Flat (Santa Monica Mountains) from trailheads in the Conejo Valley, Simi Valley, and via Upper Las Virgenes Canyon Open Space Preserve (Ahmanson Ranch) from Calabasas and the San Fernando Valley. The trail to the summit of Simi Peak (2403 ft.) passes through China Flat. China Flat (Santa Monica Mountains) China Flat is a plateau in the north−central Simi Hills, in Ventura County, Southern California. The plateau sits at a elevation and is situated just below Simi Peak, which is the highest point in the Simi Hills. The plateau averages around in elevation. It features native oak woodlands and chaparral habitats, with large sandstone outcroppings.

neg: North Dakota the Badlands. The region is abundant in fossil fuels including natural gas, crude oil and lignite coal. The Missouri River forms Lake Sakakawea, the third largest artificial lake in the United States, behind the Garrison Dam. The central region of the state is divided into the Drift Prairie and the Missouri Plateau. The eastern part of the state consists of the flat Red River Valley, the bottom of glacial Lake Agassiz. Its fertile soil, drained by the meandering Red River flowing northward into Lake Winnipeg, supports a large agriculture industry. Devils Lake, the largest natural lake in the state, is

neg: North American Cordillera and Utah, bisected by the Colorado River which flows westward through the southern part, and the Green River which flows south from the northernmost part of the plateau. The Green is a tributary of the Colorado, the confluence being west of Moab, Utah in Canyonlands National Park. The Mexican Plateau is one of six distinct physiographic sections of the Basin and Range Province, which in turn is part of the Intermontane Plateaus physiographic division. It is a large arid-to-semiarid plateau that occupies much of northern and central Mexico. Averaging above sea level, it extends from the United States border in

neg: Dobrogea Plateau flow through it from west to east. There are several lakes, including some lagoons, the most important being Oltina Lake, Bugeac Lake, Mangalia Lake, Techirghiol Lake, Siutghiol Lake, Taşaul Lake, and Razim Lake. Its main subdivisions are: Dobrogea Plateau The Dobrogea Plateau (Romanian: "Podişul Dobrogei") is a plateau in Eastern Romania located in the Dobruja region, surrounded to the north and west by the Danube and to the east by the Danube Delta and the Black Sea. Its average altitude is around 200–300 metres, higher in the northern part. The highest point is the Ţuţuiatu/Greci Peak in the Măcin Mountains,

neg: Aintab plateau Nur Mountains and Sof (Qarṭal) Mountains. The river ʼAswad (Kara-su) runs in the southern half of the valley. Aintab plateau slopes up in south-north and southeast-northwest direction. The eastern part of the plateau is occupied by the vast plains of Tall Bashar (Oğuzeli), Yavuzeli, and Araban in Gaziantep Province. The western part holds the Sof mountain (1,496 m) and Karadağ mountain (1,081 m). The Alleben and Sajur rivers rise from Sof Mountain and flow southeast to the Euphrates across the plain of Tall Bashar. The Nizip Stream rises from Nizip and joins the Euphrates near the city. The Merzimen (Bozatlı)

neg: South American–Antarctic Ridge in the Mid- to Late Jurassic in what is today the Mozambique Basin east of Africa, whereas the South American and African plates started to brake apart during the Early Cretaceous. Between these events neither the Mid-Atlantic Ridge nor the Bouvet Triple Junction existed and the SAAR formed a continuous ridge together with the Southwest Indian Ridge. Around 106 Ma the eastern end of the Falkland Plateau separated from the Agulhas Bank, opening the South Atlantic which, however, remained an enclosed basin north of the Falkland Plateau until 85–83 Ma. Around 97 Ma the Northeast Georgia Rise (today north of

neg: Shumen fortress within the Shumen Plateau Nature Park. From the entrance of the fortress, about away is the "Creators of the Bulgarian State" Monument erected in 1981 during the communist regime to commemorate the 1300th anniversary of the Bulgarian state. An information center is away from this monument and a track from here leads to the fortress. The fortress represents a substantial part of the history of Bulgaria. The Ancient Bulgars, semi-nomadic warrior tribes of Turkic peoples, not to be confused with Turkish, arrived in what is in now north-eastern Bulgaria to the south of the Danube in the late 7th century

neg: White Plains (Cookeville, Tennessee) (1813–1892), built the White Plains house sometime around 1848, and in the late 1950s Harvey Draper bought the house and made numerous renovations. White Plains is located on the eastern Highland Rim, a plateau-like upland between the higher Cumberland Plateau to the east and the lower Nashville Basin to the west. The western escarpments of the Cumberland Plateau, known locally as "Algood Mountain" and "Buck Mountain," rise about a mile to the east. The house stands along Old Walton Road just outside the municipal boundary of Algood. What is now White Plains was part of Cherokee lands ceded to the

neg: Penhill Penhill Penhill (526 metres high at the trig point, 553 metres at Height of Hazely) is a prominent hill in the Pennines in North Yorkshire, England. It forms a ridge that commands the southern side of Wensleydale and the northern side of Coverdale. Its concave shape was formed during the last ice age, when glaciers carved Wensleydale into a U-shape. The summit plateau has a trig point, small tarns on the peat moor, and, visible from the valley floor, a beacon at its eastern end, part of the large network built to warn of a Spanish invasion. Penhill is accessed

neg: East Agoura, Agoura Hills, California East Agoura, Agoura Hills, California East Agoura is a district on the eastern side of the city of Agoura Hills, located on the city's, in western Los Angeles County, California. The city of Oak Park is on the north East Agoura is the most dense of the suburban city's districts, as the area contains a mix of apartment buildings and large offices as a result of construction in the 1990s. This district is located immediately south of the residential and more rural Old Agoura, and it is sometimes referred to as part of Old Agoura as both are north of

neg: Ordos Plateau desert) and is part of Inner Mongolia. Because of its low and variable rainfall the region was once notorious for drought and famine. At the southwest corner near where the Yellow River emerges from the Tibetan Plateau is Lanzhou, the westernmost large city in north China and the capital of Gansu. To the west of Lanzhou is Xining from whence caravans (and now the railway) started for Lhasa. North of Xining the Gansu or Hexi Corridor runs along the northern edge of the Tibetan Plateau. This corridor and the Wei River valley became the main silk road route from China

neg: Carnarvon Range Carnarvon Range The Carnarvon Range is a mountain range in Central Queensland, Australia. It is a plateau section of the Great Dividing Range. The Carnarvon Range is 160 km in length. It was first explored by Ludwig Leichhardt but named by Thomas Mitchell after the 4th Earl of Carnarvon. North eastern parts of the range have formed a plateau known as the Consuelo Tableland. The plateau contains Aboriginal paintings and sandstone gorges, including the Carnarvon Gorge. Part of the range is protected within the Carnarvon National Park. The range marks the northernmost limits of the Murray-Darling Basin and is the

neg: Geography of Syria This is part of the Harrat ash Shaam volcanic field that stretches all the way to Saudi Arabia. Northeast of Jabal al-Druze is a large lava field called Al-Safa that stands out in satellite views. The entire eastern plateau region is intersected by a low chain of mountains, the Jabal ar Ruwaq, the Jabal Abu Rujmayn, and the Jebel Bishri, extending northeastward from the Jabal Al Arab to the Euphrates. South of these mountains lies a barren desert region known as the Hamad. North of the Jabal ar Ruwaq and east of the city of Homs is another barren area

neg: Krucze Mountains Krucze Mountains The Krucze Mountains (, German: "Rabengebirge" ) are the Eastern part of the Stone Mountains, which belong to the Central Sudetes on the border of the Czech Republic and Poland. To the West and North-Western part the mountain range borders the Lubawska Plateau and the Karkonosze Mountains, to the North-Eastern part they border the mountain range Czarny Las, from the East they border the sediment basin Kotlina Krzeszowska and the Zawory mountain range and to the South the mountain range borders the Czech part of the Stołowe Mountains. To the Southern ridge of mountain range is the Polish-Czech

neg: Appalachian Mountains extension of the Laurentian Mountains of Canada. In addition to the true folded mountains, known as the ridge and valley province, the area of dissected plateau to the north and west of the mountains is usually grouped with the Appalachians. This includes the Catskill Mountains of southeastern New York, the Poconos in Pennsylvania, and the Allegheny Plateau of southwestern New York, western Pennsylvania, eastern Ohio and northern West Virginia. This same plateau is known as the Cumberland Plateau in southern West Virginia, eastern Kentucky, western Virginia, eastern Tennessee, and northern Alabama. The dissected plateau area, while not actually made up

neg: Eastern Thailand Eastern Thailand Eastern Thailand is a region of Thailand bordering Cambodia on the east, Northeastern Thailand in the north, and central Thailand on the west. Eastern Thailand lies between the Sankamphaeng Range, which forms a natural border with the Khorat Plateau to the north and the Gulf of Thailand to the south. The geography of the region is characterised by short mountain ranges alternating with small basins of short rivers which drain into the Gulf of Thailand. Fruit is a major component of agriculture in the area, and tourism plays a strong part in the economy. The region's coastal location

neg: Indigenous peoples of the Northwest Plateau Indigenous peoples of the Northwest Plateau Indigenous peoples of the Northwest Plateau, also referred to by the phrase Indigenous peoples of the Plateau, and historically called the Plateau Indians (though comprising many groups) are indigenous peoples of the Interior of British Columbia, Canada, and the non-coastal regions of the United States Pacific Northwest states. Their territories are located in the inland portions of the basins of the Columbia and Fraser Rivers. These tribes live in parts of the Central and Southern Interior of British Columbia, northern Idaho, western Montana, eastern Washington, eastern Oregon, and northeastern California. The eastern flank of

neg: Siberia (continent) Siberia (continent) Siberia, also known as Angaraland (or simply Angara) and Angarida, is an ancient craton located in the heart of Siberia. Today forming the Central Siberian Plateau, it formed an independent continent before the Permian period. Angaraland was named in the 1880s by Austrian geologist Eduard Suess who erroneously believed that in the Paleozoic there were two large continents in the Northern Hemisphere: "Atlantis", North America connected to Europe by a peninsula (=Greenland and Iceland); and "Angara-land", eastern Asia, named after the Angara River in Siberia. About 2.5 billion years ago (Siderian), Siberia was part of a continent of

neg: Eastern Hills, Bogotá Eastern Hills, Bogotá The Eastern Hills (Spanish: "Cerros Orientales") are a chain of hills forming the eastern natural boundary of the Colombian capital Bogotá. They are part of the Altiplano Cundiboyacense, the high plateau of the Eastern Ranges of the Colombian Andes. The Eastern Hills are bordered by the Chingaza National Natural Park to the east, the Bogotá savanna to the west and north, and the Sumapaz Páramo to the south. The north-northeast to south-southwest trending mountain chain is long and its width varies from . The highest hilltops rise to over the western flatlands at . The Torca River