Sarmila/GeoWiki-Features huggingface dataset:
Confucius Temple (Grand Canyon). Confucius Temple is a summit located in the Grand Canyon, in Coconino County of northern Arizona, US. It is situated 1.5 mile southeast of Point Sublime, four miles west-northwest of Shiva Temple, and three miles northwest of Tower of Ra, where it rises over above Hindu Amphitheater. Confucius Temple is named for Confucius (551–479 BC), the Chinese philosopher.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
Confucius Temple is named for Confucius (551–479 BC), the Chinese philosopher. This name was applied by Clarence Dutton, who began the tradition of naming geographical features in the Grand Canyon after mythological deities.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
surface_form: dutton
instance_of: Mountain
countries: United States
coordinates: lat: 55.168
lon: -162.272
Geology. The top cupola of Confucius Temple is composed of the basal layer of Permian Kaibab Limestone, upon a similar-thickness unit of slope-forming Toroweap Formation, overlaying cream-colored, cliff-forming, Permian Coconino Sandstone. The sandstone, which is the third-youngest of the strata in the Grand Canyon, was deposited 265 million years ago as sand dunes.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
aurea&quot;. Distribution and habitat. &quot;Myriopteris aurea&quot; grows throughout Mexico except for Tabasco and the Yucatan Peninsula, where it is the most widespread and abundant fern in the country. The range extends slightly north into the United States, into Arizona, New Mexico, and Trans-Pecos Texas. In the east, it is found among the Greater Antilles and in Venezuela.

Geographic entities mentioned:
surface_form: Trans-Pecos
instance_of: Valley
countries: United States
coordinates: lat: 30.56
lon: -103.79
In the east, it is found among the Greater Antilles and in Venezuela. To the south, it extends through Central America into South America and along the Andes Mountains, where it has been described as &quot;one of the characteristic ferns of the Altiplano&quot;, as far south as Chile and Argentina, and east into Brazil, Paraguay and Uruguay.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Kakwusis Lake. Kakwusis Lake is a lake in the Hayes River drainage basin in Census Division No. 22 - Thompson-North Central, Northern Region, Manitoba, Canada. The lake is about long and wide and lies at an elevation of. The primary inflow and outflow is the Bolton River, whose waters eventually flow into Gods Lake, and via the Gods River and the Hayes River into Hudson Bay.

Geographic entities mentioned:
surface_form: Gods Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.67388888888889
lon: -94.24666666666667
Kakwusis Lake. Kakwusis Lake is a lake in the Hayes River drainage basin in Census Division No. 22 - Thompson-North Central, Northern Region, Manitoba, Canada. The lake is about long and wide and lies at an elevation of. The primary inflow and outflow is the Bolton River, whose waters eventually flow into Gods Lake, and via the Gods River and the Hayes River into Hudson Bay.

Geographic entities mentioned:
surface_form: kakwusis lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.3733
lon: -95.5858
Osječenica. Osječenica () is a mountain in the municipality of Bosanski Petrovac, Bosnia and Herzegovina. It has an altitude of.

Geographic entities mentioned:
surface_form: osječenica
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 44.48333333
lon: 16.28333333
Prehistory. The oldest evidence of humans in the area trace back to 14,000 BC. There have been Paleolithic finds on the north bank of Lake Zug, which come from nomadic hunters and gatherers. Archaeologists have also found over forty lake-shore settlements, known as pile dwellings, on the shores of Lake Zug from the epoch of the first settled farmers in the Neolithic period (5,500-2,200 BC).

Geographic entities mentioned:
surface_form: Lake Zug
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.116666666667
lon: 8.4833333333333
By 2018, a Crypto Valley Association had been formed, with Oliver Bussmann as its president. Situation. The lake shore has been embanked and forms a promenade, from which views of the Rigi and Pilatus, as well as of the snowy peaks of the Bernese Oberland, are gained. Towards its northerly end, a monument marks the spot where a part of the shore slipped into the lake in 1887.

Geographic entities mentioned:
surface_form: Rigi
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.05
lon: 8.4666666666667
Zug is also at the end of Zürich S-Bahn suburban railway network, on lines S5 and S24. The Zugerbergbahn is a funicular linking the Zug suburb of Schönegg (558 m) with the Vordergeissboden (literally: anterior goat terrain, 925 m), the plateau of the Zugerberg overlooking the town and Lake Zug. The A4 motorway and other main roads connect Zug with the rest of the nation.

Geographic entities mentioned:
surface_form: Zugerberg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.139166666667
lon: 8.5383333333333
The A4 motorway and other main roads connect Zug with the rest of the nation. Water transportation on Lake Zug is centred on the town, with public transport on the lake provided by (Motor Ship) &quot;MS Zug&quot;, &quot;MS Schwyz&quot;, &quot;MS Rigi&quot; and &quot;MS Schwan&quot;.

Geographic entities mentioned:
surface_form: Lake Zug
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.116666666667
lon: 8.4833333333333
Nai Aru Lagoon. Nai Aru Lagoon (or Nay Aru Lagoon) is an estuarine lagoon in Mullaitivu District, north-east Sri Lanka. The lagoon is fed by a number of small rivers, including Nay Aru (Mullaitivu). It is linked to the sea by a narrow channel to the south that is very often blocked by a sand bar. The lagoon's water is brackish.

Geographic entities mentioned:
surface_form: nay aru
instance_of: Watercourse
countries: Sri Lanka
coordinates: lat: 9.13333333
lon: 80.81666667
surface_form: nai aru lagoon
instance_of: Lake
countries: Sri Lanka
coordinates: lat: 9.1333333333333
lon: 80.866666666667
surface_form: nay aru
instance_of: Watercourse
countries: Sri Lanka
coordinates: lat: 9
lon: 80.16666667
Nai Aru Lagoon. Nai Aru Lagoon (or Nay Aru Lagoon) is an estuarine lagoon in Mullaitivu District, north-east Sri Lanka. The lagoon is fed by a number of small rivers, including Nay Aru (Mullaitivu). It is linked to the sea by a narrow channel to the south that is very often blocked by a sand bar. The lagoon's water is brackish.

Geographic entities mentioned:
surface_form: nay aru (mullaitivu)
instance_of: Watercourse
countries: Sri Lanka
coordinates: lat: 9.13333333
lon: 80.81666667
surface_form: nay aru
instance_of: Watercourse
countries: Sri Lanka
coordinates: lat: 9
lon: 80.16666667
Nai Aru Lagoon. Nai Aru Lagoon (or Nay Aru Lagoon) is an estuarine lagoon in Mullaitivu District, north-east Sri Lanka. The lagoon is fed by a number of small rivers, including Nay Aru (Mullaitivu). It is linked to the sea by a narrow channel to the south that is very often blocked by a sand bar. The lagoon's water is brackish.

Geographic entities mentioned:
surface_form: nai aru lagoon
instance_of: Lake
countries: Sri Lanka
coordinates: lat: 9.1333333333333
lon: 80.866666666667
Huampo (Huaylas). Huampo or Wamp'u (Quechua for boat, also spelled &quot;Huampu&quot;) is a mountain in the Cordillera Negra in the Andes of Peru which reaches a height of approximately. It is located in the Ancash Region, Huaylas Province, Pamparomas District.

Geographic entities mentioned:
surface_form: wamp'u
instance_of: Mountain
countries: Peru
coordinates: lat: -9.24305556
lon: -77.99888889
surface_form: wamp'u
instance_of: Mountain
countries: Peru
coordinates: lat: -13.76111111
lon: -73.58611111
surface_form: huampo
instance_of: Mountain
countries: Peru
coordinates: lat: -9.15638889
lon: -77.89027778
Huampo (Huaylas). Huampo or Wamp'u (Quechua for boat, also spelled &quot;Huampu&quot;) is a mountain in the Cordillera Negra in the Andes of Peru which reaches a height of approximately. It is located in the Ancash Region, Huaylas Province, Pamparomas District.

Geographic entities mentioned:
surface_form: huampo (huaylas)
instance_of: Mountain
countries: Peru
coordinates: lat: -9.15638889
lon: -77.89027778
Kola Domain. The extreme northeast of Finland is part of the Kola Domain because it shows considerable affinity with the geology of the Kola Peninsula in Russia. Around Lake Inari there are paragneiss, orthogneiss and greenstone belts. Rocks in this part of Finland are of Archean and Proterozoic age.

Geographic entities mentioned:
surface_form: Lake Inari
instance_of: Lake
countries: Finland
coordinates: lat: 68.9596511
lon: 27.6017069
Granitoids that intruded in the aftermath of the Svercofennian orogeny are common in southern Finland occurring mostly within ca. 100 km of the Gulf of Finland or Lake Ladoga. These so-called Lateorogenic granites are distinguished by usually containing garnet and cordierite and being accompanied by rather few rocks of mafic and intermediate composition.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
Above these there are Upper Riphean and Vendian sandstones and shales. There is evidence suggesting that Jotnian rocks, or even a Jotnian platform, once covered much of Fennoscandia and were not restricted to a few localities like today. The limited geographical extent of Jotnian sediments at present is indebted to their erosion over geological time.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
The long river is located mostly in Innlandet county, but the headwaters are actually just over the border in Akershus county. The river generally flows north and it runs through the large lake Einavatnet as it passes through the municipalities of Hurdal, Vestre Toten, and Gjøvik. The mouth of the river is in the town of Gjøvik where it empties into the large lake Mjøsa.

Geographic entities mentioned:
surface_form: Einavatnet
instance_of: Lake
countries: Norway
coordinates: lat: 60.579722222222
lon: 10.634444444444
The river generally flows north and it runs through the large lake Einavatnet as it passes through the municipalities of Hurdal, Vestre Toten, and Gjøvik. The mouth of the river is in the town of Gjøvik where it empties into the large lake Mjøsa. The main part of the river is about long and it runs from the Einavatnet lake to the town of Gjøvik.

Geographic entities mentioned:
surface_form: Mjøsa
instance_of: Lake
countries: Norway
coordinates: lat: 60.666666666667
lon: 11
Mount Raukūmara. Mount Raukūmara is a 1413-metre (4636 ft) mountain that is the northernmost major peak in the Raukūmara Range in the northeast of New Zealand's North Island. It is part of the backbone of the range, which forms part of a line of mountains extending along the eastern side of the North Island between the Gisborne District and Wellington.

Geographic entities mentioned:
surface_form: mount raukūmara
instance_of: Mountain
countries: New Zealand
coordinates: lat: -37.763
lon: 178.126
It is part of the backbone of the range, which forms part of a line of mountains extending along the eastern side of the North Island between the Gisborne District and Wellington. Mount Raukūmara is clearly visible from a great distance at sea, being located only 25 kilometres from both Cape Runaway and East Cape.

Geographic entities mentioned:
surface_form: mount raukūmara
instance_of: Mountain
countries: New Zealand
coordinates: lat: -37.763
lon: 178.126
2001–02 FIS Ski Jumping World Cup. The 2001–02 FIS Ski Jumping World Cup wast the 23rd World Cup season in ski jumping and without any ski flying individual event held in this season (third time in history).. Season began on 23 November 2001 at Puijo in Kuopio, Finland, and finished on 24 March 2002 at Letalnica bratov Gorišek in Planica, Slovenia.

Geographic entities mentioned:
surface_form: Planica
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.476944444444
lon: 13.722222222222
His early work explores the mechanical origin and kinematic evolution of low-angle normal faults and thrust systems in the North American Cordillera. He is known for his work on the tectonic evolution of the Himalayas and Tibetan plateau. His research interests shifted in later years to slow-earthquake mechanics, early Earth tectonics, and planetary studies. Early life.

Geographic entities mentioned:
surface_form: Tibetan plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
It was an especially grand example whose particular symmetrical arrangement with an apse at both ends was repeated in the provinces as a characteristic form. To improve the quality of the Roman concrete used in the Basilica Ulpia, volcanic scoria from the Bay of Naples and Mount Vesuvius were imported which, though heavier, was stronger than the pumice available closer to Rome.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
Amphorae discovered at basilicas attest their economic uses and can reveal their position in wider networks of exchange. At Dion near Mount Olympus in Macedonia, now an Archaeological Park, the latter 5th century &quot;Cemetery Basilica&quot;, a small church, was replete with potsherds from all over the Mediterranean, evidencing extensive economic activity took place there.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
On 1 October 1975, the V Army Corps Signal Battalion was renamed 5th Signal Battalion &quot;Rolle&quot;. The battalion was named for the Rolle Pass, which connects the Fiemme valley and the Primiero valley in the Dolomites. After the reform the 5th Signal Battalion &quot;Rolle&quot; consisted of a command, a command and services platoon, four signal companies, and a repairs and recovery platoon.

Geographic entities mentioned:
surface_form: Primiero
instance_of: Valley
countries: Italy
coordinates: lat: 46.183333333333
lon: 11.833333333333
He graduated from Hitotsubashi University. Among other expeditions, in 1977 he led the second successful attempt to reach the summit of K2, which saw six Japanese climbers and one Pakistani summiting on August 8-9. Yoshizawa became a member of the Japanese Alpine Club in 1925 and became vice president in 1972; he was also a member of foreign clubs like The Alpine Club.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
state of Michigan. The population was 36,686 at the 2020 census. Independence Township was first organized in 1834. The township surrounds the city of Clarkston, but the two are administered autonomously after Clarkston incorporated as a city in 1992. The township is home to the Pine Knob Music Theatre and the Pine Knob Ski Resort. History.

Geographic entities mentioned:
surface_form: Pine Knob
instance_of: Mountain
countries: United States
coordinates: lat: 42.742222222222
lon: -83.367222222222
It is located at 9085 Big Lake Road in Independence Township. Oakhurst Golf and Country Club is a private club, located at 7000 Oakhurst Lane
in Independence Township. Oakhurst was the home of the 99th Michigan Amateur
Skiing and music. Pine Knob is a ski resort located in Independence Township. It features 17 trails and 12 lifts. It is known for its slope called &quot;The Wall&quot;.

Geographic entities mentioned:
surface_form: Pine Knob
instance_of: Mountain
countries: United States
coordinates: lat: 42.742222222222
lon: -83.367222222222
Hamangia (river). The Hamangia is a river in Tulcea County, Romania. Near Lunca, it discharges into Lake Golovița, a former lagoon of the Black Sea. Its length is and its basin size is.

Geographic entities mentioned:
surface_form: Lake Golovița
instance_of: Lake
countries: Romania
coordinates: lat: 44.71416667
lon: 28.77666667
Royal Naval Air Station Cattewater. As early as 1913 the sheltered Cattewater in Plymouth Sound was used for seaplane trials and in 1916 plans to open a Royal Navy seaplane station were agreed. In February 1917 RNAS Cattewater was opened.

Geographic entities mentioned:
surface_form: Cattewater
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 50.362222222222
lon: -4.1277777777778
Mount Gec. igai378kifil3ycuwuvvkh113h7" xml:space="preserve">#REDIRECT Mount GEC

Geographic entities mentioned:
surface_form: mount gec
instance_of: Mountain
countries: Canada
coordinates: lat: 52.33638888888889
lon: -117.45
The Geneva School combined the &quot;Austrian emphasis on the limits of knowledge and the global scale with the German ordoliberal emphasis on institutions and the moment of the political decision.&quot; Geneva School economists were instrumental in organizing the Mont Pelerin Society, a neoliberal academic society of economists and political philosophers that assembled in nearby Mont Pèlerin.

Geographic entities mentioned:
surface_form: Mont Pèlerin
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.496877777778
lon: 6.8192472222222
Historic villas. Another section of the campus are two historic villas situated by Lake Geneva, Villa Barton and Villa Moynier. Villa Barton served as the institute's main campus from 1937 to 2007. It now mostly houses administrative staff.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Geology. Gaussberg is an extremely isolated volcano although an ice rise a few kilometres southwest of Gaussberg and aeromagnetic surveys suggest that within there are other small volcanoes in the area. It is the only Antarctic volcano situated on the Antarctic Shield, where the thickest crust of Antarctica is found.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: gaussberg
instance_of: Mountain
coordinates: lat: -66.8
lon: 89.183333333333
Finally, the 90° E Fault that separates regional tectonic structures may have influenced volcanism at Gaussberg. Composition. The volcano has a uniform chemical composition consisting of lamproite (originally identified as leucitite), which defines a potassium-rich mafic rock suite. The rocks are almost free of visible crystals but contain numerous vesicles.

Geographic entities mentioned:
surface_form: rich
instance_of: Mountain
coordinates: lat: -79.7833
lon: 158.8
The source of the Gaussberg lamproites is unclear, as the processes usually proposed for the formation of such magmas do not easily apply to the Gaussberg rocks. The magma may have formed through the incomplete melting of phlogopite-rich mantle and further chemical processes such as crystal fractionation that raised the potassium/aluminium ratio above 1.

Geographic entities mentioned:
surface_form: rich
instance_of: Mountain
coordinates: lat: -79.7833
lon: 158.8
There are different views on how erosion affected Gaussberg; some think that it was largely spared and others that erosion wore down the initially much larger edifice to its current size; the latter theory is the preferred view of the Global Volcanism Program and is supported by aeromagnetic data which suggest an initial size of.

Geographic entities mentioned:
surface_form: gaussberg
instance_of: Mountain
coordinates: lat: -66.8
lon: 89.183333333333
The rocks were probably emplaced subglacially, although the occurrence of pahoehoe lava is possible. There are moraines on the southern, northwestern and northeastern foot of the volcano, and erratic blocks and glacial striations are evidence that the volcano was formerly glaciated. Geology.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Gaussberg. Gaussberg (or Schwarzen Berg, Mount Gauss) is an extinct, high volcanic cone in East Antarctica fronting on Davis Sea immediately west of Posadowsky Glacier. It is ice-free and conical in nature, having formed subglacially about 55,000 years ago. The current edifice is thought to be the remains of a once-larger mountain that has been reduced by glacial and subaerial erosion.

Geographic entities mentioned:
surface_form: gaussberg
instance_of: Mountain
coordinates: lat: -66.8
lon: 89.183333333333
Gaussberg. Gaussberg (or Schwarzen Berg, Mount Gauss) is an extinct, high volcanic cone in East Antarctica fronting on Davis Sea immediately west of Posadowsky Glacier. It is ice-free and conical in nature, having formed subglacially about 55,000 years ago. The current edifice is thought to be the remains of a once-larger mountain that has been reduced by glacial and subaerial erosion.

Geographic entities mentioned:
surface_form: gaussberg
instance_of: Mountain
coordinates: lat: -66.8
lon: 89.183333333333
surface_form: davis
instance_of: Mountain
coordinates: lat: -78.1
lon: -86.25
Drygalski observed the volcano with the help of a tethered balloon. Owing to its peculiar composition, Gaussberg has been intensively researched. The mountain was investigated in 1912 by the 1911-1914 Australasian Antarctic Expedition, by the Soviet Antarctic Expedition in 1956–1957, by Australian expeditions in 1977, 1981, 1987 and by an expedition linked to an entity &quot;K.D.C&quot; in 1997.

Geographic entities mentioned:
surface_form: gaussberg
instance_of: Mountain
coordinates: lat: -66.8
lon: 89.183333333333
Geography and geomorphology. The volcano lies in Kaiser Wilhelm II Land, Antarctica, close to the West Ice Shelf and between the Australian Davis Station and Russian Mirny Station. It lies on the Davis Sea immediately west of Posadowsky Glacier. Gaussberg is within the Antarctic territory claimed by Australia, and the only ice-free outcrop between Mirny Station and the Vestfold Hills.

Geographic entities mentioned:
surface_form: davis
instance_of: Mountain
coordinates: lat: -78.1
lon: -86.25
Why it formed about 50,000 years ago on a stable continental margin is unclear; either a mantle plume, an instability of the East Antarctic continent or lateral flow of mantle plume material are possible. The basement underneath Gaussberg is formed by gneisses of Archean to Proterozoic age. The lithosphere under Gaussberg is over thick and has an unusually high heat flow.

Geographic entities mentioned:
surface_form: gaussberg
instance_of: Mountain
coordinates: lat: -66.8
lon: 89.183333333333
The lithosphere under Gaussberg is over thick and has an unusually high heat flow. Its activity has been related to the Kerguelen Plateau, but the Kerguelen volcanoes have yielded different magma compositions and there is no major geological structure linking the two other than the so-called &quot;Kerguelen-Gaussberg Ridge&quot;, thus a connection between the two is unproven.

Geographic entities mentioned:
surface_form: gaussberg
instance_of: Mountain
coordinates: lat: -66.8
lon: 89.183333333333
A graben system in the region, which may have formed in Gondwana and may be correlated to tectonic structures on the Indian Peninsula, has been christened the &quot;Gaussberg Rift&quot;; the volcano rises on a horst on the rift but its relation to the rift is unclear. Finally, the 90° E Fault that separates regional tectonic structures may have influenced volcanism at Gaussberg. Composition.

Geographic entities mentioned:
surface_form: gaussberg
instance_of: Mountain
coordinates: lat: -66.8
lon: 89.183333333333
There are xenoliths, mostly granites coming from the Precambrian basement, and zircons recovered from the rocks are up to several billion years old. Palagonite, salt and native sulfur deposits have been found. The source of the Gaussberg lamproites is unclear, as the processes usually proposed for the formation of such magmas do not easily apply to the Gaussberg rocks.

Geographic entities mentioned:
surface_form: gaussberg
instance_of: Mountain
coordinates: lat: -66.8
lon: 89.183333333333
The magma may have formed through the incomplete melting of phlogopite-rich mantle and further chemical processes such as crystal fractionation that raised the potassium/aluminium ratio above 1. Deep mantle structures that formed through subduction billions of years ago and remained isolated since then have been proposed as the source of Gaussberg lamproites.

Geographic entities mentioned:
surface_form: gaussberg
instance_of: Mountain
coordinates: lat: -66.8
lon: 89.183333333333
The Kerguelen plume may or may not have played a role. Eruption history. Drastically different age estimates have been obtained on Gaussberg. Early research suggested a Pliocene or Miocene age based on a presumed history of the Antarctic Ice Sheet and comparisons between the appearance of Gaussberg with Kerguelen volcanoes.

Geographic entities mentioned:
surface_form: gaussberg
instance_of: Mountain
coordinates: lat: -66.8
lon: 89.183333333333
Drastically different age estimates have been obtained on Gaussberg. Early research suggested a Pliocene or Miocene age based on a presumed history of the Antarctic Ice Sheet and comparisons between the appearance of Gaussberg with Kerguelen volcanoes. Potassium-argon dating has yielded ages of 20 and 9 million years, with younger dating efforts producing an age of 56,000±5,000 years.

Geographic entities mentioned:
surface_form: gaussberg
instance_of: Mountain
coordinates: lat: -66.8
lon: 89.183333333333
The 56,000±5,000 years age is considered to be more probable than the 20 and 9 million years ones. Gaussberg was probably constructed in a single eruptive episode but there is evidence that the present-day edifice formed on an older, eroded volcano. Gaussberg formed under much thicker ice than there is today in the area, and the ice deposited moraines on its summit.

Geographic entities mentioned:
surface_form: gaussberg
instance_of: Mountain
coordinates: lat: -66.8
lon: 89.183333333333
Dust layers in the Siple Dome ice core may come from wind-driven erosion of Gaussberg rocks. Biology. Several moss species were identified at Gaussberg, as well as a protozoan fauna such as rotifers inhabiting them. Nematodes and tardigrades have been found at Gaussberg. It was the first place on the Antarctic mainland where lichens were reported.

Geographic entities mentioned:
surface_form: gaussberg
instance_of: Mountain
coordinates: lat: -66.8
lon: 89.183333333333
Several moss species were identified at Gaussberg, as well as a protozoan fauna such as rotifers inhabiting them. Nematodes and tardigrades have been found at Gaussberg. It was the first place on the Antarctic mainland where lichens were reported. Emperor penguin rookeries occur at the mountain and snow petrels were observed to breed there, but overall there is not much fauna at Gaussberg.

Geographic entities mentioned:
surface_form: gaussberg
instance_of: Mountain
coordinates: lat: -66.8
lon: 89.183333333333
The mineral gaussbergite is named after the volcano. Geography and geomorphology. The volcano lies in Kaiser Wilhelm II Land, Antarctica, close to the West Ice Shelf and between the Australian Davis Station and Russian Mirny Station. It lies on the Davis Sea immediately west of Posadowsky Glacier.

Geographic entities mentioned:
surface_form: davis
instance_of: Mountain
coordinates: lat: -78.1
lon: -86.25
Cream Roll (mountain). 1qo1lxw0hardy65fc41jrlb3s7c" xml:space="preserve">#REDIRECT List of mountain peaks of Uttarakhand

Geographic entities mentioned:
surface_form: cream roll
instance_of: Mountain
countries: India
coordinates: lat: 30.313055555555554
lon: 79.94944444444444
Ali Olo. Ali Olo is a mountain located in the northeast of Ali Sabieh Region in Djibouti. With an average elevation of 286 metres (938 ft) above sea level, they are situated near the border with Somalia.

Geographic entities mentioned:
surface_form: ali sabieh
instance_of: Mountain
countries: Djibouti
coordinates: lat: 11.15277778
lon: 42.715
surface_form: ali olo
instance_of: Mountain
countries: Djibouti
coordinates: lat: 11.35555556
lon: 43.12333333
Ali Olo. Ali Olo is a mountain located in the northeast of Ali Sabieh Region in Djibouti. With an average elevation of 286 metres (938 ft) above sea level, they are situated near the border with Somalia.

Geographic entities mentioned:
surface_form: ali olo
instance_of: Mountain
countries: Djibouti
coordinates: lat: 11.35555556
lon: 43.12333333
It is named after Edward Charles Frome, the third surveyor-general of South Australia. The electorate stretches north-eastwards from the Gawler River and Gulf St Vincent in the south, and includes many of the agricultural areas of the Clare and Gilbert Valleys. It covers a total of and takes in the towns of Auburn, Clare, Mintaro, Port Broughton, Saddleworth, Snowtown and Riverton.

Geographic entities mentioned:
surface_form: Clare
instance_of: Valley
countries: Australia
coordinates: lat: -33.83361111
lon: 138.61
&quot;Butterstick&quot; was not included as an option. Some bloggers protested this decision; there was even an attempt to hack the poll, allowing voters the option of selecting the name Butterstick. Despite these efforts, the name Tai Shan was eventually chosen, as it had won 44 percent of the 202,045 total votes cast. Media attention.

Geographic entities mentioned:
surface_form: Tai Shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.266666666667
lon: 117.1
Its purpose is to provide drinking water to local villagers and to support a horticultural project. Description. The purpose of the dam is to provide a reliable source of drinking water to 22 villages in the Tswapong area, and to provide irrigation water for a horticulture operation near Maunatlala. The dam is an earth fill embankment high and long, with an ungated long ogee crest spillway.

Geographic entities mentioned:
surface_form: Tswapong
instance_of: Mountain
countries: Botswana
coordinates: lat: -22.65
lon: 27.5167
Geography. Viso Mozzo is located in the upper Valle Po and stands east-north-est of Monviso, from which is divided by the &quot;colle dei Viso&quot; (&quot;Viso Pass&quot;). Its western side, facing Monviso, is a long and almost uniform rock-field, while the other faces of the mountain are more irregular. Access to the summit.

Geographic entities mentioned:
surface_form: Valle Po
instance_of: Valley
countries: Italy
coordinates: lat: 44.6628
lon: 7.29615
surface_form: viso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
surface_form: viso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
surface_form: monviso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
surface_form: monviso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
Viso Mozzo. The Viso Mozzo is a 3,019 metres high mountain on the Italian side of the Cottian Alps. Toponymy. In Italian &quot;viso&quot; means &quot;face&quot;, but in this context refers to the Monviso, which is very close to the Viso Mozzo, and &quot;mozzo&quot; means &quot;cut off&quot;.

Geographic entities mentioned:
surface_form: viso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
surface_form: viso mozzo
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6747
lon: 7.10972
Viso Mozzo. The Viso Mozzo is a 3,019 metres high mountain on the Italian side of the Cottian Alps. Toponymy. In Italian &quot;viso&quot; means &quot;face&quot;, but in this context refers to the Monviso, which is very close to the Viso Mozzo, and &quot;mozzo&quot; means &quot;cut off&quot;.

Geographic entities mentioned:
surface_form: viso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
surface_form: viso mozzo
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6747
lon: 7.10972
surface_form: high mountain
instance_of: Mountain
countries: Italy
coordinates: lat: 44.008763888889
lon: 10.289719444444
Toponymy. In Italian &quot;viso&quot; means &quot;face&quot;, but in this context refers to the Monviso, which is very close to the Viso Mozzo, and &quot;mozzo&quot; means &quot;cut off&quot;. Thus the whole name should mean &quot;Cut-off Monviso&quot;; an old local name of the mountain is &quot;Viso-Mout&quot;. Geography.

Geographic entities mentioned:
surface_form: viso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
surface_form: viso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
surface_form: monviso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
surface_form: viso mozzo
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6747
lon: 7.10972
Toponymy. In Italian &quot;viso&quot; means &quot;face&quot;, but in this context refers to the Monviso, which is very close to the Viso Mozzo, and &quot;mozzo&quot; means &quot;cut off&quot;. Thus the whole name should mean &quot;Cut-off Monviso&quot;; an old local name of the mountain is &quot;Viso-Mout&quot;. Geography.

Geographic entities mentioned:
surface_form: viso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
surface_form: viso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
surface_form: monviso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
Geography. Viso Mozzo is located in the upper Valle Po and stands east-north-est of Monviso, from which is divided by the &quot;colle dei Viso&quot; (&quot;Viso Pass&quot;). Its western side, facing Monviso, is a long and almost uniform rock-field, while the other faces of the mountain are more irregular. Access to the summit.

Geographic entities mentioned:
surface_form: viso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
At &quot;colle dei Viso&quot;, leaving the main footpath and turning left, following some cairns, in roughly one hour is possible to reach the mountain top, marked by a metallic summit cross and offering an interesting view both on the Monviso massif and on the Po plain.

Geographic entities mentioned:
surface_form: monviso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
Chojorusi. Chojorusi (possibly from Aymara for a colored clay used to paint houses) is a mountain in the Vilcanota mountain range in the Andes of Peru, about high. It is located in the Cusco Region, Quispicanchi Province, Marcapata District. Chojorusi lies southwest of Puicutuni and northwest of Llusca Ritti and Sullulluni.

Geographic entities mentioned:
surface_form: Puicutuni
instance_of: Mountain
countries: Peru
coordinates: lat: -13.6806
lon: -70.7239
surface_form: llusca ritti
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7253
lon: -70.7319
surface_form: llusca ritti
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7625
lon: -70.6933
surface_form: chojorusi
instance_of: Mountain
countries: Peru
coordinates: lat: -13.69944444
lon: -70.74722222
Chojorusi. Chojorusi (possibly from Aymara for a colored clay used to paint houses) is a mountain in the Vilcanota mountain range in the Andes of Peru, about high. It is located in the Cusco Region, Quispicanchi Province, Marcapata District. Chojorusi lies southwest of Puicutuni and northwest of Llusca Ritti and Sullulluni.

Geographic entities mentioned:
surface_form: chojorusi
instance_of: Mountain
countries: Peru
coordinates: lat: -13.69944444
lon: -70.74722222
International shipping traffic continues to grow as intermodal port and rail facilities are expanded. The Virginia Port Authority even operates an inland port in the Shenandoah Valley. The Wright Brothers are credited with first flight just south of Virginia at Kitty Hawk, North Carolina. Other early flights took place at Willoughby Spit near Norfolk.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
The Virginia Port Authority even operates an inland port in the Shenandoah Valley. The Wright Brothers are credited with first flight just south of Virginia at Kitty Hawk, North Carolina. Other early flights took place at Willoughby Spit near Norfolk. In modern times, major commercial airports are located around the state, with many additional general aviation facilities.

Geographic entities mentioned:
surface_form: Willoughby Spit
instance_of: Landform
countries: United States
coordinates: lat: 36.967
lon: -76.282472222222
The Hampton Roads Beltway extends on a long loop through the region, crossing the harbor on two toll-free bridge-tunnel facilities. These crossings are the Hampton Roads Bridge–Tunnel between Phoebus in Hampton and Willoughby Spit in Norfolk and the Monitor–Merrimac Memorial Bridge–Tunnel between Newport News and Suffolk. The Beltway connects with another Interstate highway and three arterial U.S.

Geographic entities mentioned:
surface_form: Willoughby Spit
instance_of: Landform
countries: United States
coordinates: lat: 36.967
lon: -76.282472222222
Massive coal loading piers and facilities were established in the late 19th and early 20th centuries by the Chesapeake and Ohio Railway (C&O), Norfolk and Western Railway (N&W), and Virginian Railway (VGN). The latter two were predecessors of the Norfolk Southern Railway, a Class I railroad headquartered in Norfolk that exports coal from a large facility at Lambert's Point on the Elizabeth River.

Geographic entities mentioned:
surface_form: Lambert's Point
instance_of: Landform
countries: United States
coordinates: lat: 36.87468
lon: -76.32348
It is situated in the Potosí Department, Antonio Quijarro Province, Tomave Municipality, between the Uyuni salt flat in the west and the town of Porco in the east and southwest of the Nuevo Mundo volcano (Jatun Mundo Quri Warani).

Geographic entities mentioned:
surface_form: Nuevo Mundo
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.774166666667
lon: -66.478333333333
Kuntur Chukuña (Antonio Quijarro). Kuntur Chukuña (Aymara &quot;kunturi&quot; condor, &quot;chukuña&quot; to squat, to cower, 'where the condor squats', also spelled &quot;Condor Chucuna, Condor Chucuña&quot;) is a mountain in the Andes of Bolivia, about high.

Geographic entities mentioned:
surface_form: kuntur chukuña
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.91666667
lon: -66.51666667
Kuntur Chukuña (Antonio Quijarro). Kuntur Chukuña (Aymara &quot;kunturi&quot; condor, &quot;chukuña&quot; to squat, to cower, 'where the condor squats', also spelled &quot;Condor Chucuna, Condor Chucuña&quot;) is a mountain in the Andes of Bolivia, about high.

Geographic entities mentioned:
surface_form: kuntur chukuña
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.91666667
lon: -66.51666667
surface_form: condor chucuña
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.91666667
lon: -66.51666667
In 1668 Father Jacques Marquette was moved by his Jesuit superiors to missions farther up the St. Lawrence River in the western Great Lakes region. He helped found missions at Sault Ste. Marie in present-day Michigan in 1668, St. Ignace in 1671, and at La Pointe on Lake Superior near the present-day city of Ashland, Wisconsin.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Dyrdalen. Dyrdalen (The Reindeer Valley) is a valley at Edgeøya, Svalbard. It is the largest valley on the island, with a length of about twenty kilometers, and runs northwards from the head of Tjuvfjorden, west of Edgeøyjøkulen.

Geographic entities mentioned:
surface_form: dyrdalen
instance_of: Valley
countries: Norway
coordinates: lat: 77.722
lon: 22.7103
Chiloglanis reticulatus. &quot;Chiloglanis reticulatus&quot; is a species of upside-down catfish native to the Dja River system in Cameroon and the Luala and Lufu River drainages in the Democratic Republic of the Congo. This species grows to a length of SL.

Geographic entities mentioned:
surface_form: Lufu River
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: -5.53712
lon: 13.66293
Dunham Pond (Carver, Massachusetts). Dunham Pond is a pond in Carver, Massachusetts, United States. The pond is located northeast of Sampsons Pond and southwest of Federal Pond.

Geographic entities mentioned:
surface_form: Sampsons Pond
instance_of: Lake
countries: United States
coordinates: lat: 41.85
lon: -70.75
surface_form: Federal Pond
instance_of: Lake
countries: United States
coordinates: lat: 41.875
lon: -70.708333333333
Dunham Pond (Carver, Massachusetts). Dunham Pond is a pond in Carver, Massachusetts, United States. The pond is located northeast of Sampsons Pond and southwest of Federal Pond.

Geographic entities mentioned:
surface_form: dunham pond (carver, massachusetts)
instance_of: Lake
countries: United States
coordinates: lat: 41.8669
lon: -70.7333
Dunham Pond (Carver, Massachusetts). Dunham Pond is a pond in Carver, Massachusetts, United States. The pond is located northeast of Sampsons Pond and southwest of Federal Pond.

Geographic entities mentioned:
surface_form: dunham pond
instance_of: Lake
countries: United States
coordinates: lat: 41.8669
lon: -70.7333
It is about long and is about wide at the mouth. All the water ends in the Pacific Ocean. The river forms as a little trickle from the little snow melt of Mont Orohena in the center of Tahiti and flows northward toward Arue. As it flows north, it collects more and more snow melt. Eventually, it becomes a wide river south of the ocean. Once it reaches the Tahiti Freeway, it becomes a wide river.

Geographic entities mentioned:
surface_form: Mont Orohena
instance_of: Mountain
countries: France
coordinates: lat: -17.623055555556
lon: -149.47694444444
Huaytunas lake. fhs4gohtpcvwqj6yqnpjs88oyi1w" xml:space="preserve">#REDIRECT Huaytunas Lake

Geographic entities mentioned:
surface_form: huaytunas lake
instance_of: Lake
countries: Bolivia
coordinates: lat: -12.917777777778
lon: -65.518333333333
Meltwater from the glaciers pooled into large lakes, including Owens Lake and the Owens River. The river traveled through to Indian Wells Valley, and its course was diverted several times by volcanic activity. The falls were formed when the river was forced to divert its course over a basalt flow, polishing and reshaping the rock into a variety of unique shapes and forms.

Geographic entities mentioned:
surface_form: Indian Wells Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.702777777778
lon: -117.68638888889
History. Sandroyd School was founded as a school for boys by L. H. Wellesley Wesley at Sandroyd House, Fairmile, in Cobham, Surrey in 1880. He was a great-grandson of Charles Wesley. In 1939, in anticipation of the Second World War, the school moved to Rushmore House, home of the Pitt-Rivers family. The house lies in the centre of Cranborne Chase on the borders of Wiltshire and Dorset.

Geographic entities mentioned:
surface_form: Cranborne Chase
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 50.961419444444
lon: -2.0440888888889
Satsar Lake. The Satsar Lake, Sat Sar or Sath Sar () consists of a group of seven small alpine lakes situated in Ganderbal district of the Kashmir Valley in Jammu and Kashmir, India. Geography. The lakes are situated in a narrow alpine valley stretching from north to south and spread over distance with a width of. It also serves a natural mountain pass between Tulail Valley and Sind Valley.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
surface_form: satsar lake
instance_of: Lake
countries: India
coordinates: lat: 34.461709
lon: 74.997935
Geography. The lakes are situated in a narrow alpine valley stretching from north to south and spread over distance with a width of. It also serves a natural mountain pass between Tulail Valley and Sind Valley. The lakes of Gangabal and Nundkol lie on the opposite side of Zajibal pass ().

Geographic entities mentioned:
surface_form: Tulail Valley
instance_of: Valley
countries: India
coordinates: lat: 34.55388888888889
lon: 75.05305555555556
surface_form: Sind Valley
instance_of: Valley
countries: India
coordinates: lat: 34.2892
lon: 74.8125
It also serves a natural mountain pass between Tulail Valley and Sind Valley. The lakes of Gangabal and Nundkol lie on the opposite side of Zajibal pass (). The Satsar Lakes are surrounded by lush green meadows which are home to shepherds during summer and serve as a camping site for tourists. Naranag is the nearest settlement and serves as the base camp for trekking to the lake in the summer.

Geographic entities mentioned:
surface_form: Gangabal
instance_of: Lake
countries: India
coordinates: lat: 34.4325
lon: 74.925
The lake can also be accessed through Bandipora and the six-day trekking starting point is Arin. It can also be accessed through Gurais via Tulail. Tourists prefer to take the Naranag trek and return via Gadsar Lake, Vishansar Lake and Sonamarg or vice versa to cover most alpine lakes of the area.

Geographic entities mentioned:
surface_form: Gadsar Lake
instance_of: Lake
countries: India
coordinates: lat: 34.421669
lon: 75.057274
surface_form: Vishansar Lake
instance_of: Lake
countries: India
coordinates: lat: 34.3881
lon: 75.1188
Satsar Lake. The Satsar Lake, Sat Sar or Sath Sar () consists of a group of seven small alpine lakes situated in Ganderbal district of the Kashmir Valley in Jammu and Kashmir, India. Geography. The lakes are situated in a narrow alpine valley stretching from north to south and spread over distance with a width of. It also serves a natural mountain pass between Tulail Valley and Sind Valley.

Geographic entities mentioned:
surface_form: satsar lake
instance_of: Lake
countries: India
coordinates: lat: 34.461709
lon: 74.997935
The Satsar Lakes are surrounded by lush green meadows which are home to shepherds during summer and serve as a camping site for tourists. Naranag is the nearest settlement and serves as the base camp for trekking to the lake in the summer. The Satsar Lake is mainly fed by melting snow. During the late summer and autumn, two or three lakes usually dry up, depending upon the precipitation.

Geographic entities mentioned:
surface_form: satsar lake
instance_of: Lake
countries: India
coordinates: lat: 34.461709
lon: 74.997935
In addition, a canoe-camping circuit on the Malbaie River begins at the foot of the dam to cross the entire park; the descent allows you to admire the wild landscape of the park. Toponymy. This toponymic designation appears on regional map number 3, 1943. The name &quot;Grand lac à Jack&quot; appeared on maps at the beginning of the 20th century. The origin of the toponym remains uncertain.

Geographic entities mentioned:
surface_form: grand lac
instance_of: Lake
countries: Canada
coordinates: lat: 48.866666666667
lon: -57.433333333333
surface_form: grand lac
instance_of: Lake
countries: Canada
coordinates: lat: 45.933611111111
lon: -66.032777777778
surface_form: lac à jack
instance_of: Lake
countries: Canada
coordinates: lat: 47.620554
lon: -71.006111
The origin of the toponym remains uncertain. However, the presence of an Amerindian named Jacques Bacon, who spent the summer camping in these areas with his family, several decades ago, could be linked to the origin of this body of water. The construction of the Lac-à-Jack dam allowed the passage of a road that links the Jacques-Cartier lake sector to the Grands-Jardins conservation park.

Geographic entities mentioned:
surface_form: jacques-cartier
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.671388888889
lon: -71.747222222222
surface_form: jacques-cartier lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.5852
lon: -71.2073