Sarmila/GeoWiki-Features huggingface dataset:
Indian Hill (Edmonson County, Kentucky). Indian Hill is a summit in Edmonson County, Kentucky, in the United States. With an elevation of, Indian Hill is the 916th highest summit in the state of Kentucky. Indian mounds are found near Indian Hill.

Geographic entities mentioned:
surface_form: indian hill (edmonson county, kentucky)
instance_of: Mountain
countries: United States
coordinates: lat: 37.20222222
lon: -86.25
surface_form: indian hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.4284
lon: -70.6809
surface_form: indian hill
instance_of: Mountain
countries: United States
coordinates: lat: 35.14353056
lon: -115.15426111
Indian Hill (Edmonson County, Kentucky). Indian Hill is a summit in Edmonson County, Kentucky, in the United States. With an elevation of, Indian Hill is the 916th highest summit in the state of Kentucky. Indian mounds are found near Indian Hill.

Geographic entities mentioned:
surface_form: indian hill
instance_of: Mountain
countries: United States
coordinates: lat: 37.20222222
lon: -86.25
surface_form: indian hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.4284
lon: -70.6809
surface_form: indian hill
instance_of: Mountain
countries: United States
coordinates: lat: 35.14353056
lon: -115.15426111
Mariner Glacier. The Mariner Glacier () is a major glacier over long, descending southeast from the plateau of Victoria Land, Antarctica, between Mountaineer Range and Malta Plateau, and terminating at Lady Newnes Bay, Ross Sea, where it forms the floating Mariner Glacier Tongue. Exploration and naming.

Geographic entities mentioned:
surface_form: Malta Plateau
instance_of: Plateau
coordinates: lat: -72.967
lon: 167.3
Geography. The Mariner Glacier forms in the Victory Mountains between The Pleiades to the east and the Barker Range to the west. It is below the Evans Névé to the northwest and the Webb Névé to the east. To the south of the Lawrence Peaks it is fed from the east by the Seafarer Glacier, which in turn is fed by the Wilhelm Glacier and the Olson Glacier.

Geographic entities mentioned:
surface_form: Evans Névé
instance_of: Landform
coordinates: lat: -72.75
lon: 164.5
To the south of the Lawrence Peaks it is fed from the east by the Seafarer Glacier, which in turn is fed by the Wilhelm Glacier and the Olson Glacier. Flowing southeast, below Mount Heg it is fed from the north by the Potts Glacier. Gair Glacier enters from the west to the north of Bunker Bluff, and Argonaut Glacier enters from the southwest before Engberg Bluff.

Geographic entities mentioned:
surface_form: Mount Heg
instance_of: Mountain
coordinates: lat: -72.95
lon: 166.75
Left tributaries. Tributaries from the left (northeast) include,
Seafarer Glacier. A tributary glacier draining southward from Webb Névé between the Lawrence Peaks and Malta Plateau, to enter Mariner Glacier. So named by the Mariner Glacier party of NZGSAE, 1966–67, in association with the name Mariner. Named after &quot;The Seafarer&quot;, an Anglo Saxon poem celebrating early harsh navigation.

Geographic entities mentioned:
surface_form: Malta Plateau
instance_of: Plateau
coordinates: lat: -72.967
lon: 167.3
Tributaries from the left (southwest) include,
Gair Glacier. A tributary glacier, long, rising close southeast of Mount Supernal in the Mountaineer Range and flowing east-northeast to enter Mariner Glacier just north of Bunker Bluff. Named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE) 1962–63, for Harry Gair, geologist and leader that season of the NZGSAE northern field party.

Geographic entities mentioned:
surface_form: Mount Supernal
instance_of: Mountain
coordinates: lat: -73.066666666667
lon: 165.7
Named by the Northern Party of NZGSAE, 1966–67, for the leader of the party, J.E.S. Lawrence. Hercules Névé. A névé at the north margin of Mountaineer Range. It is bounded by Deception Plateau, Astronaut Glacier, Retreat Hills, and by such western tributaries to the Mariner Glacier as Meander Glacier and Gair Glacier.

Geographic entities mentioned:
surface_form: Deception Plateau
instance_of: Landform
coordinates: lat: -73.25
lon: 164.833
Hobbie Ridge. A bold ridge that projects from the middle of the head of Meander Glacier, south of Mount Supernal. Mapped by USGS from surveys and United States Navy air photos, 1960–64. Named by US-ACAN for John E. Hobbie, biologist at McMurdo Station 1962–63. Bunker Bluff. A notable bluff that stands just south of the mouth of Gair Glacier and forms a part of the west wall of Mariner Glacier.

Geographic entities mentioned:
surface_form: Mount Supernal
instance_of: Mountain
coordinates: lat: -73.066666666667
lon: 165.7
Previously weakened rocks may have contributed to the collapse, which was probably started by an earthquake. Geomorphology and geology. The collapse of Tsergo Ri took place in Nepal's Langtang valley, perpendicular to the Himalaya and about north of the Nepalese capital Kathmandu. The small settlement of Kyangjin Kharka lies at the foot of the landslide deposit.

Geographic entities mentioned:
surface_form: Tsergo Ri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.212777777777777
lon: 85.6
surface_form: Langtang
instance_of: Valley
countries: Nepal
coordinates: lat: 28.25
lon: 85.5
surface_form: tsergo ri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.2132408
lon: 85.6004521
After the collapse, landslide debris was subject to glacial erosion and was largely removed in the process. About of debris is still present; it is found around Tsergo Ri mountain, which is formed by landslide debris and its location is in the central sector of the former landslide. Yala Peak and Dragpoche are in the area of the detachment, east of the seven-thousander Langtang Lirung.

Geographic entities mentioned:
surface_form: Yala Peak
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.2286
lon: 85.628
surface_form: Langtang Lirung
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.256111111111
lon: 85.519444444444
surface_form: langtang
instance_of: Valley
countries: Nepal
coordinates: lat: 28.25
lon: 85.5
The glaciers that had had their valleys cut by the landslide readvanced during the youngest phase of the Würm glaciation and partially restored the valleys. Landslides take place to this day in the area, including during the 2015 Nepal earthquake when a landslide detached from Langtang Lirung peak and killed over 350 people in the Langtang valley.

Geographic entities mentioned:
surface_form: Langtang Lirung
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.256111111111
lon: 85.519444444444
surface_form: langtang
instance_of: Valley
countries: Nepal
coordinates: lat: 28.25
lon: 85.5
surface_form: langtang
instance_of: Valley
countries: Nepal
coordinates: lat: 28.25
lon: 85.5
Tsergo Ri landslide. The Tsergo Ri landslide was a prehistoric landslide in the Nepalese Himalaya, which took place around 51,000±13,000 years ago, during the Last Glacial Period. During the collapse, a mass of rock of about detached from a previous mountain or ridge and descended with a speed of about; later, glaciers eroded almost the entire landslide mass.

Geographic entities mentioned:
surface_form: tsergo ri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.212777777777777
lon: 85.6
surface_form: tsergo ri landslide
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.2132408
lon: 85.6004521
Causes and trigger. The collapse affected Himalayan gneiss rocks, which also contain migmatites and granites; they also include older pseudotachylite and ultramylonite rocks (both of which can be formed by collapses) and which acted as a sliding plane for the Tsergo Ri collapse.

Geographic entities mentioned:
surface_form: tsergo ri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.212777777777777
lon: 85.6
surface_form: tsergo ri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.2132408
lon: 85.6004521
Rocks formed by deformation, intrusions of granite, and layers of pyrrhotite ore, which are unstable under mechanical load and neotectonic faults, may have been weak structures that facilitated the collapse. The Tsergo Ri region is one of the fastest uplifting parts of the Himalaya.

Geographic entities mentioned:
surface_form: tsergo ri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.212777777777777
lon: 85.6
surface_form: tsergo ri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.2132408
lon: 85.6004521
The Tsergo Ri region is one of the fastest uplifting parts of the Himalaya. The Tsergo Ri landslide was probably triggered by seismic activity, perhaps on the Himalayan Main Central Thrust; a water level drop in the Paleo Kathmandu Lake took place at the same time and may have been caused by the same earthquake.

Geographic entities mentioned:
surface_form: tsergo ri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.212777777777777
lon: 85.6
surface_form: tsergo ri landslide
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.2132408
lon: 85.6004521
After the collapse, landslide debris was subject to glacial erosion and was largely removed in the process. About of debris is still present; it is found around Tsergo Ri mountain, which is formed by landslide debris and its location is in the central sector of the former landslide. Yala Peak and Dragpoche are in the area of the detachment, east of the seven-thousander Langtang Lirung.

Geographic entities mentioned:
surface_form: tsergo ri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.212777777777777
lon: 85.6
surface_form: tsergo ri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.2132408
lon: 85.6004521
Landslides take place to this day in the area, including during the 2015 Nepal earthquake when a landslide detached from Langtang Lirung peak and killed over 350 people in the Langtang valley. Slow mass movements into valleys and weather/monsoon-controlled mudflows also occur, and there is evidence that the debris from the Tsergo Ri landslide is especially unstable. Research history.

Geographic entities mentioned:
surface_form: tsergo ri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.212777777777777
lon: 85.6
surface_form: tsergo ri landslide
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.2132408
lon: 85.6004521
The nearest island is known as &quot;Rocky Island&quot;. The island is slightly north of the Tropic of Cancer, and its highest point is. History. Before the mid 270s [BCE] Ptolemaic activity along the African coast of the Red Sea had been limited with few significant results other than the discovery of the 'topaz' deposits on the island of Gazirat Zabarjad southeast of Ras Banas. ... 2.

Geographic entities mentioned:
surface_form: Ras Banas
instance_of: Landform
countries: Egypt
coordinates: lat: 23.90472222
lon: 35.78888889
It has a length of and covers an area of. The starting point of the Findel Glacier is on the Cima di Jazzi at above sea level, on the border between Switzerland and Italy. From there the glacier flows to the west between the Rimpfischhorn and Strahlhorn on the north and the Stockhorn on the south. The end of glacier tongue is located at above sea level.

Geographic entities mentioned:
surface_form: Cima di Jazzi
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.981083333333
lon: 7.8946944444444
It has a length of and covers an area of. The starting point of the Findel Glacier is on the Cima di Jazzi at above sea level, on the border between Switzerland and Italy. From there the glacier flows to the west between the Rimpfischhorn and Strahlhorn on the north and the Stockhorn on the south. The end of glacier tongue is located at above sea level.

Geographic entities mentioned:
surface_form: Rimpfischhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.023055555556
lon: 7.8838888888889
surface_form: Strahlhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.013222222222
lon: 7.90175
The recent disruption of the &quot;Status quo ante&quot; in the Kodori Valley in Abkhazia led to a further downturn in the already tensed Russian-Georgian relations. In July 2006, the Georgian police and security forces took control of the Kodori Valley, hitherto controlled by the local Georgian militias led by the defiant commander Emzar Kvitsiani.

Geographic entities mentioned:
surface_form: Kodori Valley
instance_of: Valley
countries: Georgia
coordinates: lat: 43.1
lon: 41.8
Emerged zone. In the emerged zone the region is washed by numerous rivers that include the Meta, Vichada and the Inirida rivers which contribute to other major rivers like the Orinoco River, Vaupés River, Caquetá River, Putumayo River and Apaporis River. This Llanos region is also divided into three subregions;
Northern plains.

Geographic entities mentioned:
surface_form: Apaporis River
instance_of: Watercourse
countries: Colombia
coordinates: lat: 1.1847222222222222
lon: -72.72694444444444
The area of the Bogotá Savanna and the highland of Cundinamarca and Boyacá tableland. To the northeast the volcanic metamorphic formed massif in Santander and Norte de Santander formed the Andes in Venezuela and the mountain ranges of Perijá and Motilones, between the border of Colombia and Venezuela during the Pleistocene and added sedimentary rocks during the Mesozoic.

Geographic entities mentioned:
surface_form: Motilones
instance_of: Mountain
countries: Colombia
Venezuela
coordinates: lat: 9.8028
lon: -72.9525
Neighbouring municipalities are Juupajoki, Mänttä-Vilppula, Orivesi, Tampere, Virrat and Ylöjärvi. The municipality is unilingually Finnish. Helvetinjärvi National Park is located in Ruovesi. The biggest lake in the area of the municipality, Lake Ruovesi, is a part of the Kokemäki River basin. The educational department takes part in Lifelong Learning Programme 2007–2013 in Finland.

Geographic entities mentioned:
surface_form: Lake Ruovesi
instance_of: Lake
countries: Finland
coordinates: lat: 62.004128
lon: 24.11047
Ipasha Falls. Ipasha Falls is a waterfall located in Glacier National Park, Montana, US. Ipasha Falls descends from Ipasha Glacier to Ipasha Lake and is recorded as having a drop of at least. Located in a remote region north of Many Glacier, the falls can only been seen by a multiday hike on established trails to Mokowanis Lake and then from there along unmaintained trails to Ipasha Lake.

Geographic entities mentioned:
surface_form: Ipasha Lake
instance_of: Lake
countries: United States
coordinates: lat: 48.8528
lon: -113.807
Ipasha Falls. Ipasha Falls is a waterfall located in Glacier National Park, Montana, US. Ipasha Falls descends from Ipasha Glacier to Ipasha Lake and is recorded as having a drop of at least. Located in a remote region north of Many Glacier, the falls can only been seen by a multiday hike on established trails to Mokowanis Lake and then from there along unmaintained trails to Ipasha Lake.

Geographic entities mentioned:
surface_form: Mokowanis Lake
instance_of: Lake
countries: United States
coordinates: lat: 48.8792
lon: -113.815
Lower Mount Bethel Township is a township in Northampton County, Pennsylvania, United States. The population of Lower Mount Bethel Township was 3,101 at the 2010 census. Lower Mount Bethel Township is part of the Lehigh Valley metropolitan area, which had a population of 861,899 and was the 68th-most populous metropolitan area in the U.S. as of the 2020 census. Geography. According to the U.S.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
or Jizo or as a masculine Benzaiten. He is sometimes seen as having a close relationship with Shuten-dōji. This is emphasized with his link to white monkeys, the shinshi of Mount Hiei. His name is derived from a group of ten Buddhist monks, which was a prominent institution in the Heian period, but declined by the time his worship began. It means &quot;Ten Masters of Practice&quot;. History.

Geographic entities mentioned:
surface_form: Mount Hiei
instance_of: Mountain
countries: Japan
coordinates: lat: 35.066666666667
lon: 135.83833333333
History. Tendai chroniclers like Kōshū have written about Jūzenji. They keep his complex nature in their writings. They avoid simplifying him into just a symbol. The &quot;Sange yōryakki&quot;, written by Gigen during the Kamakura period tells of Saichō's first climb on Mount Hiei in 785. There, Saichō met a divine youth. This youth called himself the deity of destiny.

Geographic entities mentioned:
surface_form: Mount Hiei
instance_of: Mountain
countries: Japan
coordinates: lat: 35.066666666667
lon: 135.83833333333
A small monkey is climbing stairs towards him. Jizō is above him in a golden circle. The background shows rocks, trees, and seven stars. These stars represent the seven upper Hie shrines. Monks from Mount Hiei mostly worshipped this form. Recently, images of Jūzenji as a youth have been found. There are a few examples. They show Jūzenji with similar features to Jizo.

Geographic entities mentioned:
surface_form: Mount Hiei
instance_of: Mountain
countries: Japan
coordinates: lat: 35.066666666667
lon: 135.83833333333
Excavations at the Bnot Ya'akov Bridge site, located along the Dead Sea rift in the southern Hula Valley of northern Israel, have revealed evidence of human habitation in the area from as early as 750,000 years ago.

Geographic entities mentioned:
surface_form: Hula Valley
instance_of: Valley
countries: Israel
coordinates: lat: 33.103333333333
lon: 35.609166666667
Kennebecasis Island. Kennebecasis Island (also called McCormick's Island) is a small Canadian island located in the Province of New Brunswick at the confluence of the Saint John River and Kennebecasis River. Its proximity to the city of Saint John has resulted in a seasonal community of about 100 cottages, as well as a 3-hole golf course and tennis court being established.

Geographic entities mentioned:
surface_form: Kennebecasis River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.31666667
lon: -66.13333333
Tibetan was defeated in the battle. Two years later, Tibetan was defeated by a chinese general, Wang Xiaojie near Qinghai Lake, Gungton and Ashina Tuizi had to flee back to Tibet. The young king, Tridu Songtsen, had realised that members of the Gar family had become independent warlords and posed a threat to the central authority of the king for a long time.

Geographic entities mentioned:
surface_form: Qinghai Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 37
lon: 100
&quot;Julattenius lawrencei&quot; is a species of schizomid arachnids (commonly known as sprickets or short-tailed whip-scorpions) in the Hubbardiidae family. It is endemic to Australia. It was described in 1992 by Australian arachnologist Mark Harvey. Distribution and habitat. The species occurs in Far North Queensland. The type locality is Julatten, at the eastern edge of the Atherton Tableland.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Illicium kinabaluensis. &quot;Illicium kinabaluensis&quot; is a species of tree in the family Schisandraceae, or alternately, the Illiciaceae. It is endemic to Mount Kinabalu, the tallest mountain on Borneo. It grows in forests at an elevation of 1200 to 2000 meters.

Geographic entities mentioned:
surface_form: Mount Kinabalu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 6.075
lon: 116.5586111111111
Flat Creek (James River tributary). Flat Creek is a stream in Barry and Stone counties of southern Missouri. It is a tributary of the James River. The stream source is north of Washburn and the confluence is with the James River arm of Table Rock Lake north of Cape Fair. From its headwaters near Washburn, the stream flows northeast parallel to Missouri Route 37 passing through southeast Cassville.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.083333333333
lon: -88.933333333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 46.427189
lon: -94.473618
surface_form: table rock
instance_of: Mountain
countries: United States
coordinates: lat: 35.890833333333
lon: -81.882777777778
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.328055555556
lon: -74.590833333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 44.276111111111
lon: -95.935555555556
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 45.170555555556
lon: -94.0125
The stream course begins to meander turning east and passing under Missouri Route 39 north of Cato. It meanders east passing into Stone County to enter the James River arm of Table Rock Lake after passing under Missouri Route 173 north of Cape Fair. Flat Creek was so named on account of flat terrain near its course in the vicinity of Cassville.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.083333333333
lon: -88.933333333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 46.427189
lon: -94.473618
surface_form: table rock
instance_of: Mountain
countries: United States
coordinates: lat: 35.890833333333
lon: -81.882777777778
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.328055555556
lon: -74.590833333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 44.276111111111
lon: -95.935555555556
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 45.170555555556
lon: -94.0125
Flat Creek (James River tributary). Flat Creek is a stream in Barry and Stone counties of southern Missouri. It is a tributary of the James River. The stream source is north of Washburn and the confluence is with the James River arm of Table Rock Lake north of Cape Fair. From its headwaters near Washburn, the stream flows northeast parallel to Missouri Route 37 passing through southeast Cassville.

Geographic entities mentioned:
surface_form: flat creek (james river tributary)
instance_of: Watercourse
countries: United States
coordinates: lat: 36.74305556
lon: -93.50666667
Flat Creek (James River tributary). Flat Creek is a stream in Barry and Stone counties of southern Missouri. It is a tributary of the James River. The stream source is north of Washburn and the confluence is with the James River arm of Table Rock Lake north of Cape Fair. From its headwaters near Washburn, the stream flows northeast parallel to Missouri Route 37 passing through southeast Cassville.

Geographic entities mentioned:
surface_form: flat creek
instance_of: Watercourse
countries: United States
coordinates: lat: 36.74305556
lon: -93.50666667
From its headwaters near Washburn, the stream flows northeast parallel to Missouri Route 37 passing through southeast Cassville. It continues to the northeast until meeting Little Flat Creek south of McDowell. The stream then flows to the southeast past Jenkins and under Missouri Route 248. The stream course begins to meander turning east and passing under Missouri Route 39 north of Cato.

Geographic entities mentioned:
surface_form: flat creek
instance_of: Watercourse
countries: United States
coordinates: lat: 36.74305556
lon: -93.50666667
The stream course begins to meander turning east and passing under Missouri Route 39 north of Cato. It meanders east passing into Stone County to enter the James River arm of Table Rock Lake after passing under Missouri Route 173 north of Cape Fair. Flat Creek was so named on account of flat terrain near its course in the vicinity of Cassville.

Geographic entities mentioned:
surface_form: flat creek
instance_of: Watercourse
countries: United States
coordinates: lat: 36.74305556
lon: -93.50666667
In Israel, seven cases of decapitation have been discovered, all dating to the Roman period and involving Jewish individuals. An additional case, uncovered in Jerusalem, appears to date from the early 1st century BCE and may be linked to the Judean Civil War during the reign of Alexander Jannaeus. France.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
This method dates back 5000 years. Armenian-American cookbook author Rose Baboian explains that Armenian cheesemaking techniques date back to an era before refrigeration was widely available so cheeses had to be preserved in brine solution. In Musa Dagh, traditional cheese was made from curds called &quot;choukalig&quot;.

Geographic entities mentioned:
surface_form: Musa Dagh
instance_of: Mountain
countries: Turkey
coordinates: lat: 36.258333333333
lon: 35.903611111111
Anoushabur () is a traditional Armenian sweet porridge, whose name means “sweet soup”, or “sweet porridge” (from անուշ = sweet and ապուր = soup). According to tradition, it was made when Noah’s family, after the ark had rested on Mount Ararat, cooked remaining grains and dried fruits into a pudding to celebrate.

Geographic entities mentioned:
surface_form: Mount Ararat
instance_of: Mountain
countries: Turkey
coordinates: lat: 39.70194444444444
lon: 44.29833333333333
The trout from Lake Sevan is called &quot;ishkhan&quot; and can be prepared different ways including a filled version stuffed with dried fruits (prunes, damsons, or apricots) and a poached version marinated with red peppers. &quot;Ishkhan&quot; is also sometimes served in a walnut sauce. For a relatively land-locked country, Armenian cuisine includes a surprising number of fish dishes.

Geographic entities mentioned:
surface_form: Lake Sevan
instance_of: Lake
countries: Armenia
coordinates: lat: 40.310555555556
lon: 45.349166666667
In 1949, Dilijan and Jermuk mineral water factories were put into operation. In 1960–1980 “Sevan”, “Hankavan”, “Lichk”, “Bjni”, “Lori”, “Arpi”, “Ararat”, mineral water bottling plants and factories were launched, which are involved in the production unit &quot;mineral water of Armenia&quot;. ASSR in 1985 produced 295 million bottles of mineral water.

Geographic entities mentioned:
surface_form: Sevan
instance_of: Lake
countries: Armenia
coordinates: lat: 40.310555555556
lon: 45.349166666667
Youth. Lemuel Roberts was born 1751 in Canaan, Connecticut, to Lemuel Roberts and Lydia (Purchase) Roberts. He moved with his family to Stillwater at the age of 10. He left home in 1768 to manufacture staves with a brother on Grand Isle in Lake Champlain. The following year he helped his father clear a farm in Charlemont, Massachusetts. Revolutionary War.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Roberts became an assistant to Colonel Herrick through the Battles of Saratoga; because Allen was unable to offer him compensation. Colonel Herrick commissioned Roberts a lieutenant for a scouting expedition on 12 January 1778 to determine the status of British loyalist positions on Lake Champlain.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Lucas Valley. Lucas Valley is a valley in Marin County, California, drained to the east into San Pablo Bay by Miller Creek, as well as an unincorporated community in the valley, which forms part of the Lucas Valley-Marinwood CDP. Lucas Valley Road traverses the length of the valley, linking it to Gallinas Valley to the east and Nicasio Valley to the west.

Geographic entities mentioned:
surface_form: Gallinas Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.0275
lon: -122.567
Donga River. The Donga River is a river in Nigeria and Cameroon. The river arises from the Mambilla Plateau in Eastern Nigeria, forms part of the international border between Nigeria and Cameroon, and flows northwest to eventually merge with the Benue River in Nigeria. The Donga watershed is in area. At its peak, near the Benue the river delivers of water per second.

Geographic entities mentioned:
surface_form: Benue River
instance_of: Watercourse
countries: Cameroon
Nigeria
coordinates: lat: 7.783333
lon: 6.766667
The Donga watershed is in area. At its peak, near the Benue the river delivers of water per second. In Taraba State, Nigeria, there are three forest reserves, Baissa, Amboi and Bissaula River, in the Donga river basin. They lie on the slopes and at the foot of the Mambilla Plateau, south-west of Gashaka Gumti National Park. Pollution.

Geographic entities mentioned:
surface_form: Benue
instance_of: Watercourse
countries: Cameroon
Nigeria
coordinates: lat: 7.783333
lon: 6.766667
Donga River. The Donga River is a river in Nigeria and Cameroon. The river arises from the Mambilla Plateau in Eastern Nigeria, forms part of the international border between Nigeria and Cameroon, and flows northwest to eventually merge with the Benue River in Nigeria. The Donga watershed is in area. At its peak, near the Benue the river delivers of water per second.

Geographic entities mentioned:
surface_form: donga
instance_of: Watercourse
countries: Cameroon
Nigeria
coordinates: lat: 8.3132636
lon: 9.9642313
The Donga watershed is in area. At its peak, near the Benue the river delivers of water per second. In Taraba State, Nigeria, there are three forest reserves, Baissa, Amboi and Bissaula River, in the Donga river basin. They lie on the slopes and at the foot of the Mambilla Plateau, south-west of Gashaka Gumti National Park. Pollution.

Geographic entities mentioned:
surface_form: donga
instance_of: Watercourse
countries: Cameroon
Nigeria
coordinates: lat: 8.3132636
lon: 9.9642313
They lie on the slopes and at the foot of the Mambilla Plateau, south-west of Gashaka Gumti National Park. Pollution. Research reveals that pesticides were the predominant organic pollutant in the Donga river. Climate. The annual average temperature is around 33°C but high level of cold in January and an increased rainfall in August. Rainfal percentage is 40.35% with 54.98% relative humidity.

Geographic entities mentioned:
surface_form: donga
instance_of: Watercourse
countries: Cameroon
Nigeria
coordinates: lat: 8.3132636
lon: 9.9642313
Between many mountain ranges are several rich river valleys. The Big Hole Valley, Bitterroot Valley, Gallatin Valley, Flathead Valley, and Paradise Valley have extensive agricultural resources and multiple opportunities for tourism and recreation.

Geographic entities mentioned:
surface_form: Bitterroot Valley
instance_of: Valley
countries: United States
coordinates: lat: 46.247
lon: -114.16
M. Keck Observatory are located on Mauna Kea. In addition, she is identified with Papa, the goddess of the earth and wife of Wākea (space), which, at the time, seemed appropriate because Haumea was thought to be composed almost entirely of solid rock, without the thick ice mantle over a small rocky core typical of other known Kuiper belt objects.

Geographic entities mentioned:
surface_form: Mauna Kea
instance_of: Mountain
countries: United States
coordinates: lat: 19.820555555555554
lon: -155.46805555555557
They trekked for a total of 85 days, including four days with no water, before returning to York. Lake Lefroy was named by the explorer Charles Cooke Hunt in 1864 after Lefroy, who would have seen the lake during his visit. Lefroy retired from his position as Superintendent of Convicts in 1875, and died in Fremantle on 18 July 1879 of pneumonia. He was buried at Karrakatta Cemetery.

Geographic entities mentioned:
surface_form: Lake Lefroy
instance_of: Lake
countries: Australia
coordinates: lat: -31.3
lon: 121.7
It was known as &quot;Region A&quot; in ground-based images taken by the W. M. Keck Observatory on Mauna Kea. The crater was named after Occator, the Roman god of the harrow and a helper to Ceres. The name Occator was officially approved by the IAU on 3 July 2015.

Geographic entities mentioned:
surface_form: Mauna Kea
instance_of: Mountain
countries: United States
coordinates: lat: 19.820555555555554
lon: -155.46805555555557
Some of her early works, created during her studies at the Academy, had a strong existential subtext (&quot;Birds&quot;, 1998, &quot;Eye&quot;, 1999, &quot;Ark of the Covenant&quot;, 2000, &quot;Lamp&quot;, 2002), but Paulina Skavová also adopted her professor's distinctive ironic detachment and unkind humour, creating the installation &quot;Monument on Mount Blaník&quot; (2002), conceived as a persiflage of national myth, and the installation &quot;Bank Robbery&quot; (2002), as a training ground for bank robbers.

Geographic entities mentioned:
surface_form: Blaník
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.642222222222
lon: 14.872777777778
Seebergsee. Seebergsee is a lake in the canton of Bern, Switzerland. Its surface area is.

Geographic entities mentioned:
surface_form: seebergsee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.577222222222
lon: 7.4430555555556
The other passengers and Albert were all pinned beneath the plane. It took several diving attempts to pull the men from the plane. The accident happened about forty miles east of Pensacola near Camp Walton on the Santa Rosa sound. The &quot;Falcon&quot; was Whitted's pride and joy, having been designed and built by him. He had still been making changes to its design a short time before its crash.

Geographic entities mentioned:
surface_form: Santa Rosa sound
instance_of: Landform
countries: United States
coordinates: lat: 30.4019171
lon: -86.7768273
The mountain sits about south of the village of Fossbergom and about southwest of the village of Vågåmo. The mountain is surrounded by several other notable mountains including Surtningssue to the northeast; Blåbreahøe to the north; Memurutindene to the northwest; Reinstinden, Hinnotefjellet, and Storådalshøe to the west; and Knutsholstinden to the south.

Geographic entities mentioned:
surface_form: Surtningssue
instance_of: Mountain
countries: Norway
coordinates: lat: 61.534166666667
lon: 8.5725
surface_form: Blåbreahøe
instance_of: Mountain
countries: Norway
coordinates: lat: 61.5442
lon: 8.55639
surface_form: Memurutindene
instance_of: Mountain
countries: Norway
coordinates: lat: 61.566666666667
lon: 8.4833333333333
surface_form: Hinnotefjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 61.51888889
lon: 8.45111111
surface_form: reinstinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.51707
lon: 8.49633
surface_form: storådalshøe
instance_of: Mountain
countries: Norway
coordinates: lat: 61.4873
lon: 8.4529
surface_form: memurutindene
instance_of: Mountain
countries: Norway
coordinates: lat: 61.5675
lon: 8.4880555555556
surface_form: knutsholstinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.43625
lon: 8.55491
surface_form: knutsholstinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.41841
lon: 8.57373
Raudhamran. Raudhamran is a mountain in Lom Municipality in Innlandet county, Norway. The tall mountain is located in the Jotunheimen mountains within Jotunheimen National Park. The mountain sits about south of the village of Fossbergom and about southwest of the village of Vågåmo.

Geographic entities mentioned:
surface_form: raudhamran
instance_of: Mountain
countries: Norway
coordinates: lat: 61.51206
lon: 8.55726
Darton Peak. Darton Peak () is located in the Bighorn Mountains in the U.S. state of Wyoming. The peak is the eighth-highest in the range and it is in the Cloud Peak Wilderness of Bighorn National Forest. Darton Peak is north of Bighorn Peak and southeast of Mather Peaks.

Geographic entities mentioned:
surface_form: Bighorn Peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.2544
lon: -107.107
surface_form: Mather Peaks
instance_of: Mountain
countries: United States
coordinates: lat: 44.3242
lon: -107.147
surface_form: darton peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.2761
lon: -107.109
Darton Peak. Darton Peak () is located in the Bighorn Mountains in the U.S. state of Wyoming. The peak is the eighth-highest in the range and it is in the Cloud Peak Wilderness of Bighorn National Forest. Darton Peak is north of Bighorn Peak and southeast of Mather Peaks.

Geographic entities mentioned:
surface_form: cloud peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.382138888889
lon: -107.17391388889
Darton Peak. Darton Peak () is located in the Bighorn Mountains in the U.S. state of Wyoming. The peak is the eighth-highest in the range and it is in the Cloud Peak Wilderness of Bighorn National Forest. Darton Peak is north of Bighorn Peak and southeast of Mather Peaks.

Geographic entities mentioned:
surface_form: darton peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.2761
lon: -107.109
As such, it does not usually occur together with &quot;Sphagnum&quot; which tends to grow slightly more inland. Localities where the plant is found include, from north to south; Queulat National Park, Chonos Archipelago, Taitao Peninsula, San Rafael Lake, the vicinities of Caleta Tortel and Tierra del Fuego National Park.

Geographic entities mentioned:
surface_form: San Rafael Lake
instance_of: Lake
countries: Chile
coordinates: lat: -46.666666666667
lon: -73.933333333333
Längenbühl. Längenbühl is a village in the canton of Bern, Switzerland. The former municipality of the district of Thun merged with Forst on January 1, 2007 to form Forst-Längenbühl. There are three smaller lakes in Längenbühl: Dittligsee, Geistsee and a smaller pond.

Geographic entities mentioned:
surface_form: Dittligsee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.756111111111
lon: 7.5336111111111
surface_form: Geistsee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.761388888889
lon: 7.5344444444444
The ridge is part of the Ridge and Valley Appalachians. Description. White Oak Mountain is one of a series of paralleling ridges running approximately north-northeast in the Tennessee Valley between the Cumberland Plateau/Mountains to the west and the Blue Ridge Mountains to the east. The ridge averages 1,368 feet above sea level, the highest point being 1,495 feet.

Geographic entities mentioned:
surface_form: Tennessee Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
surface_form: Blue Ridge Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.08166667
lon: -77.86222222
surface_form: oak mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.647272
lon: -90.627068
surface_form: oak mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.205833333333
lon: -74.729166666667
surface_form: white oak mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.149166666666666
lon: -85.02388888888889
surface_form: tennessee valley
instance_of: Valley
countries: United States
coordinates: lat: 37.8611
lon: -122.534
surface_form: oak mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.515833333333
lon: -116.97722222222
North of Ooltewah, the Hamilton-Bradley County line follows the westernmost part of the rudge. Southwest of Cleveland, I-75 crosses the ridge in an artificially cut gap. West of Cleveland, SR 312 crosses the ridge in Mahan Gap. The ridge ends just south of the community of Georgetown.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
The ridge averages 1,368 feet above sea level, the highest point being 1,495 feet. The ridge begins on the north side of Ringgold Gap, the site of an 1863 Civil War battle, in Catoosa County just east of Ringgold. Interstate 75, US 41/76, and a CSX Railroad run through this gap. The ridge continues to the south as Taylor Ridge, although it is part of the same geologic formation.

Geographic entities mentioned:
surface_form: battle
instance_of: Watercourse
countries: United States
coordinates: lat: 44.9266
lon: -93.0291
Interstate 75, US 41/76, and a CSX Railroad run through this gap. The ridge continues to the south as Taylor Ridge, although it is part of the same geologic formation. The ridge has several gaps through which major highways run, including (from south to north) SR 320 near East Brainerd, Standifer Gap Road, SR 317 near Collegedale, and US 11/64 near Ooltewah in Dead Man's Gap.

Geographic entities mentioned:
surface_form: taylor ridge
instance_of: Mountain
countries: United States
coordinates: lat: 34.4469
lon: -85.3158
Interstate 75, US 41/76, and a CSX Railroad run through this gap. The ridge continues to the south as Taylor Ridge, although it is part of the same geologic formation. The ridge has several gaps through which major highways run, including (from south to north) SR 320 near East Brainerd, Standifer Gap Road, SR 317 near Collegedale, and US 11/64 near Ooltewah in Dead Man's Gap.

Geographic entities mentioned:
surface_form: dead
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
White Oak Mountain. White Oak Mountain is a ridge located in northwestern Georgia and southeastern Tennessee. The ridge is part of the Ridge and Valley Appalachians. Description. White Oak Mountain is one of a series of paralleling ridges running approximately north-northeast in the Tennessee Valley between the Cumberland Plateau/Mountains to the west and the Blue Ridge Mountains to the east.

Geographic entities mentioned:
surface_form: oak mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.647272
lon: -90.627068
surface_form: oak mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.205833333333
lon: -74.729166666667
surface_form: white oak mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.149166666666666
lon: -85.02388888888889
surface_form: oak mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.515833333333
lon: -116.97722222222
The playwright delivered the libretto to Zillig in April 1936, before committing suicide in October of the same year. The libretto of &quot;Das Opfer&quot; has drawn notoriety because the chorus members dress as penguins for much of the opera, even though penguins do not inhabit the polar plateau where the action is set.

Geographic entities mentioned:
surface_form: polar plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
Athenae (Boeotia). Athenae or Athenai () was a town of ancient Boeotia, on the river Triton, and near Lake Copais. Athenae, along with the neighbouring town of Eleusis, was destroyed by an inundation.

Geographic entities mentioned:
surface_form: Lake Copais
instance_of: Lake
countries: Greece
coordinates: lat: 38.45
lon: 23.05
The Atlungstad Distillery was established in Stange in 1855. Geography. The municipality is situated on the east side of the lake Mjøsa. It borders Hamar Municipality to the north; Løten Municipality, Våler Municipality, and Åsnes Municipality to the east; Nord-Odal Municipality to the south; and Eidsvoll Municipality (in Akershus county) to the west.

Geographic entities mentioned:
surface_form: Mjøsa
instance_of: Lake
countries: Norway
coordinates: lat: 60.666666666667
lon: 11
Their return was delayed one day past their deadline due to blizzard conditions on their return which slowed their progress. During their trek the group explored the Mertz and Ninnis glaciers, travelled over dangerous stretches of coastal ice and glaciers, climbed Aurora Peak and reached Horn Bluff. They kept detailed records of geological features and mapped the environment as they travelled.

Geographic entities mentioned:
surface_form: Aurora Peak
instance_of: Mountain
coordinates: lat: -67.383333333333
lon: 144.2
Correll left the main base on SY &quot;Aurora&quot; in February 1913 along with most of the expedition, while a smaller group stayed behind awaiting the return of the Far Eastern Party (comprising Mawson, Xavier Mertz and Belgrave Edward Sutton Ninnis). During the return trip, he acted as colour photographer. He returned to Adelaide in March 1913. Correll Nunatak is named after him.

Geographic entities mentioned:
surface_form: Correll Nunatak
instance_of: Mountain
coordinates: lat: -67.5833
lon: 144.233
Less than 4% of the city's land is zoned commercial, largely concentrated in one location, and there are no industrial areas. The city is situated at the northwest end of Lake Washington along State Route 522, which provides connections to Seattle and Bothell. Lake Forest Park includes several parks and nature reserves, access to the Burke–Gilman Trail, and organized summer events.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Until 1914 and completion of the Red Brick Road (now Bothell Way, part of State Route 522) to nearby Kenmore and Bothell, it also marked the literal end of improved roads heading north from Seattle, with the best access to points further north and east being by boat across Lake Washington or the Seattle, Lake Shore and Eastern Railway.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Lake Forest Park Town Center is also home to a branch of the King County Library System, Third Place Books, and Third Place Commons community center. Geography. Lake Forest Park is situated at the north end of Lake Washington. The city's southern boundary begins at the city limit of Seattle.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
The garbhagriha is in the form of moat. The Goddess is also known as Alankaravalli. Specialities. Nemam is on the southern banks of Cauvery. This place was known as Parijatha Vanam in Kirutha Yuga, Beemesvaram in Treta Yuga, Indira Vanam in the Dvapara Yuga and Iravathesvaram the Kali Yuga. Brahma, Indra, Rambai and Iravatham worshipped the presiding deity of the temple.

Geographic entities mentioned:
surface_form: Cauvery
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Cowichan Lake. Cowichan Lake is a large freshwater lake located on southern Vancouver Island, British Columbia, Canada. It is located along the Cowichan Valley in the Cowichan Valley Regional District, with its eastern shore about west of Duncan, British Columbia. Cowichan Lake is about in length, running mostly from west to east, and is about wide at its widest point.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: cowichan lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.875
lon: -124.26
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Cowichan Lake. Cowichan Lake is a large freshwater lake located on southern Vancouver Island, British Columbia, Canada. It is located along the Cowichan Valley in the Cowichan Valley Regional District, with its eastern shore about west of Duncan, British Columbia. Cowichan Lake is about in length, running mostly from west to east, and is about wide at its widest point.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Along the south side of the lake are the communities of Mesachie Lake and Honeymoon Bay, and also Gordon Bay Provincial Park. On the north shore is the community of Youbou. The Cowichan Valley was once a thriving lumber centre in British Columbia. In the past, two major railroads had spur lines to and around parts of the lake.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Cowichan Lake. Cowichan Lake is a large freshwater lake located on southern Vancouver Island, British Columbia, Canada. It is located along the Cowichan Valley in the Cowichan Valley Regional District, with its eastern shore about west of Duncan, British Columbia. Cowichan Lake is about in length, running mostly from west to east, and is about wide at its widest point.

Geographic entities mentioned:
surface_form: cowichan lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.875
lon: -124.26