Sarmila/GeoWiki-Features huggingface dataset:
Musala. Musala (); from Arabic through Ottoman Turkish: from &quot;Musalla&quot;, &quot;near God&quot; or &quot;place for prayer&quot; is the highest peak in the Rila Mountains, as well as in Bulgaria and the entire Balkan Peninsula, standing at. With a topographic prominence of, Musala is also the 6th highest peak by topographic prominence in mainland Europe.

Geographic entities mentioned:
surface_form: musala
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.179167
lon: 23.585278
surface_form: musalla
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.179167
lon: 23.585278
The station conducted scientific experiments using a muon telescope. The station was destroyed by an electrical fire on October 29, 1983. With an average annual temperature of -2.2 °C, Musala is the coldest place in Bulgaria and the entire Balkan Peninsula. Temperatures stay below 0 °C for about 8 months each year.

Geographic entities mentioned:
surface_form: musala
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.179167
lon: 23.585278
Temperatures stay below 0 °C for about 8 months each year. Due to this, about 45% of the annual precipitation on Musala is snow, and snow cover lasts for about 200 days (more than six months). Three of the main rivers of Bulgaria, the Iskar, Maritsa and Mesta have their sources near Musala. The next highest peaks in the vicinity of Musala are Malka (Little) Musala () and Irechek (). Climate.

Geographic entities mentioned:
surface_form: musala
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.179167
lon: 23.585278
Temperatures stay below 0 °C for about 8 months each year. Due to this, about 45% of the annual precipitation on Musala is snow, and snow cover lasts for about 200 days (more than six months). Three of the main rivers of Bulgaria, the Iskar, Maritsa and Mesta have their sources near Musala. The next highest peaks in the vicinity of Musala are Malka (Little) Musala () and Irechek (). Climate.

Geographic entities mentioned:
surface_form: musala
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.179167
lon: 23.585278
surface_form: musala
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.179167
lon: 23.585278
surface_form: musala
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.179167
lon: 23.585278
The summer season only lasts for 2 months, and snowfalls are possible. For the period 1931–2013, the highest recorded temperature was, and the lowest -. The average annual temperature is, which makes the peak the coldest place in Bulgaria. Namesakes. Musala Glacier on Greenwich Island in the South Shetland Islands, Antarctica is named after Musala Peak.

Geographic entities mentioned:
surface_form: musala
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.179167
lon: 23.585278
Vall de Núria (ski resort). Vall de Núria is a ski resort located in the Núria valley, in Catalonia. The ski area extends from 1,964 to 2,252 metres. The resort has a total of ten alpine ski trails (three green, three blue, two red and two black) and a special track for sleds. In total, seven km of marked trails. In the summer of 2006 there were 18 new snow cannons installed.

Geographic entities mentioned:
surface_form: Núria valley
instance_of: Valley
countries: Spain
coordinates: lat: 42.4
lon: 2.15
Cap Canaille. Cap Canaille () is a headland in Calanques National Park in the Bouches-du-Rhône department in Southern France, on the Mediterranean coast between the towns of Cassis and La Ciotat. It is about 27 km (16 mi) southeast of the city centre of Marseille. At, it is the highest sea cliff of France. The rock face of Cap Canaille is called &quot;Falaises de Soubeyrannes&quot;.

Geographic entities mentioned:
surface_form: cap canaille
instance_of: Mountain
countries: France
coordinates: lat: 43.194696
lon: 5.549426
It is about 27 km (16 mi) southeast of the city centre of Marseille. At, it is the highest sea cliff of France. The rock face of Cap Canaille is called &quot;Falaises de Soubeyrannes&quot;. The rock consists of layers of ochre-coloured sandstone, conglomerate and limestone from the Turonian age on top of grey marl from the Cenomanian until the Turonian age.

Geographic entities mentioned:
surface_form: cap canaille
instance_of: Mountain
countries: France
coordinates: lat: 43.194696
lon: 5.549426
surface_form: the rock
instance_of: Mountain
countries: France
coordinates: lat: 10.29236
lon: -109.20762983333333
surface_form: the rock
instance_of: Mountain
countries: France
coordinates: lat: 10.29236
lon: -109.20762983333333
The rock consists of layers of ochre-coloured sandstone, conglomerate and limestone from the Turonian age on top of grey marl from the Cenomanian until the Turonian age. The Corniche des Crêtes scenic road runs over the top of the cliff. The name in Provençal is &quot;Cap Naio&quot;. It has been misunderstood in French and changed into Cap Canaille instead of &quot;Cap Naille&quot;.

Geographic entities mentioned:
surface_form: cap canaille
instance_of: Mountain
countries: France
coordinates: lat: 43.194696
lon: 5.549426
The &quot;Dkhw’Duw’Absh&quot; and &quot;Xacuabš&quot;
(&quot;People of the Inside&quot; and &quot;People of the Large Lake&quot;, now the Duwamish tribe) of the Lushootseed (Whulshootseed, Skagit-Nisqually) Coast Salish nations inhabited at least 17 villages in the mid-1850s, living in some 93 permanent longhouses (khwaac'ál'al) along Elliott Bay, Salmon Bay, Portage Bay, Lake Washington, Lake Sammamish, and the Duwamish, Black, and Cedar rivers.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: Lake Sammamish
instance_of: Lake
countries: United States
coordinates: lat: 47.61638888888889
lon: -122.08944444444444
Nova Scotia Route 212. Route 212 is a collector road in the Canadian province of Nova Scotia. It is located in the Halifax Regional Municipality and connects Enfield at Exit 5 on Highway 102 with Route 357 at Elderbank in the Musquodoboit Valley. The route is known as the &quot;Old Guysborough Road&quot; as it was the colonial military road from Halifax to Guysborough.

Geographic entities mentioned:
surface_form: Musquodoboit Valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.0167
lon: -63.1833
Lake Tekapo (town). Lake Tekapo (often known simply as Tekapo () to avoid confusion with the lake itself) is a small township located at the southern end of the lake of the same name in the inland South Island of New Zealand. It had 558 residents according to the 2018 census, being one of five settlements in the sparsely populated Mackenzie Basin.

Geographic entities mentioned:
surface_form: lake of the same name
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.9
lon: 170.525
The lake is a popular tourist destination, and several resort hotels are located at the township. Lake Tekapo Airport is located west of the town where local tourism operator Air Safaris is based. Twizel lies 60 km (39 minutes drive) south of Lake Tekapo via Lake Pukaki and Burkes Pass lies 21 km (15 minutes drive) west along State Highway 8. History.

Geographic entities mentioned:
surface_form: Lake Pukaki
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.116666666667
lon: 170.16666666667
Also &quot;Phaeoisaria ellipsoidea&quot; and &quot;Sterigmatobotrys rudis&quot; which have been found in submerged decaying wood in Manfeilong reservoir in Xishuangbanna, Yunnan Province, China. Also &quot;Neomonodictys aquatica&quot; was collected from submerged decaying wood in Erhai Lake, Yunnan Province, China.

Geographic entities mentioned:
surface_form: Erhai Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 25.763333333333
lon: 100.1875
Inape biremis. &quot;Inape biremis&quot; is a species of moth of the family Tortricidae which is endemic to Colombia where it can be found on Nevado del Tolima.

Geographic entities mentioned:
surface_form: Nevado del Tolima
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.6666666666667
lon: -75.333333333333
It lies in the La Paz Department, Ingavi Province, Jesús de Machaca Municipality. Pukara is situated west of the mountain Q'ullq'uni and north-west of the mountains Wisk'achani and Jisk'a Sallalla. The Q'ullq'uni River &quot;(Khullkuni)&quot; flows along its slopes. It flows to the south as a tributary of Jach'a Jawira.

Geographic entities mentioned:
surface_form: Q'ullq'uni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.7253
lon: -68.5581
surface_form: Jisk'a Sallalla
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.7419
lon: -68.5664
surface_form: q'ullq'uni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.7253
lon: -68.5581
surface_form: q'ullq'uni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.7253
lon: -68.5581
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.0397
lon: -67.3411
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.24444444
lon: -67.69694444
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.28833333
lon: -66.52972222
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6408
lon: -67.7108
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.2631
lon: -66.8253
surface_form: jisk'a sallalla
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.7419
lon: -68.5664
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.09388889
lon: -67.69277778
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.48055556
lon: -66.41166667
Pukara (Jesús de Machaca). Pukara (Aymara for fortress, Hispanicized spelling &quot;Pucara&quot;) is a mountain in the Chilla-Kimsa Chata mountain range in the Andes of Bolivia. It lies in the La Paz Department, Ingavi Province, Jesús de Machaca Municipality. Pukara is situated west of the mountain Q'ullq'uni and north-west of the mountains Wisk'achani and Jisk'a Sallalla.

Geographic entities mentioned:
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.7944
lon: -68.9267
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.95138931
lon: -67.91166687
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.72972222
lon: -65.88138889
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6136
lon: -68.7567
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.30416667
lon: -66.95361111
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.28472222
lon: -67.985
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.73888889
lon: -65.78333333
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.95833333
lon: -68.01388889
surface_form: pukara (jesús de machaca)
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.7261
lon: -68.5892
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.86055556
lon: -68.65444444
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.87416667
lon: -68.21083333
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.9394
lon: -68.5722
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.86444444
lon: -68.10694444
Pukara (Jesús de Machaca). Pukara (Aymara for fortress, Hispanicized spelling &quot;Pucara&quot;) is a mountain in the Chilla-Kimsa Chata mountain range in the Andes of Bolivia. It lies in the La Paz Department, Ingavi Province, Jesús de Machaca Municipality. Pukara is situated west of the mountain Q'ullq'uni and north-west of the mountains Wisk'achani and Jisk'a Sallalla.

Geographic entities mentioned:
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.7944
lon: -68.9267
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.1058
lon: -68.3858
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.95138931
lon: -67.91166687
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.72972222
lon: -65.88138889
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.1214
lon: -68.3297
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.71666667
lon: -68.7
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6136
lon: -68.7567
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.30416667
lon: -66.95361111
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.28472222
lon: -67.985
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.73888889
lon: -65.78333333
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.95833333
lon: -68.01388889
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.10972222
lon: -67.66222222
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.7261
lon: -68.5892
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.86055556
lon: -68.65444444
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.87416667
lon: -68.21083333
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.88333333
lon: -68.85
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.9394
lon: -68.5722
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.86444444
lon: -68.10694444
Prince of Wales Glacier. Prince of Wales Glacier () is a glacier in the Queen Elizabeth Range, flowing generally north for about 10 nautical miles (18 km) between Hochstein and Kohmyr Ridges into Hamilton Glacier. Named by the northern party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1961–62) for Charles, Prince of Wales, eldest son of Elizabeth II of the United Kingdom.

Geographic entities mentioned:
surface_form: Hochstein
instance_of: Mountain
coordinates: lat: -82.75
lon: 159.78333333
Murder trial. Jayaraj helped the four killers who murdered Ramachandra and disposed of his bones in the Bay of Bengal. He arranged for dog bones to be buried instead, with an intention to mislead the investigation and exonerate the killers. Death. He was killed on 22 March 1986 by a four-member goonda team, supported by Jayaraj.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Its maximum elevation is about 645 m. Citadel Bastion lies next to Hodgson Lake. This mountain was mapped from trimetrogon air photography taken by the Ronne Antarctic Research Expedition, 1947–48, and from survey by the Falkland Islands Dependencies Survey, 1948–50.

Geographic entities mentioned:
surface_form: Hodgson Lake
instance_of: Lake
coordinates: lat: -72.016666666667
lon: -68.466666666667
surface_form: citadel bastion
instance_of: Landform
coordinates: lat: -72
lon: -68.5333
Quaternary Geology. Evidence shows that a thick ice sheet covered Citadel Bastion during the Last Glacial Maximum. Striated bedrock surfaces are found in the col on the south side of Citadel Bastion. The striations are best preserved at the edge of freshly exposed glacial tills. Striated bedrock has also been found on its slopes high as its summit.

Geographic entities mentioned:
surface_form: best
instance_of: Mountain
coordinates: lat: -66.8167
lon: 51.3833
Citadel Bastion. Citadel Bastion () is a rocky, flat-topped elevation at the south side of the terminus of Saturn Glacier, facing towards George VI Sound and the Rymill Coast, situated on the east side of Alexander Island, Antarctica. Its maximum elevation is about 645 m. Citadel Bastion lies next to Hodgson Lake.

Geographic entities mentioned:
surface_form: george
instance_of: Mountain
coordinates: lat: -67.71667
lon: 50
surface_form: citadel bastion
instance_of: Landform
coordinates: lat: -72
lon: -68.5333
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
Citadel Bastion. Citadel Bastion () is a rocky, flat-topped elevation at the south side of the terminus of Saturn Glacier, facing towards George VI Sound and the Rymill Coast, situated on the east side of Alexander Island, Antarctica. Its maximum elevation is about 645 m. Citadel Bastion lies next to Hodgson Lake.

Geographic entities mentioned:
surface_form: citadel bastion
instance_of: Landform
coordinates: lat: -72
lon: -68.5333
Geology. Citadel Bastion is one of a series of nunataks that provide outcrops of Cretaceous (Aptian–Albian) sedimentary rocks that comprise part of the 6.8 kilometer-thick Fossil Bluff Group, which underlies easternmost Alexander Island. These sedimentary rocks accumulated in shallow marine and terrestrial environments.

Geographic entities mentioned:
surface_form: citadel bastion
instance_of: Landform
coordinates: lat: -72
lon: -68.5333
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
These sedimentary rocks accumulated in shallow marine and terrestrial environments. The sedimentary rocks, which are exposed in Citadel Bastion and adjacent nunataks, consist of a 700 meter-thick sequence of laterally persistent beds of very fine to very coarse, rarely gravelly interbedded with occasional beds of sandstone (volcanic lithic arenite), mudstone, and conglomerate.

Geographic entities mentioned:
surface_form: citadel bastion
instance_of: Landform
coordinates: lat: -72
lon: -68.5333
The plant fossils consists mainly of coniferous plants (mainly podocarps). Fossils of Bennettitales, pteridophytes and liverworts, and to a lesser extent the angiosperms, are also common. Citadel Bastion is notable for bedrock outcrops that expose multiple fossil forests, which consist of upright standing trunks buried in place, and their associated paleosols.

Geographic entities mentioned:
surface_form: citadel bastion
instance_of: Landform
coordinates: lat: -72
lon: -68.5333
Citadel Bastion is notable for bedrock outcrops that expose multiple fossil forests, which consist of upright standing trunks buried in place, and their associated paleosols. The analysis of paleocurrent data from and the sedimentology of sedimentary rocks, which comprise Citadel Bastion and adjacent nunataks, found that these rocks accumulated as a large alluvial fan about 15 km in radius.

Geographic entities mentioned:
surface_form: citadel bastion
instance_of: Landform
coordinates: lat: -72
lon: -68.5333
Fossil plants found in these sedimentary rocks indicate that the palaeoclimate was warm and humid throughout the period of deposition despite their polar position. Quaternary Geology. Evidence shows that a thick ice sheet covered Citadel Bastion during the Last Glacial Maximum. Striated bedrock surfaces are found in the col on the south side of Citadel Bastion.

Geographic entities mentioned:
surface_form: citadel bastion
instance_of: Landform
coordinates: lat: -72
lon: -68.5333
Quaternary Geology. Evidence shows that a thick ice sheet covered Citadel Bastion during the Last Glacial Maximum. Striated bedrock surfaces are found in the col on the south side of Citadel Bastion. The striations are best preserved at the edge of freshly exposed glacial tills. Striated bedrock has also been found on its slopes high as its summit.

Geographic entities mentioned:
surface_form: citadel bastion
instance_of: Landform
coordinates: lat: -72
lon: -68.5333
Cosmogenic beryllium-10 isotope dating of a few of the erratics indicate that they were exposed by the thinning of the ice sheet after the Last Glacial Maximum. The erratics within the col were exposed by thinning ice sheet about 13,500 years ago. Those at the summit of Citadel Bastion were exposed by thinning ice sheet about 10,200 years ago.

Geographic entities mentioned:
surface_form: citadel bastion
instance_of: Landform
coordinates: lat: -72
lon: -68.5333
His relaxed mastery of figurative cartoon illustration, along with a superb ability for gutter dialogue, produced the kind of stories that we were always wishing for when reading Flash Gordon and Spider Man, but never got until Etienne/Stephen entered our lives.In 2006, historian Jack Fritscher wrote:&quot;If there is a gay Mount Rushmore of four great pioneer pop artists, the faces would be Chuck Arnett, Etienne, A.

Geographic entities mentioned:
surface_form: Mount Rushmore
instance_of: Mountain
countries: United States
coordinates: lat: 43.878947222222
lon: -103.459825
His works are still very popular among Slovenes. He became known for his role fostering the development of mountaineering in the Slovene Lands. By far his most well known construction is the Aljaž Tower (), built on the summit of Mount Triglav, the highest mountain of the Julian Alps and of Slovenia, which he purchased to secure the area for Slovene rather than German mountaineers.

Geographic entities mentioned:
surface_form: Triglav
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.378333
lon: 13.836667
It served as the primary highway to and from Hamlin Beach State Park prior to the construction of the Lake Ontario State Parkway. The southern terminus of the route was at an intersection with NY 360 east of the hamlet of Morton. Its northern terminus was at the park on the shore of Lake Ontario. The entirety of NY 215 was named Redman Road.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
North of Moscow Road, the fields on the highway's east side slowly gave way to forested areas as the route approached Hamlin Beach State Park and intersected Cook Road. The route terminated north of Cook Road at the southern boundary of Hamlin Beach State Park. The physical roadway continued into the park and to nearby Lake Ontario as a local highway. History.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
History. The portion of Redman Road north of modern NY 360 in Hamlin was a state highway as early as 1920; however, it was not assigned a designation until the early 1940s, when it became NY 215. At the time, it was the primary highway to and from Hamlin Beach State Park on the Lake Ontario shoreline, as no continuous east–west lakeside roadway existed at the time.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Banasura Dam is under the control of Padinjarathara KSEB Station. India's first operating floating solar power plant was established in Banasura Dam. The dam is surrounded by Banasura Hills. Dam impounds the Karamanathodu tributary of the Kabini River, is part of the Indian Banasurasagar Project consisting of a dam and a canal project started in 1979.

Geographic entities mentioned:
surface_form: Banasura Hill
instance_of: Mountain
countries: India
coordinates: lat: 11.69416667
lon: 75.90805556
It is the largest earthen dam in India and the second largest in Asia and a starting point for hikes into the surrounding mountains. It is an important tourist attraction. Banasura Sagar Dam is at the foot of the Banasura Hill. Spillway Dam. Kuttiady Augmentation Spillway dam is a concrete dam with spillways for the Banasurasagar (kutyadi Augmentation) reservoir.

Geographic entities mentioned:
surface_form: Banasura Hill
instance_of: Mountain
countries: India
coordinates: lat: 11.69416667
lon: 75.90805556
Tourism. The dam has become a popular tourist destination. Many people visit the place to go trekking at the Banasura Hill and speed boating at Banasura Sagar Dam. The Banasura Hill Resort, located about 20 km from the dam was rated as Asia's largest Earthen Resort by BBC. Current scenario.

Geographic entities mentioned:
surface_form: Banasura Hill
instance_of: Mountain
countries: India
coordinates: lat: 11.69416667
lon: 75.90805556
Giouchtas F.C.. A.O. Giouchtas F.C., short for Athlitikos Omilos Archanes “Giouchtas” (, translated &quot;Athletic Club of Archanes “Giouchtas”&quot;) and also known simply as Giouchtas, is a Greek football club, based in Archanes, Heraklion. The club is named after Mount Juktas, overlooking the town of Archanes. The club was founded in 1957 and its traditional colors are green and white.

Geographic entities mentioned:
surface_form: Mount Juktas
instance_of: Mountain
countries: Greece
coordinates: lat: 35.23994444444445
lon: 25.14413888888889
Lake Chyortovo. Lake Chyortovo or Lozil-To, also known as &quot;Chertovo&quot; (, meaning &quot;Devil's Lake&quot;; Selkup: Лозыль'-то) is a freshwater lake in Yamalo-Nenets Autonomous Okrug, Russia. The lake is a traditional sacred site for the indigenous Selkup people of the region. Legend says the lake is so deep it has no bottom. Geography.

Geographic entities mentioned:
surface_form: chyortovo
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 64.11666666666666
lon: 80.7
surface_form: lake chyortovo
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 64.11666666666666
lon: 80.7
Geography. Chyortovo is located north of the Arctic Circle, in the southeastern part of the okrug. It is a chain of lakes roughly aligned from west to east. They are connected with each other by streams. The westernmost one at is known as &quot;Upper Chyortovo&quot;. It has an hourglass shape and an island in the northern part. The largest lake is at the eastern end.

Geographic entities mentioned:
surface_form: chyortovo
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 64.11666666666666
lon: 80.7
This ice cap is centered at, and is at an elevation of. The other ice cap covers an area of approximately and is centered at an unnamed summit at, at an elevation of. The main ice cap borders the northernmost part of the Puyuhuapi Channel called Ventisquero Sound. Cascada de Ventisquero Colgante, a large waterfall, is located in the park.

Geographic entities mentioned:
surface_form: Puyuhuapi Channel
instance_of: Body of water
countries: Chile
coordinates: lat: -44.6191
lon: -72.7222
On 19 June, Æthelflæd stormed the royal &quot;llys&quot; (court) in Llangorse lake, and captured the queen of the land and 34 others. Hwgan responded by seeking an alliance with the Danes, but died soon afterwards while defending Derby (a Danish-held city) from the Saxons.

Geographic entities mentioned:
surface_form: Llangorse lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.930961111111
lon: -3.2627555555556
Hood River County comprises the Hood River, OR Micropolitan Statistical Area. The Hood River Valley produces apples, pears, and cherries. Situated between Mount Hood and the Columbia River in the middle of the Columbia River Gorge, Hood River County is a popular destination for outdoor enthusiasts, such as windsurfers, mountain-bikers, skiers, hikers, kayakers, and many more. History.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
In response to controversy surrounding county approval of locating a destination resort at Cooper Spur ski area on Mount Hood, on November 5, 2003, 62% of the voters approved a measure requiring voter approval on residential developments of 25 units or more on land zoned for forest use. Opponents claimed that this measure was not enforceable and would end up in court. Geography.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
P. Hill's Light Division, forcing the Union units back across the Potomac. One Union unit, the 118th Pennsylvania Infantry Regiment, did not withdraw at the same time as the others and suffered heavy losses. Lee's army continued its retreat into the Shenandoah Valley after the battle. Background. In June 1862, during the American Civil War, General Robert E.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Huckstep's Virginia Battery. Aftermath. Pendleton was widely criticized within the Confederate press and within Lee's army after the battle. The Confederate army withdrew into the Shenandoah Valley after the battle, and McClellan did not pursue. Due to his lack of aggression in pursuing the retreating Confederates, McClellan was relieved from command on November 5.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
He is held in high regard by those who have been coached by him. From 2005 to 2009, Wright was head coach at the Melbourne University Boat Club. Wright worked for Rowing New Zealand as coach for the men's eight, and was head coach at the Waikato Regional Performance Centre with training at Lake Karapiro. In late 2014, Wright was appointed head national coach of Switzerland.

Geographic entities mentioned:
surface_form: Lake Karapiro
instance_of: Lake
countries: New Zealand
coordinates: lat: -37.943167
lon: 175.560833
Under K. O. Lange. The MIT meteorology survey program was directed by Lange, who for several years was engaged in similar activities for the Rhon-Rossiten Geschellschaft at Darmstadt, and also on the Wasserkuppe, the birthplace of the motorless airplane. During this time he took an active part in the development of the scientific basis for soaring and gliding flight. Professor Daniel C.

Geographic entities mentioned:
surface_form: Wasserkuppe
instance_of: Mountain
countries: Germany
coordinates: lat: 50.498055555556
lon: 9.9377777777778
Minnesota House of Representatives. Thompson was elected to the Minnesota House of Representatives in November 2020 and assumed office on January 5, 2021. He represented the 67A district that encompasses northwest Saint Paul and portions of Maplewood in the Lake Phalen area. Thompson was an outspoken member of the legislature for police reform measures during the 92nd Minnesota Legislature.

Geographic entities mentioned:
surface_form: Lake Phalen
instance_of: Lake
countries: United States
coordinates: lat: 44.983333333333
lon: -93.05
An example of one of the latest large city projects is the Spaladium Arena, built in 2009. Geography. Split is situated on a peninsula between the eastern part of the Gulf of Kaštela and the Split Channel. The Marjan hill (), rises in the western part of the peninsula. The Kozjak () and Mosor () ridges protect the city from the north and northeast, and separate it from the hinterland. Climate.

Geographic entities mentioned:
surface_form: Kozjak
instance_of: Mountain
countries: Croatia
coordinates: lat: 43.570813888889
lon: 16.402588888889
In May 2009, the gallery opened its new premises in the old Split Hospital building behind Diocletian's Palace. The Ivan Meštrović Gallery (), on the Marjan peninsula is an art museum dedicated to the work of the 20th-century sculptor, Ivan Meštrović. The gallery displays some of his most significant work, and the building itself is an art monument.

Geographic entities mentioned:
surface_form: Marjan
instance_of: Mountain
countries: Croatia
coordinates: lat: 43.5085514
lon: 16.4093381
Cameley. Cameley is a village in the civil parish of Temple Cloud with Cameley, within the Chew Valley in Somerset, and on the northern slopes of the Mendip Hills, in the Bath and North East Somerset Council area just off the A37 road. It is located from Bristol, Bath and Wells. The nearest town is Midsomer Norton, which is away.

Geographic entities mentioned:
surface_form: Chew Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.337422222222
lon: -2.6151972222222
She has been considered by a number of scholars to be the founder of scientific natural history in Germany. Hildegard's convent at Disibodenberg elected her as (mother superior) in 1136. She founded the monasteries of Rupertsberg in 1150 and Eibingen in 1165. Hildegard wrote theological, botanical, and medicinal works, as well as letters, hymns, and antiphons for the liturgy.

Geographic entities mentioned:
surface_form: Rupertsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.9658
lon: 7.8892
Abbot Kuno of Disibodenberg asked Hildegard to be prioress, which would be under his authority. Hildegard wanted more independence for herself and her nuns and asked Abbot Kuno to allow them to move to Rupertsberg. This was to be a move toward poverty, from a stone complex that was well established to a temporary dwelling place.

Geographic entities mentioned:
surface_form: Rupertsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.9658
lon: 7.8892
Kenfield Nunatak. x5h13jcfm4hlpcfwcjvr1aw65kol" xml:space="preserve">#redirect Kenfield Nunatak

Geographic entities mentioned:
surface_form: kenfield nunatak
instance_of: Mountain
coordinates: lat: -73.7667
lon: -99.05
The lake has no outlet. Water is lost through sublimation and ablation of the ice cover. The lake is categorized as an ultra-oligotrophic lake. Lake Ober-See, a smaller (glacial lake, is located a few kilometres to the northeast and is similar in most respects. History. Isotope studies have established that the lake has long had a permanent ice cover.

Geographic entities mentioned:
surface_form: Lake Ober-See
instance_of: Lake
coordinates: lat: -71.2833
lon: 13.65
surface_form: ober-see
instance_of: Lake
coordinates: lat: -71.2833
lon: 13.65
Lake Untersee is an unusual lake, with pH between 9.8 and 12.1, dissolved oxygen at 150 per cent supersaturation, and very low primary production in the water column. Despite the high oxygen supersaturation in most of the lake, there is a small sub-basin at the southern end that is anoxic, and its sediments may have a higher methane concentration than those of any other known lake on Earth.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
The proportion of methane in the sediment at the lake bottom is the highest recorded for any lake in the world, according to NASA scientists. In 2008, as part of the Tawani Foundation 2008 Antarctic International Expedition (see below), Dale Andersen and Ian Hawes discovered conical stromatolites growing in Lake Untersee, the largest living ones known to date.

Geographic entities mentioned:
surface_form: untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
surface_form: lake untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
In 2008, as part of the Tawani Foundation 2008 Antarctic International Expedition (see below), Dale Andersen and Ian Hawes discovered conical stromatolites growing in Lake Untersee, the largest living ones known to date. Small microbial pinnacles are also present, and it appears that the large conical stromatolites and the small pinnacles are made by different microbial communities.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
Lake Untersee. Lake Untersee (,) is the largest surface freshwater lake in the interior of the Gruber Mountains of central Queen Maud Land in East Antarctica. It is situated to the southeast of the Schirmacher Oasis. The lake is approximately long and wide, with a surface area of, and a maximum depth of. The lake is permanently covered with ice and is partly bounded by glacier ice.

Geographic entities mentioned:
surface_form: untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
surface_form: lake untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
It is situated to the southeast of the Schirmacher Oasis. The lake is approximately long and wide, with a surface area of, and a maximum depth of. The lake is permanently covered with ice and is partly bounded by glacier ice. Lake Untersee is an unusual lake, with pH between 9.8 and 12.1, dissolved oxygen at 150 per cent supersaturation, and very low primary production in the water column.

Geographic entities mentioned:
surface_form: untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
surface_form: lake untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
In the past, the water chemistry of the lake has been compared to Clorox. However, the chemical activity of bleach is due to Cl− in addition to a pH that is higher than that measures in Lake Untersee, and Lake Untersee does not have high chlorine or chlorite concentrations. Geography.

Geographic entities mentioned:
surface_form: untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
surface_form: untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
surface_form: lake untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
surface_form: lake untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
Geography. Lake Untersee lies in the interior of the Gruber Mountains of central Queen Maud Land in East Antarctica, which is roughly on the same longitude as Huab, in the Skeleton Coast National Park on the northern coast of Namibia. It is situated 90 kilometres (56 mi) to the southeast of the Schirmacher Oasis. Aurkjosen Cirque lies at the east side of the lake.

Geographic entities mentioned:
surface_form: untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
surface_form: lake untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
It is also stated that the lake existed during the Holocene period when it emerged from a melt-water pond. Studies of Lake Untersee have revealed that there are several large boulders which dam the lake. Geodetic studies carried out during two summer seasons indicated that the boulders move at an annual rate of. Residence time of the boulders has been estimated as 500 years.

Geographic entities mentioned:
surface_form: untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
surface_form: lake untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
Loopmann &quot;et al.&quot; (1988). Research. In studies carried out prior to 1991–92 on physical and chemical parameters of the lake water, Lake Untersee was stated to be well-mixed and unstratified. However, studies performed in the summer of 1991–92 found significant stratification in a wide trough in the southeastern part of the lake, where it is up to deep.

Geographic entities mentioned:
surface_form: untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
surface_form: lake untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
The expedition did find several new strains of extremophile microorganisms in the lake's waters, including a chemolithotroph that metabolises hydrogen. This expedition involved an interdisciplinary international team of ten scientists and two teachers who explored not only Lake Untersee but also the Schirmacher Oasis.

Geographic entities mentioned:
surface_form: untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
surface_form: lake untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
The geomicrobiological aspects of this expedition had three objectives: &quot;to test laser induced fluorescence emission (L.I.F.E.) to be used for the exploration of the Mars regolith and poles; monitor global climate change; and to evaluate methods for detecting hydrocarbon contamination and subsequent bio-remediation in a fragile, endangered ecosystem.&quot; The results indicate that Lake Untersee, as a permanently ice-covered region, has very little usable soil and could be likened to the polar regions of Mars.

Geographic entities mentioned:
surface_form: untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
surface_form: lake untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
Two scientific divers were also part of this team. Dale Andersen, with the SETI Institute's Carl Sagan Center for the Study of Life in the Universe, and Ian Hawes of Aquatic Research Solutions dived in Lake Untersee to study its unique microbial communities.

Geographic entities mentioned:
surface_form: untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
surface_form: lake untersee
instance_of: Lake
coordinates: lat: -71.333333333333
lon: 13.45
These communities provide an important analog to some of the oldest fossil stromatolites found to date. Expeditions. In November and December 2008, the &quot;Tawani Foundation 2008 Antarctic International Expedition&quot; headed by Richard Hoover of NASA's Marshall Space Flight Center used the lake as a test bed in its hunt for extreme life.

Geographic entities mentioned:
surface_form: hunt
instance_of: Mountain
coordinates: lat: -67.1167
lon: 144.3
It is replenished perennially by a process of underwater melting of the adjacent glacier ice. It is also stated that the lake existed during the Holocene period when it emerged from a melt-water pond. Studies of Lake Untersee have revealed that there are several large boulders which dam the lake.

Geographic entities mentioned:
surface_form: pond
instance_of: Mountain
coordinates: lat: -62.95
lon: -60.55
Carruthers Peak. Carruthers Peak, formerly Curruthers Peak, a mountain in the Main Range of the Great Dividing Range, is located in Snowy Mountains region in southeast New South Wales, Australia. The peak is situated between Mount Lee and Mount Twynam within the Kosciuszko National Park. With an elevation of above sea level, Carruthers Peak is the seventh-highest peak in mainland Australia.

Geographic entities mentioned:
surface_form: Mount Twynam
instance_of: Mountain
countries: Australia
coordinates: lat: -36.393333333333
lon: 148.31472222222
surface_form: kosciuszko
instance_of: Mountain
countries: Australia
coordinates: lat: -36.4558303
lon: 148.2635105
With an elevation of above sea level, Carruthers Peak is the seventh-highest peak in mainland Australia. It was named after Joseph Carruthers, a Premier of New South Wales, who, while he served as Minister for Lands, facilitated the building of the Summit Road to Mount Kosciuszko. It can be easily accessed, with the Main Range walk going straight up it. Geology.

Geographic entities mentioned:
surface_form: Mount Kosciuszko
instance_of: Mountain
countries: Australia
coordinates: lat: -36.4558303
lon: 148.2635105
surface_form: kosciuszko
instance_of: Mountain
countries: Australia
coordinates: lat: -36.4558303
lon: 148.2635105
Carruthers Peak. Carruthers Peak, formerly Curruthers Peak, a mountain in the Main Range of the Great Dividing Range, is located in Snowy Mountains region in southeast New South Wales, Australia. The peak is situated between Mount Lee and Mount Twynam within the Kosciuszko National Park. With an elevation of above sea level, Carruthers Peak is the seventh-highest peak in mainland Australia.

Geographic entities mentioned:
surface_form: carruthers peak
instance_of: Mountain
countries: Australia
coordinates: lat: -36.408611111111
lon: 148.29111111111
The peak is situated between Mount Lee and Mount Twynam within the Kosciuszko National Park. With an elevation of above sea level, Carruthers Peak is the seventh-highest peak in mainland Australia. It was named after Joseph Carruthers, a Premier of New South Wales, who, while he served as Minister for Lands, facilitated the building of the Summit Road to Mount Kosciuszko.

Geographic entities mentioned:
surface_form: carruthers peak
instance_of: Mountain
countries: Australia
coordinates: lat: -36.408611111111
lon: 148.29111111111
Due to a century of grazing on the Main Range, the area around it was heavily eroded. From the 1950s Soil Conservation Service undertook an extensive program of rehabilitation of the vegetation of the Carruthers Peak–Mount Twynam area using bitumen, wire netting and bales of straw. It lies on a vein of shale running south-southeast through the predominant granite.

Geographic entities mentioned:
surface_form: carruthers peak
instance_of: Mountain
countries: Australia
coordinates: lat: -36.408611111111
lon: 148.29111111111
surface_form: mount twynam
instance_of: Mountain
countries: Australia
coordinates: lat: -36.393333333333
lon: 148.31472222222
Geography. The range runs for approximately 30 kilometres northeast from the Lammerlaw Range before reaching the Sutton Stream which drains the saddle between it and the southern end of the Rock and Pillar Range and that flows to the east and into the Strath Taieri valley near Sutton Salt Lake, southwest of Middlemarch.

Geographic entities mentioned:
surface_form: Sutton Salt Lake
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.5764
lon: 170.087
Mount Soematsu. is located in the Hidaka Mountains, Hokkaidō, Japan.

Geographic entities mentioned:
surface_form: mount soematsu
instance_of: Mountain
countries: Japan
coordinates: lat: 42.42722222
lon: 142.94694444
History. The company was founded in 1924 by Floyd and Bess (Lugton) Shields. Floyd Shields was one of the pioneering date farmers in the still-young date industry of the Coachella Valley. He bred a number of his own hybrids and varieties including the &quot;Blonde&quot; and &quot;Brunette&quot; varieties, grown exclusively at Shields to this day. &quot;Romance and Sex Life of the Date&quot;.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
Following completion of training, the regiment moved to Wheeling, West Virginia on May 13 and then to Strasburg, Virginia to join Major General John C. Fremont's army in the Shenandoah Valley. The regiment was attached to the Mountain Department until June 1862 and participated in several engagements with the Confederates, first seeing combat at the Battle of Woodstock on June 2.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
1863 and 1864. In 1863, the regiment participated in the Battle of Kelly's Ford. Later that year, it was heavily involved in the Gettysburg Campaign, fighting at the Battle of Brandy Station and in several smaller engagements during the Union operations in the Loudoun Valley of Virginia, including the battles of Aldie, Middleburg, and Upperville.

Geographic entities mentioned:
surface_form: Loudoun Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.2329
lon: -77.735
History. On one of those benchlands is the Keatley Creek Archaeological Site, which was once a large riverside housepit (quiggly hole or &quot;kekuli&quot;) village. Of great antiquity like in the Fraser Valley, the site is among the most important in Canada and has been exhaustively studied and documented by archaeologists.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
Glisan Glacier. Glisan Glacier was an alpine glacier located on the northwest slope of Mount Hood in the US state of Oregon. It had an average altitude of, but is no longer considered to be a glacier.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
One person died in New York City due to the storm. The high waves and winds caused the greatest marine damage in a decade around New York City. More than 100 boats were overturned or beached in Jamaica Bay, and another 150 boats were wrecked between Hell Gate and the west end of Coney Island. At least ten houseboats were damaged or sank, with boaters injured and requiring rescue.

Geographic entities mentioned:
surface_form: Hell Gate
instance_of: Landform
countries: United States
coordinates: lat: 40.78102
lon: -73.92452