Sarmila/GeoWiki-Features huggingface dataset:
Yarlovo. Yarlovo () is a village in Samokov municipality of Sofia Province in southwestern Bulgaria. It is located 24 kilometers from the capital Sofia. It is situated in Samokov Valley on the west slopes of the Vitosha mountain massif; the altitude exceeds 1,000 meters. The village has over 500 inhabitants. Yarlovo Nunatak on Trinity Peninsula in Antarctica is named after the village.

Geographic entities mentioned:
surface_form: Vitosha
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.566666666667
lon: 23.283333333333
The crematorium at Mangrol is called '<nowiki/>&quot;Narsinh Nu Samshan, and commemorates the first poet known as Gujarati Adi Kavi
The Narsinh Mehta Award was established in his name to recognize excellence in Gujarati literature. Vastrapur Lake in Ahmedabad has been officially renamed in his honor. Poetic works.

Geographic entities mentioned:
surface_form: Vastrapur Lake
instance_of: Lake
countries: India
coordinates: lat: 23.0384
lon: 72.529
During this period, north Wales was subject to volcanic activity. The remains of these volcanoes are still visible, one example of which is Rhobell Fawr dating from 510 Ma. Large quantities of volcanic lava and ash known as the Borrowdale Volcanics covered the Lake District and this can still be seen in the form of mountains such as Helvellyn and Scafell Pike.

Geographic entities mentioned:
surface_form: Rhobell Fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.814
lon: -3.802
The remains of these volcanoes are still visible, one example of which is Rhobell Fawr dating from 510 Ma. Large quantities of volcanic lava and ash known as the Borrowdale Volcanics covered the Lake District and this can still be seen in the form of mountains such as Helvellyn and Scafell Pike. The Ordovician also saw the formation of the Skiddaw slate deposits around 500 Ma. Silurian period.

Geographic entities mentioned:
surface_form: Helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
surface_form: Scafell Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
The remains of these volcanoes are still visible, one example of which is Rhobell Fawr dating from 510 Ma. Large quantities of volcanic lava and ash known as the Borrowdale Volcanics covered the Lake District and this can still be seen in the form of mountains such as Helvellyn and Scafell Pike. The Ordovician also saw the formation of the Skiddaw slate deposits around 500 Ma. Silurian period.

Geographic entities mentioned:
surface_form: Skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
Volcanic ashes and lavas deposited during the Silurian are still found in the Mendip Hills and in Pembrokeshire. Devonian period. The collision between continents continued during the Devonian period, with continuing uplift, and more volcanic deposits such as those now forming Ben Nevis. Sea levels varied considerably, with the coastline advancing and retreating from north to south across England.

Geographic entities mentioned:
surface_form: Ben Nevis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.796891
lon: -5.003675
The uplifted region was gradually eroded down, resulting in the deposition of numerous sedimentary rock layers in lowlands and seas. The rocks of marine origin in the county of Devon gave the period its name, though deposits of this age are found in many other places, such as the Brecon Beacons, the Midland Valley of Scotland, and the Orkney Islands.

Geographic entities mentioned:
surface_form: Midland Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408
lon: -4.044
Palaeogene period. In the early Palaeogene period, between 63 and 52 Ma, the last volcanic rocks in Great Britain were formed. The major eruptions at this time produced the Antrim Plateau, the basaltic columns of the Giant's Causeway and the lavas and igneous intrusions of the Inner Hebrides of Scotland.

Geographic entities mentioned:
surface_form: Giant's Causeway
instance_of: Landform
countries: United Kingdom
coordinates: lat: 55.240833333333
lon: -6.5116666666667
Axiocerses nyika. &quot;Axiocerses nyika&quot; is a butterfly in the family Lycaenidae. It is found in Malawi (the Nyika Plateau and Chisange Falls) and Zambia. The habitat consists of hills with stunted, shrubby vegetation, at altitudes between 1,980 and 2,290 meters. Adults have been recorded in December.

Geographic entities mentioned:
surface_form: Nyika Plateau
instance_of: Plateau
countries: Malawi
Zambia
coordinates: lat: -10.35
lon: 33.6
In Kali Yuga, all true scriptures are bound to maya and are unhelpful. The reason, as stated in Akilam for the disintegration of the entire system is that, towards the end of Dvapara Yuga, there in Mount Kailash, Siva believing the words of devas, created Kaliyan without discussing to Vishnu, who had the responsibility to destroy Kaliyan as per previous deeds.

Geographic entities mentioned:
surface_form: Mount Kailash
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
Stage 2. Due to poor weather conditions, the general classification timing for the stage was taken 9 kilometres from the finish, prior to the technical Alto del Castillo de Monjuic. Although most of the 181.3 kilometre distance was travelled at a reasonably slow pace, multiple riders crashed, including race leader Lorenzo Milesi, Primož Roglič, and Geraint Thomas.

Geographic entities mentioned:
surface_form: Monjuic
instance_of: Mountain
countries: Spain
coordinates: lat: 41.364166666667
lon: 2.1580555555556
Quilty Nunataks. vxbkqn5e7ad95s8g1f0bzdry678" xml:space="preserve">#redirect Quilty Nunataks

Geographic entities mentioned:
surface_form: quilty nunataks
instance_of: Mountain
coordinates: lat: -75.75
lon: -71.75
Mississagi River. The Mississagi River is a river in Algoma and Sudbury Districts, Ontario, Canada, that originates in Sudbury District and flows to Lake Huron at Blind River, Algoma District. Etymology. The river's name comes from the Ojibwe &quot;misi-zaagi&quot;, meaning &quot;river with a wide mouth&quot;. Geography.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
The mountain is set on land managed by Salmon–Challis National Forest. Neighbors include Little Regret Peak two miles south, line parent Mount Breitenbach, 3.4 miles south, Leatherman Peak is 3.8 miles to the southwest, and Borah Peak, the highest peak in Idaho, is 5.6 miles to the west-northwest. Precipitation runoff from the mountain's slopes drains to tributaries of the Pahsimeroi River.

Geographic entities mentioned:
surface_form: Mount Breitenbach
instance_of: Mountain
countries: United States
coordinates: lat: 44.0666
lon: -113.673
surface_form: Leatherman Peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.0821
lon: -113.733
surface_form: Borah Peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1373891
lon: -113.78110123
Mount Corruption. Mount Corruption is an mountain summit located in Custer County, Idaho, United States. Description. Mount Corruption ranks as the 21st-highest peak in Idaho and is part of the Lost River Range which is a subset of the Rocky Mountains. The mountain is set on land managed by Salmon–Challis National Forest.

Geographic entities mentioned:
surface_form: mount corruption
instance_of: Mountain
countries: United States
coordinates: lat: 44.114367
lon: -113.670554
Topographic relief is significant as the summit rises over above the East Fork Pahsimeroi in approximately one mile. Climate. Based on the Köppen climate classification, Mount Corruption is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers. Winter temperatures can drop below −10 °F with wind chill factors below −30 °F.

Geographic entities mentioned:
surface_form: mount corruption
instance_of: Mountain
countries: United States
coordinates: lat: 44.114367
lon: -113.670554
Khukha. Khukha is a village in Jhelum District, Punjab, Pakistan. It is a union council (administrative subdivision) of Jhelum Tehsil and a &quot;model&quot; village. It lies 7 km west of Dina, 1 km east of Gaggar Khurd, 5 km north of Rohtas and 10 km northeast of Tilla Jogian. Neighbouring villages include Natain, Khojki and Mota Gharbi.

Geographic entities mentioned:
surface_form: Tilla Jogian
instance_of: Mountain
countries: Pakistan
coordinates: lat: 32.83333333
lon: 73.41666667
Resurgence and enduring popularity. The song was largely unknown outside Shaker communities until Aaron Copland used its melody for the score of Martha Graham's ballet, &quot;Appalachian Spring&quot;, first performed in 1944. (Shakers once worshipped on Holy Mount, in the Massachusetts portion of the Appalachians).

Geographic entities mentioned:
surface_form: Holy Mount
instance_of: Mountain
countries: United States
coordinates: lat: 42.451
lon: -73.3536
Climate. The ecoregion has a seasonally moist, tropical to subtropical climate. Rainfall ranges from 1000 mm per year near the coast to less than 600 mm per year inland. Most of the rain falls in the summer months. The coastal strip includes areas of wetland, the largest of which is Lake St. Lucia, the largest estuarine system in Africa. Flora.

Geographic entities mentioned:
surface_form: Lake St. Lucia
instance_of: Lake
countries: South Africa
coordinates: lat: -28
lon: 32.5
Black Hills (Washington). The Black Hills are a small range of hills in Thurston and Grays Harbor counties of Washington. They are widely considered a subset of the Willapa Hills, however, the line parent of the Black Hills is Rock Peak, in the Olympic Mountains. The tallest peak in the range is Capitol Peak with a height. The Black Hills takes its name from the Black River.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: black hills (washington)
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
Black Hills (Washington). The Black Hills are a small range of hills in Thurston and Grays Harbor counties of Washington. They are widely considered a subset of the Willapa Hills, however, the line parent of the Black Hills is Rock Peak, in the Olympic Mountains. The tallest peak in the range is Capitol Peak with a height. The Black Hills takes its name from the Black River.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
The Capitol State Forest has roughly the same boundaries as the Black Hills. The high school A.G. West Black Hills, Tumwater, Washington, is named for the hills, as is the local soccer club the Blackhills Football Club. Capital Medical Center on the west side of Olympia was named Black Hills Community Hospital from its opening in 1985 until 1991.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Black Hills (Washington). The Black Hills are a small range of hills in Thurston and Grays Harbor counties of Washington. They are widely considered a subset of the Willapa Hills, however, the line parent of the Black Hills is Rock Peak, in the Olympic Mountains. The tallest peak in the range is Capitol Peak with a height. The Black Hills takes its name from the Black River.

Geographic entities mentioned:
surface_form: capitol peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.1503
lon: -107.083
surface_form: capitol peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.9727
lon: -123.139
Black Hills (Washington). The Black Hills are a small range of hills in Thurston and Grays Harbor counties of Washington. They are widely considered a subset of the Willapa Hills, however, the line parent of the Black Hills is Rock Peak, in the Olympic Mountains. The tallest peak in the range is Capitol Peak with a height. The Black Hills takes its name from the Black River.

Geographic entities mentioned:
surface_form: rock peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.067777777778
lon: -115.655
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
They are widely considered a subset of the Willapa Hills, however, the line parent of the Black Hills is Rock Peak, in the Olympic Mountains. The tallest peak in the range is Capitol Peak with a height. The Black Hills takes its name from the Black River. A former variant name was &quot;Black Mountains&quot;. The Capitol State Forest has roughly the same boundaries as the Black Hills.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
The tallest peak in the range is Capitol Peak with a height. The Black Hills takes its name from the Black River. A former variant name was &quot;Black Mountains&quot;. The Capitol State Forest has roughly the same boundaries as the Black Hills. The high school A.G. West Black Hills, Tumwater, Washington, is named for the hills, as is the local soccer club the Blackhills Football Club.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
The Capitol State Forest has roughly the same boundaries as the Black Hills. The high school A.G. West Black Hills, Tumwater, Washington, is named for the hills, as is the local soccer club the Blackhills Football Club. Capital Medical Center on the west side of Olympia was named Black Hills Community Hospital from its opening in 1985 until 1991.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
Course. The Sopo river rises on the border with the Central African Republic, and flows in a generally northeast direction past the town of Sopo. to join the Boro River on the border with Northern Bahr el Ghazal. The combined stream is the Magadhik River, which in turn joins the Chel River to form the Lol River, a tributary of the Bahr al-Arab.

Geographic entities mentioned:
surface_form: Lol River
instance_of: Watercourse
countries: South Sudan
coordinates: lat: 9.19055556
lon: 29.19666667
surface_form: Bahr al-Arab
instance_of: Watercourse
countries: Sudan
South Sudan
coordinates: lat: 9.0333333333333
lon: 29.466666666667
He was one of the few Swiss politicians to take a stand for US-President Donald Trump. He has respect for Trump's career and supports many of his ideas. Due to an illness in his family circle, Grüter campaigns for a new legal regulation of organ donations. Personal life. Grüter is married to Luzia (née Bucher) Grüter. They have three children and reside in Eich on Lake Sempach.

Geographic entities mentioned:
surface_form: Lake Sempach
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.15
lon: 8.15
I-90 is the only divided highway crossing east–west through the state. The pass lends its name to a census-designated place (CDP) located at the summit (Snoqualmie Pass, Washington). Both the CDP and Snoqualmie Pass are named after the Snoqualmie people of the valley to the west. Climate.

Geographic entities mentioned:
surface_form: valley
instance_of: Valley
countries: United States
coordinates: lat: 47.605555555556
lon: -121.92138888889
This tree island is believed to be present-day Chekika Island, located at the beginning of Shark Valley. The observation tower at Shark Valley was designed by the prominent South Florida architect Edward M. Ghezzi. It was built in 1964 as part of the Mission 66 projects throughout the national parks. The tower design is similar to that of the tower on Kuwohi in Smoky Mountain National Park

Geographic entities mentioned:
surface_form: Kuwohi
instance_of: Mountain
countries: United States
coordinates: lat: 35.562777777778
lon: -83.498611111111
surface_form: kuwohi
instance_of: Mountain
countries: United States
coordinates: lat: 35.562777777778
lon: -83.498611111111
surface_form: smoky mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0594
lon: -113.68
Shark Valley. Shark Valley is a geological depression at the head of the Shark River Slough in far western Miami-Dade County, Florida, United States. It is currently part of Everglades National Park. Shark Valley empties into Shark River in the Ten Thousand Islands of Monroe County.

Geographic entities mentioned:
surface_form: shark valley
instance_of: Valley
countries: United States
coordinates: lat: 25.7078
lon: -80.7631
It is currently part of Everglades National Park. Shark Valley empties into Shark River in the Ten Thousand Islands of Monroe County. Shark Valley characteristically includes sawgrass prairie that floods during the rainy season, hence the name &quot;river of grass&quot;—&quot;Pa-Hay-Okee&quot;, from the Mikasuki language—for such marshes in the Everglades.

Geographic entities mentioned:
surface_form: shark valley
instance_of: Valley
countries: United States
coordinates: lat: 25.7078
lon: -80.7631
It is currently part of Everglades National Park. Shark Valley empties into Shark River in the Ten Thousand Islands of Monroe County. Shark Valley characteristically includes sawgrass prairie that floods during the rainy season, hence the name &quot;river of grass&quot;—&quot;Pa-Hay-Okee&quot;, from the Mikasuki language—for such marshes in the Everglades.

Geographic entities mentioned:
surface_form: shark valley
instance_of: Valley
countries: United States
coordinates: lat: 25.7078
lon: -80.7631
surface_form: shark valley
instance_of: Valley
countries: United States
coordinates: lat: 25.7078
lon: -80.7631
Shark Valley characteristically includes sawgrass prairie that floods during the rainy season, hence the name &quot;river of grass&quot;—&quot;Pa-Hay-Okee&quot;, from the Mikasuki language—for such marshes in the Everglades. Shark Valley features a Visitor Center with educational displays, a park video, an underwater camera and informational brochures.

Geographic entities mentioned:
surface_form: shark valley
instance_of: Valley
countries: United States
coordinates: lat: 25.7078
lon: -80.7631
Shark Valley features a Visitor Center with educational displays, a park video, an underwater camera and informational brochures. The entrance to Shark Valley is located along Tamiami Trail (US 41) near the Miami-Dade–Collier County line. Characteristics. Shark Valley contains large expanses of oolitic limestone either exposed or overlain by marl.

Geographic entities mentioned:
surface_form: shark valley
instance_of: Valley
countries: United States
coordinates: lat: 25.7078
lon: -80.7631
The area, having a brief hydroperiod, is seasonally submerged, with &quot;Cladium jamaicense&quot; (sawgrass) being the dominant vegetation. Unlike the deeper Shark River Slough, Shark Valley does not contain standing water year-round. Wildlife seen in Shark Valley includes alligators, ibis, wood storks, roseate spoonbills, raccoons, white-tailed deer, and various amphibians. History.

Geographic entities mentioned:
surface_form: shark valley
instance_of: Valley
countries: United States
coordinates: lat: 25.7078
lon: -80.7631
surface_form: shark valley
instance_of: Valley
countries: United States
coordinates: lat: 25.7078
lon: -80.7631
History. A well-known episode in the Second Seminole War occurred in or near Shark Valley. In the late 1830s, groups of Spanish Indians successively raided a guarded trading post on the Caloosahatchee River in 1839 and committed a massacre on Indian Key in 1840.

Geographic entities mentioned:
surface_form: shark valley
instance_of: Valley
countries: United States
coordinates: lat: 25.7078
lon: -80.7631
They found Chakaika with some of his rebels, shot him, and had him hanged on &quot;Chakaika's island,&quot; a tree island in the Everglades. This tree island is believed to be present-day Chekika Island, located at the beginning of Shark Valley. The observation tower at Shark Valley was designed by the prominent South Florida architect Edward M. Ghezzi.

Geographic entities mentioned:
surface_form: shark valley
instance_of: Valley
countries: United States
coordinates: lat: 25.7078
lon: -80.7631
surface_form: shark valley
instance_of: Valley
countries: United States
coordinates: lat: 25.7078
lon: -80.7631
When Union cannoneers overshot their targets, they often hit the massed infantry waiting in the woods of Seminary Ridge or in the shallow depressions just behind Alexander's guns, causing significant casualties before the charge began.

Geographic entities mentioned:
surface_form: Seminary Ridge
instance_of: Landform
countries: United States
coordinates: lat: 39.2536
lon: -77.2536
The clerk of the Privy Council, Charles Greville, wrote of him: &quot;He is King to all intents and purposes.&quot;
In 1847, Victoria and Albert spent a rainy holiday in the west of Scotland at Loch Laggan, but heard from their doctor, Sir James Clark, that Clark's son had enjoyed dry, sunny days farther east at Balmoral Castle.

Geographic entities mentioned:
surface_form: Loch Laggan
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.948055555556
lon: -4.49
Location. Cle Elum Lake is the easternmost lake of three large lakes (two are north and one is south of Interstate 90) in the Cascade Range. The middle one, Kachess Lake is also north of I-90 while the westernmost, Keechelus Lake is south of I-90. Cle Elum Lake is part of the Columbia River basin, as the Cle Elum River is a tributary of the Yakima River, which is a tributary to the Columbia River.

Geographic entities mentioned:
surface_form: Kachess Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.307795
lon: -121.232403
surface_form: Keechelus Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.34777777777778
lon: -121.36888888888889
Cle Elum Lake. Cle Elum Lake is a lake and reservoir along the course of the Cle Elum River, in Washington state, US. At the site of the future city of Cle Elum, Washington, a Northern Pacific Railway station was named Clealum after the Kittitas name Tle-el-Lum (tlielləm), meaning &quot;swift water&quot;, referring to the Cle Elum River.

Geographic entities mentioned:
surface_form: cle elum
instance_of: Lake
countries: United States
coordinates: lat: 47.282
lon: -121.107
Cle Elum Lake. Cle Elum Lake is a lake and reservoir along the course of the Cle Elum River, in Washington state, US. At the site of the future city of Cle Elum, Washington, a Northern Pacific Railway station was named Clealum after the Kittitas name Tle-el-Lum (tlielləm), meaning &quot;swift water&quot;, referring to the Cle Elum River.

Geographic entities mentioned:
surface_form: cle elum
instance_of: Lake
countries: United States
coordinates: lat: 47.282
lon: -121.107
surface_form: cle elum
instance_of: Lake
countries: United States
coordinates: lat: 47.282
lon: -121.107
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Usage. The lake is used as a storage reservoir for the Yakima Project, an irrigation project run by the United States Bureau of Reclamation. Although a natural lake, Cle Elum Lake's capacity and discharge is controlled by Cle Elum Dam, a high earthfill structure built in 1933. As a storage reservoir, Cle Elum Lake's active capacity is 436,900 acre feet (539,000,000 m³).

Geographic entities mentioned:
surface_form: cle elum
instance_of: Lake
countries: United States
coordinates: lat: 47.282
lon: -121.107
surface_form: cle elum
instance_of: Lake
countries: United States
coordinates: lat: 47.282
lon: -121.107
Usage. The lake is used as a storage reservoir for the Yakima Project, an irrigation project run by the United States Bureau of Reclamation. Although a natural lake, Cle Elum Lake's capacity and discharge is controlled by Cle Elum Dam, a high earthfill structure built in 1933. As a storage reservoir, Cle Elum Lake's active capacity is 436,900 acre feet (539,000,000 m³).

Geographic entities mentioned:
surface_form: cle elum
instance_of: Lake
countries: United States
coordinates: lat: 47.282
lon: -121.107
Cle Elum Lake is the easternmost lake of three large lakes (two are north and one is south of Interstate 90) in the Cascade Range. The middle one, Kachess Lake is also north of I-90 while the westernmost, Keechelus Lake is south of I-90. Cle Elum Lake is part of the Columbia River basin, as the Cle Elum River is a tributary of the Yakima River, which is a tributary to the Columbia River. Usage.

Geographic entities mentioned:
surface_form: cle elum
instance_of: Lake
countries: United States
coordinates: lat: 47.282
lon: -121.107
Mont de Gourze. Mont de Gourze () is a mountain in Switzerland, overlooking Lake Geneva in the canton of Vaud. On the summit is located the medieval lookout tower of Gourze.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
surface_form: mont de gourze
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.511
lon: 6.74079
Mont de Gourze. Mont de Gourze () is a mountain in Switzerland, overlooking Lake Geneva in the canton of Vaud. On the summit is located the medieval lookout tower of Gourze.

Geographic entities mentioned:
surface_form: mont de gourze
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.511
lon: 6.74079
Samson Peak. Samson Peak is a mountain summit located on the eastern shore of Maligne Lake in Jasper National Park, in the Canadian Rockies of Alberta, Canada. The nearest higher peak is Mount Charlton, to the east. Samson Peak is situated 1.72 km south of Leah Peak in the Queen Elizabeth Ranges. History.

Geographic entities mentioned:
surface_form: Maligne Lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.664444444444
lon: -117.53361111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: samson peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.680277777777775
lon: -117.51055555555556
Samson Peak is a mountain summit located on the eastern shore of Maligne Lake in Jasper National Park, in the Canadian Rockies of Alberta, Canada. The nearest higher peak is Mount Charlton, to the east. Samson Peak is situated 1.72 km south of Leah Peak in the Queen Elizabeth Ranges. History. Samson Peak was named by Mary Schäffer in her expedition through the area in 1908 to find Maligne Lake.

Geographic entities mentioned:
surface_form: Leah Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.71222222222222
lon: -117.55388888888889
surface_form: samson peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.680277777777775
lon: -117.51055555555556
History. Samson Peak was named by Mary Schäffer in her expedition through the area in 1908 to find Maligne Lake. She also named nearby Leah Peak for Leah Beaver, the wife of Samson Beaver. Samson was a Stoney Indian who befriended Mary and provided her with a hand drawn map to assist her with finding the way to the elusive lake.

Geographic entities mentioned:
surface_form: Leah Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.71222222222222
lon: -117.55388888888889
Samson was a Stoney Indian who befriended Mary and provided her with a hand drawn map to assist her with finding the way to the elusive lake. Samson visited the lake with his father at the age of 14, and 16 years later he drew the map from memory when he met Mary at Elliott Barnes' cabin on the Kootenay Plains in the Saskatchewan Valley. The first ascent of Samson Peak was made in 1928 by W.R.

Geographic entities mentioned:
surface_form: Saskatchewan Valley
instance_of: Valley
countries: Canada
surface_form: kootenay
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
The nearest higher peak is Mount Charlton, to the east. Samson Peak is situated 1.72 km south of Leah Peak in the Queen Elizabeth Ranges. History. Samson Peak was named by Mary Schäffer in her expedition through the area in 1908 to find Maligne Lake. She also named nearby Leah Peak for Leah Beaver, the wife of Samson Beaver.

Geographic entities mentioned:
surface_form: maligne lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.664444444444
lon: -117.53361111111
surface_form: samson peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.680277777777775
lon: -117.51055555555556
Climate. Based on the Köppen climate classification, Samson Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Samson Peak drains west into Maligne Lake, thence into the Maligne River which is a tributary of the Athabasca River.

Geographic entities mentioned:
surface_form: maligne lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.664444444444
lon: -117.53361111111
surface_form: athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
surface_form: athabasca
instance_of: Mountain
countries: Canada
coordinates: lat: 52.18055555555556
lon: -117.20166666666667
surface_form: samson peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.680277777777775
lon: -117.51055555555556
Samson Peak. Samson Peak is a mountain summit located on the eastern shore of Maligne Lake in Jasper National Park, in the Canadian Rockies of Alberta, Canada. The nearest higher peak is Mount Charlton, to the east. Samson Peak is situated 1.72 km south of Leah Peak in the Queen Elizabeth Ranges. History.

Geographic entities mentioned:
surface_form: mount charlton
instance_of: Mountain
countries: Canada
coordinates: lat: 52.61138888888889
lon: -117.5111111111111
The first ascent of Samson Peak was made in 1928 by W.R. Hainsworth and M.M. Strumia The mountain's name was officially adopted in 1947 by the Geographical Names Board of Canada. Climate. Based on the Köppen climate classification, Samson Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Samson Peak. Samson Peak is a mountain summit located on the eastern shore of Maligne Lake in Jasper National Park, in the Canadian Rockies of Alberta, Canada. The nearest higher peak is Mount Charlton, to the east. Samson Peak is situated 1.72 km south of Leah Peak in the Queen Elizabeth Ranges. History.

Geographic entities mentioned:
surface_form: samson peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.680277777777775
lon: -117.51055555555556
Samson visited the lake with his father at the age of 14, and 16 years later he drew the map from memory when he met Mary at Elliott Barnes' cabin on the Kootenay Plains in the Saskatchewan Valley. The first ascent of Samson Peak was made in 1928 by W.R. Hainsworth and M.M. Strumia The mountain's name was officially adopted in 1947 by the Geographical Names Board of Canada. Climate.

Geographic entities mentioned:
surface_form: samson peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.680277777777775
lon: -117.51055555555556
Hainsworth and M.M. Strumia The mountain's name was officially adopted in 1947 by the Geographical Names Board of Canada. Climate. Based on the Köppen climate classification, Samson Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: samson peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.680277777777775
lon: -117.51055555555556
Tims Ford State Park, also known as Tims Ford State Rustic Park, is a state park in Franklin County, in the U.S. state of Tennessee. The state park is situated on the north shore of Tims Ford Lake near the north escarpment of the Cumberland Plateau, about ten miles from the city of Winchester. History. In 1978, the park opened with, including a visitor center, 20 cabins, and 50 camp sites.

Geographic entities mentioned:
surface_form: Tims Ford Lake
instance_of: Lake
countries: United States
coordinates: lat: 35.196944444444
lon: -86.278611111111
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Geography. Geologically, the park is located in the Highland Rim province, a hilly, slightly dissected area characterized by karst topography and scattered knobs. Terrain within the park is generally steep, except when approaching the lake shore. Tims Ford Lake, from which the park takes its name, was formed by a TVA hydroelectric dam over the Elk River. This dam was completed in 1970.

Geographic entities mentioned:
surface_form: Tims Ford Lake
instance_of: Lake
countries: United States
coordinates: lat: 35.196944444444
lon: -86.278611111111
His music is overheard by the goddess Venus. Instantly &quot;defeated by passion&quot;, she asks Fuchs to join her on Mount Olympus. The act of lovemaking between clueless, overanxious Fuchs and the giant goddess is compromised when Fuchs decides to enter his whole body into Venus' ear.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Geography. The Val Müstair (German: &quot;Münstertal&quot;,) is a mountain valley in the Swiss Alps. It connects the Fuorn Pass, () with the Italian province of South Tyrol and the Vinschgau (). The Benedictine Convent of Saint John at Müstair (&quot;monastery&quot;), a World Heritage Site, was probably founded by Charlemagne, sharing history with its neighbor, the Marienberg Abbey.

Geographic entities mentioned:
surface_form: Vinschgau
instance_of: Valley
countries: Italy
coordinates: lat: 46.615
lon: 10.705
Frenchman Island. Frenchman Island (also known as Frenchman's Island) is a island located in Oneida Lake in Oswego County, New York, United States. It was known historically as &quot;Seven Mile Island&quot; during the American Revolution and by the Onondaga people as &quot;Kah-wha-nah-kee&quot;.

Geographic entities mentioned:
surface_form: Oneida Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.2
lon: -75.9
Howell, New South Wales. Howell is a locality, on the western slopes of the Northern Tablelands, within the New England region of New South Wales, Australia. There was once a mining village of the same name, now a ghost town. Much of the effective western boundary of the locality is part of the shoreline of Lake Copeton, as a portion of the locality is now inundated.

Geographic entities mentioned:
surface_form: Northern Tablelands
instance_of: Plateau
countries: Australia
coordinates: lat: -30.595277777777778
lon: 151.5
Colvin Mountain. Colvin Mountain is a ridge in Calhoun County and Etowah County, Alabama, USA.

Geographic entities mentioned:
surface_form: colvin mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.94871
lon: -85.80858
It is located in the Ancash Region, Bolognesi Province, Aquia District, and in the Recuay Province, Catac District. Minapata lies south of Challwa and northeast of Qiwllarahu.

Geographic entities mentioned:
surface_form: qiwllarahu
instance_of: Mountain
countries: Peru
coordinates: lat: -9.9625
lon: -77.26
Minapata. Minapata (Spanish &quot;mina&quot; mine, Quechua &quot;pata&quot; elevated place; above, at the top; edge, bank (of a river), shore) is a mountain in the southern part of the Cordillera Blanca in the Andes of Peru, about high. It is located in the Ancash Region, Bolognesi Province, Aquia District, and in the Recuay Province, Catac District.

Geographic entities mentioned:
surface_form: minapata
instance_of: Mountain
countries: Peru
coordinates: lat: -9.95167
lon: -77.2264
1913: Inauguration of the Protestant church. 1915: Inauguration of the new Protestant school. 1965: Lake Oedter See begins to be used for bathing. 1973: Traun, the 'biggest village of Austria' is elevated to a city. The Bundesschulzentrum Traun (home of the 2 high schools Bundesrealgymnasium and Handelsakademie) opens. The building's modern design served as model for schools in the 70s.

Geographic entities mentioned:
surface_form: Oedter See
instance_of: Lake
countries: Austria
coordinates: lat: 48.212222222222
lon: 14.221388888889
Sackhorn. The Sackhorn is a mountain of the Bernese Alps, located on the border between the Swiss cantons of Bern and Valais. It lies on the range east of the Lötschen Pass, between the upper Gasterntal and the Lötschental. It lies approximately halfway between the Hockenhorn and the Birghorn.

Geographic entities mentioned:
surface_form: Lötschental
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.416666666667
lon: 7.8333333333333
Sackhorn. The Sackhorn is a mountain of the Bernese Alps, located on the border between the Swiss cantons of Bern and Valais. It lies on the range east of the Lötschen Pass, between the upper Gasterntal and the Lötschental. It lies approximately halfway between the Hockenhorn and the Birghorn.

Geographic entities mentioned:
surface_form: Hockenhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.428333333333
lon: 7.7441666666667
surface_form: Birghorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.453027777778
lon: 7.7889166666667
Sackhorn. The Sackhorn is a mountain of the Bernese Alps, located on the border between the Swiss cantons of Bern and Valais. It lies on the range east of the Lötschen Pass, between the upper Gasterntal and the Lötschental. It lies approximately halfway between the Hockenhorn and the Birghorn.

Geographic entities mentioned:
surface_form: sackhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.439916666667
lon: 7.7658611111111
According to the U.S. Board on Geographic Names, variant names of the Calfpasture River include the Big Calfpasture River, Calf Pasture River, Great Calfpasture River, and North River. Course. The Calfpasture River originates on the slopes of Gordons Peak, in Augusta County, near Shenandoah Mountain, in George Washington National Forest. Its headwater tributaries drain Bald Ridge.

Geographic entities mentioned:
surface_form: Shenandoah Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.5097
lon: -79.1842
Continuing southwest, the river is joined by West Dry Branch from the east, then it enters Deerfield Valley, where the tributaries Tizzle Branch and Still Run join. Deerfield Valley is flanked by Shenandoah Mountain to the west and Great North Mountain to the east. The Calfpasture River flows by the small town of Little Baltimore, after which one of its main tributaries, Hamilton Branch, joins.

Geographic entities mentioned:
surface_form: Great North Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0356
lon: -78.5675
The Krumme Lutter is one of the two headstreams of the Lutter in the southern Harz, north of Bad Lauterberg in the district of Göttingen. It rises below 620 m on the Aschentalshalbe and flows towards the south past the former pits &quot;Wolkenhügel&quot; and &quot;Hoher Trost&quot;, before it unites with the Grade Lutter in &quot;Kupferhütte&quot; to become the Lutter.

Geographic entities mentioned:
surface_form: Aschentalshalbe
instance_of: Mountain
countries: Germany
coordinates: lat: 51.6863
lon: 10.4526
Geography. Tuanjie Lake at the southern edge of the Qaidam subbasin in the eastern Qarhan Playa at an elevation of above sea level. It has an area of. It lies southeast of Dabusun Lake, south of Xiezuo Lake, and west of South Hulsan Lake and is fed by the intermittent stream of the Shougong River &quot;Shōugōng Hé&quot;). Its depth usually does not exceed.

Geographic entities mentioned:
surface_form: Dabusun Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 37.024080555556
lon: 95.138925
surface_form: South Hulsan Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 36.75
lon: 95.81667
Susqueda Reservoir. Susqueda Reservoir (;) is a reservoir located on the Ter River, near Osor, Catalonia, Spain. The dam is located in Osor, while the main water body lies within the municipal boundaries of Susqueda and Sant Hilari Sacalm. Completed in 1968, the dam created a reservoir with a storage capacity of 233 hm³, submerging the former villages of Susqueda and Querós.

Geographic entities mentioned:
surface_form: susqueda reservoir
instance_of: Lake
countries: Spain
coordinates: lat: 41.9792
lon: 2.52722
Dawa Lake. Dawa (;), or Dawacuo, is a lake in Coqên County in the Ngari Prefecture of the Tibet Autonomous Region of China. It is located several kilometres northwest of Coqên Town. Daxiong is a village located beyond its northeastern bank. The name of lake means &quot;Moon Lake&quot; in Tibetan language.

Geographic entities mentioned:
surface_form: dawa lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 31.24444444
lon: 84.95416667
Dawa Lake. Dawa (;), or Dawacuo, is a lake in Coqên County in the Ngari Prefecture of the Tibet Autonomous Region of China. It is located several kilometres northwest of Coqên Town. Daxiong is a village located beyond its northeastern bank. The name of lake means &quot;Moon Lake&quot; in Tibetan language.

Geographic entities mentioned:
surface_form: moon lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.869444
lon: 121.539444
Background. Gallo wrote the film's screenplay while a psychology student at Pennsylvania State University. Gallo based parts of the &quot;Magic Rock&quot; on his own 15 Summers spent at Camp Cody For Boys in Freedom, New Hampshire when a boy, and filmed the project on locations in Lake Ossipee, New Hampshire.

Geographic entities mentioned:
surface_form: Lake Ossipee, New Hampshire
instance_of: Lake
countries: United States
coordinates: lat: 43.791388888889
lon: -71.139722222222
All the water in the municipality is flowing water. Of the unproductive areas, and. The municipality is located in Frauenfeld District, on the southern slope of the Seerücken hills and north of Müllheim. From 1870 until 1998 the village of Homburg, the hamlet of Hörstetten and Klingenberg Castle formed the municipality of Homburg.

Geographic entities mentioned:
surface_form: Seerücken
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.6489
lon: 9.03333
They are the home of a large salmon hatchery owned by the state of Alaska and operated by the Cook Inlet Aquaculture Association. The fish hatched at this facility are released into streams and lakes at various points on the peninsula, and are also the source of the salmon runs at the &quot;fishing hole&quot; on the Homer Spit.

Geographic entities mentioned:
surface_form: Homer Spit
instance_of: Landform
countries: United States
coordinates: lat: 59.62
lon: -151.455
surface_form: homer spit
instance_of: Landform
countries: United States
coordinates: lat: 59.62
lon: -151.455
The fish hatched at this facility are released into streams and lakes at various points on the peninsula, and are also the source of the salmon runs at the &quot;fishing hole&quot; on the Homer Spit. The hatchery was at the center of a prolonged legal battle between the Wilderness Society and the U.S. Fish and Wildlife Service.

Geographic entities mentioned:
surface_form: battle
instance_of: Watercourse
countries: United States
coordinates: lat: 44.9266
lon: -93.0291
Trail Lakes. The Trail Lakes are two lakes on the lower Kenai Peninsula, Alaska. The lakes are near the town of Moose Pass and adjacent to the Seward Highway. They are the home of a large salmon hatchery owned by the state of Alaska and operated by the Cook Inlet Aquaculture Association.

Geographic entities mentioned:
surface_form: trail lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 60.4917
lon: -149.367
The mountain is located in Grand Teton National Park in the U.S. state of Wyoming. The next closest higher summit is more than distant, and this isolation provides sweeping views of the Teton Range, much of the northern Jackson Hole area as well as the Snake River. Though located adjacent to the Tetons, Signal Mountain was not formed in the same manner or period.

Geographic entities mentioned:
surface_form: Jackson Hole
instance_of: Valley
countries: United States
coordinates: lat: 43.516666666667
lon: -110.83333333333
The peak is also partially a glacial moraine formed by a receding glacier that came south out of the Yellowstone icecap. This same glacier also created neighboring Jackson Lake. Signal Mountain has a long road providing vehicular access to an observation area located just below the main summit.

Geographic entities mentioned:
surface_form: jackson lake
instance_of: Lake
countries: United States
coordinates: lat: 33.368
lon: -83.8555
The trail splits mid-way for a portion of approximately, allowing hikers to take either a trail along the lower part of the ridge or south of the ridge past a series of small ponds. The trails then rejoin and steepen over the last mile to reach the secondary summit of the mountain, the Jackson Lake Overlook.

Geographic entities mentioned:
surface_form: jackson lake
instance_of: Lake
countries: United States
coordinates: lat: 33.368
lon: -83.8555
Signal Mountain (Wyoming). Signal Mountain is an isolated summit standing above sea level. The mountain is located in Grand Teton National Park in the U.S. state of Wyoming. The next closest higher summit is more than distant, and this isolation provides sweeping views of the Teton Range, much of the northern Jackson Hole area as well as the Snake River.

Geographic entities mentioned:
surface_form: signal mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2063
lon: -72.3252
surface_form: signal mountain (wyoming)
instance_of: Mountain
countries: United States
coordinates: lat: 43.8489
lon: -110.567
Signal Mountain (Wyoming). Signal Mountain is an isolated summit standing above sea level. The mountain is located in Grand Teton National Park in the U.S. state of Wyoming. The next closest higher summit is more than distant, and this isolation provides sweeping views of the Teton Range, much of the northern Jackson Hole area as well as the Snake River.

Geographic entities mentioned:
surface_form: signal mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2063
lon: -72.3252
surface_form: signal mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.8489
lon: -110.567
The next closest higher summit is more than distant, and this isolation provides sweeping views of the Teton Range, much of the northern Jackson Hole area as well as the Snake River. Though located adjacent to the Tetons, Signal Mountain was not formed in the same manner or period. The mountain originally was formed by volcanic ashfall from one of the eruptions of the Yellowstone hotspot.

Geographic entities mentioned:
surface_form: signal mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2063
lon: -72.3252
surface_form: signal mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.8489
lon: -110.567