Sarmila/GeoWiki-Features huggingface dataset:
Cranberry Pond (Long Lake, Hamilton County, New York). Cranberry Pond is located northwest of Raquette Lake, New York. Fish species present in the pond are brook trout, brown trout, white sucker, sunfish and black bullhead. There is access by trail from Brown Tract Road. No motors are allowed on the pond.

Geographic entities mentioned:
surface_form: cranberry pond
instance_of: Lake
countries: United States
coordinates: lat: 43.839444444444
lon: -74.701666666667
surface_form: raquette lake
instance_of: Lake
countries: United States
coordinates: lat: 43.833333333333
lon: -74.65
Skitt Mountain. Skitt Mountain is a summit in the U.S. state of Georgia. The elevation is 2,076 feet (632 meters). The mountain's name is supposedly derived from the word &quot;skit&quot;, on account of the tall tales or skits, told there by miners.

Geographic entities mentioned:
surface_form: skitt mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.505277777778
lon: -83.722222222222
Further east, Pembroke Mall was built. Gradually, the former farmlands of the two counties gave way to development, and eventually expansion of the independent cities through annexations and consolidations brought the borders of the cities of Virginia Beach and Norfolk together on Virginia Beach Boulevard, near Newtown Road. Along with a more circuitous route along U.S.

Geographic entities mentioned:
surface_form: Willoughby Spit
instance_of: Landform
countries: United States
coordinates: lat: 36.967
lon: -76.282472222222
The unit flew free fighter sweeps (&quot;Freie Jagd&quot;). This lasted only days, and I./JG 51 moved southward to Lake Ilmen to provide air cover for the vulnerable Demyansk pocket survivors. In October 1942 the unit moved south again, this time the Rzhev-Vyazma salient. It was at this location the Fw 190 started to make an impact.

Geographic entities mentioned:
surface_form: Lake Ilmen
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 58.266666666667
lon: 31.283333333333
Hungarian Fw 190 operations (November 1944–1945). On 8 November 1944, Germany delivered sixteen Fw 190 F-8 fighters (&quot;G5+01&quot; and &quot;G5+02&quot;) to the Hungarian Royal Air Force for training. They were initially based in Börgönd, near Lake Balaton, under the command of &quot;Lfl. Kdo 4, Fliegerführer 102 Hungarn&quot;/&quot;VIII Fliegerkorps&quot; (HQ in Debrecen).

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
Volvic (mineral water). Volvic () is a French brand of mineral water. Its source is in the Chaîne des Puys-Limagne Fault, Auvergne Volcanoes Natural Regional Park, at the Puy de Dôme in central France. Over 50% of the production of Volvic water is exported to more than sixty countries throughout the world.

Geographic entities mentioned:
surface_form: Puy de Dôme
instance_of: Mountain
countries: France
coordinates: lat: 45.772
lon: 2.9624
The latter would be built nearly a sea level, and would have spectators on one end and a glass wall on the other, giving a view of the Trondheimsfjord. Freestyle and snowboarding would be located at Vassfjellet. Alpine skiing and sliding sports would be located in the nearby Oppdal Municipality. With the exception of Brattøra, all venues would have been built in connection with existing venues.

Geographic entities mentioned:
surface_form: Vassfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 63.261666666667
lon: 10.355833333333
University of Utah presidents. bca7p280rv9qusxqgcwes8uffajod8" xml:space="preserve">The University of Utah presidents include all sixteen men and women who served as president of the University of Utah or its predecessor the University of Deseret, which was founded in 1850 just a few years after the Mormon Pioneers arrived in the Salt Lake Valley. List of presidents.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
The area around the lake with all the summer cottages was until recently a popular summer holiday destination for many German, Dutch and Austrian tourists, but the last ten years, after the increasing popularity of Lake Balaton and other bigger places in Hungary, these visitors are almost absent today.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
state of Utah during December 25–31, 2003. Many areas of Utah were paralyzed by up to of snow. The Wasatch Front from the Salt Lake Valley northward saw generally 1–3 feet of snow (30–90 cm), with up to four feet on the benches, while the surrounding mountains generally saw 5–7 feet of snow (1.5–2 m), with up to nine feet in some areas.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
Of the five people killed in the storm, an avalanche on the east side of Mount Timpanogos killed three snowboarders on December 26, while traffic accidents killed two people on December 28. In addition, at least one million people along the Wasatch Front lost power just on the first day of the storm, and at least 2,000 traffic accidents were reported (most of them along the Wasatch Front).

Geographic entities mentioned:
surface_form: Mount Timpanogos
instance_of: Mountain
countries: United States
coordinates: lat: 40.390836111111
lon: -111.64594444444
Judge Daly Promontory. The Judge Daly Promontory is a peninsula located on the eastern coast of Ellesmere Island, a part of the Qikiqtaaluk Region of the Canadian territory of Nunavut. It stretches from the southwest northeastward into Nares Strait. Lady Franklin Bay is to the north, Archer Fiord to the west, and Cape Baird is its northernmost point.

Geographic entities mentioned:
surface_form: Nares Strait
instance_of: Watercourse
countries: Greenland
Canada
coordinates: lat: 80
lon: -70
Distribution. Powelliphanta are endemic to New Zealand, ranging in the North Island from Lake Waikaremoana to the Kāpiti Coast, and in the South Island from the Marlborough Sounds to Fiordland and Southland. Their greatest diversity is in the mountains of northwest Nelson and north Westland.

Geographic entities mentioned:
surface_form: Lake Waikaremoana
instance_of: Lake
countries: New Zealand
coordinates: lat: -38.766666666667
lon: 177.08333333333
Juppongatana. The are a group of ten elite assassins founded and commanded by Shishio Makoto to assassinate Meiji government officials upon their planned revolution. Based in Mount Hiei, they are the primary antagonist group of the Kyoto arc. Although he does not officially join them, Aoshi works with the Juppongatana in order to fight Kenshin again, even allowing them to attack Aoi-Ya.

Geographic entities mentioned:
surface_form: Mount Hiei
instance_of: Mountain
countries: Japan
coordinates: lat: 35.066666666667
lon: 135.83833333333
In 1985, the island had 5,881 inhabitants, but by 2019 the population fell to a record low of 4,591. Geography. The highest point of Suðuroy is the mountain Gluggarnir (), but the most famous peak is definitely the mountain of Beinisvørð northwest of the village of Sumba. The Beinisvørð and its scenery have been praised by the local poet Poul F. Joensen (1898–1970), as well as other Faroese poets.

Geographic entities mentioned:
surface_form: Gluggarnir
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 61.55
lon: -6.8666666666667
surface_form: Beinisvørð
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 61.426388888889
lon: -6.7672222222222
The small fishing harbour is inside this reef. There is a lake just above the village, called Kirkjuvatn, the path starts near the church. Another attraction in Fámjin are the cliffs and gorge west of the village, called Prestgjógv (Priest Gorge). The main attraction of Fámjin however is the original Faroese flag, Merkið, which is hanging inside of the church.

Geographic entities mentioned:
surface_form: Kirkjuvatn
instance_of: Lake
countries: Faroe Islands
coordinates: lat: 61.5299
lon: -6.8757
Aneto glacier. The Aneto glacier (Aragonese: Glaciar d'Aneto, Spanish: &quot;Glaciar del Aneto&quot;) is a glacier located on the northwestern flank of Aneto in the Pyrenees. It is the greatest glacier in the Pyrenees and the Iberian Peninsula and the 8th southernmost glacier in Europe.

Geographic entities mentioned:
surface_form: Aneto
instance_of: Mountain
countries: Spain
coordinates: lat: 42.63099166666667
lon: 0.6566861111111112
Champagne Pool. Champagne Pool is a prominent geothermal feature within the Waiotapu geothermal area in the North Island of New Zealand. The terrestrial hot spring is located about southeast of Rotorua and about northeast of Taupō. The name Champagne Pool is derived from the abundant efflux of carbon dioxide (CO2), similar to a glass of bubbling champagne.

Geographic entities mentioned:
surface_form: champagne pool
instance_of: Lake
countries: New Zealand
coordinates: lat: -38.359109
lon: 176.369057
The terrestrial hot spring is located about southeast of Rotorua and about northeast of Taupō. The name Champagne Pool is derived from the abundant efflux of carbon dioxide (CO2), similar to a glass of bubbling champagne. The hot spring was formed 900 years ago by a hydrothermal eruption, which makes it in geological terms a relatively young system.

Geographic entities mentioned:
surface_form: champagne pool
instance_of: Lake
countries: New Zealand
coordinates: lat: -38.359109
lon: 176.369057
Its crater is about in diameter with a maximum depth around and is filled with an estimated volume of of geothermal fluid. Hydrochemistry. The deep geothermal water below Champagne Pool is of the order of but water temperature within the pool is maintained at to by losing heat to the atmosphere. The pH of 5.5 is relatively constant due to buffering by the flux of CO2.

Geographic entities mentioned:
surface_form: champagne pool
instance_of: Lake
countries: New Zealand
coordinates: lat: -38.359109
lon: 176.369057
The siliceous geothermal fluid is oversaturated with metalloid compounds such as orpiment (As2S3) and stibnite (Sb2S3), which precipitate and form orange subaqueous deposits. The colourful deposits are in sharp contrast to the grey-white silica sinter surrounding Champagne Pool. Biology.

Geographic entities mentioned:
surface_form: champagne pool
instance_of: Lake
countries: New Zealand
coordinates: lat: -38.359109
lon: 176.369057
Biology. Although Champagne Pool is geochemically well characterised, few studies have addressed its role as a potential habitat for microbial life forms. H2 and either CO2 or O2 would be available as metabolic energy sources for autotrophic growth of methanogenic or hydrogen-oxidising microorganisms.

Geographic entities mentioned:
surface_form: champagne pool
instance_of: Lake
countries: New Zealand
coordinates: lat: -38.359109
lon: 176.369057
H2 and either CO2 or O2 would be available as metabolic energy sources for autotrophic growth of methanogenic or hydrogen-oxidising microorganisms. Culture-independent methods provided evidence for filamentous, coccoid, and rod-shaped cell morphologies in the hot spring. Two novel bacteria and a novel archaeon have been successfully isolated from Champagne Pool.

Geographic entities mentioned:
surface_form: champagne pool
instance_of: Lake
countries: New Zealand
coordinates: lat: -38.359109
lon: 176.369057
Greenleaf Peak. Greenleaf Peak is a mountain in the Cascade Range in the U.S. state of Washington, located on the north side of the Columbia River near Table Mountain, in the Columbia River Gorge. The peak lies within the Columbia River Gorge National Scenic Area near Bonneville Dam. It is in elevation.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: greenleaf peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.7138356
lon: -121.9669576
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
It is in elevation. Botanist David Douglas climbed to the summit in September 1825, making this the first recorded mountain ascent in what is now Washington state. Just south of the summit of Greenleaf Peak there is a dramatic escarpment called Red Bluffs, which connects Greenleaf Peak and Table Mountain. Approximately of the Eagle Creek formation are exposed at Red Bluffs.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: greenleaf peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.7138356
lon: -121.9669576
surface_form: greenleaf peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.7138356
lon: -121.9669576
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
Approximately of the Eagle Creek formation are exposed at Red Bluffs. The Red Bluffs escarpment was created by the repeated collapse of Greenleaf Peak and Table Mountain. Massive landslides have fallen from the mountains, creating a area of debris called the Cascade Landslide Complex.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: greenleaf peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.7138356
lon: -121.9669576
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
The whole area is inclined south toward and beyond the Columbia River. There may have been a cinder cone between Greenleaf Peak and Table Mountain which collapsed during the Bonneville Slide. The propensity of the area south of Greenleaf Peak and Table Mountain to collapse in landslides is due to the Eagle Creek formation.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: greenleaf peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.7138356
lon: -121.9669576
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
The whole area is inclined south toward and beyond the Columbia River. There may have been a cinder cone between Greenleaf Peak and Table Mountain which collapsed during the Bonneville Slide. The propensity of the area south of Greenleaf Peak and Table Mountain to collapse in landslides is due to the Eagle Creek formation.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: greenleaf peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.7138356
lon: -121.9669576
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
The formation is topped with basalt. Water can percolate through the basalt and saturate the Eagle Creek formation. In places where the formation is relatively close to the surface and inclined downslope, such as near Greenleaf Peak and Table Mountain, water saturation can cause the formation's material to slide away, carrying the overlying basalt with it.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: greenleaf peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.7138356
lon: -121.9669576
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
In places where the formation is relatively close to the surface and inclined downslope, such as near Greenleaf Peak and Table Mountain, water saturation can cause the formation's material to slide away, carrying the overlying basalt with it. Between Greenleaf Peak and Table Mountain, and above the Red Bluffs, lies Greenleaf Basin.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: greenleaf peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.7138356
lon: -121.9669576
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
Greenleaf Creek flows south through the basin before plunging as a waterfall over the Red Bluffs escarpment. In the winter of 2007-2008, there was a large landslide on the south slope of Greenleaf Peak, in the state-owned Table Mountain Natural Resources Conservation Area. Some of a timbered rocky cliff slid, burying approximately of forest under rubble.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: greenleaf peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.7138356
lon: -121.9669576
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
The propensity of the area south of Greenleaf Peak and Table Mountain to collapse in landslides is due to the Eagle Creek formation. The rocks of the formation cover approximately of the Columbia River Gorge east of Cape Horn and consist of a mixture of past landslides, volcanic mud flows and ash falls. The formation is topped with basalt.

Geographic entities mentioned:
surface_form: cape horn
instance_of: Mountain
countries: United States
coordinates: lat: 47.657222222222
lon: -120.91694444444
The peak lies within the Columbia River Gorge National Scenic Area near Bonneville Dam. It is in elevation. Botanist David Douglas climbed to the summit in September 1825, making this the first recorded mountain ascent in what is now Washington state. Just south of the summit of Greenleaf Peak there is a dramatic escarpment called Red Bluffs, which connects Greenleaf Peak and Table Mountain.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Greenleaf Peak. Greenleaf Peak is a mountain in the Cascade Range in the U.S. state of Washington, located on the north side of the Columbia River near Table Mountain, in the Columbia River Gorge. The peak lies within the Columbia River Gorge National Scenic Area near Bonneville Dam. It is in elevation.

Geographic entities mentioned:
surface_form: greenleaf peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.7138356
lon: -121.9669576
The location operated until 2023 at which time it ceased operations. Central Penn College Lehigh Valley location (closed in 2015). In May 2009, Central Penn College opened a location in the Lehigh Valley at the Lehigh Valley Corporate Center in Bethlehem, PA. The location operated until the winter of 2015 at which time it ceased operations. Athletics.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
The Nerang River, Albert River and Coomera River all have their source in Lamington National Park. Eastern parts of the park feature high cliffs which rise above the Numinbah Valley. The park is within the City of Gold Coast and Scenic Rim Region local government areas. Southern Lamington and sections of O'Reilly, Binna Burra and Natural Bridge are protected with Lamington National Park. History.

Geographic entities mentioned:
surface_form: Numinbah Valley
instance_of: Valley
countries: Australia
coordinates: lat: -28.141127777778
lon: 153.22403055556
Geology. The Lamington National Park is located on the northern side of the Tweed volcano. This large shield volcano is over 100 kilometres in diameter, and extends from Tamborine Mountain in the north to Lismore in the south. The volcanic plug of Mount Warning marks the centre of the volcano.

Geographic entities mentioned:
surface_form: Tamborine Mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -27.927513888889
lon: 153.19430555556
The monastery was revived in the early 19th century through the strong leadership of Abbot Philaret (Danilevsky), who served as the monastery’s superior for over twenty years. He restored the monastic order and revived its hesychastic spirit through introducing a new monastic rule based on the order of monasteries on Mount Athos as well as the precepts of Paisius Velichkovsky.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Later that same year, Lakedance announced the signing of a title sponsor, Schweitzer Mountain Resort, and a modification of their name and logo to read &quot;Schweitzer Lakedance&quot;. Also, two new events were added to the film festival: The first ever outdoor screening at Sandpoint's City Beach Park, free to the public, and VIP cruises on Lake Pend Oreille aboard the Shawnodese.

Geographic entities mentioned:
surface_form: Lake Pend Oreille
instance_of: Lake
countries: United States
coordinates: lat: 48.166666666667
lon: -116.33333333333
Setting. The first quarter of the book is set in Connecticut while the rest is set in the northern part of Scotland, in the area known as Orkney. The majority of the action takes place in small towns or villages, occasionally in a forest or a castle. The castle of Castle Glanach is on the coast of the Loch of Stenness. Author.

Geographic entities mentioned:
surface_form: Loch of Stenness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 59
lon: -3.25
Potamia, Xanthi. Potamia () is a settlement in the Xanthi regional unit of Greece. It is located two kilometers west of Nea Kessani and is also three kilometers southwest of Lake Vistonida. In 1991, the settlement contained 197 inhabitants.

Geographic entities mentioned:
surface_form: Lake Vistonida
instance_of: Lake
countries: Greece
coordinates: lat: 41.039444444444
lon: 25.114722222222
The official opening took place with a train consisting of an FS Class E444 locomotive and &quot;Gran Comfort&quot; coaches. The section of line between Città della Pieve and Arezzo was completed on 29 September 1985; the section between Valdarno and Florence was opened on 30 May 1986 and finally on 26 May 1992 the section between Arezzo and Valdarno was opened. Route.

Geographic entities mentioned:
surface_form: Valdarno
instance_of: Valley
countries: Italy
coordinates: lat: 43.566666666667
lon: 11.533333333333
In 1985, Emily J. Lott proposed reclassifying &quot;A. chaplinei&quot; as &quot;Aquilegia chrysantha&quot; var. &quot;chaplinei&quot; in the journal &quot;Phytologia&quot;. Lott's proposal came out of her study of plants in the Chihuahuan Desert, stemming from her 1979 unpublished master's thesis on &quot;Aquilegia&quot; in the Trans-Pecos region of Texas.

Geographic entities mentioned:
surface_form: Trans-Pecos
instance_of: Valley
countries: United States
coordinates: lat: 30.56
lon: -103.79
On the night of April 26, 1777, after learning the news that the British had begun burning nearby Danbury, Connecticut, sixteen-year-old Sybil Ludington rode the entire night through the hamlets of Carmel, Mahopac, Kent Cliffs and Farmers Mills, warning those along the way that the British were coming before returning home at dawn. A statue memorializing the ride sits alongside Lake Gleneida.

Geographic entities mentioned:
surface_form: Lake Gleneida
instance_of: Lake
countries: United States
coordinates: lat: 41.42
lon: -73.683333333333
Whitecross Mountain. Whitecross Mountain is a summit in Hinsdale County, Colorado, United States. Description. Whitecross Mountain is set west of the Continental Divide in the San Juan Mountains which are a subrange of the Rocky Mountains. It is located north-northeast of Handies Peak on land administered by the Bureau of Land Management.

Geographic entities mentioned:
surface_form: whitecross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.930555555556
lon: -107.49305555556
Description. Whitecross Mountain is set west of the Continental Divide in the San Juan Mountains which are a subrange of the Rocky Mountains. It is located north-northeast of Handies Peak on land administered by the Bureau of Land Management. Whitecross Mountain is the seventh-highest peak in the Handies Peak Wilderness Study Area.

Geographic entities mentioned:
surface_form: Handies Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.913055555556
lon: -107.50444444444
It is located north-northeast of Handies Peak on land administered by the Bureau of Land Management. Whitecross Mountain is the seventh-highest peak in the Handies Peak Wilderness Study Area. Precipitation runoff from the mountain drains into the Lake Fork of the Gunnison River. Topographic relief is significant as the summit rises above Lake Fork in 0.8 mile (1.3 km).

Geographic entities mentioned:
surface_form: handies peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.913055555556
lon: -107.50444444444
surface_form: whitecross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.930555555556
lon: -107.49305555556
Climate. According to the Köppen climate classification system, Whitecross Mountain is located in an alpine subarctic climate zone with cold, snowy winters, and cool to warm summers. Due to its altitude, it receives precipitation all year, as snow in winter and as thunderstorms in summer, with a dry period in late spring.

Geographic entities mentioned:
surface_form: whitecross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.930555555556
lon: -107.49305555556
It has about 700 inhabitants. Geography. Chvalovice is located about southeast of Znojmo and southwest of Brno, on the border with Austria. It lies in an agricultural landscape in the Dyje–Svratka Valley. The highest point is at above sea level. History. The first written mention of Chvalovice is from 1279.

Geographic entities mentioned:
surface_form: Dyje–Svratka Valley
instance_of: Valley
countries: Czech Republic
coordinates: lat: 49
lon: 16.5
Shaheeya Peak. Shaheeya Peak () is located in the Livingston Range, Glacier National Park in the U.S. state of Montana. Shaheeya Lake is just east of the peak and Wahseeja Lake is to the northwest.

Geographic entities mentioned:
surface_form: Shaheeya Lake
instance_of: Lake
countries: United States
coordinates: lat: 48.9561
lon: -113.959
surface_form: Wahseeja Lake
instance_of: Lake
countries: United States
coordinates: lat: 48.9592
lon: -113.982
Shaheeya Peak. Shaheeya Peak () is located in the Livingston Range, Glacier National Park in the U.S. state of Montana. Shaheeya Lake is just east of the peak and Wahseeja Lake is to the northwest.

Geographic entities mentioned:
surface_form: shaheeya peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.9558
lon: -113.973
Prior to 1968, teams left at timed intervals. Major sponsor Grayling Chamber of Commerce withdrew their support in 1961 and the race began at the Camp 10 bridge in the morning and ended at Lake Huron. For most of the following seven years, all teams began on Saturday morning in Grayling, stopped for the night in Mio, with pro teams resuming the race Sunday morning from Mio to Oscoda.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Administratively the mountain belongs to the Usseglio municipality (&quot;comune&quot;). On the summit a cairn bears a small Jesus Christ statue; on another nearby cairn is located a lightning rod. In clear days it offers a good view of many important mountains of Western Alps including Argentera group, Viso, Dauphiné Alps, Bianco, Gran Paradiso and Rosa. History.

Geographic entities mentioned:
surface_form: Argentera
instance_of: Mountain
countries: Italy
coordinates: lat: 44.18
lon: 7.306
surface_form: Gran Paradiso
instance_of: Mountain
countries: Italy
coordinates: lat: 45.533333333333
lon: 7.2666666666667
surface_form: viso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
surface_form: gran paradiso
instance_of: Mountain
countries: Italy
coordinates: lat: 45.533333333333
lon: 7.2666666666667
History. The first recorded ascent to Punta Sulè was carried out by Filippo Vallino on August 16, 1880. Access to the summit. The usual route to Punta Sulè starts from lago di Malciaussia and, after Pian Sulè, reaches the summit following the SW ridge of the mountain. While long (around 1,600 metres of vertical drop) this route does not require alpinistic skills but just scrambling.

Geographic entities mentioned:
surface_form: lago di Malciaussia
instance_of: Lake
countries: Italy
coordinates: lat: 45.206944444444
lon: 7.1416666666667
surface_form: lago di malciaussia
instance_of: Lake
countries: Italy
coordinates: lat: 45.206944444444
lon: 7.1416666666667
surface_form: malciaussia
instance_of: Lake
countries: Italy
coordinates: lat: 45.206944444444
lon: 7.1416666666667
Punta Sulè. Punta Sulè (in Piedmontese Ponta Solé) is a 3,384 m a.s.l.mountain of the Graian Alps, located in Italy. Geography. The mountain is the highest elevation of the ridge between the terminal dales of the Stura di Viù valley, Peraciaval (North) and Malciaussia (South).

Geographic entities mentioned:
surface_form: punta sulè
instance_of: Mountain
countries: Italy
coordinates: lat: 45.231
lon: 7.137
Punta Sulè. Punta Sulè (in Piedmontese Ponta Solé) is a 3,384 m a.s.l.mountain of the Graian Alps, located in Italy. Geography. The mountain is the highest elevation of the ridge between the terminal dales of the Stura di Viù valley, Peraciaval (North) and Malciaussia (South).

Geographic entities mentioned:
surface_form: punta sulè
instance_of: Mountain
countries: Italy
coordinates: lat: 45.231
lon: 7.137
surface_form: ponta solé
instance_of: Mountain
countries: Italy
coordinates: lat: 45.231
lon: 7.137
Geography. The mountain is the highest elevation of the ridge between the terminal dales of the Stura di Viù valley, Peraciaval (North) and Malciaussia (South). Going NW the Sulè pass divides Punta Sulè from &quot;Testa Sulà&quot; (3,073 m a.s.l.), while going East the &quot;Colletto della Lera&quot; (3,320 m a.s.l.) separates it from Monte Lera.

Geographic entities mentioned:
surface_form: punta sulè
instance_of: Mountain
countries: Italy
coordinates: lat: 45.231
lon: 7.137
surface_form: lera
instance_of: Mountain
countries: Italy
coordinates: lat: 45.17972222
lon: 7.45388889
surface_form: lera
instance_of: Mountain
countries: Italy
coordinates: lat: 45.17972222
lon: 7.45388889
surface_form: monte lera
instance_of: Mountain
countries: Italy
coordinates: lat: 45.17972222
lon: 7.45388889
Geography. The mountain is the highest elevation of the ridge between the terminal dales of the Stura di Viù valley, Peraciaval (North) and Malciaussia (South). Going NW the Sulè pass divides Punta Sulè from &quot;Testa Sulà&quot; (3,073 m a.s.l.), while going East the &quot;Colletto della Lera&quot; (3,320 m a.s.l.) separates it from Monte Lera.

Geographic entities mentioned:
surface_form: malciaussia
instance_of: Lake
countries: Italy
coordinates: lat: 45.206944444444
lon: 7.1416666666667
USS Mount Hood (AE-29). USS &quot;Mount Hood&quot; (AE-29) was a Kilauea-class ammunition ship in the United States Navy. She was the second Navy munitions ship to be named after Mount Hood, a volcano in the Cascade Range in Oregon. &quot;Mount Hood&quot; was laid down 8 May 1967 by Bethlehem Steel Corporation, Sparrows Point, Maryland; launched 17 July 1968; sponsored by Mrs. Robert A.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
Hastings Lake (Alberta). Hastings Lake is a lake in Alberta, Canada. It is located in Strathcona County, east of Cooking Lake. The hamlet of Hastings Lake lies on the southern shore of the lake. The lake was named in 1884 for Tom Hastings, a member of Tyrell's geological survey party. The Cree name for the lake was &quot;Kawtikh&quot;, which means &quot;the lake that does not freeze&quot;.

Geographic entities mentioned:
surface_form: cooking lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4331
lon: -113.029
The Cree name for the lake was &quot;Kawtikh&quot;, which means &quot;the lake that does not freeze&quot;. The large forested area in the Hastings Lake watershed is a key area for moose and white-tailed deer. With close proximity to the Cooking Lake-Blackfoot Wildlife, Grazing and Provincial Recreation Area and the Waskahegan Staging Area, many hiking and cross-country skiing possibilities exists.

Geographic entities mentioned:
surface_form: cooking lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4331
lon: -113.029
The Cree name for the lake was &quot;Kawtikh&quot;, which means &quot;the lake that does not freeze&quot;. The large forested area in the Hastings Lake watershed is a key area for moose and white-tailed deer. With close proximity to the Cooking Lake-Blackfoot Wildlife, Grazing and Provincial Recreation Area and the Waskahegan Staging Area, many hiking and cross-country skiing possibilities exists.

Geographic entities mentioned:
surface_form: moose
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.91444444444444
lon: -118.80638888888889
surface_form: hastings lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4175
lon: -112.91
Hastings Lake (Alberta). Hastings Lake is a lake in Alberta, Canada. It is located in Strathcona County, east of Cooking Lake. The hamlet of Hastings Lake lies on the southern shore of the lake. The lake was named in 1884 for Tom Hastings, a member of Tyrell's geological survey party. The Cree name for the lake was &quot;Kawtikh&quot;, which means &quot;the lake that does not freeze&quot;.

Geographic entities mentioned:
surface_form: hastings lake (alberta)
instance_of: Lake
countries: Canada
coordinates: lat: 53.4175
lon: -112.91
Hastings Lake (Alberta). Hastings Lake is a lake in Alberta, Canada. It is located in Strathcona County, east of Cooking Lake. The hamlet of Hastings Lake lies on the southern shore of the lake. The lake was named in 1884 for Tom Hastings, a member of Tyrell's geological survey party. The Cree name for the lake was &quot;Kawtikh&quot;, which means &quot;the lake that does not freeze&quot;.

Geographic entities mentioned:
surface_form: hastings lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4175
lon: -112.91
Grauhorn. The Grauhorn is a mountain of the Lepontine Alps, located on the border between the Swiss cantons of Ticino and Graubünden. It lies north of the Rheinwaldhorn, on the range between the Val Carassino and the Länta valley. On the north side of the mountain is a glacier named &quot;Grauhorngletscher&quot;.

Geographic entities mentioned:
surface_form: Rheinwaldhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.493611111111
lon: 9.04
Grauhorn. The Grauhorn is a mountain of the Lepontine Alps, located on the border between the Swiss cantons of Ticino and Graubünden. It lies north of the Rheinwaldhorn, on the range between the Val Carassino and the Länta valley. On the north side of the mountain is a glacier named &quot;Grauhorngletscher&quot;.

Geographic entities mentioned:
surface_form: grauhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.505
lon: 9.02805556
During Indonesian rule, there was an airstrip north of Vila Maumeta, but now it is unusable by fixed-wing aircraft (IATA designation: AUT (WPAT)). At 999 m above sea level, Mount Manucoco is the island's highest point. The ocean strait between Atauro and Timor drops 3500 m below sea level; conversely, it is much shallower along the ridge leading to Wetar.

Geographic entities mentioned:
surface_form: Manucoco
instance_of: Mountain
countries: Timor-Leste
coordinates: lat: -8.26944
lon: 125.574
History. Historically, Atauro was divided into three political domains. The Makili domain, southeast of the Manucoco volcano, was composed of 12 clans (&quot;uma lisan&quot;). Macadede, in the southwest portion of the island, and Mandroni, in the north and central part of Atauro, both contained 7 clans.

Geographic entities mentioned:
surface_form: Manucoco volcano
instance_of: Mountain
countries: Timor-Leste
coordinates: lat: -8.26944
lon: 125.574
Its lowest elevation is above sea level and directs to Citarum River. Its highest elevation is above sea level, which is part of the slope of mount Tangkuban Perahu and Burangrang. The Cimahi River flows through the city and Cimahi also has two Springs, named Cikuda and Cisontok. Climate.

Geographic entities mentioned:
surface_form: Tangkuban Perahu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -6.77
lon: 107.6
It has an elevation of 1,248 metres. Angavo is situated north of Andalanimanga. An ancient lake called the Lake Alaotra is located at the foot of the massive escarpment. The south is occupied by the Mahafaly and the Androy plateaus forming precipitous cliffs hanging over the sea.

Geographic entities mentioned:
surface_form: Lake Alaotra
instance_of: Lake
countries: Madagascar
coordinates: lat: -17.5
lon: 48.5
surface_form: alaotra
instance_of: Lake
countries: Madagascar
coordinates: lat: -17.5
lon: 48.5
The south is occupied by the Mahafaly and the Androy plateaus forming precipitous cliffs hanging over the sea. The west transforms into a big expanse of steps and the central plateau is again challenged by an impassable escarpment called the Cliff of Bongolava. The Mount Ambohitra stands in the extreme north with a number of volcanic craters.

Geographic entities mentioned:
surface_form: Mount Ambohitra
instance_of: Mountain
countries: Madagascar
coordinates: lat: -12.4833
lon: 49.2
surface_form: ambohitra
instance_of: Mountain
countries: Madagascar
coordinates: lat: -12.4833
lon: 49.2