Sarmila/GeoWiki-Features huggingface dataset:
The islands were named &quot;Flenserne&quot; on a chart of 1912–13 by Norwegian whaling captain Petter Sorlle. The name Flensing Islands, suggested by the earlier Norwegian name, was used by Discovery Investigations personnel on the &quot;Discovery II&quot; who surveyed the group in 1933. Flensing is the process of stripping skin and blubber from whales.

Geographic entities mentioned:
surface_form: discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: discovery
instance_of: Body of water
coordinates: lat: -64.5167
lon: -63.0167
surface_form: discovery
instance_of: Body of water
coordinates: lat: -64.5167
lon: -63.0167
surface_form: flensing
instance_of: Mountain
coordinates: lat: -60.7
lon: -45.6833
Flensing Islands. The Flensing Islands () are a group of small islands lying west of Foca Point on the west side of Signy Island, in the South Orkney Islands. The islands were named &quot;Flenserne&quot; on a chart of 1912–13 by Norwegian whaling captain Petter Sorlle.

Geographic entities mentioned:
surface_form: flensing
instance_of: Mountain
coordinates: lat: -60.7
lon: -45.6833
Flensing Islands. The Flensing Islands () are a group of small islands lying west of Foca Point on the west side of Signy Island, in the South Orkney Islands. The islands were named &quot;Flenserne&quot; on a chart of 1912–13 by Norwegian whaling captain Petter Sorlle.

Geographic entities mentioned:
surface_form: flenserne
instance_of: Mountain
coordinates: lat: -60.7
lon: -45.6833
Hinterautal-Vomper Chain. The Hinterautal-Vomper Chain (), also called the main chain of the Karwendel (&quot;Karwendelhauptkette&quot;), is the longest mountain chain in the Karwendel Alps in Austria. It has numerous peaks that reach heights of 2,500 m, including the highest summit of the Karwendel, the Birkkarspitze (), and its neighbour, the three Ödkarspitzen.

Geographic entities mentioned:
surface_form: Birkkarspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.411389
lon: 11.4375
Garfield, Bonner County, Idaho. Garfield is an unincorporated community in Bonner County, in the U.S. state of Idaho. The community is situated on Garfield Bay, an inlet of Lake Pend Oreille. History. A variant name is &quot;Midas&quot;. A post office called Midas was established in 1909, and remained in operation until 1939. Midas' population was estimated at 50 in 1960.

Geographic entities mentioned:
surface_form: Lake Pend Oreille
instance_of: Lake
countries: United States
coordinates: lat: 48.166666666667
lon: -116.33333333333
Afon Cwmnantcol. The River Cwmnantcol (&quot;Afon Cwmnantcol&quot; in Welsh) is a river in North Wales. It is about long and has its source at the head of Cwm Nantcol below Rhinog Fawr and Y Llethr. It flows north-west from its source and joins the Afon Artro at Pentre Gwynfryn.

Geographic entities mentioned:
surface_form: Cwm Nantcol
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.819
lon: -4.018
surface_form: Rhinog Fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.841688888889
lon: -3.9968694444444
surface_form: Y Llethr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.81285
lon: -3.98763
Balgyosan. Balgyosan () is a mountain that sits between the counties of Hoengseong and Hongcheon, Gangwon Province, South Korea. It has an elevation of.

Geographic entities mentioned:
surface_form: balgyosan
instance_of: Mountain
countries: South Korea
Little San Pascual Mountain. Little San Pascual Mountain is a summit in Socorro County, New Mexico. It rises to an elevation of.

Geographic entities mentioned:
surface_form: little san pascual mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.720555555556
lon: -106.86027777778
The center of the range is covered by a long ice cap stretching from the Fuchs Dome in the west to Shotton Snowfield in the east, and bounded by cliffs as high as. Fuchs Dome extends from Stratton Glacier east to Crossover Pass, where the plateau narrows to under in width. It has an average height of around, and gradually slopes to the north down to.

Geographic entities mentioned:
surface_form: Crossover Pass
instance_of: Landform
coordinates: lat: -80.6333
lon: -26.5
surface_form: fuchs dome
instance_of: Mountain
coordinates: lat: -80.6
lon: -27.8333
The flat areas free of ice at the edge of the Fuchs Dome and Shotton Snowfield and the table mountains that surround them are the remnants of the peneplain. Stratton Glacier. A glacier long, flowing north from Pointer Nunatak and then northwest to the north of Mount Weston, in the Shackleton Range. First mapped in 1957 by the CTAE and named for David G.

Geographic entities mentioned:
surface_form: Pointer Nunatak
instance_of: Mountain
coordinates: lat: -80.6167
lon: -29
surface_form: Mount Weston
instance_of: Mountain
coordinates: lat: -80.4667
lon: -29.1667
surface_form: weston
instance_of: Mountain
coordinates: lat: -80.4667
lon: -29.1667
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
Clarkson, BAS geologist, Halley Station, 1968-70, who worked in the area for four seasons, 1968-71, 1977-78; Head, BAS Mineralogy, Geology and Geochemistry Section, 1976-89; at SPRI from 1989. Gordon Glacier. Glacier at least long, flowing north from Crossover Pass through the Shackleton Range to join Slessor Glacier. First mapped in 1957 by the CTAE and named after George P.

Geographic entities mentioned:
surface_form: Crossover Pass
instance_of: Landform
coordinates: lat: -80.6333
lon: -26.5
surface_form: crossover pass
instance_of: Landform
coordinates: lat: -80.6333
lon: -26.5
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
Fuchs Dome. Fuchs Dome () is a large ice-covered dome rising over, between Stratton Glacier and Gordon Glacier in the central part of the Shackleton Range, Antarctica. Exploration. It was first mapped in 1957 by the Commonwealth Trans-Antarctic Expedition (CTAE) and named for Sir Vivian E. Fuchs, leader of the CTAE 1955–58. Topology.

Geographic entities mentioned:
surface_form: fuchs dome
instance_of: Mountain
coordinates: lat: -80.6
lon: -27.8333
Fuchs Dome. Fuchs Dome () is a large ice-covered dome rising over, between Stratton Glacier and Gordon Glacier in the central part of the Shackleton Range, Antarctica. Exploration. It was first mapped in 1957 by the Commonwealth Trans-Antarctic Expedition (CTAE) and named for Sir Vivian E. Fuchs, leader of the CTAE 1955–58. Topology.

Geographic entities mentioned:
surface_form: fuchs dome
instance_of: Mountain
coordinates: lat: -80.6
lon: -27.8333
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
It is a rectangular horst rising above major fault zones now under the Slessor Glacier to the north and Recovery Glacier glacier to the south. The center of the range is covered by a long ice cap stretching from the Fuchs Dome in the west to Shotton Snowfield in the east, and bounded by cliffs as high as.

Geographic entities mentioned:
surface_form: fuchs dome
instance_of: Mountain
coordinates: lat: -80.6
lon: -27.8333
The plateau surface is a discontinuous and faulted undulating peneplain, most visible on the south of the range. The flat areas free of ice at the edge of the Fuchs Dome and Shotton Snowfield and the table mountains that surround them are the remnants of the peneplain. Stratton Glacier.

Geographic entities mentioned:
surface_form: fuchs dome
instance_of: Mountain
coordinates: lat: -80.6
lon: -27.8333
Petersen, captain of the Danish ship Magga Dan which transported members of the CTAE to the Filchner Ice Shelf in 1956-57. Not: Peterson Peak. Clarkson Cliffs. Ice-covered cliffs marked by rock exposures, rising to at the northeast edge of Fuchs Dome, Shackleton Range. Photographed from the air by the U.S. Navy, 1967, and surveyed by BAS, 1968-71. Named by the UK-APC after Peter D.

Geographic entities mentioned:
surface_form: fuchs dome
instance_of: Mountain
coordinates: lat: -80.6
lon: -27.8333
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
First mapped in 1957 by the CTAE and named after George P. Pirie-Gordon, member of the Committee of Management and treasurer of the CTAE, 1955-58. Clayton Ramparts. A line of east–west cliffs rising to over at the south margin of Fuchs Dome, Shackleton Range. Surveyed by the CTAE, 1957, photographed from the air by the U.S. Navy, 1967, and further surveyed by BAS, 1968-71.

Geographic entities mentioned:
surface_form: fuchs dome
instance_of: Mountain
coordinates: lat: -80.6
lon: -27.8333
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
Navy, 1967, and further surveyed by BAS, 1968-71. Named by the UK-APC after Charles A. Clayton, BAS surveyor, Halley Station, 1969-71, who worked in the area. Genghis Hills. Hills rising to to the south of Fuchs Dome and west of Stephenson Bastion, in the Shackleton Range. Photographed from the air by the U. S Navy, 1967, and surveyed by BAS, 1968-71. Named by the UK-APC in 1971 after Graham K.

Geographic entities mentioned:
surface_form: fuchs dome
instance_of: Mountain
coordinates: lat: -80.6
lon: -27.8333
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
surface_form: stephenson bastion
instance_of: Mountain
coordinates: lat: -80.7667
lon: -27.2
A glacier long, flowing north from Pointer Nunatak and then northwest to the north of Mount Weston, in the Shackleton Range. First mapped in 1957 by the CTAE and named for David G. Stratton, surveyor and deputy leader of the transpolar party of the CTAE in 1956-58. Lister Heights. Rock heights on the east side of Stratton Glacier, southwest of Flat Top in the west part of the Shackleton Range.

Geographic entities mentioned:
surface_form: lister heights
instance_of: Mountain
coordinates: lat: -80.5167
lon: -28.5833
Flat Top. Distinctive table mountain, with steep rocky cliffs, northeast of Lister Heights in the west part of the Shackleton Range. First seen and given this descriptive name during the early reconnaissance flights of the CTAE, 1955-58. Visited and mapped by the CTAE in 1957. Petersen Peak. A rock peak () standing southwest of Morris Hills in the north-central part of Shackleton Range.

Geographic entities mentioned:
surface_form: lister heights
instance_of: Mountain
coordinates: lat: -80.5167
lon: -28.5833
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
Lister Heights. Rock heights on the east side of Stratton Glacier, southwest of Flat Top in the west part of the Shackleton Range. First mapped in 1957 by the CTAE and named for Hal Lister, glaciologist with the transpolar party of the CTAE in 1956-58, and leader at the expedition's advance base, &quot;South Ice,&quot; in 1957. Flat Top.

Geographic entities mentioned:
surface_form: flat top
instance_of: Mountain
coordinates: lat: -80.44383
lon: -28.36928
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
Visited and mapped by the CTAE in 1957. Petersen Peak. A rock peak () standing southwest of Morris Hills in the north-central part of Shackleton Range. First mapped in 1957 by the CTAE and named for Hans C. Petersen, captain of the Danish ship Magga Dan which transported members of the CTAE to the Filchner Ice Shelf in 1956-57. Not: Peterson Peak. Clarkson Cliffs.

Geographic entities mentioned:
surface_form: morris
instance_of: Mountain
coordinates: lat: -78.3167
lon: -86.1667
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
It was first mapped in 1957 by the Commonwealth Trans-Antarctic Expedition (CTAE) and named for Sir Vivian E. Fuchs, leader of the CTAE 1955–58. Topology. The Shackleton Range is an ice-covered plateau between high that rises between two large glaciers. It is a rectangular horst rising above major fault zones now under the Slessor Glacier to the north and Recovery Glacier glacier to the south.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
Clayton Ramparts. A line of east–west cliffs rising to over at the south margin of Fuchs Dome, Shackleton Range. Surveyed by the CTAE, 1957, photographed from the air by the U.S. Navy, 1967, and further surveyed by BAS, 1968-71. Named by the UK-APC after Charles A. Clayton, BAS surveyor, Halley Station, 1969-71, who worked in the area. Genghis Hills.

Geographic entities mentioned:
surface_form: charles
instance_of: Mountain
coordinates: lat: -67.38333
lon: 50
Gordon Glacier. Glacier at least long, flowing north from Crossover Pass through the Shackleton Range to join Slessor Glacier. First mapped in 1957 by the CTAE and named after George P. Pirie-Gordon, member of the Committee of Management and treasurer of the CTAE, 1955-58. Clayton Ramparts. A line of east–west cliffs rising to over at the south margin of Fuchs Dome, Shackleton Range.

Geographic entities mentioned:
surface_form: george
instance_of: Mountain
coordinates: lat: -67.71667
lon: 50
Photographed from the air by the U.S. Navy, 1967, and surveyed by BAS, 1968-71. Named by the UK-APC after Peter D. Clarkson, BAS geologist, Halley Station, 1968-70, who worked in the area for four seasons, 1968-71, 1977-78; Head, BAS Mineralogy, Geology and Geochemistry Section, 1976-89; at SPRI from 1989. Gordon Glacier.

Geographic entities mentioned:
surface_form: peter
instance_of: Mountain
coordinates: lat: -70.1833
lon: 64.9333
Matchless Mountain (Colorado). Matchless Mountain is a high mountain summit in the Elk Mountains range of the Rocky Mountains of North America. The mountain is located in Gunnison National Forest, east-southeast (bearing 98°) of the Town of Crested Butte in Gunnison County, Colorado, United States. Geology.

Geographic entities mentioned:
surface_form: high mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0887
lon: -74.2351
surface_form: matchless mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.834166666667
lon: -106.645
Matchless Mountain (Colorado). Matchless Mountain is a high mountain summit in the Elk Mountains range of the Rocky Mountains of North America. The mountain is located in Gunnison National Forest, east-southeast (bearing 98°) of the Town of Crested Butte in Gunnison County, Colorado, United States. Geology.

Geographic entities mentioned:
surface_form: matchless mountain (colorado)
instance_of: Mountain
countries: United States
coordinates: lat: 38.834166666667
lon: -106.645
Geology. During the Laramide Orogeny the area near Matchless Mountain was lifted and Precambrian basement rocks and overlying Paleozoic sedimentary rock were raised high above nearby valleys. This uplift resulted in particularly dramatic rock deformation in the area of the mountain. Folding and multiple normal and thrust faults riddle the area.

Geographic entities mentioned:
surface_form: matchless mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.834166666667
lon: -106.645
Renewed uplift approximately 10 million years ago raised the region to the heights seen today. Forces of erosion by water and ice have since carved the landscape and sculpted the present Matchless Mountain. Included in these erosional forces was Pleistocene glaciation, and glacial deposits fill Dustin Gulch to the north of the mountain.

Geographic entities mentioned:
surface_form: matchless mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.834166666667
lon: -106.645
At the summit of Matchless Mountain are Lower Paleozoic sedimentary rocks, and the lower slopes of the mountain are a mosaic of older Proterozoic (Precambrian) granites and gneiss and younger Pennsylvanian sedimentary rocks of the Belden and Minturn formations along with Middle Tertiary intrusive granitic rocks. Hiking. The summit can be reached most easily from the west.

Geographic entities mentioned:
surface_form: matchless mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.834166666667
lon: -106.645
Hiking. The summit can be reached most easily from the west. The Wheelbarrow Gulch Road (Forest Road 746.1A) leads onto the western slope of Matchless Mountain. A hike to the summit can begin where the road ends at an elevation of (. The summit is a, class-2 hike southeast through subalpine forest, meadow, and alpine tundra. The elevation gain is ().

Geographic entities mentioned:
surface_form: matchless mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.834166666667
lon: -106.645
Matchless Mountain (Colorado). Matchless Mountain is a high mountain summit in the Elk Mountains range of the Rocky Mountains of North America. The mountain is located in Gunnison National Forest, east-southeast (bearing 98°) of the Town of Crested Butte in Gunnison County, Colorado, United States. Geology.

Geographic entities mentioned:
surface_form: crested butte
instance_of: Mountain
countries: United States
coordinates: lat: 38.883333333333
lon: -106.94361111111
Overview. The mountain is located on one of the two long ridges which radiate south from Ben Macdhui; it reaches a height of 1037 metres (3402 feet) and along with Macdhui and Derry Cairngorm forms the central body of the Cairngorms that lie between the two major passes of the Lairig Ghru and the Lairig an Laoigh.

Geographic entities mentioned:
surface_form: Derry Cairngorm
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.062801
lon: -3.622004
surface_form: ben macdhui
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.070368
lon: -3.669099
To the south east there is a broad ridge which ends in the crags of Coire na Poite. To the north is a narrow two kilometre-long crest which is often labelled as the only noteworthy ridge in the Cairngorms; it connects the mountain to Ben Macdhui. It drops down to the col between the two mountains at a height of around 800 metres.

Geographic entities mentioned:
surface_form: ben macdhui
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.070368
lon: -3.669099
Càrn a' Mhàim. Càrn a' Mhàim is a Scottish mountain situated in the inner part of the Cairngorms range, some 15 kilometres west of Braemar in the county of Aberdeenshire. Overview.

Geographic entities mentioned:
surface_form: càrn a' mhàim
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.036871
lon: -3.658384
A bicycle can be used on this section of the route. The path is followed for a further 2.5 kilometres past the lodge until the Robbers Copse is reached at the foot of Glen Luibeg. From here the steep southern slope of Càrn a' Mhàim are ascended to the summit. The summit of Càrn a' Mhàim gives good views of the imposing hills at the heart of the Cairngorms.

Geographic entities mentioned:
surface_form: càrn a' mhàim
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.036871
lon: -3.658384
surface_form: càrn a' mhàim
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.036871
lon: -3.658384
Various sections are rural two-lane highway, urbanized four-lane undivided highway, and one-way streets. The easternmost community along the highway is Michiana Shores at the Michigan state line. US 12 passes through urban areas and wood lands, parallel to the Lake Michigan shoreline. The highway is included in the Lake Michigan Circle Tour and passes through Indiana Dunes National Park.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
After SR 249, the route has an intersection with SR 149 and a folded diamond interchange at an access road into Burns Harbor. After this interchange, the highway narrows to a two-lane highway again. The highway is near, but not on or within sight of, the shoreline of Lake Michigan. The route reenters Indiana Dunes National Park at a traffic light for the eastern entrance of Mittal Steel Company.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
This is particularly true in Israel, where many holy Jewish leaders are buried. The Cave of the Patriarchs in Hebron, Rachel's Tomb in Bethlehem, Rabbi Shimon Bar Yochai in Mount Meron, the Baba Sali in Netivot, and that of Maimonides in Tiberius are examples of burial sites that attract large pilgrimages in the Near East.

Geographic entities mentioned:
surface_form: Mount Meron
instance_of: Mountain
countries: Mandatory Palestine
Israel
Ottoman Empire
coordinates: lat: 32.9975
lon: 35.41222222222222
Penyes Altes de Moixeró. Penyes Altes de Moixeró is a mountain of Catalonia, Spain. It has an elevation of above sea level.

Geographic entities mentioned:
surface_form: penyes altes de moixeró
instance_of: Mountain
countries: Spain
coordinates: lat: 42.3063002008
lon: 1.84247482148
Geography. The Northern Region is bordered by Tanzania to the north and northeast, Lake Malawi to the east, the Central Region to the south, and Zambia to the west. The landscape is predominantly mountainous, including parts of the Nyika Plateau, Viphya Mountains, and the Misuku Hills.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Geography. The Northern Region is bordered by Tanzania to the north and northeast, Lake Malawi to the east, the Central Region to the south, and Zambia to the west. The landscape is predominantly mountainous, including parts of the Nyika Plateau, Viphya Mountains, and the Misuku Hills.

Geographic entities mentioned:
surface_form: Nyika Plateau
instance_of: Plateau
countries: Malawi
Zambia
coordinates: lat: -10.35
lon: 33.6
Found in Guyana, Venezuela, and Ecuador, it was formally described as a new species in 2016 by Dutch lichenologist André Aptroot. The type specimen was collected by the author from the Cordillera del Cóndor (Morona-Santiago Province, Ecuador) at an altitude of. The lichen has a shiny, smooth to somewhat bullate (convex and swollen) thallus that covers an area of up to in diameter.

Geographic entities mentioned:
surface_form: Cordillera del Cóndor
instance_of: Mountain
countries: Ecuador
Peru
coordinates: lat: -4
lon: -78.5
In 1892, the Waimakariri-Ashley Water Supply Board was established. The local member of parliament, David Buddo, initiated the 1894 Waimakariri-Ashley Water-Supply Board Loan Act that gave the board power to borrow up to NZ£3,000. The elected board favoured an intake above the Waimakariri Gorge. Dixon argued for the intake to be built at Browns Rock, some downstream from the gorge.

Geographic entities mentioned:
surface_form: Waimakariri Gorge
instance_of: Valley
countries: New Zealand
coordinates: lat: -43.359722222222
lon: 172.05
The result of the poll was very close; Dixon came third and with 225 votes, he was just 9 votes behind John Verrall, the successful candidate. Family and death. In 1859, Dixon returned to England to marry Eliza Agnes Wood, the daughter of Reverend Dr James Suttell Wood of Wensleydale in Yorkshire. They reached New Zealand in December 1860 on the &quot;Matoaka&quot;.

Geographic entities mentioned:
surface_form: Wensleydale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3056
lon: -2.16667
François Valentijn visited his son Frans in March 1714. The estate was sold in parts (also Bergvliet) in 1716; the auction took four days and was very well attended. Legacy. The town of Stellenbosch (founded in 1679) was named after him and Simon's Town is also named after him, as well as the Simonsberg mountain. An early ship of the South African Navy, was also named for him, in 1952.

Geographic entities mentioned:
surface_form: Simonsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 54.436666666667
lon: 8.9719444444444
Brigham Young envisioned a Mormon domain, called the &quot;State of Deseret&quot;, spanning from the Salt Lake Valley to the Pacific Ocean and so he sent church leaders to establish colonies far and wide.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
Valsorey Hut. The Valsorey Hut () is a mountain hut of the Swiss Alpine Club, located south of Bourg-Saint-Pierre in the canton of Valais. The hut lies at a height of 3,030 metres above sea level, on the southwestern slopes of the Grand Combin in the Pennine Alps, facing Mont Vélan.

Geographic entities mentioned:
surface_form: Grand Combin
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.9375
lon: 7.2991666666667
surface_form: Mont Vélan
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.892052777778
lon: 7.2518111111111
Tepe-Kermen. Tepe-Kermen (; Ukrainian and Russian:) is a butte and an early medieval settlement in the Bakhchysarai Raion of Crimea. It is located 7 km southeast of Bakhchysarai, and 2 km northeast of the settlement Kyz-Kermen. Its height is 544 meters. The easiest way to climb the mountain is from the northern slope. There are two paths leading to the top. Settlement.

Geographic entities mentioned:
surface_form: tepe-kermen
instance_of: Mountain
countries: Ukraine
Russia
coordinates: lat: 44.715338
lon: 33.930797
There are two paths leading to the top. Settlement. The name Tepe-Kermen is of Turkic origin: in Crimean Tatar it means &quot;hill-fortress&quot; or &quot;fortress on the top&quot; (- hill, peak, - fortress). The same name is given to the remains of the medieval city-fortress (according to other sources - a monastery) Tepe-Kermen, which covers the upper part of the mountain in several levels.

Geographic entities mentioned:
surface_form: tepe-kermen
instance_of: Mountain
countries: Ukraine
Russia
coordinates: lat: 44.715338
lon: 33.930797
Settlement. The name Tepe-Kermen is of Turkic origin: in Crimean Tatar it means &quot;hill-fortress&quot; or &quot;fortress on the top&quot; (- hill, peak, - fortress). The same name is given to the remains of the medieval city-fortress (according to other sources - a monastery) Tepe-Kermen, which covers the upper part of the mountain in several levels. Its area is about 1 hectare.

Geographic entities mentioned:
surface_form: tepe-kermen
instance_of: Mountain
countries: Ukraine
Russia
coordinates: lat: 44.715338
lon: 33.930797
It is believed that from the second half of the 7th century there was the residence of the Archon, who was part of the governing authorities of the Dori region (the administrative center of the Military-Administrative District), and in the 8th-9th century Tepe-Kermen, with its main temple-basilica, was a kind of ecclesiastical center of the district.

Geographic entities mentioned:
surface_form: tepe-kermen
instance_of: Mountain
countries: Ukraine
Russia
coordinates: lat: 44.715338
lon: 33.930797
The walls have not survived. Some versions attribute the demise of the city to the raid of the Golden Horde Beylerbey Nogai in 1299. A baptistery church. In the western part of Tepe-Kermen there is a baptistery church inside the cave. In his fundamental work &quot;Byzantine Kherson (second half of 6th - first half of 10th century)&quot; from 2005, S.B. Sorochan, based on the researches of N.E.

Geographic entities mentioned:
surface_form: tepe-kermen
instance_of: Mountain
countries: Ukraine
Russia
coordinates: lat: 44.715338
lon: 33.930797
Quellacocha. Quellacocha (possibly from Quechua &quot;killa&quot; moon, month, &quot;qucha&quot; lake, &quot;moon lake&quot;) is a small lake in the Cusco Region in Peru. It is situated in the Urubamba mountain range at a height of about 4,170 metres (13,680 ft). Quellacocha lies south west of the village Lares and north of the mountains Chicón and Sirihuani.

Geographic entities mentioned:
surface_form: Chicón
instance_of: Mountain
countries: Peru
coordinates: lat: -13.23666667
lon: -72.05611111
surface_form: Sirihuani
instance_of: Mountain
countries: Peru
coordinates: lat: -13.19916667
lon: -72.04416667
surface_form: chicón
instance_of: Mountain
countries: Peru
coordinates: lat: -13.23666667
lon: -72.05611111
surface_form: sirihuani
instance_of: Mountain
countries: Peru
coordinates: lat: -13.19916667
lon: -72.04416667
Quellacocha. Quellacocha (possibly from Quechua &quot;killa&quot; moon, month, &quot;qucha&quot; lake, &quot;moon lake&quot;) is a small lake in the Cusco Region in Peru. It is situated in the Urubamba mountain range at a height of about 4,170 metres (13,680 ft). Quellacocha lies south west of the village Lares and north of the mountains Chicón and Sirihuani.

Geographic entities mentioned:
surface_form: quellacocha
instance_of: Lake
countries: Peru
coordinates: lat: -13.15805556
lon: -72.06305556
Interiors were filmed at Pinewood Studios, Buckinghamshire. Heatherden Hall, the administrative offices of Pinewood Studios, was used as the governor's residence. The scenes on the North West Frontier were filmed beneath the summit of Snowdon in North Wales. The lower part of the Watkin Path was used as the Khyber Pass with garrison and border gate.

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
In Mar Chiquita lagoon, north of Mar del Plata, Argentina, &quot;Neohelice granulata&quot; herbivory increased as a likely response to the increased nutrient value of the leaves of fertilised &quot;Spartina densiflora&quot; plots, compared to non-fertilised plots.

Geographic entities mentioned:
surface_form: Mar Chiquita lagoon
instance_of: Lake
countries: Argentina
coordinates: lat: -37.6247
lon: -57.3044
Early life. He was the eldest son and heir of William Cunningham, 6th Earl of Glencairn by his spouse Janet, daughter of Sir John Gordon of Lochinvar. When Regent Morton moved against the Hamiltons in May 1579, James Cunningham, Master of Glencairn, took the Place of Paisley for the crown. Cunningham was engaged in the notorious Raid of Ruthven in 1582. Parliamentary appointments.

Geographic entities mentioned:
surface_form: Lochinvar
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.142777777778
lon: -4.1058333333333
Major tributaries of the Upper Calder include the Walsden Water, which flows through the large village of Walsden to join the Calder at Todmorden; the Hebden Water, which flows through Hebden Dale to join the Calder at Hebden Bridge; Cragg Brook, which flows through Cragg Vale to join the Calder at Mytholmroyd, and the largest, the River Ryburn, which joins the Calder at Sowerby Bridge.

Geographic entities mentioned:
surface_form: Hebden Water
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 53.733333333333
lon: -2.0166666666667
Upper Calder Valley. The Upper Calder Valley lies in West Yorkshire, in northern England, and covers the towns of Todmorden, Hebden Bridge, Mytholmroyd, Luddendenfoot, and Sowerby Bridge, as well as a number of smaller settlements such as Portsmouth, Cornholme, Walsden, and Eastwood. The valley is the upper valley of the River Calder.

Geographic entities mentioned:
surface_form: upper calder valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.72
lon: -2.004
The Upper Calder Valley falls entirely within the much larger metropolitan district of Calderdale. The towns of the Upper Calder are situated linearly along the valley, which cuts through the eastern slopes of the Pennines from Portsmouth in the west to Sowerby Bridge, a market town on the outskirts of Halifax, in the east. In popular culture.

Geographic entities mentioned:
surface_form: upper calder valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.72
lon: -2.004
In popular culture. The rugged and steep-sided Upper Calder Valley inspired such literary artists as the poets Ted Hughes (who was born in Mytholmroyd and wrote about Scout Rock), Sylvia Plath (who is buried in Heptonstall, near Hebden Bridge) and the writer Emily Brontë. The valley has also been a popular setting for film and TV, such as the series &quot;Happy Valley&quot;.

Geographic entities mentioned:
surface_form: upper calder valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.72
lon: -2.004
Wuikinuxv. The Wuikinuxv () are an Indigenous First Nations people of the Central Coast region of the Canadian province of British Columbia, located around Rivers Inlet and Owikeno Lake, to the north of Queen Charlotte Strait. Name. The name &quot;Wuikinuxv&quot; translates to &quot;Backbone people&quot;.

Geographic entities mentioned:
surface_form: Owikeno Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.683333333333
lon: -126.91666666667
Culture. The Wuikinuxv shared cultural similarities with neighboring Indigenous peoples of the Pacific Coast. At its height, Wuikinuxv territory encompassed the mouth of Rivers Inlet to the headwaters of Owikeno Lake. The Wuikinuxv constructed a Big House in 2006. This cedar building provides a space for community gatherings and ceremonies. Ethnobotany.

Geographic entities mentioned:
surface_form: Owikeno Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.683333333333
lon: -126.91666666667
Lake Couchiching. Lake Couchiching (; from the Ojibwe &quot;gojijiing&quot; meaning &quot;inlet&quot;) is a medium-sized lake in Central Ontario, Canada, separated from Lake Simcoe by a narrow channel. Lakes Simcoe and Couchiching are popular spots for fishing in summer and ice fishing in winter. Singer-songwriter Gordon Lightfoot paid homage to the lake in the song &quot;Couchiching&quot;.

Geographic entities mentioned:
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
surface_form: lake simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
surface_form: simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
surface_form: simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
surface_form: lake couchiching
instance_of: Lake
countries: Canada
coordinates: lat: 44.6667
lon: -79.3833
The lake is long and slightly less than wide. The city of Orillia is located on the narrow channel connecting this lake with Lake Simcoe. Water quality. In a 2012 study, the lake showed a microalgae density of 2.4 × 10^7/cm^2, with a high species diversity. The lake showed low total phosphorus and high organic carbon content, when compared to Lake Simcoe.

Geographic entities mentioned:
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
surface_form: lake simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
surface_form: simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
Camp Couchiching is also located near the lake. Geography. The Trent-Severn Waterway enters Lake Simcoe by the Talbot River and exits this lake by the Severn River which empties into Georgian Bay. The lake is long and slightly less than wide. The city of Orillia is located on the narrow channel connecting this lake with Lake Simcoe. Water quality.

Geographic entities mentioned:
surface_form: lake simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
surface_form: simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
The Trent-Severn Waterway enters Lake Simcoe by the Talbot River and exits this lake by the Severn River which empties into Georgian Bay. The lake is long and slightly less than wide. The city of Orillia is located on the narrow channel connecting this lake with Lake Simcoe. Water quality. In a 2012 study, the lake showed a microalgae density of 2.4 × 10^7/cm^2, with a high species diversity.

Geographic entities mentioned:
surface_form: lake simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
surface_form: simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
Lake Couchiching. Lake Couchiching (; from the Ojibwe &quot;gojijiing&quot; meaning &quot;inlet&quot;) is a medium-sized lake in Central Ontario, Canada, separated from Lake Simcoe by a narrow channel. Lakes Simcoe and Couchiching are popular spots for fishing in summer and ice fishing in winter. Singer-songwriter Gordon Lightfoot paid homage to the lake in the song &quot;Couchiching&quot;.

Geographic entities mentioned:
surface_form: lake couchiching
instance_of: Lake
countries: Canada
coordinates: lat: 44.6667
lon: -79.3833
Outline. Karasawa Cirque lies under the peaks of Mount Hotakadake, including its highest Mount Okuhatakadake (3,190m), in the Hida Mountains or &quot;Northern Japanese Alps&quot;. Other peaks circling the glacial valley include Mount Karasawa (3,110m), Mount Kitahotakadake, and (3,106m) Maehotakadake (3,090m).

Geographic entities mentioned:
surface_form: Mount Hotakadake
instance_of: Mountain
countries: Japan
coordinates: lat: 36.28916667
lon: 137.64805556
The hike is relatively flat until Yokoo, then rises somewhat to Hontani bridge, and from there the elevation rises steeply to 2300m over a distance of 2 km. It is also possible to hike down to Yokoo from Mount Yari (3,180) or Mount Chō (2,677m) and continue to Hontani Bridge and beyond.

Geographic entities mentioned:
surface_form: Mount Yari
instance_of: Mountain
countries: Japan
coordinates: lat: 36.341944444444
lon: 137.6475
surface_form: Mount Chō
instance_of: Mountain
countries: Japan
coordinates: lat: 36.29532
lon: 137.72167
Tectonic setting. The active plate tectonics of Gansu Province located on the Tibetan Plateau is dominated by the north–south continental collision of the Indian Plate and Eurasian Plate. As the Indian Plate collides along a convergent plate boundary known as the Main Himalayan Thrust, it being of continental crust does not subduct, rather, it plows into the Eurasian Plate.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Earthquake. The Lixian-Luojiapu Fault Zone located at the triple junction between the North China Craton, Tibetan Plateau, and South China Craton was identified as the source of the earthquake. The fault is characterized by left-lateral strike-slip and normal sense of slip, and strikes in an east northeast direction.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
A' Chailleach (Monadhliath Mountains). is one of the Monadhliath Mountains of Scotland. It lies northwest of Newtonmore and the Spey Valley. It is a Munro with a summit elevation of.

Geographic entities mentioned:
surface_form: a' chailleach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.6938
lon: -5.128715
surface_form: a' chailleach (monadhliath mountains)
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.109564
lon: -4.179285
This species was endemic to Alabama, but it is now extinct. Original description. Species &quot;Amphigyra alabamensis&quot; was originally described by Henry Augustus Pilsbry in 1906. Type locality is Coosa River near or in Wetumpka, Alabama.

Geographic entities mentioned:
surface_form: Coosa River
instance_of: Watercourse
countries: United States
coordinates: lat: 32.4862464
lon: -86.2777475
Early years. Gregory Alan Calvert was born in April 1937 in Longview, Washington. He was the eldest child of Clyde Walter Calvert and Nellie Louise Nevala (Gregory would later take his mother's maiden name as his middle name). The Calvert residence was a squatter's shack on the slopes of the Mount St. Helens volcano, and the family lived in harsh rural poverty.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
As such, the government would seek to utilize hydropower to facilitate development. Given previous projects in the Bolaven Plateau in southern Laos, the POE believed that the government alone could not be looked to account and provide for the negative externalities associated with the project.

Geographic entities mentioned:
surface_form: Bolaven Plateau
instance_of: Mountain
countries: Laos
coordinates: lat: 15.11
lon: 106.44
An elderly &quot;kriwe&quot; was supposed to sacrifice himself to the gods by self-immolation though that happened infrequently. A new &quot;kriwe&quot; would be selected by lower rank priests and prophets (also known as &quot;). Augustinus Rotundus (1520–1582) described the temple of Perkūnas in Šventaragis' Valley in Vilnius and that it was attended by &quot;kriwe&quot;.

Geographic entities mentioned:
surface_form: Šventaragis' Valley
instance_of: Valley
countries: Lithuania
coordinates: lat: 54.68555555555555
lon: 25.290277777777778
Rainy River, Ontario. Rainy River is a town in north-western Ontario, Canada, southeast of Lake of the Woods. Rainy River is situated on the eponymous Rainy River, which forms part of the Ontario–Minnesota segment of the Canada–US border. Across the river is the town of Baudette, Minnesota. The two towns are connected by the Baudette – Rainy River International Bridge.

Geographic entities mentioned:
surface_form: Lake of the Woods
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.09027777777778
lon: -95.2388888888889
Munt Buffalora. Munt Buffalora (2,630 m) is a mountain of the Ortler Alps, located south of the Ofen Pass in the Swiss canton of Graubünden.

Geographic entities mentioned:
surface_form: munt buffalora
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.62694444
lon: 10.25027778
The below lists are not exhaustive; there are countless subranges throughout the country. Ben Nevis (Beinn Nibheis), the highest mountain in Scotland and the United Kingdom at, is in the Highland region at the western end of the Grampian Mountains. A Scottish mountain over is referred to as a Munro, of which there are 282.

Geographic entities mentioned:
surface_form: Ben Nevis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.796891
lon: -5.003675
Scotland's main mountainous region can be broadly further split into the Northwest Highlands, the Grampian Mountains and the islands off the west coast. As the name implies, the NW Highlands begin at the suture north and west of the Great Glen and include exactly 100 of the 282 Munros. The mountains found here are generally very rough and steep, but can also often provide walking on short grass.

Geographic entities mentioned:
surface_form: Great Glen
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
As the name implies, the NW Highlands begin at the suture north and west of the Great Glen and include exactly 100 of the 282 Munros. The mountains found here are generally very rough and steep, but can also often provide walking on short grass. Long ridges are to be found on both sides of Glen Shiel in Kintail and more range-like mountains are to be found further north, such as in the Fannichs.

Geographic entities mentioned:
surface_form: Glen Shiel
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.2103
lon: -5.4239
Long ridges are to be found on both sides of Glen Shiel in Kintail and more range-like mountains are to be found further north, such as in the Fannichs. The Torridon Hills are exceptionally well-regarded by hillwalking, scrambling and climbing communities; some of them, such as Beinn Eighe, are crowned by white quartzite, which gives a highly-distinctive appearance.

Geographic entities mentioned:
surface_form: Beinn Eighe
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.37
lon: -5.24
The Torridon Hills are exceptionally well-regarded by hillwalking, scrambling and climbing communities; some of them, such as Beinn Eighe, are crowned by white quartzite, which gives a highly-distinctive appearance. The trend continues to the north, with larger caps of the white rock at Foinaven and Arkle. Some of these hills are made of Lewisian Gneiss, one of the oldest rocks on Earth.

Geographic entities mentioned:
surface_form: Foinaven
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.4121
lon: -4.8860305555556
Many of the peaks within this region are isolated, particularly within Assynt and Sutherland, and, although sometimes smaller, possess a great grandeur. These include: Stac Pollaidh, Suilven, An Teallach and Maiden Pap. The southern portion of this area south of Glenfinnan consists of lower mountains of Corbetts and Grahams, but maintain the rough character of those found further north.

Geographic entities mentioned:
surface_form: Stac Pollaidh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.044
lon: -5.2088111111111
surface_form: Suilven
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.115
lon: -5.1370694444444
surface_form: An Teallach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.806530555556
lon: -5.2516611111111
surface_form: Maiden Pap
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.233333333333
lon: -3.6166666666667
The highest eastern ranges can be split primarily into the Monadhliath, the Cairngorms and the Mounth. Well-known mountains and hills are to be found here, such as Ben A'an, The Cobbler, Buachaille Etive Mòr, Bidean nam Bian, Schiehallion, Ben Macdui and Lochnagar. The highest mountain in this area is Ben Nevis, the highest mountain in Britain.

Geographic entities mentioned:
surface_form: The Cobbler
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.211944444444
lon: -4.8108333333333
surface_form: Buachaille Etive Mòr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.647302777778
lon: -4.8977972222222
surface_form: Bidean nam Bian
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.642768
lon: -5.029335
surface_form: Schiehallion
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.666933
lon: -4.100229
surface_form: Ben Macdui
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.070368
lon: -3.669099
surface_form: Lochnagar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.959930555556
lon: -3.2447805555556
The highest eastern ranges can be split primarily into the Monadhliath, the Cairngorms and the Mounth. Well-known mountains and hills are to be found here, such as Ben A'an, The Cobbler, Buachaille Etive Mòr, Bidean nam Bian, Schiehallion, Ben Macdui and Lochnagar. The highest mountain in this area is Ben Nevis, the highest mountain in Britain.

Geographic entities mentioned:
surface_form: Ben Nevis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.796891
lon: -5.003675
In total there are 13 island Munros (12 on Skye and 1 on Mull). Skye's Black Cuillin, composed of basalt and rough gabbro, is generally regarded as the most serious mountain terrain in Britain with bare rock, jagged in outline and steep cliffs and deep cut corries. Ropes are required for some summits and the area is host to the only Munro necessitating climbing apparatus, the In Pinn.

Geographic entities mentioned:
surface_form: In Pinn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.2127
lon: -6.2348388888889
The neighbouring Red Cuillin is composed primarily of granite and has more isolated, cone-shaped mountains of a slightly lesser height. Skye is also very well known for the Quiraing and its Old Man of Storr on the Trotternish peninsula. The isle of Rùm has its own Cuillin, also composed of gabbro but shorter, grassier; necessitating good scrambling ability, and a head for heights.

Geographic entities mentioned:
surface_form: Quiraing
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.641114
lon: -6.267263
surface_form: Old Man of Storr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.507106
lon: -6.183079