Sarmila/GeoWiki-Features huggingface dataset:
Mount Cameroon Race of Hope. The Mount Cameroon Race of Hope (in French, &quot;La Course de l'Espoir&quot;) is an annual, televised footrace held at Mount Cameroon in the Southwest Region of Cameroon in January or February. The 20th edition of the Guinness Mount Cameroon race of hope was scheduled for February 14, 2015.

Geographic entities mentioned:
surface_form: Mount Cameroon
instance_of: Mountain
countries: Cameroon
coordinates: lat: 4.2166666666667
lon: 9.1725
Lake Seminole. Lake Seminole (,) is a reservoir located in the southwest corner of Georgia along its border with Florida, maintained by the U.S. Army Corps of Engineers. The Chattahoochee and Flint rivers join in the lake, before flowing from the Jim Woodruff Lock and Dam, which impounds the lake, as the Apalachicola River. The lake contains of water, and has a shoreline of.

Geographic entities mentioned:
surface_form: Chattahoochee
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Sublette Mountain. Sublette Mountain is a mountain summit in Lincoln County, Wyoming, in elevation. It is the tallest peak of the Sublette Range, which are part of the Southern Wyoming Overthrust Belt. Sublette Mountain is near the Bear Lake County, Idaho, border.

Geographic entities mentioned:
surface_form: bear lake
instance_of: Lake
countries: United States
coordinates: lat: 42
lon: -111.33333333333
surface_form: bear lake
instance_of: Lake
countries: United States
coordinates: lat: 47.5736768
lon: -121.3948639
surface_form: sublette mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.254444444444
lon: -111.00361111111
surface_form: bear lake
instance_of: Lake
countries: United States
coordinates: lat: 47.64798
lon: -121.485943
surface_form: bear lake
instance_of: Lake
countries: United States
coordinates: lat: 60.19979
lon: -149.35443
surface_form: bear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.7284
lon: -84.9439
surface_form: bear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.598611111111
lon: -75.054722222222
surface_form: bear lake
instance_of: Lake
countries: United States
coordinates: lat: 42.3468723
lon: -79.3836174
surface_form: bear lake
instance_of: Lake
countries: United States
coordinates: lat: 34.274444444444
lon: -116.81027777778
Sublette Mountain. Sublette Mountain is a mountain summit in Lincoln County, Wyoming, in elevation. It is the tallest peak of the Sublette Range, which are part of the Southern Wyoming Overthrust Belt. Sublette Mountain is near the Bear Lake County, Idaho, border.

Geographic entities mentioned:
surface_form: sublette mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.254444444444
lon: -111.00361111111
Sublette Mountain. Sublette Mountain is a mountain summit in Lincoln County, Wyoming, in elevation. It is the tallest peak of the Sublette Range, which are part of the Southern Wyoming Overthrust Belt. Sublette Mountain is near the Bear Lake County, Idaho, border.

Geographic entities mentioned:
surface_form: sublette mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.254444444444
lon: -111.00361111111
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
The collision occurred two nautical miles off Kamarajar Port in Ennore, a natural harbour about 20 km north of Chennai on the Coromandel Coast. The Ennore Creek (swampy backwater traversing over 13 km between Pulicat Lake in the north and Kosasthalaiyar River in the south and emptying into the Bay of Bengal) separates the town of Ennore from the Government held public company Kamarajar Port.

Geographic entities mentioned:
surface_form: Pulicat Lake
instance_of: Lake
countries: India
coordinates: lat: 13.565833333333
lon: 80.174722222222
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Conditions for field workers were difficult. The fact that twice as many workers as there were jobs in the San Gabriel Valley caused the walkout as well as bad conditions and low wages. Another problem was the inconsistency and insecurity of the wages, which were given based on the number of berries picked: workers probably could not count on having a guaranteed weekly or even daily wage.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
Founding. Jacob Perkins, a prominent attorney in the city of Warren in Trumbull County, Ohio, was the leader in the movement to build a railroad between Cleveland (a fast-growing industrial center and port on the shores of Lake Erie) and the coal fields of east-central Ohio. A previous road to that area, the Ohio and Erie Railroad, was proposed earlier but nothing came of this project.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Mount Evans (Alberta). Mount Evans is a summit in Jasper National Park, Alberta, Canada. Mount Evans was named by G.E. Howard in 1914 after Admiral Edward R. G. R. Evans, an Antarctic explorer. See also. Mount Evans (disambiguation)

Geographic entities mentioned:
surface_form: mount evans
instance_of: Mountain
countries: Canada
coordinates: lat: 52.444
lon: -118.129
James Anthony Gaffney. James Anthony &quot;Tony&quot; Gaffney (1928&ndash;2016) was a British civil engineer. Gaffney was born in the Rhymney Valley, South Wales in 1928 and holds BSc and DSc degrees. He was the County Engineer for the West Riding of Yorkshire at the time of the construction of Scammonden Reservoir and M62 in the late 1960s.

Geographic entities mentioned:
surface_form: Rhymney Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.697777777778
lon: -3.2294444444444
Foundation of La Paz. Three priests (Francisco Morales, Francisco Laroca and Francisco Alcócer) suggested Mendoza the location of the new city. Many members of the staff of the Viceroyalty of Peru, many commissioners and soldiers, priests and traders were familiar with a valley known as Chukiyawu, next to the Illimani mountain, and knew that there was a small Indian village.

Geographic entities mentioned:
surface_form: Illimani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.633333333333
lon: -67.790833333333
The municipal's anti-flood commanding office reported that among the 654 meteorological monitoring stations around the city, 30 recorded of rainfall in 12 hours. 311 more saw of rainfall in 12 hours. A meteorological station at Dalan, Yuyao reported a rain accumulation of over from July 22–26, an equivalent of 37 West Lakes. More than 4,700 trees were uprooted.

Geographic entities mentioned:
surface_form: West Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.2375
lon: 120.14083333333
Weston Hill. Weston Hill is a hill, high, on the A 356, 1 kilometre west of Corscombe in the county of Dorset in southern England. It is located within the Dorset Downs. It is named after the hamlet of Weston to the northeast. The summit is marked by a trig point just north of the A 356, and there is a transmission mast about 100 metres to the northwest.

Geographic entities mentioned:
surface_form: weston hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 50.8418
lon: -2.7092
Federico Visconti was a typical bishop shaped by the Counter-Reformation. He took very seriously his service, condemned the licentious uses of the population and fought the Protestantism in Valtellina, erecting a sanctuary in Lezzeno and forbidding almost any contact of the population with the Protestant soldiers who passed throughout North Italy.

Geographic entities mentioned:
surface_form: Valtellina
instance_of: Valley
countries: Italy
coordinates: lat: 46.166666666667
lon: 9.8666666666667
Through them, it spread to the South and West. It remained particularly popular in the Ozarks and Mississippi through the Civil War. This tune was also the Regimental March of The Royal Corps of Transport, a part of the British Army formed in 1965 from The Royal Army Service Corps and elements of The Royal Engineers.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Almazny, Sakha Republic. Almazny (;) is an urban locality (an urban-type settlement) in Mirninsky District of the Sakha Republic, Russia, located from Mirny, the administrative center of the district, on the border of the Lena and Vilyuy Plateaus, on the Irelyakh River, at its confluence with the Ochchuguy-Botuobuya, a tributary of the Vilyuy. As of the 2010 Census, its population was 1,527.

Geographic entities mentioned:
surface_form: Lena
instance_of: Plateau
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.75
lon: 125
History. In 1982 Peter Oldak of South Hampton, New Hampshire, a former emergency room physician, planted six grapevines in his backyard to complement his small garden and orchard. With time he concluded the microclimate of his property was very similar to that of the Finger Lakes region of New York and was well suited to growing grapes, despite common misconceptions.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
Streams on its eastern slopes form the headwaters of the Cle Elum River. Geology. Mount Daniel's volcanic rock is composed of andesite, dacite, and rhyolite inflows, breccia, and tuff. Volcanic sandstone is interbedded. Just west of Mount Daniel is the Mount Hinman plutonic stock. Peaks. From most vantages Mount Daniel appears to be a triple-crowned mass, but five summits can be identified.

Geographic entities mentioned:
surface_form: Mount Hinman
instance_of: Mountain
countries: United States
coordinates: lat: 47.5687993
lon: -121.2146464
surface_form: mount daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
surface_form: daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
Mount Daniel. Mount Daniel is the highest summit on the Cascade Range crest of Alpine Lakes Wilderness of the central Washington, United States. It is the highest point in King and Kittitas counties. Streams on its eastern slopes form the headwaters of the Cle Elum River. Geology. Mount Daniel's volcanic rock is composed of andesite, dacite, and rhyolite inflows, breccia, and tuff.

Geographic entities mentioned:
surface_form: cle elum
instance_of: Lake
countries: United States
coordinates: lat: 47.282
lon: -121.107
West Lynch Glacier is expected to disappear in the near future. History. The first known ascent of Mount Daniel was by The Mountaineers 1925 outing, but it is likely that surveyors had already ascended Daniel. The 1925 party climbed via Lynch Glacier. Climbing Route. The standard route to the summit passes Cathedral Rock, Peggy's Pond, and then is a scramble up to summit.

Geographic entities mentioned:
surface_form: cathedral rock
instance_of: Mountain
countries: United States
coordinates: lat: 34.82
lon: -111.793
surface_form: cathedral rock
instance_of: Mountain
countries: United States
coordinates: lat: 44.153961
lon: -74.915639
surface_form: cathedral rock
instance_of: Mountain
countries: United States
coordinates: lat: 47.555277777778
lon: -121.135
Mount Daniel. Mount Daniel is the highest summit on the Cascade Range crest of Alpine Lakes Wilderness of the central Washington, United States. It is the highest point in King and Kittitas counties. Streams on its eastern slopes form the headwaters of the Cle Elum River. Geology. Mount Daniel's volcanic rock is composed of andesite, dacite, and rhyolite inflows, breccia, and tuff.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: mount daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
surface_form: daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
Peaks. From most vantages Mount Daniel appears to be a triple-crowned mass, but five summits can be identified. These elevations are based on Sea Level Datum of 1929 and are taken from the Mount Daniels 7.5 minute topographic map which was published in 1965. The United States Board on Geographic Names has assigned the name Mount Daniel to the east peak even though it is not the highest. Glaciers.

Geographic entities mentioned:
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9425
lon: -119.907
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.912222222222
lon: -115.58277777778
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.5575
lon: -72.8372
surface_form: mount daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
surface_form: daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.15
lon: -146.045
The West Lynch Glacier hangs from the north slope of the Northwest Peak of Mount Daniel. West Lynch Glacier was formerly connected to Lynch Glacier. On the north side of the ridge between the Middle Summit and East Peak is another glacier with the tentative name of Daniel Glacier. It is partially connected to Lynch Glacier. Daniel Glacier is losing mass and was once much larger.

Geographic entities mentioned:
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9425
lon: -119.907
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.912222222222
lon: -115.58277777778
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.5575
lon: -72.8372
surface_form: daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.15
lon: -146.045
Mount Daniel. Mount Daniel is the highest summit on the Cascade Range crest of Alpine Lakes Wilderness of the central Washington, United States. It is the highest point in King and Kittitas counties. Streams on its eastern slopes form the headwaters of the Cle Elum River. Geology. Mount Daniel's volcanic rock is composed of andesite, dacite, and rhyolite inflows, breccia, and tuff.

Geographic entities mentioned:
surface_form: mount daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
surface_form: daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
It is the highest point in King and Kittitas counties. Streams on its eastern slopes form the headwaters of the Cle Elum River. Geology. Mount Daniel's volcanic rock is composed of andesite, dacite, and rhyolite inflows, breccia, and tuff. Volcanic sandstone is interbedded. Just west of Mount Daniel is the Mount Hinman plutonic stock. Peaks.

Geographic entities mentioned:
surface_form: mount daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
surface_form: daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
Volcanic sandstone is interbedded. Just west of Mount Daniel is the Mount Hinman plutonic stock. Peaks. From most vantages Mount Daniel appears to be a triple-crowned mass, but five summits can be identified. These elevations are based on Sea Level Datum of 1929 and are taken from the Mount Daniels 7.5 minute topographic map which was published in 1965.

Geographic entities mentioned:
surface_form: mount daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
surface_form: daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
The United States Board on Geographic Names has assigned the name Mount Daniel to the east peak even though it is not the highest. Glaciers. Mount Daniel supports several glaciers, the largest of which is Lynch Glacier on the northwest slope of the mountain. Lynch Glacier extends from to, where it melts into Pea Soup Lake, draining to the East Fork Foss River.

Geographic entities mentioned:
surface_form: mount daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
surface_form: daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
Glaciers. Mount Daniel supports several glaciers, the largest of which is Lynch Glacier on the northwest slope of the mountain. Lynch Glacier extends from to, where it melts into Pea Soup Lake, draining to the East Fork Foss River. The West Lynch Glacier hangs from the north slope of the Northwest Peak of Mount Daniel. West Lynch Glacier was formerly connected to Lynch Glacier.

Geographic entities mentioned:
surface_form: mount daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
surface_form: daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
Daniel Glacier is losing mass and was once much larger. Several small remnants, now just perennial snow accumulations rather than living glaciers, are located east of Daniel Glacier. On the southeast side of Mount Daniel, nested against a cirque headwall, is the Hyas Creek Glacier, an isolated and small ice mass that was once much larger. It drains to Hyas Creek and Peggy's Pond.

Geographic entities mentioned:
surface_form: mount daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
surface_form: daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
On the southeast side of Mount Daniel, nested against a cirque headwall, is the Hyas Creek Glacier, an isolated and small ice mass that was once much larger. It drains to Hyas Creek and Peggy's Pond. All the glaciers on Mount Daniel are thinning and becoming stagnant. West Lynch Glacier is expected to disappear in the near future. History.

Geographic entities mentioned:
surface_form: mount daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
surface_form: daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
It drains to Hyas Creek and Peggy's Pond. All the glaciers on Mount Daniel are thinning and becoming stagnant. West Lynch Glacier is expected to disappear in the near future. History. The first known ascent of Mount Daniel was by The Mountaineers 1925 outing, but it is likely that surveyors had already ascended Daniel. The 1925 party climbed via Lynch Glacier. Climbing Route.

Geographic entities mentioned:
surface_form: mount daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
surface_form: daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
surface_form: daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
On the north side of the ridge between the Middle Summit and East Peak is another glacier with the tentative name of Daniel Glacier. It is partially connected to Lynch Glacier. Daniel Glacier is losing mass and was once much larger. Several small remnants, now just perennial snow accumulations rather than living glaciers, are located east of Daniel Glacier.

Geographic entities mentioned:
surface_form: daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
It is partially connected to Lynch Glacier. Daniel Glacier is losing mass and was once much larger. Several small remnants, now just perennial snow accumulations rather than living glaciers, are located east of Daniel Glacier. On the southeast side of Mount Daniel, nested against a cirque headwall, is the Hyas Creek Glacier, an isolated and small ice mass that was once much larger.

Geographic entities mentioned:
surface_form: daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
In 1991, the race expanded to a four-day stage race format, which continued through 2010. Stages included a time trial, a circuit race on a 3-mile loop in the Fitchburg State University area, a road race in Princeton and Westminster that finished atop Mount Wachusett, and the traditional downtown Fitchburg criterium.

Geographic entities mentioned:
surface_form: Mount Wachusett
instance_of: Mountain
countries: United States
coordinates: lat: 42.488888888889
lon: -71.8875
Lake Washburn (Antarctica). Lake Washburn is a lake that formerly existed in the Taylor Valley, McMurdo Dry Valleys, Antarctica. It formed when climatic changes and an expansion of ice caused the flooding of the valley, between 23,000 and 8,340 radiocarbon years ago. Its extent and elevation are unclear but Lake Bonney and Lake Fryxell are considered to be its present-day remnant.

Geographic entities mentioned:
surface_form: Taylor Valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
surface_form: McMurdo Dry Valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: lake washburn
instance_of: Lake
coordinates: lat: -77.65
lon: 162.76
Location of the former lake. Lake Washburn was located in Taylor Valley, McMurdo Dry Valleys. It either covered the southwestern part of the valley where Lake Bonney now lies, or the northeastern part above present-day Lake Fryxell; the present-day lakes in Taylor Valley may be remnants of Lake Washburn. The former lake was named in 1960 after Albert Lincoln Washburn.

Geographic entities mentioned:
surface_form: Taylor Valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
surface_form: McMurdo Dry Valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: lake washburn
instance_of: Lake
coordinates: lat: -77.65
lon: 162.76
Geographical and climatic context. The McMurdo Dry Valleys are presently unglaciated, as the Transantarctic Mountains block glaciers and moisture from reaching the valleys. Despite mean temperatures of, meltwater from glaciers supply fresh water to the valleys, where it forms closed lakes (lakes without an outflow) that are perennially ice-covered.

Geographic entities mentioned:
surface_form: McMurdo Dry Valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
Precise dating of these paleolakes is rendered difficult, however, by the rarity of dateable deposits and the unreliability of radiocarbon dates due to reservoir effects. The existence of Lake Washburn appears to be secure; a proposal that a lake also existed in Victoria Valley was contested as being due to landslides rather than from a former lake.

Geographic entities mentioned:
surface_form: Victoria Valley
instance_of: Valley
coordinates: lat: -77.383333333333
lon: 161.93333333333
surface_form: lake washburn
instance_of: Lake
coordinates: lat: -77.65
lon: 162.76
Delta deposits that were reinterpreted as river deposits and salt accumulations below the maximum lake levels point to a small size of Lake Washburn as do the properties of soils around the hypothesized shorelines, while soil carbonates and the presence of unfrozen groundwater in the area that would have been covered by a large Lake Washburn implies a large size.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: lake washburn
instance_of: Lake
coordinates: lat: -77.65
lon: 162.76
surface_form: lake washburn
instance_of: Lake
coordinates: lat: -77.65
lon: 162.76
Location of the former lake. Lake Washburn was located in Taylor Valley, McMurdo Dry Valleys. It either covered the southwestern part of the valley where Lake Bonney now lies, or the northeastern part above present-day Lake Fryxell; the present-day lakes in Taylor Valley may be remnants of Lake Washburn. The former lake was named in 1960 after Albert Lincoln Washburn.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: lake washburn
instance_of: Lake
coordinates: lat: -77.65
lon: 162.76
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
surface_form: bonney
instance_of: Lake
coordinates: lat: -77.71667
lon: 162.41667
surface_form: lake bonney
instance_of: Lake
coordinates: lat: -77.71667
lon: 162.41667
The former lake was named in 1960 after Albert Lincoln Washburn. It was probably dammed by ice that filled the northwestern part of Taylor Valley, when the Ross Ice Shelf expanded during the Last Glacial Maximum.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
It left carbonates and lake sediments in the Taylor Valley; organic matter in these sediments constitutes an important component of and organic matter input the present-day soils in the valley while the presence of non-marine diatoms in the sediments demonstrates that they were not deposited by the sea. The Alpine I Drift from later glacial advances overlies the Lake Washburn deposits.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
During December and January, meltwater flows from the glaciers to the lakes. Occasionally, during summer strong winds blow from the Antarctic Ice Sheet through the valleys to the sea; these winds warm as they descend into the valleys and can melt the ice, causing water levels to rise.

Geographic entities mentioned:
surface_form: strong
instance_of: Mountain
coordinates: lat: -70.583333333333
lon: -62.75
Lake Washburn (Antarctica). Lake Washburn is a lake that formerly existed in the Taylor Valley, McMurdo Dry Valleys, Antarctica. It formed when climatic changes and an expansion of ice caused the flooding of the valley, between 23,000 and 8,340 radiocarbon years ago. Its extent and elevation are unclear but Lake Bonney and Lake Fryxell are considered to be its present-day remnant.

Geographic entities mentioned:
surface_form: lake washburn (antarctica)
instance_of: Lake
coordinates: lat: -77.65
lon: 162.76
The lake extended into Hjorth Valley. Water levels reached an elevation of and its shores featured deltas and shorelines with algal mats. The Canada Glacier, Commonwealth Glacier and Howard Glacier probably reached its shores, while other glaciers such as Crescent Glacier contributed runoff to Lake Washburn. The Ross Ice Sheet formed a subaqueous moraine in Lake Washburn.

Geographic entities mentioned:
surface_form: lake washburn
instance_of: Lake
coordinates: lat: -77.65
lon: 162.76
It left carbonates and lake sediments in the Taylor Valley; organic matter in these sediments constitutes an important component of and organic matter input the present-day soils in the valley while the presence of non-marine diatoms in the sediments demonstrates that they were not deposited by the sea. The Alpine I Drift from later glacial advances overlies the Lake Washburn deposits.

Geographic entities mentioned:
surface_form: lake washburn
instance_of: Lake
coordinates: lat: -77.65
lon: 162.76
The existence of Lake Washburn appears to be secure; a proposal that a lake also existed in Victoria Valley was contested as being due to landslides rather than from a former lake. Present-day Lake Vanda may resemble the former Lake Washburn although it has a distinct diatom fauna.

Geographic entities mentioned:
surface_form: lake washburn
instance_of: Lake
coordinates: lat: -77.65
lon: 162.76
Chronology and disappearance. The ice dam existed between 23,000-8,340 radiocarbon years ago and the extent of the lake fluctuated in response to climatic and glacier changes, but they are poorly documented. Evaporation appears to be responsible for the decrease in water levels at the beginning of the Holocene, after which it split into Lake Fryxell and Lake Hoare.

Geographic entities mentioned:
surface_form: hoare
instance_of: Lake
coordinates: lat: -77.6305561111111
lon: 162.86666694444443
surface_form: lake hoare
instance_of: Lake
coordinates: lat: -77.6305561111111
lon: 162.86666694444443
Lake Washburn is a lake that formerly existed in the Taylor Valley, McMurdo Dry Valleys, Antarctica. It formed when climatic changes and an expansion of ice caused the flooding of the valley, between 23,000 and 8,340 radiocarbon years ago. Its extent and elevation are unclear but Lake Bonney and Lake Fryxell are considered to be its present-day remnant. Location of the former lake.

Geographic entities mentioned:
surface_form: bonney
instance_of: Lake
coordinates: lat: -77.71667
lon: 162.41667
surface_form: lake bonney
instance_of: Lake
coordinates: lat: -77.71667
lon: 162.41667
It was probably dammed by ice that filled the northwestern part of Taylor Valley, when the Ross Ice Shelf expanded during the Last Glacial Maximum. Depending on how much the ice shelf expanded, two different sizes of the lakes are possible, the smaller of which would have been limited to the Lake Bonney basin at the western end of the valley.

Geographic entities mentioned:
surface_form: bonney
instance_of: Lake
coordinates: lat: -77.71667
lon: 162.41667
surface_form: lake bonney
instance_of: Lake
coordinates: lat: -77.71667
lon: 162.41667
One human/Gorgon hybrid named Delphyne was assigned to serve Hippolyta's daughter Artume at a young age. She became a highly respected general, fighting in the siege of Mount Olympus against the armies of Amatsu-Mikaboshi. When Artume conceives a scheme to depose her mother, locate the Omphalos, and use it to remake the world in the Amazons' image, Delphyne joins her.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
The Aquarian Weekly. &quot;The Aquarian Weekly&quot; is a regional alternative weekly newspaper based in Little Falls, New Jersey. Founded in 1969, it covers rock music and related news and events in New Jersey, New York City, and the Lehigh Valley region of eastern Pennsylvania. From 1986 to 1992, it was called &quot;East Coast Rocker&quot;.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
He contributed to the success of several Polish famous Himalayan expeditions in the 1970s and 1980s, incl. the first winter ascent of Mount Everest in 1979/1980. He also provided financial support to building up the Children's Memorial Health Institute in Warsaw and gave many grants to private persons. To honor his mother's 90th birth anniversary, he founded the Anna Godlewska Literary Award.

Geographic entities mentioned:
surface_form: first winter ascent of Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Climate. The area around Brown Field Municipal Airport has a warm-summer Mediterranean climate (Csb) with warm summers and cool winters. Incidents and accidents. On March 16, 1991, seven members of Reba McEntire's band and her road manager were among 10 people who died in the crash of a plane that departed from Brown Field. The aircraft hit Otay Mountain northeast of the airport.

Geographic entities mentioned:
surface_form: Otay Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.5946
lon: -116.845
Gråkallen. Gråkallen is a mountain in the Bymarka area of Trondheim Municipality in Trøndelag county, Norway. The tall mountain is located in the Byåsen part of the city of Trondheim. The summit is covered by an abandoned fenced military installation. Below the summit (on the col to the right of the summit above the lake) there is a ski station accessible by bus from Trondheim.

Geographic entities mentioned:
surface_form: gråkallen
instance_of: Mountain
countries: Norway
coordinates: lat: 63.420555555556
lon: 10.251388888889
Howard Somervell. Theodore Howard Somervell OBE, FRCS (16 April 1890 – 23 January 1975) was an English surgeon, mountaineer, painter and missionary who was a member of two expeditions to Mount Everest in the 1920s, and then spent nearly 40 years working as a doctor in India. In 1924 he was awarded an Olympic Gold Medal by Pierre de Coubertin for his achievements in mountaineering (Alpinism).

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
By 18 May, Somervell, Mallory and two other climbers and several Sherpa porters had established camp on the North Col, at 7020 metres the highest man had ever camped, and prepared to make the first ever attempt on the summit of Everest along the North Ridge and then the Northeast Ridge.

Geographic entities mentioned:
surface_form: North Col
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 28.015833333333
lon: 86.925
Arrow Peak (California). Arrow Peak is a summit of the Sierra Nevada in Fresno County, California, located within Kings Canyon National Park. Arrow Peak is situated at the north end of the Muro Blanco (also known as Arrow Ridge), a chain of high cliffs along the South Fork Kings River.

Geographic entities mentioned:
surface_form: arrow peak (california)
instance_of: Mountain
countries: United States
coordinates: lat: 36.92827
lon: -118.49149
surface_form: arrow peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.6928
lon: -107.61
Arrow Peak (California). Arrow Peak is a summit of the Sierra Nevada in Fresno County, California, located within Kings Canyon National Park. Arrow Peak is situated at the north end of the Muro Blanco (also known as Arrow Ridge), a chain of high cliffs along the South Fork Kings River.

Geographic entities mentioned:
surface_form: arrow peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.92827
lon: -118.49149
surface_form: arrow peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.6928
lon: -107.61
Alberto Zerain. Alberto Zerain Berasategi (20 August 1961 – 24 June 2017) was a Spanish mountaineer. He is best known as a solo alpinist and the first person to summit K2 during the 2008 K2 disaster on 1 August. Zerain summited the mountain solo from Camp III and successfully descended before the series of events that led to the deaths of 11 climbers on 2 August 2008.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
Zerain summited the mountain solo from Camp III and successfully descended before the series of events that led to the deaths of 11 climbers on 2 August 2008. In his lifetime, he climbed at least 7 eight-thousanders. Alberto Zerain died on 24 June 2017 on Nanga Parbat with his climbing partner, while on an expedition. The 2008 K2 Disaster.

Geographic entities mentioned:
surface_form: Nanga Parbat
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.239166666667
lon: 74.59
He said he immediately noticed that other climbers were suffering from Summit Fever, and he chose to make the ascent alone while the others were still discussing their problem with fixed ropes. He summited K2 on 1 August 2008. He was the first climber to reach the summit that day. He also descended successfully and was the first climber to do so, only hours before the 2008 K2 disaster.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
Fang Mountain. Fang Mountain is a summit located in the Alaska Range, in Denali National Park and Preserve, in Alaska, United States. It is situated southwest of park headquarters and northwest of Cantwell, near the headwaters of the Savage River. This peak's local descriptive name was published in 1952 by the United States Geological Survey.

Geographic entities mentioned:
surface_form: denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
surface_form: fang mountain
instance_of: Mountain
countries: United States
coordinates: lat: 63.5592
lon: -149.1864
Fang Mountain. Fang Mountain is a summit located in the Alaska Range, in Denali National Park and Preserve, in Alaska, United States. It is situated southwest of park headquarters and northwest of Cantwell, near the headwaters of the Savage River. This peak's local descriptive name was published in 1952 by the United States Geological Survey.

Geographic entities mentioned:
surface_form: fang mountain
instance_of: Mountain
countries: United States
coordinates: lat: 63.5592
lon: -149.1864
It is situated southwest of park headquarters and northwest of Cantwell, near the headwaters of the Savage River. This peak's local descriptive name was published in 1952 by the United States Geological Survey. Rarely climbed, Fang Mountain is an unattractive climbing destination because of dangerous, loose, rotten rock and a long approach. Climate.

Geographic entities mentioned:
surface_form: fang mountain
instance_of: Mountain
countries: United States
coordinates: lat: 63.5592
lon: -149.1864
Rarely climbed, Fang Mountain is an unattractive climbing destination because of dangerous, loose, rotten rock and a long approach. Climate. Based on the Köppen climate classification, Fang Mountain is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: fang mountain
instance_of: Mountain
countries: United States
coordinates: lat: 63.5592
lon: -149.1864
Bradley Nunatak. Bradley Nunatak () is a prominent nunatak standing southwest of Mount Tidd in the Pirrit Hills, Marie Byrd Land. The peak was positioned by the U.S. Ellsworth-Byrd Traverse Party on December 7, 1958, and named for Rev. Edward A. Bradley, S.J., seismologist with the party.

Geographic entities mentioned:
surface_form: Mount Tidd
instance_of: Mountain
coordinates: lat: -81.28333333
lon: -85.21666667
surface_form: Pirrit Hills
instance_of: Mountain
coordinates: lat: -81.2833
lon: -85.35
surface_form: tidd
instance_of: Mountain
coordinates: lat: -81.28333333
lon: -85.21666667
surface_form: bradley
instance_of: Mountain
coordinates: lat: -63.8833
lon: -58.6167
surface_form: bradley nunatak
instance_of: Mountain
coordinates: lat: -81.4
lon: -85.9667
Bradley Nunatak. Bradley Nunatak () is a prominent nunatak standing southwest of Mount Tidd in the Pirrit Hills, Marie Byrd Land. The peak was positioned by the U.S. Ellsworth-Byrd Traverse Party on December 7, 1958, and named for Rev. Edward A. Bradley, S.J., seismologist with the party.

Geographic entities mentioned:
surface_form: bradley
instance_of: Mountain
coordinates: lat: -63.8833
lon: -58.6167
surface_form: bradley nunatak
instance_of: Mountain
coordinates: lat: -81.4
lon: -85.9667
Bradley Nunatak. Bradley Nunatak () is a prominent nunatak standing southwest of Mount Tidd in the Pirrit Hills, Marie Byrd Land. The peak was positioned by the U.S. Ellsworth-Byrd Traverse Party on December 7, 1958, and named for Rev. Edward A. Bradley, S.J., seismologist with the party.

Geographic entities mentioned:
surface_form: bradley
instance_of: Mountain
coordinates: lat: -63.8833
lon: -58.6167
It is the seat of São Salvador do Mundo municipality. Picos is located 4 km southeast of Assomada and 23 km northwest of the capital city of Praia, near the national road from Praia to Tarrafal via Assomada (EN1-ST01). Picos is surrounded by mountains, and lies about 4 km north of the highest peak of the island of Santiago, Pico de Antónia. History.

Geographic entities mentioned:
surface_form: Pico de Antónia
instance_of: Mountain
countries: Cape Verde
coordinates: lat: 15.05
lon: -23.625
The remnants of hush gullies are visible at many places in the Pennines and at other locations such as the extensive lead mines at Cwmystwyth in Ceredigion, Wales, and at the Stiperstones in Shropshire. Another notable example is the Great Dun Fell hush gully near Cross Fell, Cumbria, probably formed in the Georgian era in the search for lead and silver.

Geographic entities mentioned:
surface_form: Stiperstones
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.581944444444
lon: -2.935
The remnants of hush gullies are visible at many places in the Pennines and at other locations such as the extensive lead mines at Cwmystwyth in Ceredigion, Wales, and at the Stiperstones in Shropshire. Another notable example is the Great Dun Fell hush gully near Cross Fell, Cumbria, probably formed in the Georgian era in the search for lead and silver.

Geographic entities mentioned:
surface_form: Great Dun Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.683111111111
lon: -2.4513194444444
surface_form: Cross Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.702777777778
lon: -2.4872222222222
The feature is named after the settlement of Vrelo in Southern Bulgaria. Location. Vrelo Peak is located at, which is 17.35 km northeast of Madrid Dome, 13.5 km southwest of Rilets Peak, and 14.12 km northwest of Mount Mayhew. British mapping in 1976.

Geographic entities mentioned:
surface_form: Rilets Peak
instance_of: Mountain
coordinates: lat: -65.4411
lon: -62.4586
surface_form: Mount Mayhew
instance_of: Mountain
coordinates: lat: -65.5833
lon: -62.4333
surface_form: vrelo peak
instance_of: Mountain
coordinates: lat: -65.5167
lon: -62.6861
surface_form: mayhew
instance_of: Mountain
coordinates: lat: -65.5833
lon: -62.4333
Vrelo Peak. Vrelo Peak (,) is the rocky peak rising to 1323 m in the west part of Parlichev Ridge, Aristotle Mountains on Oscar II Coast in Graham Land, and surmounting Melville Glacier to the north and Pequod Glacier to the south. The feature is named after the settlement of Vrelo in Southern Bulgaria. Location.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Vrelo Peak. Vrelo Peak (,) is the rocky peak rising to 1323 m in the west part of Parlichev Ridge, Aristotle Mountains on Oscar II Coast in Graham Land, and surmounting Melville Glacier to the north and Pequod Glacier to the south. The feature is named after the settlement of Vrelo in Southern Bulgaria. Location.

Geographic entities mentioned:
surface_form: vrelo peak
instance_of: Mountain
coordinates: lat: -65.5167
lon: -62.6861
Vrelo Peak. Vrelo Peak (,) is the rocky peak rising to 1323 m in the west part of Parlichev Ridge, Aristotle Mountains on Oscar II Coast in Graham Land, and surmounting Melville Glacier to the north and Pequod Glacier to the south. The feature is named after the settlement of Vrelo in Southern Bulgaria. Location.

Geographic entities mentioned:
surface_form: vrelo peak
instance_of: Mountain
coordinates: lat: -65.5167
lon: -62.6861
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
The built-up area of the community, including Red Shirt School, is located on the flats of the valley of the Cheyenne River, below the north end of Red Shirt Table, a prominent feature of the landscape of northwestern Oglala Lakota County. Red Shirt, as are many Oglala and Lakota communities, was named for chief Red Shirt, (Ógle Lúta, ca 1845–1925) whose band settled in the area in the late 1870s.

Geographic entities mentioned:
surface_form: Red Shirt Table
instance_of: Mountain
countries: United States
coordinates: lat: 43.5833
lon: -102.9
It is vital to the local economy for tourism, irrigation, and fishing purposes. It is also known as lake Zaribar. In local Sorani Kurdish it is known as the lake Zrewar or &quot;Zrêbar&quot; or &quot;Zrêwar&quot;, &quot;زرێبار&quot;. In documents dating to the Qajar era (~1800s) it is sometimes recorded as Zerehbar and Zarbar. Description.

Geographic entities mentioned:
surface_form: zrewar
instance_of: Lake
countries: Iran
coordinates: lat: 35.533333333333
lon: 46.133333333333
surface_form: زرێبار
instance_of: Lake
countries: Iran
coordinates: lat: 35.533333333333
lon: 46.133333333333
Zrebar Lake. Lake Zarivār (), is a lake in the Zagros Mountains, within Kurdistan province of western Iran. It is vital to the local economy for tourism, irrigation, and fishing purposes. It is also known as lake Zaribar. In local Sorani Kurdish it is known as the lake Zrewar or &quot;Zrêbar&quot; or &quot;Zrêwar&quot;, &quot;زرێبار&quot;.

Geographic entities mentioned:
surface_form: zrebar lake
instance_of: Lake
countries: Iran
coordinates: lat: 35.533333333333
lon: 46.133333333333
Their fourth flying machine, the &quot;Silver Dart&quot;, also constructed in 1908, made the first controlled powered flight in Canada on 23 February 1909 when it was flown off the ice of Bras d'Or Lake near Baddeck by McCurdy, who had been one of its designers.

Geographic entities mentioned:
surface_form: Bras d'Or Lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.860277777778
lon: -60.778888888889
Armenian dance. The Armenian dance (Armenian: Հայկական պար) heritage has been considered the oldest and most varied in its respective region. From the fifth to the third millennia B.C., in the higher regions of Armenia, the land of Ararat, there are rock paintings of scenes of country dancing. These dances were most likely accompanied by certain kinds of songs or musical instruments.

Geographic entities mentioned:
surface_form: Ararat
instance_of: Mountain
countries: Turkey
coordinates: lat: 39.70194444444444
lon: 44.29833333333333
As a result of advances in technology this trig sign - like others in the other federal states - lost its significance. Surrounding area. In the vicinity of the Viktorshöhe there are several tourist attractions: the Große Teufelsmühle, the Bergrat Müller Teich (&quot;Teich&quot; = pond), the Bear Monument, the ruined castle of Erichsberg, the Bremer Teich campsite and the Erichburger Teich.

Geographic entities mentioned:
surface_form: teufelsmühle
instance_of: Mountain
countries: Germany
coordinates: lat: 48.7539
lon: 8.40833
surface_form: viktorshöhe
instance_of: Mountain
countries: Germany
coordinates: lat: 51.685833333333
lon: 11.0825
Viktorshöhe. The Viktorshöhe is a hill, 581.5 metres high, in the Harz mountains of central Germany. It lies on the Ramberg massif within the boundaries of Gernrode, a part of Quedlinburg, and about 3 kilometres northeast of Friedrichsbrunn. History. The first hunting lodge on the Viktorshöhe had been built next to a small well house at the behest of Prince Victor Frederick in 1750.

Geographic entities mentioned:
surface_form: viktorshöhe
instance_of: Mountain
countries: Germany
coordinates: lat: 51.685833333333
lon: 11.0825
It lies on the Ramberg massif within the boundaries of Gernrode, a part of Quedlinburg, and about 3 kilometres northeast of Friedrichsbrunn. History. The first hunting lodge on the Viktorshöhe had been built next to a small well house at the behest of Prince Victor Frederick in 1750. And the first observation tower here also appeared as early as the 18th century.

Geographic entities mentioned:
surface_form: viktorshöhe
instance_of: Mountain
countries: Germany
coordinates: lat: 51.685833333333
lon: 11.0825