Sarmila/GeoWiki-Features huggingface dataset:
He specialised in ascents of the Aiguille Verte in the Mont Blanc massif, which he climbed 100 times by fourteen different routes, including seven first ascents, among them the direct line on the Couturier couloir, climbed on 1 July 1932 with Alfred Couttet and Georges Devouassoux. He also made the first ascent of the wildly pinnacled Aiguilles du Diable.

Geographic entities mentioned:
surface_form: Aiguilles du Diable
instance_of: Mountain
countries: France
coordinates: lat: 45.85478889
lon: 6.89045556
He also made the first ascent of the wildly pinnacled Aiguilles du Diable. In 1928 he made the first attempt on the north face of the Grandes Jorasses, one of the six great north faces of the Alps, via the Croz Spur. His party did not use pitons or any artificial devices and did not progress far up the face.

Geographic entities mentioned:
surface_form: Grandes Jorasses
instance_of: Mountain
countries: Italy
France
coordinates: lat: 45.866666666667
lon: 6.9833333333333
M. Underhill on the first traverse from the Aiguilles du Diable to Mont Blanc du Tacul, during which he overcame a Grade V pitch on L'Isolée with a jammed ice axe (today a piton is in place). He taught at ENSA, the French national school of ski and alpinism, for many years and had a great influence on several generations of high-mountain guides.

Geographic entities mentioned:
surface_form: Mont Blanc du Tacul
instance_of: Mountain
countries: France
coordinates: lat: 45.856388888889
lon: 6.8877777777778
Ulugh Muztagh. Ulugh Muztagh or Ulugh Muztag (Uighur: Ulug muz tag) () and Muztag Feng (), is an extremely remote mountain group on the northern Qinghai-Tibetan Plateau. Located on the border between the Tibetan Autonomous Region and Xinjiang Uyghur Autonomous Region, it is part of the main range of the Kunlun Mountains of East-Central Asia.

Geographic entities mentioned:
surface_form: tibetan plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
surface_form: qinghai-tibetan plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
surface_form: muztag feng
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.4125
lon: 87.384166666667
surface_form: ulugh muztagh
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.4125
lon: 87.384166666667
surface_form: qinghai
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 37
lon: 100
Ulugh Muztagh. Ulugh Muztagh or Ulugh Muztag (Uighur: Ulug muz tag) () and Muztag Feng (), is an extremely remote mountain group on the northern Qinghai-Tibetan Plateau. Located on the border between the Tibetan Autonomous Region and Xinjiang Uyghur Autonomous Region, it is part of the main range of the Kunlun Mountains of East-Central Asia.

Geographic entities mentioned:
surface_form: ulugh muztagh
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.4125
lon: 87.384166666667
Located on the border between the Tibetan Autonomous Region and Xinjiang Uyghur Autonomous Region, it is part of the main range of the Kunlun Mountains of East-Central Asia. There have been only a few attempts to climb Ulugh Muztagh and several of them have not been even able to reach the foot of the mountain.

Geographic entities mentioned:
surface_form: ulugh muztagh
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.4125
lon: 87.384166666667
Northeast of Ulugh Muztagh an endorheic basin with several important lakes (Aqqikol, Ayakkum, Jingyu, etc.) is located. The basin is bounded by the main range of the Kunlun in the south, and by the more or less parallel range, the Altyn-Tagh, in the north. Much of the basin is officially protected as the Altun Shan Nature Reserve.

Geographic entities mentioned:
surface_form: ulugh muztagh
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.4125
lon: 87.384166666667
Portland, Maine had a record-cold wind chill of. On Mount Washington's summit in New Hampshire, the wind chill hit, the coldest ever recorded in the United States, with an air temperature of combined with wind speeds of. In early March, a massive snowstorm in Arizona led to many pileups, with interstates 17, 40, and U.S. 93 closing down. Between and of snow fell in Arizona.

Geographic entities mentioned:
surface_form: Mount Washington
instance_of: Mountain
countries: United States
coordinates: lat: 44.270827777778
lon: -71.303483333333
On December 3, 1813, Simón Bolívar learned that the Royalist forces (3,500 men), under the command of Brigadier José Ceballos, had met with those of José Yáñez in the town of Araure, and as a result, he arranged for all able bodied men in El Altar and Cojedes to muster in the town of Agua Blanca.

Geographic entities mentioned:
surface_form: El Altar
instance_of: Mountain
countries: Ecuador
coordinates: lat: -1.6641666666667
lon: -78.411111111111
She later convinced him to convert to her faith, and six months after he was released without charges they were married. Kim died in Seoul on 9 April 2025, at the age of 82. Legacy. The hiking trail from Yeoraesa Temple to Samcheonggak on Bugaksan mountain, Seoul, is named the Kim Shin-Jo Trail and was part of the route used by Unit 124 in the Blue House Raid.

Geographic entities mentioned:
surface_form: Bugaksan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.60614
lon: 126.983242
Coney Island, Lough Neagh. Coney Island is an island in Lough Neagh, Northern Ireland. It is about 1 km offshore from Maghery in County Armagh, is thickly wooded and of nearly in area. It lies between the mouths of the River Blackwater and the River Bann in the south-west corner of Lough Neagh. Boat trips to the island are available at weekends from Maghery Country Park or Kinnego Marina.

Geographic entities mentioned:
surface_form: Lough Neagh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.618333333333
lon: -6.3952777777778
On the southwestern side are St Andrew the Great church and St Andrew's Street Baptist Church. Hobson's Conduit. The St Andrew's Street branch of Hobson's Conduit was added in 1631, providing a supply of water. It flowed from the conduit head along Lensfield Road in the south of Cambridge, then through St Andrew's Street and towards Drummer Street.

Geographic entities mentioned:
surface_form: Hobson's Conduit
instance_of: Watercourse
countries: United Kingdom
It is named for the town of Martinsburg, West Virginia for which it was first described. It is the dominant rock formation of the Great Appalachian Valley in New Jersey (where it is called Kittatinny Valley) and Pennsylvania (in the Lehigh Valley and Lebanon Valley). Description. The Martinsburg is defined as a gray to dark gray, and infrequently tan and purple shale and slate.

Geographic entities mentioned:
surface_form: Great Appalachian Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
surface_form: Kittatinny Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.983333333333334
lon: -74.85
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
surface_form: Lebanon Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.453
lon: -76.493
Description. The Martinsburg is defined as a gray to dark gray, and infrequently tan and purple shale and slate. Local members of impure sandstone; thin, argillaceous limestone or phyllitic shale are present in the Cumberland Valley and the Lehigh Valley. The Martinsburg has three defined members in the Lehigh Valley: The Bushkill Member which is the basal slate unit.

Geographic entities mentioned:
surface_form: Cumberland Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.93
lon: -77.72
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Local members of impure sandstone; thin, argillaceous limestone or phyllitic shale are present in the Cumberland Valley and the Lehigh Valley. The Martinsburg has three defined members in the Lehigh Valley: The Bushkill Member which is the basal slate unit. The Ramseyburg Member which is composed of alternating turbidite sandstone units with interbeds of shale and siltstone.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Hadley Mountain. Hadley Mountain is a mountain located in the southern Adirondacks in the U.S. state of New York and is the second-highest peak in Saratoga County after neighboring Tenant Mountain. The Hadley Mountain Fire Observation Station was listed on the National Register of Historic Places on September 23, 2001 for its role as a Fire lookout tower with the New York State Forest Preserve.

Geographic entities mentioned:
surface_form: Tenant Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.3684
lon: -74.10819
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: hadley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.3739
lon: -73.9508
state of New York and is the second-highest peak in Saratoga County after neighboring Tenant Mountain. The Hadley Mountain Fire Observation Station was listed on the National Register of Historic Places on September 23, 2001 for its role as a Fire lookout tower with the New York State Forest Preserve. Hadley Mountain is the highest of the three peaks that form the West Mountain ridge. Location.

Geographic entities mentioned:
surface_form: west mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: hadley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.3739
lon: -73.9508
surface_form: west mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.86
lon: -74.706111111111
At the summit, a firetower affords a commanding 360 degree panorama, taking in Great Sacandaga Lake, the surrounding southern Adirondacks and the High Peaks of the Adirondacks. The summit of Roundtop Mountain may be reached via a bushwhack from the summit of Hadley Mountain by heading NNE. In Winter this is a popular snowshoe trail due to access and length of trail to summit. History.

Geographic entities mentioned:
surface_form: roundtop
instance_of: Mountain
countries: United States
coordinates: lat: 42.293888888889
lon: -74.490555555556
surface_form: hadley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.3739
lon: -73.9508
surface_form: roundtop mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.046111111111
lon: -74.208055555556
surface_form: roundtop mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.168333333333
lon: -74.094444444444
Hadley Mountain. Hadley Mountain is a mountain located in the southern Adirondacks in the U.S. state of New York and is the second-highest peak in Saratoga County after neighboring Tenant Mountain. The Hadley Mountain Fire Observation Station was listed on the National Register of Historic Places on September 23, 2001 for its role as a Fire lookout tower with the New York State Forest Preserve.

Geographic entities mentioned:
surface_form: hadley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.3739
lon: -73.9508
state of New York and is the second-highest peak in Saratoga County after neighboring Tenant Mountain. The Hadley Mountain Fire Observation Station was listed on the National Register of Historic Places on September 23, 2001 for its role as a Fire lookout tower with the New York State Forest Preserve. Hadley Mountain is the highest of the three peaks that form the West Mountain ridge. Location.

Geographic entities mentioned:
surface_form: hadley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.3739
lon: -73.9508
The trailhead coordinates are: 43.37386, -73.95063. Route. Hadley Mountain is a popular hike which, though short in distance at, achieves a sharp elevation gain of 1525 ft. The summit offers outstanding views of the Southern Adirondack Mountains and especially the Great Sacandaga Lake. The only trail begins from the trailhead parking area next to an Historic Marker and begins an immediate climb.

Geographic entities mentioned:
surface_form: hadley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.3739
lon: -73.9508
The trailhead coordinates are: 43.37386, -73.95063. Route. Hadley Mountain is a popular hike which, though short in distance at, achieves a sharp elevation gain of 1525 ft. The summit offers outstanding views of the Southern Adirondack Mountains and especially the Great Sacandaga Lake. The only trail begins from the trailhead parking area next to an Historic Marker and begins an immediate climb.

Geographic entities mentioned:
surface_form: sacandaga lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4864091
lon: -74.4232604
Outstanding panoramas can be viewed from clearings along the final to the summit, and from the summit itself. At the summit, a firetower affords a commanding 360 degree panorama, taking in Great Sacandaga Lake, the surrounding southern Adirondacks and the High Peaks of the Adirondacks. The summit of Roundtop Mountain may be reached via a bushwhack from the summit of Hadley Mountain by heading NNE.

Geographic entities mentioned:
surface_form: sacandaga lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4864091
lon: -74.4232604
surface_form: high peaks
instance_of: Mountain
countries: United States
coordinates: lat: 45
lon: -70.4
Williams Cone. Williams Cone is a cinder cone on the northeastern flank of Mount Edziza in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of and is one of several volcanic cones in the Desolation Lava Field at the northern end of the Big Raven Plateau.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: cinder cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9717
lon: -123.007
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
Williams Cone. Williams Cone is a cinder cone on the northeastern flank of Mount Edziza in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of and is one of several volcanic cones in the Desolation Lava Field at the northern end of the Big Raven Plateau.

Geographic entities mentioned:
surface_form: Big Raven Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
Ejecta from an eruption column was blown eastward by a strong westerly wind, some of which deposited on the eastern flank of Williams Cone. Williams Cone is part of the Mount Edziza volcanic complex, which consists of diverse landforms such as shield volcanoes, stratovolcanoes, lava domes and cinder cones.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
Williams Cone is part of the Mount Edziza volcanic complex, which consists of diverse landforms such as shield volcanoes, stratovolcanoes, lava domes and cinder cones. A large, steep-sided feature on the western side of Williams Cone resembles an amphitheatre and contains a smaller, nested cinder cone. Tsecha Creek originates adjacent to Williams Cone and is part of the Stikine River watershed.

Geographic entities mentioned:
surface_form: Tsecha Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.83296
lon: -130.42064
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
Tsecha Creek originates adjacent to Williams Cone and is part of the Stikine River watershed. Surrounding Williams Cone are a number of other volcanic features, including Eve Cone, Moraine Cone, Sidas Cone, Sleet Cone, Storm Cone, Twin Cone and the Triplex Cones, which are also part of the Desolation Lava Field. Name and etymology.

Geographic entities mentioned:
surface_form: Eve Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: Sidas Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.8589
lon: -130.628
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
surface_form: twin
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.72361111
lon: -131.21166667
Geography. Williams Cone is located in Cassiar Land District of northwestern British Columbia, Canada, about southeast of Buckley Lake on the northeastern flank of Mount Edziza. It has an elevation of and is one of several volcanic cones in the Desolation Lava Field, which is one of the largest areas of Holocene lava flows in the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.905833
lon: -130.778056
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: buckley lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.41806
lon: -78.2298
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Geography. Williams Cone is located in Cassiar Land District of northwestern British Columbia, Canada, about southeast of Buckley Lake on the northeastern flank of Mount Edziza. It has an elevation of and is one of several volcanic cones in the Desolation Lava Field, which is one of the largest areas of Holocene lava flows in the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
A large, steep-sided feature on the western side of Williams Cone resembles an amphitheatre and contains a smaller cinder cone. Adjacent to Williams Cone is the head of Tsecha Creek, which is covered with loose ejecta from the cone. Tsecha Creek is a tributary of Kakiddi Creek; this north-flowing stream enters the Klastline River which flows into the Stikine River.

Geographic entities mentioned:
surface_form: Tsecha Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.83296
lon: -130.42064
surface_form: tsecha creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.83296
lon: -130.42064
surface_form: tsecha creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.83296
lon: -130.42064
Adjacent to Williams Cone is the head of Tsecha Creek, which is covered with loose ejecta from the cone. Tsecha Creek is a tributary of Kakiddi Creek; this north-flowing stream enters the Klastline River which flows into the Stikine River. Williams Cone is therefore within the Stikine River watershed along with the rest of the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: Kakiddi Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
Apart from Mount Edziza itself which is a high stratovolcano, Williams Cone is surrounded by a number of other volcanic features. Extending about to the northwest is a linear group of four volcanic cones; Eve Cone lies at the northwesternmost end of this line whereas the three Triplex Cones are between Eve Cone and Williams Cone.

Geographic entities mentioned:
surface_form: Eve Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
Sleet Cone, Storm Cone and Moraine Cone are about east, southwest and south-southwest of Williams Cone, respectively. About to the northeast is Twin Cone whereas Sidas Cone is about north of Williams Cone. About southeast of Williams Cone is The Pyramid on the northeastern flank of Mount Edziza.

Geographic entities mentioned:
surface_form: Sidas Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.8589
lon: -130.628
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
surface_form: sidas cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.8589
lon: -130.628
About to the northeast is Twin Cone whereas Sidas Cone is about north of Williams Cone. About southeast of Williams Cone is The Pyramid on the northeastern flank of Mount Edziza. All of these features are part of the Desolation Lava Field at the northern end of the Big Raven Plateau with the exception of The Pyramid, which is separated from its surroundings by a thick apron of active talus.

Geographic entities mentioned:
surface_form: Big Raven Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
It includes not only the Mount Edziza area but also the Spectrum Range to the south, which are separated by Raspberry Pass. Mount Edziza Provincial Park is in the Tahltan Highland, a southeast-trending upland area extending along the western side of the Stikine Plateau. Background.

Geographic entities mentioned:
surface_form: Stikine Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
surface_form: stikine plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Background. As a part of the Mount Edziza volcanic complex, Williams Cone lies within a broad area of volcanoes and lava flows called the Northern Cordilleran Volcanic Province, which extends from northwestern British Columbia northwards through Yukon into easternmost Alaska.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
Although Williams Cone is the youngest volcanic cone in the Desolation Lava Field, it may not be the youngest feature of the Mount Edziza volcanic complex; The Ash Pit on the southern side of the Kitsu Plateau may be younger. Basement. Williams Cone overlies the Edziza, Ice Peak, Nido and Raspberry formations, all of which are older stratigraphic units of the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: The Ash Pit
instance_of: Mountain
countries: Canada
coordinates: lat: 57.45
lon: -130.78
surface_form: Kitsu Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
surface_form: the ash pit
instance_of: Mountain
countries: Canada
coordinates: lat: 57.45
lon: -130.78
It has an elevation of and is one of several volcanic cones in the Desolation Lava Field at the northern end of the Big Raven Plateau. Situated southeast of the community of Telegraph Creek, it lies in Mount Edziza Provincial Park, one of the largest provincial parks in British Columbia.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
In his 1992 report &quot;The Late Cenozoic Mount Edziza Volcanic Complex, British Columbia&quot;, Jack Souther gave Williams Cone the numeronym &quot;DLF-10&quot;; &quot;DLF&quot; is an acronym for the Desolation Lava Field whereas &quot;10&quot; refers to Williams Cone being the tenth youngest eruptive centre in the Desolation Lava Field.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
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surface_form: mount edziza volcanic complex
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countries: Canada
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lon: -130.6
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countries: Canada
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countries: Canada
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countries: Canada
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surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
Williams Cone lies in Mount Edziza Provincial Park southeast of the community of Telegraph Creek. With an area of, Mount Edziza Provincial Park is one of the largest provincial parks in British Columbia and was established in 1972 to showcase the volcanic landscape. It includes not only the Mount Edziza area but also the Spectrum Range to the south, which are separated by Raspberry Pass.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Tsecha Creek is a tributary of Kakiddi Creek; this north-flowing stream enters the Klastline River which flows into the Stikine River. Williams Cone is therefore within the Stikine River watershed along with the rest of the Mount Edziza volcanic complex. Apart from Mount Edziza itself which is a high stratovolcano, Williams Cone is surrounded by a number of other volcanic features.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
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surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Basement. Williams Cone overlies the Edziza, Ice Peak, Nido and Raspberry formations, all of which are older stratigraphic units of the Mount Edziza volcanic complex. The Edziza Formation is the youngest of the four geological formations; it consists mainly of Pleistocene trachyte that is in the form of pyroclastic breccia, lahar or ash flow deposits.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
The Edziza Formation is the youngest of the four geological formations; it consists mainly of Pleistocene trachyte that is in the form of pyroclastic breccia, lahar or ash flow deposits. Underlying the Edziza Formation is Pleistocene alkali basalt and hawaiite of the Ice Peak Formation, which are in the form of subaerial lava flows or pyroclastic breccia.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Williams Cone is part of the Mount Edziza volcanic complex, which consists of diverse landforms such as shield volcanoes, stratovolcanoes, lava domes and cinder cones. A large, steep-sided feature on the western side of Williams Cone resembles an amphitheatre and contains a smaller, nested cinder cone. Tsecha Creek originates adjacent to Williams Cone and is part of the Stikine River watershed.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9717
lon: -123.007
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
The volcanic complex consists of a group of overlapping shield volcanoes, stratovolcanoes, lava domes and cinder cones that have formed over the last 7.5 million years. Williams Cone rises more than above the surrounding terrain and is wide at its base, making it the largest cinder cone in the Desolation Lava Field.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9717
lon: -123.007
Williams Cone rises more than above the surrounding terrain and is wide at its base, making it the largest cinder cone in the Desolation Lava Field. A large, steep-sided feature on the western side of Williams Cone resembles an amphitheatre and contains a smaller cinder cone. Adjacent to Williams Cone is the head of Tsecha Creek, which is covered with loose ejecta from the cone.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9717
lon: -123.007
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
About to the northeast is Twin Cone whereas Sidas Cone is about north of Williams Cone. About southeast of Williams Cone is The Pyramid on the northeastern flank of Mount Edziza. All of these features are part of the Desolation Lava Field at the northern end of the Big Raven Plateau with the exception of The Pyramid, which is separated from its surroundings by a thick apron of active talus.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
All of these features are part of the Desolation Lava Field at the northern end of the Big Raven Plateau with the exception of The Pyramid, which is separated from its surroundings by a thick apron of active talus. Williams Cone lies in Mount Edziza Provincial Park southeast of the community of Telegraph Creek.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Williams Cone lies in Mount Edziza Provincial Park southeast of the community of Telegraph Creek. With an area of, Mount Edziza Provincial Park is one of the largest provincial parks in British Columbia and was established in 1972 to showcase the volcanic landscape. It includes not only the Mount Edziza area but also the Spectrum Range to the south, which are separated by Raspberry Pass.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Basement. Williams Cone overlies the Edziza, Ice Peak, Nido and Raspberry formations, all of which are older stratigraphic units of the Mount Edziza volcanic complex. The Edziza Formation is the youngest of the four geological formations; it consists mainly of Pleistocene trachyte that is in the form of pyroclastic breccia, lahar or ash flow deposits.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Situated southeast of the community of Telegraph Creek, it lies in Mount Edziza Provincial Park, one of the largest provincial parks in British Columbia. A roughly lava flow travelled down the northern side of the Big Raven Plateau from Williams Cone around 630 CE and temporarily dammed the Klastline River.

Geographic entities mentioned:
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
An eruption column was blown eastward by a strong westerly wind which resulted in the deposition of cinders and ash on the eastern flank of the cone. The ejecta from this eruption column extends east across the Big Raven Plateau to the valley of Kakiddi Creek where it is in the form of particles.

Geographic entities mentioned:
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
surface_form: kakiddi creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
Streams of lava from these vents merged to form an approximately wide and long compound flow. This lava flow is one of the largest in the Desolation Lava Field and travelled northeast down the northern side of the Big Raven Plateau into the valley of the Klastline River where it formed a temporary lava dam. Williams Cone and its eruptive products are hawaiitic in composition.

Geographic entities mentioned:
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
Williams Cone. Williams Cone is a cinder cone on the northeastern flank of Mount Edziza in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of and is one of several volcanic cones in the Desolation Lava Field at the northern end of the Big Raven Plateau.

Geographic entities mentioned:
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
A roughly lava flow travelled down the northern side of the Big Raven Plateau from Williams Cone around 630 CE and temporarily dammed the Klastline River. Ejecta from an eruption column was blown eastward by a strong westerly wind, some of which deposited on the eastern flank of Williams Cone.

Geographic entities mentioned:
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
Tsecha Creek is a tributary of Kakiddi Creek; this north-flowing stream enters the Klastline River which flows into the Stikine River. Williams Cone is therefore within the Stikine River watershed along with the rest of the Mount Edziza volcanic complex. Apart from Mount Edziza itself which is a high stratovolcano, Williams Cone is surrounded by a number of other volcanic features.

Geographic entities mentioned:
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
Extending about to the northwest is a linear group of four volcanic cones; Eve Cone lies at the northwesternmost end of this line whereas the three Triplex Cones are between Eve Cone and Williams Cone. Sleet Cone, Storm Cone and Moraine Cone are about east, southwest and south-southwest of Williams Cone, respectively.

Geographic entities mentioned:
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
The ejecta from this eruption column extends east across the Big Raven Plateau to the valley of Kakiddi Creek where it is in the form of particles. It increases in both grain size and thickness toward Williams Cone where wide cinders form beds up to thick. Small streams northeast of Williams Cone have exposed former soil underlying ejecta from the volcano.

Geographic entities mentioned:
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
It increases in both grain size and thickness toward Williams Cone where wide cinders form beds up to thick. Small streams northeast of Williams Cone have exposed former soil underlying ejecta from the volcano. The formation of Williams Cone was followed by collapse of its western flank near the end of the eruption to form the steep-sided amphitheatre.

Geographic entities mentioned:
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
Small streams northeast of Williams Cone have exposed former soil underlying ejecta from the volcano. The formation of Williams Cone was followed by collapse of its western flank near the end of the eruption to form the steep-sided amphitheatre. Some of the debris from this collapse accumulated in mounds west of the amphitheatre, but most of it was rafted away by massive lava from Williams Cone.

Geographic entities mentioned:
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
Some of the debris from this collapse accumulated in mounds west of the amphitheatre, but most of it was rafted away by massive lava from Williams Cone. The lava issued from the breached central crater of Williams Cone, as well as from vents around the base of the cone. Streams of lava from these vents merged to form an approximately wide and long compound flow.

Geographic entities mentioned:
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
Williams Cone and its eruptive products are hawaiitic in composition. They are part of the Big Raven Formation and are the most recent additions to the Desolation Lava Field. Radiocarbon dating of charred alpine willow twigs preserved in ejecta from Williams Cone suggests its eruption occurred sometime between 480 and 780 CE, most likely around 630 CE.

Geographic entities mentioned:
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
These volcanic rocks are underlain by alkali basalt lava flows or flow breccias of the Tenchen Member of the Nido Formation; they were erupted from multiple volcanoes during the Pliocene. The oldest geological formation underlying Williams Cone is the Raspberry Formation, which consists of Miocene alkali basalt and minor hawaiite and mugearite.

Geographic entities mentioned:
surface_form: williams cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
Deacon (in affiliation with the University of Stellenbosch) from 1974 to 1979 as part of an archaeological and palaeo-ecological study to provide information on changes in vegetation and fauna, the cultural sequence, and the function of the cave in the area. This project was associated with excavations at the Klasies River and sites between the Cape Fold Mountains and the coast.

Geographic entities mentioned:
surface_form: Cape Fold Mountains
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
While Pherecydes and Callimachus' fifth hymn, &quot;The Baths of Pallas&quot;, provided a different story—&quot;the youthful Tiresias&quot; was blinded by Athena after he came to sate his thirst at the bubbling spring, where Athena and her favourite attendant, the nymph Chariclo (mother of Tiresias) were enjoying a &quot;cool plunge in the fair-flowing spring of Hippocrene on Mount Helicon&quot;.

Geographic entities mentioned:
surface_form: Mount Helicon
instance_of: Mountain
countries: Greece
coordinates: lat: 38.352222222222
lon: 22.825
The mountain is reported as being discovered by Colonial Europeans and named by Edward John Eyre either in 1839 or on 27 June 1840. Eyre is quoted as saying &quot;from the lofty way it towered above the surrounding hills I named it Mount Remarkable.&quot;
Snow on the Mount. Various incidents have occurred when snow has fallen on Mount Remarkable.

Geographic entities mentioned:
surface_form: eyre
instance_of: Lake
countries: Australia
coordinates: lat: -28.406
lon: 137.2963
The mountain is reported as being discovered by Colonial Europeans and named by Edward John Eyre either in 1839 or on 27 June 1840. Eyre is quoted as saying &quot;from the lofty way it towered above the surrounding hills I named it Mount Remarkable.&quot;
Snow on the Mount. Various incidents have occurred when snow has fallen on Mount Remarkable.

Geographic entities mentioned:
surface_form: eyre
instance_of: Lake
countries: Australia
coordinates: lat: -28.406
lon: 137.2963
surface_form: mount remarkable
instance_of: Mountain
countries: Australia
coordinates: lat: -32.80603
lon: 138.16479
Mount Remarkable. Mount Remarkable is a mountain in South Australia located in the Flinders Ranges about north of the centre of the capital city of Adelaide and immediately north-west of the town of Melrose, which was once named Mount Remarkable itself, and which is located at its base. The mountain has a height of.

Geographic entities mentioned:
surface_form: mount remarkable
instance_of: Mountain
countries: Australia
coordinates: lat: -32.80603
lon: 138.16479
Mount Remarkable. Mount Remarkable is a mountain in South Australia located in the Flinders Ranges about north of the centre of the capital city of Adelaide and immediately north-west of the town of Melrose, which was once named Mount Remarkable itself, and which is located at its base. The mountain has a height of.

Geographic entities mentioned:
surface_form: mount remarkable
instance_of: Mountain
countries: Australia
coordinates: lat: -32.80603
lon: 138.16479
surface_form: mount remarkable
instance_of: Mountain
countries: Australia
coordinates: lat: -32.80603
lon: 138.16479
The mountain has a height of. It and the adjoining range is described as having “high strike ridges on quartzite” with “lower rounded ridges on shale” and as having a “cover of forest, parkland and some woodland”. Since 1972, it has been located within the boundaries of the protected area known as the Mount Remarkable National Park.

Geographic entities mentioned:
surface_form: mount remarkable
instance_of: Mountain
countries: Australia
coordinates: lat: -32.80603
lon: 138.16479
The mountain's summit can be reached via a walking trail known as the Mount Remarkable Summit Hike which starts in the town of Melrose and which is graded by the national park's managing authority as being a “moderate hike’ of a distance of and that has a “round” time of five hours.

Geographic entities mentioned:
surface_form: mount remarkable
instance_of: Mountain
countries: Australia
coordinates: lat: -32.80603
lon: 138.16479
Eyre is quoted as saying &quot;from the lofty way it towered above the surrounding hills I named it Mount Remarkable.&quot;
Snow on the Mount. Various incidents have occurred when snow has fallen on Mount Remarkable. One of the most notable times recorded was in approximately 1890 when the top half of the Mount was covered in snow. Plane Crash.

Geographic entities mentioned:
surface_form: mount remarkable
instance_of: Mountain
countries: Australia
coordinates: lat: -32.80603
lon: 138.16479
Schönwies. Schönwies is a municipality in the district of Landeck in the Austrian state of Tyrol located 8 km northeast of the city of Landeck and 7 km west of the city of Imst. The main source of income is the mining of limestone ballast stone. The highest point in the municipality is the Große Schlenkerspitze (2,827 m) which is also the highest mountain in the eastern Lechtal Alps.

Geographic entities mentioned:
surface_form: Große Schlenkerspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.25
lon: 10.6167
Chörblispitz. The Chörblispitz (2,103 m) is a mountain of the Swiss Prealps, located north of Jaun in the canton of Fribourg. It lies on the range between the valley of the Breccaschlund and the valley of the Jaunbach.

Geographic entities mentioned:
surface_form: Breccaschlund
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.64944444
lon: 7.27972222
Chörblispitz. The Chörblispitz (2,103 m) is a mountain of the Swiss Prealps, located north of Jaun in the canton of Fribourg. It lies on the range between the valley of the Breccaschlund and the valley of the Jaunbach.

Geographic entities mentioned:
surface_form: chörblispitz
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.62972222
lon: 7.26916667
In 1878 Antokolski exhibited most of his works at the Paris Universal exposition, and received the Grand Prize. In 1880, the personal exhibition of the artist was held in Saint Petersburg, and he was given the rank of professor. Antokolsky left for Paris the same year, and stayed in the French capital until the end of his life, apart from periods on Lake Maggiore, in northern Italy.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223