Sarmila/GeoWiki-Features huggingface dataset:
As a young woman, she was a passionate climber, accompanying her sister Ann Howard on climbs before she was officially old enough to join The Mountaineers. The sisters climbed Mount Noyes, Mount Queets, and the Middle Peak. In 1917, Howard was one of the organizers of the first Mountaineer Knapsack Trip.

Geographic entities mentioned:
surface_form: Mount Queets
instance_of: Mountain
countries: United States
coordinates: lat: 47.762335
lon: -123.595156
In 1917, Howard was one of the organizers of the first Mountaineer Knapsack Trip. This, wrote Stella Degenhardt, was &quot;a backpacking, rather than a pack-horse outing which explored the area from Snoqualmie Pass, via Goldmeyer Hot Springs, Lake Dorothy (with dugout canoe), Skykomish River, and Glacier Basin to Monte Cristo&quot;. Howard earned her B.A.

Geographic entities mentioned:
surface_form: Lake Dorothy
instance_of: Lake
countries: United States
coordinates: lat: 47.5864756
lon: -121.384297
Mount Amorong. Mount Amorong a potentially active lava dome, part of the Amorong Volcanic Group, is located at the northern end of the Luzon Central Plain, in Umingan, Pangasinan, Region I, on the island of Luzon, in the Philippines. Physical features. Mount Amorong is one of a cluster of small lava domes and diatremes.

Geographic entities mentioned:
surface_form: amorong
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.837777777778
lon: 120.80638888889
surface_form: mount amorong
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.837777777778
lon: 120.80638888889
Mount Amorong. Mount Amorong a potentially active lava dome, part of the Amorong Volcanic Group, is located at the northern end of the Luzon Central Plain, in Umingan, Pangasinan, Region I, on the island of Luzon, in the Philippines. Physical features. Mount Amorong is one of a cluster of small lava domes and diatremes.

Geographic entities mentioned:
surface_form: amorong
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.837777777778
lon: 120.80638888889
surface_form: amorong
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.837777777778
lon: 120.80638888889
surface_form: mount amorong
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.837777777778
lon: 120.80638888889
Physical features. Mount Amorong is one of a cluster of small lava domes and diatremes. It is the only one which currently exhibits any volcanic-related activities, being fumarolic and solfataric. Listings. Philippine Institute of Volcanology and Seismology (PHIVOLCS) lists Amorong as potentially active volcano. The Smithsonian Institution lists Amorong as being Fumarolic. Eruptions.

Geographic entities mentioned:
surface_form: amorong
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.837777777778
lon: 120.80638888889
surface_form: mount amorong
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.837777777778
lon: 120.80638888889
Physical features. Mount Amorong is one of a cluster of small lava domes and diatremes. It is the only one which currently exhibits any volcanic-related activities, being fumarolic and solfataric. Listings. Philippine Institute of Volcanology and Seismology (PHIVOLCS) lists Amorong as potentially active volcano. The Smithsonian Institution lists Amorong as being Fumarolic. Eruptions.

Geographic entities mentioned:
surface_form: amorong
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.837777777778
lon: 120.80638888889
It is the only one which currently exhibits any volcanic-related activities, being fumarolic and solfataric. Listings. Philippine Institute of Volcanology and Seismology (PHIVOLCS) lists Amorong as potentially active volcano. The Smithsonian Institution lists Amorong as being Fumarolic. Eruptions. The date of the last eruption is unknown, but possibly more than 1 million years before present.

Geographic entities mentioned:
surface_form: amorong
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.837777777778
lon: 120.80638888889
The Smithsonian Institution lists Amorong as being Fumarolic. Eruptions. The date of the last eruption is unknown, but possibly more than 1 million years before present. Geology. The volcano's rock type is principally trachyandesite. K-Ar dating of about 1.14 million years was obtained from the Amorong volcanic group. It lies along the Eastern Bataan volcanic lineament of the Philippines.

Geographic entities mentioned:
surface_form: amorong
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.837777777778
lon: 120.80638888889
Skiing. She was part of the Edinburgh Andean expedition in 1958, climbing various routes with Hugh Simpson and Bill Wallace. The group made seven ascents, including the first British ascent of Huascarán, which at 6,768m is the fourth-highest mountain in the Americas. In 1965 she skied across Greenland with four others on an unsupported expedition, the first woman to achieve this.

Geographic entities mentioned:
surface_form: Huascarán
instance_of: Mountain
countries: Peru
coordinates: lat: -9.1166666666667
lon: -77.6
The route eastward remains in limited use through Peterborough and on to Havelock where it serves several mines and quarries. However, most of the traffic between Toronto and Perth was redirected to a new CPR line running along the shoreline of Lake Ontario, the Campbellford, Lake Ontario and Western Railway.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Yala Peak. Yala Peak is a mountain in the Langtang area in Nepal. Location. The summit of the peak is located at above sea level and it provides a vantage point from where Shishapangma, can be seen. The Tsergo Ri giant landslide occurred close to Yala Peak. This peak is considered as a trekking peak by the Nepal Mountaineering Association, and is a relatively simple, non-technical climb.

Geographic entities mentioned:
surface_form: Langtang
instance_of: Valley
countries: Nepal
coordinates: lat: 28.25
lon: 85.5
surface_form: yala peak
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.2286
lon: 85.628
Yala Peak. Yala Peak is a mountain in the Langtang area in Nepal. Location. The summit of the peak is located at above sea level and it provides a vantage point from where Shishapangma, can be seen. The Tsergo Ri giant landslide occurred close to Yala Peak. This peak is considered as a trekking peak by the Nepal Mountaineering Association, and is a relatively simple, non-technical climb.

Geographic entities mentioned:
surface_form: Shishapangma
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 28.352222222222
lon: 85.779722222222
Location. The summit of the peak is located at above sea level and it provides a vantage point from where Shishapangma, can be seen. The Tsergo Ri giant landslide occurred close to Yala Peak. This peak is considered as a trekking peak by the Nepal Mountaineering Association, and is a relatively simple, non-technical climb. The climbing of Yala Peak passes through the Langtang National Park.

Geographic entities mentioned:
surface_form: Tsergo Ri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.212777777777777
lon: 85.6
surface_form: yala peak
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.2286
lon: 85.628
surface_form: tsergo ri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.2132408
lon: 85.6004521
The Tsergo Ri giant landslide occurred close to Yala Peak. This peak is considered as a trekking peak by the Nepal Mountaineering Association, and is a relatively simple, non-technical climb. The climbing of Yala Peak passes through the Langtang National Park. The flora and fauna of the peak and surrounding area consist of Rhododendron, Snow leopard, and Red panda.

Geographic entities mentioned:
surface_form: langtang
instance_of: Valley
countries: Nepal
coordinates: lat: 28.25
lon: 85.5
surface_form: yala peak
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.2286
lon: 85.628
The hike to the summit from the base camp is 9 kilometers in total, taking 5 to 6 hours of time. The climb along the southwest face does not need any fixed ropes, but crampons will be useful. The mountains from Yala Peak summit are Sisapangma (China’s 8000m peak), Langtang Lirung, Ganesh, Dorje Lukpa, and Gangchempo.

Geographic entities mentioned:
surface_form: langtang
instance_of: Valley
countries: Nepal
coordinates: lat: 28.25
lon: 85.5
surface_form: yala peak
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.2286
lon: 85.628
surface_form: langtang lirung
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.256111111111
lon: 85.519444444444
Yala Peak. Yala Peak is a mountain in the Langtang area in Nepal. Location. The summit of the peak is located at above sea level and it provides a vantage point from where Shishapangma, can be seen. The Tsergo Ri giant landslide occurred close to Yala Peak. This peak is considered as a trekking peak by the Nepal Mountaineering Association, and is a relatively simple, non-technical climb.

Geographic entities mentioned:
surface_form: yala peak
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.2286
lon: 85.628
Once acclimatized, the climbers move towards the base camp at Yala Kharka. Yala Peak climbs through the Southeast face from Kyanjin Gompa is considered among the easy 6000m peaks in Nepal and is recommended for travelers who are new to peak climbing. As the Nepal Government regards Yala Peak as a hiking trail, it doesn’t demand any special climbing permit.

Geographic entities mentioned:
surface_form: yala peak
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.2286
lon: 85.628
Yala Peak climbs through the Southeast face from Kyanjin Gompa is considered among the easy 6000m peaks in Nepal and is recommended for travelers who are new to peak climbing. As the Nepal Government regards Yala Peak as a hiking trail, it doesn’t demand any special climbing permit. The climb begins from the last campaign spot which is Yala Kharkha base camp at 4600m.

Geographic entities mentioned:
surface_form: yala peak
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.2286
lon: 85.628
The massif is almost completely covered by ice, the large Rhone Glacier on the west side, the smaller Damma Glacier on the east side and the Trift Glacier further on the north side. It was first climbed by Albert Hoffmann-Burkhardt with guides Johann Fischer and Andreas von Weissenfluh on 28 July 1864.

Geographic entities mentioned:
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50486111
lon: 7.64305556
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6608
lon: 8.05469
Dammastock. The Dammastock (3,630 m) is the highest mountain in the Urner Alps in Switzerland and is part of the Winterberg massif. Its summit ridge forms the border between the cantons of Uri and the Valais. It is the highest summit in the canton of Uri. The tripoint between the cantons of Bern, Valais and Uri lies near the Eggstock, north of the Dammastock.

Geographic entities mentioned:
surface_form: dammastock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.643694444444
lon: 8.4211111111111
Its summit ridge forms the border between the cantons of Uri and the Valais. It is the highest summit in the canton of Uri. The tripoint between the cantons of Bern, Valais and Uri lies near the Eggstock, north of the Dammastock. Politically, the Dammastock is split between the municipalities of Göschenen (Uri) and Obergoms (Valais).

Geographic entities mentioned:
surface_form: dammastock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.643694444444
lon: 8.4211111111111
surface_form: eggstock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.652388888889
lon: 8.4174444444444
The tripoint between the cantons of Bern, Valais and Uri lies near the Eggstock, north of the Dammastock. Politically, the Dammastock is split between the municipalities of Göschenen (Uri) and Obergoms (Valais). The massif is almost completely covered by ice, the large Rhone Glacier on the west side, the smaller Damma Glacier on the east side and the Trift Glacier further on the north side.

Geographic entities mentioned:
surface_form: dammastock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.643694444444
lon: 8.4211111111111
The hairy flower head contains white ray florets that develop a pinkish tinge as they dry. There are yellow disc florets at the center. Blooming occurs in May through October. This plant grows on basalt cliffs located in and around the Yakima River canyon on the Columbia Plateau in Washington. The whole distribution of the plant is within an area 17 kilometers long by 4.5 wide.

Geographic entities mentioned:
surface_form: Columbia Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 45.999444444444
lon: -119.00138888889
Approximately 1 million people live in the municipality, with 1.6 million in the urban area, and 2.5 million in the metropolitan area. The city stretches across fourteen islands where Lake Mälaren flows into the Baltic Sea. Outside the city to the east, and along the coast, is the island chain of the Stockholm archipelago.

Geographic entities mentioned:
surface_form: Lake Mälaren
instance_of: Lake
countries: Sweden
coordinates: lat: 59.5
lon: 17.2
King Street, Dundas, Ontario. King Street starts off as a collector road in the east-end of town in Dundas, Hamilton, Ontario, Canada beside Cootes Paradise and the Desjardins Canal at &quot;Olympic Drive&quot; and switches to an arterial road at &quot;York Street&quot; and cuts through the town of Dundas where it ends in the west-end by the CN railway tracks at the base of the Niagara Escarpment.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
The Desjardins Canal in pioneer days provided the essential means of transportation. Dundas, located at the head of navigation of Lake Ontario and the eastern terminus of the &quot;Governor's Road&quot;, was thus in a favoured position. However, in 1823 the government authorized the construction of a canal for larger vessels through Burlington sand-bar.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
The concession can be extended for another 50 years once the waterway is operational. The major dispute is the concern on the project's environmental impact, especially on Lake Nicaragua, which would be joint by the two world's largest oceans to form one of the busiest shipping route once the canal would be built.

Geographic entities mentioned:
surface_form: Lake Nicaragua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 11.5742
lon: -85.3563
House Creek (Chattahoochee River tributary). House Creek is a stream in the U.S. state of Georgia. It is a tributary to the Chattahoochee River. House Creek was named for a dwelling house along its course. A variant name was &quot;Old House Creek&quot;.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
The Pyramid, sometimes referred to as Pyramid Dome or Pyramid Mountain, is a prominent conical peak in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of and lies on the northeastern flank of Mount Edziza. The peak is southeast of the community of Telegraph Creek in Mount Edziza Provincial Park, which is one of the largest provincial parks in British Columbia.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
It rises above its surroundings on a gently sloping interfluve and is partially surrounded by a number of small streams. Among these streams are Cook Creek to the south and so-named Pyramid Creek to the north. This pyramidal peak 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
Although The Pyramid has not been greatly modified by erosion, fragments of the dome occur in gravel deposits on the north side of Pyramid Creek and in Cook Creek valley. Surrounding The Pyramid are a number of other volcanic features, including Williams Cone and Sphinx Dome. Name and etymology.

Geographic entities mentioned:
surface_form: Williams Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
The Pyramid is named after its resemblance to a pyramid; such peaks are called pyramidal peaks. Several features adjacent to The Pyramid also have names that were adopted simultaneously on 104G/15 for geology reporting purposes, including Eve Cone, Sidas Cone, Tsekone Ridge and Williams Cone.

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: Tsekone Ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.77
lon: -130.69
surface_form: Williams Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
Geography. The Pyramid 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 lava domes on the summit and flanks of Mount Edziza; others include Glacier Dome, Sphinx Dome, Nanook Dome and Triangle Dome.

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
Geography. The Pyramid 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 lava domes on the summit and flanks of Mount Edziza; others include Glacier Dome, Sphinx Dome, Nanook Dome and Triangle Dome.

Geographic entities mentioned:
surface_form: Glacier Dome
instance_of: Mountain
countries: Canada
coordinates: lat: 56.4029
lon: -130.9166
It has an elevation of and is one of several lava domes on the summit and flanks of Mount Edziza; others include Glacier Dome, Sphinx Dome, Nanook Dome and Triangle Dome. The Pyramid is a part of the Mount Edziza volcanic complex, which consists of a group of overlapping shield volcanoes, stratovolcanoes, lava domes and cinder cones that have formed over the last 7.5 million years.

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
As a part of the Mount Edziza volcanic complex, The Pyramid lies within the Stikine River watershed. The southern base of The Pyramid is bordered by Cook Creek, a tributary of Tenchen Creek which flows into the adjacent Kakiddi Creek. Flowing around its northern base is Pyramid Creek, which flows into Kakiddi Creek, a tributary of the Klastline River.

Geographic entities mentioned:
surface_form: Tenchen Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.76636
lon: -130.43724
surface_form: Kakiddi Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
The Pyramid (British Columbia). The Pyramid, sometimes referred to as Pyramid Dome or Pyramid Mountain, is a prominent conical peak in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of and lies on the northeastern flank of Mount Edziza.

Geographic entities mentioned:
surface_form: pyramid mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.9944
lon: -120.104
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Several features adjacent to The Pyramid also have names that were adopted simultaneously on 104G/15 for geology reporting purposes, including Eve Cone, Sidas Cone, Tsekone Ridge and Williams Cone. In a 2015 Journal of Archaeological Science article, Rudy Reimer of Simon Fraser University referred to The Pyramid as &quot;Pyramid Mountain&quot;.

Geographic entities mentioned:
surface_form: pyramid mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.9944
lon: -120.104
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
The Pyramid (British Columbia). The Pyramid, sometimes referred to as Pyramid Dome or Pyramid Mountain, is a prominent conical peak in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of and lies on the northeastern flank of Mount Edziza.

Geographic entities mentioned:
surface_form: the pyramid (british columbia)
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The peak is southeast of the community of Telegraph Creek in Mount Edziza Provincial Park, which is one of the largest provincial parks in British Columbia. About high and slightly more than wide at its base, The Pyramid gets its name from its resemblance to a pyramid. It rises above its surroundings on a gently sloping interfluve and is partially surrounded by a number of small streams.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
This pyramidal peak is part of the Mount Edziza volcanic complex, which consists of diverse landforms such as shield volcanoes, stratovolcanoes, lava domes and cinder cones. The Pyramid is one of three lava domes defined as part of the Pyramid Formation and consists mainly of trachyte that was erupted in a semi-molten state.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
The Pyramid is one of three lava domes defined as part of the Pyramid Formation and consists mainly of trachyte that was erupted in a semi-molten state. Although The Pyramid has not been greatly modified by erosion, fragments of the dome occur in gravel deposits on the north side of Pyramid Creek and in Cook Creek valley.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
Name and etymology. The name of the peak became official on January 2, 1980, and was adopted on National Topographic System map 104G/15 after being submitted to the BC Geographical Names office by the Geological Survey of Canada. The Pyramid is named after its resemblance to a pyramid; such peaks are called pyramidal peaks.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
In a 2015 Journal of Archaeological Science article, Rudy Reimer of Simon Fraser University referred to The Pyramid as &quot;Pyramid Mountain&quot;. The Pyramid is called &quot;Pyramid Dome&quot; in the Catalogue of Canadian volcanoes, an online database provided by Natural Resources Canada. Geography.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
Neighbouring features of this volcanic complex include Williams Cone about to the northwest and Sphinx Dome immediately to the southwest. As a part of the Mount Edziza volcanic complex, The Pyramid lies within the Stikine River watershed. The southern base of The Pyramid is bordered by Cook Creek, a tributary of Tenchen Creek which flows into the adjacent Kakiddi Creek.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
Flowing around its northern base is Pyramid Creek, which flows into Kakiddi Creek, a tributary of the Klastline River. Between Cook and Pyramid creeks is a gently sloping interfluve where The Pyramid rises prominently above its surroundings. The dome is about high, slightly more than wide at its base and conical in structure.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
Geology. The Pyramid consists of coarsely porphyritic trachyte of the Pyramid Formation, one of many stratigraphic units comprising the Mount Edziza volcanic complex. Alkali feldspar phenocrysts wide account for up to 50% of the trachyte and are embedded in a white, aphanitic matrix that is dotted with extremely small specks of opaque oxides.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
The growth of The Pyramid was accompanied by scaling which resulted in slabs spalling off the steaming surface of the growing dome to form a peripheral apron of brown, oxidized debris. A thick apron of active talus completely isolates The Pyramid from neighbouring rocks.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
A thick apron of active talus completely isolates The Pyramid from neighbouring rocks. The formation of The Pyramid took place during the Pyramid eruptive period of the Mount Edziza volcanic complex 1.1 million years ago. Its eruption probably originated from the same vent that erupted older pyroclastic surge deposits of the Pyramid Formation.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
A thick apron of active talus completely isolates The Pyramid from neighbouring rocks. The formation of The Pyramid took place during the Pyramid eruptive period of the Mount Edziza volcanic complex 1.1 million years ago. Its eruption probably originated from the same vent that erupted older pyroclastic surge deposits of the Pyramid Formation.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
Its eruption probably originated from the same vent that erupted older pyroclastic surge deposits of the Pyramid Formation. Up to 40% of the lava erupted from The Pyramid was in the form of solid feldspar crystals, such that no lava flows advanced beyond the edge of the dome due to their high viscosity.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
Up to 40% of the lava erupted from The Pyramid was in the form of solid feldspar crystals, such that no lava flows advanced beyond the edge of the dome due to their high viscosity. The Pyramid has not erupted since the Pleistocene epoch, neither have the younger Sphinx and Pharaoh domes which are also part of the Pyramid Formation.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
Clasts beneath the Edziza Formation are present in thick gravel deposits on the north side of Pyramid Creek whereas clasts between the Nido and Ice Peak formations occur in gravel lenses in Cook Creek valley. Underlying the base of Sphinx Dome at the head of Pyramid Creek are subrounded clasts also derived from The Pyramid.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
Underlying the base of Sphinx Dome at the head of Pyramid Creek are subrounded clasts also derived from The Pyramid. Edziza obsidian occurs at two outcrops on The Pyramid and are the only known occurrences of obsidian in the Pyramid Formation.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
However, no artifacts made of Pyramid High obsidian have been recovered from archaeological sites within Tahltan territory, suggesting the local Tahltan people either ignored or did not have control over who could access the Pyramid High source.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
It has an elevation of and lies on the northeastern flank of Mount Edziza. The peak is southeast of the community of Telegraph Creek in Mount Edziza Provincial Park, which is one of the largest provincial parks in British Columbia. About high and slightly more than wide at its base, The Pyramid gets its name from its resemblance to a pyramid.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The Pyramid 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: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Eastman Lake. H. V. Eastman Lake (commonly known as Eastman Lake) is an artificial lake in the Sierra Nevada foothills of Madera County, California. A small percentage of the northwest area of the reservoir is in Mariposa County. The lake was named in honor of Judge H. V. Eastman (1891–1972) who had served as Secretary Manager of the Chowchilla Water District.

Geographic entities mentioned:
surface_form: eastman lake
instance_of: Lake
countries: United States
coordinates: lat: 37.2166
lon: -119.984
Eastman Lake. H. V. Eastman Lake (commonly known as Eastman Lake) is an artificial lake in the Sierra Nevada foothills of Madera County, California. A small percentage of the northwest area of the reservoir is in Mariposa County. The lake was named in honor of Judge H. V. Eastman (1891–1972) who had served as Secretary Manager of the Chowchilla Water District.

Geographic entities mentioned:
surface_form: eastman lake
instance_of: Lake
countries: United States
coordinates: lat: 37.2166
lon: -119.984
surface_form: eastman lake
instance_of: Lake
countries: United States
coordinates: lat: 37.2166
lon: -119.984
The following census in 2011 counted 44,846 people in 13,353 households. The 2016 census measured the population of the city as 45,031 people in 13,953 households. Location. East of Sarab leads to Ardabil province. North lies Savalan Mountain. Westward from Sarab leads to the city of Bostanabad, and to the south are the Bozghush mountains. Environs.

Geographic entities mentioned:
surface_form: Savalan Mountain
instance_of: Mountain
countries: Iran
coordinates: lat: 38.266944444444
lon: 47.836944444444
Early life and education. Huber was born in Trostberg in Bavaria, the second of three children. His father Thomas, a climber who had ascended the north face of Les Droites, and his mother Maria, took the children mountaineering from a young age.

Geographic entities mentioned:
surface_form: Les Droites
instance_of: Mountain
countries: France
coordinates: lat: 45.933055555556
lon: 6.9891666666667
During this period, Huber also made important big wall ascents in the Karakoram (&quot;Tsering Mosong&quot; on Latok II, 1997), in Patagonia (&quot;Golden Eagle&quot; in 2006 and &quot;El Bastardo&quot; in 2008, on Fitz Roy), in Antarctica (&quot;Sound of Silence&quot; on Ulvetanna Peak, 2008), and on Baffin Island (&quot;Bavarian Direct&quot; on Mount Asgard, 2012).

Geographic entities mentioned:
surface_form: Fitz Roy
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -49.271388888889
lon: -73.043333333333
surface_form: Ulvetanna Peak
instance_of: Mountain
coordinates: lat: -71.855
lon: 8.3297222222222
surface_form: Mount Asgard
instance_of: Mountain
countries: Canada
coordinates: lat: 66.672222222222
lon: -65.274444444444
The dam mainly serves for irrigation purposes, municipal water supply and industrial uses. The hazard potential of the dam has been ranked high. The Vaalkop Dam lies near Pilanesberg, ESE from the outer perimeter of the ancient crater formation.

Geographic entities mentioned:
surface_form: Pilanesberg
instance_of: Mountain
countries: South Africa
coordinates: lat: -25.240277777778
lon: 27.075833333333
Bryce Harper tied up the game in the top of the seventh inning with a towering home run off Hunter Strickland into McCovey Cove, Harper's third home run of the series and second off of Strickland. Harper also became the third player in postseason history to hit the Cove after Barry Bonds and Rick Ankiel.

Geographic entities mentioned:
surface_form: McCovey Cove
instance_of: Body of water
countries: United States
coordinates: lat: 37.7772
lon: -122.388
It is a tehsil headquarter. The nearest railway station of Pachpadra is Balotra railway station. One of the famous attractions in the city is the Pachpadra Lake, which is known for salt collection around it. There is one Jawahar Navodaya Vidyalaya also, which will be only one in a district. Demographics.

Geographic entities mentioned:
surface_form: Pachpadra Lake
instance_of: Lake
countries: India
coordinates: lat: 25.929
lon: 72.2466
The strategic value of tungsten came to notice in the early 20th century. British authorities acted in 1912 to free the Carrock mine from the German owned Cumbrian Mining Company and, during World War I, restrict German access elsewhere. In World War II, tungsten played a more significant role in background political dealings.

Geographic entities mentioned:
surface_form: Carrock mine
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.693561111111
lon: -3.0231472222222
Nothobranchius robustus. &quot;Nothobranchius robustus&quot;, the red Victoria nothobranch, is a species of killifish in the family) Nothobranchiidae. It is found in the Lake Victoria basin, the Lake Albert basin, the Sio River and near Ahero in Kenya, Tanzania, and Uganda. Its natural habitats are rivers, intermittent rivers, swamps, and intermittent freshwater marshes.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
In February 1995, the group launched its first military operations near Lake Albert, which failed and resulted in their retreat to Zaire (present-day the Democratic Republic of Congo). Museveni denounced the rebels as Islamic fundamentalists, whose sole purpose was to destabilize the Great Lakes Region as &quot;agents of [Sudan's] NIF government&quot;.

Geographic entities mentioned:
surface_form: Great Lakes Region
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
Gua, Jharkhand. Gua is a census town in Pashchimi Singhbhum district in the Indian state of Jharkhand. It is a mining township situated in the Chotanagpur Plateau. The mines are operated by the Steel Authority of India Limited and are linked to IISCO at Burnpur. Despite its small geographical area, Gua holds a dominant position in Jharkhand politics.

Geographic entities mentioned:
surface_form: Chotanagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Hertz and his wife, Fannie Kesner Hertz (1881–1963). In his early business years in Chicago, John Hertz owned a farm near Cary, Illinois. In the 1930s, he acquired a property in Woodland Hills, California, in the San Fernando Valley where he raised Thoroughbred racehorses. He purchased Stoner Creek Stud for breeding and training, and two of his horses went on to win the Kentucky Derby.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
The site is a scheduled ancient monument. It is notable as the first site where the emergence of Iron Age technology in Britain was identified by archaeologists. In 1911 it was first investigated by Ben and Maud Cunnington after they were informed of finds of numerous hammerstones in a ploughed field in the Vale of Pewsey.

Geographic entities mentioned:
surface_form: Vale of Pewsey
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.352
lon: -1.851
The driving forces of the latter Ad Astra Aero company were the Swiss aviation pioneers Walter Mittelholzer and Alfred Comte. Using Junkers F.13, Comte and Mittelholzer undertook flights over the Alps, Ticino, Matterhorn, the Bernese Alps in late summer 1919, and on 11 September 1919 they succeeded in the crossing of the Mont Blanc (el.).

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
On May 5, 1634 he laid the foundation stone of the college church. Italians were not admitted to the college, except from areas of missionary work - Valtellina and the diocese of Como. From the outset, students were drawn from the Balkans, Northern Europe and the Middle East. The college prepared them for taking holy orders, after which they were to return to their homelands as missionaries.

Geographic entities mentioned:
surface_form: Valtellina
instance_of: Valley
countries: Italy
coordinates: lat: 46.166666666667
lon: 9.8666666666667
It is situated about north of Lienz within the Hohe Tauern mountain range of the Central Eastern Alps. Its municipal area comprises parts of the Granatspitze Group and the Venediger Group, with the Großvenediger peak () as its highest point. The population largely depends on tourism, seasonal agriculture and forestry. History.

Geographic entities mentioned:
surface_form: Großvenediger
instance_of: Mountain
countries: Austria
coordinates: lat: 47.108889
lon: 12.346389
Nantlle. Nantlle () is a small village in the slate quarrying Nantlle Valley in Gwynedd, Wales. It lies on the north shore of Llyn Nantlle Uchaf and is part of the community of Llanllyfni. The population was 228 in 2011 with 42% born in England.

Geographic entities mentioned:
surface_form: Nantlle Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.025
lon: -4.2833333333333
Nantlle. Nantlle () is a small village in the slate quarrying Nantlle Valley in Gwynedd, Wales. It lies on the north shore of Llyn Nantlle Uchaf and is part of the community of Llanllyfni. The population was 228 in 2011 with 42% born in England.

Geographic entities mentioned:
surface_form: Llyn Nantlle Uchaf
instance_of: Lake
countries: United Kingdom
coordinates: lat: 53.0542
lon: -4.21778
The Yadavas of Deogiri annexed Bagalkot in 1190 CE and ruled until approximately the thirteenth century. The Deccan invasion by the Muslim Khalji dynasty, led by Ala ud din Khalji in 1294 brought an end to the rule of the Yadavas. In the 14th century, much of this territory was overrun by Muhammad Taghlaq.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
A separate district of Bagalkot was carved out from the existing Bijapur district in 1997. Geography. The district of Bagalkot is situated entirely on the North Karnataka Plateau, which is part of the larger Deccan Plateau.

Geographic entities mentioned:
surface_form: Deccan Plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Wildwood Canyon. Wildwood Canyon is a canyon and California state park in the eastern foothills of the San Bernardino Mountains, within San Bernardino County, southern California. It is located near the city of Yucaipa, in the Inland Empire region. It is surrounded by the San Bernardino National Forest on the eastern and northern sides. History.

Geographic entities mentioned:
surface_form: wildwood canyon
instance_of: Valley
countries: United States
coordinates: lat: 34.014444444444
lon: -117.01944444444
It is surrounded by the San Bernardino National Forest on the eastern and northern sides. History. The indigenous Cahuilla were traditionally active in the area of Wildwood Canyon, as were the Serrano and Tongva. The area near Yucaipa was known as a crossroads for traveling indigenous people. Historic buildings remain in the park from the 1930s Hi Up House ranch and 1940s Hunt Ranch eras.

Geographic entities mentioned:
surface_form: wildwood canyon
instance_of: Valley
countries: United States
coordinates: lat: 34.014444444444
lon: -117.01944444444
Historic buildings remain in the park from the 1930s Hi Up House ranch and 1940s Hunt Ranch eras. After a flood threatened developers' housing subdivision plans, the California Department of Parks and Recreation acquired in the canyon. In May 2003 a park dedication ceremony was held at Wildwood Canyon. Wildwood Canyon State Park.

Geographic entities mentioned:
surface_form: wildwood canyon
instance_of: Valley
countries: United States
coordinates: lat: 34.014444444444
lon: -117.01944444444
After a flood threatened developers' housing subdivision plans, the California Department of Parks and Recreation acquired in the canyon. In May 2003 a park dedication ceremony was held at Wildwood Canyon. Wildwood Canyon State Park. Wildwood Canyon State Park is currently open only for day use, from sunrise to sunset. The primary activities are horseback riding, hiking, and mountain biking.

Geographic entities mentioned:
surface_form: wildwood canyon
instance_of: Valley
countries: United States
coordinates: lat: 34.014444444444
lon: -117.01944444444
In May 2003 a park dedication ceremony was held at Wildwood Canyon. Wildwood Canyon State Park. Wildwood Canyon State Park is currently open only for day use, from sunrise to sunset. The primary activities are horseback riding, hiking, and mountain biking. The canyon lies between the San Andreas Fault on the north and the San Jacinto Fault to the south. Wildwood Canyon hosts diverse wildlife.

Geographic entities mentioned:
surface_form: wildwood canyon
instance_of: Valley
countries: United States
coordinates: lat: 34.014444444444
lon: -117.01944444444
The primary activities are horseback riding, hiking, and mountain biking. The canyon lies between the San Andreas Fault on the north and the San Jacinto Fault to the south. Wildwood Canyon hosts diverse wildlife. Birds commonly seen include the California quail, western meadowlark, towhee, phainopepla, red-tailed hawk, Bewicks wren, Bullocks oriole, and white-tailed kite.

Geographic entities mentioned:
surface_form: wildwood canyon
instance_of: Valley
countries: United States
coordinates: lat: 34.014444444444
lon: -117.01944444444
It becomes complicated when the islands are included so one simplification is just to ignore them. The Ordnance Survey calculated that the centre of Mainland Scotland is at (). The point is 5 km east of the mountain of Schiehallion, which is sometimes claimed to be at the centre of Scotland. Including islands. The centre point including islands was found to be at ().

Geographic entities mentioned:
surface_form: Schiehallion
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.666933
lon: -4.100229
Cumbernauld, also in the Central Belt, is a watershed with one of its rivers (from which its name is derived) flowing to the east and the other flowing west. This watershed test could also apply to other sites like the summit of Ben Lomond being on the line of the Scottish watershed but Cumbernauld arguably has this property in its very name.

Geographic entities mentioned:
surface_form: Ben Lomond
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.190293
lon: -4.633009
Brynrefail, Gwynedd. Brynrefail (also Bryn-yr-Efail) is a small village in Gwynedd, Wales. The village is in the Arfon (UK Parliament constituency) and the Gwynedd Council Ward of Penisa'r Waun. It is close to the northern shore of Llyn Padarn lake. Along the main street there are mainly traditional terraced houses.

Geographic entities mentioned:
surface_form: Llyn Padarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 53.12888889
lon: -4.13305556
Hostyn, Texas. Hostyn is an unincorporated community in central Fayette County, Texas, United States. It was settled by Czech settlers and named after Hostýn, a hill in Moravia, Czech Republic.

Geographic entities mentioned:
surface_form: Hostýn
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.379722222222
lon: 17.701944444444
Templecombe. Templecombe is a village in Somerset, England, situated on the A357 road five miles south of Wincanton, east of Yeovil, and west of Salisbury. It is in the Blackmore Vale. Templecombe is the main settlement in the civil parish of Abbas and Templecombe, along with the hamlet of Combe Throop.

Geographic entities mentioned:
surface_form: Blackmore Vale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 50.94
lon: -2.31
These were the only airmail stamps ever issued but many definitives and commemoratives have been produced in values that paid the postage rate for airmail service. The stamps were designed by Richard J. King and recess printed by Waterlow and Sons, London, until 1961, and thereafter by De La Rue & Co, Dublin. The designs feature the &quot;Flight of the Angel Victor – Messenger of St.

Geographic entities mentioned:
surface_form: Croagh Patrick
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.7595
lon: -9.6584
Greg Mortimer. Greg Mortimer (born 10 December 1952) is an Australian climber. Mortimer is notable as one of the first two Australians (with Tim Macartney-Snape) to successfully climb Mount Everest, on 3 October 1984. Their ascent, without supplemental oxygen, was the first via the North Face and Norton Couloir. It is one of the climbing routes that has not been repeated often. Early life  .

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925