Sarmila/GeoWiki-Features huggingface dataset:
It is a triple-peaked mountain, high, with very steep sides and a large rock cliff on its north side, situated at the western end of the Whitmore Mountains. It was named by the Advisory Committee on Antarctic Names for William H. Chapman of the U.S. Geological Survey (USGS), a cartographer with the Horlick Mountains Traverse (1958–59), who made a survey of the Whitmore Mountains on Jan. 2, 1959.

Geographic entities mentioned:
surface_form: chapman
instance_of: Body of water
Lake
coordinates: lat: -77.0167
lon: 162.383
Geological Survey (USGS), a cartographer with the Horlick Mountains Traverse (1958–59), who made a survey of the Whitmore Mountains on Jan. 2, 1959. Chapman spent several summer seasons in the Antarctic, including a survey in the Pensacola Mountains (1957–58) and the highly successful USGS Topo North-South Survey of the mountains bordering the west side of the Ross Sea and Ross Ice Shelf.

Geographic entities mentioned:
surface_form: chapman
instance_of: Body of water
Lake
coordinates: lat: -77.0167
lon: 162.383
Mount Chapman (Antarctica). Mount Chapman is a mountain in Antarctica. It is a triple-peaked mountain, high, with very steep sides and a large rock cliff on its north side, situated at the western end of the Whitmore Mountains. It was named by the Advisory Committee on Antarctic Names for William H. Chapman of the U.S.

Geographic entities mentioned:
surface_form: william
instance_of: Mountain
coordinates: lat: -64.7833
lon: -63.6833
The village is in southeastern Chittenden County, near the western border of the town of Huntington, in the valley of the Huntington River, a north-flowing tributary of the Winooski River. It is south of Huntington village and north of Hanksville. Burlington is to the northwest. Camel's Hump rises to the northeast on the crest of the Green Mountains.

Geographic entities mentioned:
surface_form: Camel's Hump
instance_of: Mountain
countries: United States
coordinates: lat: 44.319722222222225
lon: -72.8861111111111
This area Verrazzano named &quot;Selva di Lauri&quot; and &quot;Campo di Cedri&quot;, or the Forest of Laurels and Field of Cedars. The French next passed Virginia, Maryland, Delaware, New Jersey—&quot;on a sea characterised by enormous waves&quot;—where he recorded seeing Navesink Highlands, which he called &quot;little mountain by the sea&quot;.

Geographic entities mentioned:
surface_form: Navesink Highlands
instance_of: Mountain
countries: United States
coordinates: lat: 40.3996
lon: -74.0365
In the early years after the death of Jigten Sumgön the monastery grew quickly, rivaling the Sakya sect in political and religious influence. The monastery dispatched &quot;lamas&quot; across Tibet in the 13th century to found meditation colonies at pilgrimage sites including Mount Kailash, the Lapchi caves and the sacred Tsari Mountain.

Geographic entities mentioned:
surface_form: Mount Kailash
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
Itoi drew upon various works for inspiration, some of them by Steven Spielberg, as he wanted to create a game as if it were made by Spielberg. &quot;Poltergeist&quot; inspired the game's opening sequence, and the concept of contacting extraterrestrials with music and the importance of Devils Tower in &quot;Close Encounters of the Third Kind&quot; influenced the game's final act.

Geographic entities mentioned:
surface_form: Devils Tower
instance_of: Mountain
countries: United States
coordinates: lat: 44.590277777778
lon: -104.71527777778
&quot;Leamnha&quot; is thought to mean elm-water. Geographically the valley of the Vale of Leven runs from Loch Lomond in the north to Dumbarton in the south. However, the term &quot;Vale of Leven&quot; or just &quot;The Vale&quot; is commonly used locally to refer to the urban area towards the north of the valley that consists of a number of communities.

Geographic entities mentioned:
surface_form: Loch Lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
The area's name lends itself to Alexandria's local football club, Vale of Leven F.C.; the secondary school, Vale of Leven Academy; the Vale of Leven District General Hospital and other local organisations. Geography. The Vale of Leven is the valley of the River Leven between Loch Lomond in the north and the River Clyde at Dumbarton in the south. To the east are the Kilpatrick Hills.

Geographic entities mentioned:
surface_form: Loch Lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
Two major walking and/or cycling routes cross the Vale of Leven. National Cycling Network route 7 (Glasgow to Balloch) runs along the length of the River Leven and the John Muir Way crosses the northern end of the valley. There are also many local hill walking routes leading to Cardross, Helensburgh and Glen Fruin to the west and into the Kilpatrick hills to the east. Transport.

Geographic entities mentioned:
surface_form: Glen Fruin
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.053611111111
lon: -4.7436111111111
Bogë is located in the Bjeshkët e Nemuna mountain range on an altitude of about. Nearby the village is located the peak of Hajla at and the Lumbardhi i Pejës river which has its source not far from the village. The name Bogë may have its origin from the Proto-Indo-European root *&quot;bhoĝ&quot;-, meaning &quot;the running water&quot;.

Geographic entities mentioned:
surface_form: Hajla
instance_of: Mountain
countries: Montenegro
Kosovo
coordinates: lat: 42.784722222222
lon: 20.138472222222
Historical eruptions have created the crater lakes. The Tiwu Ko'o Fai Nuwa Muri has been a source of minor phreatic eruptions in historical time. The summit of the compound high Kelimutu volcano is elongated in a WNW-ESE direction; the older cones of Kelido and Kelibara are located respectively to the north and to the south. The scenic lakes are a popular tourist destination. Geochemistry.

Geographic entities mentioned:
surface_form: kelibara
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
surface_form: kelimutu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
surface_form: kelido
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
It has three volcanic crater lakes that differ in color. Tiwu Ata Mbupu, on the western side of the island is blue in color while Tiwu Nua Muri Kooh Tai and Tiwu Ata Polo are usually colors of green and red. These lakes shift color due to changes that occur within the geology and chemistry of the volcano.

Geographic entities mentioned:
surface_form: tiwu ata polo
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
surface_form: tiwu ata mbupu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
Tiwu Ata Bupu (Lake of Old People) is usually blue and is the westernmost of the three lakes. The other two lakes, Tiwu Ko'o Fai Nuwa Muri (Lake of Young Men and Maidens) and Tiwu Ata Polo (Bewitched or Enchanted Lake) are separated by a shared crater wall and are typically green or red respectively. The lake colors vary on a periodic basis.

Geographic entities mentioned:
surface_form: tiwu ata polo
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
Studies also show that temperature fluctuations play a role in the lakes colors, with the lake temperatures ranging from 21 °C to 30 °C, depending on the lake and level of volcanic activity occurring. Tiwu Ata Polo has been observed to fluctuate between red and green colors, controlled by sulfur concentrations and gas bubbling near the lakes shore.

Geographic entities mentioned:
surface_form: tiwu ata polo
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
Usually tourists sleep one night to catch sunrise at Kelimutu. Culture. Kelimutu is sacred to the local Lio people, who believe the souls of the dead migrate here. Young people's souls go to the warmth of Tiwu Koo Fai Nuwa Muri (Lake of Young Men and Maidens), old people's to the cold of Tiwu Ata Bupu (Lake of Old People), and those of the wicked to Tiwu Ata Polo (Bewitched or Enchanted Lake).

Geographic entities mentioned:
surface_form: tiwu ata polo
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
Kelimutu. Kelimutu (pronounced) is a volcano close to the small town of Moni in central Flores island in Indonesia. It is around to the east of Ende, Indonesia, the capital of Ende regency in East Nusa Tenggara province. It has three volcanic crater lakes that differ in color.

Geographic entities mentioned:
surface_form: kelimutu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
These lakes shift color due to changes that occur within the geology and chemistry of the volcano. The science of the Kelimutu lakes is relatively well-known, and the changes in color and temperature are concluded to be related to volcanic activity and the resulting fluid flux at vents at the bottom of the lakes.

Geographic entities mentioned:
surface_form: kelimutu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
History. Kelimutu has 3 historically significant volcanic events that were recorded. The first event occurred in 1865 for more than 5 years and was a Phreatic eruption, where hot water is heated until it erupts into an explosion of steam. The two later eruptions, 1938 and 1968, have been defined as hydrothermal explosions. Background activities still occur within the lakes.

Geographic entities mentioned:
surface_form: kelimutu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
The high temperatures of the lakes are also a result of the high temperatures of the volcanic system below. Geology. Kelimutu lies within the Sunda Arc, a volcanic arc that was formed by the subduction of the Indo-Australian Plate under the Eurasian Plate. This tectonic activity creates numerous volcanoes in and across Indonesia, including Kelimutu.

Geographic entities mentioned:
surface_form: kelimutu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
Geology. Kelimutu lies within the Sunda Arc, a volcanic arc that was formed by the subduction of the Indo-Australian Plate under the Eurasian Plate. This tectonic activity creates numerous volcanoes in and across Indonesia, including Kelimutu. The volcano contains three striking summit crater lakes of varying colors.

Geographic entities mentioned:
surface_form: kelimutu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
The lake colors vary on a periodic basis. Subaqueous fumaroles are the probable cause of active upwelling that occurs at the two eastern lakes. Kelimutu's most recent eruption took place between June and July 1968, which included minor phreatic explositons. Ash and gas emissions were reported, but no significant lava flows occurred. Historical eruptions have created the crater lakes.

Geographic entities mentioned:
surface_form: kelimutu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
The scenic lakes are a popular tourist destination. Geochemistry. Kelimutu is also of interest to geologists, because the three lakes have different colors, yet are at the crest of the same volcano. According to Kelimutu National Park officials, the colour changes as a result of chemical reactions resulting from the minerals contained in the lake perhaps triggered by volcano gas activity.

Geographic entities mentioned:
surface_form: kelimutu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
Kelimutus lakes extremely low pH values increase chloride and sulfate concentrations, which further influence chemical composition. Kawah Putih lake in West Java, south of Bandung, is another crater lake in Indonesia with some similarities to the lakes at Kelimutu. Gas Emissions. Active fumaroles under the lakes continuously release gases like sulfur dioxide and carbon dioxide.

Geographic entities mentioned:
surface_form: kelimutu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
Tourism. In the early days of developing the local national park in the Kelimutu area, there were some disputes with local communities over the use of the resources. More recently, forest rangers have worked to develop better relations with nearby village communities and overall management has improved.

Geographic entities mentioned:
surface_form: kelimutu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
More recently, forest rangers have worked to develop better relations with nearby village communities and overall management has improved. Kelimutu is one of the mountains listed as a &quot;ribu&quot; in Indonesia which are mountains in Indonesia which are more than high. The area is said to have begun to attract attention after being noticed by a regional Dutch military commander, B.

Geographic entities mentioned:
surface_form: kelimutu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
Bouman wrote about the site in 1929. The closest airports are Maumere, and Ende. There are regular flights to Ende from Bali. The drive from Ende to Moni, the town at the base of Kelimutu where accommodation is available, takes about 3 hours, while from Moni to Kelimutu vehicle park, a drive, needs 45 minutes. Usually tourists sleep one night to catch sunrise at Kelimutu. Culture.

Geographic entities mentioned:
surface_form: kelimutu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
surface_form: kelimutu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
There are regular flights to Ende from Bali. The drive from Ende to Moni, the town at the base of Kelimutu where accommodation is available, takes about 3 hours, while from Moni to Kelimutu vehicle park, a drive, needs 45 minutes. Usually tourists sleep one night to catch sunrise at Kelimutu. Culture. Kelimutu is sacred to the local Lio people, who believe the souls of the dead migrate here.

Geographic entities mentioned:
surface_form: kelimutu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.77
lon: 121.82
The highway was designated in 1927 and lasted until 2003. Route description. The southern terminus of M-110 was at a junction with US 31 near Parkdale on the northern boundary of the city of Manistee. From there, the trunkline traveled north along Lake Shore Road near Lake Michigan. Along the way, the highway passed through the unincorporated community of Parkdale.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Russia Dock Woodland. Russia Dock Woodland is a long narrow park in Rotherhithe, London, created by the infilling of one of the former Surrey Commercial Docks. The woodland divides the Rotherhithe peninsula, running from Bacon's College in the North to the Dalton Cross area in the South. The former Russia Dock was originally used for the importing of softwood timber from Norway, Russia and Sweden.

Geographic entities mentioned:
surface_form: Surrey Commercial Docks
instance_of: Body of water
countries: United Kingdom
coordinates: lat: 51.495
lon: -0.038333333333333
Existing players of &quot;Pokémon Trading Card Game Online&quot; can transfer their account and in-game data to &quot;Pokémon Trading Card Game Live.&quot;
On February 27, 2024, another &quot;Pokémon Trading Card Game&quot;-based video game for Android and iOS was announced in the &quot;Pokémon Presents&quot; presentation developed by Creatures (company) and DeNA titled &quot;Pokémon Trading Card Game Pocket&quot;.

Geographic entities mentioned:
surface_form: DeNA
instance_of: Mountain
countries: Iran
coordinates: lat: 30.951666666667
lon: 51.4375
spelling T'sik Hot Spring), formerly named both Saint Agnes Well and Skookumchuck Hot Springs. The community is 28 km south of the outlet of Lillooet Lake on the east side of the Lillooet River. It is approximately 75 km south of the town of Pemberton and the large reserve of the Lil'wat branch of the St'at'imc at Mount Currie, British Columbia.

Geographic entities mentioned:
surface_form: Lillooet Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.25
lon: -122.5
See Skatin First Nations for details about the complicated Band(s) structure. Skatin is geographically an extension of both the Pemberton and Harrison Valleys, but by legal fiction is officially part of the Fraser Valley for Provincial and Federal administrative purposes. Population.

Geographic entities mentioned:
surface_form: Pemberton
instance_of: Valley
countries: Canada
coordinates: lat: 50.5
lon: -123
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
Flood control. In 1947 the Pemberton Dyking District, for flood control in the adjacent Pemberton Valley, lowered Lillooet Lake, permanently altering the character of the rapids and the water level in the Lillooet River.

Geographic entities mentioned:
surface_form: Pemberton Valley
instance_of: Valley
countries: Canada
coordinates: lat: 50.5
lon: -123
surface_form: Lillooet Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.25
lon: -122.5
Balaton/sweet kernel apricot (&quot;Prunus armeniaca var. Balaton&quot;). Oral tradition holds that BC Hydro removed (or stole) the soil from all the farms along and south of Lillooet Lake, for building the service road used to install the high tension power lines to feed California. Several raised vegetable beds have been successfully started at the nearby hot springs.

Geographic entities mentioned:
surface_form: Lillooet Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.25
lon: -122.5
Roads. Work is slowly proceeding on the 7 Nations Highway re-connecting Harrison Hot Springs with Pemberton. The last 20 miles at the head of Harrison Lake leading to Port Douglas are in very poor repair ever since the sawmill closed at Port Douglas, around 1995. Work on the Harrison Lake section was disrupted by the Wood Lake Wildfire in summer 2015.

Geographic entities mentioned:
surface_form: Harrison Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.55
lon: -121.83333333333
Work on the Harrison Lake section was disrupted by the Wood Lake Wildfire in summer 2015. The westernmost section of road was improved in the spring of 2015; In-SHUCK-ch Forest Service Road/FSR was widened from 1 to 1½ lanes to 2 lanes and two ½-lane shoulders (3 lanes &quot;in toto&quot;) for the length of Lillooet Lake.

Geographic entities mentioned:
surface_form: Lillooet Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.25
lon: -122.5
In the winter, add an axe, shovel, studs and/or chains/other traction devices to the list. Check latest updates before heading out. Air. There are charter helicopter flights, weather/visibility permitting. The closest airport is Pemberton Regional Airport. Seaplanes can be chartered out of Green Lake Water Aerodrome and &quot;land&quot; nearby at the south end of Lillooet Lake. Education.

Geographic entities mentioned:
surface_form: Lillooet Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.25
lon: -122.5
Regional geology. The Big Smoky Valley is similar to many of the desert valleys in Nevada, characterized by flanking mountain ranges running north to south. Big Smoky Valley is bounded to the south by Lone Mountain, and the east and west by the Toquima and the Toiyabe ranges, respectively. The valley floor consists primarily of alluvial fans composed of small poorly sorted gravels.

Geographic entities mentioned:
surface_form: Big Smoky Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.6644
lon: -117.171
Setter and Blaine set out to steal Ben's new land while he's off, and trouble follows. Background. The story is set in a remote wilderness valley located in northern California. The author accurately describes the geography of the region throughout the novel, identifying Mount Shasta, Tule Lake, and the landscape in and around Lava Beds National Monument.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: Tule Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
This makes its climate very different in the north and south. 21% of the prefecture's land area was designated as Natural Parks, namely Sanin Kaigan National Park; Biwako, Kyoto Tamba Kogen, Tango-Amanohashidate-Ōeyama and Wakasa Wan Quasi-National Parks; and Hozukyō, Kasagiyama, and Rurikei Prefectural Natural Parks. Municipalities. Kansai Science City is located in the southwest. Religion.

Geographic entities mentioned:
surface_form: Rurikei
instance_of: Valley
countries: Japan
coordinates: lat: 35.035817
lon: 135.404608
In 1959, the Fauna Preservation Society appointed E.P. Gee to undertake a survey of the Chitwan Valley. Gee, who had spent most of his life in India and was an authority on its wildlife, recommended creation of a national park north of the Rapti River. He also proposed creation of a wildlife sanctuary south of the river for a trial period of ten years.

Geographic entities mentioned:
surface_form: Chitwan Valley
instance_of: Valley
countries: Nepal
Kőröshegy. Kőröshegy is a village directly south of Balatonföldvár in Siófok District, Somogy County, Hungary. The settlement is known in Hungary for being a holiday destination near to Lake Balaton attracting thousands of visitors yearly. Kőröshegy is also famous for its grapes, wine and the &quot;Viaduct of Kőröshegy&quot; on the M7 Motorway which is a symbol of the village.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
&quot;István Tikos&quot; referred to Kőröshegy as &quot;Keren&quot; and &quot;Kereszthegy&quot; in 1819. Geography. Kőröshegy lies 3 km far from the southern shore of Lake Balaton in the &quot;Kőröshegy Valley&quot; south of Balatonföldvár and Szántód. The landscape is dominated by the hills (part of the &quot;Transdanubian Hill Range&quot;).

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
Following the German invasion in June 1941 &quot;Kommuna&quot; was based at Leningrad, and although damaged by bombing continued to serve throughout the siege. In March 1942 she recovered four KV tanks, two tractors and 31 vehicles from Lake Ladoga, which had fallen through the ice road, called the &quot;Road of Life&quot;, which was Leningrad's only supply route.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
JKNC and INC contested 2009 general election in alliance. INC won all the two seats of Jammu region but lost Ladakh seat to NC rebel who contested as an independent candidate. NC won all the three seats of the Kashmir Valley in 2009. During this period, the JKNC has experienced increasing controversies over the Accession of Kashmir to India.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Until 1834, Sagres was an independent municipality. Geography. Sagres is located in the extreme southwest of continental Europe, and marked by two geomorphological structures: the Cape St. Vincent and Sagres Point, which establish a transition between the eastern coastal and meridional zones.

Geographic entities mentioned:
surface_form: Sagres Point
instance_of: Landform
countries: Portugal
coordinates: lat: 36.996364
lon: -8.948965
Küsnacht Goldbach railway station. Küsnacht Goldbach is a railway station in Switzerland, situated near the eastern bank of Lake Zurich (Goldcoast) in the village of Goldbach, which is itself in the municipality of Küsnacht. The station is on the Lake Zurich right bank railway line. It is located within fare zone 140 of the Zürcher Verkehrsverbund (ZVV).

Geographic entities mentioned:
surface_form: Lake Zurich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
Many beaver, whose pelts were highly valued in Europe and China, lived up and down the rivers; they could be trapped and skinned, and their pelts sold. The Potawatomi nation, a network of tribal clans that lived around the shores of southern Lake Michigan, had a culture that centered around hunting. Many of their clan members enthusiastically cooperated with the trade.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Ahornsee. Ahornsee is a mountain lake in the Dachstein Mountains of Upper Austria.

Geographic entities mentioned:
surface_form: ahornsee
instance_of: Lake
countries: Austria
coordinates: lat: 47.4666
lon: 13.7821
Ingrid Baeyens. Ingrid M. Baeyens (8 January 1956 in Ramsel, Belgium) is a Belgian mountaineer and physical therapist. She became the first woman to summit the South Face of Annapurna in 1991, and the first Belgian woman to summit Mount Everest in 1992. Biography. Ingrid Baeyens was born in Ramsel, Antwerp, Belgium on 8 January 1956. She began mountaineering in the Alps in the early 1980s.

Geographic entities mentioned:
surface_form: Annapurna
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.5958
lon: 83.82
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
She then turned to climbing in the Himalayas, notably participating in expeditions with Krzysztof Wielicki and Rob Hall. In December 1990, she attempted a winter ascent of Makalu, which had been unclimbed in winter until that point. Alongside an expedition team of Krzysztof Wielicki, Anna Czerwinska, and Richard Pawlowski, they made it to 7,400m before descending.

Geographic entities mentioned:
surface_form: Makalu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.889166666667
lon: 87.088611111111
At the time, she was the female mountaineer with the most eight-thousanders after Wanda Rutkiewicz. In 1994, Baeyens and Paul Laeremans became hypothermic while descending the West Buttress route of Denali. After their team created a snow cave for them to rest, they were successfully helicoptered to safety.

Geographic entities mentioned:
surface_form: Denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
Highpointer Peak. Highpointer Peak is a peak of the British Empire Range on Ellesmere Island. Highpointer is located about west of Barbeau Peak (), the highest peak of the range.

Geographic entities mentioned:
surface_form: Barbeau Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 81.914722222222
lon: -75.009166666667
Highpointer Peak. Highpointer Peak is a peak of the British Empire Range on Ellesmere Island. Highpointer is located about west of Barbeau Peak (), the highest peak of the range.

Geographic entities mentioned:
surface_form: highpointer peak
instance_of: Mountain
countries: Canada
coordinates: lat: 81.6667
lon: -76.8333
Loon Lake (Cook County, Minnesota). Loon Lake is a lake in Cook County, Minnesota, off of the Gunflint Trail. Loon Lake is stocked with lake trout by the Minnesota Department of Natural Resources.

Geographic entities mentioned:
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 42.681175
lon: -83.358048
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 42.492777777778
lon: -77.566944444444
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6794
lon: -73.8581
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5958
lon: -123.844
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 48.0476
lon: -117.624
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 46.2
lon: -89.3
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 48.076
lon: -90.689
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 47.096111111111
lon: -93.870833333333
Mount Ahab. Mount Ahab is a conspicuous mountain high that rises between the lower ends of Mapple Glacier and Melville Glacier on the east coast of Graham Land. The mountain was roughly surveyed in 1947 by Falkland Islands Dependencies Survey and was resurveyed in 1955. The name was repositioned following a survey by the British Antarctic Survey in 1962.

Geographic entities mentioned:
surface_form: mount ahab
instance_of: Mountain
coordinates: lat: -65.433333333333
lon: -62.183333333333
surface_form: ahab
instance_of: Mountain
coordinates: lat: -65.433333333333
lon: -62.183333333333
Mount Ahab. Mount Ahab is a conspicuous mountain high that rises between the lower ends of Mapple Glacier and Melville Glacier on the east coast of Graham Land. The mountain was roughly surveyed in 1947 by Falkland Islands Dependencies Survey and was resurveyed in 1955. The name was repositioned following a survey by the British Antarctic Survey in 1962.

Geographic entities mentioned:
surface_form: mount ahab
instance_of: Mountain
coordinates: lat: -65.433333333333
lon: -62.183333333333
surface_form: ahab
instance_of: Mountain
coordinates: lat: -65.433333333333
lon: -62.183333333333
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
The mountain was roughly surveyed in 1947 by Falkland Islands Dependencies Survey and was resurveyed in 1955. The name was repositioned following a survey by the British Antarctic Survey in 1962. It was named by the United Kingdom Antarctic Place-Names Committee after Captain Ahab of the whaler &quot;Pequod&quot; - the central character in Herman Melville's 1851 novel &quot;Moby-Dick&quot;.

Geographic entities mentioned:
surface_form: ahab
instance_of: Mountain
coordinates: lat: -65.433333333333
lon: -62.183333333333
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
Mono–Inyo Craters. The Mono–Inyo Craters are a volcanic chain of craters, domes and lava flows in Mono County, Eastern California. The chain stretches from the northwest shore of Mono Lake to the south of Mammoth Mountain. The Mono Lake Volcanic Field forms the northernmost part of the chain and consists of two volcanic islands in the lake and one cinder cone volcano on its northwest shore.

Geographic entities mentioned:
surface_form: Mammoth Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6306
lon: -119.033
The Inyo volcanic chain form much of the southern part of the chain and consist of phreatic explosion pits, and rhyolitic lava flows and domes. The southernmost part of the chain consists of fumaroles and explosion pits on Mammoth Mountain and a set of cinder cones south of the mountain; the latter are called the Red Cones.

Geographic entities mentioned:
surface_form: Red Cones
instance_of: Mountain
countries: United States
coordinates: lat: 37.5886
lon: -119.058
The southernmost part of the chain consists of fumaroles and explosion pits on Mammoth Mountain and a set of cinder cones south of the mountain; the latter are called the Red Cones. Eruptions along the narrow fissure system under the chain began in the west moat of Long Valley Caldera 400,000 to 60,000 years ago. Mammoth Mountain was formed during this period.

Geographic entities mentioned:
surface_form: Long Valley Caldera
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
Setting. The Mono–Inyo Craters form a volcanic chain in Eastern California that sits along a narrow north–south-trending fissure system extending from the north shore of Mono Lake through the western Long Valley Caldera, south of Mammoth Mountain. The chain is within the Inyo National Forest and Mono County; the nearest incorporated community is Mammoth Lakes.

Geographic entities mentioned:
surface_form: Long Valley Caldera
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: Mammoth Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6306
lon: -119.033
surface_form: mono–inyo craters
instance_of: Mountain
countries: United States
coordinates: lat: 37.88333333
lon: -119
The fissure was formed by stretching induced by the intrusion of the Inyo dike. Stairs to the bottom of the fissure were removed after being damaged by earthquakes in 1980. Several Mono–Inyo-related explosion pits are on Mammoth Mountain. The Red Cones, south of Mammoth Mountain, are basaltic cinder cones and are the southernmost part of the Mono–Inyo Craters volcanic chain. Climate and ecology.

Geographic entities mentioned:
surface_form: Red Cones
instance_of: Mountain
countries: United States
coordinates: lat: 37.5886
lon: -119.058
surface_form: mono–inyo craters
instance_of: Mountain
countries: United States
coordinates: lat: 37.88333333
lon: -119
Typical evolution. Panum Crater is the northernmost volcano in the sequence and is a good example of both a tuff ring and a rhyolite dome. Its structure is twofold; an outer tuff ring (forming a classic crater) and an inner plug, or dome of rhyolite, pumice and obsidian created from lavas.

Geographic entities mentioned:
surface_form: Panum Crater
instance_of: Mountain
countries: United States
coordinates: lat: 37.9297
lon: -119.045
Above that layer are basaltic grading to rhyolitic volcanic rocks that are 3.5 million to less than 760,000 years old. Volcanism occurred north of the chain, in the Bodie Hills, as far back as 28 million years. Nearly all the rock east of the Sierra Nevada in the Mono Basin area is volcanic in origin. Volcanoes erupted from 3.6 to 2.3 million years ago near what is now Long Valley.

Geographic entities mentioned:
surface_form: Bodie Hills
instance_of: Landform
countries: United States
coordinates: lat: 38.2558
lon: -119.09
Volcanoes erupted from 3.6 to 2.3 million years ago near what is now Long Valley. Rhyolitic eruptions occurred in and around Glass Mountain in the same area from 2.1 to 0.8 million years ago. Volcanic ash from the massive (of ejecta) eruption of Long Valley Caldera some 760,000 years ago is preserved in the thick Bishop Tuff that covers much of the region.

Geographic entities mentioned:
surface_form: Long Valley Caldera
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
Timberland to the east of the Mono Craters was clearcut for wood. As part of the California Water Wars, the Los Angeles Department of Water and Power purchased large tracts of land in the 1930s within Mono Basin and Owens Valley in order to control water rights. Excavation of an water tunnel under the southern part of the Mono Craters dome complex started in 1934 and was completed in 1941.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
surface_form: owens valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
Multiple paved roads surround the Mono-Inyo craters. U.S. 395 is a scenic route that roughly parallels the Mono–Inyo Craters volcanic chain. California State Route 120 approaches the northern and eastern parts of the Mono Domes, including Panum Crater. Mammoth Scenic Loop approaches the Inyo Craters. Direct access to the Mono—Inyo Craters requires driving on unpaved roads, then walking.

Geographic entities mentioned:
surface_form: Panum Crater
instance_of: Mountain
countries: United States
coordinates: lat: 37.9297
lon: -119.045
Mammoth Scenic Loop approaches the Inyo Craters. Direct access to the Mono—Inyo Craters requires driving on unpaved roads, then walking. The town of Mammoth Lakes and Mammoth Mountain are located near the southern end of the chain. Mammoth Mountain Ski Area is located nearby and gondola rides can be taken year-round (weather permitting) to the mountain's summit.

Geographic entities mentioned:
surface_form: Mammoth Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6306
lon: -119.033
Mono–Inyo Craters. The Mono–Inyo Craters are a volcanic chain of craters, domes and lava flows in Mono County, Eastern California. The chain stretches from the northwest shore of Mono Lake to the south of Mammoth Mountain. The Mono Lake Volcanic Field forms the northernmost part of the chain and consists of two volcanic islands in the lake and one cinder cone volcano on its northwest shore.

Geographic entities mentioned:
surface_form: mono–inyo craters
instance_of: Mountain
countries: United States
coordinates: lat: 37.88333333
lon: -119
Jeffrey pine forests also surround the Inyo volcanic chain and Mammoth Mountain. Mule deer, coyotes, black bears, yellow-bellied marmots, raccoons and mountain lions all have ranges that are coincident with forests that cover parts of the Mono–Inyo craters. Typical evolution. Panum Crater is the northernmost volcano in the sequence and is a good example of both a tuff ring and a rhyolite dome.

Geographic entities mentioned:
surface_form: mono–inyo craters
instance_of: Mountain
countries: United States
coordinates: lat: 37.88333333
lon: -119
Volcanic ash from the massive (of ejecta) eruption of Long Valley Caldera some 760,000 years ago is preserved in the thick Bishop Tuff that covers much of the region. Eruptions of basalt and andesite 400,000 to 60,000 years ago in the west moat of Long Valley Caldera were the first activity associated with the Mono–Inyo Craters system.

Geographic entities mentioned:
surface_form: mono–inyo craters
instance_of: Mountain
countries: United States
coordinates: lat: 37.88333333
lon: -119
Steam rose in columns hundreds of feet high (tens of meters) from Hot Spring Cove on the island and the spring water was when geologist Israel Russell visited the island in the early 1880s. Human use. People have used resources on and around the Mono–Inyo Craters for centuries. Mono Paiutes gathered obsidian from the Mono–Inyo Craters to make sharp tools and arrow points.

Geographic entities mentioned:
surface_form: mono–inyo craters
instance_of: Mountain
countries: United States
coordinates: lat: 37.88333333
lon: -119
Human use. People have used resources on and around the Mono–Inyo Craters for centuries. Mono Paiutes gathered obsidian from the Mono–Inyo Craters to make sharp tools and arrow points. Unworked obsidian was carried by the Mono Paiutes over passes in the Sierra Nevada to trade with other Native American groups. Chips of Mono–Inyo obsidian can still be found at many ancient mountain campsites.

Geographic entities mentioned:
surface_form: mono–inyo craters
instance_of: Mountain
countries: United States
coordinates: lat: 37.88333333
lon: -119
The chain of craters has been the subject of several writers and naturalists. Mark Twain visited Mono Basin in the 1860s and wrote about Mono Lake, but did not mention any of the Mono–Inyo Craters except for the lake's two volcanic islands. He wrote in &quot;Roughing It&quot; (1872) that the lake was in a &quot;lifeless, hideous desert...&quot; that was the &quot;loneliest spot on earth...

Geographic entities mentioned:
surface_form: mono–inyo craters
instance_of: Mountain
countries: United States
coordinates: lat: 37.88333333
lon: -119
The Mono Basin National Forest Scenic Area, created in 1984, was the first National Scenic Area in the United States. It offers more protection than other United States Forest Service lands, surrounds Mono Lake and its two volcanic islands, Black Point, Panum Crater and much of the northern half of the Mono Craters.

Geographic entities mentioned:
surface_form: panum crater
instance_of: Mountain
countries: United States
coordinates: lat: 37.9297
lon: -119.045
heaps of loose ashes that have never been blest by either rain or snow...&quot;
In the spring of 1881 and the fall of 1882, geologist Israel Russell studied the area as a side-trip during his field research of Lake Lahontan, a now dry lake that covered much of nearby Nevada during the last glacial period.

Geographic entities mentioned:
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6282988
lon: -97.0561783
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 38.3360373
lon: -117.7898285
The domes of the chain lie on a roughly north–south-trending arc that is concave to the west and located south of Mono Lake. The highest of the Mono Craters domes is Crater Mountain (elevation 9,172 feet or 2,796 m), which rises above Pumice Valley to the west. Associated volcanic features are located in Mono Lake (Paoha and Negit Islands) and on its north shore (Black Point).

Geographic entities mentioned:
surface_form: crater mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.92206
lon: -118.42091
Straight Shore. The Straight Shore is a section of coastline on the island of Newfoundland in Newfoundland and Labrador, Canada. It follows a generally northwesterly direction from the town of Cape Freels to Musgrave Harbour and then a generally westerly direction along the southern shore of Sir Charles Hamilton Sound to Gander Bay.

Geographic entities mentioned:
surface_form: Sir Charles Hamilton Sound
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.55
lon: -54.11666666666667
Johnny Quilty won the Calder Memorial Trophy as the league's rookie of the year in the 1940–41 NHL season. Johnny Quilty grew up watching the original Ottawa Senators play at home, was the light-heavyweight boxing champion of the Ottawa Valley in 1939, and served in the military during World War II. Johnny Quilty died on September 12, 1969, at age 48. Quilty died on December 2, 1976, in Ottawa.

Geographic entities mentioned:
surface_form: Ottawa Valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
Geographic distribution. Distribution of the Gabon talapoin is centered around the River Ogooué, native to the equatorial coastal ridges between Cabinda and the Nyong River, and further extends to some Congo River branches. It can be found in Cameroon, Equatorial Guinea, Republic of the Congo and the Cabinda province of Angola.

Geographic entities mentioned:
surface_form: Nyong River
instance_of: Watercourse
countries: Cameroon
coordinates: lat: 3.9504
lon: 13.491527
Lychnis Mountain. Lychnis Mountain is a mountain summit located in Banff National Park, in the Canadian Rockies of Alberta, Canada. It is part of the Sawback Range. Its nearest higher peak is Mount St. Bride, to the north.

Geographic entities mentioned:
surface_form: Mount St. Bride
instance_of: Mountain
countries: Canada
coordinates: lat: 51.50001
lon: -115.95218
It is part of the Sawback Range. Its nearest higher peak is Mount St. Bride, to the north. The mountain is situated east of Tilted Mountain in an area of exposed Skoki Formation limestone which is known for fossils such as brachiopods, gastropods, conodonts, cephalopods, trilobites, and echinoderm fragments. History. Lychnis Mountain was named in 1911 by James F.

Geographic entities mentioned:
surface_form: Tilted Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4833
lon: -116.00218
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Lychnis Mountain. Lychnis Mountain is a mountain summit located in Banff National Park, in the Canadian Rockies of Alberta, Canada. It is part of the Sawback Range. Its nearest higher peak is Mount St. Bride, to the north.

Geographic entities mentioned:
surface_form: lychnis mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4833
lon: -115.98548
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Lychnis Mountain. Lychnis Mountain is a mountain summit located in Banff National Park, in the Canadian Rockies of Alberta, Canada. It is part of the Sawback Range. Its nearest higher peak is Mount St. Bride, to the north.

Geographic entities mentioned:
surface_form: lychnis mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4833
lon: -115.98548
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Its nearest higher peak is Mount St. Bride, to the north. The mountain is situated east of Tilted Mountain in an area of exposed Skoki Formation limestone which is known for fossils such as brachiopods, gastropods, conodonts, cephalopods, trilobites, and echinoderm fragments. History. Lychnis Mountain was named in 1911 by James F. Porter for the alpine flower &quot;Lychnis&quot;.

Geographic entities mentioned:
surface_form: lychnis mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4833
lon: -115.98548
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The first ascent of the mountain was made in 1969 by A.J. Kauffmann, W.L. Putnam, L. Putnam, and L.R. Wallace. Geology. Like other mountains in Banff Park, Lychnis Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: lychnis mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4833
lon: -115.98548
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Lychnis Mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: lychnis mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4833
lon: -115.98548
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
History. Lychnis Mountain was named in 1911 by James F. Porter for the alpine flower &quot;Lychnis&quot;. The mountain's name was officially adopted in 1956 when approved by the Geographical Names Board of Canada. The first ascent of the mountain was made in 1969 by A.J. Kauffmann, W.L. Putnam, L. Putnam, and L.R. Wallace. Geology.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Originally specializing in zoology, he became a prominent early conservationist and student of Native American life. Grinnell has been recognized for his influence on public opinion and work on legislation to preserve the American bison. Mount Grinnell in Glacier National Park in Montana is named after him. Early life and education.

Geographic entities mentioned:
surface_form: Mount Grinnell
instance_of: Mountain
countries: United States
coordinates: lat: 48.7766
lon: -113.727
Additionally, fishing employs 7% of the population. Cyclones. In 2022 the village was hit by the Cyclone Emnati. Roads. This municipality is linked by an unpaved provincial road to Analavory and the National road 12. Rivers. Vohimasina Sud lies at the southern banks of the Faraony River. On the northern side is situated Vohimasina Nord.

Geographic entities mentioned:
surface_form: Faraony River
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -21.8025
lon: 48.16611111