Sarmila/GeoWiki-Features huggingface dataset:
Anne climbed Tunnel Mountain over 8000 times over a 40-year period, averaging 200 ascents a year. Ness was even known to climb the mountain twice a day; once during lulls in her job, and a second in the evening. Famed wildlife artist Carl Rungius had his ashes scattered on the mountain, as he loved the view of Banff and the Bow Valley. Geology.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Anne climbed Tunnel Mountain over 8000 times over a 40-year period, averaging 200 ascents a year. Ness was even known to climb the mountain twice a day; once during lulls in her job, and a second in the evening. Famed wildlife artist Carl Rungius had his ashes scattered on the mountain, as he loved the view of Banff and the Bow Valley. Geology.

Geographic entities mentioned:
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
surface_form: bow valley
instance_of: Valley
countries: Canada
coordinates: lat: 51.1671
lon: -115.48
state of Montana. Description. Charlotte Peak is located in the Swan Range, a subset of the Rocky Mountains. It is situated in the Bob Marshall Wilderness, on land managed by Flathead National Forest. Precipitation runoff from the mountain drains to Big Salmon Lake and the South Fork Flathead River. Topographic relief is significant as the summit rises above Big Salmon Lake in one mile. Climate.

Geographic entities mentioned:
surface_form: salmon lake
instance_of: Lake
countries: United States
coordinates: lat: 43.946388888889
lon: -74.940277777778
surface_form: salmon lake
instance_of: Lake
countries: United States
coordinates: lat: 64.9028
lon: -165.009
Charlotte Peak. Charlotte Peak is an mountain summit located in Powell County of the U.S. state of Montana. Description. Charlotte Peak is located in the Swan Range, a subset of the Rocky Mountains. It is situated in the Bob Marshall Wilderness, on land managed by Flathead National Forest. Precipitation runoff from the mountain drains to Big Salmon Lake and the South Fork Flathead River.

Geographic entities mentioned:
surface_form: charlotte peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.571944444444
lon: -113.39
Topographic relief is significant as the summit rises above Big Salmon Lake in one mile. Climate. Based on the Köppen climate classification, Charlotte Peak is located in a subarctic climate zone characterized by long, usually very cold winters, and short, cool to mild summers. Winter temperatures can drop below −10 °F with wind chill factors below −30 °F.

Geographic entities mentioned:
surface_form: charlotte peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.571944444444
lon: -113.39
Geneva-on-the-Lake, Ohio. Geneva-on-the-Lake is a village in northwestern Ashtabula County, Ohio, United States, along the southern shore of Lake Erie. A small resort town, the population was 916 at the 2020 census. It is part of the Ashtabula micropolitan area, northeast of Cleveland. History.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
It is part of the Ashtabula micropolitan area, northeast of Cleveland. History. Settlement of the original area known as the Connecticut Western Reserve started in the early 1800s, as investors, farmers, and frontiersmen from New England and the Mid-Atlantic began to farm in the area and capitalize on the natural resources of Lake Erie and its shoreline.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Location. Broad Valley is in Graham Land towards the north of the Trinity Peninsula, which forms the tip of the Antarctic Peninsula. It is south of the Laclavère Plateau, west of Duse Bay, north of Eyrie Bay and east of Cugnot Ice Piedmont and Louis Philippe Plateau, from which it is separated by Windy Gap. Misty Pass leads northwest from the valley to the Cockerell Peninsula.

Geographic entities mentioned:
surface_form: Laclavère Plateau
instance_of: Landform
coordinates: lat: -63.45
lon: -57.7833
surface_form: Cugnot Ice Piedmont
instance_of: Landform
coordinates: lat: -63.6333
lon: -58.1667
surface_form: Louis Philippe Plateau
instance_of: Landform
coordinates: lat: -63.6
lon: -58.35
Marten Crag. A rocky peak rising to high on Trinity Peninsula. Situated between Stepup Col and the eastern foothills of Giovannini (Lobell) Ridge, northwest of McCalman Peak, north by east of Kribul Hill, east-southeast of Yarlovo Nunatak, southwest of Kanitz Nunatak and west of Kumata Hill. Surmounting Broad Valley to the north and Cugnot Ice Piedmont to the SE.

Geographic entities mentioned:
surface_form: McCalman Peak
instance_of: Mountain
coordinates: lat: -63.6167
lon: -57.7833
Broad Valley. Broad Valley () is a descriptive name for the broad glacier-filled valley on the south side of Laclavere Plateau, Trinity Peninsula, Antarctica. The name was suggested by V.I. Russell of the Falkland Islands Dependencies Survey (FIDS) following his survey in 1946. Location.

Geographic entities mentioned:
surface_form: laclavere plateau
instance_of: Landform
coordinates: lat: -63.45
lon: -57.7833
surface_form: broad valley
instance_of: Valley
coordinates: lat: -63.3667
lon: -57.9167
Kumata Hill. A partly ice-free hill rising to high on Trinity Peninsula. Situated east of Stepup Col, north-northwest of McCalman Peak, east of Marten Crag, south-southwest of Kanitz Nunatak and west-southwest of Cain Nunatak. Surmounting Broad Valley to the north and Cugnot Ice Piedmont to the S. German-British mapping in 1996.

Geographic entities mentioned:
surface_form: mccalman peak
instance_of: Mountain
coordinates: lat: -63.6167
lon: -57.7833
surface_form: cain nunatak
instance_of: Mountain
coordinates: lat: -63.566666666667
lon: -57.7
Broad Valley. Broad Valley () is a descriptive name for the broad glacier-filled valley on the south side of Laclavere Plateau, Trinity Peninsula, Antarctica. The name was suggested by V.I. Russell of the Falkland Islands Dependencies Survey (FIDS) following his survey in 1946. Location.

Geographic entities mentioned:
surface_form: broad valley
instance_of: Valley
coordinates: lat: -63.3667
lon: -57.9167
Russell of the Falkland Islands Dependencies Survey (FIDS) following his survey in 1946. Location. Broad Valley is in Graham Land towards the north of the Trinity Peninsula, which forms the tip of the Antarctic Peninsula. It is south of the Laclavère Plateau, west of Duse Bay, north of Eyrie Bay and east of Cugnot Ice Piedmont and Louis Philippe Plateau, from which it is separated by Windy Gap.

Geographic entities mentioned:
surface_form: broad valley
instance_of: Valley
coordinates: lat: -63.3667
lon: -57.9167
Features and nearby features include Stepup Col, Cain Nunatak, Abel Nunatak and View Point. Windy Gap. Pass high high, located at the northeast end of Louis Philippe Plateau. It marks the meeting place of three valleys of Trinity Peninsula, namely Broad Valley leading eastward toward Duse Bay, a valley leading northward to Lafond Bay, and another southward to Prince Gustav Channel.

Geographic entities mentioned:
surface_form: broad valley
instance_of: Valley
coordinates: lat: -63.3667
lon: -57.9167
Yarlovo Nunatak. A rocky hill rising to high on Trinity Peninsula. Situated in the northern foothills of Giovannini (Lobell) Ridge, west-northwest of Marten Crag, south of Prilep Knoll and southwest of Kanitz Nunatak. Surmounting Broad Valley to the north. Named after the settlement of Yarlovo in Western Bulgaria. Marten Crag. A rocky peak rising to high on Trinity Peninsula.

Geographic entities mentioned:
surface_form: broad valley
instance_of: Valley
coordinates: lat: -63.3667
lon: -57.9167
Situated between Stepup Col and the eastern foothills of Giovannini (Lobell) Ridge, northwest of McCalman Peak, north by east of Kribul Hill, east-southeast of Yarlovo Nunatak, southwest of Kanitz Nunatak and west of Kumata Hill. Surmounting Broad Valley to the north and Cugnot Ice Piedmont to the SE. Named after the town of Marten in Northeastern Bulgaria. Stepup Col.

Geographic entities mentioned:
surface_form: broad valley
instance_of: Valley
coordinates: lat: -63.3667
lon: -57.9167
surface_form: cugnot ice piedmont
instance_of: Landform
coordinates: lat: -63.6333
lon: -58.1667
Named after the town of Marten in Northeastern Bulgaria. Stepup Col. A snow-covered north–south running col linking Broad Valley and Cugnot Ice Piedmont, at the east end of Louis Philippe Plateau. The name given by UK Antarctic Place-Names Committee (UK-APC) is descriptive, as in height is gained when the col is traversed in a northerly direction. Kumata Hill.

Geographic entities mentioned:
surface_form: broad valley
instance_of: Valley
coordinates: lat: -63.3667
lon: -57.9167
surface_form: louis philippe plateau
instance_of: Landform
coordinates: lat: -63.6
lon: -58.35
surface_form: cugnot ice piedmont
instance_of: Landform
coordinates: lat: -63.6333
lon: -58.1667
A partly ice-free hill rising to high on Trinity Peninsula. Situated east of Stepup Col, north-northwest of McCalman Peak, east of Marten Crag, south-southwest of Kanitz Nunatak and west-southwest of Cain Nunatak. Surmounting Broad Valley to the north and Cugnot Ice Piedmont to the S. German-British mapping in 1996. Named after the Kumata locality on Vitosha Mountain in Western Bulgaria.

Geographic entities mentioned:
surface_form: broad valley
instance_of: Valley
coordinates: lat: -63.3667
lon: -57.9167
surface_form: cugnot ice piedmont
instance_of: Landform
coordinates: lat: -63.6333
lon: -58.1667
German-British mapping in 1996. Named after the Kumata locality on Vitosha Mountain in Western Bulgaria. Cain Nunatak. The westernmost of two isolated nunataks on the south side of Broad Valley. The name arose at the time of the FIDS geological survey in 1960-61 and is in association with nearby Abel Nunatak. Abel Nunatak. The easternmost of two isolated nunataks on the south side of Broad Valley.

Geographic entities mentioned:
surface_form: broad valley
instance_of: Valley
coordinates: lat: -63.3667
lon: -57.9167
The name arose at the time of the FIDS geological survey in 1960-61 and is in association with nearby Abel Nunatak. Abel Nunatak. The easternmost of two isolated nunataks on the south side of Broad Valley. The name arose at the time of the FIDS geological survey in 1960-61 and is in association with nearby Cain Nunatak. Eyrie Bay.

Geographic entities mentioned:
surface_form: broad valley
instance_of: Valley
coordinates: lat: -63.3667
lon: -57.9167
It is south of the Laclavère Plateau, west of Duse Bay, north of Eyrie Bay and east of Cugnot Ice Piedmont and Louis Philippe Plateau, from which it is separated by Windy Gap. Misty Pass leads northwest from the valley to the Cockerell Peninsula. Features and nearby features include Stepup Col, Cain Nunatak, Abel Nunatak and View Point. Windy Gap.

Geographic entities mentioned:
surface_form: cain nunatak
instance_of: Mountain
coordinates: lat: -63.566666666667
lon: -57.7
Surmounting Broad Valley to the north and Cugnot Ice Piedmont to the S. German-British mapping in 1996. Named after the Kumata locality on Vitosha Mountain in Western Bulgaria. Cain Nunatak. The westernmost of two isolated nunataks on the south side of Broad Valley. The name arose at the time of the FIDS geological survey in 1960-61 and is in association with nearby Abel Nunatak. Abel Nunatak.

Geographic entities mentioned:
surface_form: cain nunatak
instance_of: Mountain
coordinates: lat: -63.566666666667
lon: -57.7
Abel Nunatak. The easternmost of two isolated nunataks on the south side of Broad Valley. The name arose at the time of the FIDS geological survey in 1960-61 and is in association with nearby Cain Nunatak. Eyrie Bay. A bay, wide at its mouth and extending inland, lying north of Jade Point. So named by UK-APC because of the proximity to Eagle Island.

Geographic entities mentioned:
surface_form: cain nunatak
instance_of: Mountain
coordinates: lat: -63.566666666667
lon: -57.7
Features and nearby features include Stepup Col, Cain Nunatak, Abel Nunatak and View Point. Windy Gap. Pass high high, located at the northeast end of Louis Philippe Plateau. It marks the meeting place of three valleys of Trinity Peninsula, namely Broad Valley leading eastward toward Duse Bay, a valley leading northward to Lafond Bay, and another southward to Prince Gustav Channel.

Geographic entities mentioned:
surface_form: louis philippe plateau
instance_of: Landform
coordinates: lat: -63.6
lon: -58.35
The Japanese word &quot;udon-ge&quot; (, literally &quot;udon&quot;/&quot;udumbara&quot; flower&quot;) was used by Dōgen Zenji to refer to the flower of the &quot;udumbara&quot; tree in chapter 68 of the &quot;Shōbōgenzō&quot; (&quot;Treasury of the Eye of the True Dharma&quot;). Dōgen places the &quot;udonge&quot; in the context of the Flower Sermon given by Gautama Buddha on Vulture Peak.

Geographic entities mentioned:
surface_form: Vulture Peak
instance_of: Mountain
countries: India
coordinates: lat: 25.001666666666665
lon: 85.44638888888889
albiventer&quot;. The identity and exact provenance of &quot;fulgens&quot; (supposed to be from the Valley of Mexico), and consequently its relationship to &quot;O. albiventer&quot;, remain unknown. &quot;O. albiventer&quot; is part of the genus &quot;Oryzomys&quot;, which currently includes about eight species distributed from the eastern United States (&quot;O.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
Distribution and conservation. &quot;O. albiventer&quot; occurs at about elevation in northern Michoacán, southern Guanajuato, and central and eastern Jalisco, mostly in the area around Lake Chapala. Its range has seen massive agricultural development and although populations may survive, the current distribution of the species is certainly highly fragmented.

Geographic entities mentioned:
surface_form: Lake Chapala
instance_of: Lake
countries: Mexico
coordinates: lat: 20.333333333333
lon: -103
Waiontha Mountain. Waiontha Mountain is a small mountain chain in the Central New York Region of New York. It is made of two main elevations the tallest being. It is located in the Town of Springfield, east of Richfield Springs and north of Allen Lake. Wilders Hill is located northwest of Waiontha Mountain. Several lakes are at the base of the mountain.

Geographic entities mentioned:
surface_form: allen lake
instance_of: Lake
countries: United States
coordinates: lat: 42.83
lon: -74.952
surface_form: allen lake
instance_of: Lake
countries: United States
coordinates: lat: 47.18397
lon: -95.18435
surface_form: allen
instance_of: Watercourse
countries: United States
coordinates: lat: 40.44452778
lon: -92.04033333
Waiontha Mountain. Waiontha Mountain is a small mountain chain in the Central New York Region of New York. It is made of two main elevations the tallest being. It is located in the Town of Springfield, east of Richfield Springs and north of Allen Lake. Wilders Hill is located northwest of Waiontha Mountain. Several lakes are at the base of the mountain.

Geographic entities mentioned:
surface_form: waiontha mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.84224
lon: -74.94958
North Cornelly. North Cornelly is a moderately sized village in Bridgend County Borough, Wales. It is four miles from the seaside resort of Porthcawl and six miles from the town of Bridgend. The Kenfig nature reserve is less than a mile away. The village has numerous facilities and notable features.

Geographic entities mentioned:
surface_form: Kenfig nature reserve
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.5194
lon: -3.7362
According to the U.S. Census Bureau, the Kendall Park CDP has a total area of, of which, or 0.05%, are water. The community sits on high ground which drains north to Tenmile Run and Sixmile Run, and south to Heathcote Brook, all of which are tributaries of the Millstone River and part of the Raritan River watershed. 2010 census.

Geographic entities mentioned:
surface_form: Heathcote Brook
instance_of: Landform
countries: United States
coordinates: lat: 40.37361111
lon: -74.62
Grand Prairie Armed Forces Reserve Complex. The Grand Prairie Armed Forces Reserve Complex or Grand Prairie AFRC (formerly Naval Air Station Dallas or Hensley Field) is a former United States Navy Naval Air Station located on Mountain Creek Lake in southwest Dallas.

Geographic entities mentioned:
surface_form: Mountain Creek Lake
instance_of: Lake
countries: United States
coordinates: lat: 32.719269444444
lon: -96.960894444444
The total water storage capacity is 353 million gallons and the total cost of construction was $619,000. Establishment. In 1898, the British took over the New Territories and New Kowloon and the Public Works Department immediately sent engineering teams to explore water sources. However, the team found suitable valleys to build reservoirs in the west of Beacon Hill and south of Needle Hill.

Geographic entities mentioned:
surface_form: Needle Hill
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.3871
lon: 114.16
Dialects. There are three main dialects according to Halfmann (2024): Western Katë, Northeastern Katë, and Southeastern Katë (including Kamviri and Mumviri). The dialects are sometimes erroneously defined as separate languages. The Northeastern Katë dialect is commonly referred to as &quot;Shekhani&quot; in Chitral. In older literature, Southeastern Katë is split into Kamviri and Mumviri. Status.

Geographic entities mentioned:
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
Its population was 21,284 as of the 2020 census. Ozark is also the third largest city in the Springfield, Missouri Metropolitan Area, and is centered along a business loop of US 65, where it intersects with MO 14. History. Ozark was named after the Ozark Mountains, in which it is situated. The Ozark Courthouse Square Historic District was listed on the National Register of Historic Places in 2009.

Geographic entities mentioned:
surface_form: Ozark Mountains
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Drake Icefall. Drake Icefall is an icefall 2 nautical miles (4 km) wide between the Soholt Peaks and the Edson Hills in Antarctica, draining eastward from the plateau to join the general flow of Union Glacier through the Heritage Range, Ellsworth Mountains. It was named by the University of Minnesota Ellsworth Mountains Party, 1962–63, for Benjamin Drake IV, a geologist and member of the party.

Geographic entities mentioned:
surface_form: Soholt Peaks
instance_of: Mountain
coordinates: lat: -79.7167
lon: -84.2
Pichaqa. Pichaqa (Aymara &quot;pichaqa, phichaqa, piqacha&quot; a big needle, also spelled &quot;Pichaka&quot;) is a mountain in the Andes of Bolivia. It is situated in the La Paz Department, Pacajes Province, Calacoto Municipality. Pichaqa lies north-east of the Anallajsi volcano.

Geographic entities mentioned:
surface_form: pichaqa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.8097
lon: -68.8589
Pichaqa. Pichaqa (Aymara &quot;pichaqa, phichaqa, piqacha&quot; a big needle, also spelled &quot;Pichaka&quot;) is a mountain in the Andes of Bolivia. It is situated in the La Paz Department, Pacajes Province, Calacoto Municipality. Pichaqa lies north-east of the Anallajsi volcano.

Geographic entities mentioned:
surface_form: pichaqa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.8097
lon: -68.8589
surface_form: pichaqa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.8097
lon: -68.8589
Pichaqa. Pichaqa (Aymara &quot;pichaqa, phichaqa, piqacha&quot; a big needle, also spelled &quot;Pichaka&quot;) is a mountain in the Andes of Bolivia. It is situated in the La Paz Department, Pacajes Province, Calacoto Municipality. Pichaqa lies north-east of the Anallajsi volcano.

Geographic entities mentioned:
surface_form: anallajsi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.916666666667
lon: -68.916666666667
Dryhope Tower is a ruined Scottish peel tower in the valley of the Yarrow Water, in the historic county of Selkirkshire, now part of the Scottish Borders. It lies approximately equidistant between the burghs of Moffat and Selkirk, and defended the north eastern end of St Mary's Loch. The site itself was protected on two sides, to the east by the Dryhope Burn and to the west by the Kirkstead Burn.

Geographic entities mentioned:
surface_form: St Mary's Loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.492256
lon: -3.191433
Chibougamau is surrounded by, but not part of, the local municipality of Eeyou Istchee James Bay. Its remoteness from Lac Saint-Jean (over south-east) and Abitibi-Témiscamingue (over south-west) areas causes Chibougamau to provide services for a few smaller communities surrounding it (Mistissini, Oujé-Bougoumou, and Chapais) and for the regional resource-based industries.

Geographic entities mentioned:
surface_form: Lac Saint-Jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
Despite Chibougamau's remoteness, it is only about as far north as Winnipeg and is south of any part of the mainland of England. Nearby is Lac Aux Dorés, which is fed by the Chibougamau River from the larger Chibougamau Lake after which the town was named. &quot;Chibougamau&quot; means &quot;gathering place&quot; in the Cree language.

Geographic entities mentioned:
surface_form: Lac Aux Dorés
instance_of: Lake
countries: Canada
coordinates: lat: 49.8525
lon: -74.351389
surface_form: Chibougamau Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.83555555555556
lon: -74.22972222222222
It lasted two years, after which Przhevalsky published a diary of his expedition under the title, &quot;Travels in the Ussuri Region, 1867–69&quot;. His most well-known follower and student was Pyotr Kozlov, who discovered the ruins of the Tangut city Khara-Khoto in the Ejin Banner of Alxa League in western Inner Mongolia near the Juyan Lake Basin. Further expeditions.

Geographic entities mentioned:
surface_form: Juyan Lake Basin
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 42.29
lon: 101.26
Fuji Speedway. is a motorsport race track standing in the foothills of Mount Fuji, in Oyama, Suntō District, Shizuoka Prefecture, Japan. It was built in the early 1960s. In the 1980s, Fuji Speedway was used for the FIA World Sportscar Championship and national racing. Originally managed by Mitsubishi Estate, Fuji Speedway was acquired by Toyota in 2000.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
Tharaka University. Tharaka University (TUN) is a public university in Kenya. Location. The main campus of the university is located adjacent to the town of Gatunga, in Tharaka South Sub-county, in Tharaka Nithi County, on the eastern slopes of Mount Kenya in Central Kenya. Gatunga is located approximately, northeast of the city of Nairobi, the national capital. History.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
Turumtaykul. Turumtaykul (), also spelled Turumtaikul (;), is a freshwater mountain valley lake in Gorno-Badakhshan Autonomous Region, in the south-east Tajikistan, about east of the provincial capital of Khorugh. Lying in the Pamir Mountains at above sea level, it is, and has an area of with a maximum depth of. Its most numerous fish are Sattar snowtrout and false osman.

Geographic entities mentioned:
surface_form: turumtaykul
instance_of: Lake
countries: Tajikistan
coordinates: lat: 37.483055555556
lon: 72.5375
The village is located on the mainland part of Loppa Municipality, along the Bergsfjorden, across from the island of Silda. The village of Sør-Tverrfjord lies about to the southwest, across the fjord. The Svartfjellet mountain lies about straight east of the village, alongside the Svartfjelljøkelen glacier. Bergsfjord has no road connections to the rest of Norway.

Geographic entities mentioned:
surface_form: Svartfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 70.232777777778
lon: 21.998611111111
The 6th Fleet′s headquarters aboard &quot;Katori&quot; at Kwajalein attempted to contact her at midnight that night, but she did not respond. At 01:30 on 9 December 1941, &quot;I-70&quot; reported that she was southwest of Diamond Head and had sighted the United States Navy aircraft carrier arriving at Naval Station Pearl Harbor. The Japanese never heard from her again. Loss.

Geographic entities mentioned:
surface_form: Diamond Head
instance_of: Mountain
countries: United States
coordinates: lat: 21.259722222222
lon: -157.81175
Today an arcuate ridge remains of this edifice. &quot;Modern Ticsani&quot; is a complex of three lava domes which were emplaced during the Holocene. Two large eruptions took place during the Holocene, producing the so-called &quot;Grey Ticsani&quot; and &quot;Brown Ticsani&quot; deposits; the last eruption occurred after the 1600 eruption of neighbouring Huaynaputina.

Geographic entities mentioned:
surface_form: Huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223
surface_form: huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
Volcanism in South America occurs along its western coast and in several volcanic belts, including the Central Volcanic Zone that Ticsani is part of. In southern Peru the Central Volcanic Zone includes the volcanoes Solimana, Coropuna, Ampato, Sabancaya, Chachani, El Misti, Ubinas, Huaynaputina, Ticsani, Tutupaca, Calientes, Yucamane, Purupuruni and Casiri.

Geographic entities mentioned:
surface_form: Ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
surface_form: Chachani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.194166666667
lon: -71.531666666667
surface_form: Ubinas
instance_of: Mountain
countries: Peru
coordinates: lat: -16.34861111111111
lon: -70.90222222222222
surface_form: Huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223
surface_form: Tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: Yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: Purupuruni
instance_of: Mountain
countries: Peru
coordinates: lat: -17.30916667
lon: -69.91472222
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: misti
instance_of: Mountain
countries: Peru
coordinates: lat: -16.296388888888888
lon: -71.41055555555556
surface_form: el misti
instance_of: Mountain
countries: Peru
coordinates: lat: -16.296388888888888
lon: -71.41055555555556
surface_form: misti
instance_of: Mountain
countries: Peru
coordinates: lat: -15.525277777778
lon: -71.690833333333
surface_form: huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223
surface_form: ubinas
instance_of: Mountain
countries: Peru
coordinates: lat: -16.34861111111111
lon: -70.90222222222222
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
surface_form: chachani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.194166666667
lon: -71.531666666667
surface_form: purupuruni
instance_of: Mountain
countries: Peru
coordinates: lat: -17.30916667
lon: -69.91472222
surface_form: solimana
instance_of: Mountain
countries: Peru
coordinates: lat: -15.33111111
lon: -72.16222222
surface_form: solimana
instance_of: Mountain
countries: Peru
coordinates: lat: -15.41
lon: -72.893111111111
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
This subduction process is responsible for the growth of the Andes and for volcanism in the region; the oblique character of subduction has further led to the onset of strike-slip faulting. Ticsani is grouped together with the neighbouring volcanoes Huaynaputina and Ubinas, given their tectonic context, which is unusual for Peruvian volcanoes and shared geochemical traits.

Geographic entities mentioned:
surface_form: Huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223
surface_form: Ubinas
instance_of: Mountain
countries: Peru
coordinates: lat: -16.34861111111111
lon: -70.90222222222222
surface_form: huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223
surface_form: ubinas
instance_of: Mountain
countries: Peru
coordinates: lat: -16.34861111111111
lon: -70.90222222222222
surface_form: ubinas
instance_of: Mountain
countries: Peru
coordinates: lat: -16.34861111111111
lon: -70.90222222222222
The first eruption with a tephra volume of about - happened at 10,600 ± 80 years before present, and is known as the &quot;Grey Ticsani&quot; Pumice eruption. It is the most important explosive eruption at Ticsani and its deposits form large desertic landscapes east of the volcano. A second eruption formed the &quot;Grey Ticsani&quot; Ash and may have occurred in the middle Holocene.

Geographic entities mentioned:
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
The basement on which these volcanoes rose includes a Paleoproterozoic pluton. It is covered by the Mesozoic Yura Group and Matalaque Formation (sedimentary and volcanic rocks, respectively) which are exposed at the Rio Tambo. Volcanic activity continued during the Miocene, Pliocene and Pleistocene, forming ignimbrites and the Barroso Group. Composition.

Geographic entities mentioned:
surface_form: barroso
instance_of: Mountain
countries: Peru
coordinates: lat: -17.556308
lon: -69.5954717
Ticsani. Ticsani is a volcano in Peru northwest of Moquegua and consists of two volcanoes (&quot;Old Ticsani&quot; and &quot;Modern Ticsani&quot;) that form a complex. &quot;Old Ticsani&quot; is a compound volcano that underwent a large collapse in the past and shed of mass down the Rio Tambo valley. Today an arcuate ridge remains of this edifice.

Geographic entities mentioned:
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
Ticsani. Ticsani is a volcano in Peru northwest of Moquegua and consists of two volcanoes (&quot;Old Ticsani&quot; and &quot;Modern Ticsani&quot;) that form a complex. &quot;Old Ticsani&quot; is a compound volcano that underwent a large collapse in the past and shed of mass down the Rio Tambo valley. Today an arcuate ridge remains of this edifice.

Geographic entities mentioned:
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
The area is remote, which has hampered exploration efforts. There are paved roads in the area, which can be accessed mainly through the Ilo-Desaguadero highway that passes within from the Ticsani domes. Volcanism in South America occurs along its western coast and in several volcanic belts, including the Central Volcanic Zone that Ticsani is part of.

Geographic entities mentioned:
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
Ticsani features three lava domes, which were generated by latest Pleistocene and Holocene activity; two of which are located within or at the margins of craters. The southeasternmost dome is wide and high, the middle dome with a width of and a height of no less than is the largest of Ticsani. The northwestern dome has dimensions of.

Geographic entities mentioned:
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
Phenocrysts found in the later eruption products include amphibole, biotite, feldspar, plagioclase, pyroxene and quartz. Eruption history. Ticsani was active during the Pleistocene and Holocene. At first, a compound volcano developed at Ticsani.

Geographic entities mentioned:
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
Later the three lava domes were emplaced, with the southeastern dome being the oldest and the northwestern the youngest. Two or three explosive eruptions took place, accompanied by the emission of volcanic ash, blocks, lava bombs and pumice. The first eruption with a tephra volume of about - happened at 10,600 ± 80 years before present, and is known as the &quot;Grey Ticsani&quot; Pumice eruption.

Geographic entities mentioned:
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
This volcano stage also produced lava flows which filled valleys, formed a lava flow field northwest of the volcano and pyroclastic flows on the eastern side of the volcano. Ticsani is a candidate source for the Khonkho tephra, which was emplaced in Bolivia between AD 400 and 700. There are no historical eruptions at Ticsani.

Geographic entities mentioned:
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
Known springs occur at Chuchumbaya, Putina Arriba and Secolaque; the Putina River hot springs are among the most important in Peru. In 2005, earthquake activity was noted beneath Ticsani, possibly related to a hydrothermal system, which raised alarm and concern among the local population. A seismic swarm took place between 2014-2017.

Geographic entities mentioned:
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
A seismic swarm took place between 2014-2017. A characteristic trait of Ticsani are so-called &quot;hybrid&quot; earthquakes which are noticed at seismic stations of other volcanoes. A temporary seismic station installed 2015 at Ticsani recorded volcano-tectonic earthquakes, and other changes in its behaviour have been observed as well. Hazards.

Geographic entities mentioned:
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
A temporary seismic station installed 2015 at Ticsani recorded volcano-tectonic earthquakes, and other changes in its behaviour have been observed as well. Hazards. About 5,000 people live within to Ticsani and would be threatened in the case of a future eruption, with particular hazards including ash fall, lahars, pyroclastic flows and the collapse of lava domes.

Geographic entities mentioned:
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
In addition to the local population, ashfall would hit major regional roads, reservoirs, mines and airports. Additional towns in the area include Cambrune and Carumas. Pyroclastic flows are fast-moving flows of hot rock fragments and gases; at Ticsani they have reached distances of at least from the volcano.

Geographic entities mentioned:
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
Elovishka Planina. Elovishka Planina () is a mountain range in Kraishte region of western Bulgaria with an altitude of 1,329 meters above sea level. It is part of the Ruy-Verila range. The mountain has the shape of an isosceles triangle, with its apex facing northwest. Its length is about 16 km and the width reaches a maximum of 7 km.

Geographic entities mentioned:
surface_form: Verila
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.391666666667
lon: 23.263611111111
Its length is about 16 km and the width reaches a maximum of 7 km. To the north the valley of the river Leshnikovitsa, a right tributary of the Erma, separates it from the Leshnikovska Planina; to the west the upper course of the same river and the Valcha Polyana Saddle (1,105 m) form the boundary with the Bohovska Planina.

Geographic entities mentioned:
surface_form: Leshnikovska Planina
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.784
lon: 22.574
surface_form: Bohovska Planina
instance_of: Mountain
countries: Bulgaria
Serbia
coordinates: lat: 42.7419
lon: 22.5003
Elovishka Planina. Elovishka Planina () is a mountain range in Kraishte region of western Bulgaria with an altitude of 1,329 meters above sea level. It is part of the Ruy-Verila range. The mountain has the shape of an isosceles triangle, with its apex facing northwest. Its length is about 16 km and the width reaches a maximum of 7 km.

Geographic entities mentioned:
surface_form: elovishka planina
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.709
lon: 22.562
Its highest point is the summit of Plocha (1,329 m). The Elovishka Planina is built up of crystalline rocks and quartzites. The main watershed ridge of the Balkan Peninsula, separating the Black Sea drainage basin to the north and the Aegean Sea one to the south, runs in direction west–east along the mountain range. he predominant soils are brown forest soils.

Geographic entities mentioned:
surface_form: elovishka planina
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.709
lon: 22.562
Rannoch. Rannoch (or, meaning 'bracken') is an area of the Scottish Highlands between the A9 road, to the east, and the A82, to the west. The area is crossed from south to north by the West Highland railway line. Features of the area include Loch Rannoch and Rannoch Moor. The loch is in the northwest of the council area of Perth and Kinross.

Geographic entities mentioned:
surface_form: Loch Rannoch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.688299
lon: -4.30386
Boulenophrys brachykolos. &quot;Boulenophrys brachykolos&quot;, the short-legged horned toad or Peak spadefoot toad, is a frog native to southern China and Vietnam. It was first discovered in the Victoria Peak (locally known as The Peak), Hong Kong. Many populations of Hong Kong are in the country parks, such as Lung Fu Shan Country Park. Taxonomy and distribution.

Geographic entities mentioned:
surface_form: Victoria Peak
instance_of: Mountain
countries: People's Republic of China
British Hong Kong
coordinates: lat: 22.275469444444
lon: 114.14382777778
Lake City Community School is a school in Lake City, Hinsdale County, Colorado, United States. It provides Pre-K to 12th grade education for approximately 100 students. It is the only school in Hinsdale School District RE-1. This school hosts soccer games against Gunnison and Crested Butte. U-12 and U13 soccer teams consist only of Pre-K through 7th grade. The school hosts ACT and CSAP tests.

Geographic entities mentioned:
surface_form: Crested Butte
instance_of: Mountain
countries: United States
coordinates: lat: 38.883333333333
lon: -106.94361111111
Overall, the Western Satraps may have played a role in the transmission of the art of Gandhara to the western Deccan region.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Hooper, Colorado. The Town of Hooper is a Statutory Town located in the San Luis Valley in Alamosa County, Colorado, United States. The population was 81 at the 2020 census. Geography. According to the United States Census Bureau, the town has a total area of, all of it land. Nearby points of interest include the Great Sand Dunes National Park and the town of Crestone. History.

Geographic entities mentioned:
surface_form: San Luis Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.2
lon: -105.42
Major structural damage was also reported in Granada, where the Alhambra palace was affected, as well as in the towns of Guadix, Baza, Ugíjar, and Almanzora. Secondary effects. The earthquake triggered numerous landslides that blocked roads between Granada and Almería. Several springs experienced changes in their discharge rates, and the Río Andarax temporarily dried up.

Geographic entities mentioned:
surface_form: Andarax
instance_of: Watercourse
countries: Spain
coordinates: lat: 37.0153
lon: -2.88917
Gishwati Forest. Gishwati Forest is a forest in the north-western part of Rwanda, not far from Lake Kivu. It is part of Gishwati–Mukura National Park. The area's forests were largely intact in 1978, and substantial forest cover still remained in 1986. During the Rwandan genocide, wave after wave of refugees arrived in Gishwati Forest and began clearing it, often for subsistence farming.

Geographic entities mentioned:
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
History. The Gishwati Forest used to be one piece in a complex system of rainforests through the middle of Africa. It used to extend west beyond Lake Kivu connecting with the rainforests of the Congo, and south connecting with Nyungwe Forest. These forest systems have become fragmented due to population increase and deforestation.

Geographic entities mentioned:
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
The first commercial mines in the Keweenaw Peninsula (nicknamed the &quot;Copper Country&quot; and &quot;Copper Island&quot;) opened in the 1840s. Isle Royale in western Lake Superior was also a site of many tons of native copper. Some of it was extracted by native peoples, but only one of several commercial attempts at mining turned a profit there.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Communities of Italian Americans were established in many major industrial cities of the early 20th century, such as Baltimore (particularly Little Italy, Baltimore), Boston (particularly in the North End and East Boston) along with numerous nearby cities and towns, Philadelphia proper (particularly South Philadelphia) and the Philadelphia metro area (particularly neighborhoods in Delco, Atlantic City, Little Italy, Wilmington; and Vineland), Pittsburgh (particularly Bloomfield), Northeastern Pennsylvania cities, Lehigh Valley cities, Detroit, Providence (particularly Federal Hill), St.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
He served as Lieutenant of the Middlesex Yeomanry in 1803 and Lieutenant-Colonel of the Haytor Volunteer Infantry, also in 1803. Personal life. Lord Dunmore died at Glen Finart in Argyllshire on 11 November 1836, aged 74. He and was succeeded in his titles by his eldest son Alexander. Lady Dunmore died in May 1846, aged 71.

Geographic entities mentioned:
surface_form: Glen Finart
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.06667
lon: -4.93333
Legendre River. The Legendre River (&quot;in French: rivière Legendre&quot;) is a tributary of the Felton River which flows into the Baie Sauvage to the south of Grand lac Saint François which constitutes the head lake of the Saint-François River.

Geographic entities mentioned:
surface_form: Grand lac Saint François
instance_of: Lake
countries: Canada
coordinates: lat: 45.8986
lon: -71.1578
Location. The house lies on the Stripsenjoch which forms a bridge between the ridges of the Zahmer Kaiser and Wilder Kaiser at the head of the Kaiserbachtal and Kaisertal valleys at a height of 1,577 m. The Stripsenjochhaus therefore occupies a very central position and is often referred to as the turntable of the Kaisergebirge. Facilities.

Geographic entities mentioned:
surface_form: Kaisertal
instance_of: Valley
countries: Austria
coordinates: lat: 47.58416666666667
lon: 12.265833333333333
Haplochromis omnicaeruleus. &quot;Haplochromis omnicaeruleus&quot; is a species of cichlid endemic to Lake Victoria where it is known from the southeastern portion of the lake. This species can reach a length of SL.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
The eastern sand darter (&quot;Ammocrypta pellucida&quot;) is a species of freshwater ray-finned fish, a darter from the subfamily Etheostomatinae, part of the family Percidae, which also contains the perches, ruffes and pikeperches. The eastern sand darter is a relatively small fish, most plentiful in the Mississippi and Ohio Rivers, as well as Lake Champlain and the Great Lakes.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Four rowing crews had confirmed Olympic places for their boats in the women's lightweight double sculls and large-boat classes (men's four, men's & women's eight) at the 2015 FISA World Championships in Lac d'Aiguebelette, France, while rowers competing in the men's lightweight four and quadruple sculls were further added to the Russian roster with their top two finish at the 2016 European & Final Qualification Regatta in Lucerne, Switzerland.

Geographic entities mentioned:
surface_form: Lac d'Aiguebelette
instance_of: Lake
countries: France
coordinates: lat: 45.552777777778
lon: 5.7972222222222
It is the seventh-highest point in the North Wenatchee Mountains. Harding Mountain is situated within the Alpine Lakes Wilderness, northwest of Mount Stuart, and west of Eightmile Mountain, on land managed by Wenatchee National Forest. Precipitation runoff from the peak drains into tributaries of Icicle Creek, which in turn is a tributary of the Wenatchee River.

Geographic entities mentioned:
surface_form: Mount Stuart
instance_of: Mountain
countries: United States
coordinates: lat: 47.4753
lon: -120.901
surface_form: Eightmile Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.532188
lon: -120.897553
surface_form: harding mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.5275
lon: -120.98583333333
Harding Mountain. Harding Mountain is a mountain summit located in Chelan County of Washington state. It is the seventh-highest point in the North Wenatchee Mountains. Harding Mountain is situated within the Alpine Lakes Wilderness, northwest of Mount Stuart, and west of Eightmile Mountain, on land managed by Wenatchee National Forest.

Geographic entities mentioned:
surface_form: harding mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.5275
lon: -120.98583333333