Sarmila/GeoWiki-Features huggingface dataset:
Coleophora unigenella. &quot;Coleophora unigenella&quot; is a moth of the family Coleophoridae. It is found in Fennoscandia, northern Russia and the Alps. The larvae feed on &quot;Dryas octopetala&quot;. Larvae can be found from autumn to spring.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Boris studied in some European universities, where he specialized in languages and classics. &quot;At Baden-Baden in Germany, he met a Russian American, Nikolai Romanoff, and learned from him about the existence, at Point Loma, close San Diego in California, of the organization, named Universal Brotherhood and Theosophical Society. He wrote a letter to Mrs.

Geographic entities mentioned:
surface_form: Point Loma
instance_of: Landform
countries: United States
coordinates: lat: 32.67
lon: -117.24194444
Intergovernmental Authority on Development. The Intergovernmental Authority on Development (IGAD) is an eight-country trade bloc in Africa. It includes governments from the Horn of Africa, Nile Valley and the African Great Lakes. It is headquartered in Djibouti. Formation. The Intergovernmental Authority on Development was established in 1996.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
Dranse (Haute-Savoie). The Dranse () is a French river in the department of Haute-Savoie, that empties into Lake Geneva between Thonon-les-Bains and Évian-les-Bains. The name &quot;Dranse&quot; comes from the former &quot;Drantia&quot;, based on the hydronym &quot;dur-, dora&quot; and the suffix &quot;-antia&quot;. Geography.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
The Dranse empties into Lake Geneva and forms a delta, which is integrated into the Delta de la Dranse National Nature Reserve, situated to the east of the commune of Thonon-les-Bains, which although small at an area of, offers an incomparable botanic diversity. The river is long. Whitewater kayakers and commercial rafting companies frequently run this river. Hydrology.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Whitewater kayakers and commercial rafting companies frequently run this river. Hydrology. The Dranse is a high-volume river, as are all the rivers which originate in the Alpine mountain ranges. Its discharge was observed for a period of 97 years (1906–2003) in Reyvroz, a locality in the department of Haute-Savoie situated on the southern bank of Lake Geneva at the same elevation as its outlet.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Overview. The map shows a hilly area with the Rajmahal hills running from the bank of the Ganges in the extreme north to the south, beyond the area covered by the map into Dumka district. ‘Farakka’ is marked on the map and that is where Farakka Barrage is, just inside West Bengal. Rajmahal coalfield is shown in the map. The area is overwhelmingly rural with only small pockets of urbanisation.

Geographic entities mentioned:
surface_form: Rajmahal hills
instance_of: Mountain
countries: India
coordinates: lat: 25
lon: 87
Shenandoah District (VHSL). The Shenandoah District is a sports conference of the Virginia High School League which draws its members from the central part of the Shenandoah Valley, specifically clustered around Staunton and Waynesboro.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Europa Hut. The Europa Hut (German: &quot;Europahütte&quot;) is a mountain hut located in the Mattertal above Randa in the Mischabel range at 2,265 m, owned by the Swiss Alpine Club. It lies on the Grächen-Zermatt high trail, called &quot;Europaweg&quot; (also part of the Monte Rosa Tour). From the hut a trail leads to the Dom Hut, on the normal route to the Dom.

Geographic entities mentioned:
surface_form: Mattertal
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.083333333333
lon: 7.8
Khorenatsi writes that Tiran spent the rest of his years in the village of Kuash on the slopes of Mount Aragats, until he was strangled on Arshak II's orders after he admonished his son for his treatment of Gnel, Arshak's nephew; the &quot;Buzandaran Patmutʻiwnkʻ&quot; gives no information about Tiran's death. Family. Tiran was succeeded by his son Arshak II.

Geographic entities mentioned:
surface_form: Mount Aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
After removal of the meters, the remaining posts had bicycle parking rings installed on them, significantly increasing the supply of bicycle parking. He was retained by the City of Toronto government to represent the environmental group 'Save the Rouge' in the Oak Ridges Moraine Ontario Municipal Board hearing in 2000–2001.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
Krishna district. Krishna district is a district in the Coastal Andhra region in Indian state of Andhra Pradesh, with Machilipatnam as its administrative headquarters. It is surrounded on the East by Bay of Bengal, West by Guntur, Bapatla and North by Eluru and NTR districts and South again by Bay of Bengal. Etymology.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Further Again in 2022 Krishna District was divided into Krishna and NTR Districts. It was named after the Krishna River (also known as Krishnaveni in literature) the third longest river in India. The river flows through the district before it empties itself into Bay of Bengal, near Hamsaladevi village. History. The history of this region dates back to the 2nd century BCE.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The total urban population is (40.81%). There are literates with a literacy rate of 73.74%. Geography. Krishna district is surrounded on the east by Bay of Bengal, west by Guntur and Bapatla districts and north by Eluru and NTR districts and south by Bay of Bengal. The Krishna district occupies an area of. It has a total coastline of. Flora and fauna.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Suli Top. Suli Top is a Himalayan mountain peak in the Pithoragarh district of the Uttarakhand state of India. It is situated over the eastern flank of Kalabaland Glacier, east of Johar Valley. The other peaks on the massif are Chiring We (6,559 m), Trigal (5,983 m), and Bamba Dhura (6,334 m), etc. This ridge is a geographical divide between Lassar and Kalabaland valley.

Geographic entities mentioned:
surface_form: Johar Valley
instance_of: Valley
countries: India
coordinates: lat: 30.0718999
lon: 80.2348505
Suli Top. Suli Top is a Himalayan mountain peak in the Pithoragarh district of the Uttarakhand state of India. It is situated over the eastern flank of Kalabaland Glacier, east of Johar Valley. The other peaks on the massif are Chiring We (6,559 m), Trigal (5,983 m), and Bamba Dhura (6,334 m), etc. This ridge is a geographical divide between Lassar and Kalabaland valley.

Geographic entities mentioned:
surface_form: Chiring We
instance_of: Mountain
countries: India
coordinates: lat: 30.42
lon: 80.3
surface_form: Bamba Dhura
instance_of: Mountain
countries: India
coordinates: lat: 30.44
lon: 80.28
Suli Top. Suli Top is a Himalayan mountain peak in the Pithoragarh district of the Uttarakhand state of India. It is situated over the eastern flank of Kalabaland Glacier, east of Johar Valley. The other peaks on the massif are Chiring We (6,559 m), Trigal (5,983 m), and Bamba Dhura (6,334 m), etc. This ridge is a geographical divide between Lassar and Kalabaland valley.

Geographic entities mentioned:
surface_form: suli top
instance_of: Mountain
countries: India
coordinates: lat: 30.4
lon: 80.32
These traditions originated in Kashmir after 850 CE, as an adaptation to upper-class Hindu norms of 'wild' tantric Kaula traditions. Trika Shaivism later spread beyond Kashmir, particularly flourishing in the states of Odisha and Maharashtra.

Geographic entities mentioned:
surface_form: Kashmir
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Surrounded by a series of mountain ranges, it is encompassed by the Western portion of the Srednogorski mountain range. To the east lies the Golo Burdo Mountain, Verila to the southeast and south, Konyavska Mountain to the southwest, Zemenska Mountain to the west, and the lower ranges of Rudina and Cherna Gora to the northeast.

Geographic entities mentioned:
surface_form: Verila
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.391666666667
lon: 23.263611111111
Chilbongsan (North Gyeongsang). Chilbongsan ()is a mountain of North Gyeongsang Province, eastern South Korea. It has an elevation of 600 metres.

Geographic entities mentioned:
surface_form: chilbongsan
instance_of: Mountain
countries: South Korea
surface_form: chilbongsan (north gyeongsang)
instance_of: Mountain
countries: South Korea
Chilbongsan (North Gyeongsang). Chilbongsan ()is a mountain of North Gyeongsang Province, eastern South Korea. It has an elevation of 600 metres.

Geographic entities mentioned:
surface_form: chilbongsan
instance_of: Mountain
countries: South Korea
surface_form: chilbongsan
instance_of: Mountain
countries: South Korea
Occurrence. In addition to the type location in the Sandy mine in New Mexico, it has been reported from Coat-an-Noz, Cotes-du-Nord, France; in drill core from the North Sea; from Klatovy, Czech Republic; Ishimskaya Luka, northern Kazakhstan; the Slyudyanka complex, Sayan Mountains, near Lake Baikal region of Russia and the Yamoto mine, Kagoshima Prefecture, Japan.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
It was estimated to be 7.0 on the surface-wave magnitude scale with a maximum intensity of IX (&quot;Violent&quot;) on the Mercalli intensity scale. It was centered near Lake Burdur in southwestern Anatolia and the mainshock and subsequent fire destroyed more than 17,000 homes, and caused 2,344 casualties. Earthquake.

Geographic entities mentioned:
surface_form: Lake Burdur
instance_of: Lake
countries: Turkey
coordinates: lat: 37.7337
lon: 30.1781
Clarence Fahnestock Memorial State Park, also known as Fahnestock State Park, is a state park located in Putnam and Dutchess counties, New York. The park has hiking trails, a beach on Canopus Lake, and fishing on four ponds and two lakes. Spanning parts of the towns of Putnam Valley, Kent, and Carmel, most of the park is situated in northern Putnam County between the Taconic State Parkway and U.S.

Geographic entities mentioned:
surface_form: Canopus Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.4619
lon: -73.8329
Today the park covers. Description. Clarence Fahnestock State Park includes a lake (Canopus), a pond (Pelton), a beach, picnic tables with pavilions, a playground, recreation programs, a nature trail, hiking and biking, a bridle path, seasonal turkey and deer hunting, fishing and ice fishing, a campground with tent and trailer sites, a boat launch with boat rentals, and a food concession.

Geographic entities mentioned:
surface_form: Canopus
instance_of: Lake
countries: United States
coordinates: lat: 41.4619
lon: -73.8329
surface_form: Pelton
instance_of: Lake
countries: United States
coordinates: lat: 41.4606659
lon: -73.8289247
Instead it followed Boulevard Henri-Bourassa to Boulevard Pie-IX, both of which are principal urban arterial roads. Boulevard Pie-IX north of Boulevard Henri-Bourassa was used as a temporary section of Autoroute 25 across the Rivière-des-Prairies to Autoroute 440. From there, A-25 proceeded east with A-440, then continued north and east of Laval.

Geographic entities mentioned:
surface_form: Rivière-des-Prairies
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.708333333333
lon: -73.479166666667
The $207-million project will save some $226 million for the province since a private consortium will assume any cost overruns. A toll bridge using a RFID transponder automatic payment system spans the Rivière des Prairies and costs transponder-owning motorists $3.20 per crossing at peak hours (6-9 AM and 3-6 PM) and $2.24 per crossing the rest of the day.

Geographic entities mentioned:
surface_form: Rivière des Prairies
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.708333333333
lon: -73.479166666667
With the arrival of the Earl of Selkirk and his Scottish retinue (people largely displaced by the Highland Clearances), as well as the purchase of forty-five million acres of land in the Red River Valley, many Scottish culinary traditions were brought to the region. These foods included black bun, haggis, honey cakes, and rowies.

Geographic entities mentioned:
surface_form: Red River Valley
instance_of: Valley
countries: Canada
United States
coordinates: lat: 49
lon: -97.5
Üvarjärv. Üvarjärv is a lake in Soodi, Võru County, Estonia.

Geographic entities mentioned:
surface_form: üvarjärv
instance_of: Lake
countries: Estonia
coordinates: lat: 57.750833333333
lon: 27.046666666667
Ponggen Dopku, also spelled Pongen Dopku, is a mountain in Nepal. Description. Ponggen Dopku is a glaciated summit in the Nepali Himalayas. The elevation has also been reported as 5,930 metres. The peak is situated north-northeast of Kathmandu above the Langtang Valley of Langtang National Park. Precipitation runoff from the mountain's slopes drains to the Trishuli River via Lānṭān Kholā.

Geographic entities mentioned:
surface_form: Langtang Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 28.25
lon: 85.5
Climate. Based on the Köppen climate classification, Ponggen Dopku is located in a tundra climate zone with cold, snowy winters, and cool summers. Weather systems coming off the Bay of Bengal are forced upwards by the Himalaya mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall. Mid-June through early-August is the monsoon season.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
El Laco. El Laco is a volcanic complex in the Antofagasta Region of Chile. It is directly south of the Cordón de Puntas Negras volcanic chain. Part of the Central Volcanic Zone of the Andes, it is a group of seven stratovolcanoes and a caldera. It is about two million years old. The main summit of the volcano is a lava dome called Pico Laco, which is variously reported to be or high.

Geographic entities mentioned:
surface_form: Cordón de Puntas Negras
instance_of: Mountain
countries: Chile
coordinates: lat: -23.742777777778
lon: -67.534166666667
The iron-containing rocks are a less important component. Other components are diopside pegmatites. The whole rock falls into the calc-alkaline class of volcanic rocks, similar to these erupted by the neighbouring volcanoes Lascar and Llullaillaco. The andesites contain plagioclase clinopyroxene, orthopyroxene, and phenocrysts of magnetite.

Geographic entities mentioned:
surface_form: Llullaillaco
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.719863
lon: -68.536852
El Hueso volcano to the north is - high and has a basement diameter of. It has a crater with a diameter of. The city of Antofagasta is located west of El Laco. Other close towns are Calama and San Pedro de Atacama. The international road through Sico Pass connecting Salta in Argentina with Calama in Chile runs close to El Laco.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
El Laco. El Laco is a volcanic complex in the Antofagasta Region of Chile. It is directly south of the Cordón de Puntas Negras volcanic chain. Part of the Central Volcanic Zone of the Andes, it is a group of seven stratovolcanoes and a caldera. It is about two million years old. The main summit of the volcano is a lava dome called Pico Laco, which is variously reported to be or high.

Geographic entities mentioned:
surface_form: el laco
instance_of: Mountain
countries: Chile
coordinates: lat: -23.84155556
lon: -67.49016667
Similar deposits of volcanic iron oxide exist in Australia, Chile, and Iran. Geography. El Laco is part of the Cordón de Puntas Negras sector of the Central Volcanic Zone, directly south of that volcanic chain. It sits atop a quartzite and sandstone basement that was lifted from the seaground during the Acadian orogeny and is of Ordovician age.

Geographic entities mentioned:
surface_form: el laco
instance_of: Mountain
countries: Chile
coordinates: lat: -23.84155556
lon: -67.49016667
surface_form: cordón de puntas negras
instance_of: Mountain
countries: Chile
coordinates: lat: -23.742777777778
lon: -67.534166666667
Later, Mesozoic and Cenozoic sedimentation of the Salta Group occurred, which was then buried by Tertiary rhyolites. Two major volcanic lineaments cross in the El Laco area, including the so-called Calama-Olacapato-El Toro lineament. El Hueso volcano to the north is - high and has a basement diameter of. It has a crater with a diameter of. The city of Antofagasta is located west of El Laco.

Geographic entities mentioned:
surface_form: el laco
instance_of: Mountain
countries: Chile
coordinates: lat: -23.84155556
lon: -67.49016667
El Hueso volcano to the north is - high and has a basement diameter of. It has a crater with a diameter of. The city of Antofagasta is located west of El Laco. Other close towns are Calama and San Pedro de Atacama. The international road through Sico Pass connecting Salta in Argentina with Calama in Chile runs close to El Laco.

Geographic entities mentioned:
surface_form: el laco
instance_of: Mountain
countries: Chile
coordinates: lat: -23.84155556
lon: -67.49016667
The city of Antofagasta is located west of El Laco. Other close towns are Calama and San Pedro de Atacama. The international road through Sico Pass connecting Salta in Argentina with Calama in Chile runs close to El Laco. A number of tourist sites are found in the Atacama Desert adjacent to El Laco, and the dry climate also makes the area suitable for astronomy facilities. Geology.

Geographic entities mentioned:
surface_form: el laco
instance_of: Mountain
countries: Chile
coordinates: lat: -23.84155556
lon: -67.49016667
A number of tourist sites are found in the Atacama Desert adjacent to El Laco, and the dry climate also makes the area suitable for astronomy facilities. Geology. The El Laco volcanic complex is formed by about seven minor stratovolcanoes and lava domes. The complex started its activity in the Miocene-Pliocene, when porphyric andesites formed a stratovolcano.

Geographic entities mentioned:
surface_form: el laco
instance_of: Mountain
countries: Chile
coordinates: lat: -23.84155556
lon: -67.49016667
The volcanic complex is located an altitude of and covers a surface area of with a minimum volume of of volcanic rock. The main summit, Pico Laco or Pitón El Laco, has an altitude of, although a maximum height of has also been reported. Pico Laco is an andesitic lava dome with a height of above the surrounding terrain.

Geographic entities mentioned:
surface_form: el laco
instance_of: Mountain
countries: Chile
coordinates: lat: -23.84155556
lon: -67.49016667
Some minor metasomatic alteration occurred at the contact sites between andesites and iron-containing rocks. Hydrothermal alteration has also been described for lower portions of the volcanic pile and probably occurred because of gases escaping from intruded magma. Moraines found west of El Laco were generated by glaciation both on El Laco and Puntas Negras.

Geographic entities mentioned:
surface_form: el laco
instance_of: Mountain
countries: Chile
coordinates: lat: -23.84155556
lon: -67.49016667
surface_form: el laco
instance_of: Mountain
countries: Chile
coordinates: lat: -23.84155556
lon: -67.49016667
Surface exposure dating has indicated ages of 226 and 287 ka for some ice-affected lavas and argon-argon dating produced a youngest age of about 120,000 years. Further, andesitic volcanism in neighbouring volcanoes has blanketed El Laco. Reports exist of continuing fumarolic activity and hot springs with the deposition of clay and other minerals. Iron-rich deposits.

Geographic entities mentioned:
surface_form: el laco
instance_of: Mountain
countries: Chile
coordinates: lat: -23.84155556
lon: -67.49016667
Mining in Laco Sur removed about two million tons of magnetite between the 1970s and 1990s, leaving an open pit exposing of rock. The Compañía Minera del Pacífico (CMP) had processing equipment at El Laco in 2009. The latest mining activity carried out by CMP started in 1988 following the installation of a crusher and begun an extraction of 600,000 tons ore annually that lasted until to 1996.

Geographic entities mentioned:
surface_form: el laco
instance_of: Mountain
countries: Chile
coordinates: lat: -23.84155556
lon: -67.49016667
The geological interest in these kinds of mineral deposits is enhanced by their frequent association with other minerals, as has been noted at Olympic Dam, Australia. Other magnetite-apatite ore deposits in the Andes are Incahuasi (10.3±0.8 mya), southwest of El Laco next to the Argentina–Chile border, and Magnetita Pedernales (Tertiary), about south-southwest of Laco.

Geographic entities mentioned:
surface_form: el laco
instance_of: Mountain
countries: Chile
coordinates: lat: -23.84155556
lon: -67.49016667
surface_form: incahuasi
instance_of: Mountain
countries: Chile
coordinates: lat: -24.033333333333
lon: -67.55
Other magnetite-apatite ore deposits in the Andes are Incahuasi (10.3±0.8 mya), southwest of El Laco next to the Argentina–Chile border, and Magnetita Pedernales (Tertiary), about south-southwest of Laco. These have been held by some geologists to have a similar origin as those of the el El Laco. Comparable deposits.

Geographic entities mentioned:
surface_form: el laco
instance_of: Mountain
countries: Chile
coordinates: lat: -23.84155556
lon: -67.49016667
Comparable deposits. The Kiruna magnetites in Sweden resemble the El Laco ones in terms of manganese and vanadium content, and their titanium content is comparably low. The deposits at Kiruna and El Laco have been classified as &quot;Iron oxide-apatite&quot; ore deposits, and El Laco is the best preserved and youngest such deposit on Earth.

Geographic entities mentioned:
surface_form: el laco
instance_of: Mountain
countries: Chile
coordinates: lat: -23.84155556
lon: -67.49016667
surface_form: el laco
instance_of: Mountain
countries: Chile
coordinates: lat: -23.84155556
lon: -67.49016667
Comparable deposits. The Kiruna magnetites in Sweden resemble the El Laco ones in terms of manganese and vanadium content, and their titanium content is comparably low. The deposits at Kiruna and El Laco have been classified as &quot;Iron oxide-apatite&quot; ore deposits, and El Laco is the best preserved and youngest such deposit on Earth.

Geographic entities mentioned:
surface_form: el laco
instance_of: Mountain
countries: Chile
coordinates: lat: -23.84155556
lon: -67.49016667
Environment. The vegetation in the area is primarily low bushland. Short-tailed chinchillas can be found at El Laco, one of the few occurrences of this threatened species in Chile. El Laco has a classical cold mountain climate at the line between the dry Altiplano with summer precipitation and the hyper-arid Atacama Desert climate.

Geographic entities mentioned:
surface_form: el laco
instance_of: Mountain
countries: Chile
coordinates: lat: -23.84155556
lon: -67.49016667
surface_form: el laco
instance_of: Mountain
countries: Chile
coordinates: lat: -23.84155556
lon: -67.49016667
Gustav Adolf Land is to the south and Prins Oscars Land is to the east. The boundary of Gustav V Land passes through Rijpdalen and Flaumdalen to Winsnesbreen in the east, continues further southwest to Brånevatnet, and thence follows the river from Brånevatnet to the sea at Bodleybukta. The highest elevation is on the glacier Vestfonna, which covers large parts of the land.

Geographic entities mentioned:
surface_form: Rijpdalen
instance_of: Valley
countries: Norway
coordinates: lat: 79.919166666667
lon: 22.251944444444
2010 FINA World Open Water Swimming Championships – Women's 5K. The Women's 5K race at the 2010 FINA World Open Water Swimming Championships was swum on Tuesday, July 20, 2010, in Roberval, Quebec, Canada. The race began at 10:30 a.m., and was swum in the Lac Saint-Jean in the city centre. 35 women swam the event.

Geographic entities mentioned:
surface_form: Lac Saint-Jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
Modern era conflicts include the 1775 Battle of Bunker Hill (which was actually fought on Breed's Hill) in the American War of Independence; and Cemetery Hill and Culp's Hill in the 1863 Battle of Gettysburg, the turning point of the American Civil War.

Geographic entities mentioned:
surface_form: Breed's Hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.376361111111
lon: -71.060777777778
Howard Hills. The Howard Hills () are an area of low hills and meltwater lakes south of Beaver Glacier in the northeastern part of the Scott Mountains, Enderby Land, Antarctica. They were plotted from air photos taken from Australian National Antarctic Research Expeditions aircraft in 1956, and named by the Antarctic Names Committee of Australia after W.E.

Geographic entities mentioned:
surface_form: howard hills
instance_of: Landform
coordinates: lat: -67.1
lon: 51.15
Cedar Pond (Massachusetts). Cedar Pond is a small oval-shaped pond in the town of Lakeville, Massachusetts. It is located just off of Somserset Lane from Long Point Road, which is easily accessible from Route 105. The pond is primarily used for irrigating nearby bogs and farmland.

Geographic entities mentioned:
surface_form: cedar pond
instance_of: Lake
countries: United States
coordinates: lat: 44.5919
lon: -71.2694
surface_form: cedar pond
instance_of: Lake
countries: United States
coordinates: lat: 41.811
lon: -70.914
surface_form: cedar pond
instance_of: Body of water
countries: United States
coordinates: lat: 41.10833333
lon: -74.42638889
In the 1940s, James DeNormandie acquired much of the land around Mount Misery to prevent it from being developed and for his own agriculture uses. He dammed the brook and excavated soil to form the lower pond, as well as re-damming the original upper mill pond, and he built a cabin on the top of Mount Misery which later burned.

Geographic entities mentioned:
surface_form: mill pond
instance_of: Lake
countries: United States
coordinates: lat: 41.7708
lon: -70.6719
surface_form: lower pond
instance_of: Lake
countries: United States
coordinates: lat: 43.8087159
lon: -74.7014336
surface_form: mill pond
instance_of: Lake
countries: United States
coordinates: lat: 42.0181
lon: -70.7125
surface_form: mount misery
instance_of: Mountain
countries: United States
coordinates: lat: 42.420277777778
lon: -71.346111111111
surface_form: lower pond
instance_of: Lake
countries: United States
coordinates: lat: 43.8558525
lon: -74.5635555
History. Although it is unknown for certain, Mount Misery may take its name from the death of a pair of oxen or a sheep on the hill in colonial times. By 1667, the Billings family owned land around Beaver Dam Brook and eventually operated a saw mill on the brook, just below what is now the upper pond at the base of Mount Misery. Evidence of this mill remains today near the brook.

Geographic entities mentioned:
surface_form: upper pond
instance_of: Lake
countries: United States
coordinates: lat: 43.86656
lon: -74.5373405
surface_form: upper pond
instance_of: Lake
countries: United States
coordinates: lat: 43.8001149
lon: -74.7098059
surface_form: mount misery
instance_of: Mountain
countries: United States
coordinates: lat: 42.420277777778
lon: -71.346111111111
Mount Misery (Lincoln, Massachusetts). Mount Misery is a 284-foot hill and public conservation land in Lincoln, Massachusetts, on Route 117 (Great Road) and on the Bay Circuit Trail near the Sudbury River. Containing, Mount Misery is the largest piece of conservation land in the town and contains seven miles of public hiking trails through hills, wetlands and agricultural fields. History.

Geographic entities mentioned:
surface_form: mount misery (lincoln, massachusetts)
instance_of: Mountain
countries: United States
coordinates: lat: 42.420277777778
lon: -71.346111111111
Mount Misery (Lincoln, Massachusetts). Mount Misery is a 284-foot hill and public conservation land in Lincoln, Massachusetts, on Route 117 (Great Road) and on the Bay Circuit Trail near the Sudbury River. Containing, Mount Misery is the largest piece of conservation land in the town and contains seven miles of public hiking trails through hills, wetlands and agricultural fields. History.

Geographic entities mentioned:
surface_form: mount misery
instance_of: Mountain
countries: United States
coordinates: lat: 42.420277777778
lon: -71.346111111111
History. Although it is unknown for certain, Mount Misery may take its name from the death of a pair of oxen or a sheep on the hill in colonial times. By 1667, the Billings family owned land around Beaver Dam Brook and eventually operated a saw mill on the brook, just below what is now the upper pond at the base of Mount Misery. Evidence of this mill remains today near the brook.

Geographic entities mentioned:
surface_form: mount misery
instance_of: Mountain
countries: United States
coordinates: lat: 42.420277777778
lon: -71.346111111111
Evidence of this mill remains today near the brook. Concord writer Henry David Thoreau often hiked and recorded his experiences on the hill in his journal in the 1850s. In the 1940s, James DeNormandie acquired much of the land around Mount Misery to prevent it from being developed and for his own agriculture uses.

Geographic entities mentioned:
surface_form: mount misery
instance_of: Mountain
countries: United States
coordinates: lat: 42.420277777778
lon: -71.346111111111
He dammed the brook and excavated soil to form the lower pond, as well as re-damming the original upper mill pond, and he built a cabin on the top of Mount Misery which later burned. DeNormandie sold Mount Misery to the town as public conservation land in 1969.

Geographic entities mentioned:
surface_form: mount misery
instance_of: Mountain
countries: United States
coordinates: lat: 42.420277777778
lon: -71.346111111111
This led to the development of the Glasgow Corporation Water Works, with a project to raise the level of Loch Katrine and to convey clean water by gravity along a aqueduct to a holding reservoir at Milngavie, and then by pipes into the city. The project cost £980,000 and was opened by Queen Victoria in 1859. In the early 19th century an eighth of the people lived in single-room accommodation.

Geographic entities mentioned:
surface_form: Loch Katrine
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.254444444444445
lon: -4.515555555555555
Additional supplies were provided by Loch Arklet in 1902, by impounding the water and creating a tunnel to allow water to flow into Loch Katrine. A similar scheme to create a reservoir in Glen Finglas was authorised in 1903, but was deferred, and was not completed until 1965.

Geographic entities mentioned:
surface_form: Glen Finglas
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.23
lon: -4.362
Servicemen who died after the war or during their posting in northern Malaya prior to the Malayan Emergency are also interred here. The cemetery is located in Bukit Larut, Taiping, Perak, Malaysia and was erected and maintained by the Commonwealth War Graves Commission. There are more than 850 World War II casualties commemorated in this cemetery, including more than 500 who remain unidentified.

Geographic entities mentioned:
surface_form: Bukit Larut
instance_of: Mountain
countries: Malaysia
coordinates: lat: 4.86228
lon: 100.793
McGregor Pass forms the division between the Hart Ranges of the Rockies, which begin at Mount Sir Alexander just to the northwest and extend to the Peace Reach of Lake Williston, and the Continental Ranges, the largest and most well-known segment of the Canadian Rockies, which extend to Marias Pass, at the head of the North Fork Flathead River in Montana, United States.

Geographic entities mentioned:
surface_form: Mount Sir Alexander
instance_of: Mountain
countries: Canada
coordinates: lat: 53.9357
lon: -120.3877
The eponymous community of Sharbot Lake is located at the centre of the north shore of the lake. The primary outflow, at the northeast, is the Fall River, which flows via the Mississippi River and the Ottawa River to the Saint Lawrence River. Sharbot Lake Provincial Park is named for, and is partly on the northwest shore of, the lake, but mostly envelops the neighbouring Black Lake.

Geographic entities mentioned:
surface_form: black lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.636944444444445
lon: -83.03083333333333
surface_form: black lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.143055555555556
lon: -91.6
surface_form: black lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.03194
lon: -78.41667
surface_form: black lake
instance_of: Lake
countries: Canada
coordinates: lat: 59.2
lon: -105.25
surface_form: sharbot lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.7675
lon: -76.69333333333333
surface_form: black lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.60057
lon: -84.71219
surface_form: black lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.2778
lon: -82.8772
surface_form: black lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.816186
lon: -78.822783
surface_form: black lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.7764
lon: -76.7206
surface_form: black lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.5411
lon: -94.0797
Sharbot Lake (Ontario). Sharbot Lake is a lake in the municipality of Central Frontenac, Frontenac County in Eastern Ontario, Canada. It is part of the Saint Lawrence River drainage basin. The eponymous community of Sharbot Lake is located at the centre of the north shore of the lake.

Geographic entities mentioned:
surface_form: sharbot lake (ontario)
instance_of: Lake
countries: Canada
coordinates: lat: 44.7675
lon: -76.69333333333333
Sharbot Lake (Ontario). Sharbot Lake is a lake in the municipality of Central Frontenac, Frontenac County in Eastern Ontario, Canada. It is part of the Saint Lawrence River drainage basin. The eponymous community of Sharbot Lake is located at the centre of the north shore of the lake.

Geographic entities mentioned:
surface_form: sharbot lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.7675
lon: -76.69333333333333
It is part of the Saint Lawrence River drainage basin. The eponymous community of Sharbot Lake is located at the centre of the north shore of the lake. The primary outflow, at the northeast, is the Fall River, which flows via the Mississippi River and the Ottawa River to the Saint Lawrence River.

Geographic entities mentioned:
surface_form: sharbot lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.7675
lon: -76.69333333333333
Sharbot Lake Provincial Park is named for, and is partly on the northwest shore of, the lake, but mostly envelops the neighbouring Black Lake. Ontario Highway 7 runs roughly along the northwest side of the lake, and the former Ontario Highway 38, now County Road 38, crosses the lake at the location of the community of Sharbot Lake.

Geographic entities mentioned:
surface_form: sharbot lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.7675
lon: -76.69333333333333
The same crossing point is used by the multi-use K&P Rail Trail (part of the Trans Canada Trail), formerly the rail bed of the Kingston and Pembroke Railway. Sharbot Lake is named after a First Nations Chief named Francis Chabot, who was Mohawk and his wife Algonquin.

Geographic entities mentioned:
surface_form: sharbot lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.7675
lon: -76.69333333333333
Phil Crampton. Philip James Crampton, commonly known as Phil Crampton, is a British born mountaineer and expedition leader, and owner of the mountaineering company &quot;Altitude Junkies&quot;. Mountaineering. Crampton's climbing achievements include successful ascents of Everest (10 times), Cho Oyu (twice) and Manaslu (4 times). He has led more than 40 expeditions to 8,000m peaks.

Geographic entities mentioned:
surface_form: Cho Oyu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 28.094166666667
lon: 86.660833333333
surface_form: Manaslu
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.55
lon: 84.559722222222
Red Valley (South Dakota). Red Valley or Racetrack is a part of the Black Hills in South Dakota. Red Valley is a depression that rims the entire Black Hills.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: red valley
instance_of: Landform
countries: United States
coordinates: lat: 44.5525
lon: -103.385
surface_form: racetrack
instance_of: Landform
countries: United States
coordinates: lat: 44.5525
lon: -103.385
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
Red Valley (South Dakota). Red Valley or Racetrack is a part of the Black Hills in South Dakota. Red Valley is a depression that rims the entire Black Hills.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: red valley
instance_of: Landform
countries: United States
coordinates: lat: 44.5525
lon: -103.385
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
Red Valley (South Dakota). Red Valley or Racetrack is a part of the Black Hills in South Dakota. Red Valley is a depression that rims the entire Black Hills.

Geographic entities mentioned:
surface_form: red valley (south dakota)
instance_of: Landform
countries: United States
coordinates: lat: 44.5525
lon: -103.385
Otay River. The Otay River () is a river in southern San Diego County, California. The river begins at San Miguel Mountain, flows through the Upper and Lower Otay Reservoirs, and continues on between the southern part of the Chula Vista and the Otay Mesa West district of San Diego, to its river mouth on San Diego Bay. River. The river has a watershed.

Geographic entities mentioned:
surface_form: San Miguel Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.696405
lon: -116.936244
Oasis sits at an elevation of below sea level. The 2020 United States census reported Oasis's population was 4,468, down from 6,890 in 2010. Geography. One of several communities in the Coachella Valley, Oasis lies along the eastern foothills of the Santa Rosa Mountains. It also extends towards the south along the northwestern shores of the Salton Sea.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
The potential for using wireless time signals for determining longitude was soon apparent. Wireless telegraphy was used to extend and refine the telegraphic web of longitude, giving potentially greater accuracy, and reaching locations that were not connected to the wired telegraph network. An early determination was that between Potsdam and The Brocken in Germany, a distance of about, in 1906.

Geographic entities mentioned:
surface_form: The Brocken
instance_of: Mountain
countries: Germany
Kingdom of Prussia
coordinates: lat: 51.800555555556
lon: 10.617222222222
Svart Peak. Svart Peak () is a rock peak, high, lying a short distance inland from the coast on the southwest side of Law Promontory in Antarctica. It was mapped by Norwegian cartographers from aerial photographs taken by the Lars Christensen Expedition in January–February 1937, and named Svartfjell (Norwegian for black mountain} because of its black appearance.

Geographic entities mentioned:
surface_form: Law Promontory
instance_of: Landform
coordinates: lat: -67.22
lon: 58.8
surface_form: svart peak
instance_of: Mountain
coordinates: lat: -67.2667
lon: 58.4667
Svart Peak. Svart Peak () is a rock peak, high, lying a short distance inland from the coast on the southwest side of Law Promontory in Antarctica. It was mapped by Norwegian cartographers from aerial photographs taken by the Lars Christensen Expedition in January–February 1937, and named Svartfjell (Norwegian for black mountain} because of its black appearance.

Geographic entities mentioned:
surface_form: svart peak
instance_of: Mountain
coordinates: lat: -67.2667
lon: 58.4667
Svart Peak. Svart Peak () is a rock peak, high, lying a short distance inland from the coast on the southwest side of Law Promontory in Antarctica. It was mapped by Norwegian cartographers from aerial photographs taken by the Lars Christensen Expedition in January–February 1937, and named Svartfjell (Norwegian for black mountain} because of its black appearance.

Geographic entities mentioned:
surface_form: svartfjell
instance_of: Mountain
coordinates: lat: -67.2667
lon: 58.4667
South Bluff. South Bluff is a summit in the U.S. state of Wisconsin. The elevation is. South Bluff was so named on account of its location relative to nearby North Bluff.

Geographic entities mentioned:
surface_form: North Bluff
instance_of: Mountain
countries: United States
coordinates: lat: 44.321944444444
lon: -90.181944444444
Wipptal (district). Wipp Valley (;) is a district (,) in the northern part of the Italian province of South Tyrol. It comprises the South Tyrolean part of the larger geographically defined Wipptal, stretching from Brenner Pass in the north down the upper Eisack (Isarco) river to Franzensfeste in the south. It was separated from neighbouring Eisacktal district in 1980. Overview.

Geographic entities mentioned:
surface_form: Wipptal
instance_of: Valley
countries: Italy
Austria
coordinates: lat: 47
lon: 11.5
Wipptal (district). Wipp Valley (;) is a district (,) in the northern part of the Italian province of South Tyrol. It comprises the South Tyrolean part of the larger geographically defined Wipptal, stretching from Brenner Pass in the north down the upper Eisack (Isarco) river to Franzensfeste in the south. It was separated from neighbouring Eisacktal district in 1980. Overview.

Geographic entities mentioned:
surface_form: Eisacktal
instance_of: Valley
countries: Italy
coordinates: lat: 46.67
lon: 11.6
This gives the valley, what W. R. Mitchell calls, &quot;..an unusually neat appearance.&quot;
The larger part of the valley lies within the county of North Yorkshire but its highest reaches fall just within Cumbria. It is defined by the hills of Whernside to its east and Gragareth to its west.

Geographic entities mentioned:
surface_form: Whernside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.227777777778
lon: -2.4033333333333
surface_form: Gragareth
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2085
lon: -2.4814
surface_form: gragareth
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2085
lon: -2.4814
surface_form: whernside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.227777777778
lon: -2.4033333333333
The same thing happens to the River Skirfare in Littondale. Spells of wet weather often bring about a wall of water that travels down the valley across the dry riverbed. The single minor public road which serves the valley is an old packhorse route that connected Ingleton with Deepdale, then Dentdale, and which also forms the NCR 68 and the Yorkshire Dales Cycle Way.

Geographic entities mentioned:
surface_form: Deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.264
lon: -2.432
surface_form: Dentdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.278
lon: -2.454
surface_form: dentdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.278
lon: -2.454
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.264
lon: -2.432
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.54
lon: -1.99
Kingsdale. Kingsdale is a valley on the western edge of the Yorkshire Dales National Park in northern England. The name Kingsdale derives from a combination of Old Norse and Old English (&quot;Kyen&quot; and &quot;Dael&quot;) which means 'valley where the cows were kept'. Humans were active in Kingsdale from 6,700 BC onwards.

Geographic entities mentioned:
surface_form: kingsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.192
lon: -2.461
Kingsdale is a valley on the western edge of the Yorkshire Dales National Park in northern England. The name Kingsdale derives from a combination of Old Norse and Old English (&quot;Kyen&quot; and &quot;Dael&quot;) which means 'valley where the cows were kept'. Humans were active in Kingsdale from 6,700 BC onwards. Evidence of fire-pits used by hunter-gatherers have been found in the dale.

Geographic entities mentioned:
surface_form: kingsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.192
lon: -2.461
History. Kingsdale is a short narrow dale, that measures from Thornton-in-Lonsdale in the south, to High Moss in the north. During the Last Glacial Maximum, when many of the dales were affected by ice, a glacier carved out the valley of Kingsdale, and left behind a lake impounded at its southern end by a terminal moraine Raven Ray, a piece of land higher than the broad valley beyond it.

Geographic entities mentioned:
surface_form: kingsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.192
lon: -2.461
The presence of fire-pits in the dale dating back to the Mesolithic era (6850–6840 BC), provide evidence of humans using the dale, but only for hunting during the summer months, with the people expected to be from the lowlands. More permanent occupancy of the dale occurred during the Bronze Age, with sooty mounds found in Kingsdale dating back to 1500 BC.

Geographic entities mentioned:
surface_form: kingsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.192
lon: -2.461
It is defined by the hills of Whernside to its east and Gragareth to its west. Kingsdale is drained by the south-westward flowing Kingsdale Beck which assumes the name River Twiss before joining the River Doe at Ingleton to become the River Greta.

Geographic entities mentioned:
surface_form: kingsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.192
lon: -2.461
Kingsdale Beck is frequently dry on the surface between Kingsdale Head and Keld Head, with the water travelling underground before resurfacing at Keld Head. The same thing happens to the River Skirfare in Littondale. Spells of wet weather often bring about a wall of water that travels down the valley across the dry riverbed.

Geographic entities mentioned:
surface_form: kingsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.192
lon: -2.461