Sarmila/GeoWiki-Features huggingface dataset:
Mount Popomanaseu. Mount Popomanaseu is a volcanic mountain and the highest mountain in the Solomon Islands. It is located on Guadalcanal east of Mount Makarakomburu. At, it is the highest peak in the insular South Pacific, excluding New Guinea and its satellite islands. Panning east across the South Pacific, there is no higher mountain until reaching the Andes in South America.

Geographic entities mentioned:
surface_form: Mount Makarakomburu
instance_of: Mountain
countries: Solomon Islands
coordinates: lat: -9.7333333333333
lon: 160.03333333333
Mount Popomanaseu. Mount Popomanaseu is a volcanic mountain and the highest mountain in the Solomon Islands. It is located on Guadalcanal east of Mount Makarakomburu. At, it is the highest peak in the insular South Pacific, excluding New Guinea and its satellite islands. Panning east across the South Pacific, there is no higher mountain until reaching the Andes in South America.

Geographic entities mentioned:
surface_form: popomanaseu
instance_of: Mountain
countries: Solomon Islands
coordinates: lat: -9.7036111111111
lon: 160.06194444444
surface_form: mount popomanaseu
instance_of: Mountain
countries: Solomon Islands
coordinates: lat: -9.7036111111111
lon: 160.06194444444
Lake Lungern. Lake Lungern (, also spelled &quot;Lungernsee&quot; or &quot;Lungerensee&quot;) is a natural lake in Obwalden, Switzerland which is named after the town Lungern on its shore. The lake is drained by the Sarner Aa river, which flows through the Sarnersee and into Lake Lucerne. The lake was originally much larger, and covered a large part of the valley it is situated in.

Geographic entities mentioned:
surface_form: Lake Lucerne
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.0194
lon: 8.4011
surface_form: lake lucerne
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.0194
lon: 8.4011
surface_form: sarner aa
instance_of: Watercourse
countries: Switzerland
coordinates: lat: 46.783611111111
lon: 8.0980555555556
surface_form: sarnersee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.8625
lon: 8.20861111111111
Lake Lungern. Lake Lungern (, also spelled &quot;Lungernsee&quot; or &quot;Lungerensee&quot;) is a natural lake in Obwalden, Switzerland which is named after the town Lungern on its shore. The lake is drained by the Sarner Aa river, which flows through the Sarnersee and into Lake Lucerne. The lake was originally much larger, and covered a large part of the valley it is situated in.

Geographic entities mentioned:
surface_form: lungernsee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.8025
lon: 8.1633333333333
surface_form: lungerensee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.8025
lon: 8.1633333333333
surface_form: lungern
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.8025
lon: 8.1633333333333
surface_form: lungern
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.8025
lon: 8.1633333333333
surface_form: lake lungern
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.8025
lon: 8.1633333333333
Lake Lungern. Lake Lungern (, also spelled &quot;Lungernsee&quot; or &quot;Lungerensee&quot;) is a natural lake in Obwalden, Switzerland which is named after the town Lungern on its shore. The lake is drained by the Sarner Aa river, which flows through the Sarnersee and into Lake Lucerne. The lake was originally much larger, and covered a large part of the valley it is situated in.

Geographic entities mentioned:
surface_form: lungern
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.8025
lon: 8.1633333333333
surface_form: lake lungern
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.8025
lon: 8.1633333333333
The feature is named after the settlement of Kyulevcha in Northeastern Bulgaria. Location. Kyulevcha Nunatak is located at, which is 5.9 km west-southwest of Moider Peak, 10.65 km west-northwest of Mount Lagado, and 37 km east of Mount Dewey on Graham Coast. British mapping in 1976.

Geographic entities mentioned:
surface_form: Moider Peak
instance_of: Mountain
coordinates: lat: -65.9167
lon: -63.15
surface_form: Mount Lagado
instance_of: Mountain
coordinates: lat: -66
lon: -63.25
surface_form: Mount Dewey
instance_of: Mountain
coordinates: lat: -65.9
lon: -64.3167
Early life. Hawes was the grandson of William Hawes M.D., and the brother of Benjamin Hawes; his parents were Benjamin Hawes (1770–1861), in business as a soap-boiler and a philanthropist, and Ann Feltham, sister of John Feltham. In 1827 he climbed Mont Blanc with Charles Fellows (address given as 26 Russell Square).

Geographic entities mentioned:
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
In 1928 large-scale anti-Catholic voting swept a state substantially part of the Ozark “Bible Belt”, so that whereas Kansas had been less anti-Democratic than more northerly Plains states in 1920 and 1924, it became Herbert Hoover’s best state in the entire nation at the next election cycle.

Geographic entities mentioned:
surface_form: Ozark
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
A number of rare minerals are fumarole minerals, and at least 240 such minerals are known from Tolbachik volcano in Kamchatka, Russia. Other volcanoes where particular fumarole minerals have been discovered are Vulcano in Italy and Bezymyanny also in Russia. Origin and appearance.

Geographic entities mentioned:
surface_form: Vulcano
instance_of: Mountain
countries: Italy
coordinates: lat: 38.4042
lon: 14.9658
Common components are sulfur compounds and elemental sulfur. In the Valley of Ten Thousand Smokes in Alaska the fumarole minerals form both thin crusts in the vents, mixtures with tephra deposits and coloured outcrops and mounds at the sites of former fumaroles. Deposits at Tolbachik volcano have shapes likef crusts, small plates and globules.

Geographic entities mentioned:
surface_form: Valley of Ten Thousand Smokes
instance_of: Valley
countries: United States
coordinates: lat: 58.393888888889
lon: -155.38527777778
Fumarolic minerals are often unstable and are eroded or decompose, in the Valley of Ten Thousand Smokes in Alaska it took less than a century for almost all fumarole mineral deposits to disappear although others remained and were later used to identify former fumarole vents. Thus, many fumarole minerals are rare and many rare minerals are fumarole minerals.

Geographic entities mentioned:
surface_form: Valley of Ten Thousand Smokes
instance_of: Valley
countries: United States
coordinates: lat: 58.393888888889
lon: -155.38527777778
Volcanoes. Research on the mineralogy of fumarole minerals has been conducted in Central America, Russia and Europe, with detailed publications on Izalco in El Salvador, Eldfell in Iceland, Vesuvius where research goes back to the early 19th century and Vulcano in Italy, Mount Usu in Japan, Kudryavy and Tolbachik in Russia, Kilauea and Mount St. Helens in the United States.

Geographic entities mentioned:
surface_form: Eldfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 63.4333008635
lon: -20.2487692886
surface_form: Vulcano
instance_of: Mountain
countries: Italy
coordinates: lat: 38.4042
lon: 14.9658
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
Helens in the United States. Sulfur deposits containing fumarolic desublimates are found at Guallatiri and Lastarria volcanoes in the Central Volcanic Zone of the Andes. Kudryavy volcano in the Kurils is particularly known for the numerous mineralizations its fumaroles have produced and for the presence of rhenium-rich precipitates. Among the elements found there are copper-gold-silver alloys.

Geographic entities mentioned:
surface_form: Guallatiri
instance_of: Mountain
countries: Chile
coordinates: lat: -18.42361111111111
lon: -69.08972222222222
surface_form: Lastarria
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -25.166666666667
lon: -68.5
Historical lava flows of Vesuvius volcano contain fumarolic minerals. Various fumarole minerals have been discovered at Vulcano volcano in Italy, where the mineralogy has changed since 1987 and 1990 due to hotter fumarole exhalations, yielding increased sulfate and sulfur salt concentrations. Fumarolic minerals have also been encountered in multiple mud volcanoes in Siberia.

Geographic entities mentioned:
surface_form: Vulcano
instance_of: Mountain
countries: Italy
coordinates: lat: 38.4042
lon: 14.9658
It is currently the largest natural lake in Costa Rica at. Its depth varies between 6 and 18 meters. Location. Located in Cote district, Guatuso canton, of Alajuela province, between the Arenal Volcano and Tenorio Volcano. Nearby is located the largest lake in Costa Rica, Lake Arenal, of artificial origin. Physical aspects.

Geographic entities mentioned:
surface_form: Arenal Volcano
instance_of: Mountain
countries: Costa Rica
coordinates: lat: 10.463333333333
lon: -84.703333333333
The word may be based on the prefix &quot;sibi-&quot;, meaning &quot;east&quot; or &quot;si-vints&quot;, meaning &quot;people who live in the east.&quot; It is also spelled &quot;Shivwitz&quot;, &quot;Shi'-vwits&quot;, &quot;She-bits&quot;, &quot;Sübü'ts&quot;, and &quot;Sebit&quot;. The Shivwits Plateau in Arizona is named after the tribe.

Geographic entities mentioned:
surface_form: Shivwits Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36.1085951
lon: -113.5413273
(Other major celebrations include the pine nut harvest at the spring fish spawn.) In the winter they told stories of the Wolf and the Coyote, and recounted the history of their people. It is likely that the Shivwits Plateau was also once a source of ceramic pottery that contributed to a thriving ceramic trade system that linked regions around southern Nevada and northwestern Arizona.

Geographic entities mentioned:
surface_form: Shivwits Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36.1085951
lon: -113.5413273
Ślęża. The Ślęża (; or &quot;Zobtenberg&quot;, later also &quot;Siling&quot;) is a high mountain in the Sudeten Foreland in Poland. The mountain is built mostly of granite and is covered with forests.

Geographic entities mentioned:
surface_form: ślęża
instance_of: Mountain
countries: Poland
coordinates: lat: 50.865016944444
lon: 16.708816944444
Ślęża. The Ślęża (; or &quot;Zobtenberg&quot;, later also &quot;Siling&quot;) is a high mountain in the Sudeten Foreland in Poland. The mountain is built mostly of granite and is covered with forests.

Geographic entities mentioned:
surface_form: ślęża
instance_of: Mountain
countries: Poland
coordinates: lat: 50.865016944444
lon: 16.708816944444
surface_form: siling
instance_of: Mountain
countries: Poland
coordinates: lat: 50.865016944444
lon: 16.708816944444
surface_form: zobtenberg
instance_of: Mountain
countries: Poland
coordinates: lat: 50.865016944444
lon: 16.708816944444
The top of the mountain has a PTTK tourist mountain hut, a television and radio mast, the Church of the Visitation of the Blessed Virgin Mary, some poorly-visible ruins of the castle and an observation tower. The area of the peak is protected as the Góra Ślęża nature reserve. The wide area around the mountain forms the Ślęża Landscape Park protected area. Location.

Geographic entities mentioned:
surface_form: ślęża
instance_of: Mountain
countries: Poland
coordinates: lat: 50.865016944444
lon: 16.708816944444
The top of the mountain has a PTTK tourist mountain hut, a television and radio mast, the Church of the Visitation of the Blessed Virgin Mary, some poorly-visible ruins of the castle and an observation tower. The area of the peak is protected as the Góra Ślęża nature reserve. The wide area around the mountain forms the Ślęża Landscape Park protected area. Location.

Geographic entities mentioned:
surface_form: ślęża
instance_of: Mountain
countries: Poland
coordinates: lat: 50.865016944444
lon: 16.708816944444
surface_form: ślęża
instance_of: Mountain
countries: Poland
coordinates: lat: 50.865016944444
lon: 16.708816944444
Location. Ślęża is located in the territory of Sobótka in Lower Silesian Voivodeship in southern Poland, about southeast of Wrocław. Geomorphologically it is situated in the Ślęża Massif mesoregion of the Sudeten Foreland macroregion. Sacred mountain. During the Neolithic Period and at least as far back as the 7th century BC Mount Ślęża was a holy place of the tribes of the Lusatian culture.

Geographic entities mentioned:
surface_form: ślęża
instance_of: Mountain
countries: Poland
coordinates: lat: 50.865016944444
lon: 16.708816944444
Geomorphologically it is situated in the Ślęża Massif mesoregion of the Sudeten Foreland macroregion. Sacred mountain. During the Neolithic Period and at least as far back as the 7th century BC Mount Ślęża was a holy place of the tribes of the Lusatian culture. It was then settled by Slavs.

Geographic entities mentioned:
surface_form: ślęża
instance_of: Mountain
countries: Poland
coordinates: lat: 50.865016944444
lon: 16.708816944444
surface_form: mount ślęża
instance_of: Mountain
countries: Poland
coordinates: lat: 50.865016944444
lon: 16.708816944444
The name of the territory Silesia either derives from the Ślęza River, or from Mount Ślęża, which themselves derive their name from either, according to Germanist authors the Silingi people. or, according to Slavisist authors, the Ślężanie people. The Slavic Ślężanie tribe settled in the area around the 6th century AD. In the 10th century, Mieszko I incorporated Silesia into the Polish state.

Geographic entities mentioned:
surface_form: ślęża
instance_of: Mountain
countries: Poland
coordinates: lat: 50.865016944444
lon: 16.708816944444
surface_form: mount ślęża
instance_of: Mountain
countries: Poland
coordinates: lat: 50.865016944444
lon: 16.708816944444
The area of the peak is protected as the Góra Ślęża nature reserve. The wide area around the mountain forms the Ślęża Landscape Park protected area. Location. Ślęża is located in the territory of Sobótka in Lower Silesian Voivodeship in southern Poland, about southeast of Wrocław. Geomorphologically it is situated in the Ślęża Massif mesoregion of the Sudeten Foreland macroregion. Sacred mountain.

Geographic entities mentioned:
surface_form: sobótka
instance_of: Mountain
countries: Poland
coordinates: lat: 50.865016944444
lon: 16.708816944444
This peace broke down almost immediately when Five Nations warriors raided north and westward into Wendat territory in the fall of 1646. It is probable that the Five Nations did that not only for the superior pelts, but also because they had almost rendered the beaver extinct in their home territory south of Lake Ontario.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Brant's claim is supported by Mississauga oral tradition which states that the land north of eastern Lake Erie, all of Lake Ontario, and the western north shore of the St. Lawrence River has been Mississauga territory since time immemorial and they agreed to share it in the Dish With One Spoon treaty.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The official opening of Highway 155 from Green Lake to Buffalo Narrows was held in August 1963 in Green Lake. The old trail to La Loche was rebuilt soon after to become part of Highway 155. A bridge built in 1981 now crosses the Kisis Channel next to where the ferry was once located. The Kisis Channel connects Churchill Lake to Peter Pond Lake. In the 1980s, the highway was straightened and paved.

Geographic entities mentioned:
surface_form: Peter Pond Lake
instance_of: Lake
countries: Canada
coordinates: lat: 56.00918
lon: -108.86918
Tschingelsee. Tschingelsee is a lake in the valley Kiental of the canton of Bern, Switzerland. The lake formed on Tschingelalp in 1972 after severe weather. Since 1987 the area has been a nature preserve.

Geographic entities mentioned:
surface_form: tschingelsee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.55168
lon: 7.74279
Description. Mount Hanover is a peak situated in Cypress Provincial Park, north of Vancouver, in the Britannia Range of the North Shore Mountains, which are subsets of the Coast Mountains. Hanover is the second-highest peak of the North Shore Mountains, after Brunswick Mountain. Precipitation runoff from Mount Hanover drains east to the Capilano River, and west to Howe Sound via Deeks Creek.

Geographic entities mentioned:
surface_form: Brunswick Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.4878
lon: -123.201
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Hanover. Mount Hanover is a mountain summit located in British Columbia, Canada. Description. Mount Hanover is a peak situated in Cypress Provincial Park, north of Vancouver, in the Britannia Range of the North Shore Mountains, which are subsets of the Coast Mountains. Hanover is the second-highest peak of the North Shore Mountains, after Brunswick Mountain.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount hanover
instance_of: Mountain
countries: Canada
coordinates: lat: 49.499167
lon: -123.183889
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Hanover. Mount Hanover is a mountain summit located in British Columbia, Canada. Description. Mount Hanover is a peak situated in Cypress Provincial Park, north of Vancouver, in the Britannia Range of the North Shore Mountains, which are subsets of the Coast Mountains. Hanover is the second-highest peak of the North Shore Mountains, after Brunswick Mountain.

Geographic entities mentioned:
surface_form: mount hanover
instance_of: Mountain
countries: Canada
coordinates: lat: 49.499167
lon: -123.183889
Hanover is the second-highest peak of the North Shore Mountains, after Brunswick Mountain. Precipitation runoff from Mount Hanover drains east to the Capilano River, and west to Howe Sound via Deeks Creek. Mount Hanover is more notable for its steep rise above local terrain than for its absolute elevation. Topographic relief is significant as the summit rises above Howe Sound in. History.

Geographic entities mentioned:
surface_form: mount hanover
instance_of: Mountain
countries: Canada
coordinates: lat: 49.499167
lon: -123.183889
Climate. Based on the Köppen climate classification, Mount Hanover is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: mount hanover
instance_of: Mountain
countries: Canada
coordinates: lat: 49.499167
lon: -123.183889
History. The first ascent of the summit was made May 23, 1913, by Don Munday, Ben Hanafin and Edward LaPage. The mountain's toponym was officially adopted December 7, 1937, by the Geographical Names Board of Canada. The peaks in the Britannia Range (Mts. Brunswick, Hanover, Windsor) are named for British royalty, in this case the House of Hanover. Climate.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Between 1495 - 1497, he handled negotiations with the Republic of Siena, aimed at obtaining military support, at a stage where the Republic of Florence had to deal with the rebellion of Pisa (self-proclaiming as an independent republic (1494)) and of Montepulciano (1494), and with the campaign by Bartolomeo d'Alviano on behalf of the Republic of Venice, which targeted Casentino (1496–1497).

Geographic entities mentioned:
surface_form: Casentino
instance_of: Valley
countries: Italy
coordinates: lat: 43.7
lon: 11.816666666667
During January–June 2003, Simitis, as Greek Prime Minister, exercised the presidency of the European Council. Controversy and criticism. In 1996, the appointment of the PASOK-leaning &quot;To Vima&quot; newspaper editor, Stavros Psycharis, as political administrator of Mount Athos was particularly criticized by the opposition. Siemens bribery scandal.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Following this thought the blockfields would then have been reworked by periglacial action. Most known blockfields are located in the northern hemisphere. Examples can be found in Abisko National Park in Sweden, Snowdonia National Park in Wales, the Great End-Scafell Pike ridge in England, and Hickory Run Boulder Field and River of Rocks in the Appalachian Mountains of the United States.

Geographic entities mentioned:
surface_form: Great End
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.464
lon: -3.194
surface_form: Scafell Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: River of Rocks
instance_of: Mountain
countries: United States
coordinates: lat: 40.645555555556
lon: -75.98
Chungará Lake. Chungará is a lake situated in the extreme north of Chile at an elevation of, in the Altiplano of Arica y Parinacota Region in the Lauca National Park. It has a surface area of about and has a maximum depth of about.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
surface_form: chungará
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
It has a surface area of about and has a maximum depth of about. It receives inflow through the Río Chungara with some minor additional inflows, and loses most of its water to evaporation; seepage into the Laguna Quta Qutani plays a minor role. The lake formed between 8,000 and 17,000 years ago when the volcano Parinacota collapsed and the debris from the collapse dammed the Lauca River.

Geographic entities mentioned:
surface_form: Laguna Quta Qutani
instance_of: Lake
countries: Chile
coordinates: lat: -18.1879
lon: -69.2218
surface_form: chungara
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
surface_form: quta qutani
instance_of: Lake
countries: Chile
coordinates: lat: -18.1879
lon: -69.2218
The lake formed between 8,000 and 17,000 years ago when the volcano Parinacota collapsed and the debris from the collapse dammed the Lauca River. Since then the lake has progressively grown owing to decreasing seepage. The lake is part of the Lauca National Park; a planned diversion of the lake's waters into the Azapa Valley being abandoned after a decision by the Chilean Supreme Court. Name.

Geographic entities mentioned:
surface_form: Azapa Valley
instance_of: Valley
countries: Chile
coordinates: lat: -18.51722222
lon: -70.19194444
Geography. Chungará Lake is located in the northernmost part of Chile and close to the border with Bolivia. It lies at an elevation of in the Chilean Altiplano; it is one of the highest lakes in the world and the second highest-largest after Lake Titicaca in the Altiplano.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
The lake floor features platforms, flat areas and sloping areas. northwest from Chungará Lake lies the Lagunas Cotacotani. The volcanoes Parinacota () of Pliocene to Holocene age and Ajoya () of Miocene age lie north and west of the lake, respectively; the northern shore of the lake is formed by lava flows from Parinacota volcano.

Geographic entities mentioned:
surface_form: Lagunas Cotacotani
instance_of: Lake
countries: Chile
coordinates: lat: -18.1879
lon: -69.2218
The volcanoes Parinacota () of Pliocene to Holocene age and Ajoya () of Miocene age lie north and west of the lake, respectively; the northern shore of the lake is formed by lava flows from Parinacota volcano. While Parinacota is well preserved, Ajoya and Quisiquisini () on the eastern shore of the lake are moderately eroded. Farther south from Chungará Lake lies the high Guallatiri. Hydrology.

Geographic entities mentioned:
surface_form: Quisiquisini
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.233333333333
lon: -69.066666666667
The volcanoes Parinacota () of Pliocene to Holocene age and Ajoya () of Miocene age lie north and west of the lake, respectively; the northern shore of the lake is formed by lava flows from Parinacota volcano. While Parinacota is well preserved, Ajoya and Quisiquisini () on the eastern shore of the lake are moderately eroded. Farther south from Chungará Lake lies the high Guallatiri. Hydrology.

Geographic entities mentioned:
surface_form: Guallatiri
instance_of: Mountain
countries: Chile
coordinates: lat: -18.42361111111111
lon: -69.08972222222222
Since about 5,000 calibrated radiocarbon years ago lake levels have been high. The Lake Chungará is part of a large high-elevation watershed in the Altiplano, bordered on the west by the Lauca River watershed and on the east by the Bolivian frontier; the watershed is surrounded by snow-covered volcanoes.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
The largest tributary of the lake is the Río Chungara with a discharge of about which originates on Guallatiri volcano and drains the area of the Nevados de Quimsachata (Acotango, Capurata and Umurata); this river contributes about 4/5 of the water to the lake and enters Chungará Lake on its southeastern corner through a river delta.

Geographic entities mentioned:
surface_form: Acotango
instance_of: Mountain
countries: Bolivia
Chile
coordinates: lat: -18.383333333333
lon: -69.046944444444
surface_form: Capurata
instance_of: Mountain
countries: Bolivia
Chile
coordinates: lat: -18.415
lon: -69.0458
surface_form: Umurata
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -18.355555555556
lon: -69.049722222222
surface_form: guallatiri
instance_of: Mountain
countries: Chile
coordinates: lat: -18.42361111111111
lon: -69.08972222222222
surface_form: chungará
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
There are no inflows on the eastern side of Chungará Lake. Chungará Lake has no outlet; its waters evaporate at a rate of about and also seep into the groundwater table at a rate of. The water chemistry of the Cotacotani Lakes imply that they receive water from Chungará Lake at a rate of about; this constitutes over half of the inflow to the Cotacotani Lakes.

Geographic entities mentioned:
surface_form: Cotacotani Lake
instance_of: Lake
countries: Chile
coordinates: lat: -18.1879
lon: -69.2218
surface_form: chungará
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
surface_form: cotacotani
instance_of: Lake
countries: Chile
coordinates: lat: -18.1879
lon: -69.2218
A number of volcanoes such as Parinacota, Ajoya and Quisiquisini grew on a Miocene ignimbrite basement that crops out east of the lake; of these only Parinacota and an unknown volcano that erupted in AD 400-720 have been active in the Holocene, depositing tephra within the lake. Climate. Temperatures at the lake average, fluctuating between at day and at night.

Geographic entities mentioned:
surface_form: Quisiquisini
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.233333333333
lon: -69.066666666667
Environmental issues. In the 1970s water was pumped from Chungará Lake to the Azapa Valley to allow for irrigation, but quickly ceased when water levels dropped and the flora and fauna of the lake were damaged. For this purpose, the Canal Chungará was built by the Chilean Ministry of Public Works to transfer water into the Laguna Cotacotani which is the headwater of the Lauca-Azapa system.

Geographic entities mentioned:
surface_form: Azapa Valley
instance_of: Valley
countries: Chile
coordinates: lat: -18.51722222
lon: -70.19194444
surface_form: chungará
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
Environmental issues. In the 1970s water was pumped from Chungará Lake to the Azapa Valley to allow for irrigation, but quickly ceased when water levels dropped and the flora and fauna of the lake were damaged. For this purpose, the Canal Chungará was built by the Chilean Ministry of Public Works to transfer water into the Laguna Cotacotani which is the headwater of the Lauca-Azapa system.

Geographic entities mentioned:
surface_form: Laguna Cotacotani
instance_of: Lake
countries: Chile
coordinates: lat: -18.1879
lon: -69.2218
surface_form: azapa
instance_of: Valley
countries: Chile
coordinates: lat: -18.51722222
lon: -70.19194444
surface_form: cotacotani
instance_of: Lake
countries: Chile
coordinates: lat: -18.1879
lon: -69.2218
&quot;Orestias chungarensis&quot; of Chungará Lake is most closely related to other &quot;Orestias&quot; species in the Lauca National Park but also those found in Salar de Ascotan and Salar de Carcote. This reflects that these waterbodies and the Lauca River were once joined by the former Lake Tauca.

Geographic entities mentioned:
surface_form: Lake Tauca
instance_of: Lake
countries: Peru
coordinates: lat: -20
lon: -68
Chungará Lake. Chungará is a lake situated in the extreme north of Chile at an elevation of, in the Altiplano of Arica y Parinacota Region in the Lauca National Park. It has a surface area of about and has a maximum depth of about.

Geographic entities mentioned:
surface_form: chungará lake
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
Name. The name &quot;Chungará&quot; or &quot;Chungara&quot; is derived from the Aymara language and has several different meanings:, a type of bush or moss plus the suffix that signifies &quot;covered by&quot;; but this meaning appears to have fallen into disuse.

Geographic entities mentioned:
surface_form: chungará
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
surface_form: chungara
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
The lake is part of the Lauca National Park, a nationally and internationally designated protected area, and a CONAF refuge lies close to the western shores of the lake. There is also a marina and a pumping plant in the northwestern area of Chungará Lake. Chile Route 11 passes by the southern and western shores of Chungará Lake.

Geographic entities mentioned:
surface_form: chungará lake
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
There is also a marina and a pumping plant in the northwestern area of Chungará Lake. Chile Route 11 passes by the southern and western shores of Chungará Lake. The lake is about wide and covers an irregular surface of about -, with two large embayments in the northeastern and the southern sectors of the lake and a narrower one in its northwestern corner.

Geographic entities mentioned:
surface_form: chungará lake
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
In addition, springs supply water into the lake from its western and northern shores where volcanoes border the lake. There are no inflows on the eastern side of Chungará Lake. Chungará Lake has no outlet; its waters evaporate at a rate of about and also seep into the groundwater table at a rate of.

Geographic entities mentioned:
surface_form: chungará lake
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
This lake chemistry is homogeneous throughout the lake and the lake waters are subject to strong currents at the surface. Geology. The lake was formed by volcanic-tectonic phenomena; specifically, a major collapse of the Parinacota volcano dammed a former Rio Lauca, forming Chungará Lake, at some time between 8,000 and 15,000 - 17,000 years ago.

Geographic entities mentioned:
surface_form: chungará lake
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
This collapse involved about and covered about with debris; before the collapse took place the lake floor of Chungará Lake consisted of alluvial and river sediments left by the Rio Lauca which drained the area. Upon damming, water from the river accumulated and formed Chungará Lake. The exact time of the collapse is controversial.

Geographic entities mentioned:
surface_form: chungará lake
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
Faulting also played a minor role in the formation of the lake basin, with a southwest-northeast trending fault disrupting sediments in the northwestern sector of the lake. Since the birth of Chungará Lake, about of sediment have accumulated on its floor. Volcanism in the area has been ongoing since the Paleozoic and has continued until recent times, which has influenced Chungará Lake.

Geographic entities mentioned:
surface_form: chungará lake
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
Temperatures at the lake average, fluctuating between at day and at night. The climate of Chungará Lake is arid and annual precipitation on Chungará Lake amounts to about, considerably smaller than the evaporation rate. This precipitation occurs during summer when moisture is transported into the region from the Amazon and the Atlantic Ocean; this is known as the &quot;Bolivian Winter&quot;.

Geographic entities mentioned:
surface_form: chungará lake
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
On 19 December 1985 the lake was the subject of a major legal case when the Chilean Supreme Court ruled that international obligations such as the CITES need to be considered by the Chilean government and prohibited the use of the waters of Chungará Lake; the ruling by disallowing the use of the waters of Chungará Lake forced the Arica y Parinacota Region to seek other sources of water for the growing economy.

Geographic entities mentioned:
surface_form: chungará lake
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
surface_form: chungará lake
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
surface_form: chungará lake
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
Copepods such as calanoids and cladocera make up the zooplankton, which is abundant in Lake Chungará. Microbial colonies occur on the shores of Chungará Lake. Fish. The most important and only native fish in Chungará Lake are two endemics; the pupfish &quot;Orestias chungarensis&quot; and catfish &quot;Trichomycterus chungaraensis&quot;.

Geographic entities mentioned:
surface_form: chungará lake
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
Fish. The most important and only native fish in Chungará Lake are two endemics; the pupfish &quot;Orestias chungarensis&quot; and catfish &quot;Trichomycterus chungaraensis&quot;. &quot;Orestias chungarensis&quot; of Chungará Lake is most closely related to other &quot;Orestias&quot; species in the Lauca National Park but also those found in Salar de Ascotan and Salar de Carcote.

Geographic entities mentioned:
surface_form: chungará lake
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
Its deepest point is - deep and lies in the northwestern sector of the lake. The northern and western side of the lake have steep shores, while the southern and eastern ones are much more gentle; the eastern shore is covered by a large alluvial fan and the southern one by sediments deposited by the Río Chungara tributary. The lake floor features platforms, flat areas and sloping areas.

Geographic entities mentioned:
surface_form: chungara
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
Accumulation of rubbish in the area of Chungará Lake has become a major issue, as a lot of waste is discarded by for example drivers on the Chungara–Tambo Quemado road between Chile and Bolivia. The Chilean government has thus organized cleanup operations to remove some of the waste. Biology. The lake hosts a diverse plant and animal community.

Geographic entities mentioned:
surface_form: chungara
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
It prefers elevations of less than. &quot;Hoffmannseggia glauca&quot; is found outside California in Western Nevada, Texas, Mexico, and South America. In California, &quot;H. glauca&quot; may be found in the San Joaquin Valley, the Southern Coastal Ranges, and the Western Transverse Ranges. Description. &quot;Hoffmannseggia glauca&quot; is an erect perennial herb that can measure up to 30 cm tall.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
The middle one, origination from the east side of the Badagong Mountain in Sangzhi and the south place, origination from Longjiazhai of Yongshun County in Xiangxi. The three originations join the main river in Nancha of Sangzhi, then runs east. Loushui River is a tributary of Lishui River. It flows into the Dongting Lake at Xiaodukou in Jinshi. Its total length is.

Geographic entities mentioned:
surface_form: Dongting Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.316666666667
lon: 112.95
Gravenche. The gravenche (&quot;Coregonus hiemalis&quot;), also known as the Lake Geneva whitefish or the little fera, is a presumably extinct freshwater fish from Lake Geneva in Switzerland and France. Description. The gravenche was a species of freshwater whitefish (Coregoninae) that reached a length between. The status of the gravenche is disputed because there are no specimens in museums.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
The gravenche was a species of freshwater whitefish (Coregoninae) that reached a length between. The status of the gravenche is disputed because there are no specimens in museums. While Emile Dottrens described it as subspecies of the common whitefish &quot;Coregonus lavaretus&quot; in 1958, other experts like Maurice Kottelat regarded it as a full species endemic to Lake Geneva. Biology.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Spawning occurred in mid-December. Extinction. Together with the likewise extinct true fera (&quot;Coregonus fera&quot;), the gravenche was one of the most important species for fisheries in Lake Geneva in the late 19th century. In 1890 these two fishes made up 68% of all fish caught in the lake.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
However, the lighthouse constructed by the British at Kalingapatana port stands as a witness to the European regime. Tourism. Kalingapatnam Beach is the place where river Vamsadhara empties into Bay of Bengal. Buddhist stupas were excavated by the Archaeological department at Salihundam, Ramateertham etc.

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 number of unemployed rose, which was detrimental to donations. On January 26, strike pay had to be reduced by 3 marks. The suspension of shipping on the upper Elbe meant that skilled workers could be mobilised for work in the port of Hamburg. The long duration of the strike noticeably improved the performance of the strike breakers, who had now settled into their jobs.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Geography. Godda, the eponymous CD block headquarters, is located at. Godda district is a plateau region with undulating uplands, long ridges and depressions. The western portion of the Rajmahal hills passes through the district. The plain areas have lost its once rich forests but the hills still retain some. Kajhia, Sunder and Sakri rivers flow through the district.

Geographic entities mentioned:
surface_form: Rajmahal hills
instance_of: Mountain
countries: India
coordinates: lat: 25
lon: 87
Sponsorship. Since 2005 Mirabaud is the main sponsor of the Bol d’Or Mirabaud – the longest fresh water sailboat regatta in Europe that is held annually on Lake Geneva. In 2019, to celebrate its 200th anniversary the bank made the Geneva Museum of Modern Arts free to all visitors.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
A volcanic dam impounds the lake waters. A pocket of magma lies beneath the lake and leaks carbon dioxide () into the water, changing it into carbonic acid. Nyos is one of only three lakes known to be saturated with carbon dioxide in this way, and therefore prone to limnic eruptions (the others being Lake Monoun, also in Cameroon, and Lake Kivu in the Democratic Republic of Congo and Rwanda).

Geographic entities mentioned:
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
surface_form: nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
Villages along the road in the vicinity of the lake include Cha, Nyos, Munji, Djingbe, and Subum. The lake is from the Nigerian border to the north, and lies on the northern slopes of the Massif du Mbam, drained by streams running north, then northwest, to the Katsina-Ala River in Nigeria which is part of the Benue River basin.

Geographic entities mentioned:
surface_form: Benue River
instance_of: Watercourse
countries: Cameroon
Nigeria
coordinates: lat: 7.783333
lon: 6.766667
The rift is known as the Mbéré Rift Valley, and crustal extension has allowed magma to reach the surface along a line extending through Cameroon. Mount Cameroon also lies on this fault line. Lake Nyos is surrounded by old lava flows and pyroclastic deposits. Although Nyos is situated within an extinct volcano, magma still exists beneath it.

Geographic entities mentioned:
surface_form: Mount Cameroon
instance_of: Mountain
countries: Cameroon
coordinates: lat: 4.2166666666667
lon: 9.1725
The lake waters are held in place by a natural dam composed of volcanic rock. At its narrowest point, the wall measures high and wide. Gas saturation. Lake Nyos is one of only three lakes in the world known to be saturated with carbon dioxide—the others are Lake Monoun, also in Cameroon, and Lake Kivu on the border between the Democratic Republic of the Congo and Rwanda.

Geographic entities mentioned:
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
surface_form: nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
surface_form: lake nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
Following the disaster, scientists investigated other African lakes to see if a similar phenomenon could happen elsewhere. Lake Kivu, 2,000 times larger than Lake Nyos, was also found to be supersaturated, and geologists found evidence for outgassing events around the lake about every thousand years.

Geographic entities mentioned:
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
surface_form: nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
surface_form: lake nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
Lake Nyos. Lake Nyos () is a crater lake in the Northwest Region of Cameroon, located about northwest of Yaoundé, the capital. Nyos is a deep lake high on the flank of an inactive volcano in the Oku volcanic plain along the Cameroon line of volcanic activity. A volcanic dam impounds the lake waters.

Geographic entities mentioned:
surface_form: nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
surface_form: lake nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
Lake Nyos. Lake Nyos () is a crater lake in the Northwest Region of Cameroon, located about northwest of Yaoundé, the capital. Nyos is a deep lake high on the flank of an inactive volcano in the Oku volcanic plain along the Cameroon line of volcanic activity. A volcanic dam impounds the lake waters.

Geographic entities mentioned:
surface_form: nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
In 1986, possibly as the result of a landslide, Lake Nyos suddenly emitted a large cloud of, which suffocated 1,746 people and 3,500 livestock in nearby towns and villages, the most notable one being Chah, which was abandoned after the incident.

Geographic entities mentioned:
surface_form: nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
surface_form: lake nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
Geography. Lake Nyos lies within the Oku Volcanic Field, located near the northern boundary of the Cameroon Volcanic Line, a zone of volcanoes and other tectonic activity that extends southwest to the Mt. Cameroon stratovolcano. The field consists of volcanic maars and basaltic scoria cones. Formation and geologic history.

Geographic entities mentioned:
surface_form: nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
surface_form: lake nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
Cameroon stratovolcano. The field consists of volcanic maars and basaltic scoria cones. Formation and geologic history. Lake Nyos is located south of the dirt road from Wum, about to the west, to Nkambé in the east. Villages along the road in the vicinity of the lake include Cha, Nyos, Munji, Djingbe, and Subum.

Geographic entities mentioned:
surface_form: nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
surface_form: lake nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
Cameroon stratovolcano. The field consists of volcanic maars and basaltic scoria cones. Formation and geologic history. Lake Nyos is located south of the dirt road from Wum, about to the west, to Nkambé in the east. Villages along the road in the vicinity of the lake include Cha, Nyos, Munji, Djingbe, and Subum.

Geographic entities mentioned:
surface_form: nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
The lake is from the Nigerian border to the north, and lies on the northern slopes of the Massif du Mbam, drained by streams running north, then northwest, to the Katsina-Ala River in Nigeria which is part of the Benue River basin. Lake Nyos fills a roughly circular maar in the Oku Volcanic Field, an explosion crater caused when a lava flow interacted violently with groundwater.

Geographic entities mentioned:
surface_form: nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
surface_form: lake nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889