Sarmila/GeoWiki-Features huggingface dataset:
Personal life. Middlebrooks was awarded the Chancellor's Club Fellowship at University of California, Irvine. Death. On March 9, 2015, Middlebrooks was found unconscious at his home in the San Fernando Valley, pronounced dead on arrival at a Los Angeles hospital. An autopsy revealed that he suffered a fatal pulmonary embolism. One or more arteries in his lungs had become blocked by a blood clot.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Episode 51: Shiva appears and offers to teach Parshuram for ten years. Sahasrarjun turns on his allies and seizes their kingdoms. Parshuram renounces his caste and sets out for Mount Kailash, where Shiva accepts him as his pupil. Sahasrarjun meets Ravan, fights him, and takes him prisoner. Episode 52: Sahasrarjun imprisons Ravan after discovering that Ravan can't be killed.

Geographic entities mentioned:
surface_form: Mount Kailash
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
Collerson Lake. Collerson Lake is a small, kidney-shaped glacial lake southwest of Club Lake in the Vestfold Hills of Princess Elizabeth Land in Antarctica. A camp was established on the shores of this lake during geological investigations by K. Collerson, geologist at Davis Station in January 1970, for whom it was named by the Antarctic Names Committee of Australia.

Geographic entities mentioned:
surface_form: Club Lake
instance_of: Lake
coordinates: lat: -68.55
lon: 78.2333
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: elizabeth
instance_of: Mountain
coordinates: lat: -83.9
lon: 168.383
surface_form: collerson
instance_of: Lake
coordinates: lat: -68.5833
lon: 78.1833
Collerson Lake. Collerson Lake is a small, kidney-shaped glacial lake southwest of Club Lake in the Vestfold Hills of Princess Elizabeth Land in Antarctica. A camp was established on the shores of this lake during geological investigations by K. Collerson, geologist at Davis Station in January 1970, for whom it was named by the Antarctic Names Committee of Australia.

Geographic entities mentioned:
surface_form: collerson lake
instance_of: Lake
coordinates: lat: -68.5833
lon: 78.1833
Collerson Lake. Collerson Lake is a small, kidney-shaped glacial lake southwest of Club Lake in the Vestfold Hills of Princess Elizabeth Land in Antarctica. A camp was established on the shores of this lake during geological investigations by K. Collerson, geologist at Davis Station in January 1970, for whom it was named by the Antarctic Names Committee of Australia.

Geographic entities mentioned:
surface_form: collerson
instance_of: Lake
coordinates: lat: -68.5833
lon: 78.1833
surface_form: davis
instance_of: Mountain
coordinates: lat: -78.1
lon: -86.25
Sentinel Mesa. Sentinel Mesa is a summit in San Juan County, Utah, United States. It is situated north of the Monument Valley visitor center on Navajo Nation land and can be seen from Highway 163. The mesa is immediately northwest of the iconic West and East Mitten Buttes. The nearest higher neighbor is Brighams Tomb, to the north-northeast.

Geographic entities mentioned:
surface_form: West and East Mitten Buttes
instance_of: Mountain
countries: United States
coordinates: lat: 36.99
lon: -110.083
surface_form: mitten buttes
instance_of: Mountain
countries: United States
coordinates: lat: 36.99
lon: -110.083
The mesa is immediately northwest of the iconic West and East Mitten Buttes. The nearest higher neighbor is Brighams Tomb, to the north-northeast. Precipitation runoff from this mesa's west slope drains to Mitchell Butte Wash, whereas the east slope drains to West Gypsum Creek, which are both part of the San Juan River drainage basin.

Geographic entities mentioned:
surface_form: Brighams Tomb
instance_of: Mountain
countries: United States
coordinates: lat: 37.045833333333
lon: -110.08388888889
The mesa is immediately northwest of the iconic West and East Mitten Buttes. The nearest higher neighbor is Brighams Tomb, to the north-northeast. Precipitation runoff from this mesa's west slope drains to Mitchell Butte Wash, whereas the east slope drains to West Gypsum Creek, which are both part of the San Juan River drainage basin.

Geographic entities mentioned:
surface_form: mitchell butte
instance_of: Mountain
countries: United States
coordinates: lat: 36.976666666667
lon: -110.1525
Sentinel Mesa. Sentinel Mesa is a summit in San Juan County, Utah, United States. It is situated north of the Monument Valley visitor center on Navajo Nation land and can be seen from Highway 163. The mesa is immediately northwest of the iconic West and East Mitten Buttes. The nearest higher neighbor is Brighams Tomb, to the north-northeast.

Geographic entities mentioned:
surface_form: navajo
instance_of: Mountain
countries: United States
coordinates: lat: 37.034169444444
lon: -110.86888888889
Precipitation runoff from this mesa's west slope drains to Mitchell Butte Wash, whereas the east slope drains to West Gypsum Creek, which are both part of the San Juan River drainage basin. The &quot;Sentinel&quot; name refers to how the mesa oversees Monument Valley which the Navajo consider as one of the &quot;door posts&quot; to Monument Valley.

Geographic entities mentioned:
surface_form: navajo
instance_of: Mountain
countries: United States
coordinates: lat: 37.034169444444
lon: -110.86888888889
Sentinel Mesa. Sentinel Mesa is a summit in San Juan County, Utah, United States. It is situated north of the Monument Valley visitor center on Navajo Nation land and can be seen from Highway 163. The mesa is immediately northwest of the iconic West and East Mitten Buttes. The nearest higher neighbor is Brighams Tomb, to the north-northeast.

Geographic entities mentioned:
surface_form: sentinel mesa
instance_of: Mountain
countries: United States
coordinates: lat: 37.0122
lon: -110.1057
The buttes and mesas of Monument Valley are the result of the Organ Rock Shale being more easily eroded than the overlaying sandstone. Climate. Spring and fall are the most favorable seasons to visit Sentinel Mesa. According to the Köppen climate classification system, it is located in a semi-arid climate zone with cold winters and hot summers.

Geographic entities mentioned:
surface_form: sentinel mesa
instance_of: Mountain
countries: United States
coordinates: lat: 37.0122
lon: -110.1057
The bottom layer is Organ Rock Shale, the next stratum is De Chelly Sandstone, and the upper layer is Moenkopi Formation capped by Shinarump Conglomerate. The rock ranges in age from Permian at the bottom to Late Triassic at the top. The buttes and mesas of Monument Valley are the result of the Organ Rock Shale being more easily eroded than the overlaying sandstone. Climate.

Geographic entities mentioned:
surface_form: the organ
instance_of: Mountain
countries: United States
coordinates: lat: 37.2709548
lon: -112.9435175
Lake Grahovo. Lake Grahovo () is a lake in Nikšić municipality, near the town of Grahovo in southwestern Montenegro. It is an artificial lake which is an accumulation of the Grahovo River. Bottom of the lake is mostly dolomite-based. The lake itself is 700 meters long, 200 meters wide and 25 meters deep. The dam is 30 metres high, and three meters wide.

Geographic entities mentioned:
surface_form: lake grahovo
instance_of: Lake
countries: Montenegro
coordinates: lat: 42.67083333
lon: 18.63
surface_form: grahovo
instance_of: Lake
countries: Montenegro
coordinates: lat: 42.67083333
lon: 18.63
Lake Grahovo. Lake Grahovo () is a lake in Nikšić municipality, near the town of Grahovo in southwestern Montenegro. It is an artificial lake which is an accumulation of the Grahovo River. Bottom of the lake is mostly dolomite-based. The lake itself is 700 meters long, 200 meters wide and 25 meters deep. The dam is 30 metres high, and three meters wide.

Geographic entities mentioned:
surface_form: lake grahovo
instance_of: Lake
countries: Montenegro
coordinates: lat: 42.67083333
lon: 18.63
surface_form: grahovo
instance_of: Lake
countries: Montenegro
coordinates: lat: 42.67083333
lon: 18.63
surface_form: grahovo
instance_of: Lake
countries: Montenegro
coordinates: lat: 42.67083333
lon: 18.63
Lake Grahovo. Lake Grahovo () is a lake in Nikšić municipality, near the town of Grahovo in southwestern Montenegro. It is an artificial lake which is an accumulation of the Grahovo River. Bottom of the lake is mostly dolomite-based. The lake itself is 700 meters long, 200 meters wide and 25 meters deep. The dam is 30 metres high, and three meters wide.

Geographic entities mentioned:
surface_form: grahovo
instance_of: Lake
countries: Montenegro
coordinates: lat: 42.67083333
lon: 18.63
The lake itself is 700 meters long, 200 meters wide and 25 meters deep. The dam is 30 metres high, and three meters wide. The lake is a significant water reservoir used for the agricultural production of Grahovo, but is also used for sport and recreation. Construction of the dam was initiated in 1952, finished in 1962, while it has undergone a reconstruction in 1988.

Geographic entities mentioned:
surface_form: grahovo
instance_of: Lake
countries: Montenegro
coordinates: lat: 42.67083333
lon: 18.63
Biliaivka. Biliaivka (,) is a city in Odesa Raion, Odesa Oblast, Ukraine. It hosts the administration of Biliaivka urban hromada, one of the hromadas of Ukraine. The city is located in the Dniester Delta, on the left bank of the Turunchuk River. Lake Safiany is located near by the city. Population: 12.155 (2023 estimate). History.

Geographic entities mentioned:
surface_form: Lake Safiany
instance_of: Lake
countries: Ukraine
coordinates: lat: 46.473638888889
lon: 30.1895
The news presentation was no-frills and straight and remained so even as flashier news formats began to make their mark nationally in the 1970s and made 10/11's newscasts begin to appear dated, even stodgy. A 1982 story on Mains in the &quot;Lincoln Sunday Journal and Star&quot; noted that his &quot;facial expressions contain more granite than Mount Rushmore&quot;.

Geographic entities mentioned:
surface_form: Mount Rushmore
instance_of: Mountain
countries: United States
coordinates: lat: 43.878947222222
lon: -103.459825
California's 28th congressional district is a congressional district in the U.S. state of California, in Los Angeles County. The district is regarded as a Democratic stronghold and has been held by the Democratic Party since 2003 and is currently represented by. Following redistricting ahead of the 2022 election cycle, the 18th district was relocated to the San Gabriel Valley.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
Following redistricting ahead of the 2022 election cycle, the 18th district was relocated to the San Gabriel Valley. Formerly, from 2003 to 2013, the district included about half of the San Fernando Valley, including North Hollywood, in the Greater Los Angeles Area.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Langavatnet (Odda). Langavatnet is a lake in Ullensvang Municipality in Vestland county, Norway. The lake lies about straight east of the town of Odda. The lake has a dam at the north end to regulate the water level for the purposes of hydroelectric power generation.

Geographic entities mentioned:
surface_form: langavatnet (odda)
instance_of: Lake
countries: Norway
coordinates: lat: 60.06444444
lon: 6.75083333
Langavatnet (Odda). Langavatnet is a lake in Ullensvang Municipality in Vestland county, Norway. The lake lies about straight east of the town of Odda. The lake has a dam at the north end to regulate the water level for the purposes of hydroelectric power generation.

Geographic entities mentioned:
surface_form: langavatnet
instance_of: Lake
countries: Norway
coordinates: lat: 60.06444444
lon: 6.75083333
In 1906, Zhang Yintang, appointed as the assistant amban for Tibet, leveraged the provisions of the 1906 convention to reassert control over Tibet and diminish British influence. The British troops were withdrawn from the Chumbi Valley following the payment of the third installment from the Chinese government of the indemnity stipulated in the 1904 convention.

Geographic entities mentioned:
surface_form: Chumbi Valley
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 27.4893046
lon: 88.9050579
Jerichow. Jerichow () is a town on the east side of the river Elbe, in the District of Jerichower Land, of the state of Saxony-Anhalt in Germany. With about, the municipality of Jerichow is one of the largest municipalities in area size in Germany. Geography. The city of Jerichow lies on an old branch of the river Elbe between Stendal and Genthin, 31 miles (50 kilometers) northeast of Magdeburg.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Geography. The city of Jerichow lies on an old branch of the river Elbe between Stendal and Genthin, 31 miles (50 kilometers) northeast of Magdeburg. The territory of the municipality extends from the center of the city to the east along the northern boundary of the District of Jerichower Land to the state boundary of Brandenburg and from there a strip of land to the south. Divisions.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The summit is a popular ski destination, accessed from the east. The mountain is located on the eastern shore of the lake Eikesdalsvatnet, and it has a view towards the Mardalsfossen waterfall in the south and the mountain Skjorta in the north. The village of Eresfjord lies about to the northwest along the Eira River.

Geographic entities mentioned:
surface_form: Eikesdalsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 62.543055555556
lon: 8.1702777777778
surface_form: Skjorta
instance_of: Mountain
countries: Norway
coordinates: lat: 62.657777777778
lon: 8.2061111111111
Fløtatinden. Fløtatinden is a mountain in Molde Municipality in Møre og Romsdal county, Norway. The summit is a popular ski destination, accessed from the east. The mountain is located on the eastern shore of the lake Eikesdalsvatnet, and it has a view towards the Mardalsfossen waterfall in the south and the mountain Skjorta in the north.

Geographic entities mentioned:
surface_form: romsdal
instance_of: Valley
countries: Norway
coordinates: lat: 62.447222222222
lon: 7.8333333333333
surface_form: fløtatinden
instance_of: Mountain
countries: Norway
coordinates: lat: 62.608333333333
lon: 8.2141666666667
Fløtatinden. Fløtatinden is a mountain in Molde Municipality in Møre og Romsdal county, Norway. The summit is a popular ski destination, accessed from the east. The mountain is located on the eastern shore of the lake Eikesdalsvatnet, and it has a view towards the Mardalsfossen waterfall in the south and the mountain Skjorta in the north.

Geographic entities mentioned:
surface_form: fløtatinden
instance_of: Mountain
countries: Norway
coordinates: lat: 62.608333333333
lon: 8.2141666666667
The mountain is located on the eastern shore of the lake Eikesdalsvatnet, and it has a view towards the Mardalsfossen waterfall in the south and the mountain Skjorta in the north. The village of Eresfjord lies about to the northwest along the Eira River. One of the lower peaks to the north of the main peak is &quot;Trondskjortetinden&quot;.

Geographic entities mentioned:
surface_form: trondskjortetinden
instance_of: Mountain
countries: Norway
coordinates: lat: 62.608333333333
lon: 8.2141666666667
Like other volcanoes of the Central Volcanic Zone, Taapaca formed from the subduction of the Nazca Plate beneath the South America Plate. It lies on the western margin of the Altiplano high plateau, on top of older volcanic and sedimentary units. Taapaca has mainly erupted dacite, in the form of numerous lava domes, although an andesitic stratovolcano is also present.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Geography and geology. Taapaca lies in the Parinacota province of the Arica y Parinacota Region. Northern Chile has little documented volcanic activity during the last ten thousand years with the majority of eruptions documented at Guallatiri, Lascar and Parinacota. The first and the last of these three volcanoes as well as Taapaca itself are part of the Lauca National Park.

Geographic entities mentioned:
surface_form: Guallatiri
instance_of: Mountain
countries: Chile
coordinates: lat: -18.42361111111111
lon: -69.08972222222222
surface_form: guallatiri
instance_of: Mountain
countries: Chile
coordinates: lat: -18.42361111111111
lon: -69.08972222222222
This volcanic zone features the highest volcanoes in the world, which reach elevations of here. The largest historical eruption in the Central Volcanic Zone occurred at Huaynaputina in 1600 and Lascar is the most active volcano in the region; otherwise volcanic activity is poorly recorded as most edifices are remote from human habitation.

Geographic entities mentioned:
surface_form: Huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223
The largest historical eruption in the Central Volcanic Zone occurred at Huaynaputina in 1600 and Lascar is the most active volcano in the region; otherwise volcanic activity is poorly recorded as most edifices are remote from human habitation. Taapaca is located on the western margin of the Altiplano, where the Western Cordillera has developed since the Oligocene.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
In some places, a Proterozoic basement formed by amphibolites, gneisses and serpentinites crops out. The volcanoes of Condoriri, Pomerape, Larancagua and Parinacota lie to the east of Taapaca. The area of the volcano is subject to contractional tectonics, with a major thrust fault passing close by, but their relationship to Taapaca's volcanism is not clear. Volcano.

Geographic entities mentioned:
surface_form: Pomerape
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -18.126275
lon: -69.126719444444
The Quebrada Allane drains the northern flank westward into the Lluta River; parts of the mountain drain into the Rio Lauca watershed to the east. Southwest of Taapaca lies Putre, the main town of the northern Altiplano of Chile. Composition. Taapaca is mostly formed by potassium-rich dacite, although andesite was erupted early during its activity, and one occurrence of rhyolite is reported.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Taapaca. Taapaca is a Holocene volcanic complex in northern Chile's Arica y Parinacota Region. Located in the Chilean Andes, it is part of the Central Volcanic Zone of the Andean Volcanic Belt, one of four distinct volcanic chains in South America. The town of Putre lies at the southwestern foot of the volcano.

Geographic entities mentioned:
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
The town of Putre lies at the southwestern foot of the volcano. Like other volcanoes of the Central Volcanic Zone, Taapaca formed from the subduction of the Nazca Plate beneath the South America Plate. It lies on the western margin of the Altiplano high plateau, on top of older volcanic and sedimentary units.

Geographic entities mentioned:
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
It lies on the western margin of the Altiplano high plateau, on top of older volcanic and sedimentary units. Taapaca has mainly erupted dacite, in the form of numerous lava domes, although an andesitic stratovolcano is also present. Volcanic activity at Taapaca occurred in several stages starting during the Plio-Pleistocene.

Geographic entities mentioned:
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
Name. The term &quot;tara paka&quot; is Aymara for &quot;two-headed eagle&quot; or &quot;winter (prey) bird&quot;, and Quechua for Andean eagle. It is also known as Nevados de Putre; sometimes &quot;Nevados de Putre&quot; is used to refer to the volcanic complex and &quot;Taapaca&quot; to its highest summit.

Geographic entities mentioned:
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
Northern Chile has little documented volcanic activity during the last ten thousand years with the majority of eruptions documented at Guallatiri, Lascar and Parinacota. The first and the last of these three volcanoes as well as Taapaca itself are part of the Lauca National Park. Taapaca volcano can be reached from the Tambo Quemado-Arica international road. Regional setting.

Geographic entities mentioned:
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
In some places, a Proterozoic basement formed by amphibolites, gneisses and serpentinites crops out. The volcanoes of Condoriri, Pomerape, Larancagua and Parinacota lie to the east of Taapaca. The area of the volcano is subject to contractional tectonics, with a major thrust fault passing close by, but their relationship to Taapaca's volcanism is not clear. Volcano.

Geographic entities mentioned:
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
Volcano. Taapaca reaches a height of above sea level and is a volcanic complex elongated from west to east; Larancagua lies just east of Taapaca. It consists primarily of many overlapping lava domes, with shapes ranging from almost elliptical to circular. Lava flows are uncommon.

Geographic entities mentioned:
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
Moraines have been described as either poorly or well-developed with six separate stages, of which the lowest lies at elevation on the western slopes. Glacially eroded valleys have also been reported; in the past two glaciers descended Taapaca's western slopes while four glaciers developed between Taapaca and Larancagua, draining south.

Geographic entities mentioned:
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
Crustal assimilation at depths of more than was involved in the formation of the dacitic magma and contributes about 18% of the mass of the dacites. Taapaca is constructed on a fairly thick crust and rising magma, and thus undergoes substantial interaction with the crust, meaning that crustal contamination is important in the genesis of Taapaca's magmas.

Geographic entities mentioned:
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
Much of the area is protected by the Lauca National Park, which includes Taapaca. Eruptive activity. Taapaca was originally considered to have been active for the last 1.5 million years during three volcanic phases. Later a fourth stage was identified, and some rocks were interpreted as pre-dating 1.5 million years ago.

Geographic entities mentioned:
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
Eruptions at Taapaca have consisted of lava dome-forming eruptions and explosive activity with avalanches of blocks and ash, which form when lava domes collapse, as has been observed in historical time at the Soufriere Hills and Unzen volcanoes, although these events were much smaller than reconstructed episodes at Taapaca.

Geographic entities mentioned:
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
Only one subplinian eruption has occurred on Taapaca, and tephra fallout deposits are not widespread. Eruptive activity has moved south-southwestward over the history of Taapaca, with activity centred at the top of the edifice. Late Pleistocene to Holocene activity consisted of discrete episodes lasting about 10,000 years and separated by tens of thousands of years with no recognized activity.

Geographic entities mentioned:
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
Two alignments of domes date back to this time, one on the southern and the other on the eastern flank, both lined up north-south. The second and probably also the third stage were subject to glacial erosion, which together with later sector collapses resulted in the removal of much of Taapaca's edifice and the exposure of the core of the volcano.

Geographic entities mentioned:
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
At least three pyroclastic eruptions occurred within the last 8,000 years, while tephra falls took place between 7,000 and 2,000 years ago, possibly linked to the eruption of lava domes. The Global Volcanism Program lists eight separate eruptions of Taapaca during the Holocene, with the last eruption occurring 2,300 years ago around 320 BCE ± 50 years.

Geographic entities mentioned:
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
Threats and preparedness. Most of the volcanoes in northern Chile are far from towns and inhabited areas and thus their activity does not create significant human hazards, but Taapaca is an exception: Putre, the major local population centre, is constructed on pyroclastic deposits from Taapaca, facing a threat from future eruptions.

Geographic entities mentioned:
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
Eruptions between April and November (when the volcano is covered by snow) might generate lahars, as could rainfall during the wet season between December and March; the latter type of lahar happens frequently on present-day Taapaca owing to the steep slopes of the volcano, although it usually results solely in road damage.

Geographic entities mentioned:
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
The figurine was probably emplaced to obtain a supply of water, since the Inkans believed that mountains controlled weather and thus the fertility of animals and plants. Taapaca was an Inkan mountain sanctuary, and the mountain is still said to protect the community of Putre. Taapaca has deposits of sulfur in its summit area.

Geographic entities mentioned:
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
Taapaca was an Inkan mountain sanctuary, and the mountain is still said to protect the community of Putre. Taapaca has deposits of sulfur in its summit area. Starting in the 1930s the &quot;Empresa Azufrera Taapaca&quot; (&quot;Taapaca Sulfur Company&quot;) active in Putre mined this sulfur on Taapaca, and Taapaca's crater became the site of the Cánepa and Cía mining camp.

Geographic entities mentioned:
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
surface_form: taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
They are neighboured on the east by the Mackenzie Mountains and on their northwest end by the Brooks Range. To their southwest is the Yukon Plateau, while a lower southward extension of their mountain spine protrudes into British Columbia as the Liard Plateau.

Geographic entities mentioned:
surface_form: Yukon Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 62.25
lon: -137.25
surface_form: Liard Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 59.6667
lon: -125.5
But it was easy to see how the wreck had occurred. The bridge is 'blind' from both directions.&quot;
Geography. Thurmont is located at the eastern foothill of the Catoctin spur of the Blue Ridge Mountains. According to the United States Census Bureau, the town has a total area of, of which is land and is water. Climate.

Geographic entities mentioned:
surface_form: Catoctin
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
The archipelago consists of five major islands and their surrounding smaller islands. These main islands are, counterclockwise starting from northeast, Babuyan, Calayan, Dalupiri, Fuga, and Camiguin. The Babuyan Islands are separated from Luzon by the Babuyan Channel, and from the province of Batanes to the north by the Balintang Channel. Geography.

Geographic entities mentioned:
surface_form: Camiguin
instance_of: Mountain
countries: Philippines
coordinates: lat: 18.833611111111
lon: 121.86111111111
Geology. The eastern islands of the archipelago are part of the Luzon Volcanic Arc. Three volcanoes from two of the islands have erupted in historical times - Camiguin de Babuyanes on Camiguin Island, Babuyan Claro Volcano and Smith Volcano (also known as Mount Babuyan) on Babuyan Island.

Geographic entities mentioned:
surface_form: Camiguin de Babuyanes
instance_of: Mountain
countries: Philippines
coordinates: lat: 18.833611111111
lon: 121.86111111111
surface_form: Babuyan Claro Volcano
instance_of: Mountain
countries: Philippines
coordinates: lat: 19.523333333333
lon: 121.94
surface_form: Smith Volcano
instance_of: Mountain
countries: Philippines
coordinates: lat: 19.536622222222
lon: 121.91284444444
After the loss of Xuzhou, approximately 1.1 million men or 120 divisions of the National Revolutionary Army were redeployed. The commission decided to organize the defense around the Dabie Mountains, Poyang Lake, and the Yangtze River against the 200,000 Japanese in 20 divisions of the Imperial Japanese Army.

Geographic entities mentioned:
surface_form: Poyang Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.066666666667
lon: 116.38333333333
The capture Anqing's airbase enabled Japanese aircraft to assault Jiujiang, a major riverine port and railroad junction one hundred miles upstream. On the southern bank of the Yangtze River, the Chinese Ninth War Zone had one regiment stationed west of Poyang Lake and another stationed in Jiujiang.

Geographic entities mentioned:
surface_form: Poyang Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.066666666667
lon: 116.38333333333
During the break-out, there were not enough boats to evacuate the auxiliary soldiers of the defending 26th division from Hukou, and only more than 1,800 out of the more than 3,100 non-combat soldiers were taken in by the division. Most of the more than 1,300 missing soldiers drowned trying to cross the Poyang Lake. The Japanese reached Jiujiang two weeks after the fall of Hukou.

Geographic entities mentioned:
surface_form: Poyang Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.066666666667
lon: 116.38333333333
The defending Chinese 4th Army, 8th Army Group, and 29th Army Group relied on the advantageous terrain of Lushan and north of Nanxun Railway to resist. As a result, the Japanese offensive suffered a setback. On 20 August, the Japanese 101st Division crossed Poyang Lake from Hukou County to reinforce the 106th Division, which breached the Chinese 25th Army's defensive line and captured Xinzhi.

Geographic entities mentioned:
surface_form: Poyang Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.066666666667
lon: 116.38333333333
These myths have complicated conservation initiatives for Indian caecilians. &quot;Crotaphatrema lamottei&quot;, a rare species native to Mount Oku in Cameroon, is classified as a Kefa-ntie (burrowing creature) by the Oku. Kefa-ntie, a term also encompassing native moles and blind snakes, are considered poisonous, causing painful sores if encountered, contacted, or killed.

Geographic entities mentioned:
surface_form: Mount Oku
instance_of: Mountain
countries: Cameroon
coordinates: lat: 6.1997222222222
lon: 10.518888888889
The Palatine Watershed runs over its summit. The Hortenkopf is the second southernmost of a row of four peaks that reach a height of over 600 metres. To the south is the Weißenberg (610 m) near the hamlet of Hermersbergerhof in the municipality of Wilgartswiesen. To the north are the Mosisberg and the Eschkopf (jeweils 609 m).

Geographic entities mentioned:
surface_form: Mosisberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.3011
lon: 7.85556
surface_form: Eschkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.3103
lon: 7.85361
Hortenkopf. The Hortenkopf is a hill, 606 metres above sea level (NN), in the German state of Rhineland-Palatinate, which lies in the middle of the Palatine Forest between Hofstätten and Leimen. The Hortenkopf is recognisable from a long way off thanks to the transmission tower that has been erected on its summit. Geography and access.

Geographic entities mentioned:
surface_form: hortenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.2704
lon: 7.8274
Geography and access. The hill is part of the Frankenweide, a centrally located massif within this range of low mountains. The Palatine Watershed runs over its summit. The Hortenkopf is the second southernmost of a row of four peaks that reach a height of over 600 metres. To the south is the Weißenberg (610 m) near the hamlet of Hermersbergerhof in the municipality of Wilgartswiesen.

Geographic entities mentioned:
surface_form: hortenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.2704
lon: 7.8274
To the north are the Mosisberg and the Eschkopf (jeweils 609 m). From the Hortenkopf it is possible to walk to Leimen, Kaiserslautern-Mölschbach, Elmstein and via the forest lodges of Taubensuhl and Heldenstein almost as far as Neustadt on continuous hill ridges without dropping below the 450 metre contour line. At the Hortenkopf the main watershed turns southwest towards Gräfenstein Castle.

Geographic entities mentioned:
surface_form: hortenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.2704
lon: 7.8274
At the Hortenkopf the main watershed turns southwest towards Gräfenstein Castle. On the southwestern flank of the Hortenkopf rises the northern headstream of the Wieslauter, which - subsequently as the &quot;Lauter&quot; – flows directly into the River Rhine. Further northwest rises a tributary of the Merzalbe, whose waters flow via the Rodalb, Schwarzbach, Blies, Saar and Moselle into the Rhine.

Geographic entities mentioned:
surface_form: hortenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.2704
lon: 7.8274
A witness said that, on August 27 between 1 p.m. and 2 p.m. she saw Laundrie and Petito together at the Merry Piglets Tex-Mex restaurant in Jackson Hole, Wyoming. Per the witness, Laundrie was &quot;aggressive&quot; and had an argument (apparently regarding money) with the manager, waitress, and hostess.

Geographic entities mentioned:
surface_form: Jackson Hole
instance_of: Valley
countries: United States
coordinates: lat: 43.516666666667
lon: -110.83333333333
Sturgeon River (Prince Edward Island). The Sturgeon River is a river in the Atlantic Ocean drainage basin in Kings County in eastern Prince Edward Island, Canada. Course. The Sturgeon River begins in a field about southeast of the settlement of Brooklyn. It flows north, then turns east, passes over a dam, and flows past the community of Milltown Cross and Buffaloland Provincial Park.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: sturgeon river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.1167
lon: -62.5333
surface_form: sturgeon river
instance_of: Watercourse
countries: Canada
coordinates: lat: 53.2
lon: -105.867
Sturgeon River (Prince Edward Island). The Sturgeon River is a river in the Atlantic Ocean drainage basin in Kings County in eastern Prince Edward Island, Canada. Course. The Sturgeon River begins in a field about southeast of the settlement of Brooklyn. It flows north, then turns east, passes over a dam, and flows past the community of Milltown Cross and Buffaloland Provincial Park.

Geographic entities mentioned:
surface_form: sturgeon river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.1167
lon: -62.5333
surface_form: sturgeon river
instance_of: Watercourse
countries: Canada
coordinates: lat: 53.2
lon: -105.867
It flows north, then turns east, passes over a dam, and flows past the community of Milltown Cross and Buffaloland Provincial Park. The river takes in the left tributary West Branch Sturgeon River, turns southeast, takes in the right tributary South Branch Sturgeon River, and reaches its mouth at Sturgeon Bay northwest of the community of Sturgeon. Sturgeon Bay is part of the larger St.

Geographic entities mentioned:
surface_form: sturgeon river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.1167
lon: -62.5333
surface_form: sturgeon river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.1167
lon: -62.5333
surface_form: sturgeon river
instance_of: Watercourse
countries: Canada
coordinates: lat: 53.2
lon: -105.867
surface_form: sturgeon river
instance_of: Watercourse
countries: Canada
coordinates: lat: 53.2
lon: -105.867
Anticona. Anticona (possibly from Quechua for metals or minerals, the inhabitants of the rainforest or the Andes), also called &quot;Ticlio&quot;, is a mountain in the Andes of Peru, about high. It is located in the Lima Region, Huarochiri Province, Chicla District, and in the Junín Region, Yauli Province, Morococha District.

Geographic entities mentioned:
surface_form: junín
instance_of: Lake
countries: Peru
coordinates: lat: -11.0201
lon: -76.1075
surface_form: yauli
instance_of: Mountain
countries: Peru
coordinates: lat: -11.4992
lon: -76.1297
Anticona. Anticona (possibly from Quechua for metals or minerals, the inhabitants of the rainforest or the Andes), also called &quot;Ticlio&quot;, is a mountain in the Andes of Peru, about high. It is located in the Lima Region, Huarochiri Province, Chicla District, and in the Junín Region, Yauli Province, Morococha District.

Geographic entities mentioned:
surface_form: anticona
instance_of: Mountain
countries: Peru
coordinates: lat: -11.58472222
lon: -76.18055556
It is located in the Lima Region, Huarochiri Province, Chicla District, and in the Junín Region, Yauli Province, Morococha District. Anticona lies between the Ticlio mountain pass in the southwest and Yanashinga in the northeast, northwest of a lake named Huacracocha.

Geographic entities mentioned:
surface_form: yanashinga
instance_of: Mountain
countries: Peru
coordinates: lat: -11.5744
lon: -76.1719
surface_form: huacracocha
instance_of: Lake
countries: Peru
coordinates: lat: -11.593888888889
lon: -76.161388888889
Forced to face his past to continue with his future, Joe runs into an old enemy of his, Snake. Worried about him, Snake invites Joe to rejoin him in his illegal drug operation. Production. The film was shot in the Eureka Springs, Arkansas area of the Ozark Mountains. Release. The film had its world premiere at the 2004 Sundance Film Festival, where it competed in the U.S. Dramatic section.

Geographic entities mentioned:
surface_form: Ozark Mountains
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
It has a political line of the alternative left, workers' self-management and confederalism. It annually organises the acts of Montejurra. The Carlist Party holds a federal structure with the possibility of it forming sovereign Carlist parties in the associate nationalities in the Carlist Party. The youths of the different Carlist parties and Carlist groups group together in the Carlist Youths.

Geographic entities mentioned:
surface_form: Montejurra
instance_of: Mountain
countries: Spain
coordinates: lat: 42.631111111111
lon: -2.0447222222222
Ishinca. Nevado Ishinca, meaning &quot;snow covered mountain&quot;, is a mountain peak located in the Cordillera Blanca mountain range in the Peruvian Andes. It is located in the Ishinca Valley region and has a summit elevation of 5,530 meters. Ishinca is most often climbed via its normal route, the North-West Route rated Alpine PD-. Ishinca's North-West Route was first ascended by J. Fonrouge, W.

Geographic entities mentioned:
surface_form: ishinca
instance_of: Mountain
countries: Peru
coordinates: lat: -9.39268
lon: -77.4059
Ishinca. Nevado Ishinca, meaning &quot;snow covered mountain&quot;, is a mountain peak located in the Cordillera Blanca mountain range in the Peruvian Andes. It is located in the Ishinca Valley region and has a summit elevation of 5,530 meters. Ishinca is most often climbed via its normal route, the North-West Route rated Alpine PD-. Ishinca's North-West Route was first ascended by J. Fonrouge, W.

Geographic entities mentioned:
surface_form: ishinca
instance_of: Mountain
countries: Peru
coordinates: lat: -9.39268
lon: -77.4059
surface_form: nevado ishinca
instance_of: Mountain
countries: Peru
coordinates: lat: -9.39268
lon: -77.4059
Ishinca. Nevado Ishinca, meaning &quot;snow covered mountain&quot;, is a mountain peak located in the Cordillera Blanca mountain range in the Peruvian Andes. It is located in the Ishinca Valley region and has a summit elevation of 5,530 meters. Ishinca is most often climbed via its normal route, the North-West Route rated Alpine PD-. Ishinca's North-West Route was first ascended by J. Fonrouge, W.

Geographic entities mentioned:
surface_form: ishinca
instance_of: Mountain
countries: Peru
coordinates: lat: -9.39268
lon: -77.4059
surface_form: ishinca
instance_of: Mountain
countries: Peru
coordinates: lat: -9.39268
lon: -77.4059
It is located in the Ishinca Valley region and has a summit elevation of 5,530 meters. Ishinca is most often climbed via its normal route, the North-West Route rated Alpine PD-. Ishinca's North-West Route was first ascended by J. Fonrouge, W. Lindaver, H. Salger, H. Schmidbauer and V. Staudacher in 1964. At Anqash Runa Simi: ichinqa → ishinqa → ishinca (it will stand).

Geographic entities mentioned:
surface_form: ishinca
instance_of: Mountain
countries: Peru
coordinates: lat: -9.39268
lon: -77.4059
Kushan emperor Kujula Kadphises defeated the Indo-Parthians and incorporated the region under the Kushan Empire. In the Tochi Valley of North Waziristan near Bannu, Bactrian language inscriptions originally written in the 9th century have been discovered. This shows that after the collapse of the Kushan Empire, its official language continued in use for at least six more centuries.

Geographic entities mentioned:
surface_form: Tochi Valley
instance_of: Valley
countries: Pakistan
Its name was later changed to Edwardesabad in 1869. In 1903, it received its current name, Bannu. Bannu was used as the base of operations for all punitive expeditions undertaken by detachments of the British Indian Army to the Tochi Valley and the Waziristan frontier. A military road led from the town of Bannu toward Dera Ismail Khan.

Geographic entities mentioned:
surface_form: Tochi Valley
instance_of: Valley
countries: Pakistan
Dingevatn. Dingevatn or Dingevatnet is the 18th deepest lake in Norway, reaching a maximum depth of. It is located in the municipality of Gulen in Vestland county. The lake is located just east of the village of Dingja, about southeast of the mouth of the Sognefjorden. The lake lies about north of the municipal center of Eivindvik.

Geographic entities mentioned:
surface_form: dingevatn
instance_of: Lake
countries: Norway
coordinates: lat: 61.041666666667
lon: 5.0847222222222
Dingevatn. Dingevatn or Dingevatnet is the 18th deepest lake in Norway, reaching a maximum depth of. It is located in the municipality of Gulen in Vestland county. The lake is located just east of the village of Dingja, about southeast of the mouth of the Sognefjorden. The lake lies about north of the municipal center of Eivindvik.

Geographic entities mentioned:
surface_form: dingevatn
instance_of: Lake
countries: Norway
coordinates: lat: 61.041666666667
lon: 5.0847222222222
surface_form: dingevatnet
instance_of: Lake
countries: Norway
coordinates: lat: 61.041666666667
lon: 5.0847222222222
From 1894 to 1895, he was the head librarian at Beit Ariela. He was a co-founder of the Rehavia Gymnasium in Jerusalem, Israel's first modern high school. Death. During World War I, he relocated to Switzerland, where he died in 1918. Seven years later, his remains were interred on the Mount of Olives.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
Part III – Russia. Ève left Teheran on January 6, 1942, flying via Baku to Kuybyshev (now Samara), where the embassies and many Soviet central offices had been evacuated to from Moscow because of the threatening German offensive at the end of 1941. Already on board the plane she could observe the frozen Caspian Sea; biting frost and snow were to accompany her during her whole stay in the USSR.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Ridge of Capard. Ridge of Capard () is a mountain in County Laois, Ireland. Ridge of Capard's summit is at an altitude of, making it the third-highest point in Laois, the sixth-highest in the Slieve Bloom Mountains and the 615th-highest summit in Ireland.

Geographic entities mentioned:
surface_form: ridge of capard
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.09105833
lon: -7.48884444
The northeastern part of the Altiplano is more humid than the southwestern part, which has several salares (salt flats), due to its aridity. At the Bolivia–Peru border lies Lake Titicaca, the largest lake in South America. Farther south, in Bolivia, there was until recently a lake, Lake Poopó, but by December 2015 it had completely dried up, and was declared defunct.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
At the Bolivia–Peru border lies Lake Titicaca, the largest lake in South America. Farther south, in Bolivia, there was until recently a lake, Lake Poopó, but by December 2015 it had completely dried up, and was declared defunct. It is unclear whether that lake, which had been the second-largest in Bolivia, can be restored.

Geographic entities mentioned:
surface_form: Lake Poopó
instance_of: Lake
countries: Bolivia
coordinates: lat: -18.781944444444
lon: -67.024722222222
The area also attracts some international tourism. Geography. The Altiplano is an area of inland drainage (endorheism) lying in the central Andes, occupying parts of northern Chile, western Bolivia, southern Peru and northwest Argentina. Its height averages about 3,750 meters (12,300 feet), slightly less than that of the Tibetan Plateau.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88