Sarmila/GeoWiki-Features huggingface dataset:
The side vents erupted to form fissure vents, producing basalt and andesite, while the parasitic vents erupted scoria. Broken Top's volcanic crater, now in diameter, was most likely created through subsidence, which created a depression that was filled with thick basaltic andesite lava flows topped by thin lavas.

Geographic entities mentioned:
surface_form: broken top
instance_of: Mountain
countries: United States
coordinates: lat: 44.082894444444
lon: -121.69976111111
The summit cone has also undergone extensive glacial erosion, with embayments and a major cirque on its southern side. It forms an amphitheatre shape that opens to the southeast. Due to this extensive erosion, the contents of Broken Top's cone are exposed, which allows volcanologists to classify Broken Top as a complex stratovolcano.

Geographic entities mentioned:
surface_form: broken top
instance_of: Mountain
countries: United States
coordinates: lat: 44.082894444444
lon: -121.69976111111
surface_form: broken top
instance_of: Mountain
countries: United States
coordinates: lat: 44.082894444444
lon: -121.69976111111
Glaciation and flash floods. During the late Pleistocene, Broken Top and its surroundings were almost entirely covered by glaciers. The only features in the area not buried by glaciers were the summit of Tumalo Mountain and the summit of Broken Top, including the northwest ridge crest. No geologic evidence suggests that any eruptive activity took place subglacially.

Geographic entities mentioned:
surface_form: broken top
instance_of: Mountain
countries: United States
coordinates: lat: 44.082894444444
lon: -121.69976111111
When Little Ice Age glaciers retreated during the 20th century, water filled in the spaces left behind, forming moraine-dammed lakes, which are more common in the Three Sisters Wilderness than anywhere else in the contiguous United States. The local area has a history of flash floods, including at Broken Top itself, where a flash flood took place on October 7, 1966.

Geographic entities mentioned:
surface_form: broken top
instance_of: Mountain
countries: United States
coordinates: lat: 44.082894444444
lon: -121.69976111111
The local area has a history of flash floods, including at Broken Top itself, where a flash flood took place on October 7, 1966. Analysis of the event by forest ranger David Rasmussen determined that it had originated from a lake on Broken Top, located at an elevation of with an area of. This lake sits at the foot of Crook Glacier and is fed by Bend Glacier.

Geographic entities mentioned:
surface_form: broken top
instance_of: Mountain
countries: United States
coordinates: lat: 44.082894444444
lon: -121.69976111111
Additional cones. Todd Lake volcano, which erupted porphyritic andesite (andesite with distinct differences among its crystal size) with a pale gray color, sits at Broken Top's southern foot. Its lava flows have been exposed and are covered with red scoria and agglutinate from a separate volcanic vent.

Geographic entities mentioned:
surface_form: broken top
instance_of: Mountain
countries: United States
coordinates: lat: 44.082894444444
lon: -121.69976111111
surface_form: todd lake
instance_of: Lake
countries: United States
coordinates: lat: 44.0298
lon: -121.685
Its lava flows have been exposed and are covered with red scoria and agglutinate from a separate volcanic vent. It began to erupt as Broken Top stopped eruptive activity, since the two have overlapping layers of lava. As Pleistocene glaciers retreated, basaltic cinder cone volcanoes formed south of Todd Lake right as Cayuse Crater was forming.

Geographic entities mentioned:
surface_form: broken top
instance_of: Mountain
countries: United States
coordinates: lat: 44.082894444444
lon: -121.69976111111
It began to erupt as Broken Top stopped eruptive activity, since the two have overlapping layers of lava. As Pleistocene glaciers retreated, basaltic cinder cone volcanoes formed south of Todd Lake right as Cayuse Crater was forming. Cayuse Crater, an unrelated postglacial volcano which formed 11,000 years ago, also sits on Broken Top's southern flank.

Geographic entities mentioned:
surface_form: broken top
instance_of: Mountain
countries: United States
coordinates: lat: 44.082894444444
lon: -121.69976111111
Cayuse Crater, an unrelated postglacial volcano which formed 11,000 years ago, also sits on Broken Top's southern flank. It is made up of basaltic lava and scoria that erupted after Broken Top ceased activity, suggesting that it formed due to an underlying magma chamber closer to South Sister. Cayuse Crater also consists partly of yellow lapilli tuff and tuff breccia.

Geographic entities mentioned:
surface_form: broken top
instance_of: Mountain
countries: United States
coordinates: lat: 44.082894444444
lon: -121.69976111111
Williams' 1944 paper, titled &quot;Volcanoes of the Three Sisters Region, Oregon Cascades&quot;, defined the basic outline of the region, though he lacked access to chemical techniques and radiometric dating. geologist and volcanologist Edward Taylor's analysis in 1978 determined that the current Broken Top cone was constructed on basaltic andesite lavas that built a platform.

Geographic entities mentioned:
surface_form: broken top
instance_of: Mountain
countries: United States
coordinates: lat: 44.082894444444
lon: -121.69976111111
Broken Top poses significant hazards to the surrounding area, especially within the proximal hazard zone with a diameter of that surrounds Broken Top and the Three Sisters. A landslide at Broken Top, or an eruption from the nearby South Sister, could initiate a lahar (rapid flows of water, rock, and mud) that could cascade down river valleys in the surrounding area.

Geographic entities mentioned:
surface_form: broken top
instance_of: Mountain
countries: United States
coordinates: lat: 44.082894444444
lon: -121.69976111111
Motor vehicles and other mechanical means of transport such as bicycles, wagons, motorboats, and helicopters are generally prohibited within the Three Sisters Wilderness under the rules of the National Wilderness Preservation System. The hiking trail on Broken Top begins at the Green Lakes Basin at the trailhead east of Bend, running and gaining in elevation.

Geographic entities mentioned:
surface_form: broken top
instance_of: Mountain
countries: United States
coordinates: lat: 44.082894444444
lon: -121.69976111111
It runs for to Crater Creek, including of trail that passes right by the volcano and Crook Glacier. There is also an unofficial trail that runs up the moraine of Crook Glacier. The northern slopes of Broken Top can be accessed by trailheads north of Tam McArthur Rim, while its southern slopes can be reached by trailheads near Crater Creek.

Geographic entities mentioned:
surface_form: broken top
instance_of: Mountain
countries: United States
coordinates: lat: 44.082894444444
lon: -121.69976111111
Much of the current cone is occupied by flows from eruptions of mafic lava (rich in magnesium and iron) including andesite, dacite, rhyodacite, and pyroclastic flows. These deposits extend from the subordinate volcano to the summit, and reach Todd Lake Volcano as well as rhyodacitic lava at Tam MacArthur rim and Whychus Creek Falls.

Geographic entities mentioned:
surface_form: todd lake
instance_of: Lake
countries: United States
coordinates: lat: 44.0298
lon: -121.685
The United States Forest Service requires permits (of which a limited number are available) for use during the busier parts of the year, and dogs must be kept on leashes on the Green Lakes, Moraine Lakes, South Sister, Soda Creek, Todd Lake, and Crater Ditch trails from July 15 through September 15.

Geographic entities mentioned:
surface_form: todd lake
instance_of: Lake
countries: United States
coordinates: lat: 44.0298
lon: -121.685
The winter of 1941–42 is brutal and they struggle with freezing temperatures and the threat of starvation. Limited food supplies arrive via the ice road over the frozen Lake Ladoga, but they are nowhere near sufficient to feed the city of over three million people. Mikhail never recovers from his injuries and dies. Anna and Andrei cannot bury him because they are too weak.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
Found in Puerto Rico, it was formally described as a new species in 2020 by Joel Mercado‐Díaz and Robert Lücking. The type specimen was collected along a trail to Monte Guilarte in the Guilarte State Forest (Guilarte, Adjuntas), at an altitude of. The lichen is only known to occur in high-elevation forests at this location as well as the Toro Negro State Forest.

Geographic entities mentioned:
surface_form: Monte Guilarte
instance_of: Mountain
countries: United States
coordinates: lat: 18.15916667
lon: -66.77694444
Enarotali. Enarotali is a town in Paniai Regency, Central Papua, Indonesia. It is located on the shore of Lake Paniai, in Western New Guinea highlands. History. Enarotali is considered to be the only colonial city founded by the Dutch in the interior of New Guinea before World War II. The Wissel Lakes area was not known outside New Guinea until 1937.

Geographic entities mentioned:
surface_form: Lake Paniai
instance_of: Group of lakes
countries: Indonesia
coordinates: lat: -3.9022222222222
lon: 136.31777777778
History. Enarotali is considered to be the only colonial city founded by the Dutch in the interior of New Guinea before World War II. The Wissel Lakes area was not known outside New Guinea until 1937. In order to assert Dutch control over the area, a Christian mission and a radio-equipped government post were established there in May 1938.

Geographic entities mentioned:
surface_form: Wissel Lakes
instance_of: Group of lakes
countries: Indonesia
coordinates: lat: -3.9022222222222
lon: 136.31777777778
On 8 December 2014 the Indonesian army would open fire on a crowd of around 1,000 people protesting the severe beating of a group of young teens earlier that day, killing five and injuring 17. Geography. It is located in the Highlands, on the shore of Lake Paniai. Its altitude is about 1750 m, located near a fertile mountain plain surrounding the lake and it is surrounded by hills and mountains.

Geographic entities mentioned:
surface_form: Lake Paniai
instance_of: Group of lakes
countries: Indonesia
coordinates: lat: -3.9022222222222
lon: 136.31777777778
Iversenfjellet. Iversenfjellet is the highest mountain of Hopen in the Svalbard archipelago. It has a height of 371 m.a.s.l. and is located at the southern portion of Hopen. The mountain is named after fisheries consultant Thor Iversen.

Geographic entities mentioned:
surface_form: iversenfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 76.4541
lon: 24.9266
Its southeast face drops in less than one horizontal mile (1.6 km.), and is topped by an almost vertical cliff. Table Mountain is joined by the similar Greenleaf Peak to the northeast, and also by Hamilton Mountain to the southwest, which is lower, (), but similarly steep and much closer to the Columbia. Together these peaks form an impressive group on the Washington side of the Gorge.

Geographic entities mentioned:
surface_form: Greenleaf Peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.7138356
lon: -121.9669576
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: hamilton mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.411944444444
lon: -74.3675
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
Table Mountain (Skamania County, Washington). Table Mountain is a peak rising on the north side of the Columbia River in Washington state, about north-northwest of Bonneville Dam. It is one of the most spectacular landmarks of the Columbia River Gorge. Its southeast face drops in less than one horizontal mile (1.6 km.), and is topped by an almost vertical cliff.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain (skamania county, washington)
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
Table Mountain (Skamania County, Washington). Table Mountain is a peak rising on the north side of the Columbia River in Washington state, about north-northwest of Bonneville Dam. It is one of the most spectacular landmarks of the Columbia River Gorge. Its southeast face drops in less than one horizontal mile (1.6 km.), and is topped by an almost vertical cliff.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
Together these peaks form an impressive group on the Washington side of the Gorge. Between 1425 and 1450 AD the south side of Table Mountain sheared off and dammed the Columbia River in an event known as the Bonneville Slide. The river soon carved a new bend around to the south, but for a while Native Americans living in the area could walk across.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
Its southeast face drops in less than one horizontal mile (1.6 km.), and is topped by an almost vertical cliff. Table Mountain is joined by the similar Greenleaf Peak to the northeast, and also by Hamilton Mountain to the southwest, which is lower, (), but similarly steep and much closer to the Columbia. Together these peaks form an impressive group on the Washington side of the Gorge.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Yellow-tufted dacnis. The yellow-tufted dacnis (&quot;Dacnis egregia&quot;) is a species of bird in the family Thraupidae. It is commonly found typically in pairs throughout western Colombia and Ecuador and the Magdalena and Cauca valleys.

Geographic entities mentioned:
surface_form: Magdalena
instance_of: Valley
countries: Colombia
coordinates: lat: 7.05969444
lon: -73.85308333
Laval is often credited with the decimation of the indigenous population from 9,000 to just 500, but Liausu was co-responsible for the earlier part of the population decline through these projects. One of Liausu's legacies was the Rouru Convent located at the foot of Mount Duff in Rikitea, which was built to sequester the native women of the islands. He also became its first chaplain.

Geographic entities mentioned:
surface_form: Mount Duff
instance_of: Mountain
countries: France
coordinates: lat: -23.1286
lon: -134.974
He also set several new Austrian gliding records with it. Kahlbacher and Tauschegg, the other pilot on the first record duration flight, flew a Mg 9a at the Rhön (Wasserkuppe) Contest of 1938. They gained third place in the two seater class.

Geographic entities mentioned:
surface_form: Wasserkuppe
instance_of: Mountain
countries: Germany
coordinates: lat: 50.498055555556
lon: 9.9377777777778
Bughea (Râul Târgului). The Bughea is a right tributary of the Râul Târgului in Romania. Its two source rivers (Izvorul Zănoaga and Izvorul Dragoșu) originate in the Iezer Mountains. It flows into the Râul Târgului near Mihăești. Its length is and its basin size is.

Geographic entities mentioned:
surface_form: Iezer Mountains
instance_of: Mountain
countries: Romania
coordinates: lat: 45.4762
lon: 24.95414
History. Since the end of the 13th century Shtime was one of four courts of the King of Serbia in Nerodimlje župa. Its position at that time was on the northern bank of Svrčin Lake. After the mass expulsion of the Albanians from the former Sanjak of Niş by the Principality of Serbia, many Muhaxhir refugee families settled in Shtime and its surroundings.

Geographic entities mentioned:
surface_form: Svrčin Lake
instance_of: Lake
countries: Kosovo
Geology. Battleship Rock is composed of two principal strata of the Cutler Formation. The bottom layer is slope-forming Halgaito Formation and the upper stratum is cliff-forming Cedar Mesa Sandstone. Cedar Mesa Sandstone is the remains of coastal sand dunes deposited about 270 to 300 million years ago, during the Wolfcampian (early Permian).

Geographic entities mentioned:
surface_form: cedar mesa
instance_of: Landform
countries: United States
coordinates: lat: 37.433
lon: -109.917
The bottom layer is slope-forming Halgaito Formation and the upper stratum is cliff-forming Cedar Mesa Sandstone. Cedar Mesa Sandstone is the remains of coastal sand dunes deposited about 270 to 300 million years ago, during the Wolfcampian (early Permian). The buttes of Valley of the Gods are the result of the Halgaito Formation being more easily eroded than the overlaying sandstone.

Geographic entities mentioned:
surface_form: cedar mesa
instance_of: Landform
countries: United States
coordinates: lat: 37.433
lon: -109.917
Battleship Rock. Battleship Rock is a summit in San Juan County, Utah, United States. Description. Battleship Rock is situated west of Bluff, Utah, in the Valley of the Gods, on land administered by the Bureau of Land Management. Precipitation runoff from this iconic landform's slopes drains to the San Juan River via Lime Creek.

Geographic entities mentioned:
surface_form: battleship rock
instance_of: Mountain
countries: United States
coordinates: lat: 37.2925
lon: -109.83666666667
Battleship Rock. Battleship Rock is a summit in San Juan County, Utah, United States. Description. Battleship Rock is situated west of Bluff, Utah, in the Valley of the Gods, on land administered by the Bureau of Land Management. Precipitation runoff from this iconic landform's slopes drains to the San Juan River via Lime Creek.

Geographic entities mentioned:
surface_form: battleship rock
instance_of: Mountain
countries: United States
coordinates: lat: 37.2925
lon: -109.83666666667
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
This landform's toponym has been officially adopted by the United States Board on Geographic Names. Geology. Battleship Rock is composed of two principal strata of the Cutler Formation. The bottom layer is slope-forming Halgaito Formation and the upper stratum is cliff-forming Cedar Mesa Sandstone.

Geographic entities mentioned:
surface_form: battleship rock
instance_of: Mountain
countries: United States
coordinates: lat: 37.2925
lon: -109.83666666667
The valley floor is Honaker Trail Formation. Climate. Spring and fall are the most favorable seasons to visit Battleship Rock. According to the Köppen climate classification system, it is located in a cold semi-arid climate zone with cold winters and hot summers. Summers highs rarely exceed. Summer nights are comfortably cool, and temperatures drop quickly after sunset.

Geographic entities mentioned:
surface_form: battleship rock
instance_of: Mountain
countries: United States
coordinates: lat: 37.2925
lon: -109.83666666667
Precipitation runoff from this iconic landform's slopes drains to the San Juan River via Lime Creek. Access to the butte is via the 17-mile Valley of the Gods Road which passes near this butte. Topographic relief is significant as the summit rises nearly above the valley floor in 0.25 mile (0.4 km). This landform's toponym has been officially adopted by the United States Board on Geographic Names.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Cedar Mesa Sandstone is the remains of coastal sand dunes deposited about 270 to 300 million years ago, during the Wolfcampian (early Permian). The buttes of Valley of the Gods are the result of the Halgaito Formation being more easily eroded than the overlaying sandstone. The valley floor is Honaker Trail Formation. Climate. Spring and fall are the most favorable seasons to visit Battleship Rock.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Ophiolite emplacement. There are many crustal fragments in northeast Borneo that are derived from Mesozoic ophiolites placed during the initiation of the western Pacific Ocean plate subducting beneath southeast China and southeast Asia. This ophiolite basement underlies regions from Sabah in northeast Borneo and the Meratus Mountains in southeast Borneo.

Geographic entities mentioned:
surface_form: Meratus Mountains
instance_of: Mountain
countries: Indonesia
coordinates: lat: -2.75
lon: 115.66666666667
The newfound space for sediments to accumulate was introduced by Eocene rifting. Erosional material sourced from the Borneo highlands along with other older parts of the basin margins being uplifted. Cenozoic magmatism mentioned below that caused intrusions such as at Mt. Kinabalu could be potentially related to this regional uplift. Cenozoic South China Sea extension.

Geographic entities mentioned:
surface_form: Mt. Kinabalu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 6.075
lon: 116.5586111111111
This subduction period took place throughout the Eocene and ended in the Early Miocene. Late Cenozoic Magmatism and the Mount Kinabalu intrusion. Dating and defining the history of the Mount Kinabalu granitic intrusion faces many challenges due to the high erosion, difficult access through relief and rainforests, difficult to define boundaries and alteration.

Geographic entities mentioned:
surface_form: Mount Kinabalu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 6.075
lon: 116.5586111111111
Prospero (mountain). Prospero or Prospero Mountain is a prominent peak in the Mount Royal Range in New South Wales, Australia. The peak is marked by a Trig station, which was severely damaged in a storm in 2015.

Geographic entities mentioned:
surface_form: prospero
instance_of: Mountain
countries: Australia
coordinates: lat: -31.928333333333335
lon: 151.3311111111111
surface_form: prospero
instance_of: Mountain
countries: Australia
coordinates: lat: -31.928333333333335
lon: 151.3311111111111
Prospero (mountain). Prospero or Prospero Mountain is a prominent peak in the Mount Royal Range in New South Wales, Australia. The peak is marked by a Trig station, which was severely damaged in a storm in 2015.

Geographic entities mentioned:
surface_form: prospero (mountain)
instance_of: Mountain
countries: Australia
coordinates: lat: -31.928333333333335
lon: 151.3311111111111
Gobindpur is a village in the Gobindpur CD block in the Seraikela Sadar subdivision of the Seraikela Kharsawan district in the Indian state of Jharkhand. Area overview. The area shown in the map has been described as &quot;part of the southern fringe of the Chotanagpur plateau and is a hilly upland tract&quot;. 75.7% of the population lives in the rural areas and 24.3% lives in the urban areas.

Geographic entities mentioned:
surface_form: Chotanagpur plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
In October 2016, the state government's surplus operations ran an auction for &quot;Hiyu&quot;, ending with no sale. A second auction for the vessel later in the year also failed to find a buyer, but in February 2017 the state reached an agreement to sell &quot;Hiyu&quot; to a private buyer who would use her as a floating entertainment venue on Lake Union.

Geographic entities mentioned:
surface_form: Lake Union
instance_of: Lake
countries: United States
coordinates: lat: 47.6392
lon: -122.3337
While 75 percent of the trees produced are harvested from native stands those that are grown on plantations are grown by about 450 individual growers. All British Columbian Christmas tree plantations are found in the Fraser Valley, on Vancouver Island, and in the Okanagan, Thompson and Kootenays regions. Nova Scotia.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
The earliest text that deals with the Malay world is &quot;Sulalatus Salatin&quot; (&quot;Malay Annals)&quot; by Tun Sri Lanang, in 1612. According to the annals, Bukit Seguntang in modern-day Palembang in South Sumatra is where Sang Sapurba came to the world and his descendants would scatter throughout the Malay world.

Geographic entities mentioned:
surface_form: Bukit Seguntang
instance_of: Mountain
countries: Indonesia
coordinates: lat: -1.272
lon: 102.4743
He died before the age of 30, and a body claimed to be his was found in the Royal Cache above the Mortuary temple of Hatshepsut. His tomb, in the Western Wadis near the Valley of the Queens, was found in 2022 and confirmed to be his in 2025. The tomb was built under waterfalls, leading to periodic flooding, which damaged the tomb throughout the ages.

Geographic entities mentioned:
surface_form: Valley of the Queens
instance_of: Valley
countries: Egypt
coordinates: lat: 25.7275
lon: 32.593055555556
Von Beckerath additionally stresses that Egyptologists have no conclusive criteria to statistically evaluate the reign length of Thutmose II based on the number of preserved objects from his reign. Catherine Roerig has proposed that tomb KV20, generally believed to have been commissioned by Hatshepsut, was the original tomb of Thutmose II in the Valley of the Kings.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
In 2022, a joint Egyptian-British team led by the Egyptian Ministry of Tourism and Antiquities and the University of Cambridge's McDonald Institute for Archaeological Research uncovered a new tomb in the Western Wadis, near the Valley of the Kings.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
Education. There are no schools in Ocean View. The nearest government primary schools are Mount Mee State School in neighbouring Mount Mee to the north-west and Dayboro State School in Dayboro to the south. The nearest government schools are Woodford State School (to Year 10) in Woodford to the north and Bray Park State High School (to Year 12) in Bray Park to the south-east.

Geographic entities mentioned:
surface_form: Mount Mee
instance_of: Mountain
countries: Australia
coordinates: lat: -27.074166666667
lon: 152.76972222222
Other homesteads were established at Constable Hook (1646), Awiehaken (1647), and other lands at Achter Col on Bergen Neck. In 1658, Director-General Peter Stuyvesant of New Netherland negotiated a deal with the Lenape to re-purchase the area named Bergen, &quot;by the great rock above Wiehacken,&quot; including the whole peninsula from Sikakes south to Bergen Point/Constable Hook.

Geographic entities mentioned:
surface_form: Constable Hook
instance_of: Landform
countries: United States
coordinates: lat: 40.6578
lon: -74.0994
As originally constituted, Bergen Township included the area between the Hudson River on the east, the Hackensack River to the west, south to Constable Hook/Bergen Point and north to the present-day Hudson-Bergen border. For the next 127 years civic borders within the county took many forms, until they were finalized with the creation of Union City in 1925.

Geographic entities mentioned:
surface_form: Constable Hook
instance_of: Landform
countries: United States
coordinates: lat: 40.6578
lon: -74.0994
Air. Most airports which serve Hudson County are operated by the Port Authority of New York and New Jersey. Parks and points of interest. The Hudson County Park System includes Hudson County Park, Mercer Park, Lincoln Park, Washington Park, Columbus Park, and North Hudson Park, West Hudson Park and the newest, Laurel Hill.

Geographic entities mentioned:
surface_form: Laurel Hill
instance_of: Mountain
countries: United States
coordinates: lat: 40.758055555556
lon: -74.089166666667
Mgahinga Gorilla National Park is a national park in southwestern Uganda. It was created in 1991 and covers an area of. Geography. Mgahinga Gorilla National Park is located in the Virunga Mountains and encompasses three inactive volcanoes, namely Mount Muhabura, Mount Gahinga, and Mount Sabyinyo. In altitude the national park ranges from and is part of the Nile River watershed area.

Geographic entities mentioned:
surface_form: Mount Muhabura
instance_of: Mountain
countries: Rwanda
coordinates: lat: -1.3833333333333
lon: 29.666666666667
surface_form: Mount Gahinga
instance_of: Mountain
countries: Rwanda
Uganda
coordinates: lat: -1.3873
lon: 29.6435
surface_form: Mount Sabyinyo
instance_of: Mountain
countries: Rwanda
Uganda
Democratic Republic of the Congo
coordinates: lat: -1.4
lon: 29.6
It has the Great Himalayas to the north and the Sivalik Hills to the south. It extends from the Indus River Basin to the Brahmaputra Valley, traversing across Afghanistan, Pakistan, India, Nepal China and Bhutan. The sub-range has an average elevation of. Background.

Geographic entities mentioned:
surface_form: Brahmaputra Valley
instance_of: Valley
countries: India
coordinates: lat: 26.5983
lon: 92.4506
In one such tale, Ramsay is presented as a fur-trader who manages to evade natives along the north shore of Lake Erie with a boat loaded with gold, which he purportedly buries in a ridge at Long Point, planning to dig it up when the natives were no longer a problem. &quot;They went to Long Point, arriving just enough before dark to locate the spot where the treasure was.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Heyerdahl claimed a South American origin for a number of Easter Island plants, including the Totora reeds in the island's three crater lakes. These are now (by DNA analysis not available at the time) recognised as a separate species from similar ones in Lake Titicaca. He made the same claim for sweet potato and this fact remains unexplained, since this is indeed South American.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
History. According to popular folklore, Mount Tom takes its name from Rowland Thomas, a surveyor who worked for the settlement of Springfield, Massachusetts in the 1660s. Thomas supposedly named Mount Tom after himself while his fellow surveyor working on the opposite side of the Connecticut River, Elizur Holyoke, gave his name to Mount Holyoke.

Geographic entities mentioned:
surface_form: Mount Holyoke
instance_of: Mountain
countries: United States
coordinates: lat: 42.300833333333
lon: -72.586944444444
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.63
lon: -72.53
surface_form: mount holyoke
instance_of: Mountain
countries: United States
coordinates: lat: 42.300833333333
lon: -72.586944444444
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 44.2103
lon: -71.4459
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 42.2417
lon: -72.6481
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 37.3385
lon: -118.658
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.855
lon: -74.835277777778
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 47.79314
lon: -123.75825
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Massachusetts. (See Metacomet Ridge for more information on the geology and ecosystem of Mount Nonotuck.)
Recreation.

Geographic entities mentioned:
surface_form: mount nonotuck
instance_of: Mountain
countries: United States
coordinates: lat: 42.28
lon: -72.620277777778
Mount Tom (Massachusetts). Mount Tom, is a steep, rugged traprock mountain peak on the west bank of the Connecticut River 4.5 miles (7 km) northwest of downtown Holyoke, Massachusetts. The mountain is the southernmost and highest peak of the Mount Tom Range and the highest traprock peak of the long Metacomet Ridge.

Geographic entities mentioned:
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.63
lon: -72.53
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 44.2103
lon: -71.4459
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 42.2417
lon: -72.6481
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 37.3385
lon: -118.658
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.855
lon: -74.835277777778
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 47.79314
lon: -123.75825
Located in Easthampton and Holyoke, Mount Tom is traversed by the Metacomet-Monadnock Trail and is the transmitter location for three Springfield–Holyoke television stations: WGBY, WGGB, and WSHM-LD, and for radio stations WHYN-FM and WWEI. The name &quot;Mount Tom&quot; is sometimes used to describe the entire Mount Tom Range. History.

Geographic entities mentioned:
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.63
lon: -72.53
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 44.2103
lon: -71.4459
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 42.2417
lon: -72.6481
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 37.3385
lon: -118.658
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.855
lon: -74.835277777778
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 47.79314
lon: -123.75825
Located in Easthampton and Holyoke, Mount Tom is traversed by the Metacomet-Monadnock Trail and is the transmitter location for three Springfield–Holyoke television stations: WGBY, WGGB, and WSHM-LD, and for radio stations WHYN-FM and WWEI. The name &quot;Mount Tom&quot; is sometimes used to describe the entire Mount Tom Range. History.

Geographic entities mentioned:
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.63
lon: -72.53
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.63
lon: -72.53
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 44.2103
lon: -71.4459
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 44.2103
lon: -71.4459
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 42.2417
lon: -72.6481
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 42.2417
lon: -72.6481
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 37.3385
lon: -118.658
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 37.3385
lon: -118.658
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.855
lon: -74.835277777778
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.855
lon: -74.835277777778
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 47.79314
lon: -123.75825
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 47.79314
lon: -123.75825
History. According to popular folklore, Mount Tom takes its name from Rowland Thomas, a surveyor who worked for the settlement of Springfield, Massachusetts in the 1660s. Thomas supposedly named Mount Tom after himself while his fellow surveyor working on the opposite side of the Connecticut River, Elizur Holyoke, gave his name to Mount Holyoke.

Geographic entities mentioned:
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.63
lon: -72.53
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 44.2103
lon: -71.4459
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 42.2417
lon: -72.6481
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 37.3385
lon: -118.658
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.855
lon: -74.835277777778
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 47.79314
lon: -123.75825
In 1897 the Holyoke Street Railway Company began constructing the Mount Tom Railroad, as well as what would become known as &quot;Mountain Park&quot;, a trolley park and later an amusement park on the east side of the mountain.

Geographic entities mentioned:
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.63
lon: -72.53
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 44.2103
lon: -71.4459
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 42.2417
lon: -72.6481
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 37.3385
lon: -118.658
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.855
lon: -74.835277777778
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 47.79314
lon: -123.75825
The project changed hands several times until its closure in 1988 when competition from larger amusement parks gradually sapped business away from what had become affectionately known by local residents as &quot;The Queen of the Mountain&quot;. The Mount Tom Summit House was also constructed on the cliffs of Mount Tom in 1897, but it burned three years later.

Geographic entities mentioned:
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.63
lon: -72.53
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 44.2103
lon: -71.4459
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 42.2417
lon: -72.6481
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 37.3385
lon: -118.658
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.855
lon: -74.835277777778
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 47.79314
lon: -123.75825
During the heyday of northern New England's logging and river drives during the late 19th and early 20th centuries, the spring freshet, augmented by impoundments called drive-dams or squirt-dams on far-flung upper tributaries, carried logs rolled into rivers and lakes far down the Connecticut River to mills at falls where the river was pinched by bedrock at Mount Tom.

Geographic entities mentioned:
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.63
lon: -72.53
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 44.2103
lon: -71.4459
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 42.2417
lon: -72.6481
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 37.3385
lon: -118.658
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.855
lon: -74.835277777778
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 47.79314
lon: -123.75825
For many logging company workers, the specialists called river-hogs, the end of the drive at Mount Tom spelled the end of their employment until they joined crews going into the woods the next fall. On July 9, 1946, a US Army Air Force B-17G Flying Fortress, in use as a military transport, hit the northern flank of the mountain. All 25 on board died instantly in a large fireball.

Geographic entities mentioned:
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.63
lon: -72.53
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 44.2103
lon: -71.4459
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 42.2417
lon: -72.6481
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 37.3385
lon: -118.658
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.855
lon: -74.835277777778
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 47.79314
lon: -123.75825
The mountain formed near the end of the Triassic Period with the rifting apart of the North American continent from Africa and Eurasia. Lava welled up from the rift and solidified into sheets of strata hundreds of feet thick. Subsequent faulting and earthquake activity tilted the strata, creating the dramatic cliffs and ridges of Mount Tom.

Geographic entities mentioned:
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.63
lon: -72.53
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 44.2103
lon: -71.4459
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 42.2417
lon: -72.6481
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 37.3385
lon: -118.658
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 43.855
lon: -74.835277777778
surface_form: mount tom
instance_of: Mountain
countries: United States
coordinates: lat: 47.79314
lon: -123.75825
The road is used for bicycling, running, and mountain biking, and in the winter, cross country skiing and ski touring. Geocaching is popular. The mountain is also well known as a place to watch seasonal raptor migrations; an observation tower on nearby Goat Peak is maintained for that purpose. Mount Tom is registered in Amateur Radio as SOTA W1/MB-006. Conservation.

Geographic entities mentioned:
surface_form: goat peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.6322
lon: -120.404