Sarmila/GeoWiki-Features huggingface dataset:
Alternatively, largely unsorted breccia and debris deposits exist on the ridge north of Saxifraga Peak, possibly indicating the main, or a subsidiary, caldera edge. The Shield Forming Assemblage contains a series of basalt and minor comendite eruptions, and is best exposed on Far Mountain and Mount Scot. The basalts issued from fissure vents primarily located peripheral to the calderas.

Geographic entities mentioned:
surface_form: Far Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.7867
lon: -125.323
The park includes volcanic landforms, alpine environments, and forest sites scattered with wetlands. Itcha Ilgachuz Provincial Park is extremely remote and unroaded; the closest communities are Anahim Lake, Alexis Creek, Nimpo Lake, Redstone, and Nazko. The closest major centre is Quesnel, located approximately 200 km east of the park.

Geographic entities mentioned:
surface_form: Alexis Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.0803
lon: -123.305
surface_form: Nimpo Lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.3331
lon: -125.177
Lake Parangi. Lake Parangi is a small supertrophic (i.e. saturated in phosphorus and nitrogen, with excessive phytoplankton growth after a few weeks of calm, sunny weather), dune-dammed lake 3 km north of Kawhia in the Waikato region of New Zealand.

Geographic entities mentioned:
surface_form: lake parangi
instance_of: Lake
countries: New Zealand
coordinates: lat: -38.03777777777778
lon: 174.8111111111111
Lake Parangi is a small supertrophic (i.e. saturated in phosphorus and nitrogen, with excessive phytoplankton growth after a few weeks of calm, sunny weather), dune-dammed lake 3 km north of Kawhia in the Waikato region of New Zealand. In 1937, Lake Parangi was described by the &quot;Evening Post&quot; as having, &quot;a steep sand-cliff at one end of it and is reputed to be bottomless.

Geographic entities mentioned:
surface_form: lake parangi
instance_of: Lake
countries: New Zealand
coordinates: lat: -38.03777777777778
lon: 174.8111111111111
The area was divided from the local surroundings by the construction of I-91 in the 1960s. Cedar Hill's boundary runs from James Street, up the Mill River, to Rice Field, over Indian Head Rock, to the Hamden town line, across to Middletown Avenue, to the Eastern side of State Street, back up to James Street. Early settlement.

Geographic entities mentioned:
surface_form: Indian Head Rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
Today, the province comprises Lanao del Norte and Lanao del Sur. Etymology. The term &quot;Lanao&quot; is derived from a Maranao word &quot;Ranao&quot; meaning a body of water. &quot;Meranau&quot; means lake dweller. They are the natives of the place occupying the land around Lake Lanao, which is situated at the central part of Lanao del Sur. Lanao, applies to the entire area before its division.

Geographic entities mentioned:
surface_form: Lake Lanao
instance_of: Lake
countries: Philippines
coordinates: lat: 7.88
lon: 124.2525
Barren Bluff. Barren Bluff is a prominent rock bluff in the south part of the Sequence Hills along the west side of upper Rennick Glacier, Victoria Land, Antarctica.

Geographic entities mentioned:
surface_form: Sequence Hills
instance_of: Mountain
coordinates: lat: -73.05
lon: 161.25
Soon other student rowing clubs heard about the race and the Ringvaart Regatta became an annual event. Trail. The rowing race starts at the Kagerplassen and rounds the Ringvaart counterclockwise once before returning to the Kagerplassen. The rowers then enter the Vliet canal. The finish line is in Delft.

Geographic entities mentioned:
surface_form: Kagerplassen
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.205278
lon: 4.538333
Among the better known volcanoes are Acamarachi, Aguas Calientes, Arintica, Aucanquilcha, Cerro Bajo, Cerro Escorial, Chiliques, Colachi, Cordon de Puntas Negras, Escalante, Guallatiri, Guayaques, Irruputuncu, Isluga, Lascar, Lastarria, Licancabur, Llullaillaco, Olca-Paruma, Ollagüe, Ojos del Salado, Parinacota, Pular, Putana, San Pedro, Sierra Nevada de Lagunas Bravas, Socompa, Taapaca and Tacora.

Geographic entities mentioned:
surface_form: Acamarachi
instance_of: Mountain
countries: Chile
coordinates: lat: -23.295833333333
lon: -67.617222222222
surface_form: Arintica
instance_of: Mountain
countries: Chile
coordinates: lat: -18.75
lon: -69.05
surface_form: Aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
surface_form: Cerro Escorial
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -25.08
lon: -68.37
surface_form: Colachi
instance_of: Mountain
countries: Chile
coordinates: lat: -23.24192
lon: -67.64605
surface_form: Guallatiri
instance_of: Mountain
countries: Chile
coordinates: lat: -18.42361111111111
lon: -69.08972222222222
surface_form: Guayaques
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.898083333333332
lon: -67.56777777777778
surface_form: Irruputuncu
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -20.733333333333
lon: -68.566666666667
surface_form: Lastarria
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -25.166666666667
lon: -68.5
surface_form: Llullaillaco
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.719863
lon: -68.536852
surface_form: Ollagüe
instance_of: Mountain
countries: Bolivia
Chile
coordinates: lat: -21.3
lon: -68.166666666667
surface_form: Ojos del Salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: Socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
surface_form: Taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
surface_form: Tacora
instance_of: Mountain
countries: Chile
coordinates: lat: -17.716666666667
lon: -69.766666666667
These volcanoes are remote and thus, aside from potential impacts of ash clouds on aerial travel, they do not constitute a major threat to humans. Nevado Tres Cruces together with neighbouring El Fraile, El Muertito, El Muerto, El Solo, Nevado de Incahuasi, Nevado San Francisco and Ojos del Salado forms the Ojos del Salado volcanic chain.

Geographic entities mentioned:
surface_form: El Fraile
instance_of: Mountain
countries: Chile
coordinates: lat: -27.0514
lon: -68.3821
surface_form: El Muerto
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.0575
lon: -68.483888888889
surface_form: El Solo
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -27.108333333333
lon: -68.716666666667
surface_form: Nevado de Incahuasi
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.033333333333
lon: -68.3
surface_form: Nevado San Francisco
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -26.918333333333
lon: -68.263055555556
surface_form: Ojos del Salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: incahuasi
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.033333333333
lon: -68.3
surface_form: san francisco
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -26.918333333333
lon: -68.263055555556
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
The Salar de Maricunga is located west of Nevado Tres Cruces, the Almagro valley north and its tributary the Barrancas Blancas valley northeast of it. The international road between Chile and Argentina from Paso de San Francisco passes north of Nevado Tres Cruces; an unpaved road runs through the Barrancas Blancas valley.

Geographic entities mentioned:
surface_form: san francisco
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -26.918333333333
lon: -68.263055555556
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
Between it and Nevado Tres Cruces lies a wide and deep explosion crater that contains the La Espinilla dome, which is high and wide. Another lava dome is known as Domo las Vicuñas. The Tres Cruces Ignimbrite was erupted by Nevado Tres Cruces and lies between Nevado Tres Cruces and Ojos del Salado and reaches a thickness of. It covers a surface area of.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
A large explosive eruption 67,000±9,000 years ago deposited pyroclastic flows east and southeast of Nevado Tres Cruces. These pyroclastic flows form deposits extensive surrounding Ojos del Salado - to which they were originally attributed - and a thick base surge deposit is also linked to this eruption. Most recent eruption and hazards.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
The northern volcano has a summit elevation of and is capped by a glacially eroded, wide crater. There are two even more minor summits at the north end of the massif, Punta Torre and Punta Atacama. The volcanoes are formed by explosion craters, lava domes including couleés, lava flows, tephra, and base surge and pyroclastic flow deposits.

Geographic entities mentioned:
surface_form: torre
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -49.2906
lon: -73.09901
Nevado Tres Cruces. Nevado Tres Cruces is a massif of volcanic origin in the Andes Mountains on the border of Argentina and Chile. It has two main summits, Tres Cruces Sur at and Tres Cruces Centro at and a third minor summit, Tres Cruces Norte. Tres Cruces Sur is the sixth highest mountain in the Andes. The volcano has an extended history of activity, going back at least 1.5 million years.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
Nevado Tres Cruces. Nevado Tres Cruces is a massif of volcanic origin in the Andes Mountains on the border of Argentina and Chile. It has two main summits, Tres Cruces Sur at and Tres Cruces Centro at and a third minor summit, Tres Cruces Norte. Tres Cruces Sur is the sixth highest mountain in the Andes. The volcano has an extended history of activity, going back at least 1.5 million years.

Geographic entities mentioned:
surface_form: tres cruces sur
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
Nevado Tres Cruces. Nevado Tres Cruces is a massif of volcanic origin in the Andes Mountains on the border of Argentina and Chile. It has two main summits, Tres Cruces Sur at and Tres Cruces Centro at and a third minor summit, Tres Cruces Norte. Tres Cruces Sur is the sixth highest mountain in the Andes. The volcano has an extended history of activity, going back at least 1.5 million years.

Geographic entities mentioned:
surface_form: tres cruces sur
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
Geography and geomorphology. Nevado Tres Cruces is located in the High Andes of Copiapo and straddles the boundary between Chile (Atacama Region) and Argentina (Catamarca Province). The Salar de Maricunga is located west of Nevado Tres Cruces, the Almagro valley north and its tributary the Barrancas Blancas valley northeast of it.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
These volcanoes have diameters of and rise about above the surrounding terrain. The highest summit, and sixth-highest summit of South America, of Nevado Tres Cruces is the high southern summit, which is also the least eroded of the three volcanoes that make up Nevado Tres Cruces.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
The volcanoes are formed by explosion craters, lava domes including couleés, lava flows, tephra, and base surge and pyroclastic flow deposits. Fallout of explosive eruptions cover the slopes of the southern summit and deposits of a large Plinian eruption and its eruption column cover much of Nevado Tres Cruces and its surroundings.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
Normal faults cut across the volcanic structures and a north-northwest trending fault system appears to have directed the development of the three volcanoes. Domo del Indio on the southeastern flank is wide and high. Between it and Nevado Tres Cruces lies a wide and deep explosion crater that contains the La Espinilla dome, which is high and wide. Another lava dome is known as Domo las Vicuñas.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
It covers a surface area of. The ignimbrite consists of pumice and volcanic ash, is poorly welded and has a low crystal content. These edifices rise over older volcanoes, which crop out north of Nevado Tres Cruces in the form of the volcanoes Cristi (high), Lemp and Rodrigo. The latter has a caldera at elevation. Lemp is located just south of Rodrigo.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
The latter has a caldera at elevation. Lemp is located just south of Rodrigo. Puntiagudo crops out south of Nevado Tres Cruces. Two other centres lie on the southwestern foot: high Paitur and Trioblite. The older structures are smoothened by erosion and lack primary features. A thick and large lava flow crops out west of the volcano; it has a surface area of and a thickness of.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
Three older lava domes, all heavily eroded, are found on the western flank. Glaciation. Small glaciers occur on Nevado Tres Cruces on the eastern and southern sides above elevation. They are best developed above elevation and consist of small ice bodies (none exceeding) in glacial cirques and at the edges of lava flows.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
Non-moving ice without crevasses has been found on the northern summit, and there are debris-covered glaciers on the volcanoes. Some sources however deny that any glacier occurs on Nevado Tres Cruces. Moraines occur above elevation and a well-developed terminal moraine at the foot of Nevado Tres Cruces, at elevation, has been broken by the Lamas River.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
Some sources however deny that any glacier occurs on Nevado Tres Cruces. Moraines occur above elevation and a well-developed terminal moraine at the foot of Nevado Tres Cruces, at elevation, has been broken by the Lamas River. There are cirques at on the eastern sides of Nevado Tres Cruces and traces of periglacial occur.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
Moraines occur above elevation and a well-developed terminal moraine at the foot of Nevado Tres Cruces, at elevation, has been broken by the Lamas River. There are cirques at on the eastern sides of Nevado Tres Cruces and traces of periglacial occur. Presently, the equilibrium line altitude lies at about; during the last glacial maximum the equilibrium line altitude descended to. Geology.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
These are separated by gaps where Pleistocene and Holocene volcanism is absent and where the downgoing plate sinks into the mantle at a shallow angle, squeezing out the overlying asthenosphere. Nevado Tres Cruces is part of the CVZ, which spans Peru, Bolivia, Argentina and Chile and features over 1100 volcanoes.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
It is a group of mostly dacitic volcanoes that is oblique with respect to the local trend of Pleistocene-Holocene volcanoes and was active during the last one million years. During the Oligocene and Miocene volcanic activity occurred in the Maricunga Belt, then around 6 million years ago it migrated eastward. South of Nevado Tres Cruces lies the Los Patos volcano. Composition.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
South of Nevado Tres Cruces lies the Los Patos volcano. Composition. Nevado Tres Cruces has erupted rocks ranging from dacite to rhyodacite which define a potassium-rich calc-alkaline suite. They feature biotite and hornblende phenocrysts and there is evidence that magma mixing took place during the genesis of the magmas.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
At high elevations, precipitation falls mainly in winter in the form of snow and hail. The lack of visible life in the hyperarid region has led to numerous travellers deeming it a &quot;lunar landscape&quot;. There are wetlands associated with the Rio Lamas on Nevado Tres Cruces. The area is part of the Nevado Tres Cruces National Park created in 1994. Human history.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
The lack of visible life in the hyperarid region has led to numerous travellers deeming it a &quot;lunar landscape&quot;. There are wetlands associated with the Rio Lamas on Nevado Tres Cruces. The area is part of the Nevado Tres Cruces National Park created in 1994. Human history. The volcano was climbed on February 24, 1937, by members of the Second Polish Andean Expedition, Stefan Osiecki and.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
The flows are now covered with glacial and alluvial sediments and form a fan. A large explosive eruption 67,000±9,000 years ago deposited pyroclastic flows east and southeast of Nevado Tres Cruces. These pyroclastic flows form deposits extensive surrounding Ojos del Salado - to which they were originally attributed - and a thick base surge deposit is also linked to this eruption.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
Based on geochemical data, Nevado Tres Cruces has been proposed as the source of a tephra layer in the Bolson de Fiambalá that has also been identified in the Tafi del Valle area and the Valles Calchaquies. The eruption producing this tephra fall took place about 600-700 AD.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
The eruption producing this tephra fall took place about 600-700 AD. Archeological and vegetation studies observations in the Fiambalá region indicates that this tephra fall event had substantial impact on local communities and vegetation. However, the last securely dated eruption of Nevado Tres Cruces goes back to 67,000 years ago, making a correlation questionable.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
Visalia, California. Visalia () is a city in the agricultural San Joaquin Valley of California. The population was 141,384 as per the 2020 census. Visalia is the fifth-most populous city in the San Joaquin Valley, the 38th most populous in California, and 183rd in the United States.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Visalia is located at 36°19'27&quot; North, 119°18'26&quot; West (36.324100, −119.307347). The highest point in the Visalia–Porterville area is Mount Whitney. Located at the far reaches of the Sierra Nevada roughly east of the city, it reaches a height of, and was long famous as the highest mountain in the lower 48 states.

Geographic entities mentioned:
surface_form: Mount Whitney
instance_of: Mountain
countries: United States
coordinates: lat: 36.57861111111111
lon: -118.29194444444444
It is also home to the Visalia Vapor Trailers, the longest-active official National Hot Rod Association (NHRA) car club. Local government. Like much of the San Joaquin Valley, more resident voters are registered in the Republican Party than the Democratic Party. Of the 51,718 registered voters in Visalia; approximately 31.9% are Democrats and 49.1% are Republicans.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
It is southwest of the community of Bishop, and north of Mount Darwin. Subsidiary peak Mount Lamarck North (ranks as the 67th highest summit in California, and the sixth highest in the Evolution Region. Topographic relief is significant as the east aspect rises above Lake Sabrina in three miles, and the west aspect rises above Evolution Valley in three miles. History.

Geographic entities mentioned:
surface_form: Lake Sabrina
instance_of: Lake
countries: United States
coordinates: lat: 37.2073
lon: -118.619
It is situated on the shared boundary of Kings Canyon National Park with John Muir Wilderness, and along the common border of Fresno County with Inyo County. It is southwest of the community of Bishop, and north of Mount Darwin. Subsidiary peak Mount Lamarck North (ranks as the 67th highest summit in California, and the sixth highest in the Evolution Region.

Geographic entities mentioned:
surface_form: mount darwin
instance_of: Mountain
countries: United States
coordinates: lat: 37.1669
lon: -118.672
Mount Lamarck. Mount Lamarck is a mountain summit located on the crest of the Sierra Nevada mountain range in northern California, United States. It is situated on the shared boundary of Kings Canyon National Park with John Muir Wilderness, and along the common border of Fresno County with Inyo County. It is southwest of the community of Bishop, and north of Mount Darwin.

Geographic entities mentioned:
surface_form: mount lamarck
instance_of: Mountain
countries: United States
coordinates: lat: 37.19493
lon: -118.67122
It is southwest of the community of Bishop, and north of Mount Darwin. Subsidiary peak Mount Lamarck North (ranks as the 67th highest summit in California, and the sixth highest in the Evolution Region. Topographic relief is significant as the east aspect rises above Lake Sabrina in three miles, and the west aspect rises above Evolution Valley in three miles. History.

Geographic entities mentioned:
surface_form: mount lamarck
instance_of: Mountain
countries: United States
coordinates: lat: 37.19493
lon: -118.67122
The first ascent of the summit was made via the south slope on August 15, 1925, by Norman Clyde, who is credited with 130 first ascents, most of which were in the Sierra Nevada. Climate. According to the Köppen climate classification system, Mount Lamarck is located in an alpine climate zone. Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains.

Geographic entities mentioned:
surface_form: mount lamarck
instance_of: Mountain
countries: United States
coordinates: lat: 37.19493
lon: -118.67122
The endeavor helped to accelerate the town of Bathurst into the modern age; the hydro-electric dam at Tetagouche Falls was the first of its kind in New Brunswick. In 1919, the Bathurst Lumber Company amalgamated with the Bathurst Electric and Water Power Company which led to the building of a much larger dam at Grand Falls on the Nepisiguit River.

Geographic entities mentioned:
surface_form: Nepisiguit River
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.5559
lon: -65.6652
The Heyran Gondola lift has 30 ordinary cabins with six seats and also there are three special VIP cabins. The gondola lift is long through a beautiful landscape of the Alborz. It has: views east of the Caspian Sea; views southwest to the Fandog Loo forests in the Alborz, and views north to the Azerbaijan border area in the Alborz.

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
The Perijá tapaculo is a secretive bird and therefore difficult to observe; as a result its ecology is poorly known. It feeds on insects and reproduces between April and July. Its range is partially within Chamicero de Perijá Bird Reserve in Colombia and the Sierra de Perijá National Park in Venezuela. Taxonomy.

Geographic entities mentioned:
surface_form: Sierra de Perijá National Park
instance_of: Landform
countries: Venezuela
coordinates: lat: 9.5333333333333
lon: -73
However, there is a possibility that its range overlaps with that of the &quot;S. atratus nigricans&quot;, which occupies a different micro-habitat on the eastern side of the Serranía del Perijá at altitudes of; or that it may be found within the range of the pale-bellied tapaculo in the lower reaches of the Serranía de Los Motilones mountain range, south of the Serranía del Perijá.

Geographic entities mentioned:
surface_form: Serranía de Los Motilones
instance_of: Mountain
countries: Colombia
Venezuela
coordinates: lat: 9.8028
lon: -72.9525
The Colombian section of the Serranía del Perijá is dangerous for scientific excursions due to the presence of the FARC guerrilla group in the region. In Venezuela, the Sierra de Perijá National Park covers and partially protects the habitat of the Perijá tapaculo.

Geographic entities mentioned:
surface_form: Sierra de Perijá National Park
instance_of: Landform
countries: Venezuela
coordinates: lat: 9.5333333333333
lon: -73
Princess Peak. Princess Peak is a glaciated mountain summit located in the Boundary Ranges of the Coast Mountains, in the U.S. state of Alaska. Emperor Peak is situated in the Taku Range of the Juneau Icefield, north of Juneau, and south of Emperor Peak, on land managed by Tongass National Forest. The Taku Range is a north–south trending ridge on the edge of the Taku Glacier.

Geographic entities mentioned:
surface_form: emperor peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.5825
lon: -134.38472222222
surface_form: emperor peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.5825
lon: -134.38472222222
Princess Peak. Princess Peak is a glaciated mountain summit located in the Boundary Ranges of the Coast Mountains, in the U.S. state of Alaska. Emperor Peak is situated in the Taku Range of the Juneau Icefield, north of Juneau, and south of Emperor Peak, on land managed by Tongass National Forest. The Taku Range is a north–south trending ridge on the edge of the Taku Glacier.

Geographic entities mentioned:
surface_form: princess peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.559722222222
lon: -134.37527777778
Board on Geographic Names. Climate. Based on the Köppen climate classification, Princess Peak is located in a subpolar oceanic climate zone, with long, cold, snowy winters, and cool summers. Weather systems coming off the Gulf of Alaska are forced upwards by the Coast Mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall.

Geographic entities mentioned:
surface_form: princess peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.559722222222
lon: -134.37527777778
Weather systems coming off the Gulf of Alaska are forced upwards by the Coast Mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall. Temperatures can drop below −20 °C with wind chill factors below −30 °C. The month of July offers the most favorable weather to view or climb Princess Peak.

Geographic entities mentioned:
surface_form: princess peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.559722222222
lon: -134.37527777778
Monte Velha. Monte Velha is a peak in the northeastern part of the island of Fogo in Cape Verde. Its elevation is 1,482 m. It is a subpeak of the Pico do Fogo volcano, located at the northeastern end of the crater rim. It lies within the municipality of Mosteiros, 4 km southwest of the city centre. Its forest is a protected area, part of the larger Fogo Natural Park.

Geographic entities mentioned:
surface_form: monte velha
instance_of: Mountain
countries: Cape Verde
coordinates: lat: 15.0023
lon: -24.345
It lies within the municipality of Mosteiros, 4 km southwest of the city centre. Its forest is a protected area, part of the larger Fogo Natural Park. Due to the exposure of northeast winds, Monte Velha is the most humid part of the island. The annual precipitation shows much variation: in the period 1990-2000 it ranged between 214 and 1,481 mm.

Geographic entities mentioned:
surface_form: monte velha
instance_of: Mountain
countries: Cape Verde
coordinates: lat: 15.0023
lon: -24.345
The Braldu River is a long river, that originates from the Baltoro Glacier and flows to the west where it receives melt waters from the Biafo Glacier. The Baltoro Glacier and the Biafo Glacier are among the largest glaciers outside the polar regions. The Baltoro Glacier give rise to the four Eight-thousanders mountain peaks, among them is the K2, the second highest mountain peak of the world.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
Old Lake Highlands, Dallas. Old Lake Highlands is a neighborhood in east Dallas, Texas (USA). It is adjacent to White Rock Lake. It is in Dallas Council District 9. About. The neighborhood contains around 1,700 homes, and is located inside the triangle formed by Lake Highlands Drive, Northwest Highway, and White Rock Lake.

Geographic entities mentioned:
surface_form: White Rock Lake
instance_of: Lake
countries: United States
coordinates: lat: 32.834166666667
lon: -96.722777777778
It is adjacent to White Rock Lake. It is in Dallas Council District 9. About. The neighborhood contains around 1,700 homes, and is located inside the triangle formed by Lake Highlands Drive, Northwest Highway, and White Rock Lake. The area includes many parks along the creeks that feed into White Rock Lake including Norbuck Park at the southeast corner of Buckner and Northwest Highway. History.

Geographic entities mentioned:
surface_form: White Rock Lake
instance_of: Lake
countries: United States
coordinates: lat: 32.834166666667
lon: -96.722777777778
Big Reed Pond. Big Reed Pond is a freshwater pond located in Montauk, New York on Long Island. A site including the pond, brackish marshland and natural sand dunes was designated as a National Natural Landmark in 1973. The largely undeveloped pond is located within Theodore Roosevelt County Park. The Montaukett tribe lived in the vicinity of the pond until the mid-19th century.

Geographic entities mentioned:
surface_form: big reed pond
instance_of: Lake
countries: United States
coordinates: lat: 41.077702777778
lon: -71.910538888889
Big Reed Pond. Big Reed Pond is a freshwater pond located in Montauk, New York on Long Island. A site including the pond, brackish marshland and natural sand dunes was designated as a National Natural Landmark in 1973. The largely undeveloped pond is located within Theodore Roosevelt County Park. The Montaukett tribe lived in the vicinity of the pond until the mid-19th century.

Geographic entities mentioned:
surface_form: big reed pond
instance_of: Lake
countries: United States
coordinates: lat: 41.077702777778
lon: -71.910538888889
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
In 1951, he enlisted in the U.S. Air Force, beginning four years of military service. Serving during the Korean War, he spent two of those years stationed at Okinawa, after having done his boot-camp training at the since-defunct Sampson Air Force Base, near the Finger Lakes region of New York State. 1950s. After returning from the service, Lieber attended Manhattan's Art Students League.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
Brattskarvbrekka Pass. r1f7kt2ft8a2nrvzehrwizaw5da3" xml:space="preserve">Brattskarvbrekka Pass () is an east-west pass between Brattskarvet Mountain and Vendeholten Mountain, in the Sverdrup Mountains, Queen Maud Land.

Geographic entities mentioned:
surface_form: Brattskarvet Mountain
instance_of: Mountain
coordinates: lat: -72.1
lon: 1.45
surface_form: Vendeholten Mountain
instance_of: Mountain
coordinates: lat: -72.2
lon: 1.33333
Since the 2011 local government reform it is part of the municipality Penteli, of which it is the seat and a municipal unit. The municipal unit has an area of 3.956 km2. Melissia is situated at the southwestern foot of the Penteli mountains, 12 km northeast of Athens city centre. It is a green residential town.

Geographic entities mentioned:
surface_form: Penteli
instance_of: Mountain
countries: Greece
coordinates: lat: 38.08144
lon: 23.8825
One helicopter crew remained on the scene for 39 more minutes to advise ground crews on the spread of the fire. It rapidly expanded to over by 12:07 a.m., fueled by a strong Santa Ana wind event, with winds blowing northeast to southwest with wind gusts of up to reported at the nearby Mount Lukens Truck Trail north of La Cañada Flintridge. By 6:30 a.m.

Geographic entities mentioned:
surface_form: Mount Lukens
instance_of: Mountain
countries: United States
coordinates: lat: 34.2689
lon: -118.239
Seoraksan. Seoraksan (), or Mount Sorak, is the highest mountain in the Taebaek mountain range in the Gangwon Province in eastern South Korea. It is located in the Seoraksan National Park, near Sokcho. After the Hallasan volcano on Jeju Island and Jirisan in the south, Seoraksan is the third highest mountain in South Korea. The peak Daechongbong () of Seoraksan reaches 1,708 meters (5,603 feet).

Geographic entities mentioned:
surface_form: Jirisan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.336944444444
lon: 127.73055555556
surface_form: jirisan
instance_of: Mountain
countries: South Korea
coordinates: lat: 34.85166667
lon: 128.19694444
surface_form: seoraksan
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.119444444444
lon: 128.46555555556
Thousands of people have already tried to push down Heundeulbawi, but nobody gets further than waggling the rock. According to the legend Ulsanbawi comes from Ulsan in the south east of Korea. As Mount Kumgang () was built, Ulsanbawi walked to the north as the representative of the city. Unfortunately Ulsanbawi arrived too late and there was no more room.

Geographic entities mentioned:
surface_form: Mount Kumgang
instance_of: Mountain
countries: North Korea
coordinates: lat: 38.656763888889
lon: 128.10490277778
The shape of Ulsanbawi is unique in the area. To reach the rocks you need to follow a hiking path and climb over 800 steps (it is actually 888 steps according to locals). On the way there, there are two temples and a spherical rock (&quot;Heundeulbawi&quot;, 흔들바위) which is located on top of a larger rock. This rock is about 5 meters (16 feet) high and can be moved with some effort.

Geographic entities mentioned:
surface_form: heundeulbawi
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.119444444444
lon: 128.46555555556
This rock is about 5 meters (16 feet) high and can be moved with some effort. Thousands of people have already tried to push down Heundeulbawi, but nobody gets further than waggling the rock. According to the legend Ulsanbawi comes from Ulsan in the south east of Korea. As Mount Kumgang () was built, Ulsanbawi walked to the north as the representative of the city.

Geographic entities mentioned:
surface_form: heundeulbawi
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.119444444444
lon: 128.46555555556
Seoraksan. Seoraksan (), or Mount Sorak, is the highest mountain in the Taebaek mountain range in the Gangwon Province in eastern South Korea. It is located in the Seoraksan National Park, near Sokcho. After the Hallasan volcano on Jeju Island and Jirisan in the south, Seoraksan is the third highest mountain in South Korea. The peak Daechongbong () of Seoraksan reaches 1,708 meters (5,603 feet).

Geographic entities mentioned:
surface_form: seoraksan
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.119444444444
lon: 128.46555555556
It is located in the Seoraksan National Park, near Sokcho. After the Hallasan volcano on Jeju Island and Jirisan in the south, Seoraksan is the third highest mountain in South Korea. The peak Daechongbong () of Seoraksan reaches 1,708 meters (5,603 feet). The mountain is sometimes considered the backbone of South Korea.

Geographic entities mentioned:
surface_form: seoraksan
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.119444444444
lon: 128.46555555556
The mountain is sometimes considered the backbone of South Korea. The mountain is also part of a biosphere reserve: Mount Sorak Biosphere Reserve. Geography. Seoraksan is divided into Naeseorak (Inner Seorak), Oaeseorak (Outer Seorak), and Namseorak (South Seorak). Naeseorak (Inner Seorak). The area belonging to Inje-gun in the northwest. Daecheong-bong ou Daecheong Peak is called Naeseolak.

Geographic entities mentioned:
surface_form: seoraksan
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.119444444444
lon: 128.46555555556
surface_form: seorak
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.119444444444
lon: 128.46555555556
surface_form: seorak
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.119444444444
lon: 128.46555555556
surface_form: seorak
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.119444444444
lon: 128.46555555556
Outer Seorak District. The &quot;Yukdam&quot; waterfall and the &quot;Biryeong&quot; waterfall () are located on the southern side of the valley (Sangcheon river), about a forty-minute walk from the main car park. Ulsanbawi. &quot;Ulsanbawi&quot; () is a rock formation in the Seoraksan national park. The shape of Ulsanbawi is unique in the area.

Geographic entities mentioned:
surface_form: seoraksan
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.119444444444
lon: 128.46555555556
The mountain is sometimes considered the backbone of South Korea. The mountain is also part of a biosphere reserve: Mount Sorak Biosphere Reserve. Geography. Seoraksan is divided into Naeseorak (Inner Seorak), Oaeseorak (Outer Seorak), and Namseorak (South Seorak). Naeseorak (Inner Seorak). The area belonging to Inje-gun in the northwest. Daecheong-bong ou Daecheong Peak is called Naeseolak.

Geographic entities mentioned:
surface_form: seorak
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.119444444444
lon: 128.46555555556
In addition to Cheonbul-dong Valley, it is easy to access Ulsan Rock, Gwongeumseong Fortress, Geumgang Cave, Biryong Falls, and Toseong Falls. Oeseorak (Outer Seorak). Oeseorak () is the area belonging to Sokcho towards the east. It features easier hiking courses and is one of the most accessed areas of the park.

Geographic entities mentioned:
surface_form: seorak
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.119444444444
lon: 128.46555555556
It features easier hiking courses and is one of the most accessed areas of the park. In Oeseorak, there is the Towangseong Waterfall, the highest waterfall in South Korea. Mountain geography, fauna and flora. It was designated as Natural Monument No.171 in 1965, and as a national park (Mount Seorak national park) on March 24, 1970. In August 1982, UNESCO designated the area as a biosphere reserve.

Geographic entities mentioned:
surface_form: seorak
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.119444444444
lon: 128.46555555556
It is home to rare animals and plants, including natural monuments such as goats and bears. Outer Seorak District. The &quot;Yukdam&quot; waterfall and the &quot;Biryeong&quot; waterfall () are located on the southern side of the valley (Sangcheon river), about a forty-minute walk from the main car park. Ulsanbawi. &quot;Ulsanbawi&quot; () is a rock formation in the Seoraksan national park.

Geographic entities mentioned:
surface_form: seorak
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.119444444444
lon: 128.46555555556
Unfortunately Ulsanbawi arrived too late and there was no more room. Ulsanbawi was ashamed and slowly trudged back to the south. One evening the rock went to sleep in the Seorak area. Ulsanbawi felt it was so beautiful around there that it decided to stay for good. At the end of the main valley is &quot;Biseondae,&quot; a rock platform in a stream.

Geographic entities mentioned:
surface_form: seorak
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.119444444444
lon: 128.46555555556
Above the stream is a difficult to reach cave, which offers clear views of the surrounding rock formations. A bit farther from the entrance is the Valley of a Thousand Buddhas (), the primary valley of Seorak Mountain, also sometimes referred to as Seorak Valley. The valley was so named because the rock formations that line its sides resemble a line-up of Buddha statues. Dinosaur Ridge.

Geographic entities mentioned:
surface_form: seorak
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.119444444444
lon: 128.46555555556
surface_form: seorak
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.119444444444
lon: 128.46555555556
This species is endemic to the United States in the states of Georgia, Florida, and Alabama. Geography. The shinyrayed pocketbook historically occurred in 11 sub-basins and currently occupies Chipola, Middle and Lower Chattahoochee, Flint, Kinchafoonee, Ichawaynochaway, and Spring sub-basins. It was rediscovered in the Econfina sub-basin in 2006.

Geographic entities mentioned:
surface_form: Chattahoochee
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
On 10 October 1975, the III Army Corps Engineer Battalion was renamed 3rd Engineer Battalion &quot;Lario&quot;. The battalion was named for the great pre-alpine Lake Como, which is also known as Lake Lario, and located in Lombardy. After the reform the 3rd Engineer Battalion &quot;Lario&quot; consisted of a command, a command and park company, and three engineer companies.

Geographic entities mentioned:
surface_form: great pre-alpine
instance_of: Group of lakes
countries: Italy
Switzerland
Eden Memorial Park Cemetery. Eden Memorial Park Cemetery is a Jewish cemetery located at 11500 Sepulveda Boulevard, Mission Hills, California, in the San Fernando Valley of Los Angeles. Many Jews from the entertainment industry are buried here. It is located north of the San Fernando Mission Cemetery.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778