Sarmila/GeoWiki-Features huggingface dataset:
In the 1960s a new campground loop was added, and in the 1970s the campground roads were paved. Description. The heavily wooded Hoeft State Park sits on of Lake Huron shoreline and offers 144 campsites along with of hiking trails, hunting, playgrounds, a picnic pavilion and a lodge. The Huron Sunrise Trail bicycle path connects the park to Rogers City and the 40 Mile Lighthouse county park.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Eudontomyzon stankokaramani. &quot;Eudontomyzon stankokaramani&quot;, the Drin brook lamprey, is a non-predatory, freshwater resident species of lamprey found in the Drin river system of Albania and Kosovo and the basins of Lakes Ohrid and Shkodra. Conservation.

Geographic entities mentioned:
surface_form: Ohrid
instance_of: Lake
countries: North Macedonia
Albania
coordinates: lat: 41.03333333333333
lon: 20.716666666666665
Albert Kuchler (skier). Albert Kuchler (born November 30, 1998, in Bad Kötzting) is a German cross-country skier who represents the club SpVgg Lam and Germany national team. He participated at 2022 Winter Olympics in Beijing, China. His novel achievement to date is the winning bronze medal in the 4 × 5 km relay event at the 2023 World Champions in Planica, Slovenia. Cross-country ski results.

Geographic entities mentioned:
surface_form: Planica
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.476944444444
lon: 13.722222222222
Wadakapiapué-tepui. Wadakapiapué-tepui, also spelled Wadakapiapö, Wadakapiapo, Wadaka Piapo or Guadacapiapui, is a tepui of the Eastern Tepuis chain in Bolívar, Venezuela. It has an elevation of around. Its tiny tower-like summit has an area of less than, making it the smallest member of the Eastern Tepuis. It lies just west of the much larger Yuruaní-tepui.

Geographic entities mentioned:
surface_form: Yuruaní-tepui
instance_of: Mountain
countries: Venezuela
coordinates: lat: 5.315
lon: -60.8661
Wadakapiapué-tepui. Wadakapiapué-tepui, also spelled Wadakapiapö, Wadakapiapo, Wadaka Piapo or Guadacapiapui, is a tepui of the Eastern Tepuis chain in Bolívar, Venezuela. It has an elevation of around. Its tiny tower-like summit has an area of less than, making it the smallest member of the Eastern Tepuis. It lies just west of the much larger Yuruaní-tepui.

Geographic entities mentioned:
surface_form: bolívar
instance_of: Mountain
countries: Venezuela
coordinates: lat: 8.540861111111111
lon: -71.0465
surface_form: wadakapiapué-tepui
instance_of: Mountain
countries: Venezuela
coordinates: lat: 5.31639
lon: -60.9231
Wadakapiapué-tepui. Wadakapiapué-tepui, also spelled Wadakapiapö, Wadakapiapo, Wadaka Piapo or Guadacapiapui, is a tepui of the Eastern Tepuis chain in Bolívar, Venezuela. It has an elevation of around. Its tiny tower-like summit has an area of less than, making it the smallest member of the Eastern Tepuis. It lies just west of the much larger Yuruaní-tepui.

Geographic entities mentioned:
surface_form: wadakapiapué-tepui
instance_of: Mountain
countries: Venezuela
coordinates: lat: 5.31639
lon: -60.9231
Graphite pebbles were used for markings and Archaic peoples produced bone flutes. Evidence for Archaic peoples is found most recently 3890 years ago, with possible small campsites more recently from 3500 years ago along Lake Melville. Paleo-Eskimos. Little evidence of pre-Dorset Eskimo culture exists in Newfoundland and Labrador, but Dorset sites are well-studied.

Geographic entities mentioned:
surface_form: Lake Melville
instance_of: Lake
countries: Canada
coordinates: lat: 53.68222222222222
lon: -59.74861111111111
Part of the Chilean Andes' volcanic segment, it is part of the Central Volcanic Zone of the Andes, one of the four tracts of the Andean Volcanic Belt. This region of volcanism includes the world's two highest volcanoes Ojos del Salado and Llullaillaco. San Pedro, like other Andean volcanoes, was formed by the subduction of the Nazca Plate beneath the South America Plate.

Geographic entities mentioned:
surface_form: Ojos del Salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: Llullaillaco
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.719863
lon: -68.536852
Geography and geomorphology. San Pedro is located in northern Chile, in the Ollagüe commune, El Loa Province, Antofagasta Region; the border to Bolivia is away. The whole region is remote and thinly populated; towns in the area include Ascotán, Cupo, Inacaliri and Paniri; and the San Pedro railway station lies southwest of the volcano.

Geographic entities mentioned:
surface_form: Ollagüe
instance_of: Mountain
countries: Bolivia
Chile
coordinates: lat: -21.3
lon: -68.166666666667
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
Many of these volcanoes are of Pliocene-Pleistocene age and approach heights of about above sea level at Llullaillaco and Ojos del Salado; such sizes of the volcanoes occur because the edifices rise from a relatively high basement.

Geographic entities mentioned:
surface_form: Llullaillaco
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.719863
lon: -68.536852
surface_form: Ojos del Salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
This avalanche deposit covers a surface area of and its front is high in the Pampa de la Avestruz. The debris flow formed by the sector collapse does not have many of the typical hummock-like hills of volcanic sector collapse deposits and instead features grooves and radial ridges. Such flank collapse occurred notably on Mount St. Helens during its eruption in 1980.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
Regional. Volcanoes in this region of Chile often form lineaments perpendicular to the volcanic arc, with northwest–southeast and north–south lineaments common. One such lineament is the long San Pedro-Linzor lineament, which includes San Pedro, Paniri, Cerro Chao, Cerro del León, Toconce and Linzor.

Geographic entities mentioned:
surface_form: Paniri
instance_of: Mountain
countries: Chile
coordinates: lat: -22.059166666667
lon: -68.228333333333
surface_form: Cerro del León
instance_of: Mountain
countries: Chile
coordinates: lat: -22.15
lon: -68.116666666667
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
One such lineament is the long San Pedro-Linzor lineament, which includes San Pedro, Paniri, Cerro Chao, Cerro del León, Toconce and Linzor. Other volcanoes with such trends are Carasilla-Polapi-Cerro Cebollar-Cerro Ascotan-Palpana and the Aucanquilcha complex; the youngest edifice is the westernmost one.

Geographic entities mentioned:
surface_form: Cerro Cebollar
instance_of: Mountain
countries: Chile
coordinates: lat: -21.60845
lon: -68.44701
surface_form: Cerro Ascotan
instance_of: Mountain
countries: Bolivia
Chile
coordinates: lat: -21.68333333
lon: -68.11666667
surface_form: Palpana
instance_of: Mountain
countries: Chile
coordinates: lat: -21.546666666667
lon: -68.5225
surface_form: Aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
surface_form: palpana
instance_of: Mountain
countries: Chile
coordinates: lat: -21.546666666667
lon: -68.5225
Climate. The region has an arid climate with infrequent precipitation. Moisture ultimately originates on the tropical Atlantic Ocean and much of it rains out as it crosses the Eastern Cordillera and the Altiplano, so that little reaches the western Cordillera, with precipitation in the San Pedro area less than or about annually.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
San Pedro (Chile volcano). San Pedro is a Holocene composite volcano in northern Chile and at in elevation one of the highest active volcanoes in the world. Part of the Chilean Andes' volcanic segment, it is part of the Central Volcanic Zone of the Andes, one of the four tracts of the Andean Volcanic Belt.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
This region of volcanism includes the world's two highest volcanoes Ojos del Salado and Llullaillaco. San Pedro, like other Andean volcanoes, was formed by the subduction of the Nazca Plate beneath the South America Plate. It has a neighbouring volcano, San Pablo, and is itself formed by two separate edifices usually known as the Old Cone and the Young Cone.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
Geography and geomorphology. San Pedro is located in northern Chile, in the Ollagüe commune, El Loa Province, Antofagasta Region; the border to Bolivia is away. The whole region is remote and thinly populated; towns in the area include Ascotán, Cupo, Inacaliri and Paniri; and the San Pedro railway station lies southwest of the volcano.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
The whole region is remote and thinly populated; towns in the area include Ascotán, Cupo, Inacaliri and Paniri; and the San Pedro railway station lies southwest of the volcano. Tracks left by sulfur miners lead up to San Pedro's summit, and roads run around the volcano; passes around the northern, northwestern and western flanks of the volcano.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
Tracks left by sulfur miners lead up to San Pedro's summit, and roads run around the volcano; passes around the northern, northwestern and western flanks of the volcano. San Pedro is part of the long Central Volcanic Zone, one of the two belts of volcanoes in Chile, which contains a total of about 44 active volcanoes plus silicic caldera and ignimbrite systems and monogenetic volcanoes.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
Volcanism in this region is relatively poorly studied and there is not much present-day activity; with the exception of Láscar, most present-day manifestations are limited to fumarolic activity. San Pedro is one of the highest volcanoes in the world and is visible as far as away in Calama. Its height has been variously given as, or.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
The &quot;Young Cone&quot; has two craters, the eastern of which is the younger one. Lava flows emerge from a breach in this crater and have filled an older wide older crater. Hydrothermally altered rocks and sulfur deposits are found on San Pedro's summit and were mined into the 1930s. A number of lava flows of volumes between make up part of the edifice.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
A number of lava flows of volumes between make up part of the edifice. The upper part of the Younger Cone is covered with such lava flows, which have steep fronts and are up to thick. Downslope the lava flows are found mainly over the northwestern flank where they radiate away from San Pedro's crater. The total volume of the volcano is estimated to be.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
The total volume of the volcano is estimated to be. Scars at elevations of on the edifice have been the origin of mudflows; the largest is known as Estación flow and covers much of the southern and western foot of San Pedro to distances of; the debris apron reaches the Loa River and San Pedro River.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
These mudflows occurred between 110,000 – 36,000 years ago and they filled the river bed of the Loa, while the impact on the San Pedro River was much more minor. Hot avalanche deposits or pyroclastic flows are also found on the volcano; the largest of which covers large parts of the edifice and has a total volume of approximately.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
These deposits contain prismatic jointed blocks and poorly sorted pumice, with their thickness ranging from a thick layer to scattered rocks. Their formation was probably due to the steep incline of San Pedro's slopes which tended to destabilize lava bodies high on the edifice, similar to regular landslides.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
Their formation was probably due to the steep incline of San Pedro's slopes which tended to destabilize lava bodies high on the edifice, similar to regular landslides. At least one Plinian fall deposit is known from San Pedro; the size of the deposit indicates that it was as large as the AD 79 eruption of Vesuvius in Italy.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
At least one Plinian fall deposit is known from San Pedro; the size of the deposit indicates that it was as large as the AD 79 eruption of Vesuvius in Italy. This Plinian eruption was accompanied by the formation of an ignimbrite that covers much of the southern, southwestern and western slopes of San Pedro and reaches thicknesses of. It has a volume of and is called the El Encanto ignimbrite.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
It has a volume of and is called the El Encanto ignimbrite. There is evidence of a large sector collapse on San Pedro, which removed the northwestern flank of the volcano and formed a large debris avalanche deposit. This avalanche deposit covers a surface area of and its front is high in the Pampa de la Avestruz.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
Such flank collapse occurred notably on Mount St. Helens during its eruption in 1980. A high scarp west of the eastern summit was left by the collapse of San Pedro; otherwise much of the evidence was buried by later volcanic activity. As with the mudflows, the steep slopes of San Pedro probably facilitated the onset of the sector collapse, which descended over an elevation difference of about.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
As with the mudflows, the steep slopes of San Pedro probably facilitated the onset of the sector collapse, which descended over an elevation difference of about. A parasitic vent named La Poruña lies on the western foot of San Pedro, its formation was probably influenced by a normal fault that runs in that area.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
A parasitic vent named La Poruña lies on the western foot of San Pedro, its formation was probably influenced by a normal fault that runs in that area. It is a wide and high scoria cone on top of a field of lava flows which extend as far as west of San Pedro and from the cone. The cone's western side slumped and lava flows emanate from that area, reaching a considerable distance from the cone.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
These flows are subdivided into a small proximal unit and two distant ones, and feature structures such as ogives and levees. In addition, a lava dome at an elevation of lies on the southwestern flank of San Pedro and also seems to be a parasitic vent. Andesite lava flows emanate from this area as well.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
In addition, a lava dome at an elevation of lies on the southwestern flank of San Pedro and also seems to be a parasitic vent. Andesite lava flows emanate from this area as well. They are the largest found on San Pedro, with volumes of and a surface area of; they reach a distance of from the vent. San Pedro has been glaciated in the past.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
Evidence of such glaciation is found especially on the southern side of the Old Cone and it includes moraines at elevations of over as well as other glacially modified surfaces such as rock pavements and striated boulders. The chronology of glaciations in the Central Andes is poorly known but stratigraphic relations indicate that San Pedro was glaciated during the late Pleistocene.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
The chronology of glaciations in the Central Andes is poorly known but stratigraphic relations indicate that San Pedro was glaciated during the late Pleistocene. There are active rock glaciers on the mountain, with traces of past rock glaciers in cirques on the southern flank, but there are no glaciers presently on San Pedro.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
There are active rock glaciers on the mountain, with traces of past rock glaciers in cirques on the southern flank, but there are no glaciers presently on San Pedro. The San Pedro River flows at the foot of San Pedro volcano, and joins the Loa River southwest of the volcano; Pleistocene lava flows from San Pedro created a lava dam on the San Pedro River, forming a lake which no longer exists.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
There were two cycles of volcanic activity in Chile, the first during the Permian-Triassic and a second starting from the Tertiary. In the San Pedro region, this volcanic activity migrated east from its point of inception but recently has moved back westward. West of San Pedro lies the Pampa del Tamarugal and the Coastal Cordillera, neither of which show evidence of recent volcanic activity.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
At least three individual ignimbrites have been found; one of the ignimbrites, the San Pedro Ignimbrite, may have originated from a vent now covered by San Pedro volcano although the neighbouring Caracanal volcano is also a candidate source. The crust in the region is about thick.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
The crust in the region is about thick. The older composite volcano centres include Cerro Carcanal and Cerro Huiche south-southeast of San Pedro and Cerro del Diablo due north. This surface slopes down to the Loa River in the west. Composition. Old Cone lavas range from andesite to olivine-containing basaltic andesite. Young Cone lavas include both andesite and hornblende-containing dacite.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
This surface slopes down to the Loa River in the west. Composition. Old Cone lavas range from andesite to olivine-containing basaltic andesite. Young Cone lavas include both andesite and hornblende-containing dacite. Volcanic rocks erupted during both stages of San Pedro belong to the potassium-rich calc-alkaline suite. San Pedro volcanic rocks are usually glassy with only tiny phenocrysts.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
Ultimately they originate in the Altiplano-Puna Magma Body, but undergo storage in shallower crustal magma chambers and absorb crustal gneiss. The eruption of La Poruña appears to have been accompanied by a change in the magma system of the general volcano, a more recent hypothesis regards this cone as a separate volcanic system from San Pedro. Climate.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
Eruptive history. San Pedro formed in two stages, which are known as the Old Cone and the Young Cone. The Old Cone was formed by lava and scoria and later largely buried by glacial, mudflows and volcanic deposits of the Young Cone; it forms about 80% of the volume of the present-day San Pedro edifice. One date has been obtained on Old Cone lavas by argon-argon dating: 160,000 years ago.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
One date has been obtained on Old Cone lavas by argon-argon dating: 160,000 years ago. After activity of the Old Cone ceased, glacial and fluvial erosion dissected San Pedro until the large sector collapse occurred. The so-called &quot;white airfall&quot; with a volume of as well as pyroclastic flows on the western summit may have been erupted during the collapse but this is uncertain.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
In general, dates obtained by argon-argon dating range from 168,000 to 68,000 years ago. The entry of mafic magma at depth about 100,000 years ago may have stimulated the occurrence of eruptions not only at San Pedro but also at neighbouring volcanoes. A large eruption covered parts of the upper edifice with scoria about 15,000 years ago.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
Historical activity. Eruptions at San Pedro are reported from possibly 1885, when a newspaper from Valparaiso reported &quot;strong shaking of the earth&quot;, the emission of large quantities of white steam, and damage to the railway, houses and water pipes.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
All these eruptions are uncertain and apparently of phreatic nature, and no geological evidence of them has been found. The timing of eruptions at San Pedro sometimes is unclear; one eruption reported from 1877 may instead have occurred in 1891 as there are two reports of an eruption before 1910 and they may either refer to one eruption with two candidate dates or two eruptions.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
This volcanic activity makes San Pedro one of the highest active volcanoes. Presently, fumaroles in the eastern summit crater are the only ongoing activity at San Pedro; a steam plume is barely visible. The fumarole has formed sulfur deposits and its heat output is visible from space. Based on measurements made in December 2013, the output of San Pedro is about.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
The fumarole has formed sulfur deposits and its heat output is visible from space. Based on measurements made in December 2013, the output of San Pedro is about. Fumaroles were also reported from the Ojos de San Pedro area south of San Pedro volcano, and a report published in 1894 mentions a smell of sulfur at La Poruña.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
Based on measurements made in December 2013, the output of San Pedro is about. Fumaroles were also reported from the Ojos de San Pedro area south of San Pedro volcano, and a report published in 1894 mentions a smell of sulfur at La Poruña. In addition, seismic activity has been observed at the volcano, while deformation of the edifice has not been noted.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
The Chilean SERNAGEOMIN publishes a volcano hazard level for the volcano. Climbing. San Pedro is climbed relatively frequently due to its proximity to the tourist town of San Pedro de Atacama. The easiest route is by the north slopes to the col then by the east slope to the summit. It was first climbed by George Courty (France) and Filemón Morales (Chile) July 16, 1903.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
Satara city is surrounded by seven mountains. Satara lies on the slope of Ajinkyatara fort. It lies on the western side of the Deccan Plateau. Pune (110 KM), Sangli (121 KM), Kolhapur (122 KM) and Solapur (263 KM) are the main cities close to Satara. The city is surrounded by the tehsils of Koregaon on the West, Karad (51 KM) and Patan on the South, Jawali on the East and Wai on the North.

Geographic entities mentioned:
surface_form: Deccan Plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Killing of Afzal Khan by Chatrapati Shivaji was followed by decisive Maratha victory over the Bijapur army. Places to visit. Satara is located at the foot of the famous Ajinkyatara fort and on Kas plateau / Flower plateau, now a World Natural Heritage site. Satara has two palaces in the heart of the city, the Old Palace (Juna Rajwada) and the New Palace (Nava Rajwada) adjoining each other.

Geographic entities mentioned:
surface_form: Kas plateau
instance_of: Plateau
countries: India
coordinates: lat: 17.7
lon: 73.833
Horseshoe Lake (Chisago County, Minnesota). Horseshoe Lake is a lake in Chisago County, Minnesota, in the United States. Horseshoe Lake was named from the resemblance of its outline to a horseshoe.

Geographic entities mentioned:
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 40.4725
lon: -121.336
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 47.30912222222222
lon: -122.04138333333333
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 37.1489
lon: -89.355
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 46.02805556
lon: -95.68916667
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 46.3087
lon: -121.569
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 45.59194444
lon: -93.05361111
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 37.6087742
lon: -119.0194324
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 47.40822
lon: -122.6643413
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 38.6994
lon: -90.085
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 46.119166666667
lon: -94.830277777778
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 47.4411
lon: -93.4733
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 45.459166666667
lon: -93.05
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 44.131666666667
lon: -74.620833333333
A group of ski tourers attempting the Haute Route between Chamonix and Zermatt perished due to hypothermia. Expedition. A mountain guide and nine of his clients were trying to reach Zermatt from Chamonix on the slopes of the Pigne d'Arolla in the Val d'Hérens on 29 April 2018. It was on the fourth day of a planned six day expedition.

Geographic entities mentioned:
surface_form: Pigne d'Arolla
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.991111111111
lon: 7.455
&quot;Iris narbutii&quot; is now an accepted name by the RHS. It is listed in 1995 in 'Vascular plants of Russia and adjacent states (the former USSR)' by Czerepanov, S. K. It may have been named after 'Narbuta Beg'(1774-1798), a grandson of 'Abd al-Karim' (Khanate of Kokand) of the Fergana Valley, Central Asia, where the iris was found. Native. &quot;Iris narbutii&quot; is from Central Asia.

Geographic entities mentioned:
surface_form: Fergana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
Luis Eduardo Matos (born January 28, 2002) is a Venezuelan professional baseball center fielder for the San Francisco Giants of Major League Baseball (MLB). He signed with the Giants as an international free agent in 2018, and made his MLB debut in 2023. Early life. Matos was born in Valera, Venezuela, and was raised in the small town of Bobures, alongside Lake Maracaibo in Zulia State, Venezuela.

Geographic entities mentioned:
surface_form: Lake Maracaibo
instance_of: Lake
countries: Venezuela
coordinates: lat: 9.8158333333333
lon: -71.556666666667
Devil's Slide (Montana). Devil's Slide is an unusual cliff rock formation on the side of Cinnabar Mountain located in Gallatin National Forest in Park County, Montana north of Yellowstone National Park.

Geographic entities mentioned:
surface_form: yellowstone
instance_of: Lake
countries: United States
coordinates: lat: 44.466666666667
lon: -110.36666666667
surface_form: devil's slide
instance_of: Mountain
countries: United States
coordinates: lat: 45.0922
lon: -110.8
This distinctive formation can be viewed from Highway 89 and was created from alternate beds of limestone, sandstone, quartzites that have been tilted to lie nearly vertical and have eroded at different rates. History. In 1871, very few white travellers had ventured this far south in the Yellowstone River valley. The Cook–Folsom–Peterson Expedition passed the Devil's Slide in 1869.

Geographic entities mentioned:
surface_form: yellowstone
instance_of: Lake
countries: United States
coordinates: lat: 44.466666666667
lon: -110.36666666667
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
Devil's Slide (Montana). Devil's Slide is an unusual cliff rock formation on the side of Cinnabar Mountain located in Gallatin National Forest in Park County, Montana north of Yellowstone National Park.

Geographic entities mentioned:
surface_form: devil's slide
instance_of: Mountain
countries: United States
coordinates: lat: 45.0922
lon: -110.8
History. In 1871, very few white travellers had ventured this far south in the Yellowstone River valley. The Cook–Folsom–Peterson Expedition passed the Devil's Slide in 1869. Cook and Folsom described the slide in their diaries but did not name them

Geographic entities mentioned:
surface_form: devil's slide
instance_of: Mountain
countries: United States
coordinates: lat: 45.0922
lon: -110.8
During the protest of 2024, around 10,000 tourists were stuck in Cox's Bazar, who were later transported by plane and army patrol. Geography and climate. Cox's Bazar is located south of the divisional headquarter city of Chittagong. Cox's Bazar town has an area of, and is bounded by Bakkhali River on the north and East, Bay of Bengal in the West, and Jhilwanj Union in the south.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Hammertal (Ruhr region). The Hammertal &quot;(also known as Hammerthal)&quot; is a valley between Witten, Sprockhövel and Hattingen-Blankenstein. It gets drained from Pleßbach northwards into the Ruhr. The valley got its name in the 19th century by the forging hammers, which got actuated by danaides.

Geographic entities mentioned:
surface_form: hammertal (ruhr region)
instance_of: Valley
countries: Germany
coordinates: lat: 51.3892
lon: 7.26333
Hammertal (Ruhr region). The Hammertal &quot;(also known as Hammerthal)&quot; is a valley between Witten, Sprockhövel and Hattingen-Blankenstein. It gets drained from Pleßbach northwards into the Ruhr. The valley got its name in the 19th century by the forging hammers, which got actuated by danaides.

Geographic entities mentioned:
surface_form: hammertal
instance_of: Valley
countries: Germany
coordinates: lat: 51.3892
lon: 7.26333
surface_form: hammerthal
instance_of: Valley
countries: Germany
coordinates: lat: 51.3892
lon: 7.26333
It gets drained from Pleßbach northwards into the Ruhr. The valley got its name in the 19th century by the forging hammers, which got actuated by danaides. At the same time the coal mining started in the Hammertal, so the valley is one of the earliest places of Ruhr mining. Away from freeway 43 and road 551 the Hammertal kept its rurality.

Geographic entities mentioned:
surface_form: hammertal
instance_of: Valley
countries: Germany
coordinates: lat: 51.3892
lon: 7.26333
Chris Mosdell opened the show for their debut live performance at Shibuya AX. In 2009 Mosdell travelled to Machu Picchu and Lake Titicaca, Peru, to visit locations adjoined to his Fingerprints of the Gods installation soundtrack, and onward to Santiago, Chile to meet the German composer Uwe Schmidt (Atom™), who had covered several of Mosdell's songs on his Senor Coconut Yellow Fever! album.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Mud Creek Glacier. The Mud Creek Glacier is the southernmost glacier on Mount Shasta in the U.S. state of California. It lies to the east of Sargents Ridge on Shastarama point near above sea level. The glacier is smaller than the northern ones on Mount Shasta such as Whitney, Hotlum, Bolam, and Wintun Glaciers.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
The peat could be transported to the city via this small river. In the 17th century, Westerwolde came under control of the city of Groningen and the peat harvesting became more large-scaled Johan de la Haye and Johan Sems designed a line right through the western 'leg' of the bog, de Semslinie. De Semslinie is a straight line between Wolfsbarge (a village near the Zuidlaardermeer) and Ter Apel.

Geographic entities mentioned:
surface_form: Zuidlaardermeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 53.120556
lon: 6.695556
Parkstein (hill). The Parkstein, also called the Hoher Parkstein and Basaltkegel Hoher Parkstein is a well-known local hill and tourist destination in the Steinwald Mountains of central Germany. It lies northwest of Weiden in der Oberpfalz in the district of Neustadt a.d.Waldnaab and is one of the most popular walking and daytripper destinations in North Upper Palatinate.

Geographic entities mentioned:
surface_form: parkstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.7319
lon: 12.07
Parkstein (hill). The Parkstein, also called the Hoher Parkstein and Basaltkegel Hoher Parkstein is a well-known local hill and tourist destination in the Steinwald Mountains of central Germany. It lies northwest of Weiden in der Oberpfalz in the district of Neustadt a.d.Waldnaab and is one of the most popular walking and daytripper destinations in North Upper Palatinate.

Geographic entities mentioned:
surface_form: parkstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.7319
lon: 12.07
surface_form: parkstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.7319
lon: 12.07
surface_form: parkstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.7319
lon: 12.07
It lies northwest of Weiden in der Oberpfalz in the district of Neustadt a.d.Waldnaab and is one of the most popular walking and daytripper destinations in North Upper Palatinate. Around the volcanically-formed hill, which is above sea level (N.N.), is the village of the same name, Parkstein. At one time a castle (Parkstein Castle) stood on the summit.

Geographic entities mentioned:
surface_form: parkstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.7319
lon: 12.07
Around the volcanically-formed hill, which is above sea level (N.N.), is the village of the same name, Parkstein. At one time a castle (Parkstein Castle) stood on the summit. The Parkstein is famous for its impressive basalt outcrop. This basalt formation consists of pentagonal and hexagonal columns, up to one metre high, whose shafts extend into the earth to a depth of up to 30 metres.

Geographic entities mentioned:
surface_form: parkstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.7319
lon: 12.07
It is part of an old stream of lava that has been exposed at the surface after the softer rock above it had been weathered away over the course of millions of years. The wall of basalt measures 38 metres. Alexander von Humboldt viewed the Parkstein as the &quot;most beautiful basalt cone in Europe&quot;. In 2004 it was entered by the Free State of Bavaria as No.

Geographic entities mentioned:
surface_form: parkstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.7319
lon: 12.07
At, it is the largest wilderness area in the state of Colorado. Elevation in the wilderness ranges from along the Animas River to at the summit of Windom Peak. The Weminuche Wilderness is dissected by a narrow north-south corridor within the Animas River Gorge through which the Durango and Silverton Narrow Gauge Railroad travels between Silverton and Durango.

Geographic entities mentioned:
surface_form: Windom Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.621111111111
lon: -107.59194444444
Geology. The surface geology of the Weminuche Wilderness is characterized by two geologic provinces. The western third of the wilderness is within the Needle Mountains Proterozoic complex while the remainder of the wilderness is within the San Juan volcanic field. The Laramide Orogeny, which began approximately 80 million years ago in the Late Cretaceous, resulted in significant regional uplift.

Geographic entities mentioned:
surface_form: San Juan volcanic field
instance_of: Mountain
countries: United States
coordinates: lat: 37.8933
lon: -106.774
Erosion has removed the overlying rock and today the Proterozoic rock is exposed, forming the high, jagged, Needle Mountains. The highest peaks in the wilderness are in the Needle Mountains. These peaks include three fourteeners: Windom Peak, Mount Eolus, and Sunlight Peak. Eolus granite is a common rock in the Needle Mountains and these fourteeners are composed of this intrusive igneous rock.

Geographic entities mentioned:
surface_form: Windom Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.621111111111
lon: -107.59194444444
surface_form: Mount Eolus
instance_of: Mountain
countries: United States
coordinates: lat: 37.621666666667
lon: -107.62277777778
surface_form: Sunlight Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.627222222222
lon: -107.59583333333
Hekmatyar's conflict with Jamiat-e Islami and its commander Ahmad Shah Massoud was particularly contentious. Massoud was arrested in Pakistan for espionage in 1976 with Hekmatyar's cooperation. Later Massoud and Hekmatyar agreed to stage a takeover operation in the Panjshir valley. Hekmatyar at the last minute refused to engage his part of the offensive, leaving Massoud open and vulnerable.

Geographic entities mentioned:
surface_form: Panjshir valley
instance_of: Valley
countries: Afghanistan
coordinates: lat: 35.266666666667
lon: 69.466666666667
Although the arrests prevented a major uprising from occurring, a group of about 700 Poles who were assigned to the construction of the Circumbaikal Highway (a road near Lake Baikal and the Mongolian border) decided to disarm the guards and escape via Mongolia to China, where they hoped to find English ships and return to Europe by way of America. The uprising.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Portes, Achaea. Portes (Greek: Πόρτες meaning doors) is a village in the municipal unit of Olenia, Achaea, Greece. It is located on the southern end of Mount Skollis, 5 km south of Santomeri, 23 km south of Kato Achaia and 37 km southwest of Patras.

Geographic entities mentioned:
surface_form: Skollis
instance_of: Mountain
countries: Greece
coordinates: lat: 37.968
lon: 21.577
Iscuandé River. The Iscuandé River is a river of Colombia. It drains into the Pacific Ocean.

Geographic entities mentioned:
surface_form: iscuandé river
instance_of: Watercourse
countries: Colombia
coordinates: lat: 2.62
lon: -78.065833333333