Sarmila/GeoWiki-Features huggingface dataset:
Tupungatito formed less than 100,000 years ago and has had a number of historical eruptions, the latest in 1987, which were mostly small explosive eruptions. Presently, the volcano features an acidic crater lake and numerous fumaroles. Renewed eruptions could induce volcanic ash falls in Argentina and dangerous mudflows in Chile. Name and history.

Geographic entities mentioned:
surface_form: crater lake
instance_of: Lake
countries: United States
coordinates: lat: 42.943611111111
lon: -122.10666666667
Name and history. The name was assigned to the volcano by, the chair of the Chilean boundary commission, in 1897. It refers to the neighbouring Tupungato volcano; Luis Risopatrón also reported that Tupungatito was an active volcano. The volcano is also known as Volcan Bravard, a name proposed by Argentina but which fell into disuse; it references the French paleontologist Auguste Bravard.

Geographic entities mentioned:
surface_form: Tupungato
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -33.358555555555554
lon: -69.77041666666666
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Politically, it is part of the San Jose de Maipo municipality in the Metropolitan Region where about 40% of all Chileans live. East of Tupungatito is Argentina's Mendoza Province. high, Tupungato volcano rises northeast of Tupungatito. Tourism, mountaineering and hiking are the principal economic activities in the area; in addition, there are mines and hydropower plants in the valleys.

Geographic entities mentioned:
surface_form: Tupungato
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -33.358555555555554
lon: -69.77041666666666
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Tupungatito is part of the northernmost SVZ, a narrow and short chain which includes Diamante caldera/ Volcan Maipo and San Jose volcano, and is the northernmost active volcano of the SVZ. Tupungato-Tupungatito, San Jose-Marmolejo and Maipo are the highest volcanoes of the SVZ. Local.

Geographic entities mentioned:
surface_form: Marmolejo
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -33.717129
lon: -69.864514
surface_form: maipo
instance_of: Mountain
countries: Chile
coordinates: lat: -34.163916666666665
lon: -69.83216666666667
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Many eruptions appear to be linked to tectonic events in Central Chile. In 1835, Charles Darwin in his diary mentioned a muleteer telling him that he had seen smoke coming from close to Tupungato although he crossed the Andes close to Portillo de los Piuquenes rather than the Alto Colorado; this is almost certainly a reference to Tupungatito. In 1962 the volcano was reportedly smoking.

Geographic entities mentioned:
surface_form: Tupungato
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -33.358555555555554
lon: -69.77041666666666
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Since 2012, the volcano is monitored by the Southern Volcanological Observatory of the Andes. Intense eruptions could melt the ice on the volcano through the emission of incandescent rocks and pyroclastic flows, producing medium-sized or long lahars in the Quebrada de Tupungatito and Estero del Azufre valleys. Pyroclastic fallout from high eruption columns would most likely occur in Argentina.

Geographic entities mentioned:
surface_form: azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
surface_form: azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -27.30583333
lon: -69.13083333
It is a group of volcanic craters and a pyroclastic cone associated with a wide caldera, and lies just southwest of the Tupungato volcano. The caldera is filled with ice, and glaciers on the volcano are important sources of water for the Rio Maipo river and Santiago. Volcanism is caused by the subduction of the Nazca Plate underneath the South America Plate.

Geographic entities mentioned:
surface_form: maipo
instance_of: Mountain
countries: Chile
coordinates: lat: -34.163916666666665
lon: -69.83216666666667
Griebel, H. Gwinner, L. Hanisch, K. Heitmann and J. Philippi. Geography and geomorphology. Tupungatito is located in the Chilean Andes, east from Santiago de Chile. Politically, it is part of the San Jose de Maipo municipality in the Metropolitan Region where about 40% of all Chileans live. East of Tupungatito is Argentina's Mendoza Province. high, Tupungato volcano rises northeast of Tupungatito.

Geographic entities mentioned:
surface_form: maipo
instance_of: Mountain
countries: Chile
coordinates: lat: -34.163916666666665
lon: -69.83216666666667
The ice and snow cover on Tupungatito is an important source of water for the rivers in the region and Santiago. Meltwater is discharged westwards into the Colorado-Maipo river system that eventually flows through Santiago; the Quebrada Seca, Estero de Tupungatito and Estero de Tupungato originate close to the volcano and are tributaries to the Colorado.

Geographic entities mentioned:
surface_form: maipo
instance_of: Mountain
countries: Chile
coordinates: lat: -34.163916666666665
lon: -69.83216666666667
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Some glaciers drain instead eastward into the Rio Tupungato river, which as a tributary of the Rio Mendoza is an important water source for the inhabitants of Mendoza in Argentina and the surrounding agricultural areas. Arsenic pollution in the Maipo river system may originate from springs associated the volcanoes Tupungatito and San Jose. Regional.

Geographic entities mentioned:
surface_form: maipo
instance_of: Mountain
countries: Chile
coordinates: lat: -34.163916666666665
lon: -69.83216666666667
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
About 30-40 were active postglacially and 18-20 in historical times; the SVZ is the most active volcanic zone in Chile with about one eruption per year. Tupungatito is part of the northernmost SVZ, a narrow and short chain which includes Diamante caldera/ Volcan Maipo and San Jose volcano, and is the northernmost active volcano of the SVZ.

Geographic entities mentioned:
surface_form: maipo
instance_of: Mountain
countries: Chile
coordinates: lat: -34.163916666666665
lon: -69.83216666666667
surface_form: volcan maipo
instance_of: Mountain
countries: Chile
coordinates: lat: -34.163916666666665
lon: -69.83216666666667
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Tupungatito. Volcán Tupungatito is the northernmost historically active stratovolcano of the southern Andes. Part of the Chilean Andes' volcanic segment, it is the northernmost member of the Southern Volcanic Zone (SVZ), which is one of several distinct volcanic belts in the Andes. Over 70 Pleistocene or Holocene age volcanoes make up this volcanic belt, which on average has one eruption per year.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Tupungatito. Volcán Tupungatito is the northernmost historically active stratovolcano of the southern Andes. Part of the Chilean Andes' volcanic segment, it is the northernmost member of the Southern Volcanic Zone (SVZ), which is one of several distinct volcanic belts in the Andes. Over 70 Pleistocene or Holocene age volcanoes make up this volcanic belt, which on average has one eruption per year.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
surface_form: volcán tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Over 70 Pleistocene or Holocene age volcanoes make up this volcanic belt, which on average has one eruption per year. Tupungatito lies in proximity to the border between Argentina and Chile, 50 miles east of the Chilean capital Santiago. It is a group of volcanic craters and a pyroclastic cone associated with a wide caldera, and lies just southwest of the Tupungato volcano.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Volcanism is caused by the subduction of the Nazca Plate underneath the South America Plate. Tupungatito formed less than 100,000 years ago and has had a number of historical eruptions, the latest in 1987, which were mostly small explosive eruptions. Presently, the volcano features an acidic crater lake and numerous fumaroles.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Griebel, H. Gwinner, L. Hanisch, K. Heitmann and J. Philippi. Geography and geomorphology. Tupungatito is located in the Chilean Andes, east from Santiago de Chile. Politically, it is part of the San Jose de Maipo municipality in the Metropolitan Region where about 40% of all Chileans live. East of Tupungatito is Argentina's Mendoza Province. high, Tupungato volcano rises northeast of Tupungatito.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Tourism, mountaineering and hiking are the principal economic activities in the area; in addition, there are mines and hydropower plants in the valleys. Several protected areas lie in Argentina east of Tupungatito. The volcano features a wide caldera with an erupted volume of and one or two openings to the western flank, and a group of ten craters north of the caldera.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Glaciers and hydrology. Above elevation, the volcano is covered with ice. On Tupungatito ice covers an area of about, which is part of a larger ice cover on regional volcanoes. The caldera contains the Tupungatito glacier, with a volume of about it is the most important glacier of the Metropolitana Region. The cold ice lacks internal water pockets and reaches a maximum thickness of.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
The cold ice lacks internal water pockets and reaches a maximum thickness of. Outlet glaciers of glaciers in the region are typically covered with debris. In 2012, an ice core was drawn from the Tupungatito glacier. The ice and snow cover on Tupungatito is an important source of water for the rivers in the region and Santiago.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Local. The volcano lies on a thick crust, which together with the tectonic regime has influenced the composition of ascending magma. The basement underneath Tupungatito consists of evaporites and marine limestones of Cretaceous age. Cretaceous conglomerates, sandstones and volcaniclastic rocks, as well as Miocene sediments.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
The Mesozoic rocks have been deformed during regional tectonic activity and there are numerous reverse faults in the area. Southwest-northeast and north-south trending faults and fractures influence volcanic activity at Tupungatito; the SW-NE trending lineament also includes Tupungato. The volcano forms a volcanic group with Tupungato and another peak, high Nevado Sin Nombre.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Tupungato and Nevado Sin Nombre formed during the late and early Pleistocene, respectively, and are presently inactive. The caldera is to a large degree formed by rocks from Nevado Sin Nombre. high Nevado de los Piuquenes is a fourth volcano in this group and overlaps with Nevado Sin Nombre. Below elevation, Tupungatito is underlaid by an eroded volcano whose rocks resemble Tupungato. Composition.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Below elevation, Tupungatito is underlaid by an eroded volcano whose rocks resemble Tupungato. Composition. Tupungatito has erupted rocks ranging from basaltic andesite to dacite, which define a potassium-rich calc-alkaline suite. There has been little compositional variation during its history. Phenocrysts include clinopyroxene and plagioclase and less commonly olivine and orthopyroxene.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Amphibole and biotite occur as xenocrysts. Magma genesis at Tupungatito and other volcanoes in the region appears to involve a small amount of fluids but large amounts of sediments carried down by the slab, with a moderate interaction with the crust. Processes involved are fractional crystallization, low degrees of partial melting and short periods of storage in magma chambers. Climate.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Processes involved are fractional crystallization, low degrees of partial melting and short periods of storage in magma chambers. Climate. The mean annual temperature on Tupungatito is about and annual snow accumulation is about snow water equivalent. During the winter, the area above elevation is covered with up to of snow.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Glaciers have alternatively advanced and retreated during the 20th century. There is some uncertainty as sometimes snow cover is confused for glacial ice. ice covers an area of, down from in 1986; this encompasses the ice cover of Tupungatito and other volcanoes in the area. Volcanic eruptions have not significantly altered the ice extent. Eruption history.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Volcanic eruptions have not significantly altered the ice extent. Eruption history. Tupungatito is about 55,000 or less than 80,000 years old. Early activity was effusive, producing lava flows up to long as well as debris flows, lahars, and pyroclastic flows which invaded the Rio Colorado valley.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
They have been dated to 52,000±23,000 and 31,000±10,000 years ago, respectively. About 30,000 years ago, a change to a more effusive style of volcanic activity took place with shorter lava flows, although with shorter lava flows. Numerous debris avalanches took place on Tupungatito and left deposits in the western valleys.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Numerous debris avalanches took place on Tupungatito and left deposits in the western valleys. Tupungatito may be the source of late Pleistocene rhyolite deposits around the city of Mendoza and Pleistocene tephra overlying glacial deposits in the Rio Mendoza valley.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
The decline of the ice cover during the Holocene and an increased distance between glaciers and volcanic vents may have been responsible for this change in eruption style. Historical activity. Records of activity at Tupungatito go back to 1646 but its eruption record is poorly known, owing to its inaccessible location. Sometimes, eruptions at Tupungatito were incorrectly attributed to Tupungato.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Historical activity. Records of activity at Tupungatito go back to 1646 but its eruption record is poorly known, owing to its inaccessible location. Sometimes, eruptions at Tupungatito were incorrectly attributed to Tupungato. With over 19 eruptions between 1829 and 1987, Tupungatito is one of the SVZ's most active volcanoes.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
Sometimes, eruptions at Tupungatito were incorrectly attributed to Tupungato. With over 19 eruptions between 1829 and 1987, Tupungatito is one of the SVZ's most active volcanoes. The historical eruptions took place in the craters north of the caldera, and involved in total eight craters. The intensity of the eruptions did not exceed a Volcanic Explosivity Index of 2.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
In 1962 the volcano was reportedly smoking. Eruptions at Tupungatito frequently deposited volcanic ash in Mendoza. In 1958-1961 the volcano produced a long lava flow in Chile and ash fall in San Martin, Argentina, away. There is also evidence of ionospheric impacts from this eruption. The 1961 and 1964 eruptions formed one crater each, with the 1964 crater located directly south of the 1961 one.

Geographic entities mentioned:
surface_form: tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
&quot;Triton&quot; overtook the enemy and arrived at Plymouth with the news of the fleet five days before it reached Brest. &quot;Triton&quot; was then sent to watch over the fleet in Brest with a squadron of frigates. While doing so, they deterred a Spanish squadron of five ships of the line and two frigates from entering the port through the Passage du Raz.

Geographic entities mentioned:
surface_form: Passage du Raz
instance_of: Body of water
countries: France
coordinates: lat: 48.05
lon: -4.7833333333333
Great Hollow Lake. Great Hollow Lake is approximately in size and is a part of William E. Wolfe Park, located in Monroe, Connecticut. The lake includes a trout park with approximately of beach and facilities. Fishing, swimming and non-motorized boating are all permitted.

Geographic entities mentioned:
surface_form: great hollow lake
instance_of: Lake
countries: United States
coordinates: lat: 41.3111
lon: -73.2463
Mangyeongdaesan. Mangyeongdaesan is a mountain of South Korea. It has an elevation of 1,087 metres

Geographic entities mentioned:
surface_form: mangyeongdaesan
instance_of: Mountain
countries: South Korea
Ennetbaden. Ennetbaden is a municipality in the district of Baden in the canton of Aargau in Switzerland, located in the Limmat Valley (German: &quot;Limmattal&quot;). History. Ennetbaden is first mentioned about 1261-64 as &quot;Alio Badin&quot;. Geography. Ennetbaden has an area, of. Of this area, 20.9% is used for agricultural purposes, while 42.7% is forested.

Geographic entities mentioned:
surface_form: Limmat Valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 47.5
lon: 8.25
It is located in the La Paz Department, Pedro Domingo Murillo Province, La Paz Municipality, north-east of the city of La Paz. The mountains Mik'aya and Wak'ani are situated south-east of Jamp'aturi. The river &quot;Unduavi&quot; originates north-west of the mountain. Jamp'aturi lies near the &quot;La Cumbre&quot; pass which connects La Paz and the Yungas.

Geographic entities mentioned:
surface_form: Mik'aya
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.3664
lon: -67.9358
surface_form: Wak'ani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.3497
lon: -67.9442
surface_form: jamp'aturi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.3414
lon: -67.9978
Jamp'aturi. Jamp'aturi (Aymara &quot;jamp'atu&quot; frog, &quot;-ri&quot; or &quot;-iri&quot; a suffix, also spelled &quot;Jampaturi, Jamphaturi&quot;) is a mountain in the Cordillera Real in the Andes of Bolivia. It is located in the La Paz Department, Pedro Domingo Murillo Province, La Paz Municipality, north-east of the city of La Paz.

Geographic entities mentioned:
surface_form: jamp'aturi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.3414
lon: -67.9978
The ending &quot;-anum&quot; is a Latin suffix meaning &quot;pertaining to&quot; or &quot;belonging to&quot;. Distribution and habitat. &quot;Bryobium irukandjianum&quot; mostly grows on the upper branches of trees in humid situations. It is found in Queensland between the McIlwraith Range and the Atherton Tableland.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
It has an elevation of. Its elevation makes it the second highest in Incheon, next to Manisan (Incheon) which is located in Gwanghwa Island. From the top of the mountain, Gimpo Airport is visible, with a view of Seoul to the east, various islands such as Gwanghwa Island and Yeongjongdo in the west, Goyang in the north, and a whole view of Incheon to the south.

Geographic entities mentioned:
surface_form: manisan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.61666667
lon: 126.43333333
surface_form: manisan
instance_of: Mountain
countries: South Korea
Gyeyangsan. Gyeyangsan () is a mountain located in Incheon, South Korea. It has an elevation of. Its elevation makes it the second highest in Incheon, next to Manisan (Incheon) which is located in Gwanghwa Island.

Geographic entities mentioned:
surface_form: gyeyangsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.553
lon: 126.715
Mount Simmonds. 0mr3nci0hb61olwuca2uhu88s1g" xml:space="preserve">#redirect Mount Simmonds

Geographic entities mentioned:
surface_form: simmonds
instance_of: Mountain
coordinates: lat: -70.33333
lon: 159.56667
surface_form: mount simmonds
instance_of: Mountain
coordinates: lat: -70.33333
lon: 159.56667
state of Idaho. The population was 235,685 at the 2020 census. The Boise metropolitan area, also known as the Treasure Valley, includes five counties with an estimated population of 846,000, the most populous metropolitan area in Idaho and 74th-most populous in the United States. Located on the Boise River in southwestern Idaho, it is east of the Oregon border and north of the Nevada border.

Geographic entities mentioned:
surface_form: Treasure Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.0403
lon: -116.933
Etymology. The origin of the name is uncertain. One account credits Capt. B. L. E. Bonneville of the U.S. Army as its source. After trekking for weeks through dry and rough terrain, his exploration party reached an overlook with a view of the Boise River Valley. The place where they stood is called Bonneville Point, located on the Oregon Trail east of the city.

Geographic entities mentioned:
surface_form: Boise River Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.0403
lon: -116.933
About southwest of Boise, and about southwest of Nampa, the Owyhee Mountains lie entirely in neighboring Owyhee County. According to the United States Census Bureau, the city has an area of, of which is land and is water. The city is drained by the Boise River and is considered part of the Treasure Valley. Neighborhoods and areas.

Geographic entities mentioned:
surface_form: Treasure Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.0403
lon: -116.933
Babolsar County. Babolsar County () is in Mazandaran province, Iran, on the Caspian Sea. Its capital is the city of Babolsar. History. After the 2006 National Census, Fereydunkenar District was separated from the county in the establishment of Fereydunkenar County. Population. At the time of the 2006 census, the county's population was 172,600 in 46,595 households.

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
Santa Cruz Map. The Santa Cruz Map (Also known as the Uppsala map) is the earliest known city map of Mexico City as the capital of New Spain. The map depicts the city’s layout with its buildings, streets, and waterways surrounded by the lakes of the basin of the Valley of Mexico and the countryside beyond. In the map one can also see images of daily life, animals and plants.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
It weighs. Distribution and habitat. The weasel sportive lemur inhabits montane and lowland rainforests in eastern Madagascar, from south of the Nosivolo and Mangoro rivers, north to at least the Maningory River. However, Additional work is needed to determine the exact limits of its distribution.

Geographic entities mentioned:
surface_form: Mangoro
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -20.004968
lon: 48.781672
surface_form: Maningory River
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -17.20583333
lon: 49.4625
Sailboats heading towards the Strait of Gibraltar would have found protection there from powerful sea-currents and strong westerly winds. From Cerro del Villar, the Phoenicians began trading with coastal indigenous villages and the small community at present-day San Pablo near the mouth of the river Guadalmedina.

Geographic entities mentioned:
surface_form: Guadalmedina
instance_of: Watercourse
countries: Spain
coordinates: lat: 36.70621
lon: -4.425791
The farmers practiced intensive irrigation-based agriculture, while artisanry and trade flourished in the cities—leading to prosperity and an era of peace in the province. Surrounded by a walled enclosure with five large gates, Mālaqa city itself thrived; the Alcazaba, a Moorish citadel, was built in the mid-11th century on Mount Gibralfaro, a hill in the center of the city overlooking the port.

Geographic entities mentioned:
surface_form: Gibralfaro
instance_of: Mountain
countries: Spain
coordinates: lat: 36.72333333
lon: -4.41083333
Until 23 January 1944, she operated between Auckland and Noumea, Espiritu Santo, Guadalcanal, Suva, Efate, and Tulagi, supporting the South Pacific Ocean operations. She sailed from Auckland 8 January 1944 for Nouméa, where she loaded additional cargo, and Lunga Point, arriving 28 January. Shooting down a Japanese plane.

Geographic entities mentioned:
surface_form: Lunga Point
instance_of: Landform
countries: Solomon Islands
coordinates: lat: -9.416666666666666
lon: 160.03333333333333
It also fought defensive actions against the Soviet Winter campaign of 1941–42. 1942. In January 1942, the 253rd Infantry Division was encircled at Lake Volgo, but managed to break out and return to German lines with heavy casualties. Throughout the year 1942, the 253rd Infantry Division remained in the Rzhev salient. 1943.

Geographic entities mentioned:
surface_form: Lake Volgo
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.931388888889
lon: 33.145277777778
Ferlacher Badesee. Ferlacher Badesee is a lake of Carinthia, Austria.

Geographic entities mentioned:
surface_form: ferlacher badesee
instance_of: Lake
countries: Austria
coordinates: lat: 46.54527777777778
lon: 14.283333333333333
Geography. Vaucluse is bordered by the Rhône to the west and the Durance to the south. Mountains occupy a significant proportion of the eastern half of the department, with Mont Ventoux (1,912 m), also known as &quot;the Giant of Provence&quot;, dominating the landscape. Other important mountain ranges include the Dentelles de Montmirail, the Monts de Vaucluse and the Luberon.

Geographic entities mentioned:
surface_form: Mont Ventoux
instance_of: Mountain
countries: France
coordinates: lat: 44.166666666667
lon: 5.2833333333333
Name of Toronto. The name of Toronto has a history distinct from that of the city itself. Originally, the term &quot;Tkaronto&quot; referred to a channel of water between Lake Simcoe and Lake Couchiching, at what is now the city of Orillia, on maps as early as 1675 but in time the name passed southward, and was eventually applied to a new fort at the mouth of the Humber River.

Geographic entities mentioned:
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
surface_form: Lake Couchiching
instance_of: Lake
countries: Canada
coordinates: lat: 44.6667
lon: -79.3833
After 1650, and the destruction of Fort Sainte Marie, the Hurons left the region. A 1675 map in French, by Pierre Raffeix, referred to Lake Simcoe as, and the name appeared on a 1678 map of New France by cartographer Jean-Baptiste-Louis Franquelin. In 1680, it appeared as on a map created by French court official Abbé Claude Bernou.

Geographic entities mentioned:
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
The change of spelling from Taronto to Toronto is thought to originate on a 1695 map by Italian cartographer Vincenzo Coronelli. The name has also sometimes been identified with, a village marked on a 1656 map of New France by Nicolas Sanson. However, the location on this map is east of Lake Nipissing and northwest of Montreal in what is now Quebec. Town of York.

Geographic entities mentioned:
surface_form: Lake Nipissing
instance_of: Lake
countries: Canada
coordinates: lat: 46.283333333333
lon: -80
Glaciers. A number of glaciers flow from the inner ice cap to Severny Island's coastline. Mount Kruzenshtern, the highest point of Novaya Zemlya, rises on the western edge of the Severny Island ice cap, near the head of the Glazov Glacier. West coast. The following glaciers have their terminus on the coast of the Barents Sea. East coast.

Geographic entities mentioned:
surface_form: Mount Kruzenshtern
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 75.1757714
lon: 57.8259507
The following glaciers have their terminus on the coast of the Barents Sea. East coast. The following glaciers have their terminus on the coast of the Kara Sea. Nunataks. Gora Severny Nunatak is a nunatak located in the northern section of the long ice cap not far from the western coast of the island. Further to the northeast there is another nunatak between the two outlets of the Bunge Glacier.

Geographic entities mentioned:
surface_form: Gora Severny Nunatak
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 76.60982
lon: 66.33947
Battalion's size was now 381 men. It was used as a guard under the German Army's 11th Infantry Division. Despite that battalion's role was only rearguard, it was installed in January 1944 to the positions near Mehikoorma ashore of Lake Peipus. In June 1944, the battalion was taken to rear and disbanded, the men were sent to battalions 37, 38 and 40.

Geographic entities mentioned:
surface_form: Lake Peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
The 1995 India cyclone was a tropical cyclone that struck southeastern India which later spawned a rare snowstorm in Nepal, triggering the deadliest mountain trekking incident in the country's history in November 1995. The storm originated from the monsoon trough on November 7 in the Bay of Bengal, east of India, becoming the penultimate storm of the 1995 North Indian Ocean cyclone season.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The Nepal government launched the largest search and rescue mission in the country's history, rescuing 450 people, some of whom trapped for days in the snow. Meteorological history. In early November 1995, the monsoon trough was active across the Bay of Bengal, with several associated circulations. A disturbance near the Andaman Islands became the focus of the overall system on November 6.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
At higher elevations, the precipitation caused intense snowfall, reaching up to deep in Dingboche. Gorakshep recorded of snowfall. The Khumbu region of eastern Nepal received rare snowfall, as it is normally part of a rain shadow. The village of Thame was buried for eight days until people could travel freely again; the rarity of the snowfall meant that residents did not have skis or snow shoes.

Geographic entities mentioned:
surface_form: Khumbu
instance_of: Valley
countries: Nepal
coordinates: lat: 27.805
lon: 86.71
Near Gokyo, two avalanches combined and destroyed a lodge housing 25 mountain climbers, killing all but one; the survivor was rescued after being trapped for 40 hours. The hikers were climbing Gokyo Ri, a mountain southeast of Mount Everest. This marked the deadliest avalanche in Nepal to affect a hiking expedition. Another avalanche killed seven people in Kangchenjunga.

Geographic entities mentioned:
surface_form: Gokyo Ri
instance_of: Mountain
countries: Nepal
coordinates: lat: 27.961111111111
lon: 86.683333333333
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
The hikers were climbing Gokyo Ri, a mountain southeast of Mount Everest. This marked the deadliest avalanche in Nepal to affect a hiking expedition. Another avalanche killed seven people in Kangchenjunga. With levels reaching as high as the roofs of houses, the heavy snowfall damaged the roofs of several buildings, including one school, and killed about 100 animals.

Geographic entities mentioned:
surface_form: Kangchenjunga
instance_of: Mountain
countries: India
Nepal
coordinates: lat: 27.7
lon: 88.133333
Corno Zuccone. Corno Zuccone () is a mountain of Lombardy, Italy. It is located within the Bergamo Alps.

Geographic entities mentioned:
surface_form: corno zuccone
instance_of: Mountain
countries: Italy
coordinates: lat: 45.9
lon: 9.53333333
In the 1980s, Alfond helped sponsor Kevin Mahaney in the sailor's effort to compete in the Olympics. Mahaney later earned a silver medal in sailing at the 1992 Summer Olympics. Along with other investors, Alfond helped create Belgrade Lakes Golf Club, a course close to his summer home. The club has been recognized as among the best public golf courses in the country.

Geographic entities mentioned:
surface_form: Belgrade Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 44.63333333333333
lon: -69.78333333333333
Schwarzenstein (Zillertal Alps). The Schwarzenstein (;) is a mountain in the Zillertal Alps on the border between Tyrol, Austria, and South Tyrol, Italy.

Geographic entities mentioned:
surface_form: schwarzenstein
instance_of: Mountain
countries: Italy
Austria
coordinates: lat: 47.010017
lon: 11.873903
The Central Railway undertook to build the Murgenthal–Bern line and the Solothurn–Herzogenbuchsee railway within four years and in return received tax exemption and the privilege of being given preferential treatment in future grants of concessions to build railways. The Central Railway's construction now concentrated for a period on the more populated areas in the Swiss Plateau.

Geographic entities mentioned:
surface_form: Swiss Plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
Wari Warini. Wari Warini (Aymara, &quot;wari&quot; vicuña, the reduplication signifies that there is a group of something, &quot;-ni&quot; a suffix to indicate ownership, &quot;the one with many vicuñas&quot;, or from &quot;wari&quot; a liquid, &quot;wari wari&quot; very liquid, also spelled &quot;Huari Huarini&quot;) is a mountain in the Bolivian Andes, about high.

Geographic entities mentioned:
surface_form: wari warini
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.22527778
lon: -66.3575
Upon entering the town of Otis, the road passes through a small settlement titled Fletchers Lodge where a general store and an elementary school are located. Numerous roads towards the west lead to Beech Hill Pond. In this area, SR 180 meets the southern terminus of SR 181 (Mariaville Road) which heads north towards Mariaville.

Geographic entities mentioned:
surface_form: Beech Hill Pond
instance_of: Lake
countries: United States
coordinates: lat: 44.689722222222
lon: -68.456111111111
Alfarnatejo’s demonym is related to the town’s water fountain, named ‘La Teja’, which means roof tile. It is located near the Sierra del Jobo in the northwest and the Sierra de Alhama in the east in the mountainous region of Axarquía. To the east lies the town of Alfarnate, to the west lies Colmenar, and it shares its southern border with Riogordo and Periana.

Geographic entities mentioned:
surface_form: Sierra de Alhama
instance_of: Mountain
countries: Spain
coordinates: lat: 36.98118
lon: -4.195087
Leila Esfandyari. Leila Esfandyari (; February 16, 1971 – July 22, 2011) was an Iranian climber. Esfandyari was the first Iranian woman to reach the summit of Nanga Parbat in the Himalayas, the world’s ninth highest peak with an altitude of 8,125 metres and one of the deadliest peaks.

Geographic entities mentioned:
surface_form: Nanga Parbat
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.239166666667
lon: 74.59
Education and career. Leila Esfandyari was born on February 16, 1971, in Karaj, Pahlavi Iran (now Iran). She was raised and educated in Tehran, Iran, receiving a bachelor's degree in microbiology. She worked as a microbiologist in a Tehran hospital before she left her job to climb K2 in the Himalayas in 2010. Death.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
She worked as a microbiologist in a Tehran hospital before she left her job to climb K2 in the Himalayas in 2010. Death. On July 22, 2011, she completed the ascent to Gasherbrum II, one of the highest peaks in the Karakoram range of the Himalayas. Minutes after, on the way down, her foot slipped on the ice and she fell 300 meters down the mountain.

Geographic entities mentioned:
surface_form: Gasherbrum II
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.7575
lon: 76.652777777778
state of Maryland. US 40 Scenic, which is known for most of its route as National Pike, is the old alignment of US 40 over Town Hill in eastern Allegany County and Sideling Hill in far western Washington County. The highway was originally constructed as part of a turnpike connecting Baltimore with the eastern end of the National Road at Cumberland in the early 19th century.

Geographic entities mentioned:
surface_form: Sideling Hill
instance_of: Mountain
countries: United States
coordinates: lat: 39.7192
lon: -78.2836
Deer Mountain (Alaska). Deer Mountain is a mountain peak located in the Tongass National Forest in the Ketchikan Gateway Borough, Alaska, which dominates the skyline behind downtown Ketchikan.

Geographic entities mentioned:
surface_form: deer mountain (alaska)
instance_of: Mountain
countries: United States
coordinates: lat: 55.343611111111
lon: -131.59944444444
surface_form: deer mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.025555555556
lon: -74.873333333333
surface_form: deer mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.842222222222
lon: -115.47111111111
Deer Mountain (Alaska). Deer Mountain is a mountain peak located in the Tongass National Forest in the Ketchikan Gateway Borough, Alaska, which dominates the skyline behind downtown Ketchikan.

Geographic entities mentioned:
surface_form: deer mountain
instance_of: Mountain
countries: United States
coordinates: lat: 55.343611111111
lon: -131.59944444444
surface_form: deer mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.025555555556
lon: -74.873333333333
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: deer mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.842222222222
lon: -115.47111111111
The Deer Mountain National Recreation Trail provides a strenuous hiking route to the summit, passing through temperate rainforests, muskeg and alpine meadows as it gains of elevation over from the trailhead in Ketchikan to the peak.

Geographic entities mentioned:
surface_form: deer mountain
instance_of: Mountain
countries: United States
coordinates: lat: 55.343611111111
lon: -131.59944444444
surface_form: deer mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.025555555556
lon: -74.873333333333
surface_form: deer mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.842222222222
lon: -115.47111111111
Cult. While not one of the most popular divinities, Mnemosyne was the subject of some minor worship in Ancient Greece. Statues of her are mentioned in the sanctuaries of other gods, and she was often depicted alongside her daughters the Muses. She was also worshipped in Lebadeia in Boeotia, at Mount Helicon in Boeotia, and in the cult of Asclepius. Cult of Asclepius.

Geographic entities mentioned:
surface_form: Mount Helicon
instance_of: Mountain
countries: Greece
coordinates: lat: 38.352222222222
lon: 22.825
Whistlefield Inn. The Whistlefield Inn is a Category C listed building in Whistlefield, Argyll and Bute, Scotland, about twelve miles northwest of Dunoon. Built in 1663, it was originally a drover's inn on the route between Strachur and Ardentinny. It sits about from the eastern shores of Loch Eck. Today, it is an inn and restaurant. The business came under new management in September 2018.

Geographic entities mentioned:
surface_form: Loch Eck
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.08329
lon: -4.99346
Barra Strait Bridge. The Barra Strait Bridge is a Canadian road bridge crossing the Barra Strait of Bras d'Or Lake, carrying Nova Scotia Route 223 between Iona, Victoria County, on the West side, and Grand Narrows, Cape Breton County (Cape Breton Regional Municipality) on the east side.

Geographic entities mentioned:
surface_form: Bras d'Or Lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.860277777778
lon: -60.778888888889
Barcenillas, Camino del Colmenar, Campos Elíseos, Cañada de los Ingleses, Capuchinos, Centro Histórico, Conde de Ureña, Cristo de la Epidemia, El Bulto, El Ejido, El Molinillo, Ensanche Centro, Explanada de la Estación, La Aurora, La Goleta, La Manía, La Merced, La Trinidad, La Victoria, Lagunillas, Los Antonios, Mármoles, Monte de Gibralfaro, Olletas, Parque Ayala, Perchel Norte, Perchel Sur, Pinares de Olletas, Plaza de Toros Vieja, Polígono Alameda, R.E.N.F.E., San Miguel, Santa Amalia, Segalerva, Seminario, Sierra Blanquilla y Ventaja Alta.

Geographic entities mentioned:
surface_form: Monte de Gibralfaro
instance_of: Mountain
countries: Spain
coordinates: lat: 36.72333333
lon: -4.41083333
Although Bapchule is unincorporated, it has a post office (P.O. Boxes only) with the ZIP code of 85121. It lies in the Gila River Indian Community, south of the Phoenix Metropolitan Area. Most of Bapchule is located in Pinal County, while a portion of it in the north is in Maricopa County. The Bapchule locality is geographically situated at a southern coordinate to the Gila River Valley. History.

Geographic entities mentioned:
surface_form: Gila River Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.18339
lon: -110.21731
He earned the title of &quot;Baron of Duprat&quot;. He was elected as councilor and later Mayor of Sao Paulo. His mandate as mayor was marked by an acccelaration of modernization and urbanization in the city of Sao Paulo. The works that were most important out of his mandate were the construction of the Parque Trianon, the Santa Ifigenia Viaduct, and the urbanization of the Anhagabau Valley.

Geographic entities mentioned:
surface_form: Anhagabau Valley
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
Lagoa de Óbidos. The Lagoa de Óbidos is the largest coastal lagoon system on the Portuguese coast. It has a total area of approximately and an average depth of, with depths ranging from to. It is located in the Oeste region and it is bordered by the municipality of Caldas da Rainha to the north and by the municipality of Óbidos to the south.

Geographic entities mentioned:
surface_form: lagoa de óbidos
instance_of: Lake
countries: Portugal
coordinates: lat: 39.40969
lon: -9.20775
Ecosystem. As a coastal lagoon system, the Lagoa de Óbidos holds high ecological value due to its productive characteristics, particularly in terms of ecosystem and species biodiversity. It is home to a variety of faunal and floral species and serves as an important habitat for birdlife, including migratory species that can be observed throughout the year.

Geographic entities mentioned:
surface_form: lagoa de óbidos
instance_of: Lake
countries: Portugal
coordinates: lat: 39.40969
lon: -9.20775
Naejangsan National Park. Naejangsan National Park () is located in the provinces of Jeollabuk-do and Jeollanam-do, South Korea. It was designated as the 8th national park in 1971. It is named after the mountain Naejangsan. The park is home to a total of 919 plant species and 1,880 animal species. 12 of the animals are endangered.

Geographic entities mentioned:
surface_form: Naejangsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.483333333333
lon: 126.88333333333
He greatly expanded by establishing himself as a merchant and shipowner in Kristiansand. During the Great Northern War (1700–1721), he controlled large parts of the timber trade from the valley of Mandalen. He also continued in a few more years to sail as skipper on his own ships. As the dominant employer, merchant, creditor and landowner in Mandal, he ran the small town almost like a business.

Geographic entities mentioned:
surface_form: Mandalen
instance_of: Valley
countries: Norway
coordinates: lat: 58.38
lon: 7.52777778
Mount Lowe Railway. The Mount Lowe Railway was the third in a series of scenic mountain railroads in the United States created as a tourist attraction on Echo Mountain and Mount Lowe, north of Los Angeles, California. The railway, originally incorporated by Thaddeus S. C. Lowe as the Pasadena and Mt.

Geographic entities mentioned:
surface_form: Echo Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.2111
lon: -118.121
Mountain Division. The Mountain Division, originally built as a narrow-gauge line, began with a trolley that ascended Lake Avenue to a turnoff near Las Flores Street, along a private right-of-way through the Poppyfields district, and proceeded into Rubio Canyon to the foot of Echo Mountain.

Geographic entities mentioned:
surface_form: Echo Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.2111
lon: -118.121
Snagov Declaration. The Snagov Declaration () was a declaration signed on 21 June 1995 by the leaders of the parliamentary parties in Romania at the time committing to a strategy aimed at Romania's accession to the European Union (EU). The declaration is named after Lake Snagov, as it was signed in a villa on its shore.

Geographic entities mentioned:
surface_form: Lake Snagov
instance_of: Lake
countries: Romania
Socialist Republic of Romania
Romanian People's Republic
Principality of Wallachia
Kingdom of Romania
United Principalities of Moldavia and Wallachia
coordinates: lat: 44.73
lon: 26.18