Sarmila/GeoWiki-Features huggingface dataset:
James Gordon Stuart Grant. James Gordon Stuart Grant (1834 &ndash; 27 February 1902) was a New Zealand demagogue, journalist and eccentric. He was born in Glenlivet, Banffshire, Scotland in circa 1834. He unsuccessfully stood in the 1859 Town of Dunedin by-election against James Macandrew.

Geographic entities mentioned:
surface_form: Glenlivet
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.349166666667
lon: -3.3319444444444
Course. The Colo River rises on the Great Dividing Range, northeast of Newnes, formed by the confluence of the Wolgan River and the Capertee River, which respectively drain the Wolgan and Capertee Valleys north of Lithgow. Colo River flows eastwards and then south through a deep gorge in the northern section of the Blue Mountains. The majority of the river lies in Wollemi National Park.

Geographic entities mentioned:
surface_form: Wolgan
instance_of: Valley
countries: Australia
coordinates: lat: -33.24638888888889
lon: 150.1597222
surface_form: Capertee
instance_of: Valley
countries: Australia
coordinates: lat: -33.0483
lon: 150.134
Mugere Hydroelectric Power Station. MugereHydroelectric Power Station () is an run-of-the-river hydroelectric power station in the Bujumbura Rural Province of Burundi. Location. The 8 MW Mugere Hydroelectric Power Station is in the Commune of Kabezi, Bujumbura Rural Province. It is along the Mugere River. The plant is south of Bujumbura. It delivers 40 GWh per year.

Geographic entities mentioned:
surface_form: Mugere River
instance_of: Watercourse
countries: Burundi
coordinates: lat: -3.4839
lon: 29.3347
The landslides generate plumes of ash-rich water which can spread kilometres from the volcano. Such plumes are a unique trait of volcanism at NW Rota-1 and have been identified at Kavachi, Monowai, NW Rota-1 and West Mata submarine volcanoes. One such landslide took place on 14 August 2009 and removed debris that had accumulated around Brimstone Pit as well as the southern parts of the summit.

Geographic entities mentioned:
surface_form: West Mata
instance_of: Mountain
countries: Tonga
coordinates: lat: -15.101
lon: -173.759
surface_form: nw rota-1
instance_of: Mountain
countries: United States
coordinates: lat: 14.60111111
lon: 144.775
The volcano has repeatedly been targeted by dives of ROVs. Hydrophones have been placed at the summit and vent during several dives. NW Rota-1 is also known as &quot;Northwest Rota-1&quot;. NW Rota-1 is the first volcano where submarine explosive eruptions were directly observed, in 2004.

Geographic entities mentioned:
surface_form: northwest rota
instance_of: Mountain
countries: United States
coordinates: lat: 14.60111111
lon: 144.775
surface_form: nw rota-1
instance_of: Mountain
countries: United States
coordinates: lat: 14.60111111
lon: 144.775
NW Rota-1. NW Rota-1 is a seamount in the Mariana Islands, northwest of Rota, which was discovered through its hydrothermal activity in 2003. The volcano has been observed to be erupting underwater, the first time that submarine explosive eruptions have been directly witnessed. The summit of the seamount lies at below sea level, with a ridge capping off the seamount.

Geographic entities mentioned:
surface_form: nw rota-1
instance_of: Mountain
countries: United States
coordinates: lat: 14.60111111
lon: 144.775
Eruptions have been recorded in 2008–2010 and took the form of Strombolian eruptions with the emission of lava and large amounts of tephra. The erupted material is unstable and forms sediment flows and landslides; one large landslide occurred on 14 August 2009 and stripped part of the southern flank of NW Rota-1.

Geographic entities mentioned:
surface_form: nw rota-1
instance_of: Mountain
countries: United States
coordinates: lat: 14.60111111
lon: 144.775
Such landslides generate ash plumes underwater and are similar to large landslides at other active submarine volcanoes. The activity gives rise to intense hydrothermal plumes, which contain droplets of molten sulfur and bubbles of carbon dioxide, among other compounds. It is estimated that NW Rota-1 releases 400,000 ± 100,000 tonne/year of carbon dioxide.

Geographic entities mentioned:
surface_form: nw rota-1
instance_of: Mountain
countries: United States
coordinates: lat: 14.60111111
lon: 144.775
Compared to ocean island volcanoes, these volcanoes are longer lived and produce more gas-rich magma. The Mariana Arc contains 52-60 submarine volcanoes, about five times more than rise above sea level. At least 20 volcanoes including NW Rota-1 are hydrothermally active. The islands Guam, Rota and Saipan are uplifted parts of the forearc. NW Rota-1 is part of South Mariana Seamount Province.

Geographic entities mentioned:
surface_form: nw rota-1
instance_of: Mountain
countries: United States
coordinates: lat: 14.60111111
lon: 144.775
This &quot;cross-chain&quot; is perpendicular to the main volcanic arc and is correlated to a slab discontinuity. The cross-chain lies in an area of crustal extension. Another volcano close to NW Rota-1 is Chaife, about east-northeast of the former. Esmeralda Bank and the caldera West Rota lie northwest and due south of NW Rota-1, respectively.

Geographic entities mentioned:
surface_form: nw rota-1
instance_of: Mountain
countries: United States
coordinates: lat: 14.60111111
lon: 144.775
The cross-chain lies in an area of crustal extension. Another volcano close to NW Rota-1 is Chaife, about east-northeast of the former. Esmeralda Bank and the caldera West Rota lie northwest and due south of NW Rota-1, respectively. There might be a shallow magma chamber at NW Rota-1, which could explain the vigorous hydrothermal activity. Composition.

Geographic entities mentioned:
surface_form: nw rota-1
instance_of: Mountain
countries: United States
coordinates: lat: 14.60111111
lon: 144.775
Volcanic rocks are porphyritic and contain many vesicles. The magma erupted at NW Rota-1 is among the most water rich of the entire Mariana Arc. The formation of NW Rota-1 magmas appears to involve the melting of subducted, water-bearing sediments and the interaction of the resulting melts with the mantle wedge. Back-arc may also play a role.

Geographic entities mentioned:
surface_form: nw rota-1
instance_of: Mountain
countries: United States
coordinates: lat: 14.60111111
lon: 144.775
A larger animal community has been found at the northwestern summit; it includes amphipods, anenomes, copepods, crabs, fish, isopods, jellyfish, ostracods and polychaetes. The caridean shrimp &quot;Alvinocaris marimonte&quot; was discovered from populations on NW Rota-1, Myojin Knoll and NW Eifuku seamount. The animals found at NW Rota-1 and NW Eifuku have a distinct appearance.

Geographic entities mentioned:
surface_form: nw rota-1
instance_of: Mountain
countries: United States
coordinates: lat: 14.60111111
lon: 144.775
surface_form: nw rota-1
instance_of: Mountain
countries: United States
coordinates: lat: 14.60111111
lon: 144.775
Spring Creek (Bryant Creek tributary). Spring Creek is a stream in southern Douglas and northern Ozark counties in the Ozarks of southern Missouri. It is a tributary to Bryant Creek. The source is a hillside spring just south of Missouri Route N in Douglas County and the confluence with Bryant is in southern Douglas County just west of a bluff below Missouri Route 95.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Timeline and location. From its establishment in 2013, Center for Underground Physics (CUP) of the Institute for Basic Science had been planning the creation of a deep underground laboratory. Approximately three years later, the search was narrowed to sites under mountains Yemisan and Dutasan both located in Gangwon Province, South Korea. As Mt.

Geographic entities mentioned:
surface_form: Dutasan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.26
lon: 129.1
The rivers and basins it can be found in include, but are not limited to: the Amazonas estuaries and the main channel, Apure, Araguaia, Atrato, Beni-Madre de Dios, Branco, Cauca-Magdalena-Sinu, Coppename, Suriname, Saramacca, Corentyne-Demerara, Essequibo, Guapore, Itapicuru-Mearim, lapura, middle-lower Madeira, Mamore, Maroni-Approuague, Oiapoque, Orinoco (upper and lower), Parnaiba, Purus, Putumayo, upper Tocantins, Ucayali, and upper Xingu.

Geographic entities mentioned:
surface_form: Sinu
instance_of: Watercourse
countries: Colombia
coordinates: lat: 8.75825
lon: -75.88811111111112
It should be distinguished from the less ornate Miriam ossuary, which came to light in June 2011. The latter is a looted, though authenticated artifact from the Valley of Elah, bearing the inscription: &quot;Miriam daughter of Yeshua son of Caiapha, priest of Ma’azya from Beit Imri&quot;. The chamber tomb was discovered by construction workers in November 1990.

Geographic entities mentioned:
surface_form: Valley of Elah
instance_of: Valley
countries: Israel
coordinates: lat: 31.6806252
lon: 34.9891247
One very ornate ossuary contained the bones of two infants, two teenage boys, an adult woman and a man of about 60. Besides the detailed etching, there were traces of bright orange paint. It was inscribed &quot;Yehosef bar Qayafa&quot; on the long side, and &quot;Yehosef bar Qafa&quot; on the narrow side. The bones were eventually reburied on the Mount of Olives. Background.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
More generally, the contents of the burial cave increase knowledge of ossuary inscriptions and burial customs of the Second Temple period. In June 2011, archaeologists from Bar-Ilan and Tel Aviv Universities announced the recovery of a stolen ossuary, plundered from a tomb in the Valley of Elah.

Geographic entities mentioned:
surface_form: Valley of Elah
instance_of: Valley
countries: Israel
coordinates: lat: 31.6806252
lon: 34.9891247
These forest areas were categorized as Protected Landscape under the National Integrated Protected Area System (NIPAS) and the rest, unclassified forest (Non-NIPAS). A total of are located within the Mounts Palay-Palay–Mataas-na-Gulod Protected Landscape, a protected area in Ternate and Maragondon created by Proclamation Number 1594 on October 26, 1976.

Geographic entities mentioned:
surface_form: Mounts Palay-Palay–Mataas-na-Gulod Protected Landscape
instance_of: Mountain
countries: Philippines
coordinates: lat: 14.2156
lon: 120.653
A total of are located within the Mounts Palay-Palay–Mataas-na-Gulod Protected Landscape, a protected area in Ternate and Maragondon created by Proclamation Number 1594 on October 26, 1976. The park lies at the border of Cavite and Batangas and encompasses three peaks, Palay-Palay, Pico de Loro and Mataas na Gulod.

Geographic entities mentioned:
surface_form: Pico de Loro
instance_of: Mountain
countries: Philippines
coordinates: lat: 14.21427
lon: 120.64645
Seafoods, fruits, coffee, organic vegetables, tinapa, handicrafts, ornamental plants also abound in the province. Mountain climbing is also one of the outdoor activities in Cavite. This includes Mount Pico De Loro which is within the towns of Ternate and Maragondon (and some parts of it are already part of Batangas), which is a part of the Palay-Palay and Mataas na Gulod protected landscape. Mt.

Geographic entities mentioned:
surface_form: Mount Pico De Loro
instance_of: Mountain
countries: Philippines
coordinates: lat: 14.21427
lon: 120.64645
Marigny was at one point a candidate in the special gubernatorial election of 1830, but ultimately he was not on the ballot. North shore activities. Marigny's land holdings included a sugarcane plantation on the north shore of Lake Pontchartrain. This region is Saint Tammany Parish, one of the Florida Parishes, lands acquired by the U.S. in 1810, prior to Louisiana's transition to statehood.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
Main campus (Corvallis). The, tree-lined main campus serves as an internationally recognized arboretum and the centerpiece of Corvallis, Oregon. The campus is 83 miles south of Portland, near the middle of the state's Willamette Valley. Much of the main campus was designed by landscape architect John Charles Olmsted in 1906.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Fifes Peaks. Fifes Peaks is a compact group of summits and spires from an eroded volcanic cone located in Yakima County in Washington state. Fifes Peaks is situated in the Cascade Range on the east side of the crest, within the Norse Peak Wilderness.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: fifes peaks
instance_of: Landform
countries: United States
coordinates: lat: 46.9737
lon: -121.3229
Fifes Peaks. Fifes Peaks is a compact group of summits and spires from an eroded volcanic cone located in Yakima County in Washington state. Fifes Peaks is situated in the Cascade Range on the east side of the crest, within the Norse Peak Wilderness.

Geographic entities mentioned:
surface_form: fifes peaks
instance_of: Landform
countries: United States
coordinates: lat: 46.9737
lon: -121.3229
Fifes Peaks is a compact group of summits and spires from an eroded volcanic cone located in Yakima County in Washington state. Fifes Peaks is situated in the Cascade Range on the east side of the crest, within the Norse Peak Wilderness. The Fifes Peaks are remnants of a now extinct caldera which exploded 25 million years ago with volcanic activity extending from 20 to 30 million years ago.

Geographic entities mentioned:
surface_form: fifes peaks
instance_of: Landform
countries: United States
coordinates: lat: 46.9737
lon: -121.3229
Fifes Peaks is situated in the Cascade Range on the east side of the crest, within the Norse Peak Wilderness. The Fifes Peaks are remnants of a now extinct caldera which exploded 25 million years ago with volcanic activity extending from 20 to 30 million years ago. History. Fifes Peaks were named for Thomas X. Fife (1853–1922), a placer miner.

Geographic entities mentioned:
surface_form: fifes peaks
instance_of: Landform
countries: United States
coordinates: lat: 46.9737
lon: -121.3229
The Fifes Peaks are remnants of a now extinct caldera which exploded 25 million years ago with volcanic activity extending from 20 to 30 million years ago. History. Fifes Peaks were named for Thomas X. Fife (1853–1922), a placer miner. Thomas, his brothers, and their father, John, mined in the area near Chinook Pass. Tom homesteaded at Goose Prairie, near Bumping Lake.

Geographic entities mentioned:
surface_form: fifes peaks
instance_of: Landform
countries: United States
coordinates: lat: 46.9737
lon: -121.3229
Tom homesteaded at Goose Prairie, near Bumping Lake. Camp Fife, the Boy Scout Camp at Goose Prairie, also honors Tom Fife because he willed the land to the Boy Scouts. Climate. Fifes Peaks are located east of the Cascade crest. Most weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains.

Geographic entities mentioned:
surface_form: fifes peaks
instance_of: Landform
countries: United States
coordinates: lat: 46.9737
lon: -121.3229
During winter months, weather is usually cloudy, but due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Precipitation runoff from Fifes Peaks drains into tributaries of the American River and Naches River.

Geographic entities mentioned:
surface_form: fifes peaks
instance_of: Landform
countries: United States
coordinates: lat: 46.9737
lon: -121.3229
History. Fifes Peaks were named for Thomas X. Fife (1853–1922), a placer miner. Thomas, his brothers, and their father, John, mined in the area near Chinook Pass. Tom homesteaded at Goose Prairie, near Bumping Lake. Camp Fife, the Boy Scout Camp at Goose Prairie, also honors Tom Fife because he willed the land to the Boy Scouts. Climate. Fifes Peaks are located east of the Cascade crest.

Geographic entities mentioned:
surface_form: brothers
instance_of: Mountain
countries: United States
coordinates: lat: 47.6537193
lon: -123.140575
Bergisel Ski Jump. The Bergisel Ski Jump (), whose stadium has a capacity of 26,000, is a ski jumping hill located in Bergisel in Innsbruck, Austria. It is one of the more important venues in the FIS Ski Jumping World Cup, annually hosting the third competition of the prestigious Four Hills Tournament. Its first competitions were held in the 1920s using simple wood constructions.

Geographic entities mentioned:
surface_form: Bergisel
instance_of: Mountain
countries: Austria
coordinates: lat: 47.246666666667
lon: 11.399722222222
On 5 August 1906, another listing incident occurred, which resulted in complaints filed against the Chicago-South Haven Line that had purchased the ship earlier that year. Before the 1907 season, the ship was sold to the Lake Shore Navigation Company and moved to Lake Erie.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Josephine Flood argued, on the basis of a note in Alfred William Howitt, that they were attested as far south as the upper Murray site of Kauwambal between Mount Kosciuszko and Mount Cobberas, which would place their summer camping somewhat west of the Djilamatang.

Geographic entities mentioned:
surface_form: Mount Kosciuszko
instance_of: Mountain
countries: Australia
coordinates: lat: -36.4558303
lon: 148.2635105
2020 Kashmiri protests. The 2020 Kashmiri protests was a series of violent demonstrations and massive general strikes between April-December 2020 in the Kashmir Valley of Jammu and Kashmir, India which demanded an end to the 2019-2021 Jammu and Kashmir lockdown.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
She also had a lucky escape on 19 January when &quot;Kosmos II&quot; (headed by Captain Einar Gleditsch from Sandefjord Norway) tried to ram the boat off Oregon Inlet. At one point the ship was only away from the German submarine which had an inoperable diesel engine.

Geographic entities mentioned:
surface_form: Oregon Inlet
instance_of: Landform
countries: United States
coordinates: lat: 35.77463889
lon: -75.53136111
He finished a distant third of three candidates. (His candidacy may have secured the seat to the Conservative candidate as it likely split the Liberal vote and the Conservative got the seat although he did not receive a majority of the votes.)
After leaving office, Bredin returned to farming and fur trading around Lesser Slave Lake.

Geographic entities mentioned:
surface_form: Lesser Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.440556
lon: -115.488611
Casiri is also known as Paucarani or Paugarani, although Casiri and Paucarani are sometimes treated as distinct volcanoes. A lake with the name &quot;Casiri&quot; lies about north from the volcano; it is a glacial lake and a reservoir which drains into the Mauri River through the Quebrada Chungara and Rio Kallapuma. Geography and geomorphology.

Geographic entities mentioned:
surface_form: Mauri River
instance_of: Watercourse
countries: Bolivia
Peru
coordinates: lat: -17.140278
lon: -70.015278
surface_form: chungara
instance_of: Mountain
countries: Peru
coordinates: lat: -15.3972
lon: -71.5903
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
Geologically, Casiri is considered to be part of the so-called &quot;Paucarani Volcanics&quot;. Hydrology and Paucarani reservoir. The Rio Uchusuma, a tributary of the Rio Mauri, originates on Casiri. A natural lake called Paucarani or Paucarini is on the southeastern foot of Casiri, and is an important bird site. The Quebrada Achuco valley is located south of Casiri, accompanied by wetlands.

Geographic entities mentioned:
surface_form: Rio Mauri
instance_of: Watercourse
countries: Bolivia
Peru
coordinates: lat: -17.140278
lon: -70.015278
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
The Quebrada Achuco valley is located south of Casiri, accompanied by wetlands. On the other side, the southeastward-flowing Quebrada Mamuta lies to the north and northeast of the volcano, and to the northwest lie streams which flow through the lake Casiri and the lake Liñuma into the Rio Mauri. Volcanic activity has influenced the drainages through the formation of lava dams, altering watersheds.

Geographic entities mentioned:
surface_form: Rio Mauri
instance_of: Watercourse
countries: Bolivia
Peru
coordinates: lat: -17.140278
lon: -70.015278
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
This reservoir, which is run by the Junta de Usuarios del Valle de Tacna, has a capacity of of water and is a key part of the water supply of Tacna; water is transferred from the Paucarani reservoir through the Canal Uchusuma to Tacna, covering 90% of Tacna's water consumption for both irrigation and human use. The Paucarani reservoir is also involved in the regulation of the Rio Caplina.

Geographic entities mentioned:
surface_form: Rio Caplina
instance_of: Watercourse
countries: Peru
coordinates: lat: -18.300327
lon: -70.443451
surface_form: rio caplina
instance_of: Watercourse
countries: Peru
coordinates: lat: -18.300327
lon: -70.443451
surface_form: caplina
instance_of: Watercourse
countries: Peru
coordinates: lat: -18.300327
lon: -70.443451
The Central Volcanic Zone includes the volcanoes of southern Peru, a country with over 300 volcanoes. Of these, El Misti, Huaynaputina, Sabancaya, Ticsani, Tutupaca, Ubinas and Yucamane have been active during historical time. There are also geothermal manifestations such as fumaroles, geysers and hot springs in the country. Despite the activity, volcanism in Peru is poorly known. Composition.

Geographic entities mentioned:
surface_form: Huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223
surface_form: Ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
surface_form: Tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: Ubinas
instance_of: Mountain
countries: Peru
coordinates: lat: -16.34861111111111
lon: -70.90222222222222
surface_form: Yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: ubinas
instance_of: Mountain
countries: Peru
coordinates: lat: -16.34861111111111
lon: -70.90222222222222
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
Casiri (Tacna). Casiri, also known as Paucarani, is an about high complex volcano in the Barroso mountain range of the Andes, in the Tacna Region of Peru. It consists of four individual volcanic edifices with lava domes; the southeasternmost edifice has been active during the Holocene, producing thick lava flows that have overrun moraines of Pleistocene age.

Geographic entities mentioned:
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri (tacna)
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
Casiri (Tacna). Casiri, also known as Paucarani, is an about high complex volcano in the Barroso mountain range of the Andes, in the Tacna Region of Peru. It consists of four individual volcanic edifices with lava domes; the southeasternmost edifice has been active during the Holocene, producing thick lava flows that have overrun moraines of Pleistocene age.

Geographic entities mentioned:
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
surface_form: barroso
instance_of: Mountain
countries: Peru
coordinates: lat: -17.556308
lon: -69.5954717
There are two sulfur mines on the volcano, and the Paucarani reservoir that contains the bulk of Tacna's water supply is associated with Casiri: The Rio Uchusuma that flows through the reservoir originates on the volcano and the reservoir is located on the foot of Casiri. Name. The name &quot;Casiri&quot; might mean &quot;bawler&quot; in Aymara.

Geographic entities mentioned:
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
Name. The name &quot;Casiri&quot; might mean &quot;bawler&quot; in Aymara. Casiri is also known as Paucarani or Paugarani, although Casiri and Paucarani are sometimes treated as distinct volcanoes. A lake with the name &quot;Casiri&quot; lies about north from the volcano; it is a glacial lake and a reservoir which drains into the Mauri River through the Quebrada Chungara and Rio Kallapuma.

Geographic entities mentioned:
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
Name. The name &quot;Casiri&quot; might mean &quot;bawler&quot; in Aymara. Casiri is also known as Paucarani or Paugarani, although Casiri and Paucarani are sometimes treated as distinct volcanoes. A lake with the name &quot;Casiri&quot; lies about north from the volcano; it is a glacial lake and a reservoir which drains into the Mauri River through the Quebrada Chungara and Rio Kallapuma.

Geographic entities mentioned:
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
Casiri is a high stratovolcano with lava domes in the Palca district of Peru, close to the border with Chile. There are five or four individual volcanic edifices at Casiri: three older ones that form a 5 kilometre-long chain, and a southeasterly younger edifice with a well preserved lava dome in its crater which is breached to the south. An older lava dome lies in the western part of the complex.

Geographic entities mentioned:
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
An older lava dome lies in the western part of the complex. The whole Casiri volcano grew on the southern flanks of older volcanoes and rises about above the surrounding terrain. The edifice has a volume of about, with a diameter of. A cirque with a rock glacier is developed on a summit northeast from the main Casiri complex. Close to the Paucarani reservoir is a debris avalanche deposit.

Geographic entities mentioned:
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
Some parts of the volcano underwent hydrothermal alteration, producing gray-white rocks and clay, and wind-blown ash covers part of the lava flows. Casiri is part of the mountain range; generally, the terrain around Casiri is dominated by various volcanic and fluvioglacial formations along with some moraines.

Geographic entities mentioned:
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
Casiri is part of the mountain range; generally, the terrain around Casiri is dominated by various volcanic and fluvioglacial formations along with some moraines. The mountain chains Barroso and Huancune lie southwest and south from Casiri, respectively, and the neighbouring mountains Auquitapie and Iñuma are covered with snow.

Geographic entities mentioned:
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: iñuma
instance_of: Mountain
countries: Peru
coordinates: lat: -17.4606
lon: -69.8383
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
surface_form: huancune
instance_of: Mountain
countries: Peru
coordinates: lat: -17.5952
lon: -69.7893
Geologically, Casiri is considered to be part of the so-called &quot;Paucarani Volcanics&quot;. Hydrology and Paucarani reservoir. The Rio Uchusuma, a tributary of the Rio Mauri, originates on Casiri. A natural lake called Paucarani or Paucarini is on the southeastern foot of Casiri, and is an important bird site. The Quebrada Achuco valley is located south of Casiri, accompanied by wetlands.

Geographic entities mentioned:
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
Human geography. Casiri is located in the Tarata Province of the Tacna Region of Peru; it lies about northeast from the city of Tacna and close to the border with Chile and Bolivia. The volcano is situated north of the town of Paucarani; other human structures in the area south of Casiri are Calachata and Tulipiña.

Geographic entities mentioned:
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
Holocene lavas sourced from fissure vents overlie Pleistocene-age moraines and are uneroded; radiometric dating on the volcano has yielded ages of 50,000 years and surface exposure dating has found ages of 6,000 ± 900 and 2,600 ± 400 years for two dark lava flows southwest and south of Casiri's main summit, respectively.

Geographic entities mentioned:
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
There are no reported eruptions, but activity may or may not have occurred in historical time; there are hot springs and solfataras that are probably powered by Casiri's magmatic system. Casiri has been classified as a latent or potentially active volcano with a moderate threat level. Earthquakes in 2020 and 2021 in the area do not appear to relate to volcanic activity.

Geographic entities mentioned:
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
Earthquakes in 2020 and 2021 in the area do not appear to relate to volcanic activity. In 2012, the Geophysical Institute in Peru announced that it would begin monitoring Casiri, along with two other volcanoes in southern Peru, with seismometers. They consider it a &quot;low hazard&quot; volcano., there are two seismometers and one instrument measuring the deformation of the volcano at Casiri.

Geographic entities mentioned:
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
The installation of a network to detect deformation of the volcano is supposed to begin in 2022. Human use. The Casiri volcanic complex and surrounding mountains have been prospected for potential geosites. Mining. The Gloria sulfur mine lies on Casiri – specifically, on the foot of Paucarani and southeast from the lava flows.

Geographic entities mentioned:
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
Mining. The Gloria sulfur mine lies on Casiri – specifically, on the foot of Paucarani and southeast from the lava flows. The sulfur is contained in heavily altered rocks covering an area of about and is genetically related to the activity of Casiri. It has been excavated through trenches and wells; some installations could still be exploitable.

Geographic entities mentioned:
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
It has been excavated through trenches and wells; some installations could still be exploitable. Another mine known as San Luis may also be associated with Paucarani; it is located on the northwestern flank. Precious metals might occur in the hydrothermally altered areas at Casiri. Geothermal power.

Geographic entities mentioned:
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
Ogawayama. is a 2,418m tall mountain on the border of Nagano and Yamanashi prefectures in Japan. It is a famous rock climbing area. The rock in Ogawayama consists of granite. Some famous boulders can be found in Ogawayama. Such as Captain Ahab, the first boulder problem opened in Japan in 1980, and the notorious slab boulder. There is multipitch climbing up to 9 pitches.

Geographic entities mentioned:
surface_form: ogawayama
instance_of: Mountain
countries: Japan
coordinates: lat: 35.90916667
lon: 138.61222222
is a 2,418m tall mountain on the border of Nagano and Yamanashi prefectures in Japan. It is a famous rock climbing area. The rock in Ogawayama consists of granite. Some famous boulders can be found in Ogawayama. Such as Captain Ahab, the first boulder problem opened in Japan in 1980, and the notorious slab boulder. There is multipitch climbing up to 9 pitches. The routes are generally not bolted.

Geographic entities mentioned:
surface_form: ogawayama
instance_of: Mountain
countries: Japan
coordinates: lat: 35.90916667
lon: 138.61222222
Svartfjellet, Kvaløya. or is the highest mountain on the island of Kvaløya in Finnmark county, Norway. The tall summit lies in Hammerfest Municipality, about southeast of the town of Hammerfest.

Geographic entities mentioned:
surface_form: svartfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 70.232777777778
lon: 21.998611111111
surface_form: svartfjellet, kvaløya
instance_of: Mountain
countries: Norway
coordinates: lat: 70.584166666667
lon: 23.859166666667
The loss of the mill shrunk the town, and since that time it has served mainly as a tourist destination due to its beaches and Van Damme State Park, which the Little River runs through. The first road that ran through this area was the Anderson Valley and Big River Wagon Road. This road was likely widened and altered over the years until it was eventually added to the State Highway System.

Geographic entities mentioned:
surface_form: Anderson Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.06
lon: -123.43
One of the chain of four shihans in the vicinity of the Ishimbay and Sterlitamak cities. Along with Toratau, Yuraktau and Kushtau, which are selected in the short list of the project &quot;Seven Wonders of Russia&quot; (as well Shihany). The name &quot;Shakhtau&quot; is known to the Balkarians and Karachais, so they call Elbrus.

Geographic entities mentioned:
surface_form: Yuraktau
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.741666666667
lon: 56.0975
surface_form: Kushtau
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.7
lon: 56.083333333333
Like the other shihans, the remainder of the Permian period (late Paleozoic) reef massif formed over 230 million years ago in the tropical sea. Now the mountain is completely destroyed as a result of geological work to obtain raw materials for Bashkir soda company; in place of the shihan is a quarry. The fate of Shakhtau can comprehend several similar shihans.

Geographic entities mentioned:
surface_form: shihan
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.689781
lon: 56.077161
History. A detailed study of the mountain began in the 19th century. Vannheim von Kvalan in 1842 published the first information about the Shihan. Earlier (1841), Schachtau was visited by Roderick Murchison and Edmund Verney, who compiled a profile through Shakhtau in the form of a brachyanticlinal fold, complicated by a fault. Subsequently, paleontological materials on shihan were processed by S.

Geographic entities mentioned:
surface_form: shihan
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.689781
lon: 56.077161
History. A detailed study of the mountain began in the 19th century. Vannheim von Kvalan in 1842 published the first information about the Shihan. Earlier (1841), Schachtau was visited by Roderick Murchison and Edmund Verney, who compiled a profile through Shakhtau in the form of a brachyanticlinal fold, complicated by a fault. Subsequently, paleontological materials on shihan were processed by S.

Geographic entities mentioned:
surface_form: shakhtau
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.649722222222
lon: 56.0825
The similarity of Shakhtau and the buried oil and gas bearing arrays made him turn to many stratigraphs. During the war years, geologists from the Bashkir oil expedition of the USSR Academy of Sciences repeatedly turned to shihan to find out the features of the facies and the history of the formation of oil and gas bearing burials of massifs Ishimbayskoye Priuralie.

Geographic entities mentioned:
surface_form: shihan
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.689781
lon: 56.077161
Shakhtau. Shakhtau () - one of the four shihans, located in Ishimbaysky District, on the border with the Shakhtau microdistrict of the city Sterlitamak. The name of the mountain has several variations: &quot;Shachtau&quot;, &quot;Shaketau&quot;, &quot;Ashak-tau&quot;, &quot;Tsar-Gora&quot;. One of the chain of four shihans in the vicinity of the Ishimbay and Sterlitamak cities.

Geographic entities mentioned:
surface_form: shakhtau
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.649722222222
lon: 56.0825
Shakhtau. Shakhtau () - one of the four shihans, located in Ishimbaysky District, on the border with the Shakhtau microdistrict of the city Sterlitamak. The name of the mountain has several variations: &quot;Shachtau&quot;, &quot;Shaketau&quot;, &quot;Ashak-tau&quot;, &quot;Tsar-Gora&quot;. One of the chain of four shihans in the vicinity of the Ishimbay and Sterlitamak cities.

Geographic entities mentioned:
surface_form: shakhtau
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.649722222222
lon: 56.0825
surface_form: shakhtau
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.649722222222
lon: 56.0825
The fate of Shakhtau can comprehend several similar shihans. In Bashkortostan there is a campaign for the conservation of natural monuments. Activists consider the act of destroying Shakhtau as an example of a barbaric attitude toward nature, and a quarry formed in its place is called a scar on the face of Bashkortostan. Physiographic characteristic.

Geographic entities mentioned:
surface_form: shakhtau
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.649722222222
lon: 56.0825
The formation of the tectono-sedimentation structure of the reef deposits of the Shakhtau massif was also influenced by the regional dislocations of the Southern Ural and, in particular, the formation of the Shikhan upraised horst, which has punctured and elevated single mountains by, in comparison with the same-aged massifs of the western side of the marginal trough.

Geographic entities mentioned:
surface_form: shakhtau
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.649722222222
lon: 56.0825
In addition to pure limestones, dolomitic limestones of clearly secondary origin are found in the massif. The limestones of Shakhtau are extremely rich in the remains of various organisms of excellent preservation. Shakhtau is now a limestone quarry, officially a &quot;limestone deposit&quot;, for the Sterlitamak soda-cement plant (OJSC Soda). The development of limestone began in 1950.

Geographic entities mentioned:
surface_form: shakhtau
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.649722222222
lon: 56.0825
In 1959, on the eastern slope, a cemetery dating from the 13th and 14th centuries was discovered. In the 1960s and 1970s, many geologists visited the mine of Shakhtau, mostly paleontologists to collect comparative material. Data on Shakhtau were also used to understand the reservoir properties of reef-based limestones.

Geographic entities mentioned:
surface_form: shakhtau
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.649722222222
lon: 56.0825
Kundara is attempting to revive this industrial tradition and glory of bygone era now by developing Technopark Kollam and The Kerala Ceramics Limited. Kundara is also famous for backwater fishing since it is located on the shores of Kanjiracode Lake, a branch of Ashtamudi Lake. This lake recently received Marine Stewardship council recognition for sustainable fishing. History.

Geographic entities mentioned:
surface_form: Ashtamudi Lake
instance_of: Lake
countries: India
coordinates: lat: 8.9833333333333
lon: 76.6
Industrial history. Since early days Kundara developed as a market place for trade due to &quot;21 feet wide&quot; Quilon Sengotta Road that connected Travancore to Madras Presidency and proximity to water transport through Ashtamudi Lake. In 1904 the Kollam-Sengottai rail line opened up through Kundara.

Geographic entities mentioned:
surface_form: Ashtamudi Lake
instance_of: Lake
countries: India
coordinates: lat: 8.9833333333333
lon: 76.6
Viscount Hall. Viscount Hall, of Cynon Valley in the County of Glamorgan, was a title in the Peerage of the United Kingdom. It was created on 28 October 1946 for the Labour politician George Hall. The title became extinct upon the death of his son, the second Viscount, in 1985. He had married pioneering Leicestershire businesswoman Alice Walker in 1962.

Geographic entities mentioned:
surface_form: Cynon Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.657
lon: -3.461
The average elevation is around. The highest point in the immediate area is Kennesaw Mountain at, followed by Stone Mountain at, Sweat Mountain at, and Little Kennesaw Mountain at. Others include Blackjack Mountain, Lost Mountain, Brushy Mountain, Pine Mountain, and Mount Wilkinson (Vinings Mountain).

Geographic entities mentioned:
surface_form: Kennesaw Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.976213888889
lon: -84.579655555556
surface_form: Stone Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.805944444444
lon: -84.145422222222
surface_form: Sweat Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.0669
lon: -84.4556
surface_form: Little Kennesaw Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.970655555556
lon: -84.586877777778
The highest point in the immediate area is Kennesaw Mountain at, followed by Stone Mountain at, Sweat Mountain at, and Little Kennesaw Mountain at. Others include Blackjack Mountain, Lost Mountain, Brushy Mountain, Pine Mountain, and Mount Wilkinson (Vinings Mountain). Many of these play prominently in the various battles of the Atlanta Campaign during the American Civil War.

Geographic entities mentioned:
surface_form: Lost Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.3772
lon: -95.5944
surface_form: Mount Wilkinson
instance_of: Mountain
countries: United States
coordinates: lat: 33.869616666666666
lon: -84.46828888888889
Many of these play prominently in the various battles of the Atlanta Campaign during the American Civil War. If the further-north counties are included, Bear Mountain is highest, followed by Pine Log Mountain, Sawnee Mountain, and Hanging Mountain, followed by the others listed above. Stone, Sweat, Bear, and Sawnee are all home to some of the area's broadcast stations.

Geographic entities mentioned:
surface_form: Pine Log Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.3217
lon: -84.6371
surface_form: Sawnee Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.2367
lon: -84.1606
Earthquakes and fault lines. An extinct fault line called the Brevard Fault runs roughly parallel to the Chattahoochee River, but as its last movements were apparently prehistoric, it is considered extinct and not a threat to the region. Still, minor earthquakes do rattle the area (and all of Georgia) occasionally.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Environment. The area's prolific rains are drained by many different streams and creeks. The main basin is that of the Chattahoochee River, running northeast to southwest. The further northwestern suburbs drain into the Etowah River via the Little River and Lake Allatoona. The southern suburbs are drained by the Flint River, and the east-southeastern ones by the Oconee River and Yellow River.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Argan Kangri. Argan Kangri, is the highest mountain of the Arganglas group in the southern part of the Saser Muztagh in Ladakh. In 2001 a joint Indo-American-British expedition which included Chris Bonington and Harish Kapadia attempted the ascent of Argan Kangri.

Geographic entities mentioned:
surface_form: argan kangri
instance_of: Mountain
countries: India
coordinates: lat: 34.606156
lon: 77.899563