Sarmila/GeoWiki-Features huggingface dataset:
Another idea was that the kills were the result of a pathogen or other biological infestation. However, neither idea explained why all trees in the affected areas were killed regardless of age or health. Then, in March 1990, a U.S. Forest Service Ranger became ill with suffocation symptoms after being in a snow-covered cabin near Horseshoe Lake.

Geographic entities mentioned:
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 40.4725
lon: -121.336
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 47.30912222222222
lon: -122.04138333333333
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 37.1489
lon: -89.355
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 46.02805556
lon: -95.68916667
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 46.3087
lon: -121.569
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 45.59194444
lon: -93.05361111
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 37.6087742
lon: -119.0194324
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 47.40822
lon: -122.6643413
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 38.6994
lon: -90.085
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 46.119166666667
lon: -94.830277777778
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 47.4411
lon: -93.4733
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 45.459166666667
lon: -93.05
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 44.131666666667
lon: -74.620833333333
Researchers also determined that Mammoth releases about of every day. As of 2003, the concentration of carbon dioxide in soil gas at Mammoth Mountain was being monitored on a continuous, year-round basis at four sites—three at Horseshoe Lake and one near the base of the previous Chair 19 at the ski area.

Geographic entities mentioned:
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 40.4725
lon: -121.336
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 47.30912222222222
lon: -122.04138333333333
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 37.1489
lon: -89.355
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 46.02805556
lon: -95.68916667
surface_form: mammoth mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6306
lon: -119.033
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 46.3087
lon: -121.569
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 45.59194444
lon: -93.05361111
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 37.6087742
lon: -119.0194324
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 47.40822
lon: -122.6643413
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 38.6994
lon: -90.085
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 46.119166666667
lon: -94.830277777778
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 47.4411
lon: -93.4733
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 45.459166666667
lon: -93.05
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 44.131666666667
lon: -74.620833333333
Mammoth Mountain. Mammoth Mountain is a lava dome complex partially located in the town of Mammoth Lakes, California, in the Inyo National Forest of Madera and Mono counties. It is home to a large ski area primarily on the Mono County side. Mammoth Mountain was formed in a series of eruptions that ended 57,000 years ago. Mammoth mountain still produces hazardous volcanic gases that kill trees.

Geographic entities mentioned:
surface_form: mammoth mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6306
lon: -119.033
Mammoth Mountain is a lava dome complex partially located in the town of Mammoth Lakes, California, in the Inyo National Forest of Madera and Mono counties. It is home to a large ski area primarily on the Mono County side. Mammoth Mountain was formed in a series of eruptions that ended 57,000 years ago. Mammoth mountain still produces hazardous volcanic gases that kill trees. Geology.

Geographic entities mentioned:
surface_form: mammoth mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6306
lon: -119.033
It is home to a large ski area primarily on the Mono County side. Mammoth Mountain was formed in a series of eruptions that ended 57,000 years ago. Mammoth mountain still produces hazardous volcanic gases that kill trees. Geology. Mammoth Mountain is a lava dome complex in Mono County, California.

Geographic entities mentioned:
surface_form: mammoth mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6306
lon: -119.033
Mammoth Mountain was formed in a series of eruptions that ended 57,000 years ago. Mammoth mountain still produces hazardous volcanic gases that kill trees. Geology. Mammoth Mountain is a lava dome complex in Mono County, California. It lies in the southwestern corner of the Long Valley Caldera and consists of about 12 rhyodacite and dacite overlapping domes.

Geographic entities mentioned:
surface_form: mammoth mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6306
lon: -119.033
The volcano is still active with minor eruptions, the largest of which was a minor phreatic (steam) eruption 700 years ago. Mammoth Mountain also lies on the south end of the Mono-Inyo chain of volcanic craters. The magma source for Mammoth Mountain is distinct from those of both the Long Valley Caldera and the Inyo Craters.

Geographic entities mentioned:
surface_form: mammoth mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6306
lon: -119.033
Mammoth Mountain also lies on the south end of the Mono-Inyo chain of volcanic craters. The magma source for Mammoth Mountain is distinct from those of both the Long Valley Caldera and the Inyo Craters. Mammoth Mountain is composed primarily of dacite and rhyolite, part of which has been altered by hydrothermal activity from fumaroles (steam vents). Volcanic gas discharge.

Geographic entities mentioned:
surface_form: mammoth mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6306
lon: -119.033
The remarkable uniformity in chemical and isotopic composition of the and accompanying gases at different locations around Mammoth Mountain indicates that there may actually be a large reservoir of gas deep below the mountain from which gas escapes along faults to the surface.

Geographic entities mentioned:
surface_form: mammoth mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6306
lon: -119.033
Measurements of helium emissions support the theory that the gases emitted in the tree kill area have the same source as those discharged from Mammoth Mountain Fumarole. There is evidence, published in 2007, that the rate of discharge has been declining, with emissions peaking in 1991. Ski patrol fatalities incident.

Geographic entities mentioned:
surface_form: mammoth mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6306
lon: -119.033
There is evidence, published in 2007, that the rate of discharge has been declining, with emissions peaking in 1991. Ski patrol fatalities incident. In April 2006, three members of the Mammoth Mountain Ski Area ski patrol died while on duty when a fumarole caused a snow bridge to collapse under the patrollers. The 2005/2006 winter season delivered significant snow depth of.

Geographic entities mentioned:
surface_form: mammoth mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6306
lon: -119.033
It is unclear if they died as a result of the fall or as a result of the gas. Recreational use. Mammoth Mountain is home to the Mammoth Mountain Ski Area, founded by Dave McCoy in 1953. Mammoth is a ski, snowboard, and snowmobile mountain during the winter months.

Geographic entities mentioned:
surface_form: mammoth mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6306
lon: -119.033
surface_form: mammoth mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6306
lon: -119.033
Another were commissioned in 1908. The oiled road was completed by September 1910, and provided a view of Lake Elsinore and the Colorado Desert, and it was expected to help with transporting lumber and stopping fires; because of this, the federal government provided $2,000 for the construction. The road became a part of the forest highway system in 1927.

Geographic entities mentioned:
surface_form: Lake Elsinore
instance_of: Lake
countries: United States
coordinates: lat: 33.660069444444
lon: -117.35183888889
Past dinners have taken place inside of an ancient castle, underground wine cellars, private gardens at the foot of Table Mountain, urban, industrial warehouses and stunning, immaculate art galleries.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
The major tributaries are (from top to bottom) Bridge Creek, Mangels Gulch, and then Valencia Creek (shortly after the latter receives its Trout Gulch tributary). Aptos Creek serves as a drain in the Soquel-Aptos area along with Branciforte Creek and Soquel Creek along with its tributary West Branch Soquel Creek.

Geographic entities mentioned:
surface_form: west branch
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
surface_form: aptos
instance_of: Watercourse
countries: United States
coordinates: lat: 36.96972222
lon: -121.90611111
Aptos Creek. Aptos Creek is a southward flowing creek that begins on Santa Rosalia Mountain on the southwestern slope of the Santa Cruz Mountains in Santa Cruz County, California and enters Monterey Bay, at Seacliff State Beach in Aptos, California. History. The earliest record of &quot;Outos&quot; or &quot;Aptos&quot; is Arroyo de Outos in 1796, thought to be pronunciations of an Ohlone (Sp.

Geographic entities mentioned:
surface_form: aptos
instance_of: Watercourse
countries: United States
coordinates: lat: 36.96972222
lon: -121.90611111
Aptos Creek. Aptos Creek is a southward flowing creek that begins on Santa Rosalia Mountain on the southwestern slope of the Santa Cruz Mountains in Santa Cruz County, California and enters Monterey Bay, at Seacliff State Beach in Aptos, California. History. The earliest record of &quot;Outos&quot; or &quot;Aptos&quot; is Arroyo de Outos in 1796, thought to be pronunciations of an Ohlone (Sp.

Geographic entities mentioned:
surface_form: aptos
instance_of: Watercourse
countries: United States
coordinates: lat: 36.96972222
lon: -121.90611111
surface_form: aptos
instance_of: Watercourse
countries: United States
coordinates: lat: 36.96972222
lon: -121.90611111
At the mouth of the creek, beaches host 30 meter high cliffs. The lower part of the Aptos Creek basin is characterized by its location in an area of low-density residential developments. Still, over 60% of the watershed of the Aptos Creek mainstem lies within and is protected by The Forest of Nisene Marks State Park.

Geographic entities mentioned:
surface_form: aptos
instance_of: Watercourse
countries: United States
coordinates: lat: 36.96972222
lon: -121.90611111
All three are perennial streams that have a component of base flow discharge across the year. There are gaging stations for the Soquel-Aptos Area both in Aptos Creek in Aptos itself and in Aptos Creek but just outside Aptos. The former is located at 36°58'33&quot;N and the drainage area is 31.9 kilometers squared.

Geographic entities mentioned:
surface_form: aptos
instance_of: Watercourse
countries: United States
coordinates: lat: 36.96972222
lon: -121.90611111
surface_form: aptos
instance_of: Watercourse
countries: United States
coordinates: lat: 36.96972222
lon: -121.90611111
surface_form: aptos
instance_of: Watercourse
countries: United States
coordinates: lat: 36.96972222
lon: -121.90611111
surface_form: aptos
instance_of: Watercourse
countries: United States
coordinates: lat: 36.96972222
lon: -121.90611111
surface_form: aptos
instance_of: Watercourse
countries: United States
coordinates: lat: 36.96972222
lon: -121.90611111
Many visitors of the Forest of Nisene Marks like to picnic alongside the creek. Others like to hike, bike, walk dogs, and jog on the Aptos Creek Fire Road which ventures through the forest. Aptos Creek can also be accessed in Aptos Village Park on Aptos Creek Road which includes picnic areas, the Aptos Village Park Hall, barbecues, lawn areas, and redwood trees.

Geographic entities mentioned:
surface_form: aptos
instance_of: Watercourse
countries: United States
coordinates: lat: 36.96972222
lon: -121.90611111
surface_form: aptos
instance_of: Watercourse
countries: United States
coordinates: lat: 36.96972222
lon: -121.90611111
surface_form: aptos
instance_of: Watercourse
countries: United States
coordinates: lat: 36.96972222
lon: -121.90611111
History. The earliest record of &quot;Outos&quot; or &quot;Aptos&quot; is Arroyo de Outos in 1796, thought to be pronunciations of an Ohlone (Sp. Costanoan) village at the junction of Aptos and Valencia Creeks. They come together now below Highway 1 and the overpass of Spreckles Drive. Rancho de Aptos was a sheep ranch of Mission Santa Cruz shown on documents dating to July 5, 1807.

Geographic entities mentioned:
surface_form: aptos
instance_of: Watercourse
countries: United States
coordinates: lat: 36.96972222
lon: -121.90611111
Costanoan) village at the junction of Aptos and Valencia Creeks. They come together now below Highway 1 and the overpass of Spreckles Drive. Rancho de Aptos was a sheep ranch of Mission Santa Cruz shown on documents dating to July 5, 1807. Rancho Aptos was a Mexican land grant in present-day Santa Cruz County, California, given in 1833 by Governor José Figueroa to Rafael Castro.

Geographic entities mentioned:
surface_form: aptos
instance_of: Watercourse
countries: United States
coordinates: lat: 36.96972222
lon: -121.90611111
Many visitors of the Forest of Nisene Marks like to picnic alongside the creek. Others like to hike, bike, walk dogs, and jog on the Aptos Creek Fire Road which ventures through the forest. Aptos Creek can also be accessed in Aptos Village Park on Aptos Creek Road which includes picnic areas, the Aptos Village Park Hall, barbecues, lawn areas, and redwood trees.

Geographic entities mentioned:
surface_form: aptos
instance_of: Watercourse
countries: United States
coordinates: lat: 36.96972222
lon: -121.90611111
Inda Zib'i. Inda Zib'i is a reservoir located in the Inderta &quot;woreda&quot; of the Tigray Region in Ethiopia. The earthen dam that holds the reservoir was built in 1999 by SAERT. Capacity. In 2002, the life expectancy of the reservoir (the duration before it is filled with sediment) was estimated at 25 years. Environment.

Geographic entities mentioned:
surface_form: inda zib'i
instance_of: Body of water
countries: Ethiopia
coordinates: lat: 13.46980156
lon: 39.65274114
Milange District lies to the north. Mocuba District lies to the east, and Nicoadala District to the southeast. Mopeia District is to the south. Most of the district lies on the Morrumbala Plateau. The plateau drops steeply on its western edge, called the Morrumbala Escarpment, to the valley of the Shire River. Mount Morrumbala (1,172 m.) lies on the western edge of the plateau.

Geographic entities mentioned:
surface_form: Mount Morrumbala
instance_of: Mountain
countries: Mozambique
coordinates: lat: -17.445722222222223
lon: 35.391888888888886
Huldreslottet Mountain. Huldreslottet Mountain () is a prominent ice-free mountain that is the southernmost summit in the Borg Massif, Queen Maud Land, Antarctica. It was mapped by Norwegian cartographers from surveys and air photos by the Norwegian–British–Swedish Antarctic Expedition (1949–52) and named Huldreslottet (the fairy castle).

Geographic entities mentioned:
surface_form: huldreslottet
instance_of: Mountain
coordinates: lat: -72.9667
lon: -3.8
Chinese maps show the &quot;main&quot; river flowing through the town (coming from the south, and then turning to the east, toward the Tongtian River (Dri Chu), after taking on a tributary in Gyêgu) as the Batang River (). Geography. Gyêgu (Jiegu) is located in the eastern Tibetan Plateau, at an elevation of. The town is located in the Batang River (Zha Chu) valley, surrounded by mountains.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Clove Mountain. Clove Mountain is located in Union Vale, Dutchess County, New York, rising to an elevation of. It is the town's highest point. It marks the southern extent of the Taconic Mountains and its bedrock is metamorphic, composed of rocks like schist, phyllite, and metagraywacke. Flora and fauna on the mountain are consistent with those found throughout the broader New England Uplands.

Geographic entities mentioned:
surface_form: clove mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.688333333333
lon: -73.692777777778
The installation of a fire tower on Clove Mountain, as well as on Mount Beacon to the southwest, was formally proposed in 1930, on the basis of inadequate early wildfire detection in Dutchess County. The Clove Mountain tower is a Aermotor model LS-40. It remained in service through the end of the 1988 fire season, and was officially decommissioned the following year.

Geographic entities mentioned:
surface_form: clove mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.688333333333
lon: -73.692777777778
It remained in service through the end of the 1988 fire season, and was officially decommissioned the following year. The first five observers at Clove Mountain, collectively serving from April 1933 until May 1960, were each hired with a starting salary of $100 per month. Both structures survive, but are not actively maintained and are located on private property. Geography.

Geographic entities mentioned:
surface_form: clove mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.688333333333
lon: -73.692777777778
The especially prolific Clove Spring reportedly flows at several hundred gallons per minute; it was one of the factors which attracted the first European settlers of Clove Valley in the early 18th century. Several small hamlets cropped up in the valley in the 19th century, during which period extensive iron ore mining took place.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Ogoulou River. The Ogoulou River is in Gabon. It is a tributary of the Ngounié River. Yengué is by it. Paul Belloni Du Chaillu wrote about it. He reported plantations of groundnuts bordering it.

Geographic entities mentioned:
surface_form: ogoulou river
instance_of: Watercourse
countries: Gabon
coordinates: lat: -2.0244444444444
lon: 11.319722222222
342). An appeal to the House of Lords was rejected. Further conflicts. In a second case, the Court of Session summoned the Presbytery of Dunkeld for proceeding with an ordination despite a court interdict. In 1839, the General Assembly suspended seven ministers from Strathbogie for proceeding with an induction in Marnoch in defiance of its orders.

Geographic entities mentioned:
surface_form: Strathbogie
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.39
lon: -2.81
Pedicularis rainierensis. &quot;Pedicularis rainierensis&quot; is a species of flowering plant in the family Orobanchaceae commonly known as Mount Rainier lousewort. It is endemic to the vicinity of Mount Rainier in Washington state. The Mount Rainier lousewort has a imperiled status. Description. Pedicularis rainierensis is a fibrous-rooted, perennial herb that is 1.5-4 decimeters long.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
In the 1860s, mining carried on, in a large scale, with quicksilver mines operating in many areas of Napa County. The most noted mine was the Silverado Mine, near the summit of Mount Saint Helena. At this time, the first wave of rural, foreign laborers from coastal villages of China's Canton province arrived in California and at Napa County mines.

Geographic entities mentioned:
surface_form: Mount Saint Helena
instance_of: Mountain
countries: United States
coordinates: lat: 38.669333333333
lon: -122.63355
Department of the Interior in 1930–40s, the U.S. Congress authorized channel improvements on Napa River and construction of a dam on Conn Creek as part of the Flood Control Act of 1944, though funding was never approved. The City of Napa funded and built the dam in order to create the water conservation reservoir Lake Hennessey in 1948; however, flooding continued to be a problem.

Geographic entities mentioned:
surface_form: Lake Hennessey
instance_of: Lake
countries: United States
coordinates: lat: 38.4811
lon: -122.373
Syria under the French Mandate. The proclamation of the establishment of the Arab Kingdom of Syria had internal implications, reflecting tensions within both Syria and Lebanon. Muslims had attacked Christian villages in the Beqaa Valley in response to statements by the Maronite Patriarch Elias Peter Hoayek and the Board of Directors of Mount Lebanon, opposing the independence of Lebanon.

Geographic entities mentioned:
surface_form: Beqaa Valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
The broad has an abundant selection of birds and wildlife. The lake is connected to Ormesby Broad and Rollesby Broad via a narrow inlet under a road bridge and via the River Bure and the main broads network by a now unnavigable cutting with a lock gate. This cuts the broad off from the main Broadland area and that means there is no water traffic for a majority of the time.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Filby Broad. Filby Broad is one of five broads (lakes) in the Trinity Broads in Norfolk, England. It lies within the Broads National Park, adjacent to the village of Filby. The broad has an abundant selection of birds and wildlife.

Geographic entities mentioned:
surface_form: filby broad
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.662
lon: 1.633
Waipio Valley. iwc8wxkidi3mdedjhuyvap7nibq" xml:space="preserve">#REDIRECT Waipiʻo Valley

Geographic entities mentioned:
surface_form: waipio valley
instance_of: Valley
countries: United States
coordinates: lat: 20.1197
lon: -155.593
Lightning struck a single red fir tree on a north-facing slope, at about in elevation, and ignited it at approximately 5:09 p.m. PDT. The ignition point was located in a designated wilderness area, approximately northeast of Paradise Meadows and east of Lassen Peak, south of the Lassen National Park Highway. The fire was named for Reading Peak, which lay nearby.

Geographic entities mentioned:
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
He was acting bailiff of Lower Telemark and Bamble in 1818, a civil servant with the Ministry of Finance 1819–1823, deputy governor of Hedemarken 1823–1826, sheriff of Hof 1826–1830, attorney-at-law and acting judge in Hedemarken 1830–1843, bailiff of Østerdalen 1843–1858 and bailiff of Øvre Romerike 1858–1860. Early life.

Geographic entities mentioned:
surface_form: Østerdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.575916666666664
lon: 11.087111111111112
Eravimala. Eravimala (ഇരവിമല) is the highest peak located in the Anamalai Hills in the Western Ghats, India. It is situated at the Idukki District of Kerala, and stands at. It is one of the 14 highest peaks in the district which exceed a height of above sea level. The highest one is Anamala (Anamudi) at. It is the tenth highest peak in South India.

Geographic entities mentioned:
surface_form: Anamudi
instance_of: Mountain
countries: India
coordinates: lat: 10.166666666667
lon: 77.066666666667
Eravimala. Eravimala (ഇരവിമല) is the highest peak located in the Anamalai Hills in the Western Ghats, India. It is situated at the Idukki District of Kerala, and stands at. It is one of the 14 highest peaks in the district which exceed a height of above sea level. The highest one is Anamala (Anamudi) at. It is the tenth highest peak in South India.

Geographic entities mentioned:
surface_form: ഇരവിമല
instance_of: Mountain
countries: India
surface_form: eravimala
instance_of: Mountain
countries: India
Eravimala. Eravimala (ഇരവിമല) is the highest peak located in the Anamalai Hills in the Western Ghats, India. It is situated at the Idukki District of Kerala, and stands at. It is one of the 14 highest peaks in the district which exceed a height of above sea level. The highest one is Anamala (Anamudi) at. It is the tenth highest peak in South India.

Geographic entities mentioned:
surface_form: eravimala
instance_of: Mountain
countries: India
It started development in 2014 as the successor to the K computer and made its debut in 2020. It is named after an alternative name for Mount Fuji. It became the fastest supercomputer in the world in the June 2020 TOP500 list as well as becoming the first ARM architecture-based computer to achieve this.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
History. On May 23, 2019, Riken announced that the supercomputer was to be named Fugaku. In August 2019, the logo for Fugaku was unveiled; it depicts Mount Fuji, symbolising &quot;Fugaku's high performance&quot; and &quot;the wide range of its users&quot;. In November 2019, the prototype of Fugaku won first place in the Green500 list.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
The Altan Khan ceased to exist after a series of defeats at the hands of their western neighbors the Oirat Dzungar Khanate in the late 17 century. The Tüsheet Khan often exerted more influence and power over the other Khans as it occupied most of modern central Mongolia, an area that included the Orkhon Valley, the ancient Mongol capital of Karakorum, and the religious center of Erdene Zuu.

Geographic entities mentioned:
surface_form: Orkhon Valley
instance_of: Valley
countries: Mongolia
coordinates: lat: 47.556666666667
lon: 102.83138888889
Mount Khakandya. Mount Khakandya () is a peak in the Suntar-Khayata Range, East Siberian System, Russia. Administratively it is located in the Khabarovsk Krai of the Russian Far East.

Geographic entities mentioned:
surface_form: mount khakandya
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 61.60055555555556
lon: 142.83722222222224
Gachilbong (Inje County). Gachilbong () is a mountain of South Korea. It has an elevation of 1,164 metres

Geographic entities mentioned:
surface_form: gachilbong
instance_of: Mountain
countries: South Korea
surface_form: gachilbong (inje county)
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.0079
lon: 128.4284
Gachilbong (Inje County). Gachilbong () is a mountain of South Korea. It has an elevation of 1,164 metres

Geographic entities mentioned:
surface_form: gachilbong
instance_of: Mountain
countries: South Korea
surface_form: gachilbong
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.0079
lon: 128.4284
In 1868, the Persian-speakers in the Khanate of Kokand, the Farghana Valley and the cities of Samarkand and Bukhara were referred to as Tajiks by both themselves and outsiders. It was also used as a self-designation by non-Persian Iranians in several mountainous areas, such as Shughnan and Roshan.

Geographic entities mentioned:
surface_form: Farghana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
In 1868, the Persian-speakers in the Khanate of Kokand, the Farghana Valley and the cities of Samarkand and Bukhara were referred to as Tajiks by both themselves and outsiders. It was also used as a self-designation by non-Persian Iranians in several mountainous areas, such as Shughnan and Roshan.

Geographic entities mentioned:
surface_form: Shughnan
instance_of: Valley
countries: Afghanistan
Tajikistan
Khanate of Kokand
coordinates: lat: 37.616666666667
lon: 71.45
Since the 2011 local government reform it is part of the municipality Tinos, of which it is a municipal unit. The population was 566 at the 2021 census and the land area is 33.378 km². It is a small fishing village, located at the northwestern tip of the island. It shares the island of Tinos with the municipal units of Tinos (town) and Exomvourgo.

Geographic entities mentioned:
surface_form: Exomvourgo
instance_of: Mountain
countries: Greece
coordinates: lat: 37.57722222
lon: 25.1675
Slieve League. Slieve League or Slieve Liag () is a mountain on the Atlantic coast of County Donegal, Ireland. At, it has the second-highest sea cliffs in Ireland after Croaghaun, and some of the highest sea cliffs in Europe.

Geographic entities mentioned:
surface_form: Croaghaun
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.981
lon: -10.204
surface_form: croaghaun
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.6636
lon: -6.7675
Slieve League. Slieve League or Slieve Liag () is a mountain on the Atlantic coast of County Donegal, Ireland. At, it has the second-highest sea cliffs in Ireland after Croaghaun, and some of the highest sea cliffs in Europe.

Geographic entities mentioned:
surface_form: slieve league
instance_of: Mountain
countries: Ireland
coordinates: lat: 54.638055555556
lon: -8.6813888888889
Slieve League. Slieve League or Slieve Liag () is a mountain on the Atlantic coast of County Donegal, Ireland. At, it has the second-highest sea cliffs in Ireland after Croaghaun, and some of the highest sea cliffs in Europe.

Geographic entities mentioned:
surface_form: slieve league
instance_of: Mountain
countries: Ireland
coordinates: lat: 54.638055555556
lon: -8.6813888888889
surface_form: slieve liag
instance_of: Mountain
countries: Ireland
coordinates: lat: 54.638055555556
lon: -8.6813888888889
The traverse of this ridge, the &quot;One Man's Path&quot;, is one of the most remarkable walks to be found in Ireland - not actually dangerous, but needing a good head and careful progress on a stormy day...The northern precipice, which drops 1500 feet into the coomb surrounding the Little Lough Agh, harbours the majority of the alpine plants of Slieve League, the most varied group of alpines to be found anywhere in Donegal.

Geographic entities mentioned:
surface_form: slieve league
instance_of: Mountain
countries: Ireland
coordinates: lat: 54.638055555556
lon: -8.6813888888889
surface_form: slieve league
instance_of: Mountain
countries: Ireland
coordinates: lat: 54.638055555556
lon: -8.6813888888889
Venus of Arles. The &quot;Venus of Arles&quot; is a sculpture of Venus at the Musée du Louvre. It is in Hymettus marble and dates to the end of the 1st century BC. History. It may be a copy of the Aphrodite of Thespiae by Praxiteles, ordered by the courtesan Phryne.

Geographic entities mentioned:
surface_form: Hymettus marble
instance_of: Mountain
countries: Greece
coordinates: lat: 37.9465
lon: 23.816666666666666
East of the field, andesitic stratovolcanoes reach elevations of about. From north to south, the andesitic stratovolcanoes include the or high Cerro Deslinde which is the highest in the area, the high Cerro El Volcan, the high Cordillera del Tatio and the high Volcan Tatio, which collectively form the El Tatio volcanic group. The Sierra de Tucle lies to the southwest of the field.

Geographic entities mentioned:
surface_form: Cerro Deslinde
instance_of: Mountain
countries: Chile
coordinates: lat: -22.2708
lon: -67.9471
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
Surface exposure dating indicates that some moraines were emplaced at or before the Last Glacial Maximum and others in a time period 35,000 to 40,000 years before present. Smaller moraines at higher altitude may date to the Antarctic Cold Reversal or the Younger Dryas climate periods; moraines related to the Lake Tauca stage are either absent or restricted to high elevation sites.

Geographic entities mentioned:
surface_form: Lake Tauca
instance_of: Lake
countries: Peru
coordinates: lat: -20
lon: -68
Volcanic formations fill the Tatio graben, including the Miocene Rio Salado ignimbrite and related volcanics which reach thicknesses of in some places, the Sifon ignimbrite, the Pliocene Puripicar ignimbrite and the Pleistocene Tatio ignimbrite; the Puripicar ignimbrite crops out farther west. Active volcanoes in the area include Putana and Tocorpuri.

Geographic entities mentioned:
surface_form: Tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
Hydrology. Most of the water that is discharged by the hot springs appears to originate as precipitation, which enters the ground east and southeast of El Tatio. The source of heat of the complex appears to be the Laguna Colorada caldera, the El Tatio volcanic group, the Cerro Guacha and Pastos Grandes calderas or the Altiplano-Puna Magma Body.

Geographic entities mentioned:
surface_form: Cerro Guacha
instance_of: Mountain
countries: Bolivia
coordinates: lat: -22.75
lon: -67.46666667
The Puripicar ignimbrite appears to be the main hydrothermal reservoir, with temperatures reaching. The total heat output of El Tatio is about. The hydrothermal system beneath El Tatio appears to extend to the neighbouring La Torta system. Depending on the season, the hot springs yield of water at temperatures reaching the local boiling point.

Geographic entities mentioned:
surface_form: La Torta
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
Climate and biology. The climate is dry with about precipitation per year. Most of it falls between December and March, a precipitation pattern mediated by the South American monsoon and by the South Pacific High which is responsible for the dry climate. The whole Central Andes were wetter in the past, resulting in the formation of lakes such as Lake Tauca in the Altiplano.

Geographic entities mentioned:
surface_form: Lake Tauca
instance_of: Lake
countries: Peru
coordinates: lat: -20
lon: -68
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
The Pliocene Puripicar ignimbrite reaches a similar thickness, and it was later downwarped by faulting. This strong ignimbrite volcanism is associated with activity of the Altiplano–Puna volcanic complex, which has produced large volume dacite ignimbrites and sizable calderas, starting from the middle Miocene. Among these, Cerro Guacha, La Pacana, Pastos Grandes and Vilama produced supereruptions.

Geographic entities mentioned:
surface_form: La Pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
<mapframe latitude=&quot;-22.350&quot; longitude=&quot;-68.027&quot; zoom=&quot;4&quot; width=&quot;400&quot; height=&quot;300&quot; align=&quot;right&quot; text=&quot;Location of El Tatio in northern Chile close to the border between Chile and Bolivia.&quot;></mapframe>El Tatio lies in the municipality of Calama, Antofagasta Province of northern Chile close to the border between Chile and Bolivia.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
The field is located north of the town San Pedro de Atacama and east of the town of Calama; Chile Route B-245 connects El Tatio to San Pedro de Atacama. Towns close to El Tatio are Toconce to the north, Caspana to the west and Machuca to the south. A workers' camp for a sulfur mine at Volcan Tatio was reported to exist in 1959.

Geographic entities mentioned:
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
Geothermal projects in New Zealand and the United States have resulted in the extinction of geysers. While the incident ultimately did not result in lasting changes to the El Tatio geysers, the widespread media attention did create adverse publicity and social opposition - in particular among indigenous leaders in the region - against geothermal energy in Chile. Tourism.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
El Tatio. El Tatio is a geothermal field with many geysers located in the Andes Mountains of northern Chile at above mean sea level. It is the third-largest geyser field in the world and the largest in the Southern Hemisphere. Various meanings have been proposed for the name &quot;El Tatio&quot;, including &quot;oven&quot; or &quot;grandfather&quot;.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
It is the third-largest geyser field in the world and the largest in the Southern Hemisphere. Various meanings have been proposed for the name &quot;El Tatio&quot;, including &quot;oven&quot; or &quot;grandfather&quot;. The geothermal field has many geysers, hot springs, and associated sinter deposits.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
The water from these hot springs eventually forms the Rio Salado, a major tributary of the Rio Loa, significantly increasing the amount of arsenic in the river. The geothermal vents are sites of populations of extremophile microorganisms such as hyperthermophiles, and El Tatio has been studied as an analogue for the early Earth and possible past life on Mars.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
This series of volcanoes is part of the Central Volcanic Zone (one of several volcanic belts in the Andes), and of the Altiplano–Puna volcanic complex (APVC) &ndash; a system of large calderas and associated ignimbrites which were the sources of supereruptions between 10 million and 1 million years ago. Some of these calderas may be the source of heat for the El Tatio geothermal system.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
The Sierra de Tucle lies to the southwest of the field. Mountains southwest of El Tatio include the high Alto Ojo del Cablor range, while high Cerro Copacoya is situated northwest of the geothermal field.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
Mountains southwest of El Tatio include the high Alto Ojo del Cablor range, while high Cerro Copacoya is situated northwest of the geothermal field. Volcanism with dacitic composition, older than the easterly stratovolcanoes, has occurred west of El Tatio; this volcanism was known as the &quot;liparitic formation&quot; and it covers large areas in the region.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
Temperature measurements of the water flowing to the Rio Salado have yielded values of, while the discharge of the Rio Salado amounts to. The Rio Salado eventually joins the Rio Loa, a major source of freshwater for the region; thus, El Tatio plays an important role in the regional water supply.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
The Rio Salado eventually joins the Rio Loa, a major source of freshwater for the region; thus, El Tatio plays an important role in the regional water supply. In the early 20th century there were several hydraulic engineering projects at El Tatio, aiming either to use its waters or to mitigate its impact on downstream water quality. Geothermal field.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
Only the fields at Yellowstone in the United States and Dolina Geizerov in Russia are larger. They also have taller geysers than at El Tatio, where geyser fountains are on average only high. Together with Sol de Mañana, which is just east of El Tatio in Bolivia, it is also the highest-altitude geyser field in the world.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
The APVC is underpinned by a large magma chamber with the shape of a sill, the Altiplano-Puna Magma Body; a number of volcanoes and geothermal systems including El Tatio are geographically associated with the Altiplano-Puna Magma Body. The Laguna Colorada caldera lies east of El Tatio.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
Active volcanoes in the area include Putana and Tocorpuri. Hydrothermal alteration of country rock at El Tatio has yielded large deposits of alteration minerals such as illite, nobleite, smectite, teruggite and ulexite. The summit parts of several volcanoes of the El Tatio volcanic group have been bleached and discoloured by hydrothermal activity. Hydrology.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
Hydrology. Most of the water that is discharged by the hot springs appears to originate as precipitation, which enters the ground east and southeast of El Tatio. The source of heat of the complex appears to be the Laguna Colorada caldera, the El Tatio volcanic group, the Cerro Guacha and Pastos Grandes calderas or the Altiplano-Puna Magma Body.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
The source of heat of the complex appears to be the Laguna Colorada caldera, the El Tatio volcanic group, the Cerro Guacha and Pastos Grandes calderas or the Altiplano-Puna Magma Body. The movement of the water in the ground is controlled by the permeability of the volcanic material and the Serrania de Tucle–Loma Lucero tectonic block west of El Tatio that acts as an obstacle.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
As it moves through the ground, it acquires heat and minerals and loses steam through evaporation. Unlike geothermal fields in wetter parts of the world, given the dry climate of the area, local precipitation has little influence on the hot springs hydrology at El Tatio. Neither magmatic water nor water from local precipitation are mixed into this water.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
It steeply ascends under El Tatio and appears to be confined between northeast-trending fault systems such as the &quot;Tatio fault&quot;. Three separate geothermal reservoirs have been identified, which underlie the Cerros del Tatio and extend to the La Torta volcano; they are connected by, and partly formed in cavities formed by faults.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
Inorganic carbon (carbonate) occurs at a low concentration. Some of these minerals are toxic, especially arsenic which pollutes a number of waters in the region. Arsenic concentrations in waters at El Tatio can reach – among the highest concentrations found in hot springs of the whole world – and in sediments.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
Arsenic concentrations in waters at El Tatio can reach – among the highest concentrations found in hot springs of the whole world – and in sediments. Producing about, El Tatio is a principal source of arsenic in the Rio Loa system, and arsenic pollution in the region has been linked to health issues in the population.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
Apart from precipitation, the area is characterized by extreme temperature variations between day and night which can reach and induce freeze-thaw cycles. The Chilean Dirección General del Agua operates a weather station at El Tatio; according to data from this station air temperatures average and precipitation.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
The Chilean Dirección General del Agua operates a weather station at El Tatio; according to data from this station air temperatures average and precipitation. El Tatio further features high ultraviolet (UV) insolation, which can reach UV-A and UV-B. The low atmospheric pressure and high UV irradiation has led scientists to treat El Tatio as an analogue for environments on Mars.

Geographic entities mentioned:
surface_form: el tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778