Sarmila/GeoWiki-Features huggingface dataset:
Bears Ears. The Bears Ears are a pair of buttes located in San Juan County in southeastern Utah, United States. They are protected as part of and the namesake of the Bears Ears National Monument, managed by the Bureau of Land Management and United States Forest Service.

Geographic entities mentioned:
surface_form: bears ears
instance_of: Landform
countries: United States
coordinates: lat: 37.628329
lon: -109.866365
Guthrie's tenure at BOAC was marred by a two fatal incidents; the first, BOAC Flight 911, occurred in March 1966 when a Boeing 707 experienced clear-air turbulence whilst overflying Mount Fuji in Japan. The crash resulted in the deaths of all 124 passengers and crew, the most deadly accident involving a British airline to date. Guthrie travelled to Japan to be involved in the investigation.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
The station is three blocks away from the Yankees–East 153rd Street station, a Metro-North Railroad stop on the Hudson Line, which provides service to Yankee Stadium from Manhattan and the Lower Hudson Valley up to Poughkeepsie. Additional service is provided to this station in the form of shuttles from Grand Central, as well as select trains on the Harlem and New Haven lines on game days.

Geographic entities mentioned:
surface_form: Lower Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Rawnsley Bluff. Rawnsley Bluff (formerly Rawnsley's Bluff) is a geological feature in the Australian state of South Australia located within locality of Flinders Ranges and within the boundaries of the Ikara-Flinders Ranges National Park. It is a bluff forming part of Wilpena Pound, situated to the south of St Mary Peak (St Mary Peak is the tallest in the Flinders Ranges at).

Geographic entities mentioned:
surface_form: St Mary Peak
instance_of: Mountain
countries: Australia
coordinates: lat: -31.503888888889
lon: 138.55111111111
surface_form: st mary peak
instance_of: Mountain
countries: Australia
coordinates: lat: -31.503888888889
lon: 138.55111111111
Rawnsley Bluff. Rawnsley Bluff (formerly Rawnsley's Bluff) is a geological feature in the Australian state of South Australia located within locality of Flinders Ranges and within the boundaries of the Ikara-Flinders Ranges National Park. It is a bluff forming part of Wilpena Pound, situated to the south of St Mary Peak (St Mary Peak is the tallest in the Flinders Ranges at).

Geographic entities mentioned:
surface_form: rawnsley's bluff
instance_of: Mountain
countries: Australia
coordinates: lat: -31.623423
lon: 138.610336
surface_form: rawnsley bluff
instance_of: Mountain
countries: Australia
coordinates: lat: -31.623423
lon: 138.610336
It is a bluff forming part of Wilpena Pound, situated to the south of St Mary Peak (St Mary Peak is the tallest in the Flinders Ranges at). Rawnsley's Bluff connects the eastern and western mountain ranges of the pound. The Adelaide Scotch College Cadet Unit used the bluff for training each year until the unit was disbanded in the early 1970s.

Geographic entities mentioned:
surface_form: rawnsley's bluff
instance_of: Mountain
countries: Australia
coordinates: lat: -31.623423
lon: 138.610336
Training included flights with helicopters, infantry training, and practice with infantry weapons such as mortars. The unit was recognized for offering outdoor adventures to the student body. In the 1890s, a trigonometrical station, on the Rawnsley's Bluff to support surveying in South Australia.

Geographic entities mentioned:
surface_form: rawnsley's bluff
instance_of: Mountain
countries: Australia
coordinates: lat: -31.623423
lon: 138.610336
Rawnsley Bluff. Rawnsley Bluff (formerly Rawnsley's Bluff) is a geological feature in the Australian state of South Australia located within locality of Flinders Ranges and within the boundaries of the Ikara-Flinders Ranges National Park. It is a bluff forming part of Wilpena Pound, situated to the south of St Mary Peak (St Mary Peak is the tallest in the Flinders Ranges at).

Geographic entities mentioned:
surface_form: rawnsley bluff
instance_of: Mountain
countries: Australia
coordinates: lat: -31.623423
lon: 138.610336
Incidents. The area around Flesherton is in a snow belt region, and winter storms from Lake Huron and Georgian Bay can cause several &quot;snow days&quot; each year, when buses cannot safely deliver students. While this is not a problem when students are forced to stay home, there is always the question of whether to send students home early when a daytime storm threatens.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
He investigated methods of purification and electrodeposition of zinc, and published several patents regarding this and the purification and recovery of other metals. As a result of his lifelong interest in bushwalking, Bratt joined the Imperial College Exploring Society Karakorum Expedition conducted in 1957–58, the aim of which was to scale the world's second-highest mountain peak.

Geographic entities mentioned:
surface_form: second-highest mountain peak
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
As a result of his lifelong interest in bushwalking, Bratt joined the Imperial College Exploring Society Karakorum Expedition conducted in 1957–58, the aim of which was to scale the world's second-highest mountain peak. Although the expedition did not climb this peak, they did manage to successfully climb K10.

Geographic entities mentioned:
surface_form: K10
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.399578333333
lon: 76.847516666667
Geography. It forms part of Nares Strait, linking Kane Basin with Hall Basin. From the south, its beginning is marked by Capes Lawrence and Jackson; its junction with Hall Basin is marked by Capes Baird and Morton. It is about 130 kilometres in length, between 24 and 32 kilometres in width and averages water depths between 180 and 340 metres.

Geographic entities mentioned:
surface_form: Nares Strait
instance_of: Watercourse
countries: Greenland
Canada
coordinates: lat: 80
lon: -70
surface_form: Hall Basin
instance_of: Watercourse
countries: Canada
Greenland
coordinates: lat: 81.5
lon: -63.5
surface_form: kane basin
instance_of: Watercourse
countries: Canada
Greenland
coordinates: lat: 79.075
lon: -73.0861
Geography. It forms part of Nares Strait, linking Kane Basin with Hall Basin. From the south, its beginning is marked by Capes Lawrence and Jackson; its junction with Hall Basin is marked by Capes Baird and Morton. It is about 130 kilometres in length, between 24 and 32 kilometres in width and averages water depths between 180 and 340 metres.

Geographic entities mentioned:
surface_form: hall basin
instance_of: Watercourse
countries: Canada
Greenland
coordinates: lat: 81.5
lon: -63.5
Kennedy Channel. Kennedy Channel (;;) is an Arctic sea passage between Greenland and Canada's most northerly island, Ellesmere Island. It was named by Elisha Kane around 1854 during his second Arctic voyage in search of the lost Franklin expedition. It is not entirely clear, however, after which Kennedy he named the channel.

Geographic entities mentioned:
surface_form: kennedy channel
instance_of: Watercourse
countries: Canada
Greenland
coordinates: lat: 80.9167
lon: -66.5
Mary Lake (Clearwater and Hubbard counties, Minnesota). Mary Lake is a lake in Clearwater County and Hubbard County, Minnesota, in the United States. Mary Lake was named for Mary Turnbull, the wife of a government surveyor.

Geographic entities mentioned:
surface_form: mary lake
instance_of: Lake
countries: United States
coordinates: lat: 47.185277777778
lon: -95.167222222222
surface_form: mary lake
instance_of: Lake
countries: United States
coordinates: lat: 40.575
lon: -122.433
Some later Buddhists in the region laid claim to Buddhist roots predating Buddhism itself, in King Drime Kunden and the prior incarnations of Buddha, between 2000 and 1000 BC. The Mebar, or Burning Lake, is named for the legend of lama Pema Lingpa, who entered the lake to find a holy treasure, emerging not only with the relic, but with his lamp still burning.

Geographic entities mentioned:
surface_form: Mebar
instance_of: Lake
countries: Bhutan
coordinates: lat: 27.53950556
lon: 90.81234444
Various mountains ranging between meters above sea level run the length of the county from north to south, including the Korab mountains in the east with Mali i Gramës and Korab at an altitude of being the highest mountain in the county and as well as in Albania. The Dejë mountain rises in the center, while in the east the county is dominated by the Lura mountains.

Geographic entities mentioned:
surface_form: Mali i Gramës
instance_of: Mountain
countries: Albania
coordinates: lat: 41.733333333333
lon: 20.483333333333
Various mountains ranging between meters above sea level run the length of the county from north to south, including the Korab mountains in the east with Mali i Gramës and Korab at an altitude of being the highest mountain in the county and as well as in Albania. The Dejë mountain rises in the center, while in the east the county is dominated by the Lura mountains.

Geographic entities mentioned:
surface_form: Lura
instance_of: Mountain
countries: Albania
coordinates: lat: 41.785833333333
lon: 20.181388888889
The county lies about 380 meters up to 2,700 metres above sea level. The main topographic features of the county are the presence of the three major mountain ranges which are the Korab mountains in the east, the Lura mountains in the east and the Skanderbeg mountains in the west, separating the Central Mountain Range with the Western Lowlands.

Geographic entities mentioned:
surface_form: Lura
instance_of: Mountain
countries: Albania
coordinates: lat: 41.785833333333
lon: 20.181388888889
The Mat river has its source in Martanesh. It heads westwards through deep gorges and canyons to Mat and northwest through the towns of Klos and Burrel. The Black Drin flows out from the Ohrid lake and passes through Peshkopi and Maqellara. Rising in Ohrid, the Drin river originates near Kukës at the confluence of the Black Drin and White Drin.

Geographic entities mentioned:
surface_form: Ohrid
instance_of: Lake
countries: North Macedonia
Albania
coordinates: lat: 41.03333333333333
lon: 20.716666666666665
The population was 1,662 at the 2020 census, a decline from the figure of 1,727 tabulated in 2010. The town is part of the Western Connecticut Planning Region. Bridgewater is well known as being a weekend getaway for wealthy New Yorkers, due to its scenic wooded areas, location on the banks of Lake Lillinonah and proximity to New York City.

Geographic entities mentioned:
surface_form: Lake Lillinonah
instance_of: Lake
countries: United States
coordinates: lat: 41.469
lon: -73.312
Kachumbari. Kachumbari is a fresh tomato and onion salad relish that is popular in the cuisines of the African Great Lakes region. It is an uncooked salad dish consisting of chopped tomatoes, onions, and chili peppers. Variations of kachumbari can be found in Kenya, Tanzania, Rwanda, Uganda, Burundi and in the Southern African countries of Malawi and Congo.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
Piper Creek (Alberta). Piper Creek is a creek in Red Deer County, Alberta that flows into Waskasoo Creek. It flows into an intersection with Waskasoo Creek ().

Geographic entities mentioned:
surface_form: Waskasoo Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.28342
lon: -113.802
surface_form: piper creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.26682
lon: -113.8187
Piper Creek (Alberta). Piper Creek is a creek in Red Deer County, Alberta that flows into Waskasoo Creek. It flows into an intersection with Waskasoo Creek ().

Geographic entities mentioned:
surface_form: piper creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.26682
lon: -113.8187
Piper Creek (Alberta). Piper Creek is a creek in Red Deer County, Alberta that flows into Waskasoo Creek. It flows into an intersection with Waskasoo Creek ().

Geographic entities mentioned:
surface_form: waskasoo creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.28342
lon: -113.802
1888–93: Initial construction during Silver Boom. First established in 1879 as Ute City, a rough settlement of log cabins on a plain high in the Roaring Fork Valley, Aspen grew quickly when silver was found in abundance in the nearby mountains. During the Colorado Silver Boom of the 1880s, its population soared and it soon incorporated as a city.

Geographic entities mentioned:
surface_form: Roaring Fork Valley
instance_of: Valley
countries: United States
Continuing east, the northern terminus of New Mexico State Road 80 (NM 80) is intersected, serving Rodeo, followed by NM 338. Passing Lee Peak, the highway turns southeast, entering Lordsburg. US 70 is intersected in town, and becomes concurrent with the highway as it continues east past the Lordsburg Municipal Airport, before exiting the town.

Geographic entities mentioned:
surface_form: Lee Peak
instance_of: Mountain
coordinates: lat: -86.4167
lon: -151.583
Noord-Beveland. Noord-Beveland (; &quot;North Beveland&quot;) is a municipality and region in the southwestern Netherlands and a former island, now part of the Walcheren-Zuid-Beveland-Noord-Beveland peninsula. Noord-Beveland is enclosed by the Oosterschelde estuary to the north, and the former straits, now combined lake, of Veerse Meer and Zandkreek to the south.

Geographic entities mentioned:
surface_form: Veerse Meer
instance_of: Lake
countries: Netherlands
coordinates: lat: 51.533333333333
lon: 3.7166666666667
Loch Fell. Loch Fell is a hill in the Ettrick Hills range, part of the Southern Uplands of Scotland. Close to the Southern Upland Way, routes of ascent frequently incorporate its track and it is almost always climbed along with the neighbouring hills.

Geographic entities mentioned:
surface_form: loch fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.316666666667
lon: -3.3166666666667
Following its foundation, the group specialised in sniper and infiltration tactics, while continuing to participate in combat operations in Latakia. By 2019, the group primarily operated in Jabal al-Akrad, and the al-Ghab Plain. It has fought alongside other rebel groups against the Syrian government's Northwestern Syria offensive from April 2019. Ideology.

Geographic entities mentioned:
surface_form: Jabal al-Akrad
instance_of: Mountain
countries: Syria
coordinates: lat: 35.65
lon: 36.2
Snøsporvstranda. Snøsporvstranda is a beach at the western part of Kongsøya in Kong Karls Land, Svalbard. It has a length of about six kilometers, and is located south of the mountain Tordenskjoldberget.

Geographic entities mentioned:
surface_form: Tordenskjoldberget
instance_of: Mountain
countries: Norway
coordinates: lat: 78.8695
lon: 28.1861
Mount Soucek. Mount Soucek () is a mountain standing between Mount Hardy and Peacock Ridge in the northwest part of the Tula Mountains, in Enderby Land. It was plotted from air photos taken from ANARE (Australian National Antarctic Research Expeditions) aircraft in 1956 and was named by the Antarctic Names Committee of Australia (ANCA) for Dr.

Geographic entities mentioned:
surface_form: Mount Hardy
instance_of: Mountain
coordinates: lat: -66.8167
lon: 50.7167
surface_form: hardy
instance_of: Mountain
coordinates: lat: -66.8167
lon: 50.7167
surface_form: soucek
instance_of: Mountain
coordinates: lat: -66.8167
lon: 50.9667
surface_form: mount soucek
instance_of: Mountain
coordinates: lat: -66.8167
lon: 50.9667
Mount Soucek. Mount Soucek () is a mountain standing between Mount Hardy and Peacock Ridge in the northwest part of the Tula Mountains, in Enderby Land. It was plotted from air photos taken from ANARE (Australian National Antarctic Research Expeditions) aircraft in 1956 and was named by the Antarctic Names Committee of Australia (ANCA) for Dr.

Geographic entities mentioned:
surface_form: soucek
instance_of: Mountain
coordinates: lat: -66.8167
lon: 50.9667
surface_form: mount soucek
instance_of: Mountain
coordinates: lat: -66.8167
lon: 50.9667
It consists mainly of a salt flat and a number of small salt lakes, sheltering several Andean species of wildlife and plants. Arintica volcano towers over the salt flat. The protected area, along with Lauca National Park and Las Vicuñas National Reserve, were designated a World Biosphere Reserve by UNESCO in 1981, which is called Lauca.

Geographic entities mentioned:
surface_form: Arintica
instance_of: Mountain
countries: Chile
coordinates: lat: -18.75
lon: -69.05
Llanfair Dyffryn Clwyd. Llanfair Dyffryn Clwyd is a village and community in Denbighshire, Wales, situated in the Vale of Clwyd about one mile south of the town of Ruthin. In the 2001 census, it had 1048 residents and 50.6% of them could speak Welsh. The figures for the 2011 census were: population 1,053; Welsh speakers 46.9%.

Geographic entities mentioned:
surface_form: Vale of Clwyd
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.21
lon: -3.38
Church of St. Mary and St. Cynfarch. The church of St. Mary in the Vale of Clwyd – in Welsh Llanfair Dyffryn Clwyd – shares its dedication with &quot;Saint&quot; Cynfarch, apparently a Celtic chieftain from northern Britain, related to Coel Hen or &quot;Old King Cole&quot;. It is a large 15th century double-naved church with an impressive tower.

Geographic entities mentioned:
surface_form: Vale of Clwyd
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.21
lon: -3.38
However, Maguire's main force remained unscathed. First siege. Enniskillen Castle sat on the River Erne and commanded the strategic bottleneck between Upper and Lower Lough Erne. On 25 January 1594, English Captain John Dowdall arrived at Enniskillen by boat with three infantry companies.

Geographic entities mentioned:
surface_form: Lough Erne
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.48262
lon: -7.80622
In 1990&ndash;1991, the idea and the design were developed enough to apply for Israeli Government support from the Office of the Chief Scientist in the Ministry of Industry. The application allowed Bar-Natan to become a part of a technology incubator program in Jerusalem's Har Hotzvim, with a government grant covering 3/4 of the expenses connected to the research and development of the bandage.

Geographic entities mentioned:
surface_form: Har Hotzvim
instance_of: Mountain
countries: Israel
coordinates: lat: 31.802527777778
lon: 35.209636111111
Cultural history. The area of Placerita Canyon, in addition to the Santa Clarita Valley and the surrounding mountains, have been inhabited by the native Tataviam since time immemorial. In 1842, the region was annexed under Rancho San Francisco, part of the larger Mexican land grant system that was dissolved 8 years later with California statehood inside the United States.

Geographic entities mentioned:
surface_form: Santa Clarita Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.398
lon: -118.522
Geography. Placerita Canyon State Park is located along Placerita Creek in the southeastern Santa Clarita Valley, just outside the city limits of Santa Clarita but within its sphere of influence. It lies between the Santa Clarita neighborhoods of Newhall and Sand Canyon.

Geographic entities mentioned:
surface_form: Santa Clarita Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.398
lon: -118.522
Seeweiher. The Seeweiher is a reservoir north of the village of Waldernbach in the municipality of Mengerskirchen (county of Limburg-Weilburg) in the Westerwald in the German state of Hesse. It impounds the Vöhlerbach, a tributary of the Kallenbach which, in turn, flows into the River Lahn. It has a surface area of 13 hectares.

Geographic entities mentioned:
surface_form: seeweiher
instance_of: Lake
countries: Germany
coordinates: lat: 50.548
lon: 8.14954
It impounds the Vöhlerbach, a tributary of the Kallenbach which, in turn, flows into the River Lahn. It has a surface area of 13 hectares. The Seeweiher was impounded in 1452 and is thus one of the oldest reservoirs in Hesse. Leisure facilities. There was a campsite on the shores of the bathing lake and, since 1978, there has been a weekend village with 66 houses.

Geographic entities mentioned:
surface_form: seeweiher
instance_of: Lake
countries: Germany
coordinates: lat: 50.548
lon: 8.14954
The Seeweiher was impounded in 1452 and is thus one of the oldest reservoirs in Hesse. Leisure facilities. There was a campsite on the shores of the bathing lake and, since 1978, there has been a weekend village with 66 houses. Once a year the Westerwald Water Working Group holds a water work assessment for Newfoundland and Landseer dogs on land owned by the DLRG by the Seeweiher.

Geographic entities mentioned:
surface_form: seeweiher
instance_of: Lake
countries: Germany
coordinates: lat: 50.548
lon: 8.14954
Geier (Tux Alps). The Geier, at, is the second highest mountain in the Tux Alps in the Austrian state of Tyrol. The Geier lies in the center of the Tux Alps, where the south-west Schmirntal, the west Navistal, the east Tuxer Tal and the north Wattental come together. 450 meters north of the Geier lies the much more rugged Lizumer Reckner, the highest mountain in the Tux Alps.

Geographic entities mentioned:
surface_form: Wattental
instance_of: Valley
countries: Austria
coordinates: lat: 47.23
lon: 11.618611111111
surface_form: geier
instance_of: Mountain
countries: Austria
coordinates: lat: 47.14
lon: 11.6328
The Geier lies in the center of the Tux Alps, where the south-west Schmirntal, the west Navistal, the east Tuxer Tal and the north Wattental come together. 450 meters north of the Geier lies the much more rugged Lizumer Reckner, the highest mountain in the Tux Alps. About 400 meters southeast of the Geier at about 2660 m is the Junssee, which is about 200 by 100 meters in size.

Geographic entities mentioned:
surface_form: Lizumer Reckner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.1441
lon: 11.6305
surface_form: geier
instance_of: Mountain
countries: Austria
coordinates: lat: 47.14
lon: 11.6328
About 400 meters southeast of the Geier at about 2660 m is the Junssee, which is about 200 by 100 meters in size. With the exception of the south-west flank, the Geier belongs to the Lizum-Walchen military training area. Like the Lizumer Reckner, it can also be climbed from all four adjacent valleys. From the Lizumer Hütte in the Wattental, it is often climbed as a ski tour, even in winter.

Geographic entities mentioned:
surface_form: lizumer reckner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.1441
lon: 11.6305
Geier (Tux Alps). The Geier, at, is the second highest mountain in the Tux Alps in the Austrian state of Tyrol. The Geier lies in the center of the Tux Alps, where the south-west Schmirntal, the west Navistal, the east Tuxer Tal and the north Wattental come together. 450 meters north of the Geier lies the much more rugged Lizumer Reckner, the highest mountain in the Tux Alps.

Geographic entities mentioned:
surface_form: geier (tux alps)
instance_of: Mountain
countries: Austria
coordinates: lat: 47.14
lon: 11.6328
Geier (Tux Alps). The Geier, at, is the second highest mountain in the Tux Alps in the Austrian state of Tyrol. The Geier lies in the center of the Tux Alps, where the south-west Schmirntal, the west Navistal, the east Tuxer Tal and the north Wattental come together. 450 meters north of the Geier lies the much more rugged Lizumer Reckner, the highest mountain in the Tux Alps.

Geographic entities mentioned:
surface_form: geier
instance_of: Mountain
countries: Austria
coordinates: lat: 47.14
lon: 11.6328
450 meters north of the Geier lies the much more rugged Lizumer Reckner, the highest mountain in the Tux Alps. About 400 meters southeast of the Geier at about 2660 m is the Junssee, which is about 200 by 100 meters in size. With the exception of the south-west flank, the Geier belongs to the Lizum-Walchen military training area.

Geographic entities mentioned:
surface_form: geier
instance_of: Mountain
countries: Austria
coordinates: lat: 47.14
lon: 11.6328
About 400 meters southeast of the Geier at about 2660 m is the Junssee, which is about 200 by 100 meters in size. With the exception of the south-west flank, the Geier belongs to the Lizum-Walchen military training area. Like the Lizumer Reckner, it can also be climbed from all four adjacent valleys. From the Lizumer Hütte in the Wattental, it is often climbed as a ski tour, even in winter.

Geographic entities mentioned:
surface_form: geier
instance_of: Mountain
countries: Austria
coordinates: lat: 47.14
lon: 11.6328
With the exception of the south-west flank, the Geier belongs to the Lizum-Walchen military training area. Like the Lizumer Reckner, it can also be climbed from all four adjacent valleys. From the Lizumer Hütte in the Wattental, it is often climbed as a ski tour, even in winter. At the summit of the Geier there is a tin vulture, based on the name of the mountain. Geology.

Geographic entities mentioned:
surface_form: geier
instance_of: Mountain
countries: Austria
coordinates: lat: 47.14
lon: 11.6328
The Reckner complex consists of former oceanic crust, so-called ophiolites. The Reckner Complex is located in the border area between the Lower East Alps in the north and the Tauern Window in the south and is assigned to either the Penninic or the Lower East Alps. History. The 2016 Geier avalanche took place at this mountain.

Geographic entities mentioned:
surface_form: geier
instance_of: Mountain
countries: Austria
coordinates: lat: 47.14
lon: 11.6328
It is north east of Crewkerne. It occupies a central position east of the road that links Crewkerne to the A303 road and is mainly south of a brook that feeds nearby into the Parrett. The village forms the civil parish of West and Middle Chinnock with the neighbouring village of Middle Chinnock. The parish has a population of 592 (2011 census). West Chinnock was a separate civil parish until 1884.

Geographic entities mentioned:
surface_form: Parrett
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.2292
lon: -3.00861
Geography. Zheltau is located in the Kazakh Uplands, to the southwest of the Kyzyltau. The massif rises just to the south of the southern shore of lake Shalkarkol. Lake Saumalkol lies to the south of the southern edge. The Ashchysu river flows to the west of the western end and the Kyrgyn, its right tributary, heads northwestward close to the southern slopes.

Geographic entities mentioned:
surface_form: Saumalkol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.0475
lon: 75.98916667
Lake Saumalkol lies to the south of the southern edge. The Ashchysu river flows to the west of the western end and the Kyrgyn, its right tributary, heads northwestward close to the southern slopes. The Karasu has its sources on the southern side of the highest summits and flows towards lake Karasor. The Zheltau consists of an elongated cluster of hills rising quite detached from each other.

Geographic entities mentioned:
surface_form: Karasor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 49.84889
lon: 75.35222
Zheltau (massif). Zheltau (;) is a massif located in Karkaraly District, Karaganda Region and Bayanaul District, Pavlodar Region, Kazakhstan. The border between Karaganda Region and Pavlodar Region runs from east to west along the mountain massif. Zhanatilek lies to the northwest and Yegindybulak town to the southeast. Geography.

Geographic entities mentioned:
surface_form: zheltau (massif)
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 50.225
lon: 75.75
Along with Oued Abdi, it is one of the most important wadis in the Aurès massif. During the wet season, rain and melting snow flow into the valley to form the Abiod River. The valley begins at the foot of Djebel Chélia, Algeria's highest mountain, and flows southwest towards Tolga, eventually dissipating into the Sahara desert nearby. Geography.

Geographic entities mentioned:
surface_form: Djebel Chélia
instance_of: Mountain
countries: Algeria
France
coordinates: lat: 35.318333333333
lon: 6.6375
Chiputneticook Lakes. The Chiputneticook Lakes are a group of several lakes along the international boundary between Maine and New Brunswick. They are East Grand Lake, North Lake, Mud Lake, Spednic Lake, and Palfrey Lake. This lake system forms the head waters of the St. Croix River which the International Boundary follows to Passamaquoddy Bay.

Geographic entities mentioned:
surface_form: East Grand Lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.7
lon: -67.8
surface_form: Spednic Lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 45.6051
lon: -67.6278
Chiputneticook Lakes. The Chiputneticook Lakes are a group of several lakes along the international boundary between Maine and New Brunswick. They are East Grand Lake, North Lake, Mud Lake, Spednic Lake, and Palfrey Lake. This lake system forms the head waters of the St. Croix River which the International Boundary follows to Passamaquoddy Bay.

Geographic entities mentioned:
surface_form: chiputneticook lakes
instance_of: Group of lakes
countries: Canada
United States
coordinates: lat: 45.666666666667
lon: -67.75
The three days after the listed date are also part of the festival. The time before the listed date the pilgrims visit Mount Arafat and descend from it after sunrise of the listed day. In many countries, the start of any lunar Hijri month varies based on the observation of the new moon by local religious authorities, so the exact day of celebration varies by locality.

Geographic entities mentioned:
surface_form: Mount Arafat
instance_of: Mountain
countries: Saudi Arabia
coordinates: lat: 21.354831
lon: 39.983886
Description. In an attempt to relieve pressure on General John Burgoyne's forces in Saratoga, New York, British units under the command of Henry Clinton attacked and captured Fort Montgomery and Fort Clinton in the Hudson Highlands. Following this battle, Clinton sent forces under the command of John Vaughan to raid the Hudson Valley.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
The Rwegura dam and hydroelectric power station were funded by a loan from the African Development Bank. The project was approved on 29 September 1982, with a planned completion of 30 July 1988. It delivered 18 MW of power and had total production of 64 GWH. The Rwegura Dam impounds the Kitenge River, which flows from Kayanza Province. The lake is at an elevation of more than. Operations.

Geographic entities mentioned:
surface_form: Kitenge River
instance_of: Watercourse
countries: Burundi
coordinates: lat: -2.9930555555556
lon: 29.356944444444
Karoulia. Karoulia () is an Eastern Orthodox skete of the community of Mount Athos that is subordinate to the Great Lavra. It is located on the southernmost shore of Mount Athos. Karoulia has 12 huts built in the 17th century. About 10 monks live in Karoulia. Description. The monks at Karoulia practice hesychasm and asceticism.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Manzano Peak. Manzano Peak is the highest peak in the Manzano Mountains, a mountain range in the central part of the US State of New Mexico. It lies southwest of the town of Manzano and east-southeast of the town of Belen, in the Manzano Wilderness Area, part of the Mountainair Ranger District of the Cibola National Forest.

Geographic entities mentioned:
surface_form: manzano peak
instance_of: Mountain
countries: United States
coordinates: lat: 34.590894444444
lon: -106.44668611111
It forms the striking southern anchor of the range, rising in above its western base. The summit is below the tree line, but has views to the east, south, and west. Manzano Peak can be accessed via trail number 80 (the Kayser Trail), leading to the Crest Trail (number 170), from a trailhead on the east side of the range.

Geographic entities mentioned:
surface_form: manzano peak
instance_of: Mountain
countries: United States
coordinates: lat: 34.590894444444
lon: -106.44668611111
Baldy (Jackson County, Oregon). Baldy is a mountain located north-northeast of Talent and east-northeast of Phoenix in Jackson County, Oregon. It forms part of the eastern edge of the Rogue Valley, and is about west-northwest of Grizzly Peak and south-southeast of Roxy Ann Peak.

Geographic entities mentioned:
surface_form: Rogue Valley
instance_of: Valley
countries: United States
coordinates: lat: 42.440122222222
lon: -122.92615277778
surface_form: Roxy Ann Peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.35486
lon: -122.78542
surface_form: grizzly peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.269722222222
lon: -122.61638888889
surface_form: grizzly peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.7296
lon: -119.551
surface_form: grizzly peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9425
lon: -106.52194444444
surface_form: grizzly peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0425
lon: -106.598
surface_form: grizzly peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.6444
lon: -105.849
surface_form: grizzly peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.882
lon: -122.234
Baldy (Jackson County, Oregon). Baldy is a mountain located north-northeast of Talent and east-northeast of Phoenix in Jackson County, Oregon. It forms part of the eastern edge of the Rogue Valley, and is about west-northwest of Grizzly Peak and south-southeast of Roxy Ann Peak.

Geographic entities mentioned:
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 31.69612
lon: -110.8481
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 42.2983
lon: -122.751
Baldy (Jackson County, Oregon). Baldy is a mountain located north-northeast of Talent and east-northeast of Phoenix in Jackson County, Oregon. It forms part of the eastern edge of the Rogue Valley, and is about west-northwest of Grizzly Peak and south-southeast of Roxy Ann Peak.

Geographic entities mentioned:
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 31.69612
lon: -110.8481
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 42.2983
lon: -122.751
Guazapa (volcano). Guazapa is a stratovolcano in central El Salvador. Guazapa volcano an eroded basaltic stratovolcano 23 km NE of San Salvador city. It is not known whether the Pleistocene volcano is still active. It shows signs of intense erosion that have cut deep valleys into its flanks, suggesting a very long dormancy period, and there is no crater morphology left.

Geographic entities mentioned:
surface_form: guazapa
instance_of: Mountain
countries: El Salvador
coordinates: lat: 13.902219444444444
lon: -89.11363055555556
Guazapa (volcano). Guazapa is a stratovolcano in central El Salvador. Guazapa volcano an eroded basaltic stratovolcano 23 km NE of San Salvador city. It is not known whether the Pleistocene volcano is still active. It shows signs of intense erosion that have cut deep valleys into its flanks, suggesting a very long dormancy period, and there is no crater morphology left.

Geographic entities mentioned:
surface_form: guazapa
instance_of: Mountain
countries: El Salvador
coordinates: lat: 13.902219444444444
lon: -89.11363055555556
surface_form: san salvador
instance_of: Mountain
countries: El Salvador
coordinates: lat: 13.733888888889
lon: -89.293888888889
It shows signs of intense erosion that have cut deep valleys into its flanks, suggesting a very long dormancy period, and there is no crater morphology left. During the civil war of the 1980s, Guazapa was one of the main strongholds of the FMLN guerillas. The Guazapa mountains have clandestine cemeteries, bomb shelters, guerilla camps, and makeshift hospitals.

Geographic entities mentioned:
surface_form: guazapa
instance_of: Mountain
countries: El Salvador
coordinates: lat: 13.902219444444444
lon: -89.11363055555556
2013 Vuelta a Asturias. The 2013 Vuelta a Asturias was the 57th edition of the Vuelta a Asturias road cycling stage race, which was held on 11 and 12 May 2013. The race started in Oviedo and finished at Alto del Naranco. The race was won by Amets Txurruka of the team.

Geographic entities mentioned:
surface_form: Alto del Naranco
instance_of: Mountain
countries: Spain
coordinates: lat: 43.38333333
lon: -5.86666667
Erica galpinii. &quot;Erica galpinii&quot; is a plant belonging to the genus &quot;Erica&quot; and forming part of the fynbos. The species is endemic to the Western Cape and occurs in the Kleinrivier Mountains near Hermanus. This endangered and rare species consists of only 450 plant specimens that occur in two subpopulations in an area of 4 km2.

Geographic entities mentioned:
surface_form: Kleinrivier Mountains
instance_of: Mountain
countries: South Africa
coordinates: lat: -34.3833
lon: 19.4167
Gjálp 1996. &quot;(See also the main article: 1996 eruption of Gjálp&quot;
The Gjálp fissure vent eruption in 1996 revealed that an interaction may exist between Bárðarbunga and Grímsvötn. A strong earthquake at Bárðarbunga, about magnitude 5, is believed to have been related to the triggering of the eruption in Gjálp.

Geographic entities mentioned:
surface_form: Bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
surface_form: bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
surface_form: bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
surface_form: grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
Geology. There is the potential for mechanical interaction such as dyke propagation between Grímsvötn and Thordarhyrna. Interactions can also occur with the nearby Bárðarbunga volcano, which is part of a separate volcanic system. The volcano erupts predominantly tholeiitic basalt, and a close chemical affinity exists with the other lavas of the Grímsvötn-Laki volcanic system.

Geographic entities mentioned:
surface_form: Bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
surface_form: bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
It is believed that the four eruptions between 1996 and 2011 could mark the beginning of an active period, during which an eruption in Grímsvötn in Vatnajökull may be expected every 2–7 years. Parallel volcanic activity in nearby Bárðarbunga is known to be associated with increased activity in Grímsvötn.

Geographic entities mentioned:
surface_form: Bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
surface_form: bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
surface_form: grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
The Laki eruptions which were both effusive and explosive between June 1783 and February 1784, produced the Skaftáreldahraun lava flows, which cover a large part of south-east Iceland. Before this the tip of the Rauðhólar-Eldgígur fissure system was active with the production of the 4550 BCE Botnahraun lava flow which extends beyond the furtherest extent to the south of the Laki lava field.

Geographic entities mentioned:
surface_form: rauðhólar
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.09527778
lon: -21.75527778
surface_form: rauðhólar
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.95027778
lon: -16.52444444
There are two recent pre-historic but undated Bergvatnsárhraun lava flows just on the south-eastern edge of the Vatnajökull glacier, related to the line of the Rauðhólar-Eldgígur fissures. Bacteria in the subglacial lakes. In 2004, a community of bacteria was detected in water of the Grímsvötn lake under the glacier, the first time that bacteria have been found in a subglacial lake.

Geographic entities mentioned:
surface_form: rauðhólar
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.09527778
lon: -21.75527778
surface_form: rauðhólar
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.95027778
lon: -16.52444444
The volcanic system is part of the Eastern volcanic zone of Iceland, and is directly over the Iceland mantle plume. The volcanic system has crater rows extending to the south east; the long Laki–Grímsvötn fissure system and the long Rauðhólar-Eldgígur fissure system.

Geographic entities mentioned:
surface_form: rauðhólar
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.09527778
lon: -21.75527778
surface_form: rauðhólar
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.09527778
lon: -21.75527778
surface_form: grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
surface_form: rauðhólar
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.95027778
lon: -16.52444444
surface_form: rauðhólar
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.95027778
lon: -16.52444444
Grímsvötn. Grímsvötn (; &quot;vötn&quot; = &quot;waters&quot;, singular:) is an active volcano with a (partially subglacial) fissure system located in Vatnajökull National Park, Iceland. The central volcano is completely subglacial and located under the northwestern side of the Vatnajökull ice cap. The subglacial caldera is at, at an elevation of.

Geographic entities mentioned:
surface_form: grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
The central volcano is completely subglacial and located under the northwestern side of the Vatnajökull ice cap. The subglacial caldera is at, at an elevation of. Beneath the caldera is the magma chamber of the Grímsvötn volcano. Grímsvötn is a basaltic volcano which has the highest eruption frequency of all the volcanoes in Iceland. It has a southwest-northeast-trending fissure system.

Geographic entities mentioned:
surface_form: grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
surface_form: grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
Grímsvötn is a basaltic volcano which has the highest eruption frequency of all the volcanoes in Iceland. It has a southwest-northeast-trending fissure system. The massive climate-impacting Laki fissure eruption of 1783–1784 took place in a part of the same Grímsvötn-Laki volcanic system. Grímsvötn was erupting at the same time as Laki during 1783, but continued to erupt until 1785.

Geographic entities mentioned:
surface_form: grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
surface_form: grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
Jökulhlaup. Eruptions in the caldera regularly cause glacial outbursts known as jökulhlaup. Eruptions or geothermal activity, melt enough ice to fill the Grímsvötn caldera with water, and the pressure may be enough to suddenly lift the ice cap, allowing huge quantities of water to escape rapidly. Earthquakes and seismic tremor may occur.

Geographic entities mentioned:
surface_form: grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
A strong earthquake at Bárðarbunga, about magnitude 5, is believed to have been related to the triggering of the eruption in Gjálp. On the other hand, because the magma erupted showed strong connections to the Grímsvötn Volcanic System according to petrology studies, the 1996 as well as a former eruption at Gjálp in the 1930s are thought to have taken place within Grímsvötn Volcanic system.

Geographic entities mentioned:
surface_form: grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
surface_form: grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
1998 and 2004 eruptions. A week-long eruption occurred at Grímsvötn starting on 28 December 1998, but no glacial burst occurred. In November 2004, a week-long eruption occurred. Volcanic ash from the eruption fell as far away as mainland Europe and caused short-term disruption of airline traffic into Iceland, but again no glacial burst followed the eruption. 2011 eruption.

Geographic entities mentioned:
surface_form: grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
2011 eruption. Harmonic tremors were recorded twice around Grímsvötn on 2 and 3 October 2010, possibly indicating an impending eruption. At the same time, sudden inflation was measured by GPS in the volcano, indicating magma movement under the caldera.

Geographic entities mentioned:
surface_form: grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
On 21 May 2011 at 19:25 UTC, an eruption began, with high plumes accompanied by multiple earthquakes, Until 25 May, the eruption scale had been larger than that of the 2010 eruption of Eyjafjallajökull. The ash cloud from the eruption rose to, and was so far 10 times larger than the 2004 eruption, and the strongest in Grímsvötn in the last 100 years.

Geographic entities mentioned:
surface_form: grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
Jökulhlaup (glacial lake flooding) can occur before or after an eruption. On 4 December 2021, a jökulhlaup occurred from Grímsvötn into the Gígjukvísl river, with an average flow of. Two days later, the Icelandic Meteorological Office increased the alert level for Grímsvötn from yellow to orange, after a series of earthquakes was detected.

Geographic entities mentioned:
surface_form: grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
On 11 December 2023, a jökulhlaup followed in time, a earthquake. Eruption history before 1990. Tephra studies on soil samples from around the Vatnajökull ice-cap, show that the Grímsvötn volcanic system has high activity for Iceland, and had between 4 to 14 explosive eruptions every 100 years (mean about 7 eruptions every 100 years) between 7600 years ago and 870 AD.

Geographic entities mentioned:
surface_form: grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
Bacteria in the subglacial lakes. In 2004, a community of bacteria was detected in water of the Grímsvötn lake under the glacier, the first time that bacteria have been found in a subglacial lake. The lakes never freeze because of the volcanic heat. The bacteria can also survive at low concentrations of oxygen.

Geographic entities mentioned:
surface_form: grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
Geology. There is the potential for mechanical interaction such as dyke propagation between Grímsvötn and Thordarhyrna. Interactions can also occur with the nearby Bárðarbunga volcano, which is part of a separate volcanic system. The volcano erupts predominantly tholeiitic basalt, and a close chemical affinity exists with the other lavas of the Grímsvötn-Laki volcanic system.

Geographic entities mentioned:
surface_form: grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33