Sarmila/GeoWiki-Features huggingface dataset:
Pitusiray. Pitusiray is a mountain in the Urubamba mountain range in the Andes of Peru. It is located in the Cusco Region, Calca Province, Calca District, north of the Vilcanota River. Pitusiray is situated southeast of Huamanchoque and south of another mountain known as Ancasmarca, Pitusiray or Sallcasa which lies beyond the two valleys north of this mountain and northeast of Huamanchoque.

Geographic entities mentioned:
surface_form: pitusiray
instance_of: Mountain
countries: Peru
coordinates: lat: -13.27527778
lon: -71.98694444
Yanaorco (Coris-Locroja). Yanaorco (possibly from in the Quechua spelling &quot;Yana Urqu&quot;: &quot;yana&quot; black, &quot;urqu&quot; mountain, &quot;black mountain&quot;) is a mountain in the Andes of Peru which reaches a height of approximately. It is located in the Huancavelica Region, Churcampa Province, on the border of the districts of Coris and Locroja.

Geographic entities mentioned:
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.64027778
lon: -70.79055556
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7411
lon: -70.9597
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7206
lon: -70.98
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.654444
lon: -70.754722
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.27333333
lon: -72.305
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.073888888889
lon: -75.011388888889
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.085277777778
lon: -74.978055555556
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7644
lon: -71.4506
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -12.37916667
lon: -75.70944444
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -12.535555555556
lon: -74.612222222222
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.41388889
lon: -71.22972222
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5464
lon: -72.5772
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -12.33416667
lon: -75.71861111
surface_form: yanaorco
instance_of: Mountain
countries: Peru
coordinates: lat: -12.619444444444
lon: -74.450833333333
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.29861111
lon: -69.77
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.1161
lon: -75.0417
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.6828
lon: -70.9667
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -11.31777778
lon: -75.64083333
Yanaorco (Coris-Locroja). Yanaorco (possibly from in the Quechua spelling &quot;Yana Urqu&quot;: &quot;yana&quot; black, &quot;urqu&quot; mountain, &quot;black mountain&quot;) is a mountain in the Andes of Peru which reaches a height of approximately. It is located in the Huancavelica Region, Churcampa Province, on the border of the districts of Coris and Locroja.

Geographic entities mentioned:
surface_form: yanaorco
instance_of: Mountain
countries: Peru
coordinates: lat: -12.619444444444
lon: -74.450833333333
He became a Superintendent of the Survey in 1883 and retired in 1889. He contributed to Medlicott's Manual of the Geology of India, the fourth part which dealt with mineralogy. Mallet was involved with the survey of coalfields in the Naga Hills, the Son Valley, southern Mirzapur, and Rewa. He accompanied Ferdinand Stoliczka and William Theobald on expeditions to the Sutlej and Spiti valleys.

Geographic entities mentioned:
surface_form: Naga Hills
instance_of: Mountain
countries: Myanmar
India
coordinates: lat: 26
lon: 95
Mallet was involved with the survey of coalfields in the Naga Hills, the Son Valley, southern Mirzapur, and Rewa. He accompanied Ferdinand Stoliczka and William Theobald on expeditions to the Sutlej and Spiti valleys. He was the first geologist to study scientifically the Ramgarh crater, in 1869.

Geographic entities mentioned:
surface_form: Spiti
instance_of: Valley
countries: India
Qing dynasty
coordinates: lat: 32.246944444444445
lon: 78.05222222222223
Smritivan Earthquake Memorial and Museum. Smritivan Earthquake Memorial and Museum is a memorial park dedicated to the victims of 2001 Gujarat earthquake and museum on Bhujiyo Hill in Bhuj, Kutch district (Kachchh), Gujarat, India. The project is developed by Gujarat State Disaster Management Authority (GSDMA) and managed by KPMG Advisory Services Pvt Ltd. History.

Geographic entities mentioned:
surface_form: Bhujiyo Hill
instance_of: Mountain
countries: India
coordinates: lat: 23.24655
lon: 69.69074167
Gosaba River. Gosaba River is a tidal estuarine river in and around the Sundarbans in South 24 Parganas district in the Indian state of West Bengal. The Gosaba River, formed by the confluence of the Raimangal and the Matla rivers, has a broad estuary to the sea (Bay of Bengal).

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Sila used a spindle to beat Buppha. Buppha used a pestle to beat her. Then these two women died and became a mountain. Sila became Khao Ok Thalu and Buppha became Khao Hua Taek (Thaiculturebuu, 2010). Khao Ok Thalu. Khao Ok Thalu is located in Phatthalung Province, Thailand. Another name of Khao Ok Thalu is Khao Chai Buri but Khao Ok Thalu is better-known.

Geographic entities mentioned:
surface_form: Khao Ok Thalu
instance_of: Mountain
countries: Thailand
coordinates: lat: 7.625
lon: 100.09166667
Point Potrero Pond. Potrero Hills Pond is a small lake in Richmond, California. It was formed from quarrying of hills near Potrero Hills at the Blake Brothers Quarry. It is fed by underground springs. It is now polluted and surrounded by a Chevron Richmond Refinery tank farm.

Geographic entities mentioned:
surface_form: brothers
instance_of: Mountain
countries: United States
coordinates: lat: 47.6537193
lon: -123.140575
Point Potrero Pond. Potrero Hills Pond is a small lake in Richmond, California. It was formed from quarrying of hills near Potrero Hills at the Blake Brothers Quarry. It is fed by underground springs. It is now polluted and surrounded by a Chevron Richmond Refinery tank farm.

Geographic entities mentioned:
surface_form: potrero hills pond
instance_of: Lake
countries: United States
coordinates: lat: 37.934297222222
lon: -122.40252222222
Point Potrero Pond. Potrero Hills Pond is a small lake in Richmond, California. It was formed from quarrying of hills near Potrero Hills at the Blake Brothers Quarry. It is fed by underground springs. It is now polluted and surrounded by a Chevron Richmond Refinery tank farm.

Geographic entities mentioned:
surface_form: point potrero pond
instance_of: Lake
countries: United States
coordinates: lat: 37.934297222222
lon: -122.40252222222
Monk's Cowl is a mountain in the Drakensberg in KwaZulu-Natal. It is part of the Drakensberg Escarpment that forms the border between South Africa and Lesotho. Monk's Cowl is the third highest peak in the northern part of the range, after Mont-aux-Sources, which is approximately 38 metres higher. It is the highest free-standing peak and climbers require rock climbing equipment to reach the peak.

Geographic entities mentioned:
surface_form: Mont-aux-Sources
instance_of: Mountain
countries: Lesotho
South Africa
coordinates: lat: -28.759080555556
lon: 28.884644444444
It is the highest free-standing peak and climbers require rock climbing equipment to reach the peak. There is a tarred road, the R600, which leads from Winterton through Cathkin Park past Champagne Castle to the Monks Cowl campsite and Monks Cowl Cottage, slightly lower down in the valley.

Geographic entities mentioned:
surface_form: Champagne Castle
instance_of: Mountain
countries: South Africa
coordinates: lat: -29.093658
lon: 29.331262
Range and habitat. &quot;Quercus repanda&quot; is native to the southern Sierra Madre Oriental, the Trans-Mexican Volcanic Belt, the northernmost Sierra Madre de Oaxaca, and several isolated ranges on the Mexican Plateau in the states of Aguascalientes, Guanajuato, Hidalgo, Michoacán, Puebla, Queretaro, San Luis Potosi, and Veracruz.

Geographic entities mentioned:
surface_form: Mexican Plateau
instance_of: Plateau
countries: Mexico
coordinates: lat: 24
lon: -103
Devils River State Natural Area. Devils River State Natural Area is a section of three ecosystems, the Edwards Plateau, the Tamaulipan mezquital and the Chihuahuan Desert. It is located north of Del Rio, Val Verde County in the U.S. state of Texas. In 1857, future Confederate General John Bell Hood and a small U.S.

Geographic entities mentioned:
surface_form: Edwards Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 30.3
lon: -99.6
JW Marriott Chennai. JW Marriott Chennai was a five-star luxury hotel under construction in Chennai, India. The 357-room hotel, being built at MRC Nagar on the seafront of Chennai facing the Bay of Bengal near the Adyar estuary, is being developed at a cost of 6,200 million and forms part of Marriott International Inc.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
He was a member of the Queen's Jubilee Committee, acting as honorary secretary for some years and took part in the £20,000 construction of the Jubilee Road (today's Victoria Road) and the Hospital for Women and Children (later known as Victoria Hospital). He resided at the Peak and was member of the Hong Kong Club.

Geographic entities mentioned:
surface_form: the Peak
instance_of: Mountain
countries: People's Republic of China
British Hong Kong
coordinates: lat: 22.275469444444
lon: 114.14382777778
Burks Mountain. Burks Mountain is an elevated area in Columbia County, Georgia. Its summit is 474 feet above sea level. It lies within a region of the Piedmont which is characterized mainly by a broad southwest-to-northeast area of felsic igneous and metamorphic rock such as gneiss, schist, granite, and phyllite, as mapped by J. H. Hetrich.

Geographic entities mentioned:
surface_form: piedmont
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -80
The ultramafic area is not large enough to have its own soil unit mapped. Nevertheless, Burks Mountain has a particularly notable example of the &quot;Piedmont Ultramafic Barrens and Woodland&quot; community, with Longleaf Pine (usually associated with the Coastal Plain) growing alongside rare species such as Dixie Mountain Breadroot.

Geographic entities mentioned:
surface_form: piedmont
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -80
surface_form: burks mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.62094
lon: -82.23237
Burks Mountain. Burks Mountain is an elevated area in Columbia County, Georgia. Its summit is 474 feet above sea level. It lies within a region of the Piedmont which is characterized mainly by a broad southwest-to-northeast area of felsic igneous and metamorphic rock such as gneiss, schist, granite, and phyllite, as mapped by J. H. Hetrich.

Geographic entities mentioned:
surface_form: burks mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.62094
lon: -82.23237
H. Hetrich. Within the corresponding area dominated by felsic rock across the Savannah River in South Carolina, small bands of mafic rock such as amphibolite, and ultramafic rock such as dunite, soapstone, and serpentine are mapped by Horton and Dicken. Hetrich does not separate the mafic or ultramafic rock areas of Burks Mountain from his map unit of undifferentiated felsic rock.

Geographic entities mentioned:
surface_form: burks mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.62094
lon: -82.23237
Location. Watts Bar Dam is located approximately upstream from the mouth of the Tennessee River, roughly halfway between Knoxville and Chattanooga. Just north of the dam, the Tennessee absorbs the Piney River, which flows down from the Cumberland Plateau to the west. The nearest towns of note are Spring City (a few miles to the northwest) and Decatur (a few miles to the south).

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
According to Tadesse Tamrat he ruled the whole of the Maya, Genz, Fatagar, Wej, and Lake Hayq. King Eskender supported the Muslims the Negus captured and killed Amdu. When the news spread that the second most powerful monarch of Ethiopia died, Welde Silus, Amdu’s nephew, swore to kill Eskender.

Geographic entities mentioned:
surface_form: Lake Hayq
instance_of: Lake
countries: Ethiopia
coordinates: lat: 11.333333333333
lon: 39.716666666667
In Prague in 1927 he founded the Young Art group, which had its first exhibition in 1928 and from which the Prague Secession emerged in 1929. In the same year he also stayed in the Giant Mountains. In 1932 he traveled to Italy and stayed in Torbole on Lake Garda. In 1933–34 he worked on the large ceiling fresco of the former German House in Prague. His marriage to Duras ended in divorce in 1933.

Geographic entities mentioned:
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
He spent three years on the Harvard crew. He was its captain in 1885 and helped lead the Crimson to victory in that year's Harvard–Yale Regatta. Storrow met Helen Osborne, daughter of David Munson and Eliza Wright Osborne and sister of Thomas Mott Osborne, while attempting to scale the Matterhorn in Switzerland. They married and had one son, James Jackson Storrow III (1892-1977).

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
There are many national parks surrounding the Brisbane metropolitan area which are popular recreational attractions for hiking and bushwalking. The D'Aguilar National Park runs along the northwest of the metropolitan area in the D'Aguilar Range, and contains popular bushwalking and hiking peaks at Mount Nebo, Camp Mountain, Mount Pleasant, Mount Glorious, Mount Samson and Mount Mee.

Geographic entities mentioned:
surface_form: Mount Mee
instance_of: Mountain
countries: Australia
coordinates: lat: -27.074166666667
lon: 152.76972222222
Cape Moreton Light is Queensland's oldest lighthouse at Cape Moreton, a panorama that affords a great vantage point for spotting migratory whales
Mt Mee. Mount Mee, nestled in the D'Aguilar National Park, offers misty forests that provide a refreshing contrast to the coastal heat, and its scenic lookouts offer breathtaking views of the surrounding landscapes.

Geographic entities mentioned:
surface_form: Mount Mee
instance_of: Mountain
countries: Australia
coordinates: lat: -27.074166666667
lon: 152.76972222222
The Gold Coast hinterland features rainforests and wet sclerophyll forest with walking tracks and picnic areas. Some areas also offer camping sites, bed-and-breakfast accommodation, cafes and markets. Popular areas for tourism include Springbrook National Park, Lamington National Park and Tamborine Mountain. The Hinterland is promoted as &quot;The Green Behind The Gold&quot;. Bribie Island.

Geographic entities mentioned:
surface_form: Tamborine Mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -27.927513888889
lon: 153.19430555556
Ayamaru Lakes. The Ayamaru Lakes (sometimes spelled Ajamaru) are a group of lakes found in the west-central part of the Bird's Head Peninsula in Southwest Papua, Indonesia. The nearest village to the group is Greemakolo. The many villages around the Ayamaru Lakes speak the Ayamaru language, a dialect of the Maybrat language. Etymology.

Geographic entities mentioned:
surface_form: ayamaru lakes
instance_of: Group of lakes
countries: Indonesia
coordinates: lat: -1.26666667
lon: 132.2
The water in both lakes is a clear blue because of the rich material in the water. There are deep holes in the lakes that lead to underwater caverns. The vivid colors on the north shores of the Ayamaru Lakes are the result of pigmented bacteria in the microbial mats that grow around the edges of the mineral-rich water.

Geographic entities mentioned:
surface_form: ayamaru lakes
instance_of: Group of lakes
countries: Indonesia
coordinates: lat: -1.26666667
lon: 132.2
Partry House. Partry House is a Georgian country house near Lough Carra in County Mayo and the historic family seat of the Lynch-Blosse baronets. It was built in the 17th century, originally as a dower house, on the ruins of the family's Cloonlagheen Castle. History.

Geographic entities mentioned:
surface_form: Lough Carra
instance_of: Lake
countries: Ireland
coordinates: lat: 53.681388888889
lon: -9.2408333333333
Serrated Peak. Serrated Peak is a mountain summit in the US state of Alaska. Description. Serrated Peak is located in the Fairweather Range of the Saint Elias Mountains. It is set within Glacier Bay National Park and Preserve and is situated southeast of Blackthorn Peak. Precipitation runoff from the mountain drains into Dundas River, thence Icy Strait.

Geographic entities mentioned:
surface_form: Blackthorn Peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.5739
lon: -136.5717
Serrated Peak. Serrated Peak is a mountain summit in the US state of Alaska. Description. Serrated Peak is located in the Fairweather Range of the Saint Elias Mountains. It is set within Glacier Bay National Park and Preserve and is situated southeast of Blackthorn Peak. Precipitation runoff from the mountain drains into Dundas River, thence Icy Strait.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: serrated peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.5064
lon: -136.4778
Serrated Peak. Serrated Peak is a mountain summit in the US state of Alaska. Description. Serrated Peak is located in the Fairweather Range of the Saint Elias Mountains. It is set within Glacier Bay National Park and Preserve and is situated southeast of Blackthorn Peak. Precipitation runoff from the mountain drains into Dundas River, thence Icy Strait.

Geographic entities mentioned:
surface_form: serrated peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.5064
lon: -136.4778
Board on Geographic Names. Climate. Based on the Köppen climate classification, Serrated Peak is located in a marine subpolar climate zone, with long, cold, snowy winters, and cool summers. Weather systems coming off the Gulf of Alaska are forced upwards by the Saint Elias Mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall.

Geographic entities mentioned:
surface_form: serrated peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.5064
lon: -136.4778
Geography. According to the U.S. Census Bureau, the county has an area of, of which is land and (3.8%) is water. It is the second-smallest county in Nevada by area. The highest point is East Peak at, while the most topographically prominent mountain is Mount Siegel. Douglas County is in western Nevada in the western United States.

Geographic entities mentioned:
surface_form: Mount Siegel
instance_of: Mountain
countries: United States
coordinates: lat: 38.889564
lon: -119.502187
Its instructional mission includes undergraduate, graduate, professional and continuing education offered through resident instruction. Its main campus lies between central Chiang Mai and Doi Suthep in Chiang Mai province. The university was the first institution of higher education in northern Thailand, and the first provincial university in Thailand. Campuses.

Geographic entities mentioned:
surface_form: Doi Suthep
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.816388888889
lon: 98.893055555556
Amisquioumisca Lake. Amisquioumisca Lake is a freshwater body consisting of a major body of water in the Nipukatasi River, on the South Hydrographic Slope of the Broadback River, in the Municipality of Eeyou Istchee Baie-James (municipality), in the administrative region of Nord-du-Québec, in Quebec, in Canada. The forestry is the main economic activity of the sector.

Geographic entities mentioned:
surface_form: Nipukatasi River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.729166666667
lon: -76.213611111111
surface_form: amisquioumisca lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.4575
lon: -76.215
Toponymy. In the past, the word &quot;Amiskwumiska lake&quot; was used to designate this body of water. The toponym &quot;lac Amisquioumisca&quot; was formalized on December 5, 1968 at the Commission de toponymie du Québec, at the creation of this commission.

Geographic entities mentioned:
surface_form: lac amisquioumisca
instance_of: Lake
countries: Canada
coordinates: lat: 50.4575
lon: -76.215
Amisquioumisca Lake. Amisquioumisca Lake is a freshwater body consisting of a major body of water in the Nipukatasi River, on the South Hydrographic Slope of the Broadback River, in the Municipality of Eeyou Istchee Baie-James (municipality), in the administrative region of Nord-du-Québec, in Quebec, in Canada. The forestry is the main economic activity of the sector.

Geographic entities mentioned:
surface_form: amisquioumisca lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.4575
lon: -76.215
The forestry is the main economic activity of the sector. Recreational
The hydrographic slope of Amisquioumisca Lake is accessible via the James Bay Highway (North-South direction) from Matagami, passing on the west side of the lake. The surface of Amisquioumisca Lake is usually frozen from early November to mid-May, however, safe ice circulation is generally from mid-November to mid-April.

Geographic entities mentioned:
surface_form: amisquioumisca lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.4575
lon: -76.215
surface_form: matagami
instance_of: Lake
countries: Canada
coordinates: lat: 49.8667
lon: -77.4464
Recreational
The hydrographic slope of Amisquioumisca Lake is accessible via the James Bay Highway (North-South direction) from Matagami, passing on the west side of the lake. The surface of Amisquioumisca Lake is usually frozen from early November to mid-May, however, safe ice circulation is generally from mid-November to mid-April. Toponymy.

Geographic entities mentioned:
surface_form: amisquioumisca lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.4575
lon: -76.215
Mbulu Highlands. t7gthh6n12h6yer328qcvznqinyho" xml:space="preserve">The Mbulu Highlands is a plateau in north-central Tanzania. Geography. The Mbulu Highlands lie between the basins of Lake Eyasi to the west and Lake Manyara to the east. The plateau ranges from 1500 to 2300 meters in elevation. The highlands extend northeast-southwest.

Geographic entities mentioned:
surface_form: Lake Eyasi
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.66667
lon: 35.08333
surface_form: Lake Manyara
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.5833333333333
lon: 35.833333333333
surface_form: manyara
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.5833333333333
lon: 35.833333333333
surface_form: mbulu highlands
instance_of: Plateau
countries: Tanzania
coordinates: lat: -3.8556
lon: 35.5444
The plateau ranges from 1500 to 2300 meters in elevation. The highlands extend northeast-southwest. A steep northeast-southwest-running escarpment bounds the highlands on the east, overlooking the basins of Lake Manyara, and further south, Lake Balangida. The plateau descends less steeply in a series of ridges and valleys to Lake Eyasi to the west and the Yaeda Valley to the southwest.

Geographic entities mentioned:
surface_form: Lake Balangida
instance_of: Lake
countries: Tanzania
coordinates: lat: -4.33333333
lon: 35.33333333
surface_form: lake manyara
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.5833333333333
lon: 35.833333333333
surface_form: manyara
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.5833333333333
lon: 35.833333333333
The highlands extend northeast-southwest. A steep northeast-southwest-running escarpment bounds the highlands on the east, overlooking the basins of Lake Manyara, and further south, Lake Balangida. The plateau descends less steeply in a series of ridges and valleys to Lake Eyasi to the west and the Yaeda Valley to the southwest. To the north lies the volcanic Ngorongoro Highlands.

Geographic entities mentioned:
surface_form: Yaeda Valley
instance_of: Valley
countries: Tanzania
coordinates: lat: -4.0003083333333
lon: 34.999916666667
The plateau descends less steeply in a series of ridges and valleys to Lake Eyasi to the west and the Yaeda Valley to the southwest. To the north lies the volcanic Ngorongoro Highlands. The volcanic peak of Mount Hanang rises south of Lake Balangida. The highlands lie mostly in Mbulu District of Manyara Region, extending northwards into Karatu District of Arusha Region.

Geographic entities mentioned:
surface_form: Mount Hanang
instance_of: Mountain
countries: Tanzania
coordinates: lat: -4.435
lon: 35.4
To the north lies the volcanic Ngorongoro Highlands. The volcanic peak of Mount Hanang rises south of Lake Balangida. The highlands lie mostly in Mbulu District of Manyara Region, extending northwards into Karatu District of Arusha Region. The principal town on the plateau is Mbulu.

Geographic entities mentioned:
surface_form: manyara
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.5833333333333
lon: 35.833333333333
Ecology. The natural vegetation of the plateau is mostly miombo woodland. In the northern highlands, volcanic grasslands occur on soils formed from volcanic ash. Montane evergreen forests occur at higher elevations. The plateau has two forest reserves, Nou (305.19 km²) and Hassama (49.01 km²). Drier &quot;Acacia-Commiphora&quot; bushlands and thickets occupy the Eyasi and Manyara lowlands.

Geographic entities mentioned:
surface_form: manyara
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.5833333333333
lon: 35.833333333333
Mbulu Highlands. t7gthh6n12h6yer328qcvznqinyho" xml:space="preserve">The Mbulu Highlands is a plateau in north-central Tanzania. Geography. The Mbulu Highlands lie between the basins of Lake Eyasi to the west and Lake Manyara to the east. The plateau ranges from 1500 to 2300 meters in elevation. The highlands extend northeast-southwest.

Geographic entities mentioned:
surface_form: mbulu highlands
instance_of: Plateau
countries: Tanzania
coordinates: lat: -3.8556
lon: 35.5444
Sant'Elia a Pianisi is a &quot;comune&quot; (municipality) in the Province of Campobasso in the region of Molise, about northeast of Campobasso. As of 31 December 2021, it had a population of 1,585 and an area of. Near Sant'Elia, is the Occhito Lake. The neighbouring comuni are Bonefro, Carlantino, Colletorto, Macchia Valfortore, Monacilioni, Ripabottoni and San Giuliano di Puglia.

Geographic entities mentioned:
surface_form: Occhito Lake
instance_of: Lake
countries: Italy
coordinates: lat: 41.58
lon: 14.945
Qulluta (Recuay). Qulluta (Quechua for mortar, also spelled &quot;Collota&quot;) is a mountain in the Cordillera Negra in the Andes of Peru which reaches a height of approximately. It is located in the Ancash Region, Recuay Province, on the border of the districts of Huayllapampa and Marca.

Geographic entities mentioned:
surface_form: qulluta
instance_of: Mountain
countries: Peru
coordinates: lat: -13.2558
lon: -74.895
surface_form: qulluta
instance_of: Mountain
countries: Peru
coordinates: lat: -8.46666667
lon: -77.525
surface_form: qulluta
instance_of: Mountain
countries: Peru
coordinates: lat: -9.97694444
lon: -77.45583333
surface_form: qulluta
instance_of: Mountain
countries: Peru
coordinates: lat: -8.80416667
lon: -77.64944444
Félicité Carrel. Félicité Carrel was an Italian mountaineer, known for her 1867 attempt to climb Mount Matterhorn. Biography. Carrel was the daughter of Italian mountaineer Jean-Antoine Carrel. In 1867 Carrel and her father joined climbers Caesar Carrel, J.J. and J.P. Maquignaz in an attempt to scale Mount Matterhorn.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
The amphitheater is also used for concerts, graduation ceremonies, and other special events. Adjacent is the 300-seat McKelligon Canyon Pavilion. Sugarloaf Mountain stands at the entrance to the Canyon (the mountain is the leftmost peak, pictured in the adjacent image). The peak of Sugarloaf is at 31.82910° N, -106.468054° W. Description.

Geographic entities mentioned:
surface_form: mckelligon canyon
instance_of: Landform
countries: United States
coordinates: lat: 31.8211
lon: -106.468
Adjacent is the 300-seat McKelligon Canyon Pavilion. Sugarloaf Mountain stands at the entrance to the Canyon (the mountain is the leftmost peak, pictured in the adjacent image). The peak of Sugarloaf is at 31.82910° N, -106.468054° W. Description. McKelligon Canyon lies on the south eastern side of the Franklin Mountains and surrounded by canyon walls.

Geographic entities mentioned:
surface_form: sugarloaf
instance_of: Mountain
countries: United States
coordinates: lat: 43.832777777778
lon: -74.822222222222
McKelligon Canyon. McKelligon Canyon is the location of a 1,503-seat amphitheater located in El Paso, Texas, United States, where the play &quot;Viva El Paso!&quot; is presented. The amphitheater is also used for concerts, graduation ceremonies, and other special events. Adjacent is the 300-seat McKelligon Canyon Pavilion.

Geographic entities mentioned:
surface_form: mckelligon canyon
instance_of: Landform
countries: United States
coordinates: lat: 31.8211
lon: -106.468
Visitors have a variety of rock climbing routes to choose from and the symmetric terrain is filled with crevices and cracks. All hiking trails including the Ron Coleman Trail begin at the end of McKelligon Canyon and are open year-round. McKelligon Canyon is part of the Franklin Mountains State Park and is subject to fees and restrictions from the Texas parks and Wildlife Department. History.

Geographic entities mentioned:
surface_form: mckelligon canyon
instance_of: Landform
countries: United States
coordinates: lat: 31.8211
lon: -106.468
surface_form: mckelligon canyon
instance_of: Landform
countries: United States
coordinates: lat: 31.8211
lon: -106.468
Emerald Lake (Yukon). Emerald Lake is a lake in the southern Yukon, notable for its intense green colour. It is located on the South Klondike Highway at kilometre 117.5 (mile 73.5), measured from Skagway, Alaska. The colour derives from light reflecting off white deposits of marl, a mixture of clay and calcium carbonate, at the bottom of the shallow waters.

Geographic entities mentioned:
surface_form: emerald lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.18338
lon: -106.96724
surface_form: emerald lake
instance_of: Lake
countries: Canada
coordinates: lat: 60.2663
lon: -134.7507
surface_form: emerald lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.444
lon: -116.531
Talmadge River. The Talmadge River is a river in southern St. Louis County, Minnesota. It flows through Lakewood Township into Lake Superior, just north of the city of Duluth. Talmadge River is named after Josiah Talmadge, a pioneer who settled near the river in 1856.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The geothermal activity may be the source of the name &quot;Pocosol&quot;. The active volcano Arenal lies north-northwest of Laguna Poco Sol. Arenal along with Cerro Chato between Arenal and Laguna Poco Sol and Cerro Pocosol south of Laguna Poco Sol may be located along a zone of tectonic weakness that was accompanied by northeast-migrating volcanism.

Geographic entities mentioned:
surface_form: Arenal
instance_of: Mountain
countries: Costa Rica
coordinates: lat: 10.463333333333
lon: -84.703333333333
surface_form: arenal
instance_of: Mountain
countries: Costa Rica
coordinates: lat: 10.463333333333
lon: -84.703333333333
surface_form: laguna poco sol
instance_of: Lake
countries: Costa Rica
coordinates: lat: 10.35
lon: -84.67
The geothermal activity may be the source of the name &quot;Pocosol&quot;. The active volcano Arenal lies north-northwest of Laguna Poco Sol. Arenal along with Cerro Chato between Arenal and Laguna Poco Sol and Cerro Pocosol south of Laguna Poco Sol may be located along a zone of tectonic weakness that was accompanied by northeast-migrating volcanism.

Geographic entities mentioned:
surface_form: chato
instance_of: Mountain
countries: Costa Rica
coordinates: lat: 10.441944444444
lon: -84.688055555556
surface_form: arenal
instance_of: Mountain
countries: Costa Rica
coordinates: lat: 10.463333333333
lon: -84.703333333333
surface_form: laguna poco sol
instance_of: Lake
countries: Costa Rica
coordinates: lat: 10.35
lon: -84.67
surface_form: laguna poco sol
instance_of: Lake
countries: Costa Rica
coordinates: lat: 10.35
lon: -84.67
Laguna Poco Sol. Lake Poco Sol (from Spanish, &quot;Little Sunshine&quot;), or, is a volcanic lake in Costa Rica, in the Cordillera de Tilarán. The lake lies at an altitude of in a wide depression. The depth of the lake is about. Other volcanic features in the area include breccia, lahar deposits, lava flows and tuffs. The lake may be a landslide scar, or a crater left by a phreatic explosion.

Geographic entities mentioned:
surface_form: laguna poco sol
instance_of: Lake
countries: Costa Rica
coordinates: lat: 10.35
lon: -84.67
Cifuentes was elected to Parliament as a representative of Rancagua in 1867 and was reelected five times. In 1892, he was elected Senator of Llanquihue in 1892, Aconcagua in 1894, and then Santiago in 1904.

Geographic entities mentioned:
surface_form: Aconcagua
instance_of: Mountain
countries: Argentina
coordinates: lat: -32.653055555555554
lon: -70.01166666666667
Trails. The Old Depot Museum marks the beginning of the Prairie Spirit Trail. This trail is 33 miles long and follows what used to be a railroad track, which originally began at the Santa Fe Depot. This trail was Kansas' first &quot;rail-trail.&quot;
The museum can also be a trailhead for the Flint Hills Nature Trail.

Geographic entities mentioned:
surface_form: Flint Hills
instance_of: Landform
countries: United States
coordinates: lat: 37.2833
lon: -96.6753
On the board, he &quot;earned a reputation for shouldering the real or fancied troubles of dissatisfied ex-patients&quot;. He was also a member of the Lake Monger Board and the Karrakatta Cemetery Board. In the general campaign were policies of electoral, taxation, land, industrial and mining reform. Premier of Western Australia.

Geographic entities mentioned:
surface_form: Lake Monger
instance_of: Lake
countries: Australia
coordinates: lat: -31.9294
lon: 115.8265
2011 Nabro eruption. The 2011 Nabro eruption was an eruption of the Nabro stratovolcano in the Southern Red Sea Region of Eritrea, which began on 12 June 2011 after a series of earthquakes. The eruption killed seven and possibly a further 31 people and is estimated to be the highest altitude injection of sulfur dioxide (SO2) ever observed by satellite.

Geographic entities mentioned:
surface_form: Nabro stratovolcano
instance_of: Mountain
countries: Eritrea
coordinates: lat: 13.37
lon: 41.7
Eruption. On 12 June 2011, satellite images showed a large volcanic eruption shortly after 22.00 UTC 12 June (close to 01.00 13 June local time), in the Southern Red Sea Region. It was first thought to have originated at Dubbi Volcano, but has been confirmed to be from the Nabro stratovolcano in Eritrea, near the Ethiopian border.

Geographic entities mentioned:
surface_form: Dubbi Volcano
instance_of: Mountain
countries: Eritrea
coordinates: lat: 13.578888888889
lon: 41.809166666667
His own tasks were to survey the distribution of flat houses, particular to the northern slopes of Mount Elgon, and then to survey the spread of conical-roofed houses, as an indicator of the break-up or continuity of the existing culture. He later said of this trip that the &quot;themes can be seen to resonate throughout much of my academic work&quot;.

Geographic entities mentioned:
surface_form: Mount Elgon
instance_of: Mountain
countries: Uganda
Kenya
coordinates: lat: 1.1185
lon: 34.5265
It is one of the six volcanic systems under Vatnajökull. The central volcano has a rim that rises to about above sea level, making it the second highest mountain in Iceland, being lower than Hvannadalshnjúkur. The caldera is about, up to wide and about deep. The surrounding edges rise to, but the base is on average close to.

Geographic entities mentioned:
surface_form: Hvannadalshnjúkur
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.015833333333
lon: -16.674722222222
There has been frequent volcanic activity outside the glacier to the south-west in the highlands between Vatnajökull and Mýrdalsjökull, and also to the north-east toward Dyngjufjöll. The Bárðarbunga volcanic system is associated with a second central volcano Hamarinn which has been classified historically as part of a separate Loki-Fögrufjöll volcanic system.

Geographic entities mentioned:
surface_form: Loki-Fögrufjöll
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.480277777778
lon: -17.832222222222
surface_form: hamarinn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.480277777778
lon: -17.832222222222
surface_form: loki-fögrufjöll
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
To the west of the central volcanoes is the less active volcanic system of Tungnafellsjökull and to the central volcanoes south west, also under Vatnajökull is the very active Grímsvötn volcanic system.

Geographic entities mentioned:
surface_form: Grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
877. Many large eruptions have occurred south-west of the glacier; the first occurring since human settlement of Iceland was the Vatnaöldur eruption about 877 ± 2 CE which had a volcanic explosivity index (VEI) of 4. 1477. The Veiðivötn eruption in 1477 is the largest known Icelandic eruption, with a VEI of 6. 1701–1864.

Geographic entities mentioned:
surface_form: Vatnaöldur
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.119533548
lon: -18.9128769387
surface_form: vatnaöldur
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.119533548
lon: -18.9128769387
877. Many large eruptions have occurred south-west of the glacier; the first occurring since human settlement of Iceland was the Vatnaöldur eruption about 877 ± 2 CE which had a volcanic explosivity index (VEI) of 4. 1477. The Veiðivötn eruption in 1477 is the largest known Icelandic eruption, with a VEI of 6. 1701–1864.

Geographic entities mentioned:
surface_form: Veiðivötn
instance_of: Lake
countries: Iceland
coordinates: lat: 64.11613889
lon: -18.84797222
1910 was the last known significant eruption of the Bárðarbunga volcanic system before the 2014 eruptions. It occurred in the Loki-Fögrufjöll volcano. 1996. The Gjálp fissure vent eruption in 1996 revealed that an interaction may exist between Bárðarbunga and Grímsvötn. A strong earthquake in Bárðarbunga, about 5 on the Richter scale, is believed to have started the eruption in Gjálp.

Geographic entities mentioned:
surface_form: Grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
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
On 28 February 2015, it was officially reported that the eruption was over. Nevertheless, the gas pollution still existed, and the area north of Bárðarbunga, including volcanoes Askja and Herðubreið, still remained closed for visitors. On 16 March 2015, the area north of Bárðarbunga was opened for visitors, excluding the new lava field and the area within 20 metres around it. 2024.

Geographic entities mentioned:
surface_form: Herðubreið
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.183333333333
lon: -16.35
surface_form: herðubreið
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.183333333333
lon: -16.35
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
There have also been smaller eruptions in an ice-free area of Dyngjuháls to the north-east. Eruptions appear to follow a cycle: there were several eruptions in the glacier between 1701 and 1740 and since 1780. 1910 eruption. 1910 was the last known significant eruption of the Bárðarbunga volcanic system before the 2014 eruptions. It occurred in the Loki-Fögrufjöll volcano. 1996.

Geographic entities mentioned:
surface_form: bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
The Bárðarbunga volcanic system is associated with a second central volcano Hamarinn which has been classified historically as part of a separate Loki-Fögrufjöll volcanic system. Hamarinn is to the south-west of the Bárðarbunga central volcano. Context.

Geographic entities mentioned:
surface_form: hamarinn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.480277777778
lon: -17.832222222222
surface_form: bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
Bárðarbunga. Bárðarbunga (, alternative name Veiðivötn), is an active and productive stratovolcano located under Vatnajökull in Vatnajökull National Park which is Iceland's most extensive glacier. The second highest mountain in Iceland, above sea level, Bárðarbunga is also part of the Bárðarbunga-Veiðivötn volcanic system that is approximately long and wide.

Geographic entities mentioned:
surface_form: bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
Bárðarbunga. Bárðarbunga (, alternative name Veiðivötn), is an active and productive stratovolcano located under Vatnajökull in Vatnajökull National Park which is Iceland's most extensive glacier. The second highest mountain in Iceland, above sea level, Bárðarbunga is also part of the Bárðarbunga-Veiðivötn volcanic system that is approximately long and wide.

Geographic entities mentioned:
surface_form: bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
surface_form: veiðivötn
instance_of: Lake
countries: Iceland
coordinates: lat: 64.11613889
lon: -18.84797222
Bárðarbunga. Bárðarbunga (, alternative name Veiðivötn), is an active and productive stratovolcano located under Vatnajökull in Vatnajökull National Park which is Iceland's most extensive glacier. The second highest mountain in Iceland, above sea level, Bárðarbunga is also part of the Bárðarbunga-Veiðivötn volcanic system that is approximately long and wide.

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: veiðivötn
instance_of: Lake
countries: Iceland
coordinates: lat: 64.11613889
lon: -18.84797222
The second highest mountain in Iceland, above sea level, Bárðarbunga is also part of the Bárðarbunga-Veiðivötn volcanic system that is approximately long and wide. Bárðarbunga erupted in late August 2014, the eruption style effusive, which is common in Iceland, but had not been seen for a few years. Lava covered the surrounding landscape northwest of the Vatnajökull glacier. Description.

Geographic entities mentioned:
surface_form: bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
Lava covered the surrounding landscape northwest of the Vatnajökull glacier. Description. Bárðarbunga is a subglacial stratovolcano and central volcano under the ice cap of Vatnajökull glacier in the Vatnajökull National Park in Iceland. It is one of the six volcanic systems under Vatnajökull.

Geographic entities mentioned:
surface_form: bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
Bárðarbunga was a little-known volcano in Iceland due to its remote location and infrequent eruptions approximately once every 50 years, but recent studies have shown that many tephra layers originally thought to be from other volcanoes were ejected from Bárðarbunga, and that lateral dyke intrusions may trigger eruptions in adjacent volcanoes.

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
Sustained seismic activity had been gradually increasing in Bárðarbunga and its associated northern fissure system for seven years starting in 2007 and leading to an eruption towards the end of 2014. This activity had decreased after the Grímsvötn eruption in 2011, but later returned to a similar level as before the eruption. The previous Bárðarbunga eruption was in 1910.

Geographic entities mentioned:
surface_form: bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
This activity had decreased after the Grímsvötn eruption in 2011, but later returned to a similar level as before the eruption. The previous Bárðarbunga eruption was in 1910. There has been frequent volcanic activity outside the glacier to the south-west in the highlands between Vatnajökull and Mýrdalsjökull, and also to the north-east toward Dyngjufjöll.

Geographic entities mentioned:
surface_form: bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
Context. While the central volcanoes of the Bárðarbunga volcanic system are under the western edge of the Vatnajökull ice cap, the system's northern fissure swarm and lava flows extend around the southern flanks of the Askja volcano and the southern fissure swarm extends past the north-west of Torfajökull and almost reaches Tindfjallajökull.

Geographic entities mentioned:
surface_form: bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
The southern lava flows have reached the sea near Selfoss. It is now known that within the area of the rhyolitic caldera of Torfajökull there are younger extrusives that involve basaltic magma mixing events by lateral propagation, from the fissure swarm of Bárðarbunga's volcanic system.

Geographic entities mentioned:
surface_form: bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
In the 1996 eruption of Gjálp which is usually assigned to the Grímsvötn volcanic system, studies are consistent with the eruption being triggered by a lateral dyke intrusion at about depth from Bárðarbunga, although this is not proven. Etymology.

Geographic entities mentioned:
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