Sarmila/GeoWiki-Features huggingface dataset:
Patricia Lake (Alberta). Patricia Lake is a lake in Jasper National Park, Alberta, Canada, near the town of Jasper. It was named for Princess Patricia of Connaught, a granddaughter of Queen Victoria. It is connected by Pyramid Lake road and hiking trails to the town of Jasper, as well as other tourist sites such as Pyramid Lake and Pyramid Mountain. Project Habbakuk.

Geographic entities mentioned:
surface_form: patricia lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.9028
lon: -118.102
Project Habbakuk. Patricia Lake is notable for its involvement during World War II with Project Habbakuk, a plan to build an unsinkable aircraft carrier from an ice-based composite material termed &quot;Pykrete&quot;. Initial studies of natural lake ice had been carried out at Lake Louise. In January 1943, Patricia Lake was chosen as the test site for building a prototype vessel.

Geographic entities mentioned:
surface_form: patricia lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.9028
lon: -118.102
Initial studies of natural lake ice had been carried out at Lake Louise. In January 1943, Patricia Lake was chosen as the test site for building a prototype vessel. The planned vessel was to be long and the prototype was to be a 1:10 scale model of this. In fact, the beam was to approximately this scale, but the length was only 60 feet, about a third of scale.

Geographic entities mentioned:
surface_form: patricia lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.9028
lon: -118.102
Patricia Lake (Alberta). Patricia Lake is a lake in Jasper National Park, Alberta, Canada, near the town of Jasper. It was named for Princess Patricia of Connaught, a granddaughter of Queen Victoria. It is connected by Pyramid Lake road and hiking trails to the town of Jasper, as well as other tourist sites such as Pyramid Lake and Pyramid Mountain. Project Habbakuk.

Geographic entities mentioned:
surface_form: pyramid mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.9944
lon: -120.104
Pyochungsa. Pyochungsa, originally Jungnimsa, is a Korean Buddhist temple of the Jogye Order of Korean Buddhism. It stands on the slopes of Jaeyaksan mountain near Cheonhwangsan in the Yeongnam Alps in Danjang-myeon, northern Miryang, South Korea.

Geographic entities mentioned:
surface_form: Jaeyaksan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.54666667
lon: 128.98055556
March 28, and started a slow decline. The river continued to rise to the north as the crest moved downstream. Geology. The Red River flows from the United States into Lake Winnipeg in Manitoba, Canada. Since it flows northward, into colder climates, melting snow and river ice, as well as runoff from its tributaries, often create ice jams, which cause the river to overflow.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Following the 1997 Red River flood, Grand Forks and East Grand Forks smoothed out some of the river curves in those cities. Rural municipality reeves have approached the Canadian government with a CA$288,000 plan which would use the province of Manitoba's existing Amphibex ice-breaking excavators to dredge the Red River between Selkirk and the mouth of Lake Winnipeg.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
2010–11 Bobsleigh World Cup. The 2010–11 Bobsleigh World Cup was a multi race tournament over a season for bobsleigh. The season started on 22 November 2010 in Whistler, Canada and ended on 27 January 2011 in Königssee, Germany. The World Cup was organised by the FIBT who also run World Cups and Championships in skeleton. This season was sponsored by Viessmann. Calendar.

Geographic entities mentioned:
surface_form: Königssee
instance_of: Lake
countries: Germany
coordinates: lat: 47.55
lon: 12.975
Settlements. The province's capital is Bongor; other major settlements include Djodo Gassa, Fianga, Gam, Gounou Gaya, Guélengdeng, Hollom Gamé, Katoa, Kéra, Kim, Koyom, Moulkou, Nanguigoto, Tikem and Youé. Lake Fianga and Lake Tikem are located in the region. Demographics. The region's population was 495,339 inhabitants in 1993 and 774,782 in the 2009 census.

Geographic entities mentioned:
surface_form: Lake Fianga
instance_of: Lake
countries: Cameroon
Chad
coordinates: lat: 9.9666666666667
lon: 15.2
Urugua-í River. The Urugua-í River () is a river in the Misiones Province of Argentina. It is a tributary of the Paraná River. Course. The Urugua-í River, also called the Marambas or Grande River, has a length of about, including the reservoir formed by the Urugua-í Dam. Tributaries include the Sarita River, Arroyo de las Cabeceras and Uruzú River.

Geographic entities mentioned:
surface_form: urugua-í river
instance_of: Watercourse
countries: Argentina
coordinates: lat: -25.898808
lon: -54.613217
Urugua-í River. The Urugua-í River () is a river in the Misiones Province of Argentina. It is a tributary of the Paraná River. Course. The Urugua-í River, also called the Marambas or Grande River, has a length of about, including the reservoir formed by the Urugua-í Dam. Tributaries include the Sarita River, Arroyo de las Cabeceras and Uruzú River.

Geographic entities mentioned:
surface_form: urugua-í river
instance_of: Watercourse
countries: Argentina
coordinates: lat: -25.898808
lon: -54.613217
surface_form: grande river
instance_of: Watercourse
countries: Argentina
coordinates: lat: -36.870277777778
lon: -69.759722222222
Tributaries include the Sarita River, Arroyo de las Cabeceras and Uruzú River. The Urugua-í River flows through the southern part of the Urugua-í Provincial Park in a southeast – northwest direction and is impounded by the Urugua-í Dam to the west of the park. The park was created in part to compensate for the flooding of of the lower Urugua-í River basin caused by construction of the dam.

Geographic entities mentioned:
surface_form: urugua-í river
instance_of: Watercourse
countries: Argentina
coordinates: lat: -25.898808
lon: -54.613217
Lake Garfield. Lake Garfield is a lake located about north of the center of Monterey, off Route 23 in Berkshire County, Massachusetts. Overview. At the furthest western point of the lake near Tyringham Road, a public boat ramp and parking lot can be found. The town of Monterey makes these amenities unavailable during the period of June 15 through September 6 because of swimming season.

Geographic entities mentioned:
surface_form: lake garfield
instance_of: Lake
countries: United States
coordinates: lat: 42.183
lon: -73.198
The town of Monterey makes these amenities unavailable during the period of June 15 through September 6 because of swimming season. A 1979 survey recorded a total of 12 species of fish inside Lake Garfield: smallmouth bass, largemouth bass, pumpkinseed, yellow perch, chain pickerel, rainbow trout, golden shiner, brown bullhead, bluegill, white sucker, rock bass and white perch.

Geographic entities mentioned:
surface_form: lake garfield
instance_of: Lake
countries: United States
coordinates: lat: 42.183
lon: -73.198
A 1979 survey recorded a total of 12 species of fish inside Lake Garfield: smallmouth bass, largemouth bass, pumpkinseed, yellow perch, chain pickerel, rainbow trout, golden shiner, brown bullhead, bluegill, white sucker, rock bass and white perch. Lake Garfield is a popular fishing site for rainbow trout during spring.

Geographic entities mentioned:
surface_form: lake garfield
instance_of: Lake
countries: United States
coordinates: lat: 42.183
lon: -73.198
Lake Garfield is a popular fishing site for rainbow trout during spring. Due to the dominant yellow and white perch population, gamefish are usually below average size and abundance although a good bass or pickerel may occasionally be produced by the lake. Lake Garfield was named for a local family.

Geographic entities mentioned:
surface_form: lake garfield
instance_of: Lake
countries: United States
coordinates: lat: 42.183
lon: -73.198
Gunnar Gunnarsson. Gunnar Gunnarsson (18 May 1889 – 21 November 1975) was an Icelandic author who wrote mainly in Danish. He grew up, in considerable poverty, on Valþjófsstaður in Fljótsdalur valley and on Ljótsstaðir in Vopnafjörður. During the first half of 20th century he became one of the most popular novelists in Denmark and Germany.

Geographic entities mentioned:
surface_form: Fljótsdalur
instance_of: Valley
countries: Iceland
coordinates: lat: 65.033333333333
lon: -15
This track, along with two others, was released in a special limited edition 10&quot; vinyl, as a promo tool for &quot;Scenes&quot; a book of paintings and poetry by Martin Metcalfe and Paul Hullah. In 2016, the Filthy Tongues released their first album &quot;Jacob's Ladder&quot;, named after a staircase cut into Calton Hill in Edinburgh.

Geographic entities mentioned:
surface_form: Calton Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
These Serbian employees had been the ones to relay to Dubrave the message to turn in their Yugoslav military uniforms and arms, which only a minority, for example Lazo Janjanin, actually did. In their stead, Croats were hired: a local Croat, Franjo Stipetić, became the new municipal president (), while one from Posavina was chosen as the new notary.

Geographic entities mentioned:
surface_form: Posavina
instance_of: Valley
countries: Croatia
Bosnia and Herzegovina
Serbia
coordinates: lat: 45.16667
lon: 17.33333
Amalfinon Monastery. The Amalfinon Monastery (Greek: Μονή των Αμαλφηνών)() or Amalfion was the most prominent of the three former monasteries for Latin-speaking Christians on Mount Athos before the Great Schism. After the events of 1054, its affiliation with either Eastern Orthodox Church or the Catholic Church has been subject of debate.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
However, multiple ecclesiastical Eastern Orthodox scholars believe the praxis of Amalfi to have remained aligned with Eastern Orthodoxy and have pointed out that expulsions of Latin Christians from Eastern Orthodox territory had occurred before, such as the expulsion of Frankish monks from the Mount of Olives in 808 for using the &quot;filioque&quot; in the Creed, or the complete expulsion of all Latins from Constantinople in 1186.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
Rivière des Créoles. rdr1fvbhgjt7ldlbvw8eahbtqk3v" xml:space="preserve">Rivière des Créoles is a river in southeastern Mauritius. It flows southeast for 13 kilometres, reaching the Indian Ocean close to the town of Mahébourg.

Geographic entities mentioned:
surface_form: rivière des créoles
instance_of: Watercourse
countries: Mauritius
coordinates: lat: -20.4
lon: 57.683333333333
Snake Ridge. Snake Ridge () is a serpentine ridge, long, adjoining the northwest extremity of Mackin Table in the Patuxent Range, Pensacola Mountains. Exploration and name. Snake Ridge was mapped by United States Geological Survey (USGS) from surveys and United States Navy air photos in 1956–66. The descriptive name was proposed by Dwight L. Schmidt, USGS geologist to these mountains, 1962–66.

Geographic entities mentioned:
surface_form: Mackin Table
instance_of: Plateau
coordinates: lat: -84.95
lon: -64
Schmidt, USGS geologist to these mountains, 1962–66. Location. Snake Ridge is just west of the northwest end of Mackin Table, to the east of Mount Weininger. A number of nunataks are scattered in the ice-covered terrain to the south, west and north, including Brooks Nunatak, Brazitis Nunatak, Postel Nunatak, DesRoches Nunataks, DeWitt Nunatak, Lawrence Nunatak, Natani Nunatak and White Nunataks.

Geographic entities mentioned:
surface_form: Mackin Table
instance_of: Plateau
coordinates: lat: -84.95
lon: -64
surface_form: Mount Weininger
instance_of: Mountain
coordinates: lat: -84.7833
lon: -65.5
Mount Goyazan. Mount Goyazan () is a mountain which located 20 kilometres far from the northwestern Qazakh District of Azerbaijan. It is located in the vicinity of the villages Abbasbeyli and Alpout, and rises 858 metres above sea level. Ruins of a Goyazan fortress from the 14th century were found near the mountain.

Geographic entities mentioned:
surface_form: goyazan
instance_of: Mountain
countries: Azerbaijan
coordinates: lat: 41.088611111111
lon: 45.184722222222
surface_form: mount goyazan
instance_of: Mountain
countries: Azerbaijan
coordinates: lat: 41.088611111111
lon: 45.184722222222
Mount Goyazan. Mount Goyazan () is a mountain which located 20 kilometres far from the northwestern Qazakh District of Azerbaijan. It is located in the vicinity of the villages Abbasbeyli and Alpout, and rises 858 metres above sea level. Ruins of a Goyazan fortress from the 14th century were found near the mountain.

Geographic entities mentioned:
surface_form: goyazan
instance_of: Mountain
countries: Azerbaijan
coordinates: lat: 41.088611111111
lon: 45.184722222222
Small explosions of gas and ash occur every 15 to 20 minutes, but larger eruptions are less frequent. Andesite and basalt lava types dominate. The volcano is joined with Acatenango volcano to its north and collectively the complex is known as La Horqueta. Between Fuego and Acatenango is La Meseta, a scarp marking the remains of an older volcano that collapsed around 8,500 years ago.

Geographic entities mentioned:
surface_form: Acatenango
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.5
lon: -90.875833333333
surface_form: acatenango
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.5
lon: -90.875833333333
surface_form: acatenango
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.5
lon: -90.875833333333
Volcán de Fuego. Volcán de Fuego (; Spanish for &quot;Volcano of Fire&quot;, often shortened to Fuego) or Chi Q'aq' (Kaqchikel for &quot;where the fire is&quot;) is an active stratovolcano in Guatemala, on the borders of Chimaltenango, Escuintla and Sacatepéquez departments.

Geographic entities mentioned:
surface_form: fuego
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.474722222222
lon: -90.880833333333
surface_form: volcán de fuego
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.474722222222
lon: -90.880833333333
Volcán de Fuego. Volcán de Fuego (; Spanish for &quot;Volcano of Fire&quot;, often shortened to Fuego) or Chi Q'aq' (Kaqchikel for &quot;where the fire is&quot;) is an active stratovolcano in Guatemala, on the borders of Chimaltenango, Escuintla and Sacatepéquez departments.

Geographic entities mentioned:
surface_form: fuego
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.474722222222
lon: -90.880833333333
surface_form: fuego
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.474722222222
lon: -90.880833333333
surface_form: volcán de fuego
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.474722222222
lon: -90.880833333333
Andesite and basalt lava types dominate. The volcano is joined with Acatenango volcano to its north and collectively the complex is known as La Horqueta. Between Fuego and Acatenango is La Meseta, a scarp marking the remains of an older volcano that collapsed around 8,500 years ago. Fuego volcano started to grow after the collapse of La Meseta. Early expeditions.

Geographic entities mentioned:
surface_form: fuego
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.474722222222
lon: -90.880833333333
The strongest earthquakes experienced by the city of Santiago de los Caballeros before its final move in 1776 were the San Miguel earthquakes in 1717. In the city, people also believed that the proximity of the Volcán de Fuego (English: Volcano of Fire) was the cause of earthquakes; the great architect Diego de Porres even said that all the earthquakes were caused by volcano explosions.

Geographic entities mentioned:
surface_form: fuego
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.474722222222
lon: -90.880833333333
surface_form: volcán de fuego
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.474722222222
lon: -90.880833333333
On 27 August there was a strong eruption of Volcán de Fuego, which lasted until 30 August; the residents of the city asked for help to Santo Cristo of the cathedral and to the Virgen del Socorro who were sworn patrons of the Volcan de Fuego.

Geographic entities mentioned:
surface_form: fuego
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.474722222222
lon: -90.880833333333
surface_form: fuego
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.474722222222
lon: -90.880833333333
surface_form: volcan de fuego
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.474722222222
lon: -90.880833333333
surface_form: volcán de fuego
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.474722222222
lon: -90.880833333333
Paroxysmal eruptions (or 'paroxysms') produce a sustained eruptive plume from which ash falls on communities within 20 km of the volcano, lava flows reaching 1–2 km from the summit, and occasional pyroclastic density currents. The largest eruption of Fuego in its current period of activity happened on 3 June 2018, also the most powerful eruption of the volcano since 1974.

Geographic entities mentioned:
surface_form: fuego
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.474722222222
lon: -90.880833333333
The greatest impacts were on the east side of Fuego, where pyroclastic flows filled and eventually overcame the capacity of the Las Lajas ravine to descend on the nearby communities of San Miguel Los Lotes and El Rodeo in Escuintla and the private golf resort of La Reunión in Sacatepéquez.

Geographic entities mentioned:
surface_form: fuego
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.474722222222
lon: -90.880833333333
Agnuzzo. Agnuzzo is a village in the municipality of Muzzano, Canton of Ticino, Switzerland. The village borders Lake Lugano between Agno and Montagnola on the northern end of the lake's western spur. The current population is around 730.

Geographic entities mentioned:
surface_form: Lake Lugano
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46
lon: 9
Roaring Plains West Wilderness. The Roaring Plains West Wilderness is a U.S. Wilderness Area in the Allegheny Mountains of eastern West Virginia, USA. It is part of the Monongahela National Forest and includes Mount Porte Crayon, the sixth highest point in the state.

Geographic entities mentioned:
surface_form: Mount Porte Crayon
instance_of: Mountain
countries: United States
coordinates: lat: 38.928888888889
lon: -79.456111111111
The bogs serve to regulate stream flow at the headwaters for both sides of the Front. Recreational trails provide loops within the area as well as connecting to Red Creek Plains, Dolly Sods Wilderness and even further north to Canaan Valley. An average of 180 inches (15 ft) of snow falls on the area annually, affording opportunities for cross-country skiing and snowshoeing.

Geographic entities mentioned:
surface_form: Canaan Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.126666666667
lon: -79.378055555556
It is long. Geography. The Peiros is the second longest river in Achaea, after Selinountas. It rises in the northeastern part of the Erymanthos mountains, near the village Lakkomata. It passes through the municipal units of Farres, Olenia and Dymi. It empties into the Gulf of Patras between the towns Alissos and Kato Achaia.

Geographic entities mentioned:
surface_form: Erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
AD 24) identifies Caucasian Albania as a territory distinct from Atropatene and describes it as “a land extending from the Caspian Sea to the Alazani River and the land of Mede Atropatene to the south.”
Movses Kaghankatvatsi, the author of &quot;The History of the Country of Albania&quot;, which covers the period between the 4th and 10th centuries AD, describes the boundaries of Caucasian Albania as not going beyond the Aras River.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
It wasn't until 1871 that borax was discovered near the town's site, and as a result Columbus increased substantially in its importance. Borax was discovered at a salt marsh near town by William Troop in 1871. The site later became known as the Columbus Marsh. By 1873, four borax companies were actively working the deposits on the marsh.

Geographic entities mentioned:
surface_form: salt marsh
instance_of: Valley
countries: United States
coordinates: lat: 38.0858
lon: -117.965
It wasn't until 1871 that borax was discovered near the town's site, and as a result Columbus increased substantially in its importance. Borax was discovered at a salt marsh near town by William Troop in 1871. The site later became known as the Columbus Marsh. By 1873, four borax companies were actively working the deposits on the marsh.

Geographic entities mentioned:
surface_form: Columbus Marsh
instance_of: Valley
countries: United States
coordinates: lat: 38.0858
lon: -117.965
The town had a post office and local newspaper, &quot;The Borax Miner&quot;, an adobe school, an iron foundry. Stage express offered daily service to Fish Lake Valley, Candelaria, and after 1876, Wadsworth. Columbus was declined in 1875, when the Pacific Borax Company built a larger plant at Fish Lake, 30 miles south of town. By 1880, the town population had dwindled to 100 people.

Geographic entities mentioned:
surface_form: Fish Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.6947
lon: -118.078
In 2011, its population is 38,978. Geography. Khartari is situated to the north of Burhi Gandak River. It is bounded by Mishrauliya to the north, Katkuian to the east, Tharghatwa to the south, and Sopgarha to the west. It covers an area of 2378 hectares. Demographics. According to the 2011 Census of India, Khartari has a total of 8,183 households.

Geographic entities mentioned:
surface_form: Burhi Gandak River
instance_of: Watercourse
countries: India
coordinates: lat: 25.43388889
lon: 86.60694444
In the 1930s, Tobias moved to Mandatory Palestine. In 1984, she died in Haifa. Early life. Lily Shepherd was born in Swansea, to Tobias Shepherd (born Tevia Rudinsky) and Chana Beila Shepherd. She grew up in Ystalyfera in the Swansea Valley. Her parents were Polish-Jewish immigrants, and the family spoke Yiddish at home. Her father had a business selling wallpaper and glass decor items.

Geographic entities mentioned:
surface_form: Swansea Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.7593
lon: -3.7898
Beinisvørð. Beinisvørð (Beinisvord) is a high sea cliff in Suðuroy, Faroe Islands, the highest sea cliff in Suðuroy. It is located between the villages of Lopra and Sumba. Beinisvørð has vertical cliffs facing the sea and a green slope down towards the village of Sumba.

Geographic entities mentioned:
surface_form: beinisvørð
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 61.426388888889
lon: -6.7672222222222
Beinisvørð. Beinisvørð (Beinisvord) is a high sea cliff in Suðuroy, Faroe Islands, the highest sea cliff in Suðuroy. It is located between the villages of Lopra and Sumba. Beinisvørð has vertical cliffs facing the sea and a green slope down towards the village of Sumba.

Geographic entities mentioned:
surface_form: beinisvørð
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 61.426388888889
lon: -6.7672222222222
surface_form: beinisvord
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 61.426388888889
lon: -6.7672222222222
Beinisvørð (Beinisvord) is a high sea cliff in Suðuroy, Faroe Islands, the highest sea cliff in Suðuroy. It is located between the villages of Lopra and Sumba. Beinisvørð has vertical cliffs facing the sea and a green slope down towards the village of Sumba. The triangular top of Beinisvørð is visible from many places in Suðuroy, including Lopra, Nes and Marknoyri, the easternmost part of Vágur.

Geographic entities mentioned:
surface_form: beinisvørð
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 61.426388888889
lon: -6.7672222222222
Beinisvørð has vertical cliffs facing the sea and a green slope down towards the village of Sumba. The triangular top of Beinisvørð is visible from many places in Suðuroy, including Lopra, Nes and Marknoyri, the easternmost part of Vágur. In clear weather it is also visible from &quot;Smyril&quot; M/F just before she enters the fjord of Trongisvágur, Trongisvágsfjørður.

Geographic entities mentioned:
surface_form: beinisvørð
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 61.426388888889
lon: -6.7672222222222
In clear weather it is also visible from &quot;Smyril&quot; M/F just before she enters the fjord of Trongisvágur, Trongisvágsfjørður. Men from Sumba used to rappel down the steep mountain side of Beinisvørð on bird lines (it is called &quot;síging&quot;; one man hangs on a thick rope, while several men hold it at the top) in order to catch sea birds and to collect eggs.

Geographic entities mentioned:
surface_form: beinisvørð
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 61.426388888889
lon: -6.7672222222222
Both birds and their eggs were important food for the people of Sumba in the past. Several men have been killed while doing this; sometimes a stone fell on a man's head, fatally injuring him. In 1975 a big avalanche at Beinisvørð destroyed numerous bird habitats and landmarks. Beinisvørð in Faroese poetry. At least two famous Faroese poets have mentioned Beinisvørð in poems. Poul F.

Geographic entities mentioned:
surface_form: beinisvørð
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 61.426388888889
lon: -6.7672222222222
surface_form: beinisvørð
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 61.426388888889
lon: -6.7672222222222
In 1975 a big avalanche at Beinisvørð destroyed numerous bird habitats and landmarks. Beinisvørð in Faroese poetry. At least two famous Faroese poets have mentioned Beinisvørð in poems. Poul F. Joensen (born 1898 in Sumba, died 1970 in Froðba) often mentioned Beinisvørð as the guardian spirit of the country. A Faroese singer and composer from Klaksvík, Hanus G.

Geographic entities mentioned:
surface_form: beinisvørð
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 61.426388888889
lon: -6.7672222222222
At least two famous Faroese poets have mentioned Beinisvørð in poems. Poul F. Joensen (born 1898 in Sumba, died 1970 in Froðba) often mentioned Beinisvørð as the guardian spirit of the country. A Faroese singer and composer from Klaksvík, Hanus G. Johansen, set several of these poems to music and after that they became very popular and well known amongst Faroese of all ages.

Geographic entities mentioned:
surface_form: beinisvørð
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 61.426388888889
lon: -6.7672222222222
Janus Djurhuus (born 1881 in Tórshavn, died 1948) uses it as a symbol of Faroese independence in &quot;Heimferð Nólsoyar Páls&quot;. Tourism. Tourists who visit Suðuroy often wish to see Beinisvørð. It can be seen from several locations, the nearest being Hesturin, near the one-lane road between Lopra and Sumba. There is also a road tunnel from Lopra to Sumba.

Geographic entities mentioned:
surface_form: beinisvørð
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 61.426388888889
lon: -6.7672222222222
Masausi is situated near the villages of Sa'ilele and Utuloa. The village is reached from a road in Faga’itua. An archeoligcal site known as AS-23-7 is located at Masausi. Along the coast, between the Vaipito and Panota Streams, Kirch and Hunt collected two artifacts. One was a butt of a roughly flaked, quadrangular adze.

Geographic entities mentioned:
surface_form: Vaipito
instance_of: Valley
countries: United States
coordinates: lat: -14.278611111111
lon: -170.70333333333
The lake lies roughly ENE of Borovskoy, the district capital, northeast of Sosna and north of Aksuat. Geography. Tuzkol lies in the Turgay Depression, to the south of the Kazakhstan–Russia border. Larger Alakol lake is located to the south of the southern shore and Teniz to the NNW. River Ubagan flows northwards to the east of Tuzkol's eastern shore. The lake freezes in the winter.

Geographic entities mentioned:
surface_form: Turgay Depression
instance_of: Valley
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 52
lon: 64.5
The lake lies roughly ENE of Borovskoy, the district capital, northeast of Sosna and north of Aksuat. Geography. Tuzkol lies in the Turgay Depression, to the south of the Kazakhstan–Russia border. Larger Alakol lake is located to the south of the southern shore and Teniz to the NNW. River Ubagan flows northwards to the east of Tuzkol's eastern shore. The lake freezes in the winter.

Geographic entities mentioned:
surface_form: Teniz
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 54.11306
lon: 64.56806
surface_form: alakol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.081111111111
lon: 81.764166666667
surface_form: teniz
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 51.32194
lon: 62.35444
surface_form: alakol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 51.20556
lon: 69.70754
Geography. Tuzkol lies in the Turgay Depression, to the south of the Kazakhstan–Russia border. Larger Alakol lake is located to the south of the southern shore and Teniz to the NNW. River Ubagan flows northwards to the east of Tuzkol's eastern shore. The lake freezes in the winter. The A21 Highway skirts the lake on its southern part.

Geographic entities mentioned:
surface_form: ubagan
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.683333333333
lon: 64.8
Tuzkol, Mendykara District. Tuzkol () is a salt lake in Mendykara District, Kostanay Region, Kazakhstan. The lake lies roughly ENE of Borovskoy, the district capital, northeast of Sosna and north of Aksuat. Geography. Tuzkol lies in the Turgay Depression, to the south of the Kazakhstan–Russia border. Larger Alakol lake is located to the south of the southern shore and Teniz to the NNW.

Geographic entities mentioned:
surface_form: tuzkol, mendykara district
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 53.90694444444444
lon: 64.66055555555556
Tuzkol, Mendykara District. Tuzkol () is a salt lake in Mendykara District, Kostanay Region, Kazakhstan. The lake lies roughly ENE of Borovskoy, the district capital, northeast of Sosna and north of Aksuat. Geography. Tuzkol lies in the Turgay Depression, to the south of the Kazakhstan–Russia border. Larger Alakol lake is located to the south of the southern shore and Teniz to the NNW.

Geographic entities mentioned:
surface_form: aksuat
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 51.45
lon: 64.49
Historiography. The first coffee economy in Brazil grew near São Paulo in the Santos coffee zone. North of São Paulo was the Paraíba Valley, this region was home to Oeste Paulista, a once hegemon of Brazilian coffee. This region and its economy only grew because of slave labor. While later on the industry largely invited immigrant populations to work in coffee.

Geographic entities mentioned:
surface_form: Paraíba Valley
instance_of: Valley
countries: Brazil
coordinates: lat: -22.75
lon: -45.15
Of the agricultural land, 43.6% is used for growing crops and 8.6% is pasturage, while 7.5% is used for orchards or vine crops. Of the water in the municipality, 0.2% is in lakes and 1.6% is in rivers and streams. The municipality is located on the right bank of Lake Biel. It consists of the villages of Täuffelen and Gerolfingen.

Geographic entities mentioned:
surface_form: Lake Biel
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.085555555556
lon: 7.1741666666667
Tenmile Lake (Otter Tail County, Minnesota). Tenmile Lake is a lake in Otter Tail County, in the U.S. state of Minnesota. Tenmile Lake was named after the length of an old trail from the Red River to the lake, which is.

Geographic entities mentioned:
surface_form: tenmile lake
instance_of: Lake
countries: United States
coordinates: lat: 46.97
lon: -94.58
surface_form: tenmile lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5558
lon: -124.142
surface_form: tenmile lake
instance_of: Lake
countries: United States
coordinates: lat: 46.1275
lon: -95.97069444
surface_form: tenmile lake
instance_of: Lake
countries: United States
coordinates: lat: 47.765
lon: -94.94277778
Sixth Lake. Sixth Lake is located near Inlet, New York. It is part of the Fulton Chain Lakes. The inlet is connected to Seventh Lake by a channel and the outlet is connected to Fifth Lake by a creek. Fish species present in the lake are brown trout, lake whitefish, lake trout, smelt, splake, rainbow trout, white sucker, black bullhead, yellow perch, and pumpkinseed sunfish.

Geographic entities mentioned:
surface_form: Seventh Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7468513
lon: -74.7431523
surface_form: Fifth Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7480012
lon: -74.7919972
Sixth Lake. Sixth Lake is located near Inlet, New York. It is part of the Fulton Chain Lakes. The inlet is connected to Seventh Lake by a channel and the outlet is connected to Fifth Lake by a creek. Fish species present in the lake are brown trout, lake whitefish, lake trout, smelt, splake, rainbow trout, white sucker, black bullhead, yellow perch, and pumpkinseed sunfish.

Geographic entities mentioned:
surface_form: fulton chain lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 43.75
lon: -74.866666666667
surface_form: chain lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.558096
lon: -121.239866
Sixth Lake. Sixth Lake is located near Inlet, New York. It is part of the Fulton Chain Lakes. The inlet is connected to Seventh Lake by a channel and the outlet is connected to Fifth Lake by a creek. Fish species present in the lake are brown trout, lake whitefish, lake trout, smelt, splake, rainbow trout, white sucker, black bullhead, yellow perch, and pumpkinseed sunfish.

Geographic entities mentioned:
surface_form: sixth lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7492321
lon: -74.7732258
It is part of the Fulton Chain Lakes. The inlet is connected to Seventh Lake by a channel and the outlet is connected to Fifth Lake by a creek. Fish species present in the lake are brown trout, lake whitefish, lake trout, smelt, splake, rainbow trout, white sucker, black bullhead, yellow perch, and pumpkinseed sunfish. There is access via a channel from Seventh Lake.

Geographic entities mentioned:
surface_form: seventh lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7468513
lon: -74.7431523
The Coal Bog road travels through this townland and the adjacent townland of Drumacoorin. This is a traditional peat cutting area and in past times was the main highway between Lough MacNean and Lough Erne. The area is particularly notable for the remnants of a Neolithic settlement found in the coal bog.

Geographic entities mentioned:
surface_form: Lough Erne
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.48262
lon: -7.80622
New York State Route 247. New York State Route 247 (NY 247) is a north&ndash;south state highway located in the Finger Lakes region of New York in the United States. It extends for from an intersection with NY 364 in the Yates County town of Potter to a junction with U.S. Route 20 (US 20) and NY 5 in the Ontario County town of Hopewell.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
Klarälven. Klarälven (&quot;The clear river&quot; in Swedish) is a river flowing through Norway and Sweden. Together with Göta älv, which it is called as the river has passed through the lake Vänern, thus regarded as an entity, Göta älv—Klarälven is the longest river in Scandinavia and in the Nordic countries and its Swedish part is the longest river of Sweden.

Geographic entities mentioned:
surface_form: Vänern
instance_of: Lake
countries: Sweden
coordinates: lat: 58.916666666667
lon: 13.5
These two rivers also have the largest drainage basin in the same areas, including all the rivers that run into Vänern, of which is located in Sweden and in Norway. It emanates at the northeast side of Mount Brändstöten and flows through a couple of smaller lakes down to Lake Rogen in Härjedalen, Sweden, and then passes through the Norwegian Hedmark, where it flows through the lake Femunden.

Geographic entities mentioned:
surface_form: Femunden
instance_of: Lake
countries: Norway
coordinates: lat: 62.183333333333
lon: 11.9
There it is known as Femundelva and Trysilelva'&quot;. The rest of the river, the longest part, flows through Värmland to ultimately discharge in a delta into Vänern at Karlstad. In its turn, Vänern drains then into Göta älv, reaching the sea at Gothenburg.

Geographic entities mentioned:
surface_form: Vänern
instance_of: Lake
countries: Sweden
coordinates: lat: 58.916666666667
lon: 13.5
Geography and geology. The watershed of Klarälven is commonly referred to as Klarälvdalen (&quot;the Klarälv basin&quot;), where it accumulates much of its water on its journey to Vänern. Other important sources of water are the snowy mountains in the northern areas of the watershed area, providing substantial flows in the spring when the snow melts; annual floods are common.

Geographic entities mentioned:
surface_form: Vänern
instance_of: Lake
countries: Sweden
coordinates: lat: 58.916666666667
lon: 13.5
Minhag Ashkenaz was common in Germany, Austria, the Czech lands, and elsewhere in Western Europe, in contrast to the Minhag Polin of the Eastern European Ashkenazi Jews. Minhag Ashkenaz and Minhag Polin. The term &quot;Minhag Ashkenaz&quot;, strictly applied, refers only to the minhag of German Jews south and west of the Elbe, most notably the community of Frankfurt am Main.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Florida State Road 715. State Road 715 (SR 715) is a north&ndash;south route serving two cities on and near the southeastern shore of Lake Okeechobee in southern Florida.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
The First German Antarctica Expedition in 1902 charted a cape in this vicinity, from the summit of Mount Drygalski, and applied the name &quot;Kap Lerche.&quot; In November 1929 the British Australian and New Zealand Antarctic Research Expedition under Douglas Mawson charted a small point in this position and applied the name &quot;Erratic Point&quot; because of the large number of massive erratic boulders encountered there.

Geographic entities mentioned:
surface_form: Mount Drygalski
instance_of: Mountain
countries: Australia
coordinates: lat: -53.03333333333333
lon: 73.38333333333334
Minneriya tank. wyui7emsg6a3ilggp1gio0kqykr" xml:space="preserve">#REDIRECT Minneriya Tank

Geographic entities mentioned:
surface_form: minneriya tank
instance_of: Lake
countries: Sri Lanka
coordinates: lat: 8.03333
lon: 80.8833
(Jacob Horn was granted land in Eastern Passage, Nova Scotia. Jacob's son, Andrew Philip Horne, brought his family to settle at the eastern side of Shubenacadie Grand Lake which would become known as Horne Settlement and later Enfield.)
Horne worked for several years learning the trade in the gold mines of Renfrew, Nova Scotia, and Oldham near his home in Nova Scotia.

Geographic entities mentioned:
surface_form: Shubenacadie Grand Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.9183
lon: -63.5944
The Turkish name was historically spelled &quot;Erciyas&quot;, and it was changed to &quot;Erciyes&quot; to conform with vowel harmony in the 1940s–1960s. Mons Argaeus on the Moon was named for Argaeus. The &quot;Mount Harhara&quot; of Bronze Age and Iron Age inscriptions in Anatolia may be Erciyes. Geology and geomorphology. Erciyes lies in the Kayseri Province of Turkey.

Geographic entities mentioned:
surface_form: Mons Argaeus
instance_of: Mountain
coordinates: lat: 19.33
lon: 29.01
A report from 1905 says that the glacier was long. In 2009 the glacier was long and in 2011 an area of was reported; it is actively retreating and, assuming that the pace of retreat does not change, it will be gone by 2070. This is the westernmost glacier in Turkey today; other glaciers are found in the Kaçkar Mountains at the Black Sea, Mount Cilo in southeastern Turkey, and on Ararat.

Geographic entities mentioned:
surface_form: Mount Cilo
instance_of: Mountain
countries: Turkey
coordinates: lat: 37.48573
lon: 44.00416
surface_form: Ararat
instance_of: Mountain
countries: Turkey
coordinates: lat: 39.70194444444444
lon: 44.29833333333333
This eruption at first formed a tuff ring, within which the lava dome was emplaced. Lava flows extend to lengths of. The dome and flow have a total volume of, and the eruption which had a Volcano Explosivity Index of 5 has been compared to that of Mount St. Helens in North America. was extruded later on the northern flank.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
Mount Erciyes. Mount Erciyes () is an inactive volcano in Kayseri Province, Turkey. It is a large stratovolcano surrounded by many monogenetic vents and lava domes, and one maar. The bulk of the volcano is formed by lava flows of andesitic and dacitic composition. At some time in the past, part of the summit collapsed towards the east. The volcano began to form in the Miocene.

Geographic entities mentioned:
surface_form: erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
surface_form: mount erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
At first, a volcano farther east named formed from lava flows. Then, again to the east, large explosive eruptions formed a caldera. During the Pleistocene, Mount Erciyes proper grew inside the caldera together with a group of lava domes. Lateral eruptions of Erciyes may have generated ash layers in the Black Sea and the Mediterranean during the early Holocene.

Geographic entities mentioned:
surface_form: erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
surface_form: mount erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
During the Pleistocene, Mount Erciyes proper grew inside the caldera together with a group of lava domes. Lateral eruptions of Erciyes may have generated ash layers in the Black Sea and the Mediterranean during the early Holocene. The last eruptions occurred during the early Holocene and may have deposited ash as far away as Palestine; the occurrence of historical volcanism is uncertain.

Geographic entities mentioned:
surface_form: erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
The last eruptions occurred during the early Holocene and may have deposited ash as far away as Palestine; the occurrence of historical volcanism is uncertain. Future eruptions of Erciyes may endanger the nearby cities to the north. The volcano was glaciated during the Pleistocene. One regular glacier still exists, but is receding. Etymology.

Geographic entities mentioned:
surface_form: erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
Future eruptions of Erciyes may endanger the nearby cities to the north. The volcano was glaciated during the Pleistocene. One regular glacier still exists, but is receding. Etymology. &quot;Erciyes&quot; is the adoption into Turkish of the Greek name &quot;Argaios&quot; (Greek: Ἀργαῖος).

Geographic entities mentioned:
surface_form: erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
The Turkish name was historically spelled &quot;Erciyas&quot;, and it was changed to &quot;Erciyes&quot; to conform with vowel harmony in the 1940s–1960s. Mons Argaeus on the Moon was named for Argaeus. The &quot;Mount Harhara&quot; of Bronze Age and Iron Age inscriptions in Anatolia may be Erciyes. Geology and geomorphology. Erciyes lies in the Kayseri Province of Turkey.

Geographic entities mentioned:
surface_form: erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
Geology and geomorphology. Erciyes lies in the Kayseri Province of Turkey. The city of Kayseri lies - north of Erciyes volcano; some lava domes generated by the volcano are within the urban limits. Other towns in the region are Talas and Hacilar, also north of Erciyes but closer to the volcano (and, respectively), Develi, located south, and İncesu, located west and southwest of the volcano.

Geographic entities mentioned:
surface_form: erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
In central Anatolia, volcanism commenced in the Miocene. After an effusive phase and the eruption of large ignimbrite sheets, volcanoes developed, including stratovolcanoes such as Erciyes Dagi and Hasan Dagi on the one hand and monogenetic volcanoes and maars on the other hand. The tectonic environment has been compared with the Basin and Range Province.

Geographic entities mentioned:
surface_form: erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
These margin faults have been the source of earthquakes during historical times, resulting in damage to cities in the region, and ongoing extension of this crustal domain is the probable reason for volcanism at Erciyes. Local. Erciyes Dagi is a large stratovolcano, reaching a height of, or, making it the highest mountain and most voluminous volcano of Central Anatolia.

Geographic entities mentioned:
surface_form: erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
surface_form: erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
Local. Erciyes Dagi is a large stratovolcano, reaching a height of, or, making it the highest mountain and most voluminous volcano of Central Anatolia. It rises about above the basin and above the floor of the Erciyes pull-apart basin. The volcano is large, it covers a surface area of or.

Geographic entities mentioned:
surface_form: erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
It rises about above the basin and above the floor of the Erciyes pull-apart basin. The volcano is large, it covers a surface area of or. It developed over a broad shield, and dacitic domes and flows form the bulk of the volcano's exposed units, including the summit area, where several lava flows have been identified. Lava flows of Erciyes extend both from the summit and from lateral vents.

Geographic entities mentioned:
surface_form: erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45
This caldera may originally have had a volume of. Clockwise from north, these volcanic centres are,,,,,, and. About half of these centres are at distances of about from Erciyes, and most of them can be found on the northern slopes. Of these centres, wide and deep lies northwest of Erciyes.

Geographic entities mentioned:
surface_form: erciyes
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.531666666666666
lon: 35.45