Sarmila/GeoWiki-Features huggingface dataset:
Boyd Strait. Boyd Strait is the wide strait lying between Snow Island and Smith Island in the South Shetland Islands, Antarctica, and linking Drake Passage and the Bransfield Strait. The strait was named in 1823 by a British expedition under James Weddell for Captain David Boyd, Royal Navy. Location. Boyd Strait is located at. British mapping in 1823 and 1930-1931.

Geographic entities mentioned:
surface_form: Bransfield Strait
instance_of: Body of water
countries: Antarctica
coordinates: lat: -63
lon: -59
However, due to repetitive protests from the local population, the two villages were soon returned to France, but not without the loss of most of their surrounding forests, which the Germans intended to keep as a glacis for the defensive position of Mont Donon.

Geographic entities mentioned:
surface_form: Mont Donon
instance_of: Mountain
countries: France
coordinates: lat: 48.513333333333
lon: 7.165
Calvaser (&quot;Kaltwasser&quot;; &quot;Hidegvíz&quot;) was also a village until the late 20th century, when it was absorbed by Șeica Mare village. Geography. The commune is situated on the Transylvanian Plateau, on the banks of the river Vișa; the rivers Calva and Râpa flow into the Vișa in Șeica Mare. Located in the north-central part of the county, the commune is crossed by national road.

Geographic entities mentioned:
surface_form: Transylvanian Plateau
instance_of: Plateau
countries: Romania
coordinates: lat: 46.5
lon: 24.5
Every two years for the last years the Pasadena Republican Club has operated the Greater Pasadena Area Republican Headquarters in Pasadena, California with the help of volunteers. Greater Pasadena Area Republican Headquarters supports the towns in the west side of the San Gabriel Valley.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
Lac de Caderolles. Lac de Caderolles (also known as Lac de la Mane) is a lake near Bagnères-de-Bigorre in Hautes-Pyrénées, France. At an elevation of 1988 m, its surface area is 0.014 km2.

Geographic entities mentioned:
surface_form: caderolles
instance_of: Lake
countries: France
coordinates: lat: 42.895277777778
lon: 0.20527777777778
surface_form: lac de caderolles
instance_of: Lake
countries: France
coordinates: lat: 42.895277777778
lon: 0.20527777777778
Ekkehard II likewise became a teacher at the monastery school. A number of his pupils joined the order; others became bishops. About 973 Dowager Duchess Hadwig of Swabia, the widow of Duke Burchard III called Ekkehard II to her seat at Hohentwiel Castle. Hadwig, a member of the Imperial Ottonian dynasty, was wont occasionally to visit St.

Geographic entities mentioned:
surface_form: Hohentwiel
instance_of: Mountain
countries: Germany
coordinates: lat: 47.764722222222
lon: 8.8188888888889
Course. Beginning in the Cardwell Hills northwest of Corvallis, the creek flows generally south through the McDonald State Forest to near Bald Hill. It then flows southeast through the west side of the city and the Oregon State University campus to enter the river near Reser Stadium and Avery Park. It passes under U.S.

Geographic entities mentioned:
surface_form: Cardwell Hills
instance_of: Landform
countries: United States
coordinates: lat: 44.6429
lon: -123.373
Geography. The Leidy Glacier discharges from the Greenland Ice Sheet through the Academy Glacier. The glacier flows roughly from SE to NW and, after forming an unusual cross pattern, it has its terminus at the head of the Academy Fjord to the northwest and, as the Marie Glacier, at the head of the Olrik Fjord to the southwest.

Geographic entities mentioned:
surface_form: Olrik Fjord
instance_of: Body of water
countries: Greenland
coordinates: lat: 77.2
lon: -67.58194
Papua New Guinea has several volcanoes, as it is situated along the Pacific Ring of Fire. Volcanic eruptions are not rare, and the area is prone to earthquakes and tsunamis because of this. Mount Wilhelm in Papua New Guinea is the second highest mountain in the continent, and at above sea level, Puncak Jaya is the highest mountain. Flora.

Geographic entities mentioned:
surface_form: Mount Wilhelm
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -5.8
lon: 145.03333333333
surface_form: Puncak Jaya
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.0833333333333
lon: 137.18333333333
The book also addresses issues of corruption and inefficient management of charity funds by Trustees, and the urgent need for educational improvement driven by the rapid population growth that turned the Lower Lea valley into an industrial slum.

Geographic entities mentioned:
surface_form: Lower Lea valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.55
lon: -0.0166667
The young are fed by both adults. The black-headed grosbeak's monogamy is under study, but pair bonds generally last for only one breeding season. They typically have one brood per season, though two broods have been documented in foothills of the Sacramento Valley in California. Voice.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
Through midseason, possession of the overall crystal globe for the season was closely fought between four-time overall champion Hirscher and two-time overall champion Aksel Lund Svindal of Norway, with Svindal actually in the lead, but on 23 January, in the legendary &quot;Streif&quot; downhill on the Hahnenkamm at Kitzbühel, Austria, Svindal fell and suffered a season-ending ligament tear in his right knee.

Geographic entities mentioned:
surface_form: Hahnenkamm
instance_of: Mountain
countries: Austria
coordinates: lat: 47.424166666667
lon: 12.365277777778
After Svindal's departure, Hirscher won the overall crystal globe by almost 500 points over Henrik Kristoffersen of Norway. In addition to Svindal and Kristofferson, two other Norwegians placed in the top 7 in overall points: Kjetil Jansrud and Aleksander Aamodt Kilde. The finals were held in St. Moritz, Switzerland from 16 to 20 March 2016.

Geographic entities mentioned:
surface_form: St. Moritz
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50625
lon: 9.7874444444444
Coba Lake. The Coba Lake or Lake Coba (Spanish Lago Cobá) is an almost circular lake close to the ancient Maya city of Coba on the Yucatán peninsula. The lake is surrounded by a reed zone that hosts crocodiles. There is a zip line installation that crosses part of the lake. A lake of similar size and shape, Lake Makanxoc, lies close to the east.

Geographic entities mentioned:
surface_form: coba lake
instance_of: Lake
countries: Mexico
coordinates: lat: 20.491939
lon: -87.738233
Coba Lake. The Coba Lake or Lake Coba (Spanish Lago Cobá) is an almost circular lake close to the ancient Maya city of Coba on the Yucatán peninsula. The lake is surrounded by a reed zone that hosts crocodiles. There is a zip line installation that crosses part of the lake. A lake of similar size and shape, Lake Makanxoc, lies close to the east.

Geographic entities mentioned:
surface_form: coba lake
instance_of: Lake
countries: Mexico
coordinates: lat: 20.491939
lon: -87.738233
surface_form: lago cobá
instance_of: Lake
countries: Mexico
coordinates: lat: 20.491939
lon: -87.738233
On that date the 885th, while based at Blida Airport, Algeria, delivered a total of 18 agents and 67,000 pounds of war material to the Resistance in the south of France. The 2641st Special Group (Prov) received a Unit Citation for operations in Italy's Po Valley on the night of 17/18 February 1945 in which both the 885th and 859th squadrons participated.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
Flowering occurs between December and February. Taxonomy and naming. The mountain-top midge orchid was first formally described in 1945 by Herman Rupp who gave it the name &quot;Prasophyllum parvicallum&quot; from a specimen collected on Mount Greville and the description was published in &quot;The Queensland Naturalist&quot;.

Geographic entities mentioned:
surface_form: Mount Greville
instance_of: Mountain
countries: Australia
coordinates: lat: -28.074
lon: 152.502
Achachi Qala (Cairoma). Achachi Qala (Aymara for &quot;gigantic stone&quot;, also spelled &quot;Achachi Khala&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the La Paz Department, Loayza Province, Cairoma Municipality.

Geographic entities mentioned:
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.5233
lon: -67.9878
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.13055556
lon: -67.70972222
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6525
lon: -68.80694444
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.82833333
lon: -67.69222222
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.66138889
lon: -68.57888889
Achachi Qala (Cairoma). Achachi Qala (Aymara for &quot;gigantic stone&quot;, also spelled &quot;Achachi Khala&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the La Paz Department, Loayza Province, Cairoma Municipality.

Geographic entities mentioned:
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.5233
lon: -67.9878
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.13055556
lon: -67.70972222
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6525
lon: -68.80694444
surface_form: achachi khala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.82833333
lon: -67.69222222
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.82833333
lon: -67.69222222
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.66138889
lon: -68.57888889
Visolotto. Visolotto is a high mountain in the Cottian Alps, located in Piedmont, north of Monviso. Features. It is located slightly north of Monviso from which it is separated by the Cadreghe di Viso, rocky structures with the peculiar shape of chairs (&quot;cadreghe&quot; in the Piedmontese language). During clear weather days it is easily recognizable even from the Turin plain.

Geographic entities mentioned:
surface_form: Monviso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
surface_form: high mountain
instance_of: Mountain
countries: Italy
coordinates: lat: 44.008763888889
lon: 10.289719444444
surface_form: visolotto
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6757451
lon: 7.0853457
Visolotto. Visolotto is a high mountain in the Cottian Alps, located in Piedmont, north of Monviso. Features. It is located slightly north of Monviso from which it is separated by the Cadreghe di Viso, rocky structures with the peculiar shape of chairs (&quot;cadreghe&quot; in the Piedmontese language). During clear weather days it is easily recognizable even from the Turin plain.

Geographic entities mentioned:
surface_form: Monviso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
surface_form: viso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
During clear weather days it is easily recognizable even from the Turin plain. The peak, entirely in Italian territory, is on the ridge separating the Varaita valley from the Po valley, on the border between the municipal territories of Pontechianale and Crissolo.

Geographic entities mentioned:
surface_form: Varaita valley
instance_of: Valley
countries: Italy
coordinates: lat: 44.58
lon: 7.1
surface_form: Po valley
instance_of: Valley
countries: Italy
coordinates: lat: 44.6628
lon: 7.29615
surface_form: po valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
surface_form: varaita valley
instance_of: Valley
countries: Italy
coordinates: lat: 44.58
lon: 7.1
First ascents and the Montaldo-Coolidge dispute. The first ascent dates back to September 4, 1875 and was completed by engineer Felice Montaldo of the CAI of Susa, Antonio Castagneri of Balme (guide) and Francesco Perotti (carrier) on Montaldo Peak. The three followed the most direct route for the ascent, namely the northern face of the mountain (the one overlooking the Po Valley).

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 44.6628
lon: 7.29615
surface_form: po valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
Lanino and Coolidge Peaks are separated from Montaldo Peak by of rather rugged ridge. Geologically, the dominant rock type on Visolotto is epidote amphibolite, a regional metamorphic rock with basic chemism that is light green streaked with yellow-green (the same rock type also found on the summit of Monviso).

Geographic entities mentioned:
surface_form: monviso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
surface_form: visolotto
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6757451
lon: 7.0853457
Visolotto. Visolotto is a high mountain in the Cottian Alps, located in Piedmont, north of Monviso. Features. It is located slightly north of Monviso from which it is separated by the Cadreghe di Viso, rocky structures with the peculiar shape of chairs (&quot;cadreghe&quot; in the Piedmontese language). During clear weather days it is easily recognizable even from the Turin plain.

Geographic entities mentioned:
surface_form: visolotto
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6757451
lon: 7.0853457
The second ascent of Visolotto, again to Picco Montaldo following more or less the same route, was made in 1877 by three masons from Paesana: Battista Bertorello, Cristoforo and Giovanni Picca (father and son). They, having reached the top of Montaldo Peak (the East one), stuck an Italian flag into the rock.

Geographic entities mentioned:
surface_form: visolotto
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6757451
lon: 7.0853457
They, having reached the top of Montaldo Peak (the East one), stuck an Italian flag into the rock. On August 29, 1892, mountaineer Giuseppe Lanino, accompanied by guides Claudio and Giuseppe Perotti, reached the West Peak (the one that today bears the name Lanino Peak) opening a new route along the northwest face and west ridge of Visolotto.

Geographic entities mentioned:
surface_form: visolotto
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6757451
lon: 7.0853457
Tongue Mountain. Tongue Mountain is a mountain located in Adirondack Mountains of New York located in the Town of Indian Lake east-northeast of Blue Mountain Lake.

Geographic entities mentioned:
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 42.2980198
lon: -71.8120781
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7
lon: -74.3167
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 45.81402
lon: -89.30162
surface_form: mountain lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1064
lon: -74.3697
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.95481
lon: -123.25907
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 41.4793
lon: -71.4684
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 41.9947
lon: -86.2042
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 44.114166666667
lon: -93.786666666667
surface_form: mountain lake
instance_of: Lake
countries: United States
coordinates: lat: 37.36
lon: -80.5339
surface_form: blue mountain lake
instance_of: Lake
countries: United States
coordinates: lat: 43.862222222222
lon: -74.457222222222
surface_form: tongue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.911388888889
lon: -74.345555555556
surface_form: mountain lake
instance_of: Lake
countries: United States
coordinates: lat: 41.9522405
lon: -74.983331
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5083
lon: -95.5028
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.8725
lon: -74.401111111111
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.5456079
lon: -90.4940088
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 45.988888888889
lon: -86.332222222222
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.8482
lon: -120.198
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.8158
lon: -114.186
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1469
lon: -74.8489
Tongue Mountain. Tongue Mountain is a mountain located in Adirondack Mountains of New York located in the Town of Indian Lake east-northeast of Blue Mountain Lake.

Geographic entities mentioned:
surface_form: tongue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.911388888889
lon: -74.345555555556
Por Kai Shan (), is a mountain on Lantau Island, Hong Kong, with a height of above sea level. Flora. Por Kai Shan and neighbouring Pok To Yan were designated together a &quot;Site of Special Scientific Interest&quot; in 1994. According to the local government, this site has &quot;over 200 species of native plants.&quot; and &quot;a number of rare and protected indigenous plants&quot;. Geography.

Geographic entities mentioned:
surface_form: Pok To Yan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.2813
lon: 113.9557
surface_form: por kai shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.28656
lon: 113.96023
surface_form: kai shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.45837
lon: 114.01626
Por Kai Shan. Por Kai Shan (), is a mountain on Lantau Island, Hong Kong, with a height of above sea level. Flora. Por Kai Shan and neighbouring Pok To Yan were designated together a &quot;Site of Special Scientific Interest&quot; in 1994.

Geographic entities mentioned:
surface_form: por kai shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.28656
lon: 113.96023
surface_form: kai shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.45837
lon: 114.01626
Por Kai Shan. Por Kai Shan (), is a mountain on Lantau Island, Hong Kong, with a height of above sea level. Flora. Por Kai Shan and neighbouring Pok To Yan were designated together a &quot;Site of Special Scientific Interest&quot; in 1994.

Geographic entities mentioned:
surface_form: por kai shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.28656
lon: 113.96023
surface_form: lantau
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.245
lon: 113.917
surface_form: kai shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.45837
lon: 114.01626
Flora. Por Kai Shan and neighbouring Pok To Yan were designated together a &quot;Site of Special Scientific Interest&quot; in 1994. According to the local government, this site has &quot;over 200 species of native plants.&quot; and &quot;a number of rare and protected indigenous plants&quot;. Geography. To the northwest is Tung Chung, while to the south is Sunset Peak.

Geographic entities mentioned:
surface_form: sunset peak
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.2583
lon: 113.956
The reign of the king (above in Raja Neetham) was identified as a good rule by the Devas. Narayana, Brahma, Lekhsmi and all devas appreciated this rule. They went to kayilai to meet Siva to tell about this. They met Siva in Kayilai and told that the King chozha is ruling his country genuinely. They also told Siva about the judgement of the king in the matter of the Hunter and the Bird.

Geographic entities mentioned:
surface_form: kayilai
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
The Muisca inhabited mainly the area of what is now the Departments of Boyacá and Cundinamarca high plateau (&quot;Altiplano Cundiboyacense&quot;) where they formed the Muisca Confederation. The Muisca had one of the most developed political systems (Muisca Confederation) in South America, surpassed only by the Incas.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
Pico da Cruz (village). Pico da Cruz is a settlement in the northeastern part of the island of Santo Antão, Cape Verde. In 2010 its population was 138. It is situated 6 km southwest of Pombas and 10 km northeast of the island capital Porto Novo. Its elevation is about 1,400 meters. The village is named after the nearby mountain Pico da Cruz. It lies in the Cova-Paul-Ribeira da Torre Natural Park.

Geographic entities mentioned:
surface_form: Pico da Cruz
instance_of: Mountain
countries: Cape Verde
coordinates: lat: 17.1
lon: -25.029166666667
It is situated near the Peruvian border in the La Paz Department, Franz Tamayo Province, Pelechuco Municipality, east of Such'i Lake.

Geographic entities mentioned:
surface_form: Such'i Lake
instance_of: Lake
countries: Bolivia
Peru
coordinates: lat: -14.768055555556
lon: -69.271944444444
Machu Such'i Qhuchi or Machu Such'i Q'uchi (a combination of Quechua and Aymara, &quot;machu&quot; old, &quot;such'i&quot; a species of pencil catfish, &quot;qhuchi&quot; or &quot;q'uchi&quot; wetlands &quot;old such'i wetlands&quot;, Hispanicized spellings &quot;Machu Suchi Cuchi, Matchu Suchi Cuchi, Machu Suchi Coochi, Matchu Sochi Conchi&quot;) is a mountain in the Apolobamba mountain range in the Bolivian Andes, about 5,679 metres (18,632 ft) high.

Geographic entities mentioned:
surface_form: machu suchi cuchi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -14.75
lon: -69.2
surface_form: machu such'i qhuchi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -14.75
lon: -69.2
surface_form: machu suchi coochi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -14.75
lon: -69.2
surface_form: matchu suchi cuchi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -14.75
lon: -69.2
Machu Such'i Qhuchi.

Geographic entities mentioned:
surface_form: machu such'i qhuchi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -14.75
lon: -69.2
Its minimum width is 19 km. The Whale Sound separates Steensby Land —part of the Greenland mainland— to the south from Kiatak (Northumberland Island) and Qeqertarsuaq (Herbert Island) to the north. The Murchison Sound leads from the Baffin Bay to the Inglefield Fjord on the north side of the islands. the Olrik Fjord has its entrance at the eastern end of the sound.

Geographic entities mentioned:
surface_form: Olrik Fjord
instance_of: Body of water
countries: Greenland
coordinates: lat: 77.2
lon: -67.58194
&quot;Ixamatus barina&quot; is a species of mygalomorph spider in the Microstigmatidae family. It is endemic to Australia. It was described in 1982 by Australian arachnologist Robert Raven. Distribution and habitat. The species occurs in Far North Queensland. The type locality is Baldy Mountain, near Atherton on the Atherton Tableland. Behaviour. The spiders are terrestrial predators.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Rinkenwall. The Rinkenwall or Rinkenmauer is a circular rampart fortification at the southeastern tip of the Rinkenkopf mountain above the Murg valley near the village of Baiersbronn in the county of Freudenstadt in the south German state of Baden-Württemberg.

Geographic entities mentioned:
surface_form: Rinkenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 48.515555555556
lon: 8.3641666666667
Geography. Libiš is located about north of Prague and creates a conurbation with the neighbouring town of Neratovice. It lies in a flat landscape in the Central Elbe Table. The Elbe River flows along the municipal border. Part of the Úpor – Černínovsko Nature Reserve is located in the municipal territory. History. The first written mention of Libiš is from 1323.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Ngurlun languages. The Ngurlun languages, also known as Eastern Mirndi, are a branch of the Mirndi languages spoken around in the Barkly Tableland of Northern Territory, Australia. The branch consists of two to four languages, depending on what is considered a dialect: Ngarnka, Wambaya, and often Binbinka and Gurdanji.

Geographic entities mentioned:
surface_form: Barkly Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -19
lon: 138
The film grossed $7.5 million in North America and earned a cult following. Plot. A group of four teenage girls in the San Fernando Valley during the end of the 1970s have painful emotional troubles. Deirdre is a disco queen who is fascinated by her sexuality, likes boys, and has many relationship troubles. Madge is unhappily overweight and angry that she is still a virgin.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Mosvatnet. Mosvatnet is a lake in the municipality of Stavanger in Rogaland county, Norway. The lake lies just west of the centre of the city of Stavanger in the Eiganes og Våland borough. At, it is the third largest lake in the city of Stavanger after Hålandsvatnet and Stora Stokkavatnet. The lake reaches a maximum depth of and it lies at an elevation of above sea level.

Geographic entities mentioned:
surface_form: Stora Stokkavatnet
instance_of: Lake
countries: Norway
coordinates: lat: 58.96434889
lon: 5.669289
At, it is the third largest lake in the city of Stavanger after Hålandsvatnet and Stora Stokkavatnet. The lake reaches a maximum depth of and it lies at an elevation of above sea level. The lake flows out through a small stream that runs through underground culverts to the Breiavatnet lake before emptying into the nearby Byfjorden. Reservoir.

Geographic entities mentioned:
surface_form: Breiavatnet
instance_of: Lake
countries: Norway
coordinates: lat: 58.968056
lon: 5.732778
After a short time it was realized that Mosvatnet did not have enough capacity to supply the growing city with drinking water in the long term. In 1903, the city of Stavanger bought water rights for the Stora Stokkavatnet lake and in 1930 that lake became the city's new water reservoir.

Geographic entities mentioned:
surface_form: Stora Stokkavatnet
instance_of: Lake
countries: Norway
coordinates: lat: 58.96434889
lon: 5.669289
Mosvatnet. Mosvatnet is a lake in the municipality of Stavanger in Rogaland county, Norway. The lake lies just west of the centre of the city of Stavanger in the Eiganes og Våland borough. At, it is the third largest lake in the city of Stavanger after Hålandsvatnet and Stora Stokkavatnet. The lake reaches a maximum depth of and it lies at an elevation of above sea level.

Geographic entities mentioned:
surface_form: mosvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 58.957
lon: 5.712
surface_form: mosvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 59.866666666667
lon: 8.0833333333333
The lake flows out through a small stream that runs through underground culverts to the Breiavatnet lake before emptying into the nearby Byfjorden. Reservoir. Mosvatnet was Stavanger's main water source between 1863 and 1931. The Great Fire of Holmen in Stavanger in 1860 showed that the city had a weak water supply.

Geographic entities mentioned:
surface_form: mosvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 58.957
lon: 5.712
surface_form: mosvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 59.866666666667
lon: 8.0833333333333
The Great Fire of Holmen in Stavanger in 1860 showed that the city had a weak water supply. In 1863, the city initiated the building of a new waterworks at Mosvatnet that both would give residents proper drinking water and better access to water for fire crews. A pump house was erected and water pipes were laid along the road Madlaveien (Rv 509).

Geographic entities mentioned:
surface_form: mosvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 58.957
lon: 5.712
surface_form: mosvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 59.866666666667
lon: 8.0833333333333
The water level of the pond was increased significantly, and several small islets and rocks disappeared. The city took over several properties along the lake to prevent contamination of drinking water source and it made the surrounding areas into parkland. After a short time it was realized that Mosvatnet did not have enough capacity to supply the growing city with drinking water in the long term.

Geographic entities mentioned:
surface_form: mosvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 58.957
lon: 5.712
surface_form: mosvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 59.866666666667
lon: 8.0833333333333
The community includes the coastal village Platinidia. Ano Lechonia is situated in the northwestern part of the Pelion peninsula, 1.5 km from the Pagasetic Gulf coast, 3 km southwest of Agios Georgios Nileias, 4 km southeast of Agria and southeast of Volos. After 1996, Ano Lechonia is the end stop of the heritage Pelion Railway, operated by the Hellenic Train (former OSE). History.

Geographic entities mentioned:
surface_form: Pelion
instance_of: Mountain
countries: Greece
coordinates: lat: 39.433333333333
lon: 23.05
The river basin of Lake Lacha includes the southern and western parts of Kargopolsky District of Arkhangelsk Oblast, as well as north-west of Vologda Oblast. In particular, it includes two of the biggest lakes of Arkhangelsk and Vologda Oblasts, Lake Vozhe and Lake Lyokshmozero. The southern part of the Kenozersky National Park also drains into Lake Lacha.

Geographic entities mentioned:
surface_form: Lake Vozhe
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.589444444444
lon: 39.0925
surface_form: Lake Lyokshmozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.741388888889
lon: 38.088888888889
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: vozhe
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.589444444444
lon: 39.0925
surface_form: lyokshmozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.741388888889
lon: 38.088888888889
Lake Lacha. Lake Lacha () is a freshwater lake, located in the south of Kargopolsky District of Arkhangelsk Oblast in Russia, south of the town of Kargopol. It is the largest lake in Arkhangelsk Oblast, with a surface area of and a basin area of. Lake Lacha is the source of the Onega, one of the major waterways of the White Sea basin. The etymological origin of the name is unclear.

Geographic entities mentioned:
surface_form: onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
surface_form: lake lacha
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.333333333333
lon: 38.8
surface_form: lacha
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.333333333333
lon: 38.8
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The southern part of the Kenozersky National Park also drains into Lake Lacha. The stretch between Kargopol and the lake is navigable, however, neither the Svid upstream from the lake nor the Onega downstream are navigable because of the rapids. There are occasional recreational boat trips from Kargopol to the lake but no passenger or cargo navigation.

Geographic entities mentioned:
surface_form: onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Several villages are located on or close to the banks, including Morshchikhinskaya, Tobolkino, and Filosofskaya. The latter pair are located on the road connecting Kargopol with Lipin Bor via Sovza. Another unpaved road runs from Kargopol along the right bank of the Onega to the lake and then to the village of Bolshaya Kondratovskaya, several kilometers from the lakeshore.

Geographic entities mentioned:
surface_form: onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Lake Lacha. Lake Lacha () is a freshwater lake, located in the south of Kargopolsky District of Arkhangelsk Oblast in Russia, south of the town of Kargopol. It is the largest lake in Arkhangelsk Oblast, with a surface area of and a basin area of. Lake Lacha is the source of the Onega, one of the major waterways of the White Sea basin. The etymological origin of the name is unclear.

Geographic entities mentioned:
surface_form: lake lacha
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.333333333333
lon: 38.8
surface_form: lacha
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.333333333333
lon: 38.8
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Lake Lacha. Lake Lacha () is a freshwater lake, located in the south of Kargopolsky District of Arkhangelsk Oblast in Russia, south of the town of Kargopol. It is the largest lake in Arkhangelsk Oblast, with a surface area of and a basin area of. Lake Lacha is the source of the Onega, one of the major waterways of the White Sea basin. The etymological origin of the name is unclear.

Geographic entities mentioned:
surface_form: lake lacha
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.333333333333
lon: 38.8
surface_form: lacha
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.333333333333
lon: 38.8
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The etymological origin of the name is unclear. The river basin of Lake Lacha includes the southern and western parts of Kargopolsky District of Arkhangelsk Oblast, as well as north-west of Vologda Oblast. In particular, it includes two of the biggest lakes of Arkhangelsk and Vologda Oblasts, Lake Vozhe and Lake Lyokshmozero.

Geographic entities mentioned:
surface_form: lake lacha
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.333333333333
lon: 38.8
surface_form: lacha
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.333333333333
lon: 38.8
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
In particular, it includes two of the biggest lakes of Arkhangelsk and Vologda Oblasts, Lake Vozhe and Lake Lyokshmozero. The southern part of the Kenozersky National Park also drains into Lake Lacha. The stretch between Kargopol and the lake is navigable, however, neither the Svid upstream from the lake nor the Onega downstream are navigable because of the rapids.

Geographic entities mentioned:
surface_form: lake lacha
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.333333333333
lon: 38.8
surface_form: lacha
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.333333333333
lon: 38.8
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Lake Lacha. Lake Lacha () is a freshwater lake, located in the south of Kargopolsky District of Arkhangelsk Oblast in Russia, south of the town of Kargopol. It is the largest lake in Arkhangelsk Oblast, with a surface area of and a basin area of. Lake Lacha is the source of the Onega, one of the major waterways of the White Sea basin. The etymological origin of the name is unclear.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The stretch between Kargopol and the lake is navigable, however, neither the Svid upstream from the lake nor the Onega downstream are navigable because of the rapids. There are occasional recreational boat trips from Kargopol to the lake but no passenger or cargo navigation. Several villages are located on or close to the banks, including Morshchikhinskaya, Tobolkino, and Filosofskaya.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Diyadin. Diyadin (;) is a town in Ağrı Province of Turkey, at the foot of Mount Tendürek, a high peak in the Aladağlar range that stands between Ağrı and the north shore of Lake Van. It is the seat of Diyadin District. Its population is 20,302 (2021). Politics. The mayor is Betül Yaşar (HDP). Economy. As of 1920, the area was known for its sulphur production.

Geographic entities mentioned:
surface_form: Mount Tendürek
instance_of: Mountain
countries: Turkey
coordinates: lat: 39.35486
lon: 43.86703
Blatenský vrch. The Blatenský vrch () is a mountain in the Ore Mountains in the Czech Republic. It has an elevation of. It is located near the town of Horní Blatná, however, it lies in the municipal territory of Potůčky. History. The mountain massif consists mainly of granite. By the Early Modern Era there was a lively tin and iron ore mining industry in the area of the mountain.

Geographic entities mentioned:
surface_form: blatenský vrch
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.400277777778
lon: 12.781666666667
Fallow Hollow. Fallow Hollow is a tributary of Coles Creek in Columbia County, Pennsylvania, in the United States. It is approximately long and flows through Sugarloaf Township. The watershed of the stream has an area of. Fallow Hollow is listed on the Columbia County Natural Areas Inventory as a &quot;Locally Significant Area&quot;. The stream is also Class A Wild Trout Waters. Course.

Geographic entities mentioned:
surface_form: coles creek
instance_of: Watercourse
countries: United States
coordinates: lat: 31.773
lon: -91.207
surface_form: fallow hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.26314
lon: -76.34077
It flows roughly south for less than half a mile before turning west. The stream then flows a slightly longer distance before turning northwest and beginning to flow parallel to Ripple Brook Road. A short distance downstream, it reaches its confluence with Coles Creek. Fallow Hollow joins Coles Creek upstream of its mouth. Geography, watershed, and hydrology.

Geographic entities mentioned:
surface_form: coles creek
instance_of: Watercourse
countries: United States
coordinates: lat: 31.773
lon: -91.207
The stream then flows a slightly longer distance before turning northwest and beginning to flow parallel to Ripple Brook Road. A short distance downstream, it reaches its confluence with Coles Creek. Fallow Hollow joins Coles Creek upstream of its mouth. Geography, watershed, and hydrology. The elevation near the mouth of Fallow Hollow is above sea level.

Geographic entities mentioned:
surface_form: coles creek
instance_of: Watercourse
countries: United States
coordinates: lat: 31.773
lon: -91.207
Plants. In the higher elevations of the watershed of Fallow Hollow, the forest canopy consists of trees such as red maple, sugar maple, red oak, white oak, yellow birch, serviceberry, Eastern hemlock, and big-tooth aspen. The understory of this part of the watershed is inhabited by plants such as northern lady fern, hay-scented fern, New York fern, common wood fern, and starflower.

Geographic entities mentioned:
surface_form: hemlock
instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
lon: -77.608888888889
surface_form: fallow hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.26314
lon: -76.34077
These include sensitive fern, highbrush blueberry, cinnamon fern, winterberry holly, various sedges, and numerous other species. The hollow's seepy woods contain trees such as white pine, yellow birch, and eastern hemlock, and pignut hickory. Other plants in this part of the hollow include Japanese barberry, lowbush blueberry, partridge berry, red trillium, Indian cucumber, and witch hazel.

Geographic entities mentioned:
surface_form: hemlock
instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
lon: -77.608888888889
Fallow Hollow. Fallow Hollow is a tributary of Coles Creek in Columbia County, Pennsylvania, in the United States. It is approximately long and flows through Sugarloaf Township. The watershed of the stream has an area of. Fallow Hollow is listed on the Columbia County Natural Areas Inventory as a &quot;Locally Significant Area&quot;. The stream is also Class A Wild Trout Waters. Course.

Geographic entities mentioned:
surface_form: sugarloaf
instance_of: Mountain
countries: United States
coordinates: lat: 43.832777777778
lon: -74.822222222222
The stream is also Class A Wild Trout Waters. Course. Fallow Hollow begins in a pond in Sugarloaf Township, near Ranch Road. It flows roughly south for less than half a mile before turning west. The stream then flows a slightly longer distance before turning northwest and beginning to flow parallel to Ripple Brook Road. A short distance downstream, it reaches its confluence with Coles Creek.

Geographic entities mentioned:
surface_form: sugarloaf
instance_of: Mountain
countries: United States
coordinates: lat: 43.832777777778
lon: -74.822222222222
Fallow Hollow. Fallow Hollow is a tributary of Coles Creek in Columbia County, Pennsylvania, in the United States. It is approximately long and flows through Sugarloaf Township. The watershed of the stream has an area of. Fallow Hollow is listed on the Columbia County Natural Areas Inventory as a &quot;Locally Significant Area&quot;. The stream is also Class A Wild Trout Waters. Course.

Geographic entities mentioned:
surface_form: fallow hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.26314
lon: -76.34077
A short distance downstream, it reaches its confluence with Coles Creek. Fallow Hollow joins Coles Creek upstream of its mouth. Geography, watershed, and hydrology. The elevation near the mouth of Fallow Hollow is above sea level. The elevation at the source of the stream is between and. The watershed of Fallow Hollow has an area of. The entire length of the stream is on closed and private land.

Geographic entities mentioned:
surface_form: fallow hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.26314
lon: -76.34077
Fallow Hollow joins Coles Creek upstream of its mouth. Geography, watershed, and hydrology. The elevation near the mouth of Fallow Hollow is above sea level. The elevation at the source of the stream is between and. The watershed of Fallow Hollow has an area of. The entire length of the stream is on closed and private land. There are numerous types of habitats in the watershed of Fallow Hollow.

Geographic entities mentioned:
surface_form: fallow hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.26314
lon: -76.34077
The watershed of Fallow Hollow has an area of. The entire length of the stream is on closed and private land. There are numerous types of habitats in the watershed of Fallow Hollow. These include a pond, a shrub swamp, a forested ravine, a graminoid/forb opening, and a deciduous seepy forest. The last habitat has a thick understory of ferns.

Geographic entities mentioned:
surface_form: fallow hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.26314
lon: -76.34077
These include a pond, a shrub swamp, a forested ravine, a graminoid/forb opening, and a deciduous seepy forest. The last habitat has a thick understory of ferns. The total concentration of alkalinity in the waters of Fallow Hollow is eight milligrams per liter. History and etymology. The etymology of Fallow Hollow's name is unknown.

Geographic entities mentioned:
surface_form: fallow hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.26314
lon: -76.34077
The last habitat has a thick understory of ferns. The total concentration of alkalinity in the waters of Fallow Hollow is eight milligrams per liter. History and etymology. The etymology of Fallow Hollow's name is unknown. The Columbia County Natural Areas Inventory of 2004 recommended that the riparian buffer around the wetlands in Fallow Hollow remain undisturbed.

Geographic entities mentioned:
surface_form: fallow hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.26314
lon: -76.34077
History and etymology. The etymology of Fallow Hollow's name is unknown. The Columbia County Natural Areas Inventory of 2004 recommended that the riparian buffer around the wetlands in Fallow Hollow remain undisturbed. The inventory also advised against the introduction of beavers and suggested more deer hunting activity in the area.

Geographic entities mentioned:
surface_form: fallow hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.26314
lon: -76.34077
The watershed of Fallow Hollow is over-browsed by deer. The entire watershed of Fallow Hollow is designated as a Coldwater Fishery, but is used as a High-Quality Coldwater Fishery. The stream's watershed is also Class A Wild Trout Waters. Trout (specifically brook trout) reproduce naturally in the stream between its headwaters and its mouth.

Geographic entities mentioned:
surface_form: fallow hollow
instance_of: Valley
countries: United States
coordinates: lat: 41.26314
lon: -76.34077
Schirmacher Ponds. Schirmacher Ponds () is a group of meltwater ponds scattered among the Schirmacher Hills, lying 40 nautical miles (70 km) north of the Humboldt Mountains, along the coast of Queen Maud Land. Discovered by the German Antarctic Expedition under Ritscher, 1938–39, and named for Richardheinrich Schirmacher, pilot of the Boreas, one of the expedition seaplanes.

Geographic entities mentioned:
surface_form: schirmacher ponds
instance_of: Lake
coordinates: lat: -70.75
lon: 11.6667
Route description. Stonytown Road's western terminus is at the intersection of Plandome Road and North Plandome Road in Plandome Manor. Continuing east, it passes Leeds Pond and enters Plandome, continuing towards the east, passing the Plandome Country Club.

Geographic entities mentioned:
surface_form: Leeds Pond
instance_of: Lake
countries: United States
coordinates: lat: 40.8131752
lon: -73.7009529