Sarmila/GeoWiki-Features huggingface dataset:
Early life and education. Collins was born in Staunton, Virginia, the youngest of four sons of Fletcher Collins and Margaret James Collins. Raised on a small farm in Virginia's Shenandoah Valley, Collins was home schooled until the sixth grade. He attended Robert E. Lee High School in Staunton, Virginia.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Cheese themed area. Raging Waters San Jose. Raging Waters San Jose was located in Lake Cunningham Park in East San Jose, adjacent to Capitol Expressway, Eastridge Mall, Eastridge Transit Center and Reid-Hillview Airport. The park opened to the public in 1985, and was the largest water park in Northern California.

Geographic entities mentioned:
surface_form: Lake Cunningham Park
instance_of: Lake
countries: United States
coordinates: lat: 37.336613888889
lon: -121.80831666667
Spatsizi Mountain. Spatsizi Mountain is a mountain in the Spatsizi Plateau, a sub-plateau of the Stikine Plateau in north-central British Columbia, Canada. The name &quot;Spatsizi&quot; derives from the Sekani language and means &quot;red goat&quot;, as mountain goats in this region are known to roll on a particular red mountain, resulting in a red colour to their coats.

Geographic entities mentioned:
surface_form: Spatsizi Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.8333
lon: -128.483
surface_form: Stikine Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: spatsizi mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 57.529166666667
lon: -128.63333333333
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Spatsizi Mountain. Spatsizi Mountain is a mountain in the Spatsizi Plateau, a sub-plateau of the Stikine Plateau in north-central British Columbia, Canada. The name &quot;Spatsizi&quot; derives from the Sekani language and means &quot;red goat&quot;, as mountain goats in this region are known to roll on a particular red mountain, resulting in a red colour to their coats.

Geographic entities mentioned:
surface_form: red mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
surface_form: red mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.2036
lon: -122.549
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: red mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.0919
lon: -117.821
Spatsizi Mountain. Spatsizi Mountain is a mountain in the Spatsizi Plateau, a sub-plateau of the Stikine Plateau in north-central British Columbia, Canada. The name &quot;Spatsizi&quot; derives from the Sekani language and means &quot;red goat&quot;, as mountain goats in this region are known to roll on a particular red mountain, resulting in a red colour to their coats.

Geographic entities mentioned:
surface_form: spatsizi mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 57.529166666667
lon: -128.63333333333
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Plaka, Achaea. Plaka (, before 1928: Μουρόχοβα - &quot;Mourochova&quot;) is a village in the municipal unit of Aroania, Achaea, Greece. It is situated in the southern foothills of Mount Erymanthos. It is 2 km southeast of Agrampela, 4 km west of Livartzi and 25 km southwest of Kalavryta.

Geographic entities mentioned:
surface_form: Mount Erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
Other cave drawings or carvings have been later discovered in other parts of Gabon by Testa and Richard Oslisly, in Lastoursville in 2015 and 2016, and near Mouila in 2018. In 2010, Testa, with a team led by Oslisly (Shirley, Testa, Sebag, Decaens, Mabicka) went on an expedition in the upstream part of the Fernan Vaz Lagoon, Gabon.

Geographic entities mentioned:
surface_form: Fernan Vaz Lagoon
instance_of: Lake
countries: Gabon
coordinates: lat: -1.59239
lon: 9.42905
Mount Freshfield. Mount Freshfield straddles the Continental Divide marking the Alberta-British Columbia border in Canada. It was named in 1897 by J. Norman Collie after Douglas Freshfield.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount freshfield
instance_of: Mountain
countries: Canada
coordinates: lat: 51.742777777777775
lon: -116.94583333333334
Mount Freshfield. Mount Freshfield straddles the Continental Divide marking the Alberta-British Columbia border in Canada. It was named in 1897 by J. Norman Collie after Douglas Freshfield.

Geographic entities mentioned:
surface_form: mount freshfield
instance_of: Mountain
countries: Canada
coordinates: lat: 51.742777777777775
lon: -116.94583333333334
Peter—who is described as saying &quot;anything that came into his head&quot;—tells Wendy the way to Neverland is &quot;second to the right, and straight on till morning.&quot; In the novel, the children are said to have found the island only because it was &quot;out looking for them.&quot; Barrie additionally writes that Neverland is near the &quot;stars of the milky way&quot; and it is reached &quot;always at the time of sunrise.&quot;
In Barrie's &quot;Peter Pan in Kensington Gardens&quot; (1906), a proto-version of Neverland, located in the Serpentine in Kensington Gardens, is called the Birds' Island, where baby Peter reaches by flight, or by sailing in a paper boat or thrush's nest.

Geographic entities mentioned:
surface_form: Serpentine
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.505277777778
lon: -0.16944444444444
Geography. According to the United States Census Bureau, the township has a total area of, of which is land and, or 68.09%, is water. The township is located on the north shore of Mille Lacs Lake, the second-largest inland lake in Minnesota. Demographics. As of the census of 2000, there were 269 people, 128 households, and 88 families and 4 second names residing in the township.

Geographic entities mentioned:
surface_form: Mille Lacs Lake
instance_of: Lake
countries: United States
coordinates: lat: 46.2381
lon: -93.6434
This dam runs from the village of Schellingwoude in the north to the eastern side of the Amsterdam–Rhine Canal in the south. The dam closes off the Inner IJ, just north of Amsterdam, from the Outer IJ, and hence from the IJsselmeer / Markermeer. The Oranje Locks consists of the original locks called Oranje Locks and the recent Prins Willem-Alexander Lock.

Geographic entities mentioned:
surface_form: Markermeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.566666666667
lon: 5.2166666666667
The Oranje Locks consists of the original locks called Oranje Locks and the recent Prins Willem-Alexander Lock. They regulate the water level in the North Sea Canal, and prevent brackish water from reaching the IJmeer. As it is part of the waterways of national interest, the locks are managed by Rijkswaterstaat.

Geographic entities mentioned:
surface_form: IJmeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.362778
lon: 5.051944
The execution of this plan was opposed by Amsterdam, because of this closure of the IJ. When Amsterdam accepted to construct the Westerdok and Oosterdok wet docks in order to get a deep water port, the Goudriaan plan was cancelled. This way Amsterdam also again got a suitable harbor for some time. Plans for the North Sea Canal.

Geographic entities mentioned:
surface_form: Oosterdok
instance_of: Body of water
countries: Netherlands
coordinates: lat: 52.37388888888889
lon: 4.910277777777778
Instead, they wished that the dike would be constructed as close as possible to Amsterdam. They favored a location between Paardehoek (north east angle of the dam around the Oosterdok near Zeeburg) and the city. By October 1865 the government allowed the constructor of the North Sea Canal to choose between closing the IJ at Pampus or at Paardehoek.

Geographic entities mentioned:
surface_form: Oosterdok
instance_of: Body of water
countries: Netherlands
coordinates: lat: 52.37388888888889
lon: 4.910277777777778
Potentilla webberi. &quot;Potentilla webberi&quot;, commonly known as wire mousetail and Webber's ivesia, is a species of flowering plant in the rose family. It is native to the United States, where it occurs in the northernmost part of the Sierra Nevada and the adjacent Modoc Plateau in California, its range extending just into Nevada. Description.

Geographic entities mentioned:
surface_form: Modoc Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 41.6
lon: -121.2
Three of these, a kill within Fukui Castle in 1910 and two sightings from Chichibu in 1996 and nearby Mount Sobo in 2000, involved closely taken images of each animals and scientific investigations, and a potential audio recording was made in 2018.

Geographic entities mentioned:
surface_form: Mount Sobo
instance_of: Mountain
countries: Japan
coordinates: lat: 32.828055555556
lon: 131.34694444444
Black-necked cranes in Bhutan. Black-necked cranes in Bhutan (&quot;Grus nigricollis&quot;) are winter visitors during late October to mid February to the Phobjikha Valley as well as Ladakh, India, and Arunachal Pradesh, India. They arrive from the Tibetan Plateau, where they breed in the summer.

Geographic entities mentioned:
surface_form: Phobjikha Valley
instance_of: Valley
countries: Bhutan
coordinates: lat: 27.5
lon: 90.16666667
Black-necked cranes in Bhutan. Black-necked cranes in Bhutan (&quot;Grus nigricollis&quot;) are winter visitors during late October to mid February to the Phobjikha Valley as well as Ladakh, India, and Arunachal Pradesh, India. They arrive from the Tibetan Plateau, where they breed in the summer.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
They arrive from the Tibetan Plateau, where they breed in the summer. They visit the Phobjikha Valley in large numbers, which is a declared protected area for the cranes, and also to other valleys in smaller numbers in central and eastern Bhutan.

Geographic entities mentioned:
surface_form: Phobjikha Valley
instance_of: Valley
countries: Bhutan
coordinates: lat: 27.5
lon: 90.16666667
Black-necked cranes, the last to be found among the 16 known species of cranes, were first identified by Nikolay Przhevalsky of the Imperial Russian Army in 1876 in the Tibetan Plateau.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Population. Phobjika valley has recorded the maximum number of cranes in Bhutan for several years. Other places in Bhutan where the cranes have been sighted in small numbers are: Bumdeling, Lhuntshi District, Thangmachu, Thangby-Kharsa, Tashi Yangtse, Punakha Valley, Bumthang Valley, Jakhar Valley, Samtengang, Gyetsa, Khotokha Valley, Gogona and Wangdi.

Geographic entities mentioned:
surface_form: Bumthang Valley
instance_of: Valley
countries: Bhutan
coordinates: lat: 27.55
lon: 90.75
surface_form: Khotokha Valley
instance_of: Valley
countries: Bhutan
coordinates: lat: 27.4356
lon: 89.99694722222222
Namtaeryeong Station is a station on Seoul Subway Line 4 in Seoul, Korea. It is operated by Seoul Metro. It is an island platform with two lines on one side, and a screen door is installed. There are 4 exits. Name. Its name means &quot;great southern pass,&quot; referring to a passageway linking Seoul and Gwacheon, between Mt. Gwanak and Mt. Umyeon. The name came from the Choson Dynasty.

Geographic entities mentioned:
surface_form: Mt. Gwanak
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.445555555556
lon: 126.96361111111
Location. The peak is located at which is 2.38 km south by west of Karavelova Point, 3.28 km west of Inott Point, 3.28 km northwest of Edinburgh Hill, 1.9 km north by east of Helis Nunatak, 3.73 km northeast of Samuel Peak and 5.08 km east-northeast of Miziya Peak (British survey in 1957-59 and mapping in 1968, Spanish mapping in 1991, and Bulgarian in 2005 and 2009).

Geographic entities mentioned:
surface_form: Edinburgh Hill
instance_of: Mountain
coordinates: lat: -62.5425
lon: -60.0169
surface_form: Helis Nunatak
instance_of: Mountain
coordinates: lat: -62.540277777778
lon: -60.077777777778
surface_form: Samuel Peak
instance_of: Mountain
coordinates: lat: -62.5417
lon: -60.1308
surface_form: Miziya Peak
instance_of: Mountain
coordinates: lat: -62.535555555556
lon: -60.164638888889
Sharp Peak, Livingston Island. Sharp Peak is a sharp rocky peak rising to 500 m in the northeast of Vidin Heights on Varna Peninsula, Livingston Island in the South Shetland Islands, Antarctica. The peak is surmounting Rose Valley Glacier to the northwest and Debelt Glacier to the south. The feature was named descriptively in a 1935 British chart. Location.

Geographic entities mentioned:
surface_form: sharp peak
instance_of: Mountain
coordinates: lat: -62.5237
lon: -60.0692
In 2014 he appeared in films &quot;Jeziorak&quot; and &quot;Warsaw 44&quot;, for which he received awards for best acting debut at 39th Polish Film Festival in Gdynia and at 29th Tarnów Film Awards. His breakthrough roles came in 2016 when he starred as Adrian Kuś in a popular TV series &quot;Belfer&quot; and as Remigiusz Puchalski vel.

Geographic entities mentioned:
surface_form: Jeziorak
instance_of: Lake
countries: Poland
coordinates: lat: 53.738888888889
lon: 19.595
Shingle Creek, British Columbia. Shingle Creek is an unincorporated community in the southeastern Thompson Plateau of the Southern Interior of British Columbia, named after the stream of the same name, a tributary of the Okanagan River which joins that stream in the city of Penticton.

Geographic entities mentioned:
surface_form: Thompson Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 50.25
lon: -120.5
Some believe the location of Verysdale was somewhere in the Peak District (the ballad would seem to suggest so), although there are many suggestions and theories. Locations in West Yorkshire, South Yorkshire, Nottinghamshire, Derbyshire, Lancashire, and Cumbria have all been suggested. One scholar equated Verysdale with Wensleydale whilst another equated it with Kirklees.

Geographic entities mentioned:
surface_form: Wensleydale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3056
lon: -2.16667
Dollbek. Dollbek is a river of Mecklenburg-Vorpommern, Germany. It connects the Gobenowsee with the Labussee.

Geographic entities mentioned:
surface_form: Gobenowsee
instance_of: Lake
countries: Germany
coordinates: lat: 53.224638888889
lon: 12.916316666667
surface_form: Labussee
instance_of: Lake
countries: Germany
coordinates: lat: 53.205
lon: 12.891666666667
Bąkowiec Castle. Bąkowiec Castle is a fourteenth-century knight's castle ruins, located in the Kraków-Częstochowa Upland. The fortress was built as part of the Trail of the Eagles' Nests defence system, located in the village of Morsko, Silesian Voivodeship in Poland. History.

Geographic entities mentioned:
surface_form: Kraków-Częstochowa Upland
instance_of: Plateau
countries: Poland
coordinates: lat: 50.2067
lon: 19.8292
Shieli-Telikol Canal. The Shieli-Telikol Canal (), also known as &quot;Shieli Canal&quot; and &quot;Telikol Canal&quot;, is an irrigation canal in the Kyzylorda Region, Kazakhstan. It connects the Telikol lakes with Shieli. Geography. The canal begins in the Telikol lacustrine area at the mouth of the Sarysu river in the north.

Geographic entities mentioned:
surface_form: Telikol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 45.2
lon: 66.56666666666666
Hoklingen. Hoklingen is a lake in Levanger Municipality in Trøndelag county, Norway. The lake lies just to the east of the village of Åsen and about south of the village of Skogn. The lake Movatnet is the main inflow of water into Hoklingen. There is a small dam that regulates the outflow of water at the southwest end of the lake.

Geographic entities mentioned:
surface_form: Movatnet
instance_of: Lake
countries: Norway
coordinates: lat: 63.6251
lon: 11.1884
surface_form: hoklingen
instance_of: Lake
countries: Norway
coordinates: lat: 63.6198
lon: 11.1313
The lake lies just to the east of the village of Åsen and about south of the village of Skogn. The lake Movatnet is the main inflow of water into Hoklingen. There is a small dam that regulates the outflow of water at the southwest end of the lake. The water flows out into the river Fossingelva which then flows into the nearby lake Hammervatnet.

Geographic entities mentioned:
surface_form: Hammervatnet
instance_of: Lake
countries: Norway
coordinates: lat: 63.6138
lon: 11.0041
Hoklingen. Hoklingen is a lake in Levanger Municipality in Trøndelag county, Norway. The lake lies just to the east of the village of Åsen and about south of the village of Skogn. The lake Movatnet is the main inflow of water into Hoklingen. There is a small dam that regulates the outflow of water at the southwest end of the lake.

Geographic entities mentioned:
surface_form: hoklingen
instance_of: Lake
countries: Norway
coordinates: lat: 63.6198
lon: 11.1313
In the north-east, it overrides and replaces the real Walney Island. Its highest mountain is Culdee Fell, which was modelled on Snowdon: the ridge of Devil's Back copies the Clogwyn ridge on Snowdon. The summit is reached by the Culdee Fell Railway, which is based on the Snowdon Mountain Railway in Wales.

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
Trade usually took the south side and migrations the north. This is most likely because the Tarim leads to the Ferghana Valley and Iran, while Dzungaria leads only to the open steppe. The difficulty with the south side was the high mountains between the Tarim and Ferghana. Furthermore, the Taklamakan is too dry to support much grass, and therefore nomads when they are not robbing caravans.

Geographic entities mentioned:
surface_form: Ferghana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
As a political or geographical term, &quot;Dzungaria&quot; has practically disappeared from the map; but the range of mountains stretching north-east along the southern frontier of the Zhetysu, as the district to the southeast of Lake Balkhash preserves the name of Dzungarian Alatau. It also gave name to Djungarian hamsters. Geography.

Geographic entities mentioned:
surface_form: Lake Balkhash
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.540833333333
lon: 74.878888888889
All of Khorasan was soon conquered by the Arabs, who would use it as a base to attack Transoxiana. Sufeh Pir. Sufeh Pir is a cave believed to be the tomb of Piran Viseh in Kūh-Zibad mountain. He was a Turanian figure in Shahnameh, the national epic of Greater Iran. Beside Shahnameh, Piran is also mentioned in other sources such as Tabari and Tha'ālibī.

Geographic entities mentioned:
surface_form: Kūh-Zibad
instance_of: Mountain
countries: Iran
coordinates: lat: 34.23963
lon: 58.41917
Lake Cacaoui. Lake Cacaoui () is a lake in the Côte-Nord region of Quebec, Canada. It drains into the Sainte-Marguerite River. Location. Lake Cacaoui is in the unorganized territory of Lac-Walker, part of the Sept-Rivières Regional County Municipality. The Cacaoui River leaves the west of the lake and runs north through a stretch of rapids into the Sainte-Marguerite River.

Geographic entities mentioned:
surface_form: lake cacaoui
instance_of: Lake
countries: Canada
coordinates: lat: 50.89917
lon: -66.96806
It drains into the Sainte-Marguerite River. Location. Lake Cacaoui is in the unorganized territory of Lac-Walker, part of the Sept-Rivières Regional County Municipality. The Cacaoui River leaves the west of the lake and runs north through a stretch of rapids into the Sainte-Marguerite River. Little Lake Cacaoui (Petit lac Cacaoui) connects to the main lake at its south end.

Geographic entities mentioned:
surface_form: lake cacaoui
instance_of: Lake
countries: Canada
coordinates: lat: 50.89917
lon: -66.96806
Location. Lake Cacaoui is in the unorganized territory of Lac-Walker, part of the Sept-Rivières Regional County Municipality. The Cacaoui River leaves the west of the lake and runs north through a stretch of rapids into the Sainte-Marguerite River. Little Lake Cacaoui (Petit lac Cacaoui) connects to the main lake at its south end. The lake is at an elevation of. It is about northwest of Sept-Îles.

Geographic entities mentioned:
surface_form: lake cacaoui
instance_of: Lake
countries: Canada
coordinates: lat: 50.89917
lon: -66.96806
surface_form: lac cacaoui
instance_of: Lake
countries: Canada
coordinates: lat: 50.89917
lon: -66.96806
surface_form: little lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.2968
lon: -78.3107
Pisacani. Pisacani or P'isaqani (Aymara &quot;p'isaqa&quot; &quot;Nothoprocta&quot; (a kind of bird), &quot;-ni&quot; a suffix to indicate ownership, &quot;the one with the &quot;p'isaqa&quot;, also spelled &quot;Pisacani, Pisarane, Pisarone&quot;) is a mountain in the Andes of southern Peru, about high. It is situated in the Tacna Region, Tarata Province, Ticaco District.

Geographic entities mentioned:
surface_form: pisacani
instance_of: Mountain
countries: Peru
coordinates: lat: -17.2768
lon: -69.9381
Pisacani. Pisacani or P'isaqani (Aymara &quot;p'isaqa&quot; &quot;Nothoprocta&quot; (a kind of bird), &quot;-ni&quot; a suffix to indicate ownership, &quot;the one with the &quot;p'isaqa&quot;, also spelled &quot;Pisacani, Pisarane, Pisarone&quot;) is a mountain in the Andes of southern Peru, about high. It is situated in the Tacna Region, Tarata Province, Ticaco District.

Geographic entities mentioned:
surface_form: pisacani
instance_of: Mountain
countries: Peru
coordinates: lat: -17.2768
lon: -69.9381
surface_form: pisacani
instance_of: Mountain
countries: Peru
coordinates: lat: -17.2768
lon: -69.9381
surface_form: p'isaqani
instance_of: Mountain
countries: Peru
coordinates: lat: -17.2768
lon: -69.9381
In 1474 he painted two fresco lunettes of &quot;Adam and Eve&quot; and &quot;Cain and Abel&quot; in the refectory of the Abbey at Passignano in the Val di Pesa. In 1484 he painted a &quot;Madonna della Cintola with Saints&quot; for San Piero a Sieve in the Mugello, now in the Princeton University Art Museum.

Geographic entities mentioned:
surface_form: Mugello
instance_of: Valley
countries: Italy
coordinates: lat: 43.95
lon: 11.3833
Coyote Mountains Wilderness (Arizona). The Coyote Mountains Wilderness of Arizona is part of the Coyote Mountains of southern Arizona in the center of Pima County. The wilderness lies about 40 mi southwest of Tucson, in the northwest of the Altar Valley. Kitt Peak is 4 mi WSW. Description. The Coyote Mountains Wilderness makes up much of the center and northeast of the Coyote Mountains.

Geographic entities mentioned:
surface_form: Altar Valley
instance_of: Valley
countries: United States
coordinates: lat: 31.82
lon: -111.4
Coyote Mountains Wilderness (Arizona). The Coyote Mountains Wilderness of Arizona is part of the Coyote Mountains of southern Arizona in the center of Pima County. The wilderness lies about 40 mi southwest of Tucson, in the northwest of the Altar Valley. Kitt Peak is 4 mi WSW. Description. The Coyote Mountains Wilderness makes up much of the center and northeast of the Coyote Mountains.

Geographic entities mentioned:
surface_form: Kitt Peak
instance_of: Mountain
countries: United States
coordinates: lat: 31.963966666667
lon: -111.59983611111
The Coyote's are separated from the Quinlin Mountains abutting southwest; both ranges anchor the northern end of the north–south, massif of the Baboquivari Mountains. The three ranges are located at the northwest of the Altar Valley. The Coyote Mountains are a small range only about 7 mi long, and merge into lower elevation hills.

Geographic entities mentioned:
surface_form: Altar Valley
instance_of: Valley
countries: United States
coordinates: lat: 31.82
lon: -111.4
The northeast, east, and southeast of the wilderness and the Coyote Mountains descend quickly into the Altar Valley. Kitt Peak. Kitt Peak and surrounding peaks form a separate landform between the Quinlin Mountains and the Coyotes. The Quinlins are a linear range, northwest by southeast. From Kitt Peak and northeastwards, the mountains and hills separate into individual units.

Geographic entities mentioned:
surface_form: Kitt Peak
instance_of: Mountain
countries: United States
coordinates: lat: 31.963966666667
lon: -111.59983611111
Thyssus. Thyssus or Thyssos () was a town of Chalcidice in ancient Macedon, situated on the west or south side of the peninsula of &quot;Acte&quot; or &quot;Akte&quot; (Ακτή) peninsula (now Mount Athos), the easternmost of the three peninsulas forming the ancient Chalcidice, on its western coast, north of Cleonae.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
In his seventieth year Ferguson, intending to prepare a new edition of the history, visited Italy and some of the principal cities of Europe, where he was received with honour by learned societies. From 1795 he resided successively at Neidpath Castle near Peebles, at Hallyards on Manor Water, and at St Andrews, where he died on 22 February 1816.

Geographic entities mentioned:
surface_form: Manor Water
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 55.642822
lon: -3.225243
Gulmarg Gondola. Gulmarg Gondola in Gulmarg, Jammu and Kashmir, is the second longest and second highest cable car in the world. Higher lines include the Mi Teleférico in Bolivia and at Jade Dragon Snow Mountain. Background. The two-stage gondola lift ferries about 600 people per hour to and from Kongdoori Mountain, a shoulder of nearby Apharwat Peak ().

Geographic entities mentioned:
surface_form: Jade Dragon Snow Mountain
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 27.098333333333
lon: 100.175
Higher lines include the Mi Teleférico in Bolivia and at Jade Dragon Snow Mountain. Background. The two-stage gondola lift ferries about 600 people per hour to and from Kongdoori Mountain, a shoulder of nearby Apharwat Peak (). The ropeway project is a joint venture of the Jammu and Kashmir government and French firm Pomagalski.

Geographic entities mentioned:
surface_form: Apharwat Peak
instance_of: Mountain
countries: India
coordinates: lat: 33.9995
lon: 74.3255
The park is one of the most popular in southeastern Pennsylvania, with most tourists visiting in the summer months. Lake Nockamixon. Lake Nockamixon is an artificial reservoir formed by a dam on Tohickon Creek and serves as the centerpiece of Nockamixon State Park. Swimming is not allowed in the lake, but boating is popular, and the park maintains several marinas and boat rentals.

Geographic entities mentioned:
surface_form: Lake Nockamixon
instance_of: Lake
countries: United States
coordinates: lat: 40.465488888889
lon: -75.220988888889
Pontypridd Deanery. akitwwoehqh73rj3b6n6ctrmo4pvq" xml:space="preserve">The Pontypridd Deanery is a Roman Catholic deanery in the Archdiocese of Cardiff-Menevia, previously in the Archdiocese of Cardiff, which covers several churches and the university chaplaincy in Pontypridd and the surrounding area of Rhondda, the southernmost part of the Cynon Valley, and Caerphilly.

Geographic entities mentioned:
surface_form: Rhondda
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
surface_form: Cynon Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.657
lon: -3.461
Ng Uk Tsuen, Yuen Long District. Ng Uk Tsuen () or Tai Tseng Ng Uk Tsuen () is a village in Wang Chau, Yuen Long District, Hong Kong. Location. Ng Uk Tsuen is located north of Kai Shan and Yuen Long Industrial Estate, next to the villages of Tai Tseng Wai and Shing Uk Tsuen. The area north of the village, Fung Lok Wai, features fish ponds. Administration.

Geographic entities mentioned:
surface_form: Kai Shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.45837
lon: 114.01626
Two silos were constructed of 2x6 lumber laid flat, along with a concrete silo. Toomey's Mill was placed on the National Register of Historic Places in 2008. As of March 2012, Toomey's Mill was torn down and was replaced by a convenience store. The site was removed from the NRHP in 2013. The bricks were then used to reconstruct the mill at the entrance to Devils Tower.

Geographic entities mentioned:
surface_form: Devils Tower
instance_of: Mountain
countries: United States
coordinates: lat: 44.590277777778
lon: -104.71527777778
Field Marshal Radomir Putnik withdrew the First Army from Syrmia, conducting a forced march south to reinforce Serbian positions. The counteroffensive targeted the Sixth Army and initially made progress, but culminated in a prolonged and bloody four-day engagement at Mačkov Kamen, a peak of the Jagodnja mountain.

Geographic entities mentioned:
surface_form: Jagodnja
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.33
lon: 19.293
The mountain chain is characterised by steep volcanic cones, including Tajumulco Volcano, the highest point in the country and Central America. All of Guatemala's 37 volcanoes (3 of them active: Pacaya, Santiaguito and Fuego), are in this mountain chain, and are abundant in the highlands.

Geographic entities mentioned:
surface_form: Pacaya
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.380833333333
lon: -90.601111111111
surface_form: Fuego
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.474722222222
lon: -90.880833333333
The rivers are short and shallow in the Pacific vertient, larger and deeper, such as the Polochic which drains in Lake Izabal, Río Dulce, Motagua and Sarstún that forms the boundary with Belize in the Caribbean and the Gulf of Mexico vertient (Usumacinta, which forms the boundary between Chiapas, Mexico and Petén and its tributaries such as La Pasión and San Pedro.

Geographic entities mentioned:
surface_form: Lake Izabal
instance_of: Lake
countries: Guatemala
coordinates: lat: 15.5
lon: -89.166666666667
The Tocorpuri volcanoes developed in the late Pleistocene in three separate stages and were subject to glaciation and tectonic faulting. The most recent eruption generated the La Torta lava dome 34,000 ± 7,000 years ago; presently there is geothermal activity which may be connected to that of the neighbouring El Tatio geothermal field. Geomorphology.

Geographic entities mentioned:
surface_form: El Tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
The border with Bolivia runs around the eastern side of Tocorpuri's summit crater. The area lies in Chile's Antofagasta Department and on Bolivia's Potosí Department and a pre-Hispanic road connecting the Bolivian Altiplano with the San Pedro de Atacama region passes south of the volcano. This road system is considered to be the oldest in Chile, was in use since the Formative Period.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Tocorpuri volcano is a complex of three different edifices. East Tocorpuri is high and rises around the surrounding terrain. A large, slightly elongated wide summit crater caps the summit. From Tocorpuri's summit, the Salar de Atacama salt flat and the Chuquicamata mine, the largest copper mine in the world, are visible. Sulfur deposits can be found in the summit region and were mined in the past.

Geographic entities mentioned:
surface_form: Salar de Atacama
instance_of: Lake
Body of water
countries: Chile
coordinates: lat: -23.416666666666668
lon: -68.26666666666667
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
Tocorpuri is reported to be solfatarically active, and there are hot springs, gas seeps and bubbling pools at elevation north of La Torta. The El Tatio and Sol de Manana geothermal fields lie north and east of Tocorpuri, respectively, and Trujillo-Ramírez 1974 reported additional manifestations south of Tocorpuri. El Tatio may receive its heat flux from a heat reservoir under La Torta.

Geographic entities mentioned:
surface_form: El Tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
Tocorpuri. Tocorpuri is a volcano on the border between Chile and Bolivia. Its peak height is most recently given as and it features a wide summit crater. The volcano consists mainly of lava flows and pyroclastic deposits and is subdivided into two separate edifices. Just west of Tocorpuri, the La Torta lava dome is a high flat-topped structure.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
Its peak height is most recently given as and it features a wide summit crater. The volcano consists mainly of lava flows and pyroclastic deposits and is subdivided into two separate edifices. Just west of Tocorpuri, the La Torta lava dome is a high flat-topped structure. The volcanoes are formed by andesitic, dacitic and rhyolitic rocks.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
The volcano consists mainly of lava flows and pyroclastic deposits and is subdivided into two separate edifices. Just west of Tocorpuri, the La Torta lava dome is a high flat-topped structure. The volcanoes are formed by andesitic, dacitic and rhyolitic rocks. The Tocorpuri volcanoes developed in the late Pleistocene in three separate stages and were subject to glaciation and tectonic faulting.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
The most recent eruption generated the La Torta lava dome 34,000 ± 7,000 years ago; presently there is geothermal activity which may be connected to that of the neighbouring El Tatio geothermal field. Geomorphology. Tocorpuri lies in northern Chile, about east of Calama. The border with Bolivia runs around the eastern side of Tocorpuri's summit crater.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
Geomorphology. Tocorpuri lies in northern Chile, about east of Calama. The border with Bolivia runs around the eastern side of Tocorpuri's summit crater. The area lies in Chile's Antofagasta Department and on Bolivia's Potosí Department and a pre-Hispanic road connecting the Bolivian Altiplano with the San Pedro de Atacama region passes south of the volcano.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
This road system is considered to be the oldest in Chile, was in use since the Formative Period. The name comes from the Kunza language, is also known as Michina, Cerro de Tocorpuri Cerros de Tocorpuri or Volcán Tocorpuri. Tocorpuri volcano is a complex of three different edifices. East Tocorpuri is high and rises around the surrounding terrain.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
surface_form: cerro de tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
surface_form: cerros de tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
This road system is considered to be the oldest in Chile, was in use since the Formative Period. The name comes from the Kunza language, is also known as Michina, Cerro de Tocorpuri Cerros de Tocorpuri or Volcán Tocorpuri. Tocorpuri volcano is a complex of three different edifices. East Tocorpuri is high and rises around the surrounding terrain.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
The name comes from the Kunza language, is also known as Michina, Cerro de Tocorpuri Cerros de Tocorpuri or Volcán Tocorpuri. Tocorpuri volcano is a complex of three different edifices. East Tocorpuri is high and rises around the surrounding terrain. A large, slightly elongated wide summit crater caps the summit.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
Other craters are heavily eroded and old, eroded lava flows occur on the southern flank, with younger, smaller flows present in the summit region. West Tocorpuri consists mainly of blocky lava flows which are particularly noticeable on the western side while East Tocorpuri consists of lava flows, pyroclastic deposits and tuff-like breccia.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
West Tocorpuri consists mainly of blocky lava flows which are particularly noticeable on the western side while East Tocorpuri consists of lava flows, pyroclastic deposits and tuff-like breccia. There is evidence of a southeastward sector collapse of Tocorpuri, which crops out on an area of on the southeastern flank within a horseshoe-shaped scar.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
There is evidence of a southeastward sector collapse of Tocorpuri, which crops out on an area of on the southeastern flank within a horseshoe-shaped scar. Tocorpuri is part of the main volcanic chain of the border region between Chile and Bolivia. The La Torta (&quot;cake&quot; in Spanish) lava dome is located between the Tocorpuri volcano to the east and Tatio volcano to the west.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
Tocorpuri is part of the main volcanic chain of the border region between Chile and Bolivia. The La Torta (&quot;cake&quot; in Spanish) lava dome is located between the Tocorpuri volcano to the east and Tatio volcano to the west. It is a flat-topped, about high body with steep flanks that covers a surface of about in a flat area.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
It and Tocorpuri, which are distant from each other, have been described as a volcano pair, whose existence may be a consequence of tectonics. Glacial erosion has cut into the flanks of the volcanoes, with moraines and mudflow deposits covering the foot of La Torta and cirques and glacial striations occurring on the Tocorpuri volcanoes. In the past, a glacier filled the crater of Tocorpuri.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
Glacial erosion has cut into the flanks of the volcanoes, with moraines and mudflow deposits covering the foot of La Torta and cirques and glacial striations occurring on the Tocorpuri volcanoes. In the past, a glacier filled the crater of Tocorpuri. South of La Torta, moraines extending from East Tocorpuri extend south-southwestward.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
In the past, a glacier filled the crater of Tocorpuri. South of La Torta, moraines extending from East Tocorpuri extend south-southwestward. Between Tatio and La Torta, there are two tongues of moraines side-by-side. The moraines from the western valley have overrun the eastern valley moraines and are accompanied by thin drift deposits.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
The moraines from the western valley have overrun the eastern valley moraines and are accompanied by thin drift deposits. These moraines have been dated by surface exposure dating: They formed during the regional last glacial maximum and by about 30,700 years ago the western glaciers were gone. Erosional debris covers the flanks of Tocorpuri. Climate and hydrology.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
Erosional debris covers the flanks of Tocorpuri. Climate and hydrology. The region has a high-altitude steppe climate with a low mean temperature of and a diurnal temperature range of. Annual precipitation on the summit has been estimated to exceed, while about fall every year south of Tocorpuri. Most of it occurs during summer as convective precipitation.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
Most of it occurs during summer as convective precipitation. Snow has been observed on the summit, and a 1985 map displays a persistent ice/snow cover there. The Putana River south of Tocorpuri flows towards the Salar de Atacama and receives important tributaries from the Tocorpuri area, such as Quebrada La Torta, Rio Blanco o Tocorpuri and Quebrada Agua Brava. Geology.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
Surges in activity took place 8, 6 and 4 million years ago; since 2.6 million years ago activity has declined. In the late Pleistocene, the lava domes Cerro Chanka, Cerro Chao, Cerro Chascon-Runtu Jarita complex, Chillahuita and Tocorpuri were emplaced around 100,000–90,000 years ago. The total volume of these domes exceeds, of which Cerro Chao is by far the largest.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
These ignimbrites were produced by eruptions in the APVC. Geologic lineaments have influenced the development of the volcanoes, including that of Tocorpuri, and La Torta formed at the end of a thrust fault that may have served as the path of ascent of magma. Composition. The volcanic rocks of Tocorpuri consist of andesite, dacite and rhyolite and define a potassium-rich calc-alkaline suite.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
Composition. The volcanic rocks of Tocorpuri consist of andesite, dacite and rhyolite and define a potassium-rich calc-alkaline suite. Phenocrysts include biotite, clinopyroxene, hornblende, orthopyroxene and plagioclase and differ between the various rocks. An origin through fractional crystallization has been proposed. The volcanic rocks in the summit region are hydrothermally altered.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
Geologic history. Volcanism in the area commenced 800,000 years ago. Tocorpuri formed in four stages, the first two built the two Tocorpuri volcanoes, the third produced lava flows emanating from fissure vents on Tocorpuri's southern and northwestern flank, and the fourth the La Torta dome. Déruelle 1979 inferred that East Tocorpuri was more recent than La Torta or West Tocorpuri.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
Tocorpuri formed in four stages, the first two built the two Tocorpuri volcanoes, the third produced lava flows emanating from fissure vents on Tocorpuri's southern and northwestern flank, and the fourth the La Torta dome. Déruelle 1979 inferred that East Tocorpuri was more recent than La Torta or West Tocorpuri. Between the two stages of volcanic activity, the edifices were tectonically deformed.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
Déruelle 1979 inferred that East Tocorpuri was more recent than La Torta or West Tocorpuri. Between the two stages of volcanic activity, the edifices were tectonically deformed. Thrusts and normal faults have offset Pliocene to Quaternary deposits around and on Tocorpuri, including in the summit region and the summit crater. La Torta.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
As Shiva and Vishnu temples are found, this place is known as Tirupper. Location. This temple is located at Kandiyur-Thirukattupalli-Kallanai-Trichy road, at a distance of 9 km from Thirukattupalli. Thi temple can be reached after crossing the Kaveri bridge in Thirukattupalli in Kallanai road, at a distance of 8 km.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
It is part of East Macedonia and Thrace. Its capital is the city of Kavala. Kavala regional unit is the easternmost within the geographical region of Macedonia. Geography. The Pangaio mountains, reaching 1,957 m are situated in the west. The neighbouring regional units are Serres to the west, Drama to the north and Xanthi to the east. The river Nestos flows along the eastern border.

Geographic entities mentioned:
surface_form: Pangaio mountains
instance_of: Mountain
countries: Greece
coordinates: lat: 40.899166666666666
lon: 24.08361111111111
Eggjareid Station. Eggjareid Station () is a railway station along the Bergensbanen railway line. It is located at the village of Eggjareid in the Raundalen valley in the municipality of Voss in Vestland county, Norway. The station was served by the Bergen Commuter Rail until its closure in 2012. The station was opened in 1936.

Geographic entities mentioned:
surface_form: Raundalen
instance_of: Valley
countries: Norway
coordinates: lat: 60.6789
lon: 6.56167
Nestled in the Sallisaw Creek valley, Bunch is bisected by what used to be the Kansas City Southern Railroad, now CPKC, which was built in the 1890s. Bunch is in the Cookson Hills area of eastern Oklahoma which are a part of the western area of the Ozark Mountains. The Cookson Hills Wildlife Management Area is west of the town.

Geographic entities mentioned:
surface_form: Cookson Hills
instance_of: Landform
countries: United States
coordinates: lat: 35.7
lon: -94.8