Sarmila/GeoWiki-Features huggingface dataset:
Clarazia. &quot;Clarazia&quot; is an extinct genus of thalattosaur from the Middle Triassic of Monte San Giorgio in Switzerland. It is represented by a single type species, &quot;Clarazia schinzi&quot;, which was named in 1936.

Geographic entities mentioned:
surface_form: Monte San Giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
Backdrop Peak. Backdrop Peak, at above sea level is a peak in the Smoky Mountains of Idaho. Located in Sawtooth National Forest on the border of Blaine and Camas counties, Backdrop Peak is about north of Baker Peak. Baker Lake is just east of the peak.

Geographic entities mentioned:
surface_form: baker lake
instance_of: Lake
countries: United States
coordinates: lat: 47.3515175
lon: -121.3017165
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker lake
instance_of: Lake
countries: United States
coordinates: lat: 40.6481
lon: -121.376
Backdrop Peak. Backdrop Peak, at above sea level is a peak in the Smoky Mountains of Idaho. Located in Sawtooth National Forest on the border of Blaine and Camas counties, Backdrop Peak is about north of Baker Peak. Baker Lake is just east of the peak.

Geographic entities mentioned:
surface_form: backdrop peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.6889
lon: -114.687
Backdrop Peak. Backdrop Peak, at above sea level is a peak in the Smoky Mountains of Idaho. Located in Sawtooth National Forest on the border of Blaine and Camas counties, Backdrop Peak is about north of Baker Peak. Baker Lake is just east of the peak.

Geographic entities mentioned:
surface_form: backdrop peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.6889
lon: -114.687
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.6699
lon: -114.68
The surficial geology in the vicinity of these mountains includes Wisconsinan Till and bedrock, among other things. Jackson Creek is classified as a Coldwater Fishery and a Migratory Fishery. Course. Jackson Creek begins in a broad valley between Avery Mountain and Osterhout Mountain in Tunkhannock Township. It flows south-southwest for a few tenths of a mile before turning south-southeast.

Geographic entities mentioned:
surface_form: Osterhout Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5362
lon: -75.8986
Geography and geology. The elevation near the mouth of Jackson Creek is above sea level. The elevation of the creek's source is between above sea level. Avery Mountain, which has an elevation of slightly more than above sea level, occurs in the vicinity of Jackson Creek, as does Osterhout Mountain, which has an elevation of well over above sea level.

Geographic entities mentioned:
surface_form: Osterhout Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5362
lon: -75.8986
Nowadays, Stavros tis Minthis is right next to an 18-hole golf course, Minthis Hills, the first ever created in Cyprus. Here a resort will be created. To the west of the village stands the 616 m Tsiárta mountain. Transportation. Tsada lies next to a transportation hub linking most of Paphos district's villages.

Geographic entities mentioned:
surface_form: Tsiárta
instance_of: Mountain
countries: Cyprus
coordinates: lat: 34.8435
lon: 32.4543
Severely wounded, he was evacuated to Regimental base hospital. He spent the next five months in various hospitals. He was moved by ambulance train and arrived in Hyeres Base Hospital #99 by direction of his brother Ursus, where as a United States Army physician was stationed. As Portmann was infirmed, he had learned that he received a battlefield promotion to Major.

Geographic entities mentioned:
surface_form: Hyeres
instance_of: Mountain
countries: France
coordinates: lat: 43.118888888889
lon: 6.1286111111111
Kivu District. Kivu District (,) was a district of the Belgian Congo. It was formed from part of Stanleyville District in 1914. Location. Kivu District was named after Lake Kivu, on the border between the Belgian and German colonies. Between 30 June 1900 and 27 July 1901 Jules Alexandre Milz undertook a special mission to delimit the Belgian-German border in Kivu.

Geographic entities mentioned:
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
In 1971, seven villages on Brome Lake (Bondville, East Hill, Foster, Fulford, Knowlton, Iron Hill, and West Brome) were amalgamated to create the current town, which is now in the Brome-Missisquoi Regional County Municipality of the Estrie administrative region. Geography. Metamorphic rock of Cambrian age—mostly schist and phyllite—underlies the area.

Geographic entities mentioned:
surface_form: Brome Lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.2486
lon: -72.5147
Pine Ridge is in the Ridge and Valley portion of the Appalachian Mountains and occupies a series of low ridges and valleys. From east to west, they are Middle Ridge, Dugout Valley, Shinbone Ridge, and Sand Valley, with the northwestern part of the town climbing the eastern edge of Sand Mountain, a southern extension of the Cumberland Plateau.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
The Baikal yellowfin (&quot;Cottocomephorus grewingkii&quot;), also known as the yellow-finned sculpin or yellow-wing sculpin, is a species of freshwater ray-finned fish belonging to the family Cottidae, the typical sculpins. This species is endemic to Lake Baikal and its tributaries in Siberia, Russia. It is most common in the southern part of the lake and lives from near the shore to a depth of.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Middle Teton. Middle Teton () is the third-highest peak in the Teton Range, in the U.S. state of Wyoming. Located within Grand Teton National Park, the peak is immediately southwest of Grand Teton, from which it is separated by a broad high ridge at, known to local climbers as the Lower Saddle. The Middle Teton Glacier is located on the eastern slopes of the peak.

Geographic entities mentioned:
surface_form: Grand Teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.7412
lon: -110.802
surface_form: grand teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.7412
lon: -110.802
The black dike is a basaltic intrusion that occurred long after the surrounding rock was formed. Climbing. The first recorded ascent of Middle Teton was by Albert R. Ellingwood on August 23, 1923, via Ellingwood Couloir on the south side of the peak. Ellingwood made the first ascent of South Teton the same day. What is known as the southwest couloir provides the easiest route to the summit.

Geographic entities mentioned:
surface_form: South Teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.7186
lon: -110.819
The Middle Teton Glacier is located on the eastern slopes of the peak. Middle Teton is a classic pyramidal alpine peak and is sometimes included as part of the Cathedral Group of high Teton peaks. The Teton Range is the youngest mountain chain in the Rocky Mountains, beginning its uplift 9 million years ago, during the Miocene.

Geographic entities mentioned:
surface_form: alpine peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1716
lon: -115.05
surface_form: middle teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.73
lon: -110.811
surface_form: the cathedral
instance_of: Mountain
countries: United States
coordinates: lat: 40.775833333333
lon: -110.71027777778
Middle Teton. Middle Teton () is the third-highest peak in the Teton Range, in the U.S. state of Wyoming. Located within Grand Teton National Park, the peak is immediately southwest of Grand Teton, from which it is separated by a broad high ridge at, known to local climbers as the Lower Saddle. The Middle Teton Glacier is located on the eastern slopes of the peak.

Geographic entities mentioned:
surface_form: middle teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.73
lon: -110.811
Located within Grand Teton National Park, the peak is immediately southwest of Grand Teton, from which it is separated by a broad high ridge at, known to local climbers as the Lower Saddle. The Middle Teton Glacier is located on the eastern slopes of the peak. Middle Teton is a classic pyramidal alpine peak and is sometimes included as part of the Cathedral Group of high Teton peaks.

Geographic entities mentioned:
surface_form: middle teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.73
lon: -110.811
The Teton Range is the youngest mountain chain in the Rocky Mountains, beginning its uplift 9 million years ago, during the Miocene. Several periods of glaciation have carved Middle Teton and the other peaks of the range into their current shapes. From the Lower Saddle, a distinctive feature known as the black dike appears as a straight line running from near the top of the mountain down.

Geographic entities mentioned:
surface_form: middle teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.73
lon: -110.811
The black dike is a basaltic intrusion that occurred long after the surrounding rock was formed. Climbing. The first recorded ascent of Middle Teton was by Albert R. Ellingwood on August 23, 1923, via Ellingwood Couloir on the south side of the peak. Ellingwood made the first ascent of South Teton the same day. What is known as the southwest couloir provides the easiest route to the summit.

Geographic entities mentioned:
surface_form: middle teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.73
lon: -110.811
Ellingwood made the first ascent of South Teton the same day. What is known as the southwest couloir provides the easiest route to the summit. Other sections on the mountain are rated as high as class 5.11, with the Middle Teton Glacier route considered to be the most technically advanced. The first ascent of the Glacier Route was completed on August 4, 1944, by Paul Bradt and Sterling Hendricks.

Geographic entities mentioned:
surface_form: middle teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.73
lon: -110.811
Zoroastrianism in Iran. Zoroastrianism is considered to be the oldest religion still practiced in Iran. It is an Iranian religion that emerged around the 2nd millennium BCE, spreading through the Iranian plateau and eventually gaining official status under the Achaemenid Empire in the 6th century BCE.

Geographic entities mentioned:
surface_form: Iranian plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
Old Fort Providence. Old Fort Providence, located near the mouth of Yellowknife Bay, Northwest Territories, Canada, was one of the first fur trading outposts on Great Slave Lake. Peter Pond of the North West Company first proposed trading with the Dene around Great Slave Lake in 1786.

Geographic entities mentioned:
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
Puma Ranra (Quechua &quot;puma&quot; cougar, puma, &quot;ranra&quot; stony, stony place) is a mountain in the Andes of Peru, about high. It is situated in the Arequipa Region, Castilla Province, Andagua District, and in the Condesuyos Province, Salamanca District. Puma Ranra lies southwest of Usqullu and Wakapallqa and Usqullu Lake, and northeast of the Coropuna volcano.

Geographic entities mentioned:
surface_form: Usqullu
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4478
lon: -72.4889
surface_form: Wakapallqa
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4731
lon: -72.4783
surface_form: usqullu
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4478
lon: -72.4889
surface_form: usqullu
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4478
lon: -72.4889
surface_form: wakapallqa
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4731
lon: -72.4783
Puma Ranra (Castilla-Condesuyos). Puma Ranra (Quechua &quot;puma&quot; cougar, puma, &quot;ranra&quot; stony, stony place) is a mountain in the Andes of Peru, about high. It is situated in the Arequipa Region, Castilla Province, Andagua District, and in the Condesuyos Province, Salamanca District.

Geographic entities mentioned:
surface_form: puma ranra
instance_of: Mountain
countries: Peru
coordinates: lat: -12.44944444
lon: -75.74305556
surface_form: puma ranra
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4861
lon: -72.5083
surface_form: puma ranra
instance_of: Mountain
countries: Peru
coordinates: lat: -15.0056
lon: -72.3764
Dungarvon River. The Dungarvon River is a tributary of the Renous River in New Brunswick, Canada. The Dungarvon River has its origins at several lakes in the Miramichi Highlands, part of the Appalachian Mountains, in the northeast corner of York County.

Geographic entities mentioned:
surface_form: Renous River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.8137
lon: -65.794
surface_form: dungarvon river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.8213
lon: -65.7924
The Dungarvon River has its origins at several lakes in the Miramichi Highlands, part of the Appalachian Mountains, in the northeast corner of York County. Generally flowing southeast through heavy forests, the Dungarvon River joins the Renous River at Grainfield, several kilometres northwest of the community of Renous, where the Renous River joins the Main Southwest Miramichi River.

Geographic entities mentioned:
surface_form: Southwest Miramichi River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.519346
lon: -67.151946
surface_form: renous river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.8137
lon: -65.794
surface_form: renous river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.8137
lon: -65.794
surface_form: dungarvon river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.8213
lon: -65.7924
Dungarvon River. The Dungarvon River is a tributary of the Renous River in New Brunswick, Canada. The Dungarvon River has its origins at several lakes in the Miramichi Highlands, part of the Appalachian Mountains, in the northeast corner of York County.

Geographic entities mentioned:
surface_form: dungarvon river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.8213
lon: -65.7924
The annual run of Atlantic salmon occurs from mid-June through late September of each summer and early fall. Angling for Atlantic salmon is restricted to fly fishing only and all large salmon must be released. Popular flies on the Dungarvon River include both the Cosseboom and the Black Bear series. There is also a local fly pattern known as the Dungarvon Special.

Geographic entities mentioned:
surface_form: dungarvon river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.8213
lon: -65.7924
surface_form: bear
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.2833
lon: -126.967
Oguni-numa Pond. Oguni-numa Pond (Japanese Kanji: 雄国沼; Japanese Hiragana: おぐにぬま) is a pond located at the western base of Mount Nekomadake in Fukushima Prefecture, Japan. The pond is situated on the remains of a crater and has a circumference of 4 km and an area of 45 hectares. The wetland flora of the pond is a nationally designated natural monument.

Geographic entities mentioned:
surface_form: Mount Nekomadake
instance_of: Mountain
countries: Japan
coordinates: lat: 37.611638888889
lon: 140.02836111111
surface_form: oguni-numa pond
instance_of: Lake
countries: Japan
coordinates: lat: 37.61944444
lon: 140.00277778
Oguni-numa Pond. Oguni-numa Pond (Japanese Kanji: 雄国沼; Japanese Hiragana: おぐにぬま) is a pond located at the western base of Mount Nekomadake in Fukushima Prefecture, Japan. The pond is situated on the remains of a crater and has a circumference of 4 km and an area of 45 hectares. The wetland flora of the pond is a nationally designated natural monument.

Geographic entities mentioned:
surface_form: oguni-numa pond
instance_of: Lake
countries: Japan
coordinates: lat: 37.61944444
lon: 140.00277778
His father worked as an intercity bus agent in Lubuk Sikaping, a job which barely fed him and his family. He went to &quot;Schakelschool&quot; (People's School, equivalent to elementary school) and graduated at the age of 14. Rais then continued to study at the Meer Uitgebreid Lager Onderwijs (equivalent to Junior High School) near Mount Singgalang.

Geographic entities mentioned:
surface_form: Mount Singgalang
instance_of: Mountain
countries: Indonesia
coordinates: lat: -0.39138888888889
lon: 100.33111111111
In 1857, oil shale industry started in Germany. In Canada, the Craigleith Shale Oil Works started to retort oil shale of the Ordovician Whitby Formation near Collingwood, Ontario, on Lake Huron in 1859. In 1861 it became economically infeasible due to the discovery of petroleum nearby. In Australia, the first oil shale mine was commenced in 1865 at American Creek, Mount Kembla in New South Wales.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
In 1861 it became economically infeasible due to the discovery of petroleum nearby. In Australia, the first oil shale mine was commenced in 1865 at American Creek, Mount Kembla in New South Wales. At the same year, the first shale oil was produced by the Pioneer Kerosene Works at American Creek.

Geographic entities mentioned:
surface_form: Mount Kembla
instance_of: Mountain
countries: Australia
coordinates: lat: -34.426944444444445
lon: 150.8255556
In the United States the government started to create the Naval Petroleum and Oil Shale Reserves in 1909. The reserves were seen as a possible emergency source of fuel for the military, particularly the Navy. The government reserved the Roan Plateau near Rifle, Colorado which later became a federal demonstration and test site.

Geographic entities mentioned:
surface_form: Roan Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 39.585
lon: -107.958
Kagghamraåns sjösystem. The Kagghamraåns sjösystem is a system of lakes in Stockholm county, Södermanland, Sweden.

Geographic entities mentioned:
surface_form: kagghamraåns sjösystem
instance_of: Group of lakes
countries: Sweden
coordinates: lat: 59.13333333
lon: 17.81666667
Mount Victor. hwop6jx97sdmwks5i23ui5tjqef" xml:space="preserve">#redirect Belgica Mountains

Geographic entities mentioned:
surface_form: victor
instance_of: Mountain
coordinates: lat: -72.6
lon: 31.26666667
surface_form: mount victor
instance_of: Mountain
coordinates: lat: -72.6
lon: 31.26666667
After &quot;Sacramento&quot; ran aground and was wrecked in the Bay of Bengal on 6 June 1867, Rodgers served aboard the steamer on the Great Lakes from 1868 to 1869 before duty in the North Pacific Squadron successively aboard the screw steamer and sailing sloop-of-war in 1870 and the steam sloop-of-war from 1871 to 1872.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
739, listed on June 6, 1960. The location was founded by the Franciscan Fathers at the Mission San Francisco Solano. The wine produced was used for Holy communion in worship church services and Holy mass. The San Francisco Solano de Sonoma Mission Vineyard was the first vineyard in Sonoma Valley. All the California Missions lost land and building in the Mexican secularization act of 1833.

Geographic entities mentioned:
surface_form: Sonoma Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.3667
lon: -122.5
Bishazari Tal. Bishazari Tal, also spelled Beeshazar Tal, is an extensive oxbow lake system in the buffer zone of the Chitwan National Park, a protected area in the Inner Terai of central Nepal. This wetland covers an area of at an altitude of. The Mahabharat mountain range (Lower Himalayan Range) is located north of the lake, which is itself north of the Siwalik Hills.

Geographic entities mentioned:
surface_form: beeshazar tal
instance_of: Group of lakes
countries: Nepal
coordinates: lat: 27.61805556
lon: 84.43638889
surface_form: bishazari tal
instance_of: Group of lakes
countries: Nepal
coordinates: lat: 27.61805556
lon: 84.43638889
Bishazari Tal. Bishazari Tal, also spelled Beeshazar Tal, is an extensive oxbow lake system in the buffer zone of the Chitwan National Park, a protected area in the Inner Terai of central Nepal. This wetland covers an area of at an altitude of. The Mahabharat mountain range (Lower Himalayan Range) is located north of the lake, which is itself north of the Siwalik Hills.

Geographic entities mentioned:
surface_form: bishazari tal
instance_of: Group of lakes
countries: Nepal
coordinates: lat: 27.61805556
lon: 84.43638889
Utkhuqaqa. Utkhuqaqa or Utkhu Qaqa (Quechua &quot;utkhu&quot; cotton, &quot;qaqa&quot; rock, &quot;cotton rock&quot;, also spelled &quot;Utccuccacca, Utjujanja&quot;) is a mountain in the Apolobamba mountain range in the Andes of Peru. It is located in the Puno Region, Sandia Province, Cuyocuyo District. It lies northwest of the mountain Wilaquta and northeast of Qurwari and Janq'u Uma.

Geographic entities mentioned:
surface_form: utkhu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5458
lon: -72.8075
surface_form: utkhu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5458
lon: -72.8075
surface_form: utkhuqaqa
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5558
lon: -69.4581
It is located in the Puno Region, Sandia Province, Cuyocuyo District. It lies northwest of the mountain Wilaquta and northeast of Qurwari and Janq'u Uma. Little streams named Qullqipirwa &quot;(Jolljepirhua)&quot;, Janq'u Uma &quot;(Janjouma)&quot; and Utkhuqaqa &quot;(Utjujaja)&quot; flow along its slopes. They are the origin of the river Lawa Lawani which runs to the north.

Geographic entities mentioned:
surface_form: janq'u uma
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5689
lon: -69.4631
surface_form: qurwari
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5906
lon: -69.4833
It is located in the Puno Region, Sandia Province, Cuyocuyo District. It lies northwest of the mountain Wilaquta and northeast of Qurwari and Janq'u Uma. Little streams named Qullqipirwa &quot;(Jolljepirhua)&quot;, Janq'u Uma &quot;(Janjouma)&quot; and Utkhuqaqa &quot;(Utjujaja)&quot; flow along its slopes. They are the origin of the river Lawa Lawani which runs to the north.

Geographic entities mentioned:
surface_form: janq'u uma
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5689
lon: -69.4631
surface_form: utkhuqaqa
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5558
lon: -69.4581
Utkhuqaqa. Utkhuqaqa or Utkhu Qaqa (Quechua &quot;utkhu&quot; cotton, &quot;qaqa&quot; rock, &quot;cotton rock&quot;, also spelled &quot;Utccuccacca, Utjujanja&quot;) is a mountain in the Apolobamba mountain range in the Andes of Peru. It is located in the Puno Region, Sandia Province, Cuyocuyo District. It lies northwest of the mountain Wilaquta and northeast of Qurwari and Janq'u Uma.

Geographic entities mentioned:
surface_form: utkhuqaqa
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5558
lon: -69.4581
She built up an art studio which became the meeting place and source of inspiration for local artists. She was also co-founder of Artists on the Bluff, a non-profit organization for artists. She was a member of the Art Association of Jackson Hole, and organized events and art fairs there. From watercolor and acrylic to oil painting, Trentham produced pieces featuring both figures and landscapes.

Geographic entities mentioned:
surface_form: Jackson Hole
instance_of: Valley
countries: United States
coordinates: lat: 43.516666666667
lon: -110.83333333333
Úmbita. Úmbita is a town and municipality in the Márquez Province, part of the Colombian department of Boyacá. Úmbita is situated on the Altiplano Cundiboyacense at a distance of from department capital Tunja and borders Nuevo Colón and Tibaná in the north, Chinavita in the east, La Capilla and Tibiritá (Cundinamarca) in the south and in the west Villapinzón (Cundinamarca) and Turmequé.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
In descending order of land area it is located in parts of Utah, Wasatch, Juab, and Sanpete counties. One of the most prominent features of the Uinta National Forest is the Mount Timpanogos mountain peak, towering over above sea level. However, the highest point in the Unita National Forest (as well as the entire Wasatch Range) is the nearby Mount Nebo at above sea level. Wilderness areas.

Geographic entities mentioned:
surface_form: Mount Timpanogos
instance_of: Mountain
countries: United States
coordinates: lat: 40.390836111111
lon: -111.64594444444
This made Buqa to harbor resentment towards Tekuder and grow more sympathetic to Arghun. On the other hand, he lost Tekuder's favor who started to invest his trust in Aq Buqa, another Jalair general. Seeing developments, Arghun sook refuge in Kalat-e Naderi, a strong fortress on 7 July with 100 men. But he was forced to surrender to Alinaq four days later.

Geographic entities mentioned:
surface_form: Kalat-e Naderi
instance_of: Plateau
countries: Iran
coordinates: lat: 36.983333333333334
lon: 59.8675
Initially known as &quot;INS Rajali II&quot;, it was formally recommissioned as &quot;INS Parundu&quot; on 26 March 2009 by the Chief of the Naval Staff Admiral Sureesh Mehta. INS Parundu is used primarily as a reconnaissance station to monitor the South East Bay of Bengal, the Palk Strait, and the Gulf of Mannar.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Swamps on Mount Poroshiri, the tallest peak of the Hidaka Mountains, as well as mountains in the Saru District region are reputedly inhabited by the &quot;sak-somo-ayep&quot;, and though they cannot be seen, the strong smell issued by the dragons have been held responsible for the swelling or bloating developed on the skin, according to testimony by early 20th century informants.

Geographic entities mentioned:
surface_form: Mount Poroshiri
instance_of: Mountain
countries: Japan
coordinates: lat: 42.719444444444
lon: 142.68277777778
Elsie Vaalbooi. Elsie Vaalbooi (born c. 1901, died 7 October 2002) of Rietfontein in the Northern Cape was a South African woman who was a member of the ǂKhomani (Nǁnǂe) San or Bushmen and one of the last speakers of the Nǁng language (better known by the name of the primary dialect, Nǀuu).

Geographic entities mentioned:
surface_form: Rietfontein
instance_of: Mountain
countries: South Africa
coordinates: lat: -26.7333
lon: 20.0333
The earlier exploits of the Regiment includes the annexation of the entire Hill Region of Jammu and the Kashmir Valley. General Zorawar Singh, who had joined the State Forces in 1823 assisted in expansion of the state's territory to include Ladakh, Baltistan, Tibet, Gilgit, Yasin, Darel, Hunza Nagar, Chilas and Chitral between 1834 and 1895. World War I.

Geographic entities mentioned:
surface_form: Yasin
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.367777777777775
lon: 73.33777777777777
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
Betzenberg. The Betzenberg () is a 285-metre-high hill in the German city of Kaiserslautern. It rises about 50 metres above the city and gives its name to the quarter in which it stands. It was well known because it also gave its name to what is now the Fritz Walter Stadium (formerly the Betzenberg Stadium or, colloquially, the &quot;Betze&quot;). Hill.

Geographic entities mentioned:
surface_form: betzenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.6174
lon: 9.14308
surface_form: betzenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.43319406
lon: 7.79042244
Betzenberg. The Betzenberg () is a 285-metre-high hill in the German city of Kaiserslautern. It rises about 50 metres above the city and gives its name to the quarter in which it stands. It was well known because it also gave its name to what is now the Fritz Walter Stadium (formerly the Betzenberg Stadium or, colloquially, the &quot;Betze&quot;). Hill.

Geographic entities mentioned:
surface_form: betzenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.6174
lon: 9.14308
surface_form: betze
instance_of: Mountain
countries: Germany
coordinates: lat: 49.43319406
lon: 7.79042244
surface_form: betzenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.43319406
lon: 7.79042244
Hill. The Betzenberg lies south of Kaiserslautern Central Station and the main railway axis from Ludwigshafen to Saarbrücken. The southern end of the Betzenberg transitions into the Palatine Forest. City quarter. Kaiserlautern's Betzenberg quarter is fairly young. It was laid out in 1967; only the built-up area below and around the Fritz Walter Stadium is older.

Geographic entities mentioned:
surface_form: betzenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.6174
lon: 9.14308
surface_form: betzenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.43319406
lon: 7.79042244
It grows at altitudes up to 1800 m above sea level, and it has an acceptable frost tolerance within this mostly tropical genus. A specific example of occurrence is in the La Campana National Park of central Chile and amid the adjoining Cerro La Campana; in that location it is associated with the endangered Chilean wine palm, a tree with a much wider prehistoric distribution than at present.

Geographic entities mentioned:
surface_form: Cerro La Campana
instance_of: Mountain
countries: Chile
coordinates: lat: -32.953611111111
lon: -71.119444444444
St Peter's Cave, Chepstow. St Peter's Cave is a natural opening in the base of the limestone of Hardwick Cliff, below Bulwarks Camp and above the mean high-water mark on the River Wye in Chepstow. It is potentially the site of the earliest discovered evidence of human occupation in this part of the lower Wye Valley. It is a scheduled monument. Nomenclature.

Geographic entities mentioned:
surface_form: Wye Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
Pushkin Street, Kazan. Pushkin Street (;) is the main street of Kazan, the capital of the Republic of Tatarstan, Russia. The street runs from the Kaban Lakes in the southwest to the Kazanka River in the north. The street is one of the busiest in Kazan and is a major shopping area. The street is named after the Russian poet Alexander Pushkin.

Geographic entities mentioned:
surface_form: Kaban Lakes
instance_of: Group of lakes
countries: Russia
coordinates: lat: 55.775
lon: 49.123611111111
Under Katō's command, the unit recorded over 260 aerial victories over Allied aircraft. He disallowed individual victory credits for the sake of teamwork. Katō was promoted to lieutenant colonel in February 1942. On May 22, 1942, while over the Bay of Bengal, Katō was killed in action while attacking a flight of No. 60 Squadron RAF Bristol Blenheim bombers.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Protective duties. It works with the Nigeria Police Force in securing any area in the Federal Capital Territory. Ceremonial actions and other traditions. Members of the brigade stand at the Presidential Villa in Aso Rock and also raise and lower the national flag at ceremonies and parades. The brigade holds a weekly changing of the guard ceremony outside Aso Villa.

Geographic entities mentioned:
surface_form: Aso Rock
instance_of: Mountain
countries: Nigeria
coordinates: lat: 9.0833333333333
lon: 7.5361111111111
Húseyjarkvísl. Húseyjarkvísl (&quot;Húseyja Branch,&quot; named after the farm Húsey in Vallhólmur) is a rock stream in Skagafjörður, Iceland, that comes up to meet the Svartá (&quot;Black River&quot;) in Eyvindarstaðaheiði. It runs down Svartárdalur along Reykjatunga into Vallhólmur, where its name then changes to Húseyjarkvísl.

Geographic entities mentioned:
surface_form: Svartárdalur
instance_of: Valley
countries: Iceland
coordinates: lat: 65.3124260477
lon: -19.1604467741
Sigurd Lewerentz. Sigurd Lewerentz (29 July 1885 &ndash; 29 December 1975) was a Swedish architect. Biography. Lewerentz was born at Sandö in the parish of Bjärtrå in Västernorrland County, Sweden. He was the son of Gustaf Adolf Lewerentz and Hedvig Mathilda Holmgren. He initially trained as a mechanical engineer at the Chalmers University of Technology in Gothenburg (1905–8).

Geographic entities mentioned:
surface_form: Sandö
instance_of: Valley
countries: Sweden
coordinates: lat: 63
lon: 17.75
Panoramic views can be enjoyed from the slopes of Golden Hill and several places along the western ridge at the park. From these vantage points, the whole length of Smuggler's Ridge, Tai Mo Shan (the highest peak in Hong Kong), Needle Hill, Sha Tin New Town, Lion Rock and Beacon Hill can be seen.

Geographic entities mentioned:
surface_form: Tai Mo Shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.4118
lon: 114.123
surface_form: Needle Hill
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.3871
lon: 114.16
surface_form: Lion Rock
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.3531
lon: 114.187
Knežlaz. Knežlaz () is a village in Krivošije microregion in southwestern Montenegro, north of the coastal town of Risan. According to the 2011 census, the village had 26 inhabitants. The village is notable as the location of the signing of the peace agreement between the rebelled Krivošije clan and Austria-Hungary on 11 January 1870, which put an end to the Krivošije uprising of 1869.

Geographic entities mentioned:
surface_form: Krivošije
instance_of: Landform
countries: Montenegro
coordinates: lat: 42.55
lon: 18.65
Biliaivka urban hromada. Geography. The total area of the municipality is 396.4 km². The following water bodies are located on the territory of the hromada: rivers Baraboi, Turunchuk, lakes Bile, Pohorile, Safiany, also reservoirs Baraboi and Cuciurgan.

Geographic entities mentioned:
surface_form: Bile
instance_of: Lake
countries: Ukraine
coordinates: lat: 46.452399
lon: 30.180968
surface_form: Pohorile
instance_of: Lake
countries: Ukraine
coordinates: lat: 46.464777777778
lon: 30.206694444444
surface_form: Safiany
instance_of: Lake
countries: Ukraine
coordinates: lat: 46.473638888889
lon: 30.1895
Railway service to Parrsboro was abandoned on June 14, 1958, following several years of declining shipments, several months before the 1958 mining disaster. Throughout the late 19th century and first four decades of the twentieth century, Parrsboro saw daily ferry service across the Minas Basin to the Annapolis Valley ports of Kingsport and Wolfville.

Geographic entities mentioned:
surface_form: Annapolis Valley
instance_of: Valley
countries: Canada
coordinates: lat: 44.979166666666664
lon: -64.89222222222222
Blind River (Louisiana). Blind River is a waterway in southeastern Louisiana originating in the Maurepas Swamp Wildlife Management Area of St James Parish west of New Orleans and running northeasterly before turning east to flow into Lake Maurepas. The lower reaches of Blind River form the boundary between Livingston Parish on the north shore and St James and St.

Geographic entities mentioned:
surface_form: Lake Maurepas
instance_of: Lake
countries: United States
coordinates: lat: 30.258027777778
lon: -90.498677777778
It is located between Fitzroy Falls Dam and Tallowa Dam. The pondage, part of the Shoalhaven Scheme, functions as a buffer storage for out-of-balance flow between the two dams during hydro-electric power generation or water pumping at Kangaroo Valley and Bendeela pumping and power stations.

Geographic entities mentioned:
surface_form: Shoalhaven Scheme
instance_of: Lake
countries: Australia
The Agasthya hill range is famous for its abundance of rare herbs and medicinal plants. There is a tea estate in Bonacaud, established by the British. The hill resort Ponmudi is near Bonacaud. Bonacaud (natively called Bonakkad) is now used as trekking base camp to Agasthyakoodam. It has many scenic locations including the forests, waterfalls and tea estates.

Geographic entities mentioned:
surface_form: Ponmudi
instance_of: Mountain
countries: India
coordinates: lat: 8.7602777777778
lon: 77.116666666667
Seeds are explosively dehisced from the capsule. Fruiting occurs between May and June. Habitat and range. Texabama croton is restricted to the eastern Edwards Plateau and southern Cross Timbers within Travis, Bell and Coryell counties. Within this limited range, it has a very patchy distribution and is abundant in the few niches where it occurs and is absent elsewhere.

Geographic entities mentioned:
surface_form: Edwards Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 30.3
lon: -99.6
Today, public swimming is banned in the lake due to its &quot;oozy/squishy/mushy&quot; bottom. The lake is drained by an intermittent stream that travels north into the Ottawa River. Its watershed includes the nearby Beechwood Cemetery and the next-door Sand Pits Lake, better known as &quot;The Pond&quot;. The lake is fed by an intermittent stream that flows into the lake from the southeast.

Geographic entities mentioned:
surface_form: Sand Pits Lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.45089
lon: -75.66675
McKay Lake (Ottawa). McKay Lake (formerly Hemlock Lake, McKay's Lake, or MacKay Lake) is a meromictic lake located in the former Village of Rockcliffe Park in Ottawa, Ontario, Canada. The lake is named for Thomas McKay, one of the founders of Ottawa, who once owned all of Rockcliffe Park in the 19th century, including the lake.

Geographic entities mentioned:
surface_form: mackay lake
instance_of: Lake
countries: Canada
coordinates: lat: 63.916666666667
lon: -111.03333333333
surface_form: mckay lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.45194
lon: -75.66997
McKay Lake (Ottawa). McKay Lake (formerly Hemlock Lake, McKay's Lake, or MacKay Lake) is a meromictic lake located in the former Village of Rockcliffe Park in Ottawa, Ontario, Canada. The lake is named for Thomas McKay, one of the founders of Ottawa, who once owned all of Rockcliffe Park in the 19th century, including the lake.

Geographic entities mentioned:
surface_form: mckay lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.45194
lon: -75.66997
The lake is named for Thomas McKay, one of the founders of Ottawa, who once owned all of Rockcliffe Park in the 19th century, including the lake. The lake was officially named McKay Lake in 1954 after Rockcliffe Park Village Council passed a by-law. Prior to that the lake often appeared on maps as &quot;Hemlock Lake&quot;, but locals referred to it as McKay Lake. The lake was once a swimming hole.

Geographic entities mentioned:
surface_form: mckay lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.45194
lon: -75.66997
Sometimes the last two footprints of Christ on the rock are seen; these were shown to pilgrims at what is now the Chapel of the Ascension on the Mount of Olives in Jerusalem. The scene may also include the Apostles, two men in white and the Virgin Mary.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
Arrival of Jesuit Missionaries. The first of the Jesuit missionaries arrived in the Bitterroot Valley on a wagon train in September 1841 under Father Peter John De Smet, a Belgian priest appointed over the missionary efforts in the Rocky Mountains. These missionaries first established relations with the neighboring tribes to the Coeur d’Alenes.

Geographic entities mentioned:
surface_form: Bitterroot Valley
instance_of: Valley
countries: United States
coordinates: lat: 46.247
lon: -114.16
A number of bursaries and scholarships also exist in the names of the brothers at Sussex University (Adam's &quot;alma mater&quot;) and at Ben Gurion University. The brothers are buried at Mount Herzl military cemetery. Weiler became a counselor after their deaths, supporting those that lost loved ones during the Holocaust and the wars in Israel.

Geographic entities mentioned:
surface_form: Mount Herzl
instance_of: Mountain
countries: Israel
coordinates: lat: 31.774117
lon: 35.180567
Location. The glacier forms in the south of the Herbert Mountains and flows north to enter the Slessor Glacier between the Högbom Outcrops to the east and the Charlesworth Cliffs to the west. The glacier flows along a fault line from near Mount Absalom, and divides the mountains into two, with the Bernhardi Heights ridge to the east falling steeply about to the glacier.

Geographic entities mentioned:
surface_form: Högbom Outcrops
instance_of: Mountain
coordinates: lat: -80.25
lon: -24.8667
Location. The glacier forms in the south of the Herbert Mountains and flows north to enter the Slessor Glacier between the Högbom Outcrops to the east and the Charlesworth Cliffs to the west. The glacier flows along a fault line from near Mount Absalom, and divides the mountains into two, with the Bernhardi Heights ridge to the east falling steeply about to the glacier.

Geographic entities mentioned:
surface_form: Mount Absalom
instance_of: Mountain
coordinates: lat: -80.4
lon: -25.4
surface_form: Bernhardi Heights
instance_of: Mountain
coordinates: lat: -80.3333
lon: -25
Biography. Hastorf received her Phd from UCLA in 1983. Hastorf has worked on the shores of Lake Titicaca, Bolivia since 1992. At Berkeley, Hastorf directs the Archaeological Research Facility as well as the McCown Archaeobotany Laboratory, and is the Curator of South American Archaeology at the Phoebe A. Hearst Museum of Anthropology.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
As a result of frequency reallocations resulting from the Federal Communications Commission's 1952 &quot;Sixth Report and Order&quot;, WNBK was moved to channel 3, swapping frequencies with fellow NBC affiliate WLWC (now WCMH-TV) in Columbus to alleviate same-channel interference with another NBC station, WWJ-TV (now WDIV-TV) across Lake Erie in Detroit.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Geography. According to the 2010 census, the township has a total area of, of which (or 99.86%) is land and (or 0.18%) is water. The streams of Bethel Creek, Black Brook, Clay Run, Land Drain, Middle Brook, Small Run, Vernon Brook and White Creek run through this township. The highest natural point in Indiana, Hoosier Hill, is located in this township. Cemeteries.

Geographic entities mentioned:
surface_form: Hoosier Hill
instance_of: Mountain
countries: United States
coordinates: lat: 40.0003
lon: -84.8514
Cluff Lake mine. Cluff Lake mine is decommissioned former uranium mine located in northern Saskatchewan, located 30 km east of the provincial border with Alberta and approximately 75 kilometres south of Lake Athabasca. The mine and mill were owned and operated by AREVA Resources Canada, formerly COGEMA Resources and is now owned and operated by Orano Canada.

Geographic entities mentioned:
surface_form: Lake Athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
Caswell Creek. Caswell Creek is a small river in the Hart Ranges of the Northern Rockies of British Columbia. The creek is named after Mr. Caswell, superintendent of the W.C. Arnett Construction Company, which constructed part of the John Hart Highway in 1954 (Hwy 97).

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: caswell creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 55.21658
lon: -122.75308
Caswell Creek. Caswell Creek is a small river in the Hart Ranges of the Northern Rockies of British Columbia. The creek is named after Mr. Caswell, superintendent of the W.C. Arnett Construction Company, which constructed part of the John Hart Highway in 1954 (Hwy 97).

Geographic entities mentioned:
surface_form: caswell creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 55.21658
lon: -122.75308
Geography and climate. Knik River is located at (61.470970, -148.86064) (Sec. 24, T016N, R003W, Seward Meridian), in the Palmer Recording District. The community is at the head of the Knik Arm of Cook Inlet in Southcentral Alaska, northeast of Anchorage. The community has developed along the south bank of the Knik River, which flows into Knik Arm, at the southern border of the Mat-Su Borough.

Geographic entities mentioned:
surface_form: Knik Arm
instance_of: Body of water
countries: United States
coordinates: lat: 61.2
lon: -150.217
Snowshoe Lava Field. The Snowshoe Lava Field (SLF) is a largely buried volcanic field at Mount Edziza in British Columbia, Canada. It reaches an elevation of and engulfs more than of the Big Raven Plateau and adjacent valleys with blocky lava flows.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Snowshoe Lava Field. The Snowshoe Lava Field (SLF) is a largely buried volcanic field at Mount Edziza in British Columbia, Canada. It reaches an elevation of and engulfs more than of the Big Raven Plateau and adjacent valleys with blocky lava flows.

Geographic entities mentioned:
surface_form: Big Raven Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
The Snowshoe Lava Field is the southernmost of two lava fields on the Big Raven Plateau, the other being the smaller Desolation Lava Field at the northern end of the plateau. It is in Mount Edziza Provincial Park and is part of the Mount Edziza volcanic complex, the latter of which consists of several other volcanic landforms such as shield volcanoes, stratovolcanoes, lava domes and cinder cones.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
It is in Mount Edziza Provincial Park and is part of the Mount Edziza volcanic complex, the latter of which consists of several other volcanic landforms such as shield volcanoes, stratovolcanoes, lava domes and cinder cones. Sezill Creek, Shaman Creek, Taweh Creek and several other unnamed streams in the Stikine River watershed drain the Snowshoe Lava Field.

Geographic entities mentioned:
surface_form: Sezill Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.69967
lon: -130.88724
surface_form: Shaman Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.61636
lon: -130.40395
surface_form: Taweh Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
Access to the lava field is only by aircraft or by a network of horse trails from surrounding roads. The Snowshoe Lava Field issued from several eruptive centres during the Holocene, most of which are clustered on the southern and western flanks of Ice Peak at elevations more than.

Geographic entities mentioned:
surface_form: Ice Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635