Sarmila/GeoWiki-Features huggingface dataset:
Wau an Namus is sometimes considered to be part of the field, other volcanic fields in Libya are Gharyan, Gabal as Sawada, Gabal Nuqay and Tibesti some of which belong to a long line known as the Tibesti lineament.

Geographic entities mentioned:
surface_form: Wau an Namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
However, anyone entering an Islamic mosque or a Hindu temple is expected to remove their footwear. Shoe racks are usually provided near the entrance. In Christianity, most churches and holy sites can be entered wearing shoes but there are some local exceptions, such as the barefoot night ascent of Croagh Patrick in Ireland. The practice sometimes extends to secular respect as well.

Geographic entities mentioned:
surface_form: Croagh Patrick
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.7595
lon: -9.6584
This is untaken as part of vows of poverty and humility, as well as a remembrance of Moses on Mount Sinai. Hindu gurus go barefoot to allow their followers to demonstrate their love and respect by pranam, the ceremonial touching of a bare foot. It is customary in Judaism and some Christian denominations to go barefoot while mourning.

Geographic entities mentioned:
surface_form: Mount Sinai
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
Fieldwork. In 2001 she was part of an Anglo-Lebanese mission of the Council for British Research in the Levant and the Museum of Lebanese Prehistory led by Alex Wasse and Lévon Nordigiuan to excavate at Nachcharini and survey in the Anti-Lebanon. In 2002 she carried out reconnaissance surveys in the Beqaa Valley, in collaboration with J.J. Ibañez of the University of Cantabria, Spain.

Geographic entities mentioned:
surface_form: Beqaa Valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
In September 2001 she spoke on &quot;Flint Workshops of the southern Beqaa Valley (Lebanon): Preliminary results from Qaraoun&quot; at a conference called &quot;Neolithic Revolution. New perspectives on southwest Asia in light of recent discoveries in Cyprus&quot;, organized by the Council for British Research in the Levant and the Department of Antiquities in Cyprus.

Geographic entities mentioned:
surface_form: Qaraoun
instance_of: Lake
countries: Lebanon
coordinates: lat: 33.5725
lon: 35.6975
Yates next competed at the Tour of California. After being passed on the road by Bradley Wiggins () on Stage 2, the individual time trial around Folsom, he finished fourth on Stage 3, which finished on Mount Diablo, and fourth on Stage 6, which finished on Mountain High. Yates finished fifth overall in the general classification, 2 minutes and 14 seconds behind the winner, Wiggins.

Geographic entities mentioned:
surface_form: Mount Diablo
instance_of: Mountain
countries: United States
coordinates: lat: 37.881697781
lon: -121.914154997
Yates was thought to have moved into the yellow jersey on stage 12, which finished at Mont Ventoux, following an incident with a motorcycle on the final climb which delayed Froome, Porte and Bauke Mollema; the race jury later decided to give those riders the same time as Mollema – who finished 19 seconds ahead of Yates, meaning Froome actually extended his lead.

Geographic entities mentioned:
surface_form: Mont Ventoux
instance_of: Mountain
countries: France
coordinates: lat: 44.166666666667
lon: 5.2833333333333
He concluded his season in October with a stage win, the general classification and the mountains classification at the CRO Race, and a third-place finish at Milano–Torino. Yates started his 2020 campaign at the UAE Tour, where he won the third stage – finishing at Jebel Hafeet – by more than a minute, to take the lead in the general classification.

Geographic entities mentioned:
surface_form: Jebel Hafeet
instance_of: Mountain
countries: United Arab Emirates
Oman
coordinates: lat: 24.05796
lon: 55.78086
2021. For the second consecutive year, he started his season with the UAE Tour, leading the team. Having made the lead group during the crosswinds on the opening stage, Yates finished second to Tadej Pogačar on the third stage after a sprint à deux on the summit finish at Jebel Hafeet. Yates maintained second overall for the remainder of the race, despite a crash on the final day.

Geographic entities mentioned:
surface_form: Jebel Hafeet
instance_of: Mountain
countries: United Arab Emirates
Oman
coordinates: lat: 24.05796
lon: 55.78086
2022. Just as was the case in 2021, Yates finished second to Tadej Pogačar at the UAE Tour, with a pair of second-place stage finishes (both to Pogačar) on uphill finishes at Jebel Jais and Jebel Hafeet. He finished fourth overall at Paris–Nice, but withdrew from his next two starts at the Tour of the Basque Country, and the Tour de Suisse (due to a positive test for COVID-19).

Geographic entities mentioned:
surface_form: Jebel Jais
instance_of: Mountain
countries: Oman
coordinates: lat: 25.9531
lon: 56.18441
surface_form: Jebel Hafeet
instance_of: Mountain
countries: United Arab Emirates
Oman
coordinates: lat: 24.05796
lon: 55.78086
He made his first start with the team (as team leader) at the UAE Tour, with two-time defending race winner Tadej Pogačar electing to ride in Spain instead. Yates won the final stage of the race, finishing at Jebel Hafeet; he moved up from tenth overall to a podium finish, exactly one minute behind race winner Remco Evenepoel.

Geographic entities mentioned:
surface_form: Jebel Hafeet
instance_of: Mountain
countries: United Arab Emirates
Oman
coordinates: lat: 24.05796
lon: 55.78086
He then studied law and graduated from the University of Virginia in 1852. His cousin Jacob Yost (Virginia congressman) (1853–1933) (grandson of his grandfather's daughter Mary Miller Yost, who was taking care of Samuel Liggett in 1850) became a U.S. Congressman from Staunton, Virginia, also in the Shenandoah Valley. Jacob N.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
It runs roughly parallel to the Northern Muya Range just north of it. The range stretches from southwest to northeast for about 350 km from the Churo River, a tributary of the upper course of the Upper Angara river, to lake Nichatka. The gorges of the Vitim River are located in the eastern section, dividing the upper course of the Vitim from its lower basin.

Geographic entities mentioned:
surface_form: Nichatka
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 57.761915
lon: 117.65708
The highest point of the range is a high peak located between the Upper Angara sources and the Mamakan uppermost reaches. A rare, exposed argillite outcrop is found in the range. Hydrography. River Upper Angara, flowing into Lake Baikal, originates in the slopes of the range. The Mamakan cuts across the range. Lake Oron is located south of the eastern section of the range. Flora.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
A rare, exposed argillite outcrop is found in the range. Hydrography. River Upper Angara, flowing into Lake Baikal, originates in the slopes of the range. The Mamakan cuts across the range. Lake Oron is located south of the eastern section of the range. Flora. The slopes of the range are mainly covered with mountain taiga, with pre-alpine woodland and mountain tundra at higher elevations.

Geographic entities mentioned:
surface_form: Lake Oron
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 57.1025
lon: 116.53138889
In a 2005 poll, &quot;Chicago Tribune&quot; readers voted it one of the &quot;seven wonders of Chicago&quot;, behind the lakefront and Wrigley Field, and ahead of Willis Tower (formerly the Sears Tower), the Water Tower, the University of Chicago, and the Museum of Science and Industry. Pre-CTA era.

Geographic entities mentioned:
surface_form: lakefront
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
On 5 March &quot;Yūdachi&quot; conducted joint training with in the Bay of Bengal, and on the following day, she met of the Republic of Singapore Navy in a goodwill training. From 14 to 16 March 2022, &quot;Yūdachi&quot; joined and HMAS &quot;Arunta&quot; in a joint training in the South China Sea, accompinaied by the US Navy's P-8 and the RAAF's AP-3C.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
According to, when Jesus entered a Samaritan village, he was not welcomed, because he was going on to Jerusalem. (There was enmity between the Jews and their temple in Jerusalem and Samaritans and their temple on Mount Gerizim). Jesus' disciples James and his brother John wanted to call down fire from heaven on the village but Jesus reprimanded them and they continued on to another village.

Geographic entities mentioned:
surface_form: Mount Gerizim
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.199444444444
lon: 35.272777777778
Meall Greigh. Meall Greigh is a mountain in the southern part of the Scottish Highlands. With Meall Garbh it forms the north-eastern end of the Ben Lawers range.

Geographic entities mentioned:
surface_form: Ben Lawers
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.544922
lon: -4.22086
surface_form: meall garbh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.566122
lon: -4.207714
surface_form: meall garbh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.637381
lon: -4.207472
Meall Greigh. Meall Greigh is a mountain in the southern part of the Scottish Highlands. With Meall Garbh it forms the north-eastern end of the Ben Lawers range.

Geographic entities mentioned:
surface_form: meall greigh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.567426
lon: -4.159559
Administratively it belongs to the Avannaata municipality. The glacier was named by Robert Peary after the Philadelphia Academy of Natural Sciences. Geography. The Academy Glacier is located inland and discharges from the Greenland Ice Sheet into the Leidy Glacier, which bifurcates and has its terminus in the Academy Fjord, as well as in the Olrik Fjord as the smaller Marie Glacier.

Geographic entities mentioned:
surface_form: Olrik Fjord
instance_of: Body of water
countries: Greenland
coordinates: lat: 77.2
lon: -67.58194
Smith also championed the preservation of Tse-whit-zen, a historic Lower Elwha village which is approximately 2,700 years old, rediscovered during a construction project on the waterfront in Port Angeles, and the restoration of the Elwha River. The removal of the Elwha dams, beginning in September 2011, drained Lake Aldwell reservoir, which had been created before she was born.

Geographic entities mentioned:
surface_form: Lake Aldwell
instance_of: Lake
countries: United States
coordinates: lat: 48.0944
lon: -123.557
She lived to see the removal of the dams, including the Elwha Dam, from the river beginning in September 2011, and the return of the first salmon to the river. The removal of one of the dams in 2012 drained Lake Aldwell, a man-made reservoir created in 1913, revealing the Klallam ceremonial creation site in July 2012. It had been submerged since the reservoir was filled.

Geographic entities mentioned:
surface_form: Lake Aldwell
instance_of: Lake
countries: United States
coordinates: lat: 48.0944
lon: -123.557
Lough Ea. Lough Ea () is a lake located east of the town of Glenties, near the R253 road, in County Donegal, Ireland. The lake is the source of the Owenea River which meets the Atlantic Ocean to the west.

Geographic entities mentioned:
surface_form: lough ea
instance_of: Lake
countries: Ireland
coordinates: lat: 54.805833333333
lon: -8.1319444444444
Maquan Pond. Maquan Pond is a pond in Hanson, Massachusetts. Its average depth is and its maximum depth is. The pond is spring fed with an overflow on the south end that feeds into Indian Head Pond. There has been much development along the shore. The town has a right-of-way on the northern shore of the pond off Maquan Street (Route 14). The town beach Cranberry Cove is at south end of the pond.

Geographic entities mentioned:
surface_form: indian head pond
instance_of: Lake
countries: United States
coordinates: lat: 42.05
lon: -70.85
surface_form: indian head
instance_of: Mountain
countries: United States
coordinates: lat: 44.097777777778
lon: -71.698888888889
Maquan Pond. Maquan Pond is a pond in Hanson, Massachusetts. Its average depth is and its maximum depth is. The pond is spring fed with an overflow on the south end that feeds into Indian Head Pond. There has been much development along the shore. The town has a right-of-way on the northern shore of the pond off Maquan Street (Route 14). The town beach Cranberry Cove is at south end of the pond.

Geographic entities mentioned:
surface_form: maquan pond
instance_of: Lake
countries: United States
coordinates: lat: 42.060555555556
lon: -70.851388888889
The water is acidic, so fishing is poor except for pickerel, small yellow perch and pumpkinseeds. Camp Kiwanee, a former Camp Fire camp, is located on the southeastern shore of the pond. The town now owns the camp and rents camping and cabins as well as Needles Lodge for functions. The Rainbow Girls own land on the southwest shore and previously operated a summer camp there.

Geographic entities mentioned:
surface_form: needles
instance_of: Mountain
countries: United States
coordinates: lat: 43.8369
lon: -103.549
Windermere Hills. The Windermere Hills are a mountain range in Elko County, Nevada, located northeast of Wells, Nevada. In 1967, when the name was approved, the Windermere Hills were described as being bounded by the Thousand Springs Creek to the north, the Southern Pacific line to the south, the Union Pacific line to the west and an unnamed valley to the east.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: windermere hills
instance_of: Landform
countries: United States
coordinates: lat: 41.2433
lon: -114.74
Windermere Hills. The Windermere Hills are a mountain range in Elko County, Nevada, located northeast of Wells, Nevada. In 1967, when the name was approved, the Windermere Hills were described as being bounded by the Thousand Springs Creek to the north, the Southern Pacific line to the south, the Union Pacific line to the west and an unnamed valley to the east.

Geographic entities mentioned:
surface_form: windermere hills
instance_of: Landform
countries: United States
coordinates: lat: 41.2433
lon: -114.74
Battle of Bergamo. The Battle of Bergomum was fought between Alans and the Western Roman Empire in 464, and resulted in a Roman victory. In 464, the Alan king Beorgor led an invasion of Northern Italy, marching his force into the Po Valley. At Bergomum, near Mediolanum, Beorgor was confronted by the Roman general Ricimer on 6 February 464.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
Torgau. Torgau () is a town on the banks of the Elbe in northwestern Saxony, Germany. It is the capital of the district Nordsachsen. Outside Germany, the town is best known as where on 25 April 1945, the United States and Soviet Armies first met near the end of World War II. History. The settlement goes back to a Slavonic settlement named Turguo in the shire of Neletici.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Sights. Sights include the historic town center, restored since German reunification, a brewery museum, the monument for the meeting of the Russian and American troops on the Elbe, and a Russian military cemetery. Carl Loebner Torgau is claimed to be the world's oldest toy store. The first documented mention of the shop in the history of Torgau goes back to the year 1685.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Geography. The mountain is part of a ridge in the Diablo Range that includes Mount Allison and Mission Peak and forms part of the border between Alameda County and Santa Clara County. The summit of Monument Peak lies just within the southern boundary of Mission Peak Regional Preserve in Alameda County and can be reached from the south via trails originating in Ed R.

Geographic entities mentioned:
surface_form: Mount Allison
instance_of: Mountain
countries: United States
coordinates: lat: 37.4989
lon: -121.871
surface_form: Mission Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.5124
lon: -121.881
Antenna. Built on July 1, 1988, an antenna on Monument Peak broadcasts channels 36 (KICU) and 54 (PBS, KQEH) until January 17, 2018. It is a free-standing structure above ground level. In the image above, the Monument Peak antenna is the tallest one seen (far right). The peak is the point directly right of the antenna. The antenna to the far left is on Mount Allison.

Geographic entities mentioned:
surface_form: Mount Allison
instance_of: Mountain
countries: United States
coordinates: lat: 37.4989
lon: -121.871
Monument Peak (Milpitas, California). Monument Peak is a mountain peak located southeast of Fremont and northeast of Milpitas in the East Bay region of the San Francisco Bay Area in California. Geography. The mountain is part of a ridge in the Diablo Range that includes Mount Allison and Mission Peak and forms part of the border between Alameda County and Santa Clara County.

Geographic entities mentioned:
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 34.2458397
lon: -117.3533795
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.045283
lon: -115.469742
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.793888888889
lon: -120.54305555556
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.4846
lon: -121.866
Monument Peak (Milpitas, California). Monument Peak is a mountain peak located southeast of Fremont and northeast of Milpitas in the East Bay region of the San Francisco Bay Area in California. Geography. The mountain is part of a ridge in the Diablo Range that includes Mount Allison and Mission Peak and forms part of the border between Alameda County and Santa Clara County.

Geographic entities mentioned:
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 34.2458397
lon: -117.3533795
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.045283
lon: -115.469742
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.793888888889
lon: -120.54305555556
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.4846
lon: -121.866
Geography. The mountain is part of a ridge in the Diablo Range that includes Mount Allison and Mission Peak and forms part of the border between Alameda County and Santa Clara County. The summit of Monument Peak lies just within the southern boundary of Mission Peak Regional Preserve in Alameda County and can be reached from the south via trails originating in Ed R.

Geographic entities mentioned:
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 34.2458397
lon: -117.3533795
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.045283
lon: -115.469742
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.793888888889
lon: -120.54305555556
surface_form: mission peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.5124
lon: -121.881
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.4846
lon: -121.866
Levin County Park or from the north via the Bay Area Ridge Trail. Antenna. Built on July 1, 1988, an antenna on Monument Peak broadcasts channels 36 (KICU) and 54 (PBS, KQEH) until January 17, 2018. It is a free-standing structure above ground level. In the image above, the Monument Peak antenna is the tallest one seen (far right). The peak is the point directly right of the antenna.

Geographic entities mentioned:
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 34.2458397
lon: -117.3533795
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.045283
lon: -115.469742
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.793888888889
lon: -120.54305555556
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.4846
lon: -121.866
Antenna. Built on July 1, 1988, an antenna on Monument Peak broadcasts channels 36 (KICU) and 54 (PBS, KQEH) until January 17, 2018. It is a free-standing structure above ground level. In the image above, the Monument Peak antenna is the tallest one seen (far right). The peak is the point directly right of the antenna. The antenna to the far left is on Mount Allison.

Geographic entities mentioned:
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 34.2458397
lon: -117.3533795
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.045283
lon: -115.469742
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.793888888889
lon: -120.54305555556
surface_form: monument peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.4846
lon: -121.866
Ural (river). The Ural, also known as the Yaik, is a river flowing through Russia and Kazakhstan in the continental border between Europe and Asia. It originates in the southern Ural Mountains and discharges into the Caspian Sea. At, it is the third-longest river in Europe after the Volga and the Danube, and the 18th-longest river in Asia.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
As the Frisii and Chauci had only primitive canoes, he sailed unhindered with his vastly superior forces into the mouth of the Weser (Visurgis) and forced both tribes into submission. The advance of Tiberius at the Elbe (Albis) in 5 AD was accomplished by means of a combined land and sea operation. His fleet sailed the river to the area of Lauenburg and met up with the land army.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
After the battles at the Weser River and Angrivarian Wall (located between the Weser and Steinhuder Meer) in which the Angrivarii, Bructeri and Cherusci tribes were defeated, a part of the army should have been returned to their garrisons. However, almost the entire fleet as well as everyone on board fell victim to a storm.

Geographic entities mentioned:
surface_form: Steinhuder Meer
instance_of: Lake
countries: Germany
coordinates: lat: 52.466666666667
lon: 9.3333333333333
Its nearest higher neighbor is Napeequa Peak, to the west, and Buck Mountain is to the east-southeast. Berge is positioned on Chiwawa Ridge with Buck and Napeequa, and other notable peaks on this ridge include Fortress Mountain, Brahma Peak, Cirque Mountain, Helmet Butte, and Chiwawa Mountain.

Geographic entities mentioned:
surface_form: Brahma Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.06777777777778
lon: -120.91333333333334
surface_form: Helmet Butte
instance_of: Mountain
countries: United States
coordinates: lat: 48.149166666667
lon: -120.95583333333
surface_form: Chiwawa Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.163333333333
lon: -120.90722222222
surface_form: cirque mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.003888888889
lon: -107.77166666667
surface_form: cirque mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.108491
lon: -120.972701
surface_form: fortress mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.336944444444
lon: -109.79805555556
surface_form: fortress mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.15916667
lon: -120.93388889
Precipitation runoff from Berge drains to the headwaters of Napeequa River; or east into tributaries of the Chiwawa River. This peak was named to remember Richard Waldo Berge (age 23), who died while climbing Baring Mountain on July 16, 1952. He was climbing with Fred Beckey at the time of the accident. Beckey's Cascade Alpine Guide credits Berge with several first ascents in the Cascades.

Geographic entities mentioned:
surface_form: Baring Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.779051
lon: -121.4361168
Subduction and tectonic activity in the area began during the late cretaceous period, about. Extensive volcanic activity began to take place in the oligocene, about 35 million years ago. Glacier Peak, a stratovolcano that is west of Mount Berge, began forming in the mid-Pleistocene. Due to Glacier Peak's proximity to Mount Berge, volcanic ash is common in the area. Climate.

Geographic entities mentioned:
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
surface_form: mount berge
instance_of: Mountain
countries: United States
coordinates: lat: 48.103246
lon: -120.946243
Mount Berge. Mount Berge is a double-summit granitic mountain located in the Glacier Peak Wilderness of the North Cascades, in Chelan County of Washington state. The mountain is situated along the crest of the Cascade Range, on land managed by the Okanogan–Wenatchee National Forest. Its nearest higher neighbor is Napeequa Peak, to the west, and Buck Mountain is to the east-southeast.

Geographic entities mentioned:
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6081079
lon: -90.3926199
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.66388889
lon: -90.52972222
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.889722222222
lon: -74.404166666667
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.461944444444
lon: -105.43833333333
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6894
lon: -110.819
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9509
lon: -76.2074
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6047712
lon: -90.7190122
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.052777777778
lon: -74.532777777778
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.193333333333
lon: -78.563611111111
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.093611111111116
lon: -120.91222222222223
Mount Berge. Mount Berge is a double-summit granitic mountain located in the Glacier Peak Wilderness of the North Cascades, in Chelan County of Washington state. The mountain is situated along the crest of the Cascade Range, on land managed by the Okanogan–Wenatchee National Forest. Its nearest higher neighbor is Napeequa Peak, to the west, and Buck Mountain is to the east-southeast.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: mount berge
instance_of: Mountain
countries: United States
coordinates: lat: 48.103246
lon: -120.946243
Extensive volcanic activity began to take place in the oligocene, about 35 million years ago. Glacier Peak, a stratovolcano that is west of Mount Berge, began forming in the mid-Pleistocene. Due to Glacier Peak's proximity to Mount Berge, volcanic ash is common in the area. Climate. Most weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains.

Geographic entities mentioned:
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
surface_form: mount berge
instance_of: Mountain
countries: United States
coordinates: lat: 48.103246
lon: -120.946243
Mount Berge. Mount Berge is a double-summit granitic mountain located in the Glacier Peak Wilderness of the North Cascades, in Chelan County of Washington state. The mountain is situated along the crest of the Cascade Range, on land managed by the Okanogan–Wenatchee National Forest. Its nearest higher neighbor is Napeequa Peak, to the west, and Buck Mountain is to the east-southeast.

Geographic entities mentioned:
surface_form: mount berge
instance_of: Mountain
countries: United States
coordinates: lat: 48.103246
lon: -120.946243
Laugar developed around thermal springs, hence its name, which in Icelandic means &quot;hot springs&quot;. Laugar is located on the Diamond Circle tourist route. In its vicinity there are famous tourist attractions: Goðafoss waterfall (approx. to the west) and lake Mývatn (approx. to the southeast). However, to the north of the village, there is lake Vestmannsvatn.

Geographic entities mentioned:
surface_form: Mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
Further south is the heathland of the Fläming. The Havel river separates the Teltow from the Nauen Plateau to the northwest. The Nuthe-Nieplitz Lowland, an &quot;urstromtal&quot; feature, separates it from the sander plateau of the Zauche in the southwest and the Berlin Urstromtal forms the boundary with the Barnim Plateau in the northeast.

Geographic entities mentioned:
surface_form: Barnim Plateau
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
surface_form: barnim plateau
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
The Nuthe-Nieplitz Lowland, an &quot;urstromtal&quot; feature, separates it from the sander plateau of the Zauche in the southwest and the Berlin Urstromtal forms the boundary with the Barnim Plateau in the northeast. It is, however, disputed whether the Müggelberge hills, which are up to above sea level (NN), in southeast Berlin are part of the Teltow.

Geographic entities mentioned:
surface_form: Müggelberge
instance_of: Mountain
countries: Germany
coordinates: lat: 52.416111111111
lon: 13.633333333333
surface_form: müggelberge
instance_of: Mountain
countries: Germany
coordinates: lat: 52.416111111111
lon: 13.633333333333
surface_form: teltow
instance_of: Plateau
countries: Germany
coordinates: lat: 52.3667
lon: 13.3333
These deposits formed between the Elster and Saalian ice advances, when the Elbe flowed northwards from the location of present-day Torgau and crossed the area of the Fläming which did not yet exist. These sediments are of great economic importance, both as groundwater conduits and for the building materials industry. But they only outcrop at a small sand pit at Lindenberg near Jühnsdorf.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The present-day term is defined by an ice age plateau that consists mainly of ground moraine elements. Its natural northern border is defined by the range of the Tempelhofer Berge, among them the Kreuzberg rising to, along the southern bank of the Spree. To the east the borders are formed by the rivers Dahme, as well by the Havel and Nuthe to the west.

Geographic entities mentioned:
surface_form: kreuzberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.3701
lon: 9.9801
These sediments are of great economic importance, both as groundwater conduits and for the building materials industry. But they only outcrop at a small sand pit at Lindenberg near Jühnsdorf. The old Elbe strata are overlain by the very thick (40 metres or more) sediments of the Saale ice age. These are usually the depositions of proglacial lakes or glacial till.

Geographic entities mentioned:
surface_form: lindenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.2983
lon: 9.315
From a geological standpoint they certainly are, because the hills have a similar development history. However, these upland remnants are completely isolated within the Berlin Urstromtal. If the River Dahme is taken as the eastern boundary of the Teltow the Müggelberge are neither part of the Teltow geologically nor from a cultural landscape perspective. Bedrock.

Geographic entities mentioned:
surface_form: müggelberge
instance_of: Mountain
countries: Germany
coordinates: lat: 52.416111111111
lon: 13.633333333333
surface_form: teltow
instance_of: Plateau
countries: Germany
coordinates: lat: 52.3667
lon: 13.3333
surface_form: teltow
instance_of: Plateau
countries: Germany
coordinates: lat: 52.3667
lon: 13.3333
Teltow (region). 3tbtwveuhdjdj0spm2pzch6spg1rfd" xml:space="preserve">Teltow () is both a geological plateau and also a historical region in the German states of Brandenburg and Berlin. As an historical region, the Teltow was one of the eight territories out of which the March of Brandenburg was formed in the 12th and 13th centuries.

Geographic entities mentioned:
surface_form: teltow (region)
instance_of: Plateau
countries: Germany
coordinates: lat: 52.3667
lon: 13.3333
Teltow (region). 3tbtwveuhdjdj0spm2pzch6spg1rfd" xml:space="preserve">Teltow () is both a geological plateau and also a historical region in the German states of Brandenburg and Berlin. As an historical region, the Teltow was one of the eight territories out of which the March of Brandenburg was formed in the 12th and 13th centuries.

Geographic entities mentioned:
surface_form: teltow
instance_of: Plateau
countries: Germany
coordinates: lat: 52.3667
lon: 13.3333
As a result of the (1239–1245) the question of territorial lordship of the newly created heart of the expanding march was finally decided here. Between 1835 and 1952 there was also a county,; in addition a town immediately south of Berlin, in the present-day county of Potsdam-Mittelmark, bears the name Teltow. Boundary.

Geographic entities mentioned:
surface_form: teltow
instance_of: Plateau
countries: Germany
coordinates: lat: 52.3667
lon: 13.3333
Between 1835 and 1952 there was also a county,; in addition a town immediately south of Berlin, in the present-day county of Potsdam-Mittelmark, bears the name Teltow. Boundary. The Teltow is not a unified region, either from a historical or a landscape perspective. The present-day term is defined by an ice age plateau that consists mainly of ground moraine elements.

Geographic entities mentioned:
surface_form: teltow
instance_of: Plateau
countries: Germany
coordinates: lat: 52.3667
lon: 13.3333
To the east the borders are formed by the rivers Dahme, as well by the Havel and Nuthe to the west. To the southwest, the countryside around the Pfefferfließ is also counted as part of the Teltow, although it has no clear boundaries. The regional border in the south is unclear, because the ground moraines here were often eroded by &quot;urstromtal&quot; processes.

Geographic entities mentioned:
surface_form: teltow
instance_of: Plateau
countries: Germany
coordinates: lat: 52.3667
lon: 13.3333
Further south is the heathland of the Fläming. The Havel river separates the Teltow from the Nauen Plateau to the northwest. The Nuthe-Nieplitz Lowland, an &quot;urstromtal&quot; feature, separates it from the sander plateau of the Zauche in the southwest and the Berlin Urstromtal forms the boundary with the Barnim Plateau in the northeast.

Geographic entities mentioned:
surface_form: teltow
instance_of: Plateau
countries: Germany
coordinates: lat: 52.3667
lon: 13.3333
The geothermal gradient was found to be about 3 K/100 metres; this was also a first. Sperenberg gypsum was mined from the Middle Ages to 1957 in several quarries. Other salt domes, which do not quite reach the surface, occur under Mittenwalde and the Blankensee lake. For the geological structure of the Teltow, they are of secondary significance, however. Saale glaciation.

Geographic entities mentioned:
surface_form: teltow
instance_of: Plateau
countries: Germany
coordinates: lat: 52.3667
lon: 13.3333
For the geological structure of the Teltow, they are of secondary significance, however. Saale glaciation. While the deeply buried sediments of the Elster Ice Age have virtually no impact on the current appearance of the Teltow, the subsurface, sandy, gravelly sediments of the so-called Berlin Elbe course occur over a wide area.

Geographic entities mentioned:
surface_form: teltow
instance_of: Plateau
countries: Germany
coordinates: lat: 52.3667
lon: 13.3333
Weichsel glaciation and post-glacial development. Today's Teltow plateau in Brandenburg-Berlin was formed around 20,000 years ago during the Brandenburg stage of Weichsel glaciation. The Weichsel ice sheet pushed southwards right over the Teltow before reaching the northern edge of the Baruth Urstromtal, the limit of its expansion to the south.

Geographic entities mentioned:
surface_form: teltow
instance_of: Plateau
countries: Germany
coordinates: lat: 52.3667
lon: 13.3333
Terminal moraines can be found there, for example, around Dobbrikow in Luckenwalde (Weinberg) and near Sperenberg. However, the line of terminal moraines is very patchy and is traces out an ice front. To the north are ground moraines that have been deposited over a large area. Only south of Ludwigsfelde, does the contiguous ground moraine plateau of the Teltow begin.

Geographic entities mentioned:
surface_form: teltow
instance_of: Plateau
countries: Germany
coordinates: lat: 52.3667
lon: 13.3333
Eastern Rukum District. Eastern Rukum () is a mountain district of Lumbini Province of Nepal situated along the Dhaulagiri mountain range. It is also the only mountain district of the province with its tallest mountain Putha Hiunchuli (Dhaulagiri VII) situated in the west end of Dhaulagiri II mountain chain, at an elevation of 7,246 meters.

Geographic entities mentioned:
surface_form: Dhaulagiri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.696666666666665
lon: 83.49
Eastern Rukum District. Eastern Rukum () is a mountain district of Lumbini Province of Nepal situated along the Dhaulagiri mountain range. It is also the only mountain district of the province with its tallest mountain Putha Hiunchuli (Dhaulagiri VII) situated in the west end of Dhaulagiri II mountain chain, at an elevation of 7,246 meters.

Geographic entities mentioned:
surface_form: Putha Hiunchuli
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.7475
lon: 83.14583333
surface_form: Dhaulagiri II
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.76333333
lon: 83.38833333
The drainage source of ancient Airavati river, one of the five sacred rivers of Buddhism, lies in the lesser Himalayas of the district. With a Dhaulagiri mountain range, lakes, Magar culture and its political history, Eastern Rukum has been among the top travel destinations of Nepal as designated by the Government of Nepal. The district is known for having 52 ponds and 53 hills.

Geographic entities mentioned:
surface_form: Dhaulagiri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.696666666666665
lon: 83.49
Guerilla trekking route has also been developed in the district as an adventure tourism following the past trails of the rebels in the base of Himalayas providing experiences of scenic landscapes, Dhaulagiri mountain ranges and rich Kham Magar culture.

Geographic entities mentioned:
surface_form: Dhaulagiri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.696666666666665
lon: 83.49
The reserve extends along the Dhaulagiri Himalayan Range of eastern Rukum, Myagdi and Baglung and covers 1325 square kilometers. Putha, Churen and Gurja Himal extend over the northern boundary of the reserve. Eastern Rukum itself occupies over sixty percentage territory of the reserve. Dhaulagiri Mountains.

Geographic entities mentioned:
surface_form: Gurja Himal
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.67435
lon: 83.275813
All along the Dhaulagiri range, the prominent mountains in the district are Mt. Putha Hiunchuli (Dhaulagiri VII) and Mount Sisne. Mount Putha is also the tallest mountain of Lumbini Province situated in the west end of Dhaulagiri II mountain chain, at an elevation of 7,246 meters. It was first climbed in 1954 by J. O. M.

Geographic entities mentioned:
surface_form: Dhaulagiri II
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.76333333
lon: 83.38833333
Water System. Most of the district is drained by west-flowing tributaries such as Uttar Ganga draining Dhorpatan Valley and to the north of that the Sani Bheri draining southern slopes of the western Dhaulagiri Himalaya. West Rapti river has its source in Eastern Rukum in the Mahabharata range of the lesser himalayas.

Geographic entities mentioned:
surface_form: Dhaulagiri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.696666666666665
lon: 83.49
Tourism. In recent years, Eastern Rukum has become a tourist destination of the country, also reflected in the Government of Nepal's official designation. The trekking agencies usually provide trekking routes with a focus on Dhaulagiri mountain range and Magar villages of Eastern Rukum. Guerilla Trek.

Geographic entities mentioned:
surface_form: Dhaulagiri
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.696666666666665
lon: 83.49
To the east it extends out New Hampshire Route 104 beyond Hall Road, and to the north it includes all of Brookwood Park Road, Keezer Road, Wind Ridge Road, Redbone Drive, and Blue Tick Drive. New Hampshire Route 3A passes through the center of town, leading north past Newfound Lake to New Hampshire Route 25 in West Plymouth, while to the south it leads to Franklin.

Geographic entities mentioned:
surface_form: Newfound Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.662778
lon: -71.775278
Upstream of this point, the creek's elevation decreases at a rate of per mile. Downstream of that point, its elevation decreases at a rate of per mile. Harveys Creek is in the Wyoming Valley. Much of Harveys Creek, in its lower reaches, is in a forested gorge. The upper reaches of its watershed contain swamps and glacial lakes.

Geographic entities mentioned:
surface_form: Wyoming Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
In Heidelberg, Uhlig joined the German student fraternity Leonensia. From 1900 to 1906 he worked as a meteorologist and geographer for the government of German East Africa, during which time, he carried out investigations of Kilimanjaro and Mount Meru (1901) as well as scientific studies of Lake Victoria (1904).

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
The conquerors demanded and more often forcibly wrested both land owned by Hindus and Hindu women. Enslavement of women invariably led to their conversion to Islam. In battles waged by Muslims against Hindus in Malwa and Deccan plateau, a large number of captives were taken. Muslim soldiers were permitted to retain and enslave POWs as plunder.

Geographic entities mentioned:
surface_form: Deccan plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Other European tribes. Various tribes of Europe are recorded by Roman sources as owning slaves. Strabo records slaves as an export commodity from Britannia, From Llyn Cerrig Bach in Anglesey, an iron gang chain dated to 100 BCE-50 CE was found, over 3 metres long with neck-rings for five captives. Post-classical history.

Geographic entities mentioned:
surface_form: Llyn Cerrig Bach
instance_of: Lake
countries: United Kingdom
coordinates: lat: 53.25885
lon: -4.5402888888889
This species has a maximum published total length of. Distribution and habitat. The stripedfin ronquil is found in the eastern North Pacific Ocean where it is distributed from Santo Tomás, Baja California north to Point Conception in California. This is a solitary, demersal fish found in exposed rocky areas in shalloiw coastal waters down to depths of. Biology.

Geographic entities mentioned:
surface_form: Point Conception
instance_of: Landform
countries: United States
coordinates: lat: 34.448113
lon: -120.471439
Sokumvatnet. or is a lake that lies in Gildeskål Municipality in Nordland county, Norway. Sokumvatnet is located about southeast of the village of Inndyr. It lies just south of the lake Litle Sokumvatnet and northeast of the lake Langvatnet. The lake serves as a reservoir for the Sundsfjord Hydroelectric Power Station.

Geographic entities mentioned:
surface_form: Litle Sokumvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 66.958333333333
lon: 14.285
surface_form: langvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 66.36861111
lon: 14.0825
surface_form: sokumvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 66.923611111111
lon: 14.211111111111
Sokumvatnet. or is a lake that lies in Gildeskål Municipality in Nordland county, Norway. Sokumvatnet is located about southeast of the village of Inndyr. It lies just south of the lake Litle Sokumvatnet and northeast of the lake Langvatnet. The lake serves as a reservoir for the Sundsfjord Hydroelectric Power Station.

Geographic entities mentioned:
surface_form: sokumvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 66.923611111111
lon: 14.211111111111
Although the glacier is not situated within Planet Heights, its name derives from the nearby mountain range (Planet Heights) along with many other glaciers named after planets of the Solar System. The nunataks at the head of the glacier are also named after solar system features, for example the Enceladus Nunataks named for a moon of Saturn.

Geographic entities mentioned:
surface_form: Enceladus Nunataks
instance_of: Mountain
coordinates: lat: -71.716666666667
lon: -69.45
There are 500- to 600-metre-high (1,600–2,000 ft) mountain peaks that tower above the plateau. The highest peak on the plateau is the mountain knot of Tavan-Bogdo-Ula (Five Sacred Peaks) where the highest mountain is Khüiten Peak that reaches above sea level. This is the second highest peak in Siberia after Belukha Mountain.

Geographic entities mentioned:
surface_form: Tavan-Bogdo-Ula
instance_of: Mountain
countries: Mongolia
People's Republic of China
Russia
Russian Empire
Soviet Union
coordinates: lat: 49.145833333333
lon: 87.819166666667
surface_form: Khüiten Peak
instance_of: Mountain
countries: Mongolia
People's Republic of China
coordinates: lat: 49.145833333333
lon: 87.819166666667