Sarmila/GeoWiki-Features huggingface dataset:
Lake Preston (South Dakota). Lake Preston is a lake located adjacent to and northeast of the city of Lake Preston, South Dakota. The lake is near and directly north of Lake Whitewood. The lake has the name of William C. Preston, a United States Senator from South Carolina.

Geographic entities mentioned:
surface_form: lake preston
instance_of: Lake
countries: United States
coordinates: lat: 44.380277777778
lon: -97.324722222222
surface_form: lake preston
instance_of: Lake
countries: United States
coordinates: lat: 44.380277777778
lon: -97.324722222222
With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. Glacier Peak, a stratovolcano that is southwest of North Star Mountain, began forming in the mid-Pleistocene.In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago.

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: star mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.061666666667
lon: -106.53333333333
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
surface_form: north star mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3775
lon: -106.09833333333
surface_form: north star mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.222222222222
lon: -120.90111111111
North Star Mountain. North Star Mountain is an mountain summit located in the Glacier Peak Wilderness of the North Cascades, in Chelan County of Washington state. Its nearest neighbor is Cloudy Peak to the southwest, and the nearest higher neighbor is Bonanza Peak, to the northeast.

Geographic entities mentioned:
surface_form: bonanza peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.2378
lon: -120.866
surface_form: bonanza peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.5205763
lon: -142.8350518
surface_form: cloudy peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.211666666667
lon: -120.91194444444
Its nearest neighbor is Cloudy Peak to the southwest, and the nearest higher neighbor is Bonanza Peak, to the northeast. North Star Mountain was originally named Bonanza Peak, and vice versa, but the USGS’ first 1904 topographic map of the region mistakenly interchanged the names. Precipitation runoff from North Star drains into Agnes Creek and Railroad Creek, both tributaries of the Chelan River.

Geographic entities mentioned:
surface_form: bonanza peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.2378
lon: -120.866
surface_form: star mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.061666666667
lon: -106.53333333333
surface_form: bonanza peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.5205763
lon: -142.8350518
surface_form: north star mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3775
lon: -106.09833333333
surface_form: north star mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.222222222222
lon: -120.90111111111
North Star Mountain. North Star Mountain is an mountain summit located in the Glacier Peak Wilderness of the North Cascades, in Chelan County of Washington state. Its nearest neighbor is Cloudy Peak to the southwest, and the nearest higher neighbor is Bonanza Peak, to the northeast.

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: star mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.061666666667
lon: -106.53333333333
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: north star mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3775
lon: -106.09833333333
surface_form: north star mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.222222222222
lon: -120.90111111111
North Star Mountain. North Star Mountain is an mountain summit located in the Glacier Peak Wilderness of the North Cascades, in Chelan County of Washington state. Its nearest neighbor is Cloudy Peak to the southwest, and the nearest higher neighbor is Bonanza Peak, to the northeast.

Geographic entities mentioned:
surface_form: star mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.061666666667
lon: -106.53333333333
surface_form: north star mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3775
lon: -106.09833333333
surface_form: north star mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.222222222222
lon: -120.90111111111
Precipitation runoff from North Star drains into Agnes Creek and Railroad Creek, both tributaries of the Chelan River. Geology. North Star Mountain is located in the Cloudy Pass batholith, an intrusive formation that was formed approximately, during the early Miocene. The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch.

Geographic entities mentioned:
surface_form: star mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.061666666667
lon: -106.53333333333
surface_form: north star mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3775
lon: -106.09833333333
surface_form: north star mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.222222222222
lon: -120.90111111111
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. Climate. North Star Mountain is located in the marine west coast climate zone of western North America. Weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains.

Geographic entities mentioned:
surface_form: star mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.061666666667
lon: -106.53333333333
surface_form: north star mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3775
lon: -106.09833333333
surface_form: north star mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.222222222222
lon: -120.90111111111
North Star Mountain was originally named Bonanza Peak, and vice versa, but the USGS’ first 1904 topographic map of the region mistakenly interchanged the names. Precipitation runoff from North Star drains into Agnes Creek and Railroad Creek, both tributaries of the Chelan River. Geology.

Geographic entities mentioned:
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
Kuntur Sinqa (Junín). Kuntur Sinqa (Quechua &quot;kuntur&quot; condor, &quot;sinqa&quot; nose, &quot;condor nose&quot;, also spelled &quot;Cóndorsencca&quot;) is a mountain in the Andes of Peru which reaches a height of approximately. It lies in the Junín Region, Tarma Province, Tarma District.

Geographic entities mentioned:
surface_form: junín
instance_of: Lake
countries: Peru
coordinates: lat: -11.0201
lon: -76.1075
surface_form: kuntur sinqa
instance_of: Mountain
countries: Peru
coordinates: lat: -13.5533
lon: -71.2772
surface_form: sinqa
instance_of: Mountain
countries: Peru
coordinates: lat: -13.4572
lon: -72.0056
surface_form: kuntur
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4156
lon: -72.0636
surface_form: kuntur sinqa
instance_of: Mountain
countries: Peru
coordinates: lat: -11.64361111
lon: -75.69361111
surface_form: kuntur sinqa
instance_of: Mountain
countries: Peru
coordinates: lat: -9.81472
lon: -77.3153
surface_form: kuntur sinqa
instance_of: Mountain
countries: Peru
coordinates: lat: -12.8142
lon: -74.2764
surface_form: kuntur sinqa (junín)
instance_of: Mountain
countries: Peru
coordinates: lat: -11.44888889
lon: -75.82833333
Kuntur Sinqa (Junín). Kuntur Sinqa (Quechua &quot;kuntur&quot; condor, &quot;sinqa&quot; nose, &quot;condor nose&quot;, also spelled &quot;Cóndorsencca&quot;) is a mountain in the Andes of Peru which reaches a height of approximately. It lies in the Junín Region, Tarma Province, Tarma District.

Geographic entities mentioned:
surface_form: kuntur sinqa
instance_of: Mountain
countries: Peru
coordinates: lat: -13.5533
lon: -71.2772
surface_form: sinqa
instance_of: Mountain
countries: Peru
coordinates: lat: -13.4572
lon: -72.0056
surface_form: sinqa
instance_of: Mountain
countries: Peru
coordinates: lat: -13.4572
lon: -72.0056
surface_form: condor
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4156
lon: -72.0636
surface_form: condor
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4156
lon: -72.0636
surface_form: kuntur
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4156
lon: -72.0636
surface_form: kuntur
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4156
lon: -72.0636
surface_form: kuntur sinqa
instance_of: Mountain
countries: Peru
coordinates: lat: -11.64361111
lon: -75.69361111
surface_form: kuntur sinqa
instance_of: Mountain
countries: Peru
coordinates: lat: -9.81472
lon: -77.3153
surface_form: kuntur sinqa
instance_of: Mountain
countries: Peru
coordinates: lat: -12.8142
lon: -74.2764
surface_form: kuntur sinqa
instance_of: Mountain
countries: Peru
coordinates: lat: -11.44888889
lon: -75.82833333
Perseus' daughter was set to marry Prusias II of Bithynia (in north-western Anatolia, modern Turkey), who was an enemy of Eumenes II of Pergamon (in western Anatolia), an ally of Rome. Amid these alliances, Abrupolis, the king of the Thracian tribe of the Sapaei and an ally of the Romans attacked Macedon, laid it waste as far as Amphipolis, and overran the gold mines of Mount Pangaeus.

Geographic entities mentioned:
surface_form: Mount Pangaeus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.899166666666666
lon: 24.08361111111111
Five Aetolian officers were sent to Rome. The Thessalians were commended for their bravery. Perseus moved his camp to Mopselus, a hill at the entrance of the Vale of Tempe that commanded the plain of Larissa. Meanwhile, Misagenes (the son of Masinissa, king of Numidia) brought 1,000 Numidian cavalry, the same number of infantry and 22 elephants for the Romans.

Geographic entities mentioned:
surface_form: Vale of Tempe
instance_of: Valley
countries: Greece
coordinates: lat: 39.872778
lon: 22.546667
The consul started marching towards Macedon. Perseus sent troops to the mountain passes into Macedon. Quintus Marcius carried out a heroic march into Macedon through the Olympus mountains. He sent 4,000 light infantry ahead to secure the road to a pass near Octolophus, but the road was so difficult and steep that they advanced only fifteen miles and seven miles the following day.

Geographic entities mentioned:
surface_form: Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
It was also hard to pass unnoticed as the enemy was posted on the heights. The only option was the area between the bottom of Mount Olympus and the sea, but that was only one mile wide, half of which was the bog of the mouth of the River Baphirus and a large part of the remaining plain was taken up by the town.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
There were many places proposed, such as the forest areas of the Doi Saket District. Eventually, an area at the foot of Doi Suthep which is located in the sub-district of Mae Hia, Chiang Mai was chosen. The Prime Minister received approval No.90/2545 on 25 March 2002 and started a Chiang Mai Night Zoo Establishment Study Committee and Related Activities for Tourism Promotion.

Geographic entities mentioned:
surface_form: Doi Suthep
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.816388888889
lon: 98.893055555556
In 2013, Montagne de Bueren was ranked as no. 1 on &quot;The Huffington Posts list of Most Extreme Staircases. In July 2020, in response to the impact of the COVID-19 pandemic in Belgium, Belgian explorer and adventurer Louis-Philippe Loncke ascended and descended the staircase 135 times carrying a backpack, simulating an ascent of Mount Everest.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
The summit is set in Hoover Wilderness on land managed by Humboldt–Toiyabe National Forest. The peak is situated approximately four miles west of Twin Lakes, 1.3 mile southwest of Victoria Peak, and 2.4 miles southwest of line parent Eagle Peak. Precipitation runoff from this mountain drains into tributaries of Robinson and Buckeye Creeks, which are within the Walker River drainage basin.

Geographic entities mentioned:
surface_form: eagle peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.6769
lon: -108.577
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 27.893888888889
lon: -81.594722222222
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 43.4834018
lon: -74.9490486
surface_form: eagle peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.746
lon: -119.615
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 37.6181
lon: -119.008
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 44.8079
lon: -118.0867
surface_form: eagle peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.3207
lon: -110.0276
surface_form: eagle peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.2834
lon: -120.201
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 40.7433
lon: -115.283
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.0183
lon: -73.3867
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 45.23888889
lon: -111.86472222
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 60.638888888889
lon: -153.86305555556
surface_form: eagle peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.1669
lon: -149.267
surface_form: eagle peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.755702
lon: -121.7792
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 48.6494
lon: -113.718
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 45.7487796
lon: -84.4527626
surface_form: twin lakes
instance_of: Lake
countries: United States
surface_form: eagle peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.17992
lon: -119.4085
surface_form: eagle peak
instance_of: Mountain
countries: United States
coordinates: lat: 34.778611111111
lon: -114.75555555556
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 44.6375
lon: -89.41583333333334
Hunewill Peak. Hunewill Peak is a mountain with a summit elevation of located in the Sierra Nevada mountain range, in Mono County of northern California, United States. The summit is set in Hoover Wilderness on land managed by Humboldt–Toiyabe National Forest.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: hunewill peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.15881
lon: -119.44322
Hunewill Peak. Hunewill Peak is a mountain with a summit elevation of located in the Sierra Nevada mountain range, in Mono County of northern California, United States. The summit is set in Hoover Wilderness on land managed by Humboldt–Toiyabe National Forest.

Geographic entities mentioned:
surface_form: hunewill peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.15881
lon: -119.44322
Precipitation runoff from this mountain drains into tributaries of Robinson and Buckeye Creeks, which are within the Walker River drainage basin. Topographic relief is significant as the summit rises over above Robinson Creek in approximately. History. Hunewill Peak is the toponym officially adopted in 1962 by the U.S. Board on Geographic Names to remember Napoleon Bonaparte &quot;N.

Geographic entities mentioned:
surface_form: hunewill peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.15881
lon: -119.44322
Watty. Climate. According to the Köppen climate classification system, Hunewill Peak is located in an alpine climate zone. Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains. As fronts approach, they are forced upward by the peaks (orographic lift), causing moisture in the form of rain or snowfall to drop onto the range.

Geographic entities mentioned:
surface_form: hunewill peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.15881
lon: -119.44322
Geography. Bennhausen has an area of 1.49 km². It is situated in the North Palatine Uplands, at the foot of the Donnersberg, which lies about 3 km west of the village. The land to the west and north of the hilly landscape is mainly planted with orchards, and the forest almost reaches the outskirts of the village. The land to the south and east consists mainly of agricultural farmland.

Geographic entities mentioned:
surface_form: Donnersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.625280555556
lon: 7.9147194444444
He begins with the Northern Promontory (see above), and working north to south names the river &quot;Rhawiu&quot; (possibly the Erne); the town &quot;Magnata&quot; (a settlement of the &quot;Magnatai&quot; people, possibly somewhere in County Sligo); the mouth of the rivers &quot;Libniu&quot; (possibly Clew Bay), &quot;Ausoba&quot; (perhaps Galway Bay) &quot;Senu&quot; (probably the Shannon, although placed too far to the north), &quot;Dur&quot; (possibly Dingle Bay) and &quot;Iernu&quot; (possibly the Kenmare), and the Southern Promontory (any one of Slea Head, Bray Head, Dursey Head and Mizen Head).

Geographic entities mentioned:
surface_form: Bray Head
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.190527777778
lon: -6.0841666666667
Census Bureau, the township has a total area of, of which, or 0.20%, are water. The eastern part of the township is drained by the Pine River, a tributary of the Chippewa River flowing east toward Lake Huron, while the western side is drained by Fish Creek, a south-flowing tributary of the Maple River, part of the Grand River watershed flowing west toward Lake Michigan. Demographics.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Wiedersberger Horn. The Wiedersberger Horn is a mountain in the Alpbachtal valley in Austria. Its summit is. The Wiedersberger Horn is accessible from the Alpbachtal via cableways and the mountainsides are used as a skiing area. In winter it may be climbed without difficulty in safe snow conditions.

Geographic entities mentioned:
surface_form: Alpbachtal
instance_of: Valley
countries: Austria
coordinates: lat: 47.386111111111
lon: 11.952777777778
surface_form: wiedersberger horn
instance_of: Mountain
countries: Austria
coordinates: lat: 47.360833
lon: 11.9225
Wiedersberger Horn. The Wiedersberger Horn is a mountain in the Alpbachtal valley in Austria. Its summit is. The Wiedersberger Horn is accessible from the Alpbachtal via cableways and the mountainsides are used as a skiing area. In winter it may be climbed without difficulty in safe snow conditions.

Geographic entities mentioned:
surface_form: alpbachtal
instance_of: Valley
countries: Austria
coordinates: lat: 47.386111111111
lon: 11.952777777778
surface_form: wiedersberger horn
instance_of: Mountain
countries: Austria
coordinates: lat: 47.360833
lon: 11.9225
Wiedersberger Horn. The Wiedersberger Horn is a mountain in the Alpbachtal valley in Austria. Its summit is. The Wiedersberger Horn is accessible from the Alpbachtal via cableways and the mountainsides are used as a skiing area. In winter it may be climbed without difficulty in safe snow conditions.

Geographic entities mentioned:
surface_form: wiedersberger horn
instance_of: Mountain
countries: Austria
coordinates: lat: 47.360833
lon: 11.9225
The planet is probably somewhat less massive than Jupiter, although only its minimum mass is known. Its orbital distance is 1.67 AU, slightly further than Mars, and its eccentricity is low. The planet HD 4208 b is named Xolotlan. The name was selected in the NameExoWorlds campaign by Nicaragua, during the 100th anniversary of the IAU. Xolotlan is the name of Lake Managua in Nahuatl language.

Geographic entities mentioned:
surface_form: Lake Managua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 12.333333333333
lon: -86.416666666667
Etymology. The fortress town was named after Empress Maria Theresa (). Geography. Terezín is located about south of Litoměřice and southeast of Ústí nad Labem. It lies in a flat landscape of the Lower Ohře Table. It is situated on both banks of the Ohře River, near its confluence with the Elbe. The Elbe forms the northern municipal border. History.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
On September 9, 1821, the town was hit by a tornado. It leveled houses and forests in a swath of destruction beginning west of Lake Sunapee, through New London and Sutton, over the southwest spur of Mount Kearsarge and ending at the Webster line. The storm killed four people in Warner, seriously injured others and destroyed considerable property.

Geographic entities mentioned:
surface_form: Lake Sunapee
instance_of: Lake
countries: United States
coordinates: lat: 43.375833333333
lon: -72.056388888889
Mount Kearsarge is a popular hiking destination, due both to its bare, rocky summit, and to the fact that a paved road climbs from Rollins State Park to within a half mile of the summit. The peak is the highest point along the Sunapee-Ragged-Kearsarge Greenway, a hiking trail which links ten towns and encircles the Lake Sunapee region of western New Hampshire.

Geographic entities mentioned:
surface_form: Sunapee
instance_of: Mountain
countries: United States
coordinates: lat: 43.313611111111
lon: -72.074166666667
surface_form: Lake Sunapee
instance_of: Lake
countries: United States
coordinates: lat: 43.375833333333
lon: -72.056388888889
The site is placed by the Muslim literary sources somewhere between Ramla and Bayt Jibrin (modern Beit Guvrin), both in modern Israel, but is otherwise unattested by any geographer of the period. Based on the region's topography, the historian N. A. Miednikoff suggested that the battle was fought on the Wadi al-Samt river (Valley of Elah), where lies the twin village of al-Jannaba.

Geographic entities mentioned:
surface_form: Valley of Elah
instance_of: Valley
countries: Israel
coordinates: lat: 31.6806252
lon: 34.9891247
Landscape and geology. With its rather angular – in places trapezoidally-shaped – summits, the Northern Black Forest rises above the Rhine Plain by more than. By contrast, its eastern slopes descend gradually and there is less of a height difference with its neighbouring regions. Its highest peak is the Hornisgrinde at.

Geographic entities mentioned:
surface_form: Hornisgrinde
instance_of: Mountain
countries: Germany
coordinates: lat: 48.606944444444
lon: 8.2025
Lakes. Numerous tarns in the Northern Black Forest are evidence of ice age glacial formations, The best-known is the Mummelsee on the Hornisgrinde. Other tarns are the Ellbachsee, Herrenwieser See, Huzenbacher See, Sankenbachsee, Schurmsee and the Wildsee near Ruhestein. Many of them were also impounded in order to supply excess water for timber rafting which was common until the 19th century.

Geographic entities mentioned:
surface_form: Mummelsee
instance_of: Lake
countries: Germany
coordinates: lat: 48.598055555556
lon: 8.2008333333333
Lakes. Numerous tarns in the Northern Black Forest are evidence of ice age glacial formations, The best-known is the Mummelsee on the Hornisgrinde. Other tarns are the Ellbachsee, Herrenwieser See, Huzenbacher See, Sankenbachsee, Schurmsee and the Wildsee near Ruhestein. Many of them were also impounded in order to supply excess water for timber rafting which was common until the 19th century.

Geographic entities mentioned:
surface_form: Herrenwieser See
instance_of: Lake
countries: Germany
coordinates: lat: 48.6684
lon: 8.29554
surface_form: Huzenbacher See
instance_of: Lake
countries: Germany
coordinates: lat: 48.5746
lon: 8.34869
surface_form: Sankenbachsee
instance_of: Lake
countries: Germany
coordinates: lat: 48.484
lon: 8.33844
surface_form: Schurmsee
instance_of: Lake
countries: Germany
coordinates: lat: 48.6133
lon: 8.31876
The Kleine Kinzig Dam is used for drinking water, water regulation and electricity generation. Tourism. Due to the vast preserved natural scenery, the region is popular among hikers. Hiking trails (selection). In the winter time, the Northern Black Forest region attracts tourists with the ski resorts Mehliskopf, Hundseck – Bühlertallifte, Kaltenbronn, Simmersfeld.

Geographic entities mentioned:
surface_form: Mehliskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 48.6492
lon: 8.24028
Tax issues. Mirant, which owns and operates two power plants in the Hudson Valley Region of New York State, failed to pay its property taxes in a dispute with tax authorities, claiming over-assessments by the Towns of Stony Point and Haverstraw New York, as well as the North Rockland School District.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Rolf Bae. Rolf Bae (9 January 1975 – 1 August 2008) was a Norwegian Arctic adventurer and mountaineer. Bae operated an adventure company called Fram, specializing in Arctic and Antarctic travel and survival courses. He died during an ascent of K2 in 2008. Biography.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
This was the second complete ascent via this route. Death. Rolf Bae died on 1 August 2008, in a climbing accident while taking part in an international expedition on K2 mountain in which eleven climbers lost their lives. His wife, experienced climber Cecilie Skog, reported seeing her husband swept off the mountain during an ice fall accident.

Geographic entities mentioned:
surface_form: K2 mountain
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
Motto. The motto of the school is &quot;More Beyond&quot;, translated from the Latin &quot;plus ultra &quot;, the motto of Francis Bacon, who used it, along with the device of a ship of discovery, sailing past the Pillars of Hercules, out of the small Mediterranean sea into the vast Atlantic Ocean beyond, to describe the knowledge he offered mankind.

Geographic entities mentioned:
surface_form: Pillars of Hercules
instance_of: Landform
countries: Morocco
Spain
Gibraltar
coordinates: lat: 36
lon: -5.35
In 1946, Millikan became head of the Department of Physiology at Vanderbilt University School of Medicine. Death. In 1938, Millikan married Frances Clare Leigh-Mallory, daughter of George Mallory, the mountaineer who died while climbing Mount Everest. In 1947 Millikan himself was killed by a falling rock while climbing &quot;Buzzard's Roost&quot; near Fall Creek Falls State Park, Tennessee.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Crescent Lake (Florida). Crescent Lake is a freshwater lake located in Putnam and Flagler counties in North Central Florida. The lake is approximately in length and wide. At the north end it connects to the St. Johns River by way of Dunns Creek. Geology. Crescent Lake has a long and narrow shape similar to a crescent. History. Crescent Lake was formerly known as Dunn's Lake.

Geographic entities mentioned:
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 60.4483
lon: -149.519
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 47.825
lon: -90.7603
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 41.9779331
lon: -111.6280034
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 43.97424
lon: -70.45679
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 33.9089
lon: -109.419
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4756
lon: -121.992
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 42.6419784
lon: -83.3908107
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 29.4635
lon: -81.5007
The lake is approximately in length and wide. At the north end it connects to the St. Johns River by way of Dunns Creek. Geology. Crescent Lake has a long and narrow shape similar to a crescent. History. Crescent Lake was formerly known as Dunn's Lake. Search for wreckage of the &quot;Alligator&quot;.

Geographic entities mentioned:
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 60.4483
lon: -149.519
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 47.825
lon: -90.7603
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 41.9779331
lon: -111.6280034
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 43.97424
lon: -70.45679
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 33.9089
lon: -109.419
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4756
lon: -121.992
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 42.6419784
lon: -83.3908107
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 29.4635
lon: -81.5007
At the north end it connects to the St. Johns River by way of Dunns Creek. Geology. Crescent Lake has a long and narrow shape similar to a crescent. History. Crescent Lake was formerly known as Dunn's Lake. Search for wreckage of the &quot;Alligator&quot;. On December 9, 2008, a group of volunteers led by scientists from the Lighthouse Archaeological Maritime Program in St.

Geographic entities mentioned:
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 60.4483
lon: -149.519
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 47.825
lon: -90.7603
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 41.9779331
lon: -111.6280034
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 43.97424
lon: -70.45679
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 33.9089
lon: -109.419
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4756
lon: -121.992
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 42.6419784
lon: -83.3908107
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 29.4635
lon: -81.5007
History. Crescent Lake was formerly known as Dunn's Lake. Search for wreckage of the &quot;Alligator&quot;. On December 9, 2008, a group of volunteers led by scientists from the Lighthouse Archaeological Maritime Program in St. Augustine, Florida searched the east side of Crescent Lake for the sunken wreckage of the &quot;Alligator&quot;.

Geographic entities mentioned:
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 60.4483
lon: -149.519
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 47.825
lon: -90.7603
surface_form: augustine
instance_of: Mountain
countries: United States
coordinates: lat: 59.363333333333
lon: -153.43333333333
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 41.9779331
lon: -111.6280034
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 43.97424
lon: -70.45679
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 33.9089
lon: -109.419
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4756
lon: -121.992
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 42.6419784
lon: -83.3908107
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 29.4635
lon: -81.5007
Mercenaries from Badakhshan, Kokand and Kunduz fled first, then the Kashgarians lost ground. Qing troops rushed to Kashgar and, upon entering the city, embarked on the wholesale massacre of the local population of about 20,000 civilians. On January29, 1828, Jahangir managed to escape and hide himself in the mountainous Alay Valley among the Kyrgyz people.

Geographic entities mentioned:
surface_form: Alay Valley
instance_of: Valley
countries: Kyrgyzstan
coordinates: lat: 39.666666666667
lon: 72.966666666667
Jongjasan (Gyeonggi). Jongjasan () is a mountain near Pocheon, Gyeonggi Province in South Korea. It has an elevation of.

Geographic entities mentioned:
surface_form: jongjasan (gyeonggi)
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.0833
lon: 127.183
Jongjasan (Gyeonggi). Jongjasan () is a mountain near Pocheon, Gyeonggi Province in South Korea. It has an elevation of.

Geographic entities mentioned:
surface_form: jongjasan
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.0833
lon: 127.183
Øvresetertjern. Øvresetertjern is a lake in Oslo, Norway. It is located over sea level between the top of the hill Tryvannshøyden and Frognerseteren. From 1916 to 1938, the station Tryvandshøiden was located north of the lake, but it was never served by regular passenger trains.

Geographic entities mentioned:
surface_form: øvresetertjern
instance_of: Lake
countries: Norway
coordinates: lat: 59.9825
lon: 10.6719
states. It is also within Palliser's Triangle and the Great Plains ecoregion. The site is an Important Bird Area (IBA) of Canada, designated as Last Mountain Lake NWA (SK 001). Last Mountain Lake National Wildlife Area is located at the north end of Last Mountain Lake, west of Govan. The majority of the park is in the RM of Wreford No. 280.

Geographic entities mentioned:
surface_form: Last Mountain Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.1667
lon: -105.25
Land composition. The protected area includes several small islands, including Bird, Royal, and Coney. The northernmost inlet for Last Mountain Lake, Lanigan Creek and its tributary Saline Creek, runs through the heart of the park. Several dykes were built to help control water flow and levels. Natural grasslands make up about 54% of the total protected area.

Geographic entities mentioned:
surface_form: Lanigan Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 51.38337
lon: -105.21786
Lake Waitamoumou. Lake Waitamoumou is a small dune-dammed lake a kilometre north of Raglan in the Waikato region of New Zealand. Geology. Brown clay underlies the dunes, which limits the rate of seepage through the dunes, thus forming lakes where dune advance has blocked valleys. The lake bed and stream are on Awhitu sands.

Geographic entities mentioned:
surface_form: lake waitamoumou
instance_of: Lake
countries: New Zealand
coordinates: lat: -37.789372
lon: 174.842589
Nevado de Longaví is usually put into the &quot;Transitional Southern Volcanic Zone&quot;, one of the four segments which the Southern Volcanic Zone is subdivided into; they are characterized by different thicknesses of the crust that the volcanoes are constructed on and by differences in the volcanic rocks. Farther east lie the Tatara-San Pedro and Laguna del Maule volcanoes. Geology.

Geographic entities mentioned:
surface_form: Tatara-San Pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
surface_form: laguna del maule
instance_of: Lake
countries: Chile
coordinates: lat: -36.055
lon: -70.5
surface_form: maule
instance_of: Lake
countries: Chile
coordinates: lat: -36.055
lon: -70.5
surface_form: laguna del maule
instance_of: Mountain
countries: Chile
coordinates: lat: -36.0675
lon: -70.5225
The emplacement of this formation was facilitated by a decrease in the compressional stress that had affected the region prior to the Pliocene. Some isolated monogenetic volcanic centres can be found southeast of Nevado de Longaví. Aside from Villalobos, this includes Resago and Loma Blanca. The first and the last are of Pleistocene age, based on their preservation. Resago is post-glacial.

Geographic entities mentioned:
surface_form: Resago
instance_of: Mountain
countries: Chile
coordinates: lat: -36.458
lon: -70.904
surface_form: resago
instance_of: Mountain
countries: Chile
coordinates: lat: -36.458
lon: -70.904
The unusual chemical patterns appear to reflect that the magmas erupted from Nevado de Longaví were extremely rich in water. Such a pattern has also been noted at Mocho-Choshuenco and Calbuco. All these volcanoes are located above the points where fracture zones intersect the Peru–Chile Trench, and it has been proposed that these fracture zones channel water into the mantle.

Geographic entities mentioned:
surface_form: Mocho-Choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
surface_form: calbuco
instance_of: Mountain
countries: Chile
coordinates: lat: -41.332777777778
lon: -72.611111111111
surface_form: mocho
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
surface_form: choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
Regional. Nevado de Longaví lies in the Andean Mountain Range's Southern Volcanic Zone, which extends between 33 and 46 degrees southern latitude. It is one among 60 volcanoes in Chile and Argentina that lie within the Southern Volcanic Zone. Among the largest volcanic eruptions in this area were the 1932 Quizapu and the 1991 Cerro Hudson eruptions.

Geographic entities mentioned:
surface_form: quizapu
instance_of: Mountain
countries: Chile
coordinates: lat: -35.653333333333
lon: -70.760833333333
surface_form: cerro hudson
instance_of: Mountain
countries: Chile
coordinates: lat: -45.92
lon: -72.95
Nevado de Longaví. Nevado de Longaví is a volcano in the Andes of central Chile. The high volcano lies in the Linares Province, which is part of the Maule Region. It features a summit crater and several parasitic vents. The volcano is constructed principally from lava flows.

Geographic entities mentioned:
surface_form: maule
instance_of: Lake
countries: Chile
coordinates: lat: -36.055
lon: -70.5
The volcano has no historic eruptions but fumarolic activity is ongoing. Nevado de Longaví is monitored by the National Geology and Mining Service of Chile. Geography. Nevado de Longaví lies in the Longaví commune of Linares Province, Maule Region. Regional. Nevado de Longaví lies in the Andean Mountain Range's Southern Volcanic Zone, which extends between 33 and 46 degrees southern latitude.

Geographic entities mentioned:
surface_form: maule
instance_of: Lake
countries: Chile
coordinates: lat: -36.055
lon: -70.5
surface_form: nevado de longaví
instance_of: Mountain
countries: Chile
coordinates: lat: -36.193055555556
lon: -71.160833333333
Nevado de Longaví. Nevado de Longaví is a volcano in the Andes of central Chile. The high volcano lies in the Linares Province, which is part of the Maule Region. It features a summit crater and several parasitic vents. The volcano is constructed principally from lava flows.

Geographic entities mentioned:
surface_form: nevado de longaví
instance_of: Mountain
countries: Chile
coordinates: lat: -36.193055555556
lon: -71.160833333333
After a first phase characterized by the production of basaltic andesite, the bulk of the edifice was constructed by andesitic lava flows. The volcanic rock that makes up Nevado de Longaví features an unusual magma chemistry that resembles adakite (having geochemical characteristics of magma thought to have formed by partial melting of altered basalt that is subducted below volcanic arcs).

Geographic entities mentioned:
surface_form: nevado de longaví
instance_of: Mountain
countries: Chile
coordinates: lat: -36.193055555556
lon: -71.160833333333
It may be the consequence of the magma being unusually water-rich, which may occur because the Mocha fracture zone subducts beneath the volcano. Nevado de Longaví was active during the Holocene. 6,835 ± 65 or 7,500 years before present an explosive eruption deposited pumice more than away from the volcano. A lava flow was then erupted over the pumice.

Geographic entities mentioned:
surface_form: nevado de longaví
instance_of: Mountain
countries: Chile
coordinates: lat: -36.193055555556
lon: -71.160833333333
A lava flow was then erupted over the pumice. The last eruption occurred about 5,700 years ago and formed a lava dome. The volcano has no historic eruptions but fumarolic activity is ongoing. Nevado de Longaví is monitored by the National Geology and Mining Service of Chile. Geography. Nevado de Longaví lies in the Longaví commune of Linares Province, Maule Region. Regional.

Geographic entities mentioned:
surface_form: nevado de longaví
instance_of: Mountain
countries: Chile
coordinates: lat: -36.193055555556
lon: -71.160833333333
Geography. Nevado de Longaví lies in the Longaví commune of Linares Province, Maule Region. Regional. Nevado de Longaví lies in the Andean Mountain Range's Southern Volcanic Zone, which extends between 33 and 46 degrees southern latitude. It is one among 60 volcanoes in Chile and Argentina that lie within the Southern Volcanic Zone.

Geographic entities mentioned:
surface_form: nevado de longaví
instance_of: Mountain
countries: Chile
coordinates: lat: -36.193055555556
lon: -71.160833333333
Nevado de Longaví is usually put into the &quot;Transitional Southern Volcanic Zone&quot;, one of the four segments which the Southern Volcanic Zone is subdivided into; they are characterized by different thicknesses of the crust that the volcanoes are constructed on and by differences in the volcanic rocks. Farther east lie the Tatara-San Pedro and Laguna del Maule volcanoes. Geology.

Geographic entities mentioned:
surface_form: nevado de longaví
instance_of: Mountain
countries: Chile
coordinates: lat: -36.193055555556
lon: -71.160833333333
Nevado de Longaví is a relatively small volcano. With a diameter of, a basal surface area of and a height above base level of, Nevado de Longaví has a volume of about. The basement beneath the volcano is formed by the volcaniclastic Cura-Mallín Formation of Eocene–Miocene age, Miocene plutons and the lavic-breccia Pliocene-Pleistocene Cola de Zorro formation.

Geographic entities mentioned:
surface_form: nevado de longaví
instance_of: Mountain
countries: Chile
coordinates: lat: -36.193055555556
lon: -71.160833333333
The basement beneath the volcano is formed by the volcaniclastic Cura-Mallín Formation of Eocene–Miocene age, Miocene plutons and the lavic-breccia Pliocene-Pleistocene Cola de Zorro formation. This last formation was identified as forming a deeply eroded volcano in the Cordón de Villalobos south of Nevado de Longaví. This volcano south of Nevado de Longaví is known as Villalobos.

Geographic entities mentioned:
surface_form: nevado de longaví
instance_of: Mountain
countries: Chile
coordinates: lat: -36.193055555556
lon: -71.160833333333
This last formation was identified as forming a deeply eroded volcano in the Cordón de Villalobos south of Nevado de Longaví. This volcano south of Nevado de Longaví is known as Villalobos. The emplacement of this formation was facilitated by a decrease in the compressional stress that had affected the region prior to the Pliocene.

Geographic entities mentioned:
surface_form: nevado de longaví
instance_of: Mountain
countries: Chile
coordinates: lat: -36.193055555556
lon: -71.160833333333
This volcano south of Nevado de Longaví is known as Villalobos. The emplacement of this formation was facilitated by a decrease in the compressional stress that had affected the region prior to the Pliocene. Some isolated monogenetic volcanic centres can be found southeast of Nevado de Longaví. Aside from Villalobos, this includes Resago and Loma Blanca.

Geographic entities mentioned:
surface_form: nevado de longaví
instance_of: Mountain
countries: Chile
coordinates: lat: -36.193055555556
lon: -71.160833333333
The first and the last are of Pleistocene age, based on their preservation. Resago is post-glacial. The last two centres appear to be related to a geological lineament that flanks the eastern slopes of Nevado de Longaví. A glacier is found on the southern slope, between 1989 and 2017 glacier cover has decreased by over 95% with less than of glacier cover remaining.

Geographic entities mentioned:
surface_form: nevado de longaví
instance_of: Mountain
countries: Chile
coordinates: lat: -36.193055555556
lon: -71.160833333333
Previous glaciation is also supported by the presence of glacial striations on lava flows and of lahar deposits. The Rio Blanco originates on the southeastern slope of Nevado de Longaví, within the collapse scar. It turns south and west around the volcano in a fishhook pattern.

Geographic entities mentioned:
surface_form: nevado de longaví
instance_of: Mountain
countries: Chile
coordinates: lat: -36.193055555556
lon: -71.160833333333
The Rio Blanco originates on the southeastern slope of Nevado de Longaví, within the collapse scar. It turns south and west around the volcano in a fishhook pattern. The Estero Martinez and Quebrada Los Bueyes rivers also originate on Nevado de Longaví, on the western and southern flank respectively. They are both tributaries of the Rio Blanco.

Geographic entities mentioned:
surface_form: nevado de longaví
instance_of: Mountain
countries: Chile
coordinates: lat: -36.193055555556
lon: -71.160833333333
The Estero Martinez and Quebrada Los Bueyes rivers also originate on Nevado de Longaví, on the western and southern flank respectively. They are both tributaries of the Rio Blanco. The Achibueno River also originates on the eastern flank of Nevado de Longaví in a lake of the same name. It flows first northeastward and then turns around the volcano. Composition.

Geographic entities mentioned:
surface_form: nevado de longaví
instance_of: Mountain
countries: Chile
coordinates: lat: -36.193055555556
lon: -71.160833333333