Sarmila/GeoWiki-Features huggingface dataset:
Ragged Peak (Yosemite). Ragged Peak is a mountain, in the Tuolumne Meadows area of Yosemite National Park. Of the ridge south of the Young Lakes region, Ragged Peak is the most prominent feature. It is north of Tioga Road and its summit has a great view of Mount Conness's southwest face. Ragged Peak is an isolated summit, close to Young Lakes. Ragged Peak is north of Lembert Dome and Dog Lake.

Geographic entities mentioned:
surface_form: Young Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 37.9372908
lon: -119.3395173
surface_form: ragged peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.93298
lon: -119.35321
Ragged Peak (Yosemite). Ragged Peak is a mountain, in the Tuolumne Meadows area of Yosemite National Park. Of the ridge south of the Young Lakes region, Ragged Peak is the most prominent feature. It is north of Tioga Road and its summit has a great view of Mount Conness's southwest face. Ragged Peak is an isolated summit, close to Young Lakes. Ragged Peak is north of Lembert Dome and Dog Lake.

Geographic entities mentioned:
surface_form: Mount Conness
instance_of: Mountain
countries: United States
coordinates: lat: 37.967
lon: -119.321
Ragged Peak (Yosemite). Ragged Peak is a mountain, in the Tuolumne Meadows area of Yosemite National Park. Of the ridge south of the Young Lakes region, Ragged Peak is the most prominent feature. It is north of Tioga Road and its summit has a great view of Mount Conness's southwest face. Ragged Peak is an isolated summit, close to Young Lakes. Ragged Peak is north of Lembert Dome and Dog Lake.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: ragged peak (yosemite)
instance_of: Mountain
countries: United States
coordinates: lat: 37.93298
lon: -119.35321
Ragged Peak (Yosemite). Ragged Peak is a mountain, in the Tuolumne Meadows area of Yosemite National Park. Of the ridge south of the Young Lakes region, Ragged Peak is the most prominent feature. It is north of Tioga Road and its summit has a great view of Mount Conness's southwest face. Ragged Peak is an isolated summit, close to Young Lakes. Ragged Peak is north of Lembert Dome and Dog Lake.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: ragged peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.93298
lon: -119.35321
It is north of Tioga Road and its summit has a great view of Mount Conness's southwest face. Ragged Peak is an isolated summit, close to Young Lakes. Ragged Peak is north of Lembert Dome and Dog Lake. On climbing Ragged Peak. Ragged Peak has a &mdash; southern route, and the northwest face is listed as, the northeast face as, the east face as. So, Ragged Peak is available, for rock climbing.

Geographic entities mentioned:
surface_form: dog lake
instance_of: Lake
countries: United States
coordinates: lat: 37.8911484
lon: -119.3397255
surface_form: dog lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5872406
lon: -111.5846027
surface_form: ragged peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.93298
lon: -119.35321
surface_form: dog lake
instance_of: Lake
countries: United States
coordinates: lat: 44.290555555556
lon: -93.850555555556
surface_form: dog lake
instance_of: Lake
countries: United States
coordinates: lat: 40.667214
lon: -111.6394774
Ragged Peak is a mountain, in the Tuolumne Meadows area of Yosemite National Park. Of the ridge south of the Young Lakes region, Ragged Peak is the most prominent feature. It is north of Tioga Road and its summit has a great view of Mount Conness's southwest face. Ragged Peak is an isolated summit, close to Young Lakes. Ragged Peak is north of Lembert Dome and Dog Lake. On climbing Ragged Peak.

Geographic entities mentioned:
surface_form: ragged peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.93298
lon: -119.35321
surface_form: young lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 37.9372908
lon: -119.3395173
It is north of Tioga Road and its summit has a great view of Mount Conness's southwest face. Ragged Peak is an isolated summit, close to Young Lakes. Ragged Peak is north of Lembert Dome and Dog Lake. On climbing Ragged Peak. Ragged Peak has a &mdash; southern route, and the northwest face is listed as, the northeast face as, the east face as. So, Ragged Peak is available, for rock climbing.

Geographic entities mentioned:
surface_form: ragged peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.93298
lon: -119.35321
It is north of Tioga Road and its summit has a great view of Mount Conness's southwest face. Ragged Peak is an isolated summit, close to Young Lakes. Ragged Peak is north of Lembert Dome and Dog Lake. On climbing Ragged Peak. Ragged Peak has a &mdash; southern route, and the northwest face is listed as, the northeast face as, the east face as. So, Ragged Peak is available, for rock climbing.

Geographic entities mentioned:
surface_form: ragged peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.93298
lon: -119.35321
surface_form: ragged peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.93298
lon: -119.35321
Jacob Peak. Jacob Peak is a rock formation in Zion National Park in Washington County, Utah, United States. Jacob Peak is part of the Three Patriarchs, along with (and located to the north of) Abraham Peak and Isaac Peak. Name. Zion National Park was first named Mukuntuweap National Monument by Geologist John Wesley Powell.

Geographic entities mentioned:
surface_form: Three Patriarchs
instance_of: Mountain
countries: United States
coordinates: lat: 37.2372
lon: -112.965
surface_form: Abraham Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.2451674
lon: -112.9814476
surface_form: Isaac Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.2447
lon: -112.97327
surface_form: jacob peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.2497
lon: -112.96633
Jacob Peak. Jacob Peak is a rock formation in Zion National Park in Washington County, Utah, United States. Jacob Peak is part of the Three Patriarchs, along with (and located to the north of) Abraham Peak and Isaac Peak. Name. Zion National Park was first named Mukuntuweap National Monument by Geologist John Wesley Powell.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: jacob peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.2497
lon: -112.96633
Shortly afterward, Methodist minister Frederick Vining Fisher explored the park along with two Latter-Day Saints youth and among them named many of the peaks in the park. Along with its neighbor peaks, names were chosen from biblical patriarchs. The name for Isaac Peak was suggested by Claud Hirschi, one of the youth with Fisher and named after Isaac.

Geographic entities mentioned:
surface_form: isaac peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.2447
lon: -112.97327
Jacob Peak. Jacob Peak is a rock formation in Zion National Park in Washington County, Utah, United States. Jacob Peak is part of the Three Patriarchs, along with (and located to the north of) Abraham Peak and Isaac Peak. Name. Zion National Park was first named Mukuntuweap National Monument by Geologist John Wesley Powell.

Geographic entities mentioned:
surface_form: jacob peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.2497
lon: -112.96633
Each business developed a sandy beach on their shorelines for guests; and Red Oaks Resort also operated a small boat livery. All three of the family-owned resorts on Alma Lake were subdivided between 1965 and 1974. Property owners formed the Alma-Moon Lake Association in 1969–1970, and by 1971 the owners had agreed to institute a 5 mph speed-limit on Alma Lake. Physical aspects.

Geographic entities mentioned:
surface_form: moon lake
instance_of: Lake
countries: United States
coordinates: lat: 45.953611111111
lon: -95.59
surface_form: alma lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
surface_form: moon lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5624
lon: -110.49
surface_form: moon lake
instance_of: Lake
countries: United States
coordinates: lat: 34.4261
lon: -90.5025
surface_form: moon lake
instance_of: Lake
countries: United States
coordinates: lat: 44.2525804
lon: -75.7367215
surface_form: moon lake
instance_of: Lake
countries: United States
coordinates: lat: 41.847331
lon: -86.381588
Physical aspects. Alma Lake is a seepage lake, meaning that it has no inflowing or outflowing streams; however, Alma lake is connected by a channel to Moon Lake. Alma Lake becomes stratified during the summer, turns over and completely mixes in the fall, re-stratifies during winter, and then mixes again during spring. This makes it classified as a dimictic lake.

Geographic entities mentioned:
surface_form: moon lake
instance_of: Lake
countries: United States
coordinates: lat: 45.953611111111
lon: -95.59
surface_form: alma lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
surface_form: alma lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
surface_form: moon lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5624
lon: -110.49
surface_form: moon lake
instance_of: Lake
countries: United States
coordinates: lat: 34.4261
lon: -90.5025
surface_form: moon lake
instance_of: Lake
countries: United States
coordinates: lat: 44.2525804
lon: -75.7367215
surface_form: moon lake
instance_of: Lake
countries: United States
coordinates: lat: 41.847331
lon: -86.381588
Alma Lake (Wisconsin). Alma Lake, located in North-Central Wisconsin in Vilas County, near the town of St. Germain, is a small 57.7-acre (233,500 sq. meters) lake with a maximum depth of 5.5 meters (18 feet), and a mean depth of 3.4 meters (11 feet). The lake bottom is composed of 50% sand, 40% gravel, and 10% mulch.

Geographic entities mentioned:
surface_form: alma lake (wisconsin)
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
Alma Lake (Wisconsin). Alma Lake, located in North-Central Wisconsin in Vilas County, near the town of St. Germain, is a small 57.7-acre (233,500 sq. meters) lake with a maximum depth of 5.5 meters (18 feet), and a mean depth of 3.4 meters (11 feet). The lake bottom is composed of 50% sand, 40% gravel, and 10% mulch.

Geographic entities mentioned:
surface_form: alma lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
Germain, is a small 57.7-acre (233,500 sq. meters) lake with a maximum depth of 5.5 meters (18 feet), and a mean depth of 3.4 meters (11 feet). The lake bottom is composed of 50% sand, 40% gravel, and 10% mulch. Alma Lake has one public boat landing located on Red Oak Road, off Birchwood Drive. The lake always has a slow, no-wake ordinance. History.

Geographic entities mentioned:
surface_form: alma lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
The lake bottom is composed of 50% sand, 40% gravel, and 10% mulch. Alma Lake has one public boat landing located on Red Oak Road, off Birchwood Drive. The lake always has a slow, no-wake ordinance. History. In 1902, the Red Oak Resort was built on Alma Lake by George Jackson. The resort was then purchased by Walter and Wilka deHaas in the 1920s.

Geographic entities mentioned:
surface_form: alma lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
The resort was then purchased by Walter and Wilka deHaas in the 1920s. By the 1960s, Alma Lake was home to three resorts; The Twilight Resort, which was located at the southern end of the lake, Lindquist's Log Cabins, which was located on the northwestern bay, and deHaas Red Oaks, which was located on the east side of the southern bowl of the lake.

Geographic entities mentioned:
surface_form: alma lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
Each business developed a sandy beach on their shorelines for guests; and Red Oaks Resort also operated a small boat livery. All three of the family-owned resorts on Alma Lake were subdivided between 1965 and 1974. Property owners formed the Alma-Moon Lake Association in 1969–1970, and by 1971 the owners had agreed to institute a 5 mph speed-limit on Alma Lake. Physical aspects.

Geographic entities mentioned:
surface_form: alma lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
Physical aspects. Alma Lake is a seepage lake, meaning that it has no inflowing or outflowing streams; however, Alma lake is connected by a channel to Moon Lake. Alma Lake becomes stratified during the summer, turns over and completely mixes in the fall, re-stratifies during winter, and then mixes again during spring. This makes it classified as a dimictic lake.

Geographic entities mentioned:
surface_form: alma lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
This makes it classified as a dimictic lake. In winter, Alma Lake is usually frozen by the end of November and stays frozen until late April to early May with water temperatures dropping to 0 °C just below the ice. The highest recorded temperature in the lake was 27.6 °C in July 2006. Alma Lake has relatively clear, blue water, with Secchi disk depths averaging 3.6 meters (11.9 feet).

Geographic entities mentioned:
surface_form: alma lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
The highest recorded temperature in the lake was 27.6 °C in July 2006. Alma Lake has relatively clear, blue water, with Secchi disk depths averaging 3.6 meters (11.9 feet). Secchi depths in Alma Lake have historically been highly correlated with the amount of chlorophyll-&quot;a&quot; in the water. The summer chlorophyll-&quot;a&quot; average is 4.3 ug/L.

Geographic entities mentioned:
surface_form: alma lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
Secchi depths in Alma Lake have historically been highly correlated with the amount of chlorophyll-&quot;a&quot; in the water. The summer chlorophyll-&quot;a&quot; average is 4.3 ug/L. Like most lakes in northern Wisconsin, Alma lake is Phosphorus limited with a Nitrogen: Phosphorus ratio of 33:1. Wildlife.

Geographic entities mentioned:
surface_form: alma lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
surface_form: alma lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
Wildlife. Alma Lake is home to 34 native aquatic plant species including one species listed as a species special concern by the Wisconsin Natural Heritage Inventory Program; the northeastern bladderwort. The most common plant in Alma Lake is dwarf watermilfoil. The only invasive species that has been identified in Alma Lake is the Chinese mystery snail.

Geographic entities mentioned:
surface_form: alma lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
The most common plant in Alma Lake is dwarf watermilfoil. The only invasive species that has been identified in Alma Lake is the Chinese mystery snail. Alma Lake has not been invaded by zebra mussels due to its pH of 6.8 and its very low concentration of calcium.

Geographic entities mentioned:
surface_form: alma lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
surface_form: alma lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
The only invasive species that has been identified in Alma Lake is the Chinese mystery snail. Alma Lake has not been invaded by zebra mussels due to its pH of 6.8 and its very low concentration of calcium. Alma Lake is also home to a number of fish including: muskellunge, panfish, largemouth bass, smallmouth bass, walleye, crappie, rock bass, sunfish, bluegill, perch, and northern pike.

Geographic entities mentioned:
surface_form: alma lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
Alma Lake has not been invaded by zebra mussels due to its pH of 6.8 and its very low concentration of calcium. Alma Lake is also home to a number of fish including: muskellunge, panfish, largemouth bass, smallmouth bass, walleye, crappie, rock bass, sunfish, bluegill, perch, and northern pike. With intermediate levels of primary production, Alma Lake's trophic status is mesotrophic. Human use.

Geographic entities mentioned:
surface_form: alma lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
surface_form: alma lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9097631
lon: -89.4282752
The XIII SS Army Corps retreated into the Saarland and the Palatinate where it started to destroy the Rhine bridges. In April 1945, between Main and Jagst, it came up against the 4th US Armored Division and took part in heavy fighting around the Tauber – Colombia line and around Würzburg and Nuremberg. The Corps then fought a withdrawal to the Danube and around Munich.

Geographic entities mentioned:
surface_form: Tauber
instance_of: Watercourse
countries: Germany
coordinates: lat: 49.25
lon: 10.114861111111
The nearest Darjeeling tea estate is Glenburn Tea Estate, separated by a hill. Takdah is also close-by. Located at a height of nestles in a glen overlooking the majestic Kangchenjunga peak. Lopchu has under tea cultivation. Most of tea plants were transplanted from Yunan province in China, and much of the tea gets exported to Germany and other European countries.

Geographic entities mentioned:
surface_form: Kangchenjunga
instance_of: Mountain
countries: India
Nepal
coordinates: lat: 27.7
lon: 88.133333
But later, they decided to switch to biathlon. She began competing internationally a year earlier than Vita. In 2004 she took part at Junior World Championships in Maurienne, France. In 2005 she won two medals at Junior World and one at Junior European Championships. On 17 December 2005, she debuted in Biathlon World Cup.

Geographic entities mentioned:
surface_form: Maurienne
instance_of: Valley
countries: France
coordinates: lat: 45.2
lon: 6.6666666666667
Southowram. Southowram () is a village and former civil parish in Calderdale, West Yorkshire, England. It stands on hill top between Halifax and Brighouse, on the south side of the Shibden Valley. Northowram is on the northern side of the valley. Southowram falls within the Town ward of Calderdale Council.

Geographic entities mentioned:
surface_form: Shibden Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.726
lon: -1.839
Babak organized local mountain communities in opposition to the increasing encroachment of the Abbasid territorial pressure from southern territories. This resistance took place in the Elburz mountain range near the southern shores of the Caspian Sea. The Khurramites seized control of Azerbaijan and other regions, seeking to restore the faith to Mazdakism.

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
Papermaking is favoured because of the uniform temperature and volume of the water year-round, partly due to the river Touvre, which joins the Charente at Angoulême. The Touvre is the second largest river with an underground source in France after the Sorgue (Fontaine-de-Vaucluse). The Touvre emerges as a full-blown river from the head of the valley at Ruelle.

Geographic entities mentioned:
surface_form: Sorgue
instance_of: Watercourse
countries: France
coordinates: lat: 43.966666666667
lon: 5
Meteorite Mountain. Meteorite Mountain is a prominent glaciated mountain summit located in the Chugach Mountains, in the U.S. state of Alaska. It is situated southeast of Valdez, south of Hogback Ridge, and southeast of Mount Francis. In January 1927, a meteorite hit this mountain, which is how the mountain got its name.

Geographic entities mentioned:
surface_form: meteorite mountain
instance_of: Mountain
countries: United States
coordinates: lat: 60.9772
lon: -145.9633
Climate. Based on the Köppen climate classification, Meteorite Mountain is located in a subarctic climate zone with long, cold, snowy winters, and cool summers. Weather systems coming off the Gulf of Alaska are forced upwards by the Chugach Mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall.

Geographic entities mentioned:
surface_form: meteorite mountain
instance_of: Mountain
countries: United States
coordinates: lat: 60.9772
lon: -145.9633
Meteorite Mountain is a prominent glaciated mountain summit located in the Chugach Mountains, in the U.S. state of Alaska. It is situated southeast of Valdez, south of Hogback Ridge, and southeast of Mount Francis. In January 1927, a meteorite hit this mountain, which is how the mountain got its name. The mountain's name was in local use when it was first published in 1953 by U.S.

Geographic entities mentioned:
surface_form: mount francis
instance_of: Mountain
countries: United States
coordinates: lat: 61.0417
lon: -146.2086
surface_form: hogback
instance_of: Mountain
countries: United States
coordinates: lat: 42.706388888889
lon: -74.465
Distribution. It is found in the IBRA regions of: the Arnhem Coast, the Arnhem Plateau, the Central Kimberley, the Daly Basin, Dampierland, Darwin Coastal, Gulf Coastal, Gulf Fall and Uplands, Northern Kimberley, Ord Victoria Plain, Pine Creek, Sturt Plateau, Tiwi Cobourg, and Victoria Bonaparte,
Habitat.

Geographic entities mentioned:
surface_form: Arnhem Plateau
instance_of: Plateau
countries: Australia
coordinates: lat: -13.1911
lon: 133.181
Ghent Kangri. Ghent Kangri (or Mount Ghent, Ghaint I) is a high peak near the north end of the Saltoro Mountains, a subrange of the Karakoram range. It is located west of the Siachen Glacier near the Actual Ground Position Line between India and Pakistan. Ghent Kangri was first climbed on 4 June 1961, by Wolfgang Axt, a member of an Austrian expedition led by Erich Waschak, via the West Ridge.

Geographic entities mentioned:
surface_form: mount ghent
instance_of: Mountain
countries: India
coordinates: lat: 35.5175
lon: 76.800277777778
surface_form: ghaint i
instance_of: Mountain
countries: India
coordinates: lat: 35.5175
lon: 76.800277777778
surface_form: ghent kangri
instance_of: Mountain
countries: India
coordinates: lat: 35.5175
lon: 76.800277777778
Ghent Kangri. Ghent Kangri (or Mount Ghent, Ghaint I) is a high peak near the north end of the Saltoro Mountains, a subrange of the Karakoram range. It is located west of the Siachen Glacier near the Actual Ground Position Line between India and Pakistan. Ghent Kangri was first climbed on 4 June 1961, by Wolfgang Axt, a member of an Austrian expedition led by Erich Waschak, via the West Ridge.

Geographic entities mentioned:
surface_form: ghent kangri
instance_of: Mountain
countries: India
coordinates: lat: 35.5175
lon: 76.800277777778
It is located west of the Siachen Glacier near the Actual Ground Position Line between India and Pakistan. Ghent Kangri was first climbed on 4 June 1961, by Wolfgang Axt, a member of an Austrian expedition led by Erich Waschak, via the West Ridge. He climbed solo above the high camp. According to the, there have been three subsequent ascents of the peak, in 1977, 1980, and 1984.

Geographic entities mentioned:
surface_form: ghent kangri
instance_of: Mountain
countries: India
coordinates: lat: 35.5175
lon: 76.800277777778
Cassels objected to game hunting for pleasure as a conservationist before this was a common approach to wildlife, and helped found a bird sanctuary and in 1924 one of the first Canadian wildlife refuges at Gaetz Lakes, Alberta. Biography. Elsie McAlister was born in February 1864 near St. Mary's Loch south of Edinburgh to father, Free Church teacher, Archibald McAlister, and mother Janet Reid.

Geographic entities mentioned:
surface_form: St. Mary's Loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.492256
lon: -3.191433
Grinnell Falls. Grinnell Falls is a waterfall in Glacier National Park, Montana, US. Grinnell Falls have several major drops in its descent from Grinnell Glacier with the highest estimated at. The falls are in the Many Glacier region of the park, between Mount Grinnell and Angel Wing.

Geographic entities mentioned:
surface_form: Mount Grinnell
instance_of: Mountain
countries: United States
coordinates: lat: 48.7766
lon: -113.727
Ampatuyoc (Ayacucho). Ampatuyoc (possibly from Quechua &quot;hamp'atu&quot; frog, &quot;-yuq&quot; a suffix to indicate ownership, &quot;the one with a frog (or frogs)&quot;) is a mountain in the Andes of Peru, about high. It is located in the Ayacucho Region, Víctor Fajardo Province, Sarhua District.

Geographic entities mentioned:
surface_form: ampatuyoc
instance_of: Mountain
countries: Peru
coordinates: lat: -12.56138889
lon: -74.46277778
surface_form: ampatuyoc (ayacucho)
instance_of: Mountain
countries: Peru
coordinates: lat: -13.6528
lon: -74.3989
surface_form: ampatuyoc
instance_of: Mountain
countries: Peru
coordinates: lat: -12.67583333
lon: -74.39527778
Ampatuyoc (Ayacucho). Ampatuyoc (possibly from Quechua &quot;hamp'atu&quot; frog, &quot;-yuq&quot; a suffix to indicate ownership, &quot;the one with a frog (or frogs)&quot;) is a mountain in the Andes of Peru, about high. It is located in the Ayacucho Region, Víctor Fajardo Province, Sarhua District.

Geographic entities mentioned:
surface_form: ampatuyoc
instance_of: Mountain
countries: Peru
coordinates: lat: -12.56138889
lon: -74.46277778
surface_form: ampatuyoc
instance_of: Mountain
countries: Peru
coordinates: lat: -13.6528
lon: -74.3989
surface_form: ampatuyoc
instance_of: Mountain
countries: Peru
coordinates: lat: -12.67583333
lon: -74.39527778
Reservoirs. It also operated the filtration works at the Elan Valley Reservoirs
It also had abstraction licences for river abstractions which included operating rules linked to storage at both Clywedog reservoir and Lake Vyrnwy although no water from those reservoirs was directly piped to supply.

Geographic entities mentioned:
surface_form: Elan Valley Reservoirs
instance_of: Group of lakes
countries: United Kingdom
coordinates: lat: 52.27222222222222
lon: -3.688888888888889
Mount Cromwell. Mount Cromwell is a mountain located in the Sunwapta River Valley of Jasper National Park, in Alberta, Canada. Cromwell lies two kilometres north of the east summit of Stutfield Peak. The mountain was named in 1972 by J. Monroe Thorington after Oliver Eaton (Tony) Cromwell, an American climber who made many first ascents in the Canadian Rockies.

Geographic entities mentioned:
surface_form: Stutfield Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.23833333333334
lon: -117.4075
Climate. Based on the Köppen climate classification, Cromwell is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below with wind chill factors below. Precipitation runoff from the mountain drains into the Athabasca River. Geology.

Geographic entities mentioned:
surface_form: athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
surface_form: athabasca
instance_of: Mountain
countries: Canada
coordinates: lat: 52.18055555555556
lon: -117.20166666666667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Cromwell. Mount Cromwell is a mountain located in the Sunwapta River Valley of Jasper National Park, in Alberta, Canada. Cromwell lies two kilometres north of the east summit of Stutfield Peak. The mountain was named in 1972 by J. Monroe Thorington after Oliver Eaton (Tony) Cromwell, an American climber who made many first ascents in the Canadian Rockies.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount cromwell
instance_of: Mountain
countries: Canada
coordinates: lat: 52.26888888888889
lon: -117.39305555555555
Mount Cromwell is a mountain located in the Sunwapta River Valley of Jasper National Park, in Alberta, Canada. Cromwell lies two kilometres north of the east summit of Stutfield Peak. The mountain was named in 1972 by J. Monroe Thorington after Oliver Eaton (Tony) Cromwell, an American climber who made many first ascents in the Canadian Rockies. The first ascent was made in 1936 by Oliver E.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Cromwell. Mount Cromwell is a mountain located in the Sunwapta River Valley of Jasper National Park, in Alberta, Canada. Cromwell lies two kilometres north of the east summit of Stutfield Peak. The mountain was named in 1972 by J. Monroe Thorington after Oliver Eaton (Tony) Cromwell, an American climber who made many first ascents in the Canadian Rockies.

Geographic entities mentioned:
surface_form: mount cromwell
instance_of: Mountain
countries: Canada
coordinates: lat: 52.26888888888889
lon: -117.39305555555555
The first ascent was made in 1936 by Oliver E. Cromwell, E. Cromwell jr., Francis S. North, and J. Monroe Thorington. Another source declares the ascent was made in 1938 by the same party but it included the guide Edward Feuz jr
In 2005, Bill Corbett, author of &quot;The 11,000ers of the Canadian Rockies,&quot; climbed to the top of Mount Cromwell. At the summit, his GPS registered 11,006 feet.

Geographic entities mentioned:
surface_form: mount cromwell
instance_of: Mountain
countries: Canada
coordinates: lat: 52.26888888888889
lon: -117.39305555555555
At the summit, his GPS registered 11,006 feet. So perhaps Mount Cromwell should be included in the list of the Canadian Rocky Mountains that are over 11,000 feet in elevation. Climate. Based on the Köppen climate classification, Cromwell is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below with wind chill factors below.

Geographic entities mentioned:
surface_form: mount cromwell
instance_of: Mountain
countries: Canada
coordinates: lat: 52.26888888888889
lon: -117.39305555555555
Since the early 1900s, the area has been surrounded by the Lolo National Forest. The eastern mouth of the valley is defined by a narrow pass between Mount Jumbo and Mount Sentinel, which leads to Hellgate Canyon. The western mouth is less well-defined and narrow, and leads to Ninemile Divide.

Geographic entities mentioned:
surface_form: Mount Jumbo
instance_of: Mountain
countries: United States
coordinates: lat: 46.8792
lon: -113.956
surface_form: Mount Sentinel
instance_of: Mountain
countries: United States
coordinates: lat: 46.8525
lon: -113.963
Worden and Higgins had intended to settle at Fort Owen in the Bitterroot Valley, but instead chose the Hell Gate Valley because it was halfway between Fort Owen and the federal government trading post at Jocko on the new Indian reservation. This, they believed, would draw more traffic than a store closer to either existing settlement.

Geographic entities mentioned:
surface_form: Bitterroot Valley
instance_of: Valley
countries: United States
coordinates: lat: 46.247
lon: -114.16
Louis, Missouri. The first post office in Montana was established at Hell Gate on November 24, 1862. In 1863, the discovery of gold at Alder Gulch brought hundreds of settlers to the region, allowing Hell Gate to prosper. That year, Henry Buckhouse built the town's first and only blacksmith shop. St.

Geographic entities mentioned:
surface_form: Alder Gulch
instance_of: Valley
countries: United States
coordinates: lat: 45.3253
lon: -112.077
On the night of January 27, 1864, a group of 21 vigilantes (part of the notorious Montana Vigilantes, who had instituted a reign of terror of their own in the state) from Alder Gulch rode into Hell Gate and rounded up Skinner and the other outlaws. A brief trial was held in Worden and Higgins' store, and four members of the Plummer gang were sentenced to death.

Geographic entities mentioned:
surface_form: Alder Gulch
instance_of: Valley
countries: United States
coordinates: lat: 45.3253
lon: -112.077
Valdarnese. The Valdarnese, also referred to as Valdarnese Bianca, Valdarno Bianca or Pollo del Valdarno, is a breed of large white chicken from the upper Valdarno, the valley of the Arno river, in Tuscany, central Italy. It became virtually extinct in the twentieth century, but the population is recovering.

Geographic entities mentioned:
surface_form: Valdarno
instance_of: Valley
countries: Italy
coordinates: lat: 43.566666666667
lon: 11.533333333333
Tórshavn. Tórshavn (;; Danish: &quot;Thorshavn&quot;), locally referred to as Havn, is the capital and largest city of the Faroe Islands. It is located in the southern part on the east coast of Streymoy. To the northwest of the city lies the mountain Húsareyn, and to the southwest, the Kirkjubøreyn. They are separated by the Sandá River.

Geographic entities mentioned:
surface_form: Húsareyn
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 62.01666833
lon: -6.81667222
Elm Ridge (Greene County, New York). Elm Ridge is a mountain in Greene County, New York. It is located in the Catskill Mountains north of Maplecrest. Van Loan Hill is located south-southwest of Elm Ridge.

Geographic entities mentioned:
surface_form: Van Loan Hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.26897
lon: -74.20014
Ozeros. Lake Ozeros () is a lake located west of the Greek city of Agrinio. The lake has its own catchment area but is sometimes connected to the waters of the Acheloos river, flowing from the northwest, when the river overflows. The lake has a surface of ca. 10 km2 and an average depth of 8–10 m, but this varies greatly with the season.

Geographic entities mentioned:
surface_form: ozeros
instance_of: Lake
countries: Greece
coordinates: lat: 38.655833333333
lon: 21.224166666667
He was convinced that financial gain was the main motive behind the BUND's withdrawal of its lawsuits against the wind farm in Nordergründe and the deepening of the Elbe, in return for which it received foundation funds from the operators. He also rejected what he considered to be landscape-destroying wind turbines outside built-up areas.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Also 30,000 years old are the so-called Mladeč-type blades of the Aurignacian culture, made of bone, found in Wierzchowie, Kraków County. A 27,500-year old burial of an 18-month old child, complete with burial gift decorative artifacts, pendant or necklace elements made of teeth of large ungulates, was discovered in Borsuk Cave near Kraków (southern Kraków-Częstochowa Upland).

Geographic entities mentioned:
surface_form: Kraków-Częstochowa Upland
instance_of: Plateau
countries: Poland
coordinates: lat: 50.2067
lon: 19.8292
The feature is named after Kameliya Stancheva, participant in the 1996/97 Bulgarian Antarctic campaign, for her support for the Bulgarian Antarctic programme. Location. Stancheva Peak is located at, which is 4.6 km south of Vologes Ridge, 6.68 km west-southwest of Mount Mecheva and 5.05 km northwest of Chuypetlovo Knoll. British mapping in 1976.

Geographic entities mentioned:
surface_form: Mount Mecheva
instance_of: Mountain
coordinates: lat: -66.50305556
lon: -64.00333333
In Pobitora Wildlife Sanctuary, it was sighted regularly between 1996 and 2001. In Arunachal Pradesh, repeated sightings along Namdapha and Noa Dihing Rivers indicate that Namdapha National Park is an important refuge and breeding site. In northern Myanmar, it was observed along four streams in the Hkakabo Razi landscape between March 2016 and December 2020. Behaviour and ecology.

Geographic entities mentioned:
surface_form: Hkakabo Razi
instance_of: Mountain
countries: Myanmar
coordinates: lat: 28.333055555556
lon: 97.466666666667
Dominating the town to the north are the Callander Crags, a visible part of the Highland Boundary Fault, rising to at the cairn. Ben Ledi () lies north-west of Callander. Popular local walks include Bracklinn Falls, The Meadows, Callander Crags and the Wood Walks. The Rob Roy Way passes through Callander. The town sits on the Trossachs Bird of Prey Trail.

Geographic entities mentioned:
surface_form: Ben Ledi
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.258659
lon: -4.322375
The Auchenlaich Cairn, a Neolithic chambered cairn which at in length is the longest in Britain, is situated near Keltie Bridge just east of Callander. The remains of an ancient hillfort can be seen at Dunmore overlooking Loch Venachar, near Kilmahog. This fort was likely a large defended structure visible from some distance and excavations have revealed a well and signs of vitrified stonework.

Geographic entities mentioned:
surface_form: Loch Venachar
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.22076
lon: -4.30226
Finlay's Casebook&quot;. In the fictional world of the franchise, the character Destro was born in Callander. The fictional teenager, Adrian Mole, while on holiday at Loch Lubnaig walks to Callander to buy a Mars bar and play &quot;Space Invaders&quot; (&quot;The Secret Diary of Adrian Mole, Aged 13¾&quot; by Sue Townsend).

Geographic entities mentioned:
surface_form: Loch Lubnaig
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.291638
lon: -4.294395
His mother Amina died when he was six, leaving Muhammad an orphan. He was raised under the care of his grandfather, Abd al-Muttalib, and paternal uncle, Abu Talib. In later years, he would periodically seclude himself in a mountain cave named Hira for several nights of prayer. When he was 40, in, Muhammad reported being visited by Gabriel in the cave and receiving his first revelation from God.

Geographic entities mentioned:
surface_form: Hira
instance_of: Mountain
countries: Saudi Arabia
coordinates: lat: 21.458055555556
lon: 39.861388888889
He then personally secured it within the wall. Beginnings of the Quran. The financial security Muhammad enjoyed from Khadija, his wealthy wife, gave him plenty of free time to spend in solitude in the cave of Hira. According to Islamic tradition, in 610, when he was 40 years old, the angel Gabriel appeared to him during his visit to the cave.

Geographic entities mentioned:
surface_form: cave of Hira
instance_of: Mountain
countries: Saudi Arabia
coordinates: lat: 21.458055555556
lon: 39.861388888889
Led by Abu Sufyan, they assembled an army to oppose Muhammad. Upon being alerted by his scout about the impending threat, Muhammad convened a war council. Initially, he considered defending from the city center, but later decided to meet the enemy in open battle at Mount Uhud, following the insistence of the younger faction of his followers.

Geographic entities mentioned:
surface_form: Mount Uhud
instance_of: Mountain
countries: Saudi Arabia
coordinates: lat: 24.510277777778
lon: 39.613888888889
Upon learning that Mecca had fallen to the Muslims, the Banu Hawazin gathered their entire tribe, including their families, to fight. They are estimated to have around 4,000 warriors. Muhammad led 12,000 soldiers to raid them, but they surprised him at the valley of Hunayn. The Muslims overpowered them and took their women, children and animals.

Geographic entities mentioned:
surface_form: valley of Hunayn
instance_of: Valley
countries: Saudi Arabia
coordinates: lat: 21.4333
lon: 40.35
At this interchange, US 219 continues south along the two-lane road while US 40 heads southeast concurrent with I-68 and US 219 on National Freeway, a four-lane freeway that has a third lane for trucks while climbing hills and mountains. The road curves east and passes through another section of the Savage River State Forest, heading across Negro Mountain.

Geographic entities mentioned:
surface_form: Negro Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.786111111111
lon: -79.175
Past this interchange, the freeway descends the mountain. I-68/US 40 heads east through a mix of farmland and woodland, ascending and descending two hills and crossing the Eastern Continental Divide. Farther east, the freeway curves southeast and comes to an interchange with MD 546 in Finzel. Following this, the road heads across forested Savage Mountain. Allegany County.

Geographic entities mentioned:
surface_form: Savage Mountain
instance_of: Landform
countries: United States
coordinates: lat: 39.8864
lon: -78.7361
I-68/US 40 continues east-northeast and descends a hill, passing over Spruce Hollow and MD 55 to the south of Clarysville. The median of the road widens and it heads across forested Dans Mountain, with US 40 Alt. parallel a short distance to the north in the Braddock Run valley. After crossing Dans Mountain, the freeway leaves the Allegheny Mountains.

Geographic entities mentioned:
surface_form: Dans Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.5818
lon: -78.8972
From here, the freeway runs along the north bank of the North Branch Potomac River and curves northeast through developed areas, coming to an eastbound right-out interchange with Johnson Street and a westbound right-in/right-out interchange with Beall Street that serves Cumberland along with Ridgeley, West Virginia across the river.

Geographic entities mentioned:
surface_form: North Branch Potomac River
instance_of: Watercourse
countries: United States
coordinates: lat: 39.5284255
lon: -78.5875141
From here, the I-68/US 40 descends the ridge, turning to the southeast and east as it runs through a mix of farmland and woodland closely parallel to MD 144. The freeway reaches an interchange connecting to MD 144 in Flintstone. From here, the road heads across Polish Mountain, curving southeast. I-68/US 40 turns east and continues through the Green Ridge State Forest parallel to MD 144.

Geographic entities mentioned:
surface_form: Polish Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6961
lon: -78.5247
US 40 Scenic splits from the freeway at an eastbound exit and westbound entrance with Mountain Road (MD 903). Past this interchange, I-68/US 40 turns east and passes through a massive deep cut in Sideling Hill, where the freeway curves southeast and begins to descend the hill.

Geographic entities mentioned:
surface_form: Sideling Hill
instance_of: Mountain
countries: United States
coordinates: lat: 39.7192
lon: -78.2836
Following this, the freeway continues southeast, passing an eastbound runaway truck ramp, before it comes to a diamond interchange with the eastern terminus of US 40 Scenic and the western terminus of a section of MD 144, where it turns northeast. The road curves east and crosses through a gap in Tonoloway Ridge as it continues through forested areas with some farm fields.

Geographic entities mentioned:
surface_form: Tonoloway Ridge
instance_of: Mountain
countries: United States
coordinates: lat: 39.571666666667
lon: -78.325555555556
At the summit of Fairview Mountain, MD 739A loops to the south of the route. After crossing the mountain, the road turns east and enters the Hagerstown Valley, where it passes farm fields before entering the town of Clear Spring. In Clear Spring, the route becomes Cumberland Street and is lined with homes and some businesses, coming to a junction with the western terminus of MD 68.

Geographic entities mentioned:
surface_form: Hagerstown Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.4397
lon: -77.7547
The road continues into the Middletown Valley and passes through a mix of farmland, woodland, and some residential and commercial development along a straight alignment. The route passes along the northeast border of the town of Myersville and comes to an intersection with MD 17. From here, US 40 continues southeast through agricultural land with some woods and development.

Geographic entities mentioned:
surface_form: Middletown Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.43
lon: -77.53
The route passes along the northeast border of the town of Myersville and comes to an intersection with MD 17. From here, US 40 continues southeast through agricultural land with some woods and development. Farther southeast, the road leaves the Middletown Valley and ascends forested Catoctin Mountain, passing south of Gambrill State Park and north of the community of Arch Bridge.

Geographic entities mentioned:
surface_form: Catoctin Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
Mitragyna rubrostipulata. &quot;Mitragyna rubrostipulata&quot; is a tree indigenous to East Africa. It is native from Ethiopia through east-central tropical Africa (Burundi, Kenya, Malawi, Rwanda, Tanzania, Uganda and Zaire) to Mozambique. It grows in wet forests up to 2,000 m above sea level and is abundant in swamp forests along Lake Victoria. Description.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
To win over the Dakotas, he directed his traders to go back to awarding credit and giving gifts liberally to reinforce their kinship ties, even if they resulted in short-term losses. To win over the mixed-blood community, he promised to lobby for the sale of the &quot;half-breed tract&quot; along Lake Pepin, granted to them in the 1830 Treaty of Prairie du Chien.

Geographic entities mentioned:
surface_form: Lake Pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
Haseolsan. Haseolsan is a mountain of South Korea. It has an elevation of 1,027 metres.

Geographic entities mentioned:
surface_form: haseolsan
instance_of: Mountain
countries: South Korea
Simon. It is a one-story, five-bay, steel-frame building clad in yellow/buff-colored brick on a raised foundation executed in the Colonial Revival style. The interior features a 1939 mural by artist Musa McKim titled &quot;Spanish Hill and the Early Inhabitants of the Vicinity.&quot;
It was listed on the National Register of Historic Places in 1988.

Geographic entities mentioned:
surface_form: Spanish Hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.9959
lon: -76.5494
Mount Sodom. Mount Sodom (, &quot;Har Sedom&quot;) is a hill along the southwestern part of the Dead Sea in Israel; it is part of the Judaean Desert Nature Reserve. It takes its name from the biblical city of Sodom, whose destruction is the subject of a narrative in the Bible. History. Mount Sodom began its rise hundreds of thousands of years ago and continues to grow taller at a rate of a year.

Geographic entities mentioned:
surface_form: mount sodom
instance_of: Mountain
countries: Israel
coordinates: lat: 31.092222222222
lon: 35.382777777778
surface_form: sodom
instance_of: Mountain
countries: Israel
coordinates: lat: 31.092222222222
lon: 35.382777777778
Mount Sodom. Mount Sodom (, &quot;Har Sedom&quot;) is a hill along the southwestern part of the Dead Sea in Israel; it is part of the Judaean Desert Nature Reserve. It takes its name from the biblical city of Sodom, whose destruction is the subject of a narrative in the Bible. History. Mount Sodom began its rise hundreds of thousands of years ago and continues to grow taller at a rate of a year.

Geographic entities mentioned:
surface_form: mount sodom
instance_of: Mountain
countries: Israel
coordinates: lat: 31.092222222222
lon: 35.382777777778
surface_form: sodom
instance_of: Mountain
countries: Israel
coordinates: lat: 31.092222222222
lon: 35.382777777778
surface_form: har sedom
instance_of: Mountain
countries: Israel
coordinates: lat: 31.092222222222
lon: 35.382777777778