Sarmila/GeoWiki-Features huggingface dataset:
Average yearly temperatures at Malha range between. The Meidob volcanic field lies at the southern margin of the Sahara to the Sahel, with precipitation at Malha amounting to mostly during summer months. During the early Holocene between 6,000 and 12,000 years ago, precipitation was considerably higher and orographic precipitation in the Meidob area may have supplied water to their surroundings.

Geographic entities mentioned:
surface_form: meidob
instance_of: Mountain
countries: Sudan
coordinates: lat: 15.316666666667
lon: 26.466666666667
These legends may reflect recent volcanic activity. Non-volcanic history. Apart from volcanism, aeolian processes and water erosion were active in Meidob, producing widespread sedimentary covers especially at the margins of the field. A number of wadis extend radially away from the centre of the Meidob volcanic field and carry water during flash floods, transporting sediment and floating pumice.

Geographic entities mentioned:
surface_form: meidob
instance_of: Mountain
countries: Sudan
coordinates: lat: 15.316666666667
lon: 26.466666666667
The Owyhee Mountains are a mountain range in Owyhee County, Idaho and Malheur County, Oregon. Mahogany Mountain and the associated volcanic craters of the Lake Owyhee volcanic field are in the Owyhee Mountains of Oregon just east of the Owyhee Reservoir on the Owyhee River. The southeastern end of the range including the old mining area west of Silver City is referred to as the Silver City Range.

Geographic entities mentioned:
surface_form: Mahogany Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.235
lon: -117.256
Pigi Athinas. The Pigi Athinas (Greek Πηγή Αθηνάς, Source of Athena) is an archaeological site at the eastern foot of Mount Olympus (Lower Olympus), near the village of Platamonas. History. There is evidence of the presence of humans since the first half of the 7th millennium BC (Early Neolithic period).

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
The plants are endemic to the alkali soils of the local occasionally flooded salt pan. Much of the land in the San Joaquin Valley was claimed and altered for agriculture and the water table dropped, making conditions too dry for reproduction of many species, including this &quot;Atriplex&quot;.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Starting from the coastal baseline, mathematicians and geographers triangulated vast distances across the country. One of the key achievements was measuring the height of Himalayan mountains, and determining that Mount Everest is the highest point on Earth. Historical use for multiplication.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Bridge Mountain (Utah). Bridge Mountain is a mountain made of Navajo Sandstone in Zion National Park in Washington County, of southwest Utah, United States. Description. Bridge Mountain is located east of the park headquarters near the south entrance to Zion Canyon. Bridge Mountain was once originally named Crawford Mountain after the Crawford family who were early Mormon settlers in the canyon.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: navajo
instance_of: Mountain
countries: United States
coordinates: lat: 37.034169444444
lon: -110.86888888889
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1355235
lon: -115.4905643
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.20554
lon: -112.96605
To avoid confusion, the National Park Service eventually named the span Crawford Arch. Precipitation runoff from the mountain drains into tributaries of the North Fork Virgin River. This mountain is composed of Navajo Sandstone, with a red shale outcropping of the Kayenta Formation exposed along the lower slopes. Climate. Spring and fall are the most favorable seasons to visit Bridge Mountain.

Geographic entities mentioned:
surface_form: navajo
instance_of: Mountain
countries: United States
coordinates: lat: 37.034169444444
lon: -110.86888888889
Bridge Mountain (Utah). Bridge Mountain is a mountain made of Navajo Sandstone in Zion National Park in Washington County, of southwest Utah, United States. Description. Bridge Mountain is located east of the park headquarters near the south entrance to Zion Canyon. Bridge Mountain was once originally named Crawford Mountain after the Crawford family who were early Mormon settlers in the canyon.

Geographic entities mentioned:
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1355235
lon: -115.4905643
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.20554
lon: -112.96605
Description. Bridge Mountain is located east of the park headquarters near the south entrance to Zion Canyon. Bridge Mountain was once originally named Crawford Mountain after the Crawford family who were early Mormon settlers in the canyon. But the name was officially changed to Bridge Mountain in 1934 when a natural bridge was discovered on Bridge Mountain.

Geographic entities mentioned:
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1355235
lon: -115.4905643
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.20554
lon: -112.96605
Bridge Mountain is located east of the park headquarters near the south entrance to Zion Canyon. Bridge Mountain was once originally named Crawford Mountain after the Crawford family who were early Mormon settlers in the canyon. But the name was officially changed to Bridge Mountain in 1934 when a natural bridge was discovered on Bridge Mountain. However, it was not a bridge, but a natural arch.

Geographic entities mentioned:
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1355235
lon: -115.4905643
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1355235
lon: -115.4905643
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.20554
lon: -112.96605
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.20554
lon: -112.96605
Climate. Spring and fall are the most favorable seasons to visit Bridge Mountain. According to the Köppen climate classification system, it is located in a Cold semi-arid climate zone, which is defined by the coldest month having an average mean temperature below 32 °F (0 °C), and at least 50% of the total annual precipitation being received during the spring and summer.

Geographic entities mentioned:
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1355235
lon: -115.4905643
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.20554
lon: -112.96605
Dragon Peak. Dragon Peak is a mountain summit located in the Athabasca River valley of Jasper National Park, in the Canadian Rockies of Alberta, Canada. Situated southeast of Mount Christie and Brussels Peak, Dragon Peak can be seen from the Icefields Parkway. The first ascent of the mountain was made in 1979 by D. Waterman. Dragon Peak was named in 1921 by Arthur O.

Geographic entities mentioned:
surface_form: Brussels Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.51673
lon: -117.80232
surface_form: mount christie
instance_of: Mountain
countries: Canada
coordinates: lat: 52.53111111111111
lon: -117.81083333333333
surface_form: dragon peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.45003
lon: -117.71901
Dragon Peak. Dragon Peak is a mountain summit located in the Athabasca River valley of Jasper National Park, in the Canadian Rockies of Alberta, Canada. Situated southeast of Mount Christie and Brussels Peak, Dragon Peak can be seen from the Icefields Parkway. The first ascent of the mountain was made in 1979 by D. Waterman. Dragon Peak was named in 1921 by Arthur O.

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
surface_form: dragon peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.45003
lon: -117.71901
Climate. Based on the Köppen climate classification, Dragon Peak is located in a subarctic climate with long, cold, snowy winters, and short mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Dragon Peak drains into Fryatt Creek and Luck Creek, both tributaries of the Athabasca River.

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: dragon peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.45003
lon: -117.71901
Dragon Peak. Dragon Peak is a mountain summit located in the Athabasca River valley of Jasper National Park, in the Canadian Rockies of Alberta, Canada. Situated southeast of Mount Christie and Brussels Peak, Dragon Peak can be seen from the Icefields Parkway. The first ascent of the mountain was made in 1979 by D. Waterman. Dragon Peak was named in 1921 by Arthur O.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Waterman. Dragon Peak was named in 1921 by Arthur O. Wheeler on account of a dragon-shaped rock formation. The mountain's name was officially adopted in 1935 by the Geographical Names Board of Canada. __NOTOC__
Geology. Dragon Peak is composed of sedimentary rock laid down from the Precambrian to Jurassic periods, then pushed east and over the top of younger rock during the Laramide orogeny.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Dragon Peak. Dragon Peak is a mountain summit located in the Athabasca River valley of Jasper National Park, in the Canadian Rockies of Alberta, Canada. Situated southeast of Mount Christie and Brussels Peak, Dragon Peak can be seen from the Icefields Parkway. The first ascent of the mountain was made in 1979 by D. Waterman. Dragon Peak was named in 1921 by Arthur O.

Geographic entities mentioned:
surface_form: dragon peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.45003
lon: -117.71901
Situated southeast of Mount Christie and Brussels Peak, Dragon Peak can be seen from the Icefields Parkway. The first ascent of the mountain was made in 1979 by D. Waterman. Dragon Peak was named in 1921 by Arthur O. Wheeler on account of a dragon-shaped rock formation. The mountain's name was officially adopted in 1935 by the Geographical Names Board of Canada. __NOTOC__
Geology.

Geographic entities mentioned:
surface_form: dragon peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.45003
lon: -117.71901
Dragon Peak was named in 1921 by Arthur O. Wheeler on account of a dragon-shaped rock formation. The mountain's name was officially adopted in 1935 by the Geographical Names Board of Canada. __NOTOC__
Geology. Dragon Peak is composed of sedimentary rock laid down from the Precambrian to Jurassic periods, then pushed east and over the top of younger rock during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: dragon peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.45003
lon: -117.71901
Climate. Based on the Köppen climate classification, Dragon Peak is located in a subarctic climate with long, cold, snowy winters, and short mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Dragon Peak drains into Fryatt Creek and Luck Creek, both tributaries of the Athabasca River.

Geographic entities mentioned:
surface_form: dragon peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.45003
lon: -117.71901
In the sixth season's sixth episode, &quot;Welcome to the Doll House,&quot; it's revealed that throughout history Third Street held various other names, aside from the aforementioned &quot;Sores and Boils Alley,&quot; including &quot;Constabulary Road,&quot; &quot;Crusty Bulge,&quot; and a Nipmuc name, &quot;Chargogagogmanchogagogcharbunagunggamog.&quot; The Nipmuc name is said to mean, &quot;You fish on your side of the lake, I'll fish on my side, and no one will fish in the middle.&quot; According to Kirk Gleason, it could also mean &quot;Buffalo.&quot; This place-name is based on the local name for a lake in Webster, Massachusetts, which is more formally known as Webster Lake.

Geographic entities mentioned:
surface_form: Webster Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.0425
lon: -71.843333333333
The distribution of the plant extends from Jibberding in the north west to around Lake Grace and Lake Magenta in the south east out to around Clear Streak Well in the east.

Geographic entities mentioned:
surface_form: Lake Magenta
instance_of: Lake
countries: Australia
coordinates: lat: -33.441111111111
lon: 119.18361111111
Bombardment of Fort San Carlos. The Bombardment of Fort San Carlos occurred during the Venezuelan Crisis on January 17, 1903, when two warships of the Imperial German Navy tried to penetrate into Lake Maracaibo but were repulsed by the garrison of Fort San Carlos de la Barra after a brief exchange of fire. Bombardment.

Geographic entities mentioned:
surface_form: Lake Maracaibo
instance_of: Lake
countries: Venezuela
coordinates: lat: 9.8158333333333
lon: -71.556666666667
Geography. The landscape consists of rolling terrain, rocky hills, plains, and salt-encrusted lake beds. Ephemeral salt lakes, including Lake Torrens, Lake Gairdner, Lake Macfarlane, Lake Everard, Lake Gilles, Lake Harris, and Lake Acraman, cover extensive areas. The Gawler Ranges lie in the southwestern portion of the bioregion. The Flinders Ranges bound the bioregion to the east.

Geographic entities mentioned:
surface_form: Lake Gairdner
instance_of: Lake
countries: Australia
coordinates: lat: -31.566666666667
lon: 136
Like so many Himalayan ecosystems the pine forests are split by the deep Kali Gandaki Gorge in Nepal, to the west of which the forest is slightly drier while it is wetter and thicker to the east where the monsoon rains coming off the Bay of Bengal bring more moisture. Flora. There is also a ground cover of thick grass, as regular fires do not allow a shrubby undergrowth to establish itself.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The Niklas storm was preceded by the low pressure named Mike by the Free University of Berlin, which brought hurricane strength winds to Germany on 30 March. Gust reports from this low pressure at the high-altitude stations of Brocken were of (force 12) and Zugspitze. The Niklas storm began to develop on 29 March off the Newfoundland coast.

Geographic entities mentioned:
surface_form: Brocken
instance_of: Mountain
countries: Germany
Kingdom of Prussia
coordinates: lat: 51.800555555556
lon: 10.617222222222
surface_form: Zugspitze
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.421217
lon: 10.986314
The storm field drew across Western Europe on 30 and 31 March 2015, reaching the Netherlands and large areas of Germany on 31 March 2015. Hurricane-force winds were reported in Germany, according to the German Weather service (DWD) with a peak gust at altitude on the mountains of Zugspitze (), the Brocken (), Feldberg in the Black Forest () and on Weinbiet in Neustadt ().

Geographic entities mentioned:
surface_form: Zugspitze
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.421217
lon: 10.986314
surface_form: Brocken
instance_of: Mountain
countries: Germany
Kingdom of Prussia
coordinates: lat: 51.800555555556
lon: 10.617222222222
surface_form: Weinbiet
instance_of: Mountain
countries: Germany
coordinates: lat: 49.376111111111
lon: 8.1208333333333
In the southern half of Germany the Niklas storm was stronger than either of these two winter storms. Cyclone Niklas is regarded as being not quite as strong in Germany as the Kyrill storm which had a slightly higher peak gust speed and longer duration. MeteoSwiss reported that in March winds over would be expected to recur on the Swiss Plateau approximately once every four years.

Geographic entities mentioned:
surface_form: Swiss Plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
In the Swiss lowlands such a wind event occurs about once in every two years, though locally, there were gusts which only occur at that location once every 5 to 6 years, for example at Affoltern, Zürich. In the Swiss mountains a gust of was measured on Säntis, which occurs approximately every 1 to 2 years, and on Mount Pilatus a gust of was recorded, which is expected about every 4 to 5 years.

Geographic entities mentioned:
surface_form: Säntis
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.249167
lon: 9.343333
Switzerland. In Switzerland preventative closure of railway lines, cable cars and upland areas taken out in preparation for the storm. Crap Masegn, Graubünden, with a peak of in the Alps, though even at lower elevations with gusts of recorded in Zürich. Zürich Airport was severely affected. One death related to the storm occurred in Switzerland. Elsewhere.

Geographic entities mentioned:
surface_form: Crap Masegn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.850361111111
lon: 9.1711111111111
History. Torch Lake was originally formed at the end of the Last Glacial Period, along with neighboring Lake Michigan. Receding glaciers carved the surface of the Earth, and melting glaciers filled the new basins, which are now known as the Great Lakes. Torch Lake (along with other long lakes in the region like Lake Leelanau and Elk Lake) were originally bays of the young Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: torch lake
instance_of: Lake
countries: United States
coordinates: lat: 47.1583
lon: -88.425
surface_form: torch lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9833
lon: -85.3083
Receding glaciers carved the surface of the Earth, and melting glaciers filled the new basins, which are now known as the Great Lakes. Torch Lake (along with other long lakes in the region like Lake Leelanau and Elk Lake) were originally bays of the young Lake Michigan. However, sandbars formed at the northern end of these lakes, separating them from Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Leelanau
instance_of: Lake
countries: United States
coordinates: lat: 44.85
lon: -85.73187
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: lake michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: torch lake
instance_of: Lake
countries: United States
coordinates: lat: 47.1583
lon: -88.425
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9742
lon: -121.802
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 44.025277777778
lon: -115.07138888889
surface_form: torch lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9833
lon: -85.3083
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 45.919166666667
lon: -95.521944444444
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 45.867222222222
lon: -95.804722222222
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 44.85
lon: -85.3833
surface_form: young lake
instance_of: Lake
countries: United States
coordinates: lat: 42.843888888889
lon: -74.920555555556
The Grass River flows from Lake Bellaire into Clam Lake, which in turn drains into Torch Lake via the short Clam River. Torch Lake itself is drained by the Torch River, which flows into Lake Skegemog, which opens into Elk Lake. Elk Lake flows into the east arm of Grand Traverse Bay at Elk Rapids. This watershed is popularly known as the Chain of Lakes.

Geographic entities mentioned:
surface_form: Lake Skegemog
instance_of: Lake
countries: United States
coordinates: lat: 44.810841
lon: -85.325982
surface_form: lake skegemog
instance_of: Lake
countries: United States
coordinates: lat: 44.810841
lon: -85.325982
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9742
lon: -121.802
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9742
lon: -121.802
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 44.025277777778
lon: -115.07138888889
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 44.025277777778
lon: -115.07138888889
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 45.919166666667
lon: -95.521944444444
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 45.919166666667
lon: -95.521944444444
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 45.867222222222
lon: -95.804722222222
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 45.867222222222
lon: -95.804722222222
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 44.85
lon: -85.3833
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 44.85
lon: -85.3833
Geography. Torch Lake is part of a watershed that begins in northern Antrim County with Six Mile Lake, which is connected by the Intermediate River with Lake Bellaire. The Grass River flows from Lake Bellaire into Clam Lake, which in turn drains into Torch Lake via the short Clam River. Torch Lake itself is drained by the Torch River, which flows into Lake Skegemog, which opens into Elk Lake.

Geographic entities mentioned:
surface_form: six mile lake
instance_of: Lake
countries: United States
coordinates: lat: 59.980833333333
lon: -154.80333333333
Torch Lake (Antrim County, Michigan). Torch Lake is a lake in the Northern Lower Peninsula of the U.S. state of Michigan. At long, it is Michigan's longest inland lake, and at approximately 29.3 mi2 (76 km2), it is Michigan's second largest inland lake, after Houghton Lake.

Geographic entities mentioned:
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: torch lake
instance_of: Lake
countries: United States
coordinates: lat: 47.1583
lon: -88.425
surface_form: torch lake (antrim county, michigan)
instance_of: Lake
countries: United States
coordinates: lat: 44.9833
lon: -85.3083
Torch Lake (Antrim County, Michigan). Torch Lake is a lake in the Northern Lower Peninsula of the U.S. state of Michigan. At long, it is Michigan's longest inland lake, and at approximately 29.3 mi2 (76 km2), it is Michigan's second largest inland lake, after Houghton Lake.

Geographic entities mentioned:
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: torch lake
instance_of: Lake
countries: United States
coordinates: lat: 47.1583
lon: -88.425
surface_form: torch lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9833
lon: -85.3083
Torch Lake is a lake in the Northern Lower Peninsula of the U.S. state of Michigan. At long, it is Michigan's longest inland lake, and at approximately 29.3 mi2 (76 km2), it is Michigan's second largest inland lake, after Houghton Lake. It has a maximum depth of and an average depth of, making it Michigan's deepest inland lake, as well as the state's largest by volume.

Geographic entities mentioned:
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: houghton lake
instance_of: Lake
countries: United States
coordinates: lat: 44.338888888889
lon: -84.725
Torch Lake is a lake in the Northern Lower Peninsula of the U.S. state of Michigan. At long, it is Michigan's longest inland lake, and at approximately 29.3 mi2 (76 km2), it is Michigan's second largest inland lake, after Houghton Lake. It has a maximum depth of and an average depth of, making it Michigan's deepest inland lake, as well as the state's largest by volume.

Geographic entities mentioned:
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Receding glaciers carved the surface of the Earth, and melting glaciers filled the new basins, which are now known as the Great Lakes. Torch Lake (along with other long lakes in the region like Lake Leelanau and Elk Lake) were originally bays of the young Lake Michigan. However, sandbars formed at the northern end of these lakes, separating them from Lake Michigan.

Geographic entities mentioned:
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: lake michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
It has a maximum depth of and an average depth of, making it Michigan's deepest inland lake, as well as the state's largest by volume. Surrounding it are several townships including Torch Lake, Central Lake, Forest Home, Helena, and Milton in Antrim County, and Clearwater Township of neighboring Kalkaska County.

Geographic entities mentioned:
surface_form: torch lake
instance_of: Lake
countries: United States
coordinates: lat: 47.1583
lon: -88.425
surface_form: torch lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9833
lon: -85.3083
Surrounding it are several townships including Torch Lake, Central Lake, Forest Home, Helena, and Milton in Antrim County, and Clearwater Township of neighboring Kalkaska County. Several villages and hamlets lie along its shore, including Alden, Eastport, Clam River, Torch Lake, and Torch River.

Geographic entities mentioned:
surface_form: torch lake
instance_of: Lake
countries: United States
coordinates: lat: 47.1583
lon: -88.425
surface_form: torch lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9833
lon: -85.3083
Geography. Torch Lake is part of a watershed that begins in northern Antrim County with Six Mile Lake, which is connected by the Intermediate River with Lake Bellaire. The Grass River flows from Lake Bellaire into Clam Lake, which in turn drains into Torch Lake via the short Clam River. Torch Lake itself is drained by the Torch River, which flows into Lake Skegemog, which opens into Elk Lake.

Geographic entities mentioned:
surface_form: torch lake
instance_of: Lake
countries: United States
coordinates: lat: 47.1583
lon: -88.425
surface_form: torch lake
instance_of: Lake
countries: United States
coordinates: lat: 47.1583
lon: -88.425
surface_form: torch lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9833
lon: -85.3083
surface_form: torch lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9833
lon: -85.3083
surface_form: clam lake
instance_of: Lake
countries: United States
coordinates: lat: 42.671944444444
lon: -83.397222222222
This quality has made the lake a popular spot for the development of resorts and vacation homes. At the south end of the lake is a sandbar, locally known as the Torch Lake Sandbar. This sandbar is a popular summer tourist destination, especially around the Fourth of July.

Geographic entities mentioned:
surface_form: torch lake
instance_of: Lake
countries: United States
coordinates: lat: 47.1583
lon: -88.425
surface_form: torch lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9833
lon: -85.3083
Torch Lake itself is drained by the Torch River, which flows into Lake Skegemog, which opens into Elk Lake. Elk Lake flows into the east arm of Grand Traverse Bay at Elk Rapids. This watershed is popularly known as the Chain of Lakes. The lake itself is entirely within Antrim County. However, the southern shore of the lake serves as part of the actual border between Antrim and Kalkaska counties.

Geographic entities mentioned:
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
The name of the lake is not due to its shape, rather, is derived from translation from the Ojibwe name &quot;waaswaaganing&quot; meaning &quot;Place of Torches&quot; or &quot;Place of Flames&quot;, referring to the practice of the local Native American population who once used torches at night to attract fish for harvesting with spears and nets (Lac du Flambeau in Wisconsin is named after the same Ojibwa term).

Geographic entities mentioned:
surface_form: lac du flambeau
instance_of: Lake
countries: United States
coordinates: lat: 45.9646001
lon: -89.9237414
Additional studies in Lake Malawi in East Africa show significant amounts of ash deposited by the Toba Caldera eruptions, despite a great distance from the area, but these studies offer little indication of a significant climatic effect in East Africa.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Athletics. During the Second World War, Toronto HMCS &quot;York&quot; fielded a football team in the Ontario Rugby Football Union (ORFU). Some of the notable players and coaches associated with the team were: Royal Copeland, Steve Karrys, Bob Stewart and the coach Teddy Morris. Facilities. Although located on the Lake Ontario shoreline, York has no facilities for naval ships.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Canoeing at the 1968 Summer Olympics. At the 1968 Summer Olympics in Mexico City, seven events in sprint canoe racing were contested. The program was unchanged from the previous Games in 1964. Lake Xochimilco was where the events took place.

Geographic entities mentioned:
surface_form: Lake Xochimilco
instance_of: Lake
countries: Mexico
coordinates: lat: 19.285
lon: -99.102
Settings. The setting is always a echoing with fractured French. They include Paris in the springtime, the Matterhorn, or the little village of N'est-ce Pas in the French Alps. The exotic locales, such as Algiers, are drawn from the story of the 1937 film &quot;Pépé le Moko&quot;.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
Amisk Lake was on an important fur trade route in the 18th century. Forts. Amisk Lake is along the course of the Sturgeon-Weir River, an important part of the canoe route from eastern Canada to the rich Lake Athabasca country. There was an independent trading post on Amisk Lake (Beaver Lake) in 1775 and a Hudson's Bay Company trading post in 1776. Frobisher-Henry Fort.

Geographic entities mentioned:
surface_form: Lake Athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
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: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.583333333333336
lon: -102.25027777777778
surface_form: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.59315
lon: -112.63699
On Lake Winnipeg, he was joined by Peter Pond, Joseph Frobisher, and Thomas Frobisher. From the new Hudson's Bay Company post at Cumberland Lake, Henry and the two Frobishers went north up the Sturgeon-Weir hoping to reach Frog Portage where Thomas had traded successfully the previous year. They crossed Amisk Lake on 1 November and the next morning it was frozen over.

Geographic entities mentioned:
surface_form: Cumberland Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05
lon: -102.3
Forts. Amisk Lake is along the course of the Sturgeon-Weir River, an important part of the canoe route from eastern Canada to the rich Lake Athabasca country. There was an independent trading post on Amisk Lake (Beaver Lake) in 1775 and a Hudson's Bay Company trading post in 1776. Frobisher-Henry Fort. In June 1775, Alexander Henry the elder left Montreal with 16 canoes and goods worth £3,000.

Geographic entities mentioned:
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.7183
lon: -60.5103
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.4987
lon: -73.59742
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.7058
lon: -111.816
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.0001
lon: -66.1432
surface_form: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.583333333333336
lon: -102.25027777777778
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8333
lon: -102.301
surface_form: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.59315
lon: -112.63699
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.351
lon: -62.496
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 43.8191
lon: -65.5396
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.2596
lon: -65.2402
Forts. Amisk Lake is along the course of the Sturgeon-Weir River, an important part of the canoe route from eastern Canada to the rich Lake Athabasca country. There was an independent trading post on Amisk Lake (Beaver Lake) in 1775 and a Hudson's Bay Company trading post in 1776. Frobisher-Henry Fort. In June 1775, Alexander Henry the elder left Montreal with 16 canoes and goods worth £3,000.

Geographic entities mentioned:
surface_form: frobisher
instance_of: Lake
countries: Canada
coordinates: lat: 56.36225
lon: -108.27592
In June 1775, Alexander Henry the elder left Montreal with 16 canoes and goods worth £3,000. On Lake Winnipeg, he was joined by Peter Pond, Joseph Frobisher, and Thomas Frobisher. From the new Hudson's Bay Company post at Cumberland Lake, Henry and the two Frobishers went north up the Sturgeon-Weir hoping to reach Frog Portage where Thomas had traded successfully the previous year.

Geographic entities mentioned:
surface_form: frobisher
instance_of: Lake
countries: Canada
coordinates: lat: 56.36225
lon: -108.27592
surface_form: frobisher
instance_of: Lake
countries: Canada
coordinates: lat: 56.36225
lon: -108.27592
surface_form: peter pond
instance_of: Lake
countries: Canada
coordinates: lat: 56.00918
lon: -108.86918
surface_form: lake winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
surface_form: winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
On 1 January, Henry set out on foot and spent three months visiting the Indians. Next spring they went north to Frog Portage and were successful in trade. Joseph Frobisher maintained the post of Amisk Lake until it was abandoned in 1778. Amisk Lake Recreation Site. Amisk Lake Recreation Site () is a provincial recreation site on the eastern shore of Amisk Lake.

Geographic entities mentioned:
surface_form: frobisher
instance_of: Lake
countries: Canada
coordinates: lat: 56.36225
lon: -108.27592
surface_form: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.583333333333336
lon: -102.25027777777778
surface_form: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.59315
lon: -112.63699
Amisk Lake. Amisk Lake is a lake in the east-central part of the Canadian province of Saskatchewan, about south-west of Flin Flon, Manitoba. 'Amisk' means beaver in Cree. Along the lake's shores is the community of Denare Beach, a provincial recreation site with lake access and camping, and prehistoric limestone crevices. Access to the lake and its amenities is from Highway 167.

Geographic entities mentioned:
surface_form: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.583333333333336
lon: -102.25027777777778
surface_form: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.59315
lon: -112.63699
Amisk Lake. Amisk Lake is a lake in the east-central part of the Canadian province of Saskatchewan, about south-west of Flin Flon, Manitoba. 'Amisk' means beaver in Cree. Along the lake's shores is the community of Denare Beach, a provincial recreation site with lake access and camping, and prehistoric limestone crevices. Access to the lake and its amenities is from Highway 167.

Geographic entities mentioned:
surface_form: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.583333333333336
lon: -102.25027777777778
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.59315
lon: -112.63699
'Amisk' means beaver in Cree. Along the lake's shores is the community of Denare Beach, a provincial recreation site with lake access and camping, and prehistoric limestone crevices. Access to the lake and its amenities is from Highway 167. Amisk Lake was on an important fur trade route in the 18th century. Forts.

Geographic entities mentioned:
surface_form: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.583333333333336
lon: -102.25027777777778
surface_form: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.59315
lon: -112.63699
From the new Hudson's Bay Company post at Cumberland Lake, Henry and the two Frobishers went north up the Sturgeon-Weir hoping to reach Frog Portage where Thomas had traded successfully the previous year. They crossed Amisk Lake on 1 November and the next morning it was frozen over. Since there was good fishing they stopped at the mouth of the West Weir and built a fort.

Geographic entities mentioned:
surface_form: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.583333333333336
lon: -102.25027777777778
surface_form: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.59315
lon: -112.63699
Next spring they went north to Frog Portage and were successful in trade. Joseph Frobisher maintained the post of Amisk Lake until it was abandoned in 1778. Amisk Lake Recreation Site. Amisk Lake Recreation Site () is a provincial recreation site on the eastern shore of Amisk Lake. The park is divided into two sections.

Geographic entities mentioned:
surface_form: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.583333333333336
lon: -102.25027777777778
surface_form: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.59315
lon: -112.63699
Joseph Frobisher maintained the post of Amisk Lake until it was abandoned in 1778. Amisk Lake Recreation Site. Amisk Lake Recreation Site () is a provincial recreation site on the eastern shore of Amisk Lake. The park is divided into two sections. The Sand Beach campground is located at the south-east corner of the lake and has a campground with 12 campsites and lake access.

Geographic entities mentioned:
surface_form: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.583333333333336
lon: -102.25027777777778
surface_form: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.583333333333336
lon: -102.25027777777778
surface_form: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.59315
lon: -112.63699
surface_form: amisk lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.59315
lon: -112.63699
There was an independent trading post on Amisk Lake (Beaver Lake) in 1775 and a Hudson's Bay Company trading post in 1776. Frobisher-Henry Fort. In June 1775, Alexander Henry the elder left Montreal with 16 canoes and goods worth £3,000. On Lake Winnipeg, he was joined by Peter Pond, Joseph Frobisher, and Thomas Frobisher.

Geographic entities mentioned:
surface_form: montreal
instance_of: Lake
countries: Canada
coordinates: lat: 54.3333
lon: -105.667
Some episodes feature anachronistic technology whereby Murdoch sometimes uses the existing technology of his time to improvise a crude prototype of a technology that would be more readily recognizable to the show's 21st century audience. In one episode, for instance, he creates a primitive version of sonar to locate a sunken ship in Lake Ontario.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
decreased. Illegal entry through the Mexican border became the way of entering the country for Punjabi immigrants. California's Imperial Valley had a large population of Punjabis who assisted these immigrants and provided support. Immigrants were able to blend in with this relatively homogeneous population.

Geographic entities mentioned:
surface_form: California's Imperial Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.1
lon: -115.5
Worth, Detroit, Houston, Los Angeles, Philadelphia, Phoenix, Raleigh, San Francisco–San Jose–Oakland, and Seattle. The three oldest Indian American communities going back to around 1910 are in lesser populated agricultural areas in California including Stockton and Yuba City in the Central Valley, as well as in the Imperial Valley. These were all primarily Sikh settlements. U.S.

Geographic entities mentioned:
surface_form: Imperial Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.1
lon: -115.5
Geography. The small town of Colchester lies about 40 kilometres north-east of Port Elizabeth (since 2021 renamed Gqeberha). It also lies on the N2 about 20 minutes from Port Elizabeth and an hour from Makhanda. It lies on the banks of the Sundays River and the south-eastern border of the Sundays River Valley region.

Geographic entities mentioned:
surface_form: Sundays River Valley
instance_of: Valley
countries: South Africa
coordinates: lat: -33.4
lon: 25.4333
To the southeast the range merges into the Pavant Range also part of the Fishlake National Forest; between the two, Interstate 15 traverses northeast to Scipio and then further to Nephi, Utah. The highpoint of the range is Fool Creek Peak, at, lying on the two county borders, but slightly east of the range's center (1.5 mi). North range terminus: Sevier River.

Geographic entities mentioned:
surface_form: Fool Creek Peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.393055555556
lon: -112.20722222222
North range terminus: Sevier River. The Sevier River enters the northeast Sevier Desert at the northeast, then north of the range, with the south border of the Gilson Mountains. The Sevier River makes its final exit from the mountains, and valleys associated with the western flank of the Wasatch Ranges, as well as the Wasatch and Sevier Plateaus.

Geographic entities mentioned:
surface_form: Wasatch
instance_of: Plateau
countries: United States
coordinates: lat: 39.311666666667
lon: -111.33694444444
The &quot;Belmond Hiram Bingham&quot; is a luxury train operating day return trips from Poroy station outside Cusco to Aguas Calientes, the station for Machu Picchu in Peru. The train, named after Hiram Bingham, who publicized the existence of the Inca citadel of Machu Picchu, travels from the high Andes down the Sacred Valley, and for much of the journey it runs alongside the Urubamba River.

Geographic entities mentioned:
surface_form: Sacred Valley
instance_of: Valley
countries: Peru
coordinates: lat: -13.333333333333
lon: -72.083333333333
It is also a well known song in Japan, by the name (). Lyrics. In the depths of the mountains is white ! Though one or two roots only I pull,
Eunyul Geumsanpo's white ! A root, two roots that I picked up,
in the mountain valley having bumper crop</poem>
Gangwondo Geumgangsan's white ! have such an elegant hand pose.</poem>

Geographic entities mentioned:
surface_form: Geumgangsan
instance_of: Mountain
countries: North Korea
coordinates: lat: 38.656763888889
lon: 128.10490277778
East of the town of Aquia there is a small range called Huaman Hueque (possibly from Quechua &quot;waman&quot; falcon or variable hawk, &quot;wiqi&quot; tear). It is sometimes considered a sub-range of the Huallanca range. The Huaman Hueque range is dominated by Kikash. Lakes. There are numerous mostly small lakes along the range.

Geographic entities mentioned:
surface_form: Kikash
instance_of: Mountain
countries: Peru
coordinates: lat: -10.05444444
lon: -77.1
Amber can be found present as a rare component in plant debris beds in the Wessex formation both on the Isle of Wight and the Isle of Purbeck, however, the only significant concentration and where all of the inclusions have been found is a lag channel in the L6 plant debris horizon just south-east of Chilton Chine.

Geographic entities mentioned:
surface_form: Chilton Chine
instance_of: Valley
countries: United Kingdom
Bypass Nunatak. 9koi02eg9lpyxwn89uwul0bcql2m" xml:space="preserve">Bypass Nunatak () is a nunatak about south of Mount Tritoppen in the David Range of the Framnes Mountains. It was mapped by Norwegian cartographers from air photos taken by the Lars Christensen Expedition (1936–37) and called &quot;Steinen&quot; (the stone).

Geographic entities mentioned:
surface_form: Mount Tritoppen
instance_of: Mountain
coordinates: lat: -67.9833
lon: 62.4833
surface_form: tritoppen
instance_of: Mountain
coordinates: lat: -67.9833
lon: 62.4833
surface_form: bypass nunatak
instance_of: Mountain
coordinates: lat: -68.0167
lon: 62.4667
Bypass Nunatak. 9koi02eg9lpyxwn89uwul0bcql2m" xml:space="preserve">Bypass Nunatak () is a nunatak about south of Mount Tritoppen in the David Range of the Framnes Mountains. It was mapped by Norwegian cartographers from air photos taken by the Lars Christensen Expedition (1936–37) and called &quot;Steinen&quot; (the stone).

Geographic entities mentioned:
surface_form: christensen
instance_of: Mountain
coordinates: lat: -65.1
lon: -59.5167
surface_form: steinen
instance_of: Mountain
coordinates: lat: -68.0167
lon: 62.4667
Bypass Nunatak. 9koi02eg9lpyxwn89uwul0bcql2m" xml:space="preserve">Bypass Nunatak () is a nunatak about south of Mount Tritoppen in the David Range of the Framnes Mountains. It was mapped by Norwegian cartographers from air photos taken by the Lars Christensen Expedition (1936–37) and called &quot;Steinen&quot; (the stone).

Geographic entities mentioned:
surface_form: bypass nunatak
instance_of: Mountain
coordinates: lat: -68.0167
lon: 62.4667
Two sectors can be distinguished, Alto Pisuerga and, although other sub-regions can also be mentioned, such as Fuentes Carrionas, La Pernía, La Braña, Campoo and Valdivia. The highest elevations of the entire Cantabrian mountain range (excluding the Picos de Europa massif) are located here: (2538 m), Curavacas (2524 m) and Espigüete (2450 m).

Geographic entities mentioned:
surface_form: Curavacas
instance_of: Mountain
countries: Spain
coordinates: lat: 42.9792
lon: -4.66833
surface_form: Espigüete
instance_of: Mountain
countries: Spain
coordinates: lat: 42.944722222222225
lon: -4.796111111111111