Sarmila/GeoWiki-Features huggingface dataset:
Mission to Canada. In March 1775, as a member of the Massachusetts Committee of Correspondence, Brown was sent to Montreal by way of Lake Champlain to meet with Canadians interested in joining the other 13 colonies in their dispute with the British government.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Montgomery was killed and Arnold was wounded; Brown's diversion failed. Death at Stone Arabia. Brown was killed in action on his 36th birthday, October 19, 1780, at the Battle of Stone Arabia, on the Mohawk Valley frontier. Notes. Brown died in the battle of Stone Arabia, see New York in the revolution published 1876 and many other sources.

Geographic entities mentioned:
surface_form: Mohawk Valley
instance_of: Valley
countries: United States
Isthmohyla xanthosticta. &quot;Isthmohyla xanthosticta&quot; is a species of frogs in the family Hylidae. It is endemic to Costa Rica and only known from its type locality on the south slope of Volcan Barba in the Heredia Province. Common name south fork treefrog has been coined for it. Description.

Geographic entities mentioned:
surface_form: Volcan Barba
instance_of: Mountain
countries: Costa Rica
coordinates: lat: 10.135
lon: -84.1
They are part of the Bidwell Spring chain and lie within a region that was active in the Quaternary. Formed during the Pleistocene between 25,000 and 15,000 years ago, the volcanoes erupted lava flows that coursed toward the Burney Mountain lava dome. These lava flows cover an area of and are made of basalt and dacite. The volcanoes also erupted cinder and volcanic ash that reached eastward.

Geographic entities mentioned:
surface_form: Burney Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.806666666667
lon: -121.62777777778
However, they are considered to have &quot;low to very low&quot; threat potential for future eruptive activity. Geography. The Twin Buttes are two cinder cone volcanoes that lie north of Lassen Peak in Shasta County, California. The Twin Buttes reach a summit elevation of about. Nearby towns include Burney, Old Station, and Viola.

Geographic entities mentioned:
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
surface_form: lassen peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: twin buttes
instance_of: Mountain
countries: United States
coordinates: lat: 40.7774
lon: -121.5905
Eruptive history. Located in an area that was highly active during the Quaternary, the Twin Buttes volcanoes formed during the late Pleistocene. The North and South Twin Buttes erupted blocky, partially unvegetated lava flows that moved north toward the southeastern base of Burney Mountain, a lava dome, between 25,000 and 15,000 years ago, covering an area of. They have an overall volume of.

Geographic entities mentioned:
surface_form: Burney Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.806666666667
lon: -121.62777777778
surface_form: burney mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.806666666667
lon: -121.62777777778
surface_form: twin buttes
instance_of: Mountain
countries: United States
coordinates: lat: 40.7774
lon: -121.5905
Geology. The Twin Buttes — and other volcanoes near Lassen Peak — are part of the Cascade Volcanic Arc, which was produced by subduction of the oceanic Juan de Fuca tectonic plate under the North American tectonic plate. Volcanic activity in the region is also influenced by the westward expansion of the Basin and Range Province into the Cascades.

Geographic entities mentioned:
surface_form: lassen peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
Cinder and volcanic ash erupted by the Twin Buttes extend to the east. While Twin Buttes last erupted during the late Pleistocene, the area is still monitored by the USGS given its proximity to Lassen Peak. As of 2012, there were three GPS receivers continuously monitoring Twin Buttes for deformation, an indicator of pre-eruptive activity.

Geographic entities mentioned:
surface_form: lassen peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
The Bidwell Spring chain consists of five eruptive units, including the Twin Buttes basalt. 39Ar has placed two other deposits, basaltic andesite from Black Butte and andesite from Bidwell Spring, at 62,000 ± 10,000 years old and 68,000 ± 6,000 years old, respectively. These results suggest several small eruptions between 65,000 and 45,000 years ago from the Bidwell Spring chain.

Geographic entities mentioned:
surface_form: black butte
instance_of: Mountain
countries: United States
coordinates: lat: 44.9044
lon: -111.855
surface_form: black butte
instance_of: Mountain
countries: United States
coordinates: lat: 35.88222222
lon: -115.72083333
surface_form: black butte
instance_of: Mountain
countries: United States
coordinates: lat: 39.7267
lon: -122.872
surface_form: black butte
instance_of: Mountain
countries: United States
coordinates: lat: 41.3663
lon: -122.348
surface_form: black butte
instance_of: Mountain
countries: United States
coordinates: lat: 44.3997
lon: -121.635
Twin Buttes (California). The Twin Buttes are two volcanic cinder cones located in the Cascade Range in Shasta County, California. They are part of the Bidwell Spring chain and lie within a region that was active in the Quaternary. Formed during the Pleistocene between 25,000 and 15,000 years ago, the volcanoes erupted lava flows that coursed toward the Burney Mountain lava dome.

Geographic entities mentioned:
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: twin buttes
instance_of: Mountain
countries: United States
coordinates: lat: 40.7774
lon: -121.5905
Twin Buttes (California). The Twin Buttes are two volcanic cinder cones located in the Cascade Range in Shasta County, California. They are part of the Bidwell Spring chain and lie within a region that was active in the Quaternary. Formed during the Pleistocene between 25,000 and 15,000 years ago, the volcanoes erupted lava flows that coursed toward the Burney Mountain lava dome.

Geographic entities mentioned:
surface_form: twin buttes (california)
instance_of: Mountain
countries: United States
coordinates: lat: 40.7774
lon: -121.5905
These lava flows cover an area of and are made of basalt and dacite. The volcanoes also erupted cinder and volcanic ash that reached eastward. As of 2012, the Twin Buttes were still monitored by the United States Geological Survey for deformation, an indicator of pre-eruptive activity. However, they are considered to have &quot;low to very low&quot; threat potential for future eruptive activity.

Geographic entities mentioned:
surface_form: twin buttes
instance_of: Mountain
countries: United States
coordinates: lat: 40.7774
lon: -121.5905
Volcanic activity during the Quaternary has produced basalt, basaltic andesite, and olivine tholeiite. Other major volcanic centers near the Twin Buttes include the Yana, Maidu, Dittmar, and Latour centers, which were long-lived volcanic systems with magma ranging in composition from andesite to silicic rhyolite; these four systems are now eroded with extinct hydrothermal systems.

Geographic entities mentioned:
surface_form: twin buttes
instance_of: Mountain
countries: United States
coordinates: lat: 40.7774
lon: -121.5905
Other major volcanic centers near the Twin Buttes include the Yana, Maidu, Dittmar, and Latour centers, which were long-lived volcanic systems with magma ranging in composition from andesite to silicic rhyolite; these four systems are now eroded with extinct hydrothermal systems. The Bidwell Spring chain consists of five eruptive units, including the Twin Buttes basalt.

Geographic entities mentioned:
surface_form: twin buttes
instance_of: Mountain
countries: United States
coordinates: lat: 40.7774
lon: -121.5905
Basalt from the Twin Buttes overlies eruptive material from the Poison Lake Chain and the Cone Lake Chain, which are also within the Caribou Volcanic field. Twin Buttes basalt is overlain by basaltic andesite erupted during the late Pleistocene from an unnamed volcanic vent, which is thought to be between 45,000 and 25,000 years old. Subfeatures.

Geographic entities mentioned:
surface_form: twin buttes
instance_of: Mountain
countries: United States
coordinates: lat: 40.7774
lon: -121.5905
surface_form: twin buttes
instance_of: Mountain
countries: United States
coordinates: lat: 40.7774
lon: -121.5905
Subfeatures. Subfeatures of the formation include Red Rock Hill, which has an elevation of. Other nearby features include basaltic andesite and a distinct basalt deposit southeast and northeast of the Twin Buttes, respectively, both of which were produced by eruptive activity between 50,000 and 35,000 years ago. Eruptive history.

Geographic entities mentioned:
surface_form: twin buttes
instance_of: Mountain
countries: United States
coordinates: lat: 40.7774
lon: -121.5905
Eruptive history. Located in an area that was highly active during the Quaternary, the Twin Buttes volcanoes formed during the late Pleistocene. The North and South Twin Buttes erupted blocky, partially unvegetated lava flows that moved north toward the southeastern base of Burney Mountain, a lava dome, between 25,000 and 15,000 years ago, covering an area of. They have an overall volume of.

Geographic entities mentioned:
surface_form: twin buttes
instance_of: Mountain
countries: United States
coordinates: lat: 40.7774
lon: -121.5905
They have an overall volume of. Eruptive material consisted of basalt (including picrite basalt) and dacite. Basalt erupted from Twin Buttes forms part of the Bidwell Spring chain with an 40Ar/39Ar age of about 46,000 ± 3,000 years, covering an area of. The basalt deposit has a total volume of. At the edges, lava flows are steep, with up to of relief.

Geographic entities mentioned:
surface_form: twin buttes
instance_of: Mountain
countries: United States
coordinates: lat: 40.7774
lon: -121.5905
The basalt deposit has a total volume of. At the edges, lava flows are steep, with up to of relief. The lava flows from the Twin Buttes are porphyritic with about 53% silica content; they have vesicular surfaces and dense interiors. Phenocrysts range from; there are also coarse xenoliths of quartz throughout the lava flows. Cinder and volcanic ash erupted by the Twin Buttes extend to the east.

Geographic entities mentioned:
surface_form: twin buttes
instance_of: Mountain
countries: United States
coordinates: lat: 40.7774
lon: -121.5905
Phenocrysts range from; there are also coarse xenoliths of quartz throughout the lava flows. Cinder and volcanic ash erupted by the Twin Buttes extend to the east. While Twin Buttes last erupted during the late Pleistocene, the area is still monitored by the USGS given its proximity to Lassen Peak.

Geographic entities mentioned:
surface_form: twin buttes
instance_of: Mountain
countries: United States
coordinates: lat: 40.7774
lon: -121.5905
surface_form: twin buttes
instance_of: Mountain
countries: United States
coordinates: lat: 40.7774
lon: -121.5905
While Twin Buttes last erupted during the late Pleistocene, the area is still monitored by the USGS given its proximity to Lassen Peak. As of 2012, there were three GPS receivers continuously monitoring Twin Buttes for deformation, an indicator of pre-eruptive activity. In 2014, the USGS considered Twin Buttes to have &quot;low to very low&quot; threat potential for a future eruption.

Geographic entities mentioned:
surface_form: twin buttes
instance_of: Mountain
countries: United States
coordinates: lat: 40.7774
lon: -121.5905
Pullinque Lake. The Pullinque Lake () is one of the &quot;Seven Lakes&quot; in the Panguipulli municipality, southern Chile. The lake is of glacial origin and lies between Calafquén and Panguipulli Lake. Pullinque Hydroelectric Plant is located near the southwestern outflow of the lake.

Geographic entities mentioned:
surface_form: Calafquén
instance_of: Watercourse
countries: Chile
coordinates: lat: -39.52
lon: -72.147222222222
He was elected as bishop in Mumbai and North India Regional Conferences of MCI. He was also director of Methodist Technical Institute, Baroda, also in Gujarat. As bishop, Servand also serves as chairperson of,
He is also Chief Acharya, Sattal Christian Ashram, Sattal, Uttarakhand. On 1 June 2019, he succeeded John Sadananda, CSI as Master of Serampore College (University), Serampore, West Bengal.

Geographic entities mentioned:
surface_form: Sattal
instance_of: Lake
countries: India
coordinates: lat: 29.348055555555554
lon: 79.53194444444445
Laguna de Leche. Laguna de Leche (Spanish for &quot;Milk Lagoon&quot;, also called &quot;Laguna Grande de Morón&quot;) is the largest natural fresh water lake in Cuba. It is located in the wetland of northern Ciego de Ávila Province, north of Morón, and has a total surface of. (The man-made Zaza Reservoir, at, is the largest in-land water surface by area in the country.)
Overview.

Geographic entities mentioned:
surface_form: laguna de leche
instance_of: Lake
countries: Cuba
coordinates: lat: 22.209166666667
lon: -78.621388888889
The Czipott family moved to Sopron, where Czipott studied in the Lutheran Lyceum. By 1847 Czipott studied in Vienna, where he worked as a private teacher. In 1848 Czipott fought in the First Revolution of Vienna. After the revolution he went home and worked as a government official in Kővágóörs, near Balaton. In 1853 Czipott and his mother moved to Vése (Somogy), Czipott's mother died in 1884.

Geographic entities mentioned:
surface_form: Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
Qaqinkura. Qaqinkura (Aymara for wading bird; a South American ibis &quot;(Theristicus)&quot; also spelled &quot;Caquingora&quot;) is a mountain in the eastern extensions of the Cordillera Real in the Andes of Bolivia, about high. It is situated in the La Paz Department, Sud Yungas Province, Irupana Municipality, east of Mururata.

Geographic entities mentioned:
surface_form: Mururata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.530555555556
lon: -67.8275
surface_form: mururata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.530555555556
lon: -67.8275
Qaqinkura. Qaqinkura (Aymara for wading bird; a South American ibis &quot;(Theristicus)&quot; also spelled &quot;Caquingora&quot;) is a mountain in the eastern extensions of the Cordillera Real in the Andes of Bolivia, about high. It is situated in the La Paz Department, Sud Yungas Province, Irupana Municipality, east of Mururata.

Geographic entities mentioned:
surface_form: qaqinkura
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.5197
lon: -67.6383
Geography. Lake City is located in western Erie County at (42.017349, −80.346641). It is bordered to the south by the borough of Girard, to the east and west and partially to the north by Girard Township, and partially to the north by Lake Erie. According to the United States Census Bureau, the borough has a total area of, of which, or 0.47%, is water.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Obadjiwan 15E. Obadjiwan 15E is a First Nations reserve in Algoma District, Ontario. It consists of two non-contiguous parcels of land on Batchewana Bay (Lake Superior), and is one of the reserves of the Batchewana First Nation. History. The land was originally set apart for the Department of Marine and Fisheries to build the Corbeil Point Lighthouse by order in council on 29 May 1874.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The region, an oval basin, lies below the Šar Mountains, at the source, upper stream of the Prizren Bistrica. South of the region between the Prizren mountains and Koritnik mountain, lies the Gora region. It currently includes Sredska, Pousko, Jablanica, Lokvica, Rečane, Živinjane, Planjane, Nebregošte, Manastirica, Stružje, Donje Ljubinje, Gornje Ljubinje, Drajčići, Mušnikovo, Gornje Selo.

Geographic entities mentioned:
surface_form: Koritnik
instance_of: Mountain
countries: Albania
Kosovo
coordinates: lat: 42.083333333333
lon: 20.566666666667
Geography. Dzhengal is situated on one of the external ridges of the mountain, the Polezhan Ridge, between the Dzhengal Gate saddle and the summit of Momin Dvor (2,723 m). It is flanked by the cirques Valyavishki to the west hosting the Valyavishki Lakes and Papagyolski to the east hosting the Popovi Lakes, both of the Mesta river basin.

Geographic entities mentioned:
surface_form: Valyavishki Lakes
instance_of: Group of lakes
countries: Bulgaria
coordinates: lat: 41.71
lon: 23.4825
The summit is built up of granite blocks covered in lichens and mosses. Dzhengal may be climbed from several points. One of easiest track starts from the Samodivski Lakes and ascends towards Momin Dvor. Another route begins at Tevno Ezero shelter at the Malokamenishki Lakes, ascends to a saddle to the southeast of the summit of Valyavishki Chukar (2,664 m) and reaches Dzhengal from the south.

Geographic entities mentioned:
surface_form: Samodivski Lakes
instance_of: Group of lakes
countries: Bulgaria
coordinates: lat: 41.701666666667
lon: 23.500555555556
One of easiest track starts from the Samodivski Lakes and ascends towards Momin Dvor. Another route begins at Tevno Ezero shelter at the Malokamenishki Lakes, ascends to a saddle to the southeast of the summit of Valyavishki Chukar (2,664 m) and reaches Dzhengal from the south. The other ways are more difficult and require fine preparation and experience.

Geographic entities mentioned:
surface_form: Malokamenishki Lakes
instance_of: Group of lakes
countries: Bulgaria
coordinates: lat: 41.7
lon: 23.479722222222
surface_form: tevno ezero
instance_of: Group of lakes
countries: Bulgaria
coordinates: lat: 41.7
lon: 23.479722222222
surface_form: dzhengal
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 41.706666666667
lon: 23.497777777778
Another legend says that the peak is named after the son of God Perun, Dzhengal. When the evil god Bes (Bez) decided to kidnap Perun's daughter while she was playing around the Samodivski Lakes, her brother guessed his intention and, after a fierce fight, defeated Bez and covered him with stones on the summit of Bezbog (2,645 m).

Geographic entities mentioned:
surface_form: Samodivski Lakes
instance_of: Group of lakes
countries: Bulgaria
coordinates: lat: 41.701666666667
lon: 23.500555555556
surface_form: samodivski lakes
instance_of: Group of lakes
countries: Bulgaria
coordinates: lat: 41.701666666667
lon: 23.500555555556
Dzhengal. Dzhengal () is a peak in the Pirin mountain range, south-western Bulgaria. It is located in the Pirin National Park, a UNESCO World Heritage Site. Geography. Dzhengal is situated on one of the external ridges of the mountain, the Polezhan Ridge, between the Dzhengal Gate saddle and the summit of Momin Dvor (2,723 m).

Geographic entities mentioned:
surface_form: dzhengal
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 41.706666666667
lon: 23.497777777778
Geography. Dzhengal is situated on one of the external ridges of the mountain, the Polezhan Ridge, between the Dzhengal Gate saddle and the summit of Momin Dvor (2,723 m). It is flanked by the cirques Valyavishki to the west hosting the Valyavishki Lakes and Papagyolski to the east hosting the Popovi Lakes, both of the Mesta river basin.

Geographic entities mentioned:
surface_form: dzhengal
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 41.706666666667
lon: 23.497777777778
surface_form: dzhengal
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 41.706666666667
lon: 23.497777777778
It is flanked by the cirques Valyavishki to the west hosting the Valyavishki Lakes and Papagyolski to the east hosting the Popovi Lakes, both of the Mesta river basin. Dzhengal towers to the west of Popovo Lake, the largest glacial lake in the mountain range. Its height is 2,730 m, which places it among the highest summits in Pirin.

Geographic entities mentioned:
surface_form: dzhengal
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 41.706666666667
lon: 23.497777777778
Dzhengal towers to the west of Popovo Lake, the largest glacial lake in the mountain range. Its height is 2,730 m, which places it among the highest summits in Pirin. The summit is built up of granite blocks covered in lichens and mosses. Dzhengal may be climbed from several points. One of easiest track starts from the Samodivski Lakes and ascends towards Momin Dvor.

Geographic entities mentioned:
surface_form: dzhengal
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 41.706666666667
lon: 23.497777777778
Name. According to the most popular version, the name derives from the Turkish word &quot;dzhangal&quot; which means sheep without lamb. When the herds were sheared, those sheep were marked with pendants. If the peak is viewed from the Bezbog refuge it looks like there is a pendant attached to it. Another legend says that the peak is named after the son of God Perun, Dzhengal.

Geographic entities mentioned:
surface_form: dzhengal
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 41.706666666667
lon: 23.497777777778
It is considered to be among Pirin's most beautiful summits. Name. According to the most popular version, the name derives from the Turkish word &quot;dzhangal&quot; which means sheep without lamb. When the herds were sheared, those sheep were marked with pendants. If the peak is viewed from the Bezbog refuge it looks like there is a pendant attached to it.

Geographic entities mentioned:
surface_form: dzhangal
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 41.706666666667
lon: 23.497777777778
In Bulgarian Bezbog means &quot;God Bez&quot; or &quot;without God&quot;. It has had several other names — &quot;Golets&quot;, meaning &quot;bare&quot; and &quot;Samodivski Vrah&quot;, meaning &quot;the summit of the samodiva&quot;, legendary woodland fairies or nymphs of the Bulgarian folklore.

Geographic entities mentioned:
surface_form: samodivski
instance_of: Group of lakes
countries: Bulgaria
coordinates: lat: 41.701666666667
lon: 23.500555555556
At that time Clark was in charge of administering the territory they called home. Through the perils of their trip, two of the Salish died at the home of General Clark. The remaining two Salish men secured a visit with St. Louis Bishop Joseph Rosati, who assured them that missionaries would be sent to the Bitterroot Valley when funds and missionaries were available in the future.

Geographic entities mentioned:
surface_form: Bitterroot Valley
instance_of: Valley
countries: United States
coordinates: lat: 46.247
lon: -114.16
(née Wheatley, and a primary school teacher) took place on Saturday 5 April 1958, and was registered during second ¼ 1958 in Don Valley district, West Riding of Yorkshire, England. They had children; Sally A. Hemingway (born, birth registered during second ¼ 1959 in Wharfedale district), Jonathan G. Hemingway (born, birth registered during first ¼ 1961 in Leeds district), and Elaine M.

Geographic entities mentioned:
surface_form: Wharfedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.88333
lon: -1.45
The split stages each had a combined winner. At the conclusion of the Tour, the entire West/South-West team won the overall super-combativity award, also decided by journalists. The Souvenir Henri Desgrange was given in honour of Tour founder Henri Desgrange to the first rider to pass the summit of the Ballon d'Alsace on stage 6. This prize was won by Jef Planckaert. Aftermath.

Geographic entities mentioned:
surface_form: Ballon d'Alsace
instance_of: Mountain
countries: France
coordinates: lat: 47.822222222222
lon: 6.8452777777778
It has timber, numerous lakes, and small deposits of low-grade manganese. One of the largest lakes in the Turtle Mountains is Lake Metigoshe, which straddles the international border, with about one-eighth of the lake in Canada. The region is home to Turtle Mountain Provincial Park, a state park, two historic sites, and various hunting and fishing opportunities.

Geographic entities mentioned:
surface_form: Lake Metigoshe
instance_of: Lake
countries: United States
Canada
coordinates: lat: 48.9793433
lon: -100.3535643
Turtle Mountain (plateau). Turtle Mountain, or the Turtle Mountains, is an area in central North America, in the north-central portion of the U.S. state of North Dakota and southwestern portion of the Canadian province of Manitoba, approximately south of the city of Brandon on Manitoba Highway 10 / U.S. Route 281.

Geographic entities mentioned:
surface_form: turtle mountain
instance_of: Mountain
countries: Canada
United States
coordinates: lat: 49
lon: -100.333
One of the largest lakes in the Turtle Mountains is Lake Metigoshe, which straddles the international border, with about one-eighth of the lake in Canada. The region is home to Turtle Mountain Provincial Park, a state park, two historic sites, and various hunting and fishing opportunities. Turtle Mountain is the traditional territory of the Plains Ojibwe, as well as part of the Métis homeland.

Geographic entities mentioned:
surface_form: turtle mountain
instance_of: Mountain
countries: Canada
United States
coordinates: lat: 49
lon: -100.333
Rapid colonization and settlement in the 19th century, along with the establishment of a firm border between Canada and the United States, displaced many Indigenous peoples to and from the region. Some identify as the Turtle Mountain Chippewa, who are federally recognized and whose reservation is in the valley on the southeastern edge of the plateau. History.

Geographic entities mentioned:
surface_form: turtle mountain
instance_of: Mountain
countries: Canada
United States
coordinates: lat: 49
lon: -100.333
Some identify as the Turtle Mountain Chippewa, who are federally recognized and whose reservation is in the valley on the southeastern edge of the plateau. History. The Plains Ojibwe have a long established history in the Turtle Mountain region and the surrounding area. East of Turtle Mountain at Pembina lived one Ojibwe group as well as a number of Métis families.

Geographic entities mentioned:
surface_form: turtle mountain
instance_of: Mountain
countries: Canada
United States
coordinates: lat: 49
lon: -100.333
History. The Plains Ojibwe have a long established history in the Turtle Mountain region and the surrounding area. East of Turtle Mountain at Pembina lived one Ojibwe group as well as a number of Métis families. The Métis hunted and fished in the Turtle Mountains and increasingly moved westward from Pembina in search of declining buffalo populations.

Geographic entities mentioned:
surface_form: turtle mountain
instance_of: Mountain
countries: Canada
United States
coordinates: lat: 49
lon: -100.333
The Métis hunted and fished in the Turtle Mountains and increasingly moved westward from Pembina in search of declining buffalo populations. When the federal government agreed that Pembina would be a part of the United States in 1818, the Métis living there, along with a number of Chippewa with kinship ties to the Métis, and some Ojibwe claimed land near Turtle Mountain.

Geographic entities mentioned:
surface_form: turtle mountain
instance_of: Mountain
countries: Canada
United States
coordinates: lat: 49
lon: -100.333
When the federal government agreed that Pembina would be a part of the United States in 1818, the Métis living there, along with a number of Chippewa with kinship ties to the Métis, and some Ojibwe claimed land near Turtle Mountain. The federal government recognized and designated this group the Pembina Band, but this did not include all the Ojibwe peoples already established at Turtle Mountain.

Geographic entities mentioned:
surface_form: turtle mountain
instance_of: Mountain
countries: Canada
United States
coordinates: lat: 49
lon: -100.333
The misidentification of all Ojibwe as part of the Pembina Band has prevented their full assertion of rights. Throughout the 19th century, the Pembina band was broken up and dispossessed of their lands as the government opened up the area for settlement. Among these groups are the Turtle Mountain Chippewa, and the Little Shell Tribe of Chippewa. Wildlife.

Geographic entities mentioned:
surface_form: turtle mountain
instance_of: Mountain
countries: Canada
United States
coordinates: lat: 49
lon: -100.333
Throughout the 19th century, the Pembina band was broken up and dispossessed of their lands as the government opened up the area for settlement. Among these groups are the Turtle Mountain Chippewa, and the Little Shell Tribe of Chippewa. Wildlife. The Turtle Mountain area is covered by deciduous forest.

Geographic entities mentioned:
surface_form: turtle mountain
instance_of: Mountain
countries: Canada
United States
coordinates: lat: 49
lon: -100.333
The 2nd volume of this work was published in 1840. Robert Brown (1773–1858) named the genus &quot;Bellendena&quot; of the Proteaceae in his honour in 1810. The state of Queensland in Australia has named its second highest peak Mount Bellenden Ker. The Bellenden Ker Range in the same area was also named after him.

Geographic entities mentioned:
surface_form: Mount Bellenden Ker
instance_of: Mountain
countries: Australia
coordinates: lat: -17.264166666667
lon: 145.85388888889
It is located to the south of Srinagar. Its district headquarters are situated in the city of Pulwama. It is located in the central part of the Kashmir Valley. Administration. In 1979 Anantnag district split in two, with one part remaining as Anantnag district, and the other part becoming Pulwama district.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
South Twin Lake (Wisconsin). South Twin Lake is located in the Chequamegon-Nicolet National Forest in Taylor County, Wisconsin. It is the home of the White Birch regeneration project started by Janet and Carl J. Nelson to support an ecosystem in which white birch saplings can thrive. In 2008 they retired to Oregon.

Geographic entities mentioned:
surface_form: south twin lake
instance_of: Lake
countries: United States
coordinates: lat: 45.620665
lon: -68.8605551
surface_form: south twin lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2731
lon: -90.4372
Description. Part of the Selkirk Mountains, the mountain is situated east of Revelstoke, southeast of Mount Revelstoke National Park and southwest of Glacier National Park. The nearest higher neighbor is Albert Peak, to the immediate southeast. Precipitation runoff from the mountain drains into tributaries of the nearby Illecillewaet River.

Geographic entities mentioned:
surface_form: Albert Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.03318
lon: -117.86899
Großer Traithen. Großer Traithen is a mountain of Bavaria, Germany. It is part of the Eastern Alps.

Geographic entities mentioned:
surface_form: großer traithen
instance_of: Mountain
countries: Germany
coordinates: lat: 47.647777777778
lon: 12.039444444444
Skeleton Lake (Alberta). Skeleton Lake () is a recreational, freshwater lake in Alberta, Canada. The lake is Northeast of the town of Boyle, Alberta, along Highway 63. It is in Athabasca County, northeast of the City of Edmonton. The lake's name is a translation of the Cree which means &quot;place of the skeletons.&quot; A Cree chief is buried along the eastern shore of the lake.

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
The lake drains through a small creek in Bondiss eastwards towards Amisk Lake. There are approximately 890 cottage and trailer sites around Skeleton Lake. There are 11 subdivisions surrounding the lake, which are part of the Athabasca County, containing approximately 300 lots.

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
It is in Athabasca County, northeast of the City of Edmonton. The lake's name is a translation of the Cree which means &quot;place of the skeletons.&quot; A Cree chief is buried along the eastern shore of the lake. The lake drains through a small creek in Bondiss eastwards towards Amisk Lake. There are approximately 890 cottage and trailer sites around Skeleton Lake.

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
Skeleton Lake (Alberta). Skeleton Lake () is a recreational, freshwater lake in Alberta, Canada. The lake is Northeast of the town of Boyle, Alberta, along Highway 63. It is in Athabasca County, northeast of the City of Edmonton. The lake's name is a translation of the Cree which means &quot;place of the skeletons.&quot; A Cree chief is buried along the eastern shore of the lake.

Geographic entities mentioned:
surface_form: skeleton lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.6219
lon: -112.725
surface_form: skeleton lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.2506
lon: -79.4503
The lake drains through a small creek in Bondiss eastwards towards Amisk Lake. There are approximately 890 cottage and trailer sites around Skeleton Lake. There are 11 subdivisions surrounding the lake, which are part of the Athabasca County, containing approximately 300 lots.

Geographic entities mentioned:
surface_form: skeleton lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.6219
lon: -112.725
surface_form: skeleton lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.2506
lon: -79.4503
There are 11 subdivisions surrounding the lake, which are part of the Athabasca County, containing approximately 300 lots. As well, the Summer Village of Mewatha Beach with approximately 220 properties, the Summer Village of Bondiss with approximately 195 lots and Shoreline Campground with approximately 170 sites are all on the shores of Skeleton Lake.

Geographic entities mentioned:
surface_form: skeleton lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.6219
lon: -112.725
surface_form: skeleton lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.2506
lon: -79.4503
Nahmakanta Lake. Nahmakanta Lake is the source of Nahmakanta Stream in the North Maine Woods. Nahmakanta Stream flows from the southeast end of the lake in Maine Township 1, Range 11, to the Pemadumcook Chain of Lakes in Township 1, Range 10. The Appalachian Trail follows Nahmakanta Stream and the southwest shore of Nahmakanta Lake.

Geographic entities mentioned:
surface_form: Pemadumcook Chain of Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 45.7
lon: -68.95
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
The Appalachian Trail follows Nahmakanta Stream and the southwest shore of Nahmakanta Lake. The northwest end of the lake in Township 2, Range 11, receives drainage from Rainbow Lake via Rainbow Stream, from Gould Pond via Gould Brook, from the Bean Ponds via Bean Brook, and from Female Pond, Wadleigh Pond, the Musquash Ponds, and Pollywog Pond via Pollywog Brook.

Geographic entities mentioned:
surface_form: rainbow lake
instance_of: Lake
countries: United States
coordinates: lat: 40.8803
lon: -74.4567
surface_form: rainbow lake
instance_of: Lake
countries: United States
coordinates: lat: 42.696368
lon: -83.402186
surface_form: rainbow lake
instance_of: Lake
countries: United States
coordinates: lat: 45.823888888889
lon: -69.116944444444
surface_form: rainbow lake
instance_of: Lake
countries: United States
coordinates: lat: 34.1499
lon: -109.984
surface_form: gould pond
instance_of: Lake
countries: United States
coordinates: lat: 41.9050664
lon: -75.1211848
surface_form: rainbow lake
instance_of: Lake
countries: United States
coordinates: lat: 44.4800953
lon: -74.1600758
Nahmakanta Lake. Nahmakanta Lake is the source of Nahmakanta Stream in the North Maine Woods. Nahmakanta Stream flows from the southeast end of the lake in Maine Township 1, Range 11, to the Pemadumcook Chain of Lakes in Township 1, Range 10. The Appalachian Trail follows Nahmakanta Stream and the southwest shore of Nahmakanta Lake.

Geographic entities mentioned:
surface_form: nahmakanta lake
instance_of: Lake
countries: United States
coordinates: lat: 45.75
lon: -69.13333333
Aitken State Forest is located in Mendon. The state land covers and includes a hiking trail up Bald Mountain (2,090 ft), hunting, primitive camping, cross-country skiing and snowmobiling. The Appalachian Trail/Long Trail crosses the southeast corner of the town, passing near the summit of Killington Peak. Demographics.

Geographic entities mentioned:
surface_form: Killington Peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.604444444444
lon: -72.82
Devil's Punch Bowl. The Devil's Punch Bowl is a visitor attraction and biological Site of Special Scientific Interest situated just to the east of the village of Hindhead in the English county of Surrey. It is part of the Wealden Heaths Phase II Special Protection Area. The Punch Bowl is a large natural amphitheatre and is the source of many stories about the area.

Geographic entities mentioned:
surface_form: devil's punch bowl
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.11694444444444
lon: -0.7288888888888889
The Punch Bowl is a large natural amphitheatre and is the source of many stories about the area. The London to Portsmouth road (the A3) skirted the rim of the site before the Hindhead Tunnel was built in 2011. The land is owned and maintained by the National Trust as part of the &quot;Hindhead Commons and the Devil's Punch Bowl&quot; property.

Geographic entities mentioned:
surface_form: devil's punch bowl
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.11694444444444
lon: -0.7288888888888889
The highest point of the rim of the bowl is Gibbet Hill, which is above sea level and commands a panoramic view that includes, on a clear day, the skyline of London some away. The Devil's Punch Bowl was featured on the 2005 TV programme &quot;Seven Natural Wonders&quot; as one of the wonders of the South. Toponym.

Geographic entities mentioned:
surface_form: devil's punch bowl
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.11694444444444
lon: -0.7288888888888889
Roads. During the Tudor period in the 16th Century, Portsmouth developed into a major naval dockyard, needing access to London. The steep gradients of the Devil's Punch Bowl and nearby Gibbet Hill made this difficult. As a consequence, there have been three phases of road construction through the Devil's Punch Bowl. Earliest route. The Old Portsmouth Road is the oldest highway through the area.

Geographic entities mentioned:
surface_form: devil's punch bowl
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.11694444444444
lon: -0.7288888888888889
Turnpike. In 1748 Kingston-Upon-Thames to Sheet Bridge Turnpike Company took over the management of Old Portsmouth Road. They installed mileposts, toll houses, gates and maintained the highway through the Devil's Punch Bowl. However, by the early 19th Cenutry increased pedestrian and horse-drawn traffic meant this steep section of highway between Portsmouth and London required major improvements.

Geographic entities mentioned:
surface_form: devil's punch bowl
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.11694444444444
lon: -0.7288888888888889
In 1826, the Portsmouth & Sheet Bridge Turnpike Road Trust began asking for tenders from bidders to improve the road. The winning bid resulted in a completely new highway through the Devil's Punch Bowl. Old Portmouth Road was abandoned in favour of a new cutting below the ridgeline.

Geographic entities mentioned:
surface_form: devil's punch bowl
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.11694444444444
lon: -0.7288888888888889
Return to nature. By the start of the 21st century most of the A3 had become a dual carriageway, leaving only the section through Hindhead and the Devil's Punch Bowl as single carriageway. Due to daily traffic volumes, this section operated at or above capacity for much of the day and had an accident rate 40% higher than the national average for that class of road.

Geographic entities mentioned:
surface_form: devil's punch bowl
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.11694444444444
lon: -0.7288888888888889
Conservation. The Devil's Punch Bowl, along with Hindhead Common, was acquired by the National Trust in 1906, making it one of the first open spaces acquired by the Trust. The beauty of the area and the diversity of nature it attracts resulted in the Devil's Punch Bowl being designated as a Site of Special Scientific Interest on 30 April 1986.

Geographic entities mentioned:
surface_form: devil's punch bowl
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.11694444444444
lon: -0.7288888888888889
The beauty of the area and the diversity of nature it attracts resulted in the Devil's Punch Bowl being designated as a Site of Special Scientific Interest on 30 April 1986. This ownership and status helped save the Devil's Punch Bowl from above-ground redevelopment of the A3 in the first decade of the 21st century.

Geographic entities mentioned:
surface_form: devil's punch bowl
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.11694444444444
lon: -0.7288888888888889
The tunnel preserves not only the area from the road widening originally proposed but also removes the heavy traffic congestion which previously affected this section of the A3 in peak hours. The National Trust provide car parking and a cafe at the Hindhead end of the Devil's Punch Bowl.

Geographic entities mentioned:
surface_form: devil's punch bowl
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.11694444444444
lon: -0.7288888888888889
The Hindhead youth hostel, run by the Youth Hostel Association, used to be located inside the bowl but closed in 2015. In fiction. Punch Bowl Farm, at the northern end of the Devil's Punch Bowl, was the home of children's novelist Monica Edwards from 1947 until 1998. In her books she renamed the farm Punchbowl Farm.

Geographic entities mentioned:
surface_form: devil's punch bowl
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.11694444444444
lon: -0.7288888888888889
In her books she renamed the farm Punchbowl Farm. In Charles Dickens' novel &quot;Nicholas Nickleby&quot;, Nicholas and Smike visit the Devil's Punch Bowl on their journey to Portsmouth. The third novel in the Horatio Hornblower series, &quot;Flying Colours&quot; by C.S.

Geographic entities mentioned:
surface_form: devil's punch bowl
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.11694444444444
lon: -0.7288888888888889
Forester, makes a one-line reference to the Devil's Punch Bowl in chapter eighteen as Hornblower is returning to London: &quot;Even the marvellous beauty of the Devil's Punch Bowl was lost on Hornblower as they drove past it.&quot;
The &quot;Devil's Punch-Bowl in Surrey&quot; is briefly mentioned in &quot;The Shining Pyramid&quot;, a short story by Arthur Machen, and in &quot;The Manhood of Edward Robinson&quot;, the fifth story in Agatha Christie's &quot;The Listerdale Mystery and Other Stories&quot;.

Geographic entities mentioned:
surface_form: devil's punch bowl
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.11694444444444
lon: -0.7288888888888889
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
As of 2012, 272 districts across the country were listed under this scheme. The list includes 21 districts of Jharkhand. Transport. The Sahibganj Loop line passes through this block. Taljhari railway station is situated at Taljhari. Tourism. Moti Jharna (pearl cascade) is the most picturesque waterfall in Sahebganj district, at the head of a picturesque glen of the Rajmahal hills. Education.

Geographic entities mentioned:
surface_form: Rajmahal hills
instance_of: Mountain
countries: India
coordinates: lat: 25
lon: 87
The Morgenthaus and the Roosevelts had much in common: sharing a similar upper-class background, a similar political outlook and a common interest in farming. FDR and Morgenthau were said to have engaged in a neighborly rivalry over the cultivation of squash. Fishkill Farms is currently an apple orchard and small-scale business, one of the Hudson Valley's oldest apple orchards.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Valdigne. The Valdigne () is the upper part of the Aosta Valley in north-west Italy. It is traversed by the Dora Baltea (), a tributary of the Po. Description. It extends from La Salle to Courmayeur, including the side valleys of Val Ferret, Val Veny and La Thuile Valley.

Geographic entities mentioned:
surface_form: valdigne
instance_of: Valley
countries: Italy
coordinates: lat: 45.75
lon: 7.066666666666666
It is traversed by the Dora Baltea (), a tributary of the Po. Description. It extends from La Salle to Courmayeur, including the side valleys of Val Ferret, Val Veny and La Thuile Valley. The communes of the Valdigne are Courmayeur, La Salle, La Thuile, Morgex and Pré-Saint-Didier: together they form the Unité des communes valdôtaines du Valdigne - Mont-Blanc.

Geographic entities mentioned:
surface_form: valdigne
instance_of: Valley
countries: Italy
coordinates: lat: 45.75
lon: 7.066666666666666
surface_form: valdigne
instance_of: Valley
countries: Italy
coordinates: lat: 45.75
lon: 7.066666666666666
The country is also the terminus of rail traffic into Ethiopia. Physiographic regions. Djibouti can be divided into three physiographic regions
Mountains. A great arc of mountains, consisting of the Mousa Ali, Goda Mountains, and Arrei Mountains surrounds Djibouti. Djibouti has eight mountain ranges with peaks of over. Grand Bara.

Geographic entities mentioned:
surface_form: Mousa Ali
instance_of: Mountain
countries: Eritrea
Djibouti
Ethiopia
coordinates: lat: 12.470833333333
lon: 42.405
Geography. The valley, about long and up to three-quarters of a mile (1.2 km) wide, is characterized by high, extremely steep granite walls, side canyons and waterfalls. The valley's scenery has been frequently compared to that of Yosemite Valley, starting with John Muir who first visited the area in the 1870s.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423