Sarmila/GeoWiki-Features huggingface dataset:
Queen Mary Hospital is at its west slope. Harlech, Hatton and Lugard Roads terminate at a junction on its north slope. On clear days, visitors can see Tai Mo Shan to the north, Castle Peak to the north-west, Lantau Peak to the west, Tate's Cairn to the north-east and Lamma Island to the south. Access. Unlike nearby Victoria Peak, there are no roads or cable cars up High West.

Geographic entities mentioned:
surface_form: Tai Mo Shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.4118
lon: 114.123
surface_form: Lantau Peak
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.245
lon: 113.917
surface_form: Tate's Cairn
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.358
lon: 114.218
surface_form: castle peak
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.3833
lon: 113.95
High West. High West or Sai Ko Shan, is a mountain on Hong Kong Island with a height of
It is in Central and Western District. Geography. High West is located within Pok Fu Lam Country Park and straddles the boundary of Central and Western District and Southern District. It is west of Victoria Peak, north of Pok Fu Lam and south of Lung Fu Shan. Queen Mary Hospital is at its west slope.

Geographic entities mentioned:
surface_form: high west
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.2725
lon: 114.136
High West. High West or Sai Ko Shan, is a mountain on Hong Kong Island with a height of
It is in Central and Western District. Geography. High West is located within Pok Fu Lam Country Park and straddles the boundary of Central and Western District and Southern District. It is west of Victoria Peak, north of Pok Fu Lam and south of Lung Fu Shan. Queen Mary Hospital is at its west slope.

Geographic entities mentioned:
surface_form: high west
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.2725
lon: 114.136
surface_form: sai ko shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.2725
lon: 114.136
On clear days, visitors can see Tai Mo Shan to the north, Castle Peak to the north-west, Lantau Peak to the west, Tate's Cairn to the north-east and Lamma Island to the south. Access. Unlike nearby Victoria Peak, there are no roads or cable cars up High West. East of the summit, a recently renovated trail near the junction of Hatton, Lugard and Harlech Roads leads to the top.

Geographic entities mentioned:
surface_form: high west
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.2725
lon: 114.136
East of the summit, a recently renovated trail near the junction of Hatton, Lugard and Harlech Roads leads to the top. West of the summit starting from Lung Fu Shan View Compass, there is a rock climb of about 180 metres that leads to the top for rock-climbing experts. This climb is treacherous and is not safe on windy or wet days.

Geographic entities mentioned:
surface_form: lung fu shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.27993333
lon: 114.13504167
The English name is 'Quamichan.'
There are varying historical accounts of the size of the village; however, in all descriptions the Quamichan village was large. The village extended for five kilometres along the Cowichan River, stretching from one kilometre above Quamichan Creek down almost to Comiaken village.

Geographic entities mentioned:
surface_form: Quamichan Creek
instance_of: Lake
countries: Canada
coordinates: lat: 48.80139
lon: -123.66056
Lisenser Fernerkogel. The Lisenser Fernerkogel (or Lüsener Fernerkogel) is a mountain in the Stubai Alps of Austria. Routes. From the Franz Senn Hütte hut it is approximately 3½ hours mostly over glaciers and snow, with a small (100 m) easy rock scramble at the end. Close to, and can be combined with, the Rotgratspitze and Lisenser Spitze.

Geographic entities mentioned:
surface_form: Rotgratspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.09361111111111
lon: 11.113888888888889
surface_form: Lisenser Spitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.0883987
lon: 11.1108596
It is composed of five villages: Bucium, Chilii, Giurgeni, Muncelu de Jos, and Valea Ursului. The commune lies on the Central Moldavian Plateau, on the banks of the Bârlad River, which has its source here. It is located in the southeastern extremity of Neamț County, on the border with Bacău County, from Roman and from Bacău; the county seat, Piatra Neamț, is away.

Geographic entities mentioned:
surface_form: Central Moldavian Plateau
instance_of: Plateau
countries: Moldova
coordinates: lat: 47.08333
lon: 28.33333
Whirlpool River. The Whirlpool River is a short river in Jasper National Park, Alberta, Canada. It is an early tributary of the Athabasca River. The Whirlpool is formed in Athabasca Pass, collecting meltwater from the Hooker Icefield and the Mount Brown Icefield.

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 Whirlpool River is a short river in Jasper National Park, Alberta, Canada. It is an early tributary of the Athabasca River. The Whirlpool is formed in Athabasca Pass, collecting meltwater from the Hooker Icefield and the Mount Brown Icefield. It flows north, collecting the Middle Whirlpool River before passing under Alberta Highway 93A and flowing into the Athabasca River south of Jasper.

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: mount brown
instance_of: Mountain
countries: Canada
coordinates: lat: 52.38027777777778
lon: -118.23
The Whirlpool is formed in Athabasca Pass, collecting meltwater from the Hooker Icefield and the Mount Brown Icefield. It flows north, collecting the Middle Whirlpool River before passing under Alberta Highway 93A and flowing into the Athabasca River south of Jasper. The Moab Lake Road parallels the Whirlpool near its confluence with 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: whirlpool river
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.735
lon: -117.95416667
It flows north, collecting the Middle Whirlpool River before passing under Alberta Highway 93A and flowing into the Athabasca River south of Jasper. The Moab Lake Road parallels the Whirlpool near its confluence with the Athabasca River. The Whirlpool was named by Sir James Hector in 1859. He noted the presence of many eddies in the 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
Whirlpool River. The Whirlpool River is a short river in Jasper National Park, Alberta, Canada. It is an early tributary of the Athabasca River. The Whirlpool is formed in Athabasca Pass, collecting meltwater from the Hooker Icefield and the Mount Brown Icefield.

Geographic entities mentioned:
surface_form: whirlpool river
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.735
lon: -117.95416667
Stuart MacKintosh. Stuart MacKintosh (born 20 July 1986) AKA &quot;Smack&quot;, is a shinty player and musician from Drumnadrochit, Loch Ness, Scotland. He plays in goal for Glenurquhart Shinty Club and he is the current Scotland goalkeeper. Shinty career. MacKintosh has played for Glenurquhart Shinty Club from an early age.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
Ólafsvík's economy is based on fishing industry and commerce, and provision of services for farmers in the area. The area of Ólafsvík provides many opportunities for tourists, such as birdwatching, hiking trails, long sandy beaches, and snowmobiling on the Snæfellsjökull glacier, just 10 km away (although the road is closed for much of the year).

Geographic entities mentioned:
surface_form: Snæfellsjökull
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.8071204861
lon: -23.7762279203
It is similar to a pyroclastic flow but has a lower density, having a much higher ratio of gas to rock, which makes it more turbulent and allows it to rise over ridges and hills rather than always travel downhill as pyroclastic flows do. The speed of pyroclastic density currents has been measured directly via photography only in the case of Mount St. Helens, where they reached 320-470 km/h, or.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
State Route 60 (SR 60) is an east–west state highway in the U.S. state of California. It serves the cities and communities on the eastern side of the Los Angeles metropolitan area and runs along the south side of the San Gabriel Valley. It functions as a bypass route of Interstate 10 (I-10) through the area between the East Los Angeles Interchange in Los Angeles and Beaumont.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
It functions as a bypass route of Interstate 10 (I-10) through the area between the East Los Angeles Interchange in Los Angeles and Beaumont. SR 60 provides a route across several spurs of the Peninsular Ranges, linking the Los Angeles Basin with the Pomona Valley and San Gabriel Valley. The highway also runs concurrently with SR 57 and I-215.

Geographic entities mentioned:
surface_form: Pomona Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.076
lon: -117.657
The freeway heads east from the junction after splitting off from I-10 (Santa Monica Freeway) and passes through East Los Angeles, where it has a four level interchange with I-710 (Long Beach Freeway). Continuing east through the southern San Gabriel Valley, SR 60 passes through many cities and communities, intersecting I-605 (San Gabriel River Freeway) in the City of Industry.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
It proceeds to overlap with SR 57 (Orange Freeway) in Diamond Bar, right on the edge of the San Gabriel Valley. A short overlap carries SR 60 traffic on the same roadway as SR 57. The two routes head northeast through an arm of the San Gabriel Valley; after they split, SR 60 ascends slightly and then slopes through the Puente Hills and into the Pomona Valley.

Geographic entities mentioned:
surface_form: Pomona Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.076
lon: -117.657
Götzhöhe. Götzhöhe is a mountain of Saxony, southeastern Germany.

Geographic entities mentioned:
surface_form: götzhöhe
instance_of: Mountain
countries: Germany
coordinates: lat: 50.768055555556
lon: 13.070277777778
Life and career. Terry Isaac grew up in the Willamette Valley of Oregon, and it is there that he began working with wildlife. Drawing inspiration from his own backyard and from the captivating vistas of the Northwest, he began to create dramatic wildlife art. He later called Penticton, British Columbia, Canada home.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Deeply unhappy he ran away to an uncle in Lörrach. Despite finishing his schooling in a Roman Catholic school he came under the influence of Evangelical Christians and developed an ambition to become a missionary. He enrolled in the Evangelical Training School for Foreign Missionaries in St. Chrischona and was consecrated in September 1858.

Geographic entities mentioned:
surface_form: St. Chrischona
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.573333333333
lon: 7.6802777777778
Castelluccio culture was present in the villages of south-east Sicily, Monte Casale, Cava d'Ispica, Pachino, Niscemi, Cava Lazzaro, near Noto, of Rosolini, in the rocky Byzantine district of coasts of Santa Febronia in Palagonia, in Cuddaru d' Crastu (Tornabé-Mercato d'Arrigo) near Pietraperzia, where there are the remains of a fortress partly carved in stone, and - with different ceramic forms - also near Agrigento in Monte Grande.

Geographic entities mentioned:
surface_form: Monte Casale
instance_of: Mountain
countries: Italy
coordinates: lat: 37.096388888889
lon: 14.821388888889
Daru (community development block). Daru is a community development block (CD block) that forms an administrative division in the Hazaribagh Sadar subdivision of the Hazaribagh district in the Indian state of Jharkhand. Overview. Hazaribagh district is spread over a part of the Chota Nagpur Plateau. The central plateau, averaging a height of, occupies the central part of the district.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
On 7 May 1867 at the island of Little Andaman, eastern India, in the Bay of Bengal, Assistant Surgeon Douglas and four Privates (David Bell, James Cooper, William Griffiths and Thomas Murphy) of the 2/24th Regiment risked their lives in manning a boat and proceeding through dangerous surf to rescue some of their comrades who had been sent to the island to find out the fate of the commander and seven of the crew, who had landed from the ship &quot;Assam Valley&quot; and were feared murdered by the cannibalistic islanders.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
It organizes workshops and seminars on the management of electronic records, virtual libraries and archives, multimedia and interactive publishing, intellectual property management and electronic information standards. Residential seminars are organized on Grindstone Island, Big Rideau Lake, in the Rideau Canal System.

Geographic entities mentioned:
surface_form: Big Rideau Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.75
lon: -76.2333
Lago di Muzzano. __NOTOC__
Lago di Muzzano is a lake in Ticino, Switzerland. It is bordered by the municipalities of Sorengo, Muzzano and Collina d'Oro. Its surface area is. It drains into Lake Lugano.

Geographic entities mentioned:
surface_form: Lake Lugano
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46
lon: 9
Lago di Muzzano. __NOTOC__
Lago di Muzzano is a lake in Ticino, Switzerland. It is bordered by the municipalities of Sorengo, Muzzano and Collina d'Oro. Its surface area is. It drains into Lake Lugano.

Geographic entities mentioned:
surface_form: lago di muzzano
instance_of: Lake
countries: Switzerland
coordinates: lat: 45.997222222222
lon: 8.9280555555556
Specific neighborhoods associated with the &quot;Orange Coast&quot; moniker include Surfside (Seal Beach), Sunset Beach (Huntington Beach), Balboa Island (Newport Beach), Balboa Peninsula (Newport Beach), Corona del Mar (Newport Beach), Newport Coast (Newport Beach), South Laguna (Laguna Beach), Monarch Beach (Dana Point) and Capistrano Beach (Dana Point).

Geographic entities mentioned:
surface_form: Surfside
instance_of: Landform
countries: United States
coordinates: lat: 33.7278
lon: -118.082
Barclay Bay. Barclay Bay () is a bay in the Drake Passage between Cape Shirreff and Essex Point on the north side of Livingston Island, in the South Shetland Islands. Its head is fed by Etar Snowfield. The name appears on an 1825 chart of the British sealing expedition under James Weddell, and is now established in international usage. In fiction.

Geographic entities mentioned:
surface_form: Etar Snowfield
instance_of: Landform
coordinates: lat: -62.5686
lon: -60.7742
It has been shown that lake levels have fluctuated greatly in the past. Tree stumps exist today that are rooted lower than any recorded level of the lake. Only once since records have been kept has Kenosee Lake over-flowed its bank and that was in 1928 when it flowed into another closed-basin lake, White Bear (Carlyle) Lake. Restoration of lake levels. Beaver are not native to Moose Mountain.

Geographic entities mentioned:
surface_form: white bear (carlyle) lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.7683
lon: -102.2665
surface_form: kenosee lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8167
lon: -102.283
surface_form: basin lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.63336
lon: -105.28386
surface_form: bear
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.2833
lon: -126.967
Kenosee Lake. Kenosee Lake is a closed-basin lake in the south-east corner of the Canadian province of Saskatchewan. The lake lies in Moose Mountain Provincial Park in the heart of the Moose Mountain Upland, a forested plateau that rises about above the surrounding prairie.

Geographic entities mentioned:
surface_form: kenosee lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8167
lon: -102.283
Kenosee Lake. Kenosee Lake is a closed-basin lake in the south-east corner of the Canadian province of Saskatchewan. The lake lies in Moose Mountain Provincial Park in the heart of the Moose Mountain Upland, a forested plateau that rises about above the surrounding prairie.

Geographic entities mentioned:
surface_form: kenosee lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8167
lon: -102.283
surface_form: basin lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.63336
lon: -105.28386
The lake lies in Moose Mountain Provincial Park in the heart of the Moose Mountain Upland, a forested plateau that rises about above the surrounding prairie. The village of Kenosee Lake and the neighbouring Moose Mountain subdivisions are the only places on the lake with a year-round population. There are three named islands in the lake. The largest is Hog Island.

Geographic entities mentioned:
surface_form: kenosee lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8167
lon: -102.283
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: moose
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.91444444444444
lon: -118.80638888888889
surface_form: moose mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.9383
lon: -114.838
Most of the water that flows into the lake is from rain, ground water, and melting snow. The only large body of water that flows into Kenosee Lake is from Little Kenosee Lake and that flows through Fish Creek at the northern shore. History. Like many lakes on the prairies, Kenosee Lake does not have an out-flow.

Geographic entities mentioned:
surface_form: kenosee lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8167
lon: -102.283
surface_form: kenosee lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8167
lon: -102.283
surface_form: little kenosee lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.83334
lon: -102.33383
The only large body of water that flows into Kenosee Lake is from Little Kenosee Lake and that flows through Fish Creek at the northern shore. History. Like many lakes on the prairies, Kenosee Lake does not have an out-flow. The water levels of Kenosee Lake have been monitored periodically over the last 150 years since the first land surveyors came in the 1870s.

Geographic entities mentioned:
surface_form: kenosee lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8167
lon: -102.283
History. Like many lakes on the prairies, Kenosee Lake does not have an out-flow. The water levels of Kenosee Lake have been monitored periodically over the last 150 years since the first land surveyors came in the 1870s. It has been shown that lake levels have fluctuated greatly in the past. Tree stumps exist today that are rooted lower than any recorded level of the lake.

Geographic entities mentioned:
surface_form: kenosee lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8167
lon: -102.283
The locals then decided to take out four dams on their own. The removal of those four dams increased the level of the lake, but not quite to ideal levels. According to aerial photographs, the surface of Kenosee Lake was 742 metres asl in 1928. By 1950, it had dropped to 738 metres. With the destruction of the beaver dams in 1954, the lake recovered to 740 metres by 1960.

Geographic entities mentioned:
surface_form: kenosee lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8167
lon: -102.283
They also looked at other ways to control water levels, such as through building culverts and spillways. Fish Creek, a short creek that flows from Little Kenosee Lake to Kenosee Lake had been blocked when the main road, Highway 209, through the park was built. Part of the water level restoration project was to build culverts to allow the creek to flow again.

Geographic entities mentioned:
surface_form: kenosee lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8167
lon: -102.283
surface_form: kenosee lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8167
lon: -102.283
surface_form: little kenosee lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.83334
lon: -102.33383
The village of Kenosee Lake and the neighbouring Moose Mountain subdivisions are the only places on the lake with a year-round population. There are three named islands in the lake. The largest is Hog Island. It got its name from when an early pioneering family, the Christophers, kept their hogs on that island to keep them safe from predators, such as wolves.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
There are three named islands in the lake. The largest is Hog Island. It got its name from when an early pioneering family, the Christophers, kept their hogs on that island to keep them safe from predators, such as wolves. In the 1920s, wolves were hunted to extinction on Moose Mountain. Up until the late 1890s, Manitoba Maples were very common on the upland.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Settlers and the local Indians made syrup from the sap of the maples trees. The island right to the south of Hog Island is named Maple Island because of all the syrup producing maple trees. In 1897, a massive fire swept through much of Moose Mountain, destroying most of the maple trees and ending the burgeoning syrup industry.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
In 1897, a massive fire swept through much of Moose Mountain, destroying most of the maple trees and ending the burgeoning syrup industry. The trees on Maple Island were spared from the fire because of all the water surrounding the island. The third named island is to the south of Maple Island and is called Horseshoe Island. All three islands are on the east side of the lake.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
In 1897, a massive fire swept through much of Moose Mountain, destroying most of the maple trees and ending the burgeoning syrup industry. The trees on Maple Island were spared from the fire because of all the water surrounding the island. The third named island is to the south of Maple Island and is called Horseshoe Island. All three islands are on the east side of the lake.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
By 1950, it had dropped to 738 metres. With the destruction of the beaver dams in 1954, the lake recovered to 740 metres by 1960. Without further intervention regarding beaver control, by 2008, the lake level had dropped down to 737 metres. It dropped so low that Hog Island, the lake's largest island, was no longer an island. In 2008, the Moose Mountain Water Resource Management Corp.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Between 2008 and 2013, lake water levels rose 9 feet (2.74 m). The corporation and park planned to see a rise of another 9 feet, as that would be enough for Kenosee to overflow its banks and flow into White Bear Lake, which is also well below ideal levels. By 2016, lake levels had stabilised at about 741 metres, just below the level that would see it overflow. Fish species.

Geographic entities mentioned:
surface_form: bear lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.5567
lon: -63.5053
surface_form: bear lake
instance_of: Lake
countries: Canada
coordinates: lat: 56.1
lon: -126.817
surface_form: bear lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.946
lon: -62.8121
surface_form: bear
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.2833
lon: -126.967
The largest is Hog Island. It got its name from when an early pioneering family, the Christophers, kept their hogs on that island to keep them safe from predators, such as wolves. In the 1920s, wolves were hunted to extinction on Moose Mountain. Up until the late 1890s, Manitoba Maples were very common on the upland. Settlers and the local Indians made syrup from the sap of the maples trees.

Geographic entities mentioned:
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
Kenosee Lake is a closed-basin lake in the south-east corner of the Canadian province of Saskatchewan. The lake lies in Moose Mountain Provincial Park in the heart of the Moose Mountain Upland, a forested plateau that rises about above the surrounding prairie. The village of Kenosee Lake and the neighbouring Moose Mountain subdivisions are the only places on the lake with a year-round population.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: moose
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.91444444444444
lon: -118.80638888888889
surface_form: moose
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.91444444444444
lon: -118.80638888888889
surface_form: moose mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.9383
lon: -114.838
surface_form: moose mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.9383
lon: -114.838
The largest is Hog Island. It got its name from when an early pioneering family, the Christophers, kept their hogs on that island to keep them safe from predators, such as wolves. In the 1920s, wolves were hunted to extinction on Moose Mountain. Up until the late 1890s, Manitoba Maples were very common on the upland. Settlers and the local Indians made syrup from the sap of the maples trees.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: moose
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.91444444444444
lon: -118.80638888888889
surface_form: moose mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.9383
lon: -114.838
The island right to the south of Hog Island is named Maple Island because of all the syrup producing maple trees. In 1897, a massive fire swept through much of Moose Mountain, destroying most of the maple trees and ending the burgeoning syrup industry. The trees on Maple Island were spared from the fire because of all the water surrounding the island.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: moose
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.91444444444444
lon: -118.80638888888889
surface_form: moose mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.9383
lon: -114.838
Only once since records have been kept has Kenosee Lake over-flowed its bank and that was in 1928 when it flowed into another closed-basin lake, White Bear (Carlyle) Lake. Restoration of lake levels. Beaver are not native to Moose Mountain. In 1923, two breeding pairs from Hudson Bay, Saskatchewan were brought to the lake.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: moose
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.91444444444444
lon: -118.80638888888889
surface_form: moose mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.9383
lon: -114.838
Without further intervention regarding beaver control, by 2008, the lake level had dropped down to 737 metres. It dropped so low that Hog Island, the lake's largest island, was no longer an island. In 2008, the Moose Mountain Water Resource Management Corp. partnered with Moose Mountain Provincial Park to control beavers through trapping and by blasting beaver dams.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: moose
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.91444444444444
lon: -118.80638888888889
surface_form: moose mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.9383
lon: -114.838
It dropped so low that Hog Island, the lake's largest island, was no longer an island. In 2008, the Moose Mountain Water Resource Management Corp. partnered with Moose Mountain Provincial Park to control beavers through trapping and by blasting beaver dams. They also looked at other ways to control water levels, such as through building culverts and spillways.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: moose
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.91444444444444
lon: -118.80638888888889
surface_form: moose mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.9383
lon: -114.838
Arkansas Highway 247. Highway 247 (AR 247, Ark. 247, and Hwy. 247) is a designation for four north–south state highways in the Arkansas River Valley. Two are low traffic, two-lane, rural connector highways serving sparsely populated areas of the River Valley. A third segment is a four-lane highway bypassing Pottsville.

Geographic entities mentioned:
surface_form: Arkansas River Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
Two Point Mountain is named for having two peaks: its main summit and a second summit about to the northwest that rises to an elevation of. The mountain is within the watershed of the South Fork Boise River where the south side is drained by Bear Creek and the north side by the Ross Fork. No maintained trails lead to either summit.

Geographic entities mentioned:
surface_form: bear creek
instance_of: Watercourse
countries: United States
coordinates: lat: 39.8305929
lon: -92.2301817
Two Point Mountain (Idaho). Two Point Mountain is the highest point in the Boise Mountains with a summit elevation of located in the Fairfield Ranger District of Sawtooth National Forest, Idaho. It is located from Perfect Peak in the Sawtooth Range, its line parent, giving it a prominence of.

Geographic entities mentioned:
surface_form: the sawtooth
instance_of: Mountain
countries: United States
coordinates: lat: 39.590833333333
lon: -105.66416666667
Two Point Mountain (Idaho). Two Point Mountain is the highest point in the Boise Mountains with a summit elevation of located in the Fairfield Ranger District of Sawtooth National Forest, Idaho. It is located from Perfect Peak in the Sawtooth Range, its line parent, giving it a prominence of.

Geographic entities mentioned:
surface_form: two point mountain (idaho)
instance_of: Mountain
countries: United States
coordinates: lat: 43.73722222222222
lon: -114.97666666666667
Two Point Mountain (Idaho). Two Point Mountain is the highest point in the Boise Mountains with a summit elevation of located in the Fairfield Ranger District of Sawtooth National Forest, Idaho. It is located from Perfect Peak in the Sawtooth Range, its line parent, giving it a prominence of.

Geographic entities mentioned:
surface_form: two point mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.73722222222222
lon: -114.97666666666667
It is located from Perfect Peak in the Sawtooth Range, its line parent, giving it a prominence of. Two Point Mountain is named for having two peaks: its main summit and a second summit about to the northwest that rises to an elevation of. The mountain is within the watershed of the South Fork Boise River where the south side is drained by Bear Creek and the north side by the Ross Fork.

Geographic entities mentioned:
surface_form: two point mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.73722222222222
lon: -114.97666666666667
Glen Lake Community School. Glen Lake Community School (GLCS) is a public, coeducational K–12 school in Kasson Township, Leelanau County, in the U.S. state of Michigan. Located between Burdickville and Maple City, Glen Lake Community School serves most of southwest and central Leelanau County, and lies near the eponymous Glen Lake. Most of the school district is in Leelanau County.

Geographic entities mentioned:
surface_form: Glen Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.8667
lon: -85.95
Creole Petroleum Corporation. The Creole Petroleum Corporation was an American oil company. It was formed in 1920 to produce fields on Lake Maracaibo, Venezuela. The company was acquired by Standard Oil of New Jersey in 1928. Until 1951 Creole Petroleum was the world's number one oil producer when was supplanted by Arabian American Oil Company. In 1950, Creole opened its refinery at Amuay bay.

Geographic entities mentioned:
surface_form: Lake Maracaibo
instance_of: Lake
countries: Venezuela
coordinates: lat: 9.8158333333333
lon: -71.556666666667
Koettlitz Glacier. Koettlitz Glacier () is a large Antarctic glacier lying west of Mount Morning and Mount Discovery in the Royal Society Range, flowing from the vicinity of Mount Cocks northeastward between Brown Peninsula and the mainland into the ice shelf of McMurdo Sound. Naming and exploration.

Geographic entities mentioned:
surface_form: Mount Morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: Mount Discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Reginald Koettlitz, physician and botanist of the expedition. Glaciology. The Koettlitz Glacier appears to have been smaller during the Last Glacial Maximum (LGM) than it is today, while the Ross Ice Shelf was larger. There is evidence that during the LGM the mouth of the Pyramid Trough was blocked by grounded Ross Sea ice until at least 11,000 years ago.

Geographic entities mentioned:
surface_form: Pyramid Trough
instance_of: Valley
coordinates: lat: -78.3
lon: 163.45
As of 2017 only two of these islands are still connected to the ice tongue. Course. The glacier forms to the northeast of Mount Cocks and runs northeast to the north of the Mount Discovery massif. To the north of Hooper Crags it is joined from the west by Foster Glacier and then by Reneger Glacier, below Dromedary Glacier.

Geographic entities mentioned:
surface_form: Mount Discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Some may not contribute to the Koettlitz Glacier. Koettlitz Névé. A roughly circular névé about wide at the head of Koettlitz Glacier. The névé is bounded to the west and south by Mount Talmadge, Mount Rees and Mount Cocks; to the east by Mount Morning. Named by United States Advisory Committee on Antarctic Names (US-ACAN) (1994) in association with Koettlitz Glacier. Foster Glacier.

Geographic entities mentioned:
surface_form: Mount Talmadge
instance_of: Mountain
coordinates: lat: -78.41666667
lon: 162.56666667
surface_form: Mount Morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Pipecleaner Glacier. A glacier formed by the coalescence of numerous small alpine glaciers on the east side of Mount Huggins. Together with Glimpse Glacier it joins the Radian Glacier where that stream meets the north arm of Dismal Ridge. Its surface is marked by innumerable bands of moraine reminiscent of pipecleaners. Named by New Zealand VUWAE, 1960–61. Glimpse Glacier.

Geographic entities mentioned:
surface_form: Mount Huggins
instance_of: Mountain
coordinates: lat: -78.28333333
lon: 162.48333333
Its surface is marked by innumerable bands of moraine reminiscent of pipecleaners. Named by New Zealand VUWAE, 1960–61. Glimpse Glacier. An alpine glacier composed of two segments, separated by an icefall, which flow northeast from a névé in the area between Mount Kempe and Mount Huggins. It joins the Pipecleaner Glacier south of the confluence of the latter with the Radian Glacier.

Geographic entities mentioned:
surface_form: Mount Kempe
instance_of: Mountain
coordinates: lat: -78.31666667
lon: 162.71666667
Discovered by the BrNAE (1901–04) which named it for E.L. Somers Cocks, then Treasurer of the Royal Geographical Society. Barlow Rocks. A group of rocks standing below the NW slopes of Mount Morning on the south margin of upper Koettlitz Glacier. Named by US-ACAN in 1994 after Roger A. Barlow, USGS cartographer, a member of the satellite surveying team at South Pole Station, winter party 1992.

Geographic entities mentioned:
surface_form: Mount Morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Differences have been found between the Trialetian and the Caspian Mesolithic of the southeastern part of the Caspian Sea (represented by sites like Komishan, Hotu, Kamarband and Ali Tepe), even though the Caspian Mesolithic had previously been attributed to Trialetian by Kozłowski (1994, 1996 and 1999), Kozłowski and Aurenche 2005 and Peregrine and Ember 2002.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Relation with Kmlo-2. Kmlo-2 is a rock shelter situated on the west slope of the Kasakh River valley, on the Aragats massif, in Armenia. This site seems to present three different phases of occupation (11-10k cal BC, 9-8k cal BC and 6-5k cal BC). The lithic industry of the three phases show similarities such as the predominance of microliths, small cores and obsidian as raw material.

Geographic entities mentioned:
surface_form: Aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
History and origin. The Kesarwani were cultivators or traders of saffron (&quot;kesar&quot; in Hindustani) and originated from the Kashmir Valley of India. In the 12th century, many of the Kesarwani migrated to what today comprise the states of Bihar, Madhya Pradesh and Uttar Pradesh.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Langkloof railway. In April 1902, authority was granted for the construction of the Langkloof narrow gauge railway from Port Elizabeth via Humansdorp to Avontuur, a total distance of. It was to become one of the most important narrow gauge railways in South Africa and passed through districts which were famous for general agriculture and the export of wheat and fruit, especially apples.

Geographic entities mentioned:
surface_form: Langkloof
instance_of: Valley
countries: South Africa
coordinates: lat: -33.825
lon: 23.857777777778
Gulliver Nunatak. Gulliver Nunatak () is a nunatak with a flat, ice-free summit, high, at the north side of Adie Inlet, on the east coast of Graham Land, Antarctica. It was charted by the Falkland Islands Dependencies Survey (FIDS) and photographed from the air by the Ronne Antarctic Research Expedition (RARE) in 1947.

Geographic entities mentioned:
surface_form: gulliver nunatak
instance_of: Mountain
coordinates: lat: -66.2
lon: -62.6667
Between December 1862 and October 1863, several skirmishes took place in Barton as part of the American Civil War. Confederate forces sought to prevent the Union Army from invading the Tennessee Valley from their stronghold in Corinth, Mississippi. On December 12, 1862, the 1st Alabama Cavalry Regiment under the command of Col. T. W. Sweeny engaged troops under the command of Col. Phillip Roddey.

Geographic entities mentioned:
surface_form: Tennessee Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
Mount Borchgrevink. 9qy3d6ysjtstygt1sh98wj1a1bh1" xml:space="preserve">#REDIRECT Sør Rondane Mountains

Geographic entities mentioned:
surface_form: borchgrevink
instance_of: Mountain
coordinates: lat: -72.1167
lon: 23.1333
surface_form: mount borchgrevink
instance_of: Mountain
coordinates: lat: -72.1167
lon: 23.1333
His best finishing was the 35th place in the Men's giant slalom. Lara Colturi is the daughter of former Olympic champion Daniela Ceccarelli and ski coach Alessandro Colturi. She was born in Turin and grew up in Cesana Torinese in the Susa Valley. She has one younger brother, Yuri.

Geographic entities mentioned:
surface_form: Susa Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.133333333333
lon: 7.05
Enteromius mohasicus. &quot;Enteromius mohasicus&quot; is a species of ray-finned fish in the genus &quot;Enteromius&quot; which occurs in Lake Muhazi and Lake Kivu in central Africa.

Geographic entities mentioned:
surface_form: Lake Muhazi
instance_of: Lake
countries: Rwanda
coordinates: lat: -1.85
lon: 30.4
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
Madera High School. Madera High School is the first school and original high school in the central San Joaquin Valley city of Madera, California, serving students since 1894. The school colors are royal blue & white and its mascot is the coyote. History. Madera High School's layout has been changed over the years.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Outside of the video game series, Oro also appears in the ' comic book miniseries where Ibuki's final ninja exam is to challenge him. Together with her friends Elena and Makoto, she goes to the shrine on Mount Atago, where Oro has travelled to meditate. After the fight, Oro says that she actually made him think about using both hands and commends her on an entertaining challenge.

Geographic entities mentioned:
surface_form: Mount Atago
instance_of: Mountain
countries: Japan
coordinates: lat: 35.06
lon: 135.63416666667
Badenoch Group. The Badenoch Group is a sequence of metamorphosed Tonian age sedimentary rocks that outcrop across the Central Highlands of Scotland, east of the Great Glen. This rock sequence has formerly been referred to as the Central Highland Migmatite Complex and the Central Highland Division.

Geographic entities mentioned:
surface_form: Great Glen
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
The highest elevation in the Bald Hill area is. Though local residents often claim it to be the highest point on Long Island, that honor actually belongs to Jayne's Hill in the Town of Huntington at. Also, nearby Telescope Hill, about WSW, is slightly higher at. Bald Hill in Brookhaven should also not be confused with Bald Hill in Riverhead. History.

Geographic entities mentioned:
surface_form: Jayne's Hill
instance_of: Mountain
countries: United States
coordinates: lat: 40.815
lon: -73.425
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
The highest elevation in the Bald Hill area is. Though local residents often claim it to be the highest point on Long Island, that honor actually belongs to Jayne's Hill in the Town of Huntington at. Also, nearby Telescope Hill, about WSW, is slightly higher at. Bald Hill in Brookhaven should also not be confused with Bald Hill in Riverhead. History.

Geographic entities mentioned:
surface_form: Telescope Hill
instance_of: Mountain
countries: United States
coordinates: lat: 40.8447
lon: -73.0331
When first settled in the late 18th century, the area was called &quot;Bald Hills.&quot; While the elevation and views are impressive for Long Island, George Washington found the hills to be merely &quot;trifling&quot; when he passed through in April 1790. In 1897, the cross-Island Bicycle Path was opened and passed through the Bald Hill area. In 1970–71, Patchogue-Mt.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
Bald Hill (Farmingville, New York). Bald Hill, located in the hamlet of Farmingville, New York, part of the Town of Brookhaven, is one of the highest areas of elevation on Long Island. The highest elevation in the Bald Hill area is. Though local residents often claim it to be the highest point on Long Island, that honor actually belongs to Jayne's Hill in the Town of Huntington at.

Geographic entities mentioned:
surface_form: bald hill
instance_of: Mountain
countries: United States
coordinates: lat: 38.0825513
lon: -90.7120743
surface_form: bald hill
instance_of: Mountain
countries: United States
coordinates: lat: 47.83593
lon: -122.03318
surface_form: bald hill
instance_of: Mountain
countries: United States
coordinates: lat: 39.46777778
lon: -123.75638889
surface_form: bald hill (farmingville, new york)
instance_of: Mountain
countries: United States
coordinates: lat: 40.8439
lon: -73.0216
surface_form: bald hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.501666666667
lon: -73.916944444444