Sarmila/GeoWiki-Features huggingface dataset:
History. According to R. C. Majumdar, in the distant past, a course of the Ganges river probably used to reach the Bay of Bengal through the Dhaleshwari River. The Buriganga originated from the Dhaleshwari in the south of Savar, near Dhaka
When the Mughals made Dhaka their capital in 1610, the banks of the Buriganga were already a prime location for trade.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Miya people. The Miya people, alternatively identified as &quot;Na-Asamiya&quot; by themselves (lit. neo-Assamese), denote the progeny of Bengali Muslim migrants originating from the contemporary Rangpur District, Rajshahi, and Cumilla Divisions. These individuals established residence in the Brahmaputra Valley during the 20th century, coinciding with the period of British colonial rule in Assam.

Geographic entities mentioned:
surface_form: Brahmaputra Valley
instance_of: Valley
countries: India
coordinates: lat: 26.5983
lon: 92.4506
Boreray Blackface. The Boreray Blackface, also Hebridean Blackface or Boreray, is a rare Scottish breed of sheep originating on the St Kilda archipelago off the west coast of Scotland and surviving as a feral animal on one of the islands, Boreray. It was once reared for meat and wool, but is now used mainly for conservation grazing.

Geographic entities mentioned:
surface_form: Boreray
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.871278
lon: -8.491581
It has been extirpated from the wild on Saint Thomas, U.S. Virgin Islands, where it was first described in 1855, and now only grows there in cultivation. The plant is a member of the islands' montane flora. It occurs on one mountain peak on each of the three islands: Monte Pirata on Vieques, Bordeaux Mountain on St. John, and Gorda Peak on Virgin Gorda. Its natural habitat is dry to moist forests.

Geographic entities mentioned:
surface_form: Bordeaux Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 18.33416667
lon: -64.72861111
The country's tallest mountains are located in the Jayawijaya Mountains and the Sudirman Range in Papua. The highest peak, Puncak Jaya (), is located in the Sudirman Mountains. A string of volcanoes stretches from Sumatra to Nusa Tenggara, and then loops around through to the Banda Islands of Maluku to northeastern Sulawesi. Of the 400 volcanoes, approximately 150 are active.

Geographic entities mentioned:
surface_form: Puncak Jaya
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.0833333333333
lon: 137.18333333333
A string of volcanoes stretches from Sumatra to Nusa Tenggara, and then loops around through to the Banda Islands of Maluku to northeastern Sulawesi. Of the 400 volcanoes, approximately 150 are active. Two of the most violent volcanic eruptions in modern times occurred in Indonesia; in 1815 Mount Tambora in Sumbawa erupted killing 92,000 and in 1883, Krakatau, erupted killing 36,000.

Geographic entities mentioned:
surface_form: Mount Tambora
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.2452777777778
lon: 117.99277777778
&quot;total land area:&quot; 1,904,569 km2 (&quot;land:&quot; 1,811,569 km2 (699450 mi2),
Maritime claims: measured from claimed archipelagic baselines
&quot;exclusive economic zone:&quot; with
&quot;lowest point:&quot; Sea level at 0 m (sea surface level); southern portion of the Philippine Trench, east of Miangas at &quot;highest point:&quot; Puncak Jaya (also known as &quot;Carstensz Pyramid&quot;) 4,884 m
Irrigated land: 67,220 km2 (2005) (25,953 mi2)
Total renewable water resources: 2,019 km3 (2011) (484 mi3)
Natural resources: coal, petroleum, natural gas, tin, nickel, timber, bauxite, copper, fertile soils, gold, silver

Geographic entities mentioned:
surface_form: Puncak Jaya
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.0833333333333
lon: 137.18333333333
It is located in Tajikistan's Gorno-Badakhshan Autonomous Province stretches for about 170 km between the Yazgulyam River and the Bartang River in the western Pamirs. The range rises in a north-eastern direction from the border with Afghanistan toward its highest elevation at Independence Peak (6,974 m). The average elevation ranges between 4,500 and 6,000 m.

Geographic entities mentioned:
surface_form: Independence Peak
instance_of: Mountain
countries: Tajikistan
coordinates: lat: 38.511111111111
lon: 72.354166666667
History. In 1960, Sir Edmund Hillary was in the Everest region leading the 1960-61 Silver Hut expedition, an expedition studying high altitude physiology and looking for the Yeti. At a high camp one night he asked Sirdar Urkien what, above all, would he like for his children and the Sherpa people. Urkien asked for a school in his village of Khumjung.

Geographic entities mentioned:
surface_form: Everest region
instance_of: Valley
countries: Nepal
coordinates: lat: 27.805
lon: 86.71
There is a carry down trail on the north shore via a dirt road from Silver Bay. No motors are allowed on this lake. As of 2019-08-26 Google Maps has incorrect directions to the hiking trail head at Jabe Pond. From the south, take Split Rock road, not Terrace road (which crosses private property).

Geographic entities mentioned:
surface_form: split rock
instance_of: Mountain
countries: United States
coordinates: lat: 42.48083333
lon: -107.52888889
Jabe Pond. Jabe Pond is a lake located west of Silver Bay, New York. Fish species present in the lake are brook trout, rainbow smelt, brown trout, rainbow trout, and brown bullhead. There is a carry down trail on the north shore via a dirt road from Silver Bay. No motors are allowed on this lake. As of 2019-08-26 Google Maps has incorrect directions to the hiking trail head at Jabe Pond.

Geographic entities mentioned:
surface_form: jabe pond
instance_of: Lake
countries: United States
coordinates: lat: 43.70407
lon: -73.53844
There is a carry down trail on the north shore via a dirt road from Silver Bay. No motors are allowed on this lake. As of 2019-08-26 Google Maps has incorrect directions to the hiking trail head at Jabe Pond. From the south, take Split Rock road, not Terrace road (which crosses private property).

Geographic entities mentioned:
surface_form: jabe pond
instance_of: Lake
countries: United States
coordinates: lat: 43.70407
lon: -73.53844
Greenwood Township, St. Louis County, Minnesota. Greenwood Township is a township in Saint Louis County, Minnesota, United States. The population was 939 at the 2010 census. Saint Louis County Roads 77 and 115 are two of the main routes in the township. Greenwood Township is located along part of Lake Vermilion. The city of Tower is located immediately east-southeast of the township. Geography.

Geographic entities mentioned:
surface_form: Lake Vermilion
instance_of: Lake
countries: United States
coordinates: lat: 47.857908333333
lon: -92.299611111111
Pulsatilla nuttalliana. &quot;Pulsatilla nuttalliana&quot;, known as American pasqueflower, prairie pasqueflower, prairie crocus, or simply pasqueflower, is a flowering plant native to much of North America, from the western side of Lake Michigan, to northern Canada in the Northwest Territories, south to New Mexico in the southwestern United States.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
In terms of prominence, the Kaimaktsalan summit rises 1,758 metres above its surroundings. The frontier between the two countries runs across the summit. It is the third-highest peak in Greece after Mytikas and Smolikas and the fifth-highest in North Macedonia. Etymology. The word &quot;Kajmakčalan&quot; is of Ottoman Turkish origin and inspired by its white, snowy peak: ' means 'kaymak-like'.

Geographic entities mentioned:
surface_form: Smolikas
instance_of: Mountain
countries: Greece
coordinates: lat: 40.089722222222
lon: 20.926111111111
Kajmakčalan. Kajmakčalan (Kaimakchalan), Kaimaki, Kaimaktsalan or Voras (or or,), is a mountain on the border between Greece and North Macedonia. It is the southernmost and highest peak, of a range known in Greek as the Voras Mountains and in Macedonian as Nidže. In terms of prominence, the Kaimaktsalan summit rises 1,758 metres above its surroundings.

Geographic entities mentioned:
surface_form: kajmakčalan
instance_of: Mountain
countries: Greece
North Macedonia
coordinates: lat: 40.930277777778
lon: 21.786111111111
Kajmakčalan. Kajmakčalan (Kaimakchalan), Kaimaki, Kaimaktsalan or Voras (or or,), is a mountain on the border between Greece and North Macedonia. It is the southernmost and highest peak, of a range known in Greek as the Voras Mountains and in Macedonian as Nidže. In terms of prominence, the Kaimaktsalan summit rises 1,758 metres above its surroundings.

Geographic entities mentioned:
surface_form: kajmakčalan
instance_of: Mountain
countries: Greece
North Macedonia
coordinates: lat: 40.930277777778
lon: 21.786111111111
surface_form: kaimakchalan
instance_of: Mountain
countries: Greece
North Macedonia
coordinates: lat: 40.930277777778
lon: 21.786111111111
surface_form: kaimaki
instance_of: Mountain
countries: Greece
North Macedonia
coordinates: lat: 40.930277777778
lon: 21.786111111111
surface_form: voras
instance_of: Mountain
countries: Greece
North Macedonia
coordinates: lat: 40.930277777778
lon: 21.786111111111
surface_form: kaimaktsalan
instance_of: Mountain
countries: Greece
North Macedonia
coordinates: lat: 40.930277777778
lon: 21.786111111111
The frontier between the two countries runs across the summit. It is the third-highest peak in Greece after Mytikas and Smolikas and the fifth-highest in North Macedonia. Etymology. The word &quot;Kajmakčalan&quot; is of Ottoman Turkish origin and inspired by its white, snowy peak: ' means 'kaymak-like'. &quot;Kaymak&quot; in Turkish refers to a dairy product similar to clotted cream. Geology.

Geographic entities mentioned:
surface_form: kajmakčalan
instance_of: Mountain
countries: Greece
North Macedonia
coordinates: lat: 40.930277777778
lon: 21.786111111111
Climate. Kajmakčalan has a subarctic climate (Dfc) with short, cool summers and long, cold winters. History. During World War I, in September 1916, the Battle of Kaymakchalan between Serbian and Bulgarian troops took place at Kajmakčalan and around the adjacent peaks, resulting in a Serbian victory. There is a small church and crypt for the Serbian Army soldiers who died in the battle.

Geographic entities mentioned:
surface_form: kajmakčalan
instance_of: Mountain
countries: Greece
North Macedonia
coordinates: lat: 40.930277777778
lon: 21.786111111111
There is a small church and crypt for the Serbian Army soldiers who died in the battle. Near the top of the mountain, on the Greek side, there is a small church named &quot;St. Peter's&quot; (Sveti Petar in Serbian), the peak itself is called, besides Kajmakčalan, &quot;Profitis Ilias&quot; ().

Geographic entities mentioned:
surface_form: kajmakčalan
instance_of: Mountain
countries: Greece
North Macedonia
coordinates: lat: 40.930277777778
lon: 21.786111111111
Kajmakčalan. Kajmakčalan (Kaimakchalan), Kaimaki, Kaimaktsalan or Voras (or or,), is a mountain on the border between Greece and North Macedonia. It is the southernmost and highest peak, of a range known in Greek as the Voras Mountains and in Macedonian as Nidže. In terms of prominence, the Kaimaktsalan summit rises 1,758 metres above its surroundings.

Geographic entities mentioned:
surface_form: voras
instance_of: Mountain
countries: Greece
North Macedonia
coordinates: lat: 40.930277777778
lon: 21.786111111111
It is the southernmost and highest peak, of a range known in Greek as the Voras Mountains and in Macedonian as Nidže. In terms of prominence, the Kaimaktsalan summit rises 1,758 metres above its surroundings. The frontier between the two countries runs across the summit. It is the third-highest peak in Greece after Mytikas and Smolikas and the fifth-highest in North Macedonia. Etymology.

Geographic entities mentioned:
surface_form: kaimaktsalan
instance_of: Mountain
countries: Greece
North Macedonia
coordinates: lat: 40.930277777778
lon: 21.786111111111
Mukut Parbat. Mukut Parbat or Mukut Parvat (Hindi: मुकुट पर्वत) is a mountain in Uttarakhand India, and the 20th highest located entirely within India. Nanda Devi, is the highest mountain in this category. Mukut Parbat 96th highest peak in the world. There are two summits, the main peak is and other one (Mukut Parbat East) is.

Geographic entities mentioned:
surface_form: Nanda Devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
Nanda Devi, is the highest mountain in this category. Mukut Parbat 96th highest peak in the world. There are two summits, the main peak is and other one (Mukut Parbat East) is. It lies the Kamet Zaskar Range, which does not receive the heavy monsoon. Climbing history. Mukut Parbat was first climbed in 1951 by a team from New Zealand through its sharp and steep western ridge.

Geographic entities mentioned:
surface_form: Kamet
instance_of: Mountain
countries: India
coordinates: lat: 30.92
lon: 79.593333333333
However, when the South Korean team leader reviewed photos and reports from the 1999 team, the leader realized their error and confirmed the South Koreans had mistaken a lower summit as the true Eastern summit. Glaciers and rivers. The West (Paschimi) Kamet Glacier. The branches of the West Kamet Glacier head on the western slopes of Kamet, Abi Gamin, and Mukut Parbat and Dakhini Chamrao glacier

Geographic entities mentioned:
surface_form: kamet
instance_of: Mountain
countries: India
coordinates: lat: 30.92
lon: 79.593333333333
However, when the South Korean team leader reviewed photos and reports from the 1999 team, the leader realized their error and confirmed the South Koreans had mistaken a lower summit as the true Eastern summit. Glaciers and rivers. The West (Paschimi) Kamet Glacier. The branches of the West Kamet Glacier head on the western slopes of Kamet, Abi Gamin, and Mukut Parbat and Dakhini Chamrao glacier

Geographic entities mentioned:
surface_form: kamet
instance_of: Mountain
countries: India
coordinates: lat: 30.92
lon: 79.593333333333
surface_form: kamet
instance_of: Mountain
countries: India
coordinates: lat: 30.92
lon: 79.593333333333
surface_form: mukut parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.9522
lon: 79.5703
surface_form: abi gamin
instance_of: Mountain
countries: India
coordinates: lat: 30.93
lon: 79.6
Mukut Parbat. Mukut Parbat or Mukut Parvat (Hindi: मुकुट पर्वत) is a mountain in Uttarakhand India, and the 20th highest located entirely within India. Nanda Devi, is the highest mountain in this category. Mukut Parbat 96th highest peak in the world. There are two summits, the main peak is and other one (Mukut Parbat East) is.

Geographic entities mentioned:
surface_form: mukut parvat
instance_of: Mountain
countries: India
coordinates: lat: 30.9522
lon: 79.5703
surface_form: mukut parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.9522
lon: 79.5703
surface_form: मुकुट पर्वत
instance_of: Mountain
countries: India
coordinates: lat: 30.9522
lon: 79.5703
Mukut Parbat. Mukut Parbat or Mukut Parvat (Hindi: मुकुट पर्वत) is a mountain in Uttarakhand India, and the 20th highest located entirely within India. Nanda Devi, is the highest mountain in this category. Mukut Parbat 96th highest peak in the world. There are two summits, the main peak is and other one (Mukut Parbat East) is.

Geographic entities mentioned:
surface_form: mukut parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.9522
lon: 79.5703
Mukut Parbat or Mukut Parvat (Hindi: मुकुट पर्वत) is a mountain in Uttarakhand India, and the 20th highest located entirely within India. Nanda Devi, is the highest mountain in this category. Mukut Parbat 96th highest peak in the world. There are two summits, the main peak is and other one (Mukut Parbat East) is. It lies the Kamet Zaskar Range, which does not receive the heavy monsoon.

Geographic entities mentioned:
surface_form: mukut parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.9522
lon: 79.5703
Nanda Devi, is the highest mountain in this category. Mukut Parbat 96th highest peak in the world. There are two summits, the main peak is and other one (Mukut Parbat East) is. It lies the Kamet Zaskar Range, which does not receive the heavy monsoon. Climbing history. Mukut Parbat was first climbed in 1951 by a team from New Zealand through its sharp and steep western ridge.

Geographic entities mentioned:
surface_form: mukut parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.9522
lon: 79.5703
It lies the Kamet Zaskar Range, which does not receive the heavy monsoon. Climbing history. Mukut Parbat was first climbed in 1951 by a team from New Zealand through its sharp and steep western ridge. Edmund Cotter, Pasang Dawa Lama and Earle Riddiford reached its summit from the Dakhini Chamrao glacier which joins the Saraswati from the east.

Geographic entities mentioned:
surface_form: mukut parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.9522
lon: 79.5703
An Indian army led expedition in 1989 attempted the western ridge but several summit attempts were thwarted by high winds and cold. An Indian expedition from the Nehru Institute of Mountaineering made the first ascent of Mukut Parbat East in 1999. A South Korean expedition in 1998 claimed to have made the first ascent of the East summit.

Geographic entities mentioned:
surface_form: mukut parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.9522
lon: 79.5703
These projections of the Clyde Tunnel, Kingston Bridge and Erskine Bridge expand into aerial perspectives of the Firth of Clyde and Loch Lomond as Jim Kerr sings &quot;higher and higher&quot; while the camera 'takes off'. Clips of the band performing in a studio connect these narratives together. 12&quot; single. The album version of the song is slightly longer, at 4:25.

Geographic entities mentioned:
surface_form: Loch Lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
With twice the cargo capability and range, the HU-16 opened up new avenues of opportunity as was demonstrated in 1970. Flight and Ground crews of the 143rd assisted scientists and engineers of the Naval Underwater Systems Center, conducting studies of undersea acoustics, at Lake Tanganyika in Africa during April and again in August at Hudson Bay, Canada.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
Granada Hills, Los Angeles. Granada Hills is a neighborhood in the San Fernando Valley region of Los Angeles. The community has a sports program and a range of city recreation centers. The neighborhood has fourteen public and ten private schools. History. The Granada Hills area is situated on the traditional homelands of the Tongva and Chumash.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
O'Melveny Park, the second largest park in Los Angeles, consists of a large undeveloped area and a much smaller developed section with several dozen citrus trees, a small intermittent stream, and grass and picnic areas. This park includes hiking trails and fire roads, including a grassy promontory from which a view of the northeastern portion of the San Fernando Valley may be seen.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Track description. Starting on the western outskirts of Katoomba at the Explorers tree, the track descends via steep steps through the temperate rainforest of Nellies Glen to the Megalong Valley floor. Here in the valley the track passes the historical site of the abandoned shale mining Megalong Village and continues on through farmland past the Megalong Cemetery (this is just off the track).

Geographic entities mentioned:
surface_form: Megalong Valley
instance_of: Valley
countries: Australia
coordinates: lat: -33.733333333333
lon: 150.25
Blackthorn Peak. Blackthorn Peak, also known as Black Thorn, is a 4,117 foot (1,255 meter) mountain summit located at the head of Glacier Bay's Geikie Inlet in Glacier Bay National Park and Preserve, in the Fairweather Range of the Saint Elias Mountains, in southeast Alaska.

Geographic entities mentioned:
surface_form: blackthorn peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.5739
lon: -136.5717
The mountain was given its descriptive name in 1896 by Harry Fielding Reid, an American geophysicist who studied glaciology in Glacier Bay. Weather permitting, Blackthorn Peak can be seen from Glacier Bay, which is a popular destination for cruise ships. The months May through June offer the most favorable weather for viewing or climbing the peak. Climate.

Geographic entities mentioned:
surface_form: blackthorn peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.5739
lon: -136.5717
Climate. Based on the Köppen climate classification, Blackthorn Peak is located in a subpolar oceanic climate zone, with long, cold, snowy winters, and cool summers. Weather systems coming off the Gulf of Alaska are forced upwards by the Saint Elias Mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall.

Geographic entities mentioned:
surface_form: blackthorn peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.5739
lon: -136.5717
The district center is the town of Shindand, which has an active market area. Shindand Air Base is located near the town. The Kandahar–Herat Highway passes through the district. The Zerkoh Valley is in the district. History. The ancient name of Shindand was Esfezar as still an Iranian small city, more a village, close to the border of Afghanistan on the Iranian side.

Geographic entities mentioned:
surface_form: Zerkoh Valley
instance_of: Valley
countries: Afghanistan
Travel to Goose Lake is via a dirt road, along Forest Road 60, also called the Carson Guler Road, typically free of snow by late June. Fed by several streams, Goose Lake was dammed by a lava flow from Big Lava Bed, directly to the south. The lake is 58 acres in size and includes a boat launch and a campground with 18 primitive campsites.

Geographic entities mentioned:
surface_form: Big Lava Bed
instance_of: Landform
countries: United States
coordinates: lat: 45.88373
lon: -121.74869
surface_form: goose lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9411888
lon: -121.7644477
Goose Lake Campground offers a concrete boat ramp for launching small boats, kayaks and canoes. The campground also offers activities such as camping, hiking, and berry picking. Nearby places include the Big Lava Bed, south of the campground; a trail takes hikers through a landscape dotted with pine forest and basalt lava formations.

Geographic entities mentioned:
surface_form: Big Lava Bed
instance_of: Landform
countries: United States
coordinates: lat: 45.88373
lon: -121.74869
Goose Lake (Washington). Goose Lake, in the U.S. state of Washington, is located within the Gifford Pinchot National Forest. Travel to Goose Lake is via a dirt road, along Forest Road 60, also called the Carson Guler Road, typically free of snow by late June. Fed by several streams, Goose Lake was dammed by a lava flow from Big Lava Bed, directly to the south.

Geographic entities mentioned:
surface_form: goose lake (washington)
instance_of: Lake
countries: United States
coordinates: lat: 45.9411888
lon: -121.7644477
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Goose Lake (Washington). Goose Lake, in the U.S. state of Washington, is located within the Gifford Pinchot National Forest. Travel to Goose Lake is via a dirt road, along Forest Road 60, also called the Carson Guler Road, typically free of snow by late June. Fed by several streams, Goose Lake was dammed by a lava flow from Big Lava Bed, directly to the south.

Geographic entities mentioned:
surface_form: goose lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9411888
lon: -121.7644477
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Goose Lake (Washington). Goose Lake, in the U.S. state of Washington, is located within the Gifford Pinchot National Forest. Travel to Goose Lake is via a dirt road, along Forest Road 60, also called the Carson Guler Road, typically free of snow by late June. Fed by several streams, Goose Lake was dammed by a lava flow from Big Lava Bed, directly to the south.

Geographic entities mentioned:
surface_form: goose lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9411888
lon: -121.7644477
Fed by several streams, Goose Lake was dammed by a lava flow from Big Lava Bed, directly to the south. The lake is 58 acres in size and includes a boat launch and a campground with 18 primitive campsites. Popular for fishing in summer and early fall, Goose Lake contains brook, brown, and coastal cutthroat trout. History. Goose Lake formed when the Big Lava Bed dammed up a nearby stream.

Geographic entities mentioned:
surface_form: goose lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9411888
lon: -121.7644477
Popular for fishing in summer and early fall, Goose Lake contains brook, brown, and coastal cutthroat trout. History. Goose Lake formed when the Big Lava Bed dammed up a nearby stream. The blocked stream formed the lake. On the southeast side of the lake, there is a ghostly stand of dead trees rising from the water. Recreation.

Geographic entities mentioned:
surface_form: goose lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9411888
lon: -121.7644477
On the southeast side of the lake, there is a ghostly stand of dead trees rising from the water. Recreation. The lake is a popular spot for brook, brown and coastal cutthroat trout fishing. Goose Lake Campground offers a concrete boat ramp for launching small boats, kayaks and canoes. The campground also offers activities such as camping, hiking, and berry picking.

Geographic entities mentioned:
surface_form: goose lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9411888
lon: -121.7644477
Continue through the town on State Route 141 to where it ends and Forest Route 24 begins. Drive on Forest Route 24 to the junction with Forest Route 60 (Carson Guler Road) and follow Forest Route 60 (Carson Guler Road) for 1 mile to Goose Lake. From the West, Carson, take the Wind River Highway, north to the Old State Highway.

Geographic entities mentioned:
surface_form: goose lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9411888
lon: -121.7644477
From the West, Carson, take the Wind River Highway, north to the Old State Highway. Heading towards Panther Creek Campground, continue past the campground on Forest Route 65 to the 4 corners, junction of Forest Route 65 and 60 (Carson Guler Road). From here, turn right on Forest Route 60 (Carson Guler Road), and continue on to Goose Lake.

Geographic entities mentioned:
surface_form: goose lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9411888
lon: -121.7644477
Huckleberry picking is a popular pastime too. Accessibility. The lake is reached via 8 miles of narrow gravel road from the east of Trout Lake on State Route 141 north from SR 14, to the town of Trout Lake. Continue through the town on State Route 141 to where it ends and Forest Route 24 begins.

Geographic entities mentioned:
surface_form: trout lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5377039
lon: -73.7045568
surface_form: trout lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5377039
lon: -73.7045568
Until the collapse of the Safavid government, Nakhchivan was under the administrative jurisdiction of the Erivan Province (also known as Chokhur-e Sa'd). When Ottoman soldiers attacked the region later that year, Maqsud Sultan Kangarlu was ordered by Shah Abbas I to evacuate the entire area—including the Armenian community in the city of Julfa—to Qaradagh and Dizmar.

Geographic entities mentioned:
surface_form: Qaradagh
instance_of: Mountain
countries: Iran
coordinates: lat: 38.74
lon: 46.7
Etymology and habitat. The fruit-bearing fern is named after the department Quindío where the plant has been found. Synonyms for &quot;B. quinduensis&quot; are &quot;B. chocontana&quot;, &quot;B. nitida&quot; and &quot;B. muiscarum&quot;, named after the Muisca who inhabited the highlands of Colombia (Altiplano Cundiboyacense). The fern also has been discovered in Tolima.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
Haiduk Peak. Haiduk Peak is a peak, probably after Haiduk, district, Hungary or Hideghut (Haiduk), village of Rumania. Haiduk Peak is located on the Continental Divide on the border of Banff and Kootenay National Parks at the head of Haiduk Creek. The mountain was named in 1917, probably after the Haiduks of the Balkans. The name was adopted on 31 December 1928.

Geographic entities mentioned:
surface_form: haiduk peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1025
lon: -115.95111111111112
surface_form: kootenay
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
Haiduk Peak. Haiduk Peak is a peak, probably after Haiduk, district, Hungary or Hideghut (Haiduk), village of Rumania. Haiduk Peak is located on the Continental Divide on the border of Banff and Kootenay National Parks at the head of Haiduk Creek. The mountain was named in 1917, probably after the Haiduks of the Balkans. The name was adopted on 31 December 1928.

Geographic entities mentioned:
surface_form: haiduk peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1025
lon: -115.95111111111112
Haiduk Peak. Haiduk Peak is a peak, probably after Haiduk, district, Hungary or Hideghut (Haiduk), village of Rumania. Haiduk Peak is located on the Continental Divide on the border of Banff and Kootenay National Parks at the head of Haiduk Creek. The mountain was named in 1917, probably after the Haiduks of the Balkans. The name was adopted on 31 December 1928.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The Ibar (,), also known as the Ibër and Ibri (), is a river that flows through eastern Montenegro, northern Kosovo and central Serbia, with a total length of. The river begins in the Hajla mountain, in Rožaje, eastern Montenegro, and passes through southwestern Serbia and northern Kosovo, where it leads back into Serbia to flow into the West Morava river near Kraljevo, central Serbia.

Geographic entities mentioned:
surface_form: Hajla
instance_of: Mountain
countries: Montenegro
Kosovo
coordinates: lat: 42.784722222222
lon: 20.138472222222
Some scholars has theorized that the word Ibar is related to the Basque word for &quot;river&quot; (&quot;i-ba/r/i&quot;), which is also how the Ebro river in Spain may have received its name. Upper course. The Ibar originates from six springs on the Hajla mountain in eastern Montenegro. It generally flows north-east, passing through Ibarac, Rožaje, Radetina and Bać, after which it enters Serbia.

Geographic entities mentioned:
surface_form: Hajla
instance_of: Mountain
countries: Montenegro
Kosovo
coordinates: lat: 42.784722222222
lon: 20.138472222222
There, it makes a sharp, elbow turn to the north, flowing through Zvečan, Slatina, Sočanica, Leposavić, Dren and Lešak, entering southwestern Serbia at the village of Jarinje. In Kosovo. At Kosovo, the river is dammed, creating the artificial Gazivoda Lake (area, altitude, depth). Water from the lake is used for industrial and mining facilities in the Trepča area.

Geographic entities mentioned:
surface_form: Gazivoda Lake
instance_of: Lake
countries: Serbia
Kosovo
coordinates: lat: 42.961666666667
lon: 20.566944444444
Right on its elbow turn, the Ibar receives its longest (right) tributary, the Sitnica. In Serbia. Entering southwestern Serbia again, the river receives its major tributaries: the Raška, Studenica and Lopatnica, from the left, and the Jošanica. The gorge is carved between the mountains of Golija, Čemerno and Troglav from the east, and Kopaonik, Željin and Stolovi from the west.

Geographic entities mentioned:
surface_form: Golija
instance_of: Mountain
countries: Serbia
coordinates: lat: 43.337777777778
lon: 20.276666666667
surface_form: Čemerno
instance_of: Mountain
countries: Serbia
coordinates: lat: 43.559
lon: 20.4975
surface_form: Željin
instance_of: Mountain
countries: Serbia
coordinates: lat: 43.46681
lon: 20.75189
surface_form: Stolovi
instance_of: Mountain
countries: Serbia
coordinates: lat: 43.60916667
lon: 20.61138889
Becky Hollow. Becky Hollow is a valley in Oregon County in the U.S. state of Missouri. Becky Hollow's name is derived from Rebecca &quot;Becky&quot; Willoby, an early settler of the area. Becky Hollow is surrounded by a number of current and former mines and prospecting sites, as the area is rich in minerals such as pyrite, quartz, and hematite.

Geographic entities mentioned:
surface_form: becky hollow
instance_of: Valley
countries: United States
coordinates: lat: 36.8192226
lon: -91.3776362
Becky Hollow. Becky Hollow is a valley in Oregon County in the U.S. state of Missouri. Becky Hollow's name is derived from Rebecca &quot;Becky&quot; Willoby, an early settler of the area. Becky Hollow is surrounded by a number of current and former mines and prospecting sites, as the area is rich in minerals such as pyrite, quartz, and hematite.

Geographic entities mentioned:
surface_form: becky hollow
instance_of: Valley
countries: United States
coordinates: lat: 36.8192226
lon: -91.3776362
surface_form: becky hollow
instance_of: Valley
countries: United States
coordinates: lat: 36.8192226
lon: -91.3776362
While cotton accounts for 2.4% of world water use, the water is consumed in regions that are already at a risk of water shortage. Significant environmental damage has been caused: for example, the diversion of water by the former Soviet Union from the Amu Darya and Syr Darya rivers to produce cotton was largely responsible for the disappearance of the Aral Sea. As a scientific standard.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
Common impurities include metal salts and oxides, including copper, iron, calcium and lead, and harmful bacteria, such as &quot;Vibrio&quot;. Some solutes are acceptable and even desirable for taste enhancement and to provide needed electrolytes. The single largest (by volume) freshwater resource suitable for drinking is Lake Baikal in Siberia. Chemical uses.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
The steep, narrow, sandstone-capped ridge extends from northern Bath County, Virginia to southern Hardy County, West Virginia. Along the way, its crest defines the borders between Highland and Augusta counties, Virginia, and between Pendleton County, West Virginia, and Rockingham County, Virginia. Its high point is 4397’/1340 m Reddish Knob along the Virginia/West Virginia border.

Geographic entities mentioned:
surface_form: Reddish Knob
instance_of: Landform
Mountain
countries: United States
coordinates: lat: 38.462388651563245
lon: -79.24175543749658
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.924722222222
lon: -74.288055555556
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.3209
lon: -74.6616
Its high point is 4397’/1340 m Reddish Knob along the Virginia/West Virginia border. Located in the Ridge and Valley physiographic province of the Appalachian Mountains, Shenandoah Mountain forms part of the western margin of the Shenandoah Valley, and is part of the easternmost Allegheny Mountains. It lies almost entirely within the George Washington National Forest. U.S.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
surface_form: shenandoah
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
surface_form: shenandoah mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.5097
lon: -79.1842
Shenandoah Mountain. Shenandoah Mountain is a mountain ridge approximately long in Virginia and West Virginia. The steep, narrow, sandstone-capped ridge extends from northern Bath County, Virginia to southern Hardy County, West Virginia.

Geographic entities mentioned:
surface_form: shenandoah
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
surface_form: shenandoah mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.5097
lon: -79.1842
Shenandoah Mountain. Shenandoah Mountain is a mountain ridge approximately long in Virginia and West Virginia. The steep, narrow, sandstone-capped ridge extends from northern Bath County, Virginia to southern Hardy County, West Virginia.

Geographic entities mentioned:
surface_form: shenandoah
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: shenandoah mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.5097
lon: -79.1842
It lies almost entirely within the George Washington National Forest. U.S. Route 33 crosses the mountain between Franklin, West Virginia, and Harrisonburg, Virginia. Other Shenandoah Mountain high peaks are Flagpole Knob (Virginia; 4383’/1336 m), and Bald Knob (Virginia; 3680’/1122 m).

Geographic entities mentioned:
surface_form: shenandoah
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
surface_form: shenandoah mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.5097
lon: -79.1842
surface_form: high peaks
instance_of: Mountain
countries: United States
coordinates: lat: 45
lon: -70.4
surface_form: bald knob
instance_of: Mountain
countries: United States
coordinates: lat: 37.6569958
lon: -90.5142889
Its high point is 4397’/1340 m Reddish Knob along the Virginia/West Virginia border. Located in the Ridge and Valley physiographic province of the Appalachian Mountains, Shenandoah Mountain forms part of the western margin of the Shenandoah Valley, and is part of the easternmost Allegheny Mountains. It lies almost entirely within the George Washington National Forest. U.S.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
The municipality has a population of () and covers an area of of which is water. The population density is. Neighbour municipalities are Pielavesi, Pihtipudas, Tervo, Vesanto and Viitasaari. Despite its name, the municipality is not located by the lake Keitele. The shortest distance between the municipality and the lake is roughly ten kilometers. The municipality is unilingually Finnish.

Geographic entities mentioned:
surface_form: lake Keitele
instance_of: Lake
countries: Finland
coordinates: lat: 62.933333333333
lon: 26.033333333333
Description. The creek rises on the south end of a spring-fed marsh area in the northern part of Juab Valley, in eastern Juab County, about south‑southeast of the Burriston Ponds, west of Interstate 15, and about north‑northwest of the center of the city of Nephi, with an approximate elevation of. From its source the creek runs north‑northwest though the marsh area.

Geographic entities mentioned:
surface_form: Juab Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5913
lon: -111.962
A short way down the canyon, the creek passes back under Goshen Canyon Road. Midway through the canyon the creek leaves Juab County and enters Utah County. The creek then continues flowing northwest from the canyon through the Goshen Valley until it reaches its confluence with Kimball Creek and then enters the Goshen Reservoir. Immediately north of the reservoir, the creek passes under U.S.

Geographic entities mentioned:
surface_form: Goshen Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.093888888889
lon: -111.93
Olsokbreen is a southern branch of the glacier Mefonna, which also has the northern branch Samarinbreen. Tributary glaciers to Olsokbreen are Kvithettbreen and Valettebreen, both coming from the east, from or between the mountains of Snøkrossen, Gråtinden, Kvithetta, Haitanna and Guilbaudtoppen. Olsokbreen is one of the 163 tidewater glaciers in Svalbard.

Geographic entities mentioned:
surface_form: Haitanna
instance_of: Mountain
countries: Norway
coordinates: lat: 76.7815
lon: 16.6019
surface_form: Guilbaudtoppen
instance_of: Mountain
countries: Norway
coordinates: lat: 76.7636
lon: 16.5907
West Lothian (historic). West Lothian, also known as Linlithgowshire (its official name until 1925), is a historic county in the east central Lowlands of Scotland. It is bounded geographically by the Avon to the west and the Almond to the east.

Geographic entities mentioned:
surface_form: central Lowlands
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408
lon: -4.044
The type specimen was discovered in the East Kirkton Limestone at the East Kirkton Quarry in 1984. West Lothian was extensively settled in prehistoric times, and several ancient burial sites have been uncovered, such as at Cairnpapple Hill, described as one of Scotland's richest archaeological sites and one of the earlier places of organised worship in the country.

Geographic entities mentioned:
surface_form: Cairnpapple Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.928055555556
lon: -3.6225
It had an area of 120 sq. miles (310 km2), making it the third-smallest of Scotland's 33 counties and smaller than the modern council area. The geology of West Lothian is typical for the Midland valley area geological of Scotland. Most of the bedrock surface area is underlaid by Carboniferous sedimentary rocks running in strips from north to south, with a variety of glacial deposits.

Geographic entities mentioned:
surface_form: Midland valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408
lon: -4.044
Two thirds of the land is agricultural, while a tenth is urban. Significant watercourses include the Almond and the Union Canal, while the main bodies of water are Linlithgow Loch, Dundas Loch, Humbie Reservoir, Lochcote Reservoir, Beecraigs Loch and Bangour Reservoir. The small island of Inchgarvie near the Forth Bridge lies within the historic borders of the county.

Geographic entities mentioned:
surface_form: Linlithgow Loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.980555555556
lon: -3.6
In 2008, he played in all 16 games for the second-consecutive season. He made five special team tackles in 2008. Dorenbos arrived late to training camp in 2009 after he caught shingles and could not get on an airplane to fly to Lehigh Valley, Pennsylvania, where Eagles training camp was held. He played in all 16 games in 2009, and made four special team tackles.

Geographic entities mentioned:
surface_form: Lehigh Valley, Pennsylvania
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
His offer this time included his readiness to recognize the legitimacy of the concessions made by his uncle and opponent al-Salih Ismail, the Ayyubid emir of Damascus, to the Crusaders, so that Jaffa and Ascalon, and all of Jerusalem, including Bethlehem and Majdal Yaba, in addition to Tiberias, Safed, Mount Tabor and the castles of Belvoir, were all included in the Kingdom of Jerusalem.

Geographic entities mentioned:
surface_form: Mount Tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
This was also where the community gathered to confess their sins publicly. The sculpture in the abbey, which is some of the finest in Ireland, suggests links to French styles of the period. The grounds of the abbey also contain a monks' fishing house, probably built in the 15th or 16th century, on an island in the River Cong leading towards nearby Lough Corrib.

Geographic entities mentioned:
surface_form: Lough Corrib
instance_of: Lake
countries: Ireland
coordinates: lat: 53.466666666667
lon: -9.2833333333333
Lake Superior Chippewa. The Lake Superior Chippewa (Anishinaabe: Gichigamiwininiwag) are a large number of Ojibwe (Anishinaabe) bands living around Lake Superior; this territory is considered part of northern Michigan, Wisconsin, and Minnesota in the United States.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
History. Up until 1854, the square was little more than a public green and an informal meeting place. Much of it was used for the Catholic Sainte-Antoine Cemetery, a hastily arranged cemetery for the victims of the 1851 Cholera Epidemic. In that year, the bodies were exhumed and moved to Notre-Dame-des-Neiges Cemetery on the northwestern side of Mount Royal. In 1869, St.

Geographic entities mentioned:
surface_form: Mount Royal
instance_of: Mountain
countries: Canada
coordinates: lat: 45.506388888889
lon: -73.588888888889
Uetliberg railway station. Uetliberg railway station, situated near the summit of Uetliberg mountain, the &quot;Hausberg&quot; of the city of Zurich in Switzerland, is the upper terminus of the Uetliberg line of the Sihltal Zürich Uetliberg Bahn (SZU), within fare zone 155 of the Zürcher Verkehrsverbund (ZVV).

Geographic entities mentioned:
surface_form: Uetliberg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.349722222222
lon: 8.4902777777778
It is endemic to Australia. It was described in 1918 by Australian arachnologists William Joseph Rainbow and Robert Henry Pulleine. Distribution and habitat. The species occurs in south-east Queensland in closed forest habitats. The type locality is Tamborine Mountain, in the Scenic Rim Region. Behaviour. The spiders are fossorial, terrestrial predators.

Geographic entities mentioned:
surface_form: Tamborine Mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -27.927513888889
lon: 153.19430555556
Revaya. Revaya () is a moshav in the Beit She'an Valley in northern Israel. Located about six kilometres south of Beit She'an, near Sde Trumot and west of Israel Highway 90, it falls under the jurisdiction of Valley of Springs Regional Council. In it had a population of. The moshav is one of four settlements established as a group: Revaya, Sde Trumot, Tel Teomim, and Rehov. History.

Geographic entities mentioned:
surface_form: Beit She'an Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.4794
lon: 35.5058
It was originally named &quot;Farwana B&quot;, corresponding to the adjacent &quot;Farwana&quot; (Tel Rehov); the name was later changed to Revaya, corresponding to the nearby Revaya spring (the Hebrew word &quot;revaya&quot; means &quot;overflowing&quot; or &quot;saturated&quot;). The moshav accepted some Ethiopian Jews who immigrated to Israel in the 1990s.

Geographic entities mentioned:
surface_form: Tel Rehov
instance_of: Mountain
countries: Israel
coordinates: lat: 32.457125
lon: 35.498241666667
Kumano River. The is a river in the Kii Peninsula of central Japan, located in Nara, Wakayama and Mie Prefectures. It is long and has a watershed of. The river rises from Mount Ōmine in the Yoshino-Kumano National Park in Tenkawa, Nara and follows a generally southward course to drain into the Pacific Ocean on the border between Shingū, Wakayama and Kihō, Mie.

Geographic entities mentioned:
surface_form: Mount Ōmine
instance_of: Mountain
countries: Japan
coordinates: lat: 34.252777777778
lon: 135.94055555556