Sarmila/GeoWiki-Features huggingface dataset:
In the middle of the mountain there is a small U-valley where the waterfall begins, and the U-valley lies between two mountain peaks as seen in the image. Melderskin is the nearest mountain to Ben Nevis (the highest mountain in the United Kingdom) that is higher than Ben Nevis, and therefore defines the topographic isolation of Ben Nevis:.

Geographic entities mentioned:
surface_form: Ben Nevis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.796891
lon: -5.003675
surface_form: ben nevis
instance_of: Mountain
countries: Norway
coordinates: lat: 79.6474
lon: 12.4189
surface_form: ben nevis
instance_of: Mountain
countries: Norway
coordinates: lat: 79.6474
lon: 12.4189
surface_form: ben nevis
instance_of: Mountain
countries: Norway
coordinates: lat: 79.6474
lon: 12.4189
surface_form: melderskin
instance_of: Mountain
countries: Norway
coordinates: lat: 60.0065
lon: 6.08153
Melderskin. Melderskin is a mountain peak in Kvinnherad kommune in Hordaland. The mountain, which has a height of above sea level, is located just behind Barony of Rosendal. In the middle of the mountain there is a small U-valley where the waterfall begins, and the U-valley lies between two mountain peaks as seen in the image.

Geographic entities mentioned:
surface_form: melderskin
instance_of: Mountain
countries: Norway
coordinates: lat: 60.0065
lon: 6.08153
Bivens Arm. Bivens Arm is a body of water in Gainesville, Florida. Located west of U.S. Route 441 and south of Archer Road, it is a part of Paynes Prairie. Bivens Arm is a small shallow lake covering approximately in southwest Gainesville. Bivens Arm is a unique environment, which supports a wide diversity of plant and animal life in an urban setting.

Geographic entities mentioned:
surface_form: shallow lake
instance_of: Lake
countries: United States
coordinates: lat: 43.49
lon: -74.444
surface_form: bivens arm
instance_of: Lake
countries: United States
coordinates: lat: 29.6245
lon: -82.344588888889
Bivens Arm. Bivens Arm is a body of water in Gainesville, Florida. Located west of U.S. Route 441 and south of Archer Road, it is a part of Paynes Prairie. Bivens Arm is a small shallow lake covering approximately in southwest Gainesville. Bivens Arm is a unique environment, which supports a wide diversity of plant and animal life in an urban setting.

Geographic entities mentioned:
surface_form: bivens arm
instance_of: Lake
countries: United States
coordinates: lat: 29.6245
lon: -82.344588888889
Route 441 and south of Archer Road, it is a part of Paynes Prairie. Bivens Arm is a small shallow lake covering approximately in southwest Gainesville. Bivens Arm is a unique environment, which supports a wide diversity of plant and animal life in an urban setting. Tumblin Creek, which is fed by small springs and seeps, drains into Bivens Arm and is the primary source of drainage into the lake.

Geographic entities mentioned:
surface_form: bivens arm
instance_of: Lake
countries: United States
coordinates: lat: 29.6245
lon: -82.344588888889
Bivens Arm is a unique environment, which supports a wide diversity of plant and animal life in an urban setting. Tumblin Creek, which is fed by small springs and seeps, drains into Bivens Arm and is the primary source of drainage into the lake. Bivens Arm overflows onto Paynes Prairie and eventually discharges to the aquifer via Alachua Sink. History.

Geographic entities mentioned:
surface_form: bivens arm
instance_of: Lake
countries: United States
coordinates: lat: 29.6245
lon: -82.344588888889
Bivens Arm overflows onto Paynes Prairie and eventually discharges to the aquifer via Alachua Sink. History. The early history of Bivens Arm is not well documented given that it is a relatively small body of water. The earliest known use of the land around the lake was as hunting grounds by Native Americans.

Geographic entities mentioned:
surface_form: bivens arm
instance_of: Lake
countries: United States
coordinates: lat: 29.6245
lon: -82.344588888889
Beginning in the late 1800s, the land was used mostly for agricultural purposes including cattle ranching, swine farms, vegetable farms, and orange groves. In the 1930s, Bivens Arm was designated as a bird sanctuary and rookery and even had a resident ranger to care for the sanctuary. In 1965, the state of Florida designated the lake area as a wildlife sanctuary (Bill No. 1356 Chap. 65 1005).

Geographic entities mentioned:
surface_form: bivens arm
instance_of: Lake
countries: United States
coordinates: lat: 29.6245
lon: -82.344588888889
In 1965, the state of Florida designated the lake area as a wildlife sanctuary (Bill No. 1356 Chap. 65 1005). In 1981, the City of Gainesville purchased the land between the lake and Williston Road (SR 331) to form the Bivens Arm Nature Park. This park features a lush Live Oak Hammock habitat and marshlands, which periodically become inundated with rising water levels from the lake.

Geographic entities mentioned:
surface_form: bivens arm
instance_of: Lake
countries: United States
coordinates: lat: 29.6245
lon: -82.344588888889
Course. The Panther–Wotan line went in a north-south direction, stretching from Narva at the Baltic Sea in the north to the Dnieper Estuary at the Black Sea in the south. The line ran along the Narva river, the western shore of Lake Peipus, followed the course of the Velikaya river, and then crossed land to Vitebsk, Mogilev, Gomel, and Kiev respectively.

Geographic entities mentioned:
surface_form: Lake Peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
Besides loaning five bucks to every newspaperman down on his luck 'Curley' brought up his young brother Saul, now one of Southern California's leading dermatologists.&quot; Years later, San Fernando Valley newspaper columnist Florabel Muir recalled that when she'd been a young scenario writer at Universal Studios, one of Carl Laemmle's male relatives who lived on the studio lot had a weakness for slot machines.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Käbelicksee. Käbelicksee is a lake in the Mecklenburgische Seenplatte district in Mecklenburg-Vorpommern, Germany. It is part of the Müritz National Park. At an elevation of 62.4 m, its surface area is 2.64 km².

Geographic entities mentioned:
surface_form: käbelicksee
instance_of: Lake
countries: Germany
coordinates: lat: 53.417308333333
lon: 12.942580555556
Käbelicksee. Käbelicksee is a lake in the Mecklenburgische Seenplatte district in Mecklenburg-Vorpommern, Germany. It is part of the Müritz National Park. At an elevation of 62.4 m, its surface area is 2.64 km².

Geographic entities mentioned:
surface_form: müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
The St. Onuphrius Monastery () is an Orthodox monastery for women located in the potter's field (&quot;Akeldama&quot; in Aramaic) that the Jewish elders purchased with the thirty pieces of silver returned by Judas Iscariot that had been given for betraying Jesus. The location is south of the Old City of Jerusalem and on the southern slope of the Gehenna valley, close to the Kidron Valley.

Geographic entities mentioned:
surface_form: Gehenna
instance_of: Valley
countries: Israel
coordinates: lat: 31.76916667
lon: 35.22805556
surface_form: Kidron Valley
instance_of: Valley
countries: State of Palestine
coordinates: lat: 31.776972222222224
lon: 35.23897222222222
Katun (river). The Katun (;) is a river in the Altai Republic and the Altai Krai of Russia. It forms the Ob as it joins the Biya some southwest of Biysk. The Katun is long, and its drainage basin covers. It originates in the Katun glaciers on the southwestern slope of Belukha Mountain. The river freezes up in late November or early December and breaks up in early or mid-April.

Geographic entities mentioned:
surface_form: Belukha Mountain
instance_of: Mountain
countries: Russia
Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 49.806944444444
lon: 86.589722222222
He retired from TBS in 1995, because he disagreed with the active commercialization of television. In April 1991, he shot a film, with a group of Japanese journalists, about the state of the Aral Sea in Kazakhstan. From January 1996, he engaged in organic farming with rice and mushrooms in the Abukuma mountains in the town Takine, near Tamura, Fukushima, Fukushima Prefecture.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
R. Koolemans Beynen was third officer. The expedition sailed from Southampton late in June 1875, but heavy ice in Peel Sound prevented the vessel from reaching the search area, and the expedition returned unsuccessful. By this time Lady Franklin had died. In 1876 Allen Young took the &quot;Pandora&quot; on a second voyage to the Arctic with stores to relieve the British Arctic Expedition.

Geographic entities mentioned:
surface_form: Peel Sound
instance_of: Watercourse
countries: Canada
coordinates: lat: 73
lon: -96.5
For example, during the 2003 World Series, the company would have given away a free soft drink and a taco to everyone in the United States if a player hit a home run onto a sign placed in Pro Player Stadium. A similar promotion had been staged in the 2002 World Series, with a floating target placed in McCovey Cove in San Francisco.

Geographic entities mentioned:
surface_form: McCovey Cove
instance_of: Body of water
countries: United States
coordinates: lat: 37.7772
lon: -122.388
Inveruglas Isle. Inveruglas Isle () is a small uninhabited island within Loch Lomond, and lies off the shore at Inveruglas opposite Inversnaid at the north end of the loch. It is opposite the Loch Sloy powerstation. The name &quot;Inbhir Dhu(bh)ghlais&quot; means &quot;mouth of the black stream&quot;; Inveruglas Isle is therefore, quite literally, the island at the mouth of the black stream.

Geographic entities mentioned:
surface_form: Loch Lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
The construction of a hydroelectric dam would also supply the city with much needed power. A major issue with converting the Hetch Hetchy Valley into a municipally owned reservoir was that it was within the borders of the newly formed Yosemite National Park.

Geographic entities mentioned:
surface_form: Hetch Hetchy Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.9475
lon: -119.78694444
Bosque Peak. Bosque Peak is located on the western flank of the Manzano Mountains in Torrance County, New Mexico. Bosque Peak is within the Cibola National Forest and is ranked the 318th highest peak in New Mexico, and 101st by prominence.

Geographic entities mentioned:
surface_form: bosque peak
instance_of: Mountain
countries: United States
coordinates: lat: 34.765555555556
lon: -106.42972222222
In July 2024, California Resources Corporation completed a $2.1 billion, all-stock purchase acquisition of Aera. Business areas. Most of Aera's production is located in the San Joaquin Valley. The company also has oil field operations in Ventura, Monterey and Fresno counties and has begun the permitting process to redevelop the East Cat Canyon oilfield in northern Santa Barbara County.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Mount Adam Joachim. Mount Adam Joachim is a mountain four kilometres ENE of Gong Lake in Canada's Jasper National Park. It was named in 1968 by J. Monroe Thorington after Adam Joachim. Joachim, a partial Cree Indian, was a horse packer who accompanied Alfred J. Ostheimer on his 1927 expedition into the Columbia Icefield.

Geographic entities mentioned:
surface_form: Gong Lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.076
lon: -83.534
surface_form: mount adam
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1206
lon: -126.223
surface_form: mount adam joachim
instance_of: Mountain
countries: Canada
coordinates: lat: 52.404444444444444
lon: -117.52777777777777
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Adam Joachim. Mount Adam Joachim is a mountain four kilometres ENE of Gong Lake in Canada's Jasper National Park. It was named in 1968 by J. Monroe Thorington after Adam Joachim. Joachim, a partial Cree Indian, was a horse packer who accompanied Alfred J. Ostheimer on his 1927 expedition into the Columbia Icefield.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Mount Adam Joachim. Mount Adam Joachim is a mountain four kilometres ENE of Gong Lake in Canada's Jasper National Park. It was named in 1968 by J. Monroe Thorington after Adam Joachim. Joachim, a partial Cree Indian, was a horse packer who accompanied Alfred J. Ostheimer on his 1927 expedition into the Columbia Icefield.

Geographic entities mentioned:
surface_form: mount adam
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1206
lon: -126.223
surface_form: mount adam joachim
instance_of: Mountain
countries: Canada
coordinates: lat: 52.404444444444444
lon: -117.52777777777777
SR 178 serves many different purposes. It connects Downtown Bakersfield with East Bakersfield and Lake Isabella. It is one of three crossings over the Sierra Nevada south of Yosemite (SR 120, Tioga Pass Road), connecting the southern San Joaquin Valley with the upper Mojave Desert and the Owens Valley. This also provides access to Death Valley National Park.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
Here, the highway becomes gentler, and widens to a four-lane undivided expressway. The route continues east and reaches the town of Lake Isabella in the Kern River Valley. The road briefly expands to a divided freeway, and meets a junction with State Route 155 at an overpass, before narrowing back to a two-lane undivided highway at the intersection with Lake Isabella Boulevard.

Geographic entities mentioned:
surface_form: Kern River Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.6232
lon: -118.4845
Then, the highway descends eight miles to an intersection with State Route 14 at Freeman, an elevation of. SR 178 runs concurrently with SR 14 for three miles, then proceeds eastward across the Indian Wells Valley into the city of Ridgecrest. The constructed highway then ends east of Ridgecrest at the turnoff for the Trona Pinnacles National Natural Landmark in Searles Valley.

Geographic entities mentioned:
surface_form: Indian Wells Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.702777777778
lon: -117.68638888889
Then, the highway descends eight miles to an intersection with State Route 14 at Freeman, an elevation of. SR 178 runs concurrently with SR 14 for three miles, then proceeds eastward across the Indian Wells Valley into the city of Ridgecrest. The constructed highway then ends east of Ridgecrest at the turnoff for the Trona Pinnacles National Natural Landmark in Searles Valley.

Geographic entities mentioned:
surface_form: Searles Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.6
lon: -117.3
Eastern extensions have been constructed since 1968, one interchange at a time as the need arises. In the Kern Canyon section, which is between Bakersfield and the Kern River Valley, a bypass route was identified in 1964. By 1968, a deed from the US Forest Service issued an easement to the State for the construction of the highway through National Forest lands.

Geographic entities mentioned:
surface_form: Kern River Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.6232
lon: -118.4845
It is a tributary of the Connecticut River, which flows south to Long Island Sound, an arm of the Atlantic Ocean. Perry Stream rises in the highlands forming the Canada–United States border, just west of the Connecticut Lakes. The entire length of the stream is within the town of Pittsburg, New Hampshire, the largest town in the state.

Geographic entities mentioned:
surface_form: Connecticut Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 45.0936
lon: -71.2478
In 2008 the album &quot;Pilegrim&quot; was released to great acclaim, securing the third bestseller in a row for the artist. In the autumn of the same year Nordstoga, together with his brother Aasmund Nordstoga and fiddler Per Anders Buen Garnås, toured Norway with a revamped version of the Storegut performance. &quot;Strålande Jul&quot; and sales record.

Geographic entities mentioned:
surface_form: Storegut
instance_of: Mountain
countries: Norway
coordinates: lat: 61.43
lon: 8.24167
The river was called Tokmak () by the Nogais. The Molochna is formed by the confluence of the Chynhul and Tokmak rivers, just north of Molochansk. It flows roughly southwards, through Melitopol and into the Molochnyi Estuary in the Azov Sea. Its length is and its drainage basin is 3,450 km2. A former island in the river contains the archaeological site of Kamyana Mohyla.

Geographic entities mentioned:
surface_form: Molochnyi Estuary
instance_of: Lake
countries: Ukraine
Soviet Union
Russian Empire
Russia
coordinates: lat: 46.50163
lon: 35.35004
Bolton Lake (Kenora District). Bolton Lake is a lake in Kenora District, Ontario, Canada. It is about long and wide, and lies at an elevation of about south of the community of Dryden. The primary outflow is an unnamed creek, which flows into Lower Manitou Lake just south of Watson's Narrows. Bolton Lake lies just west over a small ridge of Bolton Bay on Lower Manitou Lake.

Geographic entities mentioned:
surface_form: bolton lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.8525
lon: -81.0286
surface_form: bolton lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.2667
lon: -95.7833
surface_form: bolton lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.4003
lon: -80.2631
surface_form: bolton lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.7003
lon: -67.5853
surface_form: bolton lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.7831
lon: -126.417
surface_form: bolton lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.5667
lon: -108.684
surface_form: bolton lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3467
lon: -92.8272
Bolton Lake (Kenora District). Bolton Lake is a lake in Kenora District, Ontario, Canada. It is about long and wide, and lies at an elevation of about south of the community of Dryden. The primary outflow is an unnamed creek, which flows into Lower Manitou Lake just south of Watson's Narrows. Bolton Lake lies just west over a small ridge of Bolton Bay on Lower Manitou Lake.

Geographic entities mentioned:
surface_form: bolton lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.8525
lon: -81.0286
surface_form: bolton lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.2667
lon: -95.7833
surface_form: bolton lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.4003
lon: -80.2631
surface_form: manitou lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.7167
lon: -109.717
surface_form: bolton lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.7003
lon: -67.5853
surface_form: bolton lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.7831
lon: -126.417
surface_form: bolton lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.5667
lon: -108.684
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
surface_form: bolton lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3467
lon: -92.8272
Bolton Lake (Kenora District). Bolton Lake is a lake in Kenora District, Ontario, Canada. It is about long and wide, and lies at an elevation of about south of the community of Dryden. The primary outflow is an unnamed creek, which flows into Lower Manitou Lake just south of Watson's Narrows. Bolton Lake lies just west over a small ridge of Bolton Bay on Lower Manitou Lake.

Geographic entities mentioned:
surface_form: manitou lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.7167
lon: -109.717
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
Belford railway station, New South Wales. Belford railway station was a railway station on the Main North railway line. It served the settlement of Belford in the Hunter Region of New South Wales, Australia. Services were provided by CityRail's Hunter line until 4 September 2005, when the station was closed for safety reasons. The station consisted of 2 platforms about 3 metres long.

Geographic entities mentioned:
surface_form: Hunter Region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Tobin became a widow in 1918. Seán Treacy, Dan Breen and Seán Hogan arrived on her doorstep on 22 January 1919, they had walked across the Galtees from Soloheadbeg. She hid the men then, and went on to hide men, arms, documents and evidence, she would clean guns and deliver people and messages for the Irish Republican Army. Her land was used to conduct drills.

Geographic entities mentioned:
surface_form: the Galtees
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.366
lon: -8.179
state of Washington. It is the main headwater tributary of the Cowlitz River, which begins at the confluence of the Ohanapecosh River and the Clear Fork Cowlitz River. The Ohanapecosh originates near Ohanapecosh Glacier on the southeast side of Mount Rainier. Most of the river is within Mount Rainier National Park. Its final reach is in Gifford Pinchot National Forest.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Geology. Like the Fichtel Mountains, the Steinwald consists mainly of granite. In the south and east it is surrounded by a basalt landscape of &quot;Kuppen&quot; - gentle, rounded summits - (Kemnather Land, Nördlicher Steinwald), whose most striking elevations are the Parkstein near Weiden, the Rauhe Kulm near Kemnath, the Schlossberg near Waldeck, the Armesberg, the Teichelberg and the Ruheberg.

Geographic entities mentioned:
surface_form: Armesberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.8903276088564
lon: 11.9458835098343
White Hill (Forest of Bowland). White Hill is a hill in the Forest of Bowland in north-western England. It lies between Slaidburn and High Bentham, on the boundary between the City of Lancaster and Ribble Valley districts. The summit houses a tower and a trig point. In medieval times, the hill marked one of the northernmost limits of the Lordship of Bowland.

Geographic entities mentioned:
surface_form: white hill (forest of bowland)
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.0233
lon: -2.50062
White Hill (Forest of Bowland). White Hill is a hill in the Forest of Bowland in north-western England. It lies between Slaidburn and High Bentham, on the boundary between the City of Lancaster and Ribble Valley districts. The summit houses a tower and a trig point. In medieval times, the hill marked one of the northernmost limits of the Lordship of Bowland.

Geographic entities mentioned:
surface_form: white hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.0233
lon: -2.50062
Southwest Elgin Forest Complex. The Southwest Elgin Forest Complex comprises a 20-kilometer subzone of discontinuous woodlots in southern Ontario within 5 kilometres of the Lake Erie shoreline from John E. Pearce Provincial Park at the eastern end to the Elgin-Kent county border at the western end.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
This required new or expanded towns, commuting, or both. Llanberis grew considerably through the first part of the 19th century, but not sufficiently to keep pace with the opportunities the quarries offered. The first &quot;mass transport&quot; commuting to and from Dinorwic's quarries was by boat across Llyn Peris and, especially, Llyn Padarn, with an estimated 26 boats involved.

Geographic entities mentioned:
surface_form: Llyn Padarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 53.12888889
lon: -4.13305556
As a result, the territories remained thinly populated, with only around 150,000 First Nations, Inuit and occasional small groups of Europeans, and more substantial communities of around 12,000 Métis settled in the Red River valley of Manitoba and a further 8,500 European settlers in the colony of British Columbia.

Geographic entities mentioned:
surface_form: Red River valley
instance_of: Valley
countries: Canada
United States
coordinates: lat: 49
lon: -97.5
The police opened temporary detachments around York Factory in 1912, and then at Port Nelson in 1913, where the police established their divisional headquarters. Patrols pushed up into Baker Lake and along the Coppermine River until, by the end of the decade, the police presence in Hudson Bay had been reduced to a bare minimum, with the force focusing on reaching out into ever more remote areas.

Geographic entities mentioned:
surface_form: Coppermine River
instance_of: Watercourse
countries: Canada
coordinates: lat: 67.816666666667
lon: -115.06666666667
The mounted police also purchased various boats for work along Canada's coasts and rivers. The &quot;Keewatin&quot;, a sailing vessel, was bought in 1890 for use on Lake Winnipeg, but it capsized later the same year. In 1902, the steamboat &quot;Vidette&quot; was acquired to transport the police along the Yukon River, supported by three launches.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
South Pennines. The South Pennines is a region of moorland and hill country in northern England lying towards the southern end of the Pennines. In the west it includes the Rossendale Valley and the West Pennine Moors. It is bounded by the Greater Manchester conurbation in the west and the Bowland Fells and Yorkshire Dales to the north.

Geographic entities mentioned:
surface_form: Rossendale Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.7031
lon: -2.2893
The district covered almost the whole Congo Basin south of the Stanley Falls. The boundary with Aruwimi District was defined by the Lomami River. From north to south, the eastern border included Lake Albert Nyassa, Lake Albert-Edward, Lake Tanganyika, Lake Moero and Lake Bangwelo. Later, Lake Bangweulu was determined to be within Northern Rhodesia.

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
From north to south, the eastern border included Lake Albert Nyassa, Lake Albert-Edward, Lake Tanganyika, Lake Moero and Lake Bangwelo. Later, Lake Bangweulu was determined to be within Northern Rhodesia. Lake Kivu was shown as contained within the district, although later it was found to be on the border between Rwanda and the Belgian Congo.

Geographic entities mentioned:
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
Tectonic depositional setting. The ancient marine basin that the Great Valley Sequence was deposited in very closely approximates the combined extent of the modern Sacramento Valley and San Joaquin Valley as delineated by the California Coast Ranges on the west side and the Sierra Nevada on the east.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Parts of the sequence are well exposed at several places along a line of outcrops that extends for about along the west side of the Sacramento and San Joaquin valleys (both of which make up the Great Valley of California). These same rocks are also found in several deep wells in oil and gas fields located in the center of the valley.

Geographic entities mentioned:
surface_form: Sacramento
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
surface_form: San Joaquin valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Yet refinements in dating the ages of the different units has led to the realization that an interval of rock in one area may be exactly the same age as the rocks in another area, yet be referred to by a completely different formation name. Some of the best outcrops for these rocks are on the west side of the southern Sacramento Valley at Putah Creek and Cache Creek canyons.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
The same is not true for the San Joaquin Valley to the south, where another area of well-known outcrops is found in the hills to the west of Coalinga. This area uses a completely different set of formation names for exactly the same group of rocks as are found to the north.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
The highway runs from Highway 984 near Somme and McNab Creek to Highway 982 near the Pepaw Lake Recreation Site. The highway's route from west to east follows along the Piwei River, Pepaw River, Eldredge Lake, McBride Lake, through the McBride Lake Recreation Site, and on to Highway 982 near Pepaw Lake. Highway 983 connects with Highway 9 near where the Etomami River meets the Piwei River.

Geographic entities mentioned:
surface_form: Piwei River
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.4333
lon: -102.68424
surface_form: Pepaw River
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.66672
lon: -102.36764
surface_form: McBride Lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.4501
lon: -102.4171
The highway's route from west to east follows along the Piwei River, Pepaw River, Eldredge Lake, McBride Lake, through the McBride Lake Recreation Site, and on to Highway 982 near Pepaw Lake. Highway 983 connects with Highway 9 near where the Etomami River meets the Piwei River. It is about long.

Geographic entities mentioned:
surface_form: Etomami River
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.32811
lon: -96.88732
Thomson's map of 1832 shows a Lochside and an East Lochgate with the outflow running into the Avon water. Loch Gate is recorded on the 1897 OS maps as a remnant, close to Lochgate Farm with only a small area (0.290 Acre) of open water In the late 1880s it is recorded that the deep waters of Gate Loch (sic) had been drained. The Battle of Loudoun Hill. The Battle of Loudoun Hill took place in 1307.

Geographic entities mentioned:
surface_form: loudoun hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.614719444444
lon: -4.2116805555556
Loch Gate is recorded on the 1897 OS maps as a remnant, close to Lochgate Farm with only a small area (0.290 Acre) of open water In the late 1880s it is recorded that the deep waters of Gate Loch (sic) had been drained. The Battle of Loudoun Hill. The Battle of Loudoun Hill took place in 1307. Robert the Bruce encounter English forces, under Aymer de Valence, 2nd Earl of Pembroke.

Geographic entities mentioned:
surface_form: loudoun hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.614719444444
lon: -4.2116805555556
Loch Gate. Loch Gate (NS 62389 37170), previously known as Loch Gait, was a freshwater loch, partly in the East Ayrshire Council Area and partly in South Lanarkshire, now mainly drained, near Darvel, lying in a glacial kettle hole, Parish of Galston, Scotland. The loch.

Geographic entities mentioned:
surface_form: loch gate
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.6083
lon: -4.18583
The loch. Loch Gate, at the eastern extremity of Galston Pavi’s, was once a sheet of deep water, but now is a small area of open water in a marsh. By 1846 the loch is recorded as being little more than an area of marshy ground. Cartographic evidence. Armstrong's map of 1775 clearly shows the loch close to the Strathaven to Galston toll road.

Geographic entities mentioned:
surface_form: loch gate
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.6083
lon: -4.18583
Thomson's map of 1832 shows a Lochside and an East Lochgate with the outflow running into the Avon water. Loch Gate is recorded on the 1897 OS maps as a remnant, close to Lochgate Farm with only a small area (0.290 Acre) of open water In the late 1880s it is recorded that the deep waters of Gate Loch (sic) had been drained. The Battle of Loudoun Hill. The Battle of Loudoun Hill took place in 1307.

Geographic entities mentioned:
surface_form: loch gate
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.6083
lon: -4.18583
After several years he grew disenchanted with the life of the big city and its focus on material possessions. Having spent much of his youth being involved with the Boy Scouts and his love of the outdoors, he read the story &quot;The Shepherd of the Hills&quot; by Harold Bell Wright and an article by Horace Kephart about camping in the Ozarks.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
July and August gave Harrison several impediments to defending Indiana. First, Chief Little Turtle died on July 14, which meant that the United States lost one of the Indian leaders they could rely on to maintain peace. This was followed three days later by British forces gaining control of Lake Michigan by the capture of the American fort at Mackinac Island.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Kalmyk Steppe. Kalmuk Steppe, or Kalmyk Steppe is a steppe with a land area of approximately 100,000 km², bordering the northwest Caspian Sea, bounded by the Volga on the northeast, the Manych on the southwest, and the territory of the Don Cossacks on the northwest. The historic home to the Kalmuck or Kalmyks, it is in the Federal subject of Astrakhan Oblast in Russia.

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
The western Kalmuk Steppe occupied by the Yergeni hills, is deeply trenched by ravines and rises 300 and occasionally 630 ft. above the sea. It is built up of Tertiary deposits, belonging to the Sarmatian division of the Miocene period and covered with bess and black earth, and its escarpments represent the old shore-line of the Caspian. No Caspian deposits are found on or within the Yergeni.

Geographic entities mentioned:
surface_form: Caspian
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
In the words of Niels Nielsen,
Even as a child he felt attracted to the interior, desolate highlands, and it was one of his key experiences that he as a boy was allowed to embark on the adventure to take part in the autumn sheep collections whereby people searched the highlands on horseback up to glaciers.

Geographic entities mentioned:
surface_form: highlands
instance_of: Plateau
countries: Iceland
coordinates: lat: 64.84
lon: -18.11
Dovre Township is a township in Kandiyohi County, Minnesota, United States. The population was 1,968 at the 2000 census. Dovre Township was organized in 1869, and derives its name from the Dovrefjell mountain range in Norway. Geography. According to the United States Census Bureau, the township has a total area of, of which is land and (21.10%) is water. Demographics.

Geographic entities mentioned:
surface_form: Dovrefjell
instance_of: Mountain
countries: Norway
coordinates: lat: 62.1
lon: 9.41666667
It fought in western Virginia, East Tennessee, with the Army of Northern Virginia and the Shenandoah Valley. The 1st Battalion, Virginia Mounted Rifles was organized in December, 1861 and was absorbed into Virginia's 34th Cavalry Battalion in December 1862. Lieutenant Colonel Vincent &quot;Clawhammer&quot; Witcher and Majors John A. McFarlane and [John] William Straton were in command.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
During April, 1864, after new recruits in the new state of West Virginia added Company K, it contained 222 effectives. It saw action at the Battle of Piedmont Augusta County, Virginia in which CSA Gen. Jones died, and fought with CSA General Early in the Shenandoah Valley. The 34th disbanded at Lynchburg in April, 1865.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Interior Plateau. The Interior Plateau comprises a large region of the Interior of British Columbia, and lies between the Cariboo and Monashee Mountains on the east, and the Hazelton Mountains, Coast Mountains and Cascade Range on the west. The continuation of the plateau into the United States is known there as the Columbia Plateau.

Geographic entities mentioned:
surface_form: Columbia Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 45.999444444444
lon: -119.00138888889
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Subdivisions. The Cariboo and Chilcotin Plateaus are separated by the Fraser River. The Nechako Plateau flanks the Fraser on both sides; its southern boundary is defined by the West Road River (aka the Blackwater River) and the Quesnel River, and its northern boundary consists of the Omineca Mountains and the Cassiar Mountains, which are two major subdivisions of the Interior Mountains.

Geographic entities mentioned:
surface_form: Cariboo
instance_of: Plateau
countries: Canada
coordinates: lat: 50.81652
lon: -118.81904
surface_form: Chilcotin Plateau
instance_of: Mountain
countries: Canada
coordinates: lat: 52.166666666666664
lon: -123.41666666666667
The Cariboo and Chilcotin Plateaus are separated by the Fraser River. The Nechako Plateau flanks the Fraser on both sides; its southern boundary is defined by the West Road River (aka the Blackwater River) and the Quesnel River, and its northern boundary consists of the Omineca Mountains and the Cassiar Mountains, which are two major subdivisions of the Interior Mountains. Mountain ranges.

Geographic entities mentioned:
surface_form: Nechako Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 54.49979
lon: -126.00334
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The presence of sea shells gives an indication that trading took place. A small, oval-shaped dwelling was also found at the Paulina Lake site in Oregon, dating to 7100 BC. The Cascade phase took place from 7100 to 4300 BC, and was marked by a slight change in toolkit technology from the Windust peoples. A residential structure was found for this group, dating between 5500 and 4300 BC.

Geographic entities mentioned:
surface_form: Paulina Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7198736
lon: -121.2583009
Interior Plateau. The Interior Plateau comprises a large region of the Interior of British Columbia, and lies between the Cariboo and Monashee Mountains on the east, and the Hazelton Mountains, Coast Mountains and Cascade Range on the west. The continuation of the plateau into the United States is known there as the Columbia Plateau.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: interior plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 52
lon: -123
The Interior Plateau is &quot;not&quot; part of the Interior Mountains, a huge area that constitutes most of the northern two thirds of the Canadian province of British Columbia between the Coast Mountains, Rocky Mountains and the various small ranges on the inland lea of the Coast Mountains between the Bulkley Ranges and the Bella Coola River. Subdivisions.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: interior plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 52
lon: -123
The location of the Interior Plateau in North America is between the Rocky Mountains and the Pacific Coast Ranges. It is cut by the basins and tributaries of two rivers: the Columbia and the Fraser. The northern region is largely wooded, except in lowland and more southerly areas which resemble the sagebrush grasslands which typify the southern part of the plateau in the Columbia drainage.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
It is cut by the basins and tributaries of two rivers: the Columbia and the Fraser. The northern region is largely wooded, except in lowland and more southerly areas which resemble the sagebrush grasslands which typify the southern part of the plateau in the Columbia drainage. The first documented human presence was in 8500 BC.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Also, the Cariboo Mountains are sometimes included as part of the Interior Plateau. Three areas liminal to the plateau, i.e. sometimes considered part of it rather than the adjoining mountain ranges, are the Shuswap Highland, Okanagan Highland and Quesnel Highland. History. The location of the Interior Plateau in North America is between the Rocky Mountains and the Pacific Coast Ranges.

Geographic entities mentioned:
surface_form: okanagan
instance_of: Lake
countries: Canada
coordinates: lat: 49.920833333333
lon: -119.5
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Interior Plateau. The Interior Plateau comprises a large region of the Interior of British Columbia, and lies between the Cariboo and Monashee Mountains on the east, and the Hazelton Mountains, Coast Mountains and Cascade Range on the west. The continuation of the plateau into the United States is known there as the Columbia Plateau.

Geographic entities mentioned:
surface_form: interior plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 52
lon: -123
The continuation of the plateau into the United States is known there as the Columbia Plateau. Physiographically, the Interior Plateau is a section of the larger Northern Plateaus province, which in turn is part of the Intermontane Plateaus physiographic division.

Geographic entities mentioned:
surface_form: interior plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 52
lon: -123
Mountain ranges. Some classifications systems assign the Pattullo Rangez to the Hazelton Mountains, which are part of the larger Skeena Mountains complex, but then theoretically so zalso is the Quanchus Range. Also, the Cariboo Mountains are sometimes included as part of the Interior Plateau. Three areas liminal to the plateau, i.e.

Geographic entities mentioned:
surface_form: interior plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 52
lon: -123
Three areas liminal to the plateau, i.e. sometimes considered part of it rather than the adjoining mountain ranges, are the Shuswap Highland, Okanagan Highland and Quesnel Highland. History. The location of the Interior Plateau in North America is between the Rocky Mountains and the Pacific Coast Ranges. It is cut by the basins and tributaries of two rivers: the Columbia and the Fraser.

Geographic entities mentioned:
surface_form: interior plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 52
lon: -123
8 September 1999 — Las Rozas to Salamanca,
Stage 5. 9 September 1999 — Béjar to Ciudad Rodrigo,
Stage 6. 10 September 1999 — Salamanca to Salamanca, (ITT)
Stage 7. 11 September 1999 — Salamanca to León,
Stage 8. 12 September 1999 — León to Alto de l'Angliru,
Stage 9. 13 September 1999 — Gijón to Los Corrales de Buelna,
Stage 10. 15 September 1999 — Zaragoza to Zaragoza,

Geographic entities mentioned:
surface_form: Alto de l'Angliru
instance_of: Mountain
countries: Spain
coordinates: lat: 43.221389
lon: -5.942222
Seabird Island First Nation. The Seabird Island First Nation, or Seabird Island Band (), is a band government of the people located on Sea Bird Island in the Upper Fraser Valley region, 3 km east of Agassiz, British Columbia, Canada. They are a member government of the.

Geographic entities mentioned:
surface_form: Upper Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
Bras Saint-Nicolas. The Bras Saint-Nicolas (&quot;in English: Saint-Nicolas Arm&quot;) is a tributary of the south-eastern bank of the rivière du Sud (Montmagny), which flows north-east to the south bank of the St. Lawrence River.

Geographic entities mentioned:
surface_form: bras saint-nicolas
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.979166666667
lon: -70.553333333333
Bras Saint-Nicolas. The Bras Saint-Nicolas (&quot;in English: Saint-Nicolas Arm&quot;) is a tributary of the south-eastern bank of the rivière du Sud (Montmagny), which flows north-east to the south bank of the St. Lawrence River.

Geographic entities mentioned:
surface_form: bras saint-nicolas
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.979166666667
lon: -70.553333333333
surface_form: bras saint-nicolas
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.979166666667
lon: -70.553333333333
This confluence is located upstream from the route 132 bridge, downstream from the route 283 bridge, in the heart of the village of Montmagny. Toponymy. In a lower segment, parallel to the St. Lawrence River, the Bras Saint-Nicolas meanders at an altitude of about fifteen meters, crossing a stronghold granted in 1672 to Nicolas Gamache by the intendant Jean Talon.

Geographic entities mentioned:
surface_form: bras saint-nicolas
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.979166666667
lon: -70.553333333333
Toponymy. In a lower segment, parallel to the St. Lawrence River, the Bras Saint-Nicolas meanders at an altitude of about fifteen meters, crossing a stronghold granted in 1672 to Nicolas Gamache by the intendant Jean Talon. A first hypothesis associates the origin of the toponym &quot;Bras Saint-Nicolas&quot; with this pioneer.

Geographic entities mentioned:
surface_form: bras saint-nicolas
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.979166666667
lon: -70.553333333333
Lawrence River. The Bras Saint-Nicolas flows in the municipalities of Sainte-Apolline-de-Patton, Cap-Saint-Ignace, Saint-Cyrille-de-Lessard, Saint-Eugène, Notre-Dame-de-Bonsecours and Montmagny, in the Montmagny Regional County Municipality, in the administrative region of Chaudière-Appalaches, in Quebec, in Canada. Geography.

Geographic entities mentioned:
surface_form: chaudière
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.742777777777775
lon: -71.2786111111111