Sarmila/GeoWiki-Features huggingface dataset:
The other subspecies, &quot;Argyroxiphium sandwicense&quot; subsp. &quot;sandwicense&quot; (Mauna Kea silversword), is found on Mauna Kea. They differ primarily in the inflorescence shapebroader in the Haleakalā plants (less than 4 times as long as wide) and narrower on Mauna Kea (4.3–8.6 times as long as wide).

Geographic entities mentioned:
surface_form: Mauna Kea
instance_of: Mountain
countries: United States
coordinates: lat: 19.820555555555554
lon: -155.46805555555557
The &quot;SS Indiana&quot; was a freighter built in 1848. It was built with an 18-foot steam engine with an Erickson Screw Propeller. It served Lake Superior as a passenger ship and later became a transporter for iron ore after the opening of the Soo Locks. During a storm, the boat started leaking near the propeller shaft, causing the ship to founder at Crisp Point Light on June 6, 1856.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
During the 1990s, the commune became ill-famed as a hub for contraband in petroleum products. Location and demographics. The Coronini commune is located on the foothills of the Southern Carpathians, where these meet the Danube, and in proximity to the Clisura Dunării and Iron Gates areas. Facing Serbia on the right bank of the Danube, it is also close to a canyon formed by the Alibeg River.

Geographic entities mentioned:
surface_form: Iron Gates
instance_of: Valley
countries: Serbia
Romania
coordinates: lat: 44.671111111111
lon: 22.529722222222
Previously collected specimens of the species had been incorrectly identified as &quot;Cylindrophis ruffus&quot;. The specific name &quot;monticola&quot; is Latin for &quot;inhabitant of mountains&quot;, referring to the species's type locality, Mount Kinabalu. &quot;A.

Geographic entities mentioned:
surface_form: Mount Kinabalu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 6.075
lon: 116.5586111111111
Moose River Mountain. Moose River Mountain is a mountain in the Adirondack Mountains of New York. It is located west of Old Forge in the town of Webb in Herkimer County. In 1919, a steel fire lookout tower was built on the mountain. The tower ceased fire lookout operations at the end of the 1970, and was later removed in 1977. History.

Geographic entities mentioned:
surface_form: moose river mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7084
lon: -75.04601
Moose River Mountain. Moose River Mountain is a mountain in the Adirondack Mountains of New York. It is located west of Old Forge in the town of Webb in Herkimer County. In 1919, a steel fire lookout tower was built on the mountain. The tower ceased fire lookout operations at the end of the 1970, and was later removed in 1977. History.

Geographic entities mentioned:
surface_form: moose river mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7084
lon: -75.04601
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
Mount Pan. Mount Pan () is a mountain in Jizhou District, Tianjin, People's Republic of China. It is located from Tianjin and from Beijing. It has an area of 20 square kilometers and its highest peak is 858 meters above the sea level.

Geographic entities mentioned:
surface_form: mount pan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 40.083333333333
lon: 117.26666666667
To the southeast is the Boskovice Furrow in the mid-Moravian part of the Brno Highlands as well and in the east the Svitavy Uplands. The Svratka river stream naturally established Bohemian-Moravian border, the other part of Elbe–Danube main European watershed
The mountain range is 63% forested, though mainly by plantations - spruces, maples, beeches, elmeses. The forests are in well condition.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Cerro Bonete. Cerro Bonete is a mountain in the north of the province of La Rioja, Argentina, near the provincial border with Catamarca. Its summit is 6,759 m above mean sea level, making it the fifth-highest separate mountain in the Americas (after Aconcagua, Ojos del Salado, Monte Pissis, and Huascaran). SRTM data disproves the frequently-made claim that its summit is 6,872 m above sea level.

Geographic entities mentioned:
surface_form: Aconcagua
instance_of: Mountain
countries: Argentina
coordinates: lat: -32.653055555555554
lon: -70.01166666666667
surface_form: Ojos del Salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: Monte Pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
Cerro Bonete. Cerro Bonete is a mountain in the north of the province of La Rioja, Argentina, near the provincial border with Catamarca. Its summit is 6,759 m above mean sea level, making it the fifth-highest separate mountain in the Americas (after Aconcagua, Ojos del Salado, Monte Pissis, and Huascaran). SRTM data disproves the frequently-made claim that its summit is 6,872 m above sea level.

Geographic entities mentioned:
surface_form: bonete
instance_of: Mountain
countries: Argentina
coordinates: lat: -28.01861111111111
lon: -68.75611111111111
surface_form: cerro bonete
instance_of: Mountain
countries: Argentina
coordinates: lat: -28.01861111111111
lon: -68.75611111111111
Its summit is 6,759 m above mean sea level, making it the fifth-highest separate mountain in the Americas (after Aconcagua, Ojos del Salado, Monte Pissis, and Huascaran). SRTM data disproves the frequently-made claim that its summit is 6,872 m above sea level. Within the last 3.5 million years, volcanic activity at Cerro Bonete has formed lava domes of dacite and rhyodacite.

Geographic entities mentioned:
surface_form: bonete
instance_of: Mountain
countries: Argentina
coordinates: lat: -28.01861111111111
lon: -68.75611111111111
surface_form: cerro bonete
instance_of: Mountain
countries: Argentina
coordinates: lat: -28.01861111111111
lon: -68.75611111111111
Salash Nunatak. Salash Nunatak (, ‘Nunatak Salash’ \'nu-na-tak 'sa-lash\) is a rocky peak of elevation 220 m in Breznik Heights projecting from the upper Wulfila Glacier on Greenwich Island in the South Shetland Islands, Antarctica. Situated 400 m southwest of the summit of Oborishte Ridge and 1.35 km west of Nevlya Peak. The peak is named after the settlement of Salash in northwestern Bulgaria.

Geographic entities mentioned:
surface_form: Nevlya Peak
instance_of: Mountain
coordinates: lat: -62.5383
lon: -59.7297
Salash Nunatak. Salash Nunatak (, ‘Nunatak Salash’ \'nu-na-tak 'sa-lash\) is a rocky peak of elevation 220 m in Breznik Heights projecting from the upper Wulfila Glacier on Greenwich Island in the South Shetland Islands, Antarctica. Situated 400 m southwest of the summit of Oborishte Ridge and 1.35 km west of Nevlya Peak. The peak is named after the settlement of Salash in northwestern Bulgaria.

Geographic entities mentioned:
surface_form: salash nunatak
instance_of: Mountain
coordinates: lat: -62.5373
lon: -59.7558
Salash Nunatak. Salash Nunatak (, ‘Nunatak Salash’ \'nu-na-tak 'sa-lash\) is a rocky peak of elevation 220 m in Breznik Heights projecting from the upper Wulfila Glacier on Greenwich Island in the South Shetland Islands, Antarctica. Situated 400 m southwest of the summit of Oborishte Ridge and 1.35 km west of Nevlya Peak. The peak is named after the settlement of Salash in northwestern Bulgaria.

Geographic entities mentioned:
surface_form: salash nunatak
instance_of: Mountain
coordinates: lat: -62.5373
lon: -59.7558
surface_form: nunatak salash
instance_of: Mountain
coordinates: lat: -62.5373
lon: -59.7558
Situated 400 m southwest of the summit of Oborishte Ridge and 1.35 km west of Nevlya Peak. The peak is named after the settlement of Salash in northwestern Bulgaria. Location. Salash Nunatak is located at. Bulgarian topographic survey 05 and mapping in 2009. Map. L.L. Ivanov. Scale 1:120000 topographic map. Troyan: Manfred Wörner Foundation, 2009.

Geographic entities mentioned:
surface_form: salash nunatak
instance_of: Mountain
coordinates: lat: -62.5373
lon: -59.7558
At an elevation of, it has a surface area of. Its maximum depth is. Since 2007 the lake has been part of the Jungfrau-Aletsch-Bietschhorn UNESCO World Heritage Site. As of summer 2021, a circumnavigation of Lake Oeschinen is not possible. The reason for this is the danger of an imminent rockfall on the south shore, which is why paths are closed there. Emergence and hydrology.

Geographic entities mentioned:
surface_form: Jungfrau
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.536944444444
lon: 7.9625
surface_form: Bietschhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.39125
lon: 7.850075
Oeschinen Lake. Oeschinen Lake () is a lake in the Bernese Oberland, Switzerland, east of Kandersteg in the Oeschinen Valley. At an elevation of, it has a surface area of. Its maximum depth is. Since 2007 the lake has been part of the Jungfrau-Aletsch-Bietschhorn UNESCO World Heritage Site. As of summer 2021, a circumnavigation of Lake Oeschinen is not possible.

Geographic entities mentioned:
surface_form: oeschinen
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.498333333333
lon: 7.7269444444444
Oeschinen Lake. Oeschinen Lake () is a lake in the Bernese Oberland, Switzerland, east of Kandersteg in the Oeschinen Valley. At an elevation of, it has a surface area of. Its maximum depth is. Since 2007 the lake has been part of the Jungfrau-Aletsch-Bietschhorn UNESCO World Heritage Site. As of summer 2021, a circumnavigation of Lake Oeschinen is not possible.

Geographic entities mentioned:
surface_form: oeschinen
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.498333333333
lon: 7.7269444444444
surface_form: oeschinen
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.498333333333
lon: 7.7269444444444
At an elevation of, it has a surface area of. Its maximum depth is. Since 2007 the lake has been part of the Jungfrau-Aletsch-Bietschhorn UNESCO World Heritage Site. As of summer 2021, a circumnavigation of Lake Oeschinen is not possible. The reason for this is the danger of an imminent rockfall on the south shore, which is why paths are closed there. Emergence and hydrology.

Geographic entities mentioned:
surface_form: oeschinen
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.498333333333
lon: 7.7269444444444
surface_form: lake oeschinen
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.498333333333
lon: 7.7269444444444
From time to time ice skating is possible on the ice. Fauna. Fish in the lake include Arctic char (), lake trout (), and rainbow trout (). From January to March, ice fishing is popular. Transport. A gondola lift from Kandersteg leads to Oeschinen. The top station is 25 minutes away by foot from the lake. A bus links the valley station of the gondola lift with Kandersteg railway station.

Geographic entities mentioned:
surface_form: oeschinen
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.498333333333
lon: 7.7269444444444
This prairie southeast of Snoqualmie Falls was the ancestral home, hunting and forage grounds for the Snoqualmie people and was located in the upper Snoqualmie Valley near the Snoqualmie River fork confluence, Mount Si, and the western foothills of the Cascade Range. One of the first American explorers to the upper Snoqualmie Valley was Samuel Hancock, who arrived in 1851.

Geographic entities mentioned:
surface_form: Snoqualmie Valley
instance_of: Valley
countries: United States
coordinates: lat: 47.605555555556
lon: -121.92138888889
surface_form: Mount Si
instance_of: Mountain
countries: United States
coordinates: lat: 47.5076
lon: -121.74
The city is bordered to the northwest by the city of Snoqualmie. Both communities lie near the center of the Mountains to Sound Greenway. North Bend is located near the geographic center of King County. Mount Si, the most prominent geological feature nearby, looms over the town. To the south is Rattlesnake Ridge. Mount Si stands at and towers above the town, itself at around.

Geographic entities mentioned:
surface_form: Mount Si
instance_of: Mountain
countries: United States
coordinates: lat: 47.5076
lon: -121.74
Both communities lie near the center of the Mountains to Sound Greenway. North Bend is located near the geographic center of King County. Mount Si, the most prominent geological feature nearby, looms over the town. To the south is Rattlesnake Ridge. Mount Si stands at and towers above the town, itself at around. A trail zigzags up to the summit with a vertical climb of.

Geographic entities mentioned:
surface_form: Rattlesnake Ridge
instance_of: Mountain
countries: United States
coordinates: lat: 47.458333333333
lon: -121.80611111111
North Bend has a city trail system that also connects with the regional network. The Snoqualmie Valley Regional Trail stretches from Duvall through Carnation, Fall City, Snoqualmie, and North Bend to Rattlesnake Lake. This trail connects to the Palouse to Cascades State Park Trail (which goes clear across Washington to the Idaho border) and to the city of Snoqualmie's extensive trail network.

Geographic entities mentioned:
surface_form: Rattlesnake Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.4303
lon: -121.773
Rock Lake (Lyon County, Minnesota). Rock Lake is a lake in Lyon County, in the U.S. state of Minnesota. Rock Lake was named for the large boulders found in and around the lake.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.083333333333
lon: -88.933333333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 46.427189
lon: -94.473618
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.328055555556
lon: -74.590833333333
surface_form: rock lake (lyon county, minnesota)
instance_of: Lake
countries: United States
coordinates: lat: 44.276111111111
lon: -95.935555555556
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 45.170555555556
lon: -94.0125
Rock Lake (Lyon County, Minnesota). Rock Lake is a lake in Lyon County, in the U.S. state of Minnesota. Rock Lake was named for the large boulders found in and around the lake.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.083333333333
lon: -88.933333333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 46.427189
lon: -94.473618
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.328055555556
lon: -74.590833333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 44.276111111111
lon: -95.935555555556
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 45.170555555556
lon: -94.0125
Prior to the completion of reservoirs and irrigation works in the mid-20th century, the Tarim's waters eventually reached Lop Nur (now a salt-encrusted lake bed). The
river's waters now drain intermittently into Taitema Lake, which is located about southwest of Lop Nur. Flora and fauna. Vegetation in the Tarim Basin is mainly located along the river and its branches.

Geographic entities mentioned:
surface_form: Taitema Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 39.4763
lon: 88.2573
Kilakarai lies on National Highway 49 (NH 49), which connects Madurai to Rameswaram. The nearest railway station is in Ramanathapuram, situated about 27 km from Erwadi, providing rail connectivity to major cities across Tamil Nadu. Erwadi is also connected to the coastal ports along the Bay of Bengal and serves as a junction point for fishing steamers.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Like Gautama, Tönpa Shenrab was of royal birth. Tonpa Shenrab renounced his royal inheritance at the age of thirty-one to travel the path to enlightenment. Tonpa Shenrab embraced the life of a renunciate and commenced austerities, spreading the doctrine of Bon; at length, he arrived in the land of Zhangzhung near what is widely held to be Mount Kailash.

Geographic entities mentioned:
surface_form: Mount Kailash
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
Akaagerger made provision of health care his priority. In December 2008, he stated that his free medical scheme in the state, which was being executed in partnership with the Grassroots Doctors Society, had spent ₦50 million and had benefited 23,000 people. In October 2009, he raised the alarm over the Lake Nyos natural dam, located in the Cameroons, which empties into the Benue River.

Geographic entities mentioned:
surface_form: Lake Nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
surface_form: Benue River
instance_of: Watercourse
countries: Cameroon
Nigeria
coordinates: lat: 7.783333
lon: 6.766667
Meråker Line. The Meråker Line ([ˈmeːroːkərˌbɑːnən]) is a railway line which runs through the district and valley of Stjørdalen in Trøndelag county, Norway. The line branches off from the Nordland Line at Hell Station and runs eastwards to the Norway–Sweden border, with Storlien Station acting as the border station. From there, the line continues as the Central Line.

Geographic entities mentioned:
surface_form: Stjørdalen
instance_of: Valley
countries: Norway
coordinates: lat: 63.4372
lon: 11.3444
The line largely follows the coast of the Trondheimsfjord from Trondheim until reaching Hell. From there the line heads inland through the valley of Stjørdalen, initially following the river of Stjørdalselva. The line runs predominantly due east from Trondheim, passing through the current municipalities of Trondheim, Malvik, Stjørdal and Meråker.

Geographic entities mentioned:
surface_form: Stjørdalen
instance_of: Valley
countries: Norway
coordinates: lat: 63.4372
lon: 11.3444
Background. Since the Middle Ages, both the Stjørdalen and Verdal valleys were important trade routes connecting Trøndelag and Jämtland. In particular, Levanger grew into an important trading town for Jämtland farmers, who would travel across the Verdal Mountains.

Geographic entities mentioned:
surface_form: Stjørdalen
instance_of: Valley
countries: Norway
coordinates: lat: 63.4372
lon: 11.3444
Mesquite, NV is downstream, and on Interstate 15 in Nevada, about. Mesquite is the approximate center of the valley. The South Virgin Mountains are southeast of the Virgin Valley and Mountains, and separate the northern Overton Arm of Lake Mead from the Colorado River arm. The area north of the South Virgin Mountains is the Mormon Mesa, the southwest border of Virgin Valley.

Geographic entities mentioned:
surface_form: Mormon Mesa
instance_of: Mountain
countries: United States
coordinates: lat: 36.51222222
lon: -114.37583333
surface_form: virgin valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -114.082
surface_form: mormon mesa
instance_of: Mountain
countries: United States
coordinates: lat: 36.51222222
lon: -114.37583333
surface_form: mormon mesa
instance_of: Mountain
countries: United States
coordinates: lat: 36.51222222
lon: -114.37583333
Mesquite, NV is downstream, and on Interstate 15 in Nevada, about. Mesquite is the approximate center of the valley. The South Virgin Mountains are southeast of the Virgin Valley and Mountains, and separate the northern Overton Arm of Lake Mead from the Colorado River arm. The area north of the South Virgin Mountains is the Mormon Mesa, the southwest border of Virgin Valley.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The Virgin Valley is vertically bisected, north-south by the Nevada-Arizona border. The downstream Nevada half of the valley has the very beginnings of Lake Mead, about upstream, where the Virgin River used to flow. Littlefield, AZ in the valley's northeast is located at. Mesquite, NV in the valley's center is located at.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The Virgin Valley is vertically bisected, north-south by the Nevada-Arizona border. The downstream Nevada half of the valley has the very beginnings of Lake Mead, about upstream, where the Virgin River used to flow. Littlefield, AZ in the valley's northeast is located at. Mesquite, NV in the valley's center is located at.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Virgin Valley. The Virgin Valley is a valley in northwest Arizona and southeast Nevada on the Virgin River. The Virgin River drains southwest Utah and southeast Nevada; parts of Arizona, especially the Arizona Strip region drain southwards into the Virgin River and Valley.

Geographic entities mentioned:
surface_form: virgin valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -114.082
The Virgin River drains southwest Utah and southeast Nevada; parts of Arizona, especially the Arizona Strip region drain southwards into the Virgin River and Valley. The Virgin Valley begins as the Virgin River exits the Virgin River Gorge between the Beaver Dam Mountains and Wilderness north, and the northeast of the Virgin Mountains on the south of the Gorge.

Geographic entities mentioned:
surface_form: virgin valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -114.082
The Virgin Valley begins as the Virgin River exits the Virgin River Gorge between the Beaver Dam Mountains and Wilderness north, and the northeast of the Virgin Mountains on the south of the Gorge. Lake Mead on the Virgin River extends slightly upstream into the Virgin Valley. History. There are two Virgin Valleys in Nevada.

Geographic entities mentioned:
surface_form: virgin valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -114.082
The two valleys are approximately 600 miles apart. The Opal mines are located in the Northern valley. The Virgin Valley has mines that are rich in opals. The opals were discovered in about 1913. The richest mines were owned by Flora Haines Loughead who had been a writer and a farmer but bought a string of claims after being sent to do a story for the San Francisco Chronicle.

Geographic entities mentioned:
surface_form: virgin valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -114.082
Mesquite, NV is downstream, and on Interstate 15 in Nevada, about. Mesquite is the approximate center of the valley. The South Virgin Mountains are southeast of the Virgin Valley and Mountains, and separate the northern Overton Arm of Lake Mead from the Colorado River arm. The area north of the South Virgin Mountains is the Mormon Mesa, the southwest border of Virgin Valley.

Geographic entities mentioned:
surface_form: virgin valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -114.082
The area north of the South Virgin Mountains is the Mormon Mesa, the southwest border of Virgin Valley. Mormon Mesa is an extension south from the Mormon Mountains which are separated east from the Meadow Valley Wash tributary to north Lake Mead. The Virgin Valley is vertically bisected, north-south by the Nevada-Arizona border.

Geographic entities mentioned:
surface_form: north lake
instance_of: Lake
countries: United States
coordinates: lat: 43.538333333333
lon: -74.928055555556
surface_form: north lake
instance_of: Lake
countries: United States
coordinates: lat: 32.9405819
lon: -96.9796312
Mountaineer Ian Clough was born in Baildon. After he was killed on an expedition to the Himalayan mountain Annapurna in 1970, Ian Clough Hall, a meeting-place and arts venue, was established in Baildon in his memory. The hall was demolished in late 2023; the site is destined to become a complex of private retirement flats but is currently not in use and is off limits to the public.

Geographic entities mentioned:
surface_form: Annapurna
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.5958
lon: 83.82
In the 1960s, Clough and close friend Chris Bonington were known to have practised their climbing techniques on Baildon Bank – a, ex-quarry rock-face that looks out towards Bradford. In 1962, Clough and Bonington were the first Britons to successfully scale the treacherous north face of the Eiger in the Swiss Alps.

Geographic entities mentioned:
surface_form: Eiger
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.577607529
lon: 8.005286822
Bow Fell, Cumberland. &quot;Bow Fell, Cumberland&quot; is an 1807 landscape painting by the British artist John Constable. It depicts a view of Bowfell in the county of Cumberland. Located in the Southern Fells, Constable made sketches on the spot when on a two month visit to the Lake District in 1806.

Geographic entities mentioned:
surface_form: Bowfell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.447369444444
lon: -3.1658194444444
Międzyodrze. Międzyodrze is an area in Poland located in the Lower Odra Valley between two branches of the Oder River: West Oder and East Oder, a segment from the village Widuchowa to Iński Nurt channel. Międzyodrze area also includes islands located between the Oder, its anabranch Cegielinka and Dąbie Lake, as well as part of Szczecin. Polders. The historical polders are in the Międzyodrze area.

Geographic entities mentioned:
surface_form: Dąbie Lake
instance_of: Lake
countries: Poland
coordinates: lat: 53.465833333333
lon: 14.653055555556
An early proposal suggested that the Whitecliffs Branch should be extended from Whitecliffs to the West Coast via the Wilberforce River and Browning's Pass. Another proposal called for a line departing the branch at Homebush and running via Lake Lyndon up to Cass, from where it would have followed roughly the same route as the present-day line via Arthur's Pass.

Geographic entities mentioned:
surface_form: Lake Lyndon
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.3
lon: 171.7
Doucier. Doucier () is a commune in the Jura department in Bourgogne-Franche-Comté in eastern France. World Heritage Site. The western shore of Lac de Chalain is home to one or more prehistoric pile-dwelling (or stilt house) settlements that are part of the Prehistoric Pile dwellings around the Alps UNESCO World Heritage Site.

Geographic entities mentioned:
surface_form: Lac de Chalain
instance_of: Lake
countries: France
coordinates: lat: 46.670727777778
lon: 5.7913055555556
Four natural water streams, including Bor stream, used to feed the river. It also receives water from the outlet of Gorewada Dam in North West Nagpur and Chambhar Nala in Central Nagpur
The river serves as a part of drainage for Nagpur and as a result its ecosystem is heavily polluted by urban waste from the city. The river is also threatened by encroachment at many places.

Geographic entities mentioned:
surface_form: Gorewada Dam
instance_of: Lake
countries: India
coordinates: lat: 21.1983
lon: 79.0376
There was also a pilgrimage site in the hills nearby, and the walls of the Wadi are covered with ancient pictographs. The city ceased in about 100AD with the control of the trade routes by the Nabataeans to the east and incursions by the Romans. The wadi has been tentatively identified with Wadi al-Qura of early Islamic times. Etymology. The name means “valley of villages”.

Geographic entities mentioned:
surface_form: Wadi al-Qura
instance_of: Valley
countries: Saudi Arabia
coordinates: lat: 26.5
lon: 37.5
Grand Bay (Georgia). Grand Bay is a swamp located in Lanier County and Lowndes County, Georgia. It consists of Grand Bay Wildlife Management Area, an educational wildlife area, and Banks Lake National Wildlife Refuge, a recreational and educational lake. Grand Bay Wetland Education Center.

Geographic entities mentioned:
surface_form: grand bay (georgia)
instance_of: Landform
countries: United States
coordinates: lat: 30.9347
lon: -83.1733
Grand Bay (Georgia). Grand Bay is a swamp located in Lanier County and Lowndes County, Georgia. It consists of Grand Bay Wildlife Management Area, an educational wildlife area, and Banks Lake National Wildlife Refuge, a recreational and educational lake. Grand Bay Wetland Education Center.

Geographic entities mentioned:
surface_form: grand bay
instance_of: Landform
countries: United States
coordinates: lat: 30.9347
lon: -83.1733
It consists of Grand Bay Wildlife Management Area, an educational wildlife area, and Banks Lake National Wildlife Refuge, a recreational and educational lake. Grand Bay Wetland Education Center. The Grand Bay Wetland Education Center is operated as a partnership by the Coastal Plains Regional Educational Service Agency and the Georgia Department of Natural Resources.

Geographic entities mentioned:
surface_form: grand bay
instance_of: Landform
countries: United States
coordinates: lat: 30.9347
lon: -83.1733
Grand Bay Wetland Education Center. The Grand Bay Wetland Education Center is operated as a partnership by the Coastal Plains Regional Educational Service Agency and the Georgia Department of Natural Resources. The Center features a boardwalk, education rooms and observation tower, and offers environmental education programs about the wetlands, field trips and accredited teacher training.

Geographic entities mentioned:
surface_form: grand bay
instance_of: Landform
countries: United States
coordinates: lat: 30.9347
lon: -83.1733
Johns arrived there from San Bois County in the Choctaw Nation, which was north and east of present-day McAlester, Oklahoma. Jack's Fork County was a geographic behemoth—it was bounded by the Kiamichi River on the east and Muddy Boggy River on the west, Beaver Creek (south of present-day Antlers, Oklahoma) on its south, and the mountains north of present-day Sardis Lake on its north.

Geographic entities mentioned:
surface_form: muddy
instance_of: Watercourse
countries: United States
coordinates: lat: 36.737500000000004
lon: -114.74416666666667
surface_form: sardis lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6583
lon: -95.3789
They are thought to have towered several thousand feet above sea level. Geologists believe that during an ancient glacial era ocean currents carried icebergs or glaciers containing these boulders northeast from these mountain ranges, dropping the massive boulders to sink to the ocean floor. Additional groupings of transported boulders in the Johns Valley region are known as the McKinley Rocks.

Geographic entities mentioned:
surface_form: mckinley
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
surface_form: johns valley
instance_of: Landform
countries: United States
coordinates: lat: 34.465
lon: -95.6136
Difficulties of another sort—with international repercussions—were experienced during World War II, when the Moyers and Johns Valley areas were the site of two lethal air crashes. British pilots operating from a Royal Air Force base in Texas crashed into White Rock Mountain and Big Mountain, killing four crewmen.

Geographic entities mentioned:
surface_form: white rock
instance_of: Mountain
countries: United States
coordinates: lat: 42.7539
lon: -73.28
surface_form: rock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.799444444444
lon: -120.97444444444
surface_form: big mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.4153
lon: -95.6144
surface_form: big mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.4153
lon: -95.6144
surface_form: big mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.9504
lon: -77.9367
surface_form: big mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.9504
lon: -77.9367
Johns Valley is an oval-shaped basin, long and wide. The valley is geographically isolated by formidable mountains. To its east are the lofty Pine Creek (1,460 ft.), Wildhorse (1,260 ft.) and Bull Creek (1,060 ft.) mountains. To its west is Buck Creek Mountain (1,184 ft.). Its northern limit is generally defined as Big Caney Mountain (1,467 ft.), and its southern limit as Big Mountain (1,145 ft.).

Geographic entities mentioned:
surface_form: bull creek
instance_of: Watercourse
countries: United States
surface_form: bull
instance_of: Watercourse
countries: United States
coordinates: lat: 49.46663
lon: -115.45205
surface_form: pine creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.08666667
lon: -91.82555556
Johns Valley, Oklahoma. Johns Valley is a geographic feature and place name located in the Kiamichi Mountains in northwestern Pushmataha County, Oklahoma. The valley is formally classified by geologists as a &quot;basin&quot; due to its complete encirclement by mountains. Location. The valley is approximately 22 miles north of Antlers, Oklahoma.

Geographic entities mentioned:
surface_form: johns valley, oklahoma
instance_of: Landform
countries: United States
coordinates: lat: 34.465
lon: -95.6136
Johns Valley, Oklahoma. Johns Valley is a geographic feature and place name located in the Kiamichi Mountains in northwestern Pushmataha County, Oklahoma. The valley is formally classified by geologists as a &quot;basin&quot; due to its complete encirclement by mountains. Location. The valley is approximately 22 miles north of Antlers, Oklahoma.

Geographic entities mentioned:
surface_form: johns valley
instance_of: Landform
countries: United States
coordinates: lat: 34.465
lon: -95.6136
Its latitude is N34.46510 and longitude is W95.61359. History. The first settler in Johns Valley was American Civil War veteran Henry Amos Johns. Johns, a Choctaw Indian who had fought in a Choctaw Indian battalion in the Confederate States Army, moved to the valley after the war, establishing a church there in 1865.

Geographic entities mentioned:
surface_form: johns valley
instance_of: Landform
countries: United States
coordinates: lat: 34.465
lon: -95.6136
Johns named the valley Big Caney Valley, due to the thick stands of cane he found there. Later white settlers called it Johns Valley, in deference to Amos Johns. Johns and later Choctaw Indian settlers drove oxen teams to Fort Smith, Arkansas, to purchase groceries and other goods. The trip usually took one month. After the St.

Geographic entities mentioned:
surface_form: johns valley
instance_of: Landform
countries: United States
coordinates: lat: 34.465
lon: -95.6136
It was the only church in the valley. Johns built it out of logs, and split logs formed its pews. A school was also established for Johns Valley, and it met in the church. After statehood the valley was settled by white people, who built a new school of lumber. The school appears to have been intermittent, starting and stopping occasionally.

Geographic entities mentioned:
surface_form: johns valley
instance_of: Landform
countries: United States
coordinates: lat: 34.465
lon: -95.6136
Regardless of family affiliation, all residents of the valley worked together for mutual benefit when a large labor force was needed such as when baling hay or rounding up cattle. When the Basket Family sold their property and moved from the valley, most of the other families followed. Johns Valley has had no permanent residents since the mid-1950s.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Johns Valley has had no permanent residents since the mid-1950s. At the time of white settlement, Johns Valley was home to an array of wildlife, much of which disappeared after the whites’ arrival due to their propensity to hunt. Early-day Choctaw settlers coexisted—sometimes peaceably and sometimes not—with a fairly large bear population, and a great many panthers.

Geographic entities mentioned:
surface_form: johns valley
instance_of: Landform
countries: United States
coordinates: lat: 34.465
lon: -95.6136
You could see them at any time during the day.” By the time of her interview she believed the rattlesnakes to be far fewer in number than previously, and credited the valley's later white settlers with eradicating them. A United States Post Office was established in Johns Valley and operated from September 28, 1912 to May 15, 1915. It was called Johns, Oklahoma.

Geographic entities mentioned:
surface_form: johns valley
instance_of: Landform
countries: United States
coordinates: lat: 34.465
lon: -95.6136
It was called Johns, Oklahoma. Despite its formal designation by the post office—which failed to include &quot;Valley&quot; in the formal name—the area has always been known as Johns Valley. Johns Valley was and continues to be very isolated, with only one road of any note entering or leaving it.

Geographic entities mentioned:
surface_form: johns valley
instance_of: Landform
countries: United States
coordinates: lat: 34.465
lon: -95.6136
surface_form: johns valley
instance_of: Landform
countries: United States
coordinates: lat: 34.465
lon: -95.6136
Johns Valley was and continues to be very isolated, with only one road of any note entering or leaving it. This road is not much better today than it was in 1927, when a team of geologists entered the valley to study its massive boulders. “The road into Johns Valley is not a good automobile road. In fact, it is one of the worst automobile roads imaginable,” the chief geologist wrote.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
“The road into Johns Valley is not a good automobile road. In fact, it is one of the worst automobile roads imaginable,” the chief geologist wrote. Difficulties of another sort—with international repercussions—were experienced during World War II, when the Moyers and Johns Valley areas were the site of two lethal air crashes.

Geographic entities mentioned:
surface_form: johns valley
instance_of: Landform
countries: United States
coordinates: lat: 34.465
lon: -95.6136
British pilots operating from a Royal Air Force base in Texas crashed into White Rock Mountain and Big Mountain, killing four crewmen. Big Mountain is generally accepted as the southern geographical limit of Johns Valley. Two planes were destroyed. A third plane crash-landed successfully at Jumbo.

Geographic entities mentioned:
surface_form: johns valley
instance_of: Landform
countries: United States
coordinates: lat: 34.465
lon: -95.6136
On February 20, 2000, the AT6 Monument was dedicated in the fliers' honor at the crash site on Big Mountain. Over 1,000 people attended the ceremony, and the story was carried by the British Broadcasting Corporation and many newspapers around the world. More information on Johns Valley and the surrounding Kiamichi Mountains may be found in the Pushmataha County Historical Society. Geology.

Geographic entities mentioned:
surface_form: johns valley
instance_of: Landform
countries: United States
coordinates: lat: 34.465
lon: -95.6136
surface_form: johns valley
instance_of: Landform
countries: United States
coordinates: lat: 34.465
lon: -95.6136
To its east are the lofty Pine Creek (1,460 ft.), Wildhorse (1,260 ft.) and Bull Creek (1,060 ft.) mountains. To its west is Buck Creek Mountain (1,184 ft.). Its northern limit is generally defined as Big Caney Mountain (1,467 ft.), and its southern limit as Big Mountain (1,145 ft.). The distant geological past is immediately present in Johns Valley.

Geographic entities mentioned:
surface_form: johns valley
instance_of: Landform
countries: United States
coordinates: lat: 34.465
lon: -95.6136
The largest weigh over 50,000 tons. Although the boulders by themselves are of great interest, the story of how they came to rest there formed a mystery which geologists spent decades unraveling. During prehistoric times Johns Valley was on the floor of an ocean. The nearby—and no longer extant—Wichita-Criner Mountains, Red River Mountains and Amarillo Mountains (now buried) lay to the southwest.

Geographic entities mentioned:
surface_form: johns valley
instance_of: Landform
countries: United States
coordinates: lat: 34.465
lon: -95.6136
Johns Valley, Oklahoma. Johns Valley is a geographic feature and place name located in the Kiamichi Mountains in northwestern Pushmataha County, Oklahoma. The valley is formally classified by geologists as a &quot;basin&quot; due to its complete encirclement by mountains. Location. The valley is approximately 22 miles north of Antlers, Oklahoma.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
History. The first settler in Johns Valley was American Civil War veteran Henry Amos Johns. Johns, a Choctaw Indian who had fought in a Choctaw Indian battalion in the Confederate States Army, moved to the valley after the war, establishing a church there in 1865. At the time the valley was part of Jack's Fork County of the Choctaw Nation, in the Indian Territory.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Johns, a Choctaw Indian who had fought in a Choctaw Indian battalion in the Confederate States Army, moved to the valley after the war, establishing a church there in 1865. At the time the valley was part of Jack's Fork County of the Choctaw Nation, in the Indian Territory. Johns arrived there from San Bois County in the Choctaw Nation, which was north and east of present-day McAlester, Oklahoma.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Jack's Fork County was a geographic behemoth—it was bounded by the Kiamichi River on the east and Muddy Boggy River on the west, Beaver Creek (south of present-day Antlers, Oklahoma) on its south, and the mountains north of present-day Sardis Lake on its north. Johns named the valley Big Caney Valley, due to the thick stands of cane he found there.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
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countries: United States
coordinates: lat: 47.7174
lon: -117.047423
After the St. Louis and San Francisco Railroad opened through the Kiamichi River valley in 1887 they traded at what are now the communities of Tuskahoma, Oklahoma, and Kosoma, Oklahoma. The church founded by Johns was Presbyterian and came to be called Big Caney Presbyterian Church. It was the only church in the valley. Johns built it out of logs, and split logs formed its pews.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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countries: United States
coordinates: lat: 61.3833
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countries: United States
coordinates: lat: 47.7174
lon: -117.047423
It was the only church in the valley. Johns built it out of logs, and split logs formed its pews. A school was also established for Johns Valley, and it met in the church. After statehood the valley was settled by white people, who built a new school of lumber. The school appears to have been intermittent, starting and stopping occasionally.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The school appears to have been intermittent, starting and stopping occasionally. It reopened again for the last time during the 1930s or 1940s, but has been closed for decades. Logging and cattle ranching were the valley's first and only major industries. Timber companies logged the valley for its valuable hardwood and pine trees.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
It reopened again for the last time during the 1930s or 1940s, but has been closed for decades. Logging and cattle ranching were the valley's first and only major industries. Timber companies logged the valley for its valuable hardwood and pine trees. After logging ceased the valley became home to the immense Basket Ranch, operated by the Basket family.

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