Sarmila/GeoWiki-Features huggingface dataset:
Whinlatter is in the most northerly sector, rising between Whinlatter Pass and the Vale of Embleton. The hub of this group of fells is Lord's Seat, the highest point north of Whinlatter Pass. The main line of high ground runs east to west, taking in Barf, Lord's Seat, Broom Fell and Graystones, before petering out in the direction of Cockermouth.

Geographic entities mentioned:
surface_form: Lord's Seat
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.627
lon: -3.235
surface_form: lord's seat
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.627
lon: -3.235
surface_form: whinlatter
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.614
lon: -3.252
The hub of this group of fells is Lord's Seat, the highest point north of Whinlatter Pass. The main line of high ground runs east to west, taking in Barf, Lord's Seat, Broom Fell and Graystones, before petering out in the direction of Cockermouth. Lord's Seat however sends out a substantial additional ridge which starts southward, curves west and finally turns back north.

Geographic entities mentioned:
surface_form: Broom Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.631
lon: -3.248
surface_form: Graystones
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.627
lon: -3.275
surface_form: graystones
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.627
lon: -3.275
surface_form: lord's seat
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.627
lon: -3.235
surface_form: lord's seat
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.627
lon: -3.235
surface_form: broom fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.631
lon: -3.248
surface_form: barf
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.63
lon: -3.218
This is composed of Greywacke sandstone turbidities. Summit. Brown How bears a large circular hide or windshelter, whilst Whinlatter Top itself has only a modest cairn. The Lake District views are poor, except for the close-ups of Hopegill Head and Grisedale Pike across the pass. Through Whinlatter Pass there is also a sight of the Helvellyn range and Skiddaw group.

Geographic entities mentioned:
surface_form: Hopegill Head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5875
lon: -3.2626694444444
surface_form: Grisedale Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.592
lon: -3.241
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: grisedale pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.592
lon: -3.241
surface_form: hopegill head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5875
lon: -3.2626694444444
The Lake District views are poor, except for the close-ups of Hopegill Head and Grisedale Pike across the pass. Through Whinlatter Pass there is also a sight of the Helvellyn range and Skiddaw group. This is made up for by the northward views to the Solway Firth and the Scottish mountains beyond, best viewed from the westerly peak, Brown How. Ascents.

Geographic entities mentioned:
surface_form: Skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
Modern maps of the Ordnance Survey appear to have conceded the point. Geology. In the summit areas of Whinlatter are rocks of the Loweswater Formation. This is composed of Greywacke sandstone turbidities. Summit. Brown How bears a large circular hide or windshelter, whilst Whinlatter Top itself has only a modest cairn.

Geographic entities mentioned:
surface_form: loweswater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5825
lon: -3.355277777777778
surface_form: whinlatter
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.614
lon: -3.252
From the road summit, Whinlatter Beck runs westward beneath the steepest face of the fell; Whinlatter Crag being a little below the highest point. To the north of Whinlatter is the quiet valley of Aiken Beck, its entrance neatly hidden in the woods between Brown How and Graystones. Its tributaries Willybrag Gill and Drycloff Gill drain the slopes of the fell.

Geographic entities mentioned:
surface_form: graystones
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.627
lon: -3.275
surface_form: whinlatter
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.614
lon: -3.252
Ascents. The easiest line is direct from the top of the pass, either up the side of the forest fence or snaking through the woodland along the forest roads. Brown How can be reached from Aiken, allowing a start from Scawgill Bridge on the western side of the pass. The full circuit of Aiken Beck, taking in Graystones, Broom Fell, Lord's Seat and Whinlatter is also a possibility.

Geographic entities mentioned:
surface_form: graystones
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.627
lon: -3.275
surface_form: lord's seat
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.627
lon: -3.235
surface_form: broom fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.631
lon: -3.248
surface_form: whinlatter
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.614
lon: -3.252
Lord's Seat however sends out a substantial additional ridge which starts southward, curves west and finally turns back north. This is Whinlatter, and the valley enclosed between it and the main ridge is that of Aiken Beck. The descending ridge from Lord's Seat has a number of tops along its length. First is Ullister Hill at, which is normally reckoned part of the parent fell.

Geographic entities mentioned:
surface_form: lord's seat
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.627
lon: -3.235
This is composed of Greywacke sandstone turbidities. Summit. Brown How bears a large circular hide or windshelter, whilst Whinlatter Top itself has only a modest cairn. The Lake District views are poor, except for the close-ups of Hopegill Head and Grisedale Pike across the pass. Through Whinlatter Pass there is also a sight of the Helvellyn range and Skiddaw group.

Geographic entities mentioned:
surface_form: whinlatter
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.614
lon: -3.252
Whinlatter. Whinlatter is a small fell in the north west of the English Lake District, just north of the Whinlatter Pass. It is easily climbed from the top of the Whinlatter Pass, through the Forestry England plantations. The Whinlatter Visitor's Centre, a popular tourist attraction, is on the south side of the fell. The hill is part of a horseshoe around the valley of Aiken Beck.

Geographic entities mentioned:
surface_form: whinlatter
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.614
lon: -3.252
Whinlatter. Whinlatter is a small fell in the north west of the English Lake District, just north of the Whinlatter Pass. It is easily climbed from the top of the Whinlatter Pass, through the Forestry England plantations. The Whinlatter Visitor's Centre, a popular tourist attraction, is on the south side of the fell. The hill is part of a horseshoe around the valley of Aiken Beck.

Geographic entities mentioned:
surface_form: whinlatter
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.614
lon: -3.252
surface_form: whinlatter
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.614
lon: -3.252
Two roads cross from east to west, dividing the fells into three convenient groups. Whinlatter is in the most northerly sector, rising between Whinlatter Pass and the Vale of Embleton. The hub of this group of fells is Lord's Seat, the highest point north of Whinlatter Pass.

Geographic entities mentioned:
surface_form: whinlatter
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.614
lon: -3.252
The descending ridge from Lord's Seat has a number of tops along its length. First is Ullister Hill at, which is normally reckoned part of the parent fell. The ridge then narrows at Tarbarrel Moss at, before rising again as it turns westward to arrive at Whinlatter Top, the summit. A final top, Brown How at, stands above the terminal descent to Aiken Beck.

Geographic entities mentioned:
surface_form: whinlatter
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.614
lon: -3.252
Access problems have now been resolved and the landowner welcomes walkers, with many marked trails being available through the woodland. The southern boundary of the fell is formed by the Whinlatter Pass road. The summit of the pass lies south east of Whinlatter Top, marking the line of the Derwent-Cocker watershed.

Geographic entities mentioned:
surface_form: whinlatter
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.614
lon: -3.252
The southern boundary of the fell is formed by the Whinlatter Pass road. The summit of the pass lies south east of Whinlatter Top, marking the line of the Derwent-Cocker watershed. This falls from Tarbarrel Moss to the road, bypassing the highest point of the fell so that all of its waters flow to the Cocker.

Geographic entities mentioned:
surface_form: whinlatter
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.614
lon: -3.252
The summit of the pass lies south east of Whinlatter Top, marking the line of the Derwent-Cocker watershed. This falls from Tarbarrel Moss to the road, bypassing the highest point of the fell so that all of its waters flow to the Cocker. From the road summit, Whinlatter Beck runs westward beneath the steepest face of the fell; Whinlatter Crag being a little below the highest point.

Geographic entities mentioned:
surface_form: whinlatter
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.614
lon: -3.252
surface_form: whinlatter
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.614
lon: -3.252
To the north of Whinlatter is the quiet valley of Aiken Beck, its entrance neatly hidden in the woods between Brown How and Graystones. Its tributaries Willybrag Gill and Drycloff Gill drain the slopes of the fell. One wonders at the derivation of the former name. Aiken Beck and Whinlatter Gill combine to form Blaze Beck, a sizeable stream flowing into the Cocker at Low Lorton. Position of summit.

Geographic entities mentioned:
surface_form: whinlatter
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.614
lon: -3.252
Popokabaka. Popokabaka is a city in the Kwango Province, Democratic Republic of the Congo. It is the administrative center of Popokabaka Territory. Popokabaka lies on the right bank of the river Kwango River. Francis Dhanis, an agent of the Congo Free State, established a station here around 1890. The territory of Popokabaka borders with Angola in the southwest.

Geographic entities mentioned:
surface_form: Kwango River
instance_of: Watercourse
countries: Angola
Democratic Republic of the Congo
coordinates: lat: -3.3713888888889
lon: 17.358055555556
First played in 1894, it is the fifth-most played college football rivalry game in the Football Bowl Subdivision. Oregon State is still a member of the Pac-12 Conference while Oregon moved to the Big Ten Conference on August 1, 2024. The campuses are less than apart in the Willamette Valley. The series has now been played continuously since 1945.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
However, once Oregon students got out of class, the situation escalated with Webfoots pelting Beavers with tomatoes and water balloons, some Oregon State students were thrown into the millrace, and other OSU students taken to Skinner Butte, stripped and forced to repaint the &quot;O&quot; hillside letter yellow and slide down the painted surface.

Geographic entities mentioned:
surface_form: Skinner Butte
instance_of: Landform
countries: United States
coordinates: lat: 44.0586
lon: -123.093
Sykes' collections of animals resulted in the publications of catalogues of birds and mammals from the Deccan region, many of which were published in the &quot;Proceedings of the Zoological Society&quot;. His discoveries included fifty-six birds new to science, including the Indian pond heron. Sykes also studied the fish of the area, and wrote papers on the quails and hemipodes of India.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
More recent excavations show that the process of Edomite settlement in the southern parts of Judah and parts of the Negev down to Timna had started already before the destruction of the kingdom by Nebuchadnezzar II in 587/86 BC, both by peaceful penetration and by military means and taking advantage of the already-weakened state of Judah.

Geographic entities mentioned:
surface_form: Timna
instance_of: Valley
countries: Israel
coordinates: lat: 29.78777778
lon: 34.98888889
The existence of the Kingdom of Edom was asserted by archaeologists led by Ezra Ben-Yosef and Tom Levy, by using a methodology called the punctuated equilibrium model in 2019. Archaeologists mainly took copper samples from Timna Valley and Faynan in Jordan’s Arava valley dated to 1300-800 BC.

Geographic entities mentioned:
surface_form: Timna Valley
instance_of: Valley
countries: Israel
coordinates: lat: 29.78777778
lon: 34.98888889
surface_form: Faynan
instance_of: Valley
countries: Jordan
coordinates: lat: 30.62282
lon: 35.44775
The king of Edom did not attack the Israelites, though he prepared to resist aggression. Nothing further is recorded of the Edomites in the Tanakh until their defeat by King Saul of Israel in the late 11th century BC (). Forty years later King David and his general Joab defeated the Edomites in the &quot;Valley of Salt&quot; (probably near the Dead Sea;;).

Geographic entities mentioned:
surface_form: Valley of Salt
instance_of: Valley
Lake Arpin. Lake Arpin is a small lake located in the Laurentian Mountains of Quebec, Canada. This is a non populated lake. The first house to be built close to the water was in 2005. Until this house was built, the only access point was Chemin du Sentier, an almost fully grown-in dirt road. A bridge now gives access from Chemin du Lac Arpin to a small river which connects to the lake.

Geographic entities mentioned:
surface_form: lac arpin
instance_of: Lake
countries: Canada
coordinates: lat: 46.13078
lon: -74.281483
Lake Arpin. Lake Arpin is a small lake located in the Laurentian Mountains of Quebec, Canada. This is a non populated lake. The first house to be built close to the water was in 2005. Until this house was built, the only access point was Chemin du Sentier, an almost fully grown-in dirt road. A bridge now gives access from Chemin du Lac Arpin to a small river which connects to the lake.

Geographic entities mentioned:
surface_form: lake arpin
instance_of: Lake
countries: Canada
coordinates: lat: 46.13078
lon: -74.281483
Quaibrücke, Zurich. Quaibrücke () is a road, tramway, pedestrian and bicycle bridge over the river Limmat, at the outflow of Lake Zurich in the city of Zurich, Switzerland. It was built simultaneously with the construction of Zurich's new quays between 1881 and 1887. Geography.

Geographic entities mentioned:
surface_form: Lake Zurich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
It was built simultaneously with the construction of Zurich's new quays between 1881 and 1887. Geography. The Quaibrücke is situated at the outflow of Lake Zurich and connects Bürkliplatz with Bellevueplatz, and thus the lake's left (or western) shore with the right (or eastern) shore. It is a nodal point of tram lines,, and, as well of the road traffic between General-Guisan-Quai and Utoquai.

Geographic entities mentioned:
surface_form: Lake Zurich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
It is a National Wild and Scenic River. Its two forks rise in the Cascades in eastern Snohomish County, in the Glacier Peak Wilderness and join to form the mainstem Sauk River at Bedal Peak. From there the river flows northwest from there through a remote section of the Mount Baker-Snoqualmie National Forest to Darrington, then north to join the Skagit River from the south at Rockport.

Geographic entities mentioned:
surface_form: Bedal Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.068611111111
lon: -121.35361111111
The name &quot;Sauk&quot; comes from the &quot;Sah-kee-ma-hu&quot; (Sauk-Suiattle tribe), a group related to the Skagit tribes, not from the Sauk tribe of the Midwestern U.S. South Fork. The South Fork Sauk River's headwaters flow from a glacier on the northwest side of Columbia Peak. The river flows generally northwest through Seventysix Gulch to Monte Cristo, where it is joined by Glacier Creek.

Geographic entities mentioned:
surface_form: Columbia Peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.9615814
lon: -121.3613536
Dickson Lake. Dickson Lake is a glacier lake in southern Patagonia located in the Southern Patagonian Ice Field, which since 1998 has been transformed into an international lake as it is crossed by the international boundary between Argentina and Chile due to the retreat of the Dickson glacier.

Geographic entities mentioned:
surface_form: dickson
instance_of: Lake
countries: Argentina
Chile
coordinates: lat: -50.833333333333
lon: -73.116666666667
Dickson Lake. Dickson Lake is a glacier lake in southern Patagonia located in the Southern Patagonian Ice Field, which since 1998 has been transformed into an international lake as it is crossed by the international boundary between Argentina and Chile due to the retreat of the Dickson glacier.

Geographic entities mentioned:
surface_form: dickson
instance_of: Lake
countries: Argentina
Chile
coordinates: lat: -50.833333333333
lon: -73.116666666667
surface_form: dickson
instance_of: Lake
countries: Argentina
Chile
coordinates: lat: -50.833333333333
lon: -73.116666666667
Until that year, Dickson Lake was entirely within Chilean territory, at the northern end of the Torres del Paine National Park in the Magallanes y la Antártica Chilena Region, but it was unified with a lake that began to form in the 1980s by defrosting the melting of the Dickson, Cubo (or Cincuentenario) and Frías (or Grande) glaciers.

Geographic entities mentioned:
surface_form: dickson
instance_of: Lake
countries: Argentina
Chile
coordinates: lat: -50.833333333333
lon: -73.116666666667
surface_form: dickson
instance_of: Lake
countries: Argentina
Chile
coordinates: lat: -50.833333333333
lon: -73.116666666667
Radar Lake. Radar Lake is located in Woodinville, Washington and is one of the first man-made lakes built specifically for water sports. The land it is built on was initially bought and developed by water sports innovator Herb O'Brien in 1972.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: radar lake
instance_of: Lake
countries: United States
coordinates: lat: 47.73
lon: -122.0236111
Radar Lake. Radar Lake is located in Woodinville, Washington and is one of the first man-made lakes built specifically for water sports. The land it is built on was initially bought and developed by water sports innovator Herb O'Brien in 1972.

Geographic entities mentioned:
surface_form: radar lake
instance_of: Lake
countries: United States
coordinates: lat: 47.73
lon: -122.0236111
The land it is built on was initially bought and developed by water sports innovator Herb O'Brien in 1972. O'Brien, drawing from his water sports experiences as a young man, envisioned Radar Lake to be an isolated and private area where enthusiasts could come and enjoy not only the thrill of the sport but also the pristine natural environment.

Geographic entities mentioned:
surface_form: radar lake
instance_of: Lake
countries: United States
coordinates: lat: 47.73
lon: -122.0236111
Wilbur McPherson who gave it its current name in honor of his company. McPherson and O'Brien maintained a close relationship, and O'Brien bought Radar Lake back from McPherson in 2000. McPherson continued to live on the property, along with O'Brien and their respective families, until he lost his life to cancer in 2007.

Geographic entities mentioned:
surface_form: radar lake
instance_of: Lake
countries: United States
coordinates: lat: 47.73
lon: -122.0236111
He was enthroned on 22 November 2005, despite initial Israeli objections. The Israeli government officially recognized Theophilos' election on 16 December 2007. Prior to becoming Patriarch of Jerusalem, Theophilos was the Eastern Orthodox Archbishop of Tabor. Biography.

Geographic entities mentioned:
surface_form: Tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
He subsequently served as Exarch of the Holy Sepulchre in Qatar. From 2000 to 2003, he was church envoy to the Patriarchate of Moscow. In February 2005, he was consecrated Archbishop of Tabor. He was officially enthroned as Patriarch of Jerusalem and All Palestine on November 22, 2005.

Geographic entities mentioned:
surface_form: Tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
Jabba Lake. Jabba Lake, also known as Jaba Lake is an alpine glacial lake located in the Ushu valley of Swat Kohistan region in northern Pakistan. Elevation of lake is about 14,000 feet above sea level.

Geographic entities mentioned:
surface_form: jabba lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 35.62388888888889
lon: 72.79861111111111
Fort Collinson. Fort Collinson was a trading post operated by the Hudson's Bay Company (Post Number B.405) located on Victoria Island in the Northwest Territories, Canada. It is situated on the Prince Albert Peninsula on the north side of Walker Bay, just north of Minto Inlet.

Geographic entities mentioned:
surface_form: Minto Inlet
instance_of: Body of water
countries: Canada
coordinates: lat: 71.25
lon: -117
Subsequently, the 1876 Constantinople Conference of the Great Powers confirmed that early delimitation in its more comprehensive definition of ethnic Bulgarian lands as of the late 19th century. Honour. Riggs Peak on Smith Island, South Shetland Islands is named after Elias Riggs.

Geographic entities mentioned:
surface_form: Riggs Peak
instance_of: Mountain
coordinates: lat: -63.035555555556
lon: -62.613888888889
The isolated habitat has many endemic species. It is relatively stable and intact. Location. The Cordillera de Merida páramo is to the south of the Lake Maracaibo in the Cordillera de Mérida massif of northeastern Venezuela. It is surrounded by the Venezuelan Andes montane forests ecoregion. Terrain.

Geographic entities mentioned:
surface_form: Lake Maracaibo
instance_of: Lake
countries: Venezuela
coordinates: lat: 9.8158333333333
lon: -71.556666666667
Terrain. Páramos in the southwest of the Cordillera de Merida include Batalló at above sea level and Nariño at. The highest point in the central section is the Piedras Blancas peak at, surrounded by extensive páramos, glaciers and lakes. From the Piedras Blancas páramo the land descends to the Mucuchíes páramo at, then continues to gradually descend towards the northeast. Climate.

Geographic entities mentioned:
surface_form: Piedras Blancas peak
instance_of: Mountain
countries: Venezuela
coordinates: lat: 8.858833333333333
lon: -70.95166666666667
Tricorner Knob. Tricorner Knob is a mountain in the Great Smoky Mountains, located in the southeastern United States. It has an elevation of 6,120 feet (1,865 m), with 160 feet (48 m) of clean prominence. The Appalachian and Balsam Mountain trails intersect near the mountain's summit, making Tricorner Knob the great crossroads of the eastern Smokies. Description.

Geographic entities mentioned:
surface_form: tricorner knob
instance_of: Mountain
countries: United States
coordinates: lat: 35.695561111111
lon: -83.254169444444
Tricorner Knob. Tricorner Knob is a mountain in the Great Smoky Mountains, located in the southeastern United States. It has an elevation of 6,120 feet (1,865 m), with 160 feet (48 m) of clean prominence. The Appalachian and Balsam Mountain trails intersect near the mountain's summit, making Tricorner Knob the great crossroads of the eastern Smokies. Description.

Geographic entities mentioned:
surface_form: tricorner knob
instance_of: Mountain
countries: United States
coordinates: lat: 35.695561111111
lon: -83.254169444444
surface_form: balsam mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0908
lon: -74.488
Description. Like much of the Smokies crest, Tricorner Knob is on the border between Tennessee and North Carolina. As its name implies, the mountain is at the point where the Balsam Mountains intersect the crest of the Great Smokies, creating a triangular-shaped ridge.

Geographic entities mentioned:
surface_form: tricorner knob
instance_of: Mountain
countries: United States
coordinates: lat: 35.695561111111
lon: -83.254169444444
Tricorner is the ninth-highest mountain in Tennessee and the 27th-highest mountain in North Carolina. History. Tricorner Knob's remote situation in the dense Southern Appalachian spruce–fir forest of the eastern Smokies has left it largely untouched by human history. Arnold Guyot measured its elevation on his survey of the crest of the Smokies in 1859, placing Tricorner's elevation at.

Geographic entities mentioned:
surface_form: tricorner knob
instance_of: Mountain
countries: United States
coordinates: lat: 35.695561111111
lon: -83.254169444444
Other than surveyors and the occasional naturalist, the mountain was devoid of human visitors until a segment of the Appalachian Trail was constructed across its western slope in 1935. An isolated spring on the mountain's southern slope was the key reason behind its selection for the back country campsite where the Tricorner Knob Shelter sits today.

Geographic entities mentioned:
surface_form: tricorner knob
instance_of: Mountain
countries: United States
coordinates: lat: 35.695561111111
lon: -83.254169444444
An isolated spring on the mountain's southern slope was the key reason behind its selection for the back country campsite where the Tricorner Knob Shelter sits today. Laura Thornborough, a writer who visited the mountain in the late 1930s, called Tricorner Knob one of the last &quot;true wilderness areas, where one can commune with nature and leave the cares of the world behind.&quot;
Access.

Geographic entities mentioned:
surface_form: tricorner knob
instance_of: Mountain
countries: United States
coordinates: lat: 35.695561111111
lon: -83.254169444444
surface_form: tricorner knob
instance_of: Mountain
countries: United States
coordinates: lat: 35.695561111111
lon: -83.254169444444
The latter can be accessed via a sharp bend in Straight Fork Road, a rugged gravel road rising out of Cherokee, North Carolina. From this bend, Tricorner Knob is just over away. A section of the Appalachian Trail connects Tricorner Knob with Newfound Gap in the central Smokies. The Tricorner Knob Shelter can accommodate 12 people.

Geographic entities mentioned:
surface_form: tricorner knob
instance_of: Mountain
countries: United States
coordinates: lat: 35.695561111111
lon: -83.254169444444
The latter can be accessed via a sharp bend in Straight Fork Road, a rugged gravel road rising out of Cherokee, North Carolina. From this bend, Tricorner Knob is just over away. A section of the Appalachian Trail connects Tricorner Knob with Newfound Gap in the central Smokies. The Tricorner Knob Shelter can accommodate 12 people.

Geographic entities mentioned:
surface_form: tricorner knob
instance_of: Mountain
countries: United States
coordinates: lat: 35.695561111111
lon: -83.254169444444
surface_form: tricorner knob
instance_of: Mountain
countries: United States
coordinates: lat: 35.695561111111
lon: -83.254169444444
From the Cosby Campground (specifically behind Campsite B51), the Snake Den Ridge Trail winds up the ridge to its junction with the Appalachian Trail. From this junction, Tricorner is away, with the trail first crossing the slopes of Old Black and Mount Guyot. The Balsam Mountain Trail is a trail connecting the Appalachian Trail in the west with the Benton MacKaye Trail to the east.

Geographic entities mentioned:
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 39.4587
lon: -105.938
Pirania. &quot;Pirania&quot; is an extinct genus of sea sponge known from the Middle Cambrian Burgess Shale and the Ordovician Fezouata formation. It is named after Mount St. Piran, a mountain situated in the Bow River Valley in Banff National Park, Alberta. It was first described in 1920 by Charles Doolittle Walcott.

Geographic entities mentioned:
surface_form: Mount St. Piran
instance_of: Mountain
countries: Canada
coordinates: lat: 51.42138888888889
lon: -116.25277777777778
Fearing for his life, he approached his old friends for help and the best they could do was draft him. In the autumn of 1942, Pannwitz was drafted by Abwehr office for the Wehrmacht, and was posted for several months as a Non-commissioned officer to a unit of the Brandenburgh Division run by the Abwehr that was located on Lake Ladoga on the Finnish-Russian border.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
It is a natural monument sculpted by erosive actions, mainly of glaciers. Its form is very similar to a giant castle, in the front flow the Malargüe River and very near the Pincheira Stream. According to the legend, this site was a refuge for the Chilean bandits called Pincheira brothers, during the beginning of the 20th century.

Geographic entities mentioned:
surface_form: Malargüe River
instance_of: Watercourse
countries: Argentina
coordinates: lat: -35.5
lon: -70
After making a three-month pilgrimage to the Holy Land in the summer of 1964, she returned the following year to study Sacred Scripture and Hebrew Literature at the Hebrew University of Jerusalem, graduating in 1969. In Jerusalem, she settled in a small hut on the Mount of Olives, but always welcomed those who visited her. It was her belief that all Christians had a part to play in the Holy Land.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
Geography. Boykin is located along U.S. Route 27 in southern Miller County, southeast of Colquitt, the county seat, and northwest of Bainbridge. The CDP is bordered to the south by Big Drain, which flows west to Spring Creek, which continues south to Lake Seminole near the confluence of the Flint and Chattahoochee rivers to form the Apalachicola River. According to the U.S.

Geographic entities mentioned:
surface_form: Chattahoochee
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Meanwhile, other German emigrants from Pennsylvania continued south past the Shenandoah Valley into North Carolina to avoid disputes after they developed farms. By 1745 the sixth Lord Fairfax, a bachelor, took a trip to the Virginia colony, settled there in 1747 and died at his Greenway Court hunting lodge in 1781.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Mount Washington (disambiguation). ebl2ndczmhja4u4bittrjs58kjmz2" xml:space="preserve">Mount Washington is a mountain in New Hampshire.

Geographic entities mentioned:
surface_form: Mount Washington
instance_of: Mountain
countries: United States
coordinates: lat: 44.270827777778
lon: -71.303483333333
Gutenstein Alps. The Gutenstein Alps () are a mountain range in the Eastern Alps in Central Europe, and the northeasternmost part of the Northern Limestone Alps, reaching heights over 1,000 m. Topography. Die Gutenstein Alps are separated in the north from the Vienna Woods by the valleys of the Gölsen and Triesting. In the east they descend to the Vienna Basin.

Geographic entities mentioned:
surface_form: Triesting
instance_of: Watercourse
countries: Austria
coordinates: lat: 48.0811
lon: 16.3992
Husdal. Husdal () is a short valley running west-southwest from the head of Husvik Harbour, South Georgia. It was named by the UK Antarctic Place-Names Committee in the Norwegian form &quot;Husdal&quot; (house valley) in association with the disused Husvik whaling station at the head of Husvik Harbour.

Geographic entities mentioned:
surface_form: husdal
instance_of: Valley
countries: United Kingdom
coordinates: lat: -54.1833
lon: -36.7167
That &quot;crinitus&quot;, which occurs at over altitude in the Valley of Mexico, was the same species as &quot;peninsulae&quot; from the lowlands of the Baja California Peninsula they could not accept and they recommended further research to determine the relationships of &quot;crinitus&quot;.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
According to Jones and Engstrom, rice rats from the island of Ometepe in Lake Nicaragua are distinctive in their large skull and small external measurements, with an especially short tail, soft fur that is orange-brown above and buffish below, and lack of sphenopalatine vacuities (openings in the roof of the mesopterygoid fossa, the gap behind the end of the bony palate).

Geographic entities mentioned:
surface_form: Lake Nicaragua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 11.5742
lon: -85.3563
The Hamilton and Lake Erie Railway (H&LE) is a historical shortline railway in Ontario, Canada. It ran from Hamilton to Port Dover, about, providing trans-shipping service between Lake Erie and Lake Ontario, and with connections, to Lake Huron at Georgian Bay. Formed in 1834 as the Hamilton and Port Dover Railway, it rechartered in 1853 and purchased the Hamilton and Southwestern Railway in 1855.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Nothing came of any of these companies. When the charter was renewed in December 1869, it was purchased by the newly formed H&LE. Construction began in 1873, but the $1 million cost of driving up the Hamilton Mountain (part of the Niagara Escarpment at Hamilton) and building a bridge at the Grand River at Caledonia was too much too bear.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
The company ran out of cash after reaching Jarvis in January 1875, only a few miles short of Port Dover. The company was purchased by the well-financed Hamilton and North-Western Railway (H&NW) in 1877. Through this merger, the H&NW controlled a network that connected Lake Erie, Ontario, Simcoe and Huron. The line was finally completed to Port Dover the next year.

Geographic entities mentioned:
surface_form: Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
surface_form: Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Looking to address this problem, businessmen in Hamilton began planning a network of new rail lines that would provide more convenient shipping than Toronto due to their location at the very western tip of Lake Ontario.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
By January 1875 the line was complete for to Jarvis, only short of its goal in Port Dover. However, the $1 million cost of running the line up Mount Hamilton (part of the Niagara Escarpment) and building a bridge across the Grand River at Caledonia had eaten up the company's funding, and further construction was abandoned.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
The first station was on Ferguson at Main Street. A short distance beyond the station the line bends 90 degrees to run southeastward upward along the edge of the Niagara Escarpment. It runs about to the area near modern Kenilworth Avenue, where it turned southwest again, now on top of Hamilton Mountain. After another was Rymal station.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
Jochköpfl (Bavaria). The Jochköpfl (also: Feuerspitz) is a mountain, in the Latten Mountains in the Berchtesgaden Alps. It is located in the German federal state of Bavaria.

Geographic entities mentioned:
surface_form: feuerspitz
instance_of: Mountain
countries: Germany
coordinates: lat: 47.6433
lon: 12.8758
surface_form: jochköpfl
instance_of: Mountain
countries: Germany
coordinates: lat: 47.6433
lon: 12.8758
Jochköpfl (Bavaria). The Jochköpfl (also: Feuerspitz) is a mountain, in the Latten Mountains in the Berchtesgaden Alps. It is located in the German federal state of Bavaria.

Geographic entities mentioned:
surface_form: jochköpfl (bavaria)
instance_of: Mountain
countries: Germany
coordinates: lat: 47.6433
lon: 12.8758
The Graafwater rocks can best be seen just above the contour path on the front of Table Mountain, and around Devils Peak. They can also been seen in the cutting along Chapman's Peak Drive. These rocks are believed to have originated in shallow tidal flats, in which a few Ordovician fossils, and fossil tracks have been preserved.

Geographic entities mentioned:
surface_form: Chapman's Peak
instance_of: Mountain
countries: South Africa
coordinates: lat: -34.0872
lon: 18.3606
The anticline, or highest point of the series of folds that Table Mountain was once part of, lay to the east, but that has been weathered away, together with the underlying softer Malmesbury shale and granite basement, to form the &quot;Cape Flats&quot;, the isthmus that connects the Cape Peninsula to the mainland.

Geographic entities mentioned:
surface_form: series of folds that Table Mountain was once part of
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
Commercial groups also offer abseiling from the upper cable station. Caving. Most of the world's important caves occur in limestone but Table Mountain is unusual in having several large cave systems that have developed in sandstone. The biggest systems are the Wynberg Caves, located on the Back Table, not far from the Jeep Track, in ridges overlooking Orange Kloof and Hout Bay. Mountain biking.

Geographic entities mentioned:
surface_form: Orange Kloof
instance_of: Valley
countries: South Africa
coordinates: lat: -34.0022
lon: 18.3894
Features. The main feature of Table Mountain is the level plateau approximately from side to side, edged by steep cliffs. The plateau, flanked by Devil's Peak to the east and by Lion's Head to the west, forms a dramatic backdrop to Cape Town. This broad sweep of mountainous heights, together with Signal Hill, forms the natural amphitheatre of the City Bowl and Table Bay harbour.

Geographic entities mentioned:
surface_form: devil's peak
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.954752777778
lon: 18.439263888889
surface_form: lion's head
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.934722222222
lon: 18.389166666667
The eastern side of this portion of the Peninsula's mountain chain, extending from Devil's Peak, the eastern side of Table Mountain (Erica and Fernwood Buttresses), and the Back Table to Constantia Nek, does not have a single name, as on the western side.

Geographic entities mentioned:
surface_form: devil's peak
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.954752777778
lon: 18.439263888889
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Table Mountain is the northernmost end of a and roughly Cape Fold Mountain range that forms the backbone of the Cape Peninsula, stretching from the Cape of Good Hope in the south to Table Mountain and its flanking Devil's Peak (to the east) and Lion's Head and Signal Hill (to the west) in the north. Table Mountain forms the highest point of this range.

Geographic entities mentioned:
surface_form: devil's peak
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.954752777778
lon: 18.439263888889
surface_form: lion's head
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.934722222222
lon: 18.389166666667
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
surface_form: signal hill
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.917777777778
lon: 18.402777777778
The frequency of the fires obviously determines precisely which mix of plants will dominate any particular region, but intervals of 10–15 years between fires are considered to promote the proliferation of the larger Protea species, a rare local colony of which, the &quot;Aulax umbellata&quot; (Family: Proteaceae), was wiped out on the Peninsula by more frequent fires, as have been the silky-haired pincushion, &quot;Leucospermum vestitum&quot;, the red sugarbush, &quot;Protea grandiceps&quot; and Burchell's sugarbush, &quot;Protea burchellii&quot;, although a stand of a dozen or so plants has recently been &quot;rediscovered&quot; in the saddle between Table Mountain and Devil's Peak.

Geographic entities mentioned:
surface_form: devil's peak
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.954752777778
lon: 18.439263888889
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
The &quot;Back Table&quot; extends southwards for approximately 6 km to the Constantia Nek-Hout Bay valley. The Atlantic side of the Back Table is known as the Twelve Apostles, which extends from Kloof Nek (the saddle between Table Mountain and Lion's Head) to Hout Bay.

Geographic entities mentioned:
surface_form: lion's head
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.934722222222
lon: 18.389166666667
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
They are of late Precambrian age, pre-dating the &quot;Graafwater rocks&quot; by at least 40 million years. The basement rocks are not nearly as resistant to weathering as the TMS, but significant outcrops of the Cape Granite are visible on the western side of Lion's Head, and elsewhere on the Peninsula (especially below Chapman's Peak Drive, and The Boulders near Simon's Town).

Geographic entities mentioned:
surface_form: lion's head
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.934722222222
lon: 18.389166666667
surface_form: chapman's peak
instance_of: Mountain
countries: South Africa
coordinates: lat: -34.0872
lon: 18.3606
Table Mountain. Table Mountain (;) is a flat-topped mountain forming a prominent landmark overlooking the city of Cape Town in South Africa. It is a significant tourist attraction, with many visitors using the cableway or hiking to the top. The mountain has 8,200 plant species, of which around 80% are fynbos (Afrikaans for 'fine bush').

Geographic entities mentioned:
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
The mountain has 8,200 plant species, of which around 80% are fynbos (Afrikaans for 'fine bush'). Table Mountain National Park is the most visited national park in South Africa, attracting 4.2 million people every year for various activities. It forms part of the lands formerly ranged by Khoe-speaking clans, such as the (the &quot;High Clan&quot;).

Geographic entities mentioned:
surface_form: table mountain national park
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Features. The main feature of Table Mountain is the level plateau approximately from side to side, edged by steep cliffs. The plateau, flanked by Devil's Peak to the east and by Lion's Head to the west, forms a dramatic backdrop to Cape Town. This broad sweep of mountainous heights, together with Signal Hill, forms the natural amphitheatre of the City Bowl and Table Bay harbour.

Geographic entities mentioned:
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
This broad sweep of mountainous heights, together with Signal Hill, forms the natural amphitheatre of the City Bowl and Table Bay harbour. The highest point on Table Mountain is towards the eastern end of the plateau and is marked by Maclear's Beacon, a stone cairn built in 1865 by Sir Thomas Maclear for trigonometrical survey.

Geographic entities mentioned:
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Legend attributes this phenomenon to a smoking contest between the Devil and a local pirate called Van Hunks. When the table cloth is seen, it symbolizes the contest. Table Mountain is at the northern end of a sandstone mountain range that forms the spine of the Cape Peninsula that terminates approximately to the south at the Cape of Good Hope and Cape Point.

Geographic entities mentioned:
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Table Mountain is at the northern end of a sandstone mountain range that forms the spine of the Cape Peninsula that terminates approximately to the south at the Cape of Good Hope and Cape Point. Immediately to the south of Table Mountain is a rugged &quot;plateau&quot; at a somewhat lower elevation than the Table Mountain Plateau (at about), called the &quot;Back Table&quot;.

Geographic entities mentioned:
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
The uppermost, and younger of the two layers, consists of extremely hard quartzitic sandstone, commonly referred to as &quot;Table Mountain Sandstone&quot; (TMS), or &quot;Peninsula Formation Sandstone&quot; (as it is known as at present), which is highly resistant to erosion and forms characteristic steep grey crags.

Geographic entities mentioned:
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
The lower layer, known as the &quot;Graafwater Formation&quot;, consists of distinctively maroon-colored mudstones, which were laid down in much thinner horizontal strata than the Table Mountain Sandstone strata above it. The Graafwater rocks can best be seen just above the contour path on the front of Table Mountain, and around Devils Peak.

Geographic entities mentioned:
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Most of the vineyards found on the Cape Peninsula are therefore found on these granitic slopes of the Table Mountain range. The mountain owes its table-top flatness to the fact that it is a syncline mountain, meaning that it was once the floor of a valley (see diagram on the right).

Geographic entities mentioned:
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352