Sarmila/GeoWiki-Features huggingface dataset:
Located on the east bank of the Fraser River, Soda Creek was originally the home of the Xat'sull First Nation. Soda Creek Indian Reserve No. 1 is located on the left (E) bank of the Fraser River, one mile south of the Soda Creek BCR (CN) station, 431.10 ha. Xat'sull means &quot;on the cliff where the bubbling water comes out&quot;.

Geographic entities mentioned:
surface_form: soda creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.331944
lon: -122.280833
Xat'sull means &quot;on the cliff where the bubbling water comes out&quot;. European settlement began in the 1860s with the onset of the Cariboo Gold Rush and the building of the Old Cariboo Road. History. The Old Cariboo Road was built from Lillooet to Alexandria, beginning in 1859 and completed to Soda Creek in 1863. The roadbuilder for that section was Gustavus Blin Wright.

Geographic entities mentioned:
surface_form: soda creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.331944
lon: -122.280833
The Fraser River was not considered navigable by sternwheeler north of Yale due to many hazardous rapids and canyons. However, from Soda Creek to Quesnel, the Fraser was relatively free of obstructions, therefore Soda Creek was the logical terminus for sternwheelers on the upper Fraser River.

Geographic entities mentioned:
surface_form: soda creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.331944
lon: -122.280833
surface_form: soda creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.331944
lon: -122.280833
The &quot;Enterprise&quot; was launched in the spring of 1863 and most of the travelers on their way to the goldfields, by foot, horseback, or wagon, took the &quot;Enterprise&quot; as the wagon road would not be not completed to Quesnel until 1865. With the launching of the &quot;Enterprise&quot; the government placed a land reserve on Soda Creek. Almost at once land lots were sold.

Geographic entities mentioned:
surface_form: soda creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.331944
lon: -122.280833
The Fort George Lumber and Navigation Company of South Fort George built two sternwheelers at Soda Creek, both in the winter of 1909/10, the &quot; Chilcotin&quot; and the &quot;Fort Fraser&quot; which were used along with the &quot;Chilco&quot;, &quot;Charlotte&quot; and &quot;Quesnel&quot; to deliver passengers and supplies to the new communities in Fort George.

Geographic entities mentioned:
surface_form: soda creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.331944
lon: -122.280833
The BC Express Company built a company office and construction site at Soda Creek and in the winter of 1909/10 they built the &quot;BX&quot; and then the &quot;BC Express&quot; in the winter of 1911/12. The automobiles were Winton Sixes, purchased in 1910 from a car manufacturer in Seattle.

Geographic entities mentioned:
surface_form: soda creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.331944
lon: -122.280833
In April 1936 she took the new Viceroy of India, the Marquess of Linlithgow, to Bombay with his wife, daughters, and personal staff, and brought home his predecessor, the Marquess of Willingdon. Later in 1936 she took a British-American climbing expedition, including Bill Tilman, Noel Odell, and Charles Snead Houston, to India for the successful first ascent of Nanda Devi.

Geographic entities mentioned:
surface_form: Nanda Devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
Avalanche Spire. Avalanche Spire is a mountain in the Alaska Range located south of Denali. It is very technical due to its steep slopes. The mountain's toponym was officially adopted in 1968 by the United States Board on Geographic Names. Climate. Based on the Köppen climate classification, Avalanche Spire is located in a tundra climate zone with long, cold, snowy winters, and cool summers.

Geographic entities mentioned:
surface_form: Denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: avalanche spire
instance_of: Mountain
countries: United States
coordinates: lat: 62.8064
lon: -151.153
Avalanche Spire. Avalanche Spire is a mountain in the Alaska Range located south of Denali. It is very technical due to its steep slopes. The mountain's toponym was officially adopted in 1968 by the United States Board on Geographic Names. Climate. Based on the Köppen climate classification, Avalanche Spire is located in a tundra climate zone with long, cold, snowy winters, and cool summers.

Geographic entities mentioned:
surface_form: avalanche spire
instance_of: Mountain
countries: United States
coordinates: lat: 62.8064
lon: -151.153
The mountain's toponym was officially adopted in 1968 by the United States Board on Geographic Names. Climate. Based on the Köppen climate classification, Avalanche Spire is located in a tundra climate zone with long, cold, snowy winters, and cool summers. Weather systems are forced upwards by the Alaska Range (orographic lift), causing heavy precipitation in the form of snowfall.

Geographic entities mentioned:
surface_form: avalanche spire
instance_of: Mountain
countries: United States
coordinates: lat: 62.8064
lon: -151.153
It is also believed that the Ashvins were the first one to prepare the &quot;chayavanprasham&quot; formulation for Sage Chyavana believed in local tradition to be located at his ashram on Dhosi Hill near Narnaul, Haryana, India, the etymology behind the modern rendering of &quot;chyavanprash&quot;.

Geographic entities mentioned:
surface_form: Dhosi Hill
instance_of: Mountain
countries: India
coordinates: lat: 28.061
lon: 76.0313
Gapyeongcheon. 3lah9r2pe04o2y4nfc9qnuapff8l" xml:space="preserve">Gapyeongcheon () is a river of South Korea. It is a river of the Han River system. The Gapyeong Rail Park is located adjacent to the stream. The stream was found to be contaminated by bis(2-ethylhexyl) phthalate (DEHP) with 50 ppb.

Geographic entities mentioned:
surface_form: gapyeongcheon
instance_of: Watercourse
countries: South Korea
Hyperolius spinigularis. &quot;Hyperolius spinigularis&quot; is a species of frog in the family Hyperoliidae. It is found in the Mulanje Massif in southern Malawi and the Namuli Massif in adjacent Mozambique. Records from Tanzania refers to other species. Males of this species have characteristic small spines during the breeding season.

Geographic entities mentioned:
surface_form: Namuli Massif
instance_of: Mountain
countries: Mozambique
coordinates: lat: -15.366666666667
lon: 37.033333333333
The site was occupied from the Middle Ages, and the house incorporates part of a 17th-century castle. This was remodelled in the 19th century, but the house has been derelict since the mid-20th century. It was the seat of the Gordon family of Lochinvar, later raised to the peerage as Viscounts of Kenmure. The ruin is a scheduled monument. History.

Geographic entities mentioned:
surface_form: Lochinvar
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.142777777778
lon: -4.1058333333333
It later belonged to the Douglas and Maxwell families. Kenmure became a property of the Gordon family from 1297, when they arrived from Berwickshire. The Gordons also built a castle on an island in Lochinvar, some to the north. James IV of Scotland came to Kenmure in March 1508 following a pilgrimage to Whithorn.

Geographic entities mentioned:
surface_form: Lochinvar
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.142777777778
lon: -4.1058333333333
The city of Dasmariñas is landlocked. However, it is not too far from the coastal towns of Rosario, Kawit, Bacoor, Noveleta and Cavite City whose average distance from Poblacion is less than. It is about the same distance from Laguna de Bay and from the resort city of Tagaytay and the famous Taal Lake.

Geographic entities mentioned:
surface_form: Taal Lake
instance_of: Lake
countries: Philippines
coordinates: lat: 13.986944
lon: 121.012222
Api Chamber. Api Chamber is a chamber in Whiterock Cave in Mount Api, Gunung Mulu National Park, Sarawak, Malaysia. Measuring 300 m by 200 m and with a surveyed circumference of 900 m it is the ninth largest cave chamber by area in the world. Its height is over 100 m and its plan area is 58,000 square metres. It is the second largest chamber in Malaysia after Sarawak Chamber.

Geographic entities mentioned:
surface_form: Mount Api
instance_of: Mountain
countries: Malaysia
coordinates: lat: 4.101944444444444
lon: 114.89305555555555
Scoat Fell. Scoat Fell is a fell in the western part of the English Lake District. It stands at the head of the Mosedale Horseshoe with its back to Ennerdale. Paths lead to Scoat Fell from Ennerdale over Steeple, from Wasdale over Red Pike, and along the ridge from Pillar. Topography.

Geographic entities mentioned:
surface_form: Wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
surface_form: pillar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.497
lon: -3.282
surface_form: steeple
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493
lon: -3.302
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.526
lon: -3.3
surface_form: scoat fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.490038888889
lon: -3.2998
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Paths lead to Scoat Fell from Ennerdale over Steeple, from Wasdale over Red Pike, and along the ridge from Pillar. Topography. The Western Fells occupy a triangular sector of the Lake District, bordered by the River Cocker to the north east and Wasdale to the south east. Westwards the hills diminish toward the coastal plain of Cumberland.

Geographic entities mentioned:
surface_form: Wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Westwards the hills diminish toward the coastal plain of Cumberland. At the central hub of the high country are Great Gable and its satellites, while two principal ridges fan out on either flank of Ennerdale, the western fells in effect being a great horseshoe around this long wild valley. Scoat Fell is on the southern arm.

Geographic entities mentioned:
surface_form: Great Gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
surface_form: Ennerdale
instance_of: Valley
countries: United Kingdom
Scoat Fell is on the southern arm. The main watershed runs broadly westwards from Great Gable, dividing the headwaters of Ennerdale and Wasdale. The principal fells in this section are Kirk Fell, Pillar, Scoat Fell, Haycock and Caw Fell, followed by the lower Lank Rigg group. Scoat Fell occupies an important position at the crossroads of five ridges.

Geographic entities mentioned:
surface_form: Wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: great gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Scoat Fell is on the southern arm. The main watershed runs broadly westwards from Great Gable, dividing the headwaters of Ennerdale and Wasdale. The principal fells in this section are Kirk Fell, Pillar, Scoat Fell, Haycock and Caw Fell, followed by the lower Lank Rigg group. Scoat Fell occupies an important position at the crossroads of five ridges.

Geographic entities mentioned:
surface_form: Kirk Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.242
surface_form: Caw Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.486
lon: -3.343
surface_form: Lank Rigg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.494
lon: -3.403
surface_form: haycock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4844
lon: -3.32278
surface_form: pillar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.497
lon: -3.282
surface_form: scoat fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.490038888889
lon: -3.2998
Scoat Fell occupies an important position at the crossroads of five ridges. To the east, across the subsidiary top of Black Crag, is Pillar. Southward is a long descending ridge heading toward the shore of Wastwater. The high point is Red Pike, before the terminal height of Yewbarrow. The main watershed continues west to Haycock, while two short spurs jut north into Ennerdale.

Geographic entities mentioned:
surface_form: Yewbarrow
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.464211111111
lon: -3.2773805555556
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.526
lon: -3.3
Southward is a long descending ridge heading toward the shore of Wastwater. The high point is Red Pike, before the terminal height of Yewbarrow. The main watershed continues west to Haycock, while two short spurs jut north into Ennerdale. These are Tewit How which descends from the western end of the plateau and Steeple, running from the summit.

Geographic entities mentioned:
surface_form: haycock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4844
lon: -3.32278
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Finally Nether Beck Bridge on the shore of Wastwater provides access via Scoat Tarn onto the southern flanks. From the upper recesses of Nether Beck the walker can aim for either of the cols which connect the objective to Red Pike or Haycock. Perhaps the greatest number of visitors will cross the top as part of the Mosedale Horseshoe, also climbing Red Pike and Pillar.

Geographic entities mentioned:
surface_form: haycock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4844
lon: -3.32278
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.526
lon: -3.3
As the radial point of so many ridges Scoat Fell forms the head of several valleys, the major ones being the Wasdale feeders of Mosedale and Nether Beck. Mosedale begins on the eastern flanks of Scoat Fell, between Red Pike and Pillar, in the hollow of Black Comb. There are crags in the headwall, particularly to the south.

Geographic entities mentioned:
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
surface_form: pillar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.497
lon: -3.282
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.526
lon: -3.3
surface_form: scoat fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.490038888889
lon: -3.2998
Finally Nether Beck Bridge on the shore of Wastwater provides access via Scoat Tarn onto the southern flanks. From the upper recesses of Nether Beck the walker can aim for either of the cols which connect the objective to Red Pike or Haycock. Perhaps the greatest number of visitors will cross the top as part of the Mosedale Horseshoe, also climbing Red Pike and Pillar.

Geographic entities mentioned:
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
surface_form: pillar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.497
lon: -3.282
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.526
lon: -3.3
Finally Mirklin Cove is the corrie between Steeple and Tewit How, drained into Ennerdale by Low Beck. All of the northern coves are home to impressive crags. Of Scoat Fell's various satellites, Little Scoat Fell and Black Fell are generally considered to be a part of the parent fell, while Steeple, despite its clearly derivative position, is counted as a separate fell.

Geographic entities mentioned:
surface_form: black fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4056
lon: -3.01673
surface_form: steeple
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493
lon: -3.302
surface_form: scoat fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.490038888889
lon: -3.2998
surface_form: scoat fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.490038888889
lon: -3.2998
surface_form: black fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.7932
lon: -2.54897
Geology. Successive rock strata are displayed along the descending ridge of Tewit How to the north west, displaying the architecture of the fell. At the top is the plagioclase-phyric andesite lava of the Birker Fell Formation, followed by the siltstone, sandstone, conglomerate, tuff and lapilli tuff of the Eagle Crag Member.

Geographic entities mentioned:
surface_form: eagle crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.499
lon: -3.12097
The principal fells in this section are Kirk Fell, Pillar, Scoat Fell, Haycock and Caw Fell, followed by the lower Lank Rigg group. Scoat Fell occupies an important position at the crossroads of five ridges. To the east, across the subsidiary top of Black Crag, is Pillar. Southward is a long descending ridge heading toward the shore of Wastwater.

Geographic entities mentioned:
surface_form: pillar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.497
lon: -3.282
Nether Beck has its birth at Scoat Tarn, a large pool to the south of the fell. This corrie tarn, held in place by grassy moraines is around 65 ft deep. Between Steeple and Pillar to the north is Windgap Cove with Black Crag, a Hewitt at its head. Wind Gap is the col between Black Crag and Pillar, while the small Mirk Cove lies between Black Crag and the summit.

Geographic entities mentioned:
surface_form: pillar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.497
lon: -3.282
surface_form: steeple
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493
lon: -3.302
This corrie tarn, held in place by grassy moraines is around 65 ft deep. Between Steeple and Pillar to the north is Windgap Cove with Black Crag, a Hewitt at its head. Wind Gap is the col between Black Crag and Pillar, while the small Mirk Cove lies between Black Crag and the summit. Finally Mirklin Cove is the corrie between Steeple and Tewit How, drained into Ennerdale by Low Beck.

Geographic entities mentioned:
surface_form: pillar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.497
lon: -3.282
These names are based on area rather than height, Great Scoat Fell being lower. Pillar reduces the field of view, without showing its better side, but almost the full horseshoe of the Western Fells can be seen. The wall makes it difficult to observe the full panorama from one point. Ascents.

Geographic entities mentioned:
surface_form: pillar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.497
lon: -3.282
These are Tewit How which descends from the western end of the plateau and Steeple, running from the summit. As the radial point of so many ridges Scoat Fell forms the head of several valleys, the major ones being the Wasdale feeders of Mosedale and Nether Beck. Mosedale begins on the eastern flanks of Scoat Fell, between Red Pike and Pillar, in the hollow of Black Comb.

Geographic entities mentioned:
surface_form: wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: scoat fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.490038888889
lon: -3.2998
Ascents. From Ennerdale many walkers will ascend indirectly via Steeple, but the ridge of Tewit How can also be used. Wasdale Head can be used as a base, first walking up Mosedale and then climbing up to the ridge via Black Comb. Finally Nether Beck Bridge on the shore of Wastwater provides access via Scoat Tarn onto the southern flanks.

Geographic entities mentioned:
surface_form: wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
Scoat Fell occupies an important position at the crossroads of five ridges. To the east, across the subsidiary top of Black Crag, is Pillar. Southward is a long descending ridge heading toward the shore of Wastwater. The high point is Red Pike, before the terminal height of Yewbarrow. The main watershed continues west to Haycock, while two short spurs jut north into Ennerdale.

Geographic entities mentioned:
surface_form: wastwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
Wasdale Head can be used as a base, first walking up Mosedale and then climbing up to the ridge via Black Comb. Finally Nether Beck Bridge on the shore of Wastwater provides access via Scoat Tarn onto the southern flanks. From the upper recesses of Nether Beck the walker can aim for either of the cols which connect the objective to Red Pike or Haycock.

Geographic entities mentioned:
surface_form: wastwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
The main watershed continues west to Haycock, while two short spurs jut north into Ennerdale. These are Tewit How which descends from the western end of the plateau and Steeple, running from the summit. As the radial point of so many ridges Scoat Fell forms the head of several valleys, the major ones being the Wasdale feeders of Mosedale and Nether Beck.

Geographic entities mentioned:
surface_form: steeple
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493
lon: -3.302
Between Steeple and Pillar to the north is Windgap Cove with Black Crag, a Hewitt at its head. Wind Gap is the col between Black Crag and Pillar, while the small Mirk Cove lies between Black Crag and the summit. Finally Mirklin Cove is the corrie between Steeple and Tewit How, drained into Ennerdale by Low Beck. All of the northern coves are home to impressive crags.

Geographic entities mentioned:
surface_form: steeple
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493
lon: -3.302
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Summit. The top is a long plateau, running broadly east to west. Along it runs the stone wall of the Ennerdale fence, crossing the summit exactly. Purists have built a small cairn atop the wall, although a larger edifice lies just to the north, pointing the way to Steeple. The whole area is stony, with fine views into the northern coves.

Geographic entities mentioned:
surface_form: steeple
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493
lon: -3.302
The wall makes it difficult to observe the full panorama from one point. Ascents. From Ennerdale many walkers will ascend indirectly via Steeple, but the ridge of Tewit How can also be used. Wasdale Head can be used as a base, first walking up Mosedale and then climbing up to the ridge via Black Comb.

Geographic entities mentioned:
surface_form: steeple
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.493
lon: -3.302
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Scoat Fell. Scoat Fell is a fell in the western part of the English Lake District. It stands at the head of the Mosedale Horseshoe with its back to Ennerdale. Paths lead to Scoat Fell from Ennerdale over Steeple, from Wasdale over Red Pike, and along the ridge from Pillar. Topography.

Geographic entities mentioned:
surface_form: scoat fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.490038888889
lon: -3.2998
At the central hub of the high country are Great Gable and its satellites, while two principal ridges fan out on either flank of Ennerdale, the western fells in effect being a great horseshoe around this long wild valley. Scoat Fell is on the southern arm. The main watershed runs broadly westwards from Great Gable, dividing the headwaters of Ennerdale and Wasdale.

Geographic entities mentioned:
surface_form: scoat fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.490038888889
lon: -3.2998
The main watershed runs broadly westwards from Great Gable, dividing the headwaters of Ennerdale and Wasdale. The principal fells in this section are Kirk Fell, Pillar, Scoat Fell, Haycock and Caw Fell, followed by the lower Lank Rigg group. Scoat Fell occupies an important position at the crossroads of five ridges. To the east, across the subsidiary top of Black Crag, is Pillar.

Geographic entities mentioned:
surface_form: scoat fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.490038888889
lon: -3.2998
The whole area is stony, with fine views into the northern coves. Ordnance Survey maps label the summit as Little Scoat Fell and a small hillock at the western end of the plateau as Great Scoat Fell. These names are based on area rather than height, Great Scoat Fell being lower.

Geographic entities mentioned:
surface_form: scoat fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.490038888889
lon: -3.2998
surface_form: scoat fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.490038888889
lon: -3.2998
Ordnance Survey maps label the summit as Little Scoat Fell and a small hillock at the western end of the plateau as Great Scoat Fell. These names are based on area rather than height, Great Scoat Fell being lower. Pillar reduces the field of view, without showing its better side, but almost the full horseshoe of the Western Fells can be seen.

Geographic entities mentioned:
surface_form: scoat fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.490038888889
lon: -3.2998
Scoat Fell. Scoat Fell is a fell in the western part of the English Lake District. It stands at the head of the Mosedale Horseshoe with its back to Ennerdale. Paths lead to Scoat Fell from Ennerdale over Steeple, from Wasdale over Red Pike, and along the ridge from Pillar. Topography.

Geographic entities mentioned:
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Of Scoat Fell's various satellites, Little Scoat Fell and Black Fell are generally considered to be a part of the parent fell, while Steeple, despite its clearly derivative position, is counted as a separate fell. This is due to its impressive appearance from Ennerdale rather than any great relative height, a triumph of the emotions over logic. Geology.

Geographic entities mentioned:
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
At the top is the plagioclase-phyric andesite lava of the Birker Fell Formation, followed by the siltstone, sandstone, conglomerate, tuff and lapilli tuff of the Eagle Crag Member. Further outcrops of the Birker Fell Formation are followed by a band of dacite before the igneous rocks of the Ennerdale Intrusion complete the picture. Summit. The top is a long plateau, running broadly east to west.

Geographic entities mentioned:
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Summit. The top is a long plateau, running broadly east to west. Along it runs the stone wall of the Ennerdale fence, crossing the summit exactly. Purists have built a small cairn atop the wall, although a larger edifice lies just to the north, pointing the way to Steeple. The whole area is stony, with fine views into the northern coves.

Geographic entities mentioned:
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
When they reached Fort Hall, near present-day Pocatello, Idaho, Thornton's party met Jesse Applegate, Lindsay Applegate, David Goff, and Levi Scott, who were authorized by the Provisional Government of Oregon to survey a new route to the Willamette Valley that would avoid the Columbia River.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Especially interesting is the findings after early description of iron. The oldest historical documentation in the area consist of runic stones and a very rare stone carving dated to 970 CE. It is rare because such carvings usually do not appear north of lake Mälaren. Gästriklands only ancient castle is located in Hedesunda.

Geographic entities mentioned:
surface_form: Mälaren
instance_of: Lake
countries: Sweden
coordinates: lat: 59.5
lon: 17.2
Kellerberg (Forchheim). Kellerberg (Forchheim) is a mountain of Bavaria, Germany.

Geographic entities mentioned:
surface_form: kellerberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.8944
lon: 6.761
surface_form: kellerberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.7296
lon: 11.075
A by-election for the seat was held on February 14, 2018. Under the 2021 redistribution that took effect with the 2024 general election the riding was divided, with portions on the west side of Okanagan Lake being redistributed to the new district of West Kelowna-Peachland and portions east of Okanagan Lake in the city of Kelowna transferring to the new district of Kelowna Centre. Geography.

Geographic entities mentioned:
surface_form: Okanagan Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.920833333333
lon: -119.5
Distribution and habitat. The song thrush breeds in most of Europe (although not in the greater part of Iberia, lowland Italy or southern Greece), and across Ukraine and Russia almost to Lake Baikal. It reaches to 75°N in Norway, but only to about 60°N in Siberia.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Tour de France. On July 14, 2014, the Tour de France cycle race crossed the col for the first time en route from Mulhouse to La Planche des Belles Filles. When announcing the route, Christian Prudhomme explained his reasons for deciding to send the 2014 Tour over passes not used previously: &quot;I like to use the other massifs than the usual Alps and Pyrenees.

Geographic entities mentioned:
surface_form: La Planche des Belles Filles
instance_of: Mountain
countries: France
coordinates: lat: 47.7672
lon: 6.77417
In Dalag. In Dalag (also written I-n-Daladj) is a village in the commune of Tamanrasset, in Tamanrasset District, Tamanrasset Province, Algeria. It lies on the west bank of Oued i-n-Daladj in the Hoggar Mountains, east of Tamanrasset city.

Geographic entities mentioned:
surface_form: Hoggar Mountains
instance_of: Plateau
countries: Algeria
France
coordinates: lat: 23.288611
lon: 5.534167
Consolação Street. Consolação Street (Portuguese: &quot;Rua da Consolação&quot;) is an important thoroughfare in the Brazilian city of São Paulo. It begins in the central area of the city, near the Anhangabaú Valley, and ends at Estados Unidos Street, in the Jardins district. It has three different stretches.

Geographic entities mentioned:
surface_form: Anhangabaú Valley
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
Kopa is used for fishery. Location and description. Lake Kopa is located in the north of Kazakhstan. Lake Kopa is long, up to wide and its area is. The lake lies near the foot of the Kokshetau Massif, and near the north-western part of the city of Kokshetau. Lake Zholdybay lies about to the WNW. Lake Kopa has an area of and an average depth of.

Geographic entities mentioned:
surface_form: Zholdybay
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 53.3969444
lon: 68.9663889
The lake bottom is viscous, smooth, and covered with a layer of silt clay, loam, and sand, it averages, but can reach a depth of as much as in the northern part. 50–70 m-high hills (Bukpa Hill) come close to the lake from south-west. In 1955, the volume of water in the lake was, with a surface area of. From 1955 to 1990 the volume of the lake has decreased by and now stands at only.

Geographic entities mentioned:
surface_form: Bukpa Hill
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 53.27194444444444
lon: 69.33055555555555
Lake Kopa. Lake Kopa (,;) is a lake in the city of Kokshetau, located on the territory of Akmola Region close to the foot of Kokshetau Elevation in the northern part of Kazakhstan. Its elevation is above sea level and has a maximum depth of about 6 m. It is 5.6 km long and 12 km wide. The total surface area of it the lake is about depending on water level.

Geographic entities mentioned:
surface_form: lake kopa
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 53.3
lon: 69.35
surface_form: kopa
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 53.3
lon: 69.35
It is 5.6 km long and 12 km wide. The total surface area of it the lake is about depending on water level. It is fed by 2 rivers and is drained by the Shagalaly. The area of Lake Kopa fluctuates year to year, but in recent years the size of the lake has been decreasing overall. Kopa is used for fishery. Location and description. Lake Kopa is located in the north of Kazakhstan.

Geographic entities mentioned:
surface_form: lake kopa
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 53.3
lon: 69.35
surface_form: kopa
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 53.3
lon: 69.35
The area of Lake Kopa fluctuates year to year, but in recent years the size of the lake has been decreasing overall. Kopa is used for fishery. Location and description. Lake Kopa is located in the north of Kazakhstan. Lake Kopa is long, up to wide and its area is. The lake lies near the foot of the Kokshetau Massif, and near the north-western part of the city of Kokshetau.

Geographic entities mentioned:
surface_form: lake kopa
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 53.3
lon: 69.35
surface_form: kopa
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 53.3
lon: 69.35
Kopa is used for fishery. Location and description. Lake Kopa is located in the north of Kazakhstan. Lake Kopa is long, up to wide and its area is. The lake lies near the foot of the Kokshetau Massif, and near the north-western part of the city of Kokshetau. Lake Zholdybay lies about to the WNW. Lake Kopa has an area of and an average depth of.

Geographic entities mentioned:
surface_form: lake kopa
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 53.3
lon: 69.35
surface_form: kopa
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 53.3
lon: 69.35
The lake lies near the foot of the Kokshetau Massif, and near the north-western part of the city of Kokshetau. Lake Zholdybay lies about to the WNW. Lake Kopa has an area of and an average depth of. Most of the total catchment area of, is accounted for by the tributaries of the lake: the Shagalaly river to the southwest, and the Kylshakty river to southeast.

Geographic entities mentioned:
surface_form: lake kopa
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 53.3
lon: 69.35
surface_form: kopa
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 53.3
lon: 69.35
From 1955 to 1990 the volume of the lake has decreased by and now stands at only. The lake sees amplitude fluctuations of between. Shagalaly flows into the lake from south-west and flows out from the north part, therefore, Lake Kopa regulates flow of Shagalaly river in its lower stream. Administratively, the lake and the adjacent land are within Akmola Region of Kazakhstan.

Geographic entities mentioned:
surface_form: lake kopa
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 53.3
lon: 69.35
surface_form: kopa
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 53.3
lon: 69.35
The total surface area of it the lake is about depending on water level. It is fed by 2 rivers and is drained by the Shagalaly. The area of Lake Kopa fluctuates year to year, but in recent years the size of the lake has been decreasing overall. Kopa is used for fishery. Location and description. Lake Kopa is located in the north of Kazakhstan. Lake Kopa is long, up to wide and its area is.

Geographic entities mentioned:
surface_form: kopa
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 53.3
lon: 69.35
It is situated eight miles west-northwest of Grand Canyon Village, and immediately northeast of Mimbreno Point. Marsh Butte is one mile northeast, Eremita Mesa immediately southeast, and nearest higher neighbor Diana Temple is one mile north. Topographic relief is significant as Vesta Temple rises above the Colorado River in 2.5 miles.

Geographic entities mentioned:
surface_form: Marsh Butte
instance_of: Mountain
countries: United States
coordinates: lat: 36.12054
lon: -112.24517
Vesta Temple. Vesta Temple is a summit located in the Grand Canyon, in Coconino County of northern Arizona, US. It is situated eight miles west-northwest of Grand Canyon Village, and immediately northeast of Mimbreno Point. Marsh Butte is one mile northeast, Eremita Mesa immediately southeast, and nearest higher neighbor Diana Temple is one mile north.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
surface_form: vesta temple
instance_of: Mountain
countries: United States
coordinates: lat: 36.09359
lon: -112.26878
Vesta Temple. Vesta Temple is a summit located in the Grand Canyon, in Coconino County of northern Arizona, US. It is situated eight miles west-northwest of Grand Canyon Village, and immediately northeast of Mimbreno Point. Marsh Butte is one mile northeast, Eremita Mesa immediately southeast, and nearest higher neighbor Diana Temple is one mile north.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
Topographic relief is significant as Vesta Temple rises above the Colorado River in 2.5 miles. Vesta Temple is named for Vesta, the goddess of the hearth, home, and family according to Roman mythology. Clarence Dutton began the practice of naming geographical features in the Grand Canyon after mythological deities. This geographical feature's toponym was officially adopted in 1908 by the U.S.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
Geology. The summit of Vesta Temple is composed of Permian Kaibab Limestone and Toroweap Formation overlaying cream-colored, cliff-forming, Permian Coconino Sandstone. The sandstone, which is the third-youngest of the strata in the Grand Canyon, was deposited 265 million years ago as sand dunes.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
Vesta Temple. Vesta Temple is a summit located in the Grand Canyon, in Coconino County of northern Arizona, US. It is situated eight miles west-northwest of Grand Canyon Village, and immediately northeast of Mimbreno Point. Marsh Butte is one mile northeast, Eremita Mesa immediately southeast, and nearest higher neighbor Diana Temple is one mile north.

Geographic entities mentioned:
surface_form: vesta temple
instance_of: Mountain
countries: United States
coordinates: lat: 36.09359
lon: -112.26878
Marsh Butte is one mile northeast, Eremita Mesa immediately southeast, and nearest higher neighbor Diana Temple is one mile north. Topographic relief is significant as Vesta Temple rises above the Colorado River in 2.5 miles. Vesta Temple is named for Vesta, the goddess of the hearth, home, and family according to Roman mythology.

Geographic entities mentioned:
surface_form: vesta temple
instance_of: Mountain
countries: United States
coordinates: lat: 36.09359
lon: -112.26878
Topographic relief is significant as Vesta Temple rises above the Colorado River in 2.5 miles. Vesta Temple is named for Vesta, the goddess of the hearth, home, and family according to Roman mythology. Clarence Dutton began the practice of naming geographical features in the Grand Canyon after mythological deities. This geographical feature's toponym was officially adopted in 1908 by the U.S.

Geographic entities mentioned:
surface_form: vesta temple
instance_of: Mountain
countries: United States
coordinates: lat: 36.09359
lon: -112.26878
This geographical feature's toponym was officially adopted in 1908 by the U.S. Board on Geographic Names. According to the Köppen climate classification system, Vesta Temple is located in a Cold semi-arid climate zone. Geology. The summit of Vesta Temple is composed of Permian Kaibab Limestone and Toroweap Formation overlaying cream-colored, cliff-forming, Permian Coconino Sandstone.

Geographic entities mentioned:
surface_form: vesta temple
instance_of: Mountain
countries: United States
coordinates: lat: 36.09359
lon: -112.26878
Geology. The summit of Vesta Temple is composed of Permian Kaibab Limestone and Toroweap Formation overlaying cream-colored, cliff-forming, Permian Coconino Sandstone. The sandstone, which is the third-youngest of the strata in the Grand Canyon, was deposited 265 million years ago as sand dunes.

Geographic entities mentioned:
surface_form: vesta temple
instance_of: Mountain
countries: United States
coordinates: lat: 36.09359
lon: -112.26878
Further down are strata of the conspicuous cliff-forming Mississippian Redwall Limestone, the Cambrian Tonto Group, and finally granite of the Paleoproterozoic Vishnu Basement Rocks at river level in Granite Gorge. Precipitation runoff from Vesta Temple drains northeast to the Colorado River via Topaz Canyon and Boucher Creek.

Geographic entities mentioned:
surface_form: vesta temple
instance_of: Mountain
countries: United States
coordinates: lat: 36.09359
lon: -112.26878
The point is named for Bulgarian educator Nedelya Petkova (1826–1894). Location. Nedelya Point is located at, which is 1.8 km southwest of Bilyar Point, 5.37 km west-northwest of Rotch Dome, 1.58 km northeast of Sparadok Point and 2.86 km east of Lair Point. British mapping was done in 1968, Chilean in 1971, Argentine in 1980, Spanish in 1993 and Bulgarian in 2005, 2009 and 2017.

Geographic entities mentioned:
surface_form: Rotch Dome
instance_of: Mountain
coordinates: lat: -62.6333
lon: -60.8831
According to the United States Census Bureau, the village has a total area of, of which is land and is water. The East Fork of the Black River enters the village from the north and turns back north to empty into Lake Erie, as Lodi is on the north–south continental divide. Rain water runs off in either a northerly direction to Lake Erie or a southernly direction to the Ohio River. 2010 census.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Twin towns — Sister cities. Since 2011 Tryavna is a member of the Douzelage, a unique town twinning association of 27 towns across the European Union. Since 1994 Tryavna is also twinned with Brienz, Switzerland. Honour. Tryavna Peak on Livingston Island in the South Shetland Islands, Antarctica is named after Tryavna.

Geographic entities mentioned:
surface_form: Tryavna Peak
instance_of: Mountain
coordinates: lat: -62.622444444444
lon: -59.845277777778
The station was a changeover from train to steam ship. It was eventually closed along with the Røykenvik Line. The name. The station is named after a nearby inlet in Randsfjorden. The first element is the name of the old farm Røyken (Norse &quot;Raukvin&quot;), the last element is &quot;vik&quot; 'inlet, cove'. For the meaning of the farm name see Røyken.

Geographic entities mentioned:
surface_form: Randsfjorden
instance_of: Lake
countries: Norway
coordinates: lat: 60.390277777778
lon: 10.394166666667
Prace, Czech Republic. Prace () is a municipality and village in Brno-Country District in the South Moravian Region of the Czech Republic. It has about 1,000 inhabitants. Geography. Prace is located about southeast of Brno. It lies in the Dyje–Svratka Valley. The highest point is the hill Pracký kopec at above sea level. History. The first written mention of Prace is from 1274.

Geographic entities mentioned:
surface_form: Dyje–Svratka Valley
instance_of: Valley
countries: Czech Republic
coordinates: lat: 49
lon: 16.5
The city was conferred the status of &quot;City of Military Glory&quot; by President Medvedev on October 28, 2008, for &quot;courage, endurance and mass heroism, exhibited by defenders of the city in the struggle for the freedom and independence of the Motherland&quot;. See also: Perimilovsky Heights. Kalach-na-Donu.

Geographic entities mentioned:
surface_form: Perimilovsky Heights
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.2977
lon: 37.501
Saline Valley Hot Springs. Saline Valley Hot Springs are a series of three thermal springs located in the remote Saline Valley area of Death Valley National Park. Description. Each of the three main springs have several primitive soaking pools constructed from local rock, concrete and tile. Locals from the area constructed nearby showers, and a dishwashing station for visitors.

Geographic entities mentioned:
surface_form: Saline Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.75
lon: -117.81
Allen Lake (New York). Allen Lake is a lake located southeast of the Village of Richfield Springs in northern Otsego County, New York. It is a natural lake, but a low earthen dam and concrete spillway were installed to raise the lake level. The main outflow is Trout Brook, also known as White Creek, which flows into Otsego Lake. Allen Lake is the water supply for Richfield Springs. History.

Geographic entities mentioned:
surface_form: allen lake
instance_of: Lake
countries: United States
coordinates: lat: 42.83
lon: -74.952
It is a natural lake, but a low earthen dam and concrete spillway were installed to raise the lake level. The main outflow is Trout Brook, also known as White Creek, which flows into Otsego Lake. Allen Lake is the water supply for Richfield Springs. History. By 1820, fresh water was being shipped in to the Village of Richfield Springs from Weatherby Pond to the north.

Geographic entities mentioned:
surface_form: allen lake
instance_of: Lake
countries: United States
coordinates: lat: 42.83
lon: -74.952
As the village grew, it required a steadier supply of fresh water. At first water came from the two holding reservoirs along US Route 20 east of Richfield Springs. This was still not enough water, and Allen Lake was purchased by the village. At first a steam pump pumped the water above ground but later it was buried and tunnelled through the divide so it could be gravity fed.

Geographic entities mentioned:
surface_form: allen lake
instance_of: Lake
countries: United States
coordinates: lat: 42.83
lon: -74.952
Lower reservoirs. There are two small reservoirs located directly east of the village along US 20. The upper reservoir, at an elevation of, is used to hold most of the water coming through the pipe from Allen Lake. It is kept full by throttling a manual valve on a branch line coming off the main line from Allen Lake.

Geographic entities mentioned:
surface_form: allen lake
instance_of: Lake
countries: United States
coordinates: lat: 42.83
lon: -74.952
There are two small reservoirs located directly east of the village along US 20. The upper reservoir, at an elevation of, is used to hold most of the water coming through the pipe from Allen Lake. It is kept full by throttling a manual valve on a branch line coming off the main line from Allen Lake. The water travels through the aerial fountain on the upper reservoir to aerate the raw water.

Geographic entities mentioned:
surface_form: allen lake
instance_of: Lake
countries: United States
coordinates: lat: 42.83
lon: -74.952