Sarmila/GeoWiki-Features huggingface dataset:
Llyn Eiddwen. Llyn Eiddwen () is a lake and site of special scientific interest near Trefenter in Ceredigion, Wales. It is the source of the River Aeron. This natural lake provides an environment to preserve rare local water-plant life and seasonal animals. It is owned and managed by the Wildlife Trust of South and West Wales.

Geographic entities mentioned:
surface_form: llyn eiddwen
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.283
lon: -4.044
Surrounded by sheep-grazed common land, it is part of a national nature reserve. Visitors come on foot from the north or on bridleways from the south. Remote and peaceful, Llyn Eiddwen National Nature Reserve lies in the gentle slopes of Mynydd Bach, to the north west of Tregaron town in Ceredigion. The wet and quiet nature of its habitats suits shy creatures such as water voles and otters.

Geographic entities mentioned:
surface_form: llyn eiddwen
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.283
lon: -4.044
Remote and peaceful, Llyn Eiddwen National Nature Reserve lies in the gentle slopes of Mynydd Bach, to the north west of Tregaron town in Ceredigion. The wet and quiet nature of its habitats suits shy creatures such as water voles and otters. A climb to the summit of the surrounding hills reveals views of Cardigan Bay to the west, and of the Pumlumon and Elenydd uplands to the north and east.

Geographic entities mentioned:
surface_form: pumlumon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.4675
lon: -3.7828
Cahuilla Hills, California. Cahuilla Hills is an unincorporated community in the Coachella Valley of Riverside County, California. It lies at an elevation of 932 feet (284 m) in the foothills of the Santa Rosa Mountains. Cahuilla Hills is located southwest of the civic center of Palm Desert.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
The mountain is surrounded by several other notable mountains including Storjuvtinden, Svellnosbreahesten, Store Tverråtinden, and Midtre Tverråtinden to the northeast; Sauhøi to the west; Bukkeholstindene and Tverrbottindene to the southwest; Store Styggehøe and Bukkeholshøe to the southeast; and Lindbergtinden to the east. Name.

Geographic entities mentioned:
surface_form: Storjuvtinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.630277777778
lon: 8.2936111111111
surface_form: Svellnosbreahesten
instance_of: Mountain
countries: Norway
coordinates: lat: 61.6214
lon: 8.3075
surface_form: Store Tverråtinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.615277777778
lon: 8.3019444444444
surface_form: Midtre Tverråtinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.614444444444
lon: 8.3152777777778
surface_form: Sauhøi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.60122
lon: 8.20591
surface_form: Tverrbottindene
instance_of: Mountain
countries: Norway
coordinates: lat: 61.57553
lon: 8.25538
surface_form: Store Styggehøe
instance_of: Mountain
countries: Norway
coordinates: lat: 61.5911
lon: 8.33722
surface_form: Lindbergtinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.604336
lon: 8.280225
surface_form: bukkeholshøe
instance_of: Mountain
countries: Norway
coordinates: lat: 61.57972222
lon: 8.35583333
surface_form: tverråtinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.6142
lon: 8.30139
surface_form: tverråtinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.6142
lon: 8.30139
surface_form: styggehøe
instance_of: Mountain
countries: Norway
coordinates: lat: 61.5911
lon: 8.33722
surface_form: styggehøe
instance_of: Mountain
countries: Norway
coordinates: lat: 61.58853
lon: 8.61946
surface_form: styggehøe
instance_of: Mountain
countries: Norway
coordinates: lat: 61.46639
lon: 8.92042
Bukkehøe. Bukkehøe or Bukkehøi is a mountain in Lom Municipality in Innlandet county, Norway. The tall mountain is located in the Jotunheimen mountains within Jotunheimen National Park. The mountain sits about southwest of the village of Fossbergom and about northeast of the village of Øvre Årdal.

Geographic entities mentioned:
surface_form: bukkehøi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.604166666667
lon: 8.2661111111111
surface_form: bukkehøe
instance_of: Mountain
countries: Norway
coordinates: lat: 61.604166666667
lon: 8.2661111111111
Bukkehøe. Bukkehøe or Bukkehøi is a mountain in Lom Municipality in Innlandet county, Norway. The tall mountain is located in the Jotunheimen mountains within Jotunheimen National Park. The mountain sits about southwest of the village of Fossbergom and about northeast of the village of Øvre Årdal.

Geographic entities mentioned:
surface_form: bukkehøe
instance_of: Mountain
countries: Norway
coordinates: lat: 61.604166666667
lon: 8.2661111111111
Background. Wayanad is at risk of landslides during monsoon seasons. Located in the Western Ghats mountain range, its hills consist of faulted and eroded mountain edges of the Deccan Plateau. Geological evidence suggests that this region was shaped during the breakup of the supercontinent Gondwana.

Geographic entities mentioned:
surface_form: Deccan Plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
1761), but the reinforcement only raised the squadron to seven small line-of-battle ships. War being now in progress between France and England the French sent a naval force from their islands in the Indian Ocean into the Bay of Bengal to the assistance of Pondicherry. To intercept the arrival of these reinforcements for the enemy now became the object of Pocock.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
After the Partition of India, Niyogi moved to Silchar permanently. Martyrdom. As the Bengali Language Movement gained momentum in the Barak Valley, Niyogi was drawn into it. In spite of being a railway official, he took part in the Satyagraha on 19 May 1961. The primary agenda of the satyagrahis was a rail blockade at Tarapur railway station demanding the official status of Bengali in Assam.

Geographic entities mentioned:
surface_form: Barak Valley
instance_of: Valley
countries: India
coordinates: lat: 24.833333333333332
lon: 92.8
Alana's paternal grandmother was originally from Bulgaria. She has two older sisters, Este (born 1986) and Danielle (born 1989). Alana was raised in the San Fernando Valley in a musical family. Her father was a drummer in a choir group; her mother was a folk singer, and a winning contestant on &quot;The Gong Show&quot; in the 1970s.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Multan is located near the Sulaiman Mountain Range which is the extension of the southern Hindu Kush of Pakistan and Afghanistan. The most well-known peak of the Sulaiman mountains is the twin-peaked Takht-e-Sulaiman or &quot;Throne of Prophet Solomon&quot; at 3,487 metres (11,440 ft). Climate.

Geographic entities mentioned:
surface_form: Takht-e-Sulaiman
instance_of: Mountain
countries: Pakistan
coordinates: lat: 31.682683333333
lon: 69.936566666667
The peak, complete with a cairn at, is the high point of the moorland. Redmonds Edge links Spitlers Edge to Great Hill and is paved. As of 2017, there are plans to extend the paving along the length of Spitlers Edge - with funding secured from the Lancashire Environmental Fund and United Utilities.

Geographic entities mentioned:
surface_form: Great Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.667169444444
lon: -2.53725
Baia, Tulcea. Baia is a commune in Tulcea County, Northern Dobruja, Romania. History. In 1953, archaeological excavations on a site along the Lake Golovița, near Baia, led to the discovery of a new Middle Neolithic culture, named after the commune. Further research has shown that the culture, with Mediterranean origins, extended across Dobruja and North-Eastern Bulgaria.

Geographic entities mentioned:
surface_form: Lake Golovița
instance_of: Lake
countries: Romania
coordinates: lat: 44.71416667
lon: 28.77666667
With the exception of the Mackenzie River, Canada's longest river, this watershed has been little used for hydroelectricity. The Peace and Athabasca rivers, along with Great Bear and Great Slave Lake (respectively the largest and second largest lakes wholly enclosed within Canada), are significant elements of the Arctic watershed.

Geographic entities mentioned:
surface_form: Great Bear
instance_of: Lake
countries: Canada
coordinates: lat: 66
lon: -121
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
Geography and environment. The growth of the National Park led to an increase in tourism in the region. In particular, Backbarrow has great views of the turbulent nature of the River Leven, just south of Windermere. The river has also been used to develop a small hydro-electric plant, installed in 2000, generating electricity for the National Grid.

Geographic entities mentioned:
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
Vase Rock. Vase Rock is a rock just off Liuqiu Island of Pingtung County, Taiwan. Geology. The rock was formed by the rising of the coastal coral reef. Its lower part has been eroded by the sea thus forming a vase-shaped structure. Its highest point stands at a height of. Legacy.

Geographic entities mentioned:
surface_form: vase rock
instance_of: Mountain
countries: Taiwan
coordinates: lat: 22.35566667
lon: 120.38075
Legacy. The Liuqiu township's tourism department ascribes the island's former name &quot;Golden Lion Island&quot; to Vase Rock's supposed resemblance to a lion's head, although the name actually honors the slaughtered crew of the Dutch ship ', the punitive reprisals for whichparticularly the Liuqiu Island Massacredepopulated the island in the 1630s and 1640s.

Geographic entities mentioned:
surface_form: vase rock
instance_of: Mountain
countries: Taiwan
coordinates: lat: 22.35566667
lon: 120.38075
Much of the animosity between the two men can be traced back to Byron's belief that Southey had spread rumours about him and Percy Bysshe Shelley being in a &quot;League of Incest&quot; during their time on Lake Geneva in 1816, an accusation that Southey strenuously denied.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Crag Fell. Crag Fell is a hill in the English Lake District. It is part of the Lank Rigg group, standing above Ennerdale Water in the Western Fells. The craggy northern face above the lake gives the fell its name, prominent in views from the car park at Bowness Knott. Ascents are commonly made from the foot of Ennerdale Water. Topography.

Geographic entities mentioned:
surface_form: Lank Rigg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.494
lon: -3.403
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Ascents are commonly made from the foot of Ennerdale Water. 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. Crag Fell stands near the extremity of 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
Crag Fell stands near the extremity of the southern arm. The main watershed runs broadly westwards from Great Gable, dividing the headwaters of Ennerdale and Wasdale. The fells in this section are Kirk Fell, Pillar, Scoat Fell, Haycock and Caw Fell. The surrounding valleys gradually diverge until other rivers spring up to drain the intervening country.

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
Crag Fell stands near the extremity of the southern arm. The main watershed runs broadly westwards from Great Gable, dividing the headwaters of Ennerdale and Wasdale. The fells in this section are Kirk Fell, Pillar, Scoat Fell, Haycock and Caw Fell. The surrounding valleys gradually diverge until other rivers spring up to drain the intervening country.

Geographic entities mentioned:
surface_form: Kirk Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.242
surface_form: Scoat Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.490038888889
lon: -3.2998
surface_form: Caw Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.486
lon: -3.343
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
Worm Gill is one such watercourse, running south westward from Caw Fell, and forcing the ridge to detour northwards around the head of its valley. Beyond this stand the fells of the Lank Rigg group, the final high country within the National Park. Crag Fell and Grike complete the westward line of the ridge, whilst Lank Rigg lies to the south across the head of the River Calder.

Geographic entities mentioned:
surface_form: Lank Rigg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.494
lon: -3.403
There is a wide panorama to seaward, taking in what Alfred Wainwright described as the &quot;grotesque collection of towers and minarets of the Calder Hall atomic power station&quot;. The head of Ennerdale Water is seen to the east, surrounded by the high cirque of the Western Fells. Distant Fairfield and Ullscarf put in unexpected appearances through the gaps. Ascents.

Geographic entities mentioned:
surface_form: Ullscarf
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.500161111111
lon: -3.09475
surface_form: ullscarf
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.500161111111
lon: -3.09475
Crag Fell. Crag Fell is a hill in the English Lake District. It is part of the Lank Rigg group, standing above Ennerdale Water in the Western Fells. The craggy northern face above the lake gives the fell its name, prominent in views from the car park at Bowness Knott. Ascents are commonly made from the foot of Ennerdale Water. Topography.

Geographic entities mentioned:
surface_form: knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
There is a wide panorama to seaward, taking in what Alfred Wainwright described as the &quot;grotesque collection of towers and minarets of the Calder Hall atomic power station&quot;. The head of Ennerdale Water is seen to the east, surrounded by the high cirque of the Western Fells. Distant Fairfield and Ullscarf put in unexpected appearances through the gaps. Ascents.

Geographic entities mentioned:
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
By contrast the southern slopes fall steadily to the headstream of the Calder, the lower section being planted with conifers. South eastward from Crag Fell begins the long ridge to Caw Fell, first descending to a col at 1,320 ft and then rising gently over the intermediate top of Iron Crag. To the west a narrower ridge runs along above the plantation to Grike.

Geographic entities mentioned:
surface_form: caw fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.486
lon: -3.343
surface_form: crag fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.517
lon: -3.397
surface_form: iron crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4951
lon: -3.35506
Crag Fell. Crag Fell is a hill in the English Lake District. It is part of the Lank Rigg group, standing above Ennerdale Water in the Western Fells. The craggy northern face above the lake gives the fell its name, prominent in views from the car park at Bowness Knott. Ascents are commonly made from the foot of Ennerdale Water. Topography.

Geographic entities mentioned:
surface_form: crag fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.517
lon: -3.397
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. Crag Fell stands near the extremity of the southern arm. The main watershed runs broadly westwards from Great Gable, dividing the headwaters of Ennerdale and Wasdale.

Geographic entities mentioned:
surface_form: crag fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.517
lon: -3.397
Beyond this stand the fells of the Lank Rigg group, the final high country within the National Park. Crag Fell and Grike complete the westward line of the ridge, whilst Lank Rigg lies to the south across the head of the River Calder. The northern flanks of Crag Fell tumble roughly down to the shore of Ennerdale Water.

Geographic entities mentioned:
surface_form: crag fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.517
lon: -3.397
surface_form: grike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.513
lon: -3.415
surface_form: lank rigg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.494
lon: -3.403
Crag Fell and Grike complete the westward line of the ridge, whilst Lank Rigg lies to the south across the head of the River Calder. The northern flanks of Crag Fell tumble roughly down to the shore of Ennerdale Water. One tier of crags is directly below the summit, Revelin Crag being a notable feature, whilst a second abuts the lake itself. This is Anglers Crag, also known as Robin Hood's Chair.

Geographic entities mentioned:
surface_form: crag fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.517
lon: -3.397
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
South eastward from Crag Fell begins the long ridge to Caw Fell, first descending to a col at 1,320 ft and then rising gently over the intermediate top of Iron Crag. To the west a narrower ridge runs along above the plantation to Grike. Crag Fell is bounded by Ben Gill in the west and Red Beck in the east. Mining. The remains of a number of iron mines can be found above the shore of the lake.

Geographic entities mentioned:
surface_form: crag fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.517
lon: -3.397
Ascents. A narrow road runs east from the village of Ennerdale Bridge, giving access to a pair of car parks near the outflow of the lake. Two principal alternatives are available from here to climb Crag Fell. The first is to loosely follow the course of Ben Gill up beside the plantation, before swinging left toward the summit.

Geographic entities mentioned:
surface_form: crag fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.517
lon: -3.397
A more interesting route is to use the lakeshore path to reach the top of Anglers Crag, before working up the hillside to turn Revelin Crag to the west. This takes the walker past what Wainwright called the Crag Fell Pinnacles, a fractured spine of rock rising 80 ft above the angle of the slope. Other ascents can be made from the Coldfell Road, south of Ennerdale Bridge.

Geographic entities mentioned:
surface_form: crag fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.517
lon: -3.397
Crag Fell and Grike complete the westward line of the ridge, whilst Lank Rigg lies to the south across the head of the River Calder. The northern flanks of Crag Fell tumble roughly down to the shore of Ennerdale Water. One tier of crags is directly below the summit, Revelin Crag being a notable feature, whilst a second abuts the lake itself. This is Anglers Crag, also known as Robin Hood's Chair.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Crag Fell is bounded by Ben Gill in the west and Red Beck in the east. Mining. The remains of a number of iron mines can be found above the shore of the lake. Small trials were driven beneath Revelin Crag, above Anglers Crag and on the upper eastern slopes above Red Beck. Although haematite was found, the quantities were never sufficient and all of the mines had closed by 1896. Summit.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
The head of Ennerdale Water is seen to the east, surrounded by the high cirque of the Western Fells. Distant Fairfield and Ullscarf put in unexpected appearances through the gaps. Ascents. A narrow road runs east from the village of Ennerdale Bridge, giving access to a pair of car parks near the outflow of the lake. Two principal alternatives are available from here to climb Crag Fell.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Crag Fell. Crag Fell is a hill in the English Lake District. It is part of the Lank Rigg group, standing above Ennerdale Water in the Western Fells. The craggy northern face above the lake gives the fell its name, prominent in views from the car park at Bowness Knott. Ascents are commonly made from the foot of Ennerdale Water. Topography.

Geographic entities mentioned:
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
This takes the walker past what Wainwright called the Crag Fell Pinnacles, a fractured spine of rock rising 80 ft above the angle of the slope. Other ascents can be made from the Coldfell Road, south of Ennerdale Bridge. A track, formerly the mine road, can be followed almost to the summit, passing over the flanks of Grike.

Geographic entities mentioned:
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
South eastward from Crag Fell begins the long ridge to Caw Fell, first descending to a col at 1,320 ft and then rising gently over the intermediate top of Iron Crag. To the west a narrower ridge runs along above the plantation to Grike. Crag Fell is bounded by Ben Gill in the west and Red Beck in the east. Mining. The remains of a number of iron mines can be found above the shore of the lake.

Geographic entities mentioned:
surface_form: grike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.513
lon: -3.415
Other ascents can be made from the Coldfell Road, south of Ennerdale Bridge. A track, formerly the mine road, can be followed almost to the summit, passing over the flanks of Grike. A circuit of the upper Calder, taking in the whole Lank Rigg group can also be started from here.

Geographic entities mentioned:
surface_form: grike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.513
lon: -3.415
Other ascents can be made from the Coldfell Road, south of Ennerdale Bridge. A track, formerly the mine road, can be followed almost to the summit, passing over the flanks of Grike. A circuit of the upper Calder, taking in the whole Lank Rigg group can also be started from here.

Geographic entities mentioned:
surface_form: lank rigg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.494
lon: -3.403
Rautispitz. The Rautispitz is a mountain of the Schwyzer Alps, overlooking Netstal in the canton of Glarus. It lies between the Obersee and the Klöntalersee and culminates at 2,283 metres above sea level. Its summit is generally accessed from the west side, with several trails starting at the Obersee.

Geographic entities mentioned:
surface_form: obersee
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.08695
lon: 9.0137777777778
surface_form: obersee
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2189
lon: 8.84657
surface_form: obersee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.7845
lon: 9.68147
Rautispitz. The Rautispitz is a mountain of the Schwyzer Alps, overlooking Netstal in the canton of Glarus. It lies between the Obersee and the Klöntalersee and culminates at 2,283 metres above sea level. Its summit is generally accessed from the west side, with several trails starting at the Obersee.

Geographic entities mentioned:
surface_form: rautispitz
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.071138888889
lon: 9.0282222222222
On May 20, 1917, he engaged in aerial combat with three Austrian fighters, including the Hansa-Brandenburg D.I of the Godwin Brumowski flying ace claiming the eighth victory, in collaboration with the ace Károly Kaszala (8 wins), over the Banjšice Plateau, with the plane out of order he was wounded twice and received another silver medal.

Geographic entities mentioned:
surface_form: Banjšice Plateau
instance_of: Plateau
countries: Slovenia
coordinates: lat: 46.04905
lon: 13.69995
Through the efforts of his scouts, McDonnell believed that Te Kooti and his followers had gathered at the village of Papakai. McDonnell now moved his force to Kotukutuku, which was at the northern side of Lake Rotoaira, to the west of Lake Taupō, departing on 2 October. Te Keepa's Wanganui contingent and the Kahungunu &quot;kūpapa&quot; were ordered to move in behind Papakai, leaving on 3 October.

Geographic entities mentioned:
surface_form: Lake Rotoaira
instance_of: Lake
countries: New Zealand
coordinates: lat: -39.0545
lon: 175.7143
The second fortification was referred to as the lower redoubt; this was positioned on the west or left bank of the upper reaches of the Whanganui River, which flowed from the western side of Tongariro mountain. It was a complex of several trenches and while providing cover nearly all round, the position lacked depth and had a limited field of view.

Geographic entities mentioned:
surface_form: Tongariro mountain
instance_of: Mountain
countries: New Zealand
coordinates: lat: -39.12972222222222
lon: 175.63583333333332
Other local references include mention of a person &quot;swallowing a yo-yo&quot; in nearby Griffith, the Old Man being one of the fiercest &quot;furnace fighters in Northern Indiana&quot; and that his obscenities were &quot;hanging in space over Lake Michigan&quot;, a mention of the Indianapolis 500, and the line to Santa Claus &quot;stretching all the way to Terre Haute&quot;.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Ganboa. Ganboa (1,412 m) is a summit on the Gipuzkoan side of the Aralar Range (Basque Country), the mount having long been held as the highest in the range, while nowadays it trails second to Irumugarrieta. The peak, crowned with a mountaineer postbox, is surrounded by grasslands, secondary peaks and limestone karst terrain, where deep fissures are not rare to be seen. Access points.

Geographic entities mentioned:
surface_form: ganboa
instance_of: Mountain
countries: Spain
coordinates: lat: 43.006188888889
lon: -2.0627222222222
The peak, crowned with a mountaineer postbox, is surrounded by grasslands, secondary peaks and limestone karst terrain, where deep fissures are not rare to be seen. Access points. Ganboa's central position at the heart of Aralar sets the summit far away and at a similar distance from any access point.

Geographic entities mentioned:
surface_form: ganboa
instance_of: Mountain
countries: Spain
coordinates: lat: 43.006188888889
lon: -2.0627222222222
Whiddon Lake (Ontario). Whiddon Lake is a lake in Thunder Bay District, Ontario, Canada. It is long and wide and lies at an elevation of about northeast of the community of Armstrong. The primary outflow is an unnamed creek that joins the Whitesand River at a point between the mouth of Blackett Creek upstream and Whitesand Lake downstream.

Geographic entities mentioned:
surface_form: Blackett Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.40972222222222
lon: -88.81361111111111
surface_form: whitesand lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.37555555555556
lon: -88.84916666666666
surface_form: whitesand lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.852777777777774
lon: -87.38111111111111
Whiddon Lake (Ontario). Whiddon Lake is a lake in Thunder Bay District, Ontario, Canada. It is long and wide and lies at an elevation of about northeast of the community of Armstrong. The primary outflow is an unnamed creek that joins the Whitesand River at a point between the mouth of Blackett Creek upstream and Whitesand Lake downstream.

Geographic entities mentioned:
surface_form: whiddon lake (ontario)
instance_of: Lake
countries: Canada
coordinates: lat: 50.4206
lon: -88.8519
Whiddon Lake (Ontario). Whiddon Lake is a lake in Thunder Bay District, Ontario, Canada. It is long and wide and lies at an elevation of about northeast of the community of Armstrong. The primary outflow is an unnamed creek that joins the Whitesand River at a point between the mouth of Blackett Creek upstream and Whitesand Lake downstream.

Geographic entities mentioned:
surface_form: whiddon lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.4206
lon: -88.8519
Whiddon Lake (Ontario). Whiddon Lake is a lake in Thunder Bay District, Ontario, Canada. It is long and wide and lies at an elevation of about northeast of the community of Armstrong. The primary outflow is an unnamed creek that joins the Whitesand River at a point between the mouth of Blackett Creek upstream and Whitesand Lake downstream.

Geographic entities mentioned:
surface_form: armstrong
instance_of: Mountain
countries: Canada
coordinates: lat: 50.35027777777778
lon: -114.76638888888888
Temperature. Temperatures at sea level generally range from highs of during the summer months to during the winter months. Rarely does the temperature rise from above or drop below at lower elevations. Temperatures are lower at higher altitudes. During the winter, snowfall is common at the summits of Mauna Kea and Mauna Loa on Hawaii Island.

Geographic entities mentioned:
surface_form: Mauna Kea
instance_of: Mountain
countries: United States
coordinates: lat: 19.820555555555554
lon: -155.46805555555557
The storms may be associated with the passage of a cold front, the leading edge of a mass of relatively cool air that is moving from west to east or from northwest to southeast. Annual mean rainfall ranges from on the summit of Mauna Kea to in Big Bog. Windward slopes have greater rainfall than leeward lowlands and tall mountains.

Geographic entities mentioned:
surface_form: Mauna Kea
instance_of: Mountain
countries: United States
coordinates: lat: 19.820555555555554
lon: -155.46805555555557
It is situated in the Oruro Department, Pantaleón Dalence Province, Huanuni Municipality. Muru Qullu lies between Ch'iyara Ch'ankha in the northwest and Juch'uy Yaritani in the southeast. The river Jalantaña flows east of Muru Qullu.

Geographic entities mentioned:
surface_form: Ch'iyara Ch'ankha
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.2083
lon: -66.8294
surface_form: muru qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.72944444
lon: -66.03833333
surface_form: yaritani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.1436
lon: -68.35
surface_form: muru qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.2228
lon: -66.8264
surface_form: yaritani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.43611111
lon: -66.63166667
Muru Qullu (Oruro). Muru Qullu (Aymara &quot;muru&quot; truncated, &quot;qullu&quot; mountain, &quot;truncated mountain&quot;, also spelled &quot;Muru Kkollu&quot;) is a mountain in the Andes of Bolivia. It is situated in the Oruro Department, Pantaleón Dalence Province, Huanuni Municipality. Muru Qullu lies between Ch'iyara Ch'ankha in the northwest and Juch'uy Yaritani in the southeast.

Geographic entities mentioned:
surface_form: muru qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.72944444
lon: -66.03833333
surface_form: muru qullu (oruro)
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.2228
lon: -66.8264
Muru Qullu (Oruro). Muru Qullu (Aymara &quot;muru&quot; truncated, &quot;qullu&quot; mountain, &quot;truncated mountain&quot;, also spelled &quot;Muru Kkollu&quot;) is a mountain in the Andes of Bolivia. It is situated in the Oruro Department, Pantaleón Dalence Province, Huanuni Municipality. Muru Qullu lies between Ch'iyara Ch'ankha in the northwest and Juch'uy Yaritani in the southeast.

Geographic entities mentioned:
surface_form: muru qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.72944444
lon: -66.03833333
surface_form: muru qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.2228
lon: -66.8264
Together with the Moriscos, they thronged to the ports of North Africa, and mingled with native Jewish people. In the 16th century there were large Jewish communities in places such as Oran, Bejaïa and Algiers. Jews were also present in the cities of the interior, such as Tlemcen and Constantine, and as far as Touggourt and M'zab in the south, with the permission of the Muslim authorities.

Geographic entities mentioned:
surface_form: M'zab
instance_of: Valley
countries: Algeria
coordinates: lat: 32.487222222222
lon: 3.6813888888889
After the 1882 conquest of the M'zab, the French government in Algeria legally categorized southern Algerian Jews, like the Muslims, as &quot;indigènes&quot;, and thus subject to restricted and decreased rights under the indigénat compared to their northern Jewish counterparts, who were still French citizens under the Crémieux Decree of 1870.

Geographic entities mentioned:
surface_form: M'zab
instance_of: Valley
countries: Algeria
coordinates: lat: 32.487222222222
lon: 3.6813888888889
Between late 1961 and late summer 1962, 130,000 of Algeria's approximately 140,000 Jews left for France, while about 10,000 of them emigrated to Israel. Moroccan Jews who were living in Algeria and Jews from the M'zab Valley in the Algerian Sahara, who did not have French citizenship, as well as a small number of Algerian Jews from Constantine, also emigrated to Israel at that time.

Geographic entities mentioned:
surface_form: M'zab Valley
instance_of: Valley
countries: Algeria
coordinates: lat: 32.487222222222
lon: 3.6813888888889
Děvín. Děvín () is a double peak mountain in the Pavlov municipality in the South Moravian Region of the Czech Republic. With an elevation of, it is the highest mountain of the Pavlov Hills within the Mikulov Highlands, and of the Pálava Protected Landscape Area. It is located right on trace where runs line of drainage divide of Upper Thaya drainage and Thaya/Morava meso-level drainage. History.

Geographic entities mentioned:
surface_form: děvín
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 48.8694
lon: 16.6497
History. The summit of Děvín has the remains of a huge Iron Age hill fort, while the ancient Amber Route runs neighbors of the mountains base, and all archaic roads in landscape, originally created by animals and later overtaken by humans. The area around base of the mountain is permanently settled longer than last 30,000 years.

Geographic entities mentioned:
surface_form: děvín
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 48.8694
lon: 16.6497
The area around base of the mountain is permanently settled longer than last 30,000 years. Since Cromagnos hunters, ower Celtic tribes settlement, Roman fortress, Great Moravia hillforts (Strachotín and Děvín). Geology. The entire Děvín massif consists mainly by Jurassic limestone, i.e. series of rocks generated during sedimentation.

Geographic entities mentioned:
surface_form: děvín
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 48.8694
lon: 16.6497
series of rocks generated during sedimentation. The body of the Děvín is strongly modulated, with outcrops and crag) of pure, hard and white limestone of Later Jurassic origin, called Ernstbrunn limestone. Sedimentation of Ernstbrunn limestone was preceded by the sedimentation of grey calcareous
Děvín claystone and clay limestone, called Klentnice layers.

Geographic entities mentioned:
surface_form: děvín
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 48.8694
lon: 16.6497
During the following 9 Ma, up to 3 km thick layers of maritime and lacustrine sediments were deposited on its bottom. Flora. Děvín as a whole eastern part of the Mikulov Highlands lies in the northwest promontory of the Panonian plain. It is the warmest and almost the most arid area in the Czech Republic, and therefore vines are cultivated here.

Geographic entities mentioned:
surface_form: děvín
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 48.8694
lon: 16.6497
Because of this climate some plant species that do not occur anywhere else in the country grow here. The colourful mosaic of arid rock grass, fringe tree communities, thermophilous bushes and thermophilous oakwoods on the Děvín slopes, which originated partly due to the influence of grazing, is called karst forest steppe.

Geographic entities mentioned:
surface_form: děvín
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 48.8694
lon: 16.6497
The Děvín forest plateaus are dominated by sparse loess oakwoods together with a species-rich herbaceous layer, while Panonian oak-hornbeam dominates the north-facing slopes and valleys. Riparian forests with pedunculate oaks and narrow-leaved ashes and quite small areas of alluvial meadows have been preserved in the Dyje floodplain in the vicinity of Křivé lake.

Geographic entities mentioned:
surface_form: děvín
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 48.8694
lon: 16.6497
Piz Nair. Piz Nair () is a mountain of the Albula Alps in Switzerland, overlooking St. Moritz in the canton of Graubünden. The peak is easily accessible from the village with a funicular and a cable car; the upper station unloads below the summit. Below the summit to the east is the Corviglia ski area. The mountain hosted the alpine skiing events for the 1948 Winter Olympics in neighboring St.

Geographic entities mentioned:
surface_form: piz nair
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.699
lon: 8.70897
surface_form: piz nair
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50625
lon: 9.7874444444444
It also passes through three Heritage Landscapes: Merthyr Mawr and Kenfig Margam Burrows (which stretches from Neath Port Talbot through Bridgend to Vale of Glamorgan), Caldicot and Wentloog Levels (Cardiff, Newport, Monmouthshire), and Lower Wye Valley (Monmouthshire).

Geographic entities mentioned:
surface_form: Wye Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
Preston Lake (Renville County, Minnesota). Preston Lake is a lake in Renville County, in the U.S. state of Minnesota. Preston Lake bears the name of a pioneer settler.

Geographic entities mentioned:
surface_form: preston lake (renville county, minnesota)
instance_of: Lake
countries: United States
coordinates: lat: 44.782777777778
lon: -94.538333333333
Preston Lake (Renville County, Minnesota). Preston Lake is a lake in Renville County, in the U.S. state of Minnesota. Preston Lake bears the name of a pioneer settler.

Geographic entities mentioned:
surface_form: preston lake
instance_of: Lake
countries: United States
coordinates: lat: 44.782777777778
lon: -94.538333333333
Biography. In 73BC, Crixus was part of what started as a small slave revolt in the gladiatorial training school of Lentulus Batiatus in Capua, in which about 70 gladiators escaped. The escaped slaves defeated a small force sent to recapture them, then made camp on the slopes of Mount Vesuvius. Word of the escaped gladiators' revolt spread, and other escaped slaves started to join their ranks.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
Campylomormyrus bredoi. The Mweru elephantfish, &quot;Campylomormyrus bredoi&quot; is a species of electric fish in the family Mormyridae, found only in Lake Mweru. It is native to the Democratic Republic of the Congo and can reach a size of approximately. Regarding its conservation status, according to the IUCN, this species can be classified in the &quot;vulnerable (VU)&quot; category. Size.

Geographic entities mentioned:
surface_form: Lake Mweru
instance_of: Lake
countries: Zambia
Democratic Republic of the Congo
coordinates: lat: -9.1666666666667
lon: 28.5
Kirkmichael, Moray. Kirkmichael is a parish in the council area of Moray, Scotland. It lies south of Ballindalloch and includes the Tomintoul Distillery. Geography. The parish includes the largely unpopulated upper Stratha'an up to and including Loch A'an and the Shelter Stone. The village of Tomintoul is the largest settlement and the total area of the parish is. Demography.

Geographic entities mentioned:
surface_form: Stratha'an
instance_of: Valley
countries: United Kingdom
surface_form: Loch A'an
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.1
lon: -3.6333333333333
Lockport Powerhouse. The Lockport Powerhouse is an American run-of-the-river dam used by the Metropolitan Water Reclamation District of Greater Chicago to control the outflow of the Sanitary and Ship Canal and limit the diversion of water from Lake Michigan into the Des Plaines River. History. The Chicago Sanitary and Ship Canal reached Lockport, Illinois in the 1890s.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Geography. North of the village lies an intermittent lake named Lake Palčje. It is the largest among the Pivka lakes, with an average maximum water area around. The highest elevations are in the Javornik Hills in the far eastern part of the settlement's territory, at Kozlovka Peak (&quot;Vrh Kozlovke&quot;,), Mount Kalič (), and Mount Lamovšek () above the small Prevale Valley. Name.

Geographic entities mentioned:
surface_form: Javornik Hills
instance_of: Plateau
countries: Slovenia
coordinates: lat: 45.73333333
lon: 14.28333333
The medieval transcription indicates that today's name (a neuter singular) is derived from the accusative plural demonym &quot;*Paličane&quot;, derived from the common noun &quot;*palič&quot;, likely meaning 'small lake' (cognate with Lake Palić, Serbia), a diminutive of the Slavic noun &quot;palъ&quot;, preserved in the Slovene common noun &quot;pal&quot; 'mud' (and cognate with German &quot;Pfuhl&quot; 'puddle', English &quot;pool&quot;).

Geographic entities mentioned:
surface_form: Lake Palić
instance_of: Lake
countries: Serbia
coordinates: lat: 46.07
lon: 19.7475
Chomjakovbreen. Chomjakovbreen is a glacier in Sørkapp Land at Spitsbergen, Svalbard. It has a length of about nine kilometers, and is located between the mountain ridges of Bredichinryggen and Påskefjella. It debouches into the bay Svovelbukta at the southern side of Hornsund. The glacier is named after a participant of the Swedish-Russian Arc-of-Meridian Expedition from 1899 to 1902.

Geographic entities mentioned:
surface_form: Bredichinryggen
instance_of: Mountain
countries: Norway
coordinates: lat: 76.9228
lon: 16.4769
surface_form: Påskefjella
instance_of: Mountain
countries: Norway
coordinates: lat: 76.9321
lon: 16.374
Bailadila Range. Bailadila Range, is a mountain range rising in the Deccan Plateau about 200 km west of the Eastern Ghats. It has been named 'Bailadila' because it resembles the hump of an ox. It is located near Kirandul town in the Dantewada district of southern Chhattisgarh, India. Hematite ore is found here, which is exported from Visakhapatnam port to Japan and South Korea.

Geographic entities mentioned:
surface_form: Deccan Plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
This large fault marks the boundary between the Indian and Burma plates. The megathrust emerges from the seafloor in Bangladesh, where it runs parallel and east of the Chin Hills. This boundary continues to north of Myanmar where it ends at the eastern Himalayas. A transform fault runs through Myanmar and connects the Andaman spreading center to a collision zone in the north.

Geographic entities mentioned:
surface_form: Chin Hills
instance_of: Mountain
countries: Myanmar
coordinates: lat: 22.5
lon: 93.5
One flaw of this translation process is that if the language a word is being translated into does not have a concept for it, the word may not be correctly translated or understood. For example, the Romans don't have a word or a general understanding of &quot;volcano&quot; as Mount Vesuvius has not erupted yet. &quot;Farscape&quot;.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
Gour de Tazenat. The Gour de Tazenat is a volcanic lake in the French department of Puy-de-Dôme. It was formed by a phreatomagmatic eruption about 29,000 years ago. Topography. The lake marks the northern limit of the Chaîne des Puys. It is located in Charbonnières-les-Vieilles, near Manzat in the French department of Puy-de-Dôme.

Geographic entities mentioned:
surface_form: gour de tazenat
instance_of: Lake
countries: France
coordinates: lat: 45.98
lon: 2.991
surface_form: tazenat
instance_of: Lake
countries: France
coordinates: lat: 45.98
lon: 2.991
Gour de Tazenat. The Gour de Tazenat is a volcanic lake in the French department of Puy-de-Dôme. It was formed by a phreatomagmatic eruption about 29,000 years ago. Topography. The lake marks the northern limit of the Chaîne des Puys. It is located in Charbonnières-les-Vieilles, near Manzat in the French department of Puy-de-Dôme.

Geographic entities mentioned:
surface_form: gour de tazenat
instance_of: Lake
countries: France
coordinates: lat: 45.98
lon: 2.991
surface_form: tazenat
instance_of: Lake
countries: France
coordinates: lat: 45.98
lon: 2.991
surface_form: puy-de-dôme
instance_of: Mountain
countries: France
coordinates: lat: 45.772
lon: 2.9624
The crater of this volcano is on average deep and wide. A 2.8 km trail can be used to walk around it. Navigation on the lake is prohibited. Geology. Gour de Tazenat is a volcanic crater formed by a phreatomagmatic eruption. The banks of the lake have a volcanic crescent moon shape (north, east and south) formed by projections arranged in layers.

Geographic entities mentioned:
surface_form: gour de tazenat
instance_of: Lake
countries: France
coordinates: lat: 45.98
lon: 2.991
surface_form: tazenat
instance_of: Lake
countries: France
coordinates: lat: 45.98
lon: 2.991
It causes heavy explosions capable of breaking fragments of crystalline basement, and the appearance of volcanic bombs in cauliflower shapes. Thereafter, water is removed and activity becomes more magmatic than phreatic. After cessation of eruptive activity, the Gour de Tazenat gradually filled with rainwater. Fauna and flora.

Geographic entities mentioned:
surface_form: gour de tazenat
instance_of: Lake
countries: France
coordinates: lat: 45.98
lon: 2.991
surface_form: tazenat
instance_of: Lake
countries: France
coordinates: lat: 45.98
lon: 2.991