Sarmila/GeoWiki-Features huggingface dataset:
Reedy Lake. Reedy Lake, historically also known as Lake Reedy, is a shallow intermittent freshwater lake or swamp on the lower reaches of the Barwon River, on the Bellarine Peninsula southeast of Geelong in the Australian state of Victoria. Location and features.

Geographic entities mentioned:
surface_form: reedy lake
instance_of: Lake
countries: Australia
coordinates: lat: -38.2083
lon: 144.425
History. Six thousand years ago Reedy Lake was part of a large marine bay. With a subsequent change in relative sea level it was cut off from the sea by a barrier of sand dunes, and its bed covered by a layer of alluvial clay deposited by the Barwon River.

Geographic entities mentioned:
surface_form: reedy lake
instance_of: Lake
countries: Australia
coordinates: lat: -38.2083
lon: 144.425
The first barrier across the Barwon was built in 1838 to provide fresh water for Geelong. In 1899 a second barrier, known as the 'lower breakwater' was built further downstream on the river at the southern boundary of Reedy Lake, making it a predominantly freshwater wetland, with an extensive cover of vegetation, that supported diverse populations of waterbirds and other aquatic wildlife.

Geographic entities mentioned:
surface_form: reedy lake
instance_of: Lake
countries: Australia
coordinates: lat: -38.2083
lon: 144.425
Agrotis kuamauna. &quot;Agrotis kuamauna&quot; is a species of owlet moth endemic to the alpine high elevations of Mauna Kea on the big island of Hawai'i. Description. &quot;Agrotis kuamauna&quot; adults have forewing lengths ranging from 31-40mm. Forewings are brown with small darker splotches. The abdomen is brown with tufts of scales. &quot;A.

Geographic entities mentioned:
surface_form: Mauna Kea
instance_of: Mountain
countries: United States
coordinates: lat: 19.820555555555554
lon: -155.46805555555557
Distribution and habitat. &quot;Agrotis kuamauna&quot; is endemic to the harsh high elevation alpine zones near the summit of Mauna Kea, occupying elevations from 3000m up to the summit (~4200m). Larvae are found associated with volcanic ash substrates within this habitat, as opposed to the more rocky cinders preferred by some other summit insects such as the Wekiu bug. Ecology.

Geographic entities mentioned:
surface_form: Mauna Kea
instance_of: Mountain
countries: United States
coordinates: lat: 19.820555555555554
lon: -155.46805555555557
Umsaskis Lake. Umsaskis Lake is a lake on the Allagash River in the North Maine Woods region of Maine. It is located in Aroostook County and lies approximately from the Canada-U.S. border. The lake is on the Northern Forest Canoe Trail.

Geographic entities mentioned:
surface_form: umsaskis lake
instance_of: Lake
countries: United States
coordinates: lat: 46.591666666667
lon: -69.375
Buffalo Peak. Buffalo Peak is a mountain summit in the Kenosha Mountains range of the Rocky Mountains of North America. The peak is located in the Lost Creek Wilderness of Pike National Forest, west by north (bearing 280°) of the community of Deckers, Colorado, United States. Buffalo Peak is the highest point in Jefferson County, Colorado.

Geographic entities mentioned:
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: buffalo peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.2756
lon: -105.368
Buffalo Peak. Buffalo Peak is a mountain summit in the Kenosha Mountains range of the Rocky Mountains of North America. The peak is located in the Lost Creek Wilderness of Pike National Forest, west by north (bearing 280°) of the community of Deckers, Colorado, United States. Buffalo Peak is the highest point in Jefferson County, Colorado.

Geographic entities mentioned:
surface_form: buffalo peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.2756
lon: -105.368
Greenwood, Halifax County, Nova Scotia. Greenwood, Halifax County is a rural community of the Halifax Regional Municipality in the Canadian province of Nova Scotia. It is located along Route 224, in the Musquodoboit Valley.

Geographic entities mentioned:
surface_form: Musquodoboit Valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.0167
lon: -63.1833
It is situated in the Apurímac Region, Antabamba Province, Oropesa District, in the Arequipa Region, La Unión Province, Puyca District, and in the Cusco Region, Chumbivilcas Province, Santo Tomás District, south of the mountain Chankuwaña.

Geographic entities mentioned:
surface_form: Chankuwaña
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6231
lon: -72.4692
Waytani. Waytani (Aymara &quot;wayta&quot; headdress made of feathers or flowers, &quot;-ni&quot;, a suffix to indicate ownership, 'the one with the decoration on the head', Hispanicized spelling &quot;Huaytane&quot;) is a mountain in the Wansu mountain range in the Andes of Peru, about high.

Geographic entities mentioned:
surface_form: waytani
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6581
lon: -72.4678
Waytani. Waytani (Aymara &quot;wayta&quot; headdress made of feathers or flowers, &quot;-ni&quot;, a suffix to indicate ownership, 'the one with the decoration on the head', Hispanicized spelling &quot;Huaytane&quot;) is a mountain in the Wansu mountain range in the Andes of Peru, about high.

Geographic entities mentioned:
surface_form: waytani
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6581
lon: -72.4678
surface_form: huaytane
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6581
lon: -72.4678
Union Peak. Union Peak is a heavily eroded shield volcano in the Cascade Range of central Oregon, located along the Cascade Crest less than southwest of the rim of Crater Lake. Ice age glaciers eroded away most of the flanks of the volcano, leaving numerous deep cirques surrounding a central glacial horn.

Geographic entities mentioned:
surface_form: Crater Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.943611111111
lon: -122.10666666667
surface_form: union peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.4556
lon: -109.788
surface_form: crater lake
instance_of: Lake
countries: United States
coordinates: lat: 46.9382689
lon: -121.8620654
surface_form: union peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.831122222222
lon: -122.22332777778
surface_form: crater lake
instance_of: Lake
countries: United States
coordinates: lat: 39.0853
lon: -106.967
Ice age glaciers eroded away most of the flanks of the volcano, leaving numerous deep cirques surrounding a central glacial horn. This is the same process that formed the summit horns of Three Fingered Jack, Mount Washington, Howlock Mountain, and Mount Thielsen from other shield volcanoes farther north in the Oregon Cascades.

Geographic entities mentioned:
surface_form: Three Fingered Jack
instance_of: Mountain
countries: United States
coordinates: lat: 44.478965122
lon: -121.843058797
surface_form: Howlock Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.19235
lon: -122.03975
surface_form: Mount Thielsen
instance_of: Mountain
countries: United States
coordinates: lat: 43.152837292
lon: -122.066514283
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 47.5311964
lon: -123.2459807
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 42.1019
lon: -73.4325
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 38.9149
lon: -114.309
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 40.4271
lon: -80.0112
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 44.270827777778
lon: -71.303483333333
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 44.3321
lon: -121.839
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 47.4259
lon: -121.7
This is the same process that formed the summit horns of Three Fingered Jack, Mount Washington, Howlock Mountain, and Mount Thielsen from other shield volcanoes farther north in the Oregon Cascades. Union Peak is located within Crater Lake National Park, and the summit was used as a post for fire lookouts from the 1930s to the 1950s.

Geographic entities mentioned:
surface_form: crater lake
instance_of: Lake
countries: United States
coordinates: lat: 42.943611111111
lon: -122.10666666667
surface_form: union peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.4556
lon: -109.788
surface_form: crater lake
instance_of: Lake
countries: United States
coordinates: lat: 46.9382689
lon: -121.8620654
surface_form: union peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.831122222222
lon: -122.22332777778
surface_form: crater lake
instance_of: Lake
countries: United States
coordinates: lat: 39.0853
lon: -106.967
Union Peak. Union Peak is a heavily eroded shield volcano in the Cascade Range of central Oregon, located along the Cascade Crest less than southwest of the rim of Crater Lake. Ice age glaciers eroded away most of the flanks of the volcano, leaving numerous deep cirques surrounding a central glacial horn.

Geographic entities mentioned:
surface_form: union peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.4556
lon: -109.788
surface_form: union peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.831122222222
lon: -122.22332777778
Vauréal Peak. Vauréal Peak () is a rocky peak at the east side of the entrance to Admiralty Bay, King George Island, in the South Shetland Islands. The name &quot;Cap Vauréal&quot; was assigned in this location by the French Antarctic Expedition under J.B. Charcot in 1908–10. Air photos now show that the most prominent feature in the vicinity is this peak.

Geographic entities mentioned:
surface_form: vauréal peak
instance_of: Mountain
coordinates: lat: -62.1833
lon: -58.3
Vauréal Peak. Vauréal Peak () is a rocky peak at the east side of the entrance to Admiralty Bay, King George Island, in the South Shetland Islands. The name &quot;Cap Vauréal&quot; was assigned in this location by the French Antarctic Expedition under J.B. Charcot in 1908–10. Air photos now show that the most prominent feature in the vicinity is this peak.

Geographic entities mentioned:
surface_form: vauréal peak
instance_of: Mountain
coordinates: lat: -62.1833
lon: -58.3
surface_form: george
instance_of: Mountain
coordinates: lat: -67.71667
lon: 50
Vauréal Peak. Vauréal Peak () is a rocky peak at the east side of the entrance to Admiralty Bay, King George Island, in the South Shetland Islands. The name &quot;Cap Vauréal&quot; was assigned in this location by the French Antarctic Expedition under J.B. Charcot in 1908–10. Air photos now show that the most prominent feature in the vicinity is this peak.

Geographic entities mentioned:
surface_form: vauréal
instance_of: Mountain
coordinates: lat: -62.1833
lon: -58.3
Samaritan synagogue. The Samaritan synagogue, oriented westwards toward Mount Gerizim—the holiest site in Samaritanism—comprised a central hall, a long exedra on the north side, and courtyards to the south and at the entrance; the latter was probably surrounded by columns in antiquity.

Geographic entities mentioned:
surface_form: Mount Gerizim
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.199444444444
lon: 35.272777777778
He was reelected in the 64th Assembly District in 1966 and 1968,
City. McGee gave up his Assembly position to run in the conservatively oriented Los Angeles City Council District 3 in the West San Fernando Valley, which included Woodland Hills, Encino, Tarzana, Northridge, Reseda and Canoga Park. He won an easy victory in the 1957 primary for a four-year term.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Trampolines, 1960. He urged the city Health Department to study the health effects of the popular trampoline centers then opening up in the city. Boroughs, 1960. He urged the establishment of a borough system to provide more local representation for the San Fernando Valley.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Milford Track. The Milford Track is a hiking route in New Zealand, located amidst mountains and temperate rain forest in Fiordland National Park in the southwest of the South Island. The 53.5 km (33.2 mi) hike starts at Glade Wharf at the head of Lake Te Anau and finishes in Milford Sound at Sandfly Point, traversing rainforests, wetlands, and an alpine pass.

Geographic entities mentioned:
surface_form: Lake Te Anau
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.2
lon: 167.8
The evolution of Cain's &quot;The Butterfly&quot; spans over two decades, beginning with his first visit to West Virginia in 1922 at age 30, where he acquired knowledge for two elements that appear in the novel: &quot;moonshining and [coal] mines.&quot;
Cain's idea for a novel addressing incest had initially occurred to him while driving in the mountains north of the San Fernando Valley of California in the early 1930s.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
It is situated in the Potosí Department, Cornelio Saavedra Province, Tacobamba Municipality, near the border with the Tomás Frías Province, Potosí Municipality. Milluni lies south-east of the lake Urqu Qucha.

Geographic entities mentioned:
surface_form: urqu qucha
instance_of: Lake
countries: Bolivia
coordinates: lat: -19.36777777777778
lon: -65.56472222222222
Milluni (Potosí). Milluni Aymara &quot;millu&quot; light brown, reddish, fair-haired, dark chestnut, &quot;-ni&quot; suffix to indicate ownership, &quot;the brown one&quot;) is a mountain in the Bolivian Andes. It is situated in the Potosí Department, Cornelio Saavedra Province, Tacobamba Municipality, near the border with the Tomás Frías Province, Potosí Municipality.

Geographic entities mentioned:
surface_form: milluni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.3864
lon: -65.5481
Lake Naplás. Lake Naplás (Hungarian: &quot;Naplás-tó&quot;, officially called Szilas-pataki flood control reservoir) is the largest lake of Budapest. The lake is artificial, surrounded by the second largest natural reserve of Budapest, including a moorland and a forest. Rare flora and fauna could be found here, therefore it has been a protected since 1997.

Geographic entities mentioned:
surface_form: naplás-tó
instance_of: Lake
countries: Hungary
coordinates: lat: 47.50944444
lon: 19.24638889
surface_form: lake naplás
instance_of: Lake
countries: Hungary
coordinates: lat: 47.50944444
lon: 19.24638889
Lake Naplás. Lake Naplás (Hungarian: &quot;Naplás-tó&quot;, officially called Szilas-pataki flood control reservoir) is the largest lake of Budapest. The lake is artificial, surrounded by the second largest natural reserve of Budapest, including a moorland and a forest. Rare flora and fauna could be found here, therefore it has been a protected since 1997.

Geographic entities mentioned:
surface_form: lake naplás
instance_of: Lake
countries: Hungary
coordinates: lat: 47.50944444
lon: 19.24638889
Qillqata (Cochabamba). Qillqata (Aymara &quot;qillqaña&quot; to write, &quot;-ta&quot; a suffix, &quot;written&quot; or &quot;something written&quot;, also spelled &quot;Khellkhata&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the Cochabamba Department, Quillacollo Province, Quillacollo Municipality. Qillqata lies southeast of Uqi Salli Punta.

Geographic entities mentioned:
surface_form: Uqi Salli Punta
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.04527778
lon: -66.30277778
Qillqata (Cochabamba). Qillqata (Aymara &quot;qillqaña&quot; to write, &quot;-ta&quot; a suffix, &quot;written&quot; or &quot;something written&quot;, also spelled &quot;Khellkhata&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the Cochabamba Department, Quillacollo Province, Quillacollo Municipality. Qillqata lies southeast of Uqi Salli Punta.

Geographic entities mentioned:
surface_form: qillqata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.06
lon: -65.28333333
surface_form: qillqata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.60333333
lon: -66.7775
surface_form: qillqata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.0642
lon: -67.4914
surface_form: qillqata (cochabamba)
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.06638889
lon: -66.28861111
Qillqata (Cochabamba). Qillqata (Aymara &quot;qillqaña&quot; to write, &quot;-ta&quot; a suffix, &quot;written&quot; or &quot;something written&quot;, also spelled &quot;Khellkhata&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the Cochabamba Department, Quillacollo Province, Quillacollo Municipality. Qillqata lies southeast of Uqi Salli Punta.

Geographic entities mentioned:
surface_form: qillqata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.06
lon: -65.28333333
surface_form: qillqata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.60333333
lon: -66.7775
surface_form: qillqata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.0642
lon: -67.4914
surface_form: qillqata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.06638889
lon: -66.28861111
Streif. Streif is a World Cup downhill ski course in Austria, located on Hahnenkamm mountain (Kitzbühel Alps) in Kitzbühel, Tyrol, and has hosted the Hahnenkamm Races since 1937. It runs on natural terrain (pasture in summer) with minor modifications done over the years, adjacent to the &quot;Ganslern&quot; slalom course.

Geographic entities mentioned:
surface_form: Hahnenkamm
instance_of: Mountain
countries: Austria
coordinates: lat: 47.424166666667
lon: 12.365277777778
Club5+. In 1986, elite Club5 was originally founded by prestigious classic downhill organizers: Kitzbühel, Wengen, Garmisch, Val d’Isère and Gröden, with goal to bring alpine ski sport on the highest levels possible.

Geographic entities mentioned:
surface_form: Gröden
instance_of: Valley
countries: Italy
coordinates: lat: 46.56
lon: 11.704722
The Heleneum is a villa on the shores of Lake Lugano built between 1930 and 1934 on the architectural model of the &quot;Petit Trianon&quot; in Versailles by Hélène Bieber, a strong-willed cosmopolitan lady who wanted to transform it into a centre for social and cultural entertainment and who lived there until 1967.

Geographic entities mentioned:
surface_form: Lake Lugano
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46
lon: 9
Big Timothy Mountain. Big Timothy Mountain, formerly called Boss Mountain and Takomkane Mountain, is a cinder cone in central British Columbia, Canada, located west of Hendrix Lake and southwest of Mount Perseus.

Geographic entities mentioned:
surface_form: big timothy mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.102222222222
lon: -120.93111111111
Big Timothy Mountain. Big Timothy Mountain, formerly called Boss Mountain and Takomkane Mountain, is a cinder cone in central British Columbia, Canada, located west of Hendrix Lake and southwest of Mount Perseus.

Geographic entities mentioned:
surface_form: big timothy mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.102222222222
lon: -120.93111111111
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Allen Crags. Allen Crags is a fell in the English Lake District, it lies in a group of very popular hills and is regarded as part of the Scafell group of fells. It is a hill that is frequently traversed by walkers along its ridge but is seldom climbed as the sole objective. Name.

Geographic entities mentioned:
surface_form: Scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
surface_form: allen crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4661
lon: -3.1802388888889
To the north Allen Crags is connected to the fell of Glaramara by a three kilometre undulating ridge which is a joy to walk taking in three subsidiary tops along the way to the main top. To the south the fell drops to connect with the mountain pass of Esk Hause from where it is possible to reach the neighbouring fells of Esk Pike and Great End and even Scafell Pike with a little more effort.

Geographic entities mentioned:
surface_form: Glaramara
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483319444444
lon: -3.1653
surface_form: allen crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4661
lon: -3.1802388888889
To the north Allen Crags is connected to the fell of Glaramara by a three kilometre undulating ridge which is a joy to walk taking in three subsidiary tops along the way to the main top. To the south the fell drops to connect with the mountain pass of Esk Hause from where it is possible to reach the neighbouring fells of Esk Pike and Great End and even Scafell Pike with a little more effort.

Geographic entities mentioned:
surface_form: Esk Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456219444444
lon: -3.17995
surface_form: Great End
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.464
lon: -3.194
surface_form: Scafell Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
However, a direct climb is possible from Borrowdale ascending the Grains Gill path from Seathwaite to Esk Hause and then climbing easily up the fell from the south. The fell can also be included in a horseshoe walk from Seathwaite also taking in Seathwaite Fell as well as Glaramara and Allen Crags. Summit. The top of the fell has three cairns with the middle one set on rocks being the highest.

Geographic entities mentioned:
surface_form: Seathwaite Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.478
lon: -3.192
surface_form: allen crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4661
lon: -3.1802388888889
surface_form: glaramara
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483319444444
lon: -3.1653
Summit. The top of the fell has three cairns with the middle one set on rocks being the highest. The highlight of the view is an excellent vista of Great Gable, the southern part of the view is restricted by higher fells but the northern panorama from west to east is a fine view.

Geographic entities mentioned:
surface_form: Great Gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
Geology. The summit rocks comprise the laminated volcaniclastic claystones and siltstones of the Esk Pike Formation. There is a narrow intrusion of andesite and hybridized andesite porphyry running across the high point. The majority of the ridge displays the underlying dacitic welded lapilli tuff of the Lincomb Tarns Formation. Ascents.

Geographic entities mentioned:
surface_form: esk pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456219444444
lon: -3.17995
Allen Crags. Allen Crags is a fell in the English Lake District, it lies in a group of very popular hills and is regarded as part of the Scafell group of fells. It is a hill that is frequently traversed by walkers along its ridge but is seldom climbed as the sole objective. Name.

Geographic entities mentioned:
surface_form: allen crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4661
lon: -3.1802388888889
The name originates from “Alein” or “Aleyn” which was a popular personal name after the Norman conquest of England, it is of Breton origin and the fell was named after an unknown French conqueror. Topography. Allen Crags is situated at the southern end of a long north-south ridge that starts at Stonethwaite in Borrowdale and concludes at the strategically important mountain pass of Esk Hause.

Geographic entities mentioned:
surface_form: allen crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4661
lon: -3.1802388888889
surface_form: borrowdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.42
lon: -2.665
Ascents. As mentioned Allen Crags is quite often approached along its northern ridge from Glaramara and this is the most popular ascent of the fell. However, a direct climb is possible from Borrowdale ascending the Grains Gill path from Seathwaite to Esk Hause and then climbing easily up the fell from the south.

Geographic entities mentioned:
surface_form: allen crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4661
lon: -3.1802388888889
surface_form: glaramara
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483319444444
lon: -3.1653
Ascents. As mentioned Allen Crags is quite often approached along its northern ridge from Glaramara and this is the most popular ascent of the fell. However, a direct climb is possible from Borrowdale ascending the Grains Gill path from Seathwaite to Esk Hause and then climbing easily up the fell from the south.

Geographic entities mentioned:
surface_form: borrowdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.42
lon: -2.665
Gap Mountain (Alberta). Gap Mountain is a mountain summit located at the southern end of the Opal Range in the Canadian Rockies of Alberta, Canada. The nearest higher neighbor is Elpoca Mountain, to the east. Gap Mountain is situated south of Mount Wintour, within Peter Lougheed Provincial Park. Gap Mountain is a conspicuous peak seen from Alberta Highway 40 at Highwood Pass.

Geographic entities mentioned:
surface_form: Elpoca Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.66676
lon: -115.0187
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Gap Mountain (Alberta). Gap Mountain is a mountain summit located at the southern end of the Opal Range in the Canadian Rockies of Alberta, Canada. The nearest higher neighbor is Elpoca Mountain, to the east. Gap Mountain is situated south of Mount Wintour, within Peter Lougheed Provincial Park. Gap Mountain is a conspicuous peak seen from Alberta Highway 40 at Highwood Pass.

Geographic entities mentioned:
surface_form: Mount Wintour
instance_of: Mountain
countries: Canada
coordinates: lat: 50.70005
lon: -115.0853
surface_form: gap mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.65611111111111
lon: -115.05416666666666
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Gap Mountain (Alberta). Gap Mountain is a mountain summit located at the southern end of the Opal Range in the Canadian Rockies of Alberta, Canada. The nearest higher neighbor is Elpoca Mountain, to the east. Gap Mountain is situated south of Mount Wintour, within Peter Lougheed Provincial Park. Gap Mountain is a conspicuous peak seen from Alberta Highway 40 at Highwood Pass.

Geographic entities mentioned:
surface_form: gap mountain (alberta)
instance_of: Mountain
countries: Canada
coordinates: lat: 50.65611111111111
lon: -115.05416666666666
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Gap Mountain (Alberta). Gap Mountain is a mountain summit located at the southern end of the Opal Range in the Canadian Rockies of Alberta, Canada. The nearest higher neighbor is Elpoca Mountain, to the east. Gap Mountain is situated south of Mount Wintour, within Peter Lougheed Provincial Park. Gap Mountain is a conspicuous peak seen from Alberta Highway 40 at Highwood Pass.

Geographic entities mentioned:
surface_form: gap mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.65611111111111
lon: -115.05416666666666
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The nearest higher neighbor is Elpoca Mountain, to the east. Gap Mountain is situated south of Mount Wintour, within Peter Lougheed Provincial Park. Gap Mountain is a conspicuous peak seen from Alberta Highway 40 at Highwood Pass. It is a popular climbing destination because it offers exposed scrambling on its eastern flanks with excellent summit views of Kananaskis Country. History.

Geographic entities mentioned:
surface_form: gap mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.65611111111111
lon: -115.05416666666666
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The mountain's toponym was officially adopted in 1978 by the Geographical Names Board of Canada. Geology. Gap Mountain is composed of limestone laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Gap Mountain was created during the Lewis Overthrust.

Geographic entities mentioned:
surface_form: gap mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.65611111111111
lon: -115.05416666666666
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Gap Mountain was created during the Lewis Overthrust. The steeply tilted strata are virtually the same in each peak of the Opal Range, with softer layers sandwiched between harder layers. Climate.

Geographic entities mentioned:
surface_form: gap mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.65611111111111
lon: -115.05416666666666
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Gap Mountain was created during the Lewis Overthrust. The steeply tilted strata are virtually the same in each peak of the Opal Range, with softer layers sandwiched between harder layers. Climate. Based on the Köppen climate classification, Gap Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below.

Geographic entities mentioned:
surface_form: gap mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.65611111111111
lon: -115.05416666666666
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Climate. Based on the Köppen climate classification, Gap Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below. June through September offer the most favorable weather to climb or view Gap Mountain. Precipitation runoff from the mountain drains into Pocaterra Creek, a tributary of the Kananaskis River.

Geographic entities mentioned:
surface_form: gap mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.65611111111111
lon: -115.05416666666666
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
History. George Pocaterra named it for its location at the gap between the Opal Range and Elk Range. The mountain's toponym was officially adopted in 1978 by the Geographical Names Board of Canada. Geology. Gap Mountain is composed of limestone laid down during the Precambrian to Jurassic periods.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Climate. Based on the Köppen climate classification, Gap Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below. June through September offer the most favorable weather to climb or view Gap Mountain. Precipitation runoff from the mountain drains into Pocaterra Creek, a tributary of the Kananaskis River.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Benyellary. 0v2a83g1jxnmxw7vv6e3gqa7agn9" xml:space="preserve">#REDIRECT Subsidiary SMC Summits

Geographic entities mentioned:
surface_form: benyellary
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.1241
lon: -4.4874
Mount Golub. Mount Golub is a prominent mountain summit located in the Chilkat Range of the Saint Elias Mountains, in the U.S. state of Alaska. This peak is situated northwest of Juneau, and west of Lynn Canal, on land managed by Tongass National Forest. Although modest in elevation, relief is significant since Mount Golub rises above tidewater in less than two miles.

Geographic entities mentioned:
surface_form: mount golub
instance_of: Mountain
countries: United States
coordinates: lat: 58.465
lon: -135.1739
state of Alaska. This peak is situated northwest of Juneau, and west of Lynn Canal, on land managed by Tongass National Forest. Although modest in elevation, relief is significant since Mount Golub rises above tidewater in less than two miles. The mountain's name was officially adopted in 1972 by the U.S.

Geographic entities mentioned:
surface_form: mount golub
instance_of: Mountain
countries: United States
coordinates: lat: 58.465
lon: -135.1739
Climate. Based on the Köppen climate classification, Mount Golub has a subarctic climate with cold, snowy winters, and cool summers. Weather systems coming off the Gulf of Alaska are forced upwards by the Saint Elias Mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall. Winter temperatures can drop to 0 °F with wind chill factors below −10 °F.

Geographic entities mentioned:
surface_form: mount golub
instance_of: Mountain
countries: United States
coordinates: lat: 58.465
lon: -135.1739
Weather systems coming off the Gulf of Alaska are forced upwards by the Saint Elias Mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall. Winter temperatures can drop to 0 °F with wind chill factors below −10 °F. The month of July offers the most favorable weather for viewing or climbing Mount Golub.

Geographic entities mentioned:
surface_form: mount golub
instance_of: Mountain
countries: United States
coordinates: lat: 58.465
lon: -135.1739
Mount Olivine (Quebec). The Mont Olivine is a mountain in Gaspésie National Park, in the unincorporated territory of Mont-Albert, in the La Haute-Gaspésie Regional County Municipality (MRC), in the region of Gaspésie–Îles-de-la-Madeleine, in Quebec, in Canada. Mount Olivine is one of the Chic-Choc Mountains. Main activities.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mont-albert
instance_of: Mountain
countries: Canada
coordinates: lat: 48.9214
lon: -66.1949
surface_form: mont olivine
instance_of: Mountain
countries: Canada
coordinates: lat: 48.9125
lon: -66.11361111111111
The summit is at. At the top of Mount Olivine, the panorama is splendid. The bare summit allows you to admire the Mount Albert nearby. Mount Olivine is one of the only mountains in the area accessible by snowshoeing in winter. The trailhead starts at the Discovery and Visitors Center of Gaspésie National Park.

Geographic entities mentioned:
surface_form: mount albert
instance_of: Mountain
countries: Canada
coordinates: lat: 48.9214
lon: -66.1949
surface_form: mount albert
instance_of: Mountain
countries: Canada
coordinates: lat: 50.2371
lon: -123.8712
From the third kilometer, very close to the Devil's Fall, the ascent becomes more demanding. After the first big stage of the climb, the hikers arrive at an intersection where the left path leads to the top of Mount Olivine. Along the way, hikers can admire the Mount Albert plateau. The return of the hike is done by doing the reverse route. Toponymy.

Geographic entities mentioned:
surface_form: mount albert
instance_of: Mountain
countries: Canada
coordinates: lat: 48.9214
lon: -66.1949
surface_form: mount albert
instance_of: Mountain
countries: Canada
coordinates: lat: 50.2371
lon: -123.8712
The return of the hike is done by doing the reverse route. Toponymy. The toponym &quot;Mont Olivine&quot; refers to the fact that a prospector found olivine near Mont Albert. Olivine is a green mineral very rich in magnesium, from the group of silicates. The toponym &quot;Mont Olivine&quot; was formalized on February 7, 1989 at the place name bank of the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: mont albert
instance_of: Mountain
countries: Canada
coordinates: lat: 48.9214
lon: -66.1949
surface_form: mont olivine
instance_of: Mountain
countries: Canada
coordinates: lat: 48.9125
lon: -66.11361111111111
Mount Olivine is one of the only mountains in the area accessible by snowshoeing in winter. The trailhead starts at the Discovery and Visitors Center of Gaspésie National Park. Hikers then take the La Grande Traversée trail (westbound), and pay attention to the signs indicating the direction of Mont Olivine. By first following the Sainte-Anne River, the trail turns out to be relatively flat.

Geographic entities mentioned:
surface_form: mont olivine
instance_of: Mountain
countries: Canada
coordinates: lat: 48.9125
lon: -66.11361111111111
The return of the hike is done by doing the reverse route. Toponymy. The toponym &quot;Mont Olivine&quot; refers to the fact that a prospector found olivine near Mont Albert. Olivine is a green mineral very rich in magnesium, from the group of silicates. The toponym &quot;Mont Olivine&quot; was formalized on February 7, 1989 at the place name bank of the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: mont olivine
instance_of: Mountain
countries: Canada
coordinates: lat: 48.9125
lon: -66.11361111111111
Mount Olivine (Quebec). The Mont Olivine is a mountain in Gaspésie National Park, in the unincorporated territory of Mont-Albert, in the La Haute-Gaspésie Regional County Municipality (MRC), in the region of Gaspésie–Îles-de-la-Madeleine, in Quebec, in Canada. Mount Olivine is one of the Chic-Choc Mountains. Main activities.

Geographic entities mentioned:
surface_form: mount olivine (quebec)
instance_of: Mountain
countries: Canada
coordinates: lat: 48.9125
lon: -66.11361111111111
In 1835, the Lake Champlain Transportation Company bought her and converted her into a schooner. Piloted by Captain Thomas Mock, who had on board his wife and three children and overloaded with iron ore, &quot;Water Witch&quot; sank in Lake Champlain during a storm on April 26, 1866. The Mocks′ infant, Roa, was in the cabin, and was lost.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
It is located in the Puno Region, Sandia Province, Patambuco District. It lies northeast of the mountain Rit'ikunka. South of Qaqa Wasi there is a group of small lakes, among them Rit'iqucha (&quot;snow lake&quot;, &quot;Riticocha&quot;) and Yanaqucha (&quot;black lake&quot;, &quot;Yanacocha&quot;). The lake Quchak'uchu is situated in the Rit'ipata valley southeast of the mountain.

Geographic entities mentioned:
surface_form: yanaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -12.8997
lon: -74.1439
surface_form: yanacocha
instance_of: Lake
countries: Peru
coordinates: lat: -12.8997
lon: -74.1439
surface_form: yanaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -10.8611
lon: -75.9903
surface_form: rit'iqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7644
lon: -70.5736
surface_form: riticocha
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7644
lon: -70.5736
surface_form: yanaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -10.04233333
lon: -77.20836111
Qaqa Wasi. Qaqa Wasi or Qaqawasi (Quechua &quot;qaqa&quot; rock, &quot;wasi&quot; house, &quot;rock house&quot;, Hispanicized spelling &quot;Jajahuasi&quot;) is a mountain in the Andes of Peru, about high. It is located in the Puno Region, Sandia Province, Patambuco District. It lies northeast of the mountain Rit'ikunka.

Geographic entities mentioned:
surface_form: qaqa wasi
instance_of: Mountain
countries: Peru
coordinates: lat: -14.3508
lon: -69.7158
Bridge Mountain (Nevada). Bridge Mountain is a mountain located in the Spring Mountain range of southern Nevada. It is located on land managed by the United States Bureau of Land Management as the Red Rock Canyon National Conservation Area, part of the Rainbow Mountain Wilderness. Bridge Mountain is named for the natural feature of a bridge-like natural arch of sandstone near the summit.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1355235
lon: -115.4905643
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.20554
lon: -112.96605
Bridge Mountain (Nevada). Bridge Mountain is a mountain located in the Spring Mountain range of southern Nevada. It is located on land managed by the United States Bureau of Land Management as the Red Rock Canyon National Conservation Area, part of the Rainbow Mountain Wilderness. Bridge Mountain is named for the natural feature of a bridge-like natural arch of sandstone near the summit.

Geographic entities mentioned:
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 63.3090952
lon: -145.6326361
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.73473611111111
lon: -86.72911666666667
surface_form: rainbow mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1080241
lon: -115.4902857
Bridge Mountain (Nevada). Bridge Mountain is a mountain located in the Spring Mountain range of southern Nevada. It is located on land managed by the United States Bureau of Land Management as the Red Rock Canyon National Conservation Area, part of the Rainbow Mountain Wilderness. Bridge Mountain is named for the natural feature of a bridge-like natural arch of sandstone near the summit.

Geographic entities mentioned:
surface_form: bridge mountain (nevada)
instance_of: Mountain
countries: United States
coordinates: lat: 36.1355235
lon: -115.4905643
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.20554
lon: -112.96605
Bridge Mountain is a mountain located in the Spring Mountain range of southern Nevada. It is located on land managed by the United States Bureau of Land Management as the Red Rock Canyon National Conservation Area, part of the Rainbow Mountain Wilderness. Bridge Mountain is named for the natural feature of a bridge-like natural arch of sandstone near the summit. Hiking Route.

Geographic entities mentioned:
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1355235
lon: -115.4905643
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.20554
lon: -112.96605
Bridge Mountain is named for the natural feature of a bridge-like natural arch of sandstone near the summit. Hiking Route. The Bridge Mountain hike begins at the Rocky Gap Summit Trailhead, accessible by 4WD drive only. Hikers can park at the north Willow Springs campground and walk to the summit.

Geographic entities mentioned:
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1355235
lon: -115.4905643
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.20554
lon: -112.96605
Heading south for several hundred feet, one then must climb along a steep, difficult ridge to get near the top. At the top, a small ammunition box contains the peak's sign-in book. In a cleft in the sandstone of Bridge Mountain's summit, there is a small hidden forest of Ponderosa pine. Expansive views of the Las Vegas Valley can be seen from the Eastern end of the hidden forest.

Geographic entities mentioned:
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1355235
lon: -115.4905643
surface_form: bridge mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.20554
lon: -112.96605
A marked trail along the crest descends to the sandstone escarpment. Here, steep free climbing down a chimney—possible without technical gear—takes the hiker to a narrow neck of rock that separates the drainages of Pine Creek to the south and Icebox Canyon to the north.

Geographic entities mentioned:
surface_form: pine creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.08666667
lon: -91.82555556
Besides these transverse depressions (some of them marking lines of ancient interoceanic communication), others were occupied by either more or less extensive lakes, such as the Yagagtoo, Musters, and Colhue Huapi, and others situated to the south of Puerto Deseado in the center of the country.

Geographic entities mentioned:
surface_form: Musters
instance_of: Lake
countries: Argentina
coordinates: lat: -45.41
lon: -69.19
surface_form: Colhue Huapi
instance_of: Group of lakes
countries: Argentina
coordinates: lat: -45.5
lon: -68.75
The Vils has a drainage basin of approximately, with an average annual precipitation of nearly. It originates in the Allgäu Alps in Tyrol from the supplies of the Vilsalpsee, and is its only discharge. Its water flows first in the northern and northwestern directions, in the Reutte district through the Vils Valley and the Tannheim Valley.

Geographic entities mentioned:
surface_form: Vilsalpsee
instance_of: Lake
countries: Austria
coordinates: lat: 47.462777777778
lon: 10.502222222222
On 15 January, the MMS raised the alert level to Class III. The Sir Seewoosagur Ramgoolam International Airport, government offices and schools on the island were closed. Réunion. Gusts of were reported in Saint-Denis, and up to at Maïdo. On the coast, the waves reached almost and the storm surge caused coastal flooding. More than of rain fell on, in the center of the island.

Geographic entities mentioned:
surface_form: Maïdo
instance_of: Mountain
countries: France
coordinates: lat: -21.068889
lon: 55.387778
More than of rain fell on, in the center of the island. From 13 to 16 January, the total rainfall were recorded as follows: at the Commerson Crater, at the Plaine des Palmistes, at Grand-Îlet (Salazie), at Plaine des Cafres, at La Nouvelle (Mafate), and at Cilaos. Near the northern and eastern coast, Le Port recorded, Baril (Saint-Philippe) recorded, and la Possession recorded.

Geographic entities mentioned:
surface_form: Plaine des Cafres
instance_of: Plateau
countries: France
coordinates: lat: -21.2225
lon: 55.555
Lastly, next to the southern city gate is an open space, believed to be the precursor of present-day Kornhamnstorg, the square where ships from the Lake Mälaren region used to deliver corn and iron. Other buildings and surrounding ridges. The turret on the right side of the church and the palace was the Blackfriars monastery, inaugurated in 1343 and demolished in 1547.

Geographic entities mentioned:
surface_form: Lake Mälaren
instance_of: Lake
countries: Sweden
coordinates: lat: 59.5
lon: 17.2