Sarmila/GeoWiki-Features huggingface dataset:
Alma Wagen. Alma Wagen (1878 – December 7, 1967) was an American mountain guide on Mount Rainier. She was the first female guide employed by Mount Rainier National Park. Biography. Wagen was born in 1878 and raised in Mankato, Minnesota.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Wagen became an official member of The Mountaineers in 1913. In 1914, she traveled to Glacier National Park where she &quot;found [her] life's work right in the National Parks&quot; and climbed Mount Rainier for the first time in 1915. She spent the summer of 1916 hiking in Yellowstone National Park and in 1917 she climbed Mount Adams, Mount St. Helens and Mount Hood with the Mountaineers.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Wagen became an official member of The Mountaineers in 1913. In 1914, she traveled to Glacier National Park where she &quot;found [her] life's work right in the National Parks&quot; and climbed Mount Rainier for the first time in 1915. She spent the summer of 1916 hiking in Yellowstone National Park and in 1917 she climbed Mount Adams, Mount St. Helens and Mount Hood with the Mountaineers.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
Lake Placid (Highlands County, Florida). Lake Placid, a gourd-shaped lake, has a surface area of. This lake is south of the city of Lake Placid, Florida; it is just outside the south city limits of the city. This lake was once known as Lake Childs. The area immediately surrounding it is mostly rural, but there are housing developments abutting the lake on part of its west side.

Geographic entities mentioned:
surface_form: lake placid
instance_of: Lake
countries: United States
coordinates: lat: 27.2425
lon: -81.363611111111
surface_form: lake placid
instance_of: Lake
countries: United States
coordinates: lat: 44.312978
lon: -73.993864
Placid View Drive runs along part of the west side and Old State Route 8 runs along part of the east side. Lake Placid provides public access along part of its shore. There are two public boat ramps on shore, one at 150 Harris Drive (on the northeast side) and the other at 3349 Placid View Drive (on the west side of the lake).

Geographic entities mentioned:
surface_form: lake placid
instance_of: Lake
countries: United States
coordinates: lat: 27.2425
lon: -81.363611111111
surface_form: lake placid
instance_of: Lake
countries: United States
coordinates: lat: 44.312978
lon: -73.993864
There are no public swimming areas along the lake shore, but it can be fished from the shore. This lake has a variety of game fish: largemouth bass, catfish, bream, bluegill, redear sunfish, blue catfish, crappie. This lake named Lake Placid is one of several Lake Placids in Florida, as well as other places.

Geographic entities mentioned:
surface_form: lake placid
instance_of: Lake
countries: United States
coordinates: lat: 27.2425
lon: -81.363611111111
surface_form: lake placid
instance_of: Lake
countries: United States
coordinates: lat: 44.312978
lon: -73.993864
It rises in the Kartal Mountains in Gaziantep Province of Turkey, flows south through the city of Afrin in northwest Syria, then reenters Turkey. It joins the Karasu at the site of the former Lake Amik, and its waters flow to the Orontes by a canal. The total length of the river is, of which is in Syria. The source of around a quarter of the river water is in Syria.

Geographic entities mentioned:
surface_form: Lake Amik
instance_of: Lake
countries: Turkey
coordinates: lat: 36.3
lon: 36.3
Peitahigan Lake. Peitahigan Lake is a lake in Meadow Lake Provincial Park in the Canadian Province of Saskatchewan in the boreal forest ecozone of Canada. The lake is one of six notable lakes in the Rusty Creek watershed. The other lakes include Rusty, First Mustus, Second Mustus, Third Mustus, and Fourth Mustus. Rusty Creek and the lakes are part of the Waterhen River drainage basin.

Geographic entities mentioned:
surface_form: Rusty Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.40019
lon: -108.73479
Peitahigan Lake. Peitahigan Lake is a lake in Meadow Lake Provincial Park in the Canadian Province of Saskatchewan in the boreal forest ecozone of Canada. The lake is one of six notable lakes in the Rusty Creek watershed. The other lakes include Rusty, First Mustus, Second Mustus, Third Mustus, and Fourth Mustus. Rusty Creek and the lakes are part of the Waterhen River drainage basin.

Geographic entities mentioned:
surface_form: Rusty
instance_of: Lake
countries: Canada
coordinates: lat: 54.41676
lon: -108.76741
surface_form: First Mustus
instance_of: Lake
countries: Canada
coordinates: lat: 54.43343
lon: -108.81742
Rusty Creek and the lakes are part of the Waterhen River drainage basin. The Waterhen River is a tributary of the Beaver River, which flows north into Lac Île-à-la-Crosse and the Churchill River, a major tributary in the Hudson Bay drainage basin. Several streams feed into Peitahigan Lake, including ones that drain the southern slopes of the Mostoos Hills.

Geographic entities mentioned:
surface_form: Lac Île-à-la-Crosse
instance_of: Lake
countries: Canada
coordinates: lat: 55.4444
lon: -107.849
Peitahigan Lake. Peitahigan Lake is a lake in Meadow Lake Provincial Park in the Canadian Province of Saskatchewan in the boreal forest ecozone of Canada. The lake is one of six notable lakes in the Rusty Creek watershed. The other lakes include Rusty, First Mustus, Second Mustus, Third Mustus, and Fourth Mustus. Rusty Creek and the lakes are part of the Waterhen River drainage basin.

Geographic entities mentioned:
surface_form: meadow lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.1168
lon: -108.334
surface_form: peitahigan lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.45009
lon: -108.95077
surface_form: meadow lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.8333
lon: -108.167
Peitahigan Lake. Peitahigan Lake is a lake in Meadow Lake Provincial Park in the Canadian Province of Saskatchewan in the boreal forest ecozone of Canada. The lake is one of six notable lakes in the Rusty Creek watershed. The other lakes include Rusty, First Mustus, Second Mustus, Third Mustus, and Fourth Mustus. Rusty Creek and the lakes are part of the Waterhen River drainage basin.

Geographic entities mentioned:
surface_form: peitahigan lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.45009
lon: -108.95077
The Waterhen River is a tributary of the Beaver River, which flows north into Lac Île-à-la-Crosse and the Churchill River, a major tributary in the Hudson Bay drainage basin. Several streams feed into Peitahigan Lake, including ones that drain the southern slopes of the Mostoos Hills. The outflow is a short east-flowing creek that flows into Third Mustus Lake.

Geographic entities mentioned:
surface_form: peitahigan lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.45009
lon: -108.95077
The outflow is a short east-flowing creek that flows into Third Mustus Lake. Access to the lake is via a gravel road that runs along the west side of the lake that connects up with Highway 224 south of Peitahigan Lake. An 11-kilometre section of the Boreal Trail goes around the lake and over by the Mustus Lakes. Fish species.

Geographic entities mentioned:
surface_form: peitahigan lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.45009
lon: -108.95077
The other lakes include Rusty, First Mustus, Second Mustus, Third Mustus, and Fourth Mustus. Rusty Creek and the lakes are part of the Waterhen River drainage basin. The Waterhen River is a tributary of the Beaver River, which flows north into Lac Île-à-la-Crosse and the Churchill River, a major tributary in the Hudson Bay drainage basin.

Geographic entities mentioned:
surface_form: rusty creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.40019
lon: -108.73479
After being informed of the practice, acoustician and ' (university educator) at the École pratique des hautes études, documented the whistled language in 1950. The natural use of the language in the Ossau Valley ceased toward the end of the 20th century as the agricultural lifestyle disappeared along with the passing of the final remaining goatherds who used the language.

Geographic entities mentioned:
surface_form: Ossau Valley
instance_of: Valley
countries: France
coordinates: lat: 42.983333333333
lon: -0.41666666666667
Hamarøyskaftet. Hamarøyskaftet is a mountain in Hamarøy Municipality in Nordland county, Norway. The mountain is a characteristic landmark of the region. It is located about west of the villages of Oppeid and Presteid and about north of the village of Skutvika. The mountain was first ascended by Martin Hoff Ekroll in 1885.

Geographic entities mentioned:
surface_form: hamarøyskaftet
instance_of: Mountain
countries: Norway
coordinates: lat: 68.0807
lon: 15.40497
It is located about west of the villages of Oppeid and Presteid and about north of the village of Skutvika. The mountain was first ascended by Martin Hoff Ekroll in 1885. The normal route to the peak is described as technically easy, with some exposed parts. In 1998, Hamarøyskaftet was featured on a Norwegian postage stamp (&quot;NK 1333&quot; with a value of).

Geographic entities mentioned:
surface_form: hamarøyskaftet
instance_of: Mountain
countries: Norway
coordinates: lat: 68.0807
lon: 15.40497
Alluaud's haplo. Alluaud's haplo (&quot;Astatoreochromis alluaudi&quot;) is a species of freshwater fish in the cichlid family, Cichlidae. It is native to East Africa, where it occurs in many lakes, including Lake Victoria. This fish reaches about 19 centimeters in maximum length. It lives in swampy waters. It is omnivorous and is utilized to control snails.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Mount Blaurock. Mount Blaurock is a high mountain summit of the Collegiate Peaks in the Sawatch Range of the Rocky Mountains of North America. The thirteener is located in San Isabel National Forest, northwest by west (bearing 307°) of the Town of Buena Vista in Chaffee County, Colorado, United States.

Geographic entities mentioned:
surface_form: Collegiate Peaks
instance_of: Landform
countries: United States
coordinates: lat: 38.9244
lon: -106.321
surface_form: mount blaurock
instance_of: Mountain
countries: United States
coordinates: lat: 39.0111
lon: -106.454
surface_form: high mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0887
lon: -74.2351
Mount Blaurock. Mount Blaurock is a high mountain summit of the Collegiate Peaks in the Sawatch Range of the Rocky Mountains of North America. The thirteener is located in San Isabel National Forest, northwest by west (bearing 307°) of the Town of Buena Vista in Chaffee County, Colorado, United States.

Geographic entities mentioned:
surface_form: mount blaurock
instance_of: Mountain
countries: United States
coordinates: lat: 39.0111
lon: -106.454
The thirteener is located in San Isabel National Forest, northwest by west (bearing 307°) of the Town of Buena Vista in Chaffee County, Colorado, United States. Mount Blaurock was named in honor of Carl Blaurock, a co-founder of the Colorado Mountain Club and one of the first two persons to climb all of Colorado's fourteeners.

Geographic entities mentioned:
surface_form: mount blaurock
instance_of: Mountain
countries: United States
coordinates: lat: 39.0111
lon: -106.454
Dumoulin made a late selection in stage 3, joining nine other riders who finished just ahead of the rest of the peloton, and won the sprint to the finish line. Later in February, Moncoutié won the queen stage of the Tour Méditerranéen, finishing at Mont Faron. He had previously won stages there in 2003 and 2009, but his win this year was enough to win him the race overall thanks to his time gap.

Geographic entities mentioned:
surface_form: Mont Faron
instance_of: Mountain
countries: France
coordinates: lat: 43.149444444444
lon: 5.9511111111111
Taaramäe, Dumoulin, El Fares, and Vogondy were also named to the squad. Taaramäe finished near the front of the race on stage 1 atop the short Mont des Alouettes hill. He was distanced by stage winner Philippe Gilbert and eventual Tour de France winner Cadel Evans, but finished with the main front group six seconds back for eighth on the day.

Geographic entities mentioned:
surface_form: Mont des Alouettes
instance_of: Mountain
countries: France
coordinates: lat: 46.894722222222
lon: -1.0102777777778
Moncoutié all but clinched his mountains classification triumph on stage 15. While he finished nine minutes behind Cobo on Angliru, he won the day's second climb to score ten mountain points and increase his lead over Montaguti to 22 points. He scored his final mountain classification points on stage 17, ending with a total of 63.

Geographic entities mentioned:
surface_form: Angliru
instance_of: Mountain
countries: Spain
coordinates: lat: 43.221389
lon: -5.942222
La Gaiba lake. aebw62ki9xlepk54m88kpuzxltq3" xml:space="preserve">#REDIRECT La Gaiba Lake

Geographic entities mentioned:
surface_form: gaiba
instance_of: Lake
countries: Bolivia
Brazil
coordinates: lat: -17.772222222222
lon: -57.720277777778
surface_form: la gaiba lake
instance_of: Lake
countries: Bolivia
Brazil
coordinates: lat: -17.772222222222
lon: -57.720277777778
The context is unclear but it is likely that this is the same Gille Coemgáin, connected to Kenneth III. Kenneth III was killed in battle at Monzievaird in Strathearn by King Malcolm II (Máel Coluim mac Cináeda), which took place about 25 March 1005. Whether Boite mac Cináeda was a son of this Kenneth, or of Kenneth II, is uncertain, although most propose this Kenneth.

Geographic entities mentioned:
surface_form: Strathearn
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.3325
lon: -3.6825
As the fifth Mughal emperor, his reign marked the zenith of Mughal architectural and cultural achievements. The third son of Jahangir (), Shah Jahan participated in the military campaigns against the Sisodia Rajputs of Mewar and the rebel Lodi nobles of the Deccan.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
In 1616, on Khurram's departure to Deccan, Jahangir awarded him the title Shah Sultan Khurram. In 1617, Khurram was directed to deal with the Lodis in the Deccan to secure the Empire's southern borders and to restore imperial control over the region.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Fung Mei Wai. Fung Mei Wai (), formerly Kau Shi Wai (, literally &quot;dog shit walled (village)&quot;), is a village in Fung Yuen, Tai Po, Hong Kong. Administration. Fung Mei Wai is one of the villages represented within the Tai Po Rural Committee. For electoral purposes, Fung Mei Wai is part of the Hong Lok Yuen constituency, which was formerly represented by Zero Yiu Yeuk-sang until May 2021.

Geographic entities mentioned:
surface_form: Fung Yuen
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 22.46163
lon: 114.18049
The plant is well-known but had been misidentified. It is native to the Great Basin and Colorado Plateau of the western United States (Colorado, Utah, Arizona, Nevada, California), where it grows in warmer, drier habitat than most related orchids. &quot;Platanthera tescamnis&quot; produces a slender, erect flowering stem which may exceed in height.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
It is in the centre of the Skiddaw Group SSSI. Topography. Skiddaw and Blencathra are the best known of the Northern Fells, fronting the range as they loom above Keswick and the road to Penrith. Behind this wall is a further group of fells, commonly referred to as Back o' Skiddaw. This group is centred upon Knott and Great Calva is its southernmost top.

Geographic entities mentioned:
surface_form: Skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: Blencathra
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.63985
lon: -3.0504611111111
Behind this wall is a further group of fells, commonly referred to as Back o' Skiddaw. This group is centred upon Knott and Great Calva is its southernmost top. To the south of Great Calva – at the centre of the Northern Fells – is Skiddaw Forest, a marshy upland area at around surrounded on all sides by higher fells.

Geographic entities mentioned:
surface_form: Knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
surface_form: great calva
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.669
lon: -3.102
Little Calva sends out a further descending ridge to the north west, running alongside Dash Beck. A series of spurs named Black Nettle Hause, Little Nettle Hause and White Hause drop toward the river. Between Black Nettle Hause and Birkett Edge on Bakestall the beck reaches Whitewater Dash, a fine series of waterfalls. Summit.

Geographic entities mentioned:
surface_form: Bakestall
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.666
lon: -3.13952
There is some rock in evidence but grass and heather predominate. The view southward, particularly from the lower cairn is unexpectedly good. Looking directly down the Glenderaterra Valley and the Vale of St John, the gap gives an unimpeded view as far as Loughrigg and Steel Fell. Additionally above the flanks of Lonscale Fell Great Gable and the Scafells appear.

Geographic entities mentioned:
surface_form: Steel Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4915
lon: -3.05283
Looking directly down the Glenderaterra Valley and the Vale of St John, the gap gives an unimpeded view as far as Loughrigg and Steel Fell. Additionally above the flanks of Lonscale Fell Great Gable and the Scafells appear. The nearer fells by contrast turn their backs upon Great Calva, the northward vista being less inspiring. Ascents.

Geographic entities mentioned:
surface_form: Lonscale Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.634838888889
lon: -3.1092111111111
surface_form: Great Gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
As a result, it is distant from roads and quite remote by Lakeland standards. Great Calva stands at the head of a major geological fault running through the centre of the Lake District, and so from the summit it is possible to see all the way south over Thirlmere. The subsidiary summit of Little Calva lies to the west. It is in the centre of the Skiddaw Group SSSI. Topography.

Geographic entities mentioned:
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
It is in the centre of the Skiddaw Group SSSI. Topography. Skiddaw and Blencathra are the best known of the Northern Fells, fronting the range as they loom above Keswick and the road to Penrith. Behind this wall is a further group of fells, commonly referred to as Back o' Skiddaw. This group is centred upon Knott and Great Calva is its southernmost top.

Geographic entities mentioned:
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
This group is centred upon Knott and Great Calva is its southernmost top. To the south of Great Calva – at the centre of the Northern Fells – is Skiddaw Forest, a marshy upland area at around surrounded on all sides by higher fells. Three streams flow from Skiddaw Forest, dividing the Northern Fells into three sectors.

Geographic entities mentioned:
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: great calva
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.669
lon: -3.102
To the south of Great Calva – at the centre of the Northern Fells – is Skiddaw Forest, a marshy upland area at around surrounded on all sides by higher fells. Three streams flow from Skiddaw Forest, dividing the Northern Fells into three sectors. Dash Beck runs north west, the River Caldew north east and the River Glenderaterra south.

Geographic entities mentioned:
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
Dash Beck runs north west, the River Caldew north east and the River Glenderaterra south. The three groups of fells can conveniently be thought of as the Skiddaw massif, the Blencathra group and Back O'Skiddaw. The single building in Skiddaw Forest is Skiddaw House which has variously seen service as a shepherds' bothy and a Youth Hostel.

Geographic entities mentioned:
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: blencathra
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.63985
lon: -3.0504611111111
The three groups of fells can conveniently be thought of as the Skiddaw massif, the Blencathra group and Back O'Skiddaw. The single building in Skiddaw Forest is Skiddaw House which has variously seen service as a shepherds' bothy and a Youth Hostel. Great Calva appears from Skiddaw Forest as a steep sided pyramid, clad predominantly in heather.

Geographic entities mentioned:
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
The single building in Skiddaw Forest is Skiddaw House which has variously seen service as a shepherds' bothy and a Youth Hostel. Great Calva appears from Skiddaw Forest as a steep sided pyramid, clad predominantly in heather. The summit is a curving ridge long, with Great Calva at the eastern end and Little Calva to the west. The ridge itself is extremely wet underfoot.

Geographic entities mentioned:
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: great calva
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.669
lon: -3.102
Great Calva has a prominent southern spur, around which the Caldew flows before steering north east for the Eden Valley. In a strict topographical sense Candleseaves Bog is the connection between Great Calva and Skiddaw, but it could hardly be described as a ridge route. Running north east from Little Calva is a ridge which drops to a col at, before rising up the flanks of Knott.

Geographic entities mentioned:
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: great calva
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.669
lon: -3.102
Ascents. Great Calva is mainly covered in heather, which makes walking relatively difficult. Approaching from the northwest, one can take the bridleway between Great Cockup and Little Calva from Orthwaite to reach the col between Knott and the summit. Alternatively, Great Calva can be climbed up the pathless south ridge from Skiddaw Forest, which creates a number of options for starting points.

Geographic entities mentioned:
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: great calva
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.669
lon: -3.102
Alternatively, Great Calva can be climbed up the pathless south ridge from Skiddaw Forest, which creates a number of options for starting points. The Skiddaw House supply road follows Dash Beck up from Peter House Farm, or a good track runs alongside the Caldew from the road at Mosedale.

Geographic entities mentioned:
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
In a strict topographical sense Candleseaves Bog is the connection between Great Calva and Skiddaw, but it could hardly be described as a ridge route. Running north east from Little Calva is a ridge which drops to a col at, before rising up the flanks of Knott. There are a couple of small tarns on the Great Calva side of the depression.

Geographic entities mentioned:
surface_form: knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
Ascents. Great Calva is mainly covered in heather, which makes walking relatively difficult. Approaching from the northwest, one can take the bridleway between Great Cockup and Little Calva from Orthwaite to reach the col between Knott and the summit. Alternatively, Great Calva can be climbed up the pathless south ridge from Skiddaw Forest, which creates a number of options for starting points.

Geographic entities mentioned:
surface_form: knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
surface_form: great cockup
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6895
lon: -3.12931
Great Calva. Great Calva is a fell in the Lake District, England. It is in the Northern Fells, lying roughly at the centre of this region of high ground. As a result, it is distant from roads and quite remote by Lakeland standards.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: great calva
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.669
lon: -3.102
As a result, it is distant from roads and quite remote by Lakeland standards. Great Calva stands at the head of a major geological fault running through the centre of the Lake District, and so from the summit it is possible to see all the way south over Thirlmere. The subsidiary summit of Little Calva lies to the west. It is in the centre of the Skiddaw Group SSSI. Topography.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: great calva
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.669
lon: -3.102
Great Calva. Great Calva is a fell in the Lake District, England. It is in the Northern Fells, lying roughly at the centre of this region of high ground. As a result, it is distant from roads and quite remote by Lakeland standards.

Geographic entities mentioned:
surface_form: great calva
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.669
lon: -3.102
The single building in Skiddaw Forest is Skiddaw House which has variously seen service as a shepherds' bothy and a Youth Hostel. Great Calva appears from Skiddaw Forest as a steep sided pyramid, clad predominantly in heather. The summit is a curving ridge long, with Great Calva at the eastern end and Little Calva to the west. The ridge itself is extremely wet underfoot.

Geographic entities mentioned:
surface_form: great calva
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.669
lon: -3.102
From between the two tops, Dead Beck runs down into Candleseaves Bog, the source of both the Caldew and Dash Beck. Great Calva has a prominent southern spur, around which the Caldew flows before steering north east for the Eden Valley. In a strict topographical sense Candleseaves Bog is the connection between Great Calva and Skiddaw, but it could hardly be described as a ridge route.

Geographic entities mentioned:
surface_form: great calva
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.669
lon: -3.102
Running north east from Little Calva is a ridge which drops to a col at, before rising up the flanks of Knott. There are a couple of small tarns on the Great Calva side of the depression. From the col Wiley Gill runs south east to join the Caldew and Hause Gill flows westward to Dash Beck. Little Calva sends out a further descending ridge to the north west, running alongside Dash Beck.

Geographic entities mentioned:
surface_form: great calva
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.669
lon: -3.102
Looking directly down the Glenderaterra Valley and the Vale of St John, the gap gives an unimpeded view as far as Loughrigg and Steel Fell. Additionally above the flanks of Lonscale Fell Great Gable and the Scafells appear. The nearer fells by contrast turn their backs upon Great Calva, the northward vista being less inspiring. Ascents.

Geographic entities mentioned:
surface_form: great calva
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.669
lon: -3.102
The nearer fells by contrast turn their backs upon Great Calva, the northward vista being less inspiring. Ascents. Great Calva is mainly covered in heather, which makes walking relatively difficult. Approaching from the northwest, one can take the bridleway between Great Cockup and Little Calva from Orthwaite to reach the col between Knott and the summit.

Geographic entities mentioned:
surface_form: great calva
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.669
lon: -3.102
Zharen. Zharen, also Zaring or Zharencun () is a small town and township-level division of Amdo County in the Nagqu Prefecture of the Tibet Autonomous Region, in China. It is located at the side of the G109 road, south of Amdo Town on the road from Nagchu Town, and approximately east of the southern tip of Cona Lake. It has a population of 7875, living in 1479 households. History.

Geographic entities mentioned:
surface_form: Cona Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 32.0167
lon: 91.4667
TRAX (light rail). TRAX is a light rail system in the Salt Lake Valley of Utah, in the United States, serving Salt Lake City and many of its suburbs throughout Salt Lake County. The system's official name, Transit Express, is rarely, if ever, used. The system is operated by the Utah Transit Authority (UTA). All TRAX trains are electric, receiving power from overhead wires.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
Other plans. In conjunction with the Mountain View Corridor project, plans were made by UTA to build a new TRAX line on the west side of the Salt Lake Valley along 5600 West (in the same general area as the Mountain View Corridor). The proposed line however hasn't gone through any studies, and isn't currently in UTA's future planning documents anymore.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
The &quot;Dauphins&quot; also held, in addition to the southwestern slopes of the range (Briançon and Queyras, now on the French side), the upper part of some of the valleys that were tributaries of the Po River (Valle di Susa, Chisone valley, Varaita Valley). The Alpine territory of Dauphiné, known as &quot;Escartons&quot;, used to have a limited autonomy and elected its own parliament.

Geographic entities mentioned:
surface_form: Varaita Valley
instance_of: Valley
countries: Italy
coordinates: lat: 44.58
lon: 7.1
Both mountains are the highest in their respective mountain ranges. Huascarán is the highest point in Peru. The city gets little to no precipitation; however, thick fog predominates through the months of May to November, usually overnight. Rainfall usually comes in February. Population. A large number of people migrated to Chimbote in the early 1970s.

Geographic entities mentioned:
surface_form: Huascarán
instance_of: Mountain
countries: Peru
coordinates: lat: -9.1166666666667
lon: -77.6
The axis of development moved from the Pima cotton, sugarcane, and rice plantations to the large city. In addition, Chimbote was a natural exit channel for the exports of the Santa valley, and a starting point for the entry to the Callejón de Huaylas. The Peruvian anchoveta boom created wealth in the city, but it soon ended due to indiscriminate fishing that overwhelmed the bio-mass.

Geographic entities mentioned:
surface_form: Callejón de Huaylas
instance_of: Valley
countries: Peru
coordinates: lat: -9.2666666666667
lon: -77.116666666667
Hamilton Incline Railway. The Mount Hamilton Incline Railway was a funicular railway in Hamilton, Ontario, Canada, climbing the Niagara Escarpment. It opened August 26, 1895 in Hamilton, Ontario. It was the second Hamilton furnicular, after the Hamilton and Barton.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
Of the rest of the land, 0.8% is settled (buildings or roads) and the remainder (35.4%) is non-productive (rivers, glaciers or mountains). The former municipality was the capital of the Safien sub-district of the Surselva district in the mid and upper Safien valley. The only other municipality in the sub-district was Tenna, which occupied the lower Safien valley.

Geographic entities mentioned:
surface_form: Safien valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.696666666667
lon: 9.3244444444444
The only other municipality in the sub-district was Tenna, which occupied the lower Safien valley. The valley is drained by the Rabiusa river. The former municipality consists of the village of Safien-Platz (elevation:) and scattered hamlets and single farm houses throughout the valley. Coat of arms.

Geographic entities mentioned:
surface_form: Rabiusa
instance_of: Watercourse
countries: Switzerland
coordinates: lat: 46.8044
lon: 9.33028
Shire of Yarrawonga. The Shire of Yarrawonga was a local government area on the Murray River, in the Goulburn Valley region, about northeast of Melbourne, the state capital of Victoria, Australia. The shire covered an area of, and existed from 1891 until 1994. History. Yarrawonga was once part of the vast Echuca Road District, which formed in 1864 and becoming a shire in 1871.

Geographic entities mentioned:
surface_form: Goulburn Valley
instance_of: Valley
countries: Australia
coordinates: lat: -36.3831
lon: 145.399
To protect their expansive holdings, the family built Clanx Castle in Appenzell, Hohensax Castle in Sennwald and Mesocco Castle in Mesocco in Graubünden. In 1220, they expanded their southern holdings into the Leventina and Blenio Valleys. The next 28 years marked a high point in the family's power. In 1248, the family holdings were divided between two of Heinrich's grandsons.

Geographic entities mentioned:
surface_form: Blenio Valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.427563888889
lon: 8.9698222222222
After the decline of the imperial Hohenstaufen family the Sax-Misox lost the Blenio Valley, Monte Dongo and Clanx Castle. Their lands were reduced to the Core of the Misox Valley with the San Bernardino Pass and the Walser settlements in the Rheinwald Valley. The distant estate at Arth was granted as a fief to Heinrich and Albrecht von Grünenfels in 1295.

Geographic entities mentioned:
surface_form: Rheinwald
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.551778
lon: 9.319788
In the peace treaty they returned the ruins of Hohensax and the village of Gams, but retained Frischenberg Castle and the village of Sax. The son of Albert and Ursula, Ulrich of Hohensax (1463–1538) consolidated the family lands in the Rhine valley and the Thurgau and was the mayor of Zurich. During the Burgundian Wars, he fought on the side of Zurich and was knighted.

Geographic entities mentioned:
surface_form: Rhine valley
instance_of: Valley
countries: Switzerland
Austria
Liechtenstein
coordinates: lat: 47.07013888888889
lon: 9.483347222222223
The Yangtze Plain starts east of Yichang (Hubei province), China. The Middle Yangtze Plain is made up of parts of the north-eastern and south-eastern Hunan, Hubei, and north-central Jiangxi provinces, and includes the Dongting, Poyang, and Hong lakes. The Middle-Lower Yangtze Plain stretches eastward from Mount Wu to the coast.

Geographic entities mentioned:
surface_form: Dongting
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.316666666667
lon: 112.95
The town is home to the Vaughn Memorial Cemetery which was adjacent to the Double Branch Baptist Church until the church burned down in the late 2000s. The surrounding area consists primarily of farmland and forest situated in the Poteau River Valley region between Sugar Loaf Mountain, Oklahoma Peak, and Cavanal Hill with a tributary of the Poteau River, Nail Creek running through Gilmore.

Geographic entities mentioned:
surface_form: Cavanal Hill
instance_of: Mountain
countries: United States
coordinates: lat: 35.070833333333
lon: -94.679444444444
Rauher Jakob. The Rauher Jakob (literally &quot;Rough James&quot;) is a hilltop between Tanne and Elend in the Harz mountains of central Germany. It is 568.6 metres above sea level. In the vicinity are the sources of the Spielbach and Allerbach, two tributary streams of the Warme Bode. The Ramsenhöhe is a sub-peak of the Rauher Jakob with a height of 565 metres AMSL.

Geographic entities mentioned:
surface_form: rauher jakob
instance_of: Mountain
countries: Germany
coordinates: lat: 51.723486111111
lon: 10.702916666667
Alabama State Route 77 passes through the southern section of Attalla, leading north to US 431 and southeast to Rainbow City. According to the U.S. Census Bureau, the city has a total area of, all of it land. Big Wills Creek, a tributary of the Coosa River, flows southeasterly through the city. The southern end of Lookout Mountain rises to the east overlooking the city. 2000 census.

Geographic entities mentioned:
surface_form: Coosa River
instance_of: Watercourse
countries: United States
coordinates: lat: 32.4862464
lon: -86.2777475
According to the U.S. Census Bureau, the city has a total area of, all of it land. Big Wills Creek, a tributary of the Coosa River, flows southeasterly through the city. The southern end of Lookout Mountain rises to the east overlooking the city. 2000 census. At the 2000 census there were 6,795 people, 2,672 households, and 1,976 families living in the city. The population density was.

Geographic entities mentioned:
surface_form: Lookout Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.863713888889
lon: -85.392452777778
The North Butte's volume is 0.16 cubic miles (0.70 cubic km) and the South Butte measures at 0.07 cubic miles (0.30 cubic km). In comparison, the better known tuff cone Diamond Head on Oahu has a volume of 0.15 cubic miles (0.6 cubic km). The larger buttes in the Menan Complex are asymmetrical.

Geographic entities mentioned:
surface_form: Diamond Head
instance_of: Mountain
countries: United States
coordinates: lat: 21.259722222222
lon: -157.81175
surface_form: diamond head
instance_of: Mountain
countries: United States
coordinates: lat: 21.259722222222
lon: -157.81175
The larger buttes in the Menan Complex are asymmetrical. Each has a greater accumulation of material on the northeast, presumably due to strong southwest winds during the initial eruption. The Menan Buttes are located in Madison County, with lower slopes extending westward into Jefferson County. Nearby communities include Menan, Rigby, Rexburg and Idaho Falls, Idaho.

Geographic entities mentioned:
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
Menan Buttes. The North and South Menan Buttes in southeastern Idaho are two of the world's largest volcanic tuff cones. The two cones, with four smaller associated cones, align along a north-northwest line and comprise the Menan Complex.

Geographic entities mentioned:
surface_form: menan buttes
instance_of: Mountain
countries: United States
coordinates: lat: 43.7844
lon: -111.973
The US Bureau of Land Management designated the North Butte as an Area of Critical Environmental Concern (ACEC). The volcanoes forming the two major Menan Buttes were created when basaltic magma came into contact with a shallow aquifer or with the precursor of the modern Snake River.

Geographic entities mentioned:
surface_form: menan buttes
instance_of: Mountain
countries: United States
coordinates: lat: 43.7844
lon: -111.973
state of Washington. Course. For most of its length Goodell Creek flows through North Cascades National Park. It originates in the Picket Range of the North Cascades. Its headwaters drain the south and west sides of the high peaks around Mount Fury and the eastern slope of Mount Crowder. The creek flows generally south collecting the waters of numerous tributaries, many of which are glacial fed.

Geographic entities mentioned:
surface_form: Mount Fury
instance_of: Mountain
countries: United States
coordinates: lat: 48.8122
lon: -121.323
Crescent Creek drains the southwestern slopes of Mount Terror, then flows west to join Goodell Creek. Below the Crescent Creek confluence Goodell Creek turns to the southeast, collecting tributaries draining Mount Despair and Mount Triumph to the west. Terror Creek, which drains the southern slopes of Mount Terror, joins Goodell Creek from the north.

Geographic entities mentioned:
surface_form: Mount Triumph
instance_of: Mountain
countries: United States
coordinates: lat: 48.7065
lon: -121.355
Terror Creek, which drains the southern slopes of Mount Terror, joins Goodell Creek from the north. In its last reach Goodell Creek passes between Trappers Peak to the west and Mount Ross to the east. The creek then enters Ross Lake National Recreation Area and empties into the Skagit River near Newhalem.

Geographic entities mentioned:
surface_form: Trappers Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.68846
lon: -121.32179
surface_form: Mount Ross
instance_of: Mountain
countries: United States
coordinates: lat: 48.709258
lon: -121.244946
Hoyleton, South Australia. Hoyleton (formerly Hoyle's Plains) is a former railway town in South Australia, west of the Clare Valley, halfway between Leasingham and Halbury. Hoyle's Plains was the original terminus of the Port Wakefield railway line. This was constructed in 1869 as a horse-drawn tramway to assist farmers on the newly settled Hoyles Plains to get their grain to the port.

Geographic entities mentioned:
surface_form: Clare Valley
instance_of: Valley
countries: Australia
coordinates: lat: -33.83361111
lon: 138.61
Läckö Castle. Läckö Castle (Swedish: &quot;Läckö Slott&quot;) is a medieval castle in Sweden, located on Kållandsö island on Lake Vänern, 25 kilometers north of Lidköping in Västergötland, Sweden. History. Brynolf Algotsson, Bishop of the Diocese of Skara, laid the foundations for a fortified castle in 1298 originally as a fort that consisted of two or three houses surrounded by a wall.

Geographic entities mentioned:
surface_form: Vänern
instance_of: Lake
countries: Sweden
coordinates: lat: 58.916666666667
lon: 13.5
The ridge is located at the north side of Van Keulenfjorden. It has a length of about eight kilometers, and its highest peak is 904 m.a.s.l. The ridge is named after French paleontologist Adolphe-Théodore Brongniart. First known ascent dates from 1920. The valley of Wittrockdalen separates Brogniartfjella from Wittrockfjellet.

Geographic entities mentioned:
surface_form: Wittrockfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 77.607
lon: 15.796
surface_form: brogniartfjella
instance_of: Mountain
countries: Norway
coordinates: lat: 77.575
lon: 15.881
Brogniartfjella. Brogniartfjella is a mountain ridge in Nathorst Land at Spitsbergen, Svalbard. The ridge is located at the north side of Van Keulenfjorden. It has a length of about eight kilometers, and its highest peak is 904 m.a.s.l. The ridge is named after French paleontologist Adolphe-Théodore Brongniart. First known ascent dates from 1920.

Geographic entities mentioned:
surface_form: brogniartfjella
instance_of: Mountain
countries: Norway
coordinates: lat: 77.575
lon: 15.881
The Rhône divides into the &quot;Grand Rhône&quot; and &quot;Petit Rhône&quot; south of Arles; the area between forms the Camargue. The principal mountains of the department are the Sainte-Baume massif (1,042 metres – 3,418 feet), Montagne Sainte-Victoire (1,011 metres – 3,316 feet), the Garlaban and Alpilles massifs. Seismic activity.

Geographic entities mentioned:
surface_form: Garlaban
instance_of: Mountain
countries: France
coordinates: lat: 43.331388888889
lon: 5.5536111111111
Zushan Mountain. Zushan Mountain () is a mountain in Qinglong, China. It is around two hours drive from Qinhuangdao in Hebei province. The main peak, the Heavenly Goddess Peak, has an elevation of.

Geographic entities mentioned:
surface_form: zushan mountain
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 40.14173
lon: 119.45134
The Central Volcanic Zone spans Peru, Bolivia, Chile and Argentina and includes 44 active volcanoes as well as the Altiplano–Puna volcanic complex, a system of large calderas and ignimbrites of which Purico is a member. Licancabur to the north, La Pacana southeast and Guayaques to the east are separate volcanic systems.

Geographic entities mentioned:
surface_form: La Pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: Guayaques
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.898083333333332
lon: -67.56777777777778
Regional. Licancabur volcano was constructed on ignimbrites from Purico just north of the complex. Guayaques lies east of Purico, the La Pacana caldera is located southeast of the complex, and La Pacana's Filo Delgado ignimbrite has buried part of the Purico ignimbrite. The known volcanoes Lascár and El Tatio are found at larger distances from Purico.

Geographic entities mentioned:
surface_form: Guayaques
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.898083333333332
lon: -67.56777777777778
surface_form: La Pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
Regional. Licancabur volcano was constructed on ignimbrites from Purico just north of the complex. Guayaques lies east of Purico, the La Pacana caldera is located southeast of the complex, and La Pacana's Filo Delgado ignimbrite has buried part of the Purico ignimbrite. The known volcanoes Lascár and El Tatio are found at larger distances from Purico.

Geographic entities mentioned:
surface_form: El Tatio
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -22.331388888889
lon: -68.010277777778
The CVZ segment includes 44 active systems, 18 minor volcanic centres and over 6 large ignimbrite or caldera systems. One of these volcanoes, Ojos del Salado, is the highest volcano in the world. The largest historical eruption in the CVZ occurred in 1600 at Huaynaputina in Peru while Lascár is its most active member, with a major eruption in 1993. Local.

Geographic entities mentioned:
surface_form: Ojos del Salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
The CVZ segment includes 44 active systems, 18 minor volcanic centres and over 6 large ignimbrite or caldera systems. One of these volcanoes, Ojos del Salado, is the highest volcano in the world. The largest historical eruption in the CVZ occurred in 1600 at Huaynaputina in Peru while Lascár is its most active member, with a major eruption in 1993. Local.

Geographic entities mentioned:
surface_form: Huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223