Sarmila/GeoWiki-Features huggingface dataset:
Müggelberge. The Müggelberge (also formerly called the &quot;Müggelsberge&quot;;) are a wooded line of hills with heights up to in the southeast of Berlin's Treptow-Köpenick quarter. They are dominated by the Kleiner Müggelberg (88.3 m) and Großer Müggelberg (114.7 m). The &quot;Müggelberge&quot; cover an area of around seven square kilometres. The ridge was formed during the ice age.

Geographic entities mentioned:
surface_form: müggelsberge
instance_of: Mountain
countries: Germany
coordinates: lat: 52.416111111111
lon: 13.633333333333
surface_form: müggelberge
instance_of: Mountain
countries: Germany
coordinates: lat: 52.416111111111
lon: 13.633333333333
Müggelberge. The Müggelberge (also formerly called the &quot;Müggelsberge&quot;;) are a wooded line of hills with heights up to in the southeast of Berlin's Treptow-Köpenick quarter. They are dominated by the Kleiner Müggelberg (88.3 m) and Großer Müggelberg (114.7 m). The &quot;Müggelberge&quot; cover an area of around seven square kilometres. The ridge was formed during the ice age.

Geographic entities mentioned:
surface_form: müggelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 52.416111111111
lon: 13.633333333333
surface_form: müggelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 52.416111111111
lon: 13.633333333333
Müggelberge. The Müggelberge (also formerly called the &quot;Müggelsberge&quot;;) are a wooded line of hills with heights up to in the southeast of Berlin's Treptow-Köpenick quarter. They are dominated by the Kleiner Müggelberg (88.3 m) and Großer Müggelberg (114.7 m). The &quot;Müggelberge&quot; cover an area of around seven square kilometres. The ridge was formed during the ice age.

Geographic entities mentioned:
surface_form: müggelberge
instance_of: Mountain
countries: Germany
coordinates: lat: 52.416111111111
lon: 13.633333333333
Lingtren. Lingtren (), is a mountain in the Mahalangur Himal area of Himalaya, about distant in a direct line from Mount Everest. It lies on the international border between Nepal and the Tibet Autonomous Region of China and it was first climbed in 1935. A mountain nearby to the west was originally named Lingtrennup but is now more commonly called Xi Lingchain. Geography.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
surface_form: lingtren
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
Geography. A long chain of mountains extends generally somewhat north of west from Mount Everest whose west ridge descends to the col of Lho La () before rising to Khumbutse (). The ridge drops to an unnamed col at and then ascends to Lingtren from where it continues to another unnamed col at and then to Pumori ().

Geographic entities mentioned:
surface_form: Khumbutse
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 28.020277777778
lon: 86.873055555556
Geography. A long chain of mountains extends generally somewhat north of west from Mount Everest whose west ridge descends to the col of Lho La () before rising to Khumbutse (). The ridge drops to an unnamed col at and then ascends to Lingtren from where it continues to another unnamed col at and then to Pumori ().

Geographic entities mentioned:
surface_form: Pumori
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.015555555555554
lon: 86.82805555555555
surface_form: lingtren
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
Discovery. Lingtren can easily be seen from inhabited villages in the Khumbu valley of Nepal but it may be that the first time it was seen by western explorers was from Tibet in 1921. During the 1921 British Mount Everest reconnaissance expedition George Mallory and Guy Bullock were exploring the region to the north of Mount Everest hoping to find a route to the summit.

Geographic entities mentioned:
surface_form: Khumbu
instance_of: Valley
countries: Nepal
coordinates: lat: 27.805
lon: 86.71
surface_form: lingtren
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
Subsequent events. When ascending the Khumbu valley at the start of the successful 1953 Everest expedition, John Hunt said that the glacier appeared as if it could only originate at an apparent valley head between Lingtren and Nuptse – the Icefall and Western Cwm were completely invisible around the sharp bend in the glacier.

Geographic entities mentioned:
surface_form: Nuptse
instance_of: Mountain
countries: Nepal
coordinates: lat: 27.966388888889
lon: 86.89
surface_form: lingtren
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
surface_form: lingtren
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
Geologically the south face of the mountain is of black gneiss overlain by a thick sill of massive granite. The gneiss has been intruded with many thinner granite sills. The summit elevation is alternatively stated to be and using different elevation models. Lingtren's prominence is about above its key col, which is between it and its nearest higher neighbour Pumori. Discovery.

Geographic entities mentioned:
surface_form: pumori
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.015555555555554
lon: 86.82805555555555
surface_form: lingtren
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
Lingtren. Lingtren (), is a mountain in the Mahalangur Himal area of Himalaya, about distant in a direct line from Mount Everest. It lies on the international border between Nepal and the Tibet Autonomous Region of China and it was first climbed in 1935. A mountain nearby to the west was originally named Lingtrennup but is now more commonly called Xi Lingchain. Geography.

Geographic entities mentioned:
surface_form: lingtrennup
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
First ascent. The 1935 British Mount Everest reconnaissance expedition again explored the region and on this occasion, during what Eric Shipton called &quot;a veritable orgy of mountain climbing&quot;, Shipton and Leslie Vickery &quot;Dan&quot; Bryant climbed for the first time an outlying peak of Lingtren, Lingtrennup and then the main peak of Lingtren.

Geographic entities mentioned:
surface_form: lingtrennup
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
surface_form: lingtren
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
surface_form: lingtren
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
Lingtren. Lingtren (), is a mountain in the Mahalangur Himal area of Himalaya, about distant in a direct line from Mount Everest. It lies on the international border between Nepal and the Tibet Autonomous Region of China and it was first climbed in 1935. A mountain nearby to the west was originally named Lingtrennup but is now more commonly called Xi Lingchain. Geography.

Geographic entities mentioned:
surface_form: lingtren
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
Bounded on the north by this chain of mountains is the Western Cwm in Nepal down which the Khumbu Glacier descends to the northwest over the Icefall before it turns sharply southwest. Lingtren lies at the apex of this right-angled bend. North of the mountain chain in Tibet the West Rongbuk Glacier flows east to join the main Rongbuk Glacier.

Geographic entities mentioned:
surface_form: lingtren
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
Lingtren lies at the apex of this right-angled bend. North of the mountain chain in Tibet the West Rongbuk Glacier flows east to join the main Rongbuk Glacier. Near Lingtren, the Khumbu glacier is at about whereas the West Rongbuk glacier is at about. Geologically the south face of the mountain is of black gneiss overlain by a thick sill of massive granite.

Geographic entities mentioned:
surface_form: lingtren
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
Everest's west ridge did not seem promising so they tried to reach the watershed at some point to see what lay to the south. In doing this they discovered Lingtren (but did not climb it) and skirted its flanks to reach a col from where they were able to see the Western Cwm for the first time.

Geographic entities mentioned:
surface_form: lingtren
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
Naming. The peak now known as Lingtren is actually part of a complex formation extending to the north into the West Rongbuk Glacier &quot;(see 1921 expedition map)&quot;. The northern section, at the junction of the west and main Rongbuk glaciers, is now generally called Guangming Peak () and has an elevation of.

Geographic entities mentioned:
surface_form: lingtren
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
The northern section, at the junction of the west and main Rongbuk glaciers, is now generally called Guangming Peak () and has an elevation of. The name &quot;Lingtren&quot; now only refers to the highest summit, which is immediately to the north of the Khumbu Glacier.

Geographic entities mentioned:
surface_form: lingtren
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
Mallory and Bullock suggested names for the many topographical features they discovered and these were endorsed by the expedition and passed to Charles Bell, Britain's special ambassador to Lhasa, for approval. With reference to the whole Lingtren complex, they chose the name &quot;Lingtren&quot; as Tibetan for &quot;subcontinent&quot; or &quot;island&quot;.

Geographic entities mentioned:
surface_form: lingtren
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
surface_form: lingtren
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
He described one summit of Lingtren as being &quot;square and steep-ridged&quot; and another to the east (he called it Lingtren Two) as &quot;thin as a wafer at its top, looking incredibly fragile&quot;. There has been no fully accepted record of the mountain having been climbed since 1935 and this would mean it has never been climbed from the Nepalese side.

Geographic entities mentioned:
surface_form: lingtren
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
This is perhaps remarkable because from Everest Base Camp, along with Pumori and Khumbutse (which have both been climbed), the mountain is very noticeable being less than away. A planned South-African expedition on Lingtren was canceled in 2013. In &quot;Hoger dan de Dhaulagiri&quot;, claimed he had climbed Lingtren in 1993 saying he started in Nepal and then crossed into Tibet.

Geographic entities mentioned:
surface_form: lingtren
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.0167
lon: 86.85
Kogaionon. Kogaionon was the holy mountain of the Geto-Dacians, the place where Zalmoxis stayed in a cave for three years. After his disappearance into Kogaionon, he was considered dead by the Getae but after three years he resurrected and showed himself to the people, who became convinced by his holy preaching when he emerged from Kogaionon.

Geographic entities mentioned:
surface_form: kogaionon
instance_of: Mountain
countries: Romania
Kogaionon. Kogaionon was the holy mountain of the Geto-Dacians, the place where Zalmoxis stayed in a cave for three years. After his disappearance into Kogaionon, he was considered dead by the Getae but after three years he resurrected and showed himself to the people, who became convinced by his holy preaching when he emerged from Kogaionon.

Geographic entities mentioned:
surface_form: kogaionon
instance_of: Mountain
countries: Romania
surface_form: kogaionon
instance_of: Mountain
countries: Romania
Strabo claims that a river with the same name flowed in the vicinity. One modern translation of Kogaionon is &quot;sacred mountain&quot;, which would be connected to a probable Dacian word &quot;kaga&quot; meaning &quot;sacred&quot;, attested in two early 2nd century inscriptions from Tomis.

Geographic entities mentioned:
surface_form: kogaionon
instance_of: Mountain
countries: Romania
surface_form: kogaionon
instance_of: Mountain
countries: Romania
Pic de Contraix. Pic de Contraix is a mountain of Catalonia, Spain. Located in the Pyrenees, it has an altitude of above sea level.

Geographic entities mentioned:
surface_form: pic de contraix
instance_of: Mountain
countries: Spain
coordinates: lat: 42.58524
lon: 0.906931
The icon screen dates from the 1740s. The church has gone through more renovations in the 19th century but was restored to its original medieval appearance under the supervision of Leon David in the 1950s. The church forms the nucleus of the Athonite metochion, a Moscow mission of the Rossikon Monastery on Mount Athos. Future Athonite monks reside there.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Balnacoil. Balnacoil () is a small crofting village, lying in the strath of Brora, one mile west of Loch Brora, in the east county of Sutherland, in Highland, Scotland. The River Brora, which rises in Ben Armine, runs through Balnacoil, draining into the loch. Balnacoil is in the Scottish council area of Highland.

Geographic entities mentioned:
surface_form: Loch Brora
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.0447
lon: -3.9455
Balnacoil. Balnacoil () is a small crofting village, lying in the strath of Brora, one mile west of Loch Brora, in the east county of Sutherland, in Highland, Scotland. The River Brora, which rises in Ben Armine, runs through Balnacoil, draining into the loch. Balnacoil is in the Scottish council area of Highland.

Geographic entities mentioned:
surface_form: Ben Armine
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.2
lon: -4.2333333333333
&quot;Sandhayak&quot; is powered by two diesel engines and is capable of sustained speeds and can also undertake a variety of tasks including rescue operations. In March 2017 in a rare case of insubordination and indiscipline 3 sailors were airlifted from the ship while it was conducting training session off the coast of Paradip, Odisha in the Bay of Bengal. Survey Task.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Brooksee. Brooksee is a lake in the Rostock district in Mecklenburg-Vorpommern, Germany. At an elevation of 23.9 m, its surface area is 0.114 km².

Geographic entities mentioned:
surface_form: brooksee
instance_of: Lake
countries: Germany
coordinates: lat: 53.9742
lon: 12.079519444444
They were also used in ceremonial functions, as when a &quot;paranymph&quot;, or friend of a bridegroom, went with him in a chariot to fetch the bride home. Herodotus (&quot;Histories&quot;, 5. 9) Reports that chariots were widely used in the Pontic–Caspian steppe by the Sigynnae. Greek chariots were made to be drawn by two horses attached to a central pole.

Geographic entities mentioned:
surface_form: Caspian
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
It has been said that Cárdenas was the only president associated with the Institutional Revolutionary Party (PRI) who did not use the office to make himself wealthy. He retired to a modest home by Lake Pátzcuaro, Michoacán, and worked the rest of his life supervising irrigation projects and promoting free medical clinics and education for the nation's poor.

Geographic entities mentioned:
surface_form: Lake Pátzcuaro
instance_of: Lake
countries: Mexico
coordinates: lat: 19.615
lon: -101.65
In the 1940s, he became increasingly interested in painting, which he had studied as a teenager. Salemme's annual summer visits to Rockport, Massachusetts resulted in several post-Impressionist-inspired sea and landscapes. After a 43-year career in New York City, Salemme and his wife Martha returned to the Lehigh Valley region of eastern Pennsylvania in 1962.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Danville River. The Danville River (&quot;in French: rivière Danville&quot;) is a tributary of the east bank of the Landry River whose current flows successively into the Nicolet Southwest River, Nicolet River, Lake Saint-Pierre and St. Lawrence River.

Geographic entities mentioned:
surface_form: Nicolet Southwest River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.21666666666667
lon: -72.60138888888889
surface_form: Nicolet River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.255
lon: -72.6525
All instruments and vocals were provided by the band members Robert Plant (vocals), Jimmy Page (guitar), John Paul Jones (bass, keyboards), and John Bonham (drums). The album was produced by Page and mixed by Eddie Kramer. The cover was the first for the band to be designed by Hipgnosis and was based on a photograph taken at Giant's Causeway in Northern Ireland.

Geographic entities mentioned:
surface_form: Giant's Causeway
instance_of: Landform
countries: United Kingdom
coordinates: lat: 55.240833333333
lon: -6.5116666666667
The cover art for &quot;Houses of the Holy&quot; was inspired by Arthur C. Clarke's novel &quot;Childhood's End&quot;. The cover is a collage of several photographs which were taken at the Giant's Causeway, Northern Ireland, by Aubrey Powell of Hipgnosis. This location was chosen ahead of an alternative one in Peru which had also been considered.

Geographic entities mentioned:
surface_form: Giant's Causeway
instance_of: Landform
countries: United Kingdom
coordinates: lat: 55.240833333333
lon: -6.5116666666667
Geography. The commune covers an area of. The eastern (and smaller) part of its territory lies within the fertile, central plain or &quot;depresión intermedia&quot;, (Chilean Central Valley) but the extense western part is hilly and somewhat drier, a typical &quot;Cordillera de la Costa&quot; terrain, which requires supplemental irrigation to support its varied cultivations.

Geographic entities mentioned:
surface_form: Chilean Central Valley
instance_of: Valley
countries: Chile
coordinates: lat: -35.5
lon: -71.5
This area lends itself nicely to wine growing and cereal cultivation. Therefore, San Javier has some of the better vineyards and quality wines of the bountiful Maule Valley, in the Chile's central valley viticultural regions or appellations.

Geographic entities mentioned:
surface_form: Chile's central valley
instance_of: Valley
countries: Chile
coordinates: lat: -35.5
lon: -71.5
Townsend Point. Townsend Point is a mountain summit in Brewster County, Texas, United States. Description. Townsend Point is located in the Chisos Mountains. It ranks as the second-highest peak in Big Bend National Park, Brewster County, and the Chisos Mountains, but only the 19th-highest in Texas. The mountain is composed of extrusive volcanic rock which formed during the Oligocene period.

Geographic entities mentioned:
surface_form: townsend point
instance_of: Mountain
countries: United States
coordinates: lat: 29.23826
lon: -103.29073
The slopes of the peak are covered by juniper, oak, and piñon. Based on the Köppen climate classification, Townsend Point is located in a hot arid climate zone with hot summers and mild winters. Any scant precipitation runoff from the mountain's slopes drains into Fresno Creek and Juniper Draw which are both part of the Rio Grande watershed.

Geographic entities mentioned:
surface_form: townsend point
instance_of: Mountain
countries: United States
coordinates: lat: 29.23826
lon: -103.29073
Lord Byron and his young physician John Polidori were staying at the Villa Diodati by Lake Geneva and were visited by Percy Bysshe Shelley, Mary Shelley, and Claire Clairmont. Kept indoors by the &quot;incessant rain&quot; of that &quot;wet, ungenial summer&quot;, over three days in June the five turned to telling fantastical tales, and then writing their own.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Bolton upon Dearne. Bolton upon Dearne is a village in the Metropolitan Borough of Barnsley, South Yorkshire, England, in the part of the Dearne Valley through which the River Dearne passes. Historically part of the West Riding of Yorkshire, it is approximately east of Barnsley, west of Doncaster and north of Rotherham. History. Bolton upon Dearne was an ancient parish.

Geographic entities mentioned:
surface_form: Dearne Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.5
lon: -1.2166666666667
There are two sister taxa: Eoastrapostylopidae and Trigonostylopidae. Around 1900, Argentine paleontologist Florentino Ameghino described eight Colhuehuapian (Early Miocene) species from specimens he found south of Lake Colhué Huapi in Patagonia and grouped them into three genera: &quot;Parastrapotherium&quot;, &quot;Astrapotherium&quot;, and &quot;Astrapothericulus&quot;.

Geographic entities mentioned:
surface_form: Lake Colhué Huapi
instance_of: Group of lakes
countries: Argentina
coordinates: lat: -45.5
lon: -68.75
Barcam. Barcam (&quot;An Barr Cam&quot;) is a mountain in County Offaly, Ireland. Geography. The mountain stands at high making it the fourth-highest mountain in County Offaly, the fifth-highest mountain in the Slieve Bloom Mountains, and the 613th-highest summit in Ireland.

Geographic entities mentioned:
surface_form: barcam
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.05099722
lon: -7.66086389
Barcam. Barcam (&quot;An Barr Cam&quot;) is a mountain in County Offaly, Ireland. Geography. The mountain stands at high making it the fourth-highest mountain in County Offaly, the fifth-highest mountain in the Slieve Bloom Mountains, and the 613th-highest summit in Ireland.

Geographic entities mentioned:
surface_form: barcam
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.05099722
lon: -7.66086389
surface_form: an barr cam
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.05099722
lon: -7.66086389
The canal travels east-west across Ismailia Governorate. It was dug to provide fresh water to the arid area, from Lake Timsah to Suez and Port Said. The canal facilitated the growth of agriculture settlements along the Suez Canal, and it is particularly important for supplying water to the city of Port Said.

Geographic entities mentioned:
surface_form: Lake Timsah
instance_of: Lake
countries: Egypt
coordinates: lat: 30.577777777778
lon: 32.288888888889
Crystal Spring is an unincorporated community in Brush Creek Township, Fulton County, Pennsylvania, United States, south of Breezewood. Just to the west, across the county line in Bedford County, is Gapsville. The community lies east of a water gap, where Brush Creek passes through Rays Hill, which forms the western border of Fulton County. The elevation is approximately 1161 feet.

Geographic entities mentioned:
surface_form: Rays Hill
instance_of: Mountain
countries: United States
coordinates: lat: 39.905555555556
lon: -78.266111111111
The river is fed by the Vallei Canal and a number of Veluwe creeks, the most important of which are the Heiligenberger Beek, the Barneveldse Beek and the Lunterse Beek, all of which come together in Amersfoort. The river then runs through the Eem Valley to the east of Soest, Baarn and Eemnes before emptying into the Eemmeer.

Geographic entities mentioned:
surface_form: Eemmeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.280556
lon: 5.330833
When water levels drop in the summer, water is pumped from the Nederrijn to the Eem through the Vallei Canal. Because of agricultural pollution carried by the Eem towards the Eemmeer, the biological richness of this lake is less than that of the other lakes which surround Flevoland. The Eem gives its name to the Eemian interglacial era.

Geographic entities mentioned:
surface_form: Eemmeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.280556
lon: 5.330833
Graduates of the college receive the Doctor of Osteopathic Medicine degree. The university eventually plans to open additional colleges at the Lebanon campus. History. Plans for the school were announced as early as 2007, and in January 2008 it was announced the school would partner with Willamette Valley based Samaritan Health Services.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Chancellor Peak. Chancellor Peak is a mountain summit located in Yoho National Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Mount Vaux, to the north-northwest. Both are part of the Ottertail Range. Chancellor Peak is a landmark in the Kicking Horse River valley and can be seen from the Trans-Canada Highway midway between Golden and Field. History.

Geographic entities mentioned:
surface_form: Mount Vaux
instance_of: Mountain
countries: Canada
coordinates: lat: 51.26666
lon: -116.53549
Chancellor Peak. Chancellor Peak is a mountain summit located in Yoho National Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Mount Vaux, to the north-northwest. Both are part of the Ottertail Range. Chancellor Peak is a landmark in the Kicking Horse River valley and can be seen from the Trans-Canada Highway midway between Golden and Field. History.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: chancellor peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.22416666666667
lon: -116.51027777777777
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Climate. Based on the Köppen climate classification, Chancellor Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Chancellor Peak drains into the Kicking Horse River which is a tributary of the Columbia River.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: chancellor peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.22416666666667
lon: -116.51027777777777
Chancellor Peak. Chancellor Peak is a mountain summit located in Yoho National Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Mount Vaux, to the north-northwest. Both are part of the Ottertail Range. Chancellor Peak is a landmark in the Kicking Horse River valley and can be seen from the Trans-Canada Highway midway between Golden and Field. History.

Geographic entities mentioned:
surface_form: chancellor peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.22416666666667
lon: -116.51027777777777
History. The mountain was named in 1898 to honor Sir John Alexander Boyd (1837–1916), who was Chancellor of the High Court of Justice of the Province of Ontario. The first ascent of Chancellor Peak was made on July 30, 1901 by James Outram, J. Henry Scattergood, and George M. Weed, with Christian Hasler Sr. as guide.

Geographic entities mentioned:
surface_form: chancellor peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.22416666666667
lon: -116.51027777777777
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Chancellor Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: chancellor peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.22416666666667
lon: -116.51027777777777
Chancellor Peak is a landmark in the Kicking Horse River valley and can be seen from the Trans-Canada Highway midway between Golden and Field. History. The mountain was named in 1898 to honor Sir John Alexander Boyd (1837–1916), who was Chancellor of the High Court of Justice of the Province of Ontario. The first ascent of Chancellor Peak was made on July 30, 1901 by James Outram, J.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Outram wrote of it: &quot;The Chancellor, that mighty pyramid from whose frowning precipices, black and forbidding, loom aloft nigh upon 7,000 feet above the Kicking Horse River cannot fail to impress the traveler with a sense of awe and grandeur, as he approaches eastward from the grim gateway of the lower canyon.&quot;
The mountain's name was officially adopted in 1924 when approved by the Geographical Names Board of Canada.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Le Prese. Le Prese is a village in the Val Poschiavo in the canton of Graubünden, Switzerland. It lies at above sea level at the northern end of Lago di Poschiavo, and is in the municipality of Poschiavo, some south of the village of the same name. The Poschiavino river enters the lake by the village.

Geographic entities mentioned:
surface_form: Val Poschiavo
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.308888888889
lon: 10.061388888889
In the middle of the 19th century, Le Prese was developed as a spa town, with the 1856 construction of the spa building and further improvements in 1861. It sold itself as the ideal acclimatization station between the north of Italy and the health resorts of the Engadin. The sulphur spa was well frequented until 1914.

Geographic entities mentioned:
surface_form: Engadin
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
He started armateur ski mountaineering sports in 1990 and competed first at the &quot;Arflina race&quot;. In 1999 and 2000 he won the &quot;Pizol Challenge&quot;, and has been member of the national team since 2000. He enjoys also mountain biking, climbing and mountain running. Together with Beat Good and Andreas Zimmermann he created the &quot;Pizol Altiski&quot;, which he organized in 2003.

Geographic entities mentioned:
surface_form: Pizol
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.959166666667
lon: 9.3866666666667
Thomas George Montgomerie. Lieutenant-Colonel Thomas George Montgomerie FRS (1830–1878) was a British surveyor who participated in the Great Trigonometric Survey of British India as a lieutenant in the 1850s. He was the person to label K2, the second highest mountain in the world, the K standing for Karakoram.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
In 1867 Major Montgomerie was assigned to Peshawar where he was tasked with recruiting native agents to explore Central Asia. Montgomerie recruited a number of individuals to survey Chitral and Badakhshan, including Hyder Shah, who in 1870 travelled through the princely states of Swat and Dir and Badakhshan.

Geographic entities mentioned:
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
The Tay originates in western Scotland on the slopes of Ben Lui (), then flows easterly across the Highlands, through Loch Dochart, Loch Iubhair and Loch Tay, then continues east through Strathtay (see Strath), in the centre of Scotland, then southeasterly through Perth, where it becomes tidal, to its mouth at the Firth of Tay, south of Dundee.

Geographic entities mentioned:
surface_form: Ben Lui
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.397004
lon: -4.810525
surface_form: Loch Dochart
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.3964
lon: -4.58417
surface_form: Loch Iubhair
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.407309
lon: -4.555857
surface_form: Loch Tay
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.515555555556
lon: -4.1461111111111
Course. The Tay drains much of the lower region of the Highlands. It originates on the slopes of Ben Lui (&quot;Beinn Laoigh&quot;), around from the west coast town of Oban, in Argyll and Bute. In 2011, the Tay Western Catchments Partnership determined as its source (based on its 'most dominant and longest' tributary) a small lochan on Allt Coire Laoigh south of the summit.

Geographic entities mentioned:
surface_form: Ben Lui
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.397004
lon: -4.810525
The river has a variety of names in its upper catchment: for the first few miles it is known as the River Connonish; then the River Fillan; the name then changes to the River Dochart until it flows into Loch Tay at Killin. The River Tay emerges from Loch Tay at Kenmore and flows from there to Perth which, in historical times, was its lowest bridging point.

Geographic entities mentioned:
surface_form: Loch Tay
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.515555555556
lon: -4.1461111111111
Belgian Congo and the East Africa Campaign. German presence in Africa posed no direct threat to the Belgian Congo; however, in 1914 a German gunboat sank a number of Belgian vessels on Lake Tanganyika. Congolese forces, under Belgian officers, fought German colonial forces in the Cameroons and seized control of the western third of German East Africa, advancing as far as the town at Tabora.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
The southwest side of Baker Mountain drains into North Brook, then into Upper and Lower Wilson Ponds, Eagle Stream, Big Wilson Stream, Sebec Lake, and the Sebec River, another tributary of the Piscataquis River. The northwest side of Baker Mountain drains into South Brook, then into Moosehead Lake, the source of the Kennebec River, which drains into the Gulf of Maine.

Geographic entities mentioned:
surface_form: Moosehead Lake
instance_of: Lake
countries: United States
coordinates: lat: 45.633333333333
lon: -69.65
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.1625
lon: -78.5569
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.376111111111
lon: -106.60083333333
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.335
lon: -74.103611111111
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.571
lon: -69.3938
The northwest side of Baker Mountain drains into South Brook, then into Moosehead Lake, the source of the Kennebec River, which drains into the Gulf of Maine. Baker Mountain sits on of land purchased by the Appalachian Mountain Club in 2015. The southern slopes of the mountain are part of the Katahdin Iron Works conservation property.

Geographic entities mentioned:
surface_form: katahdin
instance_of: Mountain
countries: United States
coordinates: lat: 45.904355555556
lon: -68.921275
Baker Mountain (Piscataquis County, Maine). Baker Mountain is a wild, trail-less mountain located in Beaver Cove (TA.2 R.13&14, WELS), Piscataquis County, Maine. It is flanked to the northwest by Lily Bay Mountain. Elephant Mountain is about to the southwest, and White Cap Mountain is about to the east.

Geographic entities mentioned:
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.1625
lon: -78.5569
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.376111111111
lon: -106.60083333333
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.335
lon: -74.103611111111
surface_form: baker mountain (piscataquis county, maine)
instance_of: Mountain
countries: United States
coordinates: lat: 45.571
lon: -69.3938
Baker Mountain (Piscataquis County, Maine). Baker Mountain is a wild, trail-less mountain located in Beaver Cove (TA.2 R.13&14, WELS), Piscataquis County, Maine. It is flanked to the northwest by Lily Bay Mountain. Elephant Mountain is about to the southwest, and White Cap Mountain is about to the east.

Geographic entities mentioned:
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.1625
lon: -78.5569
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.376111111111
lon: -106.60083333333
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.335
lon: -74.103611111111
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.571
lon: -69.3938
It is flanked to the northwest by Lily Bay Mountain. Elephant Mountain is about to the southwest, and White Cap Mountain is about to the east. The east side of Baker Mountain drains into Baker Mountain Brook, then into the West Branch of the Pleasant River, the Piscataquis River, the Penobscot River, and into Penobscot Bay.

Geographic entities mentioned:
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.1625
lon: -78.5569
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.1625
lon: -78.5569
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.376111111111
lon: -106.60083333333
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.376111111111
lon: -106.60083333333
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: west branch
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.335
lon: -74.103611111111
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.335
lon: -74.103611111111
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.571
lon: -69.3938
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.571
lon: -69.3938
The east side of Baker Mountain drains into Baker Mountain Brook, then into the West Branch of the Pleasant River, the Piscataquis River, the Penobscot River, and into Penobscot Bay. The southwest side of Baker Mountain drains into North Brook, then into Upper and Lower Wilson Ponds, Eagle Stream, Big Wilson Stream, Sebec Lake, and the Sebec River, another tributary of the Piscataquis River.

Geographic entities mentioned:
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.1625
lon: -78.5569
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.376111111111
lon: -106.60083333333
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.335
lon: -74.103611111111
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.571
lon: -69.3938
The northwest side of Baker Mountain drains into South Brook, then into Moosehead Lake, the source of the Kennebec River, which drains into the Gulf of Maine. Baker Mountain sits on of land purchased by the Appalachian Mountain Club in 2015. The southern slopes of the mountain are part of the Katahdin Iron Works conservation property.

Geographic entities mentioned:
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.1625
lon: -78.5569
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.376111111111
lon: -106.60083333333
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.335
lon: -74.103611111111
surface_form: baker mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.571
lon: -69.3938
It is flanked to the northwest by Lily Bay Mountain. Elephant Mountain is about to the southwest, and White Cap Mountain is about to the east. The east side of Baker Mountain drains into Baker Mountain Brook, then into the West Branch of the Pleasant River, the Piscataquis River, the Penobscot River, and into Penobscot Bay.

Geographic entities mentioned:
surface_form: white cap mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.5547
lon: -69.2463
surface_form: elephant mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.7682
lon: -70.7817
surface_form: white cap mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.2362
lon: -70.8182
surface_form: elephant mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.5157
lon: -69.4257
Rattlesnake Island (New Hampshire). Rattlesnake Island is a large island in Lake Winnipesaukee, New Hampshire. There are conflicting accounts of where it got its name, because its shape looks somewhat like a snake, but some say it is named for a rattlesnake population that lived there. The island is located within the town of Alton. Topography and physical features.

Geographic entities mentioned:
surface_form: Lake Winnipesaukee
instance_of: Lake
countries: United States
coordinates: lat: 43.598888888889
lon: -71.323055555556
Sawtooth Crater. Sawtooth Crater, also known as Sawtooth Ridge, is a shield volcano and volcanic crater in Baker and Union counties of Oregon. Geography. Sawtooth Crater is bordered to the north and northeast by the Wallowa Mountains and is located northeast of Baker City, Oregon. Geology. Sawtooth Crater is a shield volcano of unknown age. It has a volcanic plug and two radial dikes.

Geographic entities mentioned:
surface_form: sawtooth crater
instance_of: Mountain
coordinates: lat: 44.97555555555556
lon: -117.54222222222222
Geography. Sawtooth Crater is bordered to the north and northeast by the Wallowa Mountains and is located northeast of Baker City, Oregon. Geology. Sawtooth Crater is a shield volcano of unknown age. It has a volcanic plug and two radial dikes. It also has olivine basalt and platy andesite. Hiking. Sawtooth Crater can be hiked to via a road used by the U.S.

Geographic entities mentioned:
surface_form: sawtooth crater
instance_of: Mountain
coordinates: lat: 44.97555555555556
lon: -117.54222222222222
Sawtooth Crater is bordered to the north and northeast by the Wallowa Mountains and is located northeast of Baker City, Oregon. Geology. Sawtooth Crater is a shield volcano of unknown age. It has a volcanic plug and two radial dikes. It also has olivine basalt and platy andesite. Hiking. Sawtooth Crater can be hiked to via a road used by the U.S. Forest Service road that starts at Medical Springs.

Geographic entities mentioned:
surface_form: sawtooth crater
instance_of: Mountain
coordinates: lat: 44.97555555555556
lon: -117.54222222222222
Prior to its adoption in 1969, Crevasse Crag was climbed by Adam et al. on August 16, 1967. Crevasse Crag is the remains of an extinct volcano that formed 16 million years ago when the Pemberton Belt was volcanically active. This volcano erupted breccias, tuffs and plagioclase-phyric flows, all of which form the present day edifice of Crevasse Crag.

Geographic entities mentioned:
surface_form: Pemberton Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 50.58051944
lon: -122.93235278
Istállós-kő. Istállós-kő () is a mountain in Hungary. With a height of above sea level, it is the second highest mountain of the Bükk mountains and the sixth highest of Hungary. Before 2014 it was considered to be the highest point of the area, but according to recent surveys Szilvási-kő is meters high.

Geographic entities mentioned:
surface_form: istállós-kő
instance_of: Mountain
countries: Hungary
coordinates: lat: 48.07
lon: 20.43194444
Before 2014 it was considered to be the highest point of the area, but according to recent surveys Szilvási-kő is meters high. It is easily accessible from Szilvásvárad on a few hundred meters long tourist path, which leads to a cave in the mountain. Istállós-kő cave. The cave was first explored by Pál Roskó in 1911.

Geographic entities mentioned:
surface_form: istállós-kő
instance_of: Mountain
countries: Hungary
coordinates: lat: 48.07
lon: 20.43194444
Padlei. Padlei is a former community in the Kivalliq Region of Nunavut, Canada. It is located on the mainland on the north shore of Kinga (Kingarvalik) Lake at the juncture of the Maguse River. Whale Cove is to the east, while the Henik Lakes are to the southwest. History. Containing three buildings, Padlei was the site of a trading post operated by the Hudson's Bay Company from 1926 to 1960.

Geographic entities mentioned:
surface_form: Henik Lake
instance_of: Group of lakes
countries: Canada
coordinates: lat: 61.64982
lon: -97.54021
Recent experience includes the Air & Style Snowboard Contest from 1994 to 1999 and 2008, the 2005 Men's World Ice Hockey Championships, and the 2005 Winter Universiade (with Seefeld). Innsbruck's Bergisel is expected to once again be the centerpiece of the bid. Martin Schnitzer, CEO of Innsbruck 2012, outlined Innsbruck’s plan on June 19, 2008.

Geographic entities mentioned:
surface_form: Bergisel
instance_of: Mountain
countries: Austria
coordinates: lat: 47.246666666667
lon: 11.399722222222
Finalist city overview. Kuopio is a first time bidder. On the shores of Lake Kallavesi, it is the cultural centre of Eastern Finland and has a winter sports infrastructure in place. Puijo hill serves as a site for the yearly FIS Ski Jumping World Cup. Kuopio is a small city with a large University and many active young people - a model that may exemplify what the IOC is looking for in these Games.

Geographic entities mentioned:
surface_form: Kallavesi
instance_of: Lake
countries: Finland
coordinates: lat: 62.816666666667
lon: 27.783333333333
Lake of the Woods State Forest. The Lake of the Woods State Forest is a state forest located south of Lake of the Woods in Beltrami, Koochiching, Lake of the Woods and Roseau counties in Minnesota, USA. The forest borders the Pine Island State Forest to the east and the Beltrami Island State Forest to the west. Outdoor recreational activities include boating, canoeing, kayaking and fishing.

Geographic entities mentioned:
surface_form: Lake of the Woods
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.09027777777778
lon: -95.2388888888889