Sarmila/GeoWiki-Features huggingface dataset:
Disappointment Peak (Wyoming). Disappointment Peak () is in the Teton Range of Wyoming, in Grand Teton National Park and immediately southeast of Grand Teton. The peak is part of the Cathedral Group, a region of the Tetons noted for particularly rugged mountains. Disappointment Peak rises to the north of Garnet Canyon and to the west of Amphitheater and Surprise lakes.

Geographic entities mentioned:
surface_form: the cathedral
instance_of: Mountain
countries: United States
coordinates: lat: 40.775833333333
lon: -110.71027777778
Pedretti's Sons, depict four important archetypes of people of Montana's early history: a Native American (intended to be of Chief Charlo), an explorer and fur trapper (Jim Bridger), a gold miner (Henry Finnis Edgar, one of the discoverers of gold at Alder Gulch), and a cowboy (unidentified, but said to be inspired by the works of C.M. Russell).

Geographic entities mentioned:
surface_form: Alder Gulch
instance_of: Valley
countries: United States
coordinates: lat: 45.3253
lon: -112.077
His godmother is Rosmarie Ebner, the wife of the Swiss financier Martin Ebner. His elder sister is now the CEO of EMS-Chemie and a member of the National Council for the Swiss People's Party. He primarily grew up in Feldmeilen on Lake Zurich. He completed a student exchange in the United States and had the desire to join the United States Army in his teens.

Geographic entities mentioned:
surface_form: Lake Zurich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
Mikami Shrine. is a Shinto shrine located in the city of Yasu, Shiga Prefecture, Japan. The &quot;kami&quot; worshipped at this shrine is, Amaterasu's grandson, who in legend, descended onto 432-meter Mount Mikami during the reign of Emperor Kōrei (290 - 215 BC) to become the &quot;shintai&quot; of the mountain. History. The foundation of Mikami Jinja is uncertain.

Geographic entities mentioned:
surface_form: Mount Mikami
instance_of: Mountain
countries: Japan
coordinates: lat: 35.05028
lon: 136.03778
Today, the crystalline igneous rocks of the Grenvillian basement form the core of the Blue Ridge Mountains, also known as the Pedlar formation, where they are exposed. To the west, they are hidden beneath the Valley and Ridge and Appalachian Plateau, while to the east they extend under the Piedmont, coastal plain, and continental shelf.

Geographic entities mentioned:
surface_form: Appalachian Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 40
lon: -78
Mont Fort. Mont Fort is a mountain of the Pennine Alps, in the Swiss canton of Valais. It lies on the range between the valleys of Nendaz and Bagnes, north of the Rosablanche. With a summit elevation of above sea level, Mont Fort is the highest peak north of the Col de Louvie ().

Geographic entities mentioned:
surface_form: Rosablanche
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.06
lon: 7.3541666666667
The cable cars from the two valleys converge at the intermediate station () north of the Col des Gentianes, the upper section reaching an elevation of. In the winter and early spring season, the mountain, including the Glacier de Tortin, is the culminating point of the &quot;4 Vallées&quot; ski area, accessible by the &quot;Mont-Fort&quot; cable car.

Geographic entities mentioned:
surface_form: mont-fort
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.080277777778
lon: 7.3188888888889
Mont Fort. Mont Fort is a mountain of the Pennine Alps, in the Swiss canton of Valais. It lies on the range between the valleys of Nendaz and Bagnes, north of the Rosablanche. With a summit elevation of above sea level, Mont Fort is the highest peak north of the Col de Louvie ().

Geographic entities mentioned:
surface_form: mont fort
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.080277777778
lon: 7.3188888888889
Mont Fort is a mountain of the Pennine Alps, in the Swiss canton of Valais. It lies on the range between the valleys of Nendaz and Bagnes, north of the Rosablanche. With a summit elevation of above sea level, Mont Fort is the highest peak north of the Col de Louvie (). Mont Fort is surrounded by several glaciers, the largest being the &quot;Glacier de Tortin&quot;, on its northwestern side.

Geographic entities mentioned:
surface_form: mont fort
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.080277777778
lon: 7.3188888888889
With a summit elevation of above sea level, Mont Fort is the highest peak north of the Col de Louvie (). Mont Fort is surrounded by several glaciers, the largest being the &quot;Glacier de Tortin&quot;, on its northwestern side. The second largest is the &quot;Glacier du Mont Fort&quot;, located on its northeastern side. On its eastern side lies the lower summit &quot;Petit Mont Fort&quot; ().

Geographic entities mentioned:
surface_form: mont fort
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.080277777778
lon: 7.3188888888889
Mont Fort is surrounded by several glaciers, the largest being the &quot;Glacier de Tortin&quot;, on its northwestern side. The second largest is the &quot;Glacier du Mont Fort&quot;, located on its northeastern side. On its eastern side lies the lower summit &quot;Petit Mont Fort&quot; (). The &quot;Glacier du Petit Mont Fort&quot; lies between the two summits.

Geographic entities mentioned:
surface_form: mont fort
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.080277777778
lon: 7.3188888888889
surface_form: mont fort
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.080277777778
lon: 7.3188888888889
On its eastern side lies the lower summit &quot;Petit Mont Fort&quot; (). The &quot;Glacier du Petit Mont Fort&quot; lies between the two summits. There are no glaciers on the south side of the mountain. A small lake named &quot;Lac du Petit Mont Fort&quot; () lies on the south flank. The summit of Mont Fort is easily accessible by cable car from the heights of Verbier or Nendaz.

Geographic entities mentioned:
surface_form: mont fort
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.080277777778
lon: 7.3188888888889
It describes Murphy's involvement with the self-sufficient mountain cultures of the Himalayas. Lured by the chance to work again with Tibetan refugees in the Pokhara Valley, Murphy moves into a tiny room above a stall in a bazaar. There she falls under the spell of Nepal and its ancient roots. The book culminates with a trek to the remote Langtang region on the border with Tibet.

Geographic entities mentioned:
surface_form: Pokhara Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 28.233333333333
lon: 83.983333333333
It describes Murphy's involvement with the self-sufficient mountain cultures of the Himalayas. Lured by the chance to work again with Tibetan refugees in the Pokhara Valley, Murphy moves into a tiny room above a stall in a bazaar. There she falls under the spell of Nepal and its ancient roots. The book culminates with a trek to the remote Langtang region on the border with Tibet.

Geographic entities mentioned:
surface_form: Langtang
instance_of: Valley
countries: Nepal
coordinates: lat: 28.25
lon: 85.5
The island is not to be confused with the Island of Montreal in southwest Quebec, on which the city of Montreal is located. Coincidentally, the Quebec island is also situated on a river known as the Back River, the colloquial English name for the Rivière des Prairies.

Geographic entities mentioned:
surface_form: Rivière des Prairies
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.708333333333
lon: -73.479166666667
The specific epithet (&quot;purpurata&quot;) is a Latin word meaning &quot;purple&quot;. Distribution and habitat. The wallum sun orchid is common in heath in coastal Queensland south of Fraser Island to Myall Lakes in New South Wales.

Geographic entities mentioned:
surface_form: Myall Lakes
instance_of: Group of lakes
countries: Australia
coordinates: lat: -32.4575
lon: 152.36194444444
Governor John Endecott in 1652 sent a survey party to determine the colony's northern boundary, which was specified by the charter to be north of the Merrimack River. This survey party discovered (incorrectly) that the northern limit of the Merrimack was near what is now known as Lake Winnipesaukee in New Hampshire.

Geographic entities mentioned:
surface_form: Lake Winnipesaukee
instance_of: Lake
countries: United States
coordinates: lat: 43.598888888889
lon: -71.323055555556
Digha. Digha () is a seaside resort town located in the Purba Medinipur district in the state of West Bengal, India. Situated at the northern end of the Bay of Bengal, it is a popular coastal tourist destination known for its low gradient and shallow sand beaches.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Dallol (hydrothermal system). Dallol is a unique, terrestrial hydrothermal system around a cinder cone volcano in the Danakil Depression, northeast of the Erta Ale Range in Ethiopia. It is known for its unearthly colors and mineral patterns, and the very acidic fluids that discharge from its hydrothermal springs. Etymology.

Geographic entities mentioned:
surface_form: dallol (hydrothermal system)
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 14.241666666667
lon: 40.3
Dallol (hydrothermal system). Dallol is a unique, terrestrial hydrothermal system around a cinder cone volcano in the Danakil Depression, northeast of the Erta Ale Range in Ethiopia. It is known for its unearthly colors and mineral patterns, and the very acidic fluids that discharge from its hydrothermal springs. Etymology.

Geographic entities mentioned:
surface_form: dallol
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 14.241666666667
lon: 40.3
It is known for its unearthly colors and mineral patterns, and the very acidic fluids that discharge from its hydrothermal springs. Etymology. The term &quot;Dallol&quot; was coined by the Afar people and means dissolution or disintegration, describing a landscape of green acid ponds and geysers (pH-values less than 1) and iron oxide, sulfur and salt desert plains. Description.

Geographic entities mentioned:
surface_form: dallol
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 14.241666666667
lon: 40.3
Formation. It was formed by the intrusion of basaltic magma into Miocene salt deposits and subsequent hydrothermal activity. Phreatic eruptions took place here in 1926, forming Dallol Volcano; numerous other eruption craters dot the salt flats nearby. These craters are the lowest known subaerial volcanic vents in the world, at or more below sea level.

Geographic entities mentioned:
surface_form: dallol
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 14.241666666667
lon: 40.3
These craters are the lowest known subaerial volcanic vents in the world, at or more below sea level. In October 2004, the shallow magma chamber beneath Dallol deflated and fed a magma intrusion southwards beneath the rift. The most recent signs of activity occurred in January 2011 in what may have been a degassing event from deep below the surface. Physical properties.

Geographic entities mentioned:
surface_form: dallol
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 14.241666666667
lon: 40.3
It is also one of the lowest land points, lying below mean sea level. Other known hydrothermal features nearby Dallol are Gaet'Ale Pond and Black Lakes. The hydrothermal springs of Dallol discharge anoxic, hyper-acidic (pH &lt; 0), hyper-saline (almost 10 times more saline than seawater), high temperature (hotter than) brines that contain more than 26 g/L of iron.

Geographic entities mentioned:
surface_form: dallol
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 14.241666666667
lon: 40.3
The main gases emitted from the springs and fumaroles are carbon dioxide, hydrogen sulfide, nitrogen, sulfur dioxide; and traces of hydrogen, argon, and oxygen. Although several other hyper-acidic (pH &lt; 2) volcanic systems exist, mainly found in crater lakes and hydrothermal sites, the pH values of Dallol decrease far below zero.

Geographic entities mentioned:
surface_form: dallol
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 14.241666666667
lon: 40.3
Although several other hyper-acidic (pH &lt; 2) volcanic systems exist, mainly found in crater lakes and hydrothermal sites, the pH values of Dallol decrease far below zero. The coexistence of such extreme physicochemical characteristics (pH, salinity, high temperature, lack of oxygen, etc.) render Dallol one of the very few ‘poly-extreme’ sites on Earth.

Geographic entities mentioned:
surface_form: dallol
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 14.241666666667
lon: 40.3
surface_form: dallol
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 14.241666666667
lon: 40.3
In contrast to other hydrothermal systems known for their colorful pools (e.g. Grand Prismatic Spring), where the colors are generated by biological activity, the color palette of Dallol is produced by the inorganic oxidation of the abundant iron phases.

Geographic entities mentioned:
surface_form: dallol
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 14.241666666667
lon: 40.3
surface_form: dallol
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 14.241666666667
lon: 40.3
Another fascinating feature of Dallol is the wide array of unusual mineral patterns such as salt-pillars, miniature geysers, water-lilies, flower-like crystals, egg-shaped crusts, and pearl-like spheres. The main mineral phases encountered at Dallol are halite, jarosite, hematite, akaganeite and other Fe-oxyhydroxides, gypsum, anhydrite, sylvite and carnallite. Absence of life.

Geographic entities mentioned:
surface_form: dallol
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 14.241666666667
lon: 40.3
In October 2019, a French-Spanish team of scientists published an article in &quot;Nature Ecology and Evolution&quot; that concludes that while the salt plains are teeming with halophilic microorganisms, there is no life in Dallol's multi-extreme ponds due to the combination of hyperacidic and hypersaline environments, and the abundance of magnesium (which catalyzes the denaturation of biomolecules).

Geographic entities mentioned:
surface_form: dallol
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 14.241666666667
lon: 40.3
Lindsey Vonn of the U.S. is currently dominant in woman's downhill racing with a lifetime total of 37 World Cup downhill wins and 7 women's titles. Risks. On some courses, such as the Lauberhorn course in Wengen, Switzerland, and the Hahnenkamm course in Kitzbühel, Austria, speeds of up to are common. Safety netting and padding are placed where race officials anticipate potential crashes.

Geographic entities mentioned:
surface_form: Hahnenkamm
instance_of: Mountain
countries: Austria
coordinates: lat: 47.424166666667
lon: 12.365277777778
Salmo ciscaucasicus. &quot;Salmo ciscaucasicus&quot;, the Caspian salmon or Terek trout, is a salmonid fish endemic to the Caspian Sea and its inflowing rivers. It was described in 1967 originally as a subspecies of &quot;Salmo trutta&quot;. &quot;S. ciscaucasicus&quot; lives on the western shore of the lake from northern Azerbaijan to the Ural River, while the main breeding river is the Terek.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Gäbris. Gäbris is a mountain of the Appenzell Alps, overlooking Gais in the canton of Appenzell Ausserrhoden.

Geographic entities mentioned:
surface_form: gäbris
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.38166667
lon: 9.46777778
Blue Lake Peak. Blue Lake Peak is a mountain summit in the North Cascades of Washington state. It is located in the Okanogan–Wenatchee National Forest on the shared border of Okanogan County and Chelan County. The peak is situated south of Early Winters Spires, Liberty Bell Mountain, and Washington Pass. Blue Lake is set below its west slope, and Stiletto Peak is to its south.

Geographic entities mentioned:
surface_form: Liberty Bell Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.5154
lon: -120.658
surface_form: bell mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.780833333333
lon: -74.153611111111
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: bell mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.236666666667
lon: -113.19527777778
surface_form: bell mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.5828
lon: -117.217
surface_form: bell mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.163333333333
lon: -118.08583333333
surface_form: bell mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.6589
lon: -117.152
It is located in the Okanogan–Wenatchee National Forest on the shared border of Okanogan County and Chelan County. The peak is situated south of Early Winters Spires, Liberty Bell Mountain, and Washington Pass. Blue Lake is set below its west slope, and Stiletto Peak is to its south. Blue Lake Peak can be seen from the North Cascades Highway at the Blue Lake Trailhead.

Geographic entities mentioned:
surface_form: Stiletto Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.48347
lon: -120.66594
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 27.4354
lon: -81.5117
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 41.1635044
lon: -74.2603249
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 46.1666
lon: -86.6321
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 47.415277777778
lon: -121.51861111111
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 40.501944444444
lon: -114.03222222222
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 37.68
lon: -119.282
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 47.017222222222
lon: -95.005
Blue Lake Peak. Blue Lake Peak is a mountain summit in the North Cascades of Washington state. It is located in the Okanogan–Wenatchee National Forest on the shared border of Okanogan County and Chelan County. The peak is situated south of Early Winters Spires, Liberty Bell Mountain, and Washington Pass. Blue Lake is set below its west slope, and Stiletto Peak is to its south.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 27.4354
lon: -81.5117
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 41.1635044
lon: -74.2603249
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 46.1666
lon: -86.6321
surface_form: blue lake peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.50666667
lon: -120.65722222
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 47.415277777778
lon: -121.51861111111
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 40.501944444444
lon: -114.03222222222
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 37.68
lon: -119.282
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 47.017222222222
lon: -95.005
surface_form: lake peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.563888888889
lon: -115.39388888889
Blue Lake Peak. Blue Lake Peak is a mountain summit in the North Cascades of Washington state. It is located in the Okanogan–Wenatchee National Forest on the shared border of Okanogan County and Chelan County. The peak is situated south of Early Winters Spires, Liberty Bell Mountain, and Washington Pass. Blue Lake is set below its west slope, and Stiletto Peak is to its south.

Geographic entities mentioned:
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 27.4354
lon: -81.5117
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 41.1635044
lon: -74.2603249
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 46.1666
lon: -86.6321
surface_form: blue lake peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.50666667
lon: -120.65722222
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 47.415277777778
lon: -121.51861111111
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 40.501944444444
lon: -114.03222222222
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 37.68
lon: -119.282
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 47.017222222222
lon: -95.005
surface_form: lake peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.563888888889
lon: -115.39388888889
The peak is situated south of Early Winters Spires, Liberty Bell Mountain, and Washington Pass. Blue Lake is set below its west slope, and Stiletto Peak is to its south. Blue Lake Peak can be seen from the North Cascades Highway at the Blue Lake Trailhead. Precipitation runoff from Blue Lake Peak drains into tributaries of the Chelan River and Methow River.

Geographic entities mentioned:
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 27.4354
lon: -81.5117
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 27.4354
lon: -81.5117
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 41.1635044
lon: -74.2603249
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 41.1635044
lon: -74.2603249
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 46.1666
lon: -86.6321
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 46.1666
lon: -86.6321
surface_form: blue lake peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.50666667
lon: -120.65722222
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 47.415277777778
lon: -121.51861111111
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 47.415277777778
lon: -121.51861111111
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 40.501944444444
lon: -114.03222222222
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 40.501944444444
lon: -114.03222222222
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 37.68
lon: -119.282
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 37.68
lon: -119.282
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 47.017222222222
lon: -95.005
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 47.017222222222
lon: -95.005
surface_form: lake peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.563888888889
lon: -115.39388888889
Blue Lake is set below its west slope, and Stiletto Peak is to its south. Blue Lake Peak can be seen from the North Cascades Highway at the Blue Lake Trailhead. Precipitation runoff from Blue Lake Peak drains into tributaries of the Chelan River and Methow River. Topographic relief is significant as the summit rises above Early Winters Creek in one mile (1.6 km).

Geographic entities mentioned:
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 27.4354
lon: -81.5117
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 41.1635044
lon: -74.2603249
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 46.1666
lon: -86.6321
surface_form: blue lake peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.50666667
lon: -120.65722222
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 47.415277777778
lon: -121.51861111111
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 40.501944444444
lon: -114.03222222222
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 37.68
lon: -119.282
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 47.017222222222
lon: -95.005
surface_form: lake peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.563888888889
lon: -115.39388888889
Blue Lake Peak. Blue Lake Peak is a mountain summit in the North Cascades of Washington state. It is located in the Okanogan–Wenatchee National Forest on the shared border of Okanogan County and Chelan County. The peak is situated south of Early Winters Spires, Liberty Bell Mountain, and Washington Pass. Blue Lake is set below its west slope, and Stiletto Peak is to its south.

Geographic entities mentioned:
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
It has received a PAN Parks certificate. Geography. Paanajärvi National Park is located in the Maanselkä hills of Karelia Region, along the Finnish–Russian border, northern Europe. It protects of pristine Scandinavian and Russian Taiga ecoregion forest habitats, lakes, and rivers. Nuorunen, the highest point of Karelia, is located in the park area. Oulanka National Park.

Geographic entities mentioned:
surface_form: Nuorunen
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 66.144722222222
lon: 30.244722222222
Reindeer Island. Reindeer Island is an island located in the north basin of Lake Winnipeg, in the Canadian province of Manitoba, closer to the western shore of the lake. Uninhabited by people, it was named Manitoba's first ecological reserve in May 1976, and was created under The Crown Lands Act. Reindeer Island is located approximately southeast of the community of Grand Rapids. Geography.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
In 1993, she moved to the Department of Animal Breeding and Genetics, Federal University of Agriculture, Abeokuta, Nigeria. She is currently a member of the University's Governing Council. She has served as a visiting scholar at the Roslin Institute in Scotland; the Poultry Breeding Institute in Hesaraghatta, India and Ohio State University in the United States. Awards and recognition.

Geographic entities mentioned:
surface_form: Hesaraghatta
instance_of: Lake
countries: India
coordinates: lat: 13.15
lon: 77.49
Iraq Ajami, along with the provinces on the southern shore of the Caspian Sea, also came under Muhammad ibn Abdallah's jurisdiction. In the latter, Gurgan and Tabaristan, he had appointed his brother Sulayman, whose administration was so oppressive that the local people rose in revolt in 864 and invited another Alid, Hasan ibn Zayd, to lead them.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Ali Dirani. Ali Dirani (born 1986 in Ryak, Bekaa, Lebanon) is a Lebanese graphic and visual artist, musician and drummer. Education. He graduated from the Fine Arts Institute of the Lebanese University and held his first solo exhibition, &quot;FRONT ROW&quot;, at the age of 24. This art exhibition consisted of nitrocellulose on canvas and neo-realism.

Geographic entities mentioned:
surface_form: Bekaa
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
Anderson, known commonly by his middle name Noble, was born in Ireland in 1865, and graduated in engineering and arts. Following short engineering engagements in Ireland, he came to Victoria in 1889, undertaking his first engineering in Victoria in connection with the Laanecoorie Weir. He then took up a lectureship in mechanical engineering at the University of Melbourne, where he met John Monash.

Geographic entities mentioned:
surface_form: Laanecoorie Weir
instance_of: Lake
countries: Australia
coordinates: lat: -36.836
lon: 143.889
Origins. SPC was incorporated in 1876 to purchase the unfinished Santa Clara Valley Company railroad at Dumbarton Point. Dumbarton Point was then a landing to transfer agricultural produce from the Santa Clara Valley for transport to San Francisco. Railway shops were built in Newark and a narrow gauge line to San Jose was completed in 1876.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
Zhanbay Island. Zhanbay Aral, or Dzhambayskiy Island (, &quot;Janbai araly&quot;), is a low, flat island in the Caspian Sea. It is located east of the mouths of the Volga. Administratively, Zhanbay Island belongs to Atyrau Region of Kazakhstan. Geography. Zhanbay Island is separated from the Kazakh coast by a 1.2 km wide channel. It has a length of 21.5 km and a maximum width of 7 km.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Nearby is the Pointe Percée. Geography. The lake is located downstream from the Bella-Cha valley, near the place called Les Confins, at the foot of the Aravis mountain range, below on the adret of the Col des Confins which allows you to reach the Bouchet valley on foot. Located at an altitude of 1,358 metres, it freezes over in winter. Activities.

Geographic entities mentioned:
surface_form: bouchet
instance_of: Lake
countries: France
coordinates: lat: 44.909166666667
lon: 3.7902777777778
Lac des Confins. Lac des Confins is a lake located just below the station of La Clusaz in the Haute-Savoie department in the Rhône-Alpes region in south-eastern France. The lake is situated at the foot of the Aravis Range. Nearby is the Pointe Percée. Geography.

Geographic entities mentioned:
surface_form: lac des confins
instance_of: Lake
countries: France
coordinates: lat: 45.915833333333
lon: 6.4761111111111
Mount Allen (Stewart Island). Mount Allen is the second-highest peak on Stewart Island in southern New Zealand. Located in the southwest of the island, it lies from the coast at Port Pegasus. Mount Allen rises to a height of and is the highest point in a short range of hills known as Tin Range. It is part of the Rakiura National Park.

Geographic entities mentioned:
surface_form: mount allen (stewart island)
instance_of: Mountain
countries: New Zealand
coordinates: lat: -47.085895
lon: 167.79881
Mount Allen (Stewart Island). Mount Allen is the second-highest peak on Stewart Island in southern New Zealand. Located in the southwest of the island, it lies from the coast at Port Pegasus. Mount Allen rises to a height of and is the highest point in a short range of hills known as Tin Range. It is part of the Rakiura National Park.

Geographic entities mentioned:
surface_form: mount allen
instance_of: Mountain
countries: New Zealand
coordinates: lat: -47.085895
lon: 167.79881
However, there were no practical results. In 1876, President Pedro Joaquín Chamorro Alfaro enacted a decree, calling for a construction of a railway from Corinto via Chinandega and León to the nearest port on Lake Managua (later Western division). The railway would be connected to the capital through steamboats.

Geographic entities mentioned:
surface_form: Lake Managua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 12.333333333333
lon: -86.416666666667
There were plans to extend the network to the Atlantic coast. A contract was signed in 1903. The line should have stretched 288 km from San Miguelito (a port at Lake Nicaragua) through a difficult terrain to Monkey Point at the Caribbean coast. In 1909, after constructing about of tracks, the works stopped and never resumed again. Nicaraguan railways never connected both coasts.

Geographic entities mentioned:
surface_form: Lake Nicaragua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 11.5742
lon: -85.3563
In 1833, when Winfield Smith was six, the family relocated to Monroe, Michigan. His father fought in the Black Hawk War in Illinois in the 1830s, but afterward went to work on harbor improvements on Lake Erie and served two terms in the Michigan Legislature. As a newly established state, there were few schools or formal education opportunities for Winfield.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
He represented the electoral district of Hants West in the Nova Scotia House of Assembly from June 1949 to March 1950. He was a member of the Nova Scotia Liberal Party. Born in 1900 at Mount Uniacke, Nova Scotia, Cole was the son of George and Elizabeth (Ward) Cole. Prior to the 1949 election, Cole defeated former Windsor mayor Gordon B. Crossley for the Liberal nomination in Hants West.

Geographic entities mentioned:
surface_form: Mount Uniacke, Nova Scotia
instance_of: Mountain
countries: Canada
coordinates: lat: 44.89194444444445
lon: -63.826388888888886
While en route, was detached to Cape Verde and was sent to East Africa, since reports indicated the situation in West Africa had calmed. and reached the Wouri River on 17 December. Shortly before their arrival, two anti-German groups burned down the village of a pro-German tribe.

Geographic entities mentioned:
surface_form: Wouri River
instance_of: Watercourse
countries: Cameroon
coordinates: lat: 4.0833
lon: 9.7
Poaching is conducted by organized groups within Chile; the group members trap the flamingos and export them to Europe, the United States, and other overseas destinations. The exportation process is conducted mainly in the Altiplano, which is an area that has deep cultural roots in egg poaching. During the reproductive season, local families also take eggs from flamingo nests.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Interlaken ship canal. The Interlaken ship canal () is a long canal in the Swiss canton of Bern. It connects Lake Thun with a quay in the town of Interlaken adjacent to Interlaken West railway station, thus allowing shipping services on the lake to serve the town and connect with railway services. It is still in regular use by the Lake Thun passenger ships of the BLS AG.

Geographic entities mentioned:
surface_form: Lake Thun
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.683333333333
lon: 7.7166666666667
As a consequence, the water level of the canal at Interlaken West is significantly lower than that of the adjacent river and surrounding land. At the other side of Interlaken, the uppermost reach of the Interlaken section of the Aar river is used by the Lake Brienz passenger ships of the BLS AG to reach Interlaken Ost railway station.

Geographic entities mentioned:
surface_form: Lake Brienz
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.716667
lon: 7.95
History. Shipping services on Lake Thun date back to at least 1834, when the first steamship was introduced to connect the towns of Thun and Interlaken, at each end of the lake. Interlaken is actually situated on an unnavigable section of the Aar river between Lake Brienz and Lake Thun, and initially services docked at Neuhaus, some away.

Geographic entities mentioned:
surface_form: Lake Thun
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.683333333333
lon: 7.7166666666667
History. Shipping services on Lake Thun date back to at least 1834, when the first steamship was introduced to connect the towns of Thun and Interlaken, at each end of the lake. Interlaken is actually situated on an unnavigable section of the Aar river between Lake Brienz and Lake Thun, and initially services docked at Neuhaus, some away.

Geographic entities mentioned:
surface_form: Lake Brienz
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.716667
lon: 7.95
They may be saprotrophic, mycorrhizal, or in the case of &quot;Caloscypha fulgens&quot;, pathogenic. History. William Bridge Cooke was the first to discuss the snowbank fungi as a distinct ecological group in 1944 when he discussed the fungal flora of Mount Shasta in California. He followed this with another publication 11 years later.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Monte Carpegna. Monte Carpegna is a mountain of Marche, Italy. It is the source of the Conca river.

Geographic entities mentioned:
surface_form: monte carpegna
instance_of: Mountain
countries: Italy
coordinates: lat: 43.80111111
lon: 12.32027778
USNS Spica. USNS &quot;Spica&quot; (T-AFS-9), was a combat stores ship acquired by the U.S. Navy from the United Kingdom in 1981. She participated in Operation Fiery Vigil to evacuate Clark Air Base personnel following the Mount Pinatubo Eruption in 1991. She served as part of the Military Sealift Command until she was deactivated in 2008. Before her U.S.

Geographic entities mentioned:
surface_form: Mount Pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Pyramid Formation (British Columbia). The Pyramid Formation is a stratigraphic unit of Pleistocene age in northwestern British Columbia, Canada. Name. The Pyramid Formation takes its name from The Pyramid, a prominent pyramid-shaped lava dome on the northeastern flank of Mount Edziza. Geology. Two subunits comprise the Pyramid Formation. The lower unit is a basal pyroclastic member up to thick.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Among the silicic domes are Sphinx Dome, Pharaoh Dome and The Pyramid. The Pyramid Formation has a volume of, making it the eighth most voluminous geological formation of the Mount Edziza volcanic complex after the Little Iskut Formation. It overlies the Nido Formation and underlies the Ice Peak and Edziza formations, all of which have formed in the last 8 million years.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
The city has expanded to three adjacent hills. Geography. Beitar Illit lies in the northern Judean Hills at about 700 m above sea level. It is located just west of the intersection of Route 60, the north–south artery which roughly follows the watershed from Nazareth through Jerusalem to Beersheba, and Route 375, which descends west into the Elah Valley to the coastal plain and Tel Aviv area.

Geographic entities mentioned:
surface_form: Elah Valley
instance_of: Valley
countries: Israel
coordinates: lat: 31.6806252
lon: 34.9891247
The Geisberg () is a 262 m high mountain at Mülheim on Moselle, in Germany. It is a remnant of a dry fallen meander of the river Moselle. Geography. The Geisberg is a narrow, elongated mountain ridge in a valley widening of the Middle Moselle. Surrounded by a wide circulating valley, it stands isolated from the other Moselle Hills and the adjacent Haardtwald Hills of the Hunsrück.

Geographic entities mentioned:
surface_form: hunsrück
instance_of: Mountain
countries: Germany
coordinates: lat: 51.026111111111
lon: 9.1008333333333
The peaks are lying 80 to 100 m above the level of the surrounding valley. The Geisberg is located in the region of the Middle Moselle. It belongs to the right-hand side, the Hunsrück facing Moselle Hills, which are part of the Rhenish Massif on the left bank of the river Rhine.

Geographic entities mentioned:
surface_form: hunsrück
instance_of: Mountain
countries: Germany
coordinates: lat: 51.026111111111
lon: 9.1008333333333
The Geisberg became the first and oldest circulating mountain in this area, before the Noviander Hüttenkopf and the Maring Mountain. Today the rivulets Frohnbach and Veldenzer Bach are flowing through the former Moselle valley at the Geisberg. Both come from the Hunsrück and had to relocate their estuaries after the Moselle had taken another course.

Geographic entities mentioned:
surface_form: hunsrück
instance_of: Mountain
countries: Germany
coordinates: lat: 51.026111111111
lon: 9.1008333333333
Geisberg (Middle Moselle). The Geisberg () is a 262 m high mountain at Mülheim on Moselle, in Germany. It is a remnant of a dry fallen meander of the river Moselle. Geography. The Geisberg is a narrow, elongated mountain ridge in a valley widening of the Middle Moselle.

Geographic entities mentioned:
surface_form: geisberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.8889
lon: 11.0624
surface_form: geisberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.88916666666667
lon: 7.010833333333333
The Geisberg () is a 262 m high mountain at Mülheim on Moselle, in Germany. It is a remnant of a dry fallen meander of the river Moselle. Geography. The Geisberg is a narrow, elongated mountain ridge in a valley widening of the Middle Moselle. Surrounded by a wide circulating valley, it stands isolated from the other Moselle Hills and the adjacent Haardtwald Hills of the Hunsrück.

Geographic entities mentioned:
surface_form: geisberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.8889
lon: 11.0624
surface_form: geisberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.88916666666667
lon: 7.010833333333333
The peaks are lying 80 to 100 m above the level of the surrounding valley. The Geisberg is located in the region of the Middle Moselle. It belongs to the right-hand side, the Hunsrück facing Moselle Hills, which are part of the Rhenish Massif on the left bank of the river Rhine.

Geographic entities mentioned:
surface_form: geisberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.8889
lon: 11.0624
surface_form: geisberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.88916666666667
lon: 7.010833333333333
The predominant rocks are Clay Slate and Greywacke from the Lower Devonian which is not quite water resistant. Genesis. From the Quaternary onwards, the Moselle formed Meander in an originally flat plain with a balanced, flat undulating relief and cut progressively into today's narrow valley. At the beginning of the Upper Middle Terrace period, the Geisberg was a peninsula in a Moselle meander.

Geographic entities mentioned:
surface_form: geisberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.8889
lon: 11.0624
surface_form: geisberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.88916666666667
lon: 7.010833333333333
Further breakthroughs followed at the villages of Noviand and Maring. The Geisberg became the first and oldest circulating mountain in this area, before the Noviander Hüttenkopf and the Maring Mountain. Today the rivulets Frohnbach and Veldenzer Bach are flowing through the former Moselle valley at the Geisberg.

Geographic entities mentioned:
surface_form: geisberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.8889
lon: 11.0624
surface_form: geisberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.88916666666667
lon: 7.010833333333333
The Geisberg became the first and oldest circulating mountain in this area, before the Noviander Hüttenkopf and the Maring Mountain. Today the rivulets Frohnbach and Veldenzer Bach are flowing through the former Moselle valley at the Geisberg. Both come from the Hunsrück and had to relocate their estuaries after the Moselle had taken another course.

Geographic entities mentioned:
surface_form: geisberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.8889
lon: 11.0624
surface_form: geisberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.88916666666667
lon: 7.010833333333333
Silverado Resort and Spa. The Silverado Resort and Spa is a golf, tennis, and spa resort in Napa County, California, United States. The venue is named after the Silverado Mine, a quicksilver mine near Mount Saint Helena. The resort is the fifth largest employer in Napa County.

Geographic entities mentioned:
surface_form: Mount Saint Helena
instance_of: Mountain
countries: United States
coordinates: lat: 38.669333333333
lon: -122.63355
He was inducted into the U.S. Ski and Snowboard Hall of Fame in April 2012. Dorworth was also a member of the &quot;Fun Hogs&quot; expedition (together with Yvon Chouinard, Chris Jones, Douglas Tompkins, and Lito Tejada-Flores), who made the third ascent of Mount Fitz Roy in Patagonia in 1968.

Geographic entities mentioned:
surface_form: Mount Fitz Roy
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -49.271388888889
lon: -73.043333333333
The north town line is the border of Monroe County. The Genesee River defines the west town line, flowing northward past Avon village. Conesus Creek, flowing from Conesus Lake, empties into the Genesee, west of Avon village. U.S. Route 20 and New York State Route 5 are east-west highways across the town and intersect New York State Route 39 in Avon village.

Geographic entities mentioned:
surface_form: Conesus Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.779722222222
lon: -77.716666666667
It lies on the border between the Most Basin and Central Bohemian Uplands. The highest point is the hill Jizerský vrch at above sea level. The Bílina River flows through the town. A small part of Lake Milada extends into the territory of Trmice. History. In the 13th century, there was a fortress in Trmice. In the first half of the 17th century, it was rebuilt into a Baroque castle.

Geographic entities mentioned:
surface_form: Lake Milada
instance_of: Lake
countries: Czech Republic
coordinates: lat: 50.653611111111
lon: 13.944444444444
Rainbow Falls Provincial Park. Rainbow Falls Provincial Park is a recreation-class provincial park within the Ontario Parks system. This park consists of two non-contiguous parts: Whitesand Lake campground in the main park, and the historic Rossport Campground, east of the fishing community of Rossport, Ontario, which provides campsites along the rough and rocky shorelines of Lake Superior.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The FM signal - 11kW ERP - is broadcast from the Sutton Coldfield transmitter. The station is available on DAB, thanks to eight transmitters throughout the West Midlands on the MXR 12A multiplex, with strong signals from The Wrekin and Ilmington in south Warwickshire. News.

Geographic entities mentioned:
surface_form: The Wrekin
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.66916666666667
lon: -2.551388888888889
Legend of Puteri Gunung Ledang. The legend revolves around a celestial princess who lived on Mount Ledang, located in present-day Tangkak District, Johor, Malaysia. Hikayat Hang Tuah. &quot;Puteri Gunung Ledang&quot; is mentioned by name to be the sultan's daughter (or a citizen, depending on how you view the translation of anak perempuan kita&quot;<nowiki/>' as). Sejarah Melayu/Sulalatus Salatin.

Geographic entities mentioned:
surface_form: Mount Ledang
instance_of: Mountain
countries: Malaysia
coordinates: lat: 2.3741666666667
lon: 102.60777777778