Sarmila/GeoWiki-Features huggingface dataset:
Pyhäjärvi (Tampere region). Pyhäjärvi () is a lake in southern Finland. Although the name means &quot;holy lake&quot; in modern Finnish, it probably originally meant &quot;border lake&quot;. Pyhäjärvi is shaped like the letter C with the cities of Tampere and Nokia at the northern end, and the town of Lempäälä at the southern end.

Geographic entities mentioned:
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.48333333
lon: 23.66666667
Due to the Tammerkoski rapids, the water in Pyhäjärvi is warmer and richer in ozone than that in the northern lake, Näsijärvi, which results in the life in this lake being richer, even though the water is more polluted. A number of other lakes are also named Pyhäjärvi in Finland and its former territories.

Geographic entities mentioned:
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.48333333
lon: 23.66666667
Natural history. The White Peak area of the county is named after the limestone landscape of the Derbyshire Dome anticline. The carboniferous limestone was formed about 300 million years ago and the plateau is generally between 200m and 300m above sea level.

Geographic entities mentioned:
surface_form: White Peak
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 53.2
lon: -1.8
The carboniferous limestone was formed about 300 million years ago and the plateau is generally between 200m and 300m above sea level. This limestone outcrop is surrounded on the west, north and east by a horseshoe-shaped formation of younger sandstones (gritstones) and shales, known as the Dark Peak. Prehistory.

Geographic entities mentioned:
surface_form: Dark Peak
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 53.4
lon: -1.8
The remains of a Stone Age settlement (a Mesolithic timber roundhouse and of two Neolithic longhouses) was discovered in 1984 at Lismore Fields in Buxton. There were Iron Age hillforts at Castle Naze (overlooking Chapel-en-le-Frith), Fin Cop (near Ashford-in-the-Water) and Mam Tor (overlooking Castleton). These sites are nearly all protected Scheduled Monuments. Roman.

Geographic entities mentioned:
surface_form: Fin Cop
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.2358
lon: -1.73694
Lead has been mined in Derbyshire since Roman times. In the late 16th century watered-powered smelting mills, with furnaces fired by wood or charcoal, were introduced to smelt lead ore on an industrial scale. Magpie Mine near Bakewell, Lathkill Dale mines and the Beans and Bacon mine near Bonsall adopted innovative machinery to increase production throughout the 17th to 19th centuries.

Geographic entities mentioned:
surface_form: Lathkill Dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.1896
lon: -1.71446
The Sanctuary of the Immaculate Conception on San Cristóbal Hill is one of the principal places of worship for the Catholic Church of Chile, as well as being an icon of Santiago, Chile. It is notable in particular for a large statue of the Immaculate Conception, which is located at the summit of San Cristóbal Hill, some 863 meters above sea level. Sanctuary and statue.

Geographic entities mentioned:
surface_form: San Cristóbal Hill
instance_of: Mountain
countries: Chile
coordinates: lat: -33.42527778
lon: -70.63333333
It is northwest of the small community of Telegraph Creek and just southwest of Callison Ranch. With a maximum elevation of, it rises above the surrounding landscape on the Nahlin Plateau, which is part of the western Stikine Plateau. Heart Peaks has been an area of prospecting since the 1980s with the discovery of precious metals.

Geographic entities mentioned:
surface_form: Nahlin Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.44972222222222
lon: -131.41833333333332
surface_form: Stikine Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
The knowledge of Heart Peaks is limited, especially its eruptive history. Setting. Heart Peaks is part of the Northern Cordilleran Volcanic Province, a long volcanic chain extending from just north of the city of Prince Rupert in British Columbia through Yukon to the Alaska border. Along this line, the North American Plate has been rupturing.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
This indicates that Heart Peaks has a topographic prominence of at least. More than 20 unnamed creeks flow from the volcano, which drain into the nearby Dudidontu and Sheslay rivers. With an area of about and a volume of less than, Heart Peaks is the third-largest volcano in the Northern Cordilleran Volcanic Province, exceeded by the Mount Edziza and Level Mountain shields, which cover more than.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
With an area of about and a volume of less than, Heart Peaks is the third-largest volcano in the Northern Cordilleran Volcanic Province, exceeded by the Mount Edziza and Level Mountain shields, which cover more than. Heart Peaks is over five times larger than the Mount Meager massif in southwestern British Columbia, the largest stratovolcano by volume in the Garibaldi Volcanic Belt.

Geographic entities mentioned:
surface_form: Garibaldi Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
surface_form: mount meager
instance_of: Mountain
countries: Canada
coordinates: lat: 50.63166667
lon: -123.50416667
This indicates that the Finlay tephras are Early Holocene in age and were deposited shortly after the regional Fraser Glaciation retreated. The Finlay tephras are largely composed of elements most similar to those of Hoodoo Mountain, a flat-topped volcano that formed subglacially at least 100,000 years ago.

Geographic entities mentioned:
surface_form: Hoodoo Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
However, its north flank is rounded and relatively smooth while its south flank is rather pointed. The highest elevation of Heart Peaks is at a small peak roughly in the middle of its summit plateau while the regional elevation of the Nahlin Plateau is. This indicates that Heart Peaks has a topographic prominence of at least.

Geographic entities mentioned:
surface_form: nahlin plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.44972222222222
lon: -131.41833333333332
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
Heart Peaks. Heart Peaks, originally known as the Heart Mountains, is a mountain massif in the Northern Interior of British Columbia, Canada. It is northwest of the small community of Telegraph Creek and just southwest of Callison Ranch. With a maximum elevation of, it rises above the surrounding landscape on the Nahlin Plateau, which is part of the western Stikine Plateau.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
surface_form: heart mountains
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The west coast of North America is the site of plate margins between the large Pacific and North American plates, and also between the smaller Juan de Fuca and Cocos plates. Tectonic activity along the North Coast of British Columbia and Southeast Alaska is characterized by transform movements of the Queen Charlotte Fault, a plate boundary where the Pacific Plate skids by the North American Plate.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Finlay tephras. Heart Peaks is one of the four volcanoes in the Northern Cordilleran Volcanic Province suggested to have erupted the Finlay tephras. These are situated throughout northwestern British Columbia and likely extend east into the Canadian Rockies. In the Finlay River and Dease Lake areas, two tephra deposits are situated between sand, silt, mud and gravel.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The name origins are unknown as they have not been recorded. A number of other mountain features in British Columbia also had their name changed in 1947, such as the Rainbow Range, which was originally named &quot;Rainbow Mountains&quot;. The name &quot;Heart Peaks&quot; officially refers to two small peaks situated on top of the shield volcano, located at.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
However, no tephras or pyroclastic rocks have been found at Hoodoo Mountain that were erupted the same time as these lava flows. Therefore, other possible sources have been proposed. At the Mount Edziza volcanic complex, basalts of probable Late Pleistocene to Early Holocene age have been found, but their exact ages and chemical compositions are not well known.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Heart Peaks. Heart Peaks, originally known as the Heart Mountains, is a mountain massif in the Northern Interior of British Columbia, Canada. It is northwest of the small community of Telegraph Creek and just southwest of Callison Ranch. With a maximum elevation of, it rises above the surrounding landscape on the Nahlin Plateau, which is part of the western Stikine Plateau.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
With a maximum elevation of, it rises above the surrounding landscape on the Nahlin Plateau, which is part of the western Stikine Plateau. Heart Peaks has been an area of prospecting since the 1980s with the discovery of precious metals. Situated in a large area of volcanic activity, Heart Peaks consists of a large shield volcano.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
Heart Peaks has been an area of prospecting since the 1980s with the discovery of precious metals. Situated in a large area of volcanic activity, Heart Peaks consists of a large shield volcano. It was formed in the past 23 million years by repeated eruptions of lava and rock. However, present day eruptions have not been observed.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
It was formed in the past 23 million years by repeated eruptions of lava and rock. However, present day eruptions have not been observed. A number of related volcanoes are adjacent to Heart Peaks and form an extensive volcanic zone over long. The knowledge of Heart Peaks is limited, especially its eruptive history. Setting.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
Structure. The nearly oval-shaped Heart Peaks shield volcano is made of basalt and trachybasalt with a composite thickness up to; pyroclastic rocks are also present. It lies just west of the much larger Level Mountain shield and southwest of the Kawdy volcanoes.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
It lies just west of the much larger Level Mountain shield and southwest of the Kawdy volcanoes. A series of steep-sided lava domes composed of porphyritic rhyolite and minor trachyte are situated on the western flank of Heart Peaks and display colours such as light green and pink. Rhyolitic lava domes are also present on its summit.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
Rhyolitic lava domes are also present on its summit. The shield is surrounded by tributaries of the Inklin River, which flows northwest into the Taku River. Heart Peaks is at least long and no more than wide at its base. The west and east flanks of the volcano are dissected, giving it a rugged appearance.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
The highest elevation of Heart Peaks is at a small peak roughly in the middle of its summit plateau while the regional elevation of the Nahlin Plateau is. This indicates that Heart Peaks has a topographic prominence of at least. More than 20 unnamed creeks flow from the volcano, which drain into the nearby Dudidontu and Sheslay rivers.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
Heart Peaks is over five times larger than the Mount Meager massif in southwestern British Columbia, the largest stratovolcano by volume in the Garibaldi Volcanic Belt. The area surrounding Heart Peaks is largely undeveloped, with Callison Ranch being the only locality. Vegetation at the volcano is present mainly on its flanks as its broad summit consists of a rocky plateau.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
The area surrounding Heart Peaks is largely undeveloped, with Callison Ranch being the only locality. Vegetation at the volcano is present mainly on its flanks as its broad summit consists of a rocky plateau. Because of its remote location, Heart Peaks is accessed by helicopter from the small communities of Atlin and Dease Lake. Background.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
surface_form: dease lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.63502
lon: -130.03761
surface_form: atlin
instance_of: Lake
countries: Canada
coordinates: lat: 60.0133333
lon: -133.8308333
Because of its remote location, Heart Peaks is accessed by helicopter from the small communities of Atlin and Dease Lake. Background. Little is known about the eruptive history of Heart Peaks because it has not been studied in detail by scientists. The exact age of Heart Peaks is not known, but its first volcanic phase occurred during the Neogene period (between 23 and 2.5 million years ago).

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
The exact age of Heart Peaks is not known, but its first volcanic phase occurred during the Neogene period (between 23 and 2.5 million years ago). The variety of volcanic deposits at Heart Peaks indicates that it has a history of producing not only fluid and passive basaltic lava flows, but also more silica-rich trachyte and rhyolitic lavas and explosive eruptions.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
Features created by subglacial eruptions are also present. The latest volcanic phase at Heart Peaks is largely Pleistocene (between 2.5 million and 10,000 years ago) in age and late-stage Holocene (10,000 years ago to present) activity is uncertain. This is partly because it is unknown whether Holocene volcanic rocks exist at the volcano. Nevertheless, the last eruption at Heart Peaks is unknown.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
The latest volcanic phase at Heart Peaks is largely Pleistocene (between 2.5 million and 10,000 years ago) in age and late-stage Holocene (10,000 years ago to present) activity is uncertain. This is partly because it is unknown whether Holocene volcanic rocks exist at the volcano. Nevertheless, the last eruption at Heart Peaks is unknown. Finlay tephras.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
Nevertheless, the last eruption at Heart Peaks is unknown. Finlay tephras. Heart Peaks is one of the four volcanoes in the Northern Cordilleran Volcanic Province suggested to have erupted the Finlay tephras. These are situated throughout northwestern British Columbia and likely extend east into the Canadian Rockies.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
At the Mount Edziza volcanic complex, basalts of probable Late Pleistocene to Early Holocene age have been found, but their exact ages and chemical compositions are not well known. Because Heart Peaks and nearby Level Mountain have been poorly studied and it is unknown if they contain Holocene age volcanic rocks, they are also possible sources for the Finlay tephras. Naming.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Naming. The name &quot;Heart Mountains&quot; was adopted in the BC Gazetteer of 1930 with coordinates placing the massif at. Subsequently, it was renamed to &quot;Heart Peaks&quot; on May 6, 1947 and coordinates improved to. The name origins are unknown as they have not been recorded.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
The name &quot;Heart Peaks&quot; officially refers to two small peaks situated on top of the shield volcano, located at. Because the shield volcano consists of a single landmass and the name &quot;Heart Peaks&quot; was officially given for two peaks on its summit, it is sometimes known as &quot;Heart Peak&quot; to avoid confusion.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
Because the shield volcano consists of a single landmass and the name &quot;Heart Peaks&quot; was officially given for two peaks on its summit, it is sometimes known as &quot;Heart Peak&quot; to avoid confusion. Heart Peaks is also known as &quot;HP&quot; in scientific documents and on geological maps. Mineral explorations.

Geographic entities mentioned:
surface_form: heart peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
Naming. The name &quot;Heart Mountains&quot; was adopted in the BC Gazetteer of 1930 with coordinates placing the massif at. Subsequently, it was renamed to &quot;Heart Peaks&quot; on May 6, 1947 and coordinates improved to. The name origins are unknown as they have not been recorded.

Geographic entities mentioned:
surface_form: heart mountains
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
These are situated throughout northwestern British Columbia and likely extend east into the Canadian Rockies. In the Finlay River and Dease Lake areas, two tephra deposits are situated between sand, silt, mud and gravel. They are both phonolitic to trachytic in composition and high in iron(II) oxide, indicating that the tephras were possibly erupted from a single volcano.

Geographic entities mentioned:
surface_form: dease lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.63502
lon: -130.03761
As the Pacific Plate moves northward to the Aleutian subduction zone, it generates rifting in the North American continent. Magma rises along cracks created by the rifting, and eventually erupts on the surface to form a volcano. This geological process has, over time, created the Northern Cordilleran Volcanic Province, which is the most volcanically active area in Canada.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Structure. The nearly oval-shaped Heart Peaks shield volcano is made of basalt and trachybasalt with a composite thickness up to; pyroclastic rocks are also present. It lies just west of the much larger Level Mountain shield and southwest of the Kawdy volcanoes.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Two phonolitic lava flows on its south flank were erupted between 10,000 and 9,000 years ago and remain unglaciated. They have a similar chemistry to the glass composition of the Finlay tephras. However, no tephras or pyroclastic rocks have been found at Hoodoo Mountain that were erupted the same time as these lava flows. Therefore, other possible sources have been proposed.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
Progression. The fire was started by lightning strikes east of Loyalton along the eastern edge of the Sierra Valley, near Mount Ina Coolbrith on the Tahoe National Forest. A fire lookout on Smith Peak in the Plumas National Forest first reported smoke from the burgeoning fire to the Plumas dispatch center in Quincy at 4:27 p.m. PDT on Friday, August 14.

Geographic entities mentioned:
surface_form: Sierra Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.77083333
lon: -120.32777778
Lake Christabel. Lake Christabel is a small lake in the north of New Zealand's South Island. It is located 12 kilometres southwest of the Lewis Pass. The lake is the source of the Grey River, one of the longest rivers on the South Island's West Coast, although its outlet is underground. The lake lies behind a landslide dam, thought to have been created by a prehistoric earthquake.

Geographic entities mentioned:
surface_form: lake christabel
instance_of: Lake
countries: New Zealand
coordinates: lat: -42.408
lon: 172.242
Marincello. Marincello was a failed development project in Marin County, California that would have put a planned community atop the Marin Headlands, overlooking the Golden Gate. Its upheaval set the precedent for Marin County's rigid anti-development stance and push for open space. Pre-Marincello years.

Geographic entities mentioned:
surface_form: Marin Headlands
instance_of: Landform
countries: United States
coordinates: lat: 37.827777777778
lon: -122.50611111111
Pre-Marincello years. The land making up the Marin Headlands was purchased by the US military in 1851, shortly after California became a state, for the installation of coastal defense guns. Other than building Forts Barry, Baker, and Cronkhite, and planting trees and vegetation to camouflage the forts from attack, the Marin Headlands was left in its native form.

Geographic entities mentioned:
surface_form: Marin Headlands
instance_of: Landform
countries: United States
coordinates: lat: 37.827777777778
lon: -122.50611111111
Shingobee Bay. Shingobee Bay is a bay of Leech Lake, Minnesota. Information. Shingobee Bay is located three miles south of Walker, the Cass County seat, on the southern side of Leech Lake. The land adjacent to the bay is part of Shingobee Township, and a portion of it is allocated to the Leech Lake Tribe of Ojibwe.

Geographic entities mentioned:
surface_form: Leech Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.166666666667
lon: -94.366666666667
The issue of professionalism was disputed during these Games when a number of alpine skiers were found to have participated in a ski camp at Mammoth Mountain in the United States; three days before the opening ceremony, IOC president Avery Brundage threatened to bar the skiers from competing in the Games as he insisted that they were no longer amateurs having benefited financially from their status as athletes.

Geographic entities mentioned:
surface_form: Mammoth Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6306
lon: -119.033
Legore Lake. LeGore Lake is a tarn located in the Eagle Cap Wilderness of northeastern Oregon, United States. It is the highest true lake in Oregon at elevation. It is positioned near Twin Peaks and is accessed by a 4-mile &quot;extremely steep uphill&quot; hiking trail that ascends 4,000 feet and passes the LeGore mine, the lake's namesake.

Geographic entities mentioned:
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 37.7516
lon: -122.448
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 43.16
lon: -109.659
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 37.589722222222
lon: -105.51916666667
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 40.59384
lon: -111.72104
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 36.66181
lon: -118.71414
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 45.303888888889
lon: -117.34388888889
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 39.0423585
lon: -106.4254736
surface_form: twin peaks
instance_of: Landform
countries: United States
coordinates: lat: 37.0797
lon: -121.69
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 40.92892
lon: -115.84438
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 40.794722222222
lon: -111.84111111111
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 40.551944444444
lon: -111.65666666667
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 38.08298
lon: -119.35322
Legore Lake. LeGore Lake is a tarn located in the Eagle Cap Wilderness of northeastern Oregon, United States. It is the highest true lake in Oregon at elevation. It is positioned near Twin Peaks and is accessed by a 4-mile &quot;extremely steep uphill&quot; hiking trail that ascends 4,000 feet and passes the LeGore mine, the lake's namesake.

Geographic entities mentioned:
surface_form: eagle cap
instance_of: Mountain
countries: United States
coordinates: lat: 45.1636
lon: -117.302
surface_form: legore lake
instance_of: Lake
countries: United States
coordinates: lat: 45.3096
lon: -117.3466
Legore Lake. LeGore Lake is a tarn located in the Eagle Cap Wilderness of northeastern Oregon, United States. It is the highest true lake in Oregon at elevation. It is positioned near Twin Peaks and is accessed by a 4-mile &quot;extremely steep uphill&quot; hiking trail that ascends 4,000 feet and passes the LeGore mine, the lake's namesake.

Geographic entities mentioned:
surface_form: legore lake
instance_of: Lake
countries: United States
coordinates: lat: 45.3096
lon: -117.3466
It was positioned roughly south-southeast of Lake Charles at the time. The cyclone continued north-northeast and crossed the southeastern Louisiana coastline around 07:00 UTC. It progressed inland across the Eastern United States, crossed Lake Huron, and finally dissipated over southeastern Ontario by 00:00 UTC on October 28. Preparations and impact.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Only a few rivers reached flood stage and mainly minor flooding was reported across the state. Water levels of above normal in southeastern Louisiana did cause minor coastal flooding there, including across the Mandeville Lakefront along the northern shore of Lake Pontchartrain. Coastal flooding of affected the central Louisiana coastline around high tide.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
This precipitation alleviated a flash drought from September. Farther north in Ontario, already-high water levels on Lake Erie were exacerbated by strong winds, sustained at and gusting to in Port Colborne. A water rise of at least was reported, causing the lake to overflow its banks and cause a number of road closures in Port Dover, Long Point, and Turkey Point.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The nearby Niagara River also caused local inundation and road closures as waves up to crested over breakwaters across Fort Erie and Crystal Beach. Rainfall amounts of were commonplace throughout southern Ontario, highest at on the opposing end of Lake Ontario in Oswego, New York. Aftermath. In the aftermath of the storm in Louisiana, St.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Skiing Everest. &quot;Skiing Everest&quot; is a 2009 American adventure documentary directed by Les Guthman and Mike Marolt; written by Les Guthman, and featuring high-altitude ski mountaineers Mike Marolt, Steve Marolt, John Callahan, Jim Gile, Hans Kammerlander, Chris Davenport, Laura Bakos, Mark Newcomb. The film also features Fredrik Ericsson, who died skiing on K2 in 2010.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
Filmed by Mike Marolt over ten years, &quot;Skiing Everest&quot; tells the story of a group of friends, led by Marolt and his twin brother Steve, who grew up in Aspen, Colorado, and went on to become the first skiers from the Western Hemisphere to ski from above when they skied from the summit of Shisha Pangma in Tibet in 2000, and then tried the highest slopes in the world on Mount Everest and Cho Oyu.

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: Cho Oyu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 28.094166666667
lon: 86.660833333333
The main causes of biodiversity loss are changes in natural habitats due to intensive agricultural production, construction and extractive industries, over exploitation of habitats and invasions and introductions of alien species. With the exception of Fennoscandia and northern Russia, few areas of untouched wilderness are currently found in Europe, except for various national parks.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
The Chorley cake from Chorley is often seen as the most similar variant of the Eccles cake. The Blackburn cake is named after the town of Blackburn and is made with stewed apples in place of currants. In East Lancashire, a cake known as a &quot;sad cake&quot;, can be found in the Darwen, Blackburn, Accrington, Burnley, Colne, Nelson, Padiham areas and throughout the Rossendale area.

Geographic entities mentioned:
surface_form: Rossendale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.7031
lon: -2.2893
Carne in 1974, and named in honor of Ukrainian-Australian entomologist and artist Stefan Misko. The species is limited in its distribution to east New South Wales — the holotype was collected by Stefan Misko and Everard Baldwin Britton from Apsley Falls in the Northern Tablelands region of New South Wales. The beetles are medium brown in color, they are nocturnal and are attracted to lights.

Geographic entities mentioned:
surface_form: Northern Tablelands
instance_of: Plateau
countries: Australia
coordinates: lat: -30.595277777777778
lon: 151.5
Matteo Balducci. Matteo Balducci was an Italian painter of the Renaissance. He was born in Fontignano, a small town near Lake Trasimeno in Perugia. Balducci was an associate of Giovanni Antonio Bazzi between 1517 and 1523. The following year he painted an altar-piece in San Francesco di Pian Castagniano in Monte Amiata in Tuscany.

Geographic entities mentioned:
surface_form: Lake Trasimeno
instance_of: Lake
countries: Italy
coordinates: lat: 43.14
lon: 12.1
Balducci was an associate of Giovanni Antonio Bazzi between 1517 and 1523. The following year he painted an altar-piece in San Francesco di Pian Castagniano in Monte Amiata in Tuscany. He also painted in churches of Siena, including an &quot;Assumption of the Virgin&quot; in the Capella Borghesi of Santo Spirito and a &quot;Nativity&quot; in Santa Maria Maddalena.

Geographic entities mentioned:
surface_form: Monte Amiata
instance_of: Mountain
countries: Italy
coordinates: lat: 42.88775
lon: 11.624369444444
Rhondda. In Rhondda, there is a fflecsi 152 service on the former 152 scheduled bus route, covering Hendreforgan, Tonyrefail and Tonypandy. The services are operating in partnership with Stagecoach and Rhondda Cynon Taf County Borough Council. Prestatyn. In Prestatyn, fflecsi replaced the 40 bus route, operated by Townlynx.

Geographic entities mentioned:
surface_form: Rhondda
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
Butler Lake. Butler Lake is a small lake south of Wilmurt in Herkimer County, New York. It drains north via an unnamed creek that flows into West Canada Creek. Butler Lake is home to a pair of who migrate in each spring to rear their young. The lake is only just large enough as they require a &quot;long runway&quot; of water from which to take off. Atwood Lake is located east of Butler Lake.

Geographic entities mentioned:
surface_form: butler lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3667363
lon: -75.9121377
It originates about 50 km east of Curicó, at the confluence of the Colorado River and the Los Patos River. Both rivers have their origin next to the volcanos Descabezado Chico and Descabezado Grande. The Lontué River forms the Mataquito River at the union with the Teno River that runs to the north, about 10 kilometers west of Curicó near the locality of Sagrada Familia.

Geographic entities mentioned:
surface_form: Descabezado Grande
instance_of: Mountain
countries: Chile
coordinates: lat: -35.583333333333
lon: -70.75
This poppy is very rare and is found in low numbers; there could be as few as a few dozen individuals on 100 m2 It is found on limestone rocks on the slopes of Pirin's highest summit Vihren (2,914 m), the knife-edge ridge Koncheto that links the peaks Kutelo (2,908 m) and Banski Suhodol (2,884 m), Golemiya Kazan cirque and the surrounding summits.

Geographic entities mentioned:
surface_form: Koncheto
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 41.782152
lon: 23.393113
The Advanced School of the NSDAP (, literally &quot;High School of the NSDAP&quot;) was a project by the chief ideologist of the Nazi Party Alfred Rosenberg to create an elite Nazi university, a kind of academy for party officials. A monumental central university building was to be built on the shores of Lake Chiemsee, based on the architectural plans of Hermann Giesler. History.

Geographic entities mentioned:
surface_form: Chiemsee
instance_of: Lake
countries: Germany
coordinates: lat: 47.89
lon: 12.47
Early life. The son of a teacher and an electrical engineer, Bulcock was born Philip Garry Pickup in Jericho, Bury but was raised by his mother and step-father in the Rossendale Valley and Poole changing schools repeatedly due to frequent re-location. He was a student at both Bacup and Rawtenstall Grammar School and Poole Grammar School before moving to London to attend drama school. Training.

Geographic entities mentioned:
surface_form: Rossendale Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.7031
lon: -2.2893
Beginning with the 2024 edition, it became part of the Gran Canaria World Trail Majors race series. FUJI 100mi course. The 166 km course circulates around Mount Fuji, cumulatively gaining 7,038 m of altitude. Runners must complete the course in under 44.5 hours. The finish venue is Fuji Hokuroku Park.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
The main sportfish in the three lakes are Northern Pike, although Yellow Perch have been caught in the lakes. The lakes are located in Ponoka County, Alberta and Lacombe County, Alberta, and are located southeast of Ponoka and northwest of Lacombe. Red Deer, Nelson lake, and Gadsby lake are not located far from Chain lakes.

Geographic entities mentioned:
surface_form: gadsby lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.54
lon: -113.23361
surface_form: nelson lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.2759
lon: -62.7261
surface_form: nelson lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.7235
lon: -63.4277
surface_form: nelson lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.9694
lon: -63.7006
Red Deer, Nelson lake, and Gadsby lake are not located far from Chain lakes. Parlby creek, which provides inflow and outflow to all of the lakes, eventually flows into Spotted lake, Buffalo Lake, and lies in the Red Deer River basin even though it is located closer to the Battle River. North Chain Lake. North Chain lake is the northernmost of the series of lakes.

Geographic entities mentioned:
surface_form: buffalo lake
instance_of: Lake
countries: Canada
coordinates: lat: 60.233333333333
lon: -115.43333333333
surface_form: spotted lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.07805555555556
lon: -119.56666666666666
surface_form: buffalo lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.466666666667
lon: -112.9
Chain Lakes, Alberta. The Chain Lakes are a series of three lakes located north of Clive in the Canadian province of Alberta. These lakes are connected by Parlby Creek, which provides inflow and outflow for all three lakes. The main sportfish in the three lakes are Northern Pike, although Yellow Perch have been caught in the lakes.

Geographic entities mentioned:
surface_form: chain lakes, alberta
instance_of: Body of water
countries: Canada
Stellenbosch Mountain. Stellenbosch Mountain (Afrikaans: Stellenbosberg or Die Groteberg) is a mountain forming a prominent landmark overlooking the town of Stellenbosch in the Western Cape Province of South Africa. The mountain forms part of the Coetsenburg Estate, the Jonkershoek Nature Reserve, the Assegaaibosch Nature Reserve and the larger Hottentots-Holland Mountains Catchment Area. Geology.

Geographic entities mentioned:
surface_form: stellenbosch mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.9698
lon: 18.9008
The mountain forms part of the Coetsenburg Estate, the Jonkershoek Nature Reserve, the Assegaaibosch Nature Reserve and the larger Hottentots-Holland Mountains Catchment Area. Geology. The peak of Stellenbosch Mountain is 1,156m. The source of the Blaauwklippen (Blouklip) River is near the peak. The range is primarily composed of Table Mountain Sandstone.

Geographic entities mentioned:
surface_form: stellenbosch mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.9698
lon: 18.9008
In winter, there is much more rainfall than in summer. Snow is not unusual on the peak during winter. The Hottentots Holland Mountains, of which the Stellenbosch Mountain is a peak, are considered the hub of the Cape floristic region with the most biodiversity in the entire fynbos biome. The surrounding lowlands have rich alluvial soils supporting viticulture and other deciduous fruit farms.

Geographic entities mentioned:
surface_form: stellenbosch mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.9698
lon: 18.9008
Wildlife. The Jonkershoek Mountains, of which Stellenbosch Mountain is a peak, are home to leopards, caracals, klipspringer, Chacma baboons, honey badgers and mongooses, however, all but the baboons are very secretive. Birdlife includes kingfishers, black eagles, African fish eagles, spotted eagle owls, sugarbirds, orange-breasted sunbirds and protea seedeaters.

Geographic entities mentioned:
surface_form: stellenbosch mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.9698
lon: 18.9008
Venomous snakes include the Cape cobra, puff adder, berg adder, boomslang, rinkhals, and black spitting cobra. Coetsenburg Estate. Most of the northern and eastern aspects of the Stellenbosch Mountain lie on the Coetsenburg Estate which is not open to the public. The estate, which was founded by Dirk Coetsee in 1682, is owned by the influential Anglo-Huguenot Coetsee family. Painting.

Geographic entities mentioned:
surface_form: stellenbosch mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.9698
lon: 18.9008
The estate, which was founded by Dirk Coetsee in 1682, is owned by the influential Anglo-Huguenot Coetsee family. Painting. A famous painting of Stellenbosch Mountain, titled &quot;Stellenbosberg&quot; (sic) by Jacobus Hendrik Pierneef (1886-1957) sold at auction by Strauss & Co. auctioneers for 612,700ZAR

Geographic entities mentioned:
surface_form: stellenbosch mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.9698
lon: 18.9008
Geology. The peak of Stellenbosch Mountain is 1,156m. The source of the Blaauwklippen (Blouklip) River is near the peak. The range is primarily composed of Table Mountain Sandstone. The climate is typically Mediterranean; warm and temperate, classified as Csb by the Köppen-Geiger system.

Geographic entities mentioned:
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Greenland, West Virginia. Greenland is an unincorporated community between Walker's Ridge and New Creek Mountain on the North Fork Patterson Creek in Grant County, West Virginia, United States. Greenland lies at the western end of Greenland Gap in New Creek Mountain. The community most likely was named for their green land at and around the original town site.

Geographic entities mentioned:
surface_form: New Creek Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.228
lon: -79.1288
Enteromius pleurogramma. &quot;Enteromius pleurogramma&quot; is a species of ray-finned fish in the genus &quot;Enteromius&quot;. It is endemic to Ethiopia, from the basin of the Blue Nile including Lake Tana. Some authors include it in the straightfin barb (&quot;E. paludinosus&quot;). But while they are certainly extremely closely related, they appear to be distinct cryptic species.

Geographic entities mentioned:
surface_form: Lake Tana
instance_of: Lake
countries: Ethiopia
coordinates: lat: 12
lon: 37.25
Hucuktlis Lake. Henderson Lake, also known as Hucuktlis Lake (pronounced &quot;who chook-tlis&quot;), is a lake on Vancouver Island that drains south into head of Uchucklesaht Inlet on the north side of lower Alberni Inlet. Etymology. Hucuktlis means &quot;place way inside&quot;, which refers to the inland nature of the lake relative to Uchucklesit Inlet.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: henderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.0936
lon: -125.038
surface_form: hucuktlis lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.0936
lon: -125.038
The name change was supported by the Alberni-Clayoquot Regional District. Geography. The lake is located about 25 kilometres east-southeast of Port Alberni along the West Coast of Vancouver Island. Clemens Creek flows into the northern tip of the lake. The Hucuktlis River drains the lake into the northern end of Uchucklesit Inlet, an arm of Alberni Inlet. Climate.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Hucuktlis Lake. Henderson Lake, also known as Hucuktlis Lake (pronounced &quot;who chook-tlis&quot;), is a lake on Vancouver Island that drains south into head of Uchucklesaht Inlet on the north side of lower Alberni Inlet. Etymology. Hucuktlis means &quot;place way inside&quot;, which refers to the inland nature of the lake relative to Uchucklesit Inlet.

Geographic entities mentioned:
surface_form: hucuktlis lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.0936
lon: -125.038
History. In 1917, Henderson Lake was adopted as the official name of the lake, correcting a map error featured in a 1912 map of the region. In 2018, the official name of the lake was changed to Hucuktlis Lake upon the recommendation of the Uchucklesaht First Nation. The name change was supported by the Alberni-Clayoquot Regional District. Geography.

Geographic entities mentioned:
surface_form: hucuktlis lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.0936
lon: -125.038
Clemens Creek flows into the northern tip of the lake. The Hucuktlis River drains the lake into the northern end of Uchucklesit Inlet, an arm of Alberni Inlet. Climate. Weather data from the Hucuktlis Lake fish hatchery shows that the lake is situated in the wettest place in North America. Hucuktlis Lake averages of precipitation, and in 1997 fell, setting the all-time Canadian record.

Geographic entities mentioned:
surface_form: hucuktlis lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.0936
lon: -125.038
surface_form: hucuktlis lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.0936
lon: -125.038
Pizzo Campo Tencia. Pizzo Campo Tencia (or &quot;Campo Tencia&quot;) is a mountain in the Lepontine Alps, which lies in the canton of Ticino, Switzerland. Pizzo Campo Tencia is the highest peak located entirely inside the canton. The mountain lies south of Lago di Morghirolo, between the Valle Leventina and Valle Maggia.

Geographic entities mentioned:
surface_form: Lago di Morghirolo
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.4491
lon: 8.719
surface_form: Valle Maggia
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.25
lon: 8.7
surface_form: lago di morghirolo
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.4491
lon: 8.719
surface_form: valle maggia
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.25
lon: 8.7