Sarmila/GeoWiki-Features huggingface dataset:
Mount Ickes. Mount Ickes is a mountain summit located west of the crest of the Sierra Nevada mountain range, in Fresno County of northern California, United States. It is situated in eastern Kings Canyon National Park, northwest of the community of Independence, 1.5 mile west of Pinchot Pass, and west of Mount Wynne, which is the nearest higher neighbor.

Geographic entities mentioned:
surface_form: Mount Wynne
instance_of: Mountain
countries: United States
coordinates: lat: 36.93799
lon: -118.40288
It is situated in eastern Kings Canyon National Park, northwest of the community of Independence, 1.5 mile west of Pinchot Pass, and west of Mount Wynne, which is the nearest higher neighbor. Other nearby peaks include Crater Mountain to the southeast, Striped Mountain to the northeast, Arrow Peak, to the west, and Mount Ruskin to the northwest.

Geographic entities mentioned:
surface_form: Striped Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.96557
lon: -118.4038
surface_form: Mount Ruskin
instance_of: Mountain
countries: United States
coordinates: lat: 36.9784671
lon: -118.4733528
surface_form: crater mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.92206
lon: -118.42091
surface_form: arrow peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.92827
lon: -118.49149
surface_form: arrow peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.6928
lon: -107.61
surface_form: crater mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.7393
lon: -120.919
Mount Ickes. Mount Ickes is a mountain summit located west of the crest of the Sierra Nevada mountain range, in Fresno County of northern California, United States. It is situated in eastern Kings Canyon National Park, northwest of the community of Independence, 1.5 mile west of Pinchot Pass, and west of Mount Wynne, which is the nearest higher neighbor.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount ickes
instance_of: Mountain
countries: United States
coordinates: lat: 36.93271
lon: -118.43927
Mount Ickes. Mount Ickes is a mountain summit located west of the crest of the Sierra Nevada mountain range, in Fresno County of northern California, United States. It is situated in eastern Kings Canyon National Park, northwest of the community of Independence, 1.5 mile west of Pinchot Pass, and west of Mount Wynne, which is the nearest higher neighbor.

Geographic entities mentioned:
surface_form: mount ickes
instance_of: Mountain
countries: United States
coordinates: lat: 36.93271
lon: -118.43927
Other nearby peaks include Crater Mountain to the southeast, Striped Mountain to the northeast, Arrow Peak, to the west, and Mount Ruskin to the northwest. Mount Ickes ranks as the 159th highest summit in California. Topographic relief is significant as the north aspect rises in 2.5 miles. The approach to this remote peak is made via the John Muir Trail which passes to the east of the mountain.

Geographic entities mentioned:
surface_form: mount ickes
instance_of: Mountain
countries: United States
coordinates: lat: 36.93271
lon: -118.43927
Roosevelt's New Deal as Secretary of the Interior from 1933 to 1946 and was instrumental in establishing Kings Canyon National Park. Climate. According to the Köppen climate classification system, Mount Ickes is located in an alpine climate zone. Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains.

Geographic entities mentioned:
surface_form: mount ickes
instance_of: Mountain
countries: United States
coordinates: lat: 36.93271
lon: -118.43927
Most of the range is included within the Humboldt-Toiyabe National Forest. The range reaches a maximum elevation of on the summit of Ruby Dome. To the north is Secret Pass and the East Humboldt Range, and from there the Rubies run south-southwest for about. To the east lies Ruby Valley, and to the west lie Huntington and Lamoille Valleys.

Geographic entities mentioned:
surface_form: Ruby Dome
instance_of: Mountain
countries: United States
coordinates: lat: 40.621872222222
lon: -115.47505555556
The range reaches a maximum elevation of on the summit of Ruby Dome. To the north is Secret Pass and the East Humboldt Range, and from there the Rubies run south-southwest for about. To the east lies Ruby Valley, and to the west lie Huntington and Lamoille Valleys. The Ruby Mountains are the only range of an introduced bird, the Himalayan snowcock, in North America.

Geographic entities mentioned:
surface_form: Ruby Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.4
lon: -115.3
Major features. Major valleys include Lamoille Canyon (and its branches Thomas and Right Fork Canyons), Seitz Canyon, Box Canyon and Kleckner Canyon. Canyons to the north drain into the main stem of the Humboldt River above Elko, while a group of canyons above the Te-Moak tribal lands constitute the headwaters of the South Fork of the Humboldt River.

Geographic entities mentioned:
surface_form: Lamoille Canyon
instance_of: Valley
countries: United States
coordinates: lat: 40.6916
lon: -115.474
Canyons to the north drain into the main stem of the Humboldt River above Elko, while a group of canyons above the Te-Moak tribal lands constitute the headwaters of the South Fork of the Humboldt River. Major summits in the central core of the range include Ruby Dome, Thomas Peak, Liberty Peak, Mount Fitzgerald, Verdi Peak, Snow Lake Peak, Mount Silliman, and Mount Gilbert.

Geographic entities mentioned:
surface_form: Ruby Dome
instance_of: Mountain
countries: United States
coordinates: lat: 40.621872222222
lon: -115.47505555556
surface_form: Thomas Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.624569444444
lon: -115.39311111111
surface_form: Liberty Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.586519444444
lon: -115.40007777778
surface_form: Snow Lake Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.605483333333
lon: -115.39671944444
Major summits in the central core of the range include Ruby Dome, Thomas Peak, Liberty Peak, Mount Fitzgerald, Verdi Peak, Snow Lake Peak, Mount Silliman, and Mount Gilbert. Prominent peaks further south include King, Lake, Wines, Tipton, and Pearl Peaks. North of the central core, significant peaks include Old-Man-of-the-Mountain and Soldier Peak.

Geographic entities mentioned:
surface_form: Tipton
instance_of: Mountain
countries: United States
coordinates: lat: 40.423055555556
lon: -115.47916666667
North of the central core, significant peaks include Old-Man-of-the-Mountain and Soldier Peak. Glaciers gouged out basins that are now alpine lakes. The larger of these, all located in the central core of the range, include Echo, Liberty, Favre, Lamoille, Castle, and Griswold lakes, while smaller tarns also in the central core include the scenic Island, Dollar, Verdi, Snow, Box, and Seitz lakes.

Geographic entities mentioned:
surface_form: Favre
instance_of: Lake
countries: United States
coordinates: lat: 40.573
lon: -115.397
surface_form: Dollar
instance_of: Group of lakes
countries: United States
coordinates: lat: 40.5917
lon: -115.385
Pollera. The clothing of the &quot;Bolivian chola&quot;, the pollera, is an amalgam of elements initially imposed on the indigenous people of the altiplano by the colonial system that limited the use of clothing identified as belonging to pre-Hispanic American cultures, and elements and materials redefined through time and subsequent cultural processes.

Geographic entities mentioned:
surface_form: altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Inchfad. Inchfad (, &quot;long island&quot;) is an island in the south east of Loch Lomond in Scotland. Inchfad is long and 35 hectares in area. Its highest point is 25 metres. The island forms part of the parish of Buchanan in west central Scotland, formerly part of Stirlingshire and now under Stirling Council. Inchfad is partially wooded and has a single permanent resident as of 2022.

Geographic entities mentioned:
surface_form: Loch Lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
It finally lives in the northwest of Thailand, and has been reported in particular in the Doi Ang Khang, Doi Pha Hom Pok, Doi Chiang Dao, Doi Khun Tan mountains, Lum Nam Pai wildlife sanctuary, and at Mae Hong Son. It was reported in Doi Inthanon in the early 1980s, but it could be a confusion with the chestnut-vented nuthatch (&quot;S.

Geographic entities mentioned:
surface_form: Doi Inthanon
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.592222222222
lon: 98.486666666667
After graduating, he obtained his master's degree at Cornell University and his Ph.D. degree at the University of Illinois at Urbana–Champaign. He started his studies by researching the Quechuan variety spoken in his homeland: the Mantaro Valley region. Engaged by the Peruvian Ministry of Education, he wrote the first grammar and dictionary of Wanka Quechua, both published in 1976.

Geographic entities mentioned:
surface_form: Mantaro Valley
instance_of: Valley
countries: Peru
coordinates: lat: -11.91666667
lon: -75.33333333
Włodzimierz Kotoński. Włodzimierz Kotoński (23 August 1925 – 4 September 2014) was a Polish composer. Biography. Born in Warsaw, Kotoński studied there with Piotr Rytel and Tadeusz Szeligowski at the PWSM, graduating in 1951. In an initial period of activity he took an interest in folk music from the Podhale region in southern Poland.

Geographic entities mentioned:
surface_form: Podhale
instance_of: Valley
countries: Poland
coordinates: lat: 49.4793
lon: 20.0291
Their first child died in 1648. Their second child, also named Médard, was born in 1651, the same year Helène died. After the Iroquois destroyed the Huron missions and forced the people to move further west in the late 1640s, Groseilliers worked to re-establish trade, especially in the Lake Superior region.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Leaving in August 1659, Groseilliers and Radisson traveled west to the far end of Lake Superior and wintered at Lac Courte Oreilles in what is now known as Wisconsin. According to Radisson's account of the voyage, they helped repel an Iroquois attack along the Ottawa River and that the idea for trading furs from Hudson Bay came to them at this time.

Geographic entities mentioned:
surface_form: Lac Courte Oreilles
instance_of: Lake
countries: United States
coordinates: lat: 45.883333333333
lon: -91.416666666667
Cuyahoga Valley is the only national park in the state of Ohio and one of three in the Great Lakes Basin, with Isle Royale National Park in Lake Superior and Indiana Dunes National Park bordering Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Wars, coercive treaties, and legislative changes in the eighteenth and nineteenth centuries resulted in Lenapé movement both west and south from their geographic origins in present-day New York City, the lower Hudson Valley, eastern Pennsylvania, New Jersey, and northern Delaware, through the Ohio River Valley and Cuyahoga Valley, to current residencies primarily in Oklahoma and Ontario, Canada.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Before the canal was built, Ohio was a sparsely settled wilderness where travel was difficult and getting crops to market was nearly impossible. The canal, built between 1825 and 1832, provided a new transportation route from Cleveland on Lake Erie, to Portsmouth on the Ohio River. The canal connected Ohio to the rest of the eastern United States.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
1985 Bangladesh cyclone. Tropical Storm One was a mainly weak but extremely deadly and catastrophic tropical cyclone which developed in the central Bay of Bengal on May 22, strengthened to a peak of 70 mph winds before hitting Bangladesh on the 25th. The storm brought torrential rains and flooding, killing around 11,069 people and leaving hundreds of thousands homeless. Meteorological history.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The storm brought torrential rains and flooding, killing around 11,069 people and leaving hundreds of thousands homeless. Meteorological history. On May 22, a depression formed in the Bay of Bengal, it rapidly intensified to a tropical storm on May 24, it made landfall and dissipated on May 25. Impact and aftermath.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Impact and aftermath. As tropical storm one made landfall in Bangladesh, it brought winds of 70 mph and a storm surge up to 3 meters high and heavy torrential rains and flooding, killing around 11,069 people. Every single person on the island of Urir Char, approximately 500 at the time, is thought to have been swept into the Bay of Bengal.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
On July 24, troops of the White Guards and Mongolian feudal lords again penetrated Soviet territory in the region north of Lake Gusinoye, but on August 3, upon learning of the approach of superior Red Army forces, they began to retreat. Ungern wanted to continue the war with the Reds, but most of his White Guards troops wanted to go to Manchuria.

Geographic entities mentioned:
surface_form: Lake Gusinoye
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 51.201666666667
lon: 106.39222222222
Ari Sirka. Ari Sirka (Aymara &quot;ari&quot; pointed, sharp, &quot;sirka&quot; vein of the body or a mine, &quot;pointed vein&quot;, also spelled Arisirka) is a mountain in the western extensions of the Cordillera Real in the Andes of Bolivia which reaches a height of approximately. It is located in the La Paz Department, Los Andes Province, Batallas Municipality. It lies at the Lawrawani Lake.

Geographic entities mentioned:
surface_form: ari sirka
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.14638889
lon: -68.41277778
The conflict broadened and became known as the Creek War. In response, the United States built a string of forts along the Ocmulgee and Chattahoochee Rivers, including Fort Daniel on top of Hog Mountain near present-day Dacula, Georgia, and Fort Gilmer. Fort Gilmer was situated next to an important Indian site called Standing Peachtree, a Creek Indian village.

Geographic entities mentioned:
surface_form: Chattahoochee
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
From railroad terminus to Atlanta: 1836–1860. In 1836, the Georgia General Assembly voted to build the Western and Atlantic Railroad to provide a link between the port of Savannah and the Midwest. The initial route of that state-sponsored project was to run from Chattanooga, Tennessee, to a spot east of the Chattahoochee River, in present-day Fulton County.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
In 1851, a third rail line, the Western and Atlantic Railroad - for which the site of Atlanta had been identified as a terminus - finally arrived, connecting Atlanta to Chattanooga in the northwest and opening up Georgia to trade with the Tennessee and Ohio River Valleys, and the American Midwest. The union depot was completed in 1853 on State Square. That year, the depot's architect, Edward A.

Geographic entities mentioned:
surface_form: Tennessee
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
In 841, during the reign of Emperor Ninmyō, a prohibition was placed on hunting and logging on the sacred mountain. In 1873, the Dajō-kan issued a proclamation on the establishment of public parks, and in 1880 Nara Park opened. This was extended in 1888 to include the areas of Mount Kasuga and Mount Wakakusa; that same year, some two thousand trees on Mount Kasuga were felled by a typhoon.

Geographic entities mentioned:
surface_form: Mount Wakakusa
instance_of: Mountain
countries: Japan
coordinates: lat: 34.691111111111
lon: 135.85444444444
It is located 17.9 kilometers away from Novaci, Gorj County, after passing on the Transalpina (DN67C) road through the Parâng Mountains. There are views of the Parângu Mare peak and, when the weather is clear, one can see Peleaga peak of the Retezat Mountains. During the winter, there are more than five ski slopes open ranging from low to increased difficulty.

Geographic entities mentioned:
surface_form: Parângu Mare
instance_of: Mountain
countries: Romania
coordinates: lat: 45.34027777777778
lon: 23.54083333333333
surface_form: Peleaga
instance_of: Mountain
countries: Romania
coordinates: lat: 45.366111111111
lon: 22.894444444444
Gobi Lakes Valley desert steppe. The Gobi Lakes Valley desert steppe ecoregion (WWF ID: PA1315) covers the narrow, flat valley in southwestern Mongolia that lies between the Khangai Mountains (to the north), and the Gobi-Altai Mountains (to the south). The region is known as the &quot;Valley of the Lakes&quot; because runoff from the mountains collect in lakes that have no outlet to the sea.

Geographic entities mentioned:
surface_form: Valley of the Lakes
instance_of: Valley
countries: Mongolia
coordinates: lat: 45.3167
lon: 99.9667
On the south the region is bounded by the Gobi-Altai range, the easternmost extension of the Altai. A chain of shallow, saline lakes include Böön Tsagaan Lake (Lake Buuntsaagan), Taatsiin Tsagaan Lake, Adgiin Tsagaan Nuur, and Lake Orog. The lake's depths fluctuate with the variable precipitation. Some have large wetlands where the waters recede. Climate.

Geographic entities mentioned:
surface_form: Böön Tsagaan Lake
instance_of: Lake
countries: Mongolia
coordinates: lat: 45.5961
lon: 99.142
surface_form: Taatsiin Tsagaan Lake
instance_of: Lake
countries: Mongolia
coordinates: lat: 45.156
lon: 101.4689
Piló dels Senyalets. Piló dels Senyalets is a mountain in Catalonia, Spain. It has an elevation of above sea level.

Geographic entities mentioned:
surface_form: piló dels senyalets
instance_of: Mountain
countries: Spain
coordinates: lat: 41.281666666667
lon: 0.82638888888889
In favourable localities and/or favourable seasons, a partial second brood has been recorded from mid- or late August to September. In the UK, the flight period is from the end of May to the beginning of July (in the south-west) and early June to early August (in the south-east). Fennoscandian subspecies &quot;M. a. norvegica&quot; flies in June–July, precise timing being affected by the season.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
It is part of the Marie Byrd Land Volcanic Province and is its oldest volcano. Geography and geology. Mount Petras lies in the coastal region of Marie Byrd Land, Antarctica, and is located within the McCuddin Mountains together with Mount Flint which lies northwest of Mount Petras. The complex Mount Petras-Mount Flint-Reynolds Ridge is also known as Petras Range.

Geographic entities mentioned:
surface_form: Mount Flint
instance_of: Mountain
coordinates: lat: -75.8666667
lon: -128.65
surface_form: petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
surface_form: petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
surface_form: mount petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
surface_form: mount petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
surface_form: flint
instance_of: Mountain
coordinates: lat: -75.8666667
lon: -128.65
It is an angular mountain consisting of rocky spurs in an area of, which form two ridges form a semicircular ice-filled bowl. Two other summits are high Putzke Peak northeast of Mount Petras, high Schwob Peak south and high Peter Nunatak southeast. Other outcrops occur farther southwest at Navarrette Peak, southeast at Wallace Rock and northeast at Erven Nunataks.

Geographic entities mentioned:
surface_form: Putzke Peak
instance_of: Mountain
coordinates: lat: -75.8167
lon: -128.533
surface_form: Schwob Peak
instance_of: Mountain
coordinates: lat: -75.88333
lon: -128.65
surface_form: Peter Nunatak
instance_of: Mountain
coordinates: lat: -75.9167
lon: -128.55
surface_form: petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
surface_form: mount petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
surface_form: peter
instance_of: Mountain
coordinates: lat: -70.1833
lon: 64.9333
Two other summits are high Putzke Peak northeast of Mount Petras, high Schwob Peak south and high Peter Nunatak southeast. Other outcrops occur farther southwest at Navarrette Peak, southeast at Wallace Rock and northeast at Erven Nunataks. The existence of an explosion crater on its northern side was inferred by González-Ferran in 1972.

Geographic entities mentioned:
surface_form: Navarrette Peak
instance_of: Mountain
coordinates: lat: -75.9167
lon: -128.75
surface_form: Wallace Rock
instance_of: Mountain
coordinates: lat: -75.9167
lon: -128.45
surface_form: Erven Nunataks
instance_of: Mountain
coordinates: lat: -75.75
lon: -128.167
Mount Petras is part of the volcanic province of Marie Byrd Land, which may be a product of a mantle plume. Other volcanoes in this province of West Antarctic volcanoes are the Ames Range, Crary Mountains, Executive Committee Range, Flood Range, Hobbs Coast nunataks, Kohler Range, Mount Murphy, Mount Siple, Mount Takahe and Mount Waesche. Some of these volcanoes are still active today.

Geographic entities mentioned:
surface_form: Mount Murphy
instance_of: Mountain
coordinates: lat: -75.3
lon: -110.7
surface_form: Mount Siple
instance_of: Mountain
coordinates: lat: -73.433333333333
lon: -126.66666666667
surface_form: Mount Takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: Mount Waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: siple
instance_of: Mountain
coordinates: lat: -73.433333333333
lon: -126.66666666667
Beginning with the Oligocene, an ice sheet began to develop in Antarctica and acquired present-day dimensions during the Miocene or Pliocene. Mount Petras was discovered during the 1939-1941 United States Antarctic Service Expedition and named after the pilot of the expedition. It was visited in 1959, 1967–1968, 1977-1978 and 1993-1994 by field expeditions.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
The complex Mount Petras-Mount Flint-Reynolds Ridge is also known as Petras Range. It lies inland from the Amundsen Sea coast. It is an angular mountain consisting of rocky spurs in an area of, which form two ridges form a semicircular ice-filled bowl. Two other summits are high Putzke Peak northeast of Mount Petras, high Schwob Peak south and high Peter Nunatak southeast.

Geographic entities mentioned:
surface_form: amundsen
instance_of: Mountain
coordinates: lat: -67.233333333333
lon: 100.75
Mount Petras is part of the volcanic province of Marie Byrd Land, which may be a product of a mantle plume. Other volcanoes in this province of West Antarctic volcanoes are the Ames Range, Crary Mountains, Executive Committee Range, Flood Range, Hobbs Coast nunataks, Kohler Range, Mount Murphy, Mount Siple, Mount Takahe and Mount Waesche. Some of these volcanoes are still active today.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Geography and geology. Mount Petras lies in the coastal region of Marie Byrd Land, Antarctica, and is located within the McCuddin Mountains together with Mount Flint which lies northwest of Mount Petras. The complex Mount Petras-Mount Flint-Reynolds Ridge is also known as Petras Range. It lies inland from the Amundsen Sea coast.

Geographic entities mentioned:
surface_form: reynolds
instance_of: Mountain
coordinates: lat: -72.7
lon: -61.2667
surface_form: petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
surface_form: petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
surface_form: mount petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
surface_form: flint
instance_of: Mountain
coordinates: lat: -75.8666667
lon: -128.65
surface_form: mount flint
instance_of: Mountain
coordinates: lat: -75.8666667
lon: -128.65
Mount Petras. Mount Petras is a mountain in Antarctica. It consists of volcanic rocks, most of Cretaceous age but there is also an Eocene-Oligocene volcanic system that may have been emplaced inside of thin ice. It is part of the Marie Byrd Land Volcanic Province and is its oldest volcano. Geography and geology.

Geographic entities mentioned:
surface_form: petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
surface_form: mount petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
Both basement and volcanic rocks emerge from the West Antarctic Ice Sheet as a nunatak. The volcanic and basement rocks are separated by an unconformity at elevation. The highest summit of Mount Petras lies on the western ridge at elevation above sea level of which about are above the West Antarctic Ice Sheet.

Geographic entities mentioned:
surface_form: petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
surface_form: mount petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
The highest summit of Mount Petras lies on the western ridge at elevation above sea level of which about are above the West Antarctic Ice Sheet. Most of the volcanic rocks are hawaiite with some mugearite, while the basement is rhyodacitic and mostly consists of a Cretaceous volcanic complex that makes up the bulk of Mount Petras. The basement also includes schists, paragneisses and gneisses.

Geographic entities mentioned:
surface_form: petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
surface_form: mount petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
Moraine debris and talus cover exposed rocks. Mount Petras is part of the volcanic province of Marie Byrd Land, which may be a product of a mantle plume. Other volcanoes in this province of West Antarctic volcanoes are the Ames Range, Crary Mountains, Executive Committee Range, Flood Range, Hobbs Coast nunataks, Kohler Range, Mount Murphy, Mount Siple, Mount Takahe and Mount Waesche.

Geographic entities mentioned:
surface_form: petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
surface_form: mount petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
Some of these volcanoes are still active today. Marie Byrd Land itself is a crustal dome, with its &quot;summit&quot; in the area of Mount Petras; the dome was probably formed by the impingement of the mantle plume under the crust and volcanism may have spread outwards away from Mount Petras. Geologic history.

Geographic entities mentioned:
surface_form: petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
surface_form: petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
surface_form: mount petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
surface_form: mount petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
Name and research history. The volcanic history of Mount Petras is important for reconstructing the volcanic and glacial history of Marie Byrd Land. During the late Cretaceous and Eocene-late Cenozoic, continental rifting occurred in the Ross Sea and West Antarctic Ice Sheet area.

Geographic entities mentioned:
surface_form: petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
surface_form: mount petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
It was visited in 1959, 1967–1968, 1977-1978 and 1993-1994 by field expeditions. During the 20th century, Mount Petras was viewed as a volcano that had formed deep under ice on a Cenozoic marine erosion surface covering West Antarctica, which had then been deformed by tectonic uplift.

Geographic entities mentioned:
surface_form: petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
surface_form: mount petras
instance_of: Mountain
coordinates: lat: -75.86667
lon: -128.65
Formation. It is estimated that the whirlpool formed approximately 4,200 years ago by the upstream erosion of the Niagara Escarpment by the Niagara River. Niagara Falls is located along the boundary of the Niagara Escarpment and has been retreating upstream since its formation.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
Redstone Lake (Sudbury District). Redstone Lake is a lake located in geographic Semple Township in the Unorganized North Part of Sudbury District in Northeastern Ontario, Canada. It is in the James Bay drainage basin and is part of the Redstone River system. Hydrology. The primary inflow, at the southwest, and outflow, at the northeast, is the Redstone River.

Geographic entities mentioned:
surface_form: redstone river
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.4553
lon: -81.04
It is in the James Bay drainage basin and is part of the Redstone River system. Hydrology. The primary inflow, at the southwest, and outflow, at the northeast, is the Redstone River. The Redstone River flows via the Frederick House River, the Abitibi River and the Moose River to James Bay.

Geographic entities mentioned:
surface_form: redstone river
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.4553
lon: -81.04
It is in the James Bay drainage basin and is part of the Redstone River system. Hydrology. The primary inflow, at the southwest, and outflow, at the northeast, is the Redstone River. The Redstone River flows via the Frederick House River, the Abitibi River and the Moose River to James Bay.

Geographic entities mentioned:
surface_form: redstone river
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.4553
lon: -81.04
surface_form: moose
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.91444444444444
lon: -118.80638888888889
surface_form: abitibi
instance_of: Lake
countries: Canada
coordinates: lat: 48.666666666666664
lon: -79.75
Redstone Lake (Sudbury District). Redstone Lake is a lake located in geographic Semple Township in the Unorganized North Part of Sudbury District in Northeastern Ontario, Canada. It is in the James Bay drainage basin and is part of the Redstone River system. Hydrology. The primary inflow, at the southwest, and outflow, at the northeast, is the Redstone River.

Geographic entities mentioned:
surface_form: redstone lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.9744
lon: -81.2372
surface_form: redstone lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.1831
lon: -78.5378
Verkė. The Verkė is a small (around 2 km. long) rivulet in Vilnius, Lithuania, which gave the name to the Verkiai neighborhood. According to the legend, the Verkė was the birthplace of the semi-legendary pagan priest Lizdeika, a forefather of the Radziwiłł family, a Polish princely family.

Geographic entities mentioned:
surface_form: verkė
instance_of: Watercourse
countries: Lithuania
coordinates: lat: 54.74538
lon: 25.29143
Location. Myslivny lies at a height of 950–970 metres above the sea level on the highlands of the upper Ore Mountains. The locality, which is 2 kilometres northwest of the Božídarský Špičák mountain on the Černá creek between Boží Dar and Horní Blatná is surrounded by high forest and was formerly a popular summer retreat and winter sports resort. History.

Geographic entities mentioned:
surface_form: Božídarský Špičák
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.400833333333
lon: 12.888888888889
Diamond Hill (Cumberland, Rhode Island). Diamond Hill is a large hill on Diamond Hill Road in Cumberland, Rhode Island, which contains a town park and former ski area. The summit is 481 feet above sea level. On a clear day, the Boston skyline and Mount Wachusett are visible. Diamond Hill is a massive outcropping of white quartz with a vertical drop of 350 feet.

Geographic entities mentioned:
surface_form: Mount Wachusett
instance_of: Mountain
countries: United States
coordinates: lat: 42.488888888889
lon: -71.8875
Lake Tahoma. Lake Tahoma is a private lake in the mountains of Western North Carolina, United States, in McDowell County. It is fed by the waters of Buck Creek, a tributary of the Catawba River. The lake is about northwest of Marion.

Geographic entities mentioned:
surface_form: tahoma
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: lake tahoma
instance_of: Lake
countries: United States
coordinates: lat: 35.7233
lon: -82.08
In exchange, Ted Turner agreed to donate $500,000 to Civil War battlefield preservation. The movie was filmed in Virginia's Shenandoah Valley, western Maryland, and in the Eastern Panhandle of West Virginia. Actual historic locations in the film include Virginia Military Institute and Washington & Lee University, known as Washington College during the Civil War.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Weingartensee. __NOTOC__
The Weingartensee is a small lake located east of Täsch at the foot of the Alphubel, in the Swiss canton of Valais. The lake has a surface area of 0.64 ha and is located at 3,058 metres above sea level. It lies near the bottom of the Weingartengletscher glacier. Following the flood of June 2001, a dam was built and the water level was slightly reduced.

Geographic entities mentioned:
surface_form: Alphubel
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.062938888889
lon: 7.8639111111111
surface_form: weingartensee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.06333333333333
lon: 7.838888888888889
Weingartensee. __NOTOC__
The Weingartensee is a small lake located east of Täsch at the foot of the Alphubel, in the Swiss canton of Valais. The lake has a surface area of 0.64 ha and is located at 3,058 metres above sea level. It lies near the bottom of the Weingartengletscher glacier. Following the flood of June 2001, a dam was built and the water level was slightly reduced.

Geographic entities mentioned:
surface_form: weingartensee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.06333333333333
lon: 7.838888888888889
Chandos Lake is in the Atlantic watershed; fed by springs, it drains from its north end into Flat Creek, which flows into Paudash Lake, thence to the Crowe River, the Trent River, and Lake Ontario. Chandos is the largest lake in the Crowe River watershed. Chandos Lake measures 1,387 hectares and has a maximum depth of 48 metres.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: chandos lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.825
lon: -77.975
Chandos Lake measures 1,387 hectares and has a maximum depth of 48 metres. Chandos Lake was originally called Mongosogan by the Mississauga Anishinabe, on whose traditional territory it lies. Although not one of the Kawartha Lakes proper, Chandos Lake is part of the Kawartha cottage country; the lake is lined with some 1,200 cottages. The lake features three marinas and a public beach.

Geographic entities mentioned:
surface_form: kawartha
instance_of: Group of lakes
countries: Canada
coordinates: lat: 44.4994
lon: -78.441
surface_form: kawartha
instance_of: Group of lakes
countries: Canada
coordinates: lat: 44.4994
lon: -78.441
surface_form: chandos lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.825
lon: -77.975
Chandos Lake. Chandos Lake is a lake in North Kawartha, Ontario, Canada. The lake is in the shape of a reversed L, with three main bays: West Bay, connected to the main body of the lake by a long Narrows; South Bay, extending southwest and separated by a curved peninsula; and Gilmour Bay, a smaller, two-lobed bay on the southern tip of the lake, connected by Gilmour Bay Narrows.

Geographic entities mentioned:
surface_form: kawartha
instance_of: Group of lakes
countries: Canada
coordinates: lat: 44.4994
lon: -78.441
surface_form: chandos lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.825
lon: -77.975
Chandos Lake. Chandos Lake is a lake in North Kawartha, Ontario, Canada. The lake is in the shape of a reversed L, with three main bays: West Bay, connected to the main body of the lake by a long Narrows; South Bay, extending southwest and separated by a curved peninsula; and Gilmour Bay, a smaller, two-lobed bay on the southern tip of the lake, connected by Gilmour Bay Narrows.

Geographic entities mentioned:
surface_form: chandos lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.825
lon: -77.975
Chandos is the largest lake in the Crowe River watershed. Chandos Lake measures 1,387 hectares and has a maximum depth of 48 metres. Chandos Lake was originally called Mongosogan by the Mississauga Anishinabe, on whose traditional territory it lies. Although not one of the Kawartha Lakes proper, Chandos Lake is part of the Kawartha cottage country; the lake is lined with some 1,200 cottages.

Geographic entities mentioned:
surface_form: chandos lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.825
lon: -77.975
SR 397 was added to the state highway system in 1991, as a short route connecting Finley to Pasco. Two years later, the highway was extended further south into Finley. The remaining highway between I-82 and Finley in the Horse Heaven Hills was constructed by the state government and Benton County from 2004 to 2008 and was signed as part of SR 397 in 2009. Route description.

Geographic entities mentioned:
surface_form: Horse Heaven Hills
instance_of: Landform
countries: United States
coordinates: lat: 46.13
lon: -119.87
Two years later, the highway was extended further south into Finley. The remaining highway between I-82 and Finley in the Horse Heaven Hills was constructed by the state government and Benton County from 2004 to 2008 and was signed as part of SR 397 in 2009. Route description. SR 397 begins at an interchange with I-82 and U.S. Route 395 (US 395) in the Horse Heaven Hills southwest of Kennewick.

Geographic entities mentioned:
surface_form: Horse Heaven Hills
instance_of: Landform
countries: United States
coordinates: lat: 46.13
lon: -119.87
Namarunu. Namarunu is a shield volcano located in the Great Rift Valley, Kenya. Location. Namarunu is located in the Suguta Valley, a section of the Kenyan Rift Valley just south of Lake Turkana. It extends from the western side of the rift past the center. The mountain forms a broad shield. The large basal part is about deep, made up of outward-dipping trachytic lavas, breccias and tuffs.

Geographic entities mentioned:
surface_form: Suguta Valley
instance_of: Valley
countries: Kenya
coordinates: lat: 2.0910583333333
lon: 36.513747222222
It extends from the western side of the rift past the center. The mountain forms a broad shield. The large basal part is about deep, made up of outward-dipping trachytic lavas, breccias and tuffs. A few thousand years ago the Suguta valley was filled by a major lake, but now it is extremely dry and hot, with only the small Lake Logipi at the northern end.

Geographic entities mentioned:
surface_form: Lake Logipi
instance_of: Lake
countries: Kenya
coordinates: lat: 2.2333333333333
lon: 36.566666666667
In the 2001 census the parish had a population of 1,058, decreasing at the 2011 census to 928. Within the boundaries of the historic county of Lancashire, it is in the southern part of the Lake District National Park, between Coniston Water, the third longest lake in the Lake District, and Coniston Old Man. Coniston is northeast of Barrow-in-Furness, west of Kendal and north of Lancaster. Toponym.

Geographic entities mentioned:
surface_form: Coniston Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.35
lon: -3.0666666666667
Since 7 March 2007 a hydro-electric scheme has been in use to power up to 300 homes; being sited near the original. Geography. Coniston is located on the western shore of the northern end of Coniston Water. It sits at the mouth of Coppermines Valley and Yewdale Beck, which descend from the Coniston Fells, historically the location of ore and slate mining.

Geographic entities mentioned:
surface_form: Coniston Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.35
lon: -3.0666666666667
Coniston is a popular spot for hill-walking and rock-climbing; there are fine walks to be had on the nearby Furness Fells and Grizedale Forest, and some of the finest rock in the Lake District on the eastern face of Dow Crag, from the village. The Grizedale Stages rally also takes place in Coniston, using the surrounding Grizedale and Broughton Moor (or Postlethwaite Allotment) forests.

Geographic entities mentioned:
surface_form: Dow Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.369438888889
lon: -3.1374388888889
Hazar, Turkmenistan. Hazar (until 1999 known as Çeleken, also written Cheleken;; Persian: Chaharken) is a seaport town located on the Cheleken Peninsula of the Caspian Sea. It is directly subordinate to the city of Balkanabat in Balkan Province of western Turkmenistan.

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
Blueberry Mountain is a mountain located in western Maine. Named because of the abundant blueberries on its summit and upper slopes, it is a popular day hike. The summit area is partially open and has good views over Evans Notch and toward North and South Baldface in New Hampshire. It is ascended by the White Cairn, Stone House, and Blueberry Ridge trails.

Geographic entities mentioned:
surface_form: North
instance_of: Mountain
countries: United States
coordinates: lat: 44.2428
lon: -71.0869
surface_form: South Baldface
instance_of: Landform
Mountain
countries: United States
coordinates: lat: 44.2306
lon: -71.0781
Named because of the abundant blueberries on its summit and upper slopes, it is a popular day hike. The summit area is partially open and has good views over Evans Notch and toward North and South Baldface in New Hampshire. It is ascended by the White Cairn, Stone House, and Blueberry Ridge trails. It is considered a spur of Speckled Mountain.

Geographic entities mentioned:
surface_form: Speckled Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2911
lon: -70.9544
Blueberry Mountain (Oxford County, Maine). Blueberry Mountain is a mountain located in western Maine. Named because of the abundant blueberries on its summit and upper slopes, it is a popular day hike. The summit area is partially open and has good views over Evans Notch and toward North and South Baldface in New Hampshire.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: blueberry mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2658
lon: -70.9786
Blueberry Mountain (Oxford County, Maine). Blueberry Mountain is a mountain located in western Maine. Named because of the abundant blueberries on its summit and upper slopes, it is a popular day hike. The summit area is partially open and has good views over Evans Notch and toward North and South Baldface in New Hampshire.

Geographic entities mentioned:
surface_form: blueberry mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2658
lon: -70.9786
Old Jewish Cemetery, Sarajevo. The OId Jewish Cemetery is a cemetery in Sarajevo, Bosnia and Herzegovina. It is located on the slopes of Trebević mountain, in the Kovačići-Debelo Brdo area, in the south-western part of the city. It is the largest Jewish cemetery in Southeast Europe, and second largest sepulchral complex in Europe after the Old Jewish Cemetery in Prague.

Geographic entities mentioned:
surface_form: Trebević
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.823333333333
lon: 18.448888888889
Los Placeres. Los Placeres is an archeological site located between the “Waspán” and “Tabacalera Nicaragüense” neighborhoods at kilometer 4 of the “Carretera Norte”, in Managua, en Nicaragua. The site extends to the coast of Lake Managua.

Geographic entities mentioned:
surface_form: Lake Managua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 12.333333333333
lon: -86.416666666667
The northern border of the township follows the ridgecrest of Nescopeck Mountain. Other mountains in the township are McCauley Mountain in the center, the western end of Buck Mountain on the east side, and the slopes of Catawissa Mountain along the southwestern border. According to the United States Census Bureau, the township has a total area of, of which is land and, or 1.11%, is water.

Geographic entities mentioned:
surface_form: Catawissa Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
Other facts can sometimes be inferred from an observed population bottleneck. Among the Galápagos Islands giant tortoises—themselves a prime example of a bottleneck—the comparatively large population on the slopes of the Alcedo volcano is significantly less diverse than four other tortoise populations on the same island. DNA analyses date the bottleneck to around 88,000 years before present (YBP).

Geographic entities mentioned:
surface_form: Alcedo volcano
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.396583
lon: -91.109104
Along this portion of the route, tracks were laid for the Jerusalem Light Rail, which began operation in August 2011. The road passes Yad Vashem, the Mount Herzl National Cemetery and Sha'arei Tzedek Medical Center. Between Mileikowsky Square at Shmuel Beyth Street and Haft Square at HeHalutz Street, northbound traffic may continue through Beit HaKerem along Herzl Boulevard.

Geographic entities mentioned:
surface_form: Mount Herzl National Cemetery
instance_of: Mountain
countries: Israel
coordinates: lat: 31.774117
lon: 35.180567
Pinery Provincial Park. Pinery Provincial Park is a provincial park located on Lake Huron near Grand Bend, Ontario. It occupies an area of. It is a natural environment-class Provincial Park created to help preserve oak savannah and the beach dune ecology. It has 1,275 sites of which 404 have electrical hookups. These include the yurt camping area and the group camping sites.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Neffs, Pennsylvania. Neffs is a small village that is located mainly in North Whitehall Township and also partially in Washington Township in Lehigh County, Pennsylvania. It is part of the Lehigh Valley, which has a population of 861,899 and is the 68th-most populous metropolitan area in the U.S. as of the 2020 census.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5