Sarmila/GeoWiki-Features huggingface dataset:
The first visitors mostly came because their doctors had recommended a health cure, but these were soon joined by more recreational travellers. From about 1850 there was a rapid growth in mountaineering as a leisure activity. Pioneering mountain tourists, many of whom came from England, favoured Pontresina over St. Moritz as a starting point for their Engadin climbing holidays.

Geographic entities mentioned:
surface_form: Engadin
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
Instead, guest looking out from these rooms could observe the reformed-evangelical Church of San Niculò, the hamlet-district of Pontersina-Laret, and on the horizon above and beyond these, the Piz Julier (mountain). Following the 1895 rebuild, all the rooms incorporated electric lighting. The electricity came from a generator in the cellar. Boom and bubble (1901-1914).

Geographic entities mentioned:
surface_form: Piz Julier
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.490916666667
lon: 9.7599444444444
Technical progress also impacted transport links. On 1 July 1903 the Albula Railway opened between Thusis and Samedan, which connected the Engadin region with the cantonal capital, Chur. Hitherto hotel guests had been required to undergo a ten-hour journey, normally by post carriage, via the Julier or Albula Pass in order to reach Pontresina from Chur.

Geographic entities mentioned:
surface_form: Engadin
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
In response, there was a sudden increase in tourist facilities, including a number of substantial new hotels, in Pontresina. Another result and driver of the tourism boom was the Funicular service that opened in 1907 between Punt Muragl and the new Muottas Muragl viewing station, part completed even before the Pontresina rail link itself.

Geographic entities mentioned:
surface_form: Muottas Muragl
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.521888888889
lon: 9.9021944444444
From 1924 guest numbers finally began a slow recovery, benefitting most of the region's hotels, including the Hotel Pontresina. Brochures of the time indicate that management took the opportunity to resume renovations, notably of the public rooms on the ground floor.

Geographic entities mentioned:
surface_form: region's
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
Brochures of the time indicate that management took the opportunity to resume renovations, notably of the public rooms on the ground floor. There is evidence for a growth in popularity with holidaymakers during the 1920s of recreational swimming and bathing, and bathing facilities were made available at Lake Staz and in the surrounding woodlands (&quot;Stazerwald&quot;) between Pontresina and St.

Geographic entities mentioned:
surface_form: Lake Staz
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.496111111111
lon: 9.8686111111111
During the late 1940s the presence across the border in southern Germany of large numbers of US military personnel, with disposal incomes useful higher than those available to the European populations, provided the hotels in the Engadin with a welcome additional customer base, but numbers were insufficient to avert a continuation of the Sporthotel's operating losses.

Geographic entities mentioned:
surface_form: Engadin
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
Additionally, similarly to how Baal fought Yam, god of the sea, the Kiaše was also counted among Teshub's mythical adversaries, and both battles were associated with the same mountain, Ḫazzi. However, myths about Baal also contain elements which find no parallel in these focused on Teshub, such as the confrontation with Mot, the personification of death, and his temporary death resulting from it.

Geographic entities mentioned:
surface_form: Ḫazzi
instance_of: Mountain
countries: Syria
Turkey
coordinates: lat: 35.9525
lon: 35.969305555556
For some time, Ahmad Shuja then worked as a lecturer at the Osmania University in Hyderabad state (Deccan) but was not happy and returned to Lahore to seek employment there.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Buck Hill (Oneida County, New York). Buck Hill is a summit located in Central New York Region of New York located in the Town of Western in Oneida County, north of North Western.

Geographic entities mentioned:
surface_form: buck hill (oneida county, new york)
instance_of: Mountain
countries: United States
coordinates: lat: 43.364722222222
lon: -75.366944444444
Buck Hill (Oneida County, New York). Buck Hill is a summit located in Central New York Region of New York located in the Town of Western in Oneida County, north of North Western.

Geographic entities mentioned:
surface_form: buck hill
instance_of: Mountain
countries: United States
coordinates: lat: 43.364722222222
lon: -75.366944444444
Description. The original description of this species is based on a specimen measuring 84 mm in length. This species has 49 pairs of legs. Distribution. The species occurs in coastal north-eastern Queensland. The type locality is Kuranda, on the Atherton Tableland. Behaviour. The centipedes are solitary terrestrial predators that inhabit plant litter and soil.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Geology. One of the youngest islands, Isabela is located on the western edge of the archipelago near the Galápagos hotspot. At approximately 1 million years old, the seahorse-shaped island was formed by the merger of six shield volcanoes; Alcedo, Cerro Azul, Darwin, Ecuador, Sierra Negra, and Wolf.

Geographic entities mentioned:
surface_form: Alcedo
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.396583
lon: -91.109104
surface_form: Wolf
instance_of: Mountain
countries: Ecuador
coordinates: lat: 0.033333333333333
lon: -91.333333333333
All of these volcanoes except Ecuador are still active, making it one of the most volcanically active places on earth. Two of the volcanoes, Volcan Ecuador and Volcan Wolf (the island's highest point with an elevation of), lie directly on the equator.

Geographic entities mentioned:
surface_form: Volcan Wolf
instance_of: Mountain
countries: Ecuador
coordinates: lat: 0.033333333333333
lon: -91.333333333333
The relatively new lava fields and surrounding soils have not developed the sufficient nutrients required to support the varied life zones found on other islands. Another obvious difference occurs on Volcan Wolf and Cerro Azul; these volcanoes loft above the cloud cover and are arid on top. Isabela's rich bird, animal and marine life is beyond compare.

Geographic entities mentioned:
surface_form: Volcan Wolf
instance_of: Mountain
countries: Ecuador
coordinates: lat: 0.033333333333333
lon: -91.333333333333
Isabela is home to more wild tortoises than all the other islands. Isabela's large size and notable topography created barriers for the slow-moving tortoises; apparently the creatures were unable to cross lava flows and other obstacles, causing several different sub-species of tortoise to develop. Today, tortoises roam free in the calderas of Alcedo, Wolf, Cerro Azul, Darwin, and Sierra Negra.

Geographic entities mentioned:
surface_form: Alcedo
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.396583
lon: -91.109104
surface_form: Wolf
instance_of: Mountain
countries: Ecuador
coordinates: lat: 0.033333333333333
lon: -91.333333333333
surface_form: Darwin
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.18333333333333
lon: -91.283333333333
Taking Frank from his cell, they drove him to Marietta, the hometown of Mary Phagan, and hanged him from a tree. Leaders of the lynch mob would later gather at Stone Mountain to revive the Ku Klux Klan. In response to the lynching of Leo Frank, Sigmund Livingston founded the Anti-Defamation League (ADL) under the sponsorship of B'nai B'rith.

Geographic entities mentioned:
surface_form: Stone Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.805944444444
lon: -84.145422222222
Vwaza Marsh Game Reserve. Vwaza Marsh Wildlife Reserve is a national game reserve in Malawi. In contrast to the Nyika National Park on the Nyika Plateau, much of Vwaza is located on low-lying flat ground although the eastern side of the park is hilly. It is located to the southeast of the plateau and to the north of the floodplains of South Rukuru River and covers an area of 1,000 km2.

Geographic entities mentioned:
surface_form: Nyika Plateau
instance_of: Plateau
countries: Malawi
Zambia
coordinates: lat: -10.35
lon: 33.6
Typically the reserve has large herds of Cape buffaloes and elephants, and a large variety of antelope including roan, greater kudu, Lichtenstein's hartebeest, eland and impala. Warthogs are also found in this reserve as well as numerous hippopotamus pod in Lake Kazuni. Camera trap surveys have also shown that lions are present, but probably transient, as well as leopards and wild dogs.

Geographic entities mentioned:
surface_form: Lake Kazuni
instance_of: Lake
countries: Malawi
coordinates: lat: -11.1333
lon: 33.6667
Notable birdlife include Goliath herons, openbill storks and the rare white-winged starling. Lake Kazuni is located in the reserve and supports a notable hippo population. The Reserve has a wide variety of plants communities and there are 398 species of vascular plants from 71 families.

Geographic entities mentioned:
surface_form: Lake Kazuni
instance_of: Lake
countries: Malawi
coordinates: lat: -11.1333
lon: 33.6667
Bone Cave (Tasmania). Bone Cave, located in the Middle Weld Valley of Tasmania, is a small vertical limestone cave with a rich history of human occupation. History. The oldest dated materials found at the site, including charcoal and stone artifacts, date back to around 29,000 years ago.

Geographic entities mentioned:
surface_form: Weld Valley
instance_of: Valley
countries: Australia
coordinates: lat: -42.95
lon: 146.6
Arden railway station, Scotland. Arden railway station was a station on the Slamannan Railway. The line connected mines and villages in the Central Scotland. Opened by the Slamannan Railway, then joining the Edinburgh and Glasgow Railway, was absorbed into the North British Railway. It became part of the London and North Eastern Railway during the Grouping of 1923.

Geographic entities mentioned:
surface_form: Central Scotland
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408
lon: -4.044
Deneen. From April 15, 1886 through April 15, 1890, he served as postmaster of Leadville, Colorado. He was involved in getting the federal government to establish a national fish hatchery at the base of Mount Massive in Leadville, which was established in 1889 by executive order of President Benjamin Harrison. He then ran the fish hatchery. In 1891, he lost his daughter Olive, who died in Denver.

Geographic entities mentioned:
surface_form: Mount Massive
instance_of: Mountain
countries: United States
coordinates: lat: 39.1875
lon: -106.476
Lakeside is an unincorporated community in Chikaming Township of Berrien County in the U.S. state of Michigan. It is situated on the shore of Lake Michigan just west of Interstate 94. It is part of a group of communities known as &quot;Harbor Country&quot; which includes New Buffalo, Three Oaks, Harbert, Union Pier, Grand Beach and Sawyer. The ZIP code is 49116 and the FIPS place code is 45080.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
The highway was long, connecting Highway 28 south of Apsley with Highway 620 in Glen Alda. The only other community served by Highway 504 was Lasswade. Highway 504 was established, along with many other secondary highways, in 1956. Originally, the route looped around Chandos Lake back to Apsley. However, the northern portion of this loop would later become Highway 620.

Geographic entities mentioned:
surface_form: Chandos Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.825
lon: -77.975
From there, Highway 504 travelled east into the southern fringes of the Canadian Shield, with thick forests surrounding the majority of the route. However, in addition to the hamlet of Lasswade, located around the midpoint of the highway, the route also served cottagers along the southern and eastern shores of Chandos Lake and numerous residences line the length of road.

Geographic entities mentioned:
surface_form: Chandos Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.825
lon: -77.975
Camp Marbury. Camp Marbury was a summer camp for girls on Lake Champlain in Ferrisburgh, Vermont. Founded in 1921, the family-run camp operated until 1942, when it closed due to logistical difficulties associated with World War II. The camp property is listed on the National Register of Historic Places. History. The camp property was purchased in 1921 by Mary P.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
The facility designed by FaulknerBrowns Architects was opened in December 2003 at a cost of £24 million. Its main feature is a 200m indoor track, but it also hosts several other sporting arenas as well as a large gym and extensive sports medicine facilities. It is in the Lower Don Valley between the Sheffield Arena and Don Valley Bowl. It is managed by SIV (Sheffield International Venues). Sports.

Geographic entities mentioned:
surface_form: Lower Don Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.405
lon: -1.417
Range and habitat. The Nile tilapia is native to larger parts of Africa, except Maghreb and almost all of Southern Africa. It is native to tropical West Africa, the Lake Chad basin, and much of the Nile system, including lakes Tana, Albert and Edward–George, as well as lakes Kivu, Tanganyika, and Turkana, and the Awash and Omo Rivers. In Israel, it is native to coastal river basins.

Geographic entities mentioned:
surface_form: Tana
instance_of: Lake
countries: Ethiopia
coordinates: lat: 12
lon: 37.25
surface_form: Edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
surface_form: Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
surface_form: Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
n. filoa&quot; as data deficient. A population found in Lake Bogoria appears to be an undescribed subspecies. The forms referred to as &quot;Oreochromis&quot; (or &quot;Tilapia&quot;) &quot;nyabikere&quot; and &quot;kabagole&quot; seem to belong to this species, too. An undescribed population found at, for example, Wami River, Lake Manyara, and Tingaylanda seems to be a close relative. Feeding.

Geographic entities mentioned:
surface_form: Lake Bogoria
instance_of: Lake
countries: Kenya
coordinates: lat: 0.25
lon: 36.1
n. filoa&quot; as data deficient. A population found in Lake Bogoria appears to be an undescribed subspecies. The forms referred to as &quot;Oreochromis&quot; (or &quot;Tilapia&quot;) &quot;nyabikere&quot; and &quot;kabagole&quot; seem to belong to this species, too. An undescribed population found at, for example, Wami River, Lake Manyara, and Tingaylanda seems to be a close relative. Feeding.

Geographic entities mentioned:
surface_form: Lake Manyara
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.5833333333333
lon: 35.833333333333
Johnstone's son, also James, resigned the earldom and received a regrant of the title, as Earl of Annandale and Hartfell, in 1661, and a further regrant of the same title, but by crown charter, in 1662 to his heirs male of the body, whom failing, his heirs female of the body. William, the second Earl of Annandale and Hartfell, was created &quot;Marquess of Annandale&quot; in 1701.

Geographic entities mentioned:
surface_form: Annandale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.2
lon: -3.4
He left Maj. Gen. William Tecumseh Sherman in command of most of the western armies. Grant and President Abraham Lincoln devised a coordinated strategy that would strike at the heart of the Confederacy from multiple directions, including attacks against Lee near Richmond, Virginia, and in the Shenandoah Valley, West Virginia, Georgia, and Mobile, Alabama.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
After rejecting a career as a teacher, he enrolled at the Sorbonne and then at the Faculty of Law of the University of Paris. Lémery became a lawyer in 1898 and joined the bar of Paris in 1899. In May 1902 his whole family died during the eruption of Mount Pelée. In 1902 Lémery entered the office of Ernest Vallé, the Minister of Justice, as deputy to Henry de Jouvenel.

Geographic entities mentioned:
surface_form: Mount Pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
It was a town before August 6, 1965. It was named after Viau Bridge, which links it to Ahuntsic-Cartierville in Montreal, Quebec. Geography. It is delineated by the Rivière des Prairies to the south, by Duvernay to the east, by Vimont to the north and by Laval-des-Rapides to the west. Education. Commission scolaire de Laval operates French-language public schools.

Geographic entities mentioned:
surface_form: Rivière des Prairies
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.708333333333
lon: -73.479166666667
He believed to have noticed this in the works of &quot;Gândirea&quot; contributors such as Mircea Vulcănescu (in his homage to the deceased painter Sabin Popp, whom he allegedly regarded as &quot;a saint&quot;), Vasile Ciocâlteu (&quot;who asks from God, in one of his poems, the favor to hold hot coals in his hands&quot;) and the Athonite pilgrim Sandu Tudor (who believed in &quot;the workings of a mysterious miracle&quot; as explanations for various events).

Geographic entities mentioned:
surface_form: Athonite
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Its namesake, Prince of Wales Island, lies over to the east. The strait is a possible route for the Northwest Passage. The Parry Channel leads west from Baffin Bay to the strait or M'Clure Strait to the northwest. Robert McClure reached it from the west in 1850 and was frozen in. A sledge party showed that it was connected to Parry Channel;.

Geographic entities mentioned:
surface_form: Parry Channel
instance_of: Watercourse
countries: Canada
coordinates: lat: 74.33333333
lon: -93
Arcadia Lake (Oklahoma). Arcadia Lake is a reservoir in Central Oklahoma County, Oklahoma, United States. The lake is located northeast of Oklahoma City in eastern Edmond, just east of Interstate 35. The lake has a surface area of 1,820 acres (7 km²) and has about 26 miles (42 km) of shoreline. The lake was created in 1984 by an earthen dam on the Deep Fork River begun in.

Geographic entities mentioned:
surface_form: arcadia lake
instance_of: Lake
countries: United States
coordinates: lat: 44.48411
lon: -86.2394
surface_form: arcadia lake (oklahoma)
instance_of: Lake
countries: United States
coordinates: lat: 35.6445
lon: -97.3625
Arcadia Lake (Oklahoma). Arcadia Lake is a reservoir in Central Oklahoma County, Oklahoma, United States. The lake is located northeast of Oklahoma City in eastern Edmond, just east of Interstate 35. The lake has a surface area of 1,820 acres (7 km²) and has about 26 miles (42 km) of shoreline. The lake was created in 1984 by an earthen dam on the Deep Fork River begun in.

Geographic entities mentioned:
surface_form: arcadia lake
instance_of: Lake
countries: United States
coordinates: lat: 44.48411
lon: -86.2394
surface_form: arcadia lake
instance_of: Lake
countries: United States
coordinates: lat: 35.6445
lon: -97.3625
Army Corps of Engineers. It was created to control floods in the Deep Fork River Basin, supply water to the city of Edmond, and provide recreational resources to the surrounding communities. Recreational opportunities at Arcadia Lake include fishing, boating, camping, mountain biking, hiking, disc golf and equestrian trails. Waterskiing and Jet Skiing are both allowed in designated areas.

Geographic entities mentioned:
surface_form: arcadia lake
instance_of: Lake
countries: United States
coordinates: lat: 44.48411
lon: -86.2394
surface_form: arcadia lake
instance_of: Lake
countries: United States
coordinates: lat: 35.6445
lon: -97.3625
Facilities include picnic areas, a Frisbee golf course, pavilions, boat ramps, designated swim beaches and an enclosed and heated fishing dock that is handicapped accessible. Arcadia Lake also features RV campsites with full hookups and primitive tent campsites. Parks around the lake include Scissortail Park, Spring Creek Park, Central State Park and Edmond Park.

Geographic entities mentioned:
surface_form: arcadia lake
instance_of: Lake
countries: United States
coordinates: lat: 44.48411
lon: -86.2394
surface_form: arcadia lake
instance_of: Lake
countries: United States
coordinates: lat: 35.6445
lon: -97.3625
Deming Glacier (Washington). Deming Glacier is located on Mount Baker in the North Cascades of the U.S. state of Washington. Between 1850 and 1950, Deming Glacier retreated. During a cooler and wetter period from 1950 to 1979, the glacier advanced but between 1980 and 2006 retreated back.

Geographic entities mentioned:
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
During a cooler and wetter period from 1950 to 1979, the glacier advanced but between 1980 and 2006 retreated back. Situated on the southwest slopes of Mount Baker, Deming Glacier is bordered by the Easton Glacier to the east and the Black Buttes ridge to the west. Deming Glacier was named for the town of Deming, Washington, whose residents built a trail to Mount Baker in 1909.

Geographic entities mentioned:
surface_form: Black Buttes
instance_of: Landform
countries: United States
coordinates: lat: 48.7693
lon: -121.853
Although this species has been identified within a small layer of sediment, it appears to account for approximately 30% of the biovolume in Lake Chiemsee surface sediments indicating it may be a dominant fraction of the microbial community found within this layer of sediment.

Geographic entities mentioned:
surface_form: Chiemsee
instance_of: Lake
countries: Germany
coordinates: lat: 47.89
lon: 12.47
Mount Cameron (Colorado). Mount Cameron is a mountain summit in Park County, Colorado, United States. Description. Mount Cameron is set east of the Continental Divide in the Mosquito Range, which is a subrange of the Rocky Mountains. It ranks as the 2nd-highest peak in Park County, 3rd-highest in the Mosquito Range, and the 18th-highest in Colorado.

Geographic entities mentioned:
surface_form: mount cameron
instance_of: Mountain
countries: United States
coordinates: lat: 47.82537
lon: -123.32851
surface_form: mount cameron
instance_of: Mountain
countries: United States
coordinates: lat: 39.34693
lon: -106.11863
surface_form: mount cameron
instance_of: Mountain
countries: United States
coordinates: lat: 61.21
lon: -146.665
Mount Cameron (Colorado). Mount Cameron is a mountain summit in Park County, Colorado, United States. Description. Mount Cameron is set east of the Continental Divide in the Mosquito Range, which is a subrange of the Rocky Mountains. It ranks as the 2nd-highest peak in Park County, 3rd-highest in the Mosquito Range, and the 18th-highest in Colorado.

Geographic entities mentioned:
surface_form: mount cameron
instance_of: Mountain
countries: United States
coordinates: lat: 47.82537
lon: -123.32851
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount cameron
instance_of: Mountain
countries: United States
coordinates: lat: 39.34693
lon: -106.11863
surface_form: mount cameron
instance_of: Mountain
countries: United States
coordinates: lat: 61.21
lon: -146.665
Climate. According to the Köppen climate classification system, Mount Cameron is located in an alpine subarctic climate zone with cold, snowy winters, and cool to warm summers. Due to its altitude, it receives precipitation all year, as snow in winter and as thunderstorms in summer, with a dry period in late spring.

Geographic entities mentioned:
surface_form: mount cameron
instance_of: Mountain
countries: United States
coordinates: lat: 47.82537
lon: -123.32851
surface_form: mount cameron
instance_of: Mountain
countries: United States
coordinates: lat: 39.34693
lon: -106.11863
surface_form: mount cameron
instance_of: Mountain
countries: United States
coordinates: lat: 61.21
lon: -146.665
One source claims that Simon Cameron (1799–1889) is the likely namesake. Simon Cameron was the United States Secretary of War under President Abraham Lincoln at the start of the American Civil War, and Mt. Cameron is approximately one-half mile southwest of line parent Mount Lincoln.

Geographic entities mentioned:
surface_form: mt. cameron
instance_of: Mountain
countries: United States
coordinates: lat: 47.82537
lon: -123.32851
surface_form: mount lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 44.149
lon: -71.6445
surface_form: mount lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 47.55009
lon: -123.32822
surface_form: mount lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 39.35138889
lon: -106.11083333
surface_form: mount lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 39.28768
lon: -120.32798
surface_form: mt. cameron
instance_of: Mountain
countries: United States
coordinates: lat: 61.21
lon: -146.665
surface_form: mount lincoln
instance_of: Mountain
countries: United States
coordinates: lat: 42.3639
lon: -72.4231
Pennington Lake. Pennington Lake is a lake in Kanabec County, in the U.S. state of Minnesota. Pennington Lake was named for James Pennington, a pioneer farmer.

Geographic entities mentioned:
surface_form: pennington lake
instance_of: Lake
countries: United States
coordinates: lat: 45.780833333333
lon: -93.272222222222
Fossil Mountain has also been the site of paleontological research. Sedimentary strata of the Ely Springs Dolomite, Eureka Quartzite, Crystal Peak Dolomite, Watson Ranch Quartzite, and the highly fossiliferous upper Pogonip Group are exposed on it slopes and by its cliffs. History.

Geographic entities mentioned:
surface_form: crystal peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.113333333333
lon: -121.83583333333
surface_form: crystal peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.4344
lon: -106.114
surface_form: crystal peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.557777777778
lon: -120.08833333333
surface_form: crystal peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.942222222222
lon: -120.125
surface_form: crystal peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.964722222222
lon: -106.79972222222
surface_form: crystal peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.906247
lon: -121.519048
surface_form: crystal peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.9185
lon: -113.227
The formations of the upper Pogonip Group accumulated on a shallow marine shelf during the early and middle Ordovician Period (about 485 to 458 million years ago). Overlying the upper Pogonip Group, from oldest to youngest, are the Watson Ranch Quartzite, Crystal Peak Dolomite, and Eureka Quartzite. The summit of Fossil Mountain consists of Eureka Quartzite.

Geographic entities mentioned:
surface_form: crystal peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.113333333333
lon: -121.83583333333
surface_form: crystal peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.4344
lon: -106.114
surface_form: crystal peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.557777777778
lon: -120.08833333333
surface_form: crystal peak
instance_of: Mountain
countries: United States
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Fossil Mountain (Utah). Fossil Mountain is a peak in the south end of the Confusion Range in Millard County, Utah. It is a well-known and popular location with rockhounds and fossil hunters because of the variety and abundance of Ordovician fossils found on it. Fossil Mountain has also been the site of paleontological research.

Geographic entities mentioned:
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instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
Fossil Mountain (Utah). Fossil Mountain is a peak in the south end of the Confusion Range in Millard County, Utah. It is a well-known and popular location with rockhounds and fossil hunters because of the variety and abundance of Ordovician fossils found on it. Fossil Mountain has also been the site of paleontological research.

Geographic entities mentioned:
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
History. Frank Beckwith was the first person to appreciate and publicize the abundant Ordovician fossils at Fossil Mountain along with the abundant Cambrian fossils around Antelope Springs. Around 1910, he started as a cashier at the first bank in the newly founded town of Delta.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
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instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
From Delta, Utah, he and his friend, Charles Kelly, roamed the deserts of Utah and collected fossils and Native American artifacts. It was during this time that they recognized the abundance of well-preserved fossils at Fossil Mountain and around Antelope Springs. Beckwith named &quot;Fossil Mountain&quot; because of the abundance of marine invertebrate fossils found on its slopes.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
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countries: United States
coordinates: lat: 43.6536
lon: -110.919
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countries: United States
coordinates: lat: 36.19026
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Beckwith named &quot;Fossil Mountain&quot; because of the abundance of marine invertebrate fossils found on its slopes. Both Beckwith and Kelly promoted Fossil Mountain and Antelope Springs to rockhounds and fossil collectors to encourage to visit and spend time in Millard County, Utah.

Geographic entities mentioned:
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instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
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countries: United States
coordinates: lat: 43.6536
lon: -110.919
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instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
Both Beckwith and Kelly promoted Fossil Mountain and Antelope Springs to rockhounds and fossil collectors to encourage to visit and spend time in Millard County, Utah. Later, as editor of the weekly newspaper in Delta, Beckwith encouraged professional paleontologists to study the Cambrian trilobites found around Antelope Springs and Ordovician fossils found at Fossil Mountain.

Geographic entities mentioned:
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instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
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instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
As a result, in the 1930s, the University of Utah geology department conducted regular student field trips to collect Ordovician fossils. Also, Charles E. Resser, Curator of Paleontology, U.S. National Museum, visited Fossil Mountain in 1930, to conduct paleontological research. Beckwith also sent to the U.S.

Geographic entities mentioned:
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instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
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Also, Charles E. Resser, Curator of Paleontology, U.S. National Museum, visited Fossil Mountain in 1930, to conduct paleontological research. Beckwith also sent to the U.S. National Museum several collections of Ordovician fossils, including trilobites, brachiopods, ostracods, gastropods, and cephalopods, from Fossil Mountain.

Geographic entities mentioned:
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instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
Of these fossils, Ulrich and Cooper (1938) formally described the Ordovician brachiopods. In the late 1940s and early 1950s, Hintze made extensive collections of fossils from and described the stratigraphy of lower Paleozoic strata exposed at Fossil Mountain and the surrounding Confusion Range.

Geographic entities mentioned:
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
The fossils included various genera of trilobites, brachiopods, ostracods, and gastropods, nautiloids, cystoids, and a receptaculitid. Hintze also designated the east slope of Fossil Mountain as the type section for the Kanosh Shale. Geology.

Geographic entities mentioned:
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
Geology. The cliffs and slopes of Fossil Mountain expose a neatly layered set of shallow marine, early to middle Ordovician limestones, dolomites, shales, siltstones, sandstones and quartzites. At the base of Fossil Mountain, the limestones, calcium-rich siltstones, sandstones, conglomerates, and shales of the upper Pogonip Group outcrop.

Geographic entities mentioned:
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
At this location, the Pogonip Group is subdivided, from oldest to youngest, into the Wah Wah Limestone, Juab Limestone, Kanosh Shale, and Lehman Formation. The Wah Wah Limestone is poorly exposed as it is largely covered by the accumulation of colluvium and rock debris at the base of Fossil Mountain.

Geographic entities mentioned:
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
Overlying the upper Pogonip Group, from oldest to youngest, are the Watson Ranch Quartzite, Crystal Peak Dolomite, and Eureka Quartzite. The summit of Fossil Mountain consists of Eureka Quartzite. They consist of an interbedded quartzite, limestone, and dolomite.

Geographic entities mentioned:
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
This diversity of invertebrate fossils found at this location reflects the biodiversification of invertebrates at the family, genus, and species levels during the Great Ordovician Biodiversification Event. The fossils at Fossil Mountain are commonly fragmentary because they accumulated in a high-energy, wave-dominated shoreline and shallow marine environments.

Geographic entities mentioned:
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
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Typically, they are cemented together into thin beds of fossil hash. The most common fossils found on the slopes of Fossil Mountain are brachiopods, gastropods, crinoids, cephalopods, and trilobites. As part of the King Top Wilderness Area, only surface collecting is allowed, and digging is prohibited by the U.S. Bureau of Land Management Fillmore Field Office.

Geographic entities mentioned:
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
The first dry storage installation in the US was licensed by the Nuclear Regulatory Commission (NRC) in 1986 at the Surry Nuclear Power Plant in Virginia. Yucca Mountain, in Nevada, was expected to open in 2017. However, on March 5, 2009, Energy Secretary Steven Chu reiterated in a Senate hearing that the Yucca Mountain site was no longer considered an option for storing reactor waste.

Geographic entities mentioned:
surface_form: Yucca Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.9402
lon: -116.485
The steepest gradient is 1:9. The C14 is one of the major tourist routes in Namibia, leading to the tourist attractions, Kuiseb River and Canyon, Gaub River Canyon, the Tropic of Capricorn road sign (), Solitaire and Helmeringhausen. It touches the Namib-Naukluft National Park and also serves an access road to Sossusvlei, Sesriem, Duwisib Castle, and the Fish River Canyon. C14 Challenges.

Geographic entities mentioned:
surface_form: Sossusvlei
instance_of: Valley
countries: Namibia
coordinates: lat: -24.73983
lon: 15.28765
The peak is named after Midzhur Peak in western Balkan Mountains. Location. Midzhur Peak is located at, which is 3.15 km East-northeast of Mount Benson, 7.91 km south-southwest of Taylor Spur and 3.6 km northwest of Johnson Spur. US mapping in 1961, updated in 1988.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: benson
instance_of: Mountain
coordinates: lat: -78.6064
lon: -84.5308
surface_form: mount benson
instance_of: Mountain
coordinates: lat: -78.6064
lon: -84.5308
surface_form: midzhur peak
instance_of: Mountain
coordinates: lat: -78.5928
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Midzhur Peak (Antarctica). Midzhur Peak (,) is the peak rising to 1627 m in Doyran Heights, southeast Sentinel Range in Ellsworth Mountains, Antarctica, and surmounting Remington Glacier to the north and Obelya Glacier to the south. The peak is named after Midzhur Peak in western Balkan Mountains. Location.

Geographic entities mentioned:
surface_form: midzhur peak (antarctica)
instance_of: Mountain
coordinates: lat: -78.5928
lon: -84.4072
Midzhur Peak (Antarctica). Midzhur Peak (,) is the peak rising to 1627 m in Doyran Heights, southeast Sentinel Range in Ellsworth Mountains, Antarctica, and surmounting Remington Glacier to the north and Obelya Glacier to the south. The peak is named after Midzhur Peak in western Balkan Mountains. Location.

Geographic entities mentioned:
surface_form: midzhur peak
instance_of: Mountain
coordinates: lat: -78.5928
lon: -84.4072
Most of the township is drained by Swan Creek and its tributaries. The northeast corner of the township is drained by Port Creek, a tributary of the Huron River, while the southwest corner is drained by Stony Creek. Swan Creek, Stony Creek, and the Huron River are all southeast-flowing direct tributaries of Lake Erie. Education. Ash Township is served by three separate school districts.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Tussenobba Peak. Tussenobba Peak () is a peak, 2,665 m, rising 6 nautical miles (11 km) northeast of Halsknappane Hills in the east part of the Muhlig-Hofmann Mountains in Queen Maud Land. Mapped by Norwegian cartographers from surveys and air photos by the Norwegian Antarctic Expedition (1956–60) and named Tussenobba.

Geographic entities mentioned:
surface_form: tussenobba
instance_of: Mountain
coordinates: lat: -72
lon: 6.25
Tussenobba Peak. Tussenobba Peak () is a peak, 2,665 m, rising 6 nautical miles (11 km) northeast of Halsknappane Hills in the east part of the Muhlig-Hofmann Mountains in Queen Maud Land. Mapped by Norwegian cartographers from surveys and air photos by the Norwegian Antarctic Expedition (1956–60) and named Tussenobba.

Geographic entities mentioned:
surface_form: tussenobba
instance_of: Mountain
coordinates: lat: -72
lon: 6.25
surface_form: hofmann
instance_of: Mountain
coordinates: lat: -82.6667
lon: 160.6
Mountain Ash Urban District. Mountain Ash Urban District was a local authority in Mountain Ash, in the Cynon Valley, Glamorgan, Wales. It was created in 1894 as a result of the 1894 Local Government of England and Wales Act. The council replaced the Mountain Ash Local Board of Health which had been established in 1867.

Geographic entities mentioned:
surface_form: Cynon Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.657
lon: -3.461
Initially, the Council had fifteen members, but this was increased to eighteen in 1898. The council was based at Mountain Ash Town Hall. The urban district was abolished in 1974, becoming part of the borough of Cynon Valley, which was in turn abolished in 1996 to become part of Rhondda Cynon Taf. 1894 Election. The inaugural election was held in December 1894.

Geographic entities mentioned:
surface_form: Cynon Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.657
lon: -3.461
It is located in the Halifax Regional Municipality and connects Dartmouth at Exit 6 of Highway 111 with Waverley at Trunk 2. It is also called &quot;Waverley Road&quot; and &quot;Braemar Drive.&quot; The road follows the north shore of Lake Micmac, Lake Charles, Nova Scotia, and Lake William, which comprise part of the historic Shubenacadie Canal route. History.

Geographic entities mentioned:
surface_form: Lake Micmac
instance_of: Lake
countries: Canada
coordinates: lat: 44.6932
lon: -63.5534
surface_form: Shubenacadie Canal
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.7018
lon: -63.5543
Courtney Peak (Antarctica). Courtney Peak is a peak, high, in the northern part of the Gross Hills, Heritage Range. It was mapped by the United States Geological Survey from surveys and from U.S. Navy air photos, 1961–66, and named by the Advisory Committee on Antarctic Names for electronics technician Kenneth N. Courtney, U.S.

Geographic entities mentioned:
surface_form: Gross Hills
instance_of: Mountain
coordinates: lat: -79.3
lon: -83.3667
surface_form: courtney peak
instance_of: Mountain
coordinates: lat: -79.2333
lon: -83.5833
Courtney Peak (Antarctica). Courtney Peak is a peak, high, in the northern part of the Gross Hills, Heritage Range. It was mapped by the United States Geological Survey from surveys and from U.S. Navy air photos, 1961–66, and named by the Advisory Committee on Antarctic Names for electronics technician Kenneth N. Courtney, U.S.

Geographic entities mentioned:
surface_form: courtney peak
instance_of: Mountain
coordinates: lat: -79.2333
lon: -83.5833
May 2021. Sri Lanka experienced flash floods and torrential rain fall in the month of May due to Cyclone Yaas which originated in the Bay of Bengal. According to Sri Lanka's Disaster Management Centre, the floods in the month of May killed at least 4 people and about 42000 people were affected. It was reported that around 200 houses were either fully or partially damaged by the floods in May 2021.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
It had approximately 5,000 soldiers trained in mountain warfare and was commanded by General Zygmunt Szyszko-Bohusz. It was named after the region of Podhale in southern Poland. In February it was assigned to the Anglo-French expeditionary corps prepared to be sent to Finland.

Geographic entities mentioned:
surface_form: Podhale
instance_of: Valley
countries: Poland
coordinates: lat: 49.4793
lon: 20.0291
Ransome and Cape. The story follows the model of the books of Arthur Ransome, describing the school holiday adventures of children of active, adventurous families, centred on outdoor activity and a vivid landscape soaked in imagination. Ransome had boats and Windermere, &quot;The Far-Distant Oxus&quot; ponies and the moors.

Geographic entities mentioned:
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
Fin Nunatak. qxk3gj73f2bjcqcf5wstrlj07qi" xml:space="preserve">#redirect Fin Nunatak

Geographic entities mentioned:
surface_form: fin nunatak
instance_of: Mountain
coordinates: lat: -69.05
lon: -64.05
Muisca. In the centuries before the Spanish conquest of the Muisca in 1537, the Altiplano Cundiboyacense, high plateau of the Eastern Ranges of the Colombian Andes, was inhabited by the Muisca people. They were an advanced civilisation of mainly farmers and traders.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877