Sarmila/GeoWiki-Features huggingface dataset:
During the 1983 eruption, ashfall occurred at tens of kilometers from the volcano. The emission of a lava flow onto the western flank of Ol Doinyo Lengai in 2006 was accompanied by the formation of a pit crater on the summit. A large explosive eruption began on the 4 September 2007, producing a -high eruption column and a new crater deep and wide.

Geographic entities mentioned:
surface_form: doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: ol doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
Wild animals such as flamingos were also impacted by the eruption. The eruption was preceded in July by seismic activity, which was frequently mistaken for renewed eruptions, and the intrusion of a dyke less than from Ol Doinyo Lengai. General appearance of lava flows. Lavas erupted by Ol Doinyo Lengai initially have brown or black colors, but within days to hours become white like snow.

Geographic entities mentioned:
surface_form: doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: ol doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
General appearance of lava flows. Lavas erupted by Ol Doinyo Lengai initially have brown or black colors, but within days to hours become white like snow. The lavas of Ol Doinyo Lengai have temperatures of; they are so cold that during the day they look like mudflows or oil and glow only during the night.

Geographic entities mentioned:
surface_form: doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: ol doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
More viscous flows containing silicic rocks have also been observed, for example during the 1993 eruption. Hazards. Potential threats from Ol Doinyo Lengai eruptions are scarcely established. Threats from eruptions at Ol Doinyo Lengai include lahars, landslides, lava flows, pyroclastic flows, volcanic bombs, volcanic gas, and volcanic ash fall.

Geographic entities mentioned:
surface_form: doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: ol doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
Hazards. Potential threats from Ol Doinyo Lengai eruptions are scarcely established. Threats from eruptions at Ol Doinyo Lengai include lahars, landslides, lava flows, pyroclastic flows, volcanic bombs, volcanic gas, and volcanic ash fall. Beginning in 2016, the volcano is being monitored by a seismometer and GNSS stations. Climate and vegetation.

Geographic entities mentioned:
surface_form: doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: ol doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
Climate and vegetation. Vegetation in the area consists mostly of grassland, which reaches an elevation of above sea level. Volcanic ash from Ol Doinyo Lengai influences the surrounding landscape, favoring the growth of nutrient-rich plants. Precipitation falls during two wet seasons in March–May and October–December. Popular Culture.

Geographic entities mentioned:
surface_form: doinyo lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
Geography and geomorphology. Ol Doinyo Lengai lies in the Arusha region of Tanzania, south of Lake Natron and northwest of the city of Arusha. The summit was first explored between 1904 and 1915., about 300,000 people live in the region, and livestock farming is the most important economic activity, although tourism is increasingly important.

Geographic entities mentioned:
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
The summit was first explored between 1904 and 1915., about 300,000 people live in the region, and livestock farming is the most important economic activity, although tourism is increasingly important. Ol Doinyo Lengai is a symmetric cone that rises more than above the surrounding rift valley. It has two craters on either side of the mountain summit, which is formed by a high ridge.

Geographic entities mentioned:
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
Their occurrence may have been influenced by regional fault systems. Geology. Ol Doinyo Lengai is part of the Gregory Rift, which is part of the active East African Rift. The East African Rift is a continental rift extending from eastern to southern Africa over a length of, where there is high heat flow through a thinner crust.

Geographic entities mentioned:
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
Composition. Most of the volcanic cone is formed by melilite, nephelinite, and phonolite. Ol Doinyo Lengai is the only volcano on Earth known to have erupted carbonatitic lavas during historical times, although these rocks make up only a small fraction of the volcano and only occur in the northern crater; they only recently appeared on the volcano.

Geographic entities mentioned:
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
General appearance of lava flows. Lavas erupted by Ol Doinyo Lengai initially have brown or black colors, but within days to hours become white like snow. The lavas of Ol Doinyo Lengai have temperatures of; they are so cold that during the day they look like mudflows or oil and glow only during the night.

Geographic entities mentioned:
surface_form: lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
Early life. D'Albertis was born in 1841, in Voltri, Italy. At the age of eighteen he joined Garibaldi's army and later joined Odoardo Beccari in November 1871 on an expedition to western New Guinea. He reached the peak of Mount Arfak Geb but was compelled by fever to retreat and return to Sydney to recover. In 1874, D'Albertis returned to New Guinea to set up a base on Yule Island.

Geographic entities mentioned:
surface_form: Mount Arfak
instance_of: Mountain
countries: Indonesia
coordinates: lat: -1.15666
lon: 133.98007
Panticosa-Los Lagos. Panticosa-Los Lagos, officially called &quot;Aramón Panticosa&quot;, is a ski resort situated near the town of Panticosa in the upper Tena Valley of the western Pyrenees (province of Huesca, Spain). The resort. It has 34 km of marked pistes, being one of the most familiar resorts of the Pyrenees.

Geographic entities mentioned:
surface_form: Tena Valley
instance_of: Valley
countries: Spain
coordinates: lat: 42.666666666667
lon: -0.31666666666667
Geography. Betong is on the Malaysian border. To the north is Than To, to the east is Chanae (Narathiwat province). To the south is the Malaysian state of Perak and to the west is Kedah. The highest point of the Sankalakhiri Range (Northern Titiwangsa Mountains), high Ulu Titi Basah (เขาหลวง), is on the Thai–Malaysian border between Betong District and Hulu Perak District of Perak. History.

Geographic entities mentioned:
surface_form: Ulu Titi Basah
instance_of: Mountain
countries: Malaysia
coordinates: lat: 5.8
lon: 101.317
The north side drains into Sages Ravine, thence into Schenob Brook, the Housatonic River, and Long Island Sound. Round Mountain is bordered by Mount Frissell to the northwest, Mount Ashley to the north, and Bear Mountain to the east. Round Mountain is traversed by the Mount Frissell Trail which connects with the South Taconic Trail to the west and the Appalachian Trail to the east.

Geographic entities mentioned:
surface_form: Mount Frissell
instance_of: Mountain
countries: United States
coordinates: lat: 42.050555555556
lon: -73.482222222222
surface_form: bear mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.7962
lon: -123.672
surface_form: round mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0489
lon: -73.4764
surface_form: bear mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.93041
lon: -121.34152
surface_form: bear mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.3134
lon: -84.648
Round Mountain (Taconic Mountains). Round Mountain, located on the border of southwest Massachusetts and northwest Connecticut, is a prominent peak of the Taconic Range. The peak and southern slopes of the mountain are within Connecticut; the northern slope lies within Massachusetts.

Geographic entities mentioned:
surface_form: round mountain (taconic mountains)
instance_of: Mountain
countries: United States
coordinates: lat: 42.0489
lon: -73.4764
Round Mountain (Taconic Mountains). Round Mountain, located on the border of southwest Massachusetts and northwest Connecticut, is a prominent peak of the Taconic Range. The peak and southern slopes of the mountain are within Connecticut; the northern slope lies within Massachusetts.

Geographic entities mentioned:
surface_form: round mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0489
lon: -73.4764
The mountain is located within the towns of Mount Washington, Massachusetts and Salisbury, Connecticut; much of it has been conserved as part of Massachusetts' Mount Washington State Forest and Connecticut's Mount Riga Forest Preserve. The south side of Round Mountain drains into Riga Lake and South Pond, then into Wachocostinook Brook, Salmon Creek, the Housatonic River, and Long Island Sound.

Geographic entities mentioned:
surface_form: round mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0489
lon: -73.4764
The north side drains into Sages Ravine, thence into Schenob Brook, the Housatonic River, and Long Island Sound. Round Mountain is bordered by Mount Frissell to the northwest, Mount Ashley to the north, and Bear Mountain to the east. Round Mountain is traversed by the Mount Frissell Trail which connects with the South Taconic Trail to the west and the Appalachian Trail to the east.

Geographic entities mentioned:
surface_form: round mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0489
lon: -73.4764
surface_form: mount frissell
instance_of: Mountain
countries: United States
coordinates: lat: 42.050555555556
lon: -73.482222222222
The peak and southern slopes of the mountain are within Connecticut; the northern slope lies within Massachusetts. The mountain is located within the towns of Mount Washington, Massachusetts and Salisbury, Connecticut; much of it has been conserved as part of Massachusetts' Mount Washington State Forest and Connecticut's Mount Riga Forest Preserve.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 47.5311964
lon: -123.2459807
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 47.5311964
lon: -123.2459807
Devils Bedstead East. Devil's Bedstead East, at above sea level is the fifth-highest peak in the Pioneer Mountains of the U.S. state of Idaho. The peak is located Salmon-Challis National Forest in Custer County about north of the Blaine County border and north-northeast of Goat Mountain. It is the 21st-highest peak in Idaho.

Geographic entities mentioned:
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7742
lon: -114.142
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 61.047222222222
lon: -149.04972222222
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.705
lon: -113.591
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.92846
lon: -121.62625
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.86994
lon: -118.57427
Devils Bedstead East. Devil's Bedstead East, at above sea level is the fifth-highest peak in the Pioneer Mountains of the U.S. state of Idaho. The peak is located Salmon-Challis National Forest in Custer County about north of the Blaine County border and north-northeast of Goat Mountain. It is the 21st-highest peak in Idaho.

Geographic entities mentioned:
surface_form: devils bedstead east
instance_of: Mountain
countries: United States
coordinates: lat: 43.7742
lon: -114.142
Adolphus Lake. Adolphus Lake is in Alberta, Canada, on the border of Jasper National Park and Mount Robson Provincial Park. Adolphus Lake was named after Adolphus Moberly, an early Métis in the Jasper area with close links to the local Iroquois. He guided the Arthur Coleman 1908 expedition from Jasper valley up the Moose River, to Moose Pass.

Geographic entities mentioned:
surface_form: mount robson
instance_of: Mountain
countries: Canada
coordinates: lat: 53.11055555555556
lon: -119.15666666666667
surface_form: adolphus lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.17111
lon: -119.11778
Adolphus Lake was named after Adolphus Moberly, an early Métis in the Jasper area with close links to the local Iroquois. He guided the Arthur Coleman 1908 expedition from Jasper valley up the Moose River, to Moose Pass. The expedition continued into the headwaters of the Smoky River, and over Robson Pass to the foot of Robson Glacier.

Geographic entities mentioned:
surface_form: moose
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.91444444444444
lon: -118.80638888888889
surface_form: moose
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.91444444444444
lon: -118.80638888888889
Adolphus Lake. Adolphus Lake is in Alberta, Canada, on the border of Jasper National Park and Mount Robson Provincial Park. Adolphus Lake was named after Adolphus Moberly, an early Métis in the Jasper area with close links to the local Iroquois. He guided the Arthur Coleman 1908 expedition from Jasper valley up the Moose River, to Moose Pass.

Geographic entities mentioned:
surface_form: adolphus lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.17111
lon: -119.11778
The late phase of this period sees the beginnings of the Migration Period, starting with the invasions of the Teutons and the Cimbri until their defeat at the Battle of Aquae Sextiae in 102 BC, presaging the more turbulent Roman Iron Age and Migration Period. Fortified settlements from this period include Tönsberg, Erdenburg and Grotenburg in Germany, Borremose in Denmark and Atuatuca in Belgium.

Geographic entities mentioned:
surface_form: Tönsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.953577777778
lon: 8.6757666666667
Important royal or elite centres from this period include Gamla Uppsala in Sweden, Lejre and Tissø in Denmark, and Avaldsnes and Borg (Lofotr) in Norway.

Geographic entities mentioned:
surface_form: Tissø
instance_of: Lake
countries: Denmark
coordinates: lat: 55.57591
lon: 11.29205
Susunia, Purulia. Susunia (also called Sushina) is a village in the Manbazar II CD block in the Manbazar subdivision of the Purulia district in the state of West Bengal, India. Area overview. Purulia district forms the lowest step of the Chota Nagpur Plateau. The general scenario is undulating land with scattered hills.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Background. McCrory was one of six children born in the village of Hope Villa on Bayou Manchac in Ascension Parish near Baton Rouge to the former Estelle Buffington Buillon and Cecil C. McCrory (1880-1944), a cotton farmer and a graduate of Louisiana State University with degrees in both mechanical and electrical engineering.

Geographic entities mentioned:
surface_form: Bayou Manchac
instance_of: Landform
countries: United States
coordinates: lat: 30.3456
lon: -90.8919
In the, the locality of Millaa Millaa had a population of 523 people. Geography. Millaa Millaa is on the Atherton Tableland in Far North Queensland, approximately west of Innisfail, north of Ravenshoe, and south of Malanda. The town is known for the Millaa Millaa Falls, the Millaa Millaa lookout and rolling green meadows that enjoy high rainfall.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
The type locality is Taylor Pit (Concession XIV; Lot 13), Huntingdon Township, Hastings County in Ontario, Canada. Small deposits have also been found in Les Cougnasses Mine, Orpierre in the Haut-Alpes in France, Khaidarkan Sb-Hg deposit (Chaidarkan), Fergana Valley, Alai Range, Osh Oblast, Kyrgyzstan and Reese River District, Lander County, Nevada, USA.

Geographic entities mentioned:
surface_form: Fergana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
Guriel took this information in stride. However, on March 2, 1951, Ben-Natan gathered in Switzerland on the shores of Lake Geneva European residents who had previously worked under his leadership, and they actually went on strike, declaring that they would not continue their previous work.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Early life and education. Drake was born in Los Angeles, California. She grew up between Los Angeles and &quot;Naatsisʼáán&quot; (), where her mother and maternal family are from. Drake attended Yale College, where she studied English and ethnicity, race, and migration and graduated with a BA degree from each of the two departments.

Geographic entities mentioned:
surface_form: &quot;Naatsisʼáán&quot;
instance_of: Mountain
countries: United States
coordinates: lat: 37.034169444444
lon: -110.86888888889
&quot;Majenos&quot; are the most basic level of dress adorning the traditional horse riding gear. A &quot;majeta&quot; is a person who lives near the Majes River in the Andes and the attire of this character is based on that. Wool horse-riding pants, a leather cap, a harrington-like traditional Peruvian jacket, hollowed out bull's horn for the alcohol.

Geographic entities mentioned:
surface_form: Majes River
instance_of: Watercourse
countries: Peru
coordinates: lat: -16.63206
lon: -72.76484
In the south-western Majunga Basin, interbedded limestones and mudstones (shales and marls) above the Aalenian Sandstone were attributed to a Bajocian carbonate platform formed by the Bemaraha Formation. The carbonate platform at the Manambolo and Tsiribihina River gorges, which cut through the Bemaraha plateau, are likewise assigned to the Early Bajocian.

Geographic entities mentioned:
surface_form: Manambolo
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -19.24025
lon: 44.33283333333333
surface_form: Tsiribihina River
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -19.8833
lon: 44.45
Some, particularly those associated with flexed burial contexts, were constructed using clay composition and decorative painting styles that resemble ceramics found at nearby Sophy and Lovea sites. Angkor iron-and ash-glaze ceramics, Phimai Black pottery, Southern Chinese pottery, and a Kulen lid fragment were also recovered from mortuary contexts.

Geographic entities mentioned:
surface_form: Kulen
instance_of: Mountain
countries: Cambodia
coordinates: lat: 13.612777777778
lon: 104.1125
Ontario Highway 83. King's Highway 83, also known as Highway 83, was a provincially maintained highway in the Canadian province of Ontario. The route travelled inwards from the shores of Lake Huron, beginning at Highway 21 north of Grand Bend and travelling eastward to Highway 23 in Russeldale.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Zabovci. Zabovci () is a settlement in the Municipality of Markovci in northeastern Slovenia. It lies just north of Lake Ptuj east of Ptuj. The area is part of the traditional region of Styria. It is now included with the rest of the municipality in the Drava Statistical Region.

Geographic entities mentioned:
surface_form: Lake Ptuj
instance_of: Lake
countries: Slovenia
coordinates: lat: 46.40194444
lon: 15.89333333
1952 Volta a Catalunya. The 1952 Volta a Catalunya was the 32nd edition of the Volta a Catalunya cycle race and was held from 7 September to 14 September 1952. The race started in Montjuïc and finished in Barcelona. The race was won by Miguel Poblet.

Geographic entities mentioned:
surface_form: Montjuïc
instance_of: Mountain
countries: Spain
coordinates: lat: 41.364166666667
lon: 2.1580555555556
Each pump has the capacity to remove, or, per minute. Water is drained into the Markermeer, with check valves ensuring that the discharge is not returned to the polder. Fuel for the engines was originally stored aboveground; a subterranean storage facility has since been installed northeast of the station. On its southwest façade, the pumping station features a relief by.

Geographic entities mentioned:
surface_form: Markermeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.566666666667
lon: 5.2166666666667
During the visit of the expedition to the Ellice Islands (now known as Tuvalu) Alfred Thomas Agate recorded the dress and tattoo patterns of men of Nukufetau. Agate created the first known picture of Mount Shasta. Agate contributed more than half (173 of 342) of the sketches and paintings reproduced as lithographs illustrating the five volumes of the expedition's reports.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Passwang Pass. Passwang Pass (elevation) is a high mountain pass in the Jura Mountains in the canton of Solothurn in Switzerland.

Geographic entities mentioned:
surface_form: passwang pass
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.3583
lon: 7.65611
It connects the southern part of the canton of Solothurn via Mümliswil-Ramiswil (south of the pass) and Beinwil, Solothurn (northern side) with the so-called &quot;Schwarzbubenland&quot; (officially &quot;Amtei Dorneck-Thierstein&quot;, consisting of the canton of Solothurn districts Thierstein and Dorneck) north of the Passwang mountain chain, and ultimately with the Laufen District in the canton of Basel-Landschaft.

Geographic entities mentioned:
surface_form: passwang
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.3583
lon: 7.65611
Säuling. Säuling or Saulingspitze is a twin-peak mountain in the German Allgäu, though part of the mountain is in Austria. The two summits have heights of and. It is located near the town of Füssen and the castle Neuschwanstein.

Geographic entities mentioned:
surface_form: säuling
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.534722222222
lon: 10.755
Free life and death. Under her aunt and uncle's leadership, she was educated at Buxton Mission at the Elgin Settlement (now Buxton National Historic Site and Museum), twelve miles south of Chatham, Ontario, which was one of four settlements established in Canada for black people. The 9,000-acre settlement was located between Lake Erie and the Great Western Railway line.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Distribution and habitat. &quot;M. multivaga&quot; is known from Fraser fir and red spruce forests on mountain peaks at and above in the Southern Appalachian Mountains of North Carolina, Virginia and Tennessee. It has been recorded from Kuwohi and Mount Collins (both very small populations), Mount Le Conte, Mount Mitchell (where probably extirpated), Grandfather Mountain, and Roan Mountain.

Geographic entities mentioned:
surface_form: Kuwohi
instance_of: Mountain
countries: United States
coordinates: lat: 35.562777777778
lon: -83.498611111111
surface_form: Mount Collins
instance_of: Mountain
countries: United States
coordinates: lat: 35.586388888889
lon: -83.472777777778
surface_form: Grandfather Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.111111111111
lon: -81.811388888889
Kangshung Glacier. The Kangshung Glacier () is one of the three main glaciers of Mount Everest, and is in the Tibet region Himalayas, within the Tibet Autonomous Region of China. The other two are the Khumbu Glacier and Rongbuk Glacier. Geography. The Kangshung Glacier's accumulation areas lie on the three main faces of Everest.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
The Kangshung Glacier is located on the eastern side of the world's highest mountain in the government district of Shigatse in the Tibet Autonomous Region of the People's Republic of China. The common eastern face of Everest and Lhotse is called the Kangshung Face. Here, the Kangshung Glacier is fed and then becomes the Kama Chu river to flow through the Kama valley towards the east.

Geographic entities mentioned:
surface_form: Lhotse
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.961666666667
lon: 86.933333333333
Here, the Kangshung Glacier is fed and then becomes the Kama Chu river to flow through the Kama valley towards the east. South of the glacier and east of Lhotse lie the Pethangtse (6738 m), and the massif of the Makalu (8463 m) with its neighbouring peaks of Makalu II (7678 m − also called Kangshungtse) and Chomo Lonzo (7818 m), whose imposing north face hides the view of the main Makalu summit.

Geographic entities mentioned:
surface_form: Lhotse
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.961666666667
lon: 86.933333333333
surface_form: Makalu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.889166666667
lon: 87.088611111111
surface_form: Chomo Lonzo
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 27.93
lon: 87.108055555556
While the base camp on the Rongbuk Glacier can be accessed by jeep and the south side of Everest can be reached after a multi-day hike using fortified lodges for overnight stays, the Kangshung Glacier can only be reached following an approach march of several days from Kharta, including crossing via the Shao La or Langma La passes into the Kama valley. Melting.

Geographic entities mentioned:
surface_form: Kharta
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 28.1
lon: 87.1667
Anderson Canyon. Anderson Canyon in the Big Sur region of California was named after pioneering homesteaders James and Peter Andersen who were the first European settlers of the area. The canyon, Anderson Creek, and Anderson Peak () are south of McWay Falls and within the boundaries of Julia Pfeiffer Burns State Park.

Geographic entities mentioned:
surface_form: anderson peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.259033333333335
lon: -120.297175
surface_form: anderson peak
instance_of: Mountain
countries: United States
coordinates: lat: 34.1245
lon: -116.894
In 2006, two condors were discovered nesting in a hollowed out, partially burned redwood tree. These were the first natural birth of a condor in California since 1905. In 2011, PG&E began a $4.2 million project to bury power lines running from Highway One up Anderson Canyon to Anderson Peak in order to protect condors from potential electrocution.

Geographic entities mentioned:
surface_form: anderson peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.259033333333335
lon: -120.297175
surface_form: anderson canyon
instance_of: Valley
countries: United States
coordinates: lat: 36.1567
lon: -121.6652
surface_form: anderson peak
instance_of: Mountain
countries: United States
coordinates: lat: 34.1245
lon: -116.894
Anderson Canyon. Anderson Canyon in the Big Sur region of California was named after pioneering homesteaders James and Peter Andersen who were the first European settlers of the area. The canyon, Anderson Creek, and Anderson Peak () are south of McWay Falls and within the boundaries of Julia Pfeiffer Burns State Park.

Geographic entities mentioned:
surface_form: anderson canyon
instance_of: Valley
countries: United States
coordinates: lat: 36.1567
lon: -121.6652
After the camp closed, literary bohemians like Henry Miller rented the shacks, forming what Miller later called the &quot;Anderson Creek Gang&quot;. The canyon is within the boundaries of the Monterey Bay National Marine Sanctuary, Sea Otter Refuge, and California condor reintroduction area. The Staude House built in the 1960s sits on a bluff at the mouth of Anderson Canyon above sea level.

Geographic entities mentioned:
surface_form: anderson canyon
instance_of: Valley
countries: United States
coordinates: lat: 36.1567
lon: -121.6652
Pop's restaurant was a favorite of George Sterling, Jack London, and Andrew Molera. Highway construction. The section of Highway One between Anderson Canyon and Big Sur was completed in October, 1924. In 1926, construction was halted due to lack of funds. Anderson Canyon was the southern terminus of the road.

Geographic entities mentioned:
surface_form: anderson canyon
instance_of: Valley
countries: United States
coordinates: lat: 36.1567
lon: -121.6652
In 1926, construction was halted due to lack of funds. Anderson Canyon was the southern terminus of the road. Construction of the southern portion resumed in 1928, and in 1932, Anderson canyon was selected as the site of the largest prison labor camp on the coast. From the Anderson Canyon camp, the highway was built south to connect with the road at Big Creek.

Geographic entities mentioned:
surface_form: anderson canyon
instance_of: Valley
countries: United States
coordinates: lat: 36.1567
lon: -121.6652
surface_form: anderson canyon
instance_of: Valley
countries: United States
coordinates: lat: 36.1567
lon: -121.6652
Anderson Canyon was the southern terminus of the road. Construction of the southern portion resumed in 1928, and in 1932, Anderson canyon was selected as the site of the largest prison labor camp on the coast. From the Anderson Canyon camp, the highway was built south to connect with the road at Big Creek. Anderson Canyon was the last labor camp built.

Geographic entities mentioned:
surface_form: anderson canyon
instance_of: Valley
countries: United States
coordinates: lat: 36.1567
lon: -121.6652
surface_form: big creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.41361111
lon: -91.60583333
During the 1940 and early 1950s, these cabins were rented out to early Bohemians. Henry Miller lived in a shack in Anderson Canyon from 1944 to 1947. Miller wrote &quot;Into the Nightlife&quot; while living there, and he described his fellow artists as the &quot;Anderson Creek Gang&quot; in &quot;Big Sur and the Oranges of Hieronymus Bosch&quot;.

Geographic entities mentioned:
surface_form: anderson canyon
instance_of: Valley
countries: United States
coordinates: lat: 36.1567
lon: -121.6652
Staude House. In 1965, Tony Staude, former chairman of pharmaceutical wholesaler Bergen Brunswig, and his wife, sculptor Marguerite Brunswig, bought property in Anderson Canyon. They found abandoned cars and remnants of the convict labor camp, including the former infirmary.

Geographic entities mentioned:
surface_form: anderson canyon
instance_of: Valley
countries: United States
coordinates: lat: 36.1567
lon: -121.6652
Characteristic species include coastal redwood, California bay, tanbark oak, big-leaf maple, and western sword fern. Wildlife species that may occur in this community include ensatina, Pacific slender salamander, Pacific giant salamander, western-screech owl, Allen's hummingbird, purple martin, acorn woodpecker, Steller's jay, Townsend's western big-eared bat, and pallid bat. Film credits.

Geographic entities mentioned:
surface_form: allen
instance_of: Watercourse
countries: United States
coordinates: lat: 40.44452778
lon: -92.04033333
Film credits. Anderson Canyon appears in many films and photoshoots including National Geographic's &quot;Big Sur: Wild California&quot;, the Richard Burton and Liz Taylor classic &quot;The Sandpiper&quot;, and more recently in a feature film based on Jack Kerouac's &quot;Big Sur&quot;.

Geographic entities mentioned:
surface_form: anderson canyon
instance_of: Valley
countries: United States
coordinates: lat: 36.1567
lon: -121.6652
Coreys, New York. Coreys is a small unincorporated hamlet in Franklin County, New York, in the US, near Stony Creek Ponds, south of Upper Saranac Lake. It is 9 miles east of Tupper Lake, and 13 miles southwest of Saranac Lake in the Adirondack Park. Its most famous resident was Clarence Petty.

Geographic entities mentioned:
surface_form: Stony Creek Ponds
instance_of: Lake
coordinates: lat: 44.22222222222222
lon: -74.30499999999999
surface_form: Upper Saranac Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.2925
lon: -74.325555555556
River Swale. The River Swale in Yorkshire, England, is a major tributary of the River Ure, which becomes the River Ouse, that empties into the North Sea via the Humber Estuary. The river gives its name to Swaledale, the valley through which it flows. The river and its valley are home to many types of flora and fauna typical to the Yorkshire Dales.

Geographic entities mentioned:
surface_form: Swaledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.361
lon: -1.838
Annual rainfall figures average 1800 mm p.a. in the headwaters and 1300 mm p.a. in the lower waters over a drop of 148 m in 32 km. Course. The source of the Swale is at the confluence of Birkdale Beck and Great Sleddale Beck. The river flows north-north-east past lead mines on its northern bank and the end of Whitsundale and then eastwards towards the first of many waterfalls in the headwaters.

Geographic entities mentioned:
surface_form: Birkdale Beck
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.416
lon: -2.25
Kurabalakota is located at. It has an average elevation of 764 meters (2211 feet). Lat (DMS) 13° 39' 8N Long (DMS) 78° 28' 54E
Transport. It is near Madanapalle & Horsley Hills. The National Highway 340, which connects Hyderabad–Tokapalle road, bypasses the village. Sri Santhana Venugopala Swamy Temple, Thettu is located within 7 km.

Geographic entities mentioned:
surface_form: Horsley Hills
instance_of: Mountain
countries: India
coordinates: lat: 13.6508702
lon: 78.3965255
Little Lake Butte des Morts. Little Lake Butte des Morts is a lake in the US state of Wisconsin, eight miles north of Lake Butte des Morts. It is part of the Fox–Wisconsin Waterway and receives its inflow from a short segment of the Fox River which drains from the north end of Lake Winnebago around Doty Island.

Geographic entities mentioned:
surface_form: Lake Butte des Morts
instance_of: Lake
countries: United States
coordinates: lat: 44.073055555556
lon: -88.641944444444
surface_form: little lake butte des morts
instance_of: Lake
countries: United States
coordinates: lat: 44.209444444444
lon: -88.464166666667
Little Lake Butte des Morts. Little Lake Butte des Morts is a lake in the US state of Wisconsin, eight miles north of Lake Butte des Morts. It is part of the Fox–Wisconsin Waterway and receives its inflow from a short segment of the Fox River which drains from the north end of Lake Winnebago around Doty Island.

Geographic entities mentioned:
surface_form: little lake butte des morts
instance_of: Lake
countries: United States
coordinates: lat: 44.209444444444
lon: -88.464166666667
It is part of the Fox–Wisconsin Waterway and receives its inflow from a short segment of the Fox River which drains from the north end of Lake Winnebago around Doty Island. The north end of Little Lake Butte des Morts becomes the section of the Fox River running to Green Bay. The lake is part of the Butte des Morts region in Winnebago County, Wisconsin.

Geographic entities mentioned:
surface_form: little lake butte des morts
instance_of: Lake
countries: United States
coordinates: lat: 44.209444444444
lon: -88.464166666667
The southern half of the lake is located within the cities of Menasha and Neenah. The name &quot;Butte des Morts&quot; was given by French settlers, and means &quot;Mound of the Dead&quot; in reference to a nearby Indian burial mound. French archives state that in 1716, over 8000 civilians and over 500 soldiers lived within the fortified walls of Little Lake Butte des Morts.

Geographic entities mentioned:
surface_form: little lake butte des morts
instance_of: Lake
countries: United States
coordinates: lat: 44.209444444444
lon: -88.464166666667
One of the most well known, and most celebrated ghost legends in Indiana is that of Diana of the Dunes. Near Chesterton, Indiana, in the Indiana Dunes, there is a legend that fishermen around Lake Michigan would occasionally catch sight of a naked woman swimming in the lake. The legend dates back to at least 1915, and goes on to say that a beautiful woman was living as a hermit near the lake.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Drivers can access the road from State Highway M-26 on either end near Eagle Harbor to the west or Copper Harbor to the east in the Keweenaw Peninsula. The drive runs along the ridge of Brockway Mountain on the Keweenaw Fault and climbs to above sea level, above the surface of Lake Superior.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
It has an area of 80 km2 and a population of 400,000. Natural and historical sites. Qixia Mountain is in Qixia District. Qixia Temple, a Southern Tang Buddhist temple, is there. During the Qing dynasty, the Qianlong Emperor praised it as the most elegant mountain in Jinling. A number of Liang dynasty tombs are in the district, primarily in and around the Ganjiaxiang section of the district.

Geographic entities mentioned:
surface_form: Qixia Mountain
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 32.16027778
lon: 118.96472222
Heggem. Heggem (or &quot;Osmarka&quot;) is a village in Gjemnes Municipality in Møre og Romsdal county, Norway. The village is located about south of the village of Torvikbukt and about west of the village of Angvika. The Osmarka Chapel is located here. The village has a good view of the mountain Reinsfjellet, located to the northeast.

Geographic entities mentioned:
surface_form: Reinsfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 62.929722222222
lon: 7.9263888888889
Mount Inabnit. Mount Inabnit () is in the Beartooth Mountains in the U.S. state of Montana. The peak is in the Absaroka-Beartooth Wilderness in Custer National Forest.

Geographic entities mentioned:
surface_form: mount inabnit
instance_of: Mountain
countries: United States
coordinates: lat: 45.12972222
lon: -109.63166667
Bishop Peak (California). Bishop Peak is a volcanic plug in San Luis Obispo, California. It is the tallest of the Morros or &quot;Nine Sisters&quot;, a chain of similar peaks stretching to Morro Bay. Often said to take its name from its resemblance to a bishop's miter, it is named in homage to the town's name (San Luis Obispo). &quot;Obispo&quot; is the Spanish word for Bishop. Geology.

Geographic entities mentioned:
surface_form: bishop peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.3025
lon: -120.697
&quot;Obispo&quot; is the Spanish word for Bishop. Geology. Like the other Morros, Bishop Peak is primarily composed of dacite. About 20 to 25 million years ago, magma welled up underneath a layer of softer rock and solidified. The softer overlying rock has since eroded away, leaving a distinct rugged shape. Wildlife.

Geographic entities mentioned:
surface_form: bishop peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.3025
lon: -120.697
The town is situated at the confluence of two local rivers, the Cuito and the Cuanavale, from which it derives its name. The Cuanavale feeds into the Cuito, which is a principal tributary of the Okavango River, and helps to maintain the ecology of the Okavango Delta. Cuito Cuanavale covers an area of around and its population as of 2014 was 40,829 inhabitants.

Geographic entities mentioned:
surface_form: Okavango Delta
instance_of: Body of water
Watercourse
countries: Botswana
coordinates: lat: -19.4
lon: 22.9
There are no natural lakes; the tailing pond near the slag heap and the Zauckerode retention basin were both constructed in the 20th century. Geologically, the Döhlen Basin is a Rotliegendes depression that was formed at the end of the Carboniferous period. It is located between the Elbe Valley zone and the Ore Mountain gneiss massif. Neighbouring municipalities.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Goetel Glacier. Goetel Glacier () is a glacier flowing south between Ullmann Spur and the Precious Peaks into Martel Inlet, Admiralty Bay, on King George Island in the South Shetland Islands. It was named by the Polish Antarctic Expedition, 1980, after Professor Walery Goetel (1889–1972), a Polish geologist and conservationist.

Geographic entities mentioned:
surface_form: Precious Peaks
instance_of: Mountain
coordinates: lat: -62.0667
lon: -58.3333
Geography. Tallinn is situated on the southern coast of the Gulf of Finland, in north-western Estonia. The largest lake in Tallinn is Lake Ülemiste (), which serves as the main source of the city's drinking water. Lake Harku is the second-largest lake within the borders of Tallinn and its area is.

Geographic entities mentioned:
surface_form: Lake Ülemiste
instance_of: Lake
countries: Estonia
coordinates: lat: 59.3993
lon: 24.7689
In other places of the city, hard sedimentary rock is only to be found beneath Quaternary sediments at depths reaching as much as 120 m below sea level. Underlying the sedimentary rock are the rocks of the Fennoscandian Craton including gneisses and other metamorphic rocks with volcanic rock protoliths and rapakivi granites.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
The success of the pier saw day-trippers come by train from all over southern Scotland to Portobello. Pleasure boat excursions to the Isle of May, Elie, North Berwick, and Bass Rock were also offered. However, the fact that the pier was open on a Sunday caused controversy.

Geographic entities mentioned:
surface_form: Bass Rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.08
lon: -2.64
He died in an accident in Bischofshofen's ski jumping hill while on a training jump in 1952. To honour his memory, the hill was renamed after the accident to &quot;Paul-Ausserleitner-Schanze&quot;. Ausserleitner holds the hill record in the K-50 hill in Gaisberg, Salzburg with 55 metres (achieved in 1949). The Gaisberg hill was later destroyed.

Geographic entities mentioned:
surface_form: Gaisberg
instance_of: Mountain
countries: Austria
coordinates: lat: 47.805082
lon: 13.112753
However, Cyclops reprimands Magneto for acting on his own authority. Despite Xavier being apologetic and appreciative for what he'd done, Magneto leaves Utopia for nearby Mount Tamalpais in Marin County.

Geographic entities mentioned:
surface_form: Mount Tamalpais
instance_of: Mountain
countries: United States
coordinates: lat: 37.9291
lon: -122.578
Swansea, Toronto. Swansea is a neighbourhood in the city of Toronto, Ontario, Canada, bounded on the west by the Humber River, on the north by Bloor Street, on the east by High Park and on the south by Lake Ontario. The neighbourhood was originally a separate municipality, the Village of Swansea, which became part of Metropolitan Toronto in 1953.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
History. The nearby mouth of the Humber River was the southern terminus of the route First Nations people used to travel from Lake Ontario to Lake Huron, and the other upper lakes. It is at this spot between 1615 and 1618 that it is believed that Étienne Brûlé was the first European to view Lake Ontario, with his party of indigenous and French explorers.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
This is symbolic in that it recognizes that First Nations members were the first people to inhabit Swansea, thousands of years ago. The hills in the Swansea Village seal represent Swansea's rolling countryside. The water in the Swansea seal refers to Swansea's natural boundaries, which include Lake Ontario, the Humber River and Grenadier Pond. Joining Metropolitan Toronto.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
It was not to be until 1970 that Danish archaeologist Karen Frifelt, preparing a &quot;Festschrift&quot; (a collection of articles brought together in celebration of a notable academic) for Glob’s sixtieth birthday, linked the pottery that Glob’s team took from the burials in the shadow of Jebel Hafit to the Sumerian Jemdet Nasr period (3100–2900 BCE).

Geographic entities mentioned:
surface_form: Jebel Hafit
instance_of: Mountain
countries: United Arab Emirates
Oman
coordinates: lat: 24.05796
lon: 55.78086
Hafit period. The Hafit period is marked by (and named for) the distinctive 'beehive' tombs first discovered around the area of Jebel Hafit in Al Ain. The period defines early Bronze Age human settlement in the United Arab Emirates and Oman in the period from 3,200 to 2,600 BC.

Geographic entities mentioned:
surface_form: Jebel Hafit
instance_of: Mountain
countries: United Arab Emirates
Oman
coordinates: lat: 24.05796
lon: 55.78086
Caribou-Targhee National Forest borders the parkway on the west and Bridger-Teton National Forest while the Teton Wilderness forms the eastern border. This stretch of land was originally part of Teton National Forest and was transferred to the National Park Service from the United States Forest Service to assure an unbroken connection between Grand Teton and Yellowstone National Parks.

Geographic entities mentioned:
surface_form: Grand Teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.7412
lon: -110.802