Sarmila/GeoWiki-Features huggingface dataset:
Indian Wells Valley. Indian Wells Valley is an arid north–south basin in east-central California. In the geologic sense, it is a southern extension of Owens Valley to the north, with the recent volcanics of the Coso Range being the separator. It is defined by a major fault on the west side of the valley.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
The valley is part of California's South Lahontan hydrologic region. Owens Peak, located west of the Indian Wells Valley, overlooks the basin from the west at 8,452 feet, making it the tallest peak in the southern Sierra Nevada range. Other mountain ranges surrounding the valley include the Argus Range in the east, the Coso Range in the north, and the El Paso Mountains in the south. Geography.

Geographic entities mentioned:
surface_form: Owens Peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.738261111111
lon: -117.99696944444
surface_form: indian wells valley
instance_of: Valley
countries: United States
coordinates: lat: 35.702777777778
lon: -117.68638888889
Indian Wells Valley is traversed by California State Route 14, California State Route 178, and US Highway 395. The valley varies in elevation from as low as 2,150 feet to as high as 2,400 feet. China Lake, a perennial lake and namesake for the Naval Air Weapons Station China Lake and unincorporated community China Lake, is located in the northeastern segment of the valley. Settlements.

Geographic entities mentioned:
surface_form: china lake
instance_of: Lake
countries: United States
coordinates: lat: 44.433
lon: -69.547
surface_form: china lake
instance_of: Lake
countries: United States
coordinates: lat: 44.433
lon: -69.547
surface_form: china lake
instance_of: Lake
countries: United States
coordinates: lat: 44.433
lon: -69.547
Settlements. The valley's largest and only incorporated community is Ridgecrest. Other unincorporated communities include Inyokern, Pearsonville, China Lake Acres, China Lake, Ridgecrest Heights, and Indian Wells. Indian Wells Valley contains the second largest population base in Kern County with a population of 34,837 (per 2010 census). Ecology.

Geographic entities mentioned:
surface_form: china lake
instance_of: Lake
countries: United States
coordinates: lat: 44.433
lon: -69.547
surface_form: china lake
instance_of: Lake
countries: United States
coordinates: lat: 44.433
lon: -69.547
In the geologic sense, it is a southern extension of Owens Valley to the north, with the recent volcanics of the Coso Range being the separator. It is defined by a major fault on the west side of the valley. Unlike Owens Valley, it is bound by a fault to the south, the Garlock Fault (within the El Paso Mountains). The valley is part of California's South Lahontan hydrologic region.

Geographic entities mentioned:
surface_form: owens valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
Indian Wells Valley. Indian Wells Valley is an arid north–south basin in east-central California. In the geologic sense, it is a southern extension of Owens Valley to the north, with the recent volcanics of the Coso Range being the separator. It is defined by a major fault on the west side of the valley.

Geographic entities mentioned:
surface_form: indian wells valley
instance_of: Valley
countries: United States
coordinates: lat: 35.702777777778
lon: -117.68638888889
Geography. The Indian Wells Valley is shared by three separate counties; Inyo County encompassing the north, Kern County making up the south-central and western part of the valley, and San Bernardino County making up the remaining eastern segment. It lies within the 760 and 442 area code zone.

Geographic entities mentioned:
surface_form: indian wells valley
instance_of: Valley
countries: United States
coordinates: lat: 35.702777777778
lon: -117.68638888889
It lies within the 760 and 442 area code zone. Indian Wells Valley is traversed by California State Route 14, California State Route 178, and US Highway 395. The valley varies in elevation from as low as 2,150 feet to as high as 2,400 feet.

Geographic entities mentioned:
surface_form: indian wells valley
instance_of: Valley
countries: United States
coordinates: lat: 35.702777777778
lon: -117.68638888889
Settlements. The valley's largest and only incorporated community is Ridgecrest. Other unincorporated communities include Inyokern, Pearsonville, China Lake Acres, China Lake, Ridgecrest Heights, and Indian Wells. Indian Wells Valley contains the second largest population base in Kern County with a population of 34,837 (per 2010 census). Ecology.

Geographic entities mentioned:
surface_form: indian wells valley
instance_of: Valley
countries: United States
coordinates: lat: 35.702777777778
lon: -117.68638888889
Indian Wells Valley contains the second largest population base in Kern County with a population of 34,837 (per 2010 census). Ecology. Indian Wells Valley is located in the northwesternmost part of the Mojave Desert plant community and ecoregion, receiving just 4-6 inches of precipitation a year.

Geographic entities mentioned:
surface_form: indian wells valley
instance_of: Valley
countries: United States
coordinates: lat: 35.702777777778
lon: -117.68638888889
Goodenough's service in Guatemala overlapped with the contentious 1982 presidential election, and Peace Corps volunteers were given the opportunity to leave the country prior to the election. After returning to Casper, he began working as a self-employed woodcutter and timber management specialist at Casper Mountain. Early campaigns.

Geographic entities mentioned:
surface_form: Casper Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.732944
lon: -106.324167
Alexios III died on March 20, 1390, and was succeeded by his son Manuel III. During his long reign, Alexios III had repaired the physical damage to the capital, gave rich endowments to several monasteries, especially Soumela Monastery, and founded the Dionysiou monastery at Mount Athos.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Springs and Upper Sana. The Sana in its upper course is fast mountain river with upland freshwater ecology, and its waters being very clear and cold. Gushing out of the karst plateau with Ovčara as most prominent summit (1576 m), between Klekovača and Vitorog mountains, and flows toward alluvial plains of the Bosanska Krajina with lowland freshwater ecology.

Geographic entities mentioned:
surface_form: Klekovača
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 44.4302
lon: 16.5087
surface_form: Vitorog
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 44.119444444444
lon: 17.044166666667
The Žemaitija National Park and the are within the area. The rivers that begin in the highlands include: Venta, Virvyčia, Minija, Babrungas, Kražantė, Akmena, Ančia. The lakes within the area include: Plateliai Lake,, Biržulis. Its highest, central part is the, which contains the highest point in the upland: the Medvėgalis hill (234.6 m).

Geographic entities mentioned:
surface_form: Plateliai Lake
instance_of: Lake
countries: Lithuania
coordinates: lat: 56.047222222222
lon: 21.873055555556
surface_form: Biržulis
instance_of: Lake
countries: Lithuania
coordinates: lat: 55.7576828
lon: 22.43121719
The rivers that begin in the highlands include: Venta, Virvyčia, Minija, Babrungas, Kražantė, Akmena, Ančia. The lakes within the area include: Plateliai Lake,, Biržulis. Its highest, central part is the, which contains the highest point in the upland: the Medvėgalis hill (234.6 m). Its eastern part is the East Samogitian Plateau, the western part is the West Samogitian Plateau.

Geographic entities mentioned:
surface_form: East Samogitian Plateau
instance_of: Plateau
countries: Lithuania
At this meeting the rules for admittance were laid down, the society was given its name, and executive positions were decided upon; Maxwell-Lyte was chosen as the society's first vice-president. It was on the initiative of the &quot;Société Ramond&quot; that the observatory on the Pic du Midi de Bigorre was built.

Geographic entities mentioned:
surface_form: Pic du Midi de Bigorre
instance_of: Mountain
countries: France
coordinates: lat: 42.937222222222
lon: 0.14111111111111
Scum Lake (British Columbia). Scum Lake is a lake in the Chilcotin region of the Interior of British Columbia, Canada. The major inflow, at the west, and outflow, at the northeast, is Haines Creek, which flows to the Chilcotin River near the settlement of Hanceville. The Chilcotin River flows via the Fraser River to the Pacific Ocean. Scum Lake Airport is at the northeastern tip of the lake.

Geographic entities mentioned:
surface_form: scum lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.3756
lon: -88.8292
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: scum lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.7858
lon: -123.603
Scum Lake (British Columbia). Scum Lake is a lake in the Chilcotin region of the Interior of British Columbia, Canada. The major inflow, at the west, and outflow, at the northeast, is Haines Creek, which flows to the Chilcotin River near the settlement of Hanceville. The Chilcotin River flows via the Fraser River to the Pacific Ocean. Scum Lake Airport is at the northeastern tip of the lake.

Geographic entities mentioned:
surface_form: scum lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.3756
lon: -88.8292
surface_form: scum lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.7858
lon: -123.603
The Tschingelhorn (3,555 m) is a mountain of the Bernese Alps, located on the border between the Swiss cantons of Bern and Valais. The summit of the Klein Tschingelhorn (3,494 m) on the west is the tripoint between the valleys of Kandertal, Lauterbrunnental (both in the Bernese Oberland) and Lötschental (in Valais). The main summit lies between the Lauterbrunnental and the Lötschental.

Geographic entities mentioned:
surface_form: Lötschental
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.416666666667
lon: 7.8333333333333
surface_form: tschingelhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.478694444444
lon: 7.8481944444444
The summit of the Klein Tschingelhorn (3,494 m) on the west is the tripoint between the valleys of Kandertal, Lauterbrunnental (both in the Bernese Oberland) and Lötschental (in Valais). The main summit lies between the Lauterbrunnental and the Lötschental. The first ascent was made by Heinrich Feuz, W. H. Hawker, and Ulrich and Christian Lauener on 6 September 1865. W. A. B.

Geographic entities mentioned:
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50486111
lon: 7.64305556
H. Hawker, and Ulrich and Christian Lauener on 6 September 1865. W. A. B. Coolidge's dog 'Tschingel' (d. 1879) – a gift to Coolidge from Swiss guide Christian Almer in 1868 – was named after the mountain; she made eleven first ascents in the Alps and completed 66 &quot;grandes courses&quot;, and was nominated but not accepted as an honorary member of the Alpine Club on account of her gender.

Geographic entities mentioned:
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50486111
lon: 7.64305556
Tschingelhorn. The Tschingelhorn (3,555 m) is a mountain of the Bernese Alps, located on the border between the Swiss cantons of Bern and Valais. The summit of the Klein Tschingelhorn (3,494 m) on the west is the tripoint between the valleys of Kandertal, Lauterbrunnental (both in the Bernese Oberland) and Lötschental (in Valais).

Geographic entities mentioned:
surface_form: tschingelhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.478694444444
lon: 7.8481944444444
Marshall was admitted to the New Hampshire Bar in 1852. Death. On the Fourth of July, 1874, Marshall, his wife and son were setting up a picnic lunch at Penacook Lake in West Concord when his wife heard the sound of bullets over their heads. Marshall saw no one firing, shouted to the shooters to be careful, then stood up and was shot in the abdomen. Marshall died at his home later that day.

Geographic entities mentioned:
surface_form: Penacook Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.231111111111
lon: -71.591388888889
Tzeachten First Nation. x3xhw3cq5az5oxp6o55pgjant1bb6" xml:space="preserve">The Tzeachten First Nation () is a band government of the people located in the Upper Fraser Valley region near Chilliwack, British Columbia, Canada. They are a member government of the tribal council. The traditional language of the Tzeachten is Halq’eméylem.

Geographic entities mentioned:
surface_form: Upper Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
Agua del Toro Dam. The Agua del Toro Dam is an arch dam on the Diamante River about west of San Rafael in Mendoza Province, Argentina. The primary purpose of the dam is hydroelectric power generation and it supports a power station located downstream. Construction on the dam began in 1966, and it was completed in 1973. The power station was started the same year and commissioned in 1982.

Geographic entities mentioned:
surface_form: Diamante River
instance_of: Watercourse
countries: Argentina
coordinates: lat: -34.511666666667
lon: -66.757777777778
Bahir Dar. Bahir Dar () is the capital city of Amhara Region, Ethiopia. Bahir Dar is one of the leading tourist destinations in Ethiopia, with a variety of attractions in the nearby Lake Tana and Blue Nile river. The city is known for its wide avenues lined with palm trees and a variety of colorful flowers.

Geographic entities mentioned:
surface_form: Lake Tana
instance_of: Lake
countries: Ethiopia
coordinates: lat: 12
lon: 37.25
Following the attack, the European Union proscribed the LTTE as a terrorist organisation. A new crisis leading to the first large-scale fighting since signing of the ceasefire occurred when the LTTE closed the sluice gates of the Mavil Oya (Mavil Aru) reservoir on 21 July 2006, and cut the water supply to 15,000 villages in government controlled areas.

Geographic entities mentioned:
surface_form: Mavil Aru
instance_of: Watercourse
countries: Sri Lanka
coordinates: lat: 8.257942
lon: 81.269985
On the eastern side are sand beaches and waters for swimming. Directions to Rock Lake: From the intersection of Route 30 and Route 28 in Indian Lake, follow Route 28 and 30 toward Blue Mountain Lake for 6.0 miles to the trail end at the right. Type of water in Rock Lake: Rock lake is a large body of water that consists of shallow areas and rapid areas as well.

Geographic entities mentioned:
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 42.2980198
lon: -71.8120781
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7
lon: -74.3167
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 45.81402
lon: -89.30162
surface_form: mountain lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1064
lon: -74.3697
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.083333333333
lon: -88.933333333333
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.95481
lon: -123.25907
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 46.427189
lon: -94.473618
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 41.4793
lon: -71.4684
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 41.9947
lon: -86.2042
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 44.114166666667
lon: -93.786666666667
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.328055555556
lon: -74.590833333333
surface_form: mountain lake
instance_of: Lake
countries: United States
coordinates: lat: 37.36
lon: -80.5339
surface_form: blue mountain lake
instance_of: Lake
countries: United States
coordinates: lat: 43.862222222222
lon: -74.457222222222
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 44.276111111111
lon: -95.935555555556
surface_form: mountain lake
instance_of: Lake
countries: United States
coordinates: lat: 41.9522405
lon: -74.983331
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5083
lon: -95.5028
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 45.170555555556
lon: -94.0125
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.8725
lon: -74.401111111111
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.5456079
lon: -90.4940088
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 45.988888888889
lon: -86.332222222222
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.8482
lon: -120.198
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.8158
lon: -114.186
surface_form: blue mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1469
lon: -74.8489
Rock Lake (Arietta, Hamilton County, New York). Rock Lake is located southeast of Clockmill Corners, New York. Fish species present in the lake are brown bullhead, chain pickerel, brook trout, and sunfish large mouth bass yellow perch northern pike. There is trail access off Powley-Piseco Road along the west shore. Overview of Rock Lake: Rock Lake is a widened portion of the Rock River.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.083333333333
lon: -88.933333333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 46.427189
lon: -94.473618
surface_form: rock lake (arietta, hamilton county, new york)
instance_of: Lake
countries: United States
coordinates: lat: 43.328055555556
lon: -74.590833333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 44.276111111111
lon: -95.935555555556
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 45.170555555556
lon: -94.0125
Rock Lake (Arietta, Hamilton County, New York). Rock Lake is located southeast of Clockmill Corners, New York. Fish species present in the lake are brown bullhead, chain pickerel, brook trout, and sunfish large mouth bass yellow perch northern pike. There is trail access off Powley-Piseco Road along the west shore. Overview of Rock Lake: Rock Lake is a widened portion of the Rock River.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.083333333333
lon: -88.933333333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 46.427189
lon: -94.473618
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.328055555556
lon: -74.590833333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 44.276111111111
lon: -95.935555555556
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 45.170555555556
lon: -94.0125
Fish species present in the lake are brown bullhead, chain pickerel, brook trout, and sunfish large mouth bass yellow perch northern pike. There is trail access off Powley-Piseco Road along the west shore. Overview of Rock Lake: Rock Lake is a widened portion of the Rock River. Rock River can be dangerous however, with shallow waters and many rapids.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.083333333333
lon: -88.933333333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.083333333333
lon: -88.933333333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 46.427189
lon: -94.473618
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 46.427189
lon: -94.473618
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.328055555556
lon: -74.590833333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.328055555556
lon: -74.590833333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 44.276111111111
lon: -95.935555555556
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 44.276111111111
lon: -95.935555555556
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 45.170555555556
lon: -94.0125
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 45.170555555556
lon: -94.0125
Directions to Rock Lake: From the intersection of Route 30 and Route 28 in Indian Lake, follow Route 28 and 30 toward Blue Mountain Lake for 6.0 miles to the trail end at the right. Type of water in Rock Lake: Rock lake is a large body of water that consists of shallow areas and rapid areas as well. It is not well-sheltered, but it remains calm year round.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.083333333333
lon: -88.933333333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.083333333333
lon: -88.933333333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 46.427189
lon: -94.473618
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 46.427189
lon: -94.473618
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.328055555556
lon: -74.590833333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.328055555556
lon: -74.590833333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 44.276111111111
lon: -95.935555555556
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 44.276111111111
lon: -95.935555555556
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 45.170555555556
lon: -94.0125
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 45.170555555556
lon: -94.0125
Type of water in Rock Lake: Rock lake is a large body of water that consists of shallow areas and rapid areas as well. It is not well-sheltered, but it remains calm year round. Type of carry in Rock Lake: 0.85 mile carry over rough waters and a narrow trail. Would be best for a light weight canoe or kayak that can be carried.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.083333333333
lon: -88.933333333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 46.427189
lon: -94.473618
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.328055555556
lon: -74.590833333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 44.276111111111
lon: -95.935555555556
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 45.170555555556
lon: -94.0125
Type of carry in Rock Lake: 0.85 mile carry over rough waters and a narrow trail. Would be best for a light weight canoe or kayak that can be carried. Rock Lake Trail Overview: This is a short trail that is regularly utilized by fishermen and those ready to make the short side trip to paddle a separated lake. The shoreline has birding openings.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.083333333333
lon: -88.933333333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 46.427189
lon: -94.473618
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.328055555556
lon: -74.590833333333
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 44.276111111111
lon: -95.935555555556
surface_form: rock lake
instance_of: Lake
countries: United States
coordinates: lat: 45.170555555556
lon: -94.0125
It constitutes the largest continuous wilderness area within the Sonoran Desert. The eastern portion of the area contains the volcanic Pinacate Peaks region; together with the western portion, the area forms the El Pinacate y Gran Desierto de Altar Biosphere Reserve and a UNESCO World Heritage Site. Geography. The Gran Desierto covers approximately, most of it in the Mexican state of Sonora.

Geographic entities mentioned:
surface_form: Pinacate Peaks
instance_of: Mountain
countries: Mexico
coordinates: lat: 31.77
lon: -113.49
The southernmost extension of the San Andreas Fault cuts across the area and lies beneath several prominent granite inselbergs, most notably the Sierra del Rosario mountains, which are surrounded by the erg on all sides. The Sierra Enterrada is a smaller inselberg almost completely buried by the sand near the boundary of the Gran Desierto and the Pinacate volcanic complex. Sand dune distribution.

Geographic entities mentioned:
surface_form: Pinacate volcanic complex
instance_of: Mountain
countries: Mexico
coordinates: lat: 31.77
lon: -113.49
Beiar Valley. The Beiar Valley () is a valley in Beiarn Municipality in Nordland, Norway. It is about long. Most of the residents of the municipality of Beiarn live in this valley. The highest parts of the southern end of the valley are located within Saltfjellet–Svartisen National Park. The Beiar River flows through the valley before emptying into the Beiar Fjord at the north end of the valley.

Geographic entities mentioned:
surface_form: beiar valley
instance_of: Valley
countries: Norway
coordinates: lat: 66.7313
lon: 14.523
He joined the law practice of John Hillyard Cameron in Toronto as a partner. In 1841, in the first general election for the new Legislative Assembly of the Province of Canada, Strachan stood for election to the riding of Huron, located in Huron County on Lake Huron, even though he lived and worked in Toronto, located on Lake Ontario.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Stories exist about Jīvaka's purported travels to Thailand. In the Sanskrit textual traditions, Jīvaka is the ninth of the Sixteen Arhats, disciples that are entrusted to protect the Buddha's teaching until the arising of the next Buddha. He is therefore described in Buddhist texts as still being alive on a mountain peak called Gandhamādana, between India and Sri Lanka.

Geographic entities mentioned:
surface_form: Gandhamādana
instance_of: Mountain
countries: Sri Lanka
The Ellsworth Mountains are located within West Antarctica at 79°S, 85°W. In general, it is made up of mostly rugged and angular peaks such as the Vinson Massif (), the highest mountain in Antarctica. The early Cambrian, when carbonate deposits were deposited in shallow marine conditions, is when the geologic history record across the Ellsworth Mountains began.

Geographic entities mentioned:
surface_form: Vinson Massif
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
Heritage Group. Union Glacier Formation, Hyde Glacier Formation, Drake Ice Fall Formation at southern Soholt Peaks, Conglomerate Ridge Formation, Library Hills Formation, Springer Peak Formation, Frazier Ridge Formation, and Minaret Formation are the eight clastic sedimentary and volcanic rock formations that make up the Heritage Group. The Heritage Group as a whole is around thick.

Geographic entities mentioned:
surface_form: Soholt Peaks
instance_of: Mountain
coordinates: lat: -79.7167
lon: -84.2
surface_form: Springer Peak
instance_of: Mountain
coordinates: lat: -79.4
lon: -84.883333333333
Drake Icefall Formation at southern Soholt Peaks. The lower Middle Cambrian black shales and interlayered limestone carbonates of the Drake Icefall Formation are found in southern Soholt Peaks. The rocks in this formation provide an evidence that sedimentation occurred in a shallow-marine and euxinic environment where with anoxic and sulfidic conditions.

Geographic entities mentioned:
surface_form: Soholt Peaks
instance_of: Mountain
coordinates: lat: -79.7167
lon: -84.2
Type of contacts - Transitional beds. All places have conformable transitional beds of 20–60 metres, with the exception of Pojeta Peak, Soholt Peak, and Enterprise Hills. The transitional deposits are a narrow sequence of interbedded sandstone and siltstone from the Upper Cambrian period called argillite. It includes material from the inner to outer shelf and from shallow to deep environments.

Geographic entities mentioned:
surface_form: Pojeta Peak
instance_of: Mountain
coordinates: lat: -79.466666666667
lon: -84.683333333333
surface_form: Soholt Peak
instance_of: Mountain
coordinates: lat: -79.7167
lon: -84.2
surface_form: Enterprise Hills
instance_of: Mountain
coordinates: lat: -79.9167
lon: -82
After the Minaret Formation emerged, a dramatic rise in the relative sea level caused it to develop. Between the Springer Peak Formation and the Mount Twiss Member, which is a part of the Crashsite Group, there is an angular unconformity in the Pojeta Peak. Pojeta Peak's localised angular unconformity may have developed as a result of block tilting in regions of intrabasinal uplift.

Geographic entities mentioned:
surface_form: Springer Peak
instance_of: Mountain
coordinates: lat: -79.4
lon: -84.883333333333
surface_form: Mount Twiss
instance_of: Mountain
coordinates: lat: -79.3833
lon: -85.6
Pojeta Peak's localised angular unconformity may have developed as a result of block tilting in regions of intrabasinal uplift. There are concordant erosional unconformities between the Minaret Formation and the base Crashsite Group at the Soholt Peaks and Mount Dolence.

Geographic entities mentioned:
surface_form: Mount Dolence
instance_of: Mountain
coordinates: lat: -79.85
lon: -83.2
The Uppermost Cambrian to Devonian Crashsite Group. The Crashsite Group has six distinct rock types with a combined thickness of 3000 metres. It includes the Howard Nunataks Formation, the Mount Wyatt Earp Formation, the Linder Peak Member, the Mount Twiss Member, the Landmark Peak Member, and the Mount Liptak Formation. The transitional beds are primarily covered by quartzite.

Geographic entities mentioned:
surface_form: Mount Wyatt
instance_of: Mountain
coordinates: lat: -86.76167
lon: -154.025
surface_form: Linder Peak
instance_of: Mountain
coordinates: lat: -79.8667
lon: -83.2
surface_form: Mount Twiss
instance_of: Mountain
coordinates: lat: -79.3833
lon: -85.6
surface_form: Landmark Peak
instance_of: Mountain
coordinates: lat: -79.1667
lon: -85.6667
surface_form: Mount Liptak
instance_of: Mountain
coordinates: lat: -78.75
lon: -84.9
These have been shown to be closely related to the rift-related basaltic volcanic and subvolcanic rocks' extrusion and intrusion. A location with consistently sinking sedimentary strata in the Liberty Hills Formation is the High Nunatak, Horseshoe Valley.

Geographic entities mentioned:
surface_form: High Nunatak
instance_of: Mountain
coordinates: lat: -80.052777777778
lon: -82.618888888889
A sample's time-temperature route may be inferred from the relative proportions of long and short tracks that are created. The samples from the Crashsite Group that were gathered near Bowers Corner and on the western flank of the Vinson Massif have apatite ages dated on them. The age increases with elevation and is defined by a slope of around 200 metres per million years.

Geographic entities mentioned:
surface_form: Bowers Corner
instance_of: Mountain
coordinates: lat: -79.0167
lon: -84.35
surface_form: Vinson Massif
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
The only evidence is that the rocks of the Ellsworth Mountains were created in a Cambrian extensional rift environment. Geochronological information on the early Paleozoic history of the Cape fold belt shows that southern South Africa was likely that located in a continental rift basin during the Middle to Late Cambrian period.

Geographic entities mentioned:
surface_form: Cape fold belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
Southern african sector of the Paleo-Pacific margin. End-Neoproterozoic to Paleozoic rocks that were a part of the southern African sector of the paleo-Pacific margin of Gondwana have been exposed by the Cape fold belt in South Africa.

Geographic entities mentioned:
surface_form: Cape fold belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
A Middle to Late Cambrian paleogeographic reconstruction is made using a commonly accepted reconstruction of Gondwana, which places the crustal block of the Ellsworth-Whitmore Mountains oceanward of the Cape fold belt. The two zones that make up a basin are discovered to be congruent with the reconstruction.

Geographic entities mentioned:
surface_form: Cape fold belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
The succession was located closer to the rift axis. Geochronological and geobarometric studies in the western Cape fold belt suggest that the Saldanian belt may have undergone uplift and erosion prior to the Middle Cambrian rifting event that happened as fast as the rate of crustal thickening in the present.

Geographic entities mentioned:
surface_form: Cape fold belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
The Heritage Group's Middle Cambrian sedimentary strata include Early Cambrian granite clasts. It suggests that the Ellsworth Mountains Cambrian basin's origin area had a quick uplift and erosion. The geology of the Ellsworth Mountains and the Middle Cambrian to Permian are related, as shown by the tectonostratigraphic history of the Cape fold belt.

Geographic entities mentioned:
surface_form: Cape fold belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
Meanwhile, the height measured by handheld GPS shows it is with 3m accuracy. There is a debate over the highest point of Bangladesh, and some sources indicate Saka Haphong as the most elevated peak of the country. However, Tazing Dong is officially recognized as the highest point of Bangladesh. Keokradong is a popular tourist attraction in Bangladesh for mountaineers.

Geographic entities mentioned:
surface_form: Saka Haphong
instance_of: Mountain
countries: Bangladesh
Myanmar
coordinates: lat: 21.78657
lon: 92.60968
Meanwhile, the height measured by handheld GPS shows it is with 3m accuracy. There is a debate over the highest point of Bangladesh, and some sources indicate Saka Haphong as the most elevated peak of the country. However, Tazing Dong is officially recognized as the highest point of Bangladesh. Keokradong is a popular tourist attraction in Bangladesh for mountaineers.

Geographic entities mentioned:
surface_form: Tazing Dong
instance_of: Mountain
countries: Bangladesh
coordinates: lat: 21.81646
lon: 92.53066
Keokradong. Keokradong () is a peak located in Bandarban, Bangladesh, with an elevation of. Some sources claim it as the highest point of Bangladesh. On the top of Keokradong there is a small shelter and a signboard put up by Bangladesh Army proclaiming the elevation to be. Meanwhile, the height measured by handheld GPS shows it is with 3m accuracy.

Geographic entities mentioned:
surface_form: keokradong
instance_of: Mountain
countries: Bangladesh
coordinates: lat: 21.94993
lon: 92.51441
There is a debate over the highest point of Bangladesh, and some sources indicate Saka Haphong as the most elevated peak of the country. However, Tazing Dong is officially recognized as the highest point of Bangladesh. Keokradong is a popular tourist attraction in Bangladesh for mountaineers. Keokradong is one of the cloudiest places in Bangladesh.

Geographic entities mentioned:
surface_form: keokradong
instance_of: Mountain
countries: Bangladesh
coordinates: lat: 21.94993
lon: 92.51441
Geography. North of the city is the Bamenda Ring Road, a circular route through Cameroon Highlands. Along this road is Mount Oku, the Kimbi River Game Reserve, the Menchum River waterfalls, a huge Fon's palace at Bafut, and a pyramidal thatched shrine at Akum (also known as Bagangu). Climate.

Geographic entities mentioned:
surface_form: Mount Oku
instance_of: Mountain
countries: Cameroon
coordinates: lat: 6.1997222222222
lon: 10.518888888889
surface_form: Menchum River
instance_of: Watercourse
countries: Cameroon
coordinates: lat: 6.264793
lon: 10.039787
In 1885, the &quot;New York Times&quot; wrote about plans for connecting the Russian Transcaspian Railway, then under construction, with British India via Sarakhs, Herat, and Kandahar. When completed, the project would allow British officers to travel from London to British India, mostly by rail, in 11 to 12 days (crossing the English Channel, the Black Sea, and the Caspian Sea by boat).

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Mavoor Road. Mavoor Road is the busiest High street of Kozhikode city in Kerala, India. This road connects the Mananchira pond area with the Kozhikode Medical College. After the medical college, the road is extended further to the little village of Mavoor but the term 'Mavoor Road' refers to the section between the city and the Medical college. History.

Geographic entities mentioned:
surface_form: Mananchira
instance_of: Lake
countries: India
coordinates: lat: 11.254416666667
lon: 75.779972222222
History. 100 years ago the beach area was the centre of Kozhikode city. In the 1970s the downtown shifted to Mananchira area and again, in the 1980s, Mavoor Road became the centre of attraction. In 2010s, Thondayad Bypass area and Palazhi on the Airport road has emerged as the new city centre with a vibrant night life. Jaffer Khan Colony.

Geographic entities mentioned:
surface_form: Mananchira
instance_of: Lake
countries: India
coordinates: lat: 11.254416666667
lon: 75.779972222222
Ganwolsan. Ganwolsan () is a mountain in Ulsan, South Korea. It has an elevation of. It is part of the Yeongnam Alps mountain range.

Geographic entities mentioned:
surface_form: ganwolsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.551
lon: 129.041
The rest of the state reported widespread rains of. Rainfall in Alabama peaked at in some areas, and similar amounts were observed in Georgia. In Florida, rainfall peaked at in an extremely southern part of the Panhandle. Precipitation was also recorded in Lake Okeechobee, with reported there. The northeastern section of the state reported of rain. No rain was reported in the Florida Keys.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
Conversely, the Soviets could not widen it through further offensives which ended on 1 April. Fighting broke out near III./JG 54's base on Lake Ilmen in February when the Soviets began to eliminate German forces from the Demyansk pocket. The decision was made to replace III./JG 54 with I./JG 26 first. The intended swap of the wings never took place. While I.

Geographic entities mentioned:
surface_form: Lake Ilmen
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 58.266666666667
lon: 31.283333333333
Tête de Ran. The Tête de Ran (1,422 m) is a mountain of the Jura, located south-west of the Vue des Alpes in the canton of Neuchâtel. The summit is easily accessible with a road culminating at 1,329 metres. Several surface ski-lifts are located on the southern slopes, but are no longer in operation as of 2021.

Geographic entities mentioned:
surface_form: tête de ran
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.05416667
lon: 6.85333333
Two of his statues are now in Berlin and a stela belonging to him is in Hildesheim. An ostrakon mentions work on his tomb and that of Isetnofret; it implies he was buried in the area of the Valley of the Queens, though it is also possible he was buried in KV5, the tomb built for the sons of Ramesses, since a fragment of one of his canopic jars was found there. Inscriptions.

Geographic entities mentioned:
surface_form: Valley of the Queens
instance_of: Valley
countries: Egypt
coordinates: lat: 25.7275
lon: 32.593055555556
Newar traditional clothing. Traditional Newar clothing () refers to the everyday clothes worn by the Newar people of Nepal who are indigenous to the Kathmandu Valley and surrounding regions. The garments are associated with the old aristocracy, merchants, farmers, craftsmen and professionals. Most of the clothes are made of homespun. Weaving was a major industry in the Kathmandu Valley.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
Montjuïc Cemetery. Montjuïc Cemetery, known in Catalan as Cementiri del Sud-oest or Cementiri de Montjuïc, is located on one of the rocky slopes of Montjuïc hill in Barcelona. History. It was opened on 17 March 1883 by the city of Barcelona as its main cemetery, supplanting the older cemetery at Poblenou in the east.

Geographic entities mentioned:
surface_form: Montjuïc
instance_of: Mountain
countries: Spain
coordinates: lat: 41.364166666667
lon: 2.1580555555556
Sjoa. Sjoa is a river in Innlandet county, Norway. The long river runs through Vågå Municipality and Sel Municipality and it provides the outlet from lake Gjende at Gjendesheim in the Jotunheimen mountains of Norway's Jotunheim National Park. The river flows eastward through the Sjodalen valley and Heidal valley into the Gudbrandsdalslågen river at the village of Sjoa.

Geographic entities mentioned:
surface_form: Gjende
instance_of: Lake
countries: Norway
coordinates: lat: 61.489444444444
lon: 8.68
Sjoa. Sjoa is a river in Innlandet county, Norway. The long river runs through Vågå Municipality and Sel Municipality and it provides the outlet from lake Gjende at Gjendesheim in the Jotunheimen mountains of Norway's Jotunheim National Park. The river flows eastward through the Sjodalen valley and Heidal valley into the Gudbrandsdalslågen river at the village of Sjoa.

Geographic entities mentioned:
surface_form: Sjodalen
instance_of: Valley
countries: Norway
surface_form: Heidal
instance_of: Valley
countries: Norway
coordinates: lat: 61.71789
lon: 9.4512
Feast of the Transfiguration. The Feast of the Transfiguration is celebrated by various Christian communities in honor of the transfiguration of Jesus. The origins of the feast are less than certain and may have derived from the dedication of three basilicas on Mount Tabor.

Geographic entities mentioned:
surface_form: Mount Tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
Blazing Swan. Blazing Swan is an annual regional Burning Man event held adjacent to Jilakin Lake near the town of Kulin, Western Australia. It is promoted as an experiment in temporary community and artistic expression, guided by eleven main principles, including &quot;radical inclusion&quot;, &quot;gifting&quot; and &quot;radical self-reliance&quot;.

Geographic entities mentioned:
surface_form: Jilakin Lake
instance_of: Lake
countries: Australia
coordinates: lat: -32.663888888889
lon: 118.35583333333
It is also known as Sagamie in French, from the first part of &quot;Saguenay&quot; and the last part of &quot;Piekouagami&quot;, the Innu name (meaning &quot;flat lake&quot;) for Lac Saint-Jean, with the final &quot;e&quot; added to follow the model of other existing region names such as Mauricie, Témiscamie, Jamésie, and Matawinie.

Geographic entities mentioned:
surface_form: Lac Saint-Jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
It is also irrigated by several other large watercourses. Bordered by forests and mountainous massifs, the southern portion of the region constitutes a fertile enclave in the Canadian Shield called the Saguenay Graben. Both the scenery and the cultural sites and activities of Saguenay–Lac-Saint-Jean attract tourists every year.

Geographic entities mentioned:
surface_form: Saguenay Graben
instance_of: Valley
countries: Canada
coordinates: lat: 48.5
lon: -71.3333
A-thút. A-thút or A-thoot is a river in Myanmar, in the Pathein District. It is born on Kyunlaha Lake and runs southwest on flat lands until it empties into the river Kyun-kabo not far from Paya-thun-zu. It is navigable about 25 km in rainy season.

Geographic entities mentioned:
surface_form: a-thút
instance_of: Watercourse
countries: Myanmar
coordinates: lat: 16.75
lon: 94.5
A-thút. A-thút or A-thoot is a river in Myanmar, in the Pathein District. It is born on Kyunlaha Lake and runs southwest on flat lands until it empties into the river Kyun-kabo not far from Paya-thun-zu. It is navigable about 25 km in rainy season.

Geographic entities mentioned:
surface_form: a-thút
instance_of: Watercourse
countries: Myanmar
coordinates: lat: 16.75
lon: 94.5
surface_form: a-thoot
instance_of: Watercourse
countries: Myanmar
coordinates: lat: 16.75
lon: 94.5
It often flooded and formed extensive marshes. Its devastating fury in December 1935 remains fresh in memory of the elder inhabitants of the region (Veria and Alexandreia). The Haliacmon rises in the Gramos mountains of Western Macedonia, near the international border with Albania. In its upper course it flows generally towards the east, and turns southeast near Kastoria.

Geographic entities mentioned:
surface_form: Gramos
instance_of: Mountain
countries: Greece
Albania
coordinates: lat: 40.333333333333
lon: 20.75
In its upper course it flows generally towards the east, and turns southeast near Kastoria. It describes a wide curve around the Vourinos mountains, and turns northeast near the village Paliouria. It feeds the large artificial lake Polyfyto, that was created after the construction of the namesake hydroelectric dam and consists almost its entire course through the Kozani prefecture.

Geographic entities mentioned:
surface_form: Vourinos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.175833333333
lon: 21.6725
Among her first recognised competitions was the Ontario under-10s 1-metre diving championships, where at the age of 8 she scored 84.20 points and won in her age group. At the age of 9, she practised platform diving at the open-air pool in Summerville, occasionally being blown by wind from the tower due to its location near the edge of Lake Ontario.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Orenco later became part of Hillsboro. The company was responsible for introducing the Orenco Apple, a dessert apple, in the early 20th century. Geography. Orenco is located in the Tualatin Valley, with Rock Creek and other smaller streams running through the area. Major roads in the area include U.S. Route 26, Cornelius Pass Road, Cornell Road, NW 231st Avenue, and Baseline Road.

Geographic entities mentioned:
surface_form: Tualatin Valley
instance_of: Valley
countries: United States
coordinates: lat: 45.5106
lon: -122.989
New bus services were also planned to connect additional settlements to the station. Cycling. The proposed site is within 50 metres of the Erewash Valley trail, which connects towns and villages within the Erewash Valley. It is 500 metres from route 6 of the Derby-Nottingham section of the National Cycle Network. Rail.

Geographic entities mentioned:
surface_form: Erewash Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.0045
lon: -1.3131