Sarmila/GeoWiki-Features huggingface dataset:
Depths in the center range from less than in a dry summer to nearly in a wet winter. Tides do not have a significant effect on the circulation of water in Rodeo Lagoon. Instead, the circulation of water in Rodeo Lagoon is driven almost entirely by the wind.

Geographic entities mentioned:
surface_form: rodeo lagoon
instance_of: Lake
countries: United States
coordinates: lat: 37.8308
lon: -122.531
Tides do not have a significant effect on the circulation of water in Rodeo Lagoon. Instead, the circulation of water in Rodeo Lagoon is driven almost entirely by the wind. Since the Marin Headlands are often quite windy, it is not unusual to see Langmuir circulation form windrows of foam on the surface of the lagoon.

Geographic entities mentioned:
surface_form: rodeo lagoon
instance_of: Lake
countries: United States
coordinates: lat: 37.8308
lon: -122.531
Instead, the circulation of water in Rodeo Lagoon is driven almost entirely by the wind. Since the Marin Headlands are often quite windy, it is not unusual to see Langmuir circulation form windrows of foam on the surface of the lagoon. Rodeo Lagoon is a brackish water body, with salinities in most of the lagoon ranging from 2 to 10 practical salinity units (psu) over the course of the year.

Geographic entities mentioned:
surface_form: rodeo lagoon
instance_of: Lake
countries: United States
coordinates: lat: 37.8308
lon: -122.531
The bowl-shaped bathymetry of the lagoon traps this dense, salty water and prevents it from quickly draining back out in the ocean. Wildlife. Rodeo Lagoon provides habitat to a protected species, the tidewater goby. It also provides habitat to many species of migrating waterfowl. Resident fish include the threespine stickleback and prickly sculpin in addition to the tidewater goby.

Geographic entities mentioned:
surface_form: rodeo lagoon
instance_of: Lake
countries: United States
coordinates: lat: 37.8308
lon: -122.531
Near the base, it crashes onto a rock ledge and fans out towards the left bank, before dropping again vertically onto a pile of talus and cascading downwards. It is located in a steep canyon on the southwest face of Mount Rainier. Pearl Creek drains to another glacial stream, Pyramid Creek, which parallels then flows into Kautz Creek and finally into the Nisqually River.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Balkan Mountains (Turkmenistan). Balkhan Ranges or Balkan Ranges, also Balkhans, Balkans (, Balkan Mountains) are mountains by the eastern shores of the Caspian Sea in the Balkan Region of Turkmenistan. They consist of the Greater Balkan, or Uly Balkan and the Lesser Balkan. They are separated by Uzboy, a dried-out distributary of the Amu Darya.

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
Abdil Bey is regarded as the progenitor of the Kırahmetler tribe, and some studies suggest a connection between him and the Karamanoglu feudal lords. Abdil Bey migrated from the Horasan region to the vicinity of Erzurum. After residing there for some time, the tribe later settled in the Çukurova-Taşeli Region. Over time, they migrated from this area to Anamur and eventually to the Gazipaşa region.

Geographic entities mentioned:
surface_form: Taşeli
instance_of: Plateau
countries: Turkey
coordinates: lat: 36.49607
lon: 32.62693
History. Minerul Uricani was founded in the summer of 1957, backed by the Uricani Coal Mine and representing the local mining community, one of six in the Jiu Valley, which had been operational since 1947. The team competed for several decades in the Hunedoara regional and county championships.

Geographic entities mentioned:
surface_form: Jiu Valley
instance_of: Valley
countries: Romania
coordinates: lat: 43.77805556
lon: 23.81333333
Death. Ivins died in Salt Lake City of a coronary occlusion. He was buried at Salt Lake City Cemetery. Honors. The small city of Ivins, Utah, is named after him. Ivins Mountain, located in Zion National Park, was named after him in 1935. In 1958, he was inducted into the Hall of Great Westerners of the National Cowboy & Western Heritage Museum for his contributions to the cattle industry.

Geographic entities mentioned:
surface_form: Ivins Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.28748
lon: -113.00633
Sankuyo. Sankuyo is a small village in North-West District of Botswana. It is located close to Okavango Delta, and it has a primary school. The population of the village was 372 in 2001 census. It is also the name of an organisation that runs several lodges in the okavango-delta. One of these lodges is Santawani.

Geographic entities mentioned:
surface_form: Okavango Delta
instance_of: Body of water
Watercourse
countries: Botswana
coordinates: lat: -19.4
lon: 22.9
After traversing a few blocks in Mill Valley's downtown, runners climb 688 stairs (now 700 stairs, after the renovation of the middle section in Nov 2017) leading up the side of Mount Tamalpais, and then pass through Muir Woods National Monument, Mount Tamalpais State Park, and the Golden Gate National Recreation Area.

Geographic entities mentioned:
surface_form: Mount Tamalpais
instance_of: Mountain
countries: United States
coordinates: lat: 37.9291
lon: -122.578
Yes Tor. Yes Tor is the second highest point on Dartmoor, Devon, South West England, at above sea level. It is one of only two wholly English peaks south of the Peak District National Park—the other being nearby High Willhays—that are above. The name means &quot;eagle's tor&quot;, from Old English &quot;earnes torr&quot;.

Geographic entities mentioned:
surface_form: High Willhays
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 50.685174
lon: -4.0111985
The name means &quot;eagle's tor&quot;, from Old English &quot;earnes torr&quot;. It lies within a British Army firing range and safe access is only possible on days or nights when firing is not taking place, as per the current Dartmoor Firing Notice. Yes Tor is lower than the nearby High Willhays.

Geographic entities mentioned:
surface_form: High Willhays
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 50.685174
lon: -4.0111985
Ariq Böke (after 1219–1266), the components of his name also spelled Arigh, Arik and Bukha, Buka (,;), was the seventh and youngest son of Tolui and a grandson of Genghis Khan. After the death of his brother the Great Khan Möngke, Ariq Böke claimed the title of the Great Khan of the Mongol Empire and briefly took power while his brothers Kublai and Hulagu were absent from the Mongolian Plateau.

Geographic entities mentioned:
surface_form: Mongolian Plateau
instance_of: Plateau
countries: Mongolia
People's Republic of China
Russia
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 107
Chumbi. Chumbi (;) is a historic village in the Chumbi Valley or the Yadong County of the Tibet Autonomous Region of China. It is in the valley of the Amo Chu River, where the route from Sikkim's Cho La Pass meets the Amo Chu Valley. The &quot;Chumbi Valley&quot; of the European nomenclature derives its name from the village of Chumbi.

Geographic entities mentioned:
surface_form: Chumbi Valley
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 27.4893046
lon: 88.9050579
Sunnyside, Toronto. Sunnyside is a lakefront district in Toronto, Ontario, Canada. It includes a beach and park area along Lake Ontario's Humber Bay, from west of Exhibition Place to the mouth of the Humber River. The area has several recreation uses, including rowing clubs, sports clubs, picnic areas, playgrounds, a nightclub, a bathing pavilion and public pool.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
In 1615, it is believed that French explorer Étienne Brûlé was the first European to visit the area. His party first passed through Teiaiagon, an Iroquoian village situated at the site of modern-day Baby Point. Teiaigon was located along the Toronto Carrying-Place Trail, a portage route that extended from approximately the area of today's Sunnyside Pavilion north to the Lake Simcoe area.

Geographic entities mentioned:
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
Mount Aopinie. f6xq8m4xzswehxl63bw6qmt2z2jg5" xml:space="preserve">Mount Aopinie () is a mountain of central New Caledonia, with an elevation of. The source of the Poya River lies to the southwest. The landscape is dominated by dense forest.

Geographic entities mentioned:
surface_form: mount aopinie
instance_of: Mountain
countries: France
coordinates: lat: -21.17888889
lon: 165.26666667
Sebiș. Sebiș () is a town in Arad County, western Transylvania, Romania. Situated from the county capital, Sebiș is one of the most important urban centres in the Crișul Alb valley. It administers three villages: Donceni (&quot;Dancsfalva&quot;), Prunișor (&quot;Kertes&quot;), and Sălăjeni (&quot;Szelezsény&quot;). Geography.

Geographic entities mentioned:
surface_form: Crișul Alb
instance_of: Watercourse
countries: Romania
Hungary
coordinates: lat: 46.700277777778
lon: 21.269166666667
It administers three villages: Donceni (&quot;Dancsfalva&quot;), Prunișor (&quot;Kertes&quot;), and Sălăjeni (&quot;Szelezsény&quot;). Geography. The town lies on the banks of the river Sebiș and its tributaries, the Laz and the Minezel. Its territory occupies in the greater Sebiș Basin, which is a sub-unit of the Crișul Alb Basin. Demographics. At the 2021 census, Sebiș had a population of 5,410.

Geographic entities mentioned:
surface_form: Crișul Alb Basin
instance_of: Watercourse
countries: Romania
Hungary
coordinates: lat: 46.700277777778
lon: 21.269166666667
Another theory is that Antofalla is derived from the Diaguita language. Geography and structure. Antofalla lies in the Antofagasta de la Sierra department of the northern Catamarca Province, in northwestern Argentina. The towns of Antofalla, Puesto Cuevas, Botijuela and Potrero Grande are east, southeast, south and southwest of the volcano, respectively.

Geographic entities mentioned:
surface_form: Antofagasta de la Sierra
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.968055555556
lon: -67.535833333333
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
The volcanoes of the Central Volcanic Zone lie at high altitudes, and the volcanic zone spans the countries of Argentina, Bolivia, Chile and Peru. Present-day activity in the Central Volcanic Zone occurs at Lascar and Lastarria, and about 44 centres have been active in the Holocene.

Geographic entities mentioned:
surface_form: Lastarria
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -25.166666666667
lon: -68.5
Antofalla is a cluster of stratovolcanoes, with the high Antofalla volcano at its centre. An altar with a stone pyramid lies on its summit, and the mountains Llullaillaco, Pajonales and Pular can be seen from the top of the mountain. These volcanic centres overlap with each other, are all much smaller than the main Antofalla volcano and have experienced little erosion.

Geographic entities mentioned:
surface_form: Llullaillaco
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.719863
lon: -68.536852
Antofalla together with neighbouring Cerro Archibarca, Cerro Beltrán and Tebenquicho is part of a group of long lived volcanic complexes that developed in the Argentine Puna; the first and the last of these lie due north and northeast of Antofalla, respectively.

Geographic entities mentioned:
surface_form: Cerro Archibarca
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.2373
lon: -67.8653
surface_form: Tebenquicho
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.33333
lon: -67.68333
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
All of them appear to be associated with a lineament known as the Archibarca lineament, which crosses the Andes in northwest–southeast direction, and which additionally includes the Escondida ore occurrence and the volcanoes Llullaillaco, Corrida de Cori and Galán. This lineament may be an area where the crust is unusually weak.

Geographic entities mentioned:
surface_form: Llullaillaco
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.719863
lon: -68.536852
surface_form: Corrida de Cori
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.9142
lon: -68.45
surface_form: Galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: corrida de cori
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.9142
lon: -68.45
The name may be derived from,, which means &quot;metal&quot; (especially &quot;copper&quot;) in the indigenous language Quechua. Pedro Armengol Valenzuela hypothesized that the second part of the name is, &quot;collect&quot;; thus the name Antofalla would mean &quot;collection of copper&quot;. Another theory is that Antofalla is derived from the Diaguita language. Geography and structure.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
Antofalla. Antofalla is a Miocene–Pliocene volcano in Argentina's Catamarca Province. It is part of the volcanic segment of the Andes in Argentina, and it is considered to be part of the Central Volcanic Zone, one of the volcanic zones of the Andes. Antofalla forms a group of volcanoes that are aligned on and behind the main volcanic arc. Antofalla itself is a remote volcano.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
Antofalla forms a group of volcanoes that are aligned on and behind the main volcanic arc. Antofalla itself is a remote volcano. Antofalla and other Andean volcanoes form because the Nazca Plate is subducting beneath the South American Plate.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
Antofalla itself is a remote volcano. Antofalla and other Andean volcanoes form because the Nazca Plate is subducting beneath the South American Plate. Antofalla volcano is located in a region with a &quot;basins and ranges&quot; topography, where during the Miocene ranges were uplifted and basins formed through tectonic movement.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
Antofalla and other Andean volcanoes form because the Nazca Plate is subducting beneath the South American Plate. Antofalla volcano is located in a region with a &quot;basins and ranges&quot; topography, where during the Miocene ranges were uplifted and basins formed through tectonic movement. It sits on a basement formed by Eocene-Miocene sedimentary units over a much older crystalline basement.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
It sits on a basement formed by Eocene-Miocene sedimentary units over a much older crystalline basement. Antofalla is formed by a principal volcano, the high Antofalla volcano proper, and a surrounding complex of smaller volcanic systems that are formed by lava flows and pyroclastic material.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
The name may be derived from,, which means &quot;metal&quot; (especially &quot;copper&quot;) in the indigenous language Quechua. Pedro Armengol Valenzuela hypothesized that the second part of the name is, &quot;collect&quot;; thus the name Antofalla would mean &quot;collection of copper&quot;. Another theory is that Antofalla is derived from the Diaguita language. Geography and structure.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
The towns of Antofalla, Puesto Cuevas, Botijuela and Potrero Grande are east, southeast, south and southwest of the volcano, respectively. Gravel roads run along the northern, northeastern and east-southeast-southern sides of the volcanic complex, but the volcano is difficult to access. Precolumbian constructions, including a platform on the summit of Antofalla, have been found.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
An altar with a stone pyramid lies on its summit, and the mountains Llullaillaco, Pajonales and Pular can be seen from the top of the mountain. These volcanic centres overlap with each other, are all much smaller than the main Antofalla volcano and have experienced little erosion. All these volcanoes are formed by lava domes, lava flows and pyroclastic units.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
A large scale topographic anomaly surrounds the entire volcanic complex, and seismic tomography has shown the presence of low-velocity anomalies linked to the volcanic group. The Salar de Antofalla, one of the largest salt pans in the world, lies southeast of the Antofalla complex.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
The Salar de Antofalla, one of the largest salt pans in the world, lies southeast of the Antofalla complex. It is one of many salt pans that developed within closed basins of the region and its surface lies at an elevation of; other such salt pans include Salar Archibarca north-northwest of Antofalla, Salina del Fraile south-southwest and Salar del Rio Grande northwest.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
surface_form: rio grande
instance_of: Watercourse
countries: Argentina
coordinates: lat: -36.870277777778
lon: -69.759722222222
There also are several lakes such as Laguna Las Lagunitas on the northeastern foot of Antofalla, Laguna Patos west of Cerro Lila – Cerro Ojo de Antofalla and Laguna Cajeros southwest of Cerro Lila – Cerro Cajeros.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
Most of the northwestern flank of the main Antofalla volcano drains into the Salar de Archibarca, while the southeastern flank has drainages connecting it to the Salar de Antofalla through the (from northeast to southwest) Quebrada de las Cuevas, Quebrada del Volcan and Quebrada de las Minas; the latter two join before entering the salt pan in a large fan, the Campo del Volcán.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
Northeast of the Conito de Antofalla, the Rio Antofalla originates and flows southeastward into the Salar de Antofalla in a large alluvial fan, similar to other drainages that enter the Salar de Antofalla. South of Antofalla lies Vega Botijuela, where there are two hot springs. One of them discharges warm water at a rate of from the Botijuela normal fault, has emplaced a wide travertine.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
Many geologic lineaments control tectonics across the whole region, they direct the ascent of magma and the location of basins; some of these lineaments exist since the Precambrian. One of these lineaments in the region trends north-northeast and separates the Arequipa-Antofalla terrane from the Pampia terrane. Geologic record.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
The terrain beneath the volcano is formed in part by the crystalline basement of Precambrian-Paleozoic (&quot;Antofalla Metamorphites&quot;) age mainly north of the volcano and often interpreted as ophiolite, and by sedimentary units of Eocene-Miocene age that crop out on its southern side and by a conglomerate unit known as the Potrero Grande Formation.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
Parts of the basement crop out where it have been exposed by erosion, such as in the Rio Antofalla and the Quebrada de las Minas, and more generally in two sectors north and south of the volcano. Composition. Antofalla has erupted andesite and dacite, with dacite dominant and rhyolite a less common rock type; the entire spectrum from basaltic andesite to rhyolite has been found.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
Composition. Antofalla has erupted andesite and dacite, with dacite dominant and rhyolite a less common rock type; the entire spectrum from basaltic andesite to rhyolite has been found. Thin lava flows form most of the basalt-like rocks, which are subordinate at Antofalla.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
During winter snow covers the peaks; meltwater formed during spring has cut gullies into the mountains. There are not many creeks on Antofalla that carry water year round, although deep ravines with evidence of flash flood activity can be discerned. The main Antofalla volcano may have been glaciated during the Pleistocene, but this is disputed especially for the lower mountains of the complex.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
The main Antofalla volcano may have been glaciated during the Pleistocene, but this is disputed especially for the lower mountains of the complex. It is likely that in the past, more water was available and led to the deposition of alluvial fans at the margins of basins although there is no evidence that a lake ever formed in the Salar de Antofalla, unlike in other salars farther north.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
Eruptive history. The Antofalla complex has been active from the Miocene 11 million years ago into the Quaternary and has generated a large variety of volcanic rocks; it is thus considered to be a very long-lived volcano. The subsidiary peaks around Antofalla were all considered to be extinct by Ferdinand von Wolff.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
There are reports that the main volcano &quot;smoked&quot; occasionally such as in 1901 and 1911 and Antofalla is sometimes incorrectly considered the highest active volcano in the world, but the Global Volcanism Program considers the complex as Pleistocene in age, and no clear evidence of Holocene activity is found. Climbing.

Geographic entities mentioned:
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
surface_form: antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
state of Alaska. It is a very clear, small arctic river flowing south from the foothills of Baird Mountains to where it meets the Kobuk River in the village of Kiana. From Kiana, the Kobuk flows southwest into Hotham Inlet of Kotzebue Sound on the Chukchi Sea. The upper segment of the stream runs in a U molded, half-mile wide valley lying between 300-to 400-foot moving slopes.

Geographic entities mentioned:
surface_form: Hotham Inlet
instance_of: Landform
countries: United States
coordinates: lat: 66.819722222222
lon: -161.965
It is located in the Moquegua Region, Mariscal Nieto Province, Torata District, and in the Tacna Region, Candarave Province, Camilaca District. Tutupaca is situated southeast of the mountains Limani and Apachita Limani, west of Tutupaca volcano, north of Chuqi Ananta and Wañuma, and northeast of Pumani. The Asana River originates near Tutupaca and it flows to the southwest.

Geographic entities mentioned:
surface_form: Tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: ananta
instance_of: Mountain
countries: Peru
coordinates: lat: -13.81388889
lon: -70.62055556
surface_form: ananta
instance_of: Mountain
countries: Peru
coordinates: lat: -15.8128
lon: -71.6825
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
Tutupaca (Moquegua-Tacna). Tutupaca is a mountain in the Andes of southern Peru, about high. It is located in the Moquegua Region, Mariscal Nieto Province, Torata District, and in the Tacna Region, Candarave Province, Camilaca District. Tutupaca is situated southeast of the mountains Limani and Apachita Limani, west of Tutupaca volcano, north of Chuqi Ananta and Wañuma, and northeast of Pumani.

Geographic entities mentioned:
surface_form: tutupaca (moquegua-tacna)
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
Tutupaca (Moquegua-Tacna). Tutupaca is a mountain in the Andes of southern Peru, about high. It is located in the Moquegua Region, Mariscal Nieto Province, Torata District, and in the Tacna Region, Candarave Province, Camilaca District. Tutupaca is situated southeast of the mountains Limani and Apachita Limani, west of Tutupaca volcano, north of Chuqi Ananta and Wañuma, and northeast of Pumani.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
It is located in the Moquegua Region, Mariscal Nieto Province, Torata District, and in the Tacna Region, Candarave Province, Camilaca District. Tutupaca is situated southeast of the mountains Limani and Apachita Limani, west of Tutupaca volcano, north of Chuqi Ananta and Wañuma, and northeast of Pumani. The Asana River originates near Tutupaca and it flows to the southwest.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
Helvadere. Helvadere is a town (&quot;belde&quot;) and municipality in the Aksaray District, Aksaray Province, Turkey. Its population is 2,564 (2021). Geography. Helvadere is on the western slopes of Mount Hasan at about. It is south of Aksaray. History. Helvadere is situated next to ruins of the ancient town Nora, which was an important town in Hellenistic Capadocia.

Geographic entities mentioned:
surface_form: Mount Hasan
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.12652
lon: 34.16511
Kettle Falls Hotel. The Kettle Falls Hotel is a historic hotel in what is now Voyageurs National Park in the U.S. state of Minnesota. It opened in 1913 deep in the wilderness of the Boundary Waters, at the juncture of Namakan and Rainy Lakes. Today it is the only lodging operating inside the park, and remains accessible only by water.

Geographic entities mentioned:
surface_form: Namakan
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.456693
lon: -92.585364
surface_form: Rainy Lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.636944444444
lon: -93.031388888889
Edmunds Glacier. Edmunds Glacier is located on Mount Rainier in the U.S. state of Washington. Named in 1883 for Vermont senator George F. Edmunds, the glacier lies on the western flank of the volcano below the steep, rocky Mowich Face and Sunset Face. Starting from an elevation of about, the glacier flows northwest down to and ends northeast of the Jeanette Heights region of Mount Rainier.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Arambaré. Arambaré () is a municipality in the state of Rio Grande do Sul, Brazil. It is bordered by Tapes on the north, Camaquã on the west and south, and Lagoa dos Patos on the east. It is at km 396 of the BR-116, 33 km from Camaquã. It is 156 km from Porto Alegre.

Geographic entities mentioned:
surface_form: Lagoa dos Patos
instance_of: Lake
countries: Brazil
coordinates: lat: -31.15
lon: -51.39
In 1752, these reductions were destroyed by the Portuguese army. The Jesuit cattle remained as wild and feral livestock scattered throughout the region. Around 1763, Azorean couples who migrated south settled on the left bank of the Guaíba estuary and the right bank of the Lagoa dos Patos, establishing farms and charqueadas (meat-salting plants) up to the Rio Camaquã.

Geographic entities mentioned:
surface_form: Lagoa dos Patos
instance_of: Lake
countries: Brazil
coordinates: lat: -31.15
lon: -51.39
Tourism. The city is famous for its Carnival, where thousands of tourists visit, making it one of the best carnivals in the southern region of the state. In summer, the city, bathed by the Lagoa dos Patos, is filled with swimmers from all over the state. Climate. In summer, the maximum temperature reaches 40 °C, and the minimum is 20 °C.

Geographic entities mentioned:
surface_form: Lagoa dos Patos
instance_of: Lake
countries: Brazil
coordinates: lat: -31.15
lon: -51.39
Wayunka. Wayunka (Quechua for &quot;bunch of bananas&quot;, Hispanicized spelling &quot;Huayunca&quot;) is a mountain in the Wansu mountain range in the Andes of Peru that is about high. It is situated in the Apurímac Region, Antabamba Province, Oropesa District, northwest of the mountains Waytani and Chankuwaña.

Geographic entities mentioned:
surface_form: Waytani
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6581
lon: -72.4678
surface_form: Chankuwaña
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6231
lon: -72.4692
surface_form: waytani
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6581
lon: -72.4678
surface_form: chankuwaña
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6231
lon: -72.4692
Wayunka. Wayunka (Quechua for &quot;bunch of bananas&quot;, Hispanicized spelling &quot;Huayunca&quot;) is a mountain in the Wansu mountain range in the Andes of Peru that is about high. It is situated in the Apurímac Region, Antabamba Province, Oropesa District, northwest of the mountains Waytani and Chankuwaña.

Geographic entities mentioned:
surface_form: huayunca
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6067
lon: -72.4897
surface_form: wayunka
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6067
lon: -72.4897
Wayunka. Wayunka (Quechua for &quot;bunch of bananas&quot;, Hispanicized spelling &quot;Huayunca&quot;) is a mountain in the Wansu mountain range in the Andes of Peru that is about high. It is situated in the Apurímac Region, Antabamba Province, Oropesa District, northwest of the mountains Waytani and Chankuwaña.

Geographic entities mentioned:
surface_form: wayunka
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6067
lon: -72.4897
Mount Pétain. A mountain formerly known as Mount Pétain, but with no current official name, is located on the border of the Canadian provinces of Alberta and British Columbia (BC) on the Continental Divide. Original nomenclature. It was named in 1918 after French Marshal Philippe Pétain, who was then an honoured war hero for the Allies of World War I.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount pétain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.544166666667
lon: -115.18527777778
Besides the mountain several other geographical points were named for Pétain. Pétain Glacier is found next to Mount Joffre and Mount Pétain forming the Pétain Basin, with melt cascading down Pétain Creek Falls into the Pétain Creek below. Renaming. In 2019, the Government of Alberta rescinded Pétain's name from the Alberta side of the border.

Geographic entities mentioned:
surface_form: Mount Joffre
instance_of: Mountain
countries: Canada
coordinates: lat: 50.528333333333336
lon: -115.20694444444445
surface_form: mount pétain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.544166666667
lon: -115.18527777778
In 2019, the Government of Alberta rescinded Pétain's name from the Alberta side of the border. In October 2021, the Regional District of East Kootenay, upon being consulted by BC Geographical Names, voted to support removing Pétain's name from the British Columbia side. On June 29, 2022, the Government of British Columbia also rescinded the name, rendering the mountain officially nameless.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: kootenay
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
In October 2021, the Regional District of East Kootenay, upon being consulted by BC Geographical Names, voted to support removing Pétain's name from the British Columbia side. On June 29, 2022, the Government of British Columbia also rescinded the name, rendering the mountain officially nameless. The names of Pétain Creek and Pétain Glacier were also rescinded.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
As of July 2022, neither of the provinces in which the mountain sits have decided on a new name, but &quot;will work together&quot; with local stakeholders to determine one. Access. The snow-capped mountain can be reached from Height of the Rockies Provincial Park and Elk Lakes Provincial Park within British Columbia or Peter Lougheed Provincial Park in Alberta.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: elk lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 50.55
lon: -115.1
It was named in 1918 after French Marshal Philippe Pétain, who was then an honoured war hero for the Allies of World War I. The name was retained despite the later reversal in Pétain's reputation after his having been Head of State of Vichy France and being partly responsible for the murder of 76,000 Jews. Besides the mountain several other geographical points were named for Pétain.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
On June 29, 2022, the Government of British Columbia also rescinded the name, rendering the mountain officially nameless. The names of Pétain Creek and Pétain Glacier were also rescinded. As of July 2022, neither of the provinces in which the mountain sits have decided on a new name, but &quot;will work together&quot; with local stakeholders to determine one. Access.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Pétain. A mountain formerly known as Mount Pétain, but with no current official name, is located on the border of the Canadian provinces of Alberta and British Columbia (BC) on the Continental Divide. Original nomenclature. It was named in 1918 after French Marshal Philippe Pétain, who was then an honoured war hero for the Allies of World War I.

Geographic entities mentioned:
surface_form: mount pétain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.544166666667
lon: -115.18527777778
She ultimately weighed anchor from New Caledonian waters on 7 March and got underway for Guadalcanal – the scene of once-bitter fighting. She arrived off Lunga Point on the morning of the 10th and spent the majority of her days over the next three months in the Guadalcanal-Tulagi area.

Geographic entities mentioned:
surface_form: Lunga Point
instance_of: Landform
countries: Solomon Islands
coordinates: lat: -9.416666666666666
lon: 160.03333333333333
Biography. Sarkis Rizzi's family presented at this time three patriarchs to the Maronite Church: his two uncles Michel (1567 - 1581) and of the same name Sarkis (1581 - 1596) and his younger brother Joseph (October 3, 1596 - March 26, 1608). Youssef was abbot of the Monastery of Qozhaya in the Kadisha Valley after the election of his uncle Sarkis patriarch and was in 1595 appointed bishop.

Geographic entities mentioned:
surface_form: Kadisha Valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.282944
lon: 35.951611
Geography. The CDP is in eastern Blair County, in the northwestern part of Huston Township. It is in the Morrisons Cove region of the county, in the valley of Piney Creek, which flows north to the Frankstown Branch of the Juniata River at Ganister, part of the Susquehanna River watershed. Lock Mountain rises to an elevation of just west of Clappertown.

Geographic entities mentioned:
surface_form: Morrisons Cove
instance_of: Landform
countries: United States
coordinates: lat: 40.2492
lon: -78.3358
Cononley. Cononley (or) is a village and civil parish in the county of North Yorkshire, England. Cononley is in the Aire Valley south of Skipton and with an estimated population of 1,080 (2001 est.), measured at 1,172 at the 2011 census. It is situated west of the A629 road with access to Skipton, Keighley.

Geographic entities mentioned:
surface_form: Aire Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.017
lon: -1.465
The Domesday Book contains only a brief mention of Cononley, but the settlement's name had probably originated several centuries earlier. The ending 'ley' refers to a clearing in the then wooded Aire valley and is shared with other Airedale communities. The first part of the name is derived from either a personal name or a river or beck name.

Geographic entities mentioned:
surface_form: Airedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.017
lon: -1.465
Legacy. Downieville, California is named for Major Downie. He is also the namesake of Downie Peak in the Selkirks. Also named for him is the former goldrush boomtown of Downie Creek, at the confluence of the stream of the same name with the Columbia River and adjacent to the vanished boomtown of La Porte, both at the heart of the Big Bend goldfields.

Geographic entities mentioned:
surface_form: Downie Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5582
lon: -118.30233
Vallée Verte. The Vallée Verte (literally: Green Valley) is a valley in the Chablais Alps, about 15 kilometres south of Thonon-les-Bains in the Haute-Savoie area of France. The river Menoge flows through it. It has as south-southwest orientation and a length of about 20 kilometres. Many of its inhabitants work near Geneva or Annemasse.

Geographic entities mentioned:
surface_form: vallée verte
instance_of: Valley
countries: France
coordinates: lat: 46.217
lon: 6.433
Following the warm frontal passage, skies cleared rapidly and temperatures quickly began to rise. The cold front began crossing Lake Huron towards the noon hour, and with it several thunderstorms developed shortly after 1:30pm EDT, with the northernmost cell soon becoming most dominant.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Caves. There are some 60 known caves, almost all of them being of small size (the longest one is 120 m). Other tourist attractions. Cheile Turzii are just a few km away from two other canyons (Cheile Turului and Cheile Borzești) as well as from &quot;Ciucaș waterfall&quot;. Cheile Turzii is one of the main rock climbing sites in Romania.

Geographic entities mentioned:
surface_form: ciucaș
instance_of: Mountain
countries: Romania
coordinates: lat: 45.5217
lon: 25.9264
surface_form: cheile turzii
instance_of: Valley
countries: Romania
coordinates: lat: 46.56388889
lon: 23.67916667
surface_form: cheile turzii
instance_of: Valley
countries: Romania
coordinates: lat: 46.56388889
lon: 23.67916667
surface_form: ciucaș
instance_of: Mountain
countries: Romania
coordinates: lat: 45.522777777778
lon: 25.923611111111
Turda Gorge. Turda Gorge (,) is a natural reserve (on Hășdate River) situated 6 km west of Turda and about 15 km south-east of Cluj-Napoca, in Transylvania, Romania. Geography. The canyon, formed through the erosion of the Jurassic limestone of the mountain, is 2 900 m long and the walls have heights reaching 300 m. The total surface of the canyon is of 324 ha.

Geographic entities mentioned:
surface_form: turda gorge
instance_of: Valley
countries: Romania
coordinates: lat: 46.56388889
lon: 23.67916667
The total surface of the canyon is of 324 ha. Cheile Turzii contain one of the richest and most scenic karst landscapes in Romania. More than 1000 plant and animal species (some of them rare or endangered, like the wild garlic or some species of eagle) live here. History. The site has been inhabited since the Neolithic. Flora.

Geographic entities mentioned:
surface_form: cheile turzii
instance_of: Valley
countries: Romania
coordinates: lat: 46.56388889
lon: 23.67916667
Cripta de los Héroes (Tacna). The Crypt of Heroes () is a war monument located at Intiorko Hill, Tacna, Peru. Originally inaugurated by the Chilean administration in 1901 and rededicated in 1930 by the Peruvian government, the monument is currently partially destroyed. History.

Geographic entities mentioned:
surface_form: Intiorko Hill
instance_of: Mountain
countries: Peru
coordinates: lat: -17.99025
lon: -70.25857
Baldred is believed to have founded a monastery at Tyninghame. However, at times, he preferred to retire from the spiritual government of the Lothian Britons and he selected the Bass Rock as the spot to build himself a small hermitage and associated chapel, although he also sometimes resided in 'St Baldred's Cave' on Seacliff Beach. Nationality.

Geographic entities mentioned:
surface_form: Bass Rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.08
lon: -2.64
Pok Fu Lam. Pok Fu Lam () or Pokfulam is a residential area on Hong Kong Island, at the western end of the Southern District. It is a valley between Victoria Peak and Mount Kellett, around Telegraph Bay.

Geographic entities mentioned:
surface_form: Victoria Peak
instance_of: Mountain
countries: People's Republic of China
British Hong Kong
coordinates: lat: 22.275469444444
lon: 114.14382777778
surface_form: Mount Kellett
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.26184444
lon: 114.14843611
The farm supplied not only milk, but cattle to Hong Kong, and later became Dairy Farm. However, it no longer exists in Pok Fu Lam. Pok Fu Lam is connected to Lung Fu Shan, Sai Ying Pun and Aberdeen by the Pok Fu Lam Road. It's also indirectly connected to the Mid-Levels. Pok Fu Lam also overlooks Lamma Island. Pok Fu Lam is connected to Kennedy Town via Smithfield and Shek Tong Tsui via Hill Road.

Geographic entities mentioned:
surface_form: Lung Fu Shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.27993333
lon: 114.13504167
Etymology. &quot;Cyrtodactylus aravindi&quot; is named after Dr N. A. Aravind, Senior Fellow at ATREE, Bengaluru, India for his support towards herpetological research. Distribution. &quot;Cyrtodactylus aravindi&quot; is currently only known from two locations 20 kilometres from each other in straight-line distance in the Agasthaymalai hill range in the southern Western Ghats of India. Ecology.

Geographic entities mentioned:
surface_form: Agasthaymalai hill range
instance_of: Mountain
countries: India
coordinates: lat: 8.6166666666667
lon: 77.25
Corps de Garde. Corps de Garde (translation: &quot;Guardhouse&quot;) is a 720-metre-high mountain of volcanic origin, in the area Palma in the Black River district of Mauritius. The name derived from the fact that a French military post was once established on its slope to control the bands of runaway slaves.

Geographic entities mentioned:
surface_form: corps de garde
instance_of: Mountain
countries: Mauritius
coordinates: lat: -20.252222222222
lon: 57.450555555556
On the foot of that hill are the towns of Beau Bassin-Rose Hill and Quatre Bornes. Corps de Garde Nature Reserve. Corps de Garde Nature Reserve was designated in 1951. It covers an area of 0.9 km2 on the western and northwestern flank of the mountain.

Geographic entities mentioned:
surface_form: corps de garde
instance_of: Mountain
countries: Mauritius
coordinates: lat: -20.252222222222
lon: 57.450555555556
Between 1994 and 1997, he conducted over 150 live radio interviews with politicians, and later on, he conducted over 250 interviews with a variety of political figures. In the early 2000s, he worked as a consultant, offering a number of training courses in media communications and campaign management, as well as advising the World Bank on the feasibility of developing the Jiu Valley.

Geographic entities mentioned:
surface_form: Jiu Valley
instance_of: Valley
countries: Romania
coordinates: lat: 43.77805556
lon: 23.81333333
In 6th century BCE with the emergence of Mahajanapadas. Out of sixteen such states, four strong ones emerged: Kosala, Magadha, Vatsa, and Avanti, with Magadha dominating the rest by the mid-fifth century. The Magadha then transformed into the Nanda Empire under Mahapadma Nanda (345–321), extending from the Gangetic plains to the Hindu Kush and the Deccan Plateau.

Geographic entities mentioned:
surface_form: Deccan Plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
In to this power vacuum, the Yuezhi were able to establish the new Kushan Empire in 30 CE. The Gupta Empire was founded by Chandragupta I (320–335), which in sixty years expanded from the Ganges to the Bay of Bengal and the Indus River following the downfall of the Kushan Empire. Gupta governance was similar to that of the Maurya.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88