Sarmila/GeoWiki-Features huggingface dataset:
Antarcticbukta. Antarcticbukta is a wide bay at the southern side of Kongsøya in Kong Karls Land, Svalbard. It is located south of the mountain Sjögrenfjellet. The bay extends eastwards to the headland of Kapp Altmann, which separates the bay from the beach area Snøsporvstranda.

Geographic entities mentioned:
surface_form: Sjögrenfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 78.8471
lon: 27.9885
They begin at Mica Peak and Krell Hill near Spokane and extend approximately 320 km north (200 miles) from the border to Kinbasket Lake, at the now-deserted location of the onetime fur company post, Boat Encampment. The range is bounded on its west, northeast and at its northern extremity by the Columbia River, or the reservoir lakes now filling most of that river's course.

Geographic entities mentioned:
surface_form: Krell Hill
instance_of: Mountain
countries: United States
coordinates: lat: 47.3446
lon: -117.175
The range is bounded on its west, northeast and at its northern extremity by the Columbia River, or the reservoir lakes now filling most of that river's course. From the Columbia's confluence with the Beaver River, they are bounded on their east by the &quot;Purcell Trench&quot;, which contains the Beaver River, Duncan River, Duncan Lake, Kootenay Lake and the Kootenay River.

Geographic entities mentioned:
surface_form: Kootenay Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
Qiniangshan. Qiniangshan () is a mountain in Nan'ao Subdistrict, Dapeng Peninsula. At 869 metres above sea level, it is the second tallest mountain in Shenzhen after Wutongshan. It is located within the Dapeng National Geopark. Trekking here is moderately difficult and offers views of Shenzhen, Hong Kong and the South China Sea.

Geographic entities mentioned:
surface_form: qiniangshan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.525
lon: 114.5433
Traditional Homes of Clan Hall. The traditional homes of the Halls were at Redesdale, East Teviotdale, and Liddesdale. Other Halls lived in Aynstrother; Glenryg, in the barony of Lesmahagow; Garvald; Irvide; Glasgow; Sancharmvr, in Preswick; and Perth. Battle of Otterburn.

Geographic entities mentioned:
surface_form: Redesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.229
lon: -2.186
surface_form: Liddesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.2
lon: -2.75
Alestopetersius nigropterus. &quot;Alestopetersius nigropterus&quot; is a species of freshwater ray-finned fish belonging to the family Alestidae, the African tetras. This fish is found in Lake Mai-Ndombe in the middle Congo River basin in the Democratic Republic of the Congo. Description. &quot;Alestopetersius nigropterus&quot; reaches a standard length of.

Geographic entities mentioned:
surface_form: Lake Mai-Ndombe
instance_of: Lake
countries: Democratic Republic of the Congo
coordinates: lat: -2
lon: 18.33
The national park is bounded to the north by the Nattai State Conservation Area, the Burragorang State Conservation Area, and Lake Burragorang, inclusive of a exclusion zone surrounding the lake; to the east by the Bargo State Conservation Area and the now partly disused Picton – Mittagong loop railway line; to the south by the Wombeyan Caves Road; to the southwest by the Kanangra-Boyd National Park; and to the west by the Yerranderie State Conservation Area.

Geographic entities mentioned:
surface_form: Lake Burragorang
instance_of: Lake
countries: Australia
coordinates: lat: -34
lon: 150.43333333333
Nova Scotia Route 301. Route 301 is a collector road in the Canadian province of Nova Scotia. It is located in Cumberland County and connects Oxford at Route 204 with Port Howe at Trunk 6. From Port Howe it follows the western bank of River Philip to Oxford town limits. In Oxford it continues in a south-west direction to its terminus at Little River Road Route 204 as Lower Main Street.

Geographic entities mentioned:
surface_form: River Philip
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.8522
lon: -63.7387
Gannett Glacier. Gannett Glacier is the largest glacier in the Rocky Mountains within the United States. The glacier is located on the east and north slopes of Gannett Peak, the highest mountain in Wyoming, on the east side of the Continental Divide in the Wind River Range. Gannett is but one of dozens of glaciers located in the Fitzpatrick Wilderness of Shoshone National Forest.

Geographic entities mentioned:
surface_form: Gannett Peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.184202777778
lon: -109.65423333333
Giddings Peak. ih70zcq4pnubbc3qgndobsgowrz" xml:space="preserve">#redirect Athos Range

Geographic entities mentioned:
surface_form: giddings
instance_of: Mountain
coordinates: lat: -67.4
lon: 50.73333
surface_form: giddings peak
instance_of: Mountain
coordinates: lat: -70.2
lon: 64.73333
japonicum. &quot;Cirsium japonicum&quot; var. &quot;japonicum&quot; is a flowering plant in the family Asteraceae. It is a perennial thistle native to Japan, Korea, China, Taiwan, and Vietnam. It is a variety of &quot;Cirsium japonicum&quot;, and is known by many synonyms. In Chinese it is known as the Yushan thistle (), named for Yushan mountain on Taiwan. Uses. &quot;Cirsium japonicum&quot; var.

Geographic entities mentioned:
surface_form: Yushan
instance_of: Mountain
countries: Taiwan
coordinates: lat: 23.47
lon: 120.95726666667
Production. Film4 Productions boarded the feature-length adaptation of Archer, Earl and Hayward's short film in early 2019, followed by the BFI. Principal photography took place on location in rural North Wales, including Cwm Penmachno and Llyn Gwynant, during the COVID-19 pandemic. Release. The film premiered at the Sundance Film Festival on 23 January 2022.

Geographic entities mentioned:
surface_form: Llyn Gwynant
instance_of: Lake
countries: United Kingdom
coordinates: lat: 53.048
lon: -4.022
Rhea Corner. Rhea Corner () is a triangular area of exposed rock lying on the north side of Saturn Glacier in southeastern Alexander Island, Antarctica. The feature is a promontory at the west end of the massif that includes the Deimos, Pagoda and Phobos Ridge. A cliff on the north face is about 500 m high.

Geographic entities mentioned:
surface_form: rhea corner
instance_of: Mountain
coordinates: lat: -71.8833
lon: -68.8
Rhea Corner. Rhea Corner () is a triangular area of exposed rock lying on the north side of Saturn Glacier in southeastern Alexander Island, Antarctica. The feature is a promontory at the west end of the massif that includes the Deimos, Pagoda and Phobos Ridge. A cliff on the north face is about 500 m high.

Geographic entities mentioned:
surface_form: rhea corner
instance_of: Mountain
coordinates: lat: -71.8833
lon: -68.8
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
Phyllonemus. &quot;Phyllonemus&quot; is a genus of claroteid catfish native to Africa where it is only found in Lake Tanganyika.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
Mount Gibraltar. Mount Gibraltar (Ngunnawal–Gundungurra language: &quot;Bowrell&quot;) is a mountain with an elevation of that is located in the Southern Highlands region, between Bowral and Mittagong, in New South Wales, Australia. Further west is. Location and features. The mountain is locally known as 'The Gib', and is in the form of a ridge, rather than an obvious conical peak.

Geographic entities mentioned:
surface_form: mount gibraltar
instance_of: Mountain
countries: Australia
coordinates: lat: -34.465333333333
lon: 150.42826666667
The first European to climb the mountain, in 1798, was explorer John Wilson. He learned from local Aborigines the name 'Bowrell', which meant 'a high place'. Surveyor Sir Thomas Mitchell also climbed Mount Gibraltar. The former Mount Gibraltar Trachyte Quarries Complex was added to the New South Wales State Heritage Register on 2 December 2013. Railway.

Geographic entities mentioned:
surface_form: mount gibraltar
instance_of: Mountain
countries: Australia
coordinates: lat: -34.465333333333
lon: 150.42826666667
The former Mount Gibraltar Trachyte Quarries Complex was added to the New South Wales State Heritage Register on 2 December 2013. Railway. The Main South Railway skirts Mount Gibraltar at its western foothills, passing through a tunnel under Evans Street, Bowral. The original tunnel was single track, but it was replaced in the 1920s by a double track tunnel.

Geographic entities mentioned:
surface_form: mount gibraltar
instance_of: Mountain
countries: Australia
coordinates: lat: -34.465333333333
lon: 150.42826666667
The hall still exists today and is located on the southwest corner of 16th Street and Central Avenue. It was called a &quot;Hall in the Grove,&quot; and later became known as Chautauqua Hall. In 1882, the PIC purchased the Rancho Los Laureles, which was located in Carmel Valley, California. Guests from the hotel could visit the lodge on the property to ride, hunt, and explore the trails.

Geographic entities mentioned:
surface_form: Carmel Valley, California
instance_of: Valley
countries: United States
coordinates: lat: 36.4748315
lon: -121.7205075
They traveled south through the Igharghar valley past Aïn Taïba, El-Bodh and Timassinin. From Timassinin the expedition headed southeast along the Igharghar valley, and on 16 April 1880 encamped on shores of Lake Menghough on the fringe of the Tuareg of the Ajjer country. With provisions running short and the local people showing hostility, Flatters decided to return by the same route.

Geographic entities mentioned:
surface_form: Lake Menghough
instance_of: Lake
countries: Algeria
France
coordinates: lat: 26.382478
lon: 8.817555
The site is near today's city of Tamanrasset. Massacre. Before the expedition left Ouargla plans had been made to destroy it by the Kel Ahaggar Tuaregs of the Hoggar Mountains, the Awlad Sidi Shaykh confederation and the Senussi. They knew the planned route and were kept informed by the expedition's guides, who helped sabotage the expedition by leading it past wells.

Geographic entities mentioned:
surface_form: Hoggar Mountains
instance_of: Plateau
countries: Algeria
France
coordinates: lat: 23.288611
lon: 5.534167
She was the first Dean of Women at the University of Michigan, and the first woman professor to be recognized by the university. Early years and education. Eliza Maria Mosher was born near Cayuga Lake, New York in 1846. Her parents were members of the Society of Friends, and she was brought up under the influences of that religious denomination.

Geographic entities mentioned:
surface_form: Cayuga Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.68805555555556
lon: -76.70222222222222
Devol (Albania). Devol (;;) also Deabolis or Diabolis, was a medieval fortress and bishopric in western Macedonia, located south of Lake Ohrid in what is today the south-eastern corner of Albania (Devoll municipality). Its precise location is unknown today, but it is thought to have been located by the river of the same name (today Devoll River), and on the Roman Via Egnatia road.

Geographic entities mentioned:
surface_form: Lake Ohrid
instance_of: Lake
countries: North Macedonia
Albania
coordinates: lat: 41.03333333333333
lon: 20.716666666666665
Geoff Roes. Geoff Roes (born April 14, 1976 in central New York) is an American ultramarathon runner. Career. Roes grew up in Cleveland, New York which is by Oneida Lake. Cleveland is northeast of Syracuse. He excelled in track and cross country at Paul V. Moore High School in Central Square, New York southwest of Oswego.

Geographic entities mentioned:
surface_form: Oneida Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.2
lon: -75.9
Northwestern Lehigh School District. Northwestern Lehigh School District is a public school district in northwest Lehigh County, Pennsylvania in the Lehigh Valley region of eastern Pennsylvania. It serves Heidelberg, Lowhill, Lynn, and Weisenberg Townships.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
From a military background, Aylmer was commissioned into the Indian Army, and immediately involved in fierce fighting on the north-west frontier. In a singularly heroic action, still in his twenties, he helped rescue Townshend's garrison at Chitral, spearheading the relief column. For his valorous conduct he was awarded the Victoria Cross, and rapid promotion through the officer class.

Geographic entities mentioned:
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
Amsterdam, New Jersey. Amsterdam is an unincorporated community located within Holland Township in Hunterdon County, in the U.S. state of New Jersey. Located on the southern flank of the Musconetcong Mountain, the area was settled in the first half of the 18th century. It was later named after Amsterdam, Netherlands.

Geographic entities mentioned:
surface_form: Musconetcong Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.6581
lon: -75.0094
Vale of Catmose. The Vale of Catmose is an area of relatively low-lying land, much of which is flooded by Rutland Water, in western Rutland, England. Oakham, the county town, lies within its bounds. It is drained by the River Gwash and the Langham Brook.

Geographic entities mentioned:
surface_form: vale of catmose
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.65
lon: -0.68
Zeller See (Lake Constance). The Zeller See (Standard German of Germany; Swiss Standard German: &quot;Zellersee&quot;; could be translated as &quot;Lake of Radolfzell&quot;) is part of the Lower Lake, the lower part of Lake Constance. It lies in the bay of Radolfzell, and between the peninsula of Mettnau to the north and the peninsula of Höri to the south.

Geographic entities mentioned:
surface_form: zeller see (lake constance)
instance_of: Lake
countries: Germany
coordinates: lat: 47.719166666667
lon: 8.9858333333333
Zeller See (Lake Constance). The Zeller See (Standard German of Germany; Swiss Standard German: &quot;Zellersee&quot;; could be translated as &quot;Lake of Radolfzell&quot;) is part of the Lower Lake, the lower part of Lake Constance. It lies in the bay of Radolfzell, and between the peninsula of Mettnau to the north and the peninsula of Höri to the south.

Geographic entities mentioned:
surface_form: zeller see
instance_of: Lake
countries: Germany
coordinates: lat: 47.719166666667
lon: 8.9858333333333
Activity was in two phases and a depression or caldera formed in the course of its growth. The volcano was also impacted by eruptions of its neighbour to the west, Nevado Tres Cruces. The last eruption occurred around 750 CE; steam emissions observed in November 1993 may have constituted another eruptive event. An international highway between Argentina and Chile crosses north of the mountain.

Geographic entities mentioned:
surface_form: Nevado Tres Cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
Ojos del Salado can be ascended from both countries; the first ascent was made in 1937 by Jan Alfred Szczepański and, members of a Polish expedition in the Andes. During the middle of the 20th century there was a debate on whether Ojos del Salado or Aconcagua was the highest mountain in South America which was eventually resolved in favour of Aconcagua. Name.

Geographic entities mentioned:
surface_form: Aconcagua
instance_of: Mountain
countries: Argentina
coordinates: lat: -32.653055555555554
lon: -70.01166666666667
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
The occurrence of a rift-like structure with numerous small craters has also been reported. Volcanic cones form a north-northeast trending alignment on the western flank. Cerro Solo and El Fraile are large lava domes on the flanks of Ojos del Salado, and produced pyroclastic flows. Wind-driven erosion has produced megaripple sand fields on the northern flank.

Geographic entities mentioned:
surface_form: Cerro Solo
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -27.108333333333
lon: -68.716666666667
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Travellers have called the region a &quot;moonscape&quot;. There are hot springs in the region, such as the Termas Laguna Verde at the shores of Laguna Verde, which are frequented by visitors. The volcano lies in the middle of an over long east–west trending chain of volcanoes that form a drainage divide and includes the volcanoes Nevado Tres Cruces, Incahuasi and Cerro Blanco.

Geographic entities mentioned:
surface_form: Nevado Tres Cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: Incahuasi
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.033333333333
lon: -68.3
surface_form: incahuasi
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.033333333333
lon: -68.3
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
During the Quaternary, volcanism formed the edifices of Cerro Solo, El Fraile, Incahuasi, El Muerto, El Muertito, Falso Azufre, Nevado San Francisco, Nevado Tres Cruces and Ojos del Salado, which together cover over half of the area. Apart from the large volcanoes, many smaller mafic monogenetic volcanoes developed in the area, especially east of Ojos del Salado.

Geographic entities mentioned:
surface_form: El Muerto
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.0575
lon: -68.483888888889
surface_form: Falso Azufre
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -26.8
lon: -68.37
surface_form: Nevado San Francisco
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -26.918333333333
lon: -68.263055555556
surface_form: nevado san francisco
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -26.918333333333
lon: -68.263055555556
surface_form: san francisco
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -26.918333333333
lon: -68.263055555556
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
They stated that the peak may be higher than Aconcagua, which media reported as if it were proven fact. These measurements set off a debate whether Ojos del Salado was higher than Aconcagua and thus the highest summit of the Western Hemisphere, and drew attention to the mountain.

Geographic entities mentioned:
surface_form: Aconcagua
instance_of: Mountain
countries: Argentina
coordinates: lat: -32.653055555555554
lon: -70.01166666666667
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Radiometric dating has yielded ages of 1.53 ± 0.13, 1.2 ± 0.3 million and less than one million years ago for rocks in the northwestern part of Ojos del Salado, 1.08 ± 0.09 million years for flows underlying the summit, 1.08 ± 0.04 million years for the northern flank of Ojos del Salado, 700,000±50,000 for its western flank, 450,000±60,000 for El Muerto, 340,000 ± 190,000 years for the summit rocks, and 230,000±40,000 years for El Fraile.

Geographic entities mentioned:
surface_form: el muerto
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.0575
lon: -68.483888888889
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
The Argentine part is within Catamarca Province and the Chilean in Copiapo Province of the Atacama Region. The highway runs between the city of Copiapo west of the volcano and the Paso San Francisco to Argentina, lying about north of the volcano, making it more accessible than many other volcanoes there.

Geographic entities mentioned:
surface_form: san francisco
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -26.918333333333
lon: -68.263055555556
Ojos del Salado. Nevado Ojos del Salado is a dormant complex volcano in the Andes on the Argentina–Chile border. It is the highest volcano on Earth and the highest peak in Chile. The upper reaches of Ojos del Salado consist of several overlapping lava domes, lava flows and volcanic craters, with sparse ice cover.

Geographic entities mentioned:
surface_form: nevado ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Ojos del Salado. Nevado Ojos del Salado is a dormant complex volcano in the Andes on the Argentina–Chile border. It is the highest volcano on Earth and the highest peak in Chile. The upper reaches of Ojos del Salado consist of several overlapping lava domes, lava flows and volcanic craters, with sparse ice cover.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Nevado Ojos del Salado is a dormant complex volcano in the Andes on the Argentina–Chile border. It is the highest volcano on Earth and the highest peak in Chile. The upper reaches of Ojos del Salado consist of several overlapping lava domes, lava flows and volcanic craters, with sparse ice cover. The complex extends over an area of and its highest summit reaches an altitude of above sea level.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
The complex extends over an area of and its highest summit reaches an altitude of above sea level. Numerous other volcanoes rise around Ojos del Salado. Being close to the Arid Diagonal of South America, the mountain has extremely dry conditions, which prevent the formation of substantial glaciers and a permanent snow cover.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
This is the highest lake of any kind in the world. Owing to its altitude and the desiccated climate, the mountain lacks vegetation. Ojos del Salado was volcanically active during the Pleistocene and Holocene, during which it mainly produced lava flows. Activity was in two phases and a depression or caldera formed in the course of its growth.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
The last eruption occurred around 750 CE; steam emissions observed in November 1993 may have constituted another eruptive event. An international highway between Argentina and Chile crosses north of the mountain. Ojos del Salado can be ascended from both countries; the first ascent was made in 1937 by Jan Alfred Szczepański and, members of a Polish expedition in the Andes.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
In geographical terms, Ojo is commonly used in Chile and Argentina to denote a spring or source of water; e.g. the nearby source of the Las Lozas river &quot;Ojo de las Lozas&quot;. The mountain is often referred to as Ojos del Salado and Ojos del Salado; the former is a common term for &quot;mountain&quot; in Chile and the latter means &quot;snowy&quot;, referring to snow-covered mountains.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
The melting of the ice is expected to produce an increased discharge at first, but eventually ice diminishes to the point that runoff will decline. Penitentes have been encountered by climbers as early as 1937, in 1949 there were reportedly high penitentes on Ojos del Salado. Penitentes are high ice spires which form when ice sublimates in the intense insolation. Subsurface ice.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Penitentes are high ice spires which form when ice sublimates in the intense insolation. Subsurface ice. Ice buried beneath sand and encased in moraines is more important than surface ice at Ojos del Salado. It is retreating but the insulating effect of the cover slows the retreat.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Pseudokarst landforms and dolines are other structures generated by the melting of buried ice. Past glaciation. Lateral moraines altered by wind erosion occur north of Ojos del Salado and some lava flows bear traces of glaciation. Research published in 2019 found cirques and U-shaped valleys on Ojos del Salado.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Research published in 2019 found cirques and U-shaped valleys on Ojos del Salado. However, there is no evidence of Pleistocene glacier advances in the region nor any indication of a Pleistocene snowline, although cirques have been reported from Nevado Tres Cruces and some sources propose the existence of glaciers 19,000 years ago.

Geographic entities mentioned:
surface_form: tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
surface_form: nevado tres cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
Volcanism in the region commenced 26 million years ago, when the Farallon Plate broke up and subduction speed increased. Initially between 26 and 11 million years ago activity was concentrated in the Maricunga region west of the Ojos del Salado region, where only small-volume volcanism took place and which constituted the back-arc to the Maricunga arc.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
During the Quaternary, volcanism formed the edifices of Cerro Solo, El Fraile, Incahuasi, El Muerto, El Muertito, Falso Azufre, Nevado San Francisco, Nevado Tres Cruces and Ojos del Salado, which together cover over half of the area. Apart from the large volcanoes, many smaller mafic monogenetic volcanoes developed in the area, especially east of Ojos del Salado.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Apart from the large volcanoes, many smaller mafic monogenetic volcanoes developed in the area, especially east of Ojos del Salado. Pleistocene volcanism was limited to the Ojos del Salado area, where recent faulting offset volcanic rocks. The large dimensions of Ojos del Salado indicate that magmatism was focused here. Composition.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Eruption history. Volcanic activity probably commenced 3.3–1.5 million years ago or during the late Pleistocene. The 3.7±0.2 million years old Las Lozas Andesite may have been a precursor of Ojos del Salado. The oldest rocks of Ojos del Salado are 3.5–3.4 million years old dacites in the lower parts of the volcano.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Ojos del Salado may or may not have produced pyroclastic flows; the neighbouring Nevado Tres Cruces 67,000 years ago produced extensive deposits on and around Ojos del Salado and in the valley between the two volcanoes; these were originally interpreted to have originated at Ojos del Salado.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Vegetation and fauna. Due to the dry climate, the region is a desert with little vegetation occurring above elevation, and none above. However, lichens and mosses have been found at higher elevations and green growths have been reported from the summit region., there were no reports of plants in the waterbodies on Ojos del Salado.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
However, lichens and mosses have been found at higher elevations and green growths have been reported from the summit region., there were no reports of plants in the waterbodies on Ojos del Salado. Salt, acid and cold-tolerant bacteria have been recovered from sediments in the lakes on Ojos del Salado, consistent with microorganism samples from similar dry volcanic environments.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Birds such as ducks, flamingos and geese and mammals such as guanacos and vicuñas occur in the Santa Rosa-Maricunga-Negro Francisco region. Chinchillas and vicuñas live in the valleys south of Ojos del Salado, and have drawn humans to the region. Mice venture to elevations of, and earwigs have been observed at elevation. Human history.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
The positions and names of the mountains were frequently confused. The Inca used the Paso San Francisco as a major crossing of the Andes but there is no evidence of them building any structures on Ojos del Salado even though a number of such sites exist in the surrounding region. The Spanish conquistador Diego de Almagro crossed the Andes at Ojos del Salado but did not mention it.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Ascents and debate on elevation. In 1896, 1897 and 1903 the Chile-Argentina boundary commission identified a peak in the area and named it &quot;Ojos del Salado&quot;; according to a myth their &quot;Ojos del Salado&quot; was a much smaller mountain and the actual Ojos del Salado was their &quot;Peak 'e'&quot;.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
The Polish climbers and Jan Szczepański from the Second Polish Andean Expedition reached the summit on February 26, 1937 and left a cairn but most of the maps and report they drafted were lost during World War II. After the Polish expedition, the mountain remained unclimbed until 1955, although expeditions went to its lower slopes and sometimes confused other peaks for Ojos del Salado.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
After the Polish expedition, the mountain remained unclimbed until 1955, although expeditions went to its lower slopes and sometimes confused other peaks for Ojos del Salado. In that year an expedition from Tucumán ascended a mountain south of Ojos del Salado, which they mistook for the volcano. They stated that the peak may be higher than Aconcagua, which media reported as if it were proven fact.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Three separate Chilean, Argentine and Austrian parties went to Ojos del Salado in 1956; the Chilean party measured an elevation of with a barometer, a value that was once again presented as proven by the press despite the unreliability of this technique. The Chilean party also claimed seeing the Argentine pampa and the Pacific Ocean from the summit.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
The Chilean party also claimed seeing the Argentine pampa and the Pacific Ocean from the summit. In 1957, the official elevation of Ojos del Salado was according to Argentina and according to Chile. The debate on the elevation and confusion about which mountain was Ojos del Salado and who climbed which peak prompted an expedition by the American Alpine Club in 1956.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
The debate on the elevation and confusion about which mountain was Ojos del Salado and who climbed which peak prompted an expedition by the American Alpine Club in 1956. The expedition was hindered by bad weather conditions and a gust of wind stretching a measurement line may have almost frustrated the goal to determine the summit elevation of Ojos del Salado.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Mountaineering and tourism. Ojos del Salado and the surrounding mountains draw fewer mountaineers than Aconcagua, with only several hundred climbers every year. Since the 1990s commercial tours have become important facilitators for ascents, and the number of climbers has increased in the 21st century.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
A dirt road departing from the highway to Paso San Francisco heads south to Ojos del Salado, past Refugio Murray to the bivouac Refugio Universidad de Atacama/Jorge Rojas at elevation, from there a path goes to Refugio Tejos at elevation and eventually to the summit of Ojos del Salado through scree-covered slopes and a steep ridge/couloir at the end. Ropes and supports are available.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
The mountain is also accessible by vehicle, up to or elevation, through a dirt road built after a helicopter accident in 1994. West of the volcano lies the Nevado Tres Cruces National Park and in 1991/1994 there were plans to make a national park on the Argentine side as well., the establishment of a &quot;zone of touristic interest&quot; encompassing Ojos del Salado was under discussion in Chile.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Other uses. Astronomers have surveyed the volcano for the possibility of creating an observatory there. The landforms such as the gullies and crater lakes and their conditions, and climatic conditions around Ojos del Salado have also led researchers to investigate it as a potential analogue to environments on Mars. The volcano is one of several depicted on Chilean passports.

Geographic entities mentioned:
surface_form: ojos del salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Distribution. &quot;Malosma laurina&quot; is distributed along the southern California coastline (primarily from Point Conception south to La Paz), and on several of the Channel Islands lying off the coast. Several records of the species have also been made north of Point Conception, around the city of Arroyo Grande, California. &quot;Malosma laurina&quot; is not frost-hardy.

Geographic entities mentioned:
surface_form: Point Conception
instance_of: Landform
countries: United States
coordinates: lat: 34.448113
lon: -120.471439
On the second landing, they became stuck, provoking Yeager to fits of laughter. On May 21, 1962, Armstrong was involved in the &quot;Nellis Affair&quot;. He was sent in an F-104 to inspect Delamar Dry Lake in southern Nevada, again for emergency landings. He misjudged his altitude and did not realize that the landing gear had not fully extended.

Geographic entities mentioned:
surface_form: Delamar Dry Lake
instance_of: Lake
countries: United States
coordinates: lat: 37.320519444444
lon: -114.94861944444
Bob Gilruth approved my decision.&quot;
Voyage to the Moon. A Saturn V rocket launched Apollo 11 from Launch Complex 39A at the Kennedy Space Center on July 16, 1969, at 13:32:00 UTC (09:32:00 EDT local time). Armstrong's wife Janet and two sons watched from a yacht moored on the Banana River. During the launch, Armstrong's heart rate peaked at 110beats per minute.

Geographic entities mentioned:
surface_form: Banana River
instance_of: Landform
countries: United States
coordinates: lat: 28.4560146
lon: -80.6276321
Ropata Wahawaha (– 1 July 1897) was a Māori military leader and &quot;rangatira&quot; (chief) of the Ngāti Porou &quot;iwi&quot; (tribe) who rose to prominence during New Zealand's East Cape War and Te Kooti's War. Born in 1820 in the Waiapu Valley on the East Cape, he was enslaved as a boy and became known as Rāpata Wahawaha. He later obtained his freedom and as an adult, became known as Ropata.

Geographic entities mentioned:
surface_form: Waiapu Valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -37.9833
lon: 178.117
In his later years, he commanded the militia in the Ngāti Porou district, was a land agent and a member of the Legislative Council. Early life. Rāpata Wahawaha was born about 1820 either in Te Puia Springs or Akuaku, in the Waiapu Valley on the East Cape. He was the son of Hīpora Koroua and Te Hapamana Te Whao.

Geographic entities mentioned:
surface_form: Waiapu Valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -37.9833
lon: 178.117
Ropata continued to lead his war party south, this time in assistance of the Ngāti Kahungunu &quot;iwi&quot;, which was aligned with the Government. In January 1866, he and 150 Ngāti Porou landed at Wairoa. Together with 150 militia and 250 warriors from Ngāti Kahungunu &quot;iwi&quot;, they pushed towards Lake Waikaremoana in pursuit of the Hauhau.

Geographic entities mentioned:
surface_form: Lake Waikaremoana
instance_of: Lake
countries: New Zealand
coordinates: lat: -38.766666666667
lon: 177.08333333333
It consists of three fused pillars, one with a circular hole near the top. This is a few km NE of the Nourlangie Rock tourist site to the east of Koongarra saddle. Namarggon left one eye (the hole) to watch for the monsoon, but also to watch his estranged wife, whose home is a cave in a pillar near Koongarra.

Geographic entities mentioned:
surface_form: Nourlangie
instance_of: Mountain
countries: Australia
coordinates: lat: -12.8617
lon: 132.812
Geology. Pukemokemoke hill is formed of greywacke of the Jurassic Manaia Hill Group (shown as Jm on map). The rest of the Whitikahu area is largely on a drained peat bog, which lies on ash from Lake Taupō. Taupiri Fault is an inferred fault separating the peat from the Taupiri Range. Seismic testing in 2017 added evidence of the fault's position.

Geographic entities mentioned:
surface_form: Taupiri
instance_of: Mountain
countries: New Zealand
coordinates: lat: -37.603
lon: 175.186389
Taupiri Fault is an inferred fault separating the peat from the Taupiri Range. Seismic testing in 2017 added evidence of the fault's position. Whitikahu is at the north end of an alluvial fan of the ash, which drops about 60 m (200 ft) from Karapiro. After the Oruanui eruption, some 26,500 years ago, Lake Taupō was about 145 m (476 ft) above the present lake.

Geographic entities mentioned:
surface_form: Karapiro
instance_of: Lake
countries: New Zealand
coordinates: lat: -37.943167
lon: 175.560833
Its main purpose is to serve the town of Grand Bay-Westfield. Route 177 is a former alignment of Route 7 and is 19.6 kilometres long. The southern end of Route 177 is at Route 7 exit 90 at Crane Mountain in the city of Saint John. The road runs northeast to the Westfield Road, the original road built along the Saint John River.

Geographic entities mentioned:
surface_form: Crane Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.06281835
lon: -120.24083202
Maunganui Bluff. Maunganui Bluff is a prominent coastal bluff located on the west coast of New Zealand's North Island, in the Northland region. Known locally as &quot;The Bluff&quot;, it is set in a scenic reserve and rises above sea level. Maunganui Bluff marks the northern extent of long Ripiro Beach (the longest unbroken beach in New Zealand). Etymology.

Geographic entities mentioned:
surface_form: maunganui
instance_of: Mountain
countries: New Zealand
coordinates: lat: -35.75801
lon: 173.562514
Geology. Studies using remote sensing indicate these basalt layers form part of an eroded basalt shield volcano, originally centered about 10 kilometers west of Maunganui Bluff, with an estimated width of 50 kilometers. Comparatively, other Miocene basalt shield volcanoes, such as those at Banks Peninsula, Dunedin, and the Auckland Islands, each spanned roughly 20 to 30 kilometers.

Geographic entities mentioned:
surface_form: maunganui
instance_of: Mountain
countries: New Zealand
coordinates: lat: -35.75801
lon: 173.562514
Sovetskaya (lake). Sovetskaya Lake is a liquid subglacial lake found buried under the Antarctic ice sheet, below Sovetskaya Research Station. It covers about.

Geographic entities mentioned:
surface_form: sovetskaya
instance_of: Lake
coordinates: lat: -77.966666666667
lon: 89.266666666667
Sovetskaya (lake). Sovetskaya Lake is a liquid subglacial lake found buried under the Antarctic ice sheet, below Sovetskaya Research Station. It covers about.

Geographic entities mentioned:
surface_form: sovetskaya
instance_of: Lake
coordinates: lat: -77.966666666667
lon: 89.266666666667
surface_form: sovetskaya
instance_of: Lake
coordinates: lat: -77.966666666667
lon: 89.266666666667
Darkness and a lack of sunlight are common features associated with the underworld and, in this way, provide a direct contrast to both the 'normality' of the land of the living (where the sun shines) and also with the brightness associated with Mount Olympus (the realm of the gods).

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
It flows roughly northeastwards in its upper and middle course, parallel to the Teneke. As it reaches its last stretch the river divides into branches and bends northwards to the west of lake Zhalauly. In periods of adequate rainfall the river flows into the endorheic lake Siletiteniz from its southern end, but in dry years it doesn't reach the lake.

Geographic entities mentioned:
surface_form: Zhalauly
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.866461
lon: 74.119547
As it reaches its last stretch the river divides into branches and bends northwards to the west of lake Zhalauly. In periods of adequate rainfall the river flows into the endorheic lake Siletiteniz from its southern end, but in dry years it doesn't reach the lake. The main tributaries of the Sileti are Koyandy, Akzhar, Zhartas, Kedey, Sholakkarasu and Shili.

Geographic entities mentioned:
surface_form: Siletiteniz
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 53.339722222222
lon: 73.166666666667
In November of that year, he obtained command of the &quot;Granatieri di Sardegna&quot; Brigade, replacing General Luigi Pirzio Biroli. The grenadiers under his orders distinguished themselves at &quot;Altitude 188&quot;, in front of Gorizia, and then in the defense of Monte Cengio, during the very hard and bloody Battle of Asiago on June 3, 1916.

Geographic entities mentioned:
surface_form: Monte Cengio
instance_of: Mountain
countries: Italy
coordinates: lat: 45.8112
lon: 11.395
After participating in the Sixth (August 6–17), and Seventh Battle of the Isonzo from September 14 to 18, on December 4. he transferred command of the brigade to Colonel Brigadier Giovanni Albertazzi, and on September 21, he assumed the post of Chief of Staff of the 4th Army, cooperating in the defense of Cadore and the defensive actions of the Fasso Alps, to then move on to that of the 3rd Army.

Geographic entities mentioned:
surface_form: Cadore
instance_of: Valley
countries: Italy
coordinates: lat: 46.50916667
lon: 12.35722222
Tourism. Attractions included the beach, boating on Lake Annecy, walking in the hills, including Mount Rampon (957 m), Mont Veyrier (1291 m) and Mount Rampignon (894 m). Annual events included the &quot;Ancilevienne&quot;, a race for teams of runners and cyclists around Lake Annecy, and the Gabriel Fauré music festival.

Geographic entities mentioned:
surface_form: Mont Veyrier
instance_of: Mountain
countries: France
coordinates: lat: 45.9006
lon: 6.1825
The joint venture was formed in April 1993, when the government of Kazakhstan granted exclusive 40-year rights to Tengizchevroil LLP (TCO) to develop the Tengiz and Korolevskoye oil fields located in the north-eastern reaches of the Caspian Sea in Kazakhstan. History and operations.

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