Sarmila/GeoWiki-Features huggingface dataset:
It rises in the southeastern quarter of the French Massif Central in the Cévennes range (in the department of Ardèche) at near Mont Gerbier de Jonc; it flows north through Nevers to Orléans, then west through Tours and Nantes until it reaches the Bay of Biscay (Atlantic Ocean) at Saint-Nazaire.

Geographic entities mentioned:
surface_form: Mont Gerbier de Jonc
instance_of: Mountain
countries: France
coordinates: lat: 44.84462222
lon: 4.220275
Geography. The source of the river lies in the eastern Massif Central, in springs to the south side of Mont Gerbier de Jonc at. This lies in the north-eastern part of the southern Cévennes highlands, in the Ardèche commune of Sainte-Eulalie of southeastern France. It is originally a mere trickle of water located at above sea-level.

Geographic entities mentioned:
surface_form: Mont Gerbier de Jonc
instance_of: Mountain
countries: France
coordinates: lat: 44.84462222
lon: 4.220275
Three days after the attack, he visited the Israel-Jordan border at the Jordan Valley and promised to construct, in cooperation with all parties, a stronger barrier in order to fight smuggling. Hamas. Hamas praised the attack and said it was &quot;executed by a fearless Jordanian individual.&quot;
Kata'ib Hezbollah.

Geographic entities mentioned:
surface_form: Jordan Valley
instance_of: Valley
countries: Jordan
coordinates: lat: 32.317222
lon: 35.57
However, when the Belgian Consul in Egypt arrived in Gondar to negotiate with the &quot;Ras&quot;, a messenger of Muhammad came to him carrying the following message signed with the seal of the Pasha:Do not fear, your friends will be my friends and your enemies will be my enemies.His words did not match his actions as later Muhammad Ali would dispatch the Egyptian army to Wehni to take advantage of the Ethiopians who were in a difficult situation with internal matters.

Geographic entities mentioned:
surface_form: Wehni
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 12.148333333333
lon: 37.766388888889
Once the news of Massawa had reached Wube, he had surrendered to the &quot;Ras&quot; and was paid tribute. After the crisis was over, Mennen rushed quickly into Gondar and soon afterwards followed a retreating army of Kassa in the direction of the northern shores of Lake Tana.

Geographic entities mentioned:
surface_form: Lake Tana
instance_of: Lake
countries: Ethiopia
coordinates: lat: 12
lon: 37.25
Distribution. As the name suggests, &quot;C. chimalapensis&quot; is native to Oaxaca, Mexico. It is primarily concentrated within the cloud forests that cover the slopes of the Chimalapas mountains, characterized by persistent cloud cover and high humidity levels. This species is typically found at elevations between 800 and 1,500 meters above sea level.

Geographic entities mentioned:
surface_form: Oaxaca, Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 17.045
lon: -96.7669
Maling River. Maling River () is a river in northern Lipu, in Guangxi, China. It is long and is a tributary of the Lipu River, draining an area of. It rises in northwestern Lipu, and flows generally southeast, passing through the towns of Hualong, Shuangjiang and Maling and joining the Lipu River in the town of Dongchang.

Geographic entities mentioned:
surface_form: Lipu River
instance_of: Watercourse
countries: People's Republic of China
Wasenhorn (Bernese Alps). The Wasenhorn is a mountain of the Bernese Alps, located north of Blitzingen in the canton of Valais. It lies on the range south of the Oberaarrothorn, that separates the valley of the Fiescher Glacier from the main Rhone valley.

Geographic entities mentioned:
surface_form: Oberaarrothorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.520388888889
lon: 8.1809166666667
Wasenhorn (Bernese Alps). The Wasenhorn is a mountain of the Bernese Alps, located north of Blitzingen in the canton of Valais. It lies on the range south of the Oberaarrothorn, that separates the valley of the Fiescher Glacier from the main Rhone valley.

Geographic entities mentioned:
surface_form: wasenhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.497972222222
lon: 8.1657777777778
Kuta (river). The Kuta is a Siberian river north of Lake Baikal in Irkutsk Oblast, Russia, that flows into the Lena at Ust-Kut. With its right tributary, the Kupa, it forms a ‘T’ shape with the flat head pointing west and the point at Ust-Kut. The river is long and its basin is about. Course. Its source is about above sea level and its mouth.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
He finally served three years in the British East Africa Forest Service, from which he retired as Chief Conservator of Forests. In 1908 and 1909, he explored the forests around Mount Kenya.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
In 2002, he photographed Cuba, comparing what he found there to the Puerto Rico of his youth. He has exhibited photographs showing the dignity of the Dalit (&quot;Untouchable&quot;) Caste of India and the Aymara living in the arid altiplano of Bolivia. He has also photographed people from Kenya to Turkey to Thailand. His work has been featured in the April 2008 issue of Rangefinder magazine.

Geographic entities mentioned:
surface_form: altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Hornavanskolan. Hornavanskolan is a secondary school in Arjeplog Municipality in Sweden. The school was founded in 1993 and is located by Hornavan, the deepest lake in Sweden.

Geographic entities mentioned:
surface_form: Hornavan
instance_of: Lake
countries: Sweden
coordinates: lat: 66.233333333333
lon: 17.5
He had a talent for orienting himself in difficult, rocky areas, and for mountaineering. He pioneered several routes in the Tatras. These included the descent of the northern wall of Lomnický štít (1888), and the first ascents of, among others, (1892), (1895), (1902), (1904), (1904) and (1904). He made the second ascents of Mnich and.

Geographic entities mentioned:
surface_form: Lomnický štít
instance_of: Mountain
countries: Slovakia
coordinates: lat: 49.2
lon: 20.212777777778
He made the second ascents of Mnich and. He took part in the first winter ascents of (1905) (below Gerlachovský štít, the highest peak in the High Tatras), and of Bystrá (the highest peak in the Western Tatras). He climbed in groups roped together from as early as 1900. He was the first Tatra highlander to learn to ski (no later than 1902).

Geographic entities mentioned:
surface_form: Gerlachovský štít
instance_of: Mountain
countries: Slovakia
coordinates: lat: 49.16416666666667
lon: 20.13388888888889
He climbed in groups roped together from as early as 1900. He was the first Tatra highlander to learn to ski (no later than 1902). In 1901, (1871-1959, mathematician and statistician) named (), one of the passes between and Lomnický štít, in Bachleda's honour. He has more than ten (one source says fifteen) features in the Tatras named after him, including, the easternmost peak of.

Geographic entities mentioned:
surface_form: Lomnický štít
instance_of: Mountain
countries: Slovakia
coordinates: lat: 49.2
lon: 20.212777777778
On 7 March 1975, the lake and its surroundings were declared a national nature monument with an area of. The zone around it is subject of restrictions. There were recorded 16 species of freshwater molluscs in the Odlezelské jezero National Nature Monument in 2013–2023. That includes 8 species of freshwater gastropods and 8 species of bivalves.

Geographic entities mentioned:
surface_form: odlezelské jezero
instance_of: Lake
countries: Czech Republic
coordinates: lat: 50.016111111111
lon: 13.373055555556
Odlezly Lake. Odlezly Lake (, sometimes &quot;Mladotické-&quot; or &quot;Potvorovské-&quot;) is the youngest lake in the Czech Republic. The lake and its surroundings is protected as a national nature monument. The lake is located near the village of Odlezly within the municipality of Žihle, under the hill Potvorovský (546 m). Two creeks discharge here: Mladotický and Odlezelský.

Geographic entities mentioned:
surface_form: odlezly lake
instance_of: Lake
countries: Czech Republic
coordinates: lat: 50.016111111111
lon: 13.373055555556
The zone around it is subject of restrictions. There were recorded 16 species of freshwater molluscs in the Odlezelské jezero National Nature Monument in 2013–2023. That includes 8 species of freshwater gastropods and 8 species of bivalves. 13 species of freshwater molluscs were found in the Odlezly Lake.

Geographic entities mentioned:
surface_form: odlezly lake
instance_of: Lake
countries: Czech Republic
coordinates: lat: 50.016111111111
lon: 13.373055555556
He served in the Second World War. On 24 September 1939, he was appointed Commander of 3rd Jhelum Brigade, then as Commander of the Calcutta Brigade, and finally as Commander of 19th Indian Infantry Brigade in Deccan District in India. He was made Commander of British Troops in China in August 1941. He was unimpressed when he assumed the post on 19 July 1941.

Geographic entities mentioned:
surface_form: Deccan District
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Origin. There are multiple variations of Mama Ocllo's origin. One common version involves Mama Ocllo emerging with Manco Cápac from an island or cave in Lake Titicaca after Inti created them, though in some alternate versions, the rest of their siblings, as well as ten ayllus, rise from the lake, too, and they all journey together for a short time.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Doctors Lake (Florida). Doctors Lake is a body of water located off the St. Johns River in Clay County, Florida. Despite its name, it is not a true lake, as it is actually an inlet, openly connected to the St. Johns. Because of the estuarine nature of the St. Johns, Doctors Lake is itself somewhat brackish.

Geographic entities mentioned:
surface_form: doctors lake
instance_of: Lake
countries: United States
coordinates: lat: 30.152777777778
lon: -81.706388888889
Doctors Lake is a body of water located off the St. Johns River in Clay County, Florida. Despite its name, it is not a true lake, as it is actually an inlet, openly connected to the St. Johns. Because of the estuarine nature of the St. Johns, Doctors Lake is itself somewhat brackish. Many docks border the lake for recreational activity such as boating, fishing and waterskiing.

Geographic entities mentioned:
surface_form: doctors lake
instance_of: Lake
countries: United States
coordinates: lat: 30.152777777778
lon: -81.706388888889
To the south, the lake splits in half into two small creeks that flow from swampland. History. Zephaniah Kingsley originally owned much of the land around Doctors Lake, and established the Laurel Grove Plantation there in the early 1800s. Kingsley captained a ship in the West Indies and was absent from the plantation much of the time.

Geographic entities mentioned:
surface_form: doctors lake
instance_of: Lake
countries: United States
coordinates: lat: 30.152777777778
lon: -81.706388888889
Kingsley later married the girl and had four children. The community at the north end of the inlet to Doctors Lake is today named &quot;Laurel Grove&quot;, while &quot;Kingsley&quot; is a major street in nearby Orange Park. Geography. Doctors Lake has an area of 13 mi2 (34 km2). It is linked to the St. Johns River by Doctors Inlet. U.S.

Geographic entities mentioned:
surface_form: doctors lake
instance_of: Lake
countries: United States
coordinates: lat: 30.152777777778
lon: -81.706388888889
surface_form: doctors lake
instance_of: Lake
countries: United States
coordinates: lat: 30.152777777778
lon: -81.706388888889
Some older inactive volcanoes are well-preserved owing to the dry climate of the region. Many of these volcanoes are in remote regions and thus are poorly studied, but pose little threat to humans. The largest historical eruption in the Central Volcanic Zone occurred in 1600 at Huaynaputina in Peru, and the recently most active volcano is Lascar in Chile.

Geographic entities mentioned:
surface_form: Huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223
Its volume is about, making Socompa one of the largest stratovolcanoes with Quaternary activity. The volcano apparently developed within a northwest-striking valley, the southern part of which now contains Laguna Socompa. This lake lies at an elevation of; to the north the volcano is bordered by the high Monturaqui basin. The water table is at depths of, but surface runoff is only ephemeral.

Geographic entities mentioned:
surface_form: Laguna Socompa
instance_of: Lake
countries: Argentina
coordinates: lat: -24.53333
lon: -68.21667
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
The collapse happened about years ago and is estimated to have lasted around 12 minutes, based on simulations. The growth rate of the volcano increased, in the aftermath probably due to the mass removal unloading the magmatic system. A similar collapse took place in the 1980 eruption of Mount St. Helens.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
A similar collapse took place in the 1980 eruption of Mount St. Helens. Identification of the Socompa deposit as a landslide remnant was made after the occurrence of the large landslide at Mount St. Helens drew more attention to such events. Other volcanoes have suffered from large-scale collapses as well; this includes Aucanquilcha, Lastarria and Llullaillaco.

Geographic entities mentioned:
surface_form: Aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
surface_form: Lastarria
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -25.166666666667
lon: -68.5
surface_form: Llullaillaco
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.719863
lon: -68.536852
surface_form: llullaillaco
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.719863
lon: -68.536852
Landslide deposit. The collapse deposit covers a surface area of, and is thus not as large as the deposit left by the Mount Shasta or Nevado de Colima collapses. The deposit forms the Negros de Aras (also a name for the deposit) surface northwest of the volcano and the El Cenizal surface due north, where it has a hook-like surface distribution.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Around the same epoch, after the Eocene, the subduction angle increased beneath the Altiplano and caused the development of this plateau either from magmatic underplating and/or from crustal shortening; eventually the crust there became much thicker. Local.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
The presence of two calderas southeast and east of Socompa has been inferred. Monogenetic volcanoes were active in the area as well during the Pliocene and Quaternary and generated lava flows. One of these centres is El Negrillar just north of the collapse deposit, which was active during the Pleistocene and issued andesite-basaltic andesite lavas unlike the eruption products of Socompa itself.

Geographic entities mentioned:
surface_form: El Negrillar
instance_of: Mountain
countries: Chile
coordinates: lat: -24.18
lon: -68.25
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
A elongated geologic structure (a lineament) known as the Socompa Lineament is associated with the volcano. Other volcanoes such as Cordon de Puntas Negras and the rim of the large La Pacana caldera farther north are also influenced by this lineament. A north-south trending lineament called the Llullaillaco Lineament is also linked to Socompa and to the Mellado volcano farther south.

Geographic entities mentioned:
surface_form: La Pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
The basement rocks are subdivided into three named formations, the Purilactis Formation of Paleozoic–Mesozoic age, the San Pedro and Tambores formations of Oligocene–Miocene age and the Miocene–Pliocene Salin formation; part of the latter formation may have been erupted by Socompa itself. The volcano is at the point where the Sierra de Alameida meets the Puna block.

Geographic entities mentioned:
surface_form: Puna
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Socompa. Socompa is a large stratovolcano (composite volcano) on the border of Argentina and Chile. It has an elevation of and is part of the Chilean and Argentine Andean Volcanic Belt (AVB). Socompa is within the Central Volcanic Zone, one of the segments of the AVB, which contains about 44 active volcanoes. It begins in Peru and runs first through Bolivia and Chile, and then Argentina and Chile.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
It begins in Peru and runs first through Bolivia and Chile, and then Argentina and Chile. Socompa lies close to the pass of the same name where the Salta-Antofagasta railway crosses the Chilian border. Most of the northwestern slope of Socompa collapsed catastrophically 7,200 years ago to form an extensive debris avalanche deposit.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
Socompa lies close to the pass of the same name where the Salta-Antofagasta railway crosses the Chilian border. Most of the northwestern slope of Socompa collapsed catastrophically 7,200 years ago to form an extensive debris avalanche deposit. The Socompa collapse is among the largest known on land with a volume of and a surface area of; its features are well-preserved by the arid climate.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
After the landslide, the volcano was rebuilt by the effusion of lava flows and much of the scar is now filled in. Socompa is also noteworthy for the high-altitude biotic communities that are bound to fumaroles on the mountain. They are well above the sparse regular vegetation in the region, which does not extend up the mountains. The climate on the mountain is cold and dry.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
The climate on the mountain is cold and dry. Geography and geomorphology. Socompa is on the border between Argentina and Chile, east-southeast of the Monturaqui railway station of the Salta–Antofagasta railway. The railway crosses the border between the two countries just below Socompa, making the volcano easily accessible despite its remote location.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
The same pass was an important route between the two countries and reportedly between 1940 and 1970 the Carabineros de Chile had a post there. Rails and roads at Socompa go up to an elevation of; from there the volcano can be climbed from its southern, eastern and northern flank.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
This lake lies at an elevation of; to the north the volcano is bordered by the high Monturaqui basin. The water table is at depths of, but surface runoff is only ephemeral. Magnetotelluric investigation has identified a structure at depth which may be Socompa's magma chamber. Sector collapse.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
The deposit left by the collapse was first discovered on aerial photography in 1978 but it was correctly identified as a landslide in 1985; at first, it was interpreted as a form of moraine, then as a large pyroclastic flow and the scar as a caldera. Traces of such events are widespread on Central Andean volcanoes; Socompa's is the largest in the region and one of the better studied.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
Traces of such events are widespread on Central Andean volcanoes; Socompa's is the largest in the region and one of the better studied. The event removed a 70° sector (about of circumference and of radius) on Socompa's northwestern side. The landslide descended over a vertical distance of about and spread over distances of over, at a modelled speed of.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
The precise circumstances leading to the collapse are unknown, although there are several hypotheses. There is evidence in the deposit that a lava flow was being erupted on the volcano when the landslide occurred, which together with the presence of pyroclastic fallout on the southwestern side of Socompa implies the event may have been started by volcanic activity.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
The quantity of water in the edifice rocks was probably minor. Another theory assumes that the volcanic edifice was destabilized by ductile and mechanically weak layers beneath Socompa; under the weight of the volcano these layers can deform and &quot;flow&quot; outward from the edifice, causing the formation of thrusts at its foot.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
Another theory assumes that the volcanic edifice was destabilized by ductile and mechanically weak layers beneath Socompa; under the weight of the volcano these layers can deform and &quot;flow&quot; outward from the edifice, causing the formation of thrusts at its foot. Evidence of such spreading of the basement under Socompa has been found.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
These blocks form an almost closed semicircle at the mouth of the collapse amphitheatre and in part retain the previous stratigraphy of the volcano. Such toreva blocks are far more frequent in submarine landslides than subaerial ones and their occurrence at Socompa may reflect the relatively non-explosive nature of the collapse and material properties of the collapsed mass.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
Local. Socompa forms a northeast-trending alignment with neighbouring volcanoes such as Pular and Pajonales, which reach elevations of about; Socompa is their youngest member. The presence of two calderas southeast and east of Socompa has been inferred. Monogenetic volcanoes were active in the area as well during the Pliocene and Quaternary and generated lava flows.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
One of these centres is El Negrillar just north of the collapse deposit, which was active during the Pleistocene and issued andesite-basaltic andesite lavas unlike the eruption products of Socompa itself. A elongated geologic structure (a lineament) known as the Socompa Lineament is associated with the volcano.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
A elongated geologic structure (a lineament) known as the Socompa Lineament is associated with the volcano. Other volcanoes such as Cordon de Puntas Negras and the rim of the large La Pacana caldera farther north are also influenced by this lineament. A north-south trending lineament called the Llullaillaco Lineament is also linked to Socompa and to the Mellado volcano farther south.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
surface_form: llullaillaco
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.719863
lon: -68.536852
To the west Socompa is bordered by the Sierra de Alameida (or Almeida), which farther north merges into the Cordon de Lila. To the east the high Salín volcano neighbours Socompa; other volcanoes in the area are the Cerro Bayo and the Socompa Cairis, all of which show evidence of glacial activity unlike the younger Socompa. Basement.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
Basement. The basement at Socompa is formed by Paleozoic and Mesozoic formations and by Quaternary sedimentary and volcanic rocks. The former crop out in the Sierra de Alameida and Alto del Inca west of Socompa and the latter as the Quebrada Salin Beds east of the volcano.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
The former crop out in the Sierra de Alameida and Alto del Inca west of Socompa and the latter as the Quebrada Salin Beds east of the volcano. Part of these beds were taken up into the avalanche as it collapsed and form the Flexura inliner, others appear in the Loma del Inca area north and the Monturaqui area due west of Socompa.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
The basement rocks are subdivided into three named formations, the Purilactis Formation of Paleozoic–Mesozoic age, the San Pedro and Tambores formations of Oligocene–Miocene age and the Miocene–Pliocene Salin formation; part of the latter formation may have been erupted by Socompa itself. The volcano is at the point where the Sierra de Alameida meets the Puna block.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
The volcano is at the point where the Sierra de Alameida meets the Puna block. During the Pliocene this basement was covered by the Arenosa and Tucucaro ignimbrites (2.5 and 3.2 million years ago by potassium–argon dating, respectively) which also crop out west of Socompa; Socompa is probably constructed on top of these ignimbrites.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
The Arenosa ignimbrite is about thick, and the Tucucaro reaches a thickness of. Some normal faults appear in the area north of Socompa and appear to run through the edifice. Although they are not visible in the edifice itself, Socompa was uplifted on its southeastern side by the fault motion. This might have aided in the onset of edifice instability and the collapse event.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
Although they are not visible in the edifice itself, Socompa was uplifted on its southeastern side by the fault motion. This might have aided in the onset of edifice instability and the collapse event. Directly north-northwest of Socompa lie three anticlines probably formed under the influence of the mass of both Socompa and Pajonales: The Loma del Inca, Loma Alta and La Flexura. Composition.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
The present-day precipitation has been estimated to be, with other estimates assuming less than. Periglacial landforms indicate that in the past the area was wetter, possibly thanks to the Little Ice Age. The last ice age in the region ended 12,000-10,000 years ago; there is no evidence for Pleistocene glaciation on Socompa, including no cirques, which may be due to the volcano's young age.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
The last ice age in the region ended 12,000-10,000 years ago; there is no evidence for Pleistocene glaciation on Socompa, including no cirques, which may be due to the volcano's young age. Socompa features autotrophic communities associated with fumaroles and thermal anomalies at high altitude, between of elevation.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
The autotrophic communities on Socompa are the highest known in the world, and they occur both on the actual fumaroles, on &quot;cold fumaroles&quot; and at a few metres from the vents. The different species are often extremophiles since the environment on Socompa is harsh, and the communities also include heterotrophic species.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
There is a noticeable diversity between separate stands, and the vegetation is quite dissimilar to the vegetation in the surroundings but resembles that found in the paramo and cloud forests in South America and the subantarctic islands. A sparse vegetation cover is also found on the lower slopes of Socompa.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
The black-headed lizard and its relative &quot;Liolaemus porosus&quot; live on its slopes, and mice have been observed in the summit area. Eruptive history. Activity at Socompa commenced with the extrusion of andesites, which were followed later by dacites. Several Plinian eruptions have occurred from Socompa; one Holocene eruption reached a volcanic explosivity index of 5.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
Several Plinian eruptions have occurred from Socompa; one Holocene eruption reached a volcanic explosivity index of 5. Several dates have been obtained on rocks, including 2,000,000 ± 1,000,000, 1,300,000 ± 500,000, 800,000 ± 300,000 and less than 500,000 years ago. An age of 3,340,000 ± 600,000 years may be of an older volcano, now buried beneath the Socompa edifice.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
Lava domes and lava flows on the southern side of the volcano have yielded ages of 69,200 ± 6,000, 31,400 ± 3,200, 29,800 ± 3,300 and 22,100 ± 1,900 years ago. An eruption 7,220 ± 100 years before present produced the El Túnel pyroclastic deposit on the western side of Socompa. After the sector collapse 7,200 years ago, activity continued filling the collapse scar.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
After the sector collapse 7,200 years ago, activity continued filling the collapse scar. The explosion craters on the summit are the youngest volcanic landforms on Socompa. One dome in the scar has been dated to 5,910 ± 430 years ago; the Global Volcanism Program gives 5,250 BCE as the date of the last eruption.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
there is no ground-based monitoring of the volcano. Socompa is considered to be a high-risk volcano; a 2021 survey labelled it Argentina's 13th most dangerous volcano out of 38. The area is only thinly populated, and apart from the Socompa railway station and mining camps west of the volcano, there is little infrastructure that could be impacted by future eruptions.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
Large explosive eruptions during summer may result in pyroclastic fallout west of the volcano; during the other seasons fallout would be concentrated east of it. Groundwater is warmer and richer in carbon dioxide the closer to Socompa it is pumped, also suggesting that volcanic gas fluxes still occur at the volcano and that the volcano influences groundwater systems.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
Hot springs are found at Laguna Socompa as well. In 2011, the Chilean mining company Escondida Mining was considering building a geothermal power plant on Socompa to supply energy; the Argentine Servicio Geológico Minero agency started exploration work in January 2018 for geothermal power production.

Geographic entities mentioned:
surface_form: socompa
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -24.393333333333
lon: -68.256111111111
Port Simpson), B.C. The name &quot;Gitzaxłaał&quot; means literally &quot;people of (an unidentified variety of shrub).&quot; Their traditional territory includes the watershed of the Ecstall River, a tributary of the Skeena River, including the now abandoned town, Port Essington, B.C. They also own areas on Dundas Island.

Geographic entities mentioned:
surface_form: Ecstall River
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.15836
lon: -129.94543
Two tunnels, the Main Street Tunnel and the Townline Tunnel, were constructed to allow vehicles and trains to pass beneath the canal. To complement this, an aqueduct, to convey the Welland River under the new canal alignment, was built. The aqueduct's design is what is known as a four-tube inverted-syphon culvert, long, wide, and extending below the navigation channel.

Geographic entities mentioned:
surface_form: Welland River
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.0377
lon: -79.1798
Ethel Lake (Alberta). Ethel Lake is a small lake in Alberta, Canada. It is located west of Cold Lake.

Geographic entities mentioned:
surface_form: cold lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.55009
lon: -110.00084
Ethel Lake (Alberta). Ethel Lake is a small lake in Alberta, Canada. It is located west of Cold Lake.

Geographic entities mentioned:
surface_form: ethel lake (alberta)
instance_of: Lake
countries: Canada
coordinates: lat: 54.5319
lon: -110.351
Ethel Lake (Alberta). Ethel Lake is a small lake in Alberta, Canada. It is located west of Cold Lake.

Geographic entities mentioned:
surface_form: ethel lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.5319
lon: -110.351
Despite the fact that his three sons, Johnny, Andy and Charles Jr. were all less than four years old and his wife was expecting another child, Steen borrowed $1,000 from his mother and headed for the Colorado Plateau, determined to strike it rich. After being in Colorado for several months, the Steens moved into a tarpaper shack in Cisco, Utah.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Indian Hill is located on Indian Hill Road West, positioned between Watervale Road and Pompey Center Road, approximately 0.6 miles west of Pompey Center Road. It is found between the two branches of Limestone Creek. Indian Hill is located east of Jamesville Beach Park and west of Cazenovia Lake. The marker is on Indian Hill Road with an address of 8031 Indian Hill Road, Manlius, New York 13104.

Geographic entities mentioned:
surface_form: Cazenovia Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.946621944444
lon: -75.870122222222
Hayley Mills was originally offered the role of Mary. Miriam Hopkins, who portrays Lily Mortar in the remake, appeared as Martha in &quot;These Three&quot;. Filming. The film's location shooting was done at the historic Shadow Ranch, in present-day West Hills of the western San Fernando Valley. Critical response. &quot;Variety&quot; said, &quot;Audrey Hepburn and Shirley MacLaine...

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
He responded ably and survived the attacks. He managed to settle quickly the old boundary dispute with Virginia in southwestern Pennsylvania but was never able to satisfactorily disentangle disputed titles in the Wyoming Valley resulting from prior claims of Connecticut to those lands. An exhausted Dickinson left office October 18, 1785.

Geographic entities mentioned:
surface_form: Wyoming Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
The plant grows in climates featuring hot summers, cold winters, and moderate precipitation. It is a dominant grass species in many regions, including the Nebraska Sand Hills and other sand hills, the Red River Valley, many prairies and grasslands of the Great Plains, and certain beaches along the Great Lakes, such as those at Kohler-Andrae State Park and Point Beach State Forest in Wisconsin.

Geographic entities mentioned:
surface_form: Red River Valley
instance_of: Valley
countries: Canada
United States
coordinates: lat: 49
lon: -97.5
Zone, Lombardy. Zone (Brescian:) is a &quot;comune&quot; in the province of Brescia, in Lombardy, northern Italy. It is situated in a mountain valley east of Lake Iseo. The town is known for the nearby &quot;Pyramids of Zone&quot;, formations of large rock pillars created by erosion. Its coat of arms shows three of these pillars.

Geographic entities mentioned:
surface_form: Lake Iseo
instance_of: Lake
countries: Italy
coordinates: lat: 45.711666666667
lon: 10.071944444444
Alabaster is abundant in the surrounding terrain and it has been extracted and treated for industrial and commercial use in the town of Debar. After the gorge, the Radika receives its major tributary, the Valovica river from the right and flows on the northern slopes of the Stogovo mountain.

Geographic entities mentioned:
surface_form: Stogovo
instance_of: Mountain
countries: North Macedonia
coordinates: lat: 41.4833
lon: 20.65
A week later on May 7, Sydney River McDonald's murders took place in Sydney River, Nova Scotia, Canada when a botched robbery committed by employee Derek Wood and two accomplices resulted in the murder of three employees, and the permanent disablement of a fourth employee shot in the head. On October 12, 1992, Mark Hopkins was electrocuted at McDonald's Manchester Arndale store.

Geographic entities mentioned:
surface_form: Sydney River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.1903
lon: -60.2167
Lacco Ameno. Lacco Ameno is an Italian municipality with 4,464 inhabitants, located in the Metropolitan City of Naples, on the island of Ischia. It is famous for its exclusive hotels, miraculous thermal waters, Mediterranean cuisine, and shopping.”. It is located at the feet of Mount Epomeo, facing the sea. The name most likely derives from the Greek &quot;lakkos&quot;, meaning &quot;stone&quot;.

Geographic entities mentioned:
surface_form: Mount Epomeo
instance_of: Mountain
countries: Italy
coordinates: lat: 40.7301287
lon: 13.8951395
Family. Thamyris was the son of Philammon and the nymph Argiope from Mount Parnassus. One account makes him the father of Menippe, who became the mother of Orpheus by Oeagrus. Early years. When Philammon refused to take Argiope into his house as his wife, the girl left Peloponnese and went to the country of the Odrysians in Thrace where she gave birth to a son, Thamyris.

Geographic entities mentioned:
surface_form: Mount Parnassus
instance_of: Mountain
countries: Greece
coordinates: lat: 38.533
lon: 22.6167
Orocrambus cultus. &quot;Orocrambus cultus&quot; is a moth in the family Crambidae. It was first described by Alfred Philpott in 1917 from specimens collected by Merlin Owen Pasco. It is endemic to New Zealand, where it is known from Cecil Peak. The wingspan is about 20 mm. The forewings are deep yellowish brown with dusky black markings on the costa and dorsum.

Geographic entities mentioned:
surface_form: Cecil Peak
instance_of: Mountain
countries: New Zealand
coordinates: lat: -45.1088
lon: 168.628
Lake Hopatcong Yacht Club. The Lake Hopatcong Yacht Club is a private yacht club located in Mount Arlington, Morris County, New Jersey, United States, in the northwestern part of New Jersey, on the small peninsula of Bertrand Island along the state's largest lake, Lake Hopatcong. The club is non-profit, and governed by a slate of volunteers, elected by its members.

Geographic entities mentioned:
surface_form: Bertrand Island
instance_of: Landform
countries: United States
coordinates: lat: 40.9249
lon: -74.6464
The moorland covers an area of about, of which less than, about 2%, is occupied by the wind farm. Scout Moor Quarry, a open-pit mine in Edenfield, is used for the extraction of gritstone and sandstone, and formerly had its own railway line. The eastern fringe of Scout Moor Wind Farm extends to Hail Storm Hill (also known as Cowpe Moss), one of the 180 Marilyns of England.

Geographic entities mentioned:
surface_form: Hail Storm Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.669911111111
lon: -2.2512194444444
Following the meeting Catherine Pilling, a Rossendale Liberal Democrat councillor, expressed her view that the natural beauty of the Rossendale Valley was under threat as it was increasingly being targeted by wind farm developers.

Geographic entities mentioned:
surface_form: Rossendale Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.7031
lon: -2.2893
He tells Franz to &quot;Tell your Court of Crabs that I alone am guilty - of everything.&quot; Upon hearing this, Franz again descends the stairs, smiling and saying The two discuss taking Leni's Porsche on the Elbe Embankment, a road which leads to the &quot;Teufelsbrücke&quot; over the Elbe, something they used to do when Franz was young.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
It stood on the northern side of the Peneius, near the entrance of the only two passes by which an enemy can penetrate into Thessaly from the north. The celebrated vale of Tempe begins to narrow at Gonnus; and the pass across Mount Olympus a little to the west of Tempe leads into Thessaly at Gonnus. It was by the latter route that the army of Xerxes I entered Thessaly.

Geographic entities mentioned:
surface_form: vale of Tempe
instance_of: Valley
countries: Greece
coordinates: lat: 39.872778
lon: 22.546667
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
It re-enters Montenegro at Vjeternik under the name of &quot;Grnčar&quot;. Receiving the stream &quot;Vruje&quot; from the right in Gusinje, it continues as the &quot;Ljuča&quot; for a few more kilometers where it empties into the Lake Plav, creating a small delta.

Geographic entities mentioned:
surface_form: Lake Plav
instance_of: Lake
countries: Montenegro
coordinates: lat: 42.595833333333
lon: 19.925
As of 2004, the type insect was part of the amber collections housed at the British Museum of Natural History, London, England. The amber specimen was recovered from deposits exposed in the Hukawng Valley of Kachin State, Myanmar. Burmese amber has been radiometrically dated using U-Pb isotopes, yielding an age of approximately 99 million years old, close to the Albian – Cenomanian boundary.

Geographic entities mentioned:
surface_form: Hukawng Valley
instance_of: Valley
countries: Myanmar
coordinates: lat: 26.438333333333
lon: 96.558888888889
Aime Mäemets. Aime Mäemets (1930 – 1996) was an Estonian botanist and hydrobiologist. She conducted considerable research into Lake Peipus and was known for her study of Macrophytes. She finished University of Tartu in 1954. From 1961 to 1996 she worked in Estonian Institute of Zoology and Botany and was a well-known specialist of Potamogetonaceae plants.

Geographic entities mentioned:
surface_form: Lake Peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
Seattle also has some of the only permanent floating pontoon bridges in the world. Original crossings over Seattle's mudflats were typically supported by timber piles. Lake Washington and Puget Sound are to the east and west of the city, respectively. They connect via a series of canals and Lake Union that are collectively known as the Lake Washington Ship Canal.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Lake Washington and Puget Sound are to the east and west of the city, respectively. They connect via a series of canals and Lake Union that are collectively known as the Lake Washington Ship Canal. The four double-leaf bascule bridges crossing the Ship Canal are the oldest still used in the city, having opened between 1917 and 1930.

Geographic entities mentioned:
surface_form: Lake Union
instance_of: Lake
countries: United States
coordinates: lat: 47.6392
lon: -122.3337
After his high school graduation, Kalk served in the U.S. Marine Corps for four years. After his military service, Kalk worked for the federal government for 13 years, owned and operated a resort on Mille Lacs Lake, and worked as a subcontractor in carpentry.

Geographic entities mentioned:
surface_form: Mille Lacs Lake
instance_of: Lake
countries: United States
coordinates: lat: 46.2381
lon: -93.6434
On 24 May &quot;Ardito&quot;, &quot;Animoso&quot;, and &quot;Audace&quot; carried out an anti-submarine patrol in the Gulf of Drin off the coast of the Principality of Albania and subsequently off Cattaro, a major base of the Austro-Hungarian Navy.

Geographic entities mentioned:
surface_form: Gulf of Drin
instance_of: Body of water
countries: Albania
coordinates: lat: 41.76666667
lon: 19.51666667