Sarmila/GeoWiki-Features huggingface dataset:
The song wasn't played in the &quot;Liebe ist für alle da&quot; tour, but it reappeared for the Made In Germany 1995–2011 tour, Download festival 2013 and the European Stadium Tour 2019. Video. The video was filmed in the Kaun Valley and on the Großglockner in Austria. It shows the band climbing in the mountains when lead vocalist Till Lindemann falls and gets badly hurt.

Geographic entities mentioned:
surface_form: Großglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
Geography. The canyon cuts through the Sierra Pelona Mountains, which are central part of the Transverse Ranges system of California. At the San Francisquito Canyon head is the San Francisquito Pass, which the early routes between Los Angeles and the San Joaquin Valley crossed. The canyon grows wider as it approaches the Santa Clarita Valley.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
At the San Francisquito Canyon head is the San Francisquito Pass, which the early routes between Los Angeles and the San Joaquin Valley crossed. The canyon grows wider as it approaches the Santa Clarita Valley. The middle and upper portions of this canyon fall within the Angeles National Forest. Mining.

Geographic entities mentioned:
surface_form: Santa Clarita Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.398
lon: -118.522
Today, a two-lane road named after the canyon itself connects Santa Clarita to the mountain communities of Green Valley and Elizabeth Lake. It roughly parallels the river's course between San Francisquito Pass and its southern terminus in the northern Santa Clarita Valley.

Geographic entities mentioned:
surface_form: Santa Clarita Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.398
lon: -118.522
Most people are found in the town of Leknes and its suburb Gravdal, where Nordland Hospital Lofoten is located. Along the southeastern coast, one finds picturesque fishing villages like Ballstad and Stamsund, where the Hurtigruten (coastal ferry) stops. The coastline is dominated by high mountains, such as the tall Skottinden, and on the west coast also sandy white beaches.

Geographic entities mentioned:
surface_form: Skottinden
instance_of: Mountain
countries: Norway
coordinates: lat: 68.0818
lon: 13.4923
Jämsänkoski. Jämsänkoski is a former town and municipality of Finland in the Central Finland region. It is located near Lake Päijänne and the Jämsänjoki river. The town had a population of 7,351 in 2008. It covered an area of 448.67 km² of which 48.02 km² is water. The population density was 16.9 inhabitants per km².

Geographic entities mentioned:
surface_form: Lake Päijänne
instance_of: Lake
countries: Finland
coordinates: lat: 61.583333333333
lon: 25.5
Yucamane. Yucamane, Yucamani or Yucumane is an andesitic stratovolcano in the Tacna Region of southern Peru. It is part of the Peruvian segment of the Central Volcanic Zone, one of the three volcanic belts of the Andes generated by the subduction of the Nazca plate beneath the South America plate. Peru's active volcanoes Ubinas, Sabancaya and El Misti are also part of the Central Volcanic Zone.

Geographic entities mentioned:
surface_form: Ubinas
instance_of: Mountain
countries: Peru
coordinates: lat: -16.34861111111111
lon: -70.90222222222222
surface_form: misti
instance_of: Mountain
countries: Peru
coordinates: lat: -16.296388888888888
lon: -71.41055555555556
surface_form: el misti
instance_of: Mountain
countries: Peru
coordinates: lat: -16.296388888888888
lon: -71.41055555555556
surface_form: misti
instance_of: Mountain
countries: Peru
coordinates: lat: -15.525277777778
lon: -71.690833333333
The volcanic group was active in the Pleistocene epoch, with the Holocene featuring several explosive eruptions occurring at Yucamane proper and effusive eruptions at Calientes. The last dated eruption of Yucamane occurred 1,320 BCE; whether there were historical eruptions is unclear as some eruptions attributed to Yucamane probably took place at Tutupaca. Geography and geomorphology.

Geographic entities mentioned:
surface_form: Tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
The last dated eruption of Yucamane occurred 1,320 BCE; whether there were historical eruptions is unclear as some eruptions attributed to Yucamane probably took place at Tutupaca. Geography and geomorphology. Yucamane lies in the Tacna Region, Candarave Province, Candarave District of Peru, west of lake Vilacota. The town of Candarave lies - southwest from the volcano and the city of Tacna south.

Geographic entities mentioned:
surface_form: lake Vilacota
instance_of: Lake
countries: Peru
coordinates: lat: -17.15
lon: -70.0333
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: vilacota
instance_of: Lake
countries: Peru
coordinates: lat: -17.15
lon: -70.0333
surface_form: vilacota
instance_of: Mountain
countries: Peru
coordinates: lat: -14.59027778
lon: -69.445
Regional. The Andes are the longest mountain range on Earth, extending from the Tierra del Fuego archipelago in southernmost South America to Venezuela in the north. In southern Peru, the Andes consist of several mountain chains including the Western Cordillera and the Eastern Cordillera, with elevations of up to, which are separated from each other by the Altiplano.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
In Peru about four hundred heavily eroded volcanoes make up the volcanically active area along with the active volcanoes El Misti, Sabancaya and Ubinas; the volcanoes Andagua volcanic field, Casiri, Chachani, Coropuna, Firura, Huaynaputina, Tutupaca and Yucamane may have been active in recent history.

Geographic entities mentioned:
surface_form: Ubinas
instance_of: Mountain
countries: Peru
coordinates: lat: -16.34861111111111
lon: -70.90222222222222
surface_form: Andagua volcanic field
instance_of: Mountain
countries: Peru
coordinates: lat: -15.257
lon: -72.483
surface_form: Chachani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.194166666667
lon: -71.531666666667
surface_form: Firura
instance_of: Mountain
countries: Peru
coordinates: lat: -15.23608
lon: -72.64069
surface_form: Huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223
surface_form: Tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: misti
instance_of: Mountain
countries: Peru
coordinates: lat: -16.296388888888888
lon: -71.41055555555556
surface_form: el misti
instance_of: Mountain
countries: Peru
coordinates: lat: -16.296388888888888
lon: -71.41055555555556
surface_form: misti
instance_of: Mountain
countries: Peru
coordinates: lat: -15.525277777778
lon: -71.690833333333
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
The largest historical eruption in Peru occurred in 1600 at Huaynaputina and caused 1,500 fatalities and severe economic damage. Other major eruptions occurred 2,000 years before present at El Misti volcano, 1,000 years before present at Ubinas and two centuries ago at Tutupaca. Finally, the three volcanoes Ampato, Chachani and Coropuna have heights exceeding. Local.

Geographic entities mentioned:
surface_form: Ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
surface_form: Chachani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.194166666667
lon: -71.531666666667
More than 9,000 people live in the danger zone. Ash fall from an eruption could extend southeastward to the border with Chile and affect the towns of Candarave, Ilabaya, Pachia, Palca and Tarata. Volcanic earthquakes like the 1999 Ticsani earthquakes at a volcano farther north and volcanic gases constitute additional dangers.

Geographic entities mentioned:
surface_form: Ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
The largest historical eruption in Peru occurred in 1600 at Huaynaputina and caused 1,500 fatalities and severe economic damage. Other major eruptions occurred 2,000 years before present at El Misti volcano, 1,000 years before present at Ubinas and two centuries ago at Tutupaca. Finally, the three volcanoes Ampato, Chachani and Coropuna have heights exceeding. Local.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: misti
instance_of: Mountain
countries: Peru
coordinates: lat: -16.296388888888888
lon: -71.41055555555556
surface_form: el misti
instance_of: Mountain
countries: Peru
coordinates: lat: -16.296388888888888
lon: -71.41055555555556
surface_form: misti
instance_of: Mountain
countries: Peru
coordinates: lat: -15.525277777778
lon: -71.690833333333
surface_form: ubinas
instance_of: Mountain
countries: Peru
coordinates: lat: -16.34861111111111
lon: -70.90222222222222
Historical activity. Eruptions reported in 1787, 1802, 1862 and 1902 in the region have also been attributed to Yucamane, although some may actually have occurred at Tutupaca. The 1787 and 1902 events involved the emission of ash; an 1874 edition of the Arequipa-based &quot;El Deber&quot; newspaper states that Yucamane was &quot;bursting&quot; and &quot;steaming&quot; in 1787.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
The volcano is part of the. The scorpion species &quot;Brachistosternus ninapo&quot; is named after the volcano; the term &quot;ninapo&quot; is a portmanteau of the Quechua word for &quot;fire-spitting mountain&quot;. This scorpion was discovered on the sides of the volcanoes Yucamane and El Misti. Eruptive history.

Geographic entities mentioned:
surface_form: misti
instance_of: Mountain
countries: Peru
coordinates: lat: -16.296388888888888
lon: -71.41055555555556
surface_form: el misti
instance_of: Mountain
countries: Peru
coordinates: lat: -16.296388888888888
lon: -71.41055555555556
surface_form: misti
instance_of: Mountain
countries: Peru
coordinates: lat: -15.525277777778
lon: -71.690833333333
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
The largest historical eruption in Peru occurred in 1600 at Huaynaputina and caused 1,500 fatalities and severe economic damage. Other major eruptions occurred 2,000 years before present at El Misti volcano, 1,000 years before present at Ubinas and two centuries ago at Tutupaca. Finally, the three volcanoes Ampato, Chachani and Coropuna have heights exceeding. Local.

Geographic entities mentioned:
surface_form: huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223
Yucamane. Yucamane, Yucamani or Yucumane is an andesitic stratovolcano in the Tacna Region of southern Peru. It is part of the Peruvian segment of the Central Volcanic Zone, one of the three volcanic belts of the Andes generated by the subduction of the Nazca plate beneath the South America plate. Peru's active volcanoes Ubinas, Sabancaya and El Misti are also part of the Central Volcanic Zone.

Geographic entities mentioned:
surface_form: yucamani
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Yucamane. Yucamane, Yucamani or Yucumane is an andesitic stratovolcano in the Tacna Region of southern Peru. It is part of the Peruvian segment of the Central Volcanic Zone, one of the three volcanic belts of the Andes generated by the subduction of the Nazca plate beneath the South America plate. Peru's active volcanoes Ubinas, Sabancaya and El Misti are also part of the Central Volcanic Zone.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Peru's active volcanoes Ubinas, Sabancaya and El Misti are also part of the Central Volcanic Zone. Yucamane, together with the volcanoes Yucamane Chico and Calientes farther north, forms a Pleistocene volcanic group. Yucamane is constructed mainly by lava flows with subordinate pyroclastic deposits, and it has a well preserved summit crater with fumarolic activity.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Peru's active volcanoes Ubinas, Sabancaya and El Misti are also part of the Central Volcanic Zone. Yucamane, together with the volcanoes Yucamane Chico and Calientes farther north, forms a Pleistocene volcanic group. Yucamane is constructed mainly by lava flows with subordinate pyroclastic deposits, and it has a well preserved summit crater with fumarolic activity.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Yucamane is constructed mainly by lava flows with subordinate pyroclastic deposits, and it has a well preserved summit crater with fumarolic activity. The volcanic group was active in the Pleistocene epoch, with the Holocene featuring several explosive eruptions occurring at Yucamane proper and effusive eruptions at Calientes.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
The town of Candarave lies - southwest from the volcano and the city of Tacna south. A number of mostly agricultural towns exist on its slopes, such as Aricota, Cairani, Camilaca, Cucachi, Huanuara, Morjani, Pallata, Susapaya, Tarata, Ticaco, Totora and Yucamane Pampa, as well as irrigation infrastructure and major roads. Sulfur was mined on the volcano in the past.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: aricota
instance_of: Lake
countries: Peru
coordinates: lat: -17.36
lon: -70.293611111111
Sulfur was mined on the volcano in the past. The area of Yucamane is accessible by a number of roads including the international Ilo-Desaguadero highway, and a road leads up the northwestern flank of Yucamane to a point close to the mountain pass between Yucamane and Calientes. The edifice of the volcano and surrounding region are part of the Vilacota-Maure protected area. Regional.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Seven volcanoes have been active in Peru since the arrival of the Spaniards, but volcanic activity is typically poorly recorded in Peru, owing to the remote nature of the region and the scarce population. Yucamane is part of the Central Volcanic Zone, one of the three major volcanic belts in the Andes, which spans the countries of Peru, Bolivia, Chile and Argentina.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Finally, the three volcanoes Ampato, Chachani and Coropuna have heights exceeding. Local. Yucamane is a mountain whose height is variously given as, or. It is a high compound volcano, with an about wide summit crater; this depression in turn has a smaller crater with a diameter of and a depth of about nested within.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
The summit crater has a young appearance, and due to the youth of the volcano there is little trace of glaciation. Yucamane has a conical shape and is formed primarily by lava flows with some block and ash flows and pyroclastic flows. Lava flows are thick and often show characteristic flow ridges.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Based on slope angle, a &quot;Yucamane I&quot; volcano, which forms the lower part of the volcano and has a more gentle slope, has been distinguished from a &quot;Yucamane II&quot;, which sits atop &quot;Yucamane I&quot; and has steeper slopes. The lower part of the volcano bears traces of glaciation, presumably from the last glacial maximum.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
This cone is wide and has a partially destroyed crater. Several other volcanoes lie north of Yucamane, such as the, or high Yucamane Chico and the, or high Calientes, which form a long north-south volcanic chain with Yucamane. Calientes and Yucamane are considered to be a paired volcano with a volume of and a base area of.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Other volcanoes in the area include San Pedro, López Extraña and the much older Nazaparco. Nazaparco consists of andesitic rocks and rhyolitic block and ash flows, while Yucamane Chico and Calientes are surrounded by radially extending lava flows like Yucamane proper and Calientes has produced a ignimbrite south of Yucamane.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
The older volcanoes show evidence of sector collapses and have been glaciated, which has left moraines at elevations of about and glacial deposits with a volume of about. This volcanic complex is part of the Cordillera del Barroso mountain chain in southern Peru. A series of northwest-southeast trending normal faults runs along the Andes close to Yucamane.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
A series of northwest-southeast trending normal faults runs along the Andes close to Yucamane. The Yucamane fault runs in a north-south direction across the volcanoes, and another fault that runs northwest-southeast is named the Yucamane Chico fault; the Yucamane Chico volcano roughly coincides with the intersection of these faults. Hydrology.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Hydrology. The slopes of the volcano drain westward, eastward and southward towards the Calientes and Callazas rivers in the east and west of Yucamane, respectively. Both rivers flow southward and ultimately join to form the Locumba river, which ends in the Pacific Ocean.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Both rivers flow southward and ultimately join to form the Locumba river, which ends in the Pacific Ocean. The water in these rivers contains large quantities of arsenic derived from volcanic rocks, including Yucamane's volcanic rocks; arsenic in drinking water is linked to internal organ damage and cancer. Geology.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Yucamane is constructed on a basement formed by the Paleozoic Tacaza Group (lavas of the lower Tacaza formation), the Jurassic Yura Group (sediments of the Hualhuani formation), the Neogene volcanic Huaylillas formation and the 10-1 million years old Barroso Group; parts of this basement crop out on the southern side of Yucamane.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: barroso
instance_of: Mountain
countries: Peru
coordinates: lat: -17.556308
lon: -69.5954717
This basement in turn consists of two major tectonic blocks, the southern Arequipa terrane and the northern Paracas massif; both are formed by igneous and metamorphic rocks such as gneiss and are covered by Mesozoic sedimentary and Cenozoic volcanic rocks. A large ring-shaped volcanic intrusion appears to underlie Yucamane. Petrology.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
The andesites make up the bulk of the outcropping edifice. These andesitic rocks contain phenocrysts of amphibole, biotite, hornblende, oxides, plagioclase and quartz. Calientes has produced a similar rock suite but with a dominance of dacite instead of basaltic andesite and andesite as in Yucamane. The magmas formed through the assimilation of crustal material and fractionation of amphibole.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Calientes has produced a similar rock suite but with a dominance of dacite instead of basaltic andesite and andesite as in Yucamane. The magmas formed through the assimilation of crustal material and fractionation of amphibole. Arsenic in volcanic rocks causes water pollution in rivers around Yucamane. Climate and natural features.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Arsenic in volcanic rocks causes water pollution in rivers around Yucamane. Climate and natural features. The region has a dry tropical climate, with precipitation on Yucamane amounting to about. Most of it falls during the summer months, and the amount of precipitation decreases southwestward towards the coast and away from the mountains.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Its eruption probably reached a volcanic explosivity index of 6 and may have produced a now-buried caldera), 126,000 ± 3,000, 95,600 ± 16,700, 133,400 ± 13,500, 102,000 ± 6,000 and 3,000 ± 3,000 years ago. Yucamane itself has an undated first stage, lava flows dated at 380,000 ± 300,000, 23,000 ± 1,000, 7,100 ± 1,000 and 3,000 ± 2,000 years before present.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Other events occurred 29,200 + 170/−160, forming the Honda block-and-ash flow deposit, and 3,270 ± 50/3,085 ± 35 years before present; during the course of this eruption Yucamane expelled at least of material in the form of pumice, lapilli and tephra.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Historical activity. Eruptions reported in 1787, 1802, 1862 and 1902 in the region have also been attributed to Yucamane, although some may actually have occurred at Tutupaca. The 1787 and 1902 events involved the emission of ash; an 1874 edition of the Arequipa-based &quot;El Deber&quot; newspaper states that Yucamane was &quot;bursting&quot; and &quot;steaming&quot; in 1787.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Overall, historical records are fragmentary and scarce, and the Global Volcanism Program recognizes the 1,320 BCE eruption as the most recent event. Yucamane is fumarolically active in its summit crater, the fumaroles are most recognizable after precipitation and are not very intense. Presently, Yucamane is considered to be a dormant volcano.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Yucamane is fumarolically active in its summit crater, the fumaroles are most recognizable after precipitation and are not very intense. Presently, Yucamane is considered to be a dormant volcano. Thermal anomalies of about of uncertain origin have been observed on Yucamane by satellite imagery.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Presently, Yucamane is considered to be a dormant volcano. Thermal anomalies of about of uncertain origin have been observed on Yucamane by satellite imagery. The Caliente geothermal field east of Yucamane, which includes geysers and hot springs, appears to be unrelated to Yucamane. Hazards. , the volcano is monitored with seismometers, detectors of tilt and cameras.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Hazards. , the volcano is monitored with seismometers, detectors of tilt and cameras. The Peruvian geological agency INGEMMET considers Yucamane a &quot;moderately hazardous&quot; volcano; it has published ash fall, lava flow and pyroclastic flow hazard maps for Yucamane, and additional hazard maps are available on its website.

Geographic entities mentioned:
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Sulfur was mined on the volcano in the past. The area of Yucamane is accessible by a number of roads including the international Ilo-Desaguadero highway, and a road leads up the northwestern flank of Yucamane to a point close to the mountain pass between Yucamane and Calientes. The edifice of the volcano and surrounding region are part of the Vilacota-Maure protected area. Regional.

Geographic entities mentioned:
surface_form: vilacota
instance_of: Lake
countries: Peru
coordinates: lat: -17.15
lon: -70.0333
surface_form: vilacota
instance_of: Mountain
countries: Peru
coordinates: lat: -14.59027778
lon: -69.445
The older volcanoes show evidence of sector collapses and have been glaciated, which has left moraines at elevations of about and glacial deposits with a volume of about. This volcanic complex is part of the Cordillera del Barroso mountain chain in southern Peru. A series of northwest-southeast trending normal faults runs along the Andes close to Yucamane.

Geographic entities mentioned:
surface_form: barroso
instance_of: Mountain
countries: Peru
coordinates: lat: -17.556308
lon: -69.5954717
The 11,141-acre (45.1 km2) Poteau Mountain Wilderness is located in the north-central range of the Ouachita mountains in Arkansas. The 6,301-acre (25.5 km2) Dry Creek Wilderness is located in the north-central ranges of the Ouachita Mountains near Magazine Mountain. It is the state's second-smallest wilderness is known for scenic overlooks and high, secluded sandstone bluffs.

Geographic entities mentioned:
surface_form: Magazine Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.167222222222
lon: -93.645
The sale was subject to a four-year deferred payment which, subject to business performance, could generate a further $15 million for Coca-Cola on top of the money paid up-front. As part of the turnaround strategy, the business sold the IXL and Taylors brands with the Kyabram factory in 2019 to a group of farmers and growers in the Goulburn Valley.

Geographic entities mentioned:
surface_form: Goulburn Valley
instance_of: Valley
countries: Australia
coordinates: lat: -36.3831
lon: 145.399
Bryant, Florida. Bryant is an unincorporated community in Palm Beach County, Florida, United States. Bryant is located on State Road 700 near Lake Okeechobee, northeast of Pahokee. Bryant had a post office with ZIP code 33438. U.S. Sugar operated the Bryant Sugar House mill in Bryant. The mill closed in 2007, and the town was taken over by the federal government in 2011 and demolished in 2016.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
Nishat Bagh. Nishat Bagh () is a terraced Mughal garden built on the eastern bank of the Dal Lake, close to Srinagar in the union territory of Jammu and Kashmir, India. It is the second-largest Mughal garden in the Kashmir Valley. History. The garden is located on the bank of the Dal Lake, with the Zabarwan Mountains as its backdrop, and views of the lake beneath the Pir Panjal mountain range.

Geographic entities mentioned:
surface_form: Dal Lake
instance_of: Lake
countries: India
coordinates: lat: 34.12
lon: 74.87
Nishat Bagh. Nishat Bagh () is a terraced Mughal garden built on the eastern bank of the Dal Lake, close to Srinagar in the union territory of Jammu and Kashmir, India. It is the second-largest Mughal garden in the Kashmir Valley. History. The garden is located on the bank of the Dal Lake, with the Zabarwan Mountains as its backdrop, and views of the lake beneath the Pir Panjal mountain range.

Geographic entities mentioned:
surface_form: Kashmir
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Roche Lake Provincial Park. Roche Lake Provincial Park is a provincial park in British Columbia, Canada, located northeast of Stump Lake in the Nicola Country of that province's South-Central Interior. The park lies to the northwest of the city of Merritt and to the south of Kamloops.

Geographic entities mentioned:
surface_form: Stump Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.366666666667
lon: -120.36666666667
Another overhaul followed in San Francisco from 3 to 10 January 1943. After further training and tests at San Francisco and Long Beach that lasted into April, she departed to join the Aleutian Islands Campaign on 23 April. She bombarded Holtz Bay and Chichagof Harbor on 11–12 May to support the forces that went ashore on the island of Attu.

Geographic entities mentioned:
surface_form: Chichagof Harbor
instance_of: Landform
countries: United States
coordinates: lat: 52.9319
lon: 173.242
King’s partner, Albert L. Winge was a native of Norway. Early marine construction. In 1902, the passenger steamer &quot;Lady of the Lake&quot;, built at Lake Washington in 1897, burned and was rebuilt in 1905 by King and Winge as the tug &quot;Ruth&quot;. In 1909, the steam tug &quot;Elk&quot; was wrecked at Restoration Point but was salvaged and towed to King and Winge for repairs.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
2015 Mount Everest avalanches. In the afternoon of 25 April 2015, a MW 7.8 earthquake struck Nepal and surrounding countries. Tremors from the quake triggered an avalanche from Pumori into Base Camp on Mount Everest. At least 22 people were killed, surpassing the toll of an avalanche that occurred in 2014 as the deadliest disaster on the mountain. Avalanches.

Geographic entities mentioned:
surface_form: Pumori
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.015555555555554
lon: 86.82805555555555
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
The earthquake triggered several large avalanches on and around the mountain. One avalanche, originating on the nearby peak of Pumori, swept into Base Camp and blew many tents across the Khumbu Glacier towards the lower Icefall. An Indian Army mountaineering team recovered the bodies of 19 mountaineers from the South Base Camp and rescued at least 61 stranded climbers from the mountain.

Geographic entities mentioned:
surface_form: Pumori
instance_of: Mountain
countries: People's Republic of China
Nepal
coordinates: lat: 28.015555555555554
lon: 86.82805555555555
The name of the bridge itself comes from the four statues of eagles on it, which are, symbolically, its protectors and patrons. Eagles' Bridge and the junction are located in the immediate proximity of the Vasil Levski National Stadium, the Monument to the Soviet Army, the Borisova gradina park and Lake Ariana, and near Sofia University.

Geographic entities mentioned:
surface_form: Lake Ariana
instance_of: Lake
countries: Bulgaria
coordinates: lat: 42.689166666667
lon: 23.336583333333
The cost of the entire construction of the bridge was 80,000 golden leva. One of the bridge's columns and bronze eagles are depicted on the reverse print of Bulgarian 20 levs banknote, issued in 1999 and 2007. The place is often a site of protests. Orlov Most was the focus of 2012 ecological protests against construction on Vitosha mountain and on the Dyuni nature spot on the Black Sea coast.

Geographic entities mentioned:
surface_form: Vitosha
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.566666666667
lon: 23.283333333333
Needle Hill. Needle Hill or Cham Shan () is a mountain in New Territories, Hong Kong. It has an altitude of 532 m. This is a part of a popular hiking route including Grassy Hill and Tai Mo Shan. The mountain got its name due to the resemblance of a needle by its peak. Geography. At around 400 above sea level, it forms a needle-like shape at its peak.

Geographic entities mentioned:
surface_form: Grassy Hill
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.4125
lon: 114.165
surface_form: Tai Mo Shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.4118
lon: 114.123
Needle Hill. Needle Hill or Cham Shan () is a mountain in New Territories, Hong Kong. It has an altitude of 532 m. This is a part of a popular hiking route including Grassy Hill and Tai Mo Shan. The mountain got its name due to the resemblance of a needle by its peak. Geography. At around 400 above sea level, it forms a needle-like shape at its peak.

Geographic entities mentioned:
surface_form: cham shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.3871
lon: 114.16
surface_form: needle hill
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.3871
lon: 114.16
Needle Hill. Needle Hill or Cham Shan () is a mountain in New Territories, Hong Kong. It has an altitude of 532 m. This is a part of a popular hiking route including Grassy Hill and Tai Mo Shan. The mountain got its name due to the resemblance of a needle by its peak. Geography. At around 400 above sea level, it forms a needle-like shape at its peak.

Geographic entities mentioned:
surface_form: needle hill
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.3871
lon: 114.16
Geography. At around 400 above sea level, it forms a needle-like shape at its peak. The granitic rocks that form this hill is part of a granitic ridge that starts at the Tolo Channel and ends in Kwai Chung. Needle Hill is located within Shing Mun Country Park. Stage 7 of the MacLehose Trail includes the summit of Needle Hill. The Shing Mun Tunnels pass through the base of Needle Hill.

Geographic entities mentioned:
surface_form: needle hill
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.3871
lon: 114.16
The granitic rocks that form this hill is part of a granitic ridge that starts at the Tolo Channel and ends in Kwai Chung. Needle Hill is located within Shing Mun Country Park. Stage 7 of the MacLehose Trail includes the summit of Needle Hill. The Shing Mun Tunnels pass through the base of Needle Hill. The Lower Shing Mun River can also be found at the base of the hill. Geology.

Geographic entities mentioned:
surface_form: needle hill
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.3871
lon: 114.16
The Shing Mun Tunnels pass through the base of Needle Hill. The Lower Shing Mun River can also be found at the base of the hill. Geology. Needle Hill is mainly composed of granite. Wolframite, molybdenite and quartz ores can be found at the base of the hill. History. Wolframite, a tungsten ore, was discovered at Needle Hill in 1935. It was mined there from 1938 to 1967.

Geographic entities mentioned:
surface_form: needle hill
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.3871
lon: 114.16
The Lower Shing Mun River can also be found at the base of the hill. Geology. Needle Hill is mainly composed of granite. Wolframite, molybdenite and quartz ores can be found at the base of the hill. History. Wolframite, a tungsten ore, was discovered at Needle Hill in 1935. It was mined there from 1938 to 1967. The mines used to obtain wolframite ores are now abandoned.

Geographic entities mentioned:
surface_form: needle hill
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.3871
lon: 114.16
Mill Creek (Wisconsin River tributary). Mill Creek is a stream in the U.S. state of Wisconsin. It is a tributary to the Wisconsin River. Mill Creek was named for the sawmills which once lined its banks. The native Chippewa-language name was &quot;Wau-pee-tee Se-be&quot; meaning &quot;tooth river&quot;.

Geographic entities mentioned:
surface_form: wau-pee-tee se-be
instance_of: Watercourse
countries: United States
coordinates: lat: 44.4599675
lon: -89.6412311
Mill Creek (Wisconsin River tributary). Mill Creek is a stream in the U.S. state of Wisconsin. It is a tributary to the Wisconsin River. Mill Creek was named for the sawmills which once lined its banks. The native Chippewa-language name was &quot;Wau-pee-tee Se-be&quot; meaning &quot;tooth river&quot;.

Geographic entities mentioned:
surface_form: mill creek
instance_of: Watercourse
countries: United States
coordinates: lat: 44.4599675
lon: -89.6412311
Battle of Tuiteam Tarbhach. The chief of the MacLeods of Lewis had heard that his sister, wife of Angus Mackay, 6th of Strathnaver, had been mistreated and according to historian Angus Mackay the MacLeods raided the Mackay's lands of Strathnaver. The Mackays pursued the MacLeods and the Battle of Tuiteam Tarbhach took place where the MacLeods were defeated.

Geographic entities mentioned:
surface_form: Strathnaver
instance_of: Valley
countries: United Kingdom
coordinates: lat: 58.528888888888886
lon: -4.239444444444445
The chieftains including Alexander of Islay, Earl of Ross the Lord of the Isles, Angus Du Mackay of Strathnaver, Kenneth Mor, his son in law Angus Moray and MacMathen were all clapped in irons. Angus Du Mackay was soon released but his eldest son Neil was kept as a hostage and was sent for a time to the Bass Rock. Battle of Drumnacoub.

Geographic entities mentioned:
surface_form: Bass Rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.08
lon: -2.64
Thomas Neilson Mackay was then outlawed. He was betrayed by his own two brothers Neil Neilson Mackay and Morgan Neilson Mackay, instigated by Angus Moray of Pulrossie whose two daughters the two brothers had married. Angus Moray supported by his two sons-in-law, Neil Neilson Mackay and Morgan Neilson Mackay, then invaded Strathnaver the lands of their cousin, chief Angus Du Mackay.

Geographic entities mentioned:
surface_form: Strathnaver
instance_of: Valley
countries: United Kingdom
coordinates: lat: 58.528888888888886
lon: -4.239444444444445
Angus Moray supported by his two sons-in-law, Neil Neilson Mackay and Morgan Neilson Mackay, then invaded Strathnaver the lands of their cousin, chief Angus Du Mackay. Angus Du Mackay was in a weak position with his eldest son still in prison on the Bass Rock after the Parliament of Inverness, as mentioned above.

Geographic entities mentioned:
surface_form: Bass Rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.08
lon: -2.64
Angus Moray with the men of Sutherland and supported by his sons-in-law, Neil Neilson Mackay and Morgan Neilson Mackay, advanced with a force of 1500 men. At the head of a pass north of the mountain Ben Loyal, within two miles of Castle Varrich they were met by the force of John &quot;Ian&quot; Mackay of Aberach, while the helpless Angus Du Mackay was carried in a litter.

Geographic entities mentioned:
surface_form: Ben Loyal
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.404926
lon: -4.435027
A 2021 genetic study on the Tarim mummies (13 mummies, including 11 from Xiaohe Cemetery, ranging from 2,135 to 1,623 BCE) found that they were most closely related to an earlier identified group called the Ancient North Eurasians, particularly the population represented by the &quot;Afontova Gora 3&quot; specimen (AG3), genetically displaying &quot;high affinity&quot; with it.

Geographic entities mentioned:
surface_form: Afontova Gora
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 56.026404
lon: 92.736156
Tarim_EMBA1 and Altai hunter-gatherers can be successfully modeled from each other in both directions: Altai hunter-gatherers can be modeled as a 2-source admixture between Tarim_EMBA1 and Ancient Paleo-Siberians, while conversely, Tarim_EMBA1 can be modeled as an even mixture of Altai hunter-gatherers and the ANE-genome AG3 from Afontova Gora.

Geographic entities mentioned:
surface_form: Afontova Gora
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 56.026404
lon: 92.736156
Trautenfels Castle. Trautenfels Castle (German: &quot;Schloss Trautenfels&quot;) is a palace located in the district of Liezen in Styria. It lies directly on the Enns at 673m in the municipality Pürgg-Trautenfels on a cliff protrusion at the foot of the Grimming. History.

Geographic entities mentioned:
surface_form: Grimming
instance_of: Mountain
countries: Austria
coordinates: lat: 47.520555555556
lon: 14.016944444444
Chionis Island. Chionis Island is an island lying south of Awl Point, Trinity Island, in the Palmer Archipelago. The name Snow Island was used for this feature by whalers in the area in the 1920s, but has not been used on any published map. Since Snow Island in the South Shetland Islands lies just across Bransfield Strait, a new name has been substituted for this feature.

Geographic entities mentioned:
surface_form: Bransfield Strait
instance_of: Body of water
countries: Antarctica
coordinates: lat: -63
lon: -59
Yang's career as an anti-government leader began during Zhong Xiang's Revolt in 1130, where he served as a peasant soldier under the leadership of Zhong Xiang. Yang helped occupy the Dongting Lake area in the modern-day Hunan Province with some 80,000 other soldiers before Song forces arrived.

Geographic entities mentioned:
surface_form: Dongting Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.316666666667
lon: 112.95
Tunas Peak. Tunas Peak, also known as Squawteat Peak, is a breast-shaped hill in Pecos County, Texas. Archaeology. Archaeological features found at Tunas Peak include tipi rings as well as several fire-cracked rock middens. Artifacts found include various projectile points (primarily Perdiz, Livermore, and Langtry types) and shell pendants.

Geographic entities mentioned:
surface_form: tunas peak
instance_of: Mountain
countries: United States
coordinates: lat: 30.894166666667
lon: -102.32361111111
Tourism. The town of Bakersfield has long been a ghost town, but Tunas Peak's distinctive appearance, offensive local name, and location off Interstate Highway 10 has led to it becoming a notable roadside attraction. A gas station in Bakersfield sells hats and keychains depicting the peak.

Geographic entities mentioned:
surface_form: tunas peak
instance_of: Mountain
countries: United States
coordinates: lat: 30.894166666667
lon: -102.32361111111
Mount Shinn (California). Mount Shinn is a mountain summit located west of the crest of the Sierra Nevada mountain range in Fresno County of northern California, United States. It is set within the John Muir Wilderness, on land managed by Sierra National Forest. Precipitation runoff from this mountain drains north to Florence Lake via tributaries of the South Fork San Joaquin River.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount shinn
instance_of: Mountain
countries: United States
coordinates: lat: 37.2125
lon: -118.91916666667
Mount Shinn (California). Mount Shinn is a mountain summit located west of the crest of the Sierra Nevada mountain range in Fresno County of northern California, United States. It is set within the John Muir Wilderness, on land managed by Sierra National Forest. Precipitation runoff from this mountain drains north to Florence Lake via tributaries of the South Fork San Joaquin River.

Geographic entities mentioned:
surface_form: mount shinn (california)
instance_of: Mountain
countries: United States
coordinates: lat: 37.2125
lon: -118.91916666667
Corey. Climate. According to the Köppen climate classification system, Mount Shinn is located in an alpine climate zone. Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains. As fronts approach, they are forced upward by the peaks (orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the range.

Geographic entities mentioned:
surface_form: mount shinn
instance_of: Mountain
countries: United States
coordinates: lat: 37.2125
lon: -118.91916666667
The richest right contributors are Manatovac (large stream), Mala Ilomska (Little Ilomska) and Devetero vrela (Nine springs), and left tributary Crna rijeka (Black River). At the Ravni Omar (mountain meadows), below Lisina Mountain, it enters a narrow highland continuing to “Korićanski most” (Korićani's Bridge), and a deep canyon below Korićanske stijene and Marića stijene (Marići's Rocks).

Geographic entities mentioned:
surface_form: Korićanske stijene
instance_of: Landform
countries: Bosnia and Herzegovina
coordinates: lat: 44.28333333333333
lon: 17.666666666666668
History. Above Ilomska River there is Korićani village and a canyon below it (Korićanske stijene), the scaffold of more than 200 Bosniaks and Croats – the victims of the Serbs Police and Army forces (on August 21, 1992), a crime prosecuted and sentenced through number of indictments at The ICTY Tribunal in The Hague.

Geographic entities mentioned:
surface_form: Korićanske stijene
instance_of: Landform
countries: Bosnia and Herzegovina
coordinates: lat: 44.28333333333333
lon: 17.666666666666668
Leslie Lathrop. Before the fall of Bataan, Filipino troops and officers of the 1st Regular Division fought side by side with the USAFFE in Bataan, attacking Japanese troops along the Layac Line, Porac-Guagua Line, Abucay-Mauban Line, Battle of Trail 2, the Battle of the Pockets and the Battle of the Points before the invasion at Mount Samat on 3 April 1942.

Geographic entities mentioned:
surface_form: Mount Samat
instance_of: Mountain
countries: Philippines
coordinates: lat: 14.60427778
lon: 120.50758333