Sarmila/GeoWiki-Features huggingface dataset:
Volcanoes often experience the collapse of part of the cone, a so-called sector collapse, which form a landslide (&quot;debris avalanche&quot;). There are no obvious traces of such on Misti, except on its western foot and a narrow chute on the northwestern flank of Misti that reaches its summit.

Geographic entities mentioned:
surface_form: 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
This group lies at the margin of the Altiplano, next to the tectonic depression of Arequipa where the city lies. The depression has dimensions of and appears to be formed by fault activity. The terrain under Misti slopes south and this might make the mountain slip southward over time. A northwest-southeast trending fault system includes the Huanca fault at Chachani and the Chili fault on Misti.

Geographic entities mentioned:
surface_form: 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
Magma composition has varied over time and the most recent volcanic stage has produced slightly different magmas, but overall the composition of Misti magmas is highly homogeneous. The composition of Misti magmas and those of its neighbours Pichu Pichu and Chachani resemble adakite, an unusual kind of volcanic rock formed by the direct melting of a subducting plate.

Geographic entities mentioned:
surface_form: 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
Eruption history. Misti is a young volcano. It developed in four stages, numbered 1 through 4; a pre-Misti volcano may have formed the southwestern debris avalanche and the older volcanic structures lie mainly in the western sector of Misti.

Geographic entities mentioned:
surface_form: 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
Long andesitic lava flows and ignimbrites, which reach a thickness of more than, form the oldest part of the volcano. They have an age of 833,000 years, but it is not clear if they should be considered part of &quot;Misti 1&quot; or of a pre-Misti volcano. Sometimes, they are considered the first stage of Misti activity, with all the subsequent activity making up the second stage.

Geographic entities mentioned:
surface_form: 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
Sometimes, they are considered the first stage of Misti activity, with all the subsequent activity making up the second stage. After the south-southwestern collapse, the present stratovolcano began to grow 112,000 years ago. During the following 42,000 years lava flows and lava domes built a mountain with an elevation of, in the southern and eastern sectors of present-day Misti.

Geographic entities mentioned:
surface_form: 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 9,000 and 8,500 years old eruptions produced the &quot;Sándwich&quot; deposits. They extend for more than on the southwestern flank of Misti produced ash fall over the Pacific Ocean and Lake Titicaca. Radiocarbon dating has identified eruptions 8,140, 6,390, 5,200, 4,750, 3,800 and 2,050 years ago; the 3,800 eruption deposited fallout on Nevado Mismi more than northwest of Misti.

Geographic entities mentioned:
surface_form: 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 hypocentres, the actual sites of the earthquakes, are found within the volcanic structure of Misti and cluster on the northwest flank of the volcano. The seismic activity appears to be linked to Misti's hydrothemal system. Seismic swarms were recorded in August 2012, May 2014 and June 2014. No deformation of the volcano is evident in satellite images.

Geographic entities mentioned:
surface_form: 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
Clouds rising from the mountain are sometimes mistaken for renewed activity. Hazards. Misti is Peru's most dangerous volcano and one of the most dangerous in the world, owing to its location just from Arequipa, a city of over one million residents. Over time the city has expanded and new and neighbouring towns such as Chiguata get within of Misti.

Geographic entities mentioned:
surface_form: misti
instance_of: Mountain
countries: Peru
coordinates: lat: -16.296388888888888
lon: -71.41055555555556
surface_form: 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: misti
instance_of: Mountain
countries: Peru
coordinates: lat: -15.525277777778
lon: -71.690833333333
Hazards. Misti is Peru's most dangerous volcano and one of the most dangerous in the world, owing to its location just from Arequipa, a city of over one million residents. Over time the city has expanded and new and neighbouring towns such as Chiguata get within of Misti. About 8.6% of Peru's GDP depends on Arequipa and would be impacted by a future eruption of Misti.

Geographic entities mentioned:
surface_form: 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
Over time the city has expanded and new and neighbouring towns such as Chiguata get within of Misti. About 8.6% of Peru's GDP depends on Arequipa and would be impacted by a future eruption of Misti. The city is constructed on mudflow and pyroclastic flow deposits of the volcano and all the valleys that drain Misti pass directly or indirectly through Arequipa.

Geographic entities mentioned:
surface_form: 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
About 8.6% of Peru's GDP depends on Arequipa and would be impacted by a future eruption of Misti. The city is constructed on mudflow and pyroclastic flow deposits of the volcano and all the valleys that drain Misti pass directly or indirectly through Arequipa. At least 220,000 people south of Misti are threatened by floods, mudflows and pyroclastic flows channelled through the ravines.

Geographic entities mentioned:
surface_form: 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 city is constructed on mudflow and pyroclastic flow deposits of the volcano and all the valleys that drain Misti pass directly or indirectly through Arequipa. At least 220,000 people south of Misti are threatened by floods, mudflows and pyroclastic flows channelled through the ravines. Hazards at Misti not related to volcanic activity include flooding during the wet season in Arequipa.

Geographic entities mentioned:
surface_form: 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
At least 220,000 people south of Misti are threatened by floods, mudflows and pyroclastic flows channelled through the ravines. Hazards at Misti not related to volcanic activity include flooding during the wet season in Arequipa. Heavy metals, presumably from Misti and Chachani, have been found in river water. Monitoring and hazard management.

Geographic entities mentioned:
surface_form: 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 Peruvian Volcano Observatory (OVI) was inaugurated in Arequipa in 2013; it monitors Misti, Ubinas, Ticsani and other Peruvian volcanoes., the monitoring network on Misti includes seismometers, equipment that measures the composition and temperature of hot springs and fumaroles, and sensors for movements or deformations of the mountain.

Geographic entities mentioned:
surface_form: 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
These efforts have yielded an increased awareness of the dangers posed by Misti, which is now being increasingly perceived as an active volcano. Efforts have been made to slow the growth of the northern suburbs of Arequipa, which are closest to Misti. A volcano hazard map was developed in 2005 by numerous local and international organizations, and officially presented in early 2008.

Geographic entities mentioned:
surface_form: 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 second scenario involves an eruption like the eruption 2,000 years ago. Thicker ash falls (exceeding) could cause building collapse and pyroclastic flows down the steep slopes south of Misti, reaching the suburbs of Arequipa and Chiguata. Most risk assessments are based on these two scenarios.

Geographic entities mentioned:
surface_form: 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
Birds include the Andean condor. 358 plant, 37 mammal and 158 bird species have been recorded in the region, including alpacas, guanacos, llamas and vicuñas. Most of the volcano is within the Salinas y Aguada Blanca National Reserve, which extends northwest of Misti and includes the volcano among its main attractions. Religious importance.

Geographic entities mentioned:
surface_form: 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 Aymara people viewed it as an abode of deceased souls, with different regions regarding it as either a friendly or hellish final destination. According to the late 16th-century chronist Cristóbal de Albornoz, Misti was one of the important mountains (, a kind of deity or idol) of the Arequipa area of the Inca Empire, along with Ampato, Coropuna, Sara Sara and Solimana.

Geographic entities mentioned:
surface_form: misti
instance_of: Mountain
countries: Peru
coordinates: lat: -16.296388888888888
lon: -71.41055555555556
surface_form: 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: misti
instance_of: Mountain
countries: Peru
coordinates: lat: -15.525277777778
lon: -71.690833333333
This tradition probably originated with the previous inhabitants of the area and was taken over by the Inca when they conquered the region. The Middle Horizon Millo archeological site in the Rio Vitor valley was constructed in a manner that allowed a good view of Misti, which was probably the &quot;apu&quot; of this place.

Geographic entities mentioned:
surface_form: 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
Petroglyphs at Toro Muerto may represent astronomical alignments of Misti and Chachani. The Inca gave the &quot;apus&quot; cups of gold and silver and settled people around Misti that would continue the mountain veneration. People used to alter the shape of the skulls of their infant children so that they resembled the volcano.

Geographic entities mentioned:
surface_form: 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
After the Spanish conquest, the mountain was consecrated to St. Francis. According to the Jesuit College of Arequipa, &quot;Indian sorcerers&quot; thought that Huaynaputina volcano had asked Misti for assistance in expelling the Spaniards; Misti however had turned down, saying it was already Christianized, so Huaynaputina had proceeded alone.

Geographic entities mentioned:
surface_form: 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
During episodes of increased activity, the inhabitants of Arequipa carried out religious ceremonies, including public penance and flagellations, to discourage the volcano. A group of converts and Franciscans in 1600 climbed on Misti and threw saints' relics and a cross into its crater to discourage the volcano.

Geographic entities mentioned:
surface_form: 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 cross on the summit of Misti supposedly protects the city. To this day, religious ceremonies are carried out on the volcano. Peasants believe that after offering gifts to Misti will bear boys, while the same offers to Chachani will make them bear girls. Mummies. Eight or nine mummies were found on Misti by Johan Reinhard and José Antonio Chávez in 1998, inside the crater and below the summit.

Geographic entities mentioned:
surface_form: 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
To this day, religious ceremonies are carried out on the volcano. Peasants believe that after offering gifts to Misti will bear boys, while the same offers to Chachani will make them bear girls. Mummies. Eight or nine mummies were found on Misti by Johan Reinhard and José Antonio Chávez in 1998, inside the crater and below the summit. The mummies were of children, mostly boys around six years old.

Geographic entities mentioned:
surface_form: 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
Unusually, the mummies were buried in shared tombs. Along with the mummies were figurines, ceramics and other objects; the high number of figurines found on Misti (47) indicates that the site was important to the Incas. These mummies were Inca human sacrifices, called &quot;capacochas&quot;, and the Misti &quot;capacocha&quot; is the largest known.

Geographic entities mentioned:
surface_form: 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
Along with the mummies were figurines, ceramics and other objects; the high number of figurines found on Misti (47) indicates that the site was important to the Incas. These mummies were Inca human sacrifices, called &quot;capacochas&quot;, and the Misti &quot;capacocha&quot; is the largest known. However, the hostile conditions within the crater had seriously damaged the mummies.

Geographic entities mentioned:
surface_form: 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
However, the hostile conditions within the crater had seriously damaged the mummies. The sacrifices on Misti, and others on Chachani and Pichu Pichu, were probably motivated by the 1440–1470 eruption of Misti, which may explain the unusual location within the crater rather than on a summit.

Geographic entities mentioned:
surface_form: 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
According to the 16th century chronicler Martín de Murúa, the Inca emperor Thupa Yapanki sacrificed llamas to calm a volcano Putina close to Arequipa (probably Misti), going as closely as possible to the summit. According to stories, previous ceremonies had failed to calm the volcano and only the emperor's direct intervention quelled its anger.

Geographic entities mentioned:
surface_form: 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 main ascent route according to mountaineer John Biggar is from the Aguada Blanca dam; a permit is needed to cross the dam. There are campsites at around elevation, accessible from the Aguada Blanca dam and the town of Chihuata south of Misti. The ascent to the summit takes about one long day.

Geographic entities mentioned:
surface_form: 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 indigenous names are (&quot;mountain that growls&quot;) and in the Aymara language, &quot;Anukara&quot; or (&quot;dog&quot;), which both refer to the dog-like appearance of the volcano when viewed from the Andean Plateau known as the Altiplano. The volcano was originally known as Putina and only became known as Misti beginning in the 1780s.

Geographic entities mentioned:
surface_form: putina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.296388888888888
lon: -71.41055555555556
Other Peruvian volcanoes in the CVZ are Ampato, Casiri, Coropuna, Huambo volcanic field, Purupuruni and Sara Sara. Ubinas is the most active volcano in Peru, having erupted more than 23 times since 1550. The 1600 eruption of Huaynaputina claimed more than 1,000 casualties; recent eruptions of Sabancaya 1987–1998 and Ubinas 2006–2007 had severe impacts on the local populations. General outline.

Geographic entities mentioned:
surface_form: ubinas
instance_of: Mountain
countries: Peru
coordinates: lat: -16.34861111111111
lon: -70.90222222222222
Volcanic activity in southern Peru goes back to the Jurassic, but the currently recognizable volcanic arcs in Peru are more recent: the Tacaza Arc formed 30–15 million years ago, the Lower Barroso 9–4 million, the Upper Barroso 3–1 million, and the Pleistocene-Holocene Frontal Arc during the past one million years.

Geographic entities mentioned:
surface_form: barroso
instance_of: Mountain
countries: Peru
coordinates: lat: -17.556308
lon: -69.5954717
surface_form: barroso
instance_of: Mountain
countries: Peru
coordinates: lat: -17.556308
lon: -69.5954717
In 2002, he graduated from Nordonia High School in Macedonia, Ohio. Early career (2002–2008). After graduating from high school in 2002, Foster followed on his father's advice and moved out to live with an uncle in the San Fernando Valley neighborhood of Sylmar, Los Angeles. As a result he would be closer to pursuing his musical dreams.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Mount Royal National Park. The Mount Royal National Park is a protected national park located in the Hunter region of New South Wales, Australia. Gazetted in 1997, the park is situated approximately north of Sydney. Sections of the park had been subject to logging, which was disrupted by a blockade in 1989.

Geographic entities mentioned:
surface_form: Hunter
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
During the 2019 Australian Bushfire Season, the park was damaged by the 'Mount Royal 1' fire. Major Peaks. Mount Royal is the highest peak at 1,186m. Pieres Peak is a major peak south of Mount Royal at 986m. Fauna. The park is home to endangered animal species such as parma wallaby, rufous scrub bird, paradise riflebird, hastings river mouse and the glossy black-cockatoo.

Geographic entities mentioned:
surface_form: Pieres Peak
instance_of: Mountain
countries: Australia
coordinates: lat: -32.2097
lon: 151.3043
Examples. Icefalls vary greatly in height. The Roosevelt Glacier icefall, on the north face of Mount Baker (Cascade Range, U.S.), is about high. The ice cliff of the left side of the ice fall and above the debris covering the glacier is high. Typical of mountain glaciers, this icefall forms as the ice flows from a high elevation plateau or basin accumulation zone to a lower valley ablation zone.

Geographic entities mentioned:
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Icefalls are climbed because of their beauty and the challenge they pose. In some cases, an icefall may provide the only feasible or the easiest route up one face of a mountain. An example is the Khumbu Icefall on the Nepalese side of Mount Everest, variously described as &quot;treacherous&quot; and &quot;dangerous.&quot; It is about above sea level.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Finch Mountain. Finch Mountain is a summit located in Adirondack Mountains of New York located in the Town of Wells southwest of the hamlet of Wells.

Geographic entities mentioned:
surface_form: finch mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.36
lon: -74.349444444444
Weyakwin. Weyakwin is a northern hamlet in the Canadian province of Saskatchewan. It is situated along Highway 2 on the south bank of Weyakwin River. The Weyakwin River flows from Weyakwin Lake east to Montreal Lake. Name. The name of the community comes from the Cree language, meaning &quot;Foul or profane language&quot;. The community is known in Cree as ᐏᔭᐦᑵᐏᓂᕽ &quot;wiyahkwêwinihk&quot;.

Geographic entities mentioned:
surface_form: Weyakwin Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.50005
lon: -106.00049
On 23 December 1834, Nangle opened the Achill Mission's first school. Forty three children attended on the first day, and it was the first free school to open on the island. Within a couple of months there were schools in Dugort, Slievemore, Cashel and Keel, catering for 410 children. In December 1835, a printing press was established at the Mission Colony headquarters at Dugort.

Geographic entities mentioned:
surface_form: Slievemore
instance_of: Mountain
countries: Ireland
coordinates: lat: 54.00905
lon: -10.059938888889
A succession of the priests addressed the crowd and denounced the colony, pronouncing a curse on all who dared associate themselves with the nearby Protestant settlement. In 1835, after the Mission opened schools in Dugort, Cashel, Keel and Slievemore, the local parish priest responded by opening three competing schools.

Geographic entities mentioned:
surface_form: Slievemore
instance_of: Mountain
countries: Ireland
coordinates: lat: 54.00905
lon: -10.059938888889
Yuraq Urqu (Arequipa-Moquegua). Yuraq Urqu (Quechua &quot;yuraq&quot; white, &quot;urqu&quot; mountain, &quot;white mountain&quot;, also spelled &quot;Yurac Orcco&quot;) is a mountain in the Andes of Peru. It is located in the Arequipa Region, Arequipa Province, Tarucani District, and in the Moquegua Region, General Sánchez Cerro Province, Ubinas District.

Geographic entities mentioned:
surface_form: yuraq urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5025
lon: -72.7253
surface_form: yuraq urqu (arequipa-moquegua)
instance_of: Mountain
countries: Peru
coordinates: lat: -16.0417
lon: -70.8075
surface_form: yuraq urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -15.2044
lon: -72.5419
Yuraq Urqu (Arequipa-Moquegua). Yuraq Urqu (Quechua &quot;yuraq&quot; white, &quot;urqu&quot; mountain, &quot;white mountain&quot;, also spelled &quot;Yurac Orcco&quot;) is a mountain in the Andes of Peru. It is located in the Arequipa Region, Arequipa Province, Tarucani District, and in the Moquegua Region, General Sánchez Cerro Province, Ubinas District.

Geographic entities mentioned:
surface_form: yuraq urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5025
lon: -72.7253
surface_form: yurac orcco
instance_of: Mountain
countries: Peru
coordinates: lat: -16.0417
lon: -70.8075
surface_form: yuraq urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -15.2044
lon: -72.5419
Yuraq Urqu (Quechua &quot;yuraq&quot; white, &quot;urqu&quot; mountain, &quot;white mountain&quot;, also spelled &quot;Yurac Orcco&quot;) is a mountain in the Andes of Peru. It is located in the Arequipa Region, Arequipa Province, Tarucani District, and in the Moquegua Region, General Sánchez Cerro Province, Ubinas District. Yuraq Urqu lies east of Piñani Lake &quot;(Peñane)&quot;.

Geographic entities mentioned:
surface_form: ubinas
instance_of: Mountain
countries: Peru
coordinates: lat: -16.34861111111111
lon: -70.90222222222222
surface_form: tarucani
instance_of: Mountain
countries: Peru
coordinates: lat: -13.8794
lon: -70.7533
The lordships included Boyne and Enzie on the coast, plus the inland areas of Strathisla and several small lordships along the eastern side of the strath of the River Spey and its tributaries, including Glenlivet, Strathavon and Glenfiddich.

Geographic entities mentioned:
surface_form: Glenlivet
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.349166666667
lon: -3.3319444444444
surface_form: Strathavon
instance_of: Valley
countries: United Kingdom
Khunti, Ranchi, Gumla, and Chakradharpur are nearby cities. It is in the border of the Khunti District and Gumla District. Gumla District Kamdara is west from Dorma. Physiography. Uneven plains and some rocky mountains lie as this region comes under plateau region of Chotta Nagpur. Demographics. Hindi is the local language. Most of the population are Munda people, speaking Mundari language.

Geographic entities mentioned:
surface_form: Chotta Nagpur
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
It covers parts of Ternopil, Ivano-Frankivsk, Chernivtsi, and Khmelnytskyi Oblasts. It is situated on the Podolian Upland and, northeast of the Carpathian Mountains. The canyon reaches a depth of. Canyon segments. The Dniestrovo-Beremyanskyi Canyon situated between villages of Hubyn, Beremiany, and Khmeleva, is a branch of the larger Dniester Canyon. Its depth reaches, is wide, and long. Geology.

Geographic entities mentioned:
surface_form: Podolian Upland
instance_of: Plateau
countries: Ukraine
Moldova
coordinates: lat: 49.0275
lon: 27.85619444
Geography. It is one of the youngest mountain ranges of China. It is relatively narrow with a width between 5 and 12 km, and a length of around 240 km. The highest peak, Migangshan (米缸山), is at above sea level. Owing to its orientation perpendicular to humid winds, it is considered a 'green island' within the Loess Plateau. Most of the mountain's area is covered by forests.

Geographic entities mentioned:
surface_form: Loess Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
The Salmon Arm Roots and Blues Festival is a 3 day summer music festival. It has four - six stages and features an international roster of artists as well as a strong contingent of Canadian talent. The event takes place at the Salmon Arm Fair Grounds, an 18-acre site at the base of Mount Ida in Salmon Arm, a town located on the shores of the Shuswap Lake in British Columbia.

Geographic entities mentioned:
surface_form: Shuswap Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.000693
lon: -119.01263
Evidence indicates that this was a site of ritual significance. Chalcatzingo is situated near two large granodiorite hills in the Amatzinac River Valley, within an otherwise generally flat landscape. Its early residents likely sourced their water from a nearby spring. Chalcatzingo connected trade routes between Guerrero, the Valley of Mexico, Oaxaca, and the Gulf Lowlands. Monuments and carvings.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
Pindamonhangaba. Pindamonhangaba is a municipality in the state of São Paulo, Brazil, located in the Paraíba Valley, between the two most active production and consumption regions in the country, São Paulo and Rio de Janeiro. It is accessible by the Via Dutra (BR-116 &ndash; SP-60 highway) at the 99th kilometer.

Geographic entities mentioned:
surface_form: Paraíba Valley
instance_of: Valley
countries: Brazil
coordinates: lat: -22.75
lon: -45.15
It was formed in 2012, combining the territory of the former Shuanghu Special District (,) with the eastern half of Nyima County. Much of the county is within the Changtang area. Shuanghu is the highest county of China with an average elevation of more than, while its county seat is located at.

Geographic entities mentioned:
surface_form: Changtang
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 30
lon: 90
In the 1970s, population growth in Xainza and Baingoin counties led to overgrazing and frequent conflicts. Xainza County launched surveys into the uninhabited Changtang region in the north of the county from 1971 to 1975, and identified several areas suitable for grazing. In 1976, 2,053 Xainza nomads reached Shuanghu after a month-long trek, together with their 160,000 cattle, goats and sheep.

Geographic entities mentioned:
surface_form: Changtang
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 30
lon: 90
The siphuncle swelling at the apex is subtriangular in longitudinal profile. The endocones are of medium length. &quot;Chazyoceras&quot; was named by Rousseau Flower in 1958. The genotype is &quot;Chazyoceras valcourense&quot; which came from the Middle Chazyan (Lower Middle Ordovician) of Valcour Island on Lake Champlain.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
The summit was found to be 2.42 ft short. Ascent. The most normal starting point for climbing Beinn Dearg is the car park at the foot of the Abhainn Coire Mhic Nobuil, which is also the normal start point for an ascent of Beinn Alligin. From here the river is followed until the confluence with the Allt à Bhealaich.

Geographic entities mentioned:
surface_form: Beinn Alligin
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.59081
lon: -5.57283
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.78635
lon: -4.929557
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.877346
lon: -3.883719
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.5888
lon: -5.52136
From here the river is followed until the confluence with the Allt à Bhealaich. This burn may be followed up to the low bealach or saddle between Beinn Dearg and Beinn Alligin, at which point the walker can strike upwards for the western end of the summit ridge. Alternative routes of ascent may be made by continuing to follow the Abhainn Coire Mhic Nobuil under the south side of the hill.

Geographic entities mentioned:
surface_form: Beinn Alligin
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.59081
lon: -5.57283
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.78635
lon: -4.929557
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.877346
lon: -3.883719
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.5888
lon: -5.52136
Beinn Dearg (Torridon). Beinn Dearg is the fourth highest of the Torridon Hills in the highlands of Scotland. Beinn Dearg offers all the typical features of a Torridon hill, with steeply terraced rocky sides dissected by near vertical gullies.

Geographic entities mentioned:
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.78635
lon: -4.929557
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.877346
lon: -3.883719
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.5888
lon: -5.52136
Beinn Dearg is the fourth highest of the Torridon Hills in the highlands of Scotland. Beinn Dearg offers all the typical features of a Torridon hill, with steeply terraced rocky sides dissected by near vertical gullies. The summit ridge is an airy crest that offers some easy scrambling; alternatively this can be avoided by following a path that traverses the terraces on the southern side.

Geographic entities mentioned:
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.78635
lon: -4.929557
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.877346
lon: -3.883719
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.5888
lon: -5.52136
For this reason, if no other, it is climbed far less than the three major mountains surrounding it. In 2007, the Munro Society commissioned CMCR Ltd to survey Beinn Dearg in order to ascertain the precise height of the summit, and determine whether it might in fact be correctly categorised as a Munro. The summit was found to be 2.42 ft short. Ascent.

Geographic entities mentioned:
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.78635
lon: -4.929557
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.877346
lon: -3.883719
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.5888
lon: -5.52136
Two gullies offer routes to the summit ridge, either side of the subsidiary peak of Carn na Feòla at the eastern end of the 4 km long ridge. By combining two of the three routes described above one may complete a traverse of Beinn Dearg. The summit offers excellent views of the well known surrounding peaks of Torridon.

Geographic entities mentioned:
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.78635
lon: -4.929557
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.877346
lon: -3.883719
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.5888
lon: -5.52136
The castle was built in Late Antiquity around the time of Constantine the Great, rebuilt with a smaller wall around the time of Justinian I, and was strategically located where a branch of Via Egnatia met the Lissus–Naissus road. It is near the Black Drin Valley in a region where a line of late Roman forts is found and of which Grazhdan is the largest.

Geographic entities mentioned:
surface_form: Drin Valley
instance_of: Valley
countries: Albania
coordinates: lat: 40.283333
lon: 20.033333
Horner was sixth, 51 seconds down, but still held a lead of 38 seconds over Leipheimer and over a minute against the next highest rider. The two captains dominated stage 7 to Mount Baldy. They broke away from the lead group with to go to the summit and finished 43 seconds clear of any other riders.

Geographic entities mentioned:
surface_form: Mount Baldy
instance_of: Mountain
countries: United States
coordinates: lat: 34.2889
lon: -117.647
Shire of Wongan–Ballidu. The Shire of Wongan–Ballidu is a local government area in the Wheatbelt region of Western Australia, about NNE of Perth, the state capital. The Shire covers an area of and its seat of government is the town of Wongan Hills. The shire includes the Wongan Hills, after which the town is named. History. On 10 February 1887, the Melbourne Road District was created.

Geographic entities mentioned:
surface_form: Wongan Hills
instance_of: Mountain
countries: Australia
coordinates: lat: -30.8
lon: 116.617
He investigates the role of the Feminine in the history of Christianity and considers the dialogue with other spiritual traditions. Biography. Jean-Yves Leloup was born in 1950 in Angers. Theologian, novelist and essayist, initiated into Buddhism, trained at Mount Athos, became a Dominican priest, then became Orthodox.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
The village is on the edge of the Lake District National Park. The roads from St. Michael's Church towards Loweswater and from the church towards Ennerdale form part of the national park boundary, with the national park lying to the east of the roads. While parts of the village lie within the national park, almost all dwellings are outside the national park and so are cheaper than in Loweswater.

Geographic entities mentioned:
surface_form: Loweswater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5825
lon: -3.355277777777778
The roads from St. Michael's Church towards Loweswater and from the church towards Ennerdale form part of the national park boundary, with the national park lying to the east of the roads. While parts of the village lie within the national park, almost all dwellings are outside the national park and so are cheaper than in Loweswater. The boundary of this large parish is shown on 1:25,000 O.S.

Geographic entities mentioned:
surface_form: Loweswater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5825
lon: -3.355277777777778
History. It was discovered and roughly mapped on 11 January 1910, by the Fourth French Antarctic Expedition under Jean-Baptiste Charcot, and named by him in association with Mount Monique and the Marion Nunataks after his daughter, Martine. It was photographed from the air on 9 February 1947 in the course of the US Navy's Operation Highjump and mapped from these photographs by D.

Geographic entities mentioned:
surface_form: Mount Monique
instance_of: Mountain
coordinates: lat: -69.75
lon: -75.5
surface_form: Marion Nunataks
instance_of: Mountain
coordinates: lat: -69.75
lon: -75.25
surface_form: monique
instance_of: Mountain
coordinates: lat: -69.75
lon: -75.5
surface_form: martine
instance_of: Mountain
coordinates: lat: -69.75
lon: -75.0833
Mount Martine. Mount Martine is a massive mountain, about high, with a prominent rocky north face and ice-covered south slopes, overlooking the north shore of Charcot Island, south of Cheesman Island, in the east Bellinghausen Sea of Antarctica. History.

Geographic entities mentioned:
surface_form: mount martine
instance_of: Mountain
coordinates: lat: -69.75
lon: -75.0833
surface_form: martine
instance_of: Mountain
coordinates: lat: -69.75
lon: -75.0833
History. It was discovered and roughly mapped on 11 January 1910, by the Fourth French Antarctic Expedition under Jean-Baptiste Charcot, and named by him in association with Mount Monique and the Marion Nunataks after his daughter, Martine. It was photographed from the air on 9 February 1947 in the course of the US Navy's Operation Highjump and mapped from these photographs by D.

Geographic entities mentioned:
surface_form: searle
instance_of: Mountain
coordinates: lat: -67.81666667
lon: -67.25
It was photographed from the air on 9 February 1947 in the course of the US Navy's Operation Highjump and mapped from these photographs by D. Searle of the Falkland Islands Dependencies Survey in 1960. The mountain forms part of the Marion Nunataks Antarctic Specially Protected Area (ASPA No.170) designated as such for its biological values.

Geographic entities mentioned:
surface_form: marion nunataks
instance_of: Mountain
coordinates: lat: -69.75
lon: -75.25
Train services today require three changes at Brixen, Lienz and Graz and are separately operated by Trenitalia, Südtirol Bahn, ÖBB and Slovenian Railways (SZ). In 1881, a third railway line, Vinschgau railway, joined the Bolzano/Bozen station through Merano, County of Tyrol's capital city. In order to cater for frequent holiday makers, it was extended in 1906 from Merano to Mals.

Geographic entities mentioned:
surface_form: Vinschgau
instance_of: Valley
countries: Italy
coordinates: lat: 46.615
lon: 10.705
Bohlinryggen. Bohlinryggen is a mountain ridge in Wedel Jarlsberg Land at Spitsbergen, Svalbard. It has a length of about 4.5 kilometers, and the highest peak is 716 m.a.s.l. It is located between the glaciers Scottbreen and Renardbreen. The ridge is named after Swedish astronomer Karl Bohlin.

Geographic entities mentioned:
surface_form: bohlinryggen
instance_of: Mountain
countries: Norway
coordinates: lat: 77.535
lon: 14.3927
Tumala Mountain. Tumala Mountain is part of the Clackamas Foothills near Mount Hood in the U.S. state of Oregon. It is located in Mount Hood National Forest, near the city of Estacada. The summit has an elevation of. In 2007, the Board on Geographic Names renamed the mountain, which was previously called Squaw Mountain, due to the word &quot;squaw&quot; being offensive.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
surface_form: mount hood
instance_of: Mountain
countries: United States
coordinates: lat: 38.4599
lon: -122.553
surface_form: tumala mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.23035012
lon: -122.04114618
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
state of Oregon. It is located in Mount Hood National Forest, near the city of Estacada. The summit has an elevation of. In 2007, the Board on Geographic Names renamed the mountain, which was previously called Squaw Mountain, due to the word &quot;squaw&quot; being offensive. The word &quot;Tumala&quot; means &quot;tomorrow&quot; or &quot;afterlife&quot; in Chinook Wawa.

Geographic entities mentioned:
surface_form: squaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.271944444444
lon: -111.61638888889
Tumala Mountain. Tumala Mountain is part of the Clackamas Foothills near Mount Hood in the U.S. state of Oregon. It is located in Mount Hood National Forest, near the city of Estacada. The summit has an elevation of. In 2007, the Board on Geographic Names renamed the mountain, which was previously called Squaw Mountain, due to the word &quot;squaw&quot; being offensive.

Geographic entities mentioned:
surface_form: mount hood
instance_of: Mountain
countries: United States
coordinates: lat: 38.4599
lon: -122.553
surface_form: mount hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
Tumala Mountain. Tumala Mountain is part of the Clackamas Foothills near Mount Hood in the U.S. state of Oregon. It is located in Mount Hood National Forest, near the city of Estacada. The summit has an elevation of. In 2007, the Board on Geographic Names renamed the mountain, which was previously called Squaw Mountain, due to the word &quot;squaw&quot; being offensive.

Geographic entities mentioned:
surface_form: tumala mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.23035012
lon: -122.04114618
As the canal continues northwards, it reaches the first of twelve locks at Gailey, which drop the canal down to Great Haywood Junction. The M6 motorway passes between Calf Heath reservoir and the two Gailey Reservoirs, which supply water to the canal, and then runs alongside the canal for, before the canal passes through the centre of Penkridge.

Geographic entities mentioned:
surface_form: Gailey Reservoirs
instance_of: Group of lakes
countries: United Kingdom
coordinates: lat: 52.69035
lon: -2.0976
In 1876 he visited Egypt and the Arabian Desert (with Georg August Schweinfurth). He made several first ascents in the Alps, including Piz Scerscen with Hans Grass and Caspar Capat on 13 September 1877 via the north-west spur (the &quot;Eisnase&quot; route). On 12 August 1878, Hans Grass, Johann Gross and he first climbed the &quot;Biancograt&quot; north ridge of Piz Bernina.

Geographic entities mentioned:
surface_form: Piz Scerscen
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 46.37825
lon: 9.9005833333333
In 1876 he visited Egypt and the Arabian Desert (with Georg August Schweinfurth). He made several first ascents in the Alps, including Piz Scerscen with Hans Grass and Caspar Capat on 13 September 1877 via the north-west spur (the &quot;Eisnase&quot; route). On 12 August 1878, Hans Grass, Johann Gross and he first climbed the &quot;Biancograt&quot; north ridge of Piz Bernina.

Geographic entities mentioned:
surface_form: Piz Bernina
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.382388888889
lon: 9.9081111111111
On 12 August 1878, Hans Grass, Johann Gross and he first climbed the &quot;Biancograt&quot; north ridge of Piz Bernina. He made winter ascents of the Grandes Jorasses and the Gran Paradiso, as well as putting up several new routes on Mont Blanc, including the Peuterey ridge on 15–19 August 1893 (with Emile Rey, Christian Klucker and César Ollier).

Geographic entities mentioned:
surface_form: Grandes Jorasses
instance_of: Mountain
countries: Italy
France
coordinates: lat: 45.866666666667
lon: 6.9833333333333
surface_form: Gran Paradiso
instance_of: Mountain
countries: Italy
coordinates: lat: 45.533333333333
lon: 7.2666666666667
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
&quot;Pointe Güssfeldt&quot; (4,112 m), the highest summit on the Aiguille Blanche de Peuterey is named after him, as is the &quot;Güssfeldtsattel&quot;, the col between Piz Scerscen and Piz Roseg also known as the &quot;Porta da Roseg&quot;. This steep ice slope was first climbed by Güssfeldt with guides Hans Grass, Peter Jenny and Caspar Capat on 13 September 1872.

Geographic entities mentioned:
surface_form: Aiguille Blanche de Peuterey
instance_of: Mountain
countries: Italy
coordinates: lat: 45.824444444444
lon: 6.8827777777778
surface_form: Piz Roseg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.37375
lon: 9.8830833333333