Sarmila/GeoWiki-Features huggingface dataset:
A recreational trail called the W.O.W. Trail (Winnipesaukee–Opechee–Winnisquam) links several parts of the city, following the railroad tracks from Lake Winnisquam, skirting the downtown area, and running to Lakeport. A desire to extend the trail to Weirs Beach has been contested by residents in private communities abutting the rail corridor.

Geographic entities mentioned:
surface_form: Winnipesaukee
instance_of: Lake
countries: United States
coordinates: lat: 43.598888888889
lon: -71.323055555556
surface_form: Opechee
instance_of: Lake
countries: United States
coordinates: lat: 43.546666666667
lon: -71.474722222222
surface_form: Winnisquam
instance_of: Lake
countries: United States
coordinates: lat: 43.545
lon: -71.508888888889
According to the United States Census Bureau, the city has a total area of, of which are land and are water, comprising 23.93% of the city. Laconia is drained by the Winnipesaukee River. It is bounded in the southwest by Lake Winnisquam, and by Lake Winnipesaukee in the northeast. Laconia lies fully within the Merrimack River watershed.

Geographic entities mentioned:
surface_form: Lake Winnisquam
instance_of: Lake
countries: United States
coordinates: lat: 43.545
lon: -71.508888888889
The name Sennenhund refers to people called &quot;Senn&quot;, herders in the Swiss Alps. Entlebuch is a region in the canton of Lucerne in Switzerland. The breed is also known in English as the Entelbuch Mountain Dog, Entelbucher Cattle Dog, and similar combinations. History.

Geographic entities mentioned:
surface_form: Entlebuch
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.75
lon: 7.8
In the Philippines, its range includes several islands in the southern region of the archipelago, notably Basilan, Cebu, Negros, Palawan, Camiguin, and Mindanao—where it has been specifically documented on Mount Malindang—as well as the Sulu Archipelago islands of Tawi-Tawi, Bongao, Papahag, and Inampulupan.

Geographic entities mentioned:
surface_form: Mount Malindang
instance_of: Mountain
countries: Philippines
coordinates: lat: 8.2175
lon: 123.63666666667
Gens de Terre River. The Gens de Terre River (in French: &quot;Rivière Gens de Terre&quot;, literal meaning: &quot;people of the land&quot;) is a river in central Quebec, Canada. It is located on the eastern edge of the La Vérendrye Wildlife Reserve in the La Vallée-de-la-Gatineau Regional County Municipality in the Outaouais region.

Geographic entities mentioned:
surface_form: gens de terre river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.86833333333333
lon: -75.955
Gens de Terre River. The Gens de Terre River (in French: &quot;Rivière Gens de Terre&quot;, literal meaning: &quot;people of the land&quot;) is a river in central Quebec, Canada. It is located on the eastern edge of the La Vérendrye Wildlife Reserve in the La Vallée-de-la-Gatineau Regional County Municipality in the Outaouais region.

Geographic entities mentioned:
surface_form: gens de terre river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.86833333333333
lon: -75.955
surface_form: rivière gens de terre
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.86833333333333
lon: -75.955
Sairecabur. Sairecabur () is a volcano located on the frontier between Bolivia and Chile. It is part of the Andean Central Volcanic Zone. Sairecabur proper is high; other mountains in the range are high Curiquinca, high Escalante and high Cerro Colorado, all of which have erupted a number of lava flows. Also in close proximity to Sairecabur lie the volcanic centres Licancabur, Putana and Juriques.

Geographic entities mentioned:
surface_form: Curiquinca
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.59723333
lon: -67.86133333
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
It is part of the Andean Central Volcanic Zone. Sairecabur proper is high; other mountains in the range are high Curiquinca, high Escalante and high Cerro Colorado, all of which have erupted a number of lava flows. Also in close proximity to Sairecabur lie the volcanic centres Licancabur, Putana and Juriques. Sairecabur proper is accompanied by a wide caldera.

Geographic entities mentioned:
surface_form: Juriques
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.845277777778
lon: -67.824722222222
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
surface_form: putana
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.557302
lon: -67.852834
Effusion of large amounts of lava took place from several cones. Many volcanoes are extinct and only a few have documented activity. The geologist Juan Brüggen in 1950 estimated that there were about 800 volcanoes in northern Chile, about 37 of them east of the Salar de Atacama. Also part of the volcanism are large ignimbrites, which are usually thought to be of Miocene age.

Geographic entities mentioned:
surface_form: Salar de Atacama
instance_of: Lake
Body of water
countries: Chile
coordinates: lat: -23.416666666666668
lon: -68.26666666666667
In Chile, much of the area of the CVZ is desert and thus difficult to research. Sairecabur is constructed on the two Pliocene-Pleistocene Puripicar and Chaxas formations. Some lavas from Sairecabur have also overrun the Purico formation, which is of Pleistocene age and includes ignimbrites from the Purico Complex. The basement beneath Sairecabur and Licancabur contains a large number of faults.

Geographic entities mentioned:
surface_form: Purico Complex
instance_of: Mountain
countries: Chile
coordinates: lat: -23
lon: -67.75
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
The volcano saddles the frontier between Bolivia and Chile, where it lies in the Antofagasta Region. Laguna Verde lake, Licancabur volcano and Portezuelo de Chaxas pass lie south of Sairecabur. East of the Sairecabur range lie Mount Nelly and Cerro Laguna Verde. The Treaty of Peace and Friendship (1904) traced the frontier between Bolivia and Chile along the Sairecabur chain.

Geographic entities mentioned:
surface_form: Mount Nelly
instance_of: Mountain
countries: Bolivia
coordinates: lat: -22.698611111111
lon: -67.754722222222
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
The Sairecabur range forms a drainage divide between the Salar de Atacama on the western side and a number of small endorheic basins in Bolivia on the eastern side. Licancabur and Juriques farther south and Tocorpuri farther north are part of the same divide. Dry valleys on the eastern side of the Sairecabur range ultimately drain into Laguna Verde.

Geographic entities mentioned:
surface_form: Tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
The caldera is bounded by cliffs reaching a height of, which are buried by lava flows from Sairecabur on the northern rim; one of these lava flows reaches the caldera bottom. The pre-collapse volcano was about high and would have been one of the highest volcanoes in the world; Ojos del Salado reaches an altitude of. Sairecabur proper has three cones.

Geographic entities mentioned:
surface_form: Ojos del Salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Sairecabur. Sairecabur () is a volcano located on the frontier between Bolivia and Chile. It is part of the Andean Central Volcanic Zone. Sairecabur proper is high; other mountains in the range are high Curiquinca, high Escalante and high Cerro Colorado, all of which have erupted a number of lava flows. Also in close proximity to Sairecabur lie the volcanic centres Licancabur, Putana and Juriques.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Also in close proximity to Sairecabur lie the volcanic centres Licancabur, Putana and Juriques. Sairecabur proper is accompanied by a wide caldera. Before the formation of this caldera the volcano may have been high and thus one of the highest volcanoes on Earth.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Before the formation of this caldera the volcano may have been high and thus one of the highest volcanoes on Earth. After the formation of this caldera lava effusion occurred during the Pleistocene and Holocene; there is no reported historical activity, however. Eruption products on Escalante and Sairecabur include andesite and dacite. The climate is dry, cold and very sunny.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Eruption products on Escalante and Sairecabur include andesite and dacite. The climate is dry, cold and very sunny. An Inca sanctuary has been found on Sairecabur, and sulfur mines exist in the mountain chain. More recently, the Receiver Lab Telescope was installed on the volcano. It is the highest submillimeter telescope in the world at an altitude of. Geological context.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
These volcanic zones are separated from each other by zones where there is no volcanism, associated with a shallow dip of the seismic zone of the subducting plate. Sairecabur is part of the Andean Central Volcanic Zone (CVZ). A number of stratovolcanoes can be found in the area, many of which were affected by explosive eruptions that have destroyed parts of their edifices.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Also part of the volcanism are large ignimbrites, which are usually thought to be of Miocene age. Those in the area of Sairecabur often originated in the neighbourhood to the conical volcanoes. The volcanoes formed over crust with thicknesses reaching, thus the erupted magmas are heavily influenced by the crust. A number of the highest stratovolcanoes in the world are in the CVZ.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
In Chile, much of the area of the CVZ is desert and thus difficult to research. Sairecabur is constructed on the two Pliocene-Pleistocene Puripicar and Chaxas formations. Some lavas from Sairecabur have also overrun the Purico formation, which is of Pleistocene age and includes ignimbrites from the Purico Complex. The basement beneath Sairecabur and Licancabur contains a large number of faults.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Sairecabur is constructed on the two Pliocene-Pleistocene Puripicar and Chaxas formations. Some lavas from Sairecabur have also overrun the Purico formation, which is of Pleistocene age and includes ignimbrites from the Purico Complex. The basement beneath Sairecabur and Licancabur contains a large number of faults. Geography. Sairecabur is located at a distance of from San Pedro de Atacama.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
The basement beneath Sairecabur and Licancabur contains a large number of faults. Geography. Sairecabur is located at a distance of from San Pedro de Atacama. The volcano saddles the frontier between Bolivia and Chile, where it lies in the Antofagasta Region. Laguna Verde lake, Licancabur volcano and Portezuelo de Chaxas pass lie south of Sairecabur.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Geography. Sairecabur is located at a distance of from San Pedro de Atacama. The volcano saddles the frontier between Bolivia and Chile, where it lies in the Antofagasta Region. Laguna Verde lake, Licancabur volcano and Portezuelo de Chaxas pass lie south of Sairecabur. East of the Sairecabur range lie Mount Nelly and Cerro Laguna Verde.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Laguna Verde lake, Licancabur volcano and Portezuelo de Chaxas pass lie south of Sairecabur. East of the Sairecabur range lie Mount Nelly and Cerro Laguna Verde. The Treaty of Peace and Friendship (1904) traced the frontier between Bolivia and Chile along the Sairecabur chain. Disagreements between the topographic maps in the two countries mean that the naming of the mountains is often confusing.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Escalante is also known as Apagado. The volcano is associated with a mountain range of the same name. The Sairecabur range forms a drainage divide between the Salar de Atacama on the western side and a number of small endorheic basins in Bolivia on the eastern side. Licancabur and Juriques farther south and Tocorpuri farther north are part of the same divide.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Licancabur and Juriques farther south and Tocorpuri farther north are part of the same divide. Dry valleys on the eastern side of the Sairecabur range ultimately drain into Laguna Verde. The Rio Purifica originates on Sairecabur's slope at an altitude of, it later converges with the Rio Puritama to form the San Pedro de Atacama River. Geology.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Geology. The Sairecabur range is a long chain of volcanoes going from Escalante volcano (south of Putana Volcano) to Sairecabur proper in the south, including at least ten centres which have been active in postglacial time. Two additional centres exist northeast of Escalante. high Sairecabur is the highest volcano in the range.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
surface_form: putana
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.557302
lon: -67.852834
The Sairecabur range is a long chain of volcanoes going from Escalante volcano (south of Putana Volcano) to Sairecabur proper in the south, including at least ten centres which have been active in postglacial time. Two additional centres exist northeast of Escalante. high Sairecabur is the highest volcano in the range. A wide caldera exists south of Sairecabur and formed on an older volcano.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Two additional centres exist northeast of Escalante. high Sairecabur is the highest volcano in the range. A wide caldera exists south of Sairecabur and formed on an older volcano. Lava flows extend from Sairecabur as far as to the northwest, and further young lava flows formed south of this caldera. The high Escalante () has a crater lake.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
high Sairecabur is the highest volcano in the range. A wide caldera exists south of Sairecabur and formed on an older volcano. Lava flows extend from Sairecabur as far as to the northwest, and further young lava flows formed south of this caldera. The high Escalante () has a crater lake. Puritama volcano west of Sairecabur has generated lava flows that extend along tectonic canyons.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Lava flows extend from Sairecabur as far as to the northwest, and further young lava flows formed south of this caldera. The high Escalante () has a crater lake. Puritama volcano west of Sairecabur has generated lava flows that extend along tectonic canyons. high Curiquinca () and high Cerro Colorado () are found northwest and northeast, respectively, of the range.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Puritama volcano west of Sairecabur has generated lava flows that extend along tectonic canyons. high Curiquinca () and high Cerro Colorado () are found northwest and northeast, respectively, of the range. The caldera is bounded by cliffs reaching a height of, which are buried by lava flows from Sairecabur on the northern rim; one of these lava flows reaches the caldera bottom.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
The pre-collapse volcano was about high and would have been one of the highest volcanoes in the world; Ojos del Salado reaches an altitude of. Sairecabur proper has three cones. Thick () and short lava flows emanated from the northern cone. Glacial erosion has affected Sairecabur and moraines cover some lava flows south of Sairecabur. The total volume of the Sairecabur proper is about.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Sairecabur proper has three cones. Thick () and short lava flows emanated from the northern cone. Glacial erosion has affected Sairecabur and moraines cover some lava flows south of Sairecabur. The total volume of the Sairecabur proper is about. Lava flows with a young appearance extend from each of these ten centres. An older centre has generated a long lava flow that flowed southwestwards.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Sairecabur proper has three cones. Thick () and short lava flows emanated from the northern cone. Glacial erosion has affected Sairecabur and moraines cover some lava flows south of Sairecabur. The total volume of the Sairecabur proper is about. Lava flows with a young appearance extend from each of these ten centres. An older centre has generated a long lava flow that flowed southwestwards.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
The total volume of the Sairecabur proper is about. Lava flows with a young appearance extend from each of these ten centres. An older centre has generated a long lava flow that flowed southwestwards. Some older lava flows from Sairecabur were later buried by lava flows from Licancabur. Cerro Colorado and Curiquinca are aligned in a west–east pattern.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Cerro Colorado and Curiquinca are aligned in a west–east pattern. Other volcanoes in the area such as Lascar-Aguas Calientes, Licancabur-Juriques and La Torta-Tocorpuri also form such alignments which seem to be controlled by north–south tension in the crust. Sairecabur is located on faults which are also apparent at Laguna Verde. Petrology.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Sairecabur is located on faults which are also apparent at Laguna Verde. Petrology. Escalante and Sairecabur have erupted dark andesites, and later also dacites. Mafic enclaves are found in the post-caldera lavas. The colour of the rocks is black, brown or gray.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
In addition, apatite, ilmenite, iron oxides and zirconia are found. At least one lava erupted after the caldera-forming eruption contains olivine. Lavas erupted before the caldera-forming eruption of Sairecabur contain glass and have a microlithic texture. The magmas are calc-alkaline with medium-high potassium content. Fumarolically altered rocks are found on the eastern flanks of the chain.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Fumarolically altered rocks are found on the eastern flanks of the chain. Desert patine covers post-caldera lavas. Based on crystal composition, the magmas of Sairecabur formed at temperatures of. The process started by partial melting of the mantle involving peridotite and subsequent interaction with the crust and fractional crystallization.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
The isotope ratios are consistent with these found in the crust, specifically of the so-called &quot;Antofalla&quot; domain of Andean crust, the remnant of a terrane of Gondwana. Geological history. The 7 million year-old Chaxas ignimbrite massif has been related to the caldera-forming eruption at Sairecabur. These dacitic ignimbrites spread southwest towards the Salar de Atacama.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
The lava formations are named Post-Caldera Lavas I and Post-Caldera Lavas II; the first is of Pleistocene and the second of Holocene age. A fresh flow that extends northwest from Sairecabur appears to be the most recent flow. The formation of the caldera occurred before the Holocene and preceded the formation of the other cones in the range.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
The edifice this caldera formed during the Pliocene-Quaternary considering the morphology of its deposits. During the ice ages, a valley due west of the main Sairecabur summit was occupied by a long glacier that extended down to an elevation of; the main Sairecabur summit grew inside of the valley occupied by the glacier, which also left lateral and terminal moraines.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
During the ice ages, a valley due west of the main Sairecabur summit was occupied by a long glacier that extended down to an elevation of; the main Sairecabur summit grew inside of the valley occupied by the glacier, which also left lateral and terminal moraines. Sairecabur volcano is the youngest volcano in the chain; Escalante is also young but not as young as Sairecabur.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Sairecabur volcano is the youngest volcano in the chain; Escalante is also young but not as young as Sairecabur. There are no reports of contemporaneous activity nor has fumarolic activity been reported, although fumaroles and hot springs were found at the shores of Laguna Verde which border on Sairecabur.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
There are no reports of contemporaneous activity nor has fumarolic activity been reported, although fumaroles and hot springs were found at the shores of Laguna Verde which border on Sairecabur. Future activity at Sairecabur may disturb activity at Atacama Large Millimeter Array, and will most likely involve the production of lava domes and lava flows with local impacts. Climate and biology.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Climate and biology. The climate at Sairecabur is dry and cloudless, leading to the absence of glaciers and permanent snowcover at Sairecabur although a 1985 map shows a persistent ice/snow cover in the summit area. Overall the Atacama Altiplano has a desert climate with precipitation below, but during the late Pleistocene and early Holocene the climate was wetter.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
The rainshadow effect exercised by the Andes and the stability of the South Pacific High are responsible for this dryness. The dry and cloudless climate together with the low latitude and high altitude gives the region some of the highest insolations on Earth; at Sairecabur it amounts to 98% of the solar constant.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Between 1991 and 1994 the average speed of wind amounted to. Research on plant diversity in the region west of Sairecabur and Licancabur has shown that about 250 plant species occur there, and on the volcano itself extremophilic yeast species have been found. In 1955, penitentes, a form of ice, was reported to be widespread at Saciel. Pre-modern times.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Sairecabur and Curiquinca both have mountain sanctuaries made by the Inca. Licancabur and Juriques farther south were also sites of such sanctuaries. Sairecabur was considered to be a sacred mountain, and andesite found at some archeological sites in the Atacama may come from Sairecabur. Recent times. A sulfur mine is active at Saciel, north of Sairecabur.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Sairecabur was considered to be a sacred mountain, and andesite found at some archeological sites in the Atacama may come from Sairecabur. Recent times. A sulfur mine is active at Saciel, north of Sairecabur. Sulfur mining there, at Cerro Colorado and Putana in the 1950s contributed to the growth of San Pedro de Atacama, where the mined sulfur was transported to.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Recent times. A sulfur mine is active at Saciel, north of Sairecabur. Sulfur mining there, at Cerro Colorado and Putana in the 1950s contributed to the growth of San Pedro de Atacama, where the mined sulfur was transported to. A report in 1955 indicated the presence of about ore containing 55–60% sulfur. A long mining dirt road with a single lane leads from the El Tatio highway to Sairecabur.

Geographic entities mentioned:
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
surface_form: sairecabur
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.716666666667
lon: -67.891666666667
Cerro Colorado and Curiquinca are aligned in a west–east pattern. Other volcanoes in the area such as Lascar-Aguas Calientes, Licancabur-Juriques and La Torta-Tocorpuri also form such alignments which seem to be controlled by north–south tension in the crust. Sairecabur is located on faults which are also apparent at Laguna Verde. Petrology.

Geographic entities mentioned:
surface_form: tocorpuri
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.438888888889
lon: -67.8875
Recent times. A sulfur mine is active at Saciel, north of Sairecabur. Sulfur mining there, at Cerro Colorado and Putana in the 1950s contributed to the growth of San Pedro de Atacama, where the mined sulfur was transported to. A report in 1955 indicated the presence of about ore containing 55–60% sulfur. A long mining dirt road with a single lane leads from the El Tatio highway to Sairecabur.

Geographic entities mentioned:
surface_form: putana
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.557302
lon: -67.852834
Mount Roberts. See also: Roberts Mountains and Roberts Peak

Geographic entities mentioned:
surface_form: Roberts Peak
instance_of: Mountain
coordinates: lat: -78.2333
lon: -85.1667
Òkè-Ìlá Òràngún is located in Osun State, at an elevation of on one of the several mountains adjoining the eastern flanks of the Oke-Ila Ridge, a part of the Yoruba Hills. Òkè-Ìlá Òràngún is about directly west of the confluence of the Rivers Niger and Benue at Lokoja and about northeast of Osogbo, the capital of Osun State. It is about northeast of Lagos with Ibadan at about midway between.

Geographic entities mentioned:
surface_form: Benue
instance_of: Watercourse
countries: Cameroon
Nigeria
coordinates: lat: 7.783333
lon: 6.766667
Remick Ridge Vineyards. Remick Ridge Vineyards is a California-based vineyard and winery owned and operated by the Smothers Brothers. It is a monopole vineyard for Arrowood Vineyards and Winery in the Sonoma Valley. The setting of this viticulture operation is on a ridge of the northern Sonoma Mountains above Sonoma Creek.

Geographic entities mentioned:
surface_form: Sonoma Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.3667
lon: -122.5
Ben Tee. Overview. Ben Tee forms part of the Loch Lochy hills along with the Munros of Sròn a' Choire Ghairbh and Meall na Teanga which lie to the south west. It has a height of 904 metres (2966 feet) and qualifies as a Corbett and a Marilyn.

Geographic entities mentioned:
surface_form: Loch Lochy
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.968611111111
lon: -4.9105555555556
surface_form: Sròn a' Choire Ghairbh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.00784
lon: -4.928747
surface_form: Meall na Teanga
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.989012
lon: -4.930955
surface_form: ben tee
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.032511
lon: -4.899216
It has a height of 904 metres (2966 feet) and qualifies as a Corbett and a Marilyn. It is just 10 metres (33 feet) short of being a Munro and it is one of the most recognisable hills in the area with its symmetrical cone making it conspicuous in views for many miles around. The hill lies to the north of Loch Lochy where Glen Garry intersects with the Great Glen. Name.

Geographic entities mentioned:
surface_form: Great Glen
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
Name. The origins of the name Ben Tee is not entirely clear. The most widely accepted translation is &quot;Fairy Hill&quot; from Gaelic &quot;Beinn an t-Sìthidh&quot;. Ben Tee's conical shape is very similar to that of Schiehallion, also a conical &quot;fairy hill&quot;, which gives extra credibility to that translation.

Geographic entities mentioned:
surface_form: Schiehallion
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.666933
lon: -4.100229
surface_form: schiehallion
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.666933
lon: -4.100229
Local significance. An informal local name for Ben Tee is “Glengarry’s Bowling Green”, a rather sardonic name because there is hardly any grass on the rocky summit. Local legend says that nearby Invergarry Castle on the northern shores of Loch Oich was built from stone from Ben Tee's summit, with workers passing stone hand to hand down the mountain.

Geographic entities mentioned:
surface_form: Loch Oich
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.069478
lon: -4.770802
surface_form: ben tee
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.032511
lon: -4.899216
All drainage from Ben Tee reaches the Great Glen but goes to both the west and east coast of Scotland. Rainfall on the northern part of the hill goes via Glen Garry and the River Garry to reach Loch Oich from where it flows north east through Loch Ness to reach the east coast at the Moray Firth.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
The route continues across moorland which steepens to reach the broad eastern ridge and then the summit. Approaches are possible from the north and the east, one starts at the bridge over Loch Garry (grid reference), while another starts at the Forestry Commission's Alt na Cailliche car park near Invergarry (grid reference). Both these routes are longer than the Kilfinnan approach.

Geographic entities mentioned:
surface_form: Loch Garry
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.083333333333
lon: -4.9166666666667
surface_form: loch garry
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.805765
lon: -4.246576
Ben Tee. Overview. Ben Tee forms part of the Loch Lochy hills along with the Munros of Sròn a' Choire Ghairbh and Meall na Teanga which lie to the south west. It has a height of 904 metres (2966 feet) and qualifies as a Corbett and a Marilyn.

Geographic entities mentioned:
surface_form: ben tee
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.032511
lon: -4.899216
The hill lies to the north of Loch Lochy where Glen Garry intersects with the Great Glen. Name. The origins of the name Ben Tee is not entirely clear. The most widely accepted translation is &quot;Fairy Hill&quot; from Gaelic &quot;Beinn an t-Sìthidh&quot;.

Geographic entities mentioned:
surface_form: ben tee
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.032511
lon: -4.899216
Ascents. The most popular ascent of Ben Tee starts at the Laggan locks on the Caledonian Canal at grid reference where there is a car park. The minor road to Kilfinnan on the north side of Loch Lochy is taken and left about 200 metres before the Kilfinnan Burn is reached to strike north west up the steep slopes of Ben Tee.

Geographic entities mentioned:
surface_form: ben tee
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.032511
lon: -4.899216
After the gold rush the &quot;drift to the north&quot; meant the North Island displaced the South as the most populous. The South Island is shaped by the Southern Alps, which run along the island from north to south. They include New Zealand's highest peak, Mount Cook, at. The high Kaikōura Ranges lie to the northeast.

Geographic entities mentioned:
surface_form: Mount Cook
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.595
lon: 170.14194444444445
Geography. The South Island, with an area of, is the largest landmass of New Zealand; it contains about one-quarter of the New Zealand population and is the world's 12th-largest island. It is divided along its length by the Southern Alps, the highest peak of which is Mount Cook at, making it 9th-highest island, with the high Kaikōura Ranges to the northeast.

Geographic entities mentioned:
surface_form: Mount Cook
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.595
lon: 170.14194444444445
The spelling 'fiord' is used in New Zealand rather than 'fjord', although all the maritime fiords use the word Sound in their name instead. A number of lakes in the Fiordland and Otago regions also fill glacial valleys. Lake Te Anau has three western arms, which are fiords (and are named so). Whakatipu Waitai to the north of Piopiotahi is a fiord with a silted-up mouth.

Geographic entities mentioned:
surface_form: Lake Te Anau
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.2
lon: 167.8
Lake Te Anau has three western arms, which are fiords (and are named so). Whakatipu Waitai to the north of Piopiotahi is a fiord with a silted-up mouth. Lake Wakatipu fills a large glacial valley, as do lakes Hakapoua, Poteriteri, Monowai and Hauroko in the far south of Fiordland. Lake Manapouri has fiords as its west, north and south arms.

Geographic entities mentioned:
surface_form: Lake Wakatipu
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.085
lon: 168.561
surface_form: Poteriteri
instance_of: Lake
countries: New Zealand
coordinates: lat: -46.02
lon: 167.114
surface_form: Monowai
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.866666666667
lon: 167.45
surface_form: Hauroko
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.958
lon: 167.305
Lake Wakatipu fills a large glacial valley, as do lakes Hakapoua, Poteriteri, Monowai and Hauroko in the far south of Fiordland. Lake Manapouri has fiords as its west, north and south arms. The Marlborough Sounds, a series of deep indentations in the coastline at the northern tip of the South Island, are in fact rias, drowned river valleys. Glaciers.

Geographic entities mentioned:
surface_form: Lake Manapouri
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.514
lon: 167.508
When the glaciers retreated, they left basins that are now filled by lakes. The level of most glacial lakes in the upper parts of the Waitaki and Mata-Au rivers are controlled for electricity generation. Hydroelectric reservoirs are common in South Canterbury and Central Otago, the largest of which is Lake Benmore, on the Waitaki River. The South Island has 8 of New Zealand's 10 biggest lakes.

Geographic entities mentioned:
surface_form: Lake Benmore
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.415
lon: 170.22055555556
Hydroelectric reservoirs are common in South Canterbury and Central Otago, the largest of which is Lake Benmore, on the Waitaki River. The South Island has 8 of New Zealand's 10 biggest lakes. They were formed by glaciers and include Lake Wakatipu, Lake Tekapo and Lake Manapouri. The deepest (462 m) is Lake Hauroko, in western Southland. It is the 16th deepest lake in the world.

Geographic entities mentioned:
surface_form: Lake Wakatipu
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.085
lon: 168.561
surface_form: Lake Tekapo
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.9
lon: 170.525
surface_form: Lake Manapouri
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.514
lon: 167.508
The South Island has 8 of New Zealand's 10 biggest lakes. They were formed by glaciers and include Lake Wakatipu, Lake Tekapo and Lake Manapouri. The deepest (462 m) is Lake Hauroko, in western Southland. It is the 16th deepest lake in the world. Millions of years ago, Central Otago had a huge lake – Lake Manuherikia.

Geographic entities mentioned:
surface_form: Lake Hauroko
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.958
lon: 167.305
The remains of this violent origin can be seen in the basalt of the surrounding hills. The last eruptive phase ended some ten million years ago, leaving the prominent peak of Mount Cargill. Timaru was constructed on rolling hills created from the lava flows of the extinct Mount Horrible, which last erupted many thousands of years ago. Te Wāhipounamu World Heritage Site.

Geographic entities mentioned:
surface_form: Mount Cargill
instance_of: Mountain
countries: New Zealand
coordinates: lat: -45.813
lon: 170.555
History. The city was founded at the confluence of the rivers Spree and Havel. The settlement of the area can be traced back to the 6th century when the eastern territories of the Elbe river were populated by several Slavic tribes. The history of Spandau begins in the 7th or 8th century, when the Slav Hevelli settled in the area and later built a fortress there.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
In clear weather conditions, locations such as Blackpool Tower, the Dream in Sutton, St Helens, Jodrell Bank Observatory, Snaefell in the Isle of Man, the Cumbrian mountains, Snowdonia in North Wales, Liverpool, Southport, the Irish Sea, the Pennines and much of the North West of England, can be seen.

Geographic entities mentioned:
surface_form: Snaefell
instance_of: Mountain
countries: Isle of Man
coordinates: lat: 54.263288
lon: -4.461618
35 passengers and crew were killed in the accident. There is a memorial plaque to the accident at the site. In September 1965 a RAF De Havilland Chipmunk flew into the hill in cloud, without serious injury to the crew. The last crash occurred in October 1968 when a Cessna 172 force-landed between Winter Hill and Rivington Pike. 2018 wildfire. In 2018, a large wildfire broke out on the 28 June.

Geographic entities mentioned:
surface_form: Rivington Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.6196
lon: -2.5411
surface_form: winter hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.63
lon: -2.515
In total, the fire burned for 41 days, and caused a major incident to be declared. A man was later arrested for arson on suspicion of causing the wildfire. The fire, along with the Saddleworth Moor fire (which also burned over 7 square miles of land) has been described by local councillor Brenda Warrington as the &quot;worst series of moor fires in living memory&quot;.

Geographic entities mentioned:
surface_form: Saddleworth Moor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.543333333333
lon: -1.9558333333333
surface_form: saddleworth moor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.543333333333
lon: -1.9558333333333
Viewfinder plaque. A metal plaque shows the direction for Two Lads Cairn, Winter Hill TV mast, Smithills Moor, Brown Lowe, Scout Moor Wind Farm, Knowl Hill, Walker Fold Woods, Saddleworth Moor, Peak District, Kinder Scout, Manchester and Salford Quays. The image on the left shows Winter Hill and the TV mast along with Holdens Farm.

Geographic entities mentioned:
surface_form: saddleworth moor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.543333333333
lon: -1.9558333333333
surface_form: winter hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.63
lon: -2.515
Winter Hill (North West England). Winter Hill is a hill on which the three boroughs of Chorley, Blackburn with Darwen and Bolton meet in North West England. It is located on Rivington Moor, Chorley and is high. Part of the West Pennine Moors, it is a popular walking area, and has been the site of mining activity, aeroplane disasters and a murder.

Geographic entities mentioned:
surface_form: winter hill (north west england)
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.63
lon: -2.515
Winter Hill (North West England). Winter Hill is a hill on which the three boroughs of Chorley, Blackburn with Darwen and Bolton meet in North West England. It is located on Rivington Moor, Chorley and is high. Part of the West Pennine Moors, it is a popular walking area, and has been the site of mining activity, aeroplane disasters and a murder.

Geographic entities mentioned:
surface_form: winter hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.63
lon: -2.515
It is located on Rivington Moor, Chorley and is high. Part of the West Pennine Moors, it is a popular walking area, and has been the site of mining activity, aeroplane disasters and a murder. Its prominent position made it the ideal site for the Winter Hill TV Mast, transmitting to a large part of North West England.

Geographic entities mentioned:
surface_form: winter hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.63
lon: -2.515
The hill is a prominent natural landmark on the skyline for the most of Chorley and further afield. Winter Hill's topographic prominence results in it being classified as a Marilyn. The trig point on its summit marks the highest point in Blackburn with Darwen whereas the highest point in Bolton is away on its south east slope at above sea level.

Geographic entities mentioned:
surface_form: winter hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.63
lon: -2.515
There is a Bronze Age round cairn dating from 1600–1400 BC on the hill. In 1883, a local historian recorded the old name for Winter Hill as Edgar Hill, named in connection to Saxon King Edgar
Burial mounds. Two burial mounds dating from the Bronze Age are located near the peak.

Geographic entities mentioned:
surface_form: winter hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.63
lon: -2.515
Both are scheduled monuments. Two Lads. There is a large cairn on the summit of Two Lads on Crooked Edge Hill on the south west side of Winter Hill. In the late 1700s there were apparently two close together. Another cairn was built in the late 20th century by a local man. It is smaller, some 40 metres from the large cairn.

Geographic entities mentioned:
surface_form: winter hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.63
lon: -2.515
The site was originally known as 'Wilder Lads', originally united by a circular mound. The cairns height had been increased by a landowner, noted by local historian Thomas Hampson in 1883, at the time the cairns were thought to be Saxon. Hampson described the original Two Lads as the graves of two children of a Saxon king, Edgar, and recorded that Winter Hill was previously known as Edgar Hill.

Geographic entities mentioned:
surface_form: winter hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.63
lon: -2.515
Air disasters. There have been over two dozen aircraft crashes on and around Winter Hill; the earliest being a single-seat fighter of the Royal Flying Corps and include a two-seater aircraft in the 1920s. During World War II an American Fairchild UC-61 Forwarder (41-54885) of 5th Air Depot Group crashed on 7 August 1942.

Geographic entities mentioned:
surface_form: winter hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.63
lon: -2.515
Other crashes have included several Spitfires, Hurricanes and a Gloster Meteor which crashed in 1953. The worst occurred on 27 February 1958; known as the Winter Hill air disaster, a Silver City Bristol 170 Freighter (G-AICS) travelling from the Isle of Man to Manchester crashed into Winter Hill several hundred yards away from the transmitter. 35 passengers and crew were killed in the accident.

Geographic entities mentioned:
surface_form: winter hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.63
lon: -2.515
surface_form: winter hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.63
lon: -2.515
The hill and surrounding moorland area is open access land with a legally protected right to roam. Claimed UFO sightings. Winter Hill is something of a magnet for UFO sightings
UFOs have been reported on Winter Hill since 1950, when a witness described a &quot;dark flat iron shaped object hovering close to the ground&quot; and an encounter with a being that returned to a craft before disappearing.

Geographic entities mentioned:
surface_form: winter hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.63
lon: -2.515