Sarmila/GeoWiki-Features huggingface dataset:
The Tacoma Rail shortline runs along the west side of the lake, as does Orville Road connecting Eatonville to the south with the town of Kapowsin. The lake contains a number of fish species and is stocked with rainbow trout, rated &quot;excellent&quot; for fishing by Washington Department of Fish and Wildlife, as is the yellow perch.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
The two stations are short spaced to each other as the cities they are licensed to serve are apart. Under Federal Communications Commission (FCC) rules, the minimum distance between Class A and Class B1 stations operating on the same channel is. As such, the station competes for signal strength along the outer edge of its broadcast area, particularly in the San Fernando Valley.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Taxonomy. This species was first described by Edward Meyrick in 1912 using a male specimen collected by George Hudson on the banks of the Routeburn at the head of Lake Wakatipu in February and named &quot;Carposina morbida&quot;. Hudson, in his 1928 publication &quot;The Butterflies and Moths of New Zealand&quot;, discussed this species under that name.

Geographic entities mentioned:
surface_form: Lake Wakatipu
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.085
lon: 168.561
Distribution. &quot;H. morbida&quot; is endemic to New Zealand. Other than the type locality, this species has been observed in the Auckland and Wellington regions in the North Island, and at Mount Hutt, Arthur's Pass, the Homer tunnel area and Waiho Gorge in the South Island. Behaviour. Hudson stated that the adults frequent clumps of &quot;Hoheria lyallii&quot;.

Geographic entities mentioned:
surface_form: Mount Hutt
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.466666666667
lon: 171.53333333333
Of the agricultural land, 39.5% is used for growing crops and 9.1% is pastures, while 2.0% is used for orchards or vine crops. The village of Hermrigen is located on the main road between Bern, Aarberg and Biel. It is on the southern edge of the Oberholz woods, between Lake Biel and the Bernese Seeland. On 31 December 2009 Amtsbezirk Nidau, the municipality's former district, was dissolved.

Geographic entities mentioned:
surface_form: Lake Biel
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.085555555556
lon: 7.1741666666667
Early life. Richards was born in Mendon, Utah Territory. He was the oldest of ten children born to Stephen Longstroth Richards and Emma Louise Stayner. He was raised in Cache Valley. Richards was the grandson of Willard Richards, an early apostle of the church and colleague of Joseph Smith. Richards married Irene Smith Merrill (a maternal granddaughter of George A. Smith) in 1900.

Geographic entities mentioned:
surface_form: Cache Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.816666666667
lon: -111.93416666667
Sixteenmile Creek (Ontario). Sixteenmile Creek is a stream in the municipality of West Elgin, Elgin County in Southwestern Ontario, Canada. It is part of the Great Lakes Basin, and flows from a point just south of Ontario Highway 401 east of exit 129 through the community of Rodney, past the community of New Glasgow, to its mouth at the community of Port Glasgow on Lake Erie.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
An inland sea (also known as an epeiric sea or an epicontinental sea) is a continental body of water which is very large in area and is either completely surrounded by dry land (landlocked), or connected to an ocean by a river, strait or &quot;arm of the sea&quot;. An inland sea will generally be brackish, with higher salinity than a freshwater lake but usually lower salinity than seawater.

Geographic entities mentioned:
surface_form: freshwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.6453
lon: -60.3967
&quot;Baile Amhlaoibh&quot;, meaning &quot;the town of Olaf&quot;, was anglicised as &quot;Balally&quot;. The first recorded building in the area is from a record of 1280 when John de Walhope was granted 7 oak trees from the royal forest at Glencree to build a house. A later castle, built by William Walsh after 1407, was constructed on or near the site of this house.

Geographic entities mentioned:
surface_form: Glencree
instance_of: Valley
countries: Ireland
coordinates: lat: 53.17
lon: -6.23
Under his command, the IDF achieved victory over Egypt, Syria and Jordan in the Six-Day War in 1967. After the Old City of Jerusalem was captured by the IDF, Rabin was among the first to visit the Old City, and delivered a famous speech on Mount Scopus, at the Hebrew University. In the days leading up to the war, it was reported that Rabin suffered a nervous breakdown and was unable to function.

Geographic entities mentioned:
surface_form: Mount Scopus
instance_of: Mountain
countries: Israel
coordinates: lat: 31.7925
lon: 35.244166666667
Hundreds of thousands of Israelis gathered at the square where Rabin was assassinated to mourn his death. Young people, in particular, turned out in large numbers, lighting memorial candles and singing peace songs. On 6 November 1995, he was buried on Mount Herzl. Rabin's funeral was attended by many world leaders, among them U.S.

Geographic entities mentioned:
surface_form: Mount Herzl
instance_of: Mountain
countries: Israel
coordinates: lat: 31.774117
lon: 35.180567
Music video. The music video for aired for the public on MTV &quot;M-SIZE&quot; on October 23, 2006. The PV was filmed around the Mount Fuji area, and was directed by AT. The video starts off with Hitomi walking into a recording studio. She then proceeds to place headphones on, and begins singing into a microphone with a stand holding the lyrics of the song in front of her.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
Ananta (Arequipa). Ananta is a mountain in the Arequipa Region in the Andes of Peru, about high. It is situated in the Caylloma Province, on the border of the districts Achoma and Yanque. Ananta lies east of the dormant volcano Ampato and south-west of the mountain Warank'anthi.

Geographic entities mentioned:
surface_form: Ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
surface_form: ananta
instance_of: Mountain
countries: Peru
coordinates: lat: -13.81388889
lon: -70.62055556
surface_form: ananta
instance_of: Mountain
countries: Peru
coordinates: lat: -15.8128
lon: -71.6825
Ananta (Arequipa). Ananta is a mountain in the Arequipa Region in the Andes of Peru, about high. It is situated in the Caylloma Province, on the border of the districts Achoma and Yanque. Ananta lies east of the dormant volcano Ampato and south-west of the mountain Warank'anthi.

Geographic entities mentioned:
surface_form: ananta
instance_of: Mountain
countries: Peru
coordinates: lat: -13.81388889
lon: -70.62055556
surface_form: ananta (arequipa)
instance_of: Mountain
countries: Peru
coordinates: lat: -15.8128
lon: -71.6825
Ananta (Arequipa). Ananta is a mountain in the Arequipa Region in the Andes of Peru, about high. It is situated in the Caylloma Province, on the border of the districts Achoma and Yanque. Ananta lies east of the dormant volcano Ampato and south-west of the mountain Warank'anthi.

Geographic entities mentioned:
surface_form: ananta
instance_of: Mountain
countries: Peru
coordinates: lat: -13.81388889
lon: -70.62055556
surface_form: ananta
instance_of: Mountain
countries: Peru
coordinates: lat: -15.8128
lon: -71.6825
Rajsamand. Rajsamand is a city, located in Rajsamand Mewar district of Rajasthan, India. The city is named for Rajsamand Lake, an artificial lake created in the 17th century by Rana Raj Singh Rajsamand Udaipur of Mewar. It is the administrative headquarters of Rajsamand District. Geography. Rajsamand is located at. It has an average elevation of 547 metres (1794 ft). Demographics.

Geographic entities mentioned:
surface_form: Rajsamand Lake
instance_of: Lake
countries: India
coordinates: lat: 25.07
lon: 73.88
Another theory points to the similarity of the valley of the Aconcagua with that of the Casma Valley in Peru, where there was a town and valley named &quot;Chili&quot;.

Geographic entities mentioned:
surface_form: Casma Valley
instance_of: Valley
countries: Peru
The desert is fragmented by streams that originate in the area known as the pampas Tamarugal. The Andes, split in two and whose eastern arm runs through Bolivia, has a high altitude and volcanic activity, which has allowed the formation of the Andean altiplano and salt structures as the Salar de Atacama, due to the gradual accumulation of sediments over time.

Geographic entities mentioned:
surface_form: Salar de Atacama
instance_of: Lake
Body of water
countries: Chile
coordinates: lat: -23.416666666666668
lon: -68.26666666666667
Because of the Atacama desert, in the Norte Grande there are only short endorheic character streams, except for the Loa River, the longest in the country 440 km. In the high valleys, wetland areas generate Chungará Lake, located at 4500 meters above sea level. It and the Lauca River are shared with Bolivia, as well as the Lluta River.

Geographic entities mentioned:
surface_form: Chungará Lake
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
In Putre, also in the north, there is the Chungará Lake, as well as the Parinacota and the Pomerape volcanoes, with altitudes of 6,348 m and 6,282 m, respectively. Throughout the central Andes there are many ski resorts of international repute, including Portillo, Valle Nevado and Termas de Chillán.

Geographic entities mentioned:
surface_form: Chungará Lake
instance_of: Lake
countries: Chile
coordinates: lat: -18.2425
lon: -69.1525
surface_form: Pomerape
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -18.126275
lon: -69.126719444444
Finally, Easter Island in the Pacific Ocean is one of the main Chilean tourist destinations. For locals, tourism is concentrated mostly in the summer (December to March), and mainly in the coastal beach towns. Arica, Iquique, Antofagasta, La Serena and Coquimbo are the main summer centers in the north, and Pucón on the shores of Lake Villarrica is the main center in the south.

Geographic entities mentioned:
surface_form: Lake Villarrica
instance_of: Lake
countries: Chile
coordinates: lat: -39.25
lon: -72.083333333333
From around 1833 his father was manager of the Edinburgh Gas Lighting Company. The family lived at 6 Brunton Place close to Calton Hill. On the death of his father (around 1840) he took on his roles of running the Edinburgh Gas Lighting Company
In the 1860s he introduced a new style of gas lamp, specific to Edinburgh, and associated with iconic areas such as Charlotte Square.

Geographic entities mentioned:
surface_form: Calton Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
The Tooth is the descriptive name for a fin-like, andesite pillar located in King County of Washington state. It is part of the Cascade Range and is within the Alpine Lakes Wilderness. The Tooth is located northwest of Snoqualmie Pass and the Alpental ski area on land managed by Mount Baker-Snoqualmie National Forest. The nearest higher peak is Bryant Peak, to the northwest.

Geographic entities mentioned:
surface_form: Bryant Peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.451358
lon: -121.46092
The nearest higher peak is Bryant Peak, to the northwest. Originally called &quot;Denny Horn&quot; and &quot;Denny Tooth&quot;, The Tooth became the officially recognized name in 1918, with &quot;Denny&quot; referring to its position on the high ridge between Denny Mountain and Chair Peak. The Tooth is a popular rock-climbing destination, even in winter.

Geographic entities mentioned:
surface_form: Denny Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.4389642
lon: -121.4439673
surface_form: the tooth
instance_of: Mountain
countries: United States
coordinates: lat: 47.44595
lon: -121.454655
surface_form: the tooth
instance_of: Mountain
countries: United States
coordinates: lat: 47.44595
lon: -121.454655
surface_form: denny mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.4389642
lon: -121.4439673
The Tooth (Washington). The Tooth is the descriptive name for a fin-like, andesite pillar located in King County of Washington state. It is part of the Cascade Range and is within the Alpine Lakes Wilderness. The Tooth is located northwest of Snoqualmie Pass and the Alpental ski area on land managed by Mount Baker-Snoqualmie National Forest.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: the tooth (washington)
instance_of: Mountain
countries: United States
coordinates: lat: 47.44595
lon: -121.454655
The Tooth (Washington). The Tooth is the descriptive name for a fin-like, andesite pillar located in King County of Washington state. It is part of the Cascade Range and is within the Alpine Lakes Wilderness. The Tooth is located northwest of Snoqualmie Pass and the Alpental ski area on land managed by Mount Baker-Snoqualmie National Forest.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: the tooth
instance_of: Mountain
countries: United States
coordinates: lat: 47.44595
lon: -121.454655
The Tooth is the descriptive name for a fin-like, andesite pillar located in King County of Washington state. It is part of the Cascade Range and is within the Alpine Lakes Wilderness. The Tooth is located northwest of Snoqualmie Pass and the Alpental ski area on land managed by Mount Baker-Snoqualmie National Forest. The nearest higher peak is Bryant Peak, to the northwest.

Geographic entities mentioned:
surface_form: the tooth
instance_of: Mountain
countries: United States
coordinates: lat: 47.44595
lon: -121.454655
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
The next recorded European sighting of the Cape was by Vasco da Gama in 1497 while he was searching for a route that would lead directly from Europe to Asia. Table Mountain was given its name in 1503 by António de Saldanha, a Portuguese admiral and explorer. He called it &quot;Taboa do Cabo&quot; (&quot;table of the cape&quot;).

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Water from the Fresh River, which descended from Table Mountain, was channelled into canals to provide irrigation. The settlers bartered with the native Khoisan for their sheep and cattle. Forests in Hout Bay and the southern and eastern flanks of Table Mountain provided timber for ships and houses. At this point, the VOC had a monopoly on trade and prohibited any private trade.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Elliot Lake. Elliot Lake is a city in Algoma District, Ontario, Canada. It is north of Lake Huron, midway between the cities of Sudbury and Sault Ste. Marie in the Northern Ontario region.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Haemyeongsan. Haemyeongsan () is a mountain in Incheon, South Korea. It is on the island of Seongmodo in Ganghwa County. The mountain has an elevation of.

Geographic entities mentioned:
surface_form: haemyeongsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.68333333
lon: 126.35
Bunderspitz. The Bunderspitz is a mountain of the Bernese Alps, located between Adelboden and Kandersteg in the canton of Bern. The summit can be reached by a trail from both sides.

Geographic entities mentioned:
surface_form: bunderspitz
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.492444444444
lon: 7.6203333333333
Chuqisa. Chuqisa (Aymara, also spelled &quot;Choquesa&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the La Paz Department, Loayza Province, Luribay Municipality. Chuqisa lies southwest of a village of that name and west of Janq'u Willk'i.

Geographic entities mentioned:
surface_form: janq'u willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.13944444
lon: -68.39611111
surface_form: janq'u willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.7722
lon: -67.5314
surface_form: willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.39861111
lon: -69.02222222
surface_form: janq'u willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.01111111
lon: -67.57416667
Chuqisa. Chuqisa (Aymara, also spelled &quot;Choquesa&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the La Paz Department, Loayza Province, Luribay Municipality. Chuqisa lies southwest of a village of that name and west of Janq'u Willk'i.

Geographic entities mentioned:
surface_form: chuqisa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.01277778
lon: -67.59222222
The Landscape Area is situated in the Little Carpathians, part of the Carpathian Mountains, in West Slovakia. The southwesternmost area is Devínska Kobyla in Bratislava, and the northeasternmost area is the Čachtice Carpathians at the town of Nové Mesto nad Váhom and the village of Čachtice in the Trenčín Region. Both areas are separated from the main mountain strip.

Geographic entities mentioned:
surface_form: Devínska Kobyla
instance_of: Mountain
countries: Slovakia
coordinates: lat: 48.190555555556
lon: 16.995833333333
Geography. The Little Carpathians are the borderline mountains of the Inner Western Carpathians. The three highest points are Záruby at, Vysoká at and Vápenná at. Biology and ecology. Deciduous trees are dominant, with the beech, linden, European ash, and sycamore maple being most widespread.

Geographic entities mentioned:
surface_form: Záruby
instance_of: Mountain
countries: Slovakia
coordinates: lat: 48.523569444444
lon: 17.391666666667
Location. Flint Ridge is immediately north of Commonwealth Glacier. Mount Coleman is to the east, Mount Falconer to the south and Mount McLennan to the west. To the northwest Loftus Glacier flows northeast into the Wilson Piedmont Glacier. Sagittate Hill. A hill with much exposed rock rising to high at the west side of Flint Ridge.

Geographic entities mentioned:
surface_form: Mount Falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
surface_form: Mount McLennan
instance_of: Mountain
coordinates: lat: -67.2
lon: 51.0833
Dominion Hill. A rounded rock summit rising to about high in the east part of Noxon Cliff. Dominion Hill bounds the north edge of Commonwealth Glacier where it descends southeastward into Taylor Valley. Named by New Zealand Geographic Board (NZGB) (1998) after a form of government to complement the Commonwealth (of Australia) Glacier.

Geographic entities mentioned:
surface_form: Taylor Valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
Pyramid Peak (South Georgia). Pyramid Peak () is a peak, high, surmounting Cape Buller at the west side of the entrance to the Bay of Isles, South Georgia Island. It was mapped in 1902 by the Swedish Antarctic Expedition and named descriptively &quot;Die Pyramide.&quot;

Geographic entities mentioned:
surface_form: pyramid peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -54
lon: -37.38333333
The single-aisled church was built in the thirteenth century and has a five-sided closed choir and a roof turret. Lettelbert has a small marina on the Leekstermeer and a natural camping site. Near the village are the Lettelberterpetten, a peat area that was extracted between 1900 and 1920 and became overgrown with alder woods and has been a nature reserve of Het Groninger Landschap since 1961.

Geographic entities mentioned:
surface_form: Leekstermeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 53.18
lon: 6.43472
The first boathouse was constructed along Redwood Creek and remained active for the next 10 years there. In 1913, another boathouse was built on campus on the edge of Lake Lagunita for Freshmen, spring practice, and campus recreation.

Geographic entities mentioned:
surface_form: Lake Lagunita
instance_of: Lake
countries: United States
coordinates: lat: 37.423272222222
lon: -122.17607777778
Little Liqenat Lake. Little Lake Liqenat or Lake Drelaj (or &quot;Leqinati i vogël&quot;;) is a small lake found on Mount Leqinat that reaches an elevation of in the Accursed Mountains range in western Kosovo, near the border with Montenegro. The length of this lake is and the maximum width is.

Geographic entities mentioned:
surface_form: Leqinat
instance_of: Mountain
countries: Montenegro
Kosovo
coordinates: lat: 42.66861111111111
lon: 20.09111111111111
surface_form: lake liqenat
instance_of: Lake
countries: Kosovo
coordinates: lat: 42.66861111
lon: 20.09083333
surface_form: leqinat
instance_of: Lake
countries: Kosovo
coordinates: lat: 42.66861111
lon: 20.09083333
surface_form: liqenat
instance_of: Lake
countries: Kosovo
coordinates: lat: 42.66861111
lon: 20.09083333
The length of this lake is and the maximum width is. Little Lake Liqenat is at a lower elevation than the much larger Lake Liqenat found in the west of it and only a hill of pine trees separates the two.

Geographic entities mentioned:
surface_form: lake liqenat
instance_of: Lake
countries: Kosovo
coordinates: lat: 42.66861111
lon: 20.09083333
surface_form: liqenat
instance_of: Lake
countries: Kosovo
coordinates: lat: 42.66861111
lon: 20.09083333
surface_form: liqenat
instance_of: Lake
countries: Kosovo
coordinates: lat: 42.66861111
lon: 20.09083333
Little Liqenat Lake. Little Lake Liqenat or Lake Drelaj (or &quot;Leqinati i vogël&quot;;) is a small lake found on Mount Leqinat that reaches an elevation of in the Accursed Mountains range in western Kosovo, near the border with Montenegro. The length of this lake is and the maximum width is.

Geographic entities mentioned:
surface_form: liqenat
instance_of: Lake
countries: Kosovo
coordinates: lat: 42.66861111
lon: 20.09083333
surface_form: little liqenat lake
instance_of: Lake
countries: Kosovo
coordinates: lat: 42.66722222222222
lon: 20.099166666666665
Many vents cluster in an area known as the Altiplano-Puna volcanic complex which occupies a surface of about approximately north of Galán, and which includes the large calderas of La Pacana, Cerro Guacha, Pastos Grandes and Cerro Panizos as well as more recent geothermal systems.

Geographic entities mentioned:
surface_form: La Pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: Cerro Guacha
instance_of: Mountain
countries: Bolivia
coordinates: lat: -22.75
lon: -67.46666667
surface_form: Cerro Panizos
instance_of: Mountain
countries: Bolivia
coordinates: lat: -22.4375
lon: -66.7825
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
Volcanism in this &quot;back&quot; region may not be directly related to subduction processes despite the region itself being close to a subducting margin. The Galán caldera lies on the eastern margin of the Andes, where the Sierras Pampeanas begin. The region is characterized by the Puna, a high plateau similar to Tibet in Asia. Local.

Geographic entities mentioned:
surface_form: Puna
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
North of 21° degrees southern latitude ignimbritic volcanism started earlier, generating the Altos de Pica and Oxaya formations. Mafic volcanism occurred south and west of Galán both before its large eruption and afterwards, in the valley of Antofagasta de la Sierra and may have continued to less than ten thousand years ago.

Geographic entities mentioned:
surface_form: Antofagasta de la Sierra
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.968055555556
lon: -67.535833333333
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
Galán. Cerro Galán is a caldera in the Catamarca Province of Argentina. It is one of the largest exposed calderas in the world and forms part of the Central Volcanic Zone of the Andes, one of the three volcanic belts found in South America. One of several major caldera systems in the Central Volcanic Zone, the mountain is grouped into the Altiplano–Puna volcanic complex.

Geographic entities mentioned:
surface_form: cerro galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
Another Leon Muerto river drains the southern side of the caldera into Laguna Pabellon. Rivers in the caldera and neighbourhood display river terraces which may reflect pre-caldera formation uplift of the terrain and uplift associated with the resurgent dome. These drainages eventually converge in the Rio de Los Patos and end into the Salar del Hombre Muerto north of Galán.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
Galán. Cerro Galán is a caldera in the Catamarca Province of Argentina. It is one of the largest exposed calderas in the world and forms part of the Central Volcanic Zone of the Andes, one of the three volcanic belts found in South America. One of several major caldera systems in the Central Volcanic Zone, the mountain is grouped into the Altiplano–Puna volcanic complex.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
Volcanic activity at Galán is the indirect consequence of the subduction of the Nazca Plate beneath the South America Plate, and involves the infiltration of melts into the crust and the formation of secondary magmas which after storage in the crust give rise to the dacitic to rhyodacitic rocks erupted by the volcano.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
Galán was active between 5.6 and 4.51 million years ago, when it generated a number of ignimbrites known as the Toconquis group which crop out mainly west of the caldera. The largest eruption of Galán was 2.08 ± 0.02 million years ago and was the source of the Galán ignimbrite, which covered the surroundings of the caldera with volcanic material.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
Galán was active between 5.6 and 4.51 million years ago, when it generated a number of ignimbrites known as the Toconquis group which crop out mainly west of the caldera. The largest eruption of Galán was 2.08 ± 0.02 million years ago and was the source of the Galán ignimbrite, which covered the surroundings of the caldera with volcanic material.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
Geography and geomorphology. The Galán caldera lies in the northwestern Catamarca Province of Argentina and was discovered in 1975 in a remote region of the Andes, using satellite images. The town of Antofagasta de la Sierra lies west-southwest of the Galán caldera, Tacuil is almost due northeast from the caldera and El Penon southwest of the volcano. The caldera is difficult to access.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
The caldera is difficult to access. An Inka &quot;tambo&quot; was situated at Laguna Diamante, and an important prehistoric travel route passed through the caldera. Sacrificial offers were given on the summit of Galán. Galán is part of the Central Volcanic Zone of the Andes, which lies on the western margin of South America, where the Nazca Plate subducts beneath the South America Plate.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
There are about 50 volcanoes with recent activity in the Central Volcanic Zone, and additional volcanoes exist in the Northern Volcanic Zone and the Southern Volcanic Zone, two other volcanic belts north and south. The volcanic arc runs along the borders between Bolivia and Argentina with Chile, and behind the volcanic arc lies a chain of silicic volcanoes, of which Galán is a southern member.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
The Galán caldera lies on the eastern margin of the Andes, where the Sierras Pampeanas begin. The region is characterized by the Puna, a high plateau similar to Tibet in Asia. Local. Galán is a caldera with topographic dimensions of, of which about are part of the caldera proper. Such dimensions make Galán one of the biggest calderas on Earth; it has been described as a supervolcano.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
The caldera contains a resurgent dome, whose highest point in the frost-shattered Galán massif reaches an elevation of about -. Seismic tomography has identified a slow-speed anomaly beneath Galán, which has a volume of about and is considered to be a magma reservoir of the volcano.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
Summits along the caldera margin include Cerro Aguas Calientes (a lava dome) to the north, Cerro Leon Muerto to the southeast, Cerro Pabellon to the southwest and Cerro Toconquis to the northwest. On the western rim, elevations of are reached. Younger volcanoes have developed on the western and northern rim of the Galán caldera. Hydrology and hydrothermal system.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
Basements outcrops occur in the northeastern margin of the caldera. About 14.5 million years ago volcanic activity started in the region, first west of Galán but by 7 million years ago it shifted to the future caldera, forming the Cerro Colorado, Pabellon and Cerro Toconquis composite volcanoes on its future western rim. The more westerly centres are today represented by eroded volcanoes.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
The magma erupted by the Galán system was likewise channelled along such fault systems, and neighbouring volcanoes were similarly influenced by them; the fault systems at Galán proper are known as the Diablillos-Galán faults.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
Another major lineament in the area is the Archibarca lineament, which is formed by a strike-slip fault that extends from the northwest to the southeast in the region and which intersects the Diablillos-Galán faults at the location of the caldera. Composition.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
Minerals contained in the eruption products include allanite, apatite, biotite, hornblende, ilmenite, magnetite, orthopyroxene, plagioclase, quartz, sanidine and zircon. Hydrothermal alteration has left calcite in some rocks. Trace element patterns are distinct in the Galán ignimbrite in comparison to the Toconquis Group rocks.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
Further metasomatism in the crust and fractional crystallization processes completed the magma genesis process. Probably under the influence of larger scale tectonics, magma that accumulated into a mid-crustal mush zone is eventually transferred into shallow magma chambers at depths of; recharge events where deep magma entered the shallow magma bodies may have triggered eruptions at Galán.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
Based on the presence of two separate populations of pumice in the Galán ignimbrite it has been inferred that there were two types of magma in the magmatic system during the Galán eruption, a larger volume of so-called &quot;white&quot; magma and a &quot;grey&quot; magma which was injected into the &quot;white&quot; magma pool and eventually rose above the latter.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
Emission of lava flows occurred during the Toconquis phase as well, in general there was vigorous volcanic activity between the eruptions that formed the main ignimbrites. The Cueva Negra ignimbrite was emplaced after the Toconquis Group, and small lava domes and pyroclastic flows continued to be erupted until the Galán ignimbrite proper.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
2.08 ± 0.02 million years ago the rhyodacitic Galán ignimbrite proper was emplaced. Aside from a facies that remained inside the caldera and is minimally thick, ignimbrites extend outside of the caldera to distances of but with an average runout distance of and have thicknesses of; closer to the caldera it has been largely eroded away and there are more complete exposures farther away from Galán.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
A contrary view is that the Galán ignimbrite was largely eroded only on its northern side by wind action, forming yardangs. The resurgent dome consists of Galán ignimbrite material, along with basement rocks. The &quot;Toba Dacitica&quot; outcrop away from the volcano was once considered part of the Galán eruption but later compositional differences were found.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
A contrary view is that the Galán ignimbrite was largely eroded only on its northern side by wind action, forming yardangs. The resurgent dome consists of Galán ignimbrite material, along with basement rocks. The &quot;Toba Dacitica&quot; outcrop away from the volcano was once considered part of the Galán eruption but later compositional differences were found.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
Between the intracaldera ignimbrite, the parts of the ignimbrite that extend away from the caldera and outcrops at large distance, the volume is about, down from earlier estimated of volumes exceeding but the Galán eruption is still one of the biggest known volcanic eruptions and the volcano has produced almost half of the volume of ignimbrites in the southern Puna.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
The Galán ignimbrite is the largest ignimbrite erupted by this centre; there is a tendency of the volume of individual ignimbrites to increase as the volcanoes grow younger, not only at Galán but also at other Puna ignimbrite centres, and this may be a consequence of progressive changes in the crust.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
Such giant eruptions have not been observed during historical time and are considered to be among the most dangerous volcanic phenomena known. Kay &quot;et al.&quot; proposed that the Galán ignimbrite consisted of three separate units, an intracaldera one emplaced 2.13 million years ago and two extracaldera ones 2.09 and 2.06 million years ago. Post-Galán volcanism.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
This uplift encompasses both Galán ignimbrite rocks but also parts of the basement, the latter especially in the southern part of the dome. Post-caldera volcanism occurred on the northern margin of the caldera 2.01 ± 0.28 million years ago, and several small ignimbrites were emplaced after the main Galán eruption until less than 2 million years ago.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
Post-caldera volcanism occurred on the northern margin of the caldera 2.01 ± 0.28 million years ago, and several small ignimbrites were emplaced after the main Galán eruption until less than 2 million years ago. These ignimbrites have similar compositions to the Galán ignimbrite and were formed from magma left over by the main Galán eruption.

Geographic entities mentioned:
surface_form: galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
The town of Antofagasta de la Sierra lies west-southwest of the Galán caldera, Tacuil is almost due northeast from the caldera and El Penon southwest of the volcano. The caldera is difficult to access. An Inka &quot;tambo&quot; was situated at Laguna Diamante, and an important prehistoric travel route passed through the caldera. Sacrificial offers were given on the summit of Galán.

Geographic entities mentioned:
surface_form: diamante
instance_of: Watercourse
countries: Argentina
coordinates: lat: -34.511666666667
lon: -66.757777777778
On the western rim, elevations of are reached. Younger volcanoes have developed on the western and northern rim of the Galán caldera. Hydrology and hydrothermal system. The caldera contains a lake in its southwestern corner, which is known as Laguna Diamante and may formerly have occupied much of the caldera.

Geographic entities mentioned:
surface_form: diamante
instance_of: Watercourse
countries: Argentina
coordinates: lat: -34.511666666667
lon: -66.757777777778
surface_form: diamante
instance_of: Watercourse
countries: Argentina
coordinates: lat: -34.511666666667
lon: -66.757777777778
Tube-shaped microbialites have also been reported. A smaller lake known as Laguna Pabellon lies just south of Laguna Diamante. North of the resurgent dome, the Rio Aguas Calientes drains the caldera northward, while east of it the Rio Leon Muerto runs eastward out of the caldera. Another Leon Muerto river drains the southern side of the caldera into Laguna Pabellon.

Geographic entities mentioned:
surface_form: diamante
instance_of: Watercourse
countries: Argentina
coordinates: lat: -34.511666666667
lon: -66.757777777778
The first one is known as the Aguas Calientes hydrothermal spring and features deposits of tufa and boiling water. Another geothermal system is known as La Colcha and includes fumaroles as well as boiling water; it drains into Laguna Diamante. Finally, on the northeastern side of the caldera is Piscinas Burbujeantes, with mud volcanoes and small fumaroles.

Geographic entities mentioned:
surface_form: diamante
instance_of: Watercourse
countries: Argentina
coordinates: lat: -34.511666666667
lon: -66.757777777778
They continue to travel and name places after events that occurred there. Īhenga claims the land around Lake Rotorua by trickery. Ngātoro climbs Mount Tongariro, but struggles to reach the top through the snow, so he prays to the gods of Hawaiki to send fire to him and they turn the mountain into a volcano.

Geographic entities mentioned:
surface_form: Mount Tongariro
instance_of: Mountain
countries: New Zealand
coordinates: lat: -39.12972222222222
lon: 175.63583333333332
Railroads were the next major form of commercial transportation to come to Cincinnati. In 1836, the Little Miami Railroad was chartered. Construction began soon after, to connect Cincinnati with the Mad River and Lake Erie Railroad, and provide access to the ports of the Sandusky Bay on Lake Erie. Residents of Cincinnati played a major role in abolitionism.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
He was a member of the Mont Pelerin Society and the Sovereign Military Order of Malta. Irving Kristol called him &quot;the godfather of modern philanthropy&quot;. Personal life. He retired on Big Cedar Lake in West Bend, Wisconsin. He was married and had three children. He died of liver disease in a hospice in Germantown, Wisconsin, on February 24, 2006.

Geographic entities mentioned:
surface_form: Big Cedar Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.38
lon: -88.26
In addition, a black spot can almost always be found on the middle of the outer edges of the forewings. Distribution and way of life. The distribution area of &quot;Haaniella scabra&quot; is limited to the high mountain regions around Mount Kinabalu in the center of the Malaysian state of Sabah, in the northern part of Borneo. There the animals can be found at altitudes between.

Geographic entities mentioned:
surface_form: Mount Kinabalu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 6.075
lon: 116.5586111111111
Jerusalem's defenses. Jerusalem's strategic location, flanked by the Kidron Valley to the east and the Hinnom Valley to the south, provided natural barriers that made direct assaults difficult. These natural defenses were reinforced by a series of fortification walls, constructed and expanded over the city's long history.

Geographic entities mentioned:
surface_form: Kidron Valley
instance_of: Valley
countries: State of Palestine
coordinates: lat: 31.776972222222224
lon: 35.23897222222222
surface_form: Hinnom Valley
instance_of: Valley
countries: Israel
coordinates: lat: 31.76916667
lon: 35.22805556
In response, the Roman governor of Syria, Gaius Cestius Gallus, advanced on Jerusalem with an army of approximately 30,000 soldiers. He reached Mount Scopus and burned the northern suburb of Bezetha, but then unexpectedly retreated and was met with a devastating ambush by Jewish forces at Bethoron, resulting in the loss of nearly an entire legion.

Geographic entities mentioned:
surface_form: Mount Scopus
instance_of: Mountain
countries: Israel
coordinates: lat: 31.7925
lon: 35.244166666667
Legio V Macedonica, led by Sextus Vettulenus Cerialis, marched southward toward Jerusalem via Emmaus, while A. Larcius Lepidus Sulpicianus approached from the west through Jericho with Legio X Fretensis. After resting at Gophna, Titus's force camped in the &quot;Valley of Thorns&quot; near Gibeah, three miles from Jerusalem.

Geographic entities mentioned:
surface_form: Gibeah
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 31.823372222222
lon: 35.23115
Soon after, Titus advanced to Mount Scopus, northeast of Jerusalem, where he established camps for Legions XII, XV and V. Legion X set up camp on the Mount of Olives, but as they were constructing their encampment—some soldiers unarmed—they were attacked by a joint force from the rival factions. The Jews charged across the Kidron Valley, catching the Romans completely by surprise.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
Legion X set up camp on the Mount of Olives, but as they were constructing their encampment—some soldiers unarmed—they were attacked by a joint force from the rival factions. The Jews charged across the Kidron Valley, catching the Romans completely by surprise. Only Titus' personal intervention saved the situation, and the Romans managed to repel the attackers.

Geographic entities mentioned:
surface_form: Kidron Valley
instance_of: Valley
countries: State of Palestine
coordinates: lat: 31.776972222222224
lon: 35.23897222222222
John and Simon reconciled, but their factions continued to maintain separate leadership structures. The rebel leaders upheld the previous division of the city into distinct zones of control: John was in charge of defending the Temple Mount, the Ophel, and the Kidron Valley, while Simon's forces defended the city's residential areas. Battle for Jerusalem's walls.

Geographic entities mentioned:
surface_form: Ophel
instance_of: Mountain
countries: Israel
coordinates: lat: 31.775333
lon: 35.236222
On 16 December 1944, a second intelligence network, comprising five Malay SOE agents and two British liaison officers, Major Peter G. Dobree and Captain Clifford, was parachuted into Padang Cermin, near Temenggor Lake Dam in Hulu Perak under the codename Operation Hebrides.

Geographic entities mentioned:
surface_form: Temenggor Lake
instance_of: Lake
countries: Malaysia
coordinates: lat: 5.31
lon: 101.2
The state is divided by three mountain chains into the three plains of Kinta, Larut and Perak, running parallel to the coast. The Titiwangsa Range passes along the eastern borders of Perak, with its highest point, the Mount Korbu, is located in the district of Kinta near the border with the state of Kelantan. Other mountain ranges in Perak are the Bintang Mountains and the Keledang Range.

Geographic entities mentioned:
surface_form: Mount Korbu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 4.6833333333333
lon: 101.3