Sarmila/GeoWiki-Features huggingface dataset:
Mount Tuzo. Mount Tuzo is a mountain located within the Valley of the Ten Peaks in the Canadian Rockies, along the Continental Divide, which forms the provincial boundary between British Columbia and Alberta in Western Canada. It also lies on the boundary shared by Banff National Park and Kootenay National Park. The mountain was named in 1907 after its first ascendant, Henrietta L. Tuzo.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Tuzo. Tuzo was a charter member of the Alpine Club of Canada. On his 1894 map, Samuel Allen had named the peak &quot;Shagowa&quot;, which is the Nakoda word for seven as the mountain is seventh in order from south to north of the ten peaks. __NOTOC__
Geology. Like other mountains in Banff Park, Mount Tuzo is composed of sedimentary rock laid down from the Precambrian to Jurassic periods.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Tuzo. Mount Tuzo is a mountain located within the Valley of the Ten Peaks in the Canadian Rockies, along the Continental Divide, which forms the provincial boundary between British Columbia and Alberta in Western Canada. It also lies on the boundary shared by Banff National Park and Kootenay National Park. The mountain was named in 1907 after its first ascendant, Henrietta L. Tuzo.

Geographic entities mentioned:
surface_form: mount tuzo
instance_of: Mountain
countries: Canada
coordinates: lat: 51.301666666667
lon: -116.22833333333
__NOTOC__
Geology. Like other mountains in Banff Park, Mount Tuzo is composed of sedimentary rock laid down from the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: mount tuzo
instance_of: Mountain
countries: Canada
coordinates: lat: 51.301666666667
lon: -116.22833333333
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Mount Tuzo is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.

Geographic entities mentioned:
surface_form: mount tuzo
instance_of: Mountain
countries: Canada
coordinates: lat: 51.301666666667
lon: -116.22833333333
Yujomsa. Yujŏm-sa was a Korean Buddhist temple located on Mount Kumgang, North Korea. Founded under the kingdom of Silla, it underwent many successive restorations before being destroyed by American forces during the Korean War. History. Yujom Temple was founded in the 6th century under the fervently Buddhist kingdom of Silla.

Geographic entities mentioned:
surface_form: Mount Kumgang
instance_of: Mountain
countries: North Korea
coordinates: lat: 38.656763888889
lon: 128.10490277778
The species is closely related to &quot;C. kumarasinghei &quot; and &quot;C. latha&quot; morphological aspects. Ecology. The species was discovered from a tropical dry-mixed evergreen forest in Dimbulagala, Polonnaruwa. Description. Snout-to-vent length is 28.2 mm in adult male and 29.4 mm in adult female. Granular scales are subconical. Chin, gular, pectoral, and abdominal scales are smooth.

Geographic entities mentioned:
surface_form: Dimbulagala
instance_of: Mountain
countries: Sri Lanka
coordinates: lat: 7.86
lon: 81.14361111111111
Česen enjoyed a period of fame and sponsorship from his enchainment, and went on to claim a number of increasingly bolder, and in some cases, groundbreaking, solo ascents, including: &quot;No Siesta&quot; on the Grandes Jorasses, &quot;Pilier Rouge du Brouillard Direttissima&quot; on Mont Blanc, &quot;Modern Times&quot; on the south face of the Marmolada, the north face of Jannu (or Kumbhakarna), and the enormous south face of Lhotse.

Geographic entities mentioned:
surface_form: Grandes Jorasses
instance_of: Mountain
countries: Italy
France
coordinates: lat: 45.866666666667
lon: 6.9833333333333
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
surface_form: Lhotse
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.961666666667
lon: 86.933333333333
He remains a controversial figure in climbing. One of the main climbing routes on K2 is named the Česen Route, after him, when he soloed it in 1986; there is evidence that he probably summitted K2, and his earlier 19-hour solo ascent of Broad Peak (made in preparation for K2) is not disputed. His son is the mountaineer, Aleš Česen.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
surface_form: Broad Peak
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.810555555556
lon: 76.568055555556
Vilapata. Vilapata (possibly from Aymara &quot;wila&quot; blood, blood-red, &quot;pata&quot; step, stone bench, &quot;red step&quot;) is a mountain in the Vilcanota mountain range in the Andes of Peru, about high. It lies in the Puno Region, Melgar Province, Nuñoa District. It is situated at the Quenamari valley, northeast of Chiaracce.

Geographic entities mentioned:
surface_form: chiaracce
instance_of: Mountain
countries: Peru
coordinates: lat: -14.2703
lon: -70.8586
Vilapata. Vilapata (possibly from Aymara &quot;wila&quot; blood, blood-red, &quot;pata&quot; step, stone bench, &quot;red step&quot;) is a mountain in the Vilcanota mountain range in the Andes of Peru, about high. It lies in the Puno Region, Melgar Province, Nuñoa District. It is situated at the Quenamari valley, northeast of Chiaracce.

Geographic entities mentioned:
surface_form: vilapata
instance_of: Mountain
countries: Peru
coordinates: lat: -14.25194444
lon: -70.82916667
Limestone Hills (Montana). The Limestone Hills, el., is a sub-range of the Big Belt Mountains southwest of Townsend, Montana in Broadwater County, Montana.

Geographic entities mentioned:
surface_form: limestone hills
instance_of: Landform
countries: United States
coordinates: lat: 46.2497
lon: -111.626
surface_form: limestone hills
instance_of: Landform
countries: United States
coordinates: lat: 38.5472
lon: -114.267
Major tributaries. North Fork Chandalar River, long, begins near Atigun Pass in the Brooks Range and flows generally southeast through Chandalar Lake to meet the Middle Fork and form the main stem. At the North Fork, headwaters is a flat valley known as Chandalar shelf just east of the Dalton Highway, where caribou are known to winter.

Geographic entities mentioned:
surface_form: Chandalar Lake
instance_of: Lake
countries: United States
coordinates: lat: 67.5075
lon: -148.5125
Last Ice Age. After the Ice Age, around 13,000 years ago, Montreal and the Saint Lawrence Lowlands were flooded by the Champlain Sea. Within a few centuries, when these waters receded, Mount Royal and its three summits emerged as islands. With the complete withdrawal of the sea, water was retained in some depressions of the island.

Geographic entities mentioned:
surface_form: Mount Royal
instance_of: Mountain
countries: Canada
coordinates: lat: 45.506388888889
lon: -73.588888888889
Within a few centuries, when these waters receded, Mount Royal and its three summits emerged as islands. With the complete withdrawal of the sea, water was retained in some depressions of the island. This was the case of Beaver Lake, located between the summits of Mount Royal. This gradually dried up to become a fen. It was artificially dredged (excavated) in 1938. Before 19th century.

Geographic entities mentioned:
surface_form: Mount Royal
instance_of: Mountain
countries: Canada
coordinates: lat: 45.506388888889
lon: -73.588888888889
Péwé, a glacial geologist with U.S. Navy Operation Deep Freeze, 1957–58, who personally explored this peak as well as adjacent portions of Victoria Land. Nearby features. Péwé Peak is in the Denton Hills. Péwé Peak rises above Joyce Glacier to the north, and Lake Buddha to the west. Shangri-la is to the south and Catacomb Hill to the southwest. Joyce Glacier.

Geographic entities mentioned:
surface_form: Catacomb Hill
instance_of: Mountain
coordinates: lat: -78.0667
lon: 163.417
The valley reminded personnel of the VUWAE (1960-61), who applied the name, of James Hilton's Shangri-la in Lost Horizon. Kelmelis Hills. A group of hills rising to high between Brodie Ponds and Joyce Glacier, situated midway up the Blue Glacier on its east margin. Named in 1992 by US-ACAN after John A.

Geographic entities mentioned:
surface_form: Brodie Ponds
instance_of: Lake
coordinates: lat: -77.95
lon: 163.7
surface_form: joyce
instance_of: Body of water
Lake
coordinates: lat: -77.7167
lon: 161.633
Named by the N.Z. Blue Glacier Party (1956-57) after Ernest Joyce, a member of British Antarctic expeditions of 1901-04, 1907-09 and 1914-17. Zetland Glacier. A small hanging glacier on the southern slopes of Mount Alexandra. The glacier terminates on the cliffs north of Colleen Lake.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
The glacier terminates on the cliffs north of Colleen Lake. The name, applied by New Zealand Geographic Board (NZGB) in 1994, is taken from an old spelling for the Shetland Islands of Scotland. Colleen Lake. Small meltwater lake between the lower parts of Joyce Glacier and Garwood Glacier. It was first seen on the ground by U.S. geologist Troy L. Péwé on Jan. 14, 1958.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: joyce
instance_of: Body of water
Lake
coordinates: lat: -77.7167
lon: 161.633
geologist Troy L. Péwé on Jan. 14, 1958. He gave it the name Colleen because the feature is similar to many of the clear, reflecting lakes in Ireland. Nostoc Flats. A small, flat glacial outwash plain, the surface of which is covered by the algae Nostoc. The feature is located east of the south lobe of Joyce Glacier. So named by the New Zealand Geographic Board (NZGB) in 1994. Lake Buddha.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
The feature is located east of the south lobe of Joyce Glacier. So named by the New Zealand Geographic Board (NZGB) in 1994. Lake Buddha. A large proglacial lake on the south margin of Joyce Glacier in the small valley known as Shangri-la. Named in association with Shangri-la by the New Zealand Victoria University of Wellington Antarctic Expedition (VUWAE), 1960-61. Mount Steep.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: joyce
instance_of: Body of water
Lake
coordinates: lat: -77.7167
lon: 161.633
It was named by New Zealand Geographic Board (NZGB) in 1994; the name is suggested by the steep climb of the west side of the mountain. Shangri-la. A small, secluded valley area completely isolated by mountain peaks, located immediately south of Joyce Glacier and Péwé Peak. The valley reminded personnel of the VUWAE (1960-61), who applied the name, of James Hilton's Shangri-la in Lost Horizon.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: joyce
instance_of: Body of water
Lake
coordinates: lat: -77.7167
lon: 161.633
surface_form: péwé peak
instance_of: Mountain
coordinates: lat: -78.03333333
lon: 163.66666667
Péwé Peak. Péwé Peak () is a bedrock peak, high, composed of granite and topped with a dolerite sill. The peak is immediately south of Joyce Glacier and is surrounded by glacial ice except on the south side. It was named by the Advisory Committee on Antarctic Names for Troy L. Péwé, a glacial geologist with U.S.

Geographic entities mentioned:
surface_form: joyce
instance_of: Body of water
Lake
coordinates: lat: -77.7167
lon: 161.633
Péwé, a glacial geologist with U.S. Navy Operation Deep Freeze, 1957–58, who personally explored this peak as well as adjacent portions of Victoria Land. Nearby features. Péwé Peak is in the Denton Hills. Péwé Peak rises above Joyce Glacier to the north, and Lake Buddha to the west. Shangri-la is to the south and Catacomb Hill to the southwest. Joyce Glacier.

Geographic entities mentioned:
surface_form: joyce
instance_of: Body of water
Lake
coordinates: lat: -77.7167
lon: 161.633
surface_form: péwé peak
instance_of: Mountain
coordinates: lat: -78.03333333
lon: 163.66666667
Péwé Peak rises above Joyce Glacier to the north, and Lake Buddha to the west. Shangri-la is to the south and Catacomb Hill to the southwest. Joyce Glacier. Glacier immediately north of Péwé Peak, draining from the névé northeast of Catacomb Hill and terminating up-valley (west) of the snout of Garwood Glacier, which would have been a tributary to it in times of more intense glaciation.

Geographic entities mentioned:
surface_form: joyce
instance_of: Body of water
Lake
coordinates: lat: -77.7167
lon: 161.633
Glacier immediately north of Péwé Peak, draining from the névé northeast of Catacomb Hill and terminating up-valley (west) of the snout of Garwood Glacier, which would have been a tributary to it in times of more intense glaciation. Named by the N.Z. Blue Glacier Party (1956-57) after Ernest Joyce, a member of British Antarctic expeditions of 1901-04, 1907-09 and 1914-17. Zetland Glacier.

Geographic entities mentioned:
surface_form: joyce
instance_of: Body of water
Lake
coordinates: lat: -77.7167
lon: 161.633
geologist Troy L. Péwé on Jan. 14, 1958. He gave it the name Colleen because the feature is similar to many of the clear, reflecting lakes in Ireland. Nostoc Flats. A small, flat glacial outwash plain, the surface of which is covered by the algae Nostoc. The feature is located east of the south lobe of Joyce Glacier. So named by the New Zealand Geographic Board (NZGB) in 1994. Lake Buddha.

Geographic entities mentioned:
surface_form: joyce
instance_of: Body of water
Lake
coordinates: lat: -77.7167
lon: 161.633
Péwé Peak. Péwé Peak () is a bedrock peak, high, composed of granite and topped with a dolerite sill. The peak is immediately south of Joyce Glacier and is surrounded by glacial ice except on the south side. It was named by the Advisory Committee on Antarctic Names for Troy L. Péwé, a glacial geologist with U.S.

Geographic entities mentioned:
surface_form: péwé peak
instance_of: Mountain
coordinates: lat: -78.03333333
lon: 163.66666667
Péwé, a glacial geologist with U.S. Navy Operation Deep Freeze, 1957–58, who personally explored this peak as well as adjacent portions of Victoria Land. Nearby features. Péwé Peak is in the Denton Hills. Péwé Peak rises above Joyce Glacier to the north, and Lake Buddha to the west. Shangri-la is to the south and Catacomb Hill to the southwest. Joyce Glacier.

Geographic entities mentioned:
surface_form: péwé peak
instance_of: Mountain
coordinates: lat: -78.03333333
lon: 163.66666667
Shangri-la is to the south and Catacomb Hill to the southwest. Joyce Glacier. Glacier immediately north of Péwé Peak, draining from the névé northeast of Catacomb Hill and terminating up-valley (west) of the snout of Garwood Glacier, which would have been a tributary to it in times of more intense glaciation. Named by the N.Z.

Geographic entities mentioned:
surface_form: péwé peak
instance_of: Mountain
coordinates: lat: -78.03333333
lon: 163.66666667
Kimtah Glacier. Kimtah Glacier is in North Cascades National Park in the U.S. state of Washington, in a cirque to the west of Kimtah Peak and east of Cosho Peak. Both Kimtah and Cosho Peaks are prominent summits along a ridge known as Jagged Edge. Kimtah Glacier is just under in width and descends northward from and has four lobes.

Geographic entities mentioned:
surface_form: Kimtah Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.585
lon: -120.91
surface_form: Cosho Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.5889
lon: -120.927
Taïna Barioz. Taïna Barioz (born 2 June 1988, in Papeete, Tahiti) is a French alpine skier. She is the daughter of French ice hockey player Didier Barioz. Barioz won two podiums in Alpine Skiing World Cup, both in giant slalom: 3rd place in Lienz, Austria (December 2009), and then 2nd place at the World Cup finals in St. Moritz, Switzerland (March 2016). Barioz placed 1st in the 2014 FIS NorAms.

Geographic entities mentioned:
surface_form: St. Moritz
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50625
lon: 9.7874444444444
In his youth he was one of the founders of the Green Cross of Adria and graduated in Law at the University of Padua, where he became part of an irredentist group called &quot;San Giusto Battalion&quot;. He took part in the First World War with the rank of captain, earning a Silver Medal of Military Valor for the capture of an enemy outpost on Monte Asolone (Monte Grappa massif) in January 1918.

Geographic entities mentioned:
surface_form: Monte Grappa
instance_of: Mountain
countries: Italy
coordinates: lat: 45.873333333333
lon: 11.799166666667
Arve Valley. The Arve Valley (La vallée de l'Arve) is an alpine valley located in the French Haute-Savoie department. The namesake of the valley is the river at the bottom: the Arve. The valley as a whole makes up the majority of Faucigny, one of the Natural regions of France, and one of six that make up the Savoie region. Geography.

Geographic entities mentioned:
surface_form: vallée de l'arve
instance_of: Valley
countries: France
coordinates: lat: 46.067
lon: 6.5
surface_form: arve valley
instance_of: Valley
countries: France
coordinates: lat: 46.067
lon: 6.5
Arve Valley. The Arve Valley (La vallée de l'Arve) is an alpine valley located in the French Haute-Savoie department. The namesake of the valley is the river at the bottom: the Arve. The valley as a whole makes up the majority of Faucigny, one of the Natural regions of France, and one of six that make up the Savoie region. Geography.

Geographic entities mentioned:
surface_form: arve valley
instance_of: Valley
countries: France
coordinates: lat: 46.067
lon: 6.5
Geography. The Arve Valley consists of the upper reaches of the river Arve, whose source is in the Mont Blanc massif, on the Savoyard Col de Balme side. Downstream, the river passes through the plain of Annemasse, before emptying into the Rhône in the Swiss canton of Geneva. The valley came into being during the last ice age when the Alpine glaciers extended beyond Geneva.

Geographic entities mentioned:
surface_form: arve valley
instance_of: Valley
countries: France
coordinates: lat: 46.067
lon: 6.5
It is also one of the 15 cantons having summits above 2,000 metres. Topographically, the two most important summits of the canton are those of the Bös Fulen (most elevated) and the Rigi (most prominent and isolated). All of the mountains of the canton are part of the Schwyzer Alps mountain range, although not all the mountains of that range lie within the canton.

Geographic entities mentioned:
surface_form: Bös Fulen
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.967222222222
lon: 8.9458333333333
surface_form: Rigi
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.05
lon: 8.4666666666667
In total, the city has around five million trees along 400 km of streets. The Water Forest in Xinghua, Jiangsu is named after the many dawn redwood trees found there in the park. There is a large collection of dawn redwood in the Lushan Botanical Garden within Mount Lu, Jiangxi. In the United Kingdom. The dawn redwood is frequently encountered across the UK.

Geographic entities mentioned:
surface_form: Mount Lu
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.5725
lon: 115.97333333333
Prasanna Venkatachalapathy Temple. Gunaseelam Vishnu Temple (Abhimana Sthalam) is a Hindu temple dedicated to Vishnu located from Trichy, in the South Indian state of Tamil Nadu. It is located on the banks of river Kaveri. It is Classified one among the 108 Abhimana Kshethram of Vaishnavate tradition.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Cedar Park, Seattle. Cedar Park is a neighborhood in the Lake City district of Seattle, Washington. The name generally refers to the residential neighborhoods east of Lake City adjoining Lake Washington. The &quot;Cedar Park&quot; name comes from the plats that subdivided the land along Lake Washington that had previously belonged to the Puget Mill Company.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
This is because the St. Valentin/Amstetten–Villach–Tarvisio route as such is no longer significant. The term &quot;Rudolfsbahn&quot; is used particularly for the Amstetten–Waidhofen–Kleinreifling–Selzthal route through the Ybbs and Enns valley (timetable route 130). Individual sections of the original Rudolfsbahn now form parts of other lines. The Schober Pass line between Selzthal and St.

Geographic entities mentioned:
surface_form: Ybbs
instance_of: Watercourse
countries: Austria
coordinates: lat: 47.7603
lon: 15.2053
A few other counties of Colorado have some land in the Rio Grande Basin including Archuleta, Mineral, Hinsdale, and San Juan. Blanca Peak is prominent in the Sierra Blanca at the southern end of the northernmost section of the mountains, which is known as the Sangre de Cristo Range. There are several passes, with elevations between, giving access to the valley.

Geographic entities mentioned:
surface_form: Blanca Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.5772
lon: -105.486
Otto Mears, then of Saguache, built and operated a historic toll road over Poncha Pass at the north end of the valley into the San Luis Valley during Colorado's 19th century mining era when the valley was the gateway to the San Juan and Gunnison country and the Ute agency was in the mountains west of Saguache. Mount Otto on the east side of the valley is named after him.

Geographic entities mentioned:
surface_form: Mount Otto
instance_of: Mountain
countries: United States
coordinates: lat: 38.327222222222
lon: -105.88277777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Deposits include the deeper alluvial strata, overlying Precambrian basement rock, Eocene alluvial deposits from a shallow Laramide depression, the Blanco Basin Formation; and Oligocene ash and lava flows associated with the Conejos Formation, is the Santa Fe formation, mixed alluvium and lava outflows from the San Juan volcanic field to the west; later strata comprise the Alamosa formation, alternating layers of sand, gravel, and clay.

Geographic entities mentioned:
surface_form: San Juan volcanic field
instance_of: Mountain
countries: United States
coordinates: lat: 37.8933
lon: -106.774
surface_form: san juan volcanic field
instance_of: Mountain
countries: United States
coordinates: lat: 37.8933
lon: -106.774
There was a basin in its western portion which may have drained west through the course historically followed by the San Juan River. Sedimentary deposits formed in that basin during Eocene times remain in place beneath the western portion of the San Luis Valley. During the Pleistocene, parts of the valley were occupied by Lake Alamosa. Agriculture and wildlife.

Geographic entities mentioned:
surface_form: Lake Alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
The principal towns are: Alamosa, Monte Vista, Del Norte, South Fork, Saguache, Center, Moffat, Fort Garland, San Luis, Blanca, Antonito, La Jara, Capulin, Manassa, Sanford, Romeo, Crestone, Villa Grove, Hooper, Mosca, San Acacio and a number of smaller locations. A few other counties of Colorado have some land in the Rio Grande Basin including Archuleta, Mineral, Hinsdale, and San Juan.

Geographic entities mentioned:
surface_form: sanford
instance_of: Mountain
countries: United States
coordinates: lat: 62.213888888889
lon: -144.12888888889
The arts of the San Luis Valley draw from traditions of the early Utes, Apaches, and Comanches and the later Spanish-speaking immigrants. The San Luis Valley is home to five active live theaters, two at Adams State University, The Creede Repertory Theater, The Old Spanish Trails Theatre Company and Rocky Mountain Stage in Monte Vista.

Geographic entities mentioned:
surface_form: rocky mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9727
lon: -74.3732
surface_form: rocky mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.7955
lon: -79.1808
surface_form: rocky mountain
instance_of: Landform
countries: United States
coordinates: lat: 41.7958
lon: -71.055
surface_form: adams
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
surface_form: rocky mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0918
lon: -74.2151
San Luis Valley. The San Luis Valley is a region in south-central Colorado with a small portion overlapping into New Mexico. The valley is approximately long and wide, making it the largest alpine valley in the world. It extends from the Continental Divide on the northwest rim into New Mexico on the south. It contains 6 counties and portions of 3 others.

Geographic entities mentioned:
surface_form: san luis valley
instance_of: Valley
countries: United States
coordinates: lat: 37.2
lon: -105.42
The valley is a section of the Rio Grande Rift and is drained to the south by the Rio Grande, which rises in the San Juan Mountains to the west of the valley and flows south into New Mexico. The San Luis Valley has a cold desert climate but has substantial water resources from the Rio Grande and groundwater.

Geographic entities mentioned:
surface_form: san luis valley
instance_of: Valley
countries: United States
coordinates: lat: 37.2
lon: -105.42
The San Luis Valley has a cold desert climate but has substantial water resources from the Rio Grande and groundwater. The San Luis Valley was ceded to the United States by Mexico following the Mexican–American War. Hispanic settlers began moving north and settling in the valley after the United States made a treaty with the Utes and established a fort in the early 1850s.

Geographic entities mentioned:
surface_form: san luis valley
instance_of: Valley
countries: United States
coordinates: lat: 37.2
lon: -105.42
United States administration. Extensive settlement began in the San Luis Valley, primarily by Hispanic farmers and ranchers from New Mexico, in the 1850s. Early settlers built a church in the village that is now called San Luis and dedicated it on the Feast of Saint Louis, 21 June 1851.

Geographic entities mentioned:
surface_form: san luis valley
instance_of: Valley
countries: United States
coordinates: lat: 37.2
lon: -105.42
Early settlers built a church in the village that is now called San Luis and dedicated it on the Feast of Saint Louis, 21 June 1851. At present, the San Luis Valley has the largest native Hispanic population in Colorado; many families are directly descended from the original New Mexican settlers. The surge of immigration followed the construction by the U.S.

Geographic entities mentioned:
surface_form: san luis valley
instance_of: Valley
countries: United States
coordinates: lat: 37.2
lon: -105.42
The history of the U.S. military presence in the valley is preserved at Fort Garland and other historic preserves in the valley. The San Luis Valley became part of the Territory of Colorado in 1861. The original Ute population was confined to the Southern Ute and Ute Mountain Indian reservations in the late 19th century. Geography.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 37.2
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The original Ute population was confined to the Southern Ute and Ute Mountain Indian reservations in the late 19th century. Geography. The San Luis Valley is the broad, generally flat, valley at the headwaters of the Rio Grande in south central Colorado and far north central New Mexico. The northern portion of the San Luis Valley is an endorheic basin; surface water does not exit this area.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 37.2
lon: -105.42
About 50 miles from east to west and about 150 miles from north to south, the valley is bounded on the east by the Sangre de Cristo Mountains and on the west by the San Juan Mountains. Within Colorado the San Luis Valley is generally considered to comprise five Colorado counties: Saguache, Alamosa, Rio Grande, Conejos, and Costilla.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 37.2
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Otto Mears, then of Saguache, built and operated a historic toll road over Poncha Pass at the north end of the valley into the San Luis Valley during Colorado's 19th century mining era when the valley was the gateway to the San Juan and Gunnison country and the Ute agency was in the mountains west of Saguache. Mount Otto on the east side of the valley is named after him.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 37.2
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countries: United States
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Land ownership and management. About 50% of the in the San Luis Valley is privately owned. Much of the land in the south part of the Valley, in Conejos and Costilla counties, was originally part of large Mexican land grants and is private land.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 37.2
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This land is usually leased to neighboring ranches for grazing for a nominal fee. Part of the value of a ranch is its continuing lease of BLM or National Forest lands. Public lands in the mountains surrounding the San Luis Valley are generally part of the Rio Grande National Forest and are managed by the United States Forest Service.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 37.2
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Ancestral Rockies, the Central Colorado Trough, and the San Luis-Uncompahgre Highlands. The gap between the Precambrian basement rock and the Eocene alluvial deposits in the San Luis Valley is considered evidence that much of southern Colorado, including the western portion of the San Luis Valley, was highlands in the period prior to the Eocene Epoch, 56 to 34 million years ago.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 37.2
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surface_form: san luis valley
instance_of: Valley
countries: United States
coordinates: lat: 37.2
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Western Interior Seaway. In the middle and late Cretaceous Period, about 100 million years ago, the San Luis Valley lay on the shore of or beneath the Western Interior Seaway, a shallow sea which divided North America into two parts.

Geographic entities mentioned:
surface_form: san luis valley
instance_of: Valley
countries: United States
coordinates: lat: 37.2
lon: -105.42
Laramide orogeny. Building of the Rocky Mountains by folding during the Laramide orogeny 80 to 55 million years ago created a highland, the San Luis-Brazos uplift, in the area of the San Luis Valley. This process over 30 million years resulted in an elevated and highly eroded peneplain where the San Luis Valley is today.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 37.2
lon: -105.42
There was a basin in its western portion which may have drained west through the course historically followed by the San Juan River. Sedimentary deposits formed in that basin during Eocene times remain in place beneath the western portion of the San Luis Valley. During the Pleistocene, parts of the valley were occupied by Lake Alamosa. Agriculture and wildlife.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 37.2
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The barley grown here is the main supplier for Coors beer company. In 1982, quinoa was successfully grown for the first time outside of South America in the San Luis Valley of Colorado, and commercial growth has occurred since 1987. Less favored areas with a shorter growing season and less access to water rights tend to be devoted to alfalfa and grazing.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 37.2
lon: -105.42
The San Luis Valley Regional Medical Center is the largest employer in the valley, with over 600 employees. Tourism has become a more important part of the economy in recent years, coupled with attempts to develop the area as a retirement destination. The arts are becoming an increasing force in expanding the economy of the San Luis Valley. Tourist attractions.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 37.2
lon: -105.42
surface_form: san luis valley
instance_of: Valley
countries: United States
coordinates: lat: 37.2
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However, it lacked hiking trails. Then in 2022, after more than a decade of planning, Costilla County and an organization called San Luis Valley Great Outdoors built three hiking trails and one single track mountain bike trail in the park. The San Luis Valley is also home to the Colorado Gator Reptile Rescue.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 37.2
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instance_of: Valley
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coordinates: lat: 37.2
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Monte Vista is also home to the Monte Arts Council as well as several festivals and an art tour that attracts artists from as far away as California and North Carolina. The arts of the San Luis Valley draw from traditions of the early Utes, Apaches, and Comanches and the later Spanish-speaking immigrants.

Geographic entities mentioned:
surface_form: san luis valley
instance_of: Valley
countries: United States
coordinates: lat: 37.2
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It was the largest grid-connected solar electric facility in the United States at that time. It was followed in 2010 by the 19 megawatt Greater Sandhill Solar Plant, in 2011 by the 30 megawatt San Luis Valley Solar Ranch, in 2012 by the 30 megawatt Alamosa Solar Generating Project, and in 2015 by the 50 megawatt Hooper Solar PV Power Plant.

Geographic entities mentioned:
surface_form: san luis valley
instance_of: Valley
countries: United States
coordinates: lat: 37.2
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Opposition to a proposed transmission line has resulted in possible delays in development of solar facilities by Xcel Energy which together with Tri-State Generation and Transmission Association serves the valley. In 2012, the United States Department of Interior designated several Solar Energy Zones on BLM lands in the valley, although no projects have yet been announced to be in development.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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countries: United States
coordinates: lat: 61.3833
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The Minturn Formation, a limestone formation exemplified at Marble Mountain on the crest of the Sangre de Cristos, is evidence of a sea in the Central Colorado Trough during the era of the Ancestral Rockies. Western Interior Seaway.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 58.64139
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surface_form: marble mountain
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countries: United States
coordinates: lat: 40.7309
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The history of the U.S. military presence in the valley is preserved at Fort Garland and other historic preserves in the valley. The San Luis Valley became part of the Territory of Colorado in 1861. The original Ute population was confined to the Southern Ute and Ute Mountain Indian reservations in the late 19th century. Geography.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 36.9375
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San Luis Valley. The San Luis Valley is a region in south-central Colorado with a small portion overlapping into New Mexico. The valley is approximately long and wide, making it the largest alpine valley in the world. It extends from the Continental Divide on the northwest rim into New Mexico on the south. It contains 6 counties and portions of 3 others.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
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countries: United States
coordinates: lat: 47.7174
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It contains 6 counties and portions of 3 others. It is an extensive high-elevation depositional basin of approximately with an average elevation of above sea level. The valley is a section of the Rio Grande Rift and is drained to the south by the Rio Grande, which rises in the San Juan Mountains to the west of the valley and flows south into New Mexico.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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countries: United States
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coordinates: lat: 61.3833
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countries: United States
coordinates: lat: 61.3833
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countries: United States
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countries: United States
coordinates: lat: 47.7174
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The San Luis Valley was ceded to the United States by Mexico following the Mexican–American War. Hispanic settlers began moving north and settling in the valley after the United States made a treaty with the Utes and established a fort in the early 1850s. Prior to the Mexican war the Spanish and Mexican governments had reserved the valley to the Utes.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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coordinates: lat: 47.7174
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Hispanic settlers began moving north and settling in the valley after the United States made a treaty with the Utes and established a fort in the early 1850s. Prior to the Mexican war the Spanish and Mexican governments had reserved the valley to the Utes. Later in the 19th century Anglo settlers began to settle in the valley and engaged in mining, ranching, and irrigated agriculture.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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coordinates: lat: 61.3833
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coordinates: lat: 47.7174
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Prior to the Mexican war the Spanish and Mexican governments had reserved the valley to the Utes. Later in the 19th century Anglo settlers began to settle in the valley and engaged in mining, ranching, and irrigated agriculture. Today the valley has a diverse Anglo and Hispanic population. Utes. Prior to 1868 the Capote (Kapota) band of Ute Indians lived in the valley.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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surface_form: the valley
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coordinates: lat: 61.3833
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surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Later in the 19th century Anglo settlers began to settle in the valley and engaged in mining, ranching, and irrigated agriculture. Today the valley has a diverse Anglo and Hispanic population. Utes. Prior to 1868 the Capote (Kapota) band of Ute Indians lived in the valley. The Utes made a treaty of peace with the United States in 1849 after the Mexican War.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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coordinates: lat: 61.3833
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coordinates: lat: 47.7174
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Shortly thereafter settlers from New Mexico established several small settlements in what is now Colorado and in 1868 the Utes were removed to a reservation in western Colorado. They continued to play a role in Saguache in the northwestern corner of the valley from the Los Pinos Agency to the west of Saguache until they lost their extensive reservation as the result of the Meeker Massacre in 1879.

Geographic entities mentioned:
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countries: United States
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Spanish and Mexican administration. The area was administered as part of the Spanish, later Mexican, province of Nuevo Mexico. In 1843, the government of New Mexico created the Sangre de Cristo Land Grant consisting of of the valley and granted the family of Carlos Beaubien. The area was ceded to the United States in 1848 after the Mexican–American War in the Treaty of Guadalupe Hidalgo.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 34.155833333333334
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The surge of immigration followed the construction by the U.S. Army of Fort Massachusetts for protection against the Utes, who had previously barred settlers. The history of the U.S. military presence in the valley is preserved at Fort Garland and other historic preserves in the valley. The San Luis Valley became part of the Territory of Colorado in 1861.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 34.155833333333334
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The southern portion is drained by the Rio Grande. There is no clear southern boundary but the term is generally used to include the San Luis Hills of southern Colorado and the Taos Plateau of northern New Mexico. About 50 miles from east to west and about 150 miles from north to south, the valley is bounded on the east by the Sangre de Cristo Mountains and on the west by the San Juan Mountains.

Geographic entities mentioned:
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Blanca Peak is prominent in the Sierra Blanca at the southern end of the northernmost section of the mountains, which is known as the Sangre de Cristo Range. There are several passes, with elevations between, giving access to the valley. North La Veta Pass, through the Sangre de Cristo Mountains, is used by U.S.

Geographic entities mentioned:
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countries: United States
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Highway 160 and by the Colorado Pacific Rio Grande Railroad (formerly a branch of the Denver & Rio Grande Western) tracks. Other passes used historically were Medano, Mosca and Sangre de Cristo Passes. The Great Sand Dunes are a famous feature of the valley. They lie directly to the west of the Sangre de Cristo Mountains. The dunes can reach high.

Geographic entities mentioned:
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countries: United States
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The dunes can reach high. The Great Sand Dunes National Park and Preserve is now in place to protect both the dunes and the numerous archeological sites found in the area. The natural valley aquifer is close to the surface in this part of the valley, and helps with maintenance of water levels in the San Luis Lakes, just to the west of the sand dunes.

Geographic entities mentioned:
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countries: United States
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