Sarmila/GeoWiki-Features huggingface dataset:
Bald Mountain (Summit County, Colorado). Bald Mountain is a high and prominent mountain summit in the Front Range of the Rocky Mountains of North America. The thirteener is located in Arapaho National Forest, southeast (bearing 135°) of the Town of Breckenridge in Summit County, Colorado, United States.

Geographic entities mentioned:
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.655
lon: -114.409
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.8827026
lon: -88.0390147
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.8822
lon: -123.866
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6611024
lon: -107.4103338
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.4291
lon: -75.7503
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.6988
lon: -110.902
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.021388888889
lon: -75.190833333333
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.5344
lon: -119.115
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.423611111111
lon: -74.593888888889
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1209
lon: -74.2001
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.902777777778
lon: -74.724444444444
surface_form: bald mountain (summit county, colorado)
instance_of: Mountain
countries: United States
coordinates: lat: 39.4439
lon: -105.969
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7386
lon: -74.9129
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.294722222222
lon: -74.387777777778
Bald Mountain (Summit County, Colorado). Bald Mountain is a high and prominent mountain summit in the Front Range of the Rocky Mountains of North America. The thirteener is located in Arapaho National Forest, southeast (bearing 135°) of the Town of Breckenridge in Summit County, Colorado, United States.

Geographic entities mentioned:
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.655
lon: -114.409
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.8827026
lon: -88.0390147
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.8822
lon: -123.866
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6611024
lon: -107.4103338
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.4291
lon: -75.7503
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.6988
lon: -110.902
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.021388888889
lon: -75.190833333333
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.5344
lon: -119.115
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.423611111111
lon: -74.593888888889
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1209
lon: -74.2001
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.902777777778
lon: -74.724444444444
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.4439
lon: -105.969
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7386
lon: -74.9129
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.294722222222
lon: -74.387777777778
In 1616 he became a member of the Amsterdam vroedschap and represented the States faction. In 1620 he was appointed schepen. Like his father he invested in draining the polders Purmer, Schermer and Heerhugowaard. In 1624, on behalf of the city, he was appointed landlord of Amstelveen en Nieuwer-Amstel. As manager at the Wisselbank (for just one year) he visited Emden, requesting a loan.

Geographic entities mentioned:
surface_form: Purmer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.488888888889
lon: 5.0069444444444
It surmounts upper Flask Glacier to the north, and a tributary to Fleece Glacier to the south-southeast. The feature is named after the settlement of Zadruga in Northeastern Bulgaria. Location. Mount Zadruga is located at, which is 11.45 km south-southwest of Peychinov Crag, 27.7 km west of Bildad Peak, 12.9 km north of Moider Peak, and 33 km east-southeast of Mount Chevreux on Graham Coast.

Geographic entities mentioned:
surface_form: Bildad Peak
instance_of: Mountain
coordinates: lat: -65.8167
lon: -62.6
surface_form: Moider Peak
instance_of: Mountain
coordinates: lat: -65.9167
lon: -63.15
surface_form: Mount Chevreux
instance_of: Mountain
coordinates: lat: -65.7667
lon: -64
surface_form: mount zadruga
instance_of: Mountain
coordinates: lat: -65.8081
lon: -63.2153
Mount Zadruga. Mount Zadruga (,) is the ice-covered peak rising to 1700 m in the west part of Voden Heights on Oscar II Coast in Graham Land. It surmounts upper Flask Glacier to the north, and a tributary to Fleece Glacier to the south-southeast. The feature is named after the settlement of Zadruga in Northeastern Bulgaria. Location.

Geographic entities mentioned:
surface_form: mount zadruga
instance_of: Mountain
coordinates: lat: -65.8081
lon: -63.2153
Laja River (Chile). Laja River () is a river in Chile, along which can be found the Laja Falls. It is located in the Bío Bío Region. The source of the river is Laguna del Laja in the Andes, then flows westward through the Chilean Central Valley and terminates into the Bío Bío River, being an important tributary of it. Whitewater.

Geographic entities mentioned:
surface_form: Chilean Central Valley
instance_of: Valley
countries: Chile
coordinates: lat: -35.5
lon: -71.5
surface_form: central valley
instance_of: Valley
countries: Chile
coordinates: lat: -35.5
lon: -71.5
surface_form: laja
instance_of: Watercourse
countries: Chile
coordinates: lat: -37.269903
lon: -72.724342
Because the river is formed from exiting the bottom of the lake the river level is always constant. Hydropower. Three hydropower plants are located at and below the outlet of Lake Laja, including the 400 MW El Toro Hydroelectric Plant built in 1973 and the 300 MW Antuco Hydroelectric Plant built in 1981. Irrigation.

Geographic entities mentioned:
surface_form: antuco
instance_of: Mountain
countries: Chile
coordinates: lat: -37.41
lon: -71.351111111111
surface_form: laja
instance_of: Watercourse
countries: Chile
coordinates: lat: -37.269903
lon: -72.724342
Laja River (Chile). Laja River () is a river in Chile, along which can be found the Laja Falls. It is located in the Bío Bío Region. The source of the river is Laguna del Laja in the Andes, then flows westward through the Chilean Central Valley and terminates into the Bío Bío River, being an important tributary of it. Whitewater.

Geographic entities mentioned:
surface_form: laja river (chile)
instance_of: Watercourse
countries: Chile
coordinates: lat: -37.269903
lon: -72.724342
Laja River (Chile). Laja River () is a river in Chile, along which can be found the Laja Falls. It is located in the Bío Bío Region. The source of the river is Laguna del Laja in the Andes, then flows westward through the Chilean Central Valley and terminates into the Bío Bío River, being an important tributary of it. Whitewater.

Geographic entities mentioned:
surface_form: laja
instance_of: Watercourse
countries: Chile
coordinates: lat: -37.269903
lon: -72.724342
surface_form: laja
instance_of: Watercourse
countries: Chile
coordinates: lat: -37.269903
lon: -72.724342
Whitewater. The Laja River is known among whitewater kayakers in Chile as Class 5 very steep and thrilling whitewater kayaking run. The Laja river actually forms from a drainage in the Lake Laja where the water exits at the bottom of the lake through the side of a mountain. Because the river is formed from exiting the bottom of the lake the river level is always constant. Hydropower.

Geographic entities mentioned:
surface_form: laja
instance_of: Watercourse
countries: Chile
coordinates: lat: -37.269903
lon: -72.724342
Whitewater. The Laja River is known among whitewater kayakers in Chile as Class 5 very steep and thrilling whitewater kayaking run. The Laja river actually forms from a drainage in the Lake Laja where the water exits at the bottom of the lake through the side of a mountain. Because the river is formed from exiting the bottom of the lake the river level is always constant. Hydropower.

Geographic entities mentioned:
surface_form: laja
instance_of: Watercourse
countries: Chile
coordinates: lat: -37.269903
lon: -72.724342
surface_form: laja
instance_of: Watercourse
countries: Chile
coordinates: lat: -37.269903
lon: -72.724342
Irrigation. Below the lake and the hydropower plants and before the Laja Falls lie 70,000 hectares of irrigated land. History. In 1984, private companies planned to divert the Laja River to another river further north to power new hydroelectric plants there.

Geographic entities mentioned:
surface_form: laja
instance_of: Watercourse
countries: Chile
coordinates: lat: -37.269903
lon: -72.724342
Opponents argued that the interbasin transfer would dry up the Laja Falls and would increase pollution in the lower Biobío River, because the Laja River diluted the pollution from the upper BíoBío River and pollutant would be more concentrated in the absence of this dilution. Irrigators also feared their water rights would be affected.

Geographic entities mentioned:
surface_form: laja
instance_of: Watercourse
countries: Chile
coordinates: lat: -37.269903
lon: -72.724342
surface_form: laja
instance_of: Watercourse
countries: Chile
coordinates: lat: -37.269903
lon: -72.724342
Hydropower. Three hydropower plants are located at and below the outlet of Lake Laja, including the 400 MW El Toro Hydroelectric Plant built in 1973 and the 300 MW Antuco Hydroelectric Plant built in 1981. Irrigation. Below the lake and the hydropower plants and before the Laja Falls lie 70,000 hectares of irrigated land. History.

Geographic entities mentioned:
surface_form: laja
instance_of: Watercourse
countries: Chile
coordinates: lat: -37.269903
lon: -72.724342
It is in the lower middle of Austria, almost the same distance from Innsbruck in the west as it is from Vienna in the northeast. Klagenfurt is elevated above sea level and covers an area of. It is on the lake Wörthersee and on the Glan river. The city is surrounded by several forest covered hills and mountains, with heights of up to (for example Ulrichsberg).

Geographic entities mentioned:
surface_form: Wörthersee
instance_of: Lake
countries: Austria
coordinates: lat: 46.625
lon: 14.15
Local government and elections. The parish comes within the Soar Valley electoral district for purposes of electing a councillor to Nottinghamshire County Council. The most recent election was in 2009 when Linda Sykes, of the Conservative party, won the seat.

Geographic entities mentioned:
surface_form: Soar Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.74
lon: -1.14
History. The Ciuta originates in the mountainous terrain of the Val Masino and the Valchiavenna, in an area where Lombard is spoken; &quot;ciuta&quot; means &quot;little sheep&quot; in the local language. It may have common origins with the Ciavenasca breed from the same area.

Geographic entities mentioned:
surface_form: Valchiavenna
instance_of: Valley
countries: Italy
coordinates: lat: 46.25
lon: 9.4
The Germans, eager to retake the position attacked on 5 January 1915 but were repulsed by the French force. Background. The village of Edea was positioned on the Sanaga River, to the southeast of the major port city of Duala. A large portion of the German Duala garrison had withdrawn to this position following the Allied naval bombardment of the city.

Geographic entities mentioned:
surface_form: Sanaga River
instance_of: Watercourse
countries: Cameroon
coordinates: lat: 3.5593388888889
lon: 9.652175
The town has a population of 9,526 inhabitants (INDEC, 2010) and is located on National Route 38, and the Tren de las Sierras line of the General Manuel Belgrano Railway. The center of Santa Maria de Punilla is located approximately 50 km northwest of the state's capital city of Córdoba and 3 km south of the city of, Cosquín. The municipality is also located on the banks of the Cosquín River.

Geographic entities mentioned:
surface_form: Cosquín River
instance_of: Watercourse
countries: Argentina
coordinates: lat: -31.216666666667
lon: -64.483333333333
Description. It rises in the high Cascades, issuing from Maidu Lake at elevation of in the Mount Thielsen Wilderness, along the Douglas-Klamath county line approximately east of Roseburg. It follows a serpentine course down from the Cascades, westward along the southern side of the Calapooya Mountains.

Geographic entities mentioned:
surface_form: Maidu Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.255
lon: -121.99971944444
The white people are preparing to build a R. R. through our country, which will not be permitted. Some years ago we were taken by the haid & pulled here close to Texans where we have to fight. But we have cut that loos now and are all going with the Cheyennes to the Antalope Hills. When Gen Custer was here two or three years ago, he arrested me & kept me in confinement several days.

Geographic entities mentioned:
surface_form: Antalope Hills
instance_of: Landform
Mountain
countries: United States
coordinates: lat: 35.9
lon: -99.88
He was given the additional command responsibilities of the 12th Division and the Northern Territory Lines of Communications Area in December. Appointed the commanding officer of the 6th Division in April 1943 and oversaw the division's training on the Atherton Tableland, Queensland.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
He ruled from the city of Napata, located deep in Nubia, modern-day Sudan. Name. Piye adopted two throne names: Usimare and Sneferre. He was passionate about the worship of the god Amun, like many kings of Nubia. He revitalized the moribund Great Temple of Amun at Jebel Barkal, which was first built under Thutmose III of the New Kingdom, employing numerous sculptors and stonemasons from Egypt.

Geographic entities mentioned:
surface_form: Jebel Barkal
instance_of: Mountain
countries: Sudan
coordinates: lat: 18.5368
lon: 31.8276
Burial. Piye's tomb was located next to the largest Pyramid in the cemetery, designated Ku.1 (seen in the image on the right), at el-Kurru near Jebel Barkal in what is now Northern Sudan. Down a stairway of 19 steps opened to the east, the burial chamber is cut into the bedrock as an open trench and covered with a corbelled masonry roof.

Geographic entities mentioned:
surface_form: Jebel Barkal
instance_of: Mountain
countries: Sudan
coordinates: lat: 18.5368
lon: 31.8276
In addition to the main peak, Mount Garibaldi has two named sub-peaks. Atwell Peak is a sharp, conical peak slightly higher than the more rounded peak of Dalton Dome. Both were volcanically active at different times throughout Mount Garibaldi's eruptive history.

Geographic entities mentioned:
surface_form: Atwell Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8411
lon: -123.009
surface_form: dalton dome
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Flowing from the steep western face of Mount Garibaldi is the Cheekye River, a tributary of the Cheakamus River. Opal Cone on the southeastern flank is a small volcanic cone from which a lengthy lava flow descends. The western face is a landslide feature that formed in a series of collapses between 12,800 and 11,500 years ago.

Geographic entities mentioned:
surface_form: Opal Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8272
lon: -122.971
These include Garibaldi Glacier northwest of Opal Cone, North Pitt Glacier on the northeastern face of Mount Garibaldi, South Pitt Glacier southeast of Glacier Pikes, Lava Glacier west of Mamquam Lake, Sentinel Glacier southeast of Garibaldi Lake, Warren Glacier at the headwaters of Culiton Creek, Bishop Glacier south of the head of the Pitt River, Phoenix Glacier south of Deception Peak and Pike Glacier east of Glacier Pikes.

Geographic entities mentioned:
surface_form: Garibaldi Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.925
lon: -123.01
surface_form: Deception Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.89969
lon: -122.96939
surface_form: opal cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8272
lon: -122.971
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
A spur known as The Sharkin separates the Warren and North Pitt glaciers on the northeast side of Mount Garibaldi. Diamond Head is a subsidiary peak on the south side of Mount Garibaldi named for its resemblance to Diamond Head in Hawaii. Mount Garibaldi lies within the Squamish River watershed.

Geographic entities mentioned:
surface_form: Diamond Head
instance_of: Mountain
countries: United States
coordinates: lat: 21.259722222222
lon: -157.81175
surface_form: diamond head
instance_of: Mountain
countries: Canada
coordinates: lat: 49.82555555555556
lon: -123.00722222222223
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Geology. Mount Garibaldi is one of the three principal volcanoes in the southern segment of the Garibaldi Volcanic Belt, the other two being Mount Price and The Black Tusk. It represents the largest volcano in the combined Mount Garibaldi–Garibaldi Lake volcanic field, which encompasses of volcanic material.

Geographic entities mentioned:
surface_form: Garibaldi Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
surface_form: The Black Tusk
instance_of: Mountain
countries: Canada
coordinates: lat: 49.97527777777778
lon: -123.04277777777777
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
surface_form: black tusk
instance_of: Mountain
countries: Canada
coordinates: lat: 49.97527777777778
lon: -123.04277777777777
surface_form: the black tusk
instance_of: Mountain
countries: Canada
coordinates: lat: 49.97527777777778
lon: -123.04277777777777
surface_form: garibaldi volcanic belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
Structure. Mount Garibaldi is a moderately eroded stratovolcano overlooking the town of Squamish at the head of Howe Sound north of Vancouver. It is one of the three Cascade Arc volcanoes made exclusively of dacite, the other two being Glacier Peak and Mount Cayley.

Geographic entities mentioned:
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: glacier peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.35055555555556
lon: -116.28361111111111
The catchment area for the Greater Vancouver watershed is downwind from Mount Garibaldi. An eruption producing floods and lahars could destroy parts of Highway 99, threaten communities such as Brackendale and endanger water supplies from Pitt Lake. Fisheries on the Pitt River would also be at risk.

Geographic entities mentioned:
surface_form: Pitt Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.4167
lon: -122.55
surface_form: pitt lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.4167
lon: -122.55
They ascended the west face of Mount Garibaldi by approaching from the southwest, which involved traversing along the Mamquam River and then climbing Round Mountain and The Gargoyles. Hanafin and Munday also climbed neighbouring Mamquam Mountain during the same expedition. The first United States party to climb Mount Garibaldi consisted of 13 members of The Mountaineers in August 1923.

Geographic entities mentioned:
surface_form: Mamquam Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.7753
lon: -122.851
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The Brohm Ridge Chalet sleeps a total of 40 people whilst the nearby Black Tusk Snowmobile Clubhouse sleeps a further 14. A BC Parks shelter at the Elfin Lakes offers overnight stays and can sleep up to 33 people. It is equipped with a propane heater, a wash sink, pit toilet facilities, propane lights, two propane hot plates and four picnic tables.

Geographic entities mentioned:
surface_form: Elfin Lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 49.7856
lon: -122.989
It is equipped with a propane heater, a wash sink, pit toilet facilities, propane lights, two propane hot plates and four picnic tables. The Elfin Lakes Campground offers a day-use shelter, hang storage facilities, pit toilet facilities, two outdoor picnic tables, four indoor picnic tables and 35 tent platforms.

Geographic entities mentioned:
surface_form: elfin lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 49.7856
lon: -122.989
Mamquam Road then extends northeast and becomes Garibaldi Park Road. At the end of Garibaldi Park Road is the Diamond Head parking lot, which lies from Highway 99 at an elevation of. The Diamond Head hiking trail commences from the parking lot to the Elfin Lakes where Opal Cone, Columnar Peak, The Gargoyles and Mamquam Icefield can be viewed.

Geographic entities mentioned:
surface_form: diamond head
instance_of: Mountain
countries: Canada
coordinates: lat: 49.82555555555556
lon: -123.00722222222223
Mamquam Road then extends northeast and becomes Garibaldi Park Road. At the end of Garibaldi Park Road is the Diamond Head parking lot, which lies from Highway 99 at an elevation of. The Diamond Head hiking trail commences from the parking lot to the Elfin Lakes where Opal Cone, Columnar Peak, The Gargoyles and Mamquam Icefield can be viewed.

Geographic entities mentioned:
surface_form: elfin lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 49.7856
lon: -122.989
surface_form: opal cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8272
lon: -122.971
Hazards include snow cornices as well as unprotected climbing on loose rock and rime ice. The Southeast Face Routes (grade II and class 3–4) are approached via Alice Ridge or Elfin Lakes to Diamond Glacier. They ascend couloirs in steep shattered rock, one of which offers a direct climb to a point immediately south of Atwell's summit.

Geographic entities mentioned:
surface_form: elfin lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 49.7856
lon: -122.989
Another growth period began with the eruption of Atwell Peak about 13,000 years ago when Mount Garibaldi was surrounded by an ice sheet during the last glacial period. The latest period of volcanic activity took place about 10,000 years ago with eruptions from Dalton Dome and Opal Cone after the ice sheet retreated.

Geographic entities mentioned:
surface_form: opal cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8272
lon: -122.971
surface_form: dalton dome
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Dalton Dome is a blunt summit named after Arthur Tinniswood Dalton. Dalton was a Vancouver architect, city assessor and mountaineer who took part in the first ascent of Mount Garibaldi. The eastern side of Mount Garibaldi contains a peak known as The Tent. Opal Cone on the southeastern flank of Mount Garibaldi is a parasitic cone near the south side of Garibaldi Glacier.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Another dacite flow issued from Dalton Dome shortly after the ice sheet had receded, having travelled down the landslide scarp on Mount Garibaldi's western flank. Possibly contemporaneous volcanism occurred at Opal Cone with the eruption of the voluminous Ring Creek lava flow between 10,700 and 9,300 years ago.

Geographic entities mentioned:
surface_form: opal cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8272
lon: -122.971
This high percentage in silica content increases the viscosity of dacitic melts relative to that of andesite or basalt, generally resulting in the formation of steep-sided lava domes and stubby lava flows. An exception is the Ring Creek dacite flow from Opal Cone, a length that is normally attained by basaltic lava flows. Monitoring.

Geographic entities mentioned:
surface_form: opal cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8272
lon: -122.971
The Diamond Head hiking trail commences from the parking lot to the Elfin Lakes where Opal Cone, Columnar Peak, The Gargoyles and Mamquam Icefield can be viewed. A hiking trail extending from the Elfin Lakes leads down to Ring Creek then climbs Opal Cone where Mamquam Lake and the Garibaldi Névé can be viewed from its summit.

Geographic entities mentioned:
surface_form: opal cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8272
lon: -122.971
Wildlife such as grey jays, chipmunks, squirrels, flickers, Columbian black tailed deer, mountain goats, wolverines, cougars and grizzly and black bears are locally present. The communities of Whistler, Pemberton, Mount Currie, Hope and Yale are situated within the Eastern Pacific Ranges Ecosection, all of which are connected to the Lower Mainland by a network of highways. Subfeatures.

Geographic entities mentioned:
surface_form: mount currie
instance_of: Mountain
countries: Canada
coordinates: lat: 50.24861111111111
lon: -122.78194444444445
surface_form: mount currie
instance_of: Mountain
countries: Canada
coordinates: lat: 50.80305555555555
lon: -115.49222222222222
Mount Garibaldi. Mount Garibaldi (,) is a dormant stratovolcano in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It has a maximum elevation of and rises above the surrounding landscape on the east side of the Cheakamus River in New Westminster Land District. In addition to the main peak, Mount Garibaldi has two named sub-peaks.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
It lies within the Pacific Ranges Ecoregion, a mountainous region of the southern Coast Mountains characterized by high, steep and rugged mountains made of granitic rocks. Much of this ecoregion encompasses the Pacific Ranges in southwestern British Columbia, although it also includes the northwesternmost portion of the Cascade Range in Washington state.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Although the glaciers at times have seen surges reaching further down slope, a 2009 study published in the &quot;Global and Planetary Change&quot; journal found that they overall have been progressively retreating since the early 1900s. A study conducted by the University of British Columbia in 2015 determined that 70% of all the glacial ice in Canada would be melted away by the year 2100.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
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The obsidian outcrop is where lightning from the thunderbird's eyes struck ground. Garibaldi obsidian was used to create tools due to its ability to form sharp edges, but its quality is poor compared to other obsidian sources in British Columbia. Pieces of Garibaldi obsidian are distributed in the Strait of Georgia where they occur in archaeological sites as early as 4,500 years old.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
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The ski resort was to open in the winter of 1970, but financial difficulties in 1969 halted all developments. In January 1970, the three Swiss-style chalets remained unfinished, the gondola lift consisted only of towers with no lift cables, and the gondola cars were stored in another building at the foot of Mount Garibaldi.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
In 1927, Mount Garibaldi was incorporated into the newly formed, Garibaldi Provincial Park. This mountainous Class A provincial park was named after Mount Garibaldi and contains a number of other volcanoes, including Mount Price, Cinder Cone, The Black Tusk and The Table. Despite being the namesake of Garibaldi Provincial Park, Mount Garibaldi is not its highest mountain.

Geographic entities mentioned:
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countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
surface_form: the table
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8953
lon: -123.013
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countries: Canada
coordinates: lat: 49.97527777777778
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countries: Canada
coordinates: lat: 49.97527777777778
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countries: Canada
coordinates: lat: 49.9717
lon: -123.007
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
The saddle dividing Diamond Head and The Gargoyles is then traversed northeasterly on a trail to the Garibaldi Névé. It is also possible to access Mount Garibaldi from Brohm Ridge. An unmarked road just before Brohm Lake and north of the Alice Lake Provincial Park turnoff extends southward from Highway 99 towards Cat Lake. About down the road is a gate that is locked at 5 p.m.

Geographic entities mentioned:
surface_form: cat lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.7058
lon: -91.8512
C. Hanafin on July 16, 1913. They ascended the west face of Mount Garibaldi by approaching from the southwest, which involved traversing along the Mamquam River and then climbing Round Mountain and The Gargoyles. Hanafin and Munday also climbed neighbouring Mamquam Mountain during the same expedition.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: round mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.7649
lon: -123.024
This volcanic field consists of at least twelve eruptive centres that are in the form of stratovolcanoes, lava domes, cinder cones and subglacial volcanoes. These include Mount Price, The Black Tusk, The Table, Cinder Cone and Round Mountain, all of which formed in the last 1.3 million years.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 49.8953
lon: -123.013
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countries: Canada
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countries: Canada
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instance_of: Mountain
countries: Canada
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countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: round mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.7649
lon: -123.024
During winter, cold Arctic air invades from the Central Interior, resulting in extreme cloud cover and snow. A number of other volcanoes are situated within the Eastern Pacific Ranges Ecosection. This includes Mount Cayley, which lies in the Squamish River watershed, and Mount Meager, which lies near the headwaters of the Lillooet River.

Geographic entities mentioned:
surface_form: mount meager
instance_of: Mountain
countries: Canada
coordinates: lat: 50.63166667
lon: -123.50416667
The 1950s debris flow was caused by heavy rains and reached the Cheakamus River where it formed a temporary landslide dam. This is the latest debris flow to reach the Cheakamus River from the Cheekye basin. In contrast to Mount Cayley and Mount Meager, no hot springs are known in the Garibaldi area. However, there is evidence of anomalously high heat flow in Table Meadows and elsewhere.

Geographic entities mentioned:
surface_form: mount meager
instance_of: Mountain
countries: Canada
coordinates: lat: 50.63166667
lon: -123.50416667
At least three seismic events have occurred at Mount Garibaldi since 1985, indicating that the volcano is potentially active and poses a significant hazard to the area. Volcanic hazards. Mount Garibaldi is one of two volcanoes in Canada classified as a very high threat by Natural Resources Canada, the other volcano being Mount Meager to the northwest.

Geographic entities mentioned:
surface_form: mount meager
instance_of: Mountain
countries: Canada
coordinates: lat: 50.63166667
lon: -123.50416667
There is also the danger of avalanches during ripe snow conditions. A more common and less crevassed approach is via Diamond Glacier to a saddle in the moraine ridge at the foot of Atwell Peak's southeast buttress. Once the saddle has been climbed by ascending a final steep slope, the rocky summit of Mount Garibaldi is reached by proceeding up Cheekye Glacier.

Geographic entities mentioned:
surface_form: moraine
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countries: Canada
coordinates: lat: 51.3225
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surface_form: atwell peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8411
lon: -123.009
Several climbing routes ascend the flanks of Mount Garibaldi and involve traversing glaciers, snow slopes or loose rock. Mountain climbing hazards include crevasses, avalanches and rockfalls. Access to Mount Garibaldi is via hiking trails from Alice Ridge, Brohm Ridge, and the Diamond Head parking lot at the end of Garibaldi Park Road. Background.

Geographic entities mentioned:
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countries: Canada
coordinates: lat: 49.82555555555556
lon: -123.00722222222223
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
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Immediately to the north of Mount Garibaldi and directly below its northern face, the Warren Glacier flows towards the Cheakamus River. The Garibaldi Névé and its outlet glaciers have a combined area of about. Other glaciers on Mount Garibaldi include Cheekye Glacier south of the summit and Diamond Glacier between Atwell Peak and Diamond Head.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 49.82555555555556
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surface_form: atwell peak
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countries: Canada
coordinates: lat: 49.8411
lon: -123.009
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Opal Cone on the southeastern flank of Mount Garibaldi is a parasitic cone near the south side of Garibaldi Glacier. A spur known as The Sharkin separates the Warren and North Pitt glaciers on the northeast side of Mount Garibaldi. Diamond Head is a subsidiary peak on the south side of Mount Garibaldi named for its resemblance to Diamond Head in Hawaii.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Landauer fractured a leg when a ski broke while skiing on Mount Garibaldi. It was Landauer's first accident as an expert skier, having occurred as the 46-year-old neared Diamond Head Lodge. Landauer was brought down Mount Garibaldi by a party of 25 holidayers at Diamond Head Lodge and then transferred to a light truck which took him to Squamish via logging road.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 49.82555555555556
lon: -123.00722222222223
surface_form: diamond head
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countries: Canada
coordinates: lat: 49.82555555555556
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Hebden got caught in the edge of the avalanche and was sent to the Squamish General Hospital after sustaining a lung injury. Fowler escaped injury, but underwent shock treatment the next day after stumbling down the mountainside with word of the accident. Vancouver mountaineers Lloyd Williams, 26, Heinz Rostek, 22, and Don Hoover, 22, were trapped on Mount Garibaldi for four days in April 1963.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
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Recreation facilities. Overlooking the Tantalus Range is the Brohm Ridge Chalet, a three-story European-style lodge built in the 1960s as part of the attempted ski resort development. It is now operated by the Black Tusk Snowmobile Club, a non-profit organization founded in 1971 in the community of Squamish.

Geographic entities mentioned:
surface_form: black tusk
instance_of: Mountain
countries: Canada
coordinates: lat: 49.97527777777778
lon: -123.04277777777777
This activity produced mostly dacite, the main type of volcanic rock forming Mount Garibaldi. Volcanism between 260,000 and 220,000 years ago constructed an ancestral cone that was subsequently destroyed. Another growth period began with the eruption of Atwell Peak about 13,000 years ago when Mount Garibaldi was surrounded by an ice sheet during the last glacial period.

Geographic entities mentioned:
surface_form: atwell peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8411
lon: -123.009
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Mount Garibaldi contains a number of individually named peaks. Atwell Peak is a conical plug dome in elevation. It is named after Atwell Duncan Francis Joseph King, an ardent mountaineer who led the first ascent of Mount Garibaldi in 1907. Atwell Peak contains sharp and exposed ridges, as well as steep and loose faces that are prone to avalanching.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
During the ensuing long period of dormancy, the Cheekye River cut a deep valley into the cone's western flank which was later filled with the Fraser ice sheet. After reaching its maximum extent, the Fraser ice sheet was covered with volcanic ash and fragmented debris from the Atwell Peak stage.

Geographic entities mentioned:
surface_form: atwell peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8411
lon: -123.009
After reaching its maximum extent, the Fraser ice sheet was covered with volcanic ash and fragmented debris from the Atwell Peak stage. This period of growth began about 13,000 years ago with the eruption of the Atwell Peak plug dome from a ridge surrounded by the ice sheet. As the plug dome rose, massive sheets of broken lava crumbled as talus down its sides.

Geographic entities mentioned:
surface_form: atwell peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8411
lon: -123.009
The area below the summit pinnacle is exposed to rockfall and is moderately prone to avalanching. Atwell Peak routes. Two considerably more challenging and objectively dangerous routes run up the northwest face of Atwell Peak. The first route, referred to as the Armenian Express (grade V and class 4–5), involves climbing the major couloir on the far right of the northwest face.

Geographic entities mentioned:
surface_form: atwell peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8411
lon: -123.009
This couloir is ascended until loose rock forces a traverse onto the south ridge just below the summit. The second route is the Siberian Express (grade V and class 4–5) and ascends the huge central couloir just north of the summit of Atwell Peak. It leads directly to the summit ridge over moderately sloping snow and ice with a very steep finish.

Geographic entities mentioned:
surface_form: atwell peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8411
lon: -123.009
Ascents are commonly made in winter when hazards such as avalanches and snow cornices exist all along the ridge. The South Arête Route (grade IV and class 4–5) is a technical climbing route ascending a highly exposed arête that divides the southeast and southwest faces of Atwell Peak. It leads directly to Atwell's summit, climbing steep terrain throughout its entirety.

Geographic entities mentioned:
surface_form: atwell peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8411
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The Mount Garibaldi lavas are hypersthene-normative hawaiites and nepheline-normative mugearite with subordinate olivine tholeiites whereas the Garibaldi Lake lavas are calc-alkaline basaltic andesites through rhyolite. Like other volcanoes in the Garibaldi Volcanic Belt, Mount Garibaldi formed as a result of subduction zone volcanism.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
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surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
This is in contrast to most other volcanoes in the Coast Mountains, which are hidden within higher subranges. The mountain has a proximal relief of, a draping relief of, an elevation of and a height of. With a length of and a width of, Mount Garibaldi is one of the larger volcanoes in the Garibaldi Volcanic Belt. The western side of the mountain contains a scarp exposing its internal structure.

Geographic entities mentioned:
surface_form: garibaldi volcanic belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
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surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Mount Garibaldi. Mount Garibaldi (,) is a dormant stratovolcano in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It has a maximum elevation of and rises above the surrounding landscape on the east side of the Cheakamus River in New Westminster Land District. In addition to the main peak, Mount Garibaldi has two named sub-peaks.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
It has a maximum elevation of and rises above the surrounding landscape on the east side of the Cheakamus River in New Westminster Land District. In addition to the main peak, Mount Garibaldi has two named sub-peaks. Atwell Peak is a sharp, conical peak slightly higher than the more rounded peak of Dalton Dome.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Atwell Peak is a sharp, conical peak slightly higher than the more rounded peak of Dalton Dome. Both were volcanically active at different times throughout Mount Garibaldi's eruptive history. The northern and eastern flanks of Mount Garibaldi are obscured by the Garibaldi Névé, a large snowfield containing several radiating glaciers.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Both were volcanically active at different times throughout Mount Garibaldi's eruptive history. The northern and eastern flanks of Mount Garibaldi are obscured by the Garibaldi Névé, a large snowfield containing several radiating glaciers. Flowing from the steep western face of Mount Garibaldi is the Cheekye River, a tributary of the Cheakamus River.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
The northern and eastern flanks of Mount Garibaldi are obscured by the Garibaldi Névé, a large snowfield containing several radiating glaciers. Flowing from the steep western face of Mount Garibaldi is the Cheekye River, a tributary of the Cheakamus River. Opal Cone on the southeastern flank is a small volcanic cone from which a lengthy lava flow descends.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
These collapses resulted in the formation of a large debris flow deposit that fans out into the Squamish Valley. Mount Garibaldi has been the focus of intermittent volcanic activity over the last 260,000 years. This activity produced mostly dacite, the main type of volcanic rock forming Mount Garibaldi.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Mount Garibaldi has been the focus of intermittent volcanic activity over the last 260,000 years. This activity produced mostly dacite, the main type of volcanic rock forming Mount Garibaldi. Volcanism between 260,000 and 220,000 years ago constructed an ancestral cone that was subsequently destroyed.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
If this were to happen, relief efforts could be organized by teams such as the Interagency Volcanic Event Notification Plan who are prepared to notify people threatened by volcanic eruptions in Canada. The area surrounding Mount Garibaldi has been inhabited by indigenous peoples for thousands of years. Their oral history includes a story of the mountain and a great flood.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
The non-indigenous name of the mountain was given by George Henry Richards in 1860 in honour of the Italian patriot and soldier Giuseppe Garibaldi. Several mountaineers had climbed Mount Garibaldi by the early 1900s, some of whom were members of mountaineering clubs. A plane operated by Pacific Western Airlines crashed on the slopes of Mount Garibaldi in 1953; all five people aboard were killed.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Several mountaineers had climbed Mount Garibaldi by the early 1900s, some of whom were members of mountaineering clubs. A plane operated by Pacific Western Airlines crashed on the slopes of Mount Garibaldi in 1953; all five people aboard were killed. The construction of a ski resort was begun in the late 1960s, but developments were halted in 1969 due to financial difficulties.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
The construction of a ski resort was begun in the late 1960s, but developments were halted in 1969 due to financial difficulties. Several climbing routes ascend the flanks of Mount Garibaldi and involve traversing glaciers, snow slopes or loose rock. Mountain climbing hazards include crevasses, avalanches and rockfalls.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222