Sarmila/GeoWiki-Features huggingface dataset:
Background. Mount Garibaldi is located on the east side of the Cheakamus River between Squamish and Whistler in New Westminster Land District. 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.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
The Pacific Ranges Ecoregion is part of the Coast and Mountains Ecoprovince which forms part of the Humid Maritime and Highlands Ecodivision. The Pacific Ranges Ecoregion is subdivided into seven ecosections, the Eastern Pacific Ranges Ecosection being the main ecosection at Mount Garibaldi.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Subfeatures. The northern and eastern flanks of Mount Garibaldi are covered by the Garibaldi Névé, the main glacial feature at the volcano. Several individually named outlet glaciers drain the Garibaldi Névé.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
The Garibaldi and Lava glaciers issue from the south side of the Garibaldi Névé, sending their muddy waters to the Mamquam River. 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.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Atwell Peak contains sharp and exposed ridges, as well as steep and loose faces that are prone to avalanching. 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.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
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. A spur known as The Sharkin separates the Warren and North Pitt glaciers on the northeast side of Mount Garibaldi.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
The Cheekye River flows west into the Cheakamus River which flows south and southwest into the Squamish River. Cheekye is a Squamish name meaning &quot;strong rushing water&quot;. Ring Creek originates from the Bishop and Diamond glaciers on Mount Garibaldi. It flows west and southwest into the Mamquam River which flows west and south into the mouth of the Squamish River.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
It flows west and southwest into the Mamquam River which flows west and south into the mouth of the Squamish River. Zig Zag Creek drains Lava Glacier and flows southeast into Skookum Creek. The Pitt River also originates at Mount Garibaldi and flows southwest from the North Pitt and South Pitt glaciers into the Fraser River. Geology.

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
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: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
surface_form: garibaldi lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.925
lon: -123.01
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. The Mount Garibaldi–Garibaldi Lake volcanic field is normally separated into the Mount Garibaldi and Garibaldi Lake volcanic fields on the basis of differing magmatic chemistry.

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
lon: -123.00472222222
surface_form: garibaldi lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.925
lon: -123.01
surface_form: garibaldi lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.925
lon: -123.01
It is one of the three Cascade Arc volcanoes made exclusively of dacite, the other two being Glacier Peak and Mount Cayley. Rhyodacite is also a common volcanic rock at Mount Garibaldi and Mount Cayley, although high-silica rhyolite is uniquely present at Mount Garibaldi. Subordinate andesite erupted at all three volcanoes relatively early in their histories.

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
lon: -123.00472222222
The modern volcanic edifice is a supraglacial volcano, having been partially constructed over glacial ice during the Pleistocene epoch. Like many other stratovolcanoes in the Cascade Volcanic Arc, Mount Garibaldi stands out by itself above the surrounding landscape. This is in contrast to most other volcanoes in the Coast Mountains, which are hidden within higher subranges.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Mount Garibaldi is bounded by Brohm Ridge on the northwest and by Alice Ridge on the southwest. Extending from the southern flank of Mount Garibaldi is the unusually long Ring Creek lava flow. It is dacitic in composition, attains a length of approximately and contains well-defined levees along its margins.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Sediments eroded from the Ring Creek lava flow form an alluvial fan at the Mamquam River and Skookum Creek confluence. The western slopes of Mount Garibaldi are underlain by sheared and altered quartz diorite, which has undergone stream and glacial erosion to form rugged topography with relief up to. Volcanic history.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Volcanic history. At least three stages of eruptive activity contributed to the formation of Mount Garibaldi. The initial Cheekye stage took place between 260,000 and 220,000 years ago with the eruption of dacite and breccia, resulting in the formation of a broad composite cone.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
The initial Cheekye stage took place between 260,000 and 220,000 years ago with the eruption of dacite and breccia, resulting in the formation of a broad composite cone. Parts of this &quot;proto-Garibaldi&quot; or ancestral volcano are exposed on Mount Garibaldi's lower northern and eastern flanks and on the upper of Brohm Ridge.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Around where Columnar Peak and possibly Glacier Pikes are now located, several coalescing dacitic domes were constructed. Dacite from the western end of Alice Ridge, from Columnar Peak and from Mount Garibaldi have K–Ar ages of 260,000 ± 160,000 years, 220,000 ± 220,000 years and 260,000 ± 130,000 years, respectively.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Glacial overlap was most significant on the west and somewhat to the south. Subsequent melting of the ice sheet and its component glaciers removed support from the western flank of Mount Garibaldi, resulting in a series of landslides between 12,800 and 11,500 years ago that moved nearly half of the volcano's volume into the Squamish Valley.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Subsequent melting of the ice sheet and its component glaciers removed support from the western flank of Mount Garibaldi, resulting in a series of landslides between 12,800 and 11,500 years ago that moved nearly half of the volcano's volume into the Squamish Valley. This catastrophic collapse produced the Cheekye Fan and the scarp exposing the internal structure of Mount Garibaldi.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
This catastrophic collapse produced the Cheekye Fan and the scarp exposing the internal structure of Mount Garibaldi. Soon before or after the buried ice had melted away, the Dalton Dome stage commenced with the eruption of dacite lava down Mount Garibaldi's north and northeastern flanks.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
surface_form: dalton dome
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Soon before or after the buried ice had melted away, the Dalton Dome stage commenced with the eruption of dacite lava down Mount Garibaldi's north and northeastern flanks. 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.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
surface_form: dalton dome
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
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. This represents the latest known eruptive event at Mount Garibaldi and the volcano is now considered to be dormant.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
This represents the latest known eruptive event at Mount Garibaldi and the volcano is now considered to be dormant. At least two debris flows in the order of occurred at Mount Garibaldi in the 1930s and 1950s, both of which swept down the Cheekye River. The 1950s debris flow was caused by heavy rains and reached the Cheakamus River where it formed a temporary landslide dam.

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

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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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. Although Plinian eruptions have not been identified at Mount Garibaldi, Peléan eruptions can also produce large amounts of volcanic ash that could significantly affect the nearby communities of Whistler and Squamish.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Peléan eruptions might cause short and long term water supply problems for the city of Vancouver and most of the Lower Mainland. 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.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
As a result, the Cheekye linears pose potential landslide hazards to Brackendale and several Squamish Nation villages nearby. The danger of catastrophic landslides from Mount Garibaldi has restricted development on the Cheekye Fan. In 2018, a major development on the Cheekye Fan was approved by Squamish council.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
The project included 537 single-family units, 678 multi-unit dwellings and a $45 million debris flow barrier to prevent a large landslide from reaching the Cheekye Fan. Because dacite is the main type of lava erupted from Mount Garibaldi, lava flows are a low to moderate hazard. Dacite is felsic in composition, containing 62–69% silica content.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Monitoring. Like other volcanoes in Canada, Mount Garibaldi is not monitored closely enough by the Geological Survey of Canada to ascertain its activity level. The Canadian National Seismograph Network has been established to monitor earthquakes throughout Canada, but it is too far away to provide an accurate indication of activity under the mountain.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
It may sense an increase in seismic activity if Mount Garibaldi becomes highly restless, but this may only provide a warning for a large eruption; the system might detect activity only once the volcano has started erupting. If Mount Garibaldi were to erupt, mechanisms exist to orchestrate relief efforts.

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
lon: -123.00472222222
Indigenous peoples. To the Squamish people, the local indigenous people of this area, Mount Garibaldi is called Nch'ḵay̓ (). In their language it means &quot;Dirty Place&quot;, referring to the muddy waters of the Cheekye River. Mount Garibaldi is considered sacred to the Squamish people as it is an important part of their history.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
In their oral history, they passed down a story of the great flood that covered their land after the last ice age. During the flood, Mount Garibaldi was only one of two mountains that peaked over the water. The Squamish people headed for Mount Garibaldi and latched their canoes to the mountain with a rope made from woven cedar bark in order to prevent being swept away.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Mount Garibaldi is the largest volcano in Squamish Nation territory. An obsidian outcrop on the southeastern flank of Mount Garibaldi is said by the Squamish people to have been created by the thunderbird, a legendary creature in some North American indigenous peoples' history and culture.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Party members included A. Morkill, B. S. Darling, A. Cawdry, W. G. Barker, A. J. Armistead and Mr. Wedgwood. A party consisting of 13 members of the British Columbia Mountaineering Club ascended Mount Garibaldi from the southeast face on August 13, 1911. The first women to attain the summit of Mount Garibaldi were Vancouver climbers Pansy Munday and L. C. Hanafin on July 16, 1913.

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
lon: -123.00472222222
Mooers, Joseph T. Hazard and Fred Fenton of Seattle, Washington. The leader of the climbing party, Joseph T. Hazard, stated that &quot;while a little less than 9,000 feet high, Mount Garibaldi is much more difficult of ascent than any of the major peaks of Washington&quot;. In 1927, Mount Garibaldi was incorporated into the newly formed, Garibaldi Provincial Park.

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
lon: -123.00472222222
Mooers, Joseph T. Hazard and Fred Fenton of Seattle, Washington. The leader of the climbing party, Joseph T. Hazard, stated that &quot;while a little less than 9,000 feet high, Mount Garibaldi is much more difficult of ascent than any of the major peaks of Washington&quot;. In 1927, Mount Garibaldi was incorporated into the newly formed, Garibaldi Provincial Park.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Despite being the namesake of Garibaldi Provincial Park, Mount Garibaldi is not its highest mountain. On October 19, 1953, a plane operated by Pacific Western Airlines crashed on the slopes of Mount Garibaldi, killing all five people aboard. The plane was on a mercy flight from Gunn Lake to Vancouver at the time of the accident.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Post-accident investigation could not determine the cause of the crash. Vancouver teachers Christopher Clifford Harris, 33, and Margo Anne Fowler, 26, got married on the summit of Mount Garibaldi on April 14, 1973, to express their passion for mountain climbing. The couple managed to get to the nearly inaccessible, summit by helicopter. They wore traditional mountaineering garb for their wedding.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
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. In 1978, the Government of British Columbia invited California-based developer Wolfgang Richter to salvage the failed Mount Garibaldi Glacier Resorts project.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
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. The route to the Garibaldi Névé on Mount Garibaldi's eastern flank is marked by cairns.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Bergschrunds and other crevasses can pose difficulty and danger in late spring or summer when snow and ice has melted away. Rockfalls and loose rock are ever-present hazards at this time of the year; rocks regularly rumble down Mount Garibaldi's flanks without apparent provocation. For this reason, early-season, cold-weather snow ascents are recommended for most routes up Mount Garibaldi.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Paul's Hospital in Vancouver. Frank de Bruyn, a 16-year-old mountain climber from Vancouver, was killed by a small avalanche near the snow-covered summit of Mount Garibaldi on July 19, 1961. De Bruyn was one of three youths climbing Mount Garibaldi, the other two being 18-year-olds James Hebden and James Fowler.

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
lon: -123.00472222222
Vancouver mountaineers Lloyd Williams, 26, Heinz Rostek, 22, and Don Hoover, 22, were trapped on Mount Garibaldi for four days in April 1963. The trio left the Diamond Head chalet on April 11 for a skiing trip around Mount Garibaldi to Garibaldi Lake where they were to meet another group of skiers on April 14.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
surface_form: garibaldi lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.925
lon: -123.01
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: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Dalton Dome routes. At least three routes run up Mount Garibaldi to Dalton Dome, none of which are commonly climbed due to extremely poor quality rock. The most direct independent summit route to Dalton Dome is the Northwest Shoulder Route (grade II and class 4), which is approached via Brohm Ridge to the base of Mount Garibaldi's northwest shoulder.

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
The Southwest Ridge Route (grade III and class 3–4) is mainly climbed in winter when conditions are favorable. It is approached via a snow or scree traverse from Brohm Ridge below the west face of Mount Garibaldi where the southwest ridge is ascended to the summit. Ascending the Warren Glacier headwall on the far right side is the North Face Route (grade III and class 4–5).

Geographic entities mentioned:
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Dalton Dome routes. At least three routes run up Mount Garibaldi to Dalton Dome, none of which are commonly climbed due to extremely poor quality rock. The most direct independent summit route to Dalton Dome is the Northwest Shoulder Route (grade II and class 4), which is approached via Brohm Ridge to the base of Mount Garibaldi's northwest shoulder.

Geographic entities mentioned:
surface_form: dalton dome
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Ascending the Warren Glacier headwall on the far right side is the North Face Route (grade III and class 4–5). It climbs steep snow and remarkably unstable rock to a small escarpment that gains the northwest shoulder, which then leads to Dalton Dome's summit.

Geographic entities mentioned:
surface_form: dalton dome
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
The Mount Garibaldi–Garibaldi Lake volcanic field is normally separated into the Mount Garibaldi and Garibaldi Lake volcanic fields on the basis of differing magmatic chemistry. 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.

Geographic entities mentioned:
surface_form: garibaldi lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.925
lon: -123.01
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. Although the mountain is not known to have been volcanically active since that time, it could erupt again, which could endanger the nearby populace.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
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. 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.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Their oral history includes a story of the mountain and a great flood. 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.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
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:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Coastal western hemlock forests dominate nearly all the valleys and lower slopes of this ecosection, the upper slopes containing subalpine mountain hemlock forests and, to a lesser extent, Engelmann spruce and subalpine fir forests. Alpine vegetation lies just above the subalpine forests, which is normally overlain by barren rock.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Alpine vegetation lies just above the subalpine forests, which is normally overlain by barren rock. Wildlife such as grey jays, chipmunks, squirrels, flickers, Columbian black tailed deer, mountain goats, wolverines, cougars and grizzly and black bears are locally present.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Like many other stratovolcanoes in the Cascade Volcanic Arc, Mount Garibaldi stands out by itself above the surrounding landscape. 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.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
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. This scarp formed as a result of collapse of the western flank which produced a debris flow deposit in the Squamish Valley called the Cheekye Fan.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Monitoring. Like other volcanoes in Canada, Mount Garibaldi is not monitored closely enough by the Geological Survey of Canada to ascertain its activity level. The Canadian National Seismograph Network has been established to monitor earthquakes throughout Canada, but it is too far away to provide an accurate indication of activity under the mountain.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
During the flood, Mount Garibaldi was only one of two mountains that peaked over the water. The Squamish people headed for Mount Garibaldi and latched their canoes to the mountain with a rope made from woven cedar bark in order to prevent being swept away. As the flood waters started to recede, a large lake was formed and the Squamish people returned to their home site in Squamish.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: cedar
instance_of: Lake
countries: Canada
coordinates: lat: 53.366666666667
lon: -100
The first ascent of Mount Garibaldi was made by Vancouver mountaineers Gordon B. Warren, Arthur Tinniswood Dalton, Tom C. Pattison, William Tinniswood Dalton, James John Trorey and Atwell Duncan King on August 11, 1907. This mountaineering party had recognized the volcanic origin of the mountain. Another party led by A. T.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
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:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Vancouver teachers Christopher Clifford Harris, 33, and Margo Anne Fowler, 26, got married on the summit of Mount Garibaldi on April 14, 1973, to express their passion for mountain climbing. The couple managed to get to the nearly inaccessible, summit by helicopter. They wore traditional mountaineering garb for their wedding. According to Harris, &quot;You can see snow and mountain tops forever.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
From the road's end, Brohm Ridge is hiked to the Garibaldi Névé. Climbing and skiing. Mountain climbing on Mount Garibaldi is done in winter when the loose volcanic rocks comprising the mountain are frozen in place by snow and ice. Most climbing routes are confined to the glaciers and snow slopes, which are abundant in winter and spring.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Ernie Vossler, the original Golf Pro, later took the neighborhood golf community concept and created the Oak Tree developments (Oak Tree National) in Edmond, Oklahoma, as well as La Quinta Resort developments in the Coachella Valley (Palm Springs, California) area.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
The club has organized annual events aimed at providing support to children and families in need throughout the Pacific Northwest. In Southern Oregon, the club’s Rogue Valley chapter organizes the “Turkeys & Toys” ride, which raises funds to purchase holiday meals and Christmas gifts. In 2013, the second annual event raised approximately $6,000 to support local families.

Geographic entities mentioned:
surface_form: Rogue Valley
instance_of: Valley
countries: United States
coordinates: lat: 42.440122222222
lon: -122.92615277778
Its proto-cathedral (now Église Notre Dame de l’Assomption) was located on Cape Breton Island, in the port town of Arichat. In both Scottish and Canadian folklore, the first ordinary of the Diocese, Bishop William Fraser of Strathglass, is a folk hero. He is said to have been a man of enormous physical strength and to have been able to break steel horseshoes with his bare hands.

Geographic entities mentioned:
surface_form: Strathglass
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.35
lon: -4.7166666666667
List of rivers of Georgia (country). The rivers of Georgia, a country in the Caucasus, are part of either the Black Sea or Caspian Sea Drainage basins. The most spectacular rivers include the Alazani (longest river flowing through Georgia and Azerbaijan), Aragvi, Enguri (second longest river within Georgia), Kura (Mtkvari), and Rioni (longest river in Georgia).

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Ghamubar Zom. Ghamubar Zom () is a mountain in the Hindu Raj mountain range in Gilgit–Baltistan, Pakistan. It has a summit elevation of 6,518 m above sea level. The mountain is close to the border of Gilgit–Baltistan and Khyber Pakhtunkhwa. The nearest village to the mountain is Darkot in Yasin valley. The entire prominence of mountain is visible from Darkot and Rawat villages.

Geographic entities mentioned:
surface_form: Yasin
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.367777777777775
lon: 73.33777777777777
Ghamubar Zom. Ghamubar Zom () is a mountain in the Hindu Raj mountain range in Gilgit–Baltistan, Pakistan. It has a summit elevation of 6,518 m above sea level. The mountain is close to the border of Gilgit–Baltistan and Khyber Pakhtunkhwa. The nearest village to the mountain is Darkot in Yasin valley. The entire prominence of mountain is visible from Darkot and Rawat villages.

Geographic entities mentioned:
surface_form: ghamubar zom
instance_of: Mountain
countries: Pakistan
coordinates: lat: 36.59
lon: 73.341666666667
Climate. The climate in this area has mild differences between highs and lows, and there is adequate rainfall year-round. According to the Köppen Climate Classification system, Red Creek has a marine west coast climate, abbreviated &quot;Cfb&quot; on climate maps. Elkins 21 ENE is a weather station located above Red Creek on the Canaan Valley Plateau, near the Canaan Valley Ski Resort.

Geographic entities mentioned:
surface_form: Canaan Valley Plateau
instance_of: Valley
countries: United States
coordinates: lat: 39.126666666667
lon: -79.378055555556
Camp La-No-Che. Camp La-No-Che is the Boy Scout Camp located on the north shore of Lake Norris in Paisley, Florida. It is a part of Central Florida Council of the Boy Scouts of America and is home to Tipisa Lodge of the Order of the Arrow (OA). Camp La-No-Che is part of the Leonard and Marjorie Williams Family Scout Reservation.

Geographic entities mentioned:
surface_form: Lake Norris
instance_of: Lake
countries: United States
coordinates: lat: 28.9377
lon: -81.5349
The Committee to find new land suitable for a summer camp was headed by Judge Don Cheney, an Orange County judge and long time Scouting supporter who was the first president of the Central Florida Council when it was organized in the 1920s. Through various means they investigated the Gould Hunting Lodge on the north shore of Lake Norris in Lake County, FL.

Geographic entities mentioned:
surface_form: Lake Norris
instance_of: Lake
countries: United States
coordinates: lat: 28.9377
lon: -81.5349
Chullunkhäni (La Paz). Chullunkhäni (Aymara &quot;chullunkhä&quot; ('ä' stands for a long 'a') icicle, &quot;-ni&quot; a suffix, &quot;the one with icicles&quot;, also spelled &quot;Chulluncani&quot;) is a mountain in the Bolivian Andes. It is located in the La Paz Department, Aroma Province, Patacamaya Municipality. This is where the Jach'a Jawira originates.

Geographic entities mentioned:
surface_form: chullunkhäni (la paz)
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.18
lon: -67.83138889
Chullunkhäni (La Paz). Chullunkhäni (Aymara &quot;chullunkhä&quot; ('ä' stands for a long 'a') icicle, &quot;-ni&quot; a suffix, &quot;the one with icicles&quot;, also spelled &quot;Chulluncani&quot;) is a mountain in the Bolivian Andes. It is located in the La Paz Department, Aroma Province, Patacamaya Municipality. This is where the Jach'a Jawira originates.

Geographic entities mentioned:
surface_form: chullunkhäni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.18
lon: -67.83138889
Brocken (South Georgia). Brocken () is a mountain rising over close southwest of Calf Head on the north side of South Georgia. It was named by the German group of the International Polar Year Investigations, 1882–83, after the Brocken, the highest mountain in central Germany.

Geographic entities mentioned:
surface_form: Brocken
instance_of: Mountain
countries: Germany
Kingdom of Prussia
coordinates: lat: 51.800555555556
lon: 10.617222222222
surface_form: brocken
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -54.4833
lon: -36.0667
Brocken (South Georgia). Brocken () is a mountain rising over close southwest of Calf Head on the north side of South Georgia. It was named by the German group of the International Polar Year Investigations, 1882–83, after the Brocken, the highest mountain in central Germany.

Geographic entities mentioned:
surface_form: brocken (south georgia)
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -54.4833
lon: -36.0667
Brocken (South Georgia). Brocken () is a mountain rising over close southwest of Calf Head on the north side of South Georgia. It was named by the German group of the International Polar Year Investigations, 1882–83, after the Brocken, the highest mountain in central Germany.

Geographic entities mentioned:
surface_form: brocken
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -54.4833
lon: -36.0667
It opened on 31 October 1879 and closed its doors for the final time on Saturday 30 January 2005. History. The David Morgan department store was founded by David Morgan who was born near Brecon in 1833. He traded in the South wales valley areas of Abertillery, Monmouthshire and Pontlottyn in the Rhymney Valley for 21 years, before opening a small drapers shop on The Hayes in 1879.

Geographic entities mentioned:
surface_form: Rhymney Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.697777777778
lon: -3.2294444444444
Christoff Cliff. Christoff Cliff (Hristov Kamak \'hris-tov 'ka-m&k\) is a rocky cliff forming Aytos Point on the coast of Bransfield Strait, eastern Livingston Island in the South Shetland Islands, Antarctica. The cliff rises to over 300 m at the southern extremity of an offshoot of Serdica Peak and has ice-free eastern and southern slopes.

Geographic entities mentioned:
surface_form: Bransfield Strait
instance_of: Body of water
countries: Antarctica
coordinates: lat: -63
lon: -59
Christoff Cliff. Christoff Cliff (Hristov Kamak \'hris-tov 'ka-m&k\) is a rocky cliff forming Aytos Point on the coast of Bransfield Strait, eastern Livingston Island in the South Shetland Islands, Antarctica. The cliff rises to over 300 m at the southern extremity of an offshoot of Serdica Peak and has ice-free eastern and southern slopes.

Geographic entities mentioned:
surface_form: Serdica Peak
instance_of: Mountain
coordinates: lat: -62.68125
lon: -60.056111111111
The cliff overlooks Boyana Glacier to the west and Srebarna Glacier to the northeast. The cliff is named after the famous Bulgarian singer Boris Christoff (1914-93). Location. The cliff is located at which is 2 km southeast of Serdica Peak, 2.7 km southwest by south of Radichkov Peak and 2.4 km southeast by east of Silistra Knoll.

Geographic entities mentioned:
surface_form: Serdica Peak
instance_of: Mountain
coordinates: lat: -62.68125
lon: -60.056111111111
surface_form: Radichkov Peak
instance_of: Mountain
coordinates: lat: -62.681388888889
lon: -60.02125
surface_form: Silistra Knoll
instance_of: Mountain
coordinates: lat: -62.6905
lon: -60.091666666667
They are protected within the Sequoia National Forest. Geography. The range is located in eastern Kern County and Tulare County. They are east of the San Joaquin Valley, northeast of Bakersfield, and form the west side of the Kern River Valley. The range reaches an elevation of at Sunday Peak, located just south of Portuguese Pass.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
surface_form: Kern River Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.6232
lon: -118.4845
Some nicknames of the city are &quot;Sugar City&quot;, after the numerous sugarcane plantations of the Yabucoa Valley, and &quot;Pueblo de Yuca&quot; (&quot;Yuca Town&quot;) which references the Taíno origin of the name of the town. The locals are also known as the &quot;Bebe Leches&quot; (&quot;milk drinkers&quot;) after the numerous dairy farms located in the region. History.

Geographic entities mentioned:
surface_form: Yabucoa Valley
instance_of: Valley
countries: United States
coordinates: lat: 18.05526
lon: -65.82733
Geography. The municipality of Yabucoa is located in the south-eastern coast of Puerto Rico. The Valley of Yabucoa is surrounded by the hills of the San Lorenzo Batholith on three sides and by the Caribbean Sea on the fourth.

Geographic entities mentioned:
surface_form: Valley of Yabucoa
instance_of: Valley
countries: United States
coordinates: lat: 18.05526
lon: -65.82733
Rodríguez. Agriculture. Yabucoa is known for its agricultural prowess because of the surrounding fertile valley that produces most of the island's plantains and bananas. Yabucoeños are known as &quot;sugar people&quot; because most of the valley was used for sugar cane growth.

Geographic entities mentioned:
surface_form: valley
instance_of: Valley
countries: United States
coordinates: lat: 18.05526
lon: -65.82733
The walking sticks are attributes of the traveller, and refer to the holy office of the Angels as guides and companions in man's journey in his earthly life. The canes are adorned with guajana flowers, representing the wealth of the sugar cane. The green land where the angels stand symbolizes the fertile valley in which Yabucoa is located. Transportation.

Geographic entities mentioned:
surface_form: valley
instance_of: Valley
countries: United States
coordinates: lat: 18.05526
lon: -65.82733
Robert S. Kennedy Bird Conservancy Living Laboratory actively protects 500 hectares of this habitat that contains the highest density of Bagobo robin and also serves as a home for Mindanao endemic birds such as the Slaty-backed jungle flycatcher, Red-eared parrotfinch and Bukidnon woodcock. This species occurs in other protected areas such as Mount Apo and Mount Kitanglad.

Geographic entities mentioned:
surface_form: Mount Kitanglad
instance_of: Mountain
countries: Philippines
coordinates: lat: 8.1427777777778
lon: 124.9125
It is established at the south of the Paraguaná Peninsula in a coastal plain, flanked by the Médanos de Coro National Park to the north and the Sierra de Coro to the south, at a few kilometers from its port (La Vela de Coro) in the Caribbean Sea at a point equidistant between the Ensenada de La Vela and Golfete de Coro.

Geographic entities mentioned:
surface_form: Sierra de Coro
instance_of: Landform
countries: Venezuela
Geography. Coro is located at north of the Coro region, transition between the Venezuelan Coastal Range and the Cordillera de Mérida. Located on a coastal plain of xerophyte vegetation (19 msn) covering the entire western Falcón state and reaches its narrowest point just in the city, closing a few miles east of Coro by foothills of the Sierra de Falcón.

Geographic entities mentioned:
surface_form: Sierra de Falcón
instance_of: Landform
countries: Venezuela
Major features of the coast include the 250-kilometer long Rennick Glacier (one of Antarctica's largest glaciers), the Anare Mountains, and the northern ends of the Bowers and Admiralty mountain ranges. Inland, the land is dominated by numerous smaller mountain ranges (notably the Freyberg Mountains and the Concord Mountains), and by two large névés, the Rennick Névé and the Evans Névé.

Geographic entities mentioned:
surface_form: Evans Névé
instance_of: Landform
coordinates: lat: -72.75
lon: 164.5
Finkenstein am Faaker See. Finkenstein am Faaker See () is a market town in the district of Villach-Land in Carinthia, Austria. Geography. It is located south of Villach and the Drava River, on the northern slope of the Karawanks with Mt. Mittagskogel (&quot;Kepa&quot;), close to the border with Slovenia. The municipal area comprises the southern shore of Lake Faak.

Geographic entities mentioned:
surface_form: Mittagskogel
instance_of: Mountain
countries: Austria
Slovenia
coordinates: lat: 46.506833
lon: 13.952398
Finkenstein am Faaker See. Finkenstein am Faaker See () is a market town in the district of Villach-Land in Carinthia, Austria. Geography. It is located south of Villach and the Drava River, on the northern slope of the Karawanks with Mt. Mittagskogel (&quot;Kepa&quot;), close to the border with Slovenia. The municipal area comprises the southern shore of Lake Faak.

Geographic entities mentioned:
surface_form: Lake Faak
instance_of: Lake
countries: Austria
coordinates: lat: 46.577777777778
lon: 13.925
The community's general layout still appears much as it did in the late 1930s. Location. Cumberland Homesteads is located in a hilly area atop the Cumberland Plateau, just south of Crossville. Byrd Creek, a tributary of the Obed River, flows through and drains much of the community.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Byrd Creek, a tributary of the Obed River, flows through and drains much of the community. Cumberland Mountain State Park, which was developed simultaneously in the 1930s as a recreational area, is located in Cumberland Homesteads. U.S. Route 127 connects the Homestead area with Crossville and Interstate 40 to the north and the Sequatchie Valley to the south.

Geographic entities mentioned:
surface_form: Sequatchie Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.125
lon: -85.5289
The Simić brotherhood moved to Valjevo's Podgorina around the beginning of the 18th century from Polimlje area, Montenegro-Serbia border. On their way towards the Kingdom of Hungary with other refugees from Old Herzegovina and Old Montenegro, they stopped in Podgorina, at the foot of the Medvednik mountain (probably because the impassable hinterland provided security from the Ottomans).

Geographic entities mentioned:
surface_form: Medvednik
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.20917
lon: 19.63972