Sarmila/GeoWiki-Features huggingface dataset:
The steep sides and unusually large thicknesses of the trachyte flows comprising Koosick and Ornostay bluffs is attributed to them having been extruded through glacial ice. Pillow Ridge Formation. The Pillow Ridge Formation is restricted to Pillow Ridge and Tsekone Ridge on Mount Edziza's northwestern flank, both of which are glaciovolcanic in origin.

Geographic entities mentioned:
surface_form: pillow ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7594
lon: -130.652
This ridge is elliptical in structure, containing a nearly long, north–south trending axis. Nearly surrounding Tsekone Ridge are trachyte flows of the Edziza Formation which is slightly younger than the Pillow Ridge Formation.

Geographic entities mentioned:
surface_form: pillow ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7594
lon: -130.652
In contrast, potassium–argon dating has yielded an anomalously old age of 5.9 ± 0.9 million years which is inconsistent with the ages of the underlying and overlying formations. This date being much older than the fission track dates most likely results from contamination and introduction of excess argon from the partially fused granitic and gneissic xenoliths in Pillow Ridge Formation basalt.

Geographic entities mentioned:
surface_form: pillow ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7594
lon: -130.652
The northernmost cinder cone in the Desolation Lava Field is Sidas Cone which consists of two symmetrical halves and reaches an elevation of. Drainage. Mount Edziza is drained on all sides by streams within the Stikine River watershed. Elwyn Creek is a westward-flowing stream originating from the northwestern flank of Mount Edziza.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Subfeatures. High on the eastern rim of Ice Peak are two glaciated volcanic cones called Icefall Cone and Ridge Cone, both with elevations of about. Punch Cone on the western flank of Ice Peak protrudes through Mount Edziza's ice cap whereas Koosick Bluff and Ornostay Bluff, also on the western flank of Ice Peak, extend westward onto the surrounding Big Raven Plateau.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Volcanic rocks of intermediate composition such as trachybasalt, tristanite, mugearite and benmoreite are restricted to Ice Peak where they form the upper part of this subsidiary peak. Ice Peak is the only location where mugearites and benmoreites are found in the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
The third and fourth oldest geological formations comprising Mount Edziza are the Pillow Ridge and Edziza formations, which were deposited by volcanic eruptions 0.9 million years ago during the later stages of the third magmatic cycle; they both overlie the Ice Peak Formation.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
A period of volcanic activity at the end of the fourth magmatic cycle 0.3 million years ago deposited the Kakiddi Formation, the fifth oldest geological formation comprising Mount Edziza which also overlies the Ice Peak Formation. The youngest geological formation is the Big Raven Formation, which was formed by a period of volcanic activity during the fifth magmatic cycle in the last 20,000 years.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
In contrast, much of the southern edge of Sphinx Dome has been destroyed by headward erosion of Cook Creek; the western half of this rhyolite dome is also buried under trachyte of the Edziza Formation. From Cartoona Ridge north to Tennaya Creek are isolated remnants of Pharaoh Dome, the main mass of which comprises flow-layered rhyolite and is buried under basalt of the Ice Peak Formation.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Both bluffs are similar in geomorphology and composition, consisting of several lava flows up to thick. The Neck, which forms a prominent high buttress on Sorcery Ridge, is also part of the Ice Peak Formation. Potassium–argon dating of pantelleritic trachyte from the Ice Peak Formation has yielded ages of 1.6 ± 0.2 million years, 1.5 ± 0.4 million years and 1.5 ± 0.1 million years.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Mount Edziza. Mount Edziza (;) is a volcanic mountain in Cassiar Land District of northwestern British Columbia, Canada. It is located on the Big Raven Plateau of the Tahltan Highland which extends along the western side of the Stikine Plateau. Mount Edziza has an elevation of, making it the highest point of the Mount Edziza volcanic complex and one of the highest volcanoes in Canada.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
All sides of Mount Edziza are drained by tributaries of Mess Creek and Kakiddi Creek which are situated within the Stikine River watershed. Mount Edziza consists of several types of volcanic rocks and at least six geological formations that formed during six distinct stages of volcanic activity.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Basalt flows and smaller amounts of trachyte, tristanite, trachybasalt, benmoreite and mugearite produced during the second stage about 1 million years ago comprise Ice Peak, a glacially eroded stratovolcano forming the south peak of Mount Edziza. The third and fourth stages 0.9 million years ago created basalt ridges and the central trachyte stratovolcano of Mount Edziza, respectively.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Renewed volcanism could block local streams with lava flows, disrupt air traffic with volcanic ash and produce floods or lahars from melting glacial ice. Indigenous peoples have lived adjacent to Mount Edziza for thousands of years. It is a sacred mountain to the Tahltan people, who historically used volcanic glass from it to make tools and weaponry.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
It is a sacred mountain to the Tahltan people, who historically used volcanic glass from it to make tools and weaponry. Mineral exploration just southeast of Mount Edziza had commenced by the 1950s where gold, silver and other metals were discovered. This mineral exploration was conducted by several mining companies into the early 1990s.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
This mineral exploration was conducted by several mining companies into the early 1990s. Mount Edziza and the surrounding area were made into a large provincial park in the early 1970s to showcase the volcanic landscape. The mountain and provincial park can only be accessed by aircraft or by a network of horse trails from surrounding roads. Name and etymology.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Name and etymology. The mountain was labelled &quot;Edziza Peak&quot; on Geological Survey of Canada maps as early as 1926. This name for the mountain was adopted by the Geographical Names Board of Canada on September 24, 1945, as identified on the 1926 Geological Survey of Canada map sheet 309A.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Name and etymology. The mountain was labelled &quot;Edziza Peak&quot; on Geological Survey of Canada maps as early as 1926. This name for the mountain was adopted by the Geographical Names Board of Canada on September 24, 1945, as identified on the 1926 Geological Survey of Canada map sheet 309A.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The form of the name was also changed to reflect entrenched local usage and in conformation with Mount Edziza Provincial Park, which was established in 1972. To the local Tahltan people, Mount Edziza is called, which translates to. A number of explanations have been made regarding the origin of the name &quot;Edziza&quot;. A 1927 report by J.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
According to David Stevenson of University of Victoria's Anthropology Department, or is instead translated as in Tahltan. An explanation listed in the BC Parks brochure is that &quot;Edziza&quot; means in the Tahltan language. Another explanation proposed by Canadian volcanologist Jack Souther is that &quot;Edziza&quot; is a corruption of &quot;Edzerza&quot;, the name of a local Tahltan family.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Another explanation proposed by Canadian volcanologist Jack Souther is that &quot;Edziza&quot; is a corruption of &quot;Edzerza&quot;, the name of a local Tahltan family. Obsolete spellings of &quot;Edziza&quot; include &quot;Eddziza&quot;, &quot;Eddiza&quot;, &quot;Edidza&quot;, &quot;Edzia&quot; and &quot;Etseza&quot;. Location and climate.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
However, temperatures can drop below freezing during summer nights, making snow or freezing rain a possibility at any time of the year. The closest weather stations to Mount Edziza are located at Telegraph Creek and Dease Lake, which lie about to the northwest and to the northeast, respectively. Glaciation.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
At the head of Tennaya Creek on the eastern side of the ice cap is Tennaya Glacier. As a part of the Mount Edziza volcanic complex, Mount Edziza was covered by a regional ice sheet during the Pleistocene which receded and advanced periodically until about 11,000 years ago when deglaciation was essentially complete in a steadily warming climate.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Among these ridges are Idiji Ridge and Sorcery Ridge which are the namesakes of Idiji Glacier and Sorcery Creek. About south of the summit is Ice Peak, the south peak of Mount Edziza. This prominent pyramid-shaped horn has an elevation of and is the glacially eroded remains of an older stratovolcano whose northern flank is buried under the younger edifice of Mount Edziza.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Punch Cone on the western flank of Ice Peak protrudes through Mount Edziza's ice cap whereas Koosick Bluff and Ornostay Bluff, also on the western flank of Ice Peak, extend westward onto the surrounding Big Raven Plateau. The northeastern side of Mount Edziza contains The Pyramid, a pyramid-shaped lava dome in elevation.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Pillow Ridge on the northern side of Mount Edziza has an elevation of whereas Tsekone Ridge northwest of Mount Edziza has an elevation of. High on the western side of Mount Edziza is Triangle Dome, an elliptical lava dome in elevation. Glacier Dome reaches an elevation of on Mount Edziza's lower northeastern flank.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
High on the western side of Mount Edziza is Triangle Dome, an elliptical lava dome in elevation. Glacier Dome reaches an elevation of on Mount Edziza's lower northeastern flank. A circular lava dome on the southeastern crater rim of Mount Edziza called Nanook Dome has an elevation of. Sphinx Dome, in elevation, is a partially buried lava dome on the northeastern flank of Mount Edziza.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
A circular lava dome on the southeastern crater rim of Mount Edziza called Nanook Dome has an elevation of. Sphinx Dome, in elevation, is a partially buried lava dome on the northeastern flank of Mount Edziza. Remnants of a volcanic pile called Pharaoh Dome occur along the eastern flank of Mount Edziza. They lie at an elevation of between Tennaya Creek and Cartoona Ridge.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
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A saucer-shaped mound of lava called The Saucer is in elevation and has a diameter of about. The Desolation Lava Field on the northern flank of Mount Edziza contains at least 10 cinder cones, most of which are clustered near the northern trim line of Mount Edziza's ice cap. Sleet Cone and Storm Cone are rounded, mostly soil-covered, conical mounds that reach elevations of and, respectively.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Composition. A wide variety of volcanic rocks comprise Mount Edziza, the main mafic rock being basalt which comprises lava flows, cinder cones and ash beds on the flanks of the mountain. Basalt at Mount Edziza is in the form of alkali basalt and hawaiite; the latter is thought to be the product of partial fractional crystallization in subterranean magma chambers.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
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surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Ice Peak is the only location where mugearites and benmoreites are found in the Mount Edziza volcanic complex. Felsic volcanic rocks such as trachyte and rhyolite form the central stratovolcano of Mount Edziza, the upper part of Ice Peak and several lava domes and flows, as well as pyroclastic rocks. Stratigraphy.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
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Its upper surface is sparsely covered by trachyte of the Edziza Formation whereas the western edge of the ridge overlaps with a large flow of Edziza trachyte. Tsekone Ridge is an isolated volcanic pile adjacent to Pillow Ridge consisting of basaltic pillow lava and tuff breccia that has been cut by vertical north-trending feeder dikes.

Geographic entities mentioned:
surface_form: tsekone ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.77
lon: -130.69
Edziza Formation. The Edziza Formation consists mainly of trachyte that straddles the pantelleritic trachyte and comenditic trachyte boundary. It includes the central stratovolcano of Mount Edziza, as well as several satellitic features on its summit and flanks. Inside the summit crater of the stratovolcano is a succession of at least four lava lakes exposed in the breached eastern crater rim.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
They are represented by at least four cooling units, the lower two of which are about thick. The two upper cooling units reach thicknesses of about and may have originated from Nanook Dome, the largest of three lava domes consisting of Edziza Formation trachyte. Nanook Dome is about in diameter whose structure appears to be nearly identical to its original form.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Nanook Dome is about in diameter whose structure appears to be nearly identical to its original form. The other two Edziza Formation trachyte domes, Glacier Dome and Triangle Dome, are elliptical in structure and contain concentric flow layering. Potassium–argon dating of pantelleritic trachyte or comenditic trachyte from the Edziza Formation has yielded an age of 0.9 ± 0.3 million years.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Ash columns can drift for thousands of kilometres downwind and often become increasingly spread out over a larger area with increasing distance from an erupting vent. Mount Edziza lies under a major air route from Vancouver, British Columbia to Whitehorse, Yukon, suggesting the volcano poses a potential threat to air traffic.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Like other volcanoes in Canada, Mount Edziza 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
It may sense an increase in seismic activity if Mount Edziza 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 Edziza were to erupt, mechanisms exist to orchestrate relief efforts.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
This volcanic glass was used in the manufacturing of projectile points and cutting blades which were widely traded throughout the Pacific Northwest. Artifacts made of Edziza obsidian have been recovered from archaeological sites over an area of more than across Alaska, Alberta, Yukon and the British Columbia Coast, making it the most widely distributed obsidian in western North America.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
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Edzerza was buried on Mount Edziza, but his surname was erroneously spelled &quot;Edzertza&quot; on his grave marker. Williams Cone on the northeastern side of Mount Edziza was named in honour of Hank Williams whereas Eve Cone between Mount Edziza and Buckley Lake was named in honour of Johnny Edzerza's wife, Eve Brown Edzerza.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
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surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
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Protected areas. Mount Edziza and the surrounding area was designated as a provincial park in 1972 to showcase the volcanic landscape; a recreation area surrounding the park was also established in 1972. In 1989, Mount Edziza Provincial Park roughly doubled in size when was annexed from the Mount Edziza Recreation Area.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Mount Edziza and the surrounding area was designated as a provincial park in 1972 to showcase the volcanic landscape; a recreation area surrounding the park was also established in 1972. In 1989, Mount Edziza Provincial Park roughly doubled in size when was annexed from the Mount Edziza Recreation Area. With this annexation, the recreation area was greatly reduced in size to around.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
This remnant of the recreation area was east of Mount Edziza until 2003 when it was disestablished. Mount Edziza Provincial Park now covers an area of, making it one of the largest provincial parks in British Columbia. In 2021, an approximately conservation area called the Mount Edziza Conservancy was established east of Mount Edziza along the eastern border of Mount Edziza Provincial Park.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
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instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
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instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
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Accessibility. Mount Edziza lies in a remote location that is accessible only during summer and early autumn. There is no established road access to the mountain, although the Stewart–Cassiar Highway to the east and the Telegraph Creek Road to the northwest both come within of Mount Edziza. Extending from these roads are horse trails that provide access to the mountain.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
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It extends northwest and west along the Klastline River for much of its length. The trail enters Mount Edziza Provincial Park at about where Kakiddi Creek drains into the Klastline River. After entering Mount Edziza Provincial Park, the Klastline River Trail traverses northwest along the Klastline River for about and then crosses the river north of Mount Edziza.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
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instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Shaman Creek flows east and north into Kakiddi Lake from the southern flank of Mount Edziza. Tennaya Creek flows northeastward from the eastern side of Mount Edziza into Nuttlude Lake. All five streams are tributaries of Kakiddi Creek, a north-flowing tributary of the Klastline River which flows north into the Stikine River. Background.

Geographic entities mentioned:
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
However, it had an elevation of at least before its formerly cone-shaped summit was likely destroyed by a violent eruption in the geologic past; its current flat summit contains an ice-filled, crater. The mountain contains several lava domes, cinder cones and lava fields on its flanks, as well as an ice cap containing several outlet glaciers which extend to lower elevations.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Indigenous peoples have lived adjacent to Mount Edziza for thousands of years. It is a sacred mountain to the Tahltan people, who historically used volcanic glass from it to make tools and weaponry. Mineral exploration just southeast of Mount Edziza had commenced by the 1950s where gold, silver and other metals were discovered.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
This mineral exploration was conducted by several mining companies into the early 1990s. Mount Edziza and the surrounding area were made into a large provincial park in the early 1970s to showcase the volcanic landscape. The mountain and provincial park can only be accessed by aircraft or by a network of horse trails from surrounding roads. Name and etymology.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The eastern side of the ridge has been breached by active cirques where remnants of several lava lakes are exposed inside the crater. Formation of the summit crater was likely caused by a violent eruption at the zenith of the mountain's growth, although it may have also formed during the eruption of the Kakiddi Formation lava flows or the effusion of voluminous lava during dome construction.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Oswichee Creek. Oswichee Creek is a stream in the U.S. state of Georgia. It is a tributary to the Chattahoochee River. Oswichee was the name of a tribe of the indigenous peoples of the Southeastern Woodlands. A variant spelling is &quot;Oswitchee Creek&quot;.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Nesosap Lake. Nesosap Lake is a glacial lake on the Mistik Creek chain, approximately northeast of Bakers Narrows. As a segment of the Mistik Creek, it is part of the Nelson River watershed, in the Hudson Bay drainage basin in the Northern Region of Manitoba, Canada.

Geographic entities mentioned:
surface_form: Mistik Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.6256
lon: -101.568
surface_form: nesosap lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.806388888889
lon: -101.42138888889
Nesosap Lake is a glacial lake on the Mistik Creek chain, approximately northeast of Bakers Narrows. As a segment of the Mistik Creek, it is part of the Nelson River watershed, in the Hudson Bay drainage basin in the Northern Region of Manitoba, Canada. The surrounding mixed deciduous and coniferous forest is part of the Churchill River Upland portion of the Midwestern Canadian Shield forests.

Geographic entities mentioned:
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: mistik creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.6256
lon: -101.568
The region around the lake consists of rocky parallel ridges with poorly drained areas of muskeg and irregular stony shorelines due to intense glaciation. The lake is situated on the well known &quot;Mistik Creek Loop&quot;, a remote canoe route in length which can be paddled in four days. The lake contains northern pike, lake whitefish, cisco, walleye, and yellow perch.

Geographic entities mentioned:
surface_form: mistik creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.6256
lon: -101.568
The lake is situated on the well known &quot;Mistik Creek Loop&quot;, a remote canoe route in length which can be paddled in four days. The lake contains northern pike, lake whitefish, cisco, walleye, and yellow perch. &quot;Nesosap&quot; means 'twelve' in Cree, as all of the fourteen lakes on Mistik Creek are named in numeric order in Cree.

Geographic entities mentioned:
surface_form: mistik creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.6256
lon: -101.568
Nesosap Lake. Nesosap Lake is a glacial lake on the Mistik Creek chain, approximately northeast of Bakers Narrows. As a segment of the Mistik Creek, it is part of the Nelson River watershed, in the Hudson Bay drainage basin in the Northern Region of Manitoba, Canada.

Geographic entities mentioned:
surface_form: nesosap lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.806388888889
lon: -101.42138888889
Kim and Joan comb Los Angeles' clubs to look for attractive blondes and discover Cherie. They invite her to audition at a trailer park in the San Fernando Valley and to prepare a Suzi Quatro song to perform at her audition. Cherie learns Peggy Lee's &quot;Fever&quot; instead and goes to audition, but the band is disappointed at her choice.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Dolga Poljana. Dolga Poljana (,) is a village in the Vipava Valley east of Ajdovščina in the traditional Inner Carniola region of Slovenia. It is now generally regarded as part of the Slovenian Littoral. Stone arch bridge. A stone arch bridge over the Vipava River links Dolga Poljana to the village of Dolenje. The three-arch bridge was built in the 19th century.

Geographic entities mentioned:
surface_form: Vipava Valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 45.876147222222
lon: 13.907319444444
There have even been morphs with white spots on dark backgrounds. Striping abnormalities have been linked to inbreeding. Albino zebras have been recorded in the forests of Mount Kenya, with the dark stripes being blonde. The quagga had brown and white stripes on the head and neck, brown upper parts and a white belly, tail and legs. Range and habitat.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
They are water-dependent and live in more mesic environments than other African equids. They seldom wander from a water source. Zebras also live in elevations from sea level to on Mount Kenya. Depending on the population, zebra herds may be sedentary, being highly dense with small ranges, or migratory, being less populated with separate, extensive dry and wet home ranges.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
The potholes have been mentioned in several write-ups on the internet and are a popular subject for photographers. The unusual water flow, drainage from an outlet dam of Lacamas Lake, has carved many potholes in the rock underneath Lacamas Creek. These potholes range in size from approximately 3–10 feet wide and 3–13 feet deep.

Geographic entities mentioned:
surface_form: Lacamas Lake
instance_of: Lake
countries: United States
coordinates: lat: 45.6165669
lon: -122.4252954
Skriðuklaustur. Skriðuklaustur () is an old farmstead and a historic site in the valley of Fljótsdalur, Iceland. It contains the ruins of a 16th-century monastery, which were revealed by an archaeological excavation between 2002 and 2012. On site is the mansion of the famous Icelandic writer Gunnar Gunnarsson (1889–1975).

Geographic entities mentioned:
surface_form: Fljótsdalur
instance_of: Valley
countries: Iceland
coordinates: lat: 65.033333333333
lon: -15
Snæfellsstofa, one of the visitor centers for the Vatnajökull National Park is also at Skriðuklaustur. Nearby is the end of the tunnel that leads water from the Kárahnjúkastífla Dam to the power plant in Fljótsdalur (about 50 kilometers away) near Skriðuklaustur.

Geographic entities mentioned:
surface_form: Fljótsdalur
instance_of: Valley
countries: Iceland
coordinates: lat: 65.033333333333
lon: -15
He represented England at the World Mountain Running Trophy in Alaska in 2003 and in 2005, he placed second in the Skyrunner World Series. In 2015, Booth devised the “No Cure, Always Hope, Ultra Run” from the Newlands Valley based on the 10in10 challenge routes which were set up to raise money for research on multiple sclerosis, a disease with which Booth’s brother Duncan was diagnosed in 2010.

Geographic entities mentioned:
surface_form: Newlands Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.573011111111
lon: -3.1848694444444
Simone Moro. Simone Moro (born 27 October 1967 in Bergamo) is an Italian mountaineer known for having made first winter ascents of four of the fourteen eight-thousanders: Shishapangma in 2005, Makalu in 2009, Gasherbrum II in 2011, and Nanga Parbat in 2016. No other climber has made more first winter ascents of an eight-thousander in history.

Geographic entities mentioned:
surface_form: Shishapangma
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 28.352222222222
lon: 85.779722222222
surface_form: Makalu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.889166666667
lon: 87.088611111111
surface_form: Gasherbrum II
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.7575
lon: 76.652777777778
surface_form: Nanga Parbat
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.239166666667
lon: 74.59
No other climber has made more first winter ascents of an eight-thousander in history. He has summited Everest four times, in 2000, 2002, 2006, and 2010. Moro is also an experienced helicopter pilot. In 2013, he and two other rescue experts carried out the world's highest long-line rescue operation on a helicopter, on Lhotse, at 7800m.

Geographic entities mentioned:
surface_form: Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
His father was a cyclist and also fostered a lively and international environment around him. He started climbing on the Presolana and other massifs of the Bergamasque Alps at the age of 13. In 2003, at 35, he completed his university studies and graduated &quot;cum laude&quot;. Climbing career. Moro began his climbing activity on the Grigne near his home city.

Geographic entities mentioned:
surface_form: Presolana
instance_of: Mountain
countries: Italy
coordinates: lat: 45.9
lon: 10.016666666667
Climbing career. Moro began his climbing activity on the Grigne near his home city. His father was his first mentor, and later Alberto Cosonni and Bruno Tassi. At that time he was primarily involved in rock climbing, an activity he has never given up. In 1992 he participated in his first Himalayan expedition, to Mount Everest. One year later Moro climbed Aconcagua in winter.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
At that time he was primarily involved in rock climbing, an activity he has never given up. In 1992 he participated in his first Himalayan expedition, to Mount Everest. One year later Moro climbed Aconcagua in winter. He made expeditions to other mountains in the 1990s, including Cerro Mirador in winter and Makalu in 1993; Shishapangma and Lhotse in 1994, Kangchenjunga in 1995.

Geographic entities mentioned:
surface_form: Aconcagua
instance_of: Mountain
countries: Argentina
coordinates: lat: -32.653055555555554
lon: -70.01166666666667
One year later Moro climbed Aconcagua in winter. He made expeditions to other mountains in the 1990s, including Cerro Mirador in winter and Makalu in 1993; Shishapangma and Lhotse in 1994, Kangchenjunga in 1995. In 1996 Moro climbed the west wall of Fitz Roy (in Patagonia) in 25 hours from the base to the summit and back to the base.

Geographic entities mentioned:
surface_form: Makalu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.889166666667
lon: 87.088611111111
surface_form: Shishapangma
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 28.352222222222
lon: 85.779722222222
surface_form: Lhotse
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.961666666667
lon: 86.933333333333
surface_form: Kangchenjunga
instance_of: Mountain
countries: India
Nepal
coordinates: lat: 27.7
lon: 88.133333
He made expeditions to other mountains in the 1990s, including Cerro Mirador in winter and Makalu in 1993; Shishapangma and Lhotse in 1994, Kangchenjunga in 1995. In 1996 Moro climbed the west wall of Fitz Roy (in Patagonia) in 25 hours from the base to the summit and back to the base. In the same year, he climbed Shishapangma South () without oxygen in 27 hours using skis in the descent from.

Geographic entities mentioned:
surface_form: Fitz Roy
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -49.271388888889
lon: -73.043333333333
In the same year, he climbed Shishapangma South () without oxygen in 27 hours using skis in the descent from. In 1997 he summited Lhotse. In Winter of 1997 he attempted the South face of Annapurna. During this attempt, his climbing companions Anatoli Boukreev and Dimitri Sobolev died in an avalanche.

Geographic entities mentioned:
surface_form: Annapurna
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.5958
lon: 83.82
During this attempt, his climbing companions Anatoli Boukreev and Dimitri Sobolev died in an avalanche. He tried Everest again in 1998; summited four peaks Pik Lenin (), Peak Korzhenevskaya (), Ismoil Somoni Peak (, formerly known as Pik Kommunizma), Pik Khan Tengri () with young Kazakhstan guide Denis Urubko; then summited Everest with him in 2000 and Marble Wall in winter 2001.

Geographic entities mentioned:
surface_form: Ismoil Somoni Peak
instance_of: Mountain
countries: Tajikistan
coordinates: lat: 38.942732
lon: 72.015347
surface_form: Khan Tengri
instance_of: Mountain
countries: Kyrgyzstan
Kazakhstan
People's Republic of China
Russian Empire
Soviet Union
coordinates: lat: 42.210833333333
lon: 80.175
In 2002 he summited three peaks: Mount Vinson, Cho Oyu and Everest; summited three peaks: Broad Peak, Elbrus and Kilimanjaro in 2003, summited Baruntse along a new route and tried Shishapangma and Annapurna in 2004; Batura and Batokshi peaks in 2005, Broad Peak in winter 2006 and 2007. In 2005 he achieved the first winter summit of Shishapangma, with Piotr Morawski.

Geographic entities mentioned:
surface_form: Cho Oyu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 28.094166666667
lon: 86.660833333333
surface_form: Broad Peak
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.810555555556
lon: 76.568055555556
surface_form: Baruntse
instance_of: Mountain
countries: Nepal
coordinates: lat: 27.883333333333
lon: 86.983333333333
surface_form: Broad Peak
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.810555555556
lon: 76.568055555556
In 2008 he made (with Hervè Barmasse) the first ascent of Beka Brakai Chhok (Karakorum). The climbing was in pure alpine style and in 43 hours. In January 2009 Moro made the first winter ascent of Makalu with Denis Urubko, and in February 2011 the first winter ascent of Gasherbrum II with Denis Urubko and Cory Richards.

Geographic entities mentioned:
surface_form: Makalu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.889166666667
lon: 87.088611111111
surface_form: Gasherbrum II
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.7575
lon: 76.652777777778
went viral and Steck, wholly blameless in the affair, became severely depressed and disheartened&quot;. In February 2016, Moro completed the first winter ascent of Nanga Parbat with Alex Txikon and Ali Sadpara. In February 2018, he completed the first winter ascent of Peak Pobeda, Sakha along with fellow Italian mountaineer Tamara Lunger. Rescue missions.

Geographic entities mentioned:
surface_form: Nanga Parbat
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.239166666667
lon: 74.59
The subdistrict is located on the north side of Hat Yai, on the west bank of the Khlong U-Tapao River. As of 2012, the subdistrict has a population of 2,268. The village itself is even older than Hat Yai, as it used to be the gateway for upstream migration from the Songkhla Lake and the ocean in ancient times.

Geographic entities mentioned:
surface_form: Songkhla Lake
instance_of: Lake
countries: Thailand
coordinates: lat: 7.2
lon: 100.46666666667
In 1780, it became the seat of Kadnikovsky Uyezd of Vologda Viceroyalty (since 1796—Vologda Governorate) and was granted town status. The uyezd, one of the ten in the governorate, comprised vast areas in the central part of modern Vologda Oblast east and northeast of Lake Kubenskoye, as well as the south of modern Arkhangelsk Oblast.

Geographic entities mentioned:
surface_form: Lake Kubenskoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 59.640277777778
lon: 39.446944444444
590) on May 22, 1957. History. On September 5, 1876, Charles Crocker, President of the Southern Pacific Company, hammered a golden spike into a railroad tie at this spot. The golden spike was a ceremonial spike that was driven in to celebrate the completion of San Joaquin Valley rail line. The completion of the line connected Los Angeles with San Francisco and First transcontinental railroad line.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Henry Newhall later formed the city of Newhall. Newhall purchased part of Rancho San Francisco in 1875 to form the new city. In 1887 the Southern Pacific started to expand and built a line though the Santa Clarita Valley to Ventura. Along the new line, a new town was built called Saugus, the town was named after Saugus, Massachusetts, were Newhall was born.

Geographic entities mentioned:
surface_form: Santa Clarita Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.398
lon: -118.522
The lake belongs to the Kerch group of lakes, and is the sixth largest lake in Crimea. Koyashskoye Salt Lake is located to the east, and the coast of the Black Sea is to the south. Mar'ivka is the closest village to the east.

Geographic entities mentioned:
surface_form: Koyashskoye Salt Lake
instance_of: Lake
countries: Ukraine
Russia
Russian Empire
Soviet Union
coordinates: lat: 45.045
lon: 36.1875
Uzunlarske Lake. Uzunlarske Lake (Russian: Узунла́рское о́зеро, Ukrainian: Узунларське озеро, Crimean Tatar: Uzunlar gölü) is a salt lake in the south of the Kerch Peninsula in the Lenine Raion district of Crimea. The lake belongs to the Kerch group of lakes, and is the sixth largest lake in Crimea. Koyashskoye Salt Lake is located to the east, and the coast of the Black Sea is to the south.

Geographic entities mentioned:
surface_form: uzunlarske lake
instance_of: Lake
countries: Ukraine
Russia
coordinates: lat: 45.0725
lon: 36.1