Sarmila/GeoWiki-Features huggingface dataset:
Although no historical eruptions are known at Hoodoo Mountain, there have been periods of seismic activity since at least the mid-1980s, indicating possible future eruptions and volcanic hazards. Hoodoo Mountain lies in a remote area of Cassiar Land District that has undergone mineral exploration since at least the early 1900s.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
This exploration led to the discovery of copper, silver and gold within the Iskut River floodplain where two underground mines operated between 1988 and 1999. Geological studies have been conducted at Hoodoo Mountain since at least the 1940s; the most detailed studies occurred in the 1990s and 2000s. The area has a mostly cool and wet climate with heavy precipitation.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
The area has a mostly cool and wet climate with heavy precipitation. As a result, a limited number of mammals live around Hoodoo Mountain. Trees of the pine and willow families form forests in the regional river valleys and on the lower slopes of the volcano. They compose one of many ecoregions that occur throughout British Columbia.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
Trees of the pine and willow families form forests in the regional river valleys and on the lower slopes of the volcano. They compose one of many ecoregions that occur throughout British Columbia. Due to its remoteness, Hoodoo Mountain can only be accessed by air, by water or by trekking great distances on foot. The closest communities are more than away from the mountain. Biogeography.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
Trees of the pine and willow families form forests in the regional river valleys and on the lower slopes of the volcano. They compose one of many ecoregions that occur throughout British Columbia. Due to its remoteness, Hoodoo Mountain can only be accessed by air, by water or by trekking great distances on foot. The closest communities are more than away from the mountain. Biogeography.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Biogeography. Hoodoo Mountain lies within the Boundary Ranges Ecoregion, a mountainous region of the Coast Mountains in southeastern Alaska and northwestern British Columbia characterized by rugged, largely ice-capped mountains of granitic and metamorphic rocks. Mountain hemlock, western hemlock and Sitka spruce form forests on valley bottoms and lower valley slopes.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Several large river valleys with wide braided channels penetrate the Boundary Ranges Ecoregion; black cottonwood occur on their floodplains. A limited number of mammal species thrive in this ecoregion, such as hoary marmots and mountain goats, which inhabit the alpine tundra zone.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The Boundary Ranges Ecoregion is part of the Coast and Mountains Ecoprovince which forms part of the Humid Maritime and Highlands Ecodivision. The Boundary Ranges Ecoregion is subdivided into three ecosections, the Southern Boundary Ranges Ecosection being the main ecosection at Hoodoo Mountain.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
The only settlements in the Southern Boundary Ranges Ecosection are Kincolith, Stewart and Hyder, the latter two of which are connected by the Stewart Highway. There is no human population within of Hoodoo Mountain, but 2,330 people live within. Forests of this ecosection grow on the lower slopes of Hoodoo Mountain except for its northeastern flank where rock and ice are dominant.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
There is no human population within of Hoodoo Mountain, but 2,330 people live within. Forests of this ecosection grow on the lower slopes of Hoodoo Mountain except for its northeastern flank where rock and ice are dominant. Much of this forest cover lies at elevations below. Climate.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
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Climate. Hoodoo Mountain has a maritime glacial climate that is intermediate between fully coastal maritime and continental climates. Moist air from the Pacific Ocean brings intense precipitation over the region while simultaneously allowing cold Arctic air to pass down through the Portland Canal into the Dixon Entrance where it flows into British Columbia's North Coast.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
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The annual average temperature is. Glaciers. Two valley glaciers wrap partially around the base of Hoodoo Mountain, both of which are actively retreating. Hoodoo Glacier surrounding its northwestern base is the source of the Hoodoo River which flows south into the Iskut River. It has lost about of its total thickness over the last 700 years and its terminus has retreated at least since the 1920s.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
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At the terminus of Hoodoo Glacier is a roughly long and wide lake which may occupy a previously drained depression. The western side of the glacier contains a small possibly drained ice-marginal lake. Twin Glacier surrounds the northwestern base of Hoodoo Mountain and is the largest of the two valley glaciers. It is the source of the Twin River which also flows south into the Iskut River.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
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surface_form: twin
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.72361111
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A small moraine-dammed lake lies along the southwestern margin of Twin Glacier. Hoodoo Glacier and Twin Glacier are separated by a ridgeline extending north of Hoodoo Mountain. They have cut deep valleys into the older regional bedrock and have interacted with Hoodoo Mountain intermittently since the Pleistocene.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
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surface_form: twin
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countries: Canada
coordinates: lat: 56.72361111
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Hoodoo Glacier and Twin Glacier are separated by a ridgeline extending north of Hoodoo Mountain. They have cut deep valleys into the older regional bedrock and have interacted with Hoodoo Mountain intermittently since the Pleistocene. Both glaciers originate from the Andrei Icefield centered northeast of Hoodoo Mountain.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
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This large glacial field is informally named after the son of Olav Mokievsky-Zubok, a glaciologist who carried out significant glaciological work in the Coast Mountains from the 1960s to the 1970s. The summit of Hoodoo Mountain contains an ice cap that persists at elevations greater than. It varies from thick and has a diameter of, attaining a minimum volume of.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
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The cause of volcanic activity in the Northern Cordilleran Volcanic Province is thought to be due to rifting of the North American Cordillera driven by changes in relative plate motion between the North American and Pacific plates. Hoodoo Mountain is part of a subdivision of the NCVP called the Stikine Subprovince.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
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Structure. Hoodoo Mountain is one of the largest peralkaline volcanoes in the NCVP. It is a stratovolcano composed primarily of peralkaline phonolite and trachyte lava flows and hyaloclastites, although some pyroclastic rocks are also present. Its peralkalinity is unique among other volcanoes in the Iskut volcanic field, which range in composition from alkali basalt to hawaiite.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
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Its peralkalinity is unique among other volcanoes in the Iskut volcanic field, which range in composition from alkali basalt to hawaiite. Hoodoo Mountain has also been designated as a subglacial volcano due to much of the mountain having formed subglacially in the last 85,000 years.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
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This includes the formation of ice-marginal lava flows and the interlayering of glacial till with volcanic deposits. Hoodoo Mountain's constant struggle with surrounding and overlying ice is attested by its nearly flat summit, which attains an elevation of. Lava flows from Hoodoo Mountain partially bury Little Bear Mountain, a much smaller and older basaltic volcano immediately to the north.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
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Hoodoo Mountain's constant struggle with surrounding and overlying ice is attested by its nearly flat summit, which attains an elevation of. Lava flows from Hoodoo Mountain partially bury Little Bear Mountain, a much smaller and older basaltic volcano immediately to the north. Both volcanoes are underlain by plutonic rocks and metamorphosed volcanic and sedimentary rocks of Stikinia.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
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countries: Canada
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surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
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surface_form: bear
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.2833
lon: -126.967
surface_form: little bear mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.8
lon: -131.3
This is because it has a different lithological and topographical structure than most glaciated mountains in the Canadian Cordillera. In contrast to its rugged counterparts, Hoodoo Mountain is symmetrical and circular in form. It has a basal diameter of around, a volume of and a topographic prominence of, making it the smallest of the four volcanoes composing the Stikine Subprovince.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
It has a basal diameter of around, a volume of and a topographic prominence of, making it the smallest of the four volcanoes composing the Stikine Subprovince. Hoodoos, pillar-like rock formations after which the volcano is named, are as much as in height and give the mountain a unique appearance. In 1919, a landslide removed lava rock from a wide section on the western side of Hoodoo Mountain.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Hoodoos, pillar-like rock formations after which the volcano is named, are as much as in height and give the mountain a unique appearance. In 1919, a landslide removed lava rock from a wide section on the western side of Hoodoo Mountain. Two sets of prominent cliffs partially circumscribe Hoodoo Mountain, which give the volcano a discontinuous, step-like topographic profile.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
In 1919, a landslide removed lava rock from a wide section on the western side of Hoodoo Mountain. Two sets of prominent cliffs partially circumscribe Hoodoo Mountain, which give the volcano a discontinuous, step-like topographic profile. The lower set of cliffs delimit the base of the volcano except for its southeastern margin where they have been partially overrun by younger lava flows.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
The upper set of cliffs surround the summit and are between high. Both sets of cliffs formed as a result of lava erupting in a glaciated environment. As lava travelled down slope, the lava came into contact with glacial ice that completely surrounded Hoodoo Mountain and cooled very quickly, forming a barrier around the entire volcano.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
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The lava cooled, pooled and as the glacial ice receded, it left behind massive lava cliffs. Subfeatures. The south–central side of Hoodoo Mountain contains a large depression called Long Valley. This feature, having formed by glacial erosion, contains a series of domes with adjacent lava spines.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
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This feature, having formed by glacial erosion, contains a series of domes with adjacent lava spines. Pointer Ridge on the north–central side of Hoodoo Mountain consists of pyroclastic rocks that form a thick stratigraphic unit. The Wall, a more than high cliff at the western base of Hoodoo Mountain, forms the front of an ice-marginal lava flow that displays columnar jointing.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
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Pointer Ridge on the north–central side of Hoodoo Mountain consists of pyroclastic rocks that form a thick stratigraphic unit. The Wall, a more than high cliff at the western base of Hoodoo Mountain, forms the front of an ice-marginal lava flow that displays columnar jointing. The Monument on the southwestern side of Hoodoo Mountain is a vertical rock column that reaches more than in height.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
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countries: Canada
coordinates: lat: 56.772222222222
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The Wall, a more than high cliff at the western base of Hoodoo Mountain, forms the front of an ice-marginal lava flow that displays columnar jointing. The Monument on the southwestern side of Hoodoo Mountain is a vertical rock column that reaches more than in height. It is the eroded remains of a volcanic vent that was fed by a west-trending dike.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
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countries: Canada
coordinates: lat: 56.772222222222
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It is the eroded remains of a volcanic vent that was fed by a west-trending dike. Horn Ridge, a high ridge on the north side of Hoodoo Mountain, consists of highly vesicular lava flows that are locally heavily jointed. The northeastern side of Hoodoo Mountain contains a J-shaped cliff called The Hook. Like The Wall to the southwest, The Hook is the front of an ice-marginal lava flow.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
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countries: Canada
coordinates: lat: 56.772222222222
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The northeastern side of Hoodoo Mountain contains a J-shaped cliff called The Hook. Like The Wall to the southwest, The Hook is the front of an ice-marginal lava flow. Slide Canyon consists of a large chasm that cuts deeply into the southwestern side of Hoodoo Mountain. It is intruded by several dikes, including the one that fed The Monument.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
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It is intruded by several dikes, including the one that fed The Monument. Pumice Point on the northwestern side of Hoodoo Mountain contains highly vesicular, lapilli to block-sized fragments of &quot;woody pumice&quot; up to long. Extending from the northwestern side of Hoodoo Mountain is the Northwest Flow, a lava flow with well-preserved levees.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
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Pumice Point on the northwestern side of Hoodoo Mountain contains highly vesicular, lapilli to block-sized fragments of &quot;woody pumice&quot; up to long. Extending from the northwestern side of Hoodoo Mountain is the Northwest Flow, a lava flow with well-preserved levees. Lava channels up to wide occur throughout the flow.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
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Subaerial eruptions from near the summit took place during the second eruptive period 80,000 years ago. Lava travelled down slope from an elevation of roughly, but was then confined by thick glacial ice at an elevation of about. Here, the lava cooled and pooled to create the lower discontinuous set of cliffs around the entire base of Hoodoo Mountain.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
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countries: Canada
coordinates: lat: 56.772222222222
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Here, the lava cooled and pooled to create the lower discontinuous set of cliffs around the entire base of Hoodoo Mountain. These ice-marginal lava flows vary from about to more than thick and often contain horizontally oriented columnar joints, indicative of a vertical cooling surface. The Wall at the western base of Hoodoo Mountain formed during this eruptive period.

Geographic entities mentioned:
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countries: Canada
coordinates: lat: 51.4677778
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Volcanic glass of phonolitic or trachytic composition occurs within the sequence. A thick subaerial lava flow travelled down the north–central and northeast flanks of Hoodoo Mountain during the latter stages of this eruptive period. It directly overlies the pyroclastic sequence and contains abundant fresh and devitrified glass.

Geographic entities mentioned:
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coordinates: lat: 51.4677778
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Individual flows vary from thick and are separated by of lava breccia, giving the sequence a total thickness of around. The lava flows do not appear to have interacted with glacial ice, suggesting at least the upper flanks of Hoodoo Mountain were ice-free at the time of their eruption. Columnar joints more than thick characterize these flows.

Geographic entities mentioned:
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The second stage between 40,000–30,000 years ago was characterized by fissure-fed eruptions beneath relatively thin ice cover. These eruptions produced a roughly thick unit of lava flows, lava lobes and breccia on the north–central, northwestern and western flanks of Hoodoo Mountain.

Geographic entities mentioned:
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The sixth and final eruptive period began 10,000–9,000 years ago with the eruption of thick phonolitic lava flows from vents near the summit. They travelled down the north–central, northwestern, southeastern and southwestern flanks of Hoodoo Mountain without encountering any glacial ice, suggesting the flows were erupted subaerially after the regional ice had disappeared from lower elevations.

Geographic entities mentioned:
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Lava flows on the north–central flank display radially-oriented cooling joints. The Northwest Flow travelled about down slope and partially covers cliffs at the base of Hoodoo Mountain. Lava flows on the southeastern flank drape down high cliffs and extend into the Twin Glacier valley where they spread out into a broad terminal lobe.

Geographic entities mentioned:
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Radiocarbon dating of terrestrial plant macrofossils directly overlying the youngest tephra layer suggest an early Holocene age for this volcanic material. The glass composition of the tephras is similar to the average whole-rock chemistry of the phonolitic lava flows produced during the final eruptive period at Hoodoo Mountain.

Geographic entities mentioned:
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countries: Canada
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Therefore other possible sources have been considered, including Level Mountain, Heart Peaks and the Mount Edziza volcanic complex. A thick trachytic tephra layer of unknown origin occurs in sediments at Bob Quinn Lake northeast of Hoodoo Mountain. The areal distribution of this tephra is poorly constrained, but it may extend further to the east.

Geographic entities mentioned:
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countries: Canada
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The exact age of this tephra layer is unknown, but its stratigraphic position suggests it is about 7,000–8,000 calendar years old. No volcanic deposits of this age are known at Hoodoo Mountain, but there may be younger deposits that are completely covered by the summit ice cap. Hazards and monitoring.

Geographic entities mentioned:
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Air traffic between Canada, Alaska and Asia would likely be disrupted by high eruption columns due to the presence of major airways near the volcano. Like other volcanoes in the NCVP, Hoodoo Mountain is not monitored closely enough by the GSC to ascertain its activity level.

Geographic entities mentioned:
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Like other volcanoes in the NCVP, Hoodoo Mountain is not monitored closely enough by the GSC 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:
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countries: Canada
coordinates: lat: 51.4677778
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It may sense an increase in seismic activity if Hoodoo Mountain 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 Hoodoo Mountain were to erupt, mechanisms exist to orchestrate relief efforts.

Geographic entities mentioned:
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instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
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countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
The Interagency Volcanic Event Notification Plan was created to outline the notification procedure of some of the main agencies that would respond to an erupting volcano in Canada, an eruption close to the Canada–United States border or any eruption that would affect Canada. Geological studies. The volcanic deposits at Hoodoo Mountain were briefly described in 1948 by F. A.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
In 1991, Canadian volcanologist Jack Souther provided a short account of the geomorphology of Hoodoo Mountain as well as some age-constraints from preliminary K–Ar dating. Hoodoo Mountain's relatively flat-topped geomorphology led Souther to refer to it as a tuya, even though its summit lacks a capping sequence of subaerial lavas typical of tuyas.

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
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
It does, however, coincide with Souther's original use of the term &quot;tuya&quot; in that its overall geomorphology has been strongly influenced by interaction between ice and lava. The first detailed summary of the Quaternary stratigraphy and petrology of Hoodoo Mountain was compiled in 1997 by American geologist Ben Edwards who produced a detailed geological map of the volcano.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
The first detailed summary of the Quaternary stratigraphy and petrology of Hoodoo Mountain was compiled in 1997 by American geologist Ben Edwards who produced a detailed geological map of the volcano. An expedition consisting of university, GSC and industry scientists was organized in 1997 to assess the nature and magnitude of hazards posed by Hoodoo Mountain.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
Personnel involved in the 1997 expedition were Catherine Hickson and Mark Stasiuk of the GSC, Jim Nicholls of the University of Calgary, Jeff Schmok and Guy Cross of Golder Associates, Alison Rust, Ben Edwards and Kelly Russell of the University of British Columbia, and Trevor Page of Lancaster University. By 2002, Hoodoo Mountain was no longer the least studied volcano of the Stikine Subprovince.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
A total of 196,358 tonnes of ore was mined from 1988 to 1993, from which of copper, of silver and of gold was recovered. Intermittent mineral exploration has taken place at the Johnny Mountain Mine since its closure in 1993. In 1982, Cominco staked two mining claims over their Red Bluff property and adjacent ground near the junction of the Craig and Iskut rivers.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Accessibility. Hoodoo Mountain is in a remote location with no established road access. The closest point accessible by road is Bob Quinn Lake about northeast of Hoodoo Mountain along the Stewart–Cassiar Highway. From there the mountain can be reached by charter helicopter or by trekking across mountainous terrain with extreme difficulty.

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
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
From there the mountain can be reached by charter helicopter or by trekking across mountainous terrain with extreme difficulty. Alternatively, fixed-wing aircraft landings can be made on the Bronson Creek runway immediately south of Hoodoo Mountain. The mountain can also be approached from the Alaskan community of Wrangell by boating up the Stikine and Iskut rivers.

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
surface_form: hoodoo mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
Structure. Hoodoo Mountain is one of the largest peralkaline volcanoes in the NCVP. It is a stratovolcano composed primarily of peralkaline phonolite and trachyte lava flows and hyaloclastites, although some pyroclastic rocks are also present. Its peralkalinity is unique among other volcanoes in the Iskut volcanic field, which range in composition from alkali basalt to hawaiite.

Geographic entities mentioned:
surface_form: iskut volcanic field
instance_of: Mountain
countries: Canada
coordinates: lat: 56.5833
lon: -130.55
The Boundary Ranges Ecoregion is subdivided into three ecosections, the Southern Boundary Ranges Ecosection being the main ecosection at Hoodoo Mountain. This ecosection is cut by several streams, including the Salmon, Bear and Unuk rivers, which drain directly into marine channels or sounds.

Geographic entities mentioned:
surface_form: bear
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.2833
lon: -126.967
The Wall at the western base of Hoodoo Mountain formed during this eruptive period. Subsequent glacial movements over these flows created north–south trending striations that are consistent with current movements of the Hoodoo and Twin glaciers. Both of these valley glaciers are now roughly below the striations due to their ongoing glacial retreat.

Geographic entities mentioned:
surface_form: twin
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.72361111
lon: -131.21166667
The Northwest Flow travelled about down slope and partially covers cliffs at the base of Hoodoo Mountain. Lava flows on the southeastern flank drape down high cliffs and extend into the Twin Glacier valley where they spread out into a broad terminal lobe. The Southwest Flow travelled about down slope to near the Hoodoo River.

Geographic entities mentioned:
surface_form: twin
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.72361111
lon: -131.21166667
On 10 November 2018, Rao replaced Ganapathy as the new General Secretary of CPI (Maoist). 2010-2012. Rao was suspected of being behind almost all the major Maoist attacks that took place in Chhattisgarh, Maharashtra and Odisha while he was alive. According to police sources the killing of a Telugu Desam Party leader Kidari Saraveshwar Rao at Araku in Andhra Pradesh is attributed to him.

Geographic entities mentioned:
surface_form: Araku
instance_of: Valley
countries: India
coordinates: lat: 18.3333
lon: 82.8667
It is commonly accepted to have started with the historical book, &quot;Istoriya Slavyanobolgarskaya&quot;, written in 1762 by Paisius, a Bulgarian monk of the Hilandar monastery at Mount Athos, leading to the National awakening of Bulgaria and the modern Bulgarian nationalism, and lasting until the Liberation of Bulgaria in 1878 as a result of the Russo-Turkish War of 1877–1878. Characteristics.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Texas Valley. qkdaxdx7u77kccge4um48fzm8sa8" xml:space="preserve">Texas Valley is the name of two valleys in Floyd County, in the U.S. state of Georgia. The twin valleys are more precisely called Big Texas Valley and Little Texas Valley. There are two stories on the origin of the name Texas Valley; both involve pioneers who were passing through on their way to Texas.

Geographic entities mentioned:
surface_form: texas valley
instance_of: Valley
countries: United States
coordinates: lat: 34.39879166666667
lon: -85.20853611111112
Texas Valley. qkdaxdx7u77kccge4um48fzm8sa8" xml:space="preserve">Texas Valley is the name of two valleys in Floyd County, in the U.S. state of Georgia. The twin valleys are more precisely called Big Texas Valley and Little Texas Valley. There are two stories on the origin of the name Texas Valley; both involve pioneers who were passing through on their way to Texas.

Geographic entities mentioned:
surface_form: texas valley
instance_of: Valley
countries: United States
coordinates: lat: 34.39879166666667
lon: -85.20853611111112
surface_form: texas valley
instance_of: Valley
countries: United States
coordinates: lat: 34.39879166666667
lon: -85.20853611111112
Maris Nunatak. 1bipqoxjq7ydtcsdh54eg3a7tqeb" xml:space="preserve">Maris Nunatak () is a small coastal nunatak in Antarctica, east-northeast of Whisnant Nunatak at the junction of Rogers Glacier and the east side of the Amery Ice Shelf. It was delineated in 1952 by John H. Roscoe from air photos taken by U.S. Navy Operation Highjump (1946–47), and named by him for R.L.

Geographic entities mentioned:
surface_form: Whisnant Nunatak
instance_of: Mountain
coordinates: lat: -69.9833
lon: 73.0833
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: maris nunatak
instance_of: Mountain
coordinates: lat: -69.9833
lon: 73.15
Maris Nunatak. 1bipqoxjq7ydtcsdh54eg3a7tqeb" xml:space="preserve">Maris Nunatak () is a small coastal nunatak in Antarctica, east-northeast of Whisnant Nunatak at the junction of Rogers Glacier and the east side of the Amery Ice Shelf. It was delineated in 1952 by John H. Roscoe from air photos taken by U.S. Navy Operation Highjump (1946–47), and named by him for R.L.

Geographic entities mentioned:
surface_form: maris nunatak
instance_of: Mountain
coordinates: lat: -69.9833
lon: 73.15
Sharbakty District. Geography. Lakes Seiten, Bura and the eastern part of lake Maraldy are located in the district.

Geographic entities mentioned:
surface_form: Seiten
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 51.93944
lon: 78.12139
Although best known for his enthusiastic promotion of astronomy in New Zealand, including the establishment of the observatory in his name, he was also a respected explorer. Charles Gifford was one of the early photographic documenters of much of the back country within New Zealand's South Island. In 1939, Mount Gifford on South Island was named in his honour.

Geographic entities mentioned:
surface_form: Mount Gifford
instance_of: Mountain
countries: New Zealand
coordinates: lat: -44.726
lon: 168.075
The population was 1,450 as of 2010. There are 19 streets. Geography. Turka is located on the eastern shore of Lake Baikal, by the mouth of the Turka River, north of Lake Kotokel and north of Turuntayevo (the district's administrative centre) by road. Goryachinsk is the nearest rural locality.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
After five months of interrogation and torture, on the day before his trial, Bineth committed suicide in his prison cell (his wife and child were in Europe). He realized that there was no way out for him and wanted to avoid public hanging, which was the fate awaiting him after conviction. His body was re-interred in the Mount Herzl military cemetery in Jerusalem in 1959.

Geographic entities mentioned:
surface_form: Mount Herzl
instance_of: Mountain
countries: Israel
coordinates: lat: 31.774117
lon: 35.180567
Geography. The Levels occupy an area of about, bisected by the Polden Hills; the areas to the south are drained by the River Parrett, and the areas to the north by the rivers Axe and Brue. The Somerset Levels consist of marine clay &quot;levels&quot; along the coast, and inland (often peat-based) &quot;moors&quot;; agriculturally, about 70 percent is used as grassland and the rest is arable.

Geographic entities mentioned:
surface_form: River Parrett
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.2292
lon: -3.00861
On 11 February David Cameron, who had visited the area the previous day, ordered that the political bickering in government should end. Future plans. (The plans for the dredging of the Rivers Parrett and Tone had already been announced.) It also proposed improvements to the artificial Sowy River which carries excess water from the River Parrett to the King's Sedgemoor Drain.

Geographic entities mentioned:
surface_form: River Parrett
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.2292
lon: -3.00861
The crater is one of the few places in American Samoa where evidence of the more recent episodes of volcanism can be observed. The eruptions at Aunuu occurred at approximately the same time as the volcanism at Leʻala Shoreline in Taputimu, while the eruptions that formed Rainmaker Mountain, Matafao Peak, and the ridges of Vaiava Strait are much older.

Geographic entities mentioned:
surface_form: Rainmaker Mountain
instance_of: Mountain
countries: United States
coordinates: lat: -14.276388888889
lon: -170.65277777778
surface_form: Matafao Peak
instance_of: Mountain
countries: United States
coordinates: lat: -14.29972
lon: -170.7025
Balkunje. Balkunje is a panchayat town located at Mangalore taluk in Dakshina Kannada district in the Indian state of Karnataka. It is on the banks of Shambhavi River. It is next to the small village of Kavathar, Karnire. Its nearest town is Palimar in Udupi District. Geography. It has an average elevation of 24 metres.

Geographic entities mentioned:
surface_form: Shambhavi River
instance_of: Watercourse
countries: India
coordinates: lat: 13.0721
lon: 74.7774
In the text, Paul stands on the &quot;mountain of Jericho,&quot; which does not exist. Jean-Marc Rosenstiehl hypothesizes that it is Mount Nebo (near the city of Jericho), based on an unrelated Egyptian apocryphon that also makes reference to a &quot;mountain of Jericho.&quot; Michael Kaler considers Rosenstiehl's idea extremely speculative.

Geographic entities mentioned:
surface_form: Mount Nebo
instance_of: Mountain
countries: Jordan
coordinates: lat: 31.767777777778
lon: 35.725555555556
These valleys often filled with water, created a connection with the sea and formed the present-day straits and fjords of the Faroe Islands. The largest lake in the Faroe Islands, Sørvágsvatn, almost became a fjord, but remained 32 meters above sea level. East coast and inland.

Geographic entities mentioned:
surface_form: Sørvágsvatn
instance_of: Lake
countries: Faroe Islands
coordinates: lat: 62.05
lon: -7.2333333333333
They are often table mountains. The highest mountain in the archipelago, Slættaratindur (880 meters), takes its name from this fact (flat summit). To the north it slopes relatively gently (not vertically) into the Atlantic Ocean and is thus considered the highest of its kind in Europe sloping directly out of the sea.

Geographic entities mentioned:
surface_form: Slættaratindur
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 62.2967169
lon: -7.0132
WWFK. WWFK (107.1 FM, &quot;Frank FM&quot;) is a radio station broadcasting a classic rock radio format. Licensed to Plattsburgh West, New York, it serves the Champlain Valley, including the Plattsburgh-Burlington radio market. The station is owned by Jeff Shapiro, through licensee Great Eastern Radio, LLC, and operates in a simulcast with its WRFK (also on 107.1) in Barre.

Geographic entities mentioned:
surface_form: Champlain Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
It is a headstream of the Greta. The river rises on Mungrisdale Common north of Blencathra and drains much of the eastern and southern sides of the mountain. The river runs east, then north before sharply turning south at the village of Mungrisdale, skirting almost all around the bottom of Souther Fell.

Geographic entities mentioned:
surface_form: Mungrisdale Common
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6523
lon: -3.06938
surface_form: Blencathra
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.63985
lon: -3.0504611111111
It is a headstream of the Greta. The river rises on Mungrisdale Common north of Blencathra and drains much of the eastern and southern sides of the mountain. The river runs east, then north before sharply turning south at the village of Mungrisdale, skirting almost all around the bottom of Souther Fell.

Geographic entities mentioned:
surface_form: Souther Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6538
lon: -3.00122
Distribution. The Uncompahgre fritillary was first found above tree-line at Uncompahgre Peak, located in Hinsdale County, Colorado, USA by Larry Gall, Felix Sperling, Scott Graham, Kathleen Shaw, and Wendy Roberts working out of the Rocky Mountain Biological Laboratory. A few years following, another population was found at Redcloud Peak, about 10 miles south of Uncompahgre Peak.

Geographic entities mentioned:
surface_form: Uncompahgre Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.071666666667
lon: -107.46222222222
Distribution. The Uncompahgre fritillary was first found above tree-line at Uncompahgre Peak, located in Hinsdale County, Colorado, USA by Larry Gall, Felix Sperling, Scott Graham, Kathleen Shaw, and Wendy Roberts working out of the Rocky Mountain Biological Laboratory. A few years following, another population was found at Redcloud Peak, about 10 miles south of Uncompahgre Peak.

Geographic entities mentioned:
surface_form: Redcloud Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.940833333333
lon: -107.42138888889
surface_form: Uncompahgre Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.071666666667
lon: -107.46222222222
Population decline. Mark-recapture methods completed within a decade of their discovery showed low population estimates at Uncompahgre Peak and Redcloud Peak. The Uncompahgre fritillary was thought to be on the edge of extinction and was added to the Endangered Species List in 1991.

Geographic entities mentioned:
surface_form: Uncompahgre Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.071666666667
lon: -107.46222222222
surface_form: Redcloud Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.940833333333
lon: -107.42138888889