Sarmila/GeoWiki-Features huggingface dataset:
It includes not only the Mount Edziza area but also the Spectrum Range to the south, which are separated by Raspberry Pass. Mount Edziza Provincial Park is in the Tahltan Highland, a southeast-trending upland area extending along the western side of the Stikine Plateau. Structure.

Geographic entities mentioned:
surface_form: Stikine Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
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
Structure. Ice Peak is the prominent south peak of Mount Edziza, an ice-covered stratovolcano in Cassiar Land District of northwestern British Columbia, Canada. It is a pyramid-shaped horn formed by glacial erosion and represents the western rim of a small caldera which formed on the summit of an older stratovolcano.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
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
It is a pyramid-shaped horn formed by glacial erosion and represents the western rim of a small caldera which formed on the summit of an older stratovolcano. This stratovolcano is one of four felsic central volcanoes along the north–south axis of the Mount Edziza volcanic complex, the other three being Armadillo Peak, the Spectrum Range and the high edifice of Mount Edziza.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: Armadillo Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5383
lon: -130.56
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
Four cirques on the eastern flank have exposed the internal structure of the Ice Peak stratovolcano whereas the western flank is completely mantled by glaciers. The eastern cirques are at the head of Tennaya Creek which flows northeast into Nuttlude Lake, an expansion of Kakiddi Creek.

Geographic entities mentioned:
surface_form: Tennaya Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.69966
lon: -130.42065
surface_form: Kakiddi Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
The eastern cirques are at the head of Tennaya Creek which flows northeast into Nuttlude Lake, an expansion of Kakiddi Creek. Between Tennaya, Nido and Tenchen creeks are pie-shaped, gently sloping interfluves which represent the remains of the original eastern flank of the Ice Peak stratovolcano.

Geographic entities mentioned:
surface_form: Nido
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71636
lon: -130.47065
surface_form: Tenchen
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.76636
lon: -130.43724
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Although the original eastern flank has been almost completely destroyed by erosion, the northern flank is buried under the younger stratovolcano of Mount Edziza. The southern and western flanks of the Ice Peak stratovolcano are approximal to those of the original volcano and merge with the Big Raven Plateau which is one of the main physiographic features of the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: Big Raven Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
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
Most of the vents in this lava field are at elevations above near the terminus of outlet glaciers of the Mount Edziza ice cap, five of which named. The highest of these vents, Tennena Cone, attains an elevation of on the upper western flank of Ice Peak. Cocoa Crater to the southwest has an elevation of, making it the second highest of the five named vents.

Geographic entities mentioned:
surface_form: Tennena Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.68416666666667
lon: -130.66222222222223
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
The highest of these vents, Tennena Cone, attains an elevation of on the upper western flank of Ice Peak. Cocoa Crater to the southwest has an elevation of, making it the second highest of the five named vents. The third highest vent, Coffee Crater, is in elevation and lies northwest of Cocoa Crater.

Geographic entities mentioned:
surface_form: Cocoa Crater
instance_of: Mountain
countries: Canada
coordinates: lat: 57.65
lon: -130.7
Cocoa Crater to the southwest has an elevation of, making it the second highest of the five named vents. The third highest vent, Coffee Crater, is in elevation and lies northwest of Cocoa Crater. South of Coffee Crater on the south side of upper Taweh Creek is Keda Cone, the fourth highest vent with an elevation of.

Geographic entities mentioned:
surface_form: Coffee Crater
instance_of: Mountain
countries: Canada
coordinates: lat: 57.63
lon: -130.67
surface_form: cocoa crater
instance_of: Mountain
countries: Canada
coordinates: lat: 57.65
lon: -130.7
The third highest vent, Coffee Crater, is in elevation and lies northwest of Cocoa Crater. South of Coffee Crater on the south side of upper Taweh Creek is Keda Cone, the fourth highest vent with an elevation of. Between the heads of Taweh and Shaman creeks is The Saucer which, with an elevation of, is the lowest named vent in the Snowshoe Lava Field.

Geographic entities mentioned:
surface_form: Taweh Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
surface_form: coffee crater
instance_of: Mountain
countries: Canada
coordinates: lat: 57.63
lon: -130.67
South of Coffee Crater on the south side of upper Taweh Creek is Keda Cone, the fourth highest vent with an elevation of. Between the heads of Taweh and Shaman creeks is The Saucer which, with an elevation of, is the lowest named vent in the Snowshoe Lava Field. Icefall Cone and Ridge Cone are two parasitic cones on the eastern rim of Ice Peak at an elevation of about.

Geographic entities mentioned:
surface_form: Shaman
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.61636
lon: -130.40395
It is elliptical in structure and older than the Icefall and Ridge cones, although it is also younger than the main edifice of Ice Peak. Also on the western flank of Ice Peak where it merges with the surrounding Big Raven Plateau are the Koosick and Ornostay bluffs, which lie adjacent to the head of Sezill Creek.

Geographic entities mentioned:
surface_form: Koosick
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6739
lon: -130.725
surface_form: Ornostay
instance_of: Mountain
countries: Canada
coordinates: lat: 57.699722222222
lon: -130.70388888889
surface_form: Sezill Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.69967
lon: -130.88724
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
The Neck is a circular, in diameter volcanic plug on the southeastern flank with an elevation of. Background. Ice Peak is part of the Northern Cordilleran Volcanic Province, a broad area of shield volcanoes, lava domes, cinder cones and stratovolcanoes extending from northwestern British Columbia northwards through Yukon into easternmost Alaska.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
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 Ice Peak Formation pantelleritic trachyte 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: Sorcery Ridge
instance_of: Mountain
coordinates: lat: 57.65606944444444
lon: -130.61504166666666
surface_form: the neck
instance_of: Mountain
countries: Canada
coordinates: lat: 57.67
lon: -130.58
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Basement. Ice Peak is underlain by the Pyramid Formation, which consists mainly of Pleistocene rhyolite and trachyte lava flows, domes and thick piles of pyroclastic breccia. Also underlying Ice Peak are alkali basalt lava flows and flow breccia of the Tenchen Member of the Nido Formation, which were erupted from multiple volcanoes during the Pliocene.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
The Saucer was formed by a later subaerial fissure eruption that was not accompanied by lava fountaining. Instead, lava issued quietly and flowed into Shaman Creek in the east and Taweh Creek in the west. The Sheep Track Member is the product of a small but violent VEI-3 eruption from the southwestern flank of Ice Peak.

Geographic entities mentioned:
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
surface_form: shaman creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.61636
lon: -130.40395
Location. Ice Peak lies in Mount Edziza Provincial Park southeast of the community of Telegraph Creek. With an area of, Mount Edziza Provincial Park is one of the largest provincial parks in British Columbia and was established in 1972 to showcase the volcanic landscape. It includes not only the Mount Edziza area but also the Spectrum Range to the south, which are separated by Raspberry Pass.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
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 current, high horn of Ice Peak protrudes through the roughly ice cap of Mount Edziza and is completely flanked by steep-walled, active cirques. Tencho Glacier on the southern flank of Ice Peak is the largest outlet glacier of the ice cap, as well as the largest glacier of the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
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
Stratigraphy. Ice Peak is subdivided into at least three geological formations, each the product of a distinct stage of volcanic activity. These periods of volcanic activity occurred during three magmatic cycles of the Mount Edziza volcanic complex; each cycle began with the effusion of alkali basalt and culminated with the eruption of lesser volumes of felsic magma.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
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
Also on the western flank of Ice Peak where it merges with the surrounding Big Raven Plateau are the Koosick and Ornostay bluffs, which lie adjacent to the head of Sezill Creek. The Neck is a circular, in diameter volcanic plug on the southeastern flank with an elevation of. Background.

Geographic entities mentioned:
surface_form: the neck
instance_of: Mountain
countries: Canada
coordinates: lat: 57.67
lon: -130.58
Early volcanism in the Snowshoe Lava Field deposited material that was quenched by ice and meltwater, resulting in piles of tuff breccia, pillow lava and pillow breccia such as Tennena Cone. Cinder cones such as Cocoa Crater and Coffee Crater were created by subsequent lava fountain eruptions in a subaerial environment.

Geographic entities mentioned:
surface_form: cocoa crater
instance_of: Mountain
countries: Canada
coordinates: lat: 57.65
lon: -130.7
surface_form: coffee crater
instance_of: Mountain
countries: Canada
coordinates: lat: 57.63
lon: -130.67
Ice Peak. Ice Peak is the prominent south peak of Mount Edziza in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of and protrudes through Mount Edziza's ice cap, which is roughly in area. The peak is a pyramid-shaped horn formed by glacial erosion and is completely flanked by steep-walled, active cirques.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Tencho Glacier on the southern flank is the largest outlet glacier of Mount Edziza's ice cap. The summit of Ice Peak is about lower than that of Mount Edziza, but it still rises well above the general level of the Big Raven Plateau. Ice Peak and the surrounding area are in Mount Edziza Provincial Park which also includes the Spectrum Range to the south.

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
Ice Peak and the surrounding area are in Mount Edziza Provincial Park which also includes the Spectrum Range to the south. Ice Peak is the remains of an approximately 1-million-year-old stratovolcano whose original eastern flank has been almost completely destroyed by erosion.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
On the southwestern flank is the Snowshoe Lava Field, which issued from at least 12 vents mostly near the terminus of outlet glaciers in the last 20,000 years. A diverse assemblage of volcanic rocks comprises the Ice Peak stratovolcano and are subdivided into three geological formations with varying ages. Location.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Location. Ice Peak lies in Mount Edziza Provincial Park southeast of the community of Telegraph Creek. With an area of, Mount Edziza Provincial Park is one of the largest provincial parks in British Columbia and was established in 1972 to showcase the volcanic landscape. It includes not only the Mount Edziza area but also the Spectrum Range to the south, which are separated by Raspberry Pass.

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
This stratovolcano is one of four felsic central volcanoes along the north–south axis of the Mount Edziza volcanic complex, the other three being Armadillo Peak, the Spectrum Range and the high edifice of Mount Edziza. The current, high horn of Ice Peak protrudes through the roughly ice cap of Mount Edziza and is completely flanked by steep-walled, active cirques.

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
Tencho Glacier on the southern flank of Ice Peak is the largest outlet glacier of the ice cap, as well as the largest glacier of the Mount Edziza volcanic complex. Idiji Glacier occupies a cirque on the eastern flank of Ice Peak whereas Tennaya Glacier extends southeast from between Ice Peak and the summit of Mount Edziza.

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: 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
Idiji Glacier occupies a cirque on the eastern flank of Ice Peak whereas Tennaya Glacier extends southeast from between Ice Peak and the summit of Mount Edziza. Four cirques on the eastern flank have exposed the internal structure of the Ice Peak stratovolcano whereas the western flank is completely mantled by glaciers.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Subfeatures. On the southwestern flank of Ice Peak is a roughly area of lava flows and at least 12 vents called the Snowshoe Lava Field. Most of the vents in this lava field are at elevations above near the terminus of outlet glaciers of the Mount Edziza ice cap, five of which named. The highest of these vents, Tennena Cone, attains an elevation of on the upper western flank of Ice Peak.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
South of Coffee Crater on the south side of upper Taweh Creek is Keda Cone, the fourth highest vent with an elevation of. Between the heads of Taweh and Shaman creeks is The Saucer which, with an elevation of, is the lowest named vent in the Snowshoe Lava Field. Icefall Cone and Ridge Cone are two parasitic cones on the eastern rim of Ice Peak at an elevation of about.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Icefall Cone and Ridge Cone are two parasitic cones on the eastern rim of Ice Peak at an elevation of about. Both cones are younger than the main edifice of Ice Peak, but they have been greatly modified by glaciation, slumping and rockfalls due to their location near the steep headwalls of active cirques.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Both cones are younger than the main edifice of Ice Peak, but they have been greatly modified by glaciation, slumping and rockfalls due to their location near the steep headwalls of active cirques. Punch Cone on the western flank of Ice Peak is a roughly, steep-sided ridge protruding through Mount Edziza's ice cap.

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
Punch Cone on the western flank of Ice Peak is a roughly, steep-sided ridge protruding through Mount Edziza's ice cap. It is elliptical in structure and older than the Icefall and Ridge cones, although it is also younger than the main edifice of Ice Peak.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Stratigraphy. Ice Peak is subdivided into at least three geological formations, each the product of a distinct stage of volcanic activity. These periods of volcanic activity occurred during three magmatic cycles of the Mount Edziza volcanic complex; each cycle began with the effusion of alkali basalt and culminated with the eruption of lesser volumes of felsic magma.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
These periods of volcanic activity occurred during three magmatic cycles of the Mount Edziza volcanic complex; each cycle began with the effusion of alkali basalt and culminated with the eruption of lesser volumes of felsic magma. The oldest geological formation is the Ice Peak Formation, which formed during a period of volcanic activity about 1 million years ago during the third magmatic cycle.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
The oldest geological formation is the Ice Peak Formation, which formed during a period of volcanic activity about 1 million years ago during the third magmatic cycle. Another period of volcanic activity 0.3 million years ago deposited the Kakiddi Formation on the southwestern and eastern parts of the Ice Peak pile during the fourth magmatic cycle.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Another period of volcanic activity 0.3 million years ago deposited the Kakiddi Formation on the southwestern and eastern parts of the Ice Peak pile during the fourth magmatic cycle. The third oldest geological formation is the Big Raven Formation, which was deposited on the Ice Peak and Kakiddi formations during the fifth magmatic cycle in the last 20,000 years. Ice Peak Formation.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
The third oldest geological formation is the Big Raven Formation, which was deposited on the Ice Peak and Kakiddi formations during the fifth magmatic cycle in the last 20,000 years. Ice Peak Formation. The Ice Peak Formation consists of lava and pyroclastic rocks that were erupted mainly from vents near the summit of the Ice Peak stratovolcano.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Ice Peak Formation. The Ice Peak Formation consists of lava and pyroclastic rocks that were erupted mainly from vents near the summit of the Ice Peak stratovolcano. Two stratigraphic units comprise this once symmetrical stratovolcano, both of which are lithologically distinct. The lower stratigraphic unit, which forms much of the volcanic pile, is an assemblage of mostly thin basaltic lava flows.

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
Lavas of intermediate composition such as tristanite, trachybasalt and mugearite are very limited in extent. The upper stratigraphic unit is a highly varied succession of lavas and pyroclastic rocks forming the high, central edifice of Ice Peak. It consists of basalt, trachyte and a variety of intermediate rocks such as tristanite, trachybasalt, benmoreite and mugearite.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
It consists of basalt, trachyte and a variety of intermediate rocks such as tristanite, trachybasalt, benmoreite and mugearite. The Ice Peak Formation includes the Koosick and Ornostay bluffs, both of which are thick lobes of trachyte that originated under the summit ice cap. Both bluffs are similar in geomorphology and composition, consisting of several lava flows up to thick.

Geographic entities mentioned:
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 Ice Peak Formation pantelleritic trachyte 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
Potassium–argon dating of Ice Peak Formation pantelleritic trachyte has yielded ages of 1.6 ± 0.2 million years, 1.5 ± 0.4 million years and 1.5 ± 0.1 million years. These dates being older than those of the underlying Pyramid Formation may be due to excess argon in the Ice Peak Formation and are therefore considered unreliable.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
These dates being older than those of the underlying Pyramid Formation may be due to excess argon in the Ice Peak Formation and are therefore considered unreliable. Ice Peak Formation basalt flows on the northwestern flank of Mount Edziza are interbedded with diamictites recording a regional glaciation that occurred during the Early Pleistocene.

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
They are lithologically and geomorphologically similar to the older Edziza Formation trachytes, but occur south of the central stratovolcano of Mount Edziza. The remains of a nearly wide, rubble-covered trachyte flow are present on the eastern flank of Ice Peak in Sorcery Valley and in the south fork of Tennaya Valley where it is divided into two tributary branches.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Remnants of this terminal lobe are present in the form of isolated outcrops adjacent to Kakiddi Lake and Nuttlude Lake. The source of this Kakiddi flow remains unknown, but the tributary branch that descended Tennaya Valley probably originated from a vent near the summit of Ice Peak that is now covered by glaciers.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
The source of this Kakiddi flow remains unknown, but the tributary branch that descended Tennaya Valley probably originated from a vent near the summit of Ice Peak that is now covered by glaciers. A relatively small trachyte flow descended from Punch Cone on the western flank of Ice Peak and spread onto the Big Raven Plateau.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
Instead, lava issued quietly and flowed into Shaman Creek in the east and Taweh Creek in the west. The Sheep Track Member is the product of a small but violent VEI-3 eruption from the southwestern flank of Ice Peak. It was deposited on all lava flows and cinder cones in the Snowshoe Lava Field with the exception of The Saucer which likely postdates the Sheep Track eruption.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Basement. Ice Peak is underlain by the Pyramid Formation, which consists mainly of Pleistocene rhyolite and trachyte lava flows, domes and thick piles of pyroclastic breccia. Also underlying Ice Peak are alkali basalt lava flows and flow breccia of the Tenchen Member of the Nido Formation, which were erupted from multiple volcanoes during the Pliocene.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Also underlying Ice Peak are alkali basalt lava flows and flow breccia of the Tenchen Member of the Nido Formation, which were erupted from multiple volcanoes during the Pliocene. The southern edge of the Ice Peak pile laps out against Miocene comenditic or trachytic pumice and ash flows of the Armadillo Formation.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
The southern edge of the Ice Peak pile laps out against Miocene comenditic or trachytic pumice and ash flows of the Armadillo Formation. The oldest geological formation underlying Ice Peak is the Raspberry Formation, which consists of Miocene alkali basalt and minor hawaiite and mugearite.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
The name of the peak became official on January 2, 1980, and was adopted on the National Topographic System map 104G after being submitted to the BC Geographical Names office by the Geological Survey of Canada. Several other features on or near the flanks of Ice Peak have names that were also adopted on January 2, 1980, including Tennena Cone, Keda Cone, Koosick Bluff and Ornostay Bluff.

Geographic entities mentioned:
surface_form: ice peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
surface_form: koosick bluff
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6739
lon: -130.725
surface_form: tennena cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.68416666666667
lon: -130.66222222222223
surface_form: ornostay bluff
instance_of: Mountain
countries: Canada
coordinates: lat: 57.699722222222
lon: -130.70388888889
Several other features on or near the flanks of Ice Peak have names that were also adopted on January 2, 1980, including Tennena Cone, Keda Cone, Koosick Bluff and Ornostay Bluff. &quot;Ice Peak&quot; is tautological with &quot;Ice Mountain&quot;, another name for Mount Edziza referring to its cover of glacial ice. The Ice Peak stratovolcano is sometimes referred to as &quot;Ice Volcano&quot;.

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: 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: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
These rocks were deposited by volcanic eruptions from 20 million years ago to as recently as a few hundred years ago. 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. Stratigraphy.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Ice Peak. Ice Peak is the prominent south peak of Mount Edziza in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of and protrudes through Mount Edziza's ice cap, which is roughly in area. The peak is a pyramid-shaped horn formed by glacial erosion and is completely flanked by steep-walled, active cirques.

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
The peak is a pyramid-shaped horn formed by glacial erosion and is completely flanked by steep-walled, active cirques. Tencho Glacier on the southern flank is the largest outlet glacier of Mount Edziza's ice cap. The summit of Ice Peak is about lower than that of Mount Edziza, but it still rises well above the general level of the Big Raven Plateau.

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
Four cirques on the eroded eastern flank have exposed the internal structure of the stratovolcano whereas the southern and western flanks are approximal to those of the original volcano. The northern flank is buried under the younger and higher stratovolcano of Mount Edziza which reaches an elevation of.

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
Location. Ice Peak lies in Mount Edziza Provincial Park southeast of the community of Telegraph Creek. With an area of, Mount Edziza Provincial Park is one of the largest provincial parks in British Columbia and was established in 1972 to showcase the volcanic landscape. It includes not only the Mount Edziza area but also the Spectrum Range to the south, which are separated by Raspberry Pass.

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
Between Tennaya, Nido and Tenchen creeks are pie-shaped, gently sloping interfluves which represent the remains of the original eastern flank of the Ice Peak stratovolcano. Although the original eastern flank has been almost completely destroyed by erosion, the northern flank is buried under the younger stratovolcano 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. On the southwestern flank of Ice Peak is a roughly area of lava flows and at least 12 vents called the Snowshoe Lava Field. Most of the vents in this lava field are at elevations above near the terminus of outlet glaciers of the Mount Edziza ice cap, five of which named. The highest of these vents, Tennena Cone, attains an elevation of on the upper western flank of Ice Peak.

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
Kakiddi Formation. The Kakiddi Formation consists of the remains of thick trachyte lava flows and associated pyroclastic rocks. They are lithologically and geomorphologically similar to the older Edziza Formation trachytes, but occur south of the central stratovolcano of Mount Edziza.

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
All of these features consist of alkali basalt and hawaiite with the exception of the Sheep Track Member which comprises a small volume of trachyte pumice. Early volcanism in the Snowshoe Lava Field deposited material that was quenched by ice and meltwater, resulting in piles of tuff breccia, pillow lava and pillow breccia such as Tennena Cone.

Geographic entities mentioned:
surface_form: tennena cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.68416666666667
lon: -130.66222222222223
In 1969, he became seriously ill and drifted in and out of a coma for an entire year. He died in Jerusalem on the morning of 25 May 1970 (19 Iyar 5730) and was buried on Har HaMenuchot. He was succeeded as rosh yeshiva by Yehuda Tzadka, who had learned under him since the age of 14. Notable students.

Geographic entities mentioned:
surface_form: Har HaMenuchot
instance_of: Mountain
countries: Israel
coordinates: lat: 31.798133333333
lon: 35.177727777778
Missouri saddled darter. The Missouri saddled darter (&quot;Etheostoma tetrazonum&quot;) is a species of freshwater ray-finned fish, a darter from the subfamily Etheostomatinae, part of the family Percidae, which also contains the perches, ruffes and pikeperches. It is endemic to Missouri, where it occurs in the Ozarks from the Gasconade River to the Osage and Moreau rivers.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
On May 21, the White Sox officially released Keppinger. Personal life. Keppinger's older brother Billy, a left-handed pitcher, played independent baseball and minor league baseball in the Kansas City Royals system. Keppinger resides in Dacula, Georgia. He married his second wife Dihanna on October 7, 2017, at The Ritz Carlton in Lake Oconee, Georgia.

Geographic entities mentioned:
surface_form: Lake Oconee
instance_of: Lake
countries: United States
coordinates: lat: 33.35
lon: -83.157
Taxonomy. &quot;Myriopteris cucullans&quot; was first described by Antoine Laurent Apollinaire Fée in 1857, as &quot;Cheilanthes cucullans&quot;. He based it on material collected in Mexico by Johann Wilhelm Schaffner in the Valley of Mexico. The type specimen is &quot;Schaffner 82&quot; at the Rio de Janeiro Botanical Garden herbarium.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
Skiddaw Slate. Skiddaw slate is an early Ordovician metamorphosed sedimentary rock, as first identified on the slopes of Skiddaw in the English Lake District. The base of this series is unknown. The thickness could, therefore, amount to several thousand feet of sediment. These sediments were formed about 500 mya by deposition in a shallow sea, low-energy environment.

Geographic entities mentioned:
surface_form: Skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
Taiping Lake (Anhui). Taiping Lake () is a lake in Anhui, China. It is crossed by the Taiping Lake Bridge.

Geographic entities mentioned:
surface_form: taiping lake (anhui)
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.36
lon: 118
Taiping Lake (Anhui). Taiping Lake () is a lake in Anhui, China. It is crossed by the Taiping Lake Bridge.

Geographic entities mentioned:
surface_form: taiping lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.36
lon: 118
Taxkorgan Nature Reserve. The Taxkorgan Nature Reserve (officially spelled Taxkorgan Natural Reserve) is a nature reserve in Kashgar Prefecture, Xinjiang, China. It is situated around the Taghdumbash Pamir of Pamir Mountains and Karakorum Mountains. It covers about was established in 1984 mainly to protect the rare Marco Polo sheep and Tibetan argali.

Geographic entities mentioned:
surface_form: Taghdumbash Pamir
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 37.2
lon: 75.4
However, van Kinsbergen's photographs satisfied the Society and he became renowned as &quot;the Society's Photographer&quot;. His work on repairing the system for managing water flow during his trip in the Dieng Plateau in order to photograph the Javanese Hindu temple there was avidly praised by the Society.

Geographic entities mentioned:
surface_form: Dieng Plateau
instance_of: Plateau
countries: Indonesia
coordinates: lat: -7.207005
lon: 109.864111
The JCU Fitness Center, located inside the Gianicolo Residence Hall, is open for students, faculty, and staff with a full array of free weights, machines, and open workout space, along with weekly classes in abs & legs, running, yoga, and kickboxing. The JCU Athletic department also organizes trips and activities to locations such as Cinque Terre, Mount Circeo, or Sapri.

Geographic entities mentioned:
surface_form: Mount Circeo
instance_of: Mountain
countries: Italy
coordinates: lat: 41.23109
lon: 13.05553
The Tassajara Fire was a wildfire that started on September 20, 2015, in the Santa Lucia Range, in Monterey County, California. The fire swiftly burned of land in a rural, residential area near the Los Padres Forest, including 12 homes and numerous outbuildings. It was contained a week later on September 27. The smoke plume was visible throughout the Monterey Bay and Salinas Valley regions.

Geographic entities mentioned:
surface_form: Salinas Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.7654
lon: -121.7918
Ikramul Hasan Shakil. Ikramul Hasan Shakil (; born 1994) is a Bangladeshi mountaineer and adventurer who became the seventh Bangladeshi to summit Mount Everest. He reached the summit on 19 May 2025 at 6:45 am Bangladesh time.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
In the Faroese language noon refers to 15:00 in the 24-hour clock or 3pm in the 12-hour clock, whereas in the English language noon usually now refers to 12:00 or 12pm. If you are standing in the centre of the old village in Sørvágur at 15:00 you will see the sun above Nónfjall. Hence the name. Nónfjall lies above the valley of Kjóvadalur.

Geographic entities mentioned:
surface_form: Kjóvadalur
instance_of: Valley
countries: Faroe Islands
surface_form: nónfjall
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 61.517
lon: -6.833
Nónfjall. Nónfjall is a mountain on the island Vágar in the Faroe Islands. The mountain is located south of the village of Sørvágur, near Vágar Airport and east of the mountain Høgafjall. The name Nónfjall translates to 'Noon mountain'. However, the Faroese use the word noon differently from the current English usage.

Geographic entities mentioned:
surface_form: nónfjall
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 61.517
lon: -6.833
However, the Faroese use the word noon differently from the current English usage. In the Faroese language noon refers to 15:00 in the 24-hour clock or 3pm in the 12-hour clock, whereas in the English language noon usually now refers to 12:00 or 12pm. If you are standing in the centre of the old village in Sørvágur at 15:00 you will see the sun above Nónfjall. Hence the name.

Geographic entities mentioned:
surface_form: nónfjall
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 61.517
lon: -6.833
It is located in the Apurímac Region, Antabamba Province, Sabaino District, and in the Aymaraes Province, Caraybamba District. Kiswarani lies southeast of Pisti.

Geographic entities mentioned:
surface_form: Pisti
instance_of: Mountain
countries: Peru
coordinates: lat: -14.3292
lon: -73.0806
Kiswarani. Kiswarani (Aymara &quot;kiswara&quot; &quot;Buddleja incana&quot;, &quot;-ni&quot; a suffix to indicate ownership, &quot;the one with &quot;kiswara&quot;, hispanicized spelling &quot;Quishuarani&quot;) is a mountain in the Andes of Peru, about high. It is located in the Apurímac Region, Antabamba Province, Sabaino District, and in the Aymaraes Province, Caraybamba District.

Geographic entities mentioned:
surface_form: kiswarani
instance_of: Mountain
countries: Peru
coordinates: lat: -13.1383
lon: -72.0414
surface_form: kiswarani
instance_of: Mountain
countries: Peru
coordinates: lat: -14.3411
lon: -73.0678
Kiswarani. Kiswarani (Aymara &quot;kiswara&quot; &quot;Buddleja incana&quot;, &quot;-ni&quot; a suffix to indicate ownership, &quot;the one with &quot;kiswara&quot;, hispanicized spelling &quot;Quishuarani&quot;) is a mountain in the Andes of Peru, about high. It is located in the Apurímac Region, Antabamba Province, Sabaino District, and in the Aymaraes Province, Caraybamba District.

Geographic entities mentioned:
surface_form: kiswarani
instance_of: Mountain
countries: Peru
coordinates: lat: -13.1383
lon: -72.0414
surface_form: kiswarani
instance_of: Mountain
countries: Peru
coordinates: lat: -14.3411
lon: -73.0678
surface_form: kiswara
instance_of: Mountain
countries: Peru
coordinates: lat: -13.5525
lon: -74.4558
surface_form: kiswara
instance_of: Mountain
countries: Peru
coordinates: lat: -13.5525
lon: -74.4558
Christopher Myngs raided Santiago de Cuba in 1662 and Campeche the following year. Henry Morgan later took over - his most notable attacks were at Puerto del Príncipe and at Porto bello, both in 1668 and the defeat of a Spanish squadron on Lake Maracaibo the following year. The Spanish meanwhile could do little to protect themselves.

Geographic entities mentioned:
surface_form: Lake Maracaibo
instance_of: Lake
countries: Venezuela
coordinates: lat: 9.8158333333333
lon: -71.556666666667
Its radio stations DWFE-AM in Olongapo and DWFA-AM in Balanga, Bataan, and Far East 95.1 (now RW 95.1) on FM are as a part of their network's operations from 1946 to 1991 but the TV channel was forcibly shut down due to the eruption of Mount Pinatubo and the withdrawal of the U.S. military from Clark.

Geographic entities mentioned:
surface_form: Mount Pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Still, the trade in Orungu territory paled in comparison with its southern neighbor. In 1788, Cape Lopez and the Gabon estuary were exporting around 5,000 slaves per year in contrast to the 13,500 per year exported from Loango's coast. At the beginning of the 19th century, the Fernan Vaz Lagoon south of Cape Lopez supplied large numbers of slaves to the Orungu Kingdom.

Geographic entities mentioned:
surface_form: Fernan Vaz Lagoon
instance_of: Lake
countries: Gabon
coordinates: lat: -1.59239
lon: 9.42905