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Fragment of Earth's crust in British Columbia, Canada
Stikinia, or the Stikine terrane, is a terrane in British Columbia, Canada; the largest of the Canadian Cordillera. It formed as an independent, intraoceanic
Stikinia
Prehistoric superocean that surrounded Pangaea
Asia), Anadyr–Koryak (east Asia), Oku–Niikappu (Japan), and Wrangellia and Stikinia (western North America). Furthermore, seismic tomography is being used
Panthalassa
Fragment of crust formed on one tectonic plate and accreted to another
Mountain terrane Smartville Block Sonomia terrane Steel Mountain terrane Stikinia Suwannee terrane Wrangellia terrane Yakutat Block Yukon–Tanana terrane
Terrane
List of Earth's former oceans
Bridge River Ocean, the ocean between the ancient Insular Islands (that is, Stikinia) and North America Cache Creek Ocean, a Paleozoic ocean between the Wrangellia
List_of_ancient_oceans
Terrane in British Columbia, Canada
Quesnel terrane forms part of the Intermontane superterrane along with the Stikinia and Cache Creek terranes. Quesnellia contains numerous deposits of alkalic
Quesnellia
British Columbia: Implications for the Early to Middle Jurassic evolution of Stikinia". Tectonics. 11 (6): 1266–1287. Bibcode:1992Tecto..11.1266M. doi:10.1029/92TC00276
Hazelton_Group
Geologic province in the Pacific Northwest of North America
Province consists of four large terranes, known as Stikinia, Cache Creek, Yukon–Tanana and Cassiar. Stikinia is a sequence of late Paleozoic and Mesozoic aged
Northern Cordilleran Volcanic Province
Northern_Cordilleran_Volcanic_Province
Icefield in British Columbia, Canada
Crag. Underlying the icefield are Triassic volcanic rocks comprising the Stikinia terrane. Uranium–lead dating has yielded crystallization ages of around
Andrei_Icefield
Geological formation in British Columbia
overlying Armadillo Formation and younger geological formations. Rocks of the Stikinia terrane underlie the Raspberry Formation. The Raspberry Formation consists
Raspberry_Formation
Escarpment in British Columbia, Canada
geological formations are much older Paleozoic and Mesozoic rocks of the Stikinia terrane, as well as and Cretaceous and Paleocene rocks of the Sustut Group
Mess_Creek_Escarpment
Geological formation in Yukon, Canada
and is one of several volcanic features overlying the Yukon–Tanana and Stikinia terranes of northwestern North America. It is part of the Northern Cordilleran
Pelly_Formation
Group of volcanic rocks in British Columbia, Canada
British Columbia, Canada, covering more than 30,000 km2 (12,000 mi2) of the Stikinia terrane in a belt up to 50 km (31 mi) wide and over 800 km (500 mi) long
Takla_Group
Mountain range in North America
vicinity of Mount Meager massif in the Coast Mountains, where they abut the Stikinia Terrane of the Omineca-Intermontane Province that dominates the Interior
North_Cascades
River in British Columbia and Alaska
Plateau roughly corresponds with the northern part of the Stikine Terrane ("Stikinia"), part of the larger Intermontane Belt complex. The Cassiar and Omineca
Stikine_River
Inferred ancient ocean which existed between western North America and several terranes
Belt is bordered by the Quesnellia Terrane in the east and by the large Stikinia Terrane in the west. The accretion of the landmasses and the closing the
Cache_Creek_Ocean
Cinder cone in British Columbia, Canada
Raspberry Formation are sedimentary, volcanic or metamorphic rocks of the Stikinia terrane, which are Paleozoic and Mesozoic in age. Williams Cone is in a
Williams_Cone
Stratovolcano in British Columbia, Canada
by plutonic rocks and metamorphosed volcanic and sedimentary rocks of Stikinia. These basement rocks are of Paleozoic-to-Mesozoic age; pyroxene-bearing
Hoodoo_Mountain
extends as far north as Whitehorse) was surrounded on either side by the Stikinia and Quesnellia terranes. Because both include Triassic augite, have Paleozoic
Geology_of_Yukon
Mountain range in British Columbia, Canada
Raspberry Pass. The Nido and Raspberry formations are underlain by the Stikinia terrane, a Paleozoic and Mesozoic suite of volcanic and sedimentary rocks
Spectrum_Range
Volcanic complex in British Columbia, Canada
Level Mountain consists largely of felsic igneous rocks forming northern Stikinia, but sedimentary rocks are also present below the lava plateau escarpment
Level_Mountain
Volcanic complex in British Columbia, Canada
mainly make up lava domes and central volcanoes. Underlying the MEVC is the Stikinia terrane, a Paleozoic and Mesozoic suite of volcanic and sedimentary rocks
Mount_Edziza_volcanic_complex
Volcano in British Columbia, Canada
west of the mountain. These geological formations are underlain by the Stikinia terrane, a Paleozoic and Mesozoic suite of volcanic and sedimentary rocks
Mount_Edziza
flows of the Raspberry Formation. They rest directly on older rocks of the Stikinia terrane and are exposed along the Mess Creek Escarpment. The Little Iskut
Volcanism of the Mount Edziza volcanic complex
Volcanism_of_the_Mount_Edziza_volcanic_complex
Plateau in British Columbia, Canada
the Mount Edziza volcanic complex, the Kitsu Plateau is underlain by the Stikinia terrane. This is a suite of Paleozoic and Mesozoic volcanic, sedimentary
Kitsu_Plateau
Geological formation in British Columbia, Canada
Paleozoic and Mesozoic sedimentary, volcanic or metamorphic rocks of the Stikinia terrane, which accreted to the continental margin of North America during
Nido_Formation
Cinder cone in British Columbia, Canada
of the Stikine Assemblage, the oldest exposed stratified rocks of the Stikinia terrane which accreted to the continental margin of North America during
Nahta_Cone
Intermontane Belt is a flatter, more rounded region composed of three terranes, Stikinia, Quesnellia, and the Cache Creek terrane. The belt has a lower metamorphic
Geology_of_British_Columbia
Chain of volcanoes and related magmatic features in British Columbia, Canada
Chilcotin Group, which in turn overlie Devonian to Jurassic rocks of the Stikinia volcanic arc terrane. In some places the AVB lavas imperceptibly merge
Anahim_Volcanic_Belt
Hill in British Columbia, Canada
Formation basalt. Exile Hill is underlain by metasedimentary rocks of the Stikinia terrane, a Paleozoic and Mesozoic suite of volcanic and sedimentary rocks
Exile_Hill
Volcanic arc system in the Pacific Northwest
field relations in the arc suggest that the Coast Range Arc was created on Stikinia, a geologic feature that formed in an older volcanic arc environment during
Coast_Range_Arc
Hierarchical outline list of articles related to plate tectonics
Intrusive and volcanic rocks in the mid-continent region of the United States Stikinia – Fragment of Earth's crust in British Columbia, Canada Tuareg Shield –
Outline_of_plate_tectonics
Mountain in British Columbia, Canada
Raspberry Formation are sedimentary, volcanic or metamorphic rocks of the Stikinia terrane, which are Paleozoic and Mesozoic in age. The name of the peak
Ice_Peak
Geological member in British Columbia, Canada
Paleozoic and Mesozoic sedimentary, volcanic or metamorphic rocks of the Stikinia terrane, which accreted to the continental margin of North America during
Tenchen_Member
Volcanic cone in British Columbia, Canada
Raspberry Formation are sedimentary, volcanic or metamorphic rocks of the Stikinia terrane, which are Paleozoic and Mesozoic in age. Tennena Cone and its
Tennena_Cone
Plateau in British Columbia, Canada
Mount Edziza volcanic complex, the Big Raven Plateau is underlain by the Stikinia terrane. This is a suite of Paleozoic and Mesozoic volcanic, sedimentary
Big_Raven_Plateau
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