The Insular Belt is a physiogeological region on the north western North American coast. It consists of three major island groups and many smaller islands and stretches from southern British Columbia into Alaska and the Yukon . It represents the Late Cretaceous to Eocene accretion of what is known as the Insular Superterrane (formed from repeated accretion of multiple terranes ) to the North American continent .
5-733: The rocks that form the Insular Superterrane are allochthonous , meaning they are not related to the rest of the North American continent. They consist of a series of volcanics , intrusions and sedimentary rocks from the collision of an ancient island arc called the Insular Islands . The exact collision of the Insular Islands remains uncertain. The major island groups that compose the Insular Superterrane are, from south to north, Vancouver Island and
10-686: A distance from their present location. In the United States there are three notable allochthons, all of which were displaced nearly 50 km (31 miles) along thrust faults. The Golconda and Robert Mountains allochthons are both found in Nevada , a product of the Antler orogeny in the late Devonian period. Another is the Taconic allochthons found in New York , Massachusetts and Vermont formed from
15-448: Is derived from Greek: allo , meaning other, and chthon , meaning earth. For other possible mechanisms see obduction . An allochthon which is isolated from the rock that pushed it into position is called a klippe . If an allochthon has a "hole" in it so that one can view the autochthon beneath the allochthon, the hole is called a " window " (or fenster). In generalized terms, the term is applied to any geologic units that originated at
20-711: The Gulf Islands , the Haida Gwaii and the Alexander Archipelago in Alaska. The region is noteworthy as it has the greatest physiographic relief from the depths of Queen Charlotte Sound (which had been a coastal plain during the last ice age) to the heights of the Wrangell - Saint Elias Mountains . In general the region is extremely rugged with very little flat land except in certain regions (e.g.
25-468: The east coast of Vancouver Island). The region is thickly forested, having a temperate year round climate, with many of the world's largest trees. This article about a specific Canadian geological feature is a stub . You can help Misplaced Pages by expanding it . Allochthon An allochthon , or an allochthonous block, is a large block of rock which has been moved from its original site of formation, usually by low angle thrust faulting . The term
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