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subducted_plate/om5_1.txt | v:shapes="_x0000_i1031"></p>
<p>The
approach of the Insular Volcanic Islands is recorded by sediment deposited
along the margins of the Bridge River Ocean.Â
For 60 million years, sand eroded from eastern highlands in the
Omineca Arc.Â&n | |
subducted_plate/om4_4.txt | </div>
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subducted_plate/side_m5_171.txt | .38 4.08015 9.439 4.1002 9.5 4.13128 9.55 4.17037 9.609 4.21047 9.66 4.25057 9.71 4.29067 9.89 4.48214 10 4.74178 10 5.00243 10 5.13375 9.97 5.26307 9.92 5.38437 9.87 5.51369 9.8 5.62397 9.71 5.71419" clip-rule="evenodd"></path></symbol><symbol | |
subducted_plate/om4_50.txt | the Intermontane Islands collided and welded to the continent,
the edge of the continent moved to the west.Â
The new edge of the continent was located along what is
today the eastern edge of the Methow Valley in Washington, not
| |
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subducted_plate/om4_59.txt | ></p>
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<p>Approach
of the Insular Volcanic Islands </p>
<p></p>
<p>The Omineca Arc supported
a chain of continental volcanoes in Washington and British
| |
subducted_plate/side_m5_226.txt | 49-.07c-1.366-.062-2.633-.336-3.608-1.311-.975-.975-1.249-2.242-1.311-3.608-.058-1.265-.07-1.645-.07-4.849s.012-3.584.07-4.849c.062-1.366.336-2.633 1.311-3.608.975-.975 2.242-1.249 3.608-1.311 | |
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subducted_plate/om4_11.txt | nbsp; It is the name given to a remote
range of mountains in north - central British Columbia. We also use the name Omineca for a continental
arc that extended from Alaska to Washington State over Mid-Jurassic
to Mid-Cretaceous time. </p>
<p></p>
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subducted_plate/om4_61.txt | this depositional pattern happened about 130 million years ago in mid-Cretaceous
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subducted_plate/side_m5_187.txt | .053-2.925a4.61 4.61 0 0 0-.126-.662c-.077-.312-.278-.525-.568-.652a38.53 38.53 0 0 1-.494-.222c-.05-.021-.095-.051-.147-.08"></path></symbol><symbol id="wds-icons-facebook" viewBox="0 0 24 24"><use xlink:href="#facebook-a" fill-rule="evenodd"></use></symbol><symbol id="wds-icons- | |
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