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subducted_plate/side_m5_55.txt | 823a5.14 5.14 0 0 1 1.517-3.66.999.999 0 1 1 1.414 1.413A3.155 3.155 0 0 0 3 11.822c0.85.331 1.647.931 2.248 1.2 1.2 3.293 1.2 4.493 0l1.181-1.181a3.181 3.181 0 0 0 0-4.494.999.999 0 0 1 0-1.414zm5.89-4 | |
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subducted_plate/side_m5_144.txt | ,12.8878476 11.0487656,12.665981 L8.99939043,10.6167619 L6.95123438,12.665981 C6.72813167,12.8878476 6.43431881,13 6.14294422,13 C5.8503505,13 5.55775678,12.8878476 5.33465407,12.665981 C4.88844864,12.2185905 4.88844864,11. | |
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subducted_plate/side_m2_28.txt | 528 4.53 10.666 7.078 17.068 7.085h33.68c6.4-.003 12.537-2.547 17.063-7.075l46.027-46.099c2.239-2.242 4.014-4.904 5.225-7.833 1.21-2.93 1.832-6.069 1.83-9.239v-36.533c.002-3.173-.621-6.315- | |
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subducted_plate/om4_51.txt | far from the town of Twisp. The new continental shelf graded offshore
to oceanic crust of the deep ocean floor. Geologists often call this ocean the âBridge
River Ocean,â because rocks of the original oceanic crust outcrop
| |
subducted_plate/side_m5_115.txt | 1.128-.635l-.343-.316-.637.635c.98 1.06 2.237 1.59 3.774 1.59M7.221 13.87c0.495.157.9.467 1.219.309.319.677.477 1.102.477a1.49 1.49 0 0 0 1.104-.477c.308-.319.463-.724.463-1.219 0-.46-.145-.848-.44-1.167-.293-.316-.67-.476- | |
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subducted_plate/Intermontane_Plate3_1.txt | egean Sea
Anatolian
Balmoral Reef
Banda Sea
Bird's Head
Capricorn
Coiba
Conway Reef
Easter
Explorer
Futuna
Galápagos
Gonâve
Gorda
Greenland
Halmahera
Iberian
Iranian
Juan de Fuca
Juan Fernández
Kerguelen
Kermadec
Lwandle
Madagascar
Malpelo
Manus
Maoke
Mariana
Molu | |
subducted_plate/side_m5_117.txt | .911c0 1.094-.44 1.89-1.324 2.383.034.179.05.425.05.744 0 2.013-.955 3.735-2.866 5.167-1.91 1.43-4.206 2.145-6.884 2.145s-4.965-.708-6.86-2.121c-1.896-1.412-2.843-3.125-2.843-5.14 0-.352.017 | |
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subducted_plate/side_m2_31.txt | 1.209 2.35-1.574.879-.365 1.82-.553 2.772-.553.952 0 1.894.188 2.773.553.879.365 1.677.899 2.35 1.574l18.624 18.645 18.596-18.65c.672-.675 1.47-1.209 2.349-1.574.879-.365 1.821-.553 2.773-.553.951 0 1.893.188 2.772.553.8 | |
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subducted_plate/om4_16.txt | </td>
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<p><b>Volcanic
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subducted_plate/om4_56.txt | Rivers draining the volcanic highlands carried volcanic mud,
silt, sand and other debris to the new coastline.Â
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subducted_plate/side_m5_129.txt | 2.688 6.25-2.688s4.637.969 6.249 2.688A9.993 9.993 0 0 1 12 22m0-22C5.383 0 0 5.383 0 12c0 3.268 1.294 6.33 3.651 8.63l.012.013A12 12 0 0 0 12 24h.036a12.008 12.008 0 0 0 8.306-3.363C22.701 18.341 24 15.273 24 12c0-6.617- | |
subducted_plate/side_m1_82.txt | 173.15.078.527.117.725.076.232-.048 6.256-3.513 6.535-3.759.22-.194.305-.359.305-.593 0-.234-.142-.575-.312-.75-.1-.102-1.178-.746-3.258-1.945-1.71-.986-3.159-1.808-3.22-1.827a.925.925 0 0 0-.47-.042m2.933 3. | |
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subducted_plate/Intermontane_Islands3_0.txt | part3 -------------------
External links[edit]
"The Omineca Episode (180-115 million years ago) | Burke Museum". Burke Museum – University of Washington
This article about a specific Canadian geological feature is a stub. You can help Wikipedia by expanding it.vte
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subducted_plate/side_m5_96.txt | 637,10.57 C7.648,10.6 7.661,10.628 7.675,10.656 C7.69,10.687 7.707,10.716 7.724,10.744 C7.901,11.126 8,11.552 8,12 C8,12.448 7.901,12.874 7.724,13.256 M19,2 C20.654,2 22,3.346 22,5 C22,6.654 20.654,8 | |
subducted_plate/side_m5_180.txt | .89 0 0 1 1.925-.025c.329.006.662.048.984.117.591.126.88.45.924 1.062.03.439.013.882-.003 1.322-.018.462-.064.924-.089 1.386a13.41 13.41 0 0 0-.024.981c.007.384.044.77.285 1.09.233.31.279.34.621.132.189-.115.348-.294.487-. | |
subducted_plate/side_m1_58.txt | .621.629.203.097.516.099.7.004.077-.04.459-.389.85-.776l.709-.703.731.723c.672.666.748.729.96.795.219.069.24.069.448.004.425-.134.829-.623.829-1.004 0-.346-.114-.505-.959-1.342-.833-.824-1.057-.992-1.466-1.098 | |
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subducted_plate/Intermontane_Plate3_2.txt | cca Sea
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subducted_plate/om4_33.txt | to build the Intermontane
Islands offshore. When the islands
finally collided with the continent, the Intermontane subduction zone
jammed and shut down entirely. </p>
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