id stringlengths 15 145 | text stringlengths 2 241k | title stringclasses 1
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subducted_plate/ib2_15.txt | ">Belt</span></dt>
<dd itemprop="content" class="descript" lang="en"><p><span class="w"><span id="selection_index3" class="selection_index"></span>The</span> <b><span class="w">Intermontane</span> <span class="w">Belt</span></b> <span class="w">is</span> <span class="w">a</span> <r><span class=" | |
subducted_plate/om4_26.txt | montane belt to the south.</p>
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subducted_plate/side_m5_203.txt | 4.364 3.212-.316 5.985 1.127 6.193 3.221.208 2.096-2.226 4.05-5.438 4.366m9.927-12.789a5.155 5.155 0 0 0-4.888-1.572.738.738 0 1 0.31 1.444c1.234-.26 2.57.12 3.476 1.117a3.611 3.611 0 0 1.763 3.55.744.7 | |
subducted_plate/side_m5_197.txt | .457-1.67 5.398.342 2.03 2.416 3.46 4.478 3.715 2.117.234 4.23.174 6.352.03.358-.328-1.732-.319-2.612-.439-2.008-.215-4.186-.255-5.907-1.383-1.604-1.136-1.814-3.365-1.045-5.007.644-1.55 1.607-3.048 2. | |
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subducted_plate/om4_32.txt | Farallon Plate has fragmented into two smaller âmicroplates,â each with
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subducted_plate/side_m5_74.txt | -.782 3.12-2.345 4.316C13.049 17.403 11.171 18 8.98 18s-4.062-.591-5.613-1.772c-1.55-1.18-2.325-2.61-2.325-4.293 0-.295.013-.516.04-.665C.361 10.858 0 10.193 0 9.28c0-.619.2-1.144.6-1.571.402-.429.87-.643 | |
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subducted_plate/side_m2_6.txt | .011 2.94.081m12.816.003c.199.099.388.288.487.487.075.152.077.294.077 5.416 0 5.122-.002 5.264-.077 5.416-.043.086-.14.219-.216.295-.282.282-.105.267-3.407.291-3.305.025-3.133.011-3.745.302-.352.166-.591.352-1.125.87l-. | |
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subducted_plate/om4_28.txt | subduction zone. Â
Beneath the far edge of the Intermontane microplate, another
plate called the Insular microplate was sinking.</p>
<p></p>
<p></p>
<p>This arrangement with
two parallel subduction zones is unusual | |
subducted_plate/side_m5_157.txt | -5c2.756 0 5 2.243 5 5a4.983 4.983 0 0 1-1.437 3.504m5.144 3.789l-3.103-3.103A6.963 6.963 0 0 0 15 8c0-3.859-3.141-7-7-7-3.86 0-7 3.141-7 7s3.14 7 7 7a6.956 6.956 0 0 0 4.189-1.396l3.103 | |
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subducted_plate/om4_24.txt |
of seafloor. </p>
<p></p>
<p>The Intermontane terranes make up thousands of
square miles in a large plateau region in British Columbia and extend
all the way to the Yukon Territory. Along the southern end of the Intermontane
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subducted_plate/side_m1_73.txt | 487.075.152.077.294.077 5.416 0 5.146-.002 5.263-.078 5.418a1.418 1.418 0 0 1-.232.307c-.306.297.399.275-8.67.275-9.069 0-8.364.022-8.67-.275a1.418 1.418 0 0 1-.232-.307c-.076-.154-.078-.284-.089-5.318-.008-3.557.001-5. | |
subducted_plate/side_m5_105.txt | .006a.988.988 0 0 0.293.704l9 9a.997.997 0 0 0 1.414 0.999.999 0 0 0 0-1.414L3.414 13H23a1 1 0 1 0 0-2"></path><path id="question-a" d="M12 22C6.486 22 2 17.514 2 12S6.486 2 12 2s10 4.486 10 10-4.486 10-10 10m0-22C5.383 0 0 5.383 | |
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subducted_plate/om4_29.txt | .Â
The modern Philippine Islands are one of the few places on Earth
where twin subduction zones exist today.</p>
<p></p>
<p></p>
<p>Geologists call the ocean
between the Intermontane islands and North America the âSl | |
subducted_plate/side_m1_44.txt | -.501.159-.833.365-1.243.775-.4.4-.6.717-.771 1.217L.02 7.42l-.011 4c-.013 4.391-.016 4.322.227 4.903.211.503.382.701 2.061 2.38 1.679 1.679 1.877 1.85 2.38 2.061.591.247.257.236 7.323.236 7.066 0 6.732.011 7.323-.236.503 | |
subducted_plate/side_m2_26.txt | 2000/svg" viewBox="0 0 174 242"><path fill="#FA005A" d="M166.935 118.154L50.108 1.273C49.504.67 48.735.259 47.898.093c-.837-.166-1.705-.08-2.493.247-.788.327-1.461.88-1.935 1.59-.474.71-.727 1.546-.727 2.4v98.276L7.365 67.22c-. | |
subducted_plate/side_m1_41.txt | m3.264-2.232c1.064-.214 1.716-.54 2.03-.854a2.253 2.253 0 1 0-3.186-3.186c-.303.302-.627.954-.84 2.037-.14.711-.21 1.485-.233 2.235.754-.02 1.524-.09 2.229-.232Z" clip-rule="evenodd"></path>
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subducted_plate/side_m1_79.txt | .817-.371 1.217-.771.4-.4.6-.717.771-1.217l.105-.307V5.42l-.105-.307c-.171-.5-.371-.817-.771-1.217-.41-.41-.741-.616-1.243-.775l-.321-.101-8.42-.006c-4.631-.003-8.511.01-8.621.029m16.917 2.054c.199.099.388. | |
subducted_plate/side_m1_46.txt | 658-.014-1.692-.101-1.856a.874.874 0 0 0-.213-.254c-.264-.189-.721-.249-1.064-.142m9.802 6.04c.199.099.388.288.487.487.075.151.077.278.077 4.016v3.86l-.107.18c-.133.223-3.08 3.163-3.273 3.266-.135.071-.383.074- | |
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subducted_plate/side_m5_211.txt | 2.333.23 1.096.928 1.842 2.101 2.132.41.101.833.182 1.253.203 1.656.083 6.422.182 7.142.14zm.995-12.884L12.6 7.227l3.196 6.103-1.269.6-3.248-6.091L8.66 9.048l3.204 6.117-1.269.6L7.34 9.66l-2.563 1 | |
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subducted_plate/om4_27.txt | Zones</p>
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<p>The Intermontane Islands
had been accumulating as a volcanic chain somewhere out in the Pacific
Ocean since Triassic time, beginning around 245 million years ago.Â
The volcanism records yet another | |
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subducted_plate/side_m4_51.txt | 91 6.91 0 0 1-1.497 1.527l-34.32 25.523c-3.053 2.27-7.33 1.586-9.558-1.527A7.07 7.07 0 0 1 70 114.69V63.643c0-3.854 3.063-6.977 6.84-6.977 1.45 0 2.86.47 4.03 1.34z"></path>
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subducted_plate/side_m5_168.txt | .859 16 9 16M9 0C4.037 0 0 4.037 0 9C0 13.963 4.037 18 9 18C13.963 18 18 13.963 18 9C18 4.037 13.963 0 9 0" clip-rule="evenodd"></path><path d="M8 12.9975V8.00982C8 7.45545 8.447 7.00735 9 7.00735 9.553 7.00735 10 7.45545 10 8.00 | |
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