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| | The Paleozoic Era |
 | | In North America the era began with submerged geosynclines, or downward thrusts of the Earths crust, along the eastern, southeastern, and western sides of the continent, while the interior was dry land. |
 | | As the era proceeded, the marginal seas periodically washed over the stable interior, leaving sedimentary deposits to mark their incursions. |
 | | Beginning in the Ordovician period, mountain building intermittently proceeded in the eastern part of the Appalachian geosyncline throughout the rest of the era, bringing in new sediments. |
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