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Ingressive Shores |
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Ingressive Shores
broken shorelines formed as a result of the penetration of low-lying coastal land by seawater (when the sea level rises or the shore submerges). Depending on the origin of these low-lying areas, ingressive snores are classified as glacial (fjord or skerry), fluvial (ria or lagoon), eolian (Aral shore type), and structural-denudational (Dalmation type). Each type has a distinctive appearance. Want to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit the webmaster's page for free fun content. |
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