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partial pediment |
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partial pediment [′pär·shəl ′ped·ə·mənt] (geology) A broadly planate, gravel-capped, interstream bench or terrace. A broad, planate erosion surface which is formed by the coalescence of contemporaneous, valley-restricted benches developed at the same elevation in proximate valleys, and which would produce a pediment if uninterrupted planation were to continue at this level. How to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit webmaster's page for free fun content. |
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