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normal consolidation |
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normal consolidation [′nȯr·məl kən‚säl·ə′dā·shən]
(geology) Consolidation of a sedimentary material in equilibrium with overburden pressure. normal consolidation The condition that exists if a soil deposit never has been subjected to an effective pressure greater than the existing pressure, and if the deposit is completely consolidated under the existing overburden. 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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