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Conrad discontinuity |
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Conrad discontinuity [′kän‚rad dis‚känt·ən′ü·əd·ē] (geophysics) A relatively abrupt discontinuity in the velocity of elastic waves in the earth, increasing from 6.1 to 6.4-6.7 kilometers per second; occurs at various depths and marks contact of granitic and basaltic layers. 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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