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obsequent fault-line scarp |
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obsequent fault-line scarp [′äb·sə·kwənt ′fȯlt ‚līn ‚skärp] (geology) A fault-line scarp which faces in the direction opposite to that of the original fault scarp or in which the structurally upthrown block is topographically lower than the downthrown block. 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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