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pseudo cross-bedding |
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pseudo cross-bedding [′sü·dō ′krȯs ‚bed·iŋ] (geology) An inclined bedding produced by deposition in response to ripple-mark migration and characterized by foreset beds that appear to dip into the current. A structure resembling cross-bedding, caused by distortion-free slumping and sliding of a semiconsolidated mass of sediments (such as sandy shales). 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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