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Relief Inversion |
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Relief Inversion
obsequent relief, a change in the relief by agents of denudation with the formation of inverse relationships between geological structures and relief forms. For example, river valleys may occur in anticlines and mountain ranges may arise in synclines. 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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