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<p><a href="page.php?w=Denudation">Denudation</a> of these high uplifted regions produces <a href="page.php?w=sediment">sediment</a> that is transported and <a href="page.php?w=deposition_%28geology%29">deposited</a> elsewhere within the landscape or off the coast. On progressively smaller scales, similar ideas apply, where individual landforms evolve in response to the balance of additive processes (uplift and deposition) and subtractive processes (<a href="page.php?w=subsidence">subsidence</a> and <a href="page.php?w=erosion">erosion</a>). Often,</p><p>
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