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<p>other processes. <a href="page.php?w=Turbidity_current">Turbidity current</a>s can transport this sediment down the <a href="page.php?w=continental_slope">continental slope</a> to the deep ocean floor. The deep ocean floor undergoes its own process of spreading out from the mid-ocean ridge, and then slowly <a href="page.php?w=subduct">subduct</a>s accumulated sediment on the deep floor into the <a href="page.php?w=Structure_of_Earth">molten interior</a> of the earth. In turn, molten material from the interior returns to the surface of the earth</p><p>
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