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<p>develop, with climbing ripples developing if sedimentation rates are high enough. If shear is imposed on the ripple beds by an earthquake and/or by an overlying turbidite/turbidity current, the ripple laminations can be deformed into <a href="page.php?w=convolute_laminations">convolute laminations</a> and <a href="page.php?w=flame_structure">flame structure</a>s.<br/>
* Bouma B is deposited under upper flow regime conditions where energy is high enough to carry sand grains by <a href="page.php?w=Traction_%28geology%29">traction</a>, wherein they</p><p>
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