Hi to you too <img src="/images/icons/smile.gif" /><br /><br />There are many ways of getting layering (sedimentary, pyroclastic, lava flow, tectonic foliation), we don't know which ones apply here. The high atmospheric pressure on Mars, equyiavlent to neary a km of ocean on earth, means that formation of volcanic ash is strongly inhibited.<br /><br />Jon <div class="Discussion_UserSignature"> <p><em>Whether we become a multi-planet species with unlimited horizons, or are forever confined to Earth will be decided in the twenty-first century amid the vast plains, rugged canyons and lofty mountains of Mars</em> Arthur Clarke</p> </div>