Narrow ridges found in Martian impact craters in the Nilosyrtis highlands and the Nili Fossae region are the fossilized remnants of underground cracks through which water once flowed, Brown University scientists say. This 3D image of an impact crater in the Nilosyrtis area on the Red Planet shows long pipe-like ridges, fossilized evidence of ancient subsurface water flow (NASA Mars Reconnaissance Orbiter) The study, published online in the journal...
