This image of a slabbed core of the Jurassic Norphlet sandstone shows distinctive striations. The clear demarcation separating the two sets of unidirectional lines indicates a change in angle of deposition of the sand that later formed the rock.
This image of a slabbed core of the Jurassic Norphlet sandstone shows distinctive striations. The clear demarcation separating the two sets of unidirectional lines indicates a change in angle of deposition of the sand that later formed the rock.