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okay today I would like to talk a little bit about what causes variation in cross stratification when we talked about the lamination on ripples or dunes so if you have a flow going downstream you end up with deposition of lamina on the downstream side those lamina reflect the geometry of the ripple now its much easier to draw in two dimensions and thats what I usually do but the third dimension of the ripples matters docHubly in the geometry of the cross ratification so if I try to draw in the third dimension and this is the extension of the ripple the third dimension if its straight these lamina are somewhat planar as you go along the ripple itself however if the ripples curved the geometry of the lamina are also true so say some sinuous geometry going into the third dimension and thats very common in ripples particularly and more turbulent flow and also common for dunes so for lamina this pipe if the flows coming out towards us and we have a variable ripple crest so this is