What Is Lower Flow Regime
In the Lower Flow Regime, the Natural Progression Is from a Flat Bed, to Some Sediment Movement (Saltation Etc.), to Ripples, to Slightly Larger Dunes. Dunes...
In the lower flow regime, the natural progression is from a flat bed, to some sediment movement (saltation etc.), to ripples, to slightly larger dunes. Dunes have a vortex in the lee side of the dune. As the upper flow regime forms, the dunes become flattened out, and then produce antidunes.
What is a flow regime?
A flow regime (or flow pattern) is essentially a description of the flow structure, or distribution of one fluid phase relative to the other.
What are bedforms in geology?
A bedform is a feature that develops at the interface of fluid and a moveable bed, the result of bed material being moved by fluid flow. Examples include ripples and dunes on the bed of a river. Bedforms are often preserved in the rock record as a result of being present in a depositional setting.