English: Schmematic profile of a strandflat in Norway. To the right lies a higher terrain with may represent a Paleic surface or some uneven landscape. To the left of this lies a steep slope leading to the strandflat. The strandflat is both flat and undulating and forms to the left a skerry zone. The skerry zone is separated from the submarine flat surfaces of the bankflat by an underwater slope. The large island in the middle host a rauk (an isolated hill akin to an inselberg).
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