Image: Strandflat
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Description: 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).
Author: Lappspira
Usage Terms: Creative Commons Attribution-Share Alike 3.0
License: CC-BY-SA-3.0
License Link: http://creativecommons.org/licenses/by-sa/3.0/
Attribution Required?: Yes
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