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Strandflat
Strandflat is the low land on the coast and the near coast bottom of sea, typical for the landscape of the Norwegian coast. This landform is created in the Quaternary Period, and it is only to be found in arctic and antarctic areas that has been or is covered by ice, for instance Greenland and Svalbard. Strandflat is a geomorphological word of Norwegian origin, and is used in geology and geography.
==Characteristics==
The strandflat includes areas on land as well as in the sea, and might be separated in three zones: Outmost is a submarine zone, thereafter a skerry zone and innermost a supramarine zone. The strandflat ends against a steep rock on the land side, even higher mountains, and in the sea side the strandflat ends with a steep slope down to the continental shelf. The strandflat is near to the sea level of today; the areas on land side reach no more than 50 m., and the areas in sea is commonly not more than 50 m deep. The width of strandflat varies from 50 – 60 km to nearly nothing. The strandflat is a location for lots of special mountains, they are called ''rauk''. They have one common characteristic, they are all very steep. The rauks are landmarks on the Norwegian coast.
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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