39G 



l)onii to ;i Carex narc/iim tiilti: tliey mav, however, measure 

 10 — 15cm in heifjlil and niiwards ol' 1 ni in length; several 

 are not from this year, as they liave clearly been covered by 

 water, are sometimes a 111 tie water-eroded and now and then 

 intersected by drought cracks. The biggest sand drifts are 

 formed by Salix and Jhyas. 



. '^AÜüR. 



■■^f'^ 



.y-^ 



^tm^.A-tfrnt^-^ii- 



I'ig. I'J. Greatl> deiiiolished Sa^iæ-dune in Iroiil of a new sand-dritt. Klit- 

 dalen. (From photo, by Chr. Krii-.se). 



On the somewhat higher land environing the "Stensletter" 

 are rather high (up to 1 m) dunes (fig. 19) around Salix groen- 

 landica tufts in all stages of building up and demolition; the 

 intervening ground is of the nature of "Stensletten", but thi 

 sand in the drifts is fine, stonefree drift sand. This is no 

 question of any washing-out phenomenon, as there neither is 

 any running water nor can be any considerable supply thereof. 



At a still higher level are smaller flats of "living" dune sand 



