iq2I. No. 1 1. 



THE STRANDFLAT AND ISOSTASY. 



' As the map Fig. 164 shows these heights are considerably higher than the upper limit 

 of submergence found by Kaldhol at other places in the same neighbourhood, and 

 if these values be correct, they will give the isobases a very crooked course in this 

 region, but as the above figures show, the observed heights of the supposed Tapes 

 line agree fairly well with the heights computed from the observed heights of the 

 upper limit of submergence. 



