BY FRITZ NOETLING, M.A., Ph.D., ETC. 



243 



,4. THE AREA OF THE DIFFERENT STAGES 

 DESCRIBED IN PARAGRAPH 3. 



We can express the increase of land if the sea level 

 were to recede from o to 50 fathoms in absolute figures, 

 as shown in the following table : — 



<d G W 



w :z; pi; 



CO < <! 



> o ;zi 



♦^ »-H i-H 



< 2 



Ph o ffi 

 (i^ « H 



«£:$ 



■^ H '^ 



ffl < > 



C^ CQ W 

 ^ > W 



02 



Before going into details I wish to say a few words 

 with regard to my calculations. I have no such instru- 



