907 
Cur:  eut-Measu*-ements. 
25 
Z \ ^ Cn 
only  slight  changes  of  direction  throughout  a deptli  of  95  meters.  The 
velocities  did  not  show  values  higher  than  about  45  cm.  per  second, 
but  the  station  probably  did  not  lie  over  the  heart  of  the  Baltic 
Cnrrent  (see  flg.  8).  Here  too  the  water  in  the  deeper  layers,  which 
bad  come  from  the  North  Sea,  seemed  to  mo  ve  in  the  same  direc- 
