Some  Results. 
(1).  The  Fiords. 
Only  a few  measurements  of  currents  in  the  fiords  have  heen 
collected  in  1906,  and  are  here  treated.  A considerahle  material 
has  heen  since  collected,  and  this  will  he  worked  up  by  Professor 
Grund  in  the  Bergen  Biological  Station’s  Report  for  1907,^)  to 
which  the  reader  may  he  referred. 
The  measurements  from  the  fiords  shown  in  the  tables  (St.  29d, 
299,  304  and  a few  unimportant  measurements  from  St.  315  and 
318  b and  c)  are  rather  difficult  to  denote.  There  seem  to  be  very 
considerahle  changes,  in  the  directions  as  well  as  in  the  velocities. 
In  the  case  of  the  deepest  stations  (St.  297  and  304)  one  might 
feel  inclined  to  almost  distrust  our  methods.  But  the  ohservations 
appear  thoroughly  reliahle  for  this  reason  that  no  revolutions,  or 
at  any  rate  only  extremely  few  have  heen  found  at  the  depths 
where  one  would  have  naturally  expected  to  find  still  water:  so 
that  when  at  station  304  no  movement  of  the  propeller  revealed 
itself  during  the  course  of  30  minutes  at  a depth  of  400  meters, 
or  merely  a few  revolutions  during  from  15—30  minutes  at  a depth 
of  200  or  300  meters,  it  hecomes  quite  clear  that  the  apparatus  has 
not  heen  set  in  motion  by  changement  of  place.  We  have  previ- 
ously  mentioned  how  hearings  showed  that  the  movement  of  the 
hoat  might  be  quite  left  out  of  cousideration,  even  where  the  depth 
was  more  than  400  meters. 
From  the  Sondmore  Fiords  we  have  ohservations  from  the 
upper  portion  of  the  Hjorund  Fiord,  from  its  middle  portion  and 
P The  "Bergens  Museum’s  Aarbog”  for  1908. 
