
 
        
         
		t n 
 th e   co a st  (Cockburn’s  Island),  we  lan d ed   upo n   it.  The  vegetable  productions  only  
 amounted  to  tw'enty  Cryptogamic   species,  th re e   o f  th em   Seaweeds.  Unable,  afte r  a  
 series  o f  fruitless  efforts,  to  p e n e tra te   fa rth e r  th a n   65°,  and  after  h av in g   been more  or  
 less entangled in th e  ice for  th irty -s ev en   days,  Sir J am e s   Ross  finally  bore  u p , and w hen,  
 with   great  difficulty,  th e   ships  had  been  ex tricated   from  the  pack-ice,  ~we  commenced  
 tra c in g   its  edge  to   th e   eastward.  A  succession  o f  e a ste rly   gales  ren d ered   th e   p ro gress  
 in  the  advancing  season  tedious,  most  uncomfortable,  and  hazardous.  A t  last  
 however, on th e  2 2nd  of F eb ru ary   1843, th e  p ack was  lost sight of, tren d in g  to th e  south-  
 w'est.  On   th e   2 8 th   th e   A n ta rc tic   Circle  w'as  recrossed,  and  in  spite  of  th e   rapidly  
 sh o rten in g   days,  d a rk   nig h ts,  and  co ntinua l  bad  w'eather  (for  th ro u g h o u t  the month  
 of  F eb ru ary ,  corresponding  to  an   E n glish  August,  only  one  day  elapsed  without  
 snow'),  the  Commander  persevered  in  holding  a  southerly  course.  O n   Sunday  the   5th  
 o f  M a rch ,  th e  we ather  be ing  very  th ick ,  with  snow-squalls,  white  p etre ls were  seen,  a  
 bird  whose  appearance  affords  a   sure  indic ation  o f  the  p ro x imity   o f  pack-ice,  and  on  
 th e   afternoon o f th e   same  day  a  heavy  p a ck  was  descried,  only  a  few yards  ahead,  with  
 a   terrific  su rf  b eating  on  it.  T h e   ice  h e re  was  such  as  not  to   allow  o f  being  “  ta k e n ”   
 (or  ente red),  even u n d e r the most  favourable  circumstances,  an d   the   ships w'ere  accordin 
 g ly   p u t  ab o u t  in   lat.  71° 3 0 '  S.,  long.  15° W. 
 T h e   th ick n ess  of  the  wea ther made  it  impossible  to  a scerta in  th e   course  and  position  
 o f  th e   p a ck ,  and  th e  Northwa rd   Voyage  was  commenced u n d e r  violent N .E .  equin 
 octial gales.  Beating to th e  no rthw ard ,  the ice  o ccurred on b oth  tack s ,  and the vessels  
 were  found to  b e  in   a  big h t  o f the pack, with th e   ocean loaded with  bergs,  and  while  the   
 continued  snow-squalls  prev en ted   the  possibility  o f  seeing  any  ob ject  ahead,  the  heavy  
 seas  and snow-laden  s ta te  o f th e  rig g in g  rendered all h um an  exertions ineffectual.  From   
 th a t  date  till  th e   11th o f M a rch , m atters   remained m uch  th e   same,  th e   ships  b eating  to  
 the  n o rthw ard   with   as  much  press  o f  sail  as  could  b e  exposed,  tru s tin g   to   Providence  
 alone  for  guidance  among  th e   bergs.  On   th e   19th  th e   position  assigned  to  Bouvet’s  
 o r  Circumcision  Islan d  was  gained,  b u t  the  we a th er  ren d ered   all  endeavours,  for  three  
 days,  to  discover  lan d   in  th is  place  of  no  avail.  B o th   ships  h ad   a  narrow  escape  of  
 ru n n in g   foul  o f  an   iceberg,  over  which  the  sea  was  b reaking,  e ig h ty   feet  high.  The  
 “ E re b u s,”   passing  to   windward,  stru ck   one  o f  the  floating masses  from  i t ;  and  the  
 “  T e rro r,”  to  windward  o f  h e r  consort,  did  n o t  discover  th e   danger  till  almost  too  late. 
 when  be aring  up,  she  ran   along  th e   edge  of  th e   b erg   in.  th e   wash  o f  th e   surf.  On  
 th e   2 4 th   D'U rv illa a  and  Macrocystis  were  seen  in  lat.  51°  S.,  and  th e   la s t  b e rg   on  
 M arch   2 5 th ,  in  lat.  47°  S .,  th e   ships  finally  gaining  th e   Cape  o f  Good  Ho p e  on  the  
 4 th   o f A p ril  1843,  within  two  days  of  th re e   years  after  th ey   h ad   first  q u itted   th a t  p ort  
 for  the  h ig h   so u th ern   latitudes. 
 Respecting the climate o f th e  various regions v isited by th e  expedition, and especially  
 th a t which  prevails with in  th e  A n ta rc tic  Circle, little  need here  be  said ;  except  th a t  the  
 va st  p roportion  which water  bears  to   land,  ten d s  to  ren d er  th e   tem p e ra tu re   uniform  
 th ro u g h o u t  the  year,  an d   the  farth er  so u th   is  th e   p o sition,  the  more  equable  does  the  
 climate  seem  to  be.  No   analogy  c an   prove  more  in co rrect  th a n   th a t which  compares  
 th e   similar  degrees  of  latitu d e   in   th e   n o rth  with  those of  the  south.  The most  casual  
 inspection  of  th e  map  suffices  to  show  th e   immense  p ro p o rtio n   o f  sea  to  land  in  the  
 so u th e rn   hemisphere, the mass o f th e   co ntinents  term in a tin g   to  th e   n o rth   o f lat.  40°  S.,  
 America  alone  dwindling  away  to  th e   fifty-sixth  degree.  T h e   scattered   islands  d iscovered  
 to  th e  south of this  are therefore removed  from th e   influence o f any  tra c ts  which  
 enjoy  a  b e tte r  o r  co ntinental  climate.  T h e   power  o f th e   sun  is  seldom  felt,  and  unless  
 in th e   immediate  neighbourhood of land,  and  accompanied  by  a  comparatively d ry land-  
 wind,  th a t  lumin ary   only  draws  u p   such  mists  and  fogs  as  in te rcep t  its  ray s.  After  
 en terin g   th e   p ack-ice  between  55°  and  65°,  th e   th erm om e ter  seldom,  d u rin g   any  p a rt  
 of th e   summer  day,  rises  above  32°  or  falls  below  20°  ;  an d  while  th e   so u th e rly   winds  
 b rin g   snow,  th e   n o rth e rly   ones  tra n sp o rt  an  atmosphere  laden  with  moisture,  which,  
 becoming a t once condensed,  covers  th e   face  of th e   ocean with white  fogs  o f the  densest  
 de scription. 
 All  islands  and  lands  to  th e   southward  o f 45°  p a rtak e  more  o r  less  o f th is   inhospitab 
 le   climate,  which,  th o u g h   eminently  unfavourable  to  a varied  growth of p lan ts,  still,  
 from  its  equable n a tu re ,  causes  a  degree o f luxuriance to p ervade  all  th e   vegetable  k in g dom, 
   such  as  is  never  seen  in  climates where  th e   vegetable  functions  are  suspended  for  
 a  large  po rtio n   o f  the  year.  The  remoteness  o f  these  islands  from  an y   co n tin en t,  to ge 
 th e r with  th e ir  inaccessibility,  preclude  the  idea  of  th e ir b eing  ten an ted ,  even  in  a  
 single  in stan ce,  by  plants  th a t  have  m ig rated   from  o th er  cou n tries,  and  still  more  
 d istin c tly   do  th ey   forbid  the  possibility  o f m an  h av in g   been  an  active  agent  in  th e   dissemin 
 atio n   of  them.  On   th e   co n tra ry ,  th e   rem a ik ab le   fact  th a t  some  o f  the  most