4 
and the Orinoco) northward, or in the direction of the local 
bends of the oceanic streams. . , , , found in the 
Had the vegetable tropical remains, which a f 
of Ike »ertk.» 
broken fragments and meie e r , ^ nor tberly action 
latitudes migkt easily be accoun 7 fossil trees standing 
themselves have moved bodily in th^dmecti . ag the 
TldP oceanic streams radiate tiom tne souu F in 
fountain-head, and carry with them the san s> S 1 ’ some- 
icebergs of the Antarctic region to, very 1 
times approaching the boun aiy desolation and 
Hence this part of the globe is i s cene o A very 
barrenness to the parallel o a ou streams of the 
different appearance is seen m the noit . basin 
ocean flowing through the tropics all climes, 
comparatively warm, wit g g the crystalline 
and become absorbed therein. Ihe wnst, " a muc h slower 
film of the earth, has a similar action, but at a muc 
rate of movement. T i Northern Canada, and 
In Greenland, Spitsbergen Iceland, Northern u , 
Nova Scotia, we have excellent examples ^\^ in 
upright positions, with their roots still at ' “ r00 f s 0 f 
which they grew; thus very same landlas those 
their having flourished and died °“ th !7 J kerdluk; in i a t. 70°, 
that the land had been favoure ; s „ u ite certain 
Fahrenheit warmer than ^t is at^ pre t, If we 
lies about 14° to the southward In Spitsbergen^ 
.. find «» b~k. k~l-™«. SEn »»# »< 
with those from Greenland. . s 0 f Greenland is 
the growth °5 ie S coi£onsdrain from the general appearance 
S^foSil^Green^^^^^ 
Ibundantlyas we now seein California, According to the Ice- 
