| Show ANTARCTIC ICE it differ considerably ir from ont that of the northern aptton the difference in the formation ot of arctic and d antanuk A ottil ke ile AS a is well known Is 1 very areat N V bile till the berla u justly m nil cou lt ift of 0 it large larce ice liaos running i p into number numberless leos t mere mers and arches arc liei re the isaks which surrounded unde I 1 th the 0 in tiers clem from they wen vere torn the k butare tic bergs are solid mas cassea aes it autin tee with ith peri wall walls ant ALL o 0 plateau on the top all liula whether they were broken the large southerly barrier or d from roni the gladders Klat lera of actori I 1 and 41 thu tuo b irrice bergs ba bal I 1 very dl alls blue ll 11 alnea nes aar w their wall walli i dudl lat I 1 liag the annual growth by snowfall these lines wan pro of bourm oot not to be found in ta the gla 1 catrice clr ice llie latter also hobed more lekeu s to the northern feet ice than han did the former fornier the I 1 leaks eaks and tomira ot or the arctic I 1 el erga ergs are olied to be f wined by the Int influence luence of 0 ocean current currents u caring away the notier water part of the ice nia gs un on ler ter iter ter until the natural law of grivi gravitation tation for lonia alto it t to 0 ui ul sot set hut flut way why have the etarl ti L ea 1 t ggs a dit dif ferent appearance I 1 it t li Is certain that in the tho antarctic C matera tic re are alio 1 cur current renta I 1 et alven icebergs that have gone as fir north ae tie the v auth uth of new zealand rat annl have all main valued tb the e farhi of their antarctic origin I 1 cannot we see any other reason for this ills dis stint arity between the berg bergs of the north an annl I 1 those of the euth but tl ti il the arctic leet erl 4 as a rule knust r pi 14 4 through elliner which la in ton ten I 1 carature rapidly hange f anni arx tit one extreme t ti anther an liner and if tie e I 1 ebere take 1 nuch luch loncer lonier tinie in atif II 11 biting s uth ant than jo do the A it arctic leebens in a ivan ing ln north ward an ani I 1 thu thus i as a rule the tee ice leria exist thin tl if m s of the ant antarctic ir e tic I 1 hie lie I 1 ilist I 1 n the nt tit arctic Lontin continent ent I 1 ly hy 4 1 L in the january ventury |
