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Show An Optra,liuMD In ttie Korlh. Rcmcrkablei.e'.lu'crencca occur In tho senvmsof Ucjarctlo regions, ao that nt certain tlrrjei. aalt&ppcncd lost yearralj tho thaniiblNToftllie northern seas are flllcannd'elicl.rlvltlilloitlnrkonttbe breaking u'pjof .vrjnter, whllo at ulbir times tho sjfinj jclu'iinels aro comparatively compara-tively freo,.iiif-WliUlttlo leo h seen' olong tholtrncksofltho' transatlantic steamers. - '- j, . t- It la a raosHiutcrirllng fact that dm liar vlclsliuoe evidently occur In'.tl nrttlo anil lujfiirtjlo " reglomi of 'the 1 lanct Mnr(tT!u'telCKopo shows that nt llelds"Cnetiow, exist around the lles of ilart" rt( ndl whin It Is win ter nt either oDiltoso utiles and contract ing when It lJfCTracier thcro. lint tho itflnr lUOWiot'Wuts appear to bo noticeably no-ticeably law eit;niIvo In somo winter seasons thania others', sn that wo might fairly ixpictl,t' Und there, If vro coulill visit tkat'pjaaij'.corrcspondlhg differ-cncoalnthoriBicTpr.tof differ-cncoalnthoriBicTpr.tof Ico carried toward tho cqusturTtittko end of euccceslto winters. lLa , , y Our nrcrtb riavlgStora tako ailrantago of such eperi mjalcns ca tho present n- poarato boiLeiiecr they can tn l cno-trato cno-trato farther jojy aid;tho north polo. II U J crh-npavrumiuato'for'tho increnco of our Lnowledfo 'of Jthomrctlo regions, tluit Llcuteiiant'lrwiry'nnil ltls jarty,'. who darted for iforthern.Urecnlund last' year, aro nowinvtho far north. They may bring jbaiU'most Interesting no-counts no-counts of tlio condition cf Ihlugo there, i and perhaps bo'ablc to throw soino light upon tho cause, cf tho rcmarkablo varla-tlona varla-tlona lu tlio'ipiautity ot icebergs and ico Holds that eomo lloatiug unt of thoso ujstciionsr'eslona In ilHIirciiteiasons, Vuuth'i) Coinpaulon, |
