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MONTABtiHS, Ntl41E.T Ifi'ltVENAISSIN, LA JHJSSIERE. 155'fla~'Bafl)ist:errlJg,j;1l;()US graveJ! Th~ Upper Loire aiQ.d someof the hBads~f~1l1e Seine here appr,axim:t!,te. T;hr. SUlYmit..,level af tl~e i\yater$ UthetweenJ...IA COMMODITÊ'-where is na aube,ge, aJldNQGE1~TTflj[1R, VElliA~SUN, which is alike deticie,ot in this respecttothe traveUer. HereawQ:tef Îscrossed W'bich~tiIJ runs northward, sabelongs tathe8eille. Thejsluggishness a/the currents demonstra:tes thehorizontality of th;e surface in gene.Il.al; althoug4 it is here formed intoundll~a:tionsoflaIlg.eextent, b:ut VerlY little fise. Theswe.epsof rivel's areinprap:ortion ta the bOI'~~ootalit.vlof tl}.eir ,co:\ilrse. 'l':his latterJying,as ituSBa:u,dQes"het~eeDs:trati;}.Jl.Hferipg in Itheir;iQatw:e; assuredlya:o ~,tl-:­v:eSitigationinlto :principl(}s.bere:\ilpon.migbtberewar~eldwith 80Q:le Ü;}-:-sigiht intothe hither:toditt1e q.nderstoodltheor;}~Qfsp:rings~ .,Here is for the :finst ticme ,seiCn .c(a. ·1f.ar~ty i~ ,the pr:ese:t;lt .cJ.ay) a .:Wtil~,t