Show WHY SOUS LAKES ARE ane SALT jj tho the cill causa of the sal trims of so ne lie j american lakes aca sis the popular aci ence for enli is too to reame many words of epplin stion it if lathat when the continents from tie sea tle the lak lake bains hii till bem been foamed and name came up tip therefore ot of water in tl it 0 not northern thern and eistein part of the continent oni nent where the lopi uple ay linni lion rin rotin and the tie los by oration the be s sil silt b auz in continuous ly c crrie I 1 aried ht a tl ti roana their outlet ha lita no so diluted dilu teil ai as to la be an cep tible quantity la in aril regions reft ioni as the I 1 IA A tile slope ant the countie around the Uris caspan piAn where too the capor all at n is n in excess of tile su guraly ply the water leyel level of the lie 1 ikes likes continuously continuo uly ank until un on account of dim ni tit lie bcd extent of surf Ke it tie 0 equilia gium of loas loss and fain gain was attained hence bence the exceed ag u ot of great salt lake the sea eti etl I 1 lir lr a like reason the awatar ater of the mediterranean con tain more alt relatively than talat of the 0 in J 1 exceeding tile supplies from the revels and rain fall it requires a constant curlent through the tile birgit nf of ibo the taine is 14 lino of the red b S a c caus au 0 ng a liko canent thes the S rait of cicil fu 1 kandeb other salt ot 0 biniki iha lake plo probably bably owe cheit to t ie ic 1 I 1 bioni the tile laibl ian i water being the mo me t ol 01 all sol solvents vente the r rain a in it at ei et up the chloride of from ibe the foilb ind the disint egid egia in locks and wb wil re the streams jail into likes outlet is on the land it etcell elt must le be a constant Loi itani source of aline saline supply and mateis must beobi be Omi hiie and more salt until unlit their as ai a toli ent has been re reached clied ibe the utah bibin must mus tonce once hae been filled to lit lt bin with lean cean water ate I 1 hie lie outlet has been I 1 iho he 1 iko ie let edingB to its pit ent level bs lell left miny evidences ot of i i feitner ex tent |