Show WALKER WA ro laek LAKE ill lil on our r last we gave a description of walkers river niver lying to the east of the die cevada nevada mountains from front its sources amont amoni the sierra sierras to its ita most northern nort nori hiern fiern bend distant a about out twenty miles in ao an easterly direction from I 1 arson valley from this point it inflows flows nearly south a of twenty five miles to walkers lotka lae io tag about abon abou one balf balt tile the distance among a m ang barren hlll hill hilli sand tand and aud ridge with but little of allu aliu alluvial vial fand OR on 3 either other side though cottonwood cotton cotto nood trees 5 generally line the tile bialis bin iks lis ille the other half be before re reaching lh tho the lake is q much of 1 it I a baire barren plain fo liri pu icher side covered in many places with a crust of alka alk ina cinq and saline sub substances stances some sone sometimes limea limes purely rarely 1 tha that irn parts similar properties ip 19 ahe he water n tho jigli not to a degree that prevent it I 1 fr being I 1 i a fayerita fay prita resort of the natives for the P purposes ar P 9 of ships Spec Speck speckled keo led jed trout arp exceeding 9 nilmer i aj on ous luell in 11 its rapids and pools they are area jaken taken in great numbers m bers by the natives in nets neta 11 ets els mada ap an of rushes and a long tough species specia a 0 grass grasp M A AS 1 you approach ili iiI the lake lako the cottonwood cotton cotlon digap aj pears and FA low wet lyet marsh is formed bj by the j spreading hg of the water ov averit erIt i p the In lipis about twenty t mires in length lengthy and ir from three lo 10 six wide side it is not pot eil ell entirely tirey a frai h tr ir I 1 evaer lake ia ke nor is 4 very salt for nish fish are piuro J j ia a ous ip ift iti wafers this chis thi slake lake has its own t arises there are other small mountain that during th the rains raw of v winter inter empty their vy ty aters into this lake and for afew day das dayl th the tha waseng baer vaen tia ria I 1 p y rapidly eidly to q a certain height ji it then ceases JP p ris rise no io great the quantity of wafer waler flo fio I 1 I 1 in ng into it and yeti lethu aa po ino vj sibe outlet biff at alp ja distance pr three and a half miles iu iq j stelly easily fa ili cli direction tp to the east of 0 a high dividing 1 ridge and all manner matin fr of tv v trifled a j ochs 1 thele there 11 ee breaks outa out a larga stream of wate yate 1 that flowing 1 ling easterly eal terly for many miles is ii at jegg length i d J lost in ahe fhe ands sands of the tile desert and this flows p q tb water asit only occurs when the waters af thit the e ei lake reach a certain height aad entirely caseb ceases v when it recedes to a certain levelis level levei is believed belaev ed ta to I 1 v N bealie be the tho escape water from flip tile lake through bom som some b J subterranean i jj therkel by barren hills bills aud gud evell even j mountains pearly bedriy nils alls nil all of them bearing in i bla bia evidence of the action of volcanic fires fire I 1 I 1 dl lj lake aiono alono lies about forty mi lesto leslo in the soud soua a al I 1 of this a hody body tody of sait bait saltwater water clear and beautiful I 1 i et e L and will be abject of a future fatur e nc epla pla pil cerville cerrille ville american i j |