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i i' <br />e further to the ri~yht. The lower xfght sad of pieture a};ows gulch leading <br />Tellurid0 and the stratified formation dust west cf vise ahoan fn Plato Ti s <br />~ ... <br />oss San ffiigual Siver. Plate X shoes the buildfnga at mouth of the Bu111on ~i <br />el~ ,just above ft shat is knoea as the Pandora vein nutting through, and to <br />i <br /> ~ <br />e right the open cut cork cn the Cfmmsrron vein... <br />.' <br />The bedded form of the aurlotsnding rocY,a is well shoxtn. The scat diatiact- #' <br /> ' <br />e bead around the hi>;}rer peeks Barks the beginnizrd of the Rhyoiite series. ` <br />. <br /> <br />Below this band the ismeasa plies a4 talus- ar slide rockn are visible. <br />this account there is beloe the precipftous ,sane of the raountairs!c l;ttle of ;~, <br />e laver rock msaea ex~caed in piece. The demdation of the tnrntntafa rralia is <br /> 3 ii <br />ec?t, At this altitude the c}mage of teeq:erature is rapid. ~c}a day thaeting "' <br />' <br />~ each a3ght freezing is alzaost the universal order. '3his eT3ea~icai change af~ ~ <br />I <br /> <br />rds opportunity for the racisture tv sect;: is the cracks and crevices of t}:e li <br />;:, <br /> ! <br />t}ten to freeze sad exert the pressure of expansloa. Bch day by this pro- <br />c::s <br />, <br />• s eoarat ed y;? <br />a aa~ sacs beeamea axe oy~an crack sad eYentuaily this,.rpfeceor section of i' <br />sn ~' <br />_ ck fa pushed fro:c its amorfa~s to the baaln beiop. The heavy shosa of sinter II{ <br /> S <br />theft pmrt and aid !a 4zaaeporting the already broS:ea roak tG lower horfzone. '', <br />~,. <br />:e shoe 1-+ practicably turned into ice in the aprfr~y; of the year! and these large <br /> <br />assn lyizi, upon sn iaciiaed p3aas follow the leas of gravitation, punk tinrch de- If <br />~; <br />is sassed arn4 leave a path for more to laTloas. These bailee of snce and ice era i' <br />:~a <br />n a sense miniature Ylaciers of aruasal occurersna. Their-power fa almost''innaioul- 1~' <br />~j <br />bic. ;year the head of the basin there appears to be sti21 the after affects of it <br />lacfaZ action, and. it fe'thouglst by souls that the upper sad of an ancient glen- iiE <br />~' <br />er ati11 Este there. SyothistK was observed hrnaever, that eeuld sot be aeeounted ~' <br />or by t}ie betors~sxmticned"attnusl glaciate: 'Aare an anciexrt ~,Iacier at111 exist <br />vzsc[ <br />ronence would be demonstrated by a stream of water cowing <br />its <br />ed <br />,j <br />p <br />, <br />ug, but cover <br /> '~ <br />s <br />'i <br />-- <br />i Y ` <br />~. <br />`. <br />\` <br />