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Show BJISjfll rUtlUITl lr Mine. wKlj Plagitatt, u comfortable logging JKSjjj t0"n on the Uinta Fe l'aclllo IUIlwuy RH 1 In Arlionu, hat been provided by ua- flpS tura with the queereet lecmaking jnvsH pinl known. During the pait mm- flUUe mer a large part of the tuwn'a Ico aup- HQ ply haa been iccured from cavea In mHHB the pine woodi, nine rnllra to the HKS southward. KUi The OAfei are In lavik formation, the rJHMj geologleal capping of tha entire coun- lajBtaE try. Ilnterlug to the main cavern, jSfl through a narrow silt in the mnlapal PH rock, neceaaltatc a ertlcl drop of iVpfl ten feat to tbt Roar of a paaaage that P ruca farther In, till bloeked by leo PPJ lirrlcri. Tu teoiperatur In the cave PIH even In the height of aummer, li a) oat j the frcedag point Many vlittora nave been proetrat.t by the cold after making too long a atay The Ice. which la aa hard aa Ice can be. nils every nook and cranny beyond the tbort, black hallway that leadi Inward from the entrance When dg nay In whatever quantity. It aemi to grow again from behind. In the manner of the creep of glarleri The depth or alia of Ihe depoalta le not known. It la even believed that there li an underground un-derground Ice lake nf Immente. dl.nen-totve. dl.nen-totve. How the depoelt waa formed la a putile that haa not been eo'.ved by geologliU or Ice mlneri The region , la almoit dcitltute of eurfare or well water and the mean temperaturea are . far above the thermomttrle figure that would appear to render lueb a depoilt poulble Ilut the leo l there and tha product or Ihe unique mine haa been old dally In Flagitaff. |