| Show BlUI I Sa Sll the or in II Idaho is III n a The discovery of another BollI Ise Basin another aDO florence and nil another gulch b with It Its I SO 10 ounces St of gout to 10 the Ibe cable yard ard of gravel nl buried under great t lava sheet are t not tonly only possibilIties but strong tro II UH ties II says Ro Robert rt Beil the RepublIcan candidate for tate elite mine inspector of Idaho Idabo Rome Iome of th the richest iq in grovel of It California sad ad Ballarat were Weft mined from under uDder f feet t of t I lava capping Similar condl condi lion may mar obtain in III Idaho TIle The proposition offers offeN a wide field for peu tion Idaho plACer mining history may not lIot be more IIII than half hlf written A thorough au corny ot of otI the Stale would prove OW of Inestimable I benefit to It its ment and nd corn mercial prosperity The subject would be b simple a as to variety of reck romul Stone Iola for with the tx of a Vel vury limited atea ot of very ery recent sediments they are conn confused eel almost to and low lower series rice tile the great t metal Ital be beating series of the ebe world This work would tb the rela tIe the age of at our placer deposits and nd great at lava lows aad 4 prove a reliable guIde tel further in III this tint Une Jt it w also NeoN some reo r eba in fa the topo of lb Sats at large flier II 1 that it at on OD UN Sims fiT Iliff nf fI t ta present t of the upper Beak river flowed out through the present drainage of Salmon river etc Ir Ten Tell miles west ot of Kalmon Halmon City titer there is II an old ld river earn co with h soft mil mud rock that thatis I is entirely foreign to 10 that thai which had bad it origin as aa dust dustin In the wrest great I outbursts near the lit head of rh river mil miles a aa away awaya a b by similar deposits In ID region This material wu was carried to toIta Its Ita present posItIon by a slow stream trem of sri larl volume now from Ita III mUrce by a mountain divide teel ft high THIS old river channel hu has been n crosscut In iii several veral places parta by br small modern streams that run Iowa to the Lembi river at t a much low level 1411 These a expos exposto to slow millions million of tons Ion ot of this tWI old chan chanDI DI ad mud that has hall carefully urn Mm pled I a number of times and inti ro nd to ta contain a value at n 1 per ton tOIl in Ib gold There I said to bt be of acres acre ot of material ot of consistency anti and origin orilla In the upper Snake river region rellon ct even better than tha 1 is II a wen well worthy of clo Some Iome of tM th cheap cheaper er t method of gold uld might Itt r rek this material show a mar liD of it If handled fin on a I large and developed a gold miffing Ip in industry duet of a ma magnitude that kI dr dEs count anything ret yet attempted In a tit the gold 1014 producing I la De |
