E/MJ : engineering and mining journal . s, very little powderbeing used. In surface work, including stripping,25 nun mi,I 1. ten,ii( .^lii/ijiiiiil product with less limn I 0 mnl lime. Product is graded according In impuritiesand shipped in /.- [ngeles for calcining. The (inly commercial magnesite deposil oi sedimentaryorigin, known to exist in the United Stales, is situatedI mi. north of Bissell. a small station 11 mi. easl ..-Hiv,| section i -i \ of which are ma rj ing from 3 to i in The origin of the deposil is not fully understoohis repori on il Hoyl 8 G ances the theoi
E/MJ : engineering and mining journal . s, very little powderbeing used. In surface work, including stripping,25 nun mi,I 1. ten,ii( .^lii/ijiiiiil product with less limn I 0 mnl lime. Product is graded according In impuritiesand shipped in /.- [ngeles for calcining. The (inly commercial magnesite deposil oi sedimentaryorigin, known to exist in the United Stales, is situatedI mi. north of Bissell. a small station 11 mi. easl ..-Hiv,| section i -i \ of which are ma rj ing from 3 to i in The origin of the deposil is not fully understoohis repori on il Hoyl 8 G ances the theoi this region was once a lake basin contaii high onate. Springs and stn ining -Him sulphate in solution drained into Iresulting in a reaction by which magnesium carbonateand sodium sulphate were formed and the magnesiumnate i on and faulting of the various strata of the magnesite set erlaid unconformably by a more recent deposit of a few :??sand and gravel, il overburden shown. Anticline on fauli lineVIEWS OF SEDIMENTARY MAGNESITE BEDS NEAR BISSELL. CALIF. of Mojave on the main line of the Atchison, TopiSanta Fe Ii R. It is operated by the Res PLos Angeles, Calif. All other d( Ins mineral which have heretofore been exploited to any extent arcBuch as have been formed by the alteration of igrocks of high magnesia content, such as the olivines orpyroxenes, by whirl, alteration magnesite, serpenl isome allied rock is u lueed. The Bissell deposil consists of a sine- of interstratifiedbeds showing magni site, i lay, sandstoi imore or less magnesian in character and presumablj isame series as certain massive limestones which oul •Mining engineer. 512 Custon•Located in Kern County, in Gino Meridian and Base-Line. House, San Francise111 N. R. 11 W., San i in the illustratioi 8 . lent to the formation of thesedimentary beds, thej hrusl ,,! almost due east-wesl striki Thisin highly folding andpanied by many minoi (vw inches to thr< - four md vary gnto l-V : bu
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Keywords: ., bo, bookcentury1900, bookdecade1910, booksubjectmineralindustries
