. Appendix to the Journals of the Senate and Assembly of the ... session of the Legislature of the State of California. iel, driven soutii70 feet to an east and west vein, which has a widtii of two feet, and isreported to carry high values in gold. 384 REPORT OF STATE MINERAI,OflIST. Iv(iii|tiiitril coiisisls (»r . and M., in the Miniiifr Distriet. Owner. .). Martin, of ^ Shaft )() feet deep and trenches alonj? an iron-stained outcrop of qiiartzite. Idle. Ribl: State Mineralofijists lieport X\. p. 104. Ma/nimoth Mine. It is situated in the -Mammoth Lakes ]\lininir Dis-tric
. Appendix to the Journals of the Senate and Assembly of the ... session of the Legislature of the State of California. iel, driven soutii70 feet to an east and west vein, which has a widtii of two feet, and isreported to carry high values in gold. 384 REPORT OF STATE MINERAI,OflIST. Iv(iii|tiiitril coiisisls (»r . and M., in the Miniiifr Distriet. Owner. .). Martin, of ^ Shaft )() feet deep and trenches alonj? an iron-stained outcrop of qiiartzite. Idle. Ribl: State Mineralofijists lieport X\. p. 104. Ma/nimoth Mine. It is situated in the -Mammoth Lakes ]\lininir Dis-trict, in Sees. 9 and 10, T. If), 16 S., R. 27 E., M. D. H. and :\I., 4 milessouthwest of ]\Iammoth P. ()., on the west slope of the Sierra Nevadarange of mountains. EUn-ation 9000 to 10,000 feet. Owner, SatiFranrisco and Vrrsno Cuinjxuni. of San Franciseo. Outcrop of vein. Mammoth Coii.^ d .Miniiii, Ci. , .MaTiiiiiili. . County. Under option to the Mnmmnlh Consolidnfrd Mints Compovy, 1241 Ter-niiiud Subway , Los Anjreles. E. S. (Sillette, presid«nt : A. (IMahan, secretary; A. (J. Malian, jreneral manajrer. IIoldin};s formerly comprised tive claims known as Folk. Francisc. I>ionan/a and ^lammoth, two of which are ]» projjcrty was ojxrated by the Mammoth MIniiHj Conipann. of SanFraiuisco, from 1S7S until ISSl. Tlie j)roduelion durinj; this j)eriodamounted to $200,000 in jrold. The Manunoth vein occtirs in crystal-lin(> rocks, evidently (hie to alteration of the slates and has a freneralnorthwesterly course, dippinp: 70 to 80^ to the northeast. The surfacecroppiufrs show the vein to be over 100 feet in width. The jroid isreported to occur in buiuhes and spots, and the vein material isminerali/e<l with mafrnetite. oxides of iron, auriferous i)yrite. chalcojt
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Keywords: ., bookcentury1800, bookdecade1850, bookidappendixtojo, bookyear1853
