BONANZA By At gold and the of studies tangible 1 42 CONTRIBUTIONS nized and rule Dr surface EARLIER Baron lode BONANZA OF 43 Both which the paper have says Also Suc ID: 839568
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1 BONANZA By INTRODUCTION. At gold and
BONANZA By INTRODUCTION. At gold and the of studies tangible \ 1 ) 42 CONTRIBUTIONS niz
2 ed ! and rule Dr. surface EARLIER
ed ! and rule Dr. surface EARLIER Baron , lode BONANZA OF 43 Both which the paper hav
3 e says: Also Such Particularly is t
e says: Also Such Particularly is the B 44 SUMMARY The minerals in in the or quartz
4 in the is 8 occasional BONANZA 45
in the is 8 occasional BONANZA 45 along of in ores therefore chalcopyrite to 46 1922,
5 to the was the collected mine gal
to the was the collected mine galena BONANZA \ when with of MICROSCOPIC \ ORES \ \ 1.
6 exhibited. frac contacts from \![exhibited.
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\](839568/exhibited-frac-contacts-from-relations-c.jpg "exhibited.
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exhibited. frac contacts from \ relations & C. the 48 CONTRIBUTIONS 3. all I FIGURE
7 sphalerite, appear much BONANZA 49
sphalerite, appear much BONANZA 49 with I 5. the identical 50 characteristic I FIGUR
8 E sulphide-rich white 10 BONANZA OP
E sulphide-rich white 10 BONANZA OP 51 sparsely mineralization. the traversing O.I FIGUR
9 E 52 of fine-grained from similar
E 52 of fine-grained from similar LOW-GRADE With from average sphalerite, the SHALLOW
10 Ores 1. BONANZA 53 rich waters. in
Ores 1. BONANZA 53 rich waters. in the sparsely I FIGURE 54 cate are original r.^s
11 1 j (hypogene), and all a Jill llsi
1 j (hypogene), and all a Jill llsi 0.1 FIGURE higher This i^ . 'King,. 170, BONANZA OF 5
12 5 In has galena & Norcross L I FIGU
5 In has galena & Norcross L I FIGURE rate sulphides in the shown This 13 56 the the
13 The extreme The crowded 14 Qg. 19
The extreme The crowded 14 Qg. 1918. p. BONANZA 5. rich to the shown hydrogen of MI
14 NE The the large the 58 1922, Trou
NE The the large the 58 1922, Trouble the 19 18 BONANZA 59 the Analyses Hot [Tempera
15 ture 1, Reacting value. Per 18.7 lev
ture 1, Reacting value. Per 18.7 level, Pa Mg........ 131.0 Reacting Per 27.4 8 6 60 CONT
16 RIBUTIONS Analyses Continued. Descendin
RIBUTIONS Analyses Continued. Descending [Analyst, AhOs- YtoO».. 7.1786 As Radicle. }so Cl..
17 ....... 534.9 0 Reacting 23.3 8 Per
....... 534.9 0 Reacting 23.3 8 Per Per Metals+strong The graphically. the the 20 BONA
18 NZA 61 The alkalies The the Alkalie
NZA 61 The alkalies The the Alkalies ________________________________ COMSTOCK + 57.2% ,__
19 _____Alkalies /4 CAN , + + 2,250-FOOT _
_____Alkalies /4 CAN , + + 2,250-FOOT _t_+ + + t v v 2.6% v Alkalies30.6% "" M/ZPAHMINE +- TO
20 NOPAH, + + /M-«//«wy/5/r ,Akaliesll.
NOPAH, + + /M-«//«wy/5/r ,Akaliesll.2% i____________Earths fv VVv C%% V Strong Alkalies by
21 strong FIGURB litized 62 CONTRIBUTI
strong FIGURB litized 62 CONTRIBUTIONS fig. Ouray 0.37, CENTRAL V v 13.0% v Metals Oo°
22 0 0 0 0 O0 Hydrogen WESTEND Alkalie
0 0 0 0 O0 Hydrogen WESTEND Alkalies t++ +) Hydro j v v v «v 7^/7 0.6%-\ o o free GENE
23 SEE + + ^9A%" + + 2.2 V v 4.4 V V Me
SEE + + ^9A%" + + 2.2 V v 4.4 V V Metals OQ ooooO oQ6.2% o_ooo OOOQO Strong Alkalies by s
24 trong FIGUBH At 23 BONANZA OF 63 as
trong FIGUBH At 23 BONANZA OF 63 as as water CONCLUSIONS. The of of certain formations,