ECONOMIC GEOLOGY. 
ECONOMIC CONDITIONS. 
43 
The various camps herein described are connected with supply 
points by wagon roads, most of them surprisingly good considering 
the fact that many are less than a year old. Some mines have a small 
but for the present sufficient water supply near at hand. Other 
lprite 
fl\0 
G« 
3\i 
^ 
+2s. 
Xf 
N> Mex 
y \ 
■P 
Quartz 
veins 
BlaKes jr 
Camp 
w 
ACactus Pk 
Silverbow, 
Georgt -J Wateiy^ 
Spring? 
CohralSprja'" 
& Q Cactus Springs 
*4p 
%- Antetope Sprs 
Wellington j^ 
nGold Crater 
;0^° 
mteCru>to& r> 
Springs w • 
Quartz Mountain 
Camp 
Tolicha PK \i 
Indian Ranch O t) Howell Ranch 
t *Crj/$baL Spr ^s^ 
— Nicks Hot SpriiwS, jjf >"/, 
r IndumSpr^- <f 
Rhvolite S> £\ 
Bullfrog ° £/' 
> RAR F MTU 
Chloride 3 ^ O 
a Cliff .j. \ ,5 
LogSpr | 
Belted Pk 
>Gold Reed ^ 
Kawich PO 
';WSIU'ERM1N£ 
^ ng€ 
Fig. 4. — Economic map showing areas of altered Tertiary rocks. 
camps are compelled to haul their water from springs or seeps 20 
^miles distant. Pinon and juniper are rarely of sufficient size for 
mine timbers, other than stulls, but pinon makes an excellent fuel. 
The power question will probably be solved at the other successful 
camps, as it has been at Goldfielcl, by the transmission of elect ru 
