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geothermal resource potential of the safford-san simon basin, arizona

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(X)<br />

N<br />

BOUGUER GRAVITY MAP OF BOWIE' AREA WITH<br />

WATER FALLS AND PROFILE USED TO MODEL<br />

'I I<br />

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t--"-'--t-'<br />

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t~v><br />

Center<br />

LOCATIONS OF GROUND­<br />

SUBSURFACE STRUCTURE<br />

GA<br />

<strong>of</strong> Bouguer Gravity<br />

Anomaly East <strong>of</strong> BOWIe<br />

Bouguer Gravity contour<br />

Contour interval is 5 mi lIigals<br />

1975, Ground-water fall (See<br />

Figure 34, Ground-water Table<br />

Map <strong>of</strong> <strong>the</strong>.Bowie area,)<br />

A<br />

AI<br />

Gravity pr<strong>of</strong>ile used to model<br />

subsurface geology, (See Figure 31<br />

Gravity<br />

DATA<br />

Model <strong>of</strong> Bowie Area.)<br />

SOURCES:<br />

(I) 'GRAVITY-Wynn and Dansereau, 1979.<br />

(2) PROFI LE - Eaton t<br />

1972.<br />

(3}GROUND-WATER TABLE -Information<br />

for 1975 j Wilson and White, 1976.<br />

BASE:<br />

N<br />

--160-<br />

-r-<br />

US, Geological Survey 1:25Q!000, Silver City, 1970,<br />

SCALE: 1:250,000 0 6 Miles<br />

I I I « , I I<br />

Figure 32.<br />

Bouguer gravity map <strong>of</strong> Bowie area compared to' locations <strong>of</strong> ground-water falls.

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