geothermal resource potential of the safford-san simon basin, arizona
geothermal resource potential of the safford-san simon basin, arizona
geothermal resource potential of the safford-san simon basin, arizona
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Memorandum to·· Dt"ljI<br />
Ohapman<br />
copy<br />
SUBJECT I<br />
'I'BIP TO THE SAN SIMON OR Ft1NK WELt.<br />
On ju.l1 25. 1940, a.t <strong>the</strong> invitation <strong>of</strong> Mr. G. II. Ebeen, Bnd for<br />
reasons explained by <strong>the</strong> attaohed oorrespondenoe, I visited <strong>the</strong> San<br />
Simon or Funk Wolle<br />
Upon aniTUg <strong>the</strong>N I found Mr. Ebsen TOry' willing to turn1ah<br />
samples ot drill cores and cuttings and all poatdble information for<br />
our reoords, He seemed well plo8.80d that <strong>the</strong> Arizona Eureau <strong>of</strong> Mines<br />
had responded promptly to hie inntat10n to via1 t <strong>the</strong> proporty"<br />
This well 1s trIO mUos west at San Simon, 200 teet trom <strong>the</strong> 9 E<br />
Gomer. Sec. 27, T.13S., rooE•. The following 1nformation ooncer:n,....<br />
1118 it was furnished b1 Mr. !J,'b8lJJ1,<br />
The drilllng has beont1naneed by <strong>san</strong>e 1600 people who havD 1n<br />
'fested sums <strong>of</strong> ~.OO to $100 eaoh. Started in 1928, it hs8 reached<br />
a depth ot 6657 teet at a coat <strong>of</strong> approximatol1 $200,000. S. W. Funk,<br />
ot Oharter Oak, Calif., is trustee.<br />
Mr. Ebsen suggested that U;r. Funk would gladly furnish <strong>the</strong><br />
. Arisona Blreau 01' .Mines nth <strong>the</strong> drillers' log. Until we obtain that<br />
10it we' have <strong>the</strong> following statements which !l.r. Ebeen took fl'om memory:<br />
Valley 1'111 material, eons1st1ng ot more or less firmly oonsolidated<br />
gravel, saud. and s11t. was penetrated fram <strong>the</strong> eurfsce to a<br />
depth <strong>of</strong> soms"hat mOM than 2000 feet, below whioh stratified <strong>san</strong>d...<br />
atone, oODglomerate, arkose and shale (<strong>of</strong> ~retaceou8 aspeot) have<br />
continued to ,.he bottan <strong>of</strong> <strong>the</strong> hole. Abundant artas1an water Was<br />
enoountered above <strong>the</strong> ~retaceOuB, Q~oo1al1y at a dopth ot 1260 feet.<br />
In <strong>the</strong> lowest 200-300 teet <strong>of</strong> <strong>the</strong> hole this water haa a temperature<br />
<strong>of</strong> 274 ,<br />
0 J'.<br />
Mr. Ebsonstatas that 011 <strong>san</strong>d was encountered at 6643-6647 feet.<br />
and that gas which burns 10 feet high abavo <strong>the</strong> collar is produced<br />
4uri~~iVabb1%l£'<br />
CONCLUstONS ~ Possibly <strong>the</strong> 011 <strong>san</strong>d is genuine, -Qo6 Graph1ta dllS'"<br />
!,oeitJ CJoaur in <strong>the</strong> 8.retaoeoug ot <strong>the</strong> Chir1aahua rl~ountaina, soma 14<br />
milf'l8 farthor south. On tha o<strong>the</strong>r hand, 1t oannot bf3 deniod that<br />
such hot water (274 0 F) would stew oonsiderable grease <strong>of</strong>f <strong>of</strong> GOOOfeet<br />
ot drill oable.<br />
The drill oores given me by Mr. Ebaan arc <strong>of</strong> rock ot ~etnceaus<br />
aspect. Heret<strong>of</strong>ore, W8 had no proot ot <strong>the</strong> presonoe ot this formation<br />
beneath <strong>the</strong> San Simon Valley.<br />
Although this rock 1s not unfavorable, it is 1mpoonible to predict<br />
if or where favorable 011 struotures may ex1at in <strong>the</strong> tretaoeOUB be.<br />
neath <strong>the</strong> valley fill. From a oammaro1al standpoint, <strong>the</strong> search for<br />
oil under such condit~ons 15 a wildoat venture.<br />
To be ad.ded later: stayanow1s rSJ)ort on <strong>the</strong> fossil fragments<br />
in tho drill corea. .\lao H!O analysis.<br />
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