New CONTACT INFORMATION Mining Records Curator Arizona...

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Arizona Department of Mines and Mineral Resources Mining Collection

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CONTACT INFORMATION Mining Records Curator

Arizona Geological Survey 1520 West Adams St.

Phoenix, AZ 85007 602-771-1601

http://www.azgs.az.gov [email protected]

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07/16/92

ARIZONA DEPARTMENT OF MINES AND MINERAL RESOURCES FILE DATA

PRIMARY NAME: TENSTRIKE

ALTERNATE NAMES: ARAVAIPA LEASING CO. KLONDYKE MINING CO. LONE PINE LEAD DEMPSEY CASSIDY ARAVAIPA PAT. CLAIMS MS 1783 RUBAL STONE

GRAHAM COUNTY MILS NUMBER: 165B

LOCATION: TOWNSHIP 6 S RANGE 20 E SECTION 17 QUARTER S2 LATITUDE: N 32DEG 54MIN 22SEC LONGITUDE: W 110DEG 19MIN 29SEC TOPO MAP NAME: COBRE GRANDE MTN - 7.5 MIN

CURRENT STATUS:·· PAST PRODUCER

COMMODITY: LEAD SULFIDE SILVER GOLD COPPER SULFIDE VANADIUM SILICON QUARTZ

BIBLIOGRAPHY: USGS PP. 461, GEOLOGY OF THE KLONDYKE QUAD, 1964, P. 146

ROSS, CLYDE P., USGS BULL. 763, 1925, P. 88 ADMMR TENSTRIKE MINE FILE AZBM BULL. 156, AZ ZINC AND LEAD DEPOSITS,

PART 1, 1956, P. 63 . ADMMR U FILE FLAGG, A.L., VANADIUM REPORTS 2, 1942, P. 4 ELEVATORSKI, E.A., AZ INDUSTRIAL MINERALS,

ADMMR 1978, P. 34

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TEN STRIKE MINE

Imperial Group (file)

V-II A. Lo Flagg vanadium reports

USGS BuIlD 763 poSS

GRAHAM COUNTY

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, -.r~,~_~~,~._.::~'3./~-;"" \,/

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TEN STRIKE MINE GRAHAM

This property is idle. VBD WR 9/25/75

October IB t 1943

Mr. W. B. Goh.1:'ing R:1K.O. Mine Lot~U Division, 325 Heard Building Pboeni;!(, J~rizona

Dear Bill:

Pleaseref'sr to my letter 01' Sep·tember 30

regarding -the 1011@ PinoMine ..

application.

YOurs iffJry. truly J

Ooupal, Director

J:3C:LP Ene.

,L",

-\

.,"' j ., :1

I~

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BFO \ M:i,ne Loan Di, v$..a1 on 325 Heard Building Phoenix. Arizona.

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'::;,: ,;.:~"

report on the Lone P1n~ Lead Mine 'lioietherwith blue prints

Qt the workings. by ~draw~aoferlane. 1 understand that- an

app11oation for a loan has been submitted by C. W. Oass1df

_ to YQuon thte propel·ty f

I. S. Ooupal Director

• i I

\ DEPARTMENT OF MINERAL RESOURCES

STATE OF ARIZONA

FIELD ENGINEERS REPORT

Mine Lone P lne Date Sent 27th, 1943

District

Subject:

J

Klondyke

. Dept. Of Mineral Resources; Phoenix, Arizona.

Gentlemen;

Engineer~ A. Mac." D1P1. M'"lftll ftlSOUItCES

R£CElVED '[~ nnrO.3

About two weeks ago, I malled to you report and sketch of' C.W.'Cassidyt s LonalPine mine.

..-----.-;:--_"..> ___ N>

This Gentleman malled his application Into the R.li'.C. Off'iee,li but did not do as I told him, that is get' a copy of the report and skete h from you and attatch same. to his application and hand the completed matter into the R.F.C.

Will you please loo~ into the matter and see that the documents are a.ll attatc-hed and again glven to the R.F.C •

Tomorrow I am completing my examinatioll of the Manganse up on Cherry Creek for Hutchinson, and followIng this have conslderable wo"rk ln office for VcFFeo of Bisbee, try1ng for Special premium.

Will not overlook the Councll meetlngs of' Winkleman, Ray and Florence, these will slow up the office work, this' week.

Very trUly yours.

A.. Macfarlane.

/

Mine

District

Subject:

DEPARTMENT OF MINERAL RESOURCES STATE OF ARIZONA

FIELD E~GlNEERS REPORT

Lone Plne' Date Sept. 7th, 194:3

Klondyke" Graham Co. Arlzona Engineer A. Maofarlane

c.w. (Pat) Cassldy and Hale Owners. Appllcation for an R.F.C. loan

Gentlemen; SEP 8 1943

: L O't!-i Enclosed find report and skete ma-::p~p-e-r ... ta:-m g

to the Lone Pine Lead group, on whlch Mr Cassidy is seeklng a loan.

Klndly oorre,ct the spelllng and wr1tlng of the repo,It, and oopy map, ln order that our Department may ass1et th.ls mlner.

other reports follow.

Very truly Yours.

A. Maofarlane

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LJEPARTMENT OF MINERAL RESOuRCe:S STATE OF ARIZONA


Mine Date

District Klondyke or Aravt'l.1pa. Engineer garl lj'reemuu Husttngs

Subject: f~.eC(jnfrtr\:fc:t:i'on l'inance eorporation / 14ine l,oan

Docket No., D~lte ,ll..pplication Hecoived Date of' F:.teld E:x:amination Date ot Report,

l?hx 0-252 october 19. 1943 Oct{Jb(~r Lu 1943 October 20. 1943

1.. NI3lUe and addr{~ss of.' applicant t oorrespondent). Oharles w. 'Cassidy t Route I, Box 720, Globe, .lkrizona

:2. Cha:raoter ot pro ject and est imf.ftad cost thel~eof: • Pb.. Sin1< shaft 100 feet and dl'U't und~}!' 01(1 stapes, ~~5000.00

3... Location of :pro:perty~ .Aravail>f.l Mining DiErtrtat, Graham County· ~ Arizonn

4. Applioant- 6 intlil'est in or ownership ot property: Applioant is ODS of ,two partner's owning claims by lo(mtioll"

5.. Loan l'eqU(")st!:ldt :~5000.00

6. Loan 1"1300mlllended.: NOlle

7.. COllillients:

i~ ~ Added to tho docket is the rwlport of' A. Macf'a.;r'la110., ]\ieldE~ngim!lE:)r. Departm.ent of IVlinerul H0lS0UrC('Hh

B" Th(~ past shipping reeord is obscure, 'tb .. 3 only certailrby being the:t a very limited ·tonnago was produced from th:;.~ property,"

c. SanU:.lles 2, 3. and 4 show unifomn,ly satiafacimry yeJ,ues in lead, they are, howlilver. localized and <.nmnot b(~ repr'o:%,ntati-v'(:'1 of any grgat tonnago" Ore :possib1l1 ties to the rwrtl1 are limited within B. few j;~eot. of srurrple II), and to tlw sou'bh by a. pinoh and low vahws as ev1denc lsdby sampie tn. ~ .

Sampl~~ 1/6 in the South Tunnel aome 700 feet south"rly t'roru. the Ten Strike work ... ings shows 4 fH~t of 71>6Zfo lema ore in tho tace. It is this sl:lo:w1ns OIl 11Jhioh expand! ture is propos~,d.

D. Whih, the property is located in a well ll1illEn'alized o.1'@8. and adJoing a moderntely prominent past producer, it is not considerod tho:t ~)1ther pnysical Gaudi tiona (locution in respoct to end11nes, Htc,,) ore strength of ,l'Uinera.:Uze.t1on in the loor:tl 8.r(~a. to be explored justify recoDll:ncll1dation 01' this loan.

I','

Pa.ge Two

Fu:rthermol'e.Wllllssthe eXposUl.'e in the south tunnel develop€ls into a distinct shoot wi thin a lim;!. tad. llltl;}t'l3.1 diets.Twa the project \~o'l~ld I'dl. The reason being ~het funds would be insufficient to !,(,';l.lch the possible downward oontinuatiol1 of th~) winze shoat. In €ill, the risk applillar13 srEl~itOl' the.n oonditions or possible :production justify.

Eo.rl E'.Hastings Projeots Engineer

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( DEPARTMENT OF MINERAL RES<?URCES STATE OF ARIZONA


Mine Ten Strike Mine Date Feb. 19, 1954

District Aravaipa Mining Dist:i:ict, Graham Co. Engineer AXel L. Johnson

Subject: Field Engineer~s lIleport ---Information from J. F. l\Ydbom, part owner and operator.

Location being ia Sec. 20.)

Number of Claims Leasing Co.

Sees. 17,20 &29 ----T 65 ----R 20 E~ (main workings Go NW 4 miles on Aravaipa Rd. Go NE5 miles on mine road (rough)

5 claims ---unpatented, and 1 patented claim leased from Aravaipa

J I OWners 1 patented claim is owned by Aravaipa Leasing Co., R. E. calhoun, Mgr., Mills mag., El paso, T~xas. The 5 unpatented claims "' .. owned by thevKlondyke Mining Co.,

~J. F. Rydbom, and~Dale Callihan, Klondyke, Arizona.

Lessees and 9Perators· ,'heIUondyke Mining Co., J. F. Rydbom and ::£)lIe Callihan of klondyke, ArJ..z. is leasing the 1 patented claim from the Aravaipa Leasing Co., (address above) and owns the 5 unpatented claims. Their shaft is being sunk on this patented mining claim.

j principal Minerals Lead with high Silver values.

Number of Men Employed 2 men

production Rate No production at present. Operators are doing exploration and aevelopment ~ork.

Geology Vein about 10 ft. wide, with a good grade ore streak in same about 6 inches wide. Strike of vein N 10 deg. E, and dip of vein 76 deg. W. Footwall is diorite, and the h§llging wall is rhyolite. The shaft followed the footwall down at angle of 76 deg.

Ore Values 2 cars shipped from adit ran 15 and 17.5 % Lead respectively with about 2 oz. of Siiver. Most of the ore in the vein is too low a grade for direct shipping. . Operators are trying to developlllllDlt some ore, which is high enough grade for direct shipping.

Old Mine Workin~S One old adi t, about 600 ft. long, from which the 2 cars of ore were shipped. Opera ora have now retimbered this old adit, and expect to sink the shaft an additional 50 ft. in order to connect the shaft with this adit. 1 Winze, 125 ft. deep.

New Mine Workings One Inclined Shaft (inclined 76 degrees) sunk by present operators. ThIs ahaft is now 155 ft. deep. Also 165 ft. of <iBifting on the 155 ft. level (75 ft. south and 90 ft. north along the vein) .

present Operations Drifting on the 155ft. level in order to develop ore.

Proposed Plans Continue development in order to find some direct shipping ore. Sink the shaft another 50 ft. to intersect the old 3dit.

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DEPARTMENT OF MINERAL RESOURCES State of Arizona

MINE OWNER'S REPORT

Date ...... JJe.c. ..... 10.,. .. .19. 5.2 .•.............................

1. Mine: ........ ~ .. Ten .. strike. .. Mine .............. : .. 'In.t'.ormation .. f.rgm .. personal .. inspe.c.tion .. & .. .:f'rmn .. Qperators)

2. Location: Sec ............................... Twp ...... 6. . .s •............. Range ..... l..9-.. E ............... Nearest Town .. nond;y:ke ........... .

Distance., ...... 4 .. m11es ..... Direction ... north-west .. Road Condition .... .first .. 4 .. mile.s .. good., .... , ................ . then 5 miles north-east next 5 miles rough and steep

3. Mining District & County: .. Aravaipa .. Mining .. Di.st .• " ..... Graham .. GountY'.··.·.',."" .......... " ....... " ................. .

4. Former Name of Mine: ... ,,, .... none. .. ············,,···· .. ·,,,,.· ................. " ... " ..................................................................... " .... . {, " ' .... ' s. Owner: ...... IO..ondyke .. Mining ... Co .•. ; ....... JO'ondyke; .. , ... Ar.1ZQn& ....... : ...... ---.. holder.s··of···company··a-re

. (l)"IJ.C. Anglin, Tucson, Ariz., (2~lJ. F. ~dbom, Klond;y'ke, Ariz., and (3) Dale '---~- .j . . i··.. '. .1.' • t' . ~·······-oall· .han, ... IO.:<n-dy-n:e.; ... Arl.z •. ··----.. elosed .. eorpora ·];on.· .. ·········,,·····························

." h

6. Operator: ..... ' ...... .IO.:Ondy:ke ... Mining .. Co •. ,.?.the. .. owners .•... " ............ ~ ................................................................... .

Address: ............. KlonVyke.,. .. Ariz ................... ~ ................... c •••••••••••••••••••••• ! ............................................ :: ................. , ... .

7. Princi~l Minerals: ..... f. .. Le.ad .. or.es""~.""!'!' ... prinCiPalJJ': .. cer:uSsite, ... but .. .some .. .ang1esite..,& .. .galena.

8. Number of Claims: ........ , .............................................. Lode ........ yes ........................... Placer .................... _._ ... , ........... .

Patented ....... _ ..... _ ......... _.n~ ......... _ ... __ .................. _ .............. Unpatented .... ,_ .. ye.s ....... , ............ _ ................... __ .............. _ .... _ ... .

9. Type of Surrounding Terrain: ... , ............... V.ery·.rough .•.. and.·mountainous-............................. _ ................ .

•••••• • • • - - _. - - _.:. - _. _. - - • - - &, •••• ~ • "0- ~:"o .... _ .. _. -_ .. __ ---_. ---'~ -----_. ---- _. _. --_. _. _ ... -_0 • _ ••• Bo" • - •• ". - • - - -"'" - - •• -. - - - - - - •• - • - ~ ••• - •• - - - ....... - CIo- - - - - --. _. - - •• - •• -. -.: - -. -- - - ••• ________ - - - - _ -. - - - - --

••••• _ '._," • __ - - - _. __ •• _______ • __ • _____ • w __ - - __ "l_. __ ~ _____ --,-----. -----;.,.-.-_.- -•. --'to--"' •• ' _ ••• _".", • - ••••••• ~- - •••••• ;- ___ ow -. - - ~ -. -. --. :-- - - ,-.---,---- -: -. __ • _w • _0. _w, -- •••• - -- - ••• -. - _ -- -_ -,---- --.--.-,-"-

10. Geology & Mineralization: .. ~ ...... The ... V-ain-.is- .. a ... f:i&~u·re··ve-in-_~ .. from··l··to··5~·f.t.···widel.········The :strike isN 13 deg; W, and the dip is 75 deg.to·$*' The vein is principally quartz, which··c-ontains···t, he .. -ori·-miner·a;lg;.o;.;.··~ceru:ssite·····afig .. leai"te···· .. 8:iid .. g··:alefia~····· .. ·The···r-oi:)"twaIl"··is

'. " " . " . ,.

granite, and the hanging wall is rhyoli te porphyry". (also some diabase. and diorite .in ·the··f'"oo"twaIl"··of'··-ttie-·-veiil)···--··················· ......... _ ................................... : ... ::.: ........ -.~ ............. : ............................ -......... .

':'0 _ .. _. ___ ;. _ ..... _. _ ... _ ... _____ . __ .• _~ -'" _____ ... _. ___ .. __ ... __ .. _. __ .. __ .: -."~. __ 0_.· __ . ____ ..... _ . _ ... : .... __ .... : ... _ .w_.~.". _ ••. ___ • ~. __ •• ~ ___ ••• ; •• _.~ ••• o. __ • _ •••• ' _ •• ____ ••• ___ • ___ •••• _ ••• _____ ._

_ ... _._. __ ... _ ...... _-_ .. -..... _-_ .. _----.-----_ .. _--- ......... _-_ .. _------ ._------_._-.- .. -.- ..... _ ..... _-_.-._- ... --._--_._ .... _. __ ._._._._-_ .. _._----_._---._-------_ .... -.. -._---_ ............... -, .

11. Dimension &. Value of Ore Body:.: .... Or.e .. vein .. proved .. up .. for···9000._f~ ... 1n .. length .. by~ ............. :. tunnels and shallow open ·cuts.· Deepest workitJgs is a winze, 125 ft. deep. Width of .. vein ... l-.. to .. -5 .. .tt. ................... ····-········· ......... --.......... -............... -........... --............................................................................. .

'r 12. Ore "Blocked Out" or "In Sight": ........... V.e.r.y .. li.ttJ.e.~!':'.~ .. j:us.t .. a .. few..,:tD.ns ................•.................................

•• - - - - - - - __ - - - - - ___ 0. __ • __ • _. ___ .. __ ••• _ .......... _ •• _ ....... _. ~ •• _ ....... 0" _. _0 ______ •• ___ • _. ___ •• ____ •• _ 0_. _ ....... .:.. __ • _0 _0 ___ .... _. _ 00 _ ...... __ ...... _ •••••• _. _ ••••••• _. __ ......... _ •• __ •• ~ ...... __ ........ __ ••••••

OreProbable: .. :, .. Jfard:.t.o .. e.s.timate. •. , ..... May. .. be. .. as.,lIII1.Ch .. as ... '".aoa .. "tons •..........................................

• ____ 0".000_':"'_ •• _~~ ~ :. ____ 00. _.00 _ ••••• ___ • __ •••• 00 •• 0 •• 0_ •• _ ._ •• _____ ._. _. ____ •• ~'':: ____ 0. ______ 0 __ .00. _ •• 0. _0 ___ 'd'- __ 00 ~ ___ ._.0. __ • ____ •• _. _____ 0. ____ 0 _0_.0 •• 0 __ • _0 ____ 0 •• ___ • _0 _0 _______ .00 ___ ••• __ •••

-0 ___________________ • ___ ~ _0 ___ .'_0 ________ ~ _____ ~ __ ~ _____ ._0_.:'. _:.~ ___ •• _____ 0 _0 ____ 0.' _.0 ••• ____ •• _0.0.0""" •• ~ .......... _~-~-".- •• _ ••• __ •• _ •••• _ ...... _. __ • __ .~ ••• ~ ...... _ ............. " _. _ ....... _ •• _"" •• _._ ••••• ".

13. Mine Workin'gs-Amo~rit and Condition: ........ ;.; .. : ............... ~:.: ........... ; .........•. : ........................•....... , .......................... .

No. Feet Condition

Shafts ........ l ......... ,....... ··,,·,·.····)9::#.!-.. ·:···;····· ..... " ... I~;J.ined ... 7:r; .. deg!' .. , .... .c~ndition .. f~r, ............................ .

~ .. Winze ........ L .~.~ .. ~ ... 12.5 .. .ft ...... ~ ...... : .: ........ NeedS ... repair. •... :.:.srld ... to, .. contAin .. gQo.(Lbr.~.:.~hQWingli. ro·, p.

Tunnels ........ 2.............. . ........... 165. .. f.t.......... . ..... ; ... one .. 40··4.:.+.ong.,··.and .. .one.,:.l2~ .. f.t ..... ~ong ................ .

Crosscuts .... l.............. . ........... 225. .. f.t.......... . ......... X .. .au.t .. dr.1.v.en··a1smg .. :ll'efn-. ................................................... . . Stopes ......................... . uuu:uu.u .... u.: .... u·.····:·f:r· -0-"" - - - - - - ~"- r· _ .. ," •• _ ......... , ........... _":::". '." ~ ~ •• _. __ .... _~_. eo .. ~ ••• - .... _ ..... - ......... " __ e. _. ___ .. _ •• ~ ••••• __ •• ___ • _ •• _ •• _. ____ _

• _. _._. ______ • ___ • _. ______ ••••• _., •• _ •••••••• _ ••••••• ___ •••• - _",'. __ ••• ___ •• __ -0 ••• _______ • _. _____ •••• _. _ •• ______ • ___ • _ • ____ •• ____ •• ____ •• __ ............... ,, __ • _ •••• _ ••• __ •• _ •• ___ •• _____ ~_._ •• ___ ._ ••• __ ••

14 . Water Supply: ...... No.:source .. .o!.,:water-.. availa.ble···o;a···the ... pr.oper:ty ..................................................... .

" ....... -_ .. --__ . -_ .... _ ...... _ ..• _. _ ... _ ..•• -." ... _. --.... --.- -----. -. -- -........... .'. ~ -_ ....... --.. -., .• ~ •.. " ... .-.". -.. -- -~ ... -- -----.. -- -... ----.. --.... _e. _0'" ~ _. 0" •• __ • _ ••• _ ..... 0 .... ___ ......... 0 •• __ .: ............ ..

, .!r .

15.' Brief History: ..... .125. .. ft ..... tunnel .. driy.en .. by. .. Mr .•.. Dempse.;y: . .about .. 19.1Q ... or .. .l91S .•........ S.:J.nC.e ... that time'vseveral parties have had leas~ and have done some work on the property. Mr. pat··Gassidy··was··one···le.&ser·;···arld··Mr.···Rubal··ano·ther·.········Mr.··1luba1:··has:··a···leas&··in··192.,l .. and 1924~ Stone~nd Dempsey also operated property, and is said to have shipped ·200··tans··'df";·ore···ave·r~ging··JO",%u·1e-ad;···afid··yl:elm.Yig"·$15~"pe~··tm1···nrft.··························· ........ ,.: .. ;.

The present owners' took oVer the property in :Jan.,19'2, Mr. lWdqom workiiig·~a'1one';···Uritrr··Mr~·~al1J.nan··:rofiied"hiiii:·~r·irioritfiS···ag'o~""""Prese'iit"'operat;orEi"'nave':Diiil t ·4 .. ').lg ... m.t~~.~ ... 9.f .. ~9.~g, .... <:w.9.V~ ... t:tmm~;t..:·.AA~~d .. lO .. .f:\i.~.~' ... @.d ... tit.9P~.g ... ~g .. §.h?:.p.P.f!!.g ... 9.g ... §?*-~ ... ~~ .. ~.re, since taking over the property. . .. . : ................................... One .. car~oad .. or ... ore ... a.veraged .. l'l ... % ... lead, ... and .. the ... other. .. c.arloa .. d .. av.er.~ed 14.5 % le.ad. EIld about 2 oz. of Silver. Thls ore (tota1.90 tons) was shipped ~o ·tha··A.···S.··&·.···R.···Co·.···aib··E];··Paso,···Texas·.·· ............................................................................................ ~ ............. .

Operators now working 2 men cleaning out drift. After the cleaning out .. wortcifr··fii'iisned;.···tl'ieY'··expe·ct;··to:·rep·aU .. ··tl'ie .. 12:$ .. rt·.···Win;ze,···antl" ··trl'ter··tbat·:s-tope· some more'ore out. ' ." - _ ••• - _____ ..... _ ............. - •••• ---- -. --. - ..... - ___ e •• ___ • __ - __ " •• __ - • _______ ••• __ •• _ •• ___ •• _________ • - _ •• _ • ___ ........... _ •• _ •••••• _ ................ __ e •••••• ___ •• __ .: •• _0 ....... _ •• :. "~ •••• ~ ..... ____ •••••••••••

........... ---_. __ .. _--- .. -._-_ ...... _- .. _. __ .. _ ... -..... -... _.-.. _- ...... _ ....... _ .. _-.- ....... _ ...... -_ .. __ ... _-_ .. __ ._ ... _-.---- .. _- .. -......... _ .... _ ......... _----......................... _-- .. -..... -...... .

17. If Property for Sa,le, List Approximate Price and Terms: ..... .Qperators ... expe.ct .. :to ... w.ork. .. the ... mine ..... . themselves, but will consider sale of the mine on favorable terms • • - - - _ •••••••• - •••••• --- __ e' .~ _________ ........ _ ....... _ •• ~ ................................ _ ............ __ •••••••• _ ••••• __ ..... __ ........... _ ..... __ • ___ •••• ___ ... _ •• _ .......... _ .......... __ ..... _ .................. _._. __ ... _ ••• _ ........ .

- -., .. - "-

,:(j~,-- i'<lX.~Sl October If/: 1957. \1~~~~;1-~ - ,,- -L:~-:I:C - ~U:S~I~N:A:~ " r,,~ 11 It I ( ," )

~-~-Q-'".-n~lry.O\UV~~~~jt~ if the Emergency Lead-Zinc Committee's seeking relief for the lead-

~E?I' t'zin .... c:~!b.~S,f1.r-y and has it your authorization to speak fir you? ¥ EJ'

1

• "~

, p'."'--at Arizona Mines and Mills in the lead-zinc class do you control?

, . ~ I) .". l' " ' . ,,", .L,.,' • r:.. r>.l " ') J. •

~ I 1M ;S14d - /lAd"''>" I~Q c aIPflVe,p«, ~KtE4(I(gIrfJ l!a... ttyl'lk£/dlllrk£y /Y~/

1)----------------------------------------------------------------,~ich ones are operating? (1) ACt) Nt (2 ) _____________ _ ! ___ :.a:._.::o..:;z.:.r."'--___ _

/if not operating~ when shut down? (l)J"YLt' ttrS'¥f. (2)

~umber employed, prior to shut-down, in mine, mill or sections thereof producing I lead or zinc ores? (1) Z-wa C'-J (2) _______________ _

~umber so employed on January 1, 1957? (1) 414df~ ~umber so employed on October 1, 1957? (1) tftlJkC:

(2) _______ _

(2) ________ ~---------.:-~~~

Remarks Eo Reel) ro <;";11,£ ~ Q e eRe.; (~k..r Q.It Soe. "4''''* of hi/eN

. CeU'tr OF MdfJ;e/hlj Ltld:4#cI' f £A.tE,£ A:N/J ~tlLf/ P4?~G: ()J: !16'.ti?J..f )/ICf./G/f PNt~GS Fe-I{ 6!Pt-Q f SIt.. V t5,f I1A-IJ J"psJ' -rHY/e->!1 \#;14- N4t.-P

J.J' ~

Mine i

Ten Strike Mine

District Aravaipa Dist.,

Subject: Present Status.

\

DEPARTMENT OF MINERAL RESOdRCES sTATE OF ARIZONA


Date Oct. 14, 1954.

Graham Co. Engineer Axel L. J ohmo n

Information from Elton J. Kidd.

Note:- For infor~tion on location, ownership, minerals, geology, mine workings, and additional information -----see nw report of this property ~der date of Feb. 19, 1954.

Present Status Mine is now closed down. Mine x closed down a short time ago. Reasons for closing were:

(1) Insufficient ore reservev of direct shipping ore. (2) Lack of finances to carr,y on additional exploration work.

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May 6, 1953

Axel L. Johnson

{ .( J The Ten Strike mine owned by E;londyke Mining Co., composed of J. C. Anglin" Tucson,

,j Arizona, J. F~( iydbom, Klondyke, .ll.rizona and Dale Callihan, Klonc1yke, Arizona.

Operators nowwor;td.ng 2 mm and sinki'ng a new shaft on the property. This shift is

down to a depth of 85 ft. Operators expect to continue the shaft to a depth of

about 120 feet, the level of the 125 ft. tunnel on the property. Shaft is bel. ng sunk

in tle ore vein. No shipments are baing made.

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LONE'PINE' (TINSTRIKE)

;DATIll; . _ ~ D.Ar-sm:

c.vi~oe.Bsldy: Rt. 1', Box 72;';C ~144'. 'Idle ,

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Globe, Arl~ona " .. "\ ~ " ",

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~DEPA~TMENT OF MINER~L.RESOB~~ 1') ,ws Items , . i .., .. \ • ' • •

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.' . Date," June· 6," 1940. . j .... . -Mine Ten, .str~ke Ctr,oul?

Location :3uMi. NW c>i'.I<.:lonclyke

pwner Aravaipa. Leising Co •

. \&,~~r~~~. ., Under. 11ease ,·and o-otion ,to . i ' 'J ~.

Address

"·0,(j~I).l.,·Mgr. '

tMineSupt.

KlondYke • ..Arizona.··,l· . hi

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. i M"'. :;..e:;..·.n_·...::,E::,.ID--'-"-p""I9"'Y"'e:;.;·d"'·.''''',·:--' .. ·'''' ..... 3 ...... ·.''-· ~""'·'_·_:..;..·i"'-.·'.::.. .. '--'"-'-__ ·_·'-'· ::...>':..c'-.c.' ",,' '-'.., ", .... ':., .0

~P'rddtiction' Rahl ''''0' .. ' ':: J.

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• "~.: ' I' :"'_ ~'; ',,', ~\>"~'.~J:;:~ '>"I'~;":' ~:!."~: .. Signed ·W~. ~ .~ ..

(Over)

g preSe1itr~~pe:tiationS Drjf'ting ahead on ore at bottom ot' '#:I hze ,on le~ei @5feet belmv tunnel level.

New ,Work Planned ~,'",,'

E:x:;pectto "install tugger hoist and continue

drifti'or, another "75 feet' in: 'order 'to "get under'~the "shoot; 'or, ;'oi"ev:whi'ellh:as"b'eeri.'stop-,

ed on higb,e:clevels. r :,,:' :!:,~,T "';",;

Misel., Notes,

,Ag:uantity of', gob ,has been oleanedout '6f ,the winze and the old drii't,offthEFbottom,

and.,thei'ace,of,theprevious workifigShi:is

been exPosed. This shows an eighteen inch

"~reak of ~'rich ,1ead~sU:ver,jore" along'with "

aihder width of lower gra;de mi:llingorei,

",The, yeinViidth, is" sh°Wll, , by yarf.;ouscross

outs :to be eJ.eve:q. f'st9t ru,:td ,'more. ,D:I tt:l<mlt-- ,

ies due to b~d airi~ th~worki~s~re ex-

, pected to be overoome shortly,' and the, "

" ,():g~:t'ators. h():pe to ma.ke,~shi];)lD.enj; of' the higher grade ore in the near future.

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Mine Ten . Strike Ji'line Date Oct. 14, 1954.

District Graham Co .. Engineer Axel L .. JohnS) n

Subject: Present Status. Information from Elton J. Kidd.

l~ote;... 1''or inform§ltion on location, ownership, minerals, geology, mine 'Workings, and addH,ional information .. - ... --see rrw· report of this propert,y ynder date of Feb. 19, 1954.

l:resent Stat/us· Nine is now closed dOllfno Mine JE closed down til short time ago. i1easomi for clo'sing were:

(1) Insufficient ore res(u-vew of direct shipping ore~ (2) Laok of finances to carryon additional exploration work.



Mine TI;:1n Skike Nine Date Feb .. 19, 195h

District Aravaipa Nin:i.ng District, Grahan1 Co. Engineer Axel L. Johnson

Subject: li'ield JJ.:ngillecrffls lReport - ..... Inf'ormat.ion from J .. 1'''. }~dbom" part. owner and operator.

Location ~m:8~Sbdbc Secs. 17,,20 &29 ----T 6 S .. ---R 20 E (main workings 'being iB'~·SeO. 20.) Go NW h milsEl on Aravl:{ipa Rd. Go NE 5 miles on mine road (rough)

Number of Cla:tlllS 5 claIms - .... unpatonted$ and 1 patented olaim leased from Aravalpa --r- .. ,-_ t ~

I,eas::Lng Coo

Oi·mars 1 Patented cla.:l.nl is O1-Ined by Aravaipa Leasing Co.~ R. E. calhoun, Hgr~, r1illn j3Ycf€i., El paso, l'exas. The 5 unpa"i:,erl'ted cl~ims Ntcnmed by the Klondyke 1·'1ining 00., J. Fit Hydboffi)und Dale Callihan, Klondyke,l! Arizona. '

Lessees and 0 era.tors ~he Klo!l(\yke 1'fining 00., J ~ Ir. RVdbom and ])ale Calli.han of . Ion e, Ar z-. is. easing the 1 patent.ed claim from t.he Aravaipa Leasing Co., (addl'ess above) and Q'l;IDS the ~ unpatented cla:tms. 'rheir shaft. is being sunk on Nlis patented mining claim.

Princi!)al Hinorals Lead ldth high S11"lfcr values .. ,,' lIIO.. ¢! _.,.,. ."..,.

2 men.

production lin.t.e No production at prefJCnt • acive10pment 1,rork.

Operators are doing exploration and

Geology Vein about 10 ft.. lNide, with a good grade ore streak in sam~ about 6 inches ~,rido. stHkl'l of vein N 10 deg. E, and dip of vein 76 deg* W. Footli1al1 is diorite, and the h§ngine wall is rhyolit.e" The shaft followed the foot~.,all d<rr1n at angle of 76 dee ..

Ore Values 2 cars shipped from arlit ran 15 and 17.5 % Lead respectively with about 2 Oi;-of !:f{lve:c. !4oflt of the Ore in the vein is t.oo low a. grade for direct shipping. operators are t.ryi.ne to develop~ some are, .,hioh is high enou.gh grade for direct ship-pi~& .

Old Mine Wonkings One old adit, about 600 ft. long, i'rom which the 2 cars of ore were 'shipped. Operators have now retimbered this old adit" and expect to sink the shaft an additional 50 ft. in order to connect the sha.ft, i-lith this adit. 1 ~~inze, 125 ft. deep ..

New ~,!le Workingt'l One Inclined Shatt (inclined 76 degrees) sunk by-present. operators. T'I'us shaft is nON' l~~. ft. deep.. Also 165 ft. of dmfifting on tho 155 ft.. level ('75 ft •• south and 90 ft. north along the vein)

Present. Operatlop!l.. , Drifting on the 15)ft~ level in ol~der to devolopors.

proposed plans Continu.e development ill order to find SOTile direct, shipping are. Sink t:"he" shaft: "a.nother 50 ft. to ilrCersect. thel old tldit.

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Mine

DEPARTMENT, OF MINERAL RESOURC.~S STATE OF ARIZONA


Date fA ugust 4t h, 1943

District K10ndyke, Graham County, Arizona~ Engineer

Subject:

I

Examinat ion.

lOCATION SEP 8 1943 PIiOU1IX,

The Lone Pine Lead mine is situated hills of the Santa Teresa Mtns. approximately 8 ini1es by winding road northerly f'rom the store and Post Office ot K10ndyke, Graham county, Arizona.

The mining claims four in all, are a link along the north to west course of the big dyke and lode system called the GrandReef, and are about half way between Gra.nd Reef mine and the large group and mine workings of the Arivapa, now controlled by the Athe1etio Mining and Smelting Co.

Drainage of the sharply incised gullies and wash is towards Arivaps.' creek a distance of 6 miles southwest of the Lone Pine claims.

_PROPERTY,

Consists of four unpatented olaims, located' and held for many years by J80m<es~;,'Qu~'nn of K10ndyke, under the name of the Ten "Strike group and only within the past few years, these claims were transtered to Cassidy' and Hale, also fOrIDAr1y of the K10ndyke distriot, and now of Globe, Arizona_

PAST PROPUOTION

No reoord of the ores mined and sold from this mine, are ;,dn the possession of the present active OwnSI' PatJC _W~Cassidy of Route 1 Box 72 C Globe, Arizona, although several hundred tons

ha.lte been extra.cted , during severa.1 past act i ve working periods.

This.statement is ,born out by the stoping both above and below the working Adit, these stopes are gobbed and I could only roughly estimate the limits of' this mined area.

During former years the stopillg along the ,tunnel baok and from sub-levels and underhand stopes, for ab'Ollt lOO!~a1bng the vein

course is evident now; the width stoped being froII13' to over 6' •

Lessees during part of last year and early in 1943 again from a. depth of 125' in the Common winze, mined and shipped 4 or 5 car10ts; therefo're in order to determine the grade tenor of the ores, I took 6 samples and recorded the results on attatohed map.

The past low and erratio price for lead and the usual heavey smelter deduotions for lead ores, when added to a trucking oost to rail sw.1toh of about $5.00 per ton plus a rail freight of $2.00 to $3.00,per ton, only lead ores of a ~}lTalue in excess of $20. could be mine'dand marketed from this locality.

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bone Pine Pase 2·

MU·TE . DEVELOP!m~!

Principal mine workings are an ad:it tunnel fully 150' driven from just above the gulch floor and the eastern toe of the sharp

r:tdge, formed by the Reef' croppings an,d dyke matter. This adit cut, the lode, thence drifted in a general north 24 degree west course on the vein, for 115' to the end line of .the Lone Pine prope,rty.

Here at the end line a 2 compartment winze has been sunk,to a depth of more than l25'on the vein and drifting and stoping to some extent , carried towards the south back into Lone Pine ground.

It is stated that this winze is half on LonePine ground and half on the Arivapa, claim owned by the Grand Reef Company and has been used by both 'arties, in the mining operations below the tunnel level-

la The drift towrds the north continues on into the Arivapa

claim , evidencing the jOint USe of the Ten Strike tunnel, in the mining work conducted by the Grand Reef within that part of their ground contiguous to the Lone Pine on the north.

southerly some 600' from the _ portal of the Ten Strike tunnel the portal of the South tunnel is located, this near the junction of' the Cabin gulch and the main south gulch. The South tunnel has been advanced about 40' on the vein, which has a width of 3' to 4' in this sector.

In all there has been about "00' 'Sf mine development and exploration openings made on the Lone Pine property.

YEIN OCCUB,RENC[.,

As stated the Lone Pine is a 4 claim link in the long chain of claims covering the Grand Reet formation.

The bold dyke striking from the Laurel Canyon Grand Ree~ workings, along a course of North 20 degrees west for 11 miles

t,he northern end of this dyke and the vein system accompaning, together with several parrallel veins and others of a different strike, compose the Arivapa group-

Apparently this big dyke is mostly a rhyolite intrusive which thru superior force, broke the older stratified rocks along a nearly constant course, forming a major fault.

Along this fault line a.nd on the east slde of the main dyke body, vein or ore shoot s containing the l~ad m lneraliz:at ion have been formed, probably contemporaneous with the dyke intrusive formation.

Here in the Lone Pine ground, this mineralization of lead OCCUl"rs in a vein of 18" to over 6' in width, in fact ,violent vein swells are common along the mineralization of the Reef: the profundity of the ore shoots yet quite unde't'ermined. '

.RECCOMENDED.DEVELOPMENT - ---,-- .......

· .,

The South tunnel heading has exposed the vein to have a width of 4' between well defined walls; a fair sample taken here ast;1ayed 7.62% Pb. all in anglesite and eerrusite form.

This tunnel has better dumping spaO'e below its floor and head room sufficient for large ore bin, the road within 60' of the portal , and this south level is fully 30' lower than the Ten Strike adit.

For the above reasons, I reccomend a shaft to be sunk to 100' depth below the floor of the tunnel and from the bottom of the shaft, a drift elltended along the ve in, f'or the development of ore bodies and the ultimate connection with the end line wInze.

This proposed exploration consisting of 100' of shaft sunk on vein, thence 700' of drifting, should place in sight a sub stant ial tonnage of lead ore, and it seems fa ir to assume that the average grade of the ore shoots would range from 7 to 12% lead cOhtent.

The present adit and end line winze, to serve now in the production of the ores found to the south of the wInze.

Q.!,Qlogic Featqre.EL

Ore deposits in this region appear to have been formed after the intrusion of the batholith, probably begining in the Eocene and extending into the Mioeene ages; 'the rock movements takIng place during these changing ages and specifically the upheavel or formation of the Grand Reef dyke, provlded the elements suitab+e to the subsequent ore depositions.

Of course the ore agenCies along the big dyke were very varlable, the exploratlons of the past 50 years penetrating the Reef cropplngs, exposes mineralized sectors and other~ sectors

of the formation to be almost void of mlneral or ores.

The caslng rock of the east Wall of the vein wlthin Lone Pine w.orktn,ga, is apparently a brecclated Calcite, while the intrusive, rh,91ite and other igneous mat erials foming the Dyke proper, provided the west wall of the mIneralization.

More OJ" less selected or sorted ores of the Laurel Canyon or southern exposures of the Grand Reef'1 contalned several ounees of' silver in addltion to the lead..

The assays of the oxldized veln matter of .the Lone Pine group do not ShOW, pay value in silver.

Structural conditlons of the mIneral deposlts along the Reef, lndicate deep flssurlng, but erratic in l~ngth and subject

to vIolent swells and pinches affecting the ore shoots, making for breaks ln theIr cont lnuity.

Ingr9ss -:"Egresa

.The Lone PIne mlne is now reached by Auto from the Jct. of the Fort Grant road with hIghway #70 about 25 ml1es west ot' Safford,

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»thenc e south to Arlvapa creek 35 mlles, thence westerly to the st ore ana Post offle e of Klondyke a di stane e of about 10 mlles west of the Jet of the Fort Grant and the 'i'Vllcox roads t ln the Arlvapa valley.

All- thls dlstance from the Klonyke store to the main paved hlghway,' lsover cUrt road 'but .malntalned, over part rolllng terraln and (:Jome steep grades, followlng the road north from the valley.

The Lone Pine wQrkings are still about 8 miles northerly f'rom the store, the stub or mine road enters lnto broken terrain where sti!:,f grades are encountered, both entering the mine and 1" Fltuming therefrom; Howev-er th(\ road is pract leal for loaded trucks and subject to some lmp:i"ovement.

T'hls whole Klondyke Arlvapa dlstrlot, whereln are known slzable bodies of low grade lead ores and Zinc, shOUld be connected to the maln #70 hlghway at a polnt about 10 ml1es east of the e'oolldge dam and at an Indlan vlllage a few mIles west of the railrod swltch of' Calva.

A rough and poorly constructed road now extends from thleSan Carlos reservatlon vlllage, ln an almost dUe south dlrection to end at the Prlnaess Pat mlne, a distance trom the paVed highway of 10 or 12 ml1es.

Improvlng and cont inulng this road for 4 miles tu:rt'her' south, would end at Arlvapa vlllage and the lmpd'tant Arlvapamtn&s .. :_

.' T his road would pass neal" by potent 1al copper cl8,lmsYand

would be a most dlrect· route for ores to the Internatlonal. Smelter and a utlllty for l1vest ock interest, ln reaching the Glob~.~~~ta.ml and western cattle markets, by truck or train. .'

T he distance from the Arivapa mines to rail switch near Ft • Thomas, is more than 50 miles, whlle over the route herein proposed ,the rail facilities would be reached w1thin 25 miles.

Prior to the establisbmE;lnt of prt=lmiums on lead and zinc, these types of ore could not be worked in t his remote area, exe'ept at declded loss to the operator.

BUlletln #76'3 U.S.G.S. by Clyde P. Ross, publlshed during 1925 gives an approximate productlon for this entire district for a 40 year perlod of only 35,000 tons. ."

Slnce 1925 it is probable that another 5,000 to 10,eoo tons have been mined band dressed and shlpped to the lead smelter

at El Paso.

All thls is 10g1cal, as only ores of more than 25% lead sold on the general preval1ing low lead market, would leave some net smelter returns, with which the mlner could at least pay some part of the minlngc ost. The mineral exposures of t h1s district can be important if price and transportatlon f"actors are imp ro oved' •

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Mine LONE PINE Lll:.AD

DEPARTMENT OF MINERAL RESOURCES STATE·· OF ARIZONA


Date August 4. 194)

District Engineer

SubjeCt:

L001(i'IQl'H 'l'hil1J Lolle pine La&d Mine is! sit\l.uted in thewGate::rn i'oothilla of the 'Santa ~Ta!~asl!l. M'IH'h approxtma:haly .8 miles by wi:,ntling road northerly from the store and Post Offioe of. Klonilyke, Gr011$.1ll County, A:l:,:J,lltona.

The mining elaiNl8; i'oux' in f~ll,. are tl link: along the north to west course of the big dyke and lode system oulad the ill'and Reet, and tn'a about halt'way between Grand Reef l'(ltne~ and the l~trgCil group ::;m,d m .. ine wo!'ki1.l.{~s of th~ Ariva.pCt) l'l.OW controlled by the Atli8letio .Mining and Sm.elting Co ..

DI~a.1naga of th.e sherply iudsed. gullies t~,n(l Wa.Lib 1.e towHrdrJ A::rivt,qJO. oI·eek, a dig ... tanoe Of 6m1les southwest of the LonePine olt".1ms.

l.qOPER't~: Consicits of four lln.patented olaims. looated tLnd hold for mauy years 'by James (;tuinn. of Klolldyke tiD.der th~ ll~t1flO of'thtll T(~n Strike group and only within the :Pi1l)llt tew yetlX*s these oll1dn16 were transfel'l."@d to C:rAss1dy uXld Hl.lIle, also formerll of the Klolld;ykt~ district,· flnd now of Globe, Al':tzona.

l?A;.;lT :!:'n{Q:OtlCTION: No :J:'@oord of the OreiJ mined and sold from this mine are ill the .. t Ii F'Ii . r .... 1" *r •.. ' ,

possesl1.Ii<)1'! o:e th(~ pr€li:>ent active owner. (Pa.t) C .. W$ GD.~U31dy of Route 1, Box 72 OJ Globe, Arizonlia. fQltbou~;h sevliill'al htl.Xi.dl"eu ton{~ have been $',(tr,6;ctodduring several paiJt a.ot.iV~l 'N'orl:rlng periods ..

This ~rta:taHl.ent iaboru out by the s·toplna both. a'boveend below tllework1:n.g a.di t~ Theea S.tQ]:ll>.Hl el"El gObbQ(l and 1: eould. only roughly estilnate the li.mits ot' this mino('1 ar~u.

During :t~Ol"J'ilel" years the stopil1g along the tunnel back i;llld 1'rom ~.ub-16vds and. under4a.nd ~'\'tioP$$ fol' 8.ooutlOO' along th>:.>:t Veil1. ccurse is evident now. the width s"toped h~lll.g from 3' to ovex' 6'.

Lessees du.1'ing ]?flrt of la~t ye$.X' mid. early in 1.943 aga.in i'l'om. adf;lpth of'125' in the. COIllJnOll wj.uze milled ~Hld ship:Pfld 1..." 01"5 oar lote; tht'IJrefore 1n .order to d@termine

., the irade tenor of the ores I took (, Slil:filplEll3 aud reoorded trm re.~:;ults on e.tta(lhed J:lVip.

The past lou all(l erratic :pl"1oe :t'Ol' lead unO. the usual.he&vy SI~eltel' dedu.otions for lead ore.s, when addad to atru{Jl<ing cost to 1"a11 Bwit.Qll of' about ;f5.00 pel' tOll plus til r~dl tre1g11'G ot $2 .. 00 t;o $:3.00 pillX' tOll. ouly lead 01:'0£1 of f1. value in excesa ,Of $20 could -00 tuned and l!1arketed f'rom tllia loc~li try ...

MINl!: DEVEtOBU .. 1IJT: Prine! "'11.\.1 minf.b workings o:i,re ~m adi t tUllllel fully 150' driven -W_ I..". .1"

from just above ·~.he gulch floor and the "I\~$ter.n toe of' tUQ l:~ha:rp l~ldge for:madbl the Reet t:l1.'C)ppings and dyke matter. Thbadit cut the lQila, th~~loe dri:ttsd in a gena!:;, .. l north 24 \i.agrea 'Nest course ou tll"";) vainter ll5' to tbe end. line of the Lone Pine l)l;'o;perty II

Here at the end line a .2 oompartm.<Jrlt "vinze has been sunk to a depth, of .:more than 125' on the ve1.n and drifting and stop1ng to sO<"tle extent qo.rrlfldtowards the. aouthback into Lone Pin0 ground .. ,.

It is stated t,hat this winze :La halt on LonePine ground and half on the Arlvapa cl~1ffl owned by the GI'~nd R0af Oomparqr and h~lS been used by both 'parti(~s in the mining OPi.1l"<lt!Oru9 b~QW th.o tunuel 1evo1 0

ThtSi drift towf;irds 'tu@ nOJ~th continu.(lls .on i:n:to th{~ ';~r1vapa, olaim. evidenol:ng the jointu.1'b\S of thE) 'rl~tl StrIke tu.nn~~l in th~~ mln:tng work conducted by the Grmld Real' within that :pen.,"t of thai r gl'oUll..d .Qt1niiigu(1i,l.S to the Lon~ Pintl on th.~ north •.

South6J:rly, f~Olt1e 600' from. th,~ .portal of the Ten Strike tun.nal th¢ portal 01' th$ South tuxl.1'wl iel loc()I,te(l, thiB nOla" thf.~ jun~tlon of the Oabill. gulch and tho !!H';\in I~out.h gulch. rrhe Sou't;h tunnel h~i.fJ b6(~n advanced ~~bout 40' on the ,rein. which haB a width of Jt to I+~ in thilil ~!Jeotol"~

III ~ll theX'$ has been abCll;li;; 700' of mine devalo:pm.~:nt <ind explor1.;ltiol:l open1nga m.ads on the Lone Pine p~operty~

VEJ:N OCOURRENCE: M~ rjtf~t$d the l,on~it Pint)) is ~, 4 olaim link in t.he long chain of' . _ 1 r I .. j~ •

claims ($(Yrter1ng th(~ Gl":0.ncl R~~ef' f'OI'j'('jat.io.rh ,

The bold dyklS tStrlk1llti£; :t:l.'OlA the Laurel. Canyon (lr's'nd Reef" wo;rkiw,J;s) along a Qoursa of llol1th 20 desrf.~es west for 11ll1.i1es th(~ nortl'H:n;o:C.l and. of. this dyke end the Vt3in. system mooompm'.l.yirl/i;, 'tOJ;1;et;hl'~r with aevex'al parallel 'VeiXH) lind others of a different st:r!ik!i1.lj COl.'llpeee thei\r'iV~lP~t grClUl,h

AIllPa.rantly this bi~ ~1yke 1s mostly .~ ~rhyolit& intr"llsive wl'l.ich thru suporior f~o:roe. broke the QldtUc~ stl'at1tiiild :rocks along a nearly oonat1l:ntCQUl"t:Hil t i'ol'mtnga ntt.1jor f~tl.lt.

Along this i'trul t line and 00. the Glast side G.f the main dykll'~ body, vein or 01'1$ Shooti~ containing th.a lead :llliner'f.41i :t,!i;l'ti on h€lve beon :t'o:r.!t!f.Hl ~ propably con temll0ranaoUI), with thEY) d.yk(~ it1.truaiye formHtion.

BIn's in ~€:) Lone Pine gl"ou.nd this :m:tll(.~:r.alb,ation ot' l.ead oocu.l'sin 8. vain 01,' 18" to over 6' in Width, infaclt, violent vein awe!U; aI'tll oommon ~tlong th<\) minel"f4.!iZt'iltioll of the RI)ef • the p:ro1"uml1 t;y of' t1H:' OX',!! sl:\oot$ YGll; qui ta undE1'terlllined.

RliiCOMMillNDEl) DlllVli.'LOFMJ4"aT: The .Sou th '~ullllel hCll!l.dill~ h~lS exposed the v6)in to have n w1dtJi of 1..' btlJtiFf€Hilli"";;rl 'le:f'ill~d wa.lla. '.A fa.lr s8'lIlJ)le takerl here 4iaem.yed 7.6~ pb", all in fmglesl to and cel'l'Uslte ·tOlna.'

This tUn:I1Hl hat.~ bet tel' d:wllping s:pa~e belo¥f i'IH~ tloo.'r l'>fJ.t'i head room. f5u.tticient i'o~ large ,n~e bin, th~ :road within 60· of ·r.hepOl.·tal~ and tIlt,s) t:lQuth lev(ll hl 1'ul1y .30. lOWIUl( thi:'lt). ·th1~ '1:(»1\ Strike !;ld.1 t '"

]'orthi$ a.Dove I'aa,IJonf!l. I reoolllOlend a al'uift to be ~.n.Ulk to +00' d.e:pth bdow t.'h., tloor Of tlHj tUJ.11l01 and trom tha boM;ol'll of the sha:t~t t a drift extended >J.lo.ng the V(;'Iill, tor 'hh(') deV61opmen.t of' or@ bodll'$f~ idnd the ultimate conJ;l.'!H}'tion with tho end lit).e wil'l.\?;o .•

l'his :Pt'C\PQ~H'~d eXpl01~!i'l.tion consl~lrting' of 100. of shat't Bunk on velin. thence 700' 0:1: d.rittliD.e.;. t~hc)Uld XJ'la,oe in sight &.\ ~u'bstfmtiul tonnage of' lead ore. ~i\Ud it fiElerllS

fair ·to (l.8HI'Ul'll£1 ·thl'At the u,ve:rllge gr£l.de" of the ot'1!; lShoot:~ would. rlAngs :frolll 7 to 14 lead content. ' .

ffhe :present ad.it end end line winze to aerve now .in t;h~j :P'X'odllotiOn of.' the ~ras t'ound to tJ1f) south of the WiUM •.

q:1Ji91&O!(j .]'E.t}~qR1Ci:~; Ore depoilli tlil in '\ihil~ I'egion €).PJ;eu!' to haVG been fOI'llled after the intl"llsion oibho Ot'ltholl th. probably beg:iU3lil1k,} in. the .iSocane and ext0nt1i~ into -the Mioeexl,e ~013. TtI,a roek mevmu,ents taking pleul€l dud:nt; thSh1$ ohanging ages and speoli'ically tbo upheaval or tOl''1Iultion of the Grand R€lt1l:f dyke provided the elements :eui tHbla to the £)\,,! bf:>equent ore depoaitiona,

Of coux'sa. tb0 ore ageuoie[~i\lil.ong the big (lyl{l;! '~1a:re v~,ry variable. The e:xplo:r~l'\,iOnt;,

of' thc~! llf,'.st 50 yaHr~:, peur.:rtrating tho Reef cl"ov:pint~s 8:l;pOSe In.ill(!!l'ttlizad sectors ~md oth.n~ s6c.rtorf9 of the x'orms.tion to' be almof.$l't: voidO:t> miner~ll or 01"6S.

Tr~i-~ ¢t1.$!ng :rock of tIl'S 6t\St \\1811 o:e th~ viJ:)ill wi thin l~one Pina workings 1 s appa.l"ently a brtl>eoieted (i1li.lcHe, '¥1hile tho intrusiv@ rlly(-,11te IiInd othiill" igneous mater1al;'il :forrlling th(j d:yk(ll proper pro'Vi(led the wealt t'1al1 of the mineralization ..

More 01" 1«:$$ !!Joleoted or sorted. ()res of th.~ Lf};urel C!&nyon ot' south~:r.n expo,sures aI' tho Grtmd. Heef contained. /it6verfll OU!LOIlS of s:t1vor in additiOn. to the lead.

The a(;H:;l;:;.yJi~ of the oxi(l1z.ecl vain Illl;1tter of tlui Lone J?1n~l S;l"OUp do n.ot show pay vuluf.:) in sil"~r.

StrU(fl>ul'ul cOl'l.'ii"ttons of thellliu,iH::'sl d,eljO$i1:a~ a.1Qng tho Re$:t' indlo1it't;e deep fissuring t but l~l·r~lM.e in length a,ud f3Ubj(~ot to violent $w$118 8Jld. .pinohes affeotillS the Ol"e ahootrll J lll~.1t:tng for breaks in the! l' continuity.

l~q~s'"';Jjpn:E~]?; The LoJJ.€! PinE) nlill~~ ie now reacheti by U1.l'to from th.e Jot. of. the ]"Ol't Gr<mt rOI'ldw1th Hl(~hway #70 f:i.bout 25 mile~~ west of SatfaX'd. theneo south to Ariva.pl'l o:ree.k 35 mil61~:» thiililce 'wef~t(j:rly to t,he $to:.r~e (.,;n.(~ Post Oftice of Kloudyke. a di.6t~moe 01' f:loou.t 10 il1il~a 'Nest ot th!~ J ct 0 of ·th;i) .For-t Grant and the Willoox 1'olll.o.l3 i:o. the Ari'lfH .. pa ~tll1ey.

All 't1lit~ distf:ln00 front th{ll Klondyke stol'(ll to thBt11<'lin paved. h.i{.;;h.V1l\Y 1(3 over dirt l'OI1:1d but !l'1Birtta1ued ovel' DHrt rolUng tot'r~\in and SCIlla steel' g:t'e.d.~h~ following the l"oa.d north from. the valley_

The Lone Pine Vlorkings are t:diil1 about a lltUaa llorthel'ly i'roln th6 Btora;thl."J t:rlmb ot' ~"tt1nt~ roadenteril into bX'okoll taX-rain where alt.1:!t grE\tleg f.t:L"a <:lttcQuutereli, both el1tiS'l'in.g ·tih~) rubie and l'oturning th\u·$from.~ However. the .r'oadL':!. p.raot1Q~tl tor loaded tru,($kFJ €cud $ubjeot. to somr:~ improvel'fh'$ut.

Th1e wholr"Klondyk(;'l Arf.rlln.:lp~~ d1str1c'h ~ 'II/herein are known ai 'Zisl'iJ.lble bodlo[l of lo'~:\! grada l$ad orea ftl'}it z.1tl~ t $lhould. be Qonne~ted tQ- the mdn {nO hi~ghl!i&Y at a pOln:ti abot~t 10

. rnile£.. eai':lt Qf the Ooolidi$e clru:n t'l.l1d..a·t t;;<Zl In{ti1i'~u yillage a few miles W0fJt of the l'l:tilroflld awi thh of Oll'!.l Vth

A r01.1gh ~lIldpoo1;'lY" oonHtruoted l'ofi.d. !lOW G:)tt(;)ll(\~1 :t'rOtll this i3en Ci&ll'los reeervati.on vl1la{{t) in an Illmost due 8ou'tih di:reQtioJ.'i. to t)nd at th~l Pr1noe~H:l ~at mine. a distan<:e trOl'll tho pav6l'd highvlay ot 10 or 12 rnl1aslt

Impr'ovini?,: Ilud (~ontin.ulug thi:lI x'oad for 4 ml1e@i'urther Iilouth would €Iud at Aravl:lipa village and the i:t1l:pcrrtant ArlRlvaipa mines.

This roe,~t would pass lllC)61"by 'pQtenti~l ooppel" clnims tlt'\.d would be a most direot route tor oras to the Il1ternatloIlHl Stnel tel' and, a. utili tJ:y for, l1ve~ltook inteNst in reaoJrtng the Globe~U,t!J.mi ~tnd western cat'blema:.l'.'1r.ets by t).'\101\ oX' tr~~ln ..

The l'i1l!rlHlll.Oe from the AraV8.1p$ min.es to rail SWl. iH}h IUJU,!' Ft. Thomas is lllorethan ~O milil!ll:1. whIle over 'hIli;} rou,t~ herein P:t'ol}OBed th~rall tl~eili tias would bel reached within 25 l1111$$"

Prior to :t;he ElsttibliahJfhDu'C of ~n:'$m:tumB on. IlDud i5.ud zi~'w these typell'J of Ql'11} could not b~ worked in this rBxllo;\H~ area. except at deeided 10SB to the operutor.

BUlletin 19763 U .. S",G~g .. by Clyd~ f\RosS" published du:rin..~ 1925. gives an approx1-nwte ;pl."oduOtion ;tor ,tlliij ent1r* d1$tI"ict :1'ox' a 4O-year period of only 35,.000 tons.

Sinee 19:<'5 it is. prooablethat fAIlOthtl:t' ,,000 to 10;000 tons have 'been mined lumtl rlrf31sseQ ~md ahipped. "~O the lenl,d smaltell' tit J£l Paso ..

/,11 this ialogieal as only Orea ot' 'mora than 2S% lead sold. on the general :Dr&"' vai11ng low lead 11'L!';t:l;"Kat would, li1i:l~:ive il'Olll!tl u~at .f1Ulal tel' !,f)tu:rns 1/>11 th which the miner eould at ,lSiitst :ways~l'll* pt1rt of' '~h0 mining eOErt. The lltinel.'&l expo.eures of' 'this district can 'be i:m.p(rrt~4Jl .. 1; it JiJ;"hHl mlU traueportatioll taotorl'.~ ere improved.

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tIPPER S1111 ANAlYTICAl lAB., INC. DNYANENDRA A.SHAH

ARIZONA. RI:G. NO, 811a.

James G. Jones 720 N. Mmn Ave. Tucson, Az. 85710

S ..... PLE

NUMBER

-- - - - - - -- - ---- -- - - -

Kloncyke,

1

2

3 -4

5

Sarrpl e #

Klondyke

1

2

3

4

5

.

.'

Pb% - - -

~

0.10

0.20

0.14

0.12

0.12

5;:>ec. Gra

4.2

4.1

3.9

3.4

3.1

REGISTERED ASSAYER 710 E. EVANS BLVD

P. O. BOX 7517 PHONE 602-664·561 t TUCSON. ARIZONA 65725 884·5612

CaOfo $iO? %

1.58 2.8

2.29 3.2

2.48 5.2

5.3 3.6

2.04 2.4

Solu . Sal ts Ba504

9.3 78.8

16.3 68.4

12.1 69.5

18.3 77.0

5.2 71 .1

/I ~ ~ ~ ~

I A~

~

JOB # 000876 RECEIVED 2/8/82 REPORTED 2/18/82 INVOICE # C 1112

F% Fe?O~ %

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3.24 1.24 .

1.38 1.44

3.78 1.20

1.24 1.18

~

SrS04

1. 72

1.22

2.52

1.12

1 .15'

~~ ~CAfE No '!';f' •

8888 • yanendra rutlal Shah ~}

~.

IG"(I).~ lOna \). s·

.'

---- --

1 ppm ::: 0.0001% 1 troy oz./ton -=- 34.286 ppm 1 ppm = 0.0292 froy oz./Ion

-

• Gold lind Silver reported in troy oz. per 2,000 lb. fon. 005

CIPPER 911111 IIl1l1l1T/CAl l"., INC. DNy .... NENDR .... A. SH .... H

\ ARIZONA REG. NO. 111111.

James G. Jones 720 N. Nann Ave. Tucson,Az. 85710

REGISTERED ASSAYER

P. O. BOX 7517

TUCSON. ARIZONA 85725

710 E. EV .... NS BLVD

PHONE 602-884-58 I ,

884-5812

JOB # __ ,,0,,0r;::.0,,8,..:;7 ... 6_R_€P.....:......ea_ t __ _ RECEIVED _""20-'-7-:8:-:7::-8--:2::-:::-_____ _ REPORTED ___ 2_" __ 19 __ "_8_2 ____________ __ INVOICE # ____________ _

SAMPLE

NUMBER Spec. Gr

Klondyke

1

2 4.2

3 4.2

4 4.1

5 3.9

1 ppm = 0.0001% I troy o%./ton = 34.286 ppm I ppm = 0.0292 troy o%./ton

• Gold and Silver reported in troy oz. per 2.000 lb. ton. oos

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GEO Drilling Fluids, Inc. I Mining and Exploration 1150 Lamoille Hwy. 1 Elko, NV 89801 I Telephone 702 738-8415

Drilling Fluids

. January 29,1982

Mr. Jim Jones 720 North Mann Avenue Tucson, Arizona 85710

. Dear Jim:

Thank you for calling GEO about your barite property. I have checked our records and found that we have not looked at that property. If the property develops into something more than the very narrow veins you described, we would be interested in looking at it.

We are interested in buying barite that is 4.20 specific gravity or higher. We will buy all that you can produce and ship. The current price is $57.00 per ton of dry barite delivered to our mill in Olancha, California. While we do not wish to purchase anything below 4.20 S.G., we will pay 50¢ a point for material delivered over 4.20 S.G. For example, ore averaging 4.27 S.G" will be paid for at the rate of $60.50 per short dry ton.

Payment will be based on dry tons and on assay results (on the crushed and mixed ore) at the mill in Olancha.

We will require notification ?s to the size and expected time of arrival of any shipments, prior to actual shipment.

Thanks again. If we can be of any further assistance, please let us know.

William H. Listerud Senior Geologist

WHL/tb

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DEPARTMENT OF MINERAL RESOURCES STATE OF ~RIZONA


Ivllne 11arcoL te !'arite Dote November 27, 1957 District Arav1aIla Dist!'1ct ·near Klondyke EngineeLewis A. Stnith

Subjectlteported ~,y Y.Il". Dale lfuchinson

Location: ' Sec. 1.3, 14, 2~, 1.'85, R21 I

Owner 1... J. Marcotte, J\londyke, Graham County

Property:

Work:

12 claL"l1S ( 2 groups ot 5 each and 2 connecting cla1me)

430' shaft, (6'111') on vein and assessment cuts and pits. \ " '

Present Status; W. Dale Huchineon, 4691 North Central Ave., Phoenix, Arizona, 1s negotiating an option for a California firm. "

Geology:

Access:

Market:

The deposit consists of two barite veins 1n granite. The veins are parallel and are called No.1 & No.2. The No.1 vein is 6' wide and 4500 feet long. !te width 18 consiEtant to the bottom of the shaft. Huchinson, 1t he obtains the property, plana to drill at least two core-crill~hole8 aloDC the st.rike of the vein 50 as to prove tonnage. He stated that he was sure of at least 500,000 tons, but would have to prove it. The barite runs between 4.1 and ~.45 eravity ~nd 96.3~ ot BaS~. The vein strike H 40 - 550W and dip from vertical to HE, steeply. The )Jo. 2 vein appears to be silllilar to No.1, but has been little developed.

6 'miles of country road and 16 TIllIe S of county graded road to railroad, hoth now being in good condition.

\

The market i8 83Sured. '. ,',

. . . . ~

.~ • , :..-.

, ,- ~ )ne Marcott~Cl.aims

DEPARTMENT OF MINERAL RESOURC£S ST"TE OF "RIZONA


Dote November 27, 1957

District Near ilondyke Ari!. ona Graham County ...... ,.;; \ . "i. . "'--.

Engineer Lewis A. Smith

Subject: Reported by IR./Dale. Huchinso~ . '-"" ----_.------

Location:

Owner:

See. 13, 14, 24 TBS R21E

A. J. Marcotte a.-

2 groups of 5 clai..¥s and two connecting ones, a total of 12 claims acquired by Marcotte in December 1956.

Two parallel veins striking N 4SOW and dip steeply to the northeast, but mSlV vary to vertical. The main, or No.2 vein is of most importance and has been developed over the length of 3 clail'lls (4500 feet). The lesser, or parallel branching vein has been located but little prospected. The main vein has a 6nl foot shaft which is down over 430 I • The width of the vein, is 6' and it is consistent in width to the bottom of the shaft. The i~icated grade, as established by shaft samples, is 4.3-4.h5 qrarity and 95% Base h. It carries a little silver. Huchlnson's people ~aveoftered a royalty proposition for the, property of 35-40¢ per ton and he states that two holee placec along the ~k- for 2000 feet would show at least 1,000,000 tons if it proves out as far as grade and consistancy ore QQ,QQeivect is concerned. The firm has a big market for the ~~terial if proper terms are reached.

·r

'. - -'-.. --- r' -- - ~"- • .8 ~ . -., "

'\



.e J.jarcotte Barite Date Har. 5, 1958

District Clark Mining Distr·ict - Graham Co. Engineer Axel L. Johnson

Subject: r'ield frlgineers Report -- Personal Visit and Ir.iorIn3tion from A. J. Marcotte

Location Sec. 13 -- T 8 S -- R 21 E Starting fr~l Klondyke, drive 8.0 miles to the junction o~ Bonita-Willcox and Safford Roads. Cont.inue on Bonita-Willcox RO<ld for an additional 6.0 miles, i:.-urn left, (rii) and drive up Sheep -Nash for L.o 101l~fJ to Um property.

Alternate route -- starting from lQ.ondyke, dri"le 8.0 miles to the junction of the BOluta-Willcox and Safford Roads, turn left and drive on Safford Road for a distance of 10.0 miles, turn right (Si) and drive an additional 10.0 miles to the property. Roads are unimproved dirt roads and bad in places.

!h:nber of Claims 12 claims on State land (Type A)

Owners A.J. Harcotte, Box 52, Klondyke H.R. Bogan, 326 West Hitchell Drive Scottsdale, Arizona

tion to Purchase A.J .~~arcotte and Harold Bogan to Dale Hutchison F~Tchat~ price J7 ,000.00 to be paid out of a royalty of 55¢ per ton. Option made NO"lember 30, 1957, ends Harch 22, 1958 •

.-'rincipal Hinerals Barite Ore

Present ~lining Activities None

Geology The country rock is a volcanic conglomerate, which contRins large fragments of rock w~ich appear to be Andesite. Three veins of Barite outcropping at the surface was noticed on the property. These veins were vertical and from 2~ to L feat in width. The Barite ore appeared to be of medium grade quality.

Ore in Sight and Probable Ore in sight is negligible due to lack of development. Probable ore appears to be considerable. If may be as much as 15,000 to 100,000 to each 100 feet of depth.

~1illing and !·:ining Facilities No mill on the property. Owners expect to make arrangements with Athletic Mining CompanY for the milling of the Barite at the Klondyke Hill at Klondyke. This mill is now idle. Distance of haul mine to mill is about 20.0 miles. Concentrates would be hauled to Cork Siding for shipment. Distance of haul mill to shipping point about 36.0 miles. Material would be shipped to 3arite producers principally in Texas.

¥ast History a1m Production A 300 ft. shaft was sunk maQY years ago, probably in search of other minerals. No ore shipments are indicated.

Old Mine Workings 1 - 300 ft. vertical shaft, open but appears to be in bad shape.

~w Hille 1'lorkings Limited to location t..urk and a few small open cuts.

• - 2- ·8 .~"

DEPARTM'ENT OF MINERAL RESOURCES STATE OF ARIZONA


11e Marcotte Barite (continued) Dote Mar. 5, 1958

District Clark Mining District - Graham Co. Engineer Alex L. Johnson

Subject: Field Engineers Report -- Personal Visit and Information fran A. J. Marcotte

ProPQs~d Plans If the present option by Dale Hutchison is not exercised, the owner plans on selling or leasing the property to some other company for the milling of the ore at the Klondyke Mill and shipping of the concentrates as described above.

Special Difficulties Underground operation will be required with relatively high mining costs. Long haul of the ore to the mill (and concentrates to loading ramp) plus high freight rates to Texas and California Barite users.

Recormnendations

(1.) Exploration Recommend doing considerable surface exploration work by open cutting, trenChing, and sampling to determine average grade of the ore, and mill tests to determine milling technique and recovery. Also recommend same diamond drill holes be put down to intersect the veins in a number'of places.

(~)Develo~ent If the above exploration shows favorable results, recommend to repair and timb'er the present 300 ft. vertical shaft and drifting on the ore vein in order to develop the ore body. '

~.- - '- ._-- -... - --------- - '.. . .. _._-- ------_... ...

1

/ .... 'MFJii ~ 8 ;1958 c -;-. - ~ I - tI~f f";y i.I f,·c;.r;.~IIJt1. ' /

Narci5tte '"B"ar " r I I I I' 111.'-. C%mon o'JI}C~

'r ~ R:port of 3/5/58 ,. .. .,'

Owner A. J. Marcotte & H.R. Bogan

Les8~es A California Compaqy r Hr. O'Shea did not remember name.

Present l1ining Actin ties Retimbering 'f.l19 .300' vert. shaft. 8 men working. Down 50' in the sbaft now. Additional Info. " Leasing company has leased the

Y Athletic mill at Klondyke, to be used for the nrl.lling of the barite.

" Company has aleoleased the old vacant S. P. depot at Ft. Thomal5. Thi8 18 to be used tor the drying and the sacking of the barite (drying & sacking plant).

v"Bob Bush, Pima, Ariz. ia reported to be working for the Ca11f'. Co.

,,- PrOfosed PlanB Haul the oro to nondYke for m1iiTng at the Athletic }tlll.

Haul the concentrates to Ft. Thomas I , I

for drying and sacking. j Ship the dried & sacked cone. to a I

large Calif. oU compa.ny. ',' Rema.rks Visit will be made, letter with \ report 'of same. '

ADL 1. JOHNSON

• •• DEPARTMENT OF MINERAL RESOURCES STATE OF ARIZONA


, ,~ YArcotte Barite Dote June li, 1958

District Clark Mining District, Graham County . Engineer .Axel L. Johnson ",' ." .. /

Subject: Field Engineerl s Report. Information from A.J. Harcotte and Bob Bush.

References: Report of Harch 5, 1958.

Location: Sec. 13 -- T 8 S -- R 21 E. For directions see report of Harch 5, 1958.

No. of Claims: }2 claims on state land. (type "a") V

Owners: A. J. Narcotte, Box 52, K16ndJke, Arizona, and H. ~. Bogan, 326 \-1. Hitchell Drive, Scottsdale, Arizona. . ,

I J / purchasers: Cuiimrl.ns-Roberts Company (part of Roberts & Associates), L. E. Broadhurst, Pres., 2037 East Rancho Drive, Phoenix,Arizona, Bob BuShi Field Representative, Thatcher, Arizona. .

Price of sale vms reported by Mr. Marcotte to be $120,000.00 payable out of royalties of 50¢ per gross ton of minerals produced.

J Principal l-1inerals: Barite ore.

Present Mining Activity: None. Work was discontinued on J~' 4, 1958 after five weel:::s of' operation. Geology: See report of }!a.rch 5, 1958.

!-1illing and Mining Facilities: No mill on the property. Purchasers are reported to have an option on the Klondyke mill to be used for milling of the barite ore. Purchasers also are reported as having taken out a lease on the old Fort Thomas Depot to be used for the drying and 'Slioking of the barite •

.. Old Hille ''';orkings: The vertical shaft, which was reported previously as being 3001

in depth, was found to be only about 1251 deep.

}7ew JIf.ining Operations: Purchasers started operations on the property about 6 weeks ago. Since that time they have constructed a new road into the property for a distance of about 4 miles and also graded about 10 miles of old road. They have also retimbered the vertical shaft (8 1 x 151 , 3 compartment) down to the liO I level.

Note: The old vertical ::haft was found to be about 1251 in depth instead - of the depth previously reported.

Present Mining Operations: None.

proposed Plans: Mr. Marcotte did not have any definite information regarding further operating plans of the purchasing conpany •

. Bob Bush, the field representative of the company, reports running out of barite at from 60-651 , but that below this depth there is fluorspar and some fairly good values in gold and . silver. He states that the company is at present making samples and tests to determine the value of these minerals.

/f

• • , . STATE OF ARIZONA

DEPARTMENT OF MINERAL RESOURCES MINERAL BUILDING, FAIRGROUNDS

. PHOENIX, ARIZONA

~1.

Information Ca.JlB to the. attention of this Department re: .f/-

MINE: ~Brcotte - Aravapai District

Operating Company: ~~erts & Associates Agent: vEoa Bush, P. O. Box 404·

Thatcher, Arizona

Cleaning shaft now down 1371 and this is believed to be bottom

New w::>rk in progress repairing and cleaning 138' shaft

Assays on quartz footwall of the vein, which is about 8n to 18n

,dde, indicate $32.00 in gold and i oz of silver per ton. The

vein, otherwise, consists of 3-5' of barite down to Sb' of depth

where the barite is beginning to show fluorite. The fluorite

is imreasing with depth. The barite in the top 50' runs 97%

BaSC4 and 4.25 gravity.

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,,~. .' :... . This group, consisting of 12 contiguous unpatented claims (Marc~te Nos. ,:! '. 1 through 12), was located by A. J. Marcotte in December 1956. The claims are

\ largely in sec. 13, T. 8 S., R. 21 E., with slight overlaps into sees. 11, 12 t and 14, all on State,land (fig. 5). The property is accessible from U.S.

Highway No. 70 by the following logl ....... :_ ....... ..

b.o Turn southward onto Klondyke-Bonita Road' ~t 6.4 miles west of' Pima.

17.6 Turn left on Cedar Camp Road.

19.5 Pass through' gate and tUrn left. -

(For an alternate road, keep straight ahead at the gate. This road is about a mile shorter to Cedar Camp, but was badly eroded at the

• time of the examination in March 1957.) . ,_,' ,

- ' - 25.8 Keep straight ahead. . ,

26.0 ~Turn right (left fork goes to Gr~ham prospect).'

26.6 Arrive at claim No. 1. ~

Part of the property, at least, originally was located about 1900, and soon thereafter considerable work was done on what is now cl-a-im 1. J. D. Mathews, of Thatcher, Ariz., relocated the group about 1934 and sometime later allowed it to revert to public domain. It has been reported that a shaft, said to be 300 feet or more deep, was sunk in 1904 by Eastern capital and that some barite was shipped to an eastern market.

In this area' sev.eral bari te-bEtaring veins occur in relatively parallel fault fractures traversing a volcanic agglomerate formation.l The claims are 'arranged in a pattern f~ve tiers wide, covering two major and several minor veins" The courses of the outcrops of both major veins are remarkably persistent, and except for occasional"patches of overburden, each can bEr traced

. for a length of four claims. Two northeasterly trending, postmineral faults have offset the veins." The relative movement of the central segment is reflected in alinement of the claims. The strike of the ,veins varies locally from approximately N. 45°-65° W.; they are either vertical or dip steeply to the northeast.'

The barite veins usually contain various-sized fragments smali amount of green fluorspar and copper oxide staining was Lead did not appear to be associated with the mineralization. or shafts were relatively near the center of each claim. . '

of wallrock. A noted locally. Location cuts

Typical samples' of each exposure examined were composited into one sample, which assayed the following percentages I 71.1 BaS04' 6.4 CaF2' and 1.3 CaC03_; As it had been reported that the deposit had a slight gold content, this combined sampl'e was assayed, its. content was 0.80 ounce silver and 0.08 ounce gold per ton.

The collar timbers oftne old shaft on claim'l have' caved for about 30 feet down, exposing the' shaft walls, but below this point timbering appears to be in fair condition. The vein, exposed on the northwest side of the shaft, dips 85° NE. At the surface veins 14 and 30 inches wide are separated by 18 inches of waste (fig. '6) but join together about 30 feet' down the shaft to form a 4-foot veIn. On the opposite side there is less barite, distributed in thinner zones across an 8-foot face. •

------~------.-.--.,..-------------.-.---.-.---. -------.~------ ----- --._--_ .. _-_ .. _.- '-'-".- . __ .... -.- .. _- -,--', --

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50 years 8go, was 420 teet deep with two drifts at unkno~n depths and that there is barite 4 to 6 feet wide all the way down the shaft. Across the gulch to the southeast, a shallow cut shows an 8-inch vein of relatively pure barite and numerous smaller stringers across a 4-foot zone. This zone continues to the southeast but was not investigated. Following the vein to the northwest, 200 feet from the shaft, two pits show a single vein 6 to 8 inches wide. The 10-foot-deep location cut on claim 2 exposed 4 f~et'of barite at the surface, increasing to 5 feet'at the'bottom. In a draw about 75 feet·northwest of the No. 2 location cut,the vein is 20 inches wide. The work on claim 3 exposed 3 feet of solid barite with few rode inclusions; on claim 4 the vein is 2 feet wide. '

" ,

The other major occurrence, extending the length of four claims, shows thev~in trending through claims 6, 7, and 8 vary~ng from 8 inche~ to 2 feet ,wide~ The cut on claim 9, which is about 20 feet long, crosses several irregular veins 12 to 18 inches wide and a 6-foot mass of barite, which decreases to 3 feet at floor level. The barite ~n this cut occurs in large plates, with included rock fragments of several inches" in size. Immediately ahead of the face, several adrlJtiC?nal I-foot veins appear in surface outcrops, On the . crest of the hill on claim 10 the cut shows a 3-foot vein, and near the top of a knoll at the southeast 'end' of claim 11 a similar vein is exposed. ..

In the cut on claim 12, two narrow veins'separated by a l5-inch rock band' at the surface, join together near the bottom of the cut to form 14 inches of solid barite. ..,

Claim 5 was not investigated, as it was located to consolidate contiguous claims.

The property is at an average altitude of 4,500 feet. The nearest rail point is Cork, a siding on the,Southern Pacific Railway, one-half mile north of the junction of the Klondyke"-Bonita Road with U. S. Highway No. 70 •

Metallurgical Tests

A l75-pound grab sample was taken from an ore pile at the deep shaft for metallurgical testing. This sample assayed 69.6 per~ent BaS04' 11.7 percent CaF2 and 0.6 percent CaC03. T~sts employing the lignin-fluoride method of flotation yielded' a fluorspar product assaying 99.7,percentCaF2. Fluorspar recovery was 50.3 percent. The lignin-fluoride method of-fl~tation consisted of wet-grinding the ore to pass a~200-mesh sieve 'in the p~sence of soda ash, sodium fluoride, and lignin sulfonate at a pH of about 9. The flUorspar then was floated selectively with a minimum amount of oleic acid collector and cleaned four times with small quantities of lignin sulfonate to depress the barite activated during .the rougher flotation step. Subsequent flotation of the barite from the fluorspar tailing at a ~H of about 10, using oleic acid collector, also was successful. Seventy-five percent of the barite was recovered in a product ;that assayed 94.0 percent BaS04 and had a specific gravity of 4.40. •

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• .. . 23

FIGURE 6. • Arrows Point to Barite Veins in° Northlwest Side of Marcotte Shaft.

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J~ / ..1,,_ .. ·t fill :1 ~r' 4 !~ to •• \ -I'j .. t'j' .... .; IJr l .'~, 01 I·. 'f( .• , t .. l .... t"h 1 'I' ,.... ••

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17.8 miles to U.S. 70

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r---· r··.J . : CORONADO

Marcotte , r·· J camp hdqtrs~ , Cedar

I , ________ ~------------~R~.2~0~E~·------~~--+_--------~.--~~~~~--~----\l~----r-·--____ _

: NATIONAL ------. z,.' , -INSET- . I. , ., :.: ,'" ",' , ~ I'>

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To Bonita

I ---+~~~~--~----U-----, ,

I See

Inset ------~~~--+---~~

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o 2 3 4 .

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-------o 6000 Scale Miles - - -- - -

Feet . I' .. i : ..: " F.IGURE 5 •• Location and Claim Map, Marcotte Group •.

Scole

• ,0" •• : • ~'.';' .......... ",

.. I

I , • L' ..

Mr. V. F. Ostler

Roland B. Mu1chay Consulting Geologist

2732 Wren Road Salt Lake City, Utah 84117

Rocky Mountain Refractories 2436 W. Andrew Ave. Salt Lake City, Utah 84104

Dear Mr. Ostler:

March 17, 1982

Following a request by Ms. Teiko Yoshizawa by telephone, I discussed

the K10ndyke Barite Prospect with Mr. James Jones in Tucson on February 25,

1982. I received a copy of a report Mr. Jones had prepared, but not typed,

describing the property, and this report accompanies this letter.

On March 3rd I drove to Globe in the afternoon, and visited the

prospect with Mr. Jones the following day. On March 5th, I returned to

Phoenix. OWnership and similar data have been obtained from Mr. Jones.

LOCATION AND PHYSICAL FEATURES

The property is located on Arizona State land in Sections 11, 12,

13, and 14, Township 8 South, Range 21 East in Graham County. State mineral

prospecting permits are held in the name of Cassandra Resources, Inc., 720 N.

Mann Avenue, Tucson, Arizona, 85710. This company is controlled by Mr. James

G. Jones and Mr. Larry Go1etz, who can be reached at the above address. The

mineral prospecting permits can be later converted to state mineral leases.

The permits cover an area of 1120 acres at the lower northwest end

of the Graham Mountains, and can be reached over about 27 miles of county

maintained, graded road which extends westerly from Highway 70 about 14 miles

north of Safford. The Southern Pacific Railroad parallels Highway 70, and

(2)

Pima station is about 6.5 miles southeast of the Klondyke turnoff.

Numerous arroyos extend westerly across the area to Aravaipa

. '

Canyon which drains northerly and westerly to the San Pedro River. There

is no water or power source available near the permit area. Vegetation is

of typical desert type; temperatures are hot during the summer and cool in

winter. Average rainfall is about 14 - 17 inches; the climate can be termed

moderate, and year round operations could be planned. There is no equipment

on the prop erty.

GEOLOGY

The prospecting permits are within a large surface area of volcanic

rocks, chiefly coarse agglomerates, with a few andesitic tuffs and latitic

flows. The volcanics are generally fresh and unaltered with very little

alteration near the vein structures. Large granite masses are found to the

southeast near the main Graham Mountains and to the north.

Two weakly mineralized, persistent vein structures, steeply dipping

and with N 30° - 50° W strikes, have been prospected. The most easterly "A"

vein is reported to have been followed in cuts and outcrops for a distance

of more than 5000 ft. During our reconnaissance we traced it for about

2500 ft.; the southerly part of the vein is shown on the sketch map which

accompanies this letter.

Near the southern end of the "A" vein exposures, a shaft, now caved

at the collar, is reported to have been reopened to a depth of 138 ft. and

some drifting done at that level in 1958. Barite is reported to a depth of

50 ft. with increasing fluorite below. Some gold assays are reported from

the bottom, presumably in quartzy material similar to a few pieces seen in

the shaft dump. As shown on the map, narrow barite stringers are exposed in

(3)

the shaft cut on the southeast end with stronger narrow veins in a 6.0 ft.

zone at the northwest end. Sample #1 was taken as a grab from about 3 tons

of sorted barite located about 4.0 ft. southeast of the shaft. The attached

map shows the general strike of the vein, and separate 1 in. = 20 ft. sketches

of several cuts show the narrow vein widths and stringery type of mineralized

zones.

The "A" vein can be described as a remarkably persistent, steep

dipping, northwest trending fracture with little movement. Barite stringers

from an inch to two feet in thickness occur along the fracture in a zone from

1.0 to 6.0 ft. in width. As shown on the map, sample #2 was taken from a

small pile of sorted barite at a cut about 200 ft. northwest of the shaft.

About 1800 ft. to the west a similar weak but persistent structure,

called the "B" vein, is exposed at surface but has been little prospected.

It generally is parallel to the "A" vein, and weak stringery barite cari be

traced in scattered outcrops for several thousand feet. We traced it for

about 1500 ft., and a sketch of a shallow cut about 900 ft. north of the road

is shown on the map. The structure is of the same type as the "A" vein, but

barite exposures are weaker than those of that vein.

Sorted.barite at the various cuts shows few specks of galena, little

hematite and limonite, and possibly some fluorite through massive barite.

Samples taken by Mr. Jones are reported to have shown high gravity barite.

It might be expected from the trace lead content at surface that the base

metal content would increase with depth.

CONCLUS IONS

The irregular, narrow barite stringers on the vein structures at

the Klondyke Prospect do not indicate that large barite ore tonnages could be

developed by additional work. There is no positive ore reserve developed,

(4)

and it is very doubtful that the prospective 150,000 tons of reserve,

envisioned by Mr. Jones, could be found by drilling. The vein fractures

are weak, but· remarkably persistent along strike in the volcanic rocks.

Whether or not the~e structures, appearing at surface over considerable

distances, might contain important base metal zones at great depth can only

be conj ectured.

The Klondyke prospect cannot be recommended as an attractive barite

mining venture.

RBM/lh Encl.

Yours very truly,

Roland B. Mulchay

c.. 0 P'I 0 F ~,..,.. Ac:.\-\~'D

~'-\Oe.

'" I

Mr. V. F. Ostler

Roland B. Mulchay Consulting Geo~ogist

2732 Wren Road Salt Lake City, Utah 84117

Rocky Mountain Refractories 2436 W. Andrew Ave. Salt Lake City, Utah 84104

Dear Mr. Ostler:

March 17, 1982

Following a request by Ms. Teiko Yoshizawa by telephone, I discussed

the Klondyke Barite Prospect with Mr. James Jones in Tucson on February 25,

1982. I received a copy of a report Mr. Jones had prepared, but not typed,

describing the property, and this report accompanies this letter.

On March 3rd I drove to Globe in the afternoon, and visited the

prospect with Mr. Jones the following day. On March 5th, I returned to

phoenix. Ownership and similar data have been obtained from Mr. Jones.

LOCATION AND PHYSICAL FEATURES

The property is located on Arizona State land in Sections 11, 12,

13, and 14, Township 8 South, Range 21 East in Graham County. State mineral

prospecting permits are ~eld in the name of Cassandra Resources, Inc., 720 N.

Mann Avenue, Tucson, Arizona, 85710. This company is controlled by Mr. James

G. Jones and Mr. Larry Goletz, who can be reached at the above address. The.

mineral prospecting permits can be later converted to state mineral leases.

The permits cover an area of 1120 acres at the lower northwest end

of the Graham Mountains, and can be reached over about 27 miles of county

maintained, graded road which extends westerly from Highway 70 about 14 miles

north of Safford. The Southern Pacific Railroad parallels Highway 70, and

(2)

Pima station is about 6.5 miles southeas't of the Klondyke turnoff.

Numerous arroyos extend westerly across the area to Aravaipa

Canyon which drains northerly and westerly to the San Pedro River. There

is no water or power source available near the permit area. Vegetation is

of typical desert type; temperatures are hot during the summer and cool in

winter. Average rainfall is about 14 - 17 inches; the climate can be termed

moderate, and year round operations could be planned. There is no equipment

on the property.

GEOLOGY

The prospecting permits are within a large surface area of volcanic

rocks, chiefly coarse agglomerates, with a few andesitic tuffs and latitic

flows. The volcanics are generally fresh and unaltered with very little

alteration near the vein structures. Large granite masses are found to the

southeast near the main Graham Mountains and to the north.

Two weakly mineralized, persistent vein structures, steeply dipping

and with N 30° - 50° W strikes, have been prospected. The most easterly "A"

vein is reported to have been followed in cuts and outcrops for a distance

of more than 5000 ft. During our reconnaissance we traced it for about

2500 ft.; the southerly part of the vein is shown on the sketch map whi'ch

accompanies this letter.

Near the southern end of the "A" vein exposures, a shaft, now caved

at the collar, is reported to have been reopened to a depth of 138 ft. and

some drifting done at that level in 1958. Barite is reported to a depth of

50 ft. with increasing fluorite below. Some gold assays are reported from

the bottom, presumably in quartzy material similar to a few pieces seen in

the shaft dump. As shown on the map, narrow barite stringers are exposed in

(3)

the shaft cut on the southeast end with. stronger narrow veins in a 6.0 ft.

zone at the northwest end. Sample #1 was taken as a grab from about 3 tons

of sorted barite located about 40 ft. southeast of the shaft. The attached

map shows the general strike of the vein, and separate 1 in. = 20 ft. sketches

of several cuts show the narrow vein widths and stringery type of mineralized

zones.

The "A" vein can be described as a remarkably persistent, steep

dipping, northwest trending fracture with little movement. Barite stringers

from an inch to two feet in thickness occur along the fracture in a zone from

1.0 to 6.0 ft. in width. As shown on the map, sample #2 was taken from a

small pile of sorted barite at a cut about 200 ft. northwest of the shaft.

About 1800 ft. to the west a similar weak but persistent structure,

called the "B" vein, is exposed at surface but has been little prospected.

It generally is parallel to the IIAII vein, and weak stringery barite can be

traced in scattered outcrops for several thousand feet. We traced it for

about 1500 ft., and a sketch of a shallow cut about 900 ft. north of the road

is shown on the map. The structure is of the same type as the "A" vein, but

barite exposures are weaker than those of that vein.

Sorted barite at the various cuts shows few specks of galena, little

hematite and limonite, and possibly some fluorite·Othrough massive barite.

Samples taken by Mr. Jones are reported to have shown high gravity barite.

It might be expected from the trace lead content at surface that the base

metal content would increase with depth.

CONCLUS IONS

The irregular, narrow barite stringers on the vein structures at

the Klondyke Prospect do not indicate that large barite ore tonnages could be

developed by additional work. There is no positive ore reserve developed,

(4)

and it is very doubtful that the prospective 150,000 tons of reserve,

envisioned by Mr. Jones, could be found by drilling. The vein fractures

are weak, but "remarkably persistent along strike in the volcanic rocks.

Whether or not these structures, appearing at surface over considerable

distances, might contain Dnportant base metal zones at great depth can only

be conjectured.

The Klondyke prospect cannot be recommended as an attractive barite

mining venture.

RBM/lh Encl.

Yours very truly,

Roland B. Mulchay

~ " ~ ~

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