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Ivanhoe Mine (Commercial Tunnel and Shaft; Ivanhoe 1-8 claims; Commercial 1-6 claims), Squaw Gulch area, Tyndall Mining District, Santa Cruz Co., Arizona, USAi
Regional Level Types
Ivanhoe Mine (Commercial Tunnel and Shaft; Ivanhoe 1-8 claims; Commercial 1-6 claims)Mine
Squaw Gulch areaArea
Tyndall Mining DistrictMining District
Santa Cruz Co.County
ArizonaState
USACountry

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Key
Latitude & Longitude (WGS84):
31° 33' 42'' North , 110° 48' 3'' West
Latitude & Longitude (decimal):
Locality type:
Nearest Settlements:
PlacePopulationDistance
Patagonia890 (2017)4.9km
Sonoita818 (2015)18.9km
Rio Rico18,962 (2011)19.4km
Beyerville177 (2011)20.4km
Kino Springs136 (2011)22.1km


A former small underground Ag-Cu-Pb-Au-Mo-Zn-Sb mine located on 22 claims in south central (E½E½SW¼) sec. 34, T21S, R15E, 3 miles NW of Patagonia and 3 miles east of the Montezuma mine, on the east side of an eastern tributary of Squaw Gulch, in the upper part of the ridge which separates this gulch from Smith Gulch (west of Smith Gulch), ¾ mile S of Johnson Spring, at an elevation of about 4,600 feet, on National Forest land. Worked by Mexicans as early as the 1850's. Relocated in 1905. Operated until 1924. Owned at times, or in part, by the Ivanhoe Mining Co., Minneapolis, Minnesota (1906-circa 1915); Johnson; Tobin & Beasley; and, Hopkins.

Mineralization is irregular, crudely-banded, iron and manganese stained, quartz-fissure vein containing spotty ore shoots of chalcopyrite and pyrite and small pockets of galena. Oxidation and supergene enrichment produced copper carbonates, cerussite, wulfenite and silver halides. The ore zone is 12.19 meters wide, with a depth to bottom of 182.88 meters, and a thickness of 182.88 meters, striking E-W, and dipping 80SE.

The country rock is red granite, locally called quartz porphyry from the strong contrast of its greasy-lustered quartz with the red feldspars. Some of the feldspars are altered to the pale-greenish or whitish kaolinized and sericitized stage. The rock is a medium-grained granitic rock composed almost wholly of orthoclase and quartz. Some of the orthoclase is microperthitic. In the vicinity of the mine the granite is considerably leached. The associated rock units are the Squaw Gulch Granite; Lower Member of the Temporal Formation; and, rhyolite tuff and tuff breccia.

On the east the granite is overlain by gray andesite, which ascends the slope to a point about 150 feet above Smith Gulch and the Commercial tunnel, and in the tunnel at this place diorite seemingly intermediate in age between the granite and the andesite is also present.

A portion of the ridge is capped by reddish, partly silicified andesite tuff or 'burnt rock,' which near by and in the mine seems to be intrusive into the granite and is said to contain generally fair amounts of silver. Both the granite and the andesite are sliced by a north-northwest sheeting with steep easterly dip.

The mine seems to be in part on the easterly extension of the Montezuma vein, which here dips 80ºSE and with a vertical range of 600 feet trends across the ridge into the head of Smith Gulch where the Commercial tunnel opens the vein.

The tunnel is mainly in andesite, but upfaulted greenish diorite forms the hanging wall of the drift and fissure on the south. The vein is shown here to be 4½ feet wide and consists mainly of irregularly, coarsely, and crudely banded brownish iron-stained and whitish silicified and kaolinized altered and mineralized rock breccia and quartz. It is more or less porous or honeycombed, and in places, particularly in the face of the drift, it contains small pockets or bodies of galena, some cerussite, and a little wulfenite. Associated with the ore minerals are also some epidote and manganese and iron oxides.

On the westerly slope of the ridge to the south of the Montezuma vein occur two veins or lodes which trend in a northerly direction, about parallel with the ridge and the sheeting structure in the rock, and obliquely to the transverse Montezuma vein. The western vein is known as the sulphide vein and the eastern one as the horn silver vein.

The sulphide vein is about 10 feet wide and has fairly good footwalls, and the mineralized zone containing it is about 28 feet wide. It is a blind vein, without croppings other than a little brecciated gouge. It was first encountered in the shaft about 50 feet below surface. In a raise from the south drift at the bottom of the shaft the vein contains a 4 foot wide oreshoot, which contains mainly of crushed granite intruded by dark andesite, all more or less ferruginated and silicified. It carries chalcopyrite and acanthite at 140 oz. Ag/T and 12% Cu. In the north drift at the bottom of the shaft, a 16 inch (40 cm) oreshoot on the east or hanging wall side of the vein, which is banded, is richer than the corresponding part of the vein in the south drift. It contains considerable chalcocite averaging 21% Cu and 300 oz. Ag/T.

The horn silver vein lies about 100 feet east of the sulphide vein, in altered granite, and is seemingly associated with an andesite dike. It is opened by a 90 foot crosscut tunnel connecting with a 120 foot inclined winze, with about 150 feet of drift on the tunnel level and much more at the bottom of the winze. It is several feet in width and at about 140 feet below the surface changes from a steep westerly dip to a steep easterly dip. It is composed mainly of crudely banded silicified iron and manganese stained crushed rock and quartz. The ore occurs in stringers or streaks from 1 inch to several inches in width and carries good values. It contains mainly chlorargyrite and embolite.

Workings circa 1915 include about 300 feet each of tunnels, drifts and shafts to a depth of about 250 feet, with plans to sink to 400 feet. The Commercial tunnel is 200 feet long and opens the vein at 4,300 feet of altitude at the head of Smith Gulch. The workings totalled 822.96 meters in length and 76.2 meters in depth. Worked by Mexicans as early as the 1850's, and by others through 1924. Produced some 420 tons of ore averaging about 51 oz. Ag/T, 2% Cu and minor Pb. Altered area S of the Ivanhoe asssayed at 50 ppm Ag, 0.9 ppm Au, 150 ppm Mo, 300 ppm Sb, 30 ppm Be, and 200 ppm Bi, especially near the N & E margins of the altered area.

Select Mineral List Type

Standard Detailed Strunz Dana Chemical Elements

Mineral List


19 valid minerals.

Detailed Mineral List:

Acanthite
Formula: Ag2S
Reference: Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd.ed.: 101; Schrader, F.C. & J.M. Hill (1915), Mineral deposits of the Santa Rita and Patagonia Mountains, AZ, USGS Bull. 582: 218; Galbraith, F.W. (1947), Minerals of AZ, AZ Bur.Mines Bull. 153: 15.
Alunite
Formula: KAl3(SO4)2(OH)6
Reference: MRDS database Dep. ID file #10039602, MRDS ID #M050441.
Azurite
Formula: Cu3(CO3)2(OH)2
Reference: Copper Handbook 1911
Cerussite
Formula: PbCO3
Reference: Keith, Stanton B. (1975), Arizona Bureau of Mines Bull. 191, Index of Mining Properties in Santa Cruz County Arizona: 85 (Table 4); Schrader (1915): 216-218; Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd.ed.: 158; Galbraith, F.W. & D.J,. Brennan (1959), Minerals of AZ: 50; Schrader, F.C. & J.M. Hill (1915), Mineral deposits of the Santa Rita and Patagonia Mountains, AZ, USGS Bull. 582: 217; Arizona Bureau of Mines file data.
Chalcocite
Formula: Cu2S
Description: Occurs in large bodies.
Reference: Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd.ed.: 164; Schrader, F.C. & J.M. Hill (1915), Mineral deposits of the Santa Rita and Patagonia Mountains, AZ, USGS Bull. 582: 216-218; Schrader, F.C. (1917), The geologic distribution and genesis of the metals in the Santa Rita-Patagonia Mountains, AZ, Econ.Geol.: 12: 217-269; Galbraith, F.W. (1947), Minerals of AZ, AZ Bur.Mines Bull. 153: 16.; Copper Handbook 1911
Chalcopyrite
Formula: CuFeS2
Reference: Keith, Stanton B. (1975), Arizona Bureau of Mines Bull. 191, Index of Mining Properties in Santa Cruz County Arizona: 85 (Table 4); Schrader, F.C. & J.M. Hill (1915), Mineral deposits of the Santa Rita and Patagonia Mountains, AZ, USGS Bull. 582: 218; Arizona Bureau of Mines file data.
Chlorargyrite
Formula: AgCl
Reference: Keith, Stanton B. (1975), Arizona Bureau of Mines Bull. 191, Index of Mining Properties in Santa Cruz County Arizona: 85 (Table 4); Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd.ed.: 170; Schrader (1915): 216-218; Guild, F.N. (1910), The mineralogy of Arizona, The Chemical Publishing Co., Easton, PA; Arizona Bureau of Mines file data; Schrader, F.C. & J.M. Hill (1915), Mineral deposits of the Santa Rita and Patagonia Mountains, AZ, USGS Bull. 582: 218; Galbraith, F.W. & D.J,. Brennan (1959), Minerals of AZ: 42.
Chlorargyrite var: Bromian Chlorargyrite
Formula: Ag(Cl,Br)
Reference: Schrader, F.C. & J.M. Hill (1915), Mineral deposits of the Santa Rita and Patagonia Mountains, AZ, USGS Bull. 582: 218.
Epidote
Formula: {Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
Reference: MRDS database Dep. ID file #10039602, MRDS ID #M050441.
Galena
Formula: PbS
Reference: Keith, Stanton B. (1975), Arizona Bureau of Mines Bull. 191, Index of Mining Properties in Santa Cruz County Arizona: 85 (Table 4); Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd.ed.: 385; Engineering & Mining Jour. (1912), The mining news: 97: 395; Schrader, F.C. & J.M. Hill (1915), Mineral deposits of the Santa Rita and Patagonia Mountains, AZ, USGS Bull. 582: 217; Arizona Bureau of Mines file data.
Kaolinite
Formula: Al2(Si2O5)(OH)4
Reference: Schrader, F.C. & J.M. Hill (1915), Mineral deposits of the Santa Rita and Patagonia Mountains, AZ, USGS Bull. 582: 217.
Muscovite
Formula: KAl2(AlSi3O10)(OH)2
Reference: Schrader, F.C. & J.M. Hill (1915), Mineral deposits of the Santa Rita and Patagonia Mountains, AZ, USGS Bull. 582: 217.
Muscovite var: Sericite
Formula: KAl2(AlSi3O10)(OH)2
Reference: Schrader, F.C. & J.M. Hill (1915), Mineral deposits of the Santa Rita and Patagonia Mountains, AZ, USGS Bull. 582: 217.
Orthoclase
Formula: K(AlSi3O8)
Colour: Reddish
Description: A prominent component of a red granitic country rock.
Reference: Schrader, F.C. & J.M. Hill (1915), Mineral deposits of the Santa Rita and Patagonia Mountains, AZ, USGS Bull. 582: 217.
Polybasite
Formula: [(Ag,Cu)6(Sb,As)2S7][Ag9CuS4]
Reference: Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd.ed.: 333, 335, 385; Engineering & Mining Jour. (1912), The mining news: 97: 395.
Proustite
Formula: Ag3AsS3
Reference: Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd.ed.: 333, 335, 385; Engineering & Mining Jour. (1912), The mining news: 97: 395.
Pyrite
Formula: FeS2
Reference: Keith, Stanton B. (1975), Arizona Bureau of Mines Bull. 191, Index of Mining Properties in Santa Cruz County Arizona: 85 (Table 4); Schrader (1915): 216-218; Arizona Bureau of Mines file data.
Silver
Formula: Ag
Reference: Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd.ed.: 333, 335, 385; Engineering & Mining Jour. (1912), The mining news: 97: 395.
Stromeyerite
Formula: AgCuS
Reference: Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd.ed.: 333, 335, 385; Engineering & Mining Jour. (1912), The mining news: 97: 395.
Tenorite
Formula: CuO
Reference: Copper Handbook 1911
'Tetrahedrite'
Formula: Cu6(Cu4X2)Sb4S13
Reference: Copper Handbook 1911
Wulfenite
Formula: Pb(MoO4)
Reference: Keith, Stanton B. (1975), Arizona Bureau of Mines Bull. 191, Index of Mining Properties in Santa Cruz County Arizona: 85 (Table 4); Schrader, F.C. & J.M. Hill (1915), Mineral deposits of the Santa Rita and Patagonia Mountains, AZ, USGS Bull. 582: 217; Arizona Bureau of Mines file data.

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Silver1.AA.05Ag
Group 2 - Sulphides and Sulfosalts
Acanthite2.BA.35Ag2S
Chalcocite2.BA.05Cu2S
Chalcopyrite2.CB.10aCuFeS2
Galena2.CD.10PbS
Polybasite2.GB.15[(Ag,Cu)6(Sb,As)2S7][Ag9CuS4]
Proustite2.GA.05Ag3AsS3
Pyrite2.EB.05aFeS2
Stromeyerite2.BA.40AgCuS
'Tetrahedrite'2.GB.05Cu6(Cu4X2)Sb4S13
Group 3 - Halides
Chlorargyrite3.AA.15AgCl
var: Bromian Chlorargyrite3.AA.15Ag(Cl,Br)
Group 4 - Oxides and Hydroxides
Tenorite4.AB.10CuO
Group 5 - Nitrates and Carbonates
Azurite5.BA.05Cu3(CO3)2(OH)2
Cerussite5.AB.15PbCO3
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Alunite7.BC.10KAl3(SO4)2(OH)6
Wulfenite7.GA.05Pb(MoO4)
Group 9 - Silicates
Epidote9.BG.05a{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
Kaolinite9.ED.05Al2(Si2O5)(OH)4
Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
var: Sericite9.EC.15KAl2(AlSi3O10)(OH)2
Orthoclase9.FA.30K(AlSi3O8)

List of minerals arranged by Dana 8th Edition classification

Group 1 - NATIVE ELEMENTS AND ALLOYS
Metals, other than the Platinum Group
Silver1.1.1.2Ag
Group 2 - SULFIDES
AmBnXp, with (m+n):p = 2:1
Acanthite2.4.1.1Ag2S
Chalcocite2.4.7.1Cu2S
Stromeyerite2.4.6.1AgCuS
AmXp, with m:p = 1:1
Galena2.8.1.1PbS
AmBnXp, with (m+n):p = 1:1
Chalcopyrite2.9.1.1CuFeS2
AmBnXp, with (m+n):p = 1:2
Pyrite2.12.1.1FeS2
Group 3 - SULFOSALTS
ø > 4
Polybasite3.1.7.2[(Ag,Cu)6(Sb,As)2S7][Ag9CuS4]
3 <ø < 4
'Tetrahedrite'3.3.6.1Cu6(Cu4X2)Sb4S13
ø = 3
Proustite3.4.1.1Ag3AsS3
Group 4 - SIMPLE OXIDES
AX
Tenorite4.2.3.1CuO
Group 9 - NORMAL HALIDES
AX
Chlorargyrite9.1.4.1AgCl
Group 14 - ANHYDROUS NORMAL CARBONATES
A(XO3)
Cerussite14.1.3.4PbCO3
Group 16a - ANHYDROUS CARBONATES CONTAINING HYDROXYL OR HALOGEN
Azurite16a.2.1.1Cu3(CO3)2(OH)2
Group 30 - ANHYDROUS SULFATES CONTAINING HYDROXYL OR HALOGEN
(AB)2(XO4)Zq
Alunite30.2.4.1KAl3(SO4)2(OH)6
Group 48 - ANHYDROUS MOLYBDATES AND TUNGSTATES
AXO4
Wulfenite48.1.3.1Pb(MoO4)
Group 58 - SOROSILICATES Insular, Mixed, Single, and Larger Tetrahedral Groups
Insular, Mixed, Single, and Larger Tetrahedral Groups with cations in [6] and higher coordination; single and double groups (n = 1, 2)
Epidote58.2.1a.7{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
Group 71 - PHYLLOSILICATES Sheets of Six-Membered Rings
Sheets of 6-membered rings with 2:1 layers
Muscovite71.2.2a.1KAl2(AlSi3O10)(OH)2
Group 76 - TECTOSILICATES Al-Si Framework
Al-Si Framework with Al-Si frameworks
Orthoclase76.1.1.1K(AlSi3O8)
Unclassified Minerals, Mixtures, etc.
Chlorargyrite
var: Bromian Chlorargyrite
-Ag(Cl,Br)
Kaolinite-Al2(Si2O5)(OH)4
Muscovite
var: Sericite
-KAl2(AlSi3O10)(OH)2

List of minerals for each chemical element

HHydrogen
H KaoliniteAl2(Si2O5)(OH)4
H Muscovite (var: Sericite)KAl2(AlSi3O10)(OH)2
H AluniteKAl3(SO4)2(OH)6
H Epidote{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
H AzuriteCu3(CO3)2(OH)2
H MuscoviteKAl2(AlSi3O10)(OH)2
CCarbon
C CerussitePbCO3
C AzuriteCu3(CO3)2(OH)2
OOxygen
O CerussitePbCO3
O WulfenitePb(MoO4)
O KaoliniteAl2(Si2O5)(OH)4
O Muscovite (var: Sericite)KAl2(AlSi3O10)(OH)2
O OrthoclaseK(AlSi3O8)
O AluniteKAl3(SO4)2(OH)6
O Epidote{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
O AzuriteCu3(CO3)2(OH)2
O TenoriteCuO
O MuscoviteKAl2(AlSi3O10)(OH)2
AlAluminium
Al KaoliniteAl2(Si2O5)(OH)4
Al Muscovite (var: Sericite)KAl2(AlSi3O10)(OH)2
Al OrthoclaseK(AlSi3O8)
Al AluniteKAl3(SO4)2(OH)6
Al Epidote{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
Al MuscoviteKAl2(AlSi3O10)(OH)2
SiSilicon
Si KaoliniteAl2(Si2O5)(OH)4
Si Muscovite (var: Sericite)KAl2(AlSi3O10)(OH)2
Si OrthoclaseK(AlSi3O8)
Si Epidote{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
Si MuscoviteKAl2(AlSi3O10)(OH)2
SSulfur
S ChalcopyriteCuFeS2
S PyriteFeS2
S GalenaPbS
S AcanthiteAg2S
S ChalcociteCu2S
S Polybasite[(Ag,Cu)6(Sb,As)2S7][Ag9CuS4]
S StromeyeriteAgCuS
S ProustiteAg3AsS3
S AluniteKAl3(SO4)2(OH)6
S TetrahedriteCu6(Cu4X2)Sb4S13
ClChlorine
Cl ChlorargyriteAgCl
Cl Chlorargyrite (var: Bromian Chlorargyrite)Ag(Cl,Br)
KPotassium
K Muscovite (var: Sericite)KAl2(AlSi3O10)(OH)2
K OrthoclaseK(AlSi3O8)
K AluniteKAl3(SO4)2(OH)6
K MuscoviteKAl2(AlSi3O10)(OH)2
CaCalcium
Ca Epidote{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
FeIron
Fe ChalcopyriteCuFeS2
Fe PyriteFeS2
Fe Epidote{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
CuCopper
Cu ChalcopyriteCuFeS2
Cu ChalcociteCu2S
Cu Polybasite[(Ag,Cu)6(Sb,As)2S7][Ag9CuS4]
Cu StromeyeriteAgCuS
Cu AzuriteCu3(CO3)2(OH)2
Cu TenoriteCuO
Cu TetrahedriteCu6(Cu4X2)Sb4S13
AsArsenic
As Polybasite[(Ag,Cu)6(Sb,As)2S7][Ag9CuS4]
As ProustiteAg3AsS3
BrBromine
Br Chlorargyrite (var: Bromian Chlorargyrite)Ag(Cl,Br)
MoMolybdenum
Mo WulfenitePb(MoO4)
AgSilver
Ag ChlorargyriteAgCl
Ag AcanthiteAg2S
Ag Polybasite[(Ag,Cu)6(Sb,As)2S7][Ag9CuS4]
Ag StromeyeriteAgCuS
Ag ProustiteAg3AsS3
Ag SilverAg
Ag Chlorargyrite (var: Bromian Chlorargyrite)Ag(Cl,Br)
SbAntimony
Sb Polybasite[(Ag,Cu)6(Sb,As)2S7][Ag9CuS4]
Sb TetrahedriteCu6(Cu4X2)Sb4S13
PbLead
Pb GalenaPbS
Pb CerussitePbCO3
Pb WulfenitePb(MoO4)

References

Sort by

Year (asc) Year (desc) Author (A-Z) Author (Z-A)
Guild, F.N. (1910), The mineralogy of Arizona, The Chemical Publishing Co., Easton, PA.
Engineering & Mining Journal (1912), The mining news: 97: 395.
Schrader, F.C. & J.M. Hill (1915), Mineral deposits of the Santa Rita and Patagonia Mountains, Arizona, USGS Bull. 582: 216-218.
Schrader, F.C. (1917), The geologic distribution and genesis of the metals in the Santa Rita-Patagonia Mountains, Arizona, Economic Geology: 12: 217-269.
Weed, W.H. (1918) The Mines Handbook, Vol. XIII: 500.
Tenney, J.B. (1927-1929) History of Mining in Arizona, Special Collection, University of Arizona Library & Arizona Bureau of Mines Library: 318.
Elsing, M.J. and Heineman, E.S. (1936) Arizona Metal Production, Arizona Bureau of Mines Bulletin 140:
Galbraith, F.W. (1947), Minerals of Arizona, Arizona Bureau of Mines Bull. 153: 15, 16.
Galbraith, F.W. & D.J,. Brennan (1959), Minerals of AZ: 42, 50.
Drewes, H.D. (1971) Geologic map of the Mount Wrightson quadrangle, southeast of Tucson, Santa Cruz and Pima Counties, Arizona: U.S. Geological Survey Miscellaneous Geologic Investigations Map I-614, 1 sheet, scale 1:48,000.
Keith, Stanton B. (1975), Arizona Bureau of Mines Bull. 191, Index of Mining Properties in Santa Cruz County Arizona: 85 (Table 4).
Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd.ed.: 101, 158, 164, 170, 335, 385;
U.S. Bureau of Mines file data, Ivanhoe Mine.
Arizona Bureau of Mines file data.
MRDS database Dep. ID file #10039602, MRDS ID #M050441; and, Dep. ID #10161718, MAS ID #0040230231.

Other Databases

USGS MRDS Record:10039602

Other Regions, Features and Areas containing this locality

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