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Lakeman group, Gold Gulch, Greenlee County, Arizona, USAi
Regional Level Types
Lakeman group- not defined -
Gold GulchGulch
Greenlee CountyCounty
ArizonaState
USACountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
33° 3' 54'' North , 109° 24' 20'' West
Latitude & Longitude (decimal):
Nearest Settlements:
PlacePopulationDistance
Morenci1,489 (2011)4.0km
Clifton3,685 (2017)10.3km
York557 (2011)26.8km
San Jose506 (2011)32.3km
Solomon426 (2011)35.2km
Mindat Locality ID:
131392
Long-form identifier:
mindat:1:2:131392:8
GUID (UUID V4):
9129a571-b045-43e5-b10c-4676b385a879


A former surface and underground Ag-Cu-Au-Pb mine located on 8 patented claims totalling about 138 acres, in the center S½ sec. 19, T4S, R29E, 3.0 miles SW of Morenci in Gold Gulch, on private land. Discovered in 1875 by R.L. Lakeman. Produced 1904-1935. The Lakeman group consists of 8 claims: Stevens, Campbell, Tonto, Tiger, Globe, Pinetree, Minnie L., and the Katie L. The above location coordinates describe the shaft in the south half of sec. 19. Other claims located on ridge south of Gold Gulch. Operators included E. Bignell; Knapp and Lakeman; R.L. Lakeman; H.L.M. Wright and N.J. Wilson; Messabi-Morenci Mining Co. Owners included Mrs. Grace Morrison.

Mineralization is an irregular ore body with a vein that averages 3 feet (3.05 meters) wide, with a depth to bottom of 60.96 meters, and striking N60E and dipping vertically. An associated rock unit is the Morenci Granite Porphyry. Ore control was NE-trending fissure vein in a diorite porphyry mass. Ore concentration is mineralization along veins, evidenced by quartz cementation and pyritic dissemination. Alteration is sericization of diorite porphyry wall rock. The porphyry is greatly disintegrated. Gold and silver values are carried in the sulfides.

The porphyry crumbles easily to fragments and forms a sandy soil in the region of Gold Gulch. Diorite porphyry forms the southern end of the great stock of Morenci and Metcalf. Placer gold in Gold Gulch was derived from oxidized gold-bearing veins associated with the intrusive porphyry rather than regional faulting.

Area structures include porphyry that consists largely of sills and laccoliths dipping 10°-30° SW like the sedimentary strata. Porphyry appears regonally as stocks, sheets and dikes tightly interbedded wit sedimentary rocks. Tectonic component is the Gold Gulch Fault Block.

Workings included one main shaft 300 feet (91.44 meters) deep, 2 short tunnels with lengths of 30 feet and 40 feet, about 470 feet of drifts, an additional shaft, one stope, various shallow cuts and pits, and placer gold workings. This property produced notable amounts of gold ore between 1885 and 1895.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


5 valid minerals.

Detailed Mineral List:

'Biotite'
Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
'Chlorite Group'
Epidote
Formula: (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Galena
Formula: PbS
Hematite
Formula: Fe2O3
'Hornblende Root Name Group'
Formula: ◻Ca2(Z2+4Z3+)(AlSi7O22)(OH,F,Cl)2
Muscovite
Formula: KAl2(AlSi3O10)(OH)2
Muscovite var. Sericite
Formula: KAl2(AlSi3O10)(OH)2
Orthoclase
Formula: K(AlSi3O8)

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Galena2.CD.10PbS
Group 4 - Oxides and Hydroxides
Hematite4.CB.05Fe2O3
Group 9 - Silicates
Epidote9.BG.05a(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
var. Sericite9.EC.15KAl2(AlSi3O10)(OH)2
Orthoclase9.FA.30K(AlSi3O8)
Unclassified
'Biotite'-K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
'Chlorite Group'-
'Hornblende Root Name Group'-◻Ca2(Z2+4Z3+)(AlSi7O22)(OH,F,Cl)2

List of minerals for each chemical element

HHydrogen
H BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
H Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
H MuscoviteKAl2(AlSi3O10)(OH)2
H Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
H Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
OOxygen
O BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
O Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
O HematiteFe2O3
O MuscoviteKAl2(AlSi3O10)(OH)2
O OrthoclaseK(AlSi3O8)
O Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
O Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
FFluorine
F BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
F Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
MgMagnesium
Mg BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
AlAluminium
Al BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Al Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Al MuscoviteKAl2(AlSi3O10)(OH)2
Al OrthoclaseK(AlSi3O8)
Al Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
Al Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SiSilicon
Si BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Si Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Si MuscoviteKAl2(AlSi3O10)(OH)2
Si OrthoclaseK(AlSi3O8)
Si Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
Si Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SSulfur
S GalenaPbS
ClChlorine
Cl Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
KPotassium
K BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
K MuscoviteKAl2(AlSi3O10)(OH)2
K OrthoclaseK(AlSi3O8)
K Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
CaCalcium
Ca Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Ca Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
TiTitanium
Ti BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
FeIron
Fe BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Fe Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Fe HematiteFe2O3
PbLead
Pb GalenaPbS

Other Databases

Link to USGS MRDS:10048283

Other Regions, Features and Areas containing this locality

North America
North America PlateTectonic Plate
USA

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
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