Denver City Mine

Past Producer in Saguache county in Colorado, United States with commodities Zinc, Copper, Silver, Gold, Lead, Selenium, Tellurium
Sections on this page
  1. Identification information
  2. Geographic coordinates
  3. Site location context
  4. Geographic areas
  5. Public Land Survey System information
  6. Commodities
  7. Materials information
  8. Alteration
  9. Host and associated rocks
  10. Nearby scientific data
  11. Geologic structures
  12. Ore body information
  13. Controls for ore emplacement
  14. Economic information about the deposit and operations
  15. Mining district
  16. Land status
  17. Ownership information
  18. Workings at the site
  19. Links to other databases
  20. Bibliographic references
  21. General comments
  22. Reporter information

Geologic information

Identification information

Deposit ID 10013140
MRDS ID D009270
Record type Site
Current site name Denver City Mine
Alternate or previous names Patented Claim: Denver City, Ms 11792
Related records 10118866

Geographic coordinates

Geographic coordinates: -106.82868, 38.41722 (WGS84)
Elevation 2749
Relative position 10.2 MILES S30E FROM GUNNISON

Site location context

Political divisions (FIPS codes)

Saguache(county)

Colorado(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Iris(quadrangle 1:24,000 scale)

Saguache(quadrangle 1:100,000 scale)

Montrose(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Tomichi(hydrologic unit)

Gunnison(hydrologic accounting unit)

Gunnison(hydrologic subregion)

Upper Colorado(hydrologic region)

Geographic areas

Country State County
United States Colorado Saguache

Public Land Survey System information

Meridian Township Range Section Fraction State
New Mexico 048N 001E 14 SW OF SE Colorado

Comments on the location information

  • ALONG UNNAMED TRIBUTARY OF LONG GULCH, 2.4 MILES SSE OF GREEN MOUNTAIN AT IRIS ; INFO FROM LAND.ST :(1976)

Commodities

Commodity Importance
Zinc Critical Primary
Copper Primary
Silver Primary
Gold Secondary
Lead Secondary
Selenium Tertiary
Tellurium Critical Tertiary

Materials information

Materials Type of material
Chalcopyrite Ore
Galena Ore
Pyrite Ore
Sphalerite Ore
Calcite Gangue
Chlorite Gangue
Pyrrhotite Gangue
Quartz Gangue
Sericite Gangue

Alteration

  • (Local) Near Best Mineralization, Calcite Occurs As Alteration Replacement And Interstratifies With Sulfides And Tuffaceous Material. Quartz-Chlorite (Propylitic) Alteration Is Partly Sericitic. Silicification (Replacement And Veining) Ranges From Minor To Predominant. Some Argillization.

Analytical data

Result PARTIAL EXTRACTION ANALYSIS OF DUMP SAMPLE YIELDED 1.4 % CU, 0.24 % PB, 2.7 % ZN, 0.46 OZ/TON AG, 0.04 OZ/TON AU, 1.25 OZ/TON SE, 0.11 OZ/TON TE. PARTIAL EXTRACTION ANALYSIS OF MINERALIZED CORE SAMPLE (IRIS NO. 3 HOLE) CONTAINED AS MUCH AS 0.2 % CU, 2.4 % ZN, AND 0.4 % PB.

Host and associated rocks

  • Host or associated Associated
    Rock type Plutonic Rock > Granitoid > Quartz Monzonite
    Stratigraphic age (youngest) Neoproterozoic
    Stratigraphic age (youngest) Neoproterozoic
    Stratigraphic age (youngest) Neoproterozoic
  • Host or associated Associated
    Rock type Plutonic Rock > Mafic Intrusive Rock > Diorite
    Rock unit name Quartz Diorite To Quartz Monzonite Of Gold Basin
    Rock description Quartz Diorite To Quartz Monzonite Of Gold Basin
  • Host or associated Host
    Rock type Volcanic Rock (Aphanitic) > Felsic Volcanic Rock
    Rock unit name Dubois Greenstone--Felsite And Felsite Porphyry;Dubois Greenstone--Amphibolite;Metasedimentary Rocks
    Rock description Dubois Greenstone--Felsite And Felsite Porphyry;Dubois Greenstone--Amphibolite;Metasedimentary Rocks
  • Host or associated Host
    Rock type Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite

Nearby scientific data

(1) -106.82868, 38.41722

Economic information

Geologic structures

Type of structure Regional
Structure description Gunnison Uplift; San Juan Volcanic Field
Type of structure Local
Structure description Gunnison Gold Belt, Iris Syncline, Lulu Fault, Gold Basin Stock

Ore body information

  • General form LENTICULAR
    Length 9.14M
    Width 6.1M
    Depth to top 26.21M

Controls for ore emplacement

  • Original Depositional Control In Fragmental Phase Of Rhyolite Flow

Economic information about the deposit and operations

Development status Past Producer
Commodity type Metallic
Deposit size Small
Significant No
Discovery year 1898
Discoverer Frank Adams And Henry Purrier (Claimants)

Mining district

District name Green Mountain (Iris) District

Land status

Ownership category Private

Ownership information

  • Type Operator
    Owner Lanyon Zinc Co.
    First year 1906

Workings at the site

  • Type of workings Underground
    Overall depth 53.64M

Comments on the workings information

  • MINE DEVELOPED BY 176-FT SHAFT INITIALLY VERTICAL BUT INCLINED BELOW SECOND LEVEL. LEVEL 1 AT 86 FT HAS DRIFTS OF UNKNOWN LENGTH NORTH AND SOUTH OF SHAFT. LEVEL2 AT 111 FT HAS 30-FT DRIFT SOUTH OF SHAFT. LEVEL 3 AT 136 FT IS MOST EXTENSIVELY DEVELOPED, WITH 150 FT OF DRIFT NORTH-SOUTH AND 10 FT OF DRIFT EAST-WEST. LEVEL 4 AT BOTTOM OF SHAFT HAS 25-FT DRIFT NORTH OF SHAFT AND SOUTH DRIFT OF UNKNOWNLENGTH

Reference information

Bibliographic references

General comments

Subject category Comment text
Deposit MINERALIZATION DEVELOPED IN FRAGMENTAL FACIES OF QUARTZ-EYE RHYOLITE TUFF WITHIN SEQUENCE OF MASSIVE RHYOLITE TUFFS CONTAINING CHERT BEDS. RHYOLITE OR FELSITE SEQUENCE LIES ON SW LIMB OF IRIS SYNCLINE AND IS TRUNCATED BY NW-TRENDING LULU FAULT THAT DISPLACES FELSITE ON NE AGAINST METASEDIMENTARY SEQUENCE ON SW. QUARTZ-EYE RHYOLITE CONTINUES TO NW BUT IS OFFSET BY FOUR NE-TRENDING TERTIARY-AGE BLOCK FAULTS. BOTH MAIN ROCK UNITS INTRUDED BY AMPHIBOLITE (METAGABBRO?) DIKES AND SILLS. MINERALIZATION CONSISTS OF MASSIVE SPHALERITE-PYRITE-CHALCOPYRITE LENS AND MINOR MASSIVE CALCITE WITH DISSEMINATED SULFIDES. ORE SHOWS STRATIGRAPHIC ZONING FROM SPHALERITE-RICH ON SW TO CHALCOPYRITE-RICH ON NE, SUGGESTING STRATIGRAPHIC TOP TO SW. MASSIVE SULFIDE USUALLY SHOWS ALTERNATING PYRITE-RICH AND SPHALERITE-RICH LAMINAE; STRONGER ORE ALSO LAMINATED WITH CALCITE. GEOCHEMICAL TRAVERSES SHOW CU ANOMALY LYING STRATIGRAPHICALLY BELOW ZN ANOMALY WHICH LIES STRATIGRAPHICALLY BELOW SE ANOMALY (DROBECK, 1979).
Deposit SCHWARZ (1906) BELIEVED DEPOSIT WAS A CHIMNEY OCCURRING AT INTERSECTION OF SEVERAL FRACTURES. NEWER INTERPRETATION OF GUNNISON GOLD BELT DEPOSITS LED DROBECK (1979) TO POSTULATE SYNGENETIC SUBMARIN

Reporter information

Type Date Name Affiliation Comment
Reporter 01-JUL-1982 Schwochow, Stephen D. Colorado Geological Survey
Updater 01-JAN-1984 Schwochow, Stephen D. Colorado Geological Survey

Beyond USGS

Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.

External references

Authoritative Colorado resources

These are landing pages for further research — the state agencies don't currently expose per-mine deep links.