Geologic information
Identification information
Deposit ID |
10100959 |
MRDS ID |
A011459 |
Record type |
Site |
Current site name |
Cliff Mine |
Related records |
10282462 |
Geographic coordinates
Geographic coordinates:
|
-146.56589, 61.12209 (WGS84)
|
Relative position |
ON N SHORE OF PORT VALDEZ ABOUT 7 MI W OF VALDEZ, AK |
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Geographic areas
Country |
State |
United States |
Alaska |
Public Land Survey System information
Meridian |
Township |
Range |
Section |
Fraction |
State |
|
009S |
008W |
01 |
|
Alaska |
Comments on the location information
- LOCATION GIVEN AS PLOTTED ON THE VALDEZ A-7 QUADRANGLE. LAND STATUS VALUE CALCULATED 6-94 USING GIS OVERLAY ANALYSIS WITH BLM 1:2,500,000 SCALE OWNERSHIP STATUS MAP (1991).
Commodities
Commodity |
Importance |
Gold |
Primary |
Lead |
Tertiary |
Zinc |
Tertiary |
Comments on the commodity information
- SULFIDES PRESENT ARE PYRITE, ARSENOPYRITE, GALENA AND SPHALERITE; SULFIDES MAKE UP 3 TO 5% OF ORE
Materials information
Materials |
Type of material |
Galena |
Ore |
Gold |
Ore |
Sphalerite |
Ore |
Albite |
Gangue |
Calcite |
Gangue |
Chlorite |
Gangue |
Pyrite |
Gangue |
Quartz |
Gangue |
Alteration
-
(Local)
Oxidation Is Evident To 100 Ft, Distinct Over Approximately 50 Ft
Analytical data
Result |
ESTIMATED GRADE OF ABOUT 2.4 OZ/TON FROM REPORT OF 50.00 DOLLAR/TONWITH AU AT 20.67/TON, WALL ROCK ASSAYED ABOUT .07 TO 0.29 OZ/TON REPORTED AS 1.5 TO 6.00 DOLLARS/TON |
Result |
IN USGS BULL 443, P. 72-74 |
Host and associated rocks
Host or associated |
Host |
Rock type |
Sedimentary Rock
> Clastic Sedimentary Rock
> Siltstone |
Rock unit name |
Valdez Group |
Rock description |
Valdez Group;Valdez Group |
Geologic structures
Type of structure |
Regional |
Structure description |
Tightly Compressed E-W Trending Folds, Overturned Towarrd The S. Pluge Gently W |
Ore body information
General form |
PINCH AND SWELL |
Strike |
N 28 W TO N 47 W |
Dip |
65 E TO 48 W |
Thickness |
2M
|
Controls for ore emplacement
- Au Bearing Veins Are Localized Along Faults, Fractures And Shear Zones That Are Discordant With Regional Cleavage And A System Of Metamorphic Segregation Veins; The Auriferous Veins Principally Occupy The Axes And Upper Limbs Of Overturned Anticlinal Structures
Comments on the geologic information
- LODE IS TYPICAL OF THE HIGH-GRADE EPIGENETIC GOLD-QUARTZ VEINS FOUND IN ROCKS OF LOW TO MODERATE METAMORPHIC GRADE WITHIN THE VALDEZ GROUPTURBIDITES. SCHISTOSE GRAYWACKE INTERBEDDED WITH CARBONACEOUS SLATE.