Deposit ID | 10000297 |
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MRDS ID | A010345 |
Record type | Site |
Current site name | Castle Island |
Geographic coordinates: | -133.16466, 56.65252 (WGS84) |
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Relative position | SEE LOCATION COMMENTS |
(click for info) |
Country | State |
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United States | Alaska |
Commodity | Importance |
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Barium-Barite | Primary |
Silver | Tertiary |
Zinc | Tertiary |
Gold | Tertiary |
Lead | Tertiary |
Copper | Tertiary |
Materials | Type of material |
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Barite | Ore |
Chalcopyrite | Ore |
Galena | Ore |
Sphalerite | Ore |
Graphite | Gangue |
Magnetite | Gangue |
Quartz | Gangue |
Sphene | Gangue |
Result | ASSAYS INDICATE 89%-93% BA SO4, 0.79-1.05 OZ/TON AG, 0.01--003 OZ/TON AU, 1.14-1.38% ZN, 0.29% PB, 0.04-0.07% CU |
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Model code | 184 |
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USGS model code | 28a |
Deposit model name | Massive sulfide, kuroko |
Mark3 model number | 93 |
Host or associated | Host |
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Rock type | Sedimentary Rock > Carbonate > Limestone |
(1) | -133.16466, 56.65252 |
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General form | SEE DEPOSIT DESCRIPTION COMMENTS |
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Strike | N30 |
Dip | STEEPLY NE |
Development status | Past Producer |
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Commodity type | Both metallic and non-metallic |
Deposit size | Small |
Significant | No |
Agency | Database name | Acronym | Record ID | Notes |
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USGS | Mineral Resources Data System | MRDS | A010345 | |
USGS | Alaska Resource Data File | ARDF | PEO26 | |
USGS | Mineral Resources Data System | MRDS | A010345 |
Burchard, E. F., 1914, A barite deposit near Wrangell: U. S. Geological Survey Bulletin 592, p. 109-117.
Buddington, A. F., 1923, Mineral deposits of the Wrangell district; U. S. Geological Survey Bulletin 739, p. 51-75.
Buddington, A. F., 1925, Mineral investigations in southeastern Alaska: U.S. Geological Survey Bulletin 733, p. 71-139.
Buddington, A. F., and Chapin, Theodore, 1929, Geology and mineral deposits of southeastern Alaska: U. S. Geological Survey Bulletin 800, 398 p.
Race, W. H., 1963, Castle Island barite deposit, Duncan Canal, Alaska (Petersburg Quadrangle): Alaska Territorial Department of Mines Property Examination 117-9, 15 p., 1 sheet, scale 1:480.
Williams, J. A., and Decker, P. A., 1932, Exploring Castle Island barite deposit by Diamond Drilling, Duncan Canal: Alaska Territorial Department of Mines Miscellaneous Report 117-1, 47 p., 1 sheet, scale 1:250,000
Cobb, E. H., 1972, Metallic mineral resources map of the Petersburg quadrangle, Alaska: U. S. Geological Survey Miscellaneous Field Studies Map MF-415, 1 sheet, scale 1:250,000.
Cobb, E. H., 1978, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Petersburg quadrangle, Alaska: U.S. Geological Survey Open-File Report 78-870.
Karl, S. M., Berg, H. C., Grybeck, D., and Abramson, B. S., 1980, Tables describing metalliferous and selected nonmetallic mineral deposits in the Petersburg and eastern Port Alexander quadrangles, Alaska: U.S. Geological Survey Open-File Report 80-793, 14 p., 4 sheets, scale, 1:250,000.
Berg, H. C., and Grybeck, Donald, 1980, Upper Triassic volcanogenic Zn-Pb-Ag (-Cu-Au) mineral deposits near Pertersburg, Alaska: U.S. Geological Survey Open-File Report 80-527, 11 p., 1 oversize sheet.
Berg, H.C., 1981, Upper Triassic volcanogenic massive sulfide metallogenic province identified in southeastern Alaska, in Albert, N.R.D., and Hudson, T., eds, United States Geological Survey in Alaska: Accomplishments during 1979: U. S. Geological Survey Circular 823-B, p. B104-108.
Grybeck, D. J., Berg, H. C., and Karl, S. M., 1984, Map and description of the mineral deposits in the Petersburg and eastern Port Alexander quadrangles: U.S. Geological Survey Open-File Report 84-837, 86 p., 1 sheet, scale 1:250,000.
Swainbank, R. C., Bundtzen, T. K., Clough, A. H., Henning, M. W., and Hansen, E. W., 1995, Alaska's Mineral Industry 1994: Alaska Division of Geological and Geophysical Surveys Special Report 49, 77 p.
Brew, D.A., 1997, Reconnaissance geologic map of the Petersburg C-4 quadrangle, southeastern Alaska: U. S. Geological Survey Open-File Report 97-156-J, scale 63,360, one sheet, 21 p. pamphlet.
ADGGS BIENNIAL REPORT, 1974-1975, P. 34
Subject category | Comment text |
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Deposit | THE ORE BODY CONSISTED OF A LENTICULAR, MASSIVE BARITE LENS ABOUT 300 FEET LONG AND UP TO 200 FEET THICK THAT EXTENDED TO A MAXIMUM DEPTH OF ABOUT 150 FEET BELOW SEA LEVEL. THE EXACT STRATIGRAPHIC RELATIONS ARE UNCLEAR BECAUSE MOST OF THE DEPOSIT WAS UNDER SALT WATER. HOWEVER, EXAMINATION OF UNPUBLISHED DRILLING DATA AND CROSS SECTIONS MAINTAINED BY THE MINE INDICATES THAT THE BARITE LENS PROBABLY OCCURRED ALONG THE TROUGH OF A SYMMETRICAL OPEN SYNCLINE TRENDING ABOUT N70W WITH LIMBS DIPPING ABOUT 30 TO 45 DEGREES DRILLING ALSO INDICATED A CONSIDERABLE TONNAGE OF LOWER GRADE BARITE INTERBEDDED WITH 'GRAY SCHIST,' 'CHERT,' AND 'GRAPHITIC SCHISTS,' AND THE POSSIBILITY OF AT LEAST ONE MORE HIGH-GRADE BARITE LENS OFFSHORE. MINE-RUN MATERIAL WAS MASSIVE, WHITE TO LIGHT GRAY, ALMOST PURE BARITE THAT ALMOST INVARIABLY CONTAINED A PERCENT OR SO OF SULFIDES AS TINY DISSEMINATED GRAINS. ASSAYS OF THE MASSIVE BARITE INDICATE THAT IT TYPICALLY CONTAINS ABOUT 0.5-2% ZN, ABOUT 0.5% PB, A |
Deposit | CARNES, U. S. BUREAU OF MINES; UNPUBLISHED FIELD NOTES BY THE REPORTERS; AND ANALYSES SUMMARIZED IN GRYBECK, BERG, AND KARL (1984). THE CASTLE ISLANDS LARGELY -- AND THE ISLAND ON WHICH THE BARITE MINE OCCURS SPECIFICALLY -- CONSIST LARGELY OF UPPER TRIASSIC HYD GROUP ROCKS WHICH ARE DOMINANTLY FELSIC AND INTERMEDIATE VOLCANIC FLOWS AND BRECCIA, LIMESTONE AND ARGILLITE. HOWEVER, PARTS OF THE ISLANDS ALSO CONSIST OF DEVONIAN LIMESTONE AND QUATERNARY BASALT WHOSE RELATIONSHIP TO THE HYD GROUP ROCKS IS PROBABLY STRUCTURALLY COMPLICATED AND LARGELY HIDDEN UNDER WATER (BREW, 1997 [OF 97-156-J]). |
Deposit | VISITED BRIEFLY BY D. GRYBECK, USGS, IN JULY, 1996; NO SIGN OF MINING ACTIVITY SINCE 1980 OR OF RECENT SURFACE EXPLORATION. ALL THE MINING EQUIPMENT HAS BEEN REMOVED FROM THE ISLAND AND IT IS NOW LARGELY COVERED BY ALDER AND BRUSH; USGS OPEN FILE 80-793, TABLE 2 |
Deposit | SMALL AMOUNT OF CU, AND ABOUT 1 OUNCE AG PER TON. UNDER THE REFLECTING MICROSCOPE, THE SULFIDES ARE SEEN TO BE SPHALERITE, GALENA, PYRITE, PYRRHOTITE, BORNITE, TETRAHEDRITE-TENNANTITE, AND CHALCOPYRITE, TOGETHER WITH MINOR AMOUNTS OF OTHER ORE MINERALS, ALL AS TINY, GENERALLY EQUANT GRAINS. EXAMINATION OF WASTE DUMPS PROVIDE MANY SAMPLES THAT SHOW ALL TRANSITIONS FROM MASSIVE BARITE TO LAYERED PYRITE (-SPHALERITE -QUARTZ)-BARITE ROCK WITH THE OTHER SULFIDES NOTED PREVIOUSLY DISSEMINATED THOUGH THE ROCK IN MINOR AMOUNT. THE ASSOCIATION OF BARITE, LAYERED SULFIDE-BARITE ROCKS, SCHISTOSE METAFELSITE(?), AND BLACK CARBONACEOUS, CALCAREOUS PHYLLITE AT THE MINE SITE INDICATE THAT IT IS PART OF THE TRIASSIC DUNCAN CANAL-ZAREMBO CANAL BELT OF DISMEMBERED, VOLCANOGENIC MASSIVE-SULFIDE DEPOSITS DESCRIBED BY BERG AND GRYBECK (1980) AND BERG (1981). THIS DESCRIPTION IS SYNTHESIZED FROM BURCHARD (1914); BUDDINGTON (1923); BUDDINGTON (1925); UNPUBLISHED WRITTEN AND ORAL DATA FROM DAVID |
Type | Date | Name | Affiliation | Comment |
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Reporter | 01-DEC-1983 | Hirschmann, M. M. (Elliott, R. L.) | U.S. Geological Survey | |
Updater | 01-NOV-1998 | Berg, H. C. (Grybeck, D. J.) | U.S. Geological Survey |