Sumas Mountain Iron Deposit

The Sumas Mountain Iron Deposit is a iron mine located in Whatcom county, Washington.

About the MRDS Data:

All mine locations were obtained from the USGS Mineral Resources Data System. The locations and other information in this database have not been verified for accuracy. It should be assumed that all mines are on private property.

Mine Info

Name: Sumas Mountain Iron Deposit  

State:  Washington

County:  Whatcom

Elevation:

Commodity: Iron

Lat, Long: 48.90361, -122.25222

Map: View on Google Maps

Satelite View

MRDS mine locations are often very general, and in some cases are incorrect. Some mine remains have been covered or removed by modern industrial activity or by development of things like housing. The satellite view offers a quick glimpse as to whether the MRDS location corresponds to visible mine remains.


Satelite image of the Sumas Mountain Iron Deposit

Sumas Mountain Iron Deposit MRDS details

Site Name

Primary: Sumas Mountain Iron Deposit
Secondary: Ochre Point Placer 1915
Secondary: Hematite Group 1919


Commodity

Primary: Iron
Tertiary: Chromium
Tertiary: Nickel


Location

State: Washington
County: Whatcom
District: Mount Baker District


Land Status

Not available


Holdings

Not available


Workings

Not available


Ownership

Owner Name: Northern Pacific Railroad

Owner Name: Waddington Mining Corp., Ltd.
Home Office: Vancouver, B. C., Canada


Production

Not available


Deposit

Record Type: Site
Operation Category: Occurrence
Operation Type: Unknown
Discovery Year: 1915
Years of Production:
Organization:
Significant: N
Deposit Size: S


Physiography

General Physiographic Area: Pacific Mountain System
Physiographic Province: Pacific Border Province
Physiographic Section: Puget Trough


Mineral Deposit Model

Not available


Orebody

Not available


Structure

Not available


Alterations

Not available


Rocks

Not available


Analytical Data

Analytical Data: MATERIAL SAMPLED CONTAINS 16.2-48.1% FE. A PICKED SAMPLE GAVE AN ANALYSIS OF 37.21% FE, 20.83% S1O2, 0.20% P, 0.008% S. IRON DEPOSIT IS CONSIDERED TO BE LOW GRADE.


Materials

Ore: Hematite
Ore: Limonite
Ore: Magnetite
Ore: Chromite


Comments

Comment (Deposit): LOCATION AND GEOLOGIC MAP OF DEPOSIT, AND RESULTS OF CHEMICAL ANALYSES OF DEPOSIT ARE AVAILABLE, MOEN, 1969. MAP OF CLAIMS AVAILABLE, SHEDD, JENKINS, AND COOPER, 1922. ; INFO.SRC : 1 PUB LIT

Comment (Reserve-Resource): RESERVES ESTIMATED AT 375,000 TONS OF INDICATED ORE, AND 375,000 TONS OF INFERRED ORE.

Comment (Location): W SLOPE OF SUMAS MTN.

Comment (Development): MANY SAMPLES HAVE BEEN TAKEN, SOME TRENCHES DUG, AND ONE ADIT DRIVEN, BUT NO MINING HAS BEEN UNDERTAKEN

Comment (Deposit): ABSENCE OF SULFIDES SUGGESTS THAT THE NICKEL MAY BE A HYDROUS NICKEL SILICATE. CLAYSTONE UNDERLIES A BASAL CONGLOMERATE OF THE CHUCKANUT FORMATION. EXPOSURES OF THE CLAYSTONE AS MUCH AS 20-FT THICK EXTEND ABOUT 1,500 FT UP SIDE OF SUMAS MOUNTAIN.

Comment (Workings): 60 FT ADIT, OPEN CUTS

Comment (Deposit): MRDS RECORD W017830 HAS BEEN MERGED WITH THIS RECORD AND DELETED

Comment (Deposit): LATERITE DEVELOPED ON PERIDOTITE (ALMOST COMPLETELY SERPENTINIZED). RESIDUAL OLIVINE, CHROMITE, AND MAGNETITE ARE PLAINLY VISIBLE MICROSCOPICALLY. DEPOSIT CONSISTS OF BLANKET OF FERRUGINOUS CLAYSTONE ON ALTERED PERIDOTITE. CLAYSTONE HAS MAXIMUM THICKNESS OF 35 FT, BUT IRON-RICH PART GENERALLY AVERAGES ONLY 5 FT. CLAYSTONE CONSISTS OF EXTREMELY FINE GRAINED (CLAY SIZE) HYDROUS ALUMINUM SILICATES, LIMONITE, HEMATITE, MAGNETITE, AND MINOR QUARTZ AND CHROMITE. COLOR VARIES FROM GRAYISH BROWN TO GRAYISH RED; SPECIFIC GRAVITY RANGES FROM 2.67 TO 3.09. BEDDING, VISIBLE IN UPPER PARTS OFUNIT, MARKS ALTERNATING LAYERS OF CLAYSTONE AND SILTSTONE AND SEVERAL SANDY BEDS. BEDS STRIKE N 2 E TO N 20 W, AND DIP 25 TO 40 W. IRON-RICH PART OF CLAYSTONE IS MAGNETIC AND CONTAINS MAGNETITE OOLITES AND PISOLITES, WHICH ALSO FILL SMALL FRACTURES IN THE IRON BEDS. SMALL CHROMITE GRAINS, PROBABLY WEATHERED FROM THE SERPENTINITE ARE PRESENT. NICKEL IS PRESENT IN THE CLAYSTONE, BUT ITS FORM IS UNKNOWN.


References

Reference (Deposit): MOEN, W.S., 1969, MINES AND MINERAL DEPOSITS OF WHATCOM COUNTY, WASHINGTON: WASHINGTON DIVISION OF MINES AND GEOLOGY BULL. 57, P. 71-73

Reference (Deposit): HUNTTING, M.T., 1956, INVENTORY OF WASHINGTON MINERALS - PART II, METALLIC MINERALS: WASHINGTON DIVISION OF MINES AND GEOLOGY BULL. 37, P. 205

Reference (Deposit): SHEDD, SOLON, JENKINS, O.P., AND COOPER, H.H., 1922, IRON ORES, FUELS AND FLUXES OF WASHINGTON: WASHINGTON DIVISION OF GEOLOGY BUL. NO. 27, P. 105-107.

Reference (Reserve-Resource): MOEN, 1969, P. 74


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