Nova Scotia Minerals: Wittichenitespacer

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WITTICHENITE

Cu3BiS3

Turner Tin Prospect (New Ross), Lunenburg County
UTM (NAD27)
Zone 20
 Northing 4960150 / 4959950
 Easting 385160 / 385190
Details:
 The Turner Sn prospect is located along both sides of the east branch of Gold River at Mill Road, Lunenburg County. The prospect is accessible by trail from Mill Road (O'Reilly et al. 1982).
References:
 NSMOD #A16-012
Further Info:
 Mineralization: Within the greisen, mineralization is disseminated in patches of phengite and quartz and/or associated with narrow, oxidized, iron-rich veins. Minerals identified include: arsenopyrite, pyrite, sphalerite, chalcopyrite, stannite, wittichenite, cassiterite and covelite. Digenite resulted from the alteration of chalcopyrite and sphalerite. High scintillometer readings were recorded from the Discovery vein, the mineral was assumed to be torbernite or metatorbenite (Ellsworth, 1950). The presence of autenite was suggested by the existence of a green fluorescing mineral in radioactive patches (O'Reilly, 1982).
Other Minerals:
 arsenopyrite, autunite, cassiterite, chalcopyrite, covellite, pyrite, sphalerite, stannite, torbernite

Walker Moly Prospect, Lunenburg County
UTM (NAD27)
Zone 20
 Northing 4958460
 Easting 387970
Details:

 The Walker Moly Prospect is found 140 m south of the Vaughan-New Ross Road at the community of New Russell, Lunenburg County. New Russell is 6.4 km east of New Ross, a village on Highway 12. A swampy area and brook separates the prospect from the road, so best access is to the workings is by following a woods road along the south border of the swamp (O'Reilly et al., 1982). The woods road leads west from a secondary road that goes from the Vaughan-New Ross Road toward Round Lake. The entrance to the woods road is 100 m south of the paved Vaughan-New Ross Road. Follow the woods road west for 240 m to its terminus at the prospect.

References:
 NSMOD #A16-010,  Extensive info available, see the database.
The location for this prospect indicated on NSDNR Map 88-15 (Corey, 1988) is wrong. The correct coordinates are provided in this occurrence entry.
Further Info:

A shaft at the site is water filled and a cement cap has been placed over it for safety reasons. A waste rock dump surrounds the shaft and is heavily overgrown.
This prospect is an excellent mineral collecting location. Time spent rummaging through the waste rock dump will yield excellent specimens of molybdenite and bornite. The more exotic minerals reported from the prospect are less common and occur disseminated in the greisen selvages.

Other Minerals:
 molybdenite, gahnite, chalcopyrite, bornite, wolframite, cassiterite, native bismuth, uraninite, mawsonite




 

 Cleavage: absent

 Colour: lead gray, bronze, steel gray, or tin white

 Fracture:

 Hardness: 2.5

 Luster: metallic

 Streak: black

 Possible Useage:

 More Info: Mineralogy Database

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