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Tephroite Willemite & Pyrochroite

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LMB170384

Tephroite Willemite & Pyrochroite

Description Tabs

Description
Locality: 
Sterling Mine, Ogdensburg, Sussex County, New Jersey, United States of America
Size Range: 
Small cabinet (7-10 cm)
Size: 
4 × 7 × 2.3 cm
Description

clearly the willemite occurs mostly as an exsolution network in something else. The second photo reveals that the “something else” is tephroite. Based on the exsolution pattern, it appears that there are at most two or three individual tephroite xls here. Note also that the pinkish area at lower right, while clearly not tephroite, appears to also be part of the exsolution network. See the fifth (last) photo for more on this area. The third photo shows the “back side” which is mostly calcite. But note the black and cream color “blob” at lower right. The black is pyrochroite. The rest is described in the fourth photo. The fourth photo is a close-up (FOV 7.0 x 4.6 mm) of the pyrochroite “blob” on the back. This blob is small (~ 1.3 cm) for the occurrence, but it illustrates some of the typical features of such blobs: black platy pyrochroite, criss-cross veinlets of a pinkish “slow fizz” carbonate (probably rhodochrosite), relict flecks of zincite, and a creamy, fizzy carbonate. The latter could be “Mineral F” (of Dunn), but it has not been analyzed. (However, the specimen is from an occurrence known to have Mineral F – aka UM1986-10-CO:ClHMgMnZn to the IMA.) Clearly this whole mess is a replacement, but it’s not clear of what. The fifth photo shows a close-up of another replacement typical of this assemblage. This is a small example of a different type of blob, namely a “layered blob”. In this case, the layers are mostly the pink carbonate already mentioned, with embedded fluoborite needles. The brown stuff at the bottom is tephroite. The pink layers are clearly separated by thin black layers (hetaerolite?) The precursor is again unknown – but the hetaerolite is suggestive. Bigger and better examples of both types of blobs were found. Here they are just little “bonuses”. This is and interesting but inadequately studied assemblage. The specimen is much more complex than a quick look might indicate. Note: The fluoborite in the pinkish blob was verified on other specimens. The UV photos is a time exposure. Both the calcite and willemite are very bright under SW UV, but what you perceive will depend on the intensity of the UV source and the quality of the UV filters. Weight 4.9 oz.

Mineral Data
What's on the rock

Tephroite

Formula: 
Mn2+2SiO4
Strunz: 
9.AC.05
Crystal System: 
Orthorhombic Forms short prismatic crystals.
Hardness: 
6.0
Streak: 
Pale gray
Type Locality: 
Sterling Mine, Sterling Hill, Ogdensburg, Franklin Mining District, Sussex Co., New Jersey, USA

Willemite

Formula: 
Zn2SiO4
Strunz: 
9.AA.05
Hardness: 
5.5
Streak: 
White
Type Locality: 
Vieille Montagne (Altenberg; Kelmisberg), Moresnet, Kelmis, Plombières-Vieille Montagne District (Plombières-Altenberg), Verviers, Liège Province, Belgium

Pyrochroite

Formula: 
Mn(OH)2
Strunz: 
4.FE.05
Hardness: 
2.5 - 3.0
Type Locality: 
Pajsberg Mine, Pajsberg, Persberg district, Filipstad, Värmland, Sweden
LMB minerals

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In addition to the standard terms and conditions, please note the following. Almost all IDs are visual. While in most cases the ID is obvious, there may be cases where it is not. If you are doubtful about a particular ID, please ask for more information. Or do not bid! Similarly, if you are not sure that the specimen meets your criteria, do not bid. I have tdone the best I can with the photos. Nevertheless, if you are not happy with a specimen for any reason, I will refund the bid price – but not the shipping costs (unless the fault is clearly mine) – if the specimen is returned. This policy applies even if analysis of the specimen shows that my ID was incorrect. When in doubt, ask - or don’t bid. Note that most crystals at MSH and Varennes are micros - even if on large specimens. Please pay attention to the stated sizes. Any customs duties, fees etc. are the responsibility of the buyer.