 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
 |
|
|||||||||||||||||||||
 |
 |
 |
 |
 |
 |
 |
 |
 |
|
|||||||||||||
 |
 |
 |
 |
 |
 |
|
||||||||||||||||
 |
 |
 |
 |
|
||||||||||||||||||
 |
 |
 |
 |
|
||||||||||||||||||
 |
 |
 |
|
|||||||||||||||||||
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|||||||||||||||||||||
|
|
|
|
|
|
|
|
|
|
|
|||||||||||||
|
|
|
|
|
|
|
|
||||||||||||||||
|
|
|
|
|
|
||||||||||||||||||
|
|
|
|
|
|
||||||||||||||||||
|
|
|
|
|
|||||||||||||||||||
PbMoO4
Tetragonal
Wulfenite, a lead molybdate mineral, was first found at Sterling Hill by Fred Parker and subsequently verified by the writer using X-ray methods. It occurs as microscopic (0.3 mm) colorless to light-yellow crystals on a fracture surface in granular franklinite/red- willemite ore from Sterling Hill. It is an extremely rare mineral locally.
 |
|
|||
|
|
||||
|
||||
| Copyright © 1995 by Pete J. Dunn |
Website
by Herb Yeates
|
|||
|
|
|
|||
|
Link
to homepage
|
||||
|
This
page created: January 11, 2001 |
||||
|
|
|
|||
