CaCO3 - Occurs as sharp, clear to opaque flattened rhombohedral crystals up to about one inch, similar to the calcite crystals that have been found at the neigboring Cadman High Rock Quarry. | |
SiO2 - Occurs as chalcedony (blue, white, brown, colorless) in veins up to about 12-inches thick with some smaller veins consisting of banded light blue agate. Crystalline quartz is also present, with some crystals showing zoned, light-colored amethyst terminations. The most notable quartz occurence are the chalcedony pseudomorphs after melanophlogite [46SiO2 · 6(N2,CO2) · 2(CH4,N2)] in open cavities within the chalcedony veins. The individual pseudomorphs show cubic morphology, occuring as crust-like aggregates (most common), sharp cubes (some isolated on the matrix) and complex intergrown cubes showing a stepped repeating pattern on the cube faces. The pseudomorphs range in color from blue to white to colorless and range in size from about 1 to 8 mm. |
QUARTZ (Var: Chalcedony) Photo Copyright © Nick Carlson 2024 |