CHROMITE, M-195/195A. Philippine Islands.
Black metallic with a little disseminated
serpentine. Some pure enough for specific gravity tests.
Check for availability.
CHRYSOCOLLA, M-200. Arizona. Vivid blue and blue-green
crusts and masses with occasional quartz. Check.
We have some smaller than class pack sizes available at lower price of this
excellent material. E-mail us. These are a very nice color, so smaller might work for you.
CHRYSOCOLLA, M-200A. Arizona.
Light sky blue to Robin's Egg blue, up to 50% associated rock.
CHRYSOTILE ASBESTOS, M-205.
Arizona. Veins in serpentine. Shows the fibrous nature of this
category of mineral.
CINNABAR, M-210. Nevada. Varies from lean
coatings and veinlets in and on rock to richer vugs on chert. Check for availability and sizes.
COAL, see in SEDIMENTARY ROCKS or Metamorphic rocks.
COLEMANITE, M-215. California.
Classic Boron material. Compact, fine sugary colemanite with some crystals.
COPPER, M-225. Arizona. Thin
sheets and dendritic fissure filling forms.
Little or no accompanying rock. No class packs available. Check on availability.
COPPER, M-225A. Michigan. Tumbled copper pieces from
the Keweenaw Peninsula. These pieces imitate those that
were naturally tumbled by glaciers.
CORUNDUM, M-220. Brown, gray and
bluish pieces of crystals.
RUBY variety CORUNDUM. M-220R. India. Purplish red semi-translucent
crystals showing hexagonal crystal form and some with complete terminations.
1.25 to 1.75 by .75 inch crystals. Check.
CUMMINGTONITE, M-230.
DANBURITE. M- 235. Mexico.
DENDRITE, M-240. California.
Fern-like black manganese
oxide markings on white felsite. Faux fossil.
DIAMOND crystals/cubes. Educational-industrial grade.
Please check.
DIASPORE, M-245.
California, Coarse, crystalline, platy
masses usually with minor pyrophyllite
and/or andalusite. SL - Check.
DIATOMITE, (DIATOMACEOUS EARTH) see
OPAL
DIOPSIDE, M-250. Canada.
Grayish green showing cleavage, parting
and occasional crystal faces.
DOLOMlTE, M-255. California.
Medium to fine grained white to grayish
crystalline masses .
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