| Some minerals (and rocks) do not demonstrate a parting or
cleavage along specific planes, but they do have a consistency in
how they break. The resulting surfaces are described as conchoidal
(obsidian), uneven (hornblende), etc.
The important types of
fracture are demonstrated with this collection.
6 specimens
approximately 1 1/2" x 1 1/2", number-coded.
FRACTURE is the
manner of breaking and appearance of a mineral or rock when broken
other than along cleavage or parting planes. The following
collection of common minerals and rocks illustrates the different
types of fractures. |
 Fracture Collection
| 1. OBSIDIAN |
Conchoidal |
| 2. AGATE |
Uneven |
| 3. CHERT |
Uneven |
| 4. MAGNETITE |
Hackly |
| 5. SATIN SPAR GYPSUM |
Splintery |
6. QUARTZ
|
Conchoidal
|
|