Difference between revisions of "Striated"
(new entry) |
|||
| (2 intermediate revisions by 2 users not shown) | |||
| Line 1: | Line 1: | ||
| − | A '''striated''' [[Mineral Habit|mineral habit]] has very shallow, [[parallel]] grooves or depressions on one or more [[crystal]] faces. [[Pyrite]] is an example of a [[mineral]] exhibiting a striated habit. Chesterman, p. 38 | + | A '''striated''' [[Mineral Habit|mineral habit]] has very shallow, [[parallel]] grooves or depressions on one or more [[crystal]] faces. [[Pyrite]] is an example of a [[mineral]] exhibiting a striated habit.<ref>Chesterman, p. 38</ref> |
| − | =Sources= | + | ==Sources== |
*Chesterman, Charles W. ''The Audubon Society Field Guide to North American Rocks and Minerals'', Alfred A. Knopf: New York (1987) | *Chesterman, Charles W. ''The Audubon Society Field Guide to North American Rocks and Minerals'', Alfred A. Knopf: New York (1987) | ||
| + | ==References== | ||
| + | {{reflist}} | ||
| + | [[Category:Geology]] | ||
Latest revision as of 22:58, August 17, 2024
A striated mineral habit has very shallow, parallel grooves or depressions on one or more crystal faces. Pyrite is an example of a mineral exhibiting a striated habit.[1]
Sources
- Chesterman, Charles W. The Audubon Society Field Guide to North American Rocks and Minerals, Alfred A. Knopf: New York (1987)
References
- ↑ Chesterman, p. 38