Difference between revisions of "Sulfates"
Jump to navigation
Jump to search
m (cat) |
DavidB4-bot (talk | contribs) (→Sources: clean up & uniformity) |
||
| (4 intermediate revisions by 3 users not shown) | |||
| Line 1: | Line 1: | ||
| − | The '''sulfates''' are [[compounds]] of one or more [[metallic]] [[elements]] with the [[sulfate]] | + | The '''sulfates''' are [[compounds]] of one or more [[metallic]] [[elements]] with the [[sulfate]] ion. This is a large class of [[minerals]], whose members have few [[properties]] in [[common]]. In general they are light in [[color]] and [[transparency|transparent]] to [[translucency|translucent]]. None are hard, and most are [[fragile]]. |
| − | =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), ''p. 453'' |
| − | [[ | + | |
| + | [[Category:Mineralogy]] | ||
| + | [[Category:Chemical Compounds]] | ||
| + | [[Category:Soil]] | ||
Latest revision as of 01:32, June 28, 2016
The sulfates are compounds of one or more metallic elements with the sulfate ion. This is a large class of minerals, whose members have few properties in common. In general they are light in color and transparent to translucent. None are hard, and most are fragile.
Sources
- Chesterman, Charles W. The Audubon Society Field Guide to North American Rocks and Minerals, Alfred A. Knopf: New York (1987), p. 453