| Oxygen | 47.33 |
|---|---|
| Potassium | 2.46 |
| 98.05 |
The remainder of the elements exist in quantities of less than 1 per cent. None of these principal elements occur separately in nature and none of them are mined as elements for economic purposes.
RELATIVE ABUNDANCE OF THE PRINCIPAL MINERALS OF THE LITHOSPHERE
Minerals exceptionally consist of single elements, but ordinarily are combinations of two or more elements; for instance, quartz consists of a chemical combination of silicon and oxygen. The proportions of the common minerals in the outer ten miles of the lithosphere are in round numbers as follows:
PERCENTAGE OF COMMON MINERALS IN LITHOSPHERE
| Feldspar | 49 |
|---|---|
| Quartz | 21 |
| Augite, hornblende, and olivine | 15 |
| Mica | 8 |
| Magnetite | 3 |
| Titanite and ilmenite | 1 |
| Kaolin, limonite, hematite, dolomite, calcite, chlorite, etc. | 3 |
| 100 |