| |
| | Planet Earth I: Igneous Rocks |
 | | When determining whether a rock is plutonic, hypabyssal or volcanic, it is the size of the groundmass that is critical, as the groundmass shows the environment of the final crystallisation. |
 | | As plutonic rocks form deep under the earth's surface in large magma chambers, it cools slowly and, initially, relatively few nucleation centres form, so the crystals are free to grow, unhindered by the growth of neighbouring crystals. |
 | | Plutonic rocks that have less than 90% mafic minerals (the vast bulk of all plutonic rocks) are classified according to the relative percentages of quartz, alkali feldspar and plagioclase. |
| www.rpi.edu /dept/geo/pe1/chapter6.html (7841 words) |
|