images from © 2010 pearson education, inc
TRANSCRIPT
Mineral
Texture:
Explanation: Interpretation: Cooling
history
Igneous
rock:
Phaneritic
(coarse-
grained)
Crystals are all
large (visible),
interlocking
Cooled slowly underground Intrusive
Porphyritic
Some larger
crystals
surrounded by
fine-grained
material
2 stages of cooling: first cooled
slowly underground (larger
crystals), then erupted and
cooled quickly (fine-grained
material)
Extrusive
Aphanitic
(fine-grained)
No visible
crystals Cooled rapidly at Earth’s surface Extrusive
Images from geology.com
Extrusive
Fine-grained
(aphanitic)
or
porphyritic
Intrusive
Coarse-
grained
(phaneritic)
Ultramafic Mafic Intermediate Felsic