Classification of Igneous Rock
Download
Report
Transcript Classification of Igneous Rock
Classification of Igneous
Rock
Section 5.2
Mineral Composition
Intrusive
– Igneous intrusion
– Large crystals (macroscopic)
Extrusive
– Lava flow or flood basalts
– Small crystals (requires magnification)
Mineral Composition
Basaltic rocks
– Dark colored
– Lower silica content
– Contain mostly plagioclase and pyroxene
Granite rocks
– Light colored
– High silica content
– Contain mostly quartz, K+ & plagioclase
feldspar
Mineral Compositions
Intermediate rocks have a composition
of minerals between baslatic and granite
rocks
Ultrabasic rocks
– Contain only iron-rich minerals
– Always dark
Texture
Texture refers to the size, shape, and
distribution of the crystals or grains that
make up a rock
Rhyolite – fine-grained
Granite – coarse-grained
How is crystal size affected by cooling
rate?
Texture
Porphyritic texture – large well formed
crystals surrounded by finer grained
crystals of the same or different mineral
Forms when slowly cooling magma
suddenly cooled rapidly
Vesicular texture – spongy appearance;
Pumice is an example
Thin Sections
A slice of rock usually 2cm X 4 cm and
only 0.03 mm thick
Light is able to pass through it
A petrographic microscope is used to
view thin sections
Veins
Valuable ores occur within igneous
intrusions; Ores also occur in the rocks
surrounding intrusions called veins
Important metallic elements include gold,
silver, lead, and copper
Pegmatites
Pegmatites – veins of extremely largegrained minerals
Lithium and Beryllium ores form in
pegmatites
Produce beautiful crystals
Mount Rushmore in South Dakota
Kimberlites
Kimberlites are ultrabasic rocks
Form at depths of 150 to 300 km
Named for Kimberly, South Africa
Diamonds form in kimberlites
Where in the US have kimberlites been
found?
Construction Uses
Interlocking grain textures make igneous
rocks strong
Resistant to weathering
Granite is used in countertops, floors, and
statues