Geology 101 - Lecture 7
Igneous Rocks and Volcanism
(Brief Outline Only)
I. Relationship of basalt to andesite to rhyolite: Magma differentiation
- As a magma cools and crystallizes, the minerals it crystallizes do
not have the same composition as the magma itself
- Thus if the crystals are removed, the magma becomes a different
composition than it was before
- Minerals crystallize in a particular order, with the highest temperature
minerals crystallizing first, and the lower temperature minerals crystallizing
last
(Bowen's Reaction Series)
- The highest temperature minerals are the richest in Mg and Fe, and
the poorest in Si.
- Thus, progressive crystallization will cause a magma to become
depleted in Mg and Fe and enriched in Si. (i.e., basalt goes to rhyolite)
II. Extrusive (Volcanic) Rocks
A. Several types of material erupted (lava, pyroclastic
material, volcanic gases)
Pyroclastic = "fire broken". Exploded magma
B. What determines whether an eruption will be a lava
flow or an explosive eruption?
- viscosity of magma (resistance to flow) - depends on
- composition of magma (more felsic the magma, more viscous, more
potential for explosion)
- temperature of magma (the lower the temperature of the magma, the
more viscous, the more potential for explosion)
- amount of dissolved gases (more dissolved gases, more potential for
explosive eruption)
C. Materials erupted
1. Lava flows
a. Basalt lava - very fluid, erupts at approx. 1000-1200 degrees C
- Pahoehoe
- Aa
- Pillow lava
Scoria - highly vesicular basalt
b. Rhyolite lava - very viscous, erupts at approx 800-1000 degrees C
- Plugs and domes
- Dangerous - plug vents and trap gases
Obsidian - rhyolitic glass
c. Andesite lava - intermediate
2. Pyroclastic ("fire-broken") materials: Fragmented volcanic
material ejected into the air during an eruption
a. Basalt: Not common, but basaltic pyroclasts do exist
- Ash - exploded lava with an average diameter less than 2mm
- Bombs/blocks - particles with an average diameter greater than 64 mm
b. Andesite and rhyolite: typically form the truly explosive eruptions
- Ash - exploded lava with diameter less than 2mm
- Pumice - exploded lava of larger size, lots of gas bubbles
- Bombs/blocks - particles have an average diameter greater than 64 mm
3. Gas(see next lecture)
National Park Geology: Tour of Volcanoes