Objectives for the topic: Magma and Intrusive Rocks
Reading: Chapter 3 in Tarbuck and Lutgens
Images to understand: 3.2, 3, 4, 5, 7, 8, B, 20, 21, 22, 23, 24
After completing this topic, the student will be able to:
- Describe the compositional range of extrusive igneous rocks (compare basalt, andesite and rhyolite).
- Describe the relationship of texture (grain size, bubble content) in extrusive igneous rocks to the cooling history of the magma/lava.
- Describe the three factors that generate magmas from solid rock.
- Describe the processes by which magmas can change composition as they ascend through the crust (crystal settling, assimilation, magma mixing)
- Describe the plate tectonic settings in which magmas of basaltic or granitic composition are generated.
- Identify a coarse-grained intrusive texture, and distinguish it from the texture of extrusive rocks.
- Compare and contrast the texture and origin of pairs of igneous rocks (e.g. granite/rhyolite or granite/basalt).
- Name the most abundant intrusive igneous rock forming the continental crust.
David M. Hirsch
Modified on Mon, Jul 12, 2004 at 11:14 PM