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Intrusive Igneous Activity

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Presentation on theme: "Intrusive Igneous Activity"— Presentation transcript:

1 Intrusive Igneous Activity

2 Plutons intrusive igneous structures that result from the cooling/hardening of magma beneath surface. classified according to shape, size, and relationship to surrounding rock layers

3 Types of Plutons Dikes Sills Batholiths

4 Sills Horizontal plutons formed when magma is intruded in between sedimentary layers

5 Dikes intrusive igneous features that cut across preexisting rock layers. Dikes can form when magma invades fractures in the surrounding rocks.

6 must have a surface exposure greater than 100 km2
Batholiths large masses of igneous rock that formed when magma at depth, became crystallized, and was exposed by erosion must have a surface exposure greater than 100 km2

7 Geothermal Gradient Temp naturally increases with depth but is not sufficient to melt rock in the lower crust and upper mantle

8 Origin of Magma 1. Increase Temperature 2. Reduce Pressure
3. Water (Wet rocks melt easier)

9 Additional heat can be generated by
crustal rocks heating up from friction during subduction

10 Where Do Volcanoes Occur?
Convergent plate boundaries: 75% of active volcanoes Ex: Ring of Fire Subduction zone Divergent plate boundaries: as plates move apart, magma rises to fill the space

11 Do we live by a Volcano?


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