Download presentation
Presentation is loading. Please wait.
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?
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.