viscosity basaltic magma silicic magma pahoehoe
Aa pyroclastics-tephra shield volcano composite
volcano
cindercone volcanic dome caldera crater
flood basalts pillow basalts lahar
nuee ardente
Property |
Shield |
Composite (strato) |
Cinder Cone |
Composition |
Basaltic |
Andesitic |
Basaltic-Andesitic |
Temperature |
Hottest |
Intermediate |
Intermediate |
Silica content |
Least |
Intermediate |
Intermediate |
Viscosity |
Lowest (very fluid) |
Intermediate |
Intermediate |
Products |
Mostly flows |
Flows and tephra |
Tephra |
Hazards |
Lava flows |
Lahars, tephra, nuees ardentes |
Upward eruption of cinders |
Slope |
~ 2-10o |
~ 10-30o |
~ 30o |
Plate Tect. Setting |
Intraplate, Divergent |
Convergent |
Convergent |
Examples |
Hawaii, Iceland |
Mount St. Helens |
Wizard Island |
Great interactive page: http://www.learner.org/exhibits/volcanoes/
Lots of great info: http://www.cotf.edu/ete/modules/volcanoes/volcano.html
Volcanoes links page: http://www.volcanoes.com/webdocs/websitelinks.html
1. What three factors determine the nature of a volcanic eruption?
2. What do pillow lavas indicate about the environment of volcanism?
3. Why are extrusive rocks fine-grained?
4. Why do shield volcanoes have such low slopes?
5. What accounts for the differences between pahoehoe and aa lava flows?
6. Why do composite volcanoes occur near convergent plate boundaries?
7. Explain how Crater Lake formed.
7. Explain how Crater Lake formed.%MCEPASTEBIN%