plate tectonics day3
DESCRIPTION
Plate Tectonics Day3. Review. Plate tectonic Theory http://www.odsn.de/odsn/services/paleomap/animation.html Surface of earth made of rigid “plates” Float on asthenosphere and is in constant motion Explains Drifting continents Mountain building Earthquakes Volcanic activity. - PowerPoint PPT PresentationTRANSCRIPT
Plate Tectonics Day3
Review
• Plate tectonic Theoryhttp://www.odsn.de/odsn/services/paleomap/animation.html
• Surface of earth made of rigid “plates” • Float on asthenosphere and is in constant motion• Explains
Drifting continents
Mountain building
Earthquakes
Volcanic activity
Convection Currents and the Mantle
Effects of crustal plate movement!
Constructive ForcesHelp build land
There are 3Types of Boundaries
Click picture for video
http://www.learner.org/interactives/dynamicearth/plate.html
Convergent Boundaries http://www.learner.org/interactives/dynamicearth/slip2.html
• Boundaries between two plates that are colliding
Subduction http://www.learner.org/interactives/dynamicearth/slip2.html
oceanic plates collide with continental plates, and slide beneath them creating trenches.
Ex. Mt. St. Helens•http://player.discoveryeducation.com/index.cfm?guidAssetId=489D30FF-EC27-483E-825D-A5FA582A57E4
The ocean floor plunges into deep underwater canyons called deep-ocean trenches.
Subduction takes place in deep-ocean trenches. Subduction is the process by which the ocean
floor sinks beneath a deep-ocean trench and back into the mantle.
The RING of fireClick on picture
Hot Spots
hot material rises up through the mantle, heats up the lithosphere and forms a volcano.
Once the plate passes over this hotspot, the volcano becomes inactive.
Ex. Hawaiihttp://player.discoveryeducation.com/index.cfm?guidAssetId=C485747E-A115-41D6-9D42-D6FFE6CA3914
Discovery Educationhttp://player.discoveryeducation.com/index.cfm?guidAssetId=8565EFBE-6F25-42BF-A60C-0BEA7F34ADCA
Mount Nyiragongo VideoLife near the volcano
http://youtu.be/rZLSvO6vJZ0More videos-no sound
http://youtu.be/W_meqhjQxb8
http://youtu.be/6qMYmNg6K_8