DOC PREVIEW
USC GEOL 240Lg - Plate Tonics- The Mechanism and Sea Floor Spreading
Type Lecture Note
Pages 3

This preview shows page 1 out of 3 pages.

Save
View full document
Premium Document
Do you want full access? Go Premium and unlock all 3 pages.
Access to all documents
Download any document
Ad free experience

Unformatted text preview:

GEOL 240Lg 1st Edition Lecture 3 Outline of Last Lecture I II III IV V Transform boundaries San Andreas Fault Mid Oceanic Faults Transform Faults Continental Lithosphere Oceanic Lithosphere Continent Continent Collision Outline Current Lecture I II III IV V VI VII VIII IX Sea Floor Spreading Drawing w explanation Rifting of a Continent What is Decompression melting East African Rift Mount Kilimanjaro Aulacogens Diagram of the Subduction Zone Convergent Plate Boundaries Volcanoes Current Lecture The illustration below is an example of the Sea Floor Spreading It shows how Rifting and Seafloor spreading at the crest Rifting and seafloor spreading in Iceland Rifting of a continent and seafloor spreading to form a new basin This is called Decompression Melting When rift the lithosphere over rising magma plums the release in pressure causes decompression East African Rift Red Sea a lot of fault systems that are dropping of valleys Sometimes rift start to form into an ocean but not all the rifts get to form into oceans Mount Kilimanjaro this is the tallest peak in the continent of Africa This Mt is composed of 3 distinct volcanic cones Kibo 5 895 m Mawenzi 5 149m and Shira 3 962m Aulocagens Mississippi River Broke North America In simple terms aulocagens are failed rift arms Another example of this is the Nigerian River Rift Pacific Ring of Fire This is just an area where a large number of earthquakes and volcanic activity occur There are many eruptions in the Pacific Ocean This explains why we have so many earthquakes in California due to the Pacific Ocean ring of fire The picture above is the Subduction Zone It explains how deep the oceanic lithosphere is and the trenches in the ocean H2o also causes in minerals to be driven off 100km deep melting above slab occurs in 100km and then it goes straight down Convergent Plate Boundaries Lava andesite high visual thick Also there are a lot of gas carbon monoxide Gas bubbles 5km down 100 meter bubble Volcanoes kills people because the pressure is getting lower so it comes out and it stays there because of the pressure contrast Then you guessed it it explodes


View Full Document

USC GEOL 240Lg - Plate Tonics- The Mechanism and Sea Floor Spreading

Type: Lecture Note
Pages: 3
Download Plate Tonics- The Mechanism and Sea Floor Spreading
Our administrator received your request to download this document. We will send you the file to your email shortly.
Loading Unlocking...
Login

Join to view Plate Tonics- The Mechanism and Sea Floor Spreading and access 3M+ class-specific study document.

or
We will never post anything without your permission.
Don't have an account?
Sign Up

Join to view Plate Tonics- The Mechanism and Sea Floor Spreading and access 3M+ class-specific study document.

or

By creating an account you agree to our Privacy Policy and Terms Of Use

Already a member?