extra credit option: attend the public lecture by prof. antonio lazcano on tuesday (tomorrow)...
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Location of Earth’s Hot-spots PLATETECTONICSPLATETECTONICSTRANSCRIPT
Extra Credit Option:Extra Credit Option:
Attend the Public Lecture by Prof. Antonio Lazcano on Tuesday (tomorrow) evening, Feb 11 at 7:30 PM in Gammage Auditorium here on campus. Write up a short summary 2-3 paragraphs for the talk, highlighting the aspects you found most interesting. Bring your write-up to class on Wednesday. Be sure to write your name and ASU ID at the top of the page.
Today’s Lecture:Today’s Lecture:
Plate margins and associated geological pheneomena.
- Intraplate hot-spots.- Divergent plate margins in continental
settings (origin of new ocean basins).- Convergent margins- Continental margin settings.- Transform margins (ridge transforms and
on-land transforms. Brief Review Quiz Next time: Interlude A and Chapter 5!
Location of Earth’s Hot-spotsLocation of Earth’s Hot-spotsPLATEPLATETECTONICSTECTONICS
Yellowstone Hot SpotYellowstone Hot SpotPLATEPLATETECTONICSTECTONICS
Yellowstone Hot SpotYellowstone Hot SpotPLATEPLATETECTONICSTECTONICS
Types of Plate BoundariesTypes of Plate BoundariesPLATEPLATETECTONICSTECTONICS
divergent boundaries
convergent boundaries
transform fault boundaries
3 types
Continental Rifting: East AfricaContinental Rifting: East Africa PLATEPLATETECTONICSTECTONICS
Red Sea (looking southeast)
PLATEPLATETECTONICSTECTONICS Opening of the Red Sea
Opening of the Red SeaOpening of the Red SeaPLATEPLATETECTONICSTECTONICS
Formation of Triple JunctionsFormation of Triple JunctionsPLATEPLATETECTONICSTECTONICS
ocean-continent
ocean-ocean
continent-continent
3 Types of Convergent Plate Margins
Types of Continental MarginsTypes of Continental Margins
“Active” Found along convergent
plate margins: Primarily around the Pacific rim. Characterized by active narrow continental shelves and active mountain building processes (earthquakes & volcanic activity). Accretionary wedges of sediment which are scraped off the top of a subducting slab.
Types of Continental MarginsTypes of Continental Margins
“Passive” Found within plate interiors:
Continental margin not = a plate marginExamples are continental margins around Atlantic. Broad continental shelves consist of thick wedges of sediment deposited along margins Few earthquakes or volcanic eruptions.
Comparison of Active and Passive Continental Margins
Transform fault boundaries
Strike-slip faults where plates slide past each other: No production/destructionof material
Most connect mid-ocean ridge segments
Others are “on-land” transforms like the San Andreas Fault.
Transform Plate MarginsTransform Plate MarginsPLATEPLATETECTONICSTECTONICS
Transform Plate MarginsTransform Plate MarginsPLATEPLATETECTONICSTECTONICS
On-Land Transform Faults
San Francisco Peninsula and San Andreas Fault
In-class exercise. Name:______________________GLG 101 Prof. Farmer ASU ID:________________
Compare the continental margin of the west coast of S. America with the east coast of N. America.
1) South Am.
2) North Am.
Questions:a) Active or passive continental margin?b) Draw a cross-section (a side view) of each area, labeling the most important features.