1 / 38

INTRAPLATE

6. Earthquakes that shouldn’t happen. DIFFUSE BOUNDARY ZONES. INTRAPLATE. NARROW BOUNDARIES. Most earthquakes are on plate boundaries, but some are within plates - intraplate. 1900 -. Almost all large earthquakes in North America are in the western plate boundary zone.

amato
Download Presentation

INTRAPLATE

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. 6. Earthquakes that shouldn’t happen DIFFUSE BOUNDARY ZONES INTRAPLATE NARROW BOUNDARIES Most earthquakes are on plate boundaries, but some are within plates - intraplate.

  2. 1900 - Almost all large earthquakes in North America are in the western plate boundary zone. To see New Madrid, we plot down to magnitude 5, which aren’t very big & do little harm. To resolve details, plot eastern North America down to magnitude 3. See New Madrid and other similar eastern earthquake zones. M>3 DD 10.1

  3. Charleston, South Carolina 1886 M ~ 7 Similar to New Madrid 1811-12 Damaged buildings - especially brick & caused about 60 fatalities Similar sand blows Recovery took about five years DD 10.2

  4. Grand Banks, Newfoundland 1933 M 7.3 Caused landslide & tsunami Broke transatlantic cables Intensity pattern like 1811-12 GSC

  5. Earthquakes require • Faults to slip on • Force (stress) to cause motion of faults At plate boundaries, faults are the boundaries and plate motions provide stresses that cause motion What about within continental plates?

  6. Granite continents vs basalt oceans Continental crust is less dense, so continents are higher than ocean basins Continents float above denser mantle Continents don’t subduct, unlike oceans Continents formed earlier in Earth history and can reach ages of billions of years compared to 200 Ma oceans DD 10.3

  7. WILSON CYCLE Oceanic lithosphere is formed at midocean ridges & destroyed at subduction zones Continental plates are rifted apart and then collide, but survive East African Rift Gulf of Aden, Gulf of California Andes Southern Europe Himalaya Zagros Continental rifting Young ocean Ocean-continent convergence Closing ocean Stein & Wysession, 2003 Continental collision DD 10.4

  8. Global Plate TectonicsJurassic to Present Day By L.A. Lawver, M.F. Coffin, I.W.D. Dalziel L.M. Gahagan, D.A. Campbell, and R.M. Schmitz 2001, University of Texas Institute for Geophysics February 9, 2001

  9. Activity 6.1: Wilson cycle When does the North Atlantic rift open? When does the South Atlantic rift open? When does India collide with Eurasia? When does Arabia rift away from Africa?

  10. Some continental rifts fail to split a continent Leave “failed rift” - long valley of stretched & faulted rock that gets filled up & buried by sediments MCRS Midcontinent Rift system Failed to split North America ~1.1 Ga (billion years ago)

  11. Activity 6.2 Why does the MCRS show up so well in gravity & magnetic maps? USGS

  12. Shay & Trehu, 1993

  13. Over billions of years, continents retain structures formed by rifting, collisions, failed rifts, basin formation, faulting, etc Stresses within the plate - from various sources - can reactivate these & cause intraplate earthquakes S. Marshak

  14. A set of failed rifts, the Reelfoot Rift and Rough Creek Graben, are associated with the New Madrid & Wabash Valley seismic zones S. Marshak

  15. Activity 6.3: Spot formation of the MCRS and Reeflfoot/Rough creek rifts Whitmeyer & Karlstrom 2007

  16. Reelfoot Rift formed when supercontinent of Rodinia broke up DD10.5 Meert & Torsvik, 2003

More Related