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Page 1: 0',*/)-01(-)*2001&3('4)-*geoprisms.org/wpdemo/wp-content/uploads/2015/03/RIE2010_WP_D… · HEINRICH ET AL.: NEAR-HELD MODELING OF THE JULY 17, 1998 TSUNAMI — cosÐ) +hghsin + q

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Page 2: 0',*/)-01(-)*2001&3('4)-*geoprisms.org/wpdemo/wp-content/uploads/2015/03/RIE2010_WP_D… · HEINRICH ET AL.: NEAR-HELD MODELING OF THE JULY 17, 1998 TSUNAMI — cosÐ) +hghsin + q

@)'(&'AB*)3*%.?9*LMMM* N%00'(*)3*%.?9*LMML*

OP*E".J*OQQR*C%0"%*S)7*G"'()%*N-"(%$'*

Page 3: 0',*/)-01(-)*2001&3('4)-*geoprisms.org/wpdemo/wp-content/uploads/2015/03/RIE2010_WP_D… · HEINRICH ET AL.: NEAR-HELD MODELING OF THE JULY 17, 1998 TSUNAMI — cosÐ) +hghsin + q

Masson  et  al.,  2006  

Single  Events,  Margin-­‐Scale  Impacts  30-­‐45oN    US  Atlan4c  Margin  

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Why  submarine  landslides?  

1)  Widespread,  large-­‐scale  margin  evolu4on  

2)  Rapid,  m-­‐km  but  affect  overall  margin  shape    3)  Geohazard  poten4al  (process  and  society)    4)  Integrates  surface  processes  and  feedbacks  

5)  Mul4-­‐disciplinary  -­‐  geology,  geophysics,  geotechnics,  fluids…  

Page 5: 0',*/)-01(-)*2001&3('4)-*geoprisms.org/wpdemo/wp-content/uploads/2015/03/RIE2010_WP_D… · HEINRICH ET AL.: NEAR-HELD MODELING OF THE JULY 17, 1998 TSUNAMI — cosÐ) +hghsin + q

Key  Data/Observa4ons  –  Slide  and  Adjacent    

1)  Morphology  and  distribu4on      2)  In  situ  pressure,  temperature,  and  strength    

   3)  Tilt  and  strain  data    4)  Mul4ple  (4d)  images  or  measurements        

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Hornbach  et  al.  White  Paper  Sawyer  et  al.,  2009  

Page 7: 0',*/)-01(-)*2001&3('4)-*geoprisms.org/wpdemo/wp-content/uploads/2015/03/RIE2010_WP_D… · HEINRICH ET AL.: NEAR-HELD MODELING OF THE JULY 17, 1998 TSUNAMI — cosÐ) +hghsin + q

GeoPRISMS-­‐Addressable  Ques4ons  

What  dictates  size,  runout,  and  recurrence?    -­‐  margin  shape  and  evolu4on  

 What  drives  failure  along  different  margins?    What  controls  hazard  poten4al?    Is  the  failure  evolving  or  stopping?  Why?      How  are  different  failures  recorded  in  the  strata?