Award Abstract # 0538237
Elastic Stress Transfer at Mauna Loa Volcano, Hawaii: Constraints from InSAR and Gravity Measurements

NSF Org: EAR
Division Of Earth Sciences
Recipient: UNIVERSITY OF MIAMI
Initial Amendment Date: February 2, 2006
Latest Amendment Date: February 20, 2008
Award Number: 0538237
Award Instrument: Continuing Grant
Program Manager: Eva Zanzerkia
EAR
 Division Of Earth Sciences
GEO
 Directorate for Geosciences
Start Date: February 1, 2006
End Date: January 31, 2010 (Estimated)
Total Intended Award Amount: $357,000.00
Total Awarded Amount to Date: $357,000.00
Funds Obligated to Date: FY 2006 = $128,430.00
FY 2007 = $115,510.00

FY 2008 = $113,060.00
History of Investigator:
  • Falk Amelung (Principal Investigator)
    amelung@rsmas.miami.edu
Recipient Sponsored Research Office: University of Miami
1251 MEMORIAL DR
CORAL GABLES
FL  US  33146-2509
(305)421-4089
Sponsor Congressional District: 27
Primary Place of Performance: University of Miami
1251 MEMORIAL DR
CORAL GABLES
FL  US  33146-2509
Primary Place of Performance
Congressional District:
27
Unique Entity Identifier (UEI): KXN7HGCF6K91
Parent UEI: VNZZYCJ55TC4
NSF Program(s): Petrology and Geochemistry,
Geophysics
Primary Program Source: app-0106 
app-0107 

01000809DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 0000, 1576, 9196, OTHR
Program Element Code(s): 157300, 157400
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

This project funds the acquisition and analysis of new InSAR and gravity data for Mauna Loa volcano, Hawaii. The PIs will use the Canadian Radarsat satellite and multi-beam SAR imagery to optimally characterize the 3-D displacement field. The SAR data will be complemented by annual gravity surveys in the summit area. Using the new data and inversion methods the researchers will develop a time-dependent model for the magmatic plumbing system of the volcano. The combination of InSAR and gravity can resolve the geometry of the magma reservoir and whether the ongoing rift widening is caused by active intrusion of new magma or gravity-driven spreading. Data analysis is complemented by mechanical modeling of the volcano. The PIs will then use the InSAR-derived models of the magmatic system to evaluate changes of the stress field and whether changes in deformation sources are consistent with static stress change models. This will lead to a better understanding of earthquake processes, eruptions and flank instabilities on the volcano. The research will add to our knowledge of earthquake and volcanic hazards in Hawaii, as well as benefit the scientific community with the sharing of InSAR imagery through WinSAR.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

Note:  When clicking on a Digital Object Identifier (DOI) number, you will be taken to an external site maintained by the publisher. Some full text articles may not yet be available without a charge during the embargo (administrative interval).

Some links on this page may take you to non-federal websites. Their policies may differ from this site.

Amelung, F.,S-H. Yun, T.R. Walter, P. Segall and S.W. Kim "Stress control of deep rift intrusion at Mauna Loa volcano, Hawaii" Science , v.3161026 , 2007 10.1126/science.1140035
Amelung, F.,S-H. Yun, T.R. Walter, P. Segall and S.W. Kim "Stress control of deep rift intrusion at Mauna Loa volcano, Hawaii" Science , v.3161026 , 2007 , p.1 10.1126/science.1140035

Please report errors in award information by writing to: awardsearch@nsf.gov.

Print this page

Back to Top of page