
NSF Org: |
EAR Division Of Earth Sciences |
Recipient: |
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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 2007 = $115,510.00 FY 2008 = $113,060.00 |
History of Investigator: |
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Recipient Sponsored Research Office: |
1251 MEMORIAL DR CORAL GABLES FL US 33146-2509 (305)421-4089 |
Sponsor Congressional District: |
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Primary Place of Performance: |
1251 MEMORIAL DR CORAL GABLES FL US 33146-2509 |
Primary Place of
Performance Congressional District: |
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Unique Entity Identifier (UEI): |
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Parent UEI: |
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NSF Program(s): |
Petrology and Geochemistry, Geophysics |
Primary Program Source: |
app-0107 01000809DB NSF RESEARCH & RELATED ACTIVIT |
Program Reference Code(s): |
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Program Element Code(s): |
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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
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