Listening to Earthquake Faults 'Talk' in Haiti

Following the January 12, 2010 Haiti earthquake, A. M. Freed traveled to Haiti to conduct GPS fieldwork to measure crustal deformation caused by the earthquake. Here, he is shown setting up a GPS receiver in a tent city in Port-au-Prince.
(Image credit: A. M. Freed)

This ScienceLives article was provided to LiveScience in partnership with the National Science Foundation.

Andrew Freed, an associate professor of geophysics at Purdue University, seeks to understand the evolution of stresses in the crust before, during and after earthquakes. Knowledge of where stresses are building the fastest or which faults currently support the highest unrelieved stress are valuable in estimating current seismic hazards, including continuing hazards in Haiti. Freed uses measurements of surface deformation from highly sensitive GPS receivers to constrain numerical models of earthquake and plate-tectonic processes. Such models have been used to, amongst other things, understand how one earthquake can lead to another on a nearby fault and how warm rocks below the surface flow following earthquakes. Freed also uses numerical models to study the mechanics of the crust on other planets and is currently using new observations from the MESSENGER spacecraft to understand the tectonics of Mercury. Read about Freed’s recent experience conducting fieldwork in Haiti following the January 12, 2010 earthquake; learn about the latest updates on the Haitian humanitarian situation, failed buildings, and geologic threats in the Learning from Haiti website; and learn more about researcher experiences in Haiti at the NSF Geophysicists in Haiti Blog. For Freed’s answers to the ScienceLives 10 questions, see below.

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