Projects and Initiatives
CANOE
We propose a passive broad-band seismic experiment in northwestern Canada, a setting in which fundamental questions regarding the structure and dynamics of the mantle's upper and lower boundary lay
CATSCAN
Project Website for CAT/SCAN: Calabria-Apennine-Tyrrhenian/Subduction-Collision-Accretion Network
Location
Global CMT
During the summer of 2006, the main activities of the research project known as the Harvard Centroid-Moment-Tensor (CMT) Project moved with Principal Investigator Göran Ekström from Harv
Lamont Cooperative Seismographic Network (LCSN)
Lamont-Doherty Cooperative Seismographic Network (LCSN) monitors earthquakes which occur primarily in the Eastern United States.
Malawi Earthquakes Blog: Assessing Danger on the East African Rift
In December of 2009, nearly a dozen earthquakes of magnitude 5 or greater rattled the southeast African nation of Malawi, killing four, injuring hundreds, and making thousands homeless.
Multidisciplinary Observations of Onshore Subduction (MOOS)
The MOOS experiment seeks to understand the structure and dynamics of subduction in the region of the 1964 Alaska earthquake, one of the three largest recorded (Mw 9.2), where terrane collision is
Location
Nuclear Test Ban Monitoring Research Site
Lamont-Doherty Nuclear Test Ban Monitoring Research.
Ocean Bottom Seismology
Our Ocean Bottom Seismology (OBS) Laboratory develops and operates cutting-edge instrumentation for measuring deformation of the ocean floor in a variety of experimental settings. One of our
Real-Time Double-Difference Earthquake Locations for Northern California
This project develops and implements real-time, high-precision earthquake location algorithms for use in operational seismic monitoring procedures.
Rock Mechanics
Rocks and ice are slip-sliding away in the LDEO Rock Mechanics lab.
SCOOBA
Deployment of a wide-band OBS in the Gulf of California from the R/V New Horizon in Oct 2005. Seismometer is housed in the green sphere, while recording, power, and communications devices are
Strip of Destruction
We mapped the surface trace of the fault rupture for about 5 km on the west bank of the Khunar River, through Balakot and into the Sarash Valley where it apparently ends.
Location
Structure and Evolution of the Oceanic Lithosphere / Asthenosphere System
What is a plate? We undertake a comprehensive analysis designed to significantly advance our understanding of the structure and evolution of oceanic plates.
Testing the Extensional Detachment Paradigm: Scientific Drilling in the Sevier Desert Basin
Testing the Extensional Detachment Paradigm: Scientific Drilling in the Sevier Desert Basin (Basin and Range Province, Western United States)













