About PASSCAL

If this photo (below) of a 6' 1" tall individual looking up at the top of the solar panel mast doesn't cause one to wonder how much snow the mountains near Cornucopia, Oregon receive, a Snow Cat (below left) at a nearby lodge certain makes it's clear - lots of it. This temporary seismic station installed in the mountains of eastern Oregon is part of Dr. Ray Russo's Western Idaho Shear Zone Earthscope Flexible Array experiment. Spanning eastern Oregon to eastern Idaho, the seismic network covers arguably some of the most remote and rugged mountains of the contiguous United States.

The American Geophysical Union's annual fall meeting is the premiere annual event for the geoscience community, and the AGU Fall Meeting 2011 was bigger and better than ever. Several presentations at the meeting concerned IRIS/PASSCAL directly, while many others featured geoscience projects supported by IRIS.  Here are links to abstracts for selected AGU 2011 presentations by IRIS and PASSCAL personnel, and for selected projects which benefited from IRIS/PASSCAL involvement.

PASSCAL's Polar Group supported AGAP deployments in one of the most extreme polar environments on the planet.

Results are now emerging from the AGAP Project, funded by the National Science Foundation through its Office of Polar Programs. AGAP, which stands for Antarctica's Gamburtsev Province, has been probing the Gamburtsev mountain range for years. These mountains, completely covered by Antarctic ice, were not even discovered until 1958. New data now coming out are showing that these mountains have a youthful topography much like that of the Alps in Europe, and have not been weathered significantly.  Furthermore, the history of the root of the range can now be tracked back to one billion years in the past, with major rejuvenation events in the Permian and Cretaceous periods (~250 and 100 million years ago respectively). One reason the Gamburtsev range is important is that it is believed to be the initial site of Antarctic ice-sheet growth during major climatic changes some 35 million years ago.

Researchers Andy Nyblade of Penn State and Douglas Wiens and Patrick Shore of Washington University in St. Louis are part of the seismic portion of the project, called GamSeis. The IRIS/PASSCAL Instrument Center provided an array of broadband seismic stations used for the project by Wiens and Shore, along with Penn State's Nyblade, and Masaki Kanao of the National Institute of Polar Research (NIPR).

This is the time of year when the Polar group at PASSCAL is busy deploying teams to the Antarctic. Since polar conditions make for difficult site installations, PASSCAL is pleased to present the following instructive videos of Antarctic station deployments.

Courtesy of Audrey Huerta of Central Washington University, here is a time-lapse video of the difficult installation of a POLENET seismic system on a rock surface at Miller Ridge in the Transantarctic Mountains. This installation took about 4 hours in real-time. You will see shadows encroaching as the sun sets toward the end of the four-minute video.

When the earth shook near Richmond, Virginia on August 23, 2011 at 1:51 PM EDT (17:51:04 UTC), millions of inhabitants of the eastern seaboard were surprised by the magnitude 5.8 tremor. The seismic community has responded in force, rapidly deploying dozens of new stations to record aftershocks of this rare event. (The largest previous earthquake in Virginia's history was a magnitude 5.9 event in 1897.)