its majestic mountains, the Wasatch Range seems the perfect site for last month’s
Olympic competitions in skiing, snowboarding and bobsledding. But beneath the
wintry landscape, rocks are slowly grinding, lifting the mountains and creating
the potential for an earthquake. “Here in our Wasatch front urban corridor,
the major threat is posed by the Wasatch fault, which is the longest active
normal fault in North America,” says Walter Arabasz, director of the University
of Utah Seismograph Stations.
And that is where Arabasz and his team of earthquake watchers came into play in the Olympic Games. They partnered with the U.S. Geological Survey to put a real-time earthquake information system in place in time for the Olympics. “It’s a convergence of needing to have rapid earthquake information available during the Olympic time-frame, but also the building of an Advanced National Seismic System to modernize earthquake monitoring in the United States,” Arabasz says.
A Shakemap relies on a seismograph network of strong motion sensors that continuously record seismic activity to upload to a telecommunication system. In Utah, 45 sensors lie within and surrounding the urbanized area. In the picture, red circles show strong motion sensors installed in 2000. Red triangles were installed in 2001. The green triangles represent sensors with broadband.
Authorized by Congress in 2000, the Advanced National Seismic System (ANSS) calls for installing more than 6,000 seismic sensors to monitor earthquakes in 26 U.S. metropolitan areas. ANSS is only about 5 percent complete now, but Salt Lake City was one of the lucky few cities to get a head start on the project, Arabasz says. The seismic network features a Shakemap — a rapidly generated computer map that uploads directly to the program’s Web site, where anyone, including emergency managers and earthquake scientists, can view the results.
Lisa M. Pinsker
Read the full story, which appeared
as a Web Extra on February 8, 2002.
Lowest place on Earth is sinking
For the past decade,
sinkholes and wide, shallow subsidence features have become major problems along
the shores of the Dead Sea, in Israel and Jordan. Geoscientists from the Geological
Survey of Israel, the Scripps Institution of Oceanography, Tel Aviv University
and the Technion-Israel Institute are using InSAR (interferometric synthetic
aperture radar) to identify and characterize areas of instability and to measure
rates of subsidence along the Dead Sea shores, on the Lisan Peninsula. Led by
Gidon Baer of the Geological Survey of Israel, the team published their results
in the January GSA Bulletin.
This interferogram of the Lisan Peninsula and its vicinity spans the period from November 1995 to February 1997. The color changes correspond to the changes in satellite-to-ground distances. The so-called fringe color patterns show four different types of subsidence features: 1) coastal subsidence; 2) irregular subsidence at the recently exposed land strip between the peninsula and the western Dead Sea shoreline; 3) subsidence around the margins of a buried salt dome; and 4) a subsiding alluvial fan.
“Once we establish the spatial and temporal relationships between the sinkholes and the gradual subsidence features, the latter, which are easily detected, may serve to map the unstable zones of potentially higher hazard, and we might be able to estimate where future sinkholes will develop,” Baer says.
Lisa M. Pinsker