AUSTIN,
Texas — Slow slip earthquakes, a type of slow motion tremor, have
been detected at many of the world’s earthquake hotspots, including
those found around the Pacific Ring of Fire, but it is unclear how
they are connected to the damaging quakes that occur there.
Scientists at The University of Texas at Austin have now revealed the
earthquakes’ inner workings using seismic CT scans and
supercomputers to examine a region off the coast of New Zealand known
to produce them. (more…)
On 4 September 2010, a powerful 7.1 magnitude earthquake struck the South Island of New Zealand near Christchurch. The earthquake’s epicentre was 40 kilometres (25 mi) west of Christchurch, near the town of Darfield. Its known as the Canterbury earthquake or Darfield earthquake. The massive earthquake distorted railroad tracks that crossed the fault line near Rolleston.
AUSTIN, Texas — Research published in the May 6 edition of Science indicates that slow-motion earthquakes or “slow-slip events” can rupture the shallow portion of a fault that also moves in large, tsunami-generating earthquakes. The finding has important implications for assessing tsunami hazards. The discovery was made by conducting the first-ever detailed investigation of centimeter-level seafloor movement at an offshore subduction zone.(more…)
The disastrous March 22 landslide that killed 43 people in the rural Washington state community of Oso involved the “remobilization” of a 2006 landslide on the same hillside, a new federally sponsored geological study concludes.
The research indicates the landslide, the deadliest in U.S. history, happened in two major stages. The first stage remobilized the 2006 slide, including part of an adjacent forested slope from an ancient slide, and was made up largely or entirely of deposits from previous landslides. The first stage ultimately moved more than six-tenths of a mile across the north fork of the Stillaguamish River and caused nearly all the destruction in the Steelhead Haven neighborhood. (more…)
Geologic time is shorthand for slow-paced. But new measurements from steep mountaintops in New Zealand shows that rock can transform into soil more than twice as fast as previously believed possible.
The findings were published Jan. 16 in the early online edition of Science. (more…)
Jo Varner, University of Utah biology doctoral student, is currently conducting research on how small mammals like Pikas are coping with Earth’s warming climate. Her study is concentrated on Pikas in the Columbia River Gorge area in the U.S, which is an unusual habitat for this species. Recently we had the opportunity to talk to Miss Varner about her research, why it is important and how life as a research scientist is. Here is what we learned from Miss Jo Varner:(more…)
COLLEGE PARK, Md. – Cold-sensitive mangrove forests have expanded dramatically along Florida’s Atlantic Coast as the frequency of killing frosts has declined, according to a new study based on 28 years of satellite data from the University of Maryland and the Smithsonian Environmental Research Center in Edgewater, Md.
Between 1984 and 2011, the Florida Atlantic coast from the Miami area northward gained more than 3,000 acres (1,240 hectares) of mangroves. All the increase occurred north of Palm Beach County. Between Cape Canaveral National Seashore and Saint Augustine, mangroves doubled in area. Meanwhile between the study’s first five years and its last five years, nearby Daytona Beach recorded 1.4 fewer days per year when temperatures fell below 28.4 degrees Fahrenheit (-4 degrees Celsius). The number of killing frosts in southern Florida was unchanged.(more…)
New Zealand’s geologic hazards agency reported this week an ongoing, “silent” earthquake that began in January is still going strong. Though it is releasing the energy equivalent of a 7.0 earthquake, New Zealanders can’t feel it because its energy is being released over a long period of time, therefore slow, rather than a few short seconds.
These so-called “slow slip events” are common at subduction zone faults – where an oceanic plate meets a continental plate and dives beneath it. They also occur on continents along strike-slip faults like California’s San Andreas, where two plates move horizontally in opposite directions. Occurring close to the surface, in the upper 3-5 kilometers (km) of the fault, this slow, silent movement is referred to as “creep events.” (more…)
