Submitted by admin on Sun, 2011-09-18 07:00
The latest faculty to join the ranks as assistant professors in the Division of Geological and Planetary Sciences spend a lot of time gazing toward the heavens. Bethany Ehlmann has been working on understanding environmental conditions early in Mars's history, while Heather Knutson focuses on characterizing the properties of the planets that orbit stars other than our sun.
Submitted by admin on Mon, 2011-08-29 07:00
For Andrew Thompson, assistant professor of environmental science and engineering who joined GPS in August, growing up in Rhode Island gave him a natural affinity for the ocean. Now, he studies physical ocean science, focusing on eddies. While Thompson studies the way sea storms move things around, new faculty member and alum Victor Tsai, assistant professor of geophysics, is busy measuring the seismic noise produced by the movements of the ocean—partly from the crashing of waves onto the shore.
Submitted by mwoo on Mon, 2011-08-22 07:00
Astronomers at Caltech have discovered that the dwarf planet 2007 OR10—nicknamed Snow White—is an icy world, with about half its surface covered in water ice that once flowed from ancient, slush-spewing volcanoes. The new findings also suggest that the red-tinged dwarf planet may be covered in a thin layer of methane, the remnants of an atmosphere that's slowly being lost into space.
Submitted by katien on Thu, 2011-08-11 07:00
Like scars that remain on the skin long after a wound has healed, earthquake fault lines can be traced on Earth's surface long after their initial rupture. Typically, this line of intersection between the area where the fault slips and the ground is more complicated at the surface than at depth. But a new study by Caltech researchers of the April 4, 2010, El Mayor–Cucapah earthquake in Mexico reveals a reversal of this trend.
Submitted by katien on Thu, 2011-07-14 07:00
Edward M. Stolper, provost of the California Institute of Technology (Caltech) and William E. Leonard Professor of Geology, has been named a Foreign Member of Great Britain's Royal Society. He is one of eight scientists elected in 2011. Stolper’s election brings to six the number of foreign members of the Royal Society currently on the Caltech faculty.
Submitted by admin on Tue, 2011-06-28 07:00
Ever since a crash landing on Earth grounded NASA's Genesis mission in 2004, scientists have been gathering, cleaning, and analyzing solar wind particles collected by the spacecraft. Now, two new studies published in Science reveal that Earth's chemistry is less like the sun's than previously thought.
Submitted by mwoo on Thu, 2011-06-23 18:00
Were dinosaurs slow and lumbering, or quick and agile? It depends largely on whether they were cold or warm blooded. Now, a team of researchers led by Caltech has developed a new approach to take body temperatures of dinosaurs for the first time, providing new insights into whether dinosaurs were cold or warm blooded.
Submitted by lorio on Wed, 2011-05-25 07:00
A team of scientists led by researchers from Caltech report in this week's issue of the journal Nature that the rocks on which much of a theory on how the "Snowball Earth" ice age ended was based were formed millions of years after the ice age ended, and were formed at temperatures so high there could have been no living creatures associated with them.
Submitted by lorio on Wed, 2011-05-18 23:00
When the magnitude 9.0 Tohoku-Oki earthquake and resulting tsunami struck off the northeast coast of Japan on March 11, they caused widespread destruction and death. Using observations from a dense regional geodetic network (allowing measurements of earth movement to be gathered from GPS satellite data), globally distributed broadband seismographic networks, and open-ocean tsunami data, researchers have begun to construct numerous models that describe how the earth moved that day.
Submitted by lmarkle on Tue, 2011-05-03 07:00
Caltech geologists John Grotzinger and Woody Fischer have been puzzling over a surprising and controversial discovery made in the early 1990s—a discovery that provided some clues as to what might have caused a sudden burst of biodiversity 540 million years ago.