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Magma in Earth’s Mantle Forms Deeper Than Once Thought

By Guest PostJanuary 10, 2013Environmentananya mallik, anthony withers, brown university, carbon dioxide, carbonated rock, convection, crust, deeper magma, density, earth, earthquake, express lane, geologist, greg hirth, high pressure, jennifer wade, kyusei tsuno, magma, mantle, marc hirschmann, national science foundation, non carbonated rock, ocean floor, peridotite, rajdeep dasgupta, rice university, rock, seafloor, seismic wave, silicate rich mantle, temperature, university of minnesota, volcanic eruption, within the earth

Study simulating pressures in mantle beneath the ocean floor shows that rocks can melt at depths up to 250 kilometers

Magma forms far deeper than geologists previously thought, according to new research results.

A team led by geologist Rajdeep Dasgupta of Rice University put very small samples of peridotite, rock derived from Earth’s mantle, under high pressures in a laboratory.

The scientists found that the rock can and does liquify, at least in small amounts, at pressures equivalent to those found as deep as 250 kilometers down in the mantle beneath the ocean floor. (more…)

Within the Earth, Blobs of Molten Iron on the Move

By Guest PostDecember 29, 2012Scienceamount of iron, boundary zone, interior layer, iron rich blobs, mantle, metal rich blobs, morphological instability, ocean islands, rocky mantle, seismic wave

New research by Yale University scientists suggests an explanation for the amount of iron in the Earth’s largest interior layer, the mantle: migrating “iron-rich blobs” generated by chemical interactions in the zone between the planet’s core and mantle. (more…)

3-D Laser Map Shows Earthquake Zone Before and After

By Guest PostFebruary 10, 2012Science2010 mexicali earthquake, 3d post earthquake image, agricultural fields, arizona state university, austin elliott, borrego fault, China, colorado river, colorado river delta, crust, data, davis, desert floor, earth science, earthquake, earthquake zone, earthscope, fault, fault behavior, fault rupture, fault surface ruptures, floodplain, geologist, greg anderson, indiviso fault, jing liu zeng, john fletcher, ken hudnut, laser pulses, lidar, light detection and ranging, magnitude, mexicali, Mexico, michael oskin, multi fault earthquake, national science foundation, ncalm, off fault deformation, orlando teran, pescadores fault, peter gold, post earthquake topography, pre earthquake, ramon arrowsmith, ridge, rock sample, san andreas, scarp, seismic hazard, seismic wave, united states, university of california

*Geologists learn how earthquakes change the landscape — down to a few inches*

Geologists have a new tool to study how earthquakes change the landscape–down to a few inches. It’s giving scientists insights into how earthquake faults behave.

In this week’s issue of the journal Science, a team of scientists from the United States, Mexico and China reports the most comprehensive before-and-after picture yet of an earthquake zone, using data from the magnitude 7.2 event that struck near Mexicali, Mexico, in April 2010. (more…)

Tag Archives: seismic wave

Magma in Earth’s Mantle Forms Deeper Than Once Thought

Within the Earth, Blobs of Molten Iron on the Move

3-D Laser Map Shows Earthquake Zone Before and After