Researchers say that magma columns in the Earth's interior can cause continental breakup – under the right circumstances.
In some parts of the Earth, material rises upwards like a column from the boundary layer of the Earth's core and the lower mantle to just below the Earth's crust hundreds of kilometers above. Halted by the resistance of the hard crust and lithospheric mantle, the flow of material becomes wider, taking on a mushroom-like shape. Specialists call these magma columns mantle plumes or simply plumes.
The rise of the Tibetan plateau, the largest topographic anomaly above sea level on Earth, is important for both its profound effect on climate and its reflection of continental dynamics.
For a new study, Katharine Huntington and colleagues employed a cutting-edge geochemical tool - "clumped" isotope thermometry - using modern and fossil snail shells to investigate the uplift history of the Zhada basin in southwestern Tibet.
The tectonic plate that dominates the Pacific "Ring of Fire" is not as rigid as most assume, and it's getting less fiery. according to researchers at Rice University and the University of Nevada.
The makeup of the Earth's lower mantle, which makes up the largest part of the Earth by volume, is significantly different than previously thought.
Global warming has been implicated in many things, it is certainly being implicated in the latest drought in California, the worst since 2002, which was the worst since the early 1990s -and now it is being linked to a change in tectonic plates.
Scientists at Scripps Institution of Oceanography at U.C. San Diego say that the loss of water is causing the entire western U.S. to rise up like an uncoiled spring.
Water has been detected on Mars
in the form of permafrost and there is strong evidence that liquid water was a major component of the martian surface in the past.
Clays are an important mineral group for discovering the past on Mars, not only to the presence of water, since clays are hydrous minerals, but they also provide clues as to the source, type, and volume of fluids, along with indications of timescale and mineral alteration. If you are going to search for textural and chemical biosignatures, clay is a good place to start.
Nearly forgotten research from decades ago complicates the task of quantifying earthquake hazards in the Pacific Northwest, according to a new report.
The report focuses on the Cascadia subduction zone—a giant active fault that slants eastward beneath the Pacific coast of southern British Columbia, Washington, Oregon, and northern California.
Geologic studies in the past three decades have provided increasingly specific estimates of Cascadia earthquake sizes and repeat times. The estimates affect public safety through seismic provisions in building design and tsunami limits on evacuation maps.
Tokyo is a city of more than 13 million people and they are no strangers to earthquakes. The city, like much of Japan, has been devastated by earthquakes in the past and likely will be again - but when?
Ongoing slow-slip earthquakes can't usually be felt at the surface but they play a role in relieving or building up geological stress and recent research examining plate movements under Tokyo has found that, since the massive magnitude-9 Tohoku earthquake and tsunami in March 2011, recurrence intervals for non-damaging slow-slip quakes beneath Japan's capital have shortened.
This has led some seismologists to wonder if this aseismic creep could be signaling a countdown to Tokyo's next "big one."
A long lasting foreshock series controlled the rupture process of this year's great earthquake near Iquique in northern Chile, according to an international research team
The earthquake was heralded by a three quarter year long foreshock series of ever increasing magnitudes culminating in a Mw 6.7 event two weeks before the mainshock.
The mainshock (magnitude 8.2) finally broke, on April 1st, a central piece out of the most important seismic gap along the South American subduction zone. The study reveals that the Iquique earthquake occurred in a region where the two colliding tectonic plates where only partly locked.
The biggest mystery in the mid-east is why countries of one religion won't put the country of another religion on any geographical maps in any of its schools, but the second biggest mystery is why many of the oldest parts of Jerusalem's Western Wall look like they could have been placed yesterday.
The Western Wall is a remnant of the ancient wall that surrounded the courtyard of the Jewish Temple in Jerusalem. It is located in Jerusalem's Old City at the foot of the Temple Mount.