Earth and Planetary Science Letters (EPSL) is a weekly, peer-reviewed, scientific journal published by Elsevier. It was first issued in January 1966 (volume 1). The listed editors are R.W. Carlson (Carnegie Institution), P. deMenocal (Columbia University), T.M. Harrison (UCLA), Y. Ricard (Université Claude Bernard), P. Shearer (UCSD), T. Spohn (German Aerospace Center), L. Stixrude (University College London). EPSL publishes original research articles cover the processes of Earth and planets generally described as physical, chemical and mechanical. The focus of further topical coverage includes geosciences such as tectonics, crust and mantle composition, and atmosphere studies of both Earth and other solar or extrasolar planets. EPSL is indexed in the following databases: The journal has a 2009 impact factor of 4.062, ranking third in the category "Geophysics & Geochemisry".
Ferromanganese crusts record past climates
The onset of northern hemispheric glaciation cycles three million years ago has dramatically changed Arctic climate. Scientists of the GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany have now for ...
New Mercury surface composition maps illuminate the planet's history
Two new papers from members of the MESSENGER Science Team provide global-scale maps of Mercury's surface chemistry that reveal previously unrecognized geochemical terranes—large regions that have compositions ...
Gullies on Vesta suggest past water-mobilized flows
(Phys.org)—Protoplanet Vesta, visited by NASA's Dawn spacecraft from 2011 to 2013, was once thought to be completely dry, incapable of retaining water because of the low temperatures and pressures at its ...
Scientists find meteoritic evidence of Mars water reservoir
(Phys.org)—NASA and an international team of planetary scientists have found evidence in meteorites on Earth that indicates Mars has a distinct and global reservoir of water or ice near its surface.
Dust from a comet has been discovered for the first time on the Earth's surface
Why Iceland formed so differently from the gentle early Earth
How do you take the temperature of the Earth billions of years ago? The answer lies in the rocks.
Study of Chile earthquake finds new rock structure that affects earthquake rupture
Researchers from the University of Liverpool have found an unusual mass of rock deep in the active fault line beneath Chile which influenced the rupture size of a massive earthquake that struck the region ...
Early Earth less hellish than previously thought
Conditions on Earth for the first 500 million years after it formed may have been surprisingly similar to the present day, complete with oceans, continents and active crustal plates.
Solar system simulation reveals planetary mystery
When we look at the Solar System, what clues show us how it formed? We can see pieces of its formation in asteroids, comets and other small bodies that cluster on the fringes of our neighborhood (and sometimes, ...
Arctic sea ice influenced force of the Gulf Stream
The force of the Gulf Stream was significantly influenced by the sea ice situation in the Fram Strait in the past 30,000 years. Scientists at the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine ...
The bend in the Appalachian mountain chain is finally explained
The 1500 mile Appalachian mountain chain runs along a nearly straight line from Alabama to Newfoundland—except for a curious bend in Pennsylvania and New York State. Researchers from the College of New ...
Rainwater discovered at new depths
University of Southampton researchers have found that rainwater can penetrate below the Earth's fractured upper crust, which could have major implications for our understanding of earthquakes and the generation ...
Meteorite find may be 'missing half' of interstellar collision
Extinct undersea volcanoes squashed under Earth's crust cause tsunami earthquakes
New research has revealed the causes and warning signs of rare tsunami earthquakes, which may lead to improved detection measures.
Ice-loss moves the Earth 250 miles down
At the surface, Antarctica is a motionless and frozen landscape. Yet hundreds of miles down the Earth is moving at a rapid rate, new research has shown.