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Pebbles on Mars likely traveled tens of miles down a riverbed, Penn study finds

A new method developed by Penn researchers can quantify the transport distance of river pebbles from their shape alone, providing evidence for an extensive river system on Mars. The study suggests that Martian pebbles traveled around 30 miles from their source, offering insights into the planet's geological history and potential for life.

SourceUniversity of Pennsylvania·JournalNature Communications·DateOct 13, 2015

Martian glass -- window into possible past life

Researchers from Brown University have detected deposits of glass within impact craters on Mars, suggesting that it could preserve signs of life. The study found large glass deposits in several ancient yet well-preserved craters, including Hargraves near Nili Fossae trough.

SourceBrown University·JournalGeology·DateJun 8, 2015

Researchers hone technique for finding signs of life on the Red Planet

Researchers at the University of Kansas are working to improve the detection of life on Mars by combining Raman spectroscopy with gas chromatography/mass spectroscopy. They aim to analyze rocks from Earth similar to those found on Mars to strengthen evidence collection, as conditions on the Martian surface are inhospitable.

SourceUniversity of Kansas·JournalPhilosophical Transactions of the Royal Society of London·DateMay 14, 2015

Mars: The planet that lost an ocean's worth of water

Scientists have estimated that Mars once had a massive ocean covering 19% of its surface, which would have made the planet habitable for longer. The new research uses detailed observations of water in Mars' atmosphere to determine the amount of water lost over time.

SourceESO·JournalScience·DateMar 5, 2015

The highest plume ever observed on Mars

Researchers have detected a mysterious high plume on Mars, extending horizontally about 500 km and reaching an exceptional altitude of 200-250 km above the planet's surface. The team used images from amateur astronomers and spacecraft to analyze the phenomenon, exploring possible scenarios such as cloud or auroral emission.

Gully patterns document Martian climate cycles

Researchers from Brown University found new evidence of glacier-like ice deposits advancing and retreating multiple times in Mars' midlatitudes, suggesting recent climate cycles. The study suggests that the planet's wobbly rotation around its axis may have driven these ice ages.

SourceBrown University·JournalIcarus·DateJan 28, 2015

The 2 faces of Mars

A massive celestial object impacted Mars, generating a magma ocean that solidified into the mountainous highlands of the southern hemisphere. This event, occurring around 4-15 million years after Mars' formation, is believed to have triggered volcanic activity and changed the planet's magnetic field.

SourceETH Zurich·JournalGeophysical Research Letters·DateJan 28, 2015

New analyses of Martian chemical maps suggest water bound to sulfates in soil

A new study suggests that water is bound to sulfates in Martian soil, a key finding with implications for the search for life on Mars. The research team analyzed elemental data from the Gamma Ray Spectrometer onboard the Mars Odyssey orbiter and found a spatial association between sulfur and hydrogen in the southern latitudes of Mars.

SourceLouisiana State University·JournalGeophysical Research Letters·DateJan 2, 2015

Mars, too, has macroweather

A new study by McGill University and UCL finds that Mars experiences a transitional 'macroweather' regime between weather and climate. The sun plays a major role in determining macroweather on Mars, with temperature and wind fluctuations occurring over 1.8 Martian days.

SourceMcGill University·JournalGeophysical Research Letters·DateNov 13, 2014

Mars One -- and done?

A team of MIT researchers assessed the Mars One mission's technical feasibility, highlighting the need for new technologies to keep humans alive on Mars. The study found that a system to remove excess oxygen and more advanced water extraction methods are required, among other innovations.

Mars mineral could be linked to microbes

Researchers have found microbes create an environment that allows stevensite to form, raising new questions about the Martian deposits and their possible links to life on Mars. Microbialites are the earliest large-scale evidence of life on Earth, demonstrating how microscopic organisms join together to build enormous structures.

SourceAustralian National University·JournalGeology·DateMay 19, 2014

Against the current with lava flows

Researchers found that lava flows, not water, carved the massive Noctis Labyrinthus and Valles Marineris canyons on Mars. The study suggests that there was less water on Mars than previously thought, making life on the planet less likely.

SourceETH Zurich·JournalJournal of Volcanology and Geothermal Research·DateMay 12, 2014