Researchers from Brown Univ. have completed a new analysis of an ancient Martian lake system in Jezero Crater, near the planet’s equator. The study finds that the onslaught of water that filled the crater was one of at least two separate periods of water activity in the region surrounding Jezero.
Lava tubes large enough to house cities could be structurally stable on the moon, according to a...
A Carnegie Institute-led team was able to discover five new forms of silica under extreme...
A research group in the Univ. of Arizona Lunar and Planetary Laboratory has found evidence in meteorites that hint at the discovery of a previously unknown region within the swirling disk of dust and gas known as the protoplanetary disk, which gave rise to the planets in our solar system.
New modeling and analyses of fault geometry in the Earth's crust by geoscientist Michele Cooke and colleagues at the Univ. of Massachusetts Amherst are advancing knowledge about fault development in regions where one geologic plate slides past or over another, such as along California's San Andreas Fault and the Denali Fault in central Alaska.
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 distinct from their surroundings. The presence of these large terranes has important implications for the history of the planet.
As everyone who lives in the San Francisco Bay Area knows, the Earth moves under our feet. But what about the stresses that cause earthquakes? How much is known about them? Until now, our understanding of these stresses has been based on macroscopic approximations.
Violent collisions between the growing Earth and other objects in the solar system generated significant amounts of iron vapor, according to a new study by Lawrence Livermore National Laboratory. The results show that iron vaporizes easily during impact events, which forces planetary scientists to change how they think about the growth of planets and evolution of our solar system.
The activity of the sun is an important factor in the complex interaction that controls our climate. New research now shows the impact of the sun isn’t constant over time, but has greater significance when the Earth is cooler. There has been much discussion as to whether variations in the strength of the sun have played a role in triggering climate change in the past.
Geysers like Old Faithful in Yellowstone National Park erupt periodically because of loops or side-chambers in their underground plumbing, according to recent studies by volcanologists at the Univ. of California, Berkeley. The key to geysers is an underground bend or loop that traps steam and then bubbles it out slowly to heat the water column above until it is just short of boiling.
Sea levels from New York to Newfoundland jumped up about four inches in 2009 and 2010 because ocean circulation changed, a Univ. of Arizona-led team reports in Nature Communications. The team was the first to document that the extreme increase in sea level lasted two years, not just a few months.
Engineers have completed one of the most precise evaluations yet about the impact of a major tsunami event on the Columbia River. They found what forces are most important in controlling water flow and what areas might be inundated.
At least five mass extinction events have profoundly changed the history of life on Earth. But a new study led by researchers at the Univ. of Gothenburg shows that plants have been very resilient to those events. For over 400 million years, plants have played an essential role in almost all terrestrial environments and covered most of the world's surface.
A spark from a lightning bolt, interstellar dust or a subsea volcano could have triggered the very first life on Earth. But what happened next? Life can exist without oxygen; but without plentiful nitrogen to build genes, life on the early Earth would have been scarce. The ability to use atmospheric nitrogen to support more widespread life was thought to have appeared roughly 2 billion years ago.
Pioneering techniques that use satellites to monitor ocean acidification are set to revolutionize the way that marine biologists and climate scientists study the ocean. This new approach, published in Environmental Science and Technology, offers remote monitoring of large swathes of inaccessible ocean from satellites that orbit the Earth some 700 km above our heads.
New techniques are allowing scientists to understand how carbon dioxide, released from the deep ocean, helped to end the last ice age and create our current climate. An international team studied the shells of ancient marine organisms that lived in surface waters of the southern Atlantic and eastern equatorial Pacific oceans thousands of years ago.
Deep cuts in greenhouse gas emissions, while necessary, may not happen soon enough to stave off climate catastrophe. So, in addition, the world may need to resort to so-called geoengineering approaches that aim to deliberately control the planet's climate. That's according to a National Research Council committee that released a pair of sweeping reports on climate intervention techniques.
Seismic waves are helping scientists to plumb the world’s deepest mystery: the planet’s inner core. Thanks to a novel application of earthquake-reading technology, a research team at the Univ. of Illinois and colleagues at Nanjing Univ. in China have found that the Earth’s inner core has an inner core of its own, which has surprising properties that could reveal information about our planet.
A team of Carnegie Institute scientists have found “beautifully preserved” 15-million-year-old thin protein sheets in fossil shells from southern Maryland. The team collected samples from Calvert Cliffs, along the shoreline of the Chesapeake Bay, a popular fossil collecting area. They found fossilized shells of a snail-like mollusk called Ecphora that lived in the mid-Miocene era.
NWA 7034, a meteorite found a few years ago in the Moroccan desert, is like no other rock ever found on Earth. It’s been shown to be a 4.4 billion-year-old chunk of the Martian crust, and according to a new analysis, rocks just like it may cover vast swaths of Mars.
Geologists from Brown Univ. have found new evidence that glacier-like ice deposits advanced and retreated multiple times in the mid-latitude regions of Mars in the relatively recent past. For the study, the researchers looked at hundreds of gully-like features found on the walls of impact craters throughout the Martian mid-latitudes.
A technology developed by Stanford Univ. scientists for passively probing the seafloor using weak seismic waves generated by the ocean could revolutionize offshore oil and natural gas extraction by providing real-time monitoring of the subsurface while lessening the impact on marine life.
Pioneering new research has debunked the theory that the asteroid thought to have led to the extinction of dinosaurs also caused vast global firestorms that ravaged planet Earth. A team of researchers from the Univ. of Exeter, Univ. of Edinburgh and Imperial College London recreated the immense energy released from an extraterrestrial collision with Earth that occurred around the time that dinosaurs became extinct.
Carbon sequestration promises to address greenhouse gas emissions by capturing carbon dioxide from the atmosphere and injecting it deep below the Earth’s surface, where it would permanently solidify into rock. The U.S. Environmental Protection Agency estimates that current carbon sequestration technologies may eliminate up to 90% of carbon dioxide emissions from coal-fired power plants.
Yale Univ.-led research may have solved one of the biggest mysteries in geology: namely, why do tectonic plates beneath the Earth’s surface, which normally shift over the course of tens to hundreds of millions of years, sometimes move abruptly? A new study says the answer comes down to two things: thick crustal plugs and weakened mineral grains.
Minuscule, fossilized pieces of plants could tell a detailed story of what the Earth looked like 50 million years ago. An international team led by the Univ. of Washington has discovered a way to determine the tree cover and density of trees, shrubs and bushes in locations over time based on clues in the cells of plant fossils preserved in rocks and soil.
The “warming hiatus” over the past 15 years has been caused in part by small volcanic eruptions. Scientists have known volcanoes cool the atmosphere because of the sulfur dioxide that is expelled during eruptions. Droplets of sulfuric acid that form when the gas combines with oxygen in the upper atmosphere can persist for many months, reflecting sunlight away from Earth and lowering temperatures at the surface and in the lower atmosphere.
A new study is helping to answer a longstanding question that has recently moved to the forefront of Earth science: Did our planet make its own water through geologic processes, or did water come to us via icy comets from the far reaches of the solar system? The answer is likely both.
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