According to research taking place at Lawrence Livermore National Laboratory, the distortion of the ancient shoreline and flooding surface of the U.S. Atlantic Coastal Plain are the direct result of fluctuations in topography in the region and could have implications on understanding long-term climate change, according to a new study.
The massive ball of iron sitting at the center of Earth is not quite as "rock-solid" as has been thought, say two Stanford University mineral physicists. By conducting experiments that simulate the immense pressures deep in the planet's interior, the researchers determined that iron in Earth's inner core is only about 40% as strong as previous studies estimated.
Hydraulic fracturing for natural gas hasn't contaminated drinking water wells in Arkansas, according to a new study, but researchers said the geology there may be more of a natural barrier to pollution than in other areas where shale gas drilling takes place.
Scientists sampling 127 shallow drinking water wells in areas overlying Fayetteville Shale gas production in north-central Arkansas found no evidence of groundwater contamination. The team of scientists at Duke University and the U.S. Geological Survey (USGS) analyzed the samples for major and trace elements and hydrocarbons, and used isotopic tracers to identify the sources of possible contaminants.
Worldwide, hundreds of flights are diverted each year because of volcanic activity. Scientists monitoring Alaska's volcanoes have been forced to shut down stations that provide real-time tracking of eruptions and forgo repairs of seismic equipment amid ongoing federal budget cuts—moves that could mean delays in getting vital information to airline pilots and emergency planners.
The three different formations of South Pacific coral-reef islands, fringing, barrier, and atoll, have long fascinated geologists. The question of how reefs develop into these shapes over evolutionary time produced an enduring conflict between two hypotheses, one from Charles Darwin and the other from Reginald Daly. But in a recently published paper, researchers use modern measurements and computer modeling to resolve this old conundrum.
NASA's Hubble Space Telescope has found the building blocks for Earth-sized planets in an unlikely place—the atmospheres of a pair of burned-out stars called white dwarfs. Hubble's Cosmic Origins Spectrograph observed silicon and only low levels of carbon in the white dwarfs' atmospheres. Silicon is a major ingredient of the rocky material that constitutes Earth and other solid planets in our solar system.
A roughly 3.5-mile high Martian mound that scientists suspect preserves evidence of a massive lake might actually have formed as a result of the Red Planet's famously dusty atmosphere, an analysis of the mound's features suggests. If correct, the research could dilute expectations that the mound holds evidence of a large body of water, which would have important implications for understanding Mars' past habitability.
A team from the Smithsonian and the University of Rhode Island has found unsuspected linkages between the oxidation state of iron in volcanic rocks and variations in the chemistry of the deep Earth. Their detailed spectroscopic work has uncovered chemical trends that not only run counter to predictions from recent decades of study, they belie a role for carbon circulating in the deep Earth.
In an effort to determine if conditions were ever right on Mars to sustain life, a team of scientists has examined a meteorite that formed on the red planet more than a billion years ago. And although this team’s work is not specifically solving the mystery, it is laying the groundwork for future researchers to answer this age-old question.
Fans of the Ohio native credited with developing the Richter scale of rating earthquake magnitude want to be sure that Charles Richter's name and legacy remain prominent in history. They are concerned because many reports about earthquakes no longer mention the scale developed in the early 1930s and just refer to magnitudes in general.
Using a new laboratory geochemical technique to analyze heavy isotopes of carbon and oxygen in fossil snail shells, scientists have gained insights into an abrupt climate shift that transformed the planet nearly 34 million years ago. At that time, the Earth switched from a warm and high-carbon dioxide "greenhouse" state to the lower-carbon dioxide, variable climate of the modern "icehouse" world.
When superstorm Sandy turned and took aim at New York City and Long Island last October, ocean waves hitting each other and the shore rattled the seafloor and much of the United States—shaking detected by seismometers across the country, University of Utah researchers have recently found. These “microseisms” generated by Sandy were detected by Earthscope, a network of 500 portable seismometers.
A new study from a collaboration of several universities suggests that the way carbon moves from within a planet to the surface plays a big role in the evolution of a planet's atmosphere. If Mars released much of its carbon as methane, for example, it might have been warm enough to support liquid water. This finding offers important clues about the early atmospheric evolution of Mars and other terrestrial bodies.
It's the Martian version of spring break: Curiosity and Opportunity, along with their spacecraft friends circling overhead, will take it easy this month because of the sun's interference. For much of April, the sun blocks the line of sight between Earth and Mars. This celestial alignment—called a Mars solar conjunction—makes it difficult for engineers to send instructions or hear from the flotilla in orbit and on the surface.
Researchers at the University of Leeds may have solved a key puzzle about how objects from space could have kindled life on Earth. While it is generally accepted that some important ingredients for life came from meteorites bombarding the early Earth, scientists have not been able to explain how that inanimate rock transformed into the building blocks of life, until now.
A new look at conditions after a Manhattan-sized asteroid slammed into a region of Mexico in the dinosaur days indicates the event could have triggered a global firestorm that would have burned every twig, bush, and tree on Earth and led to the extinction of 80% of all Earth’s species, says a new University of Colorado Boulder study.
It’s not entirely clear what caused the end-Triassic extinction, although most scientists agree on a likely scenario: Over a relatively short period of time, massive volcanic eruptions from a large region known as the Central Atlantic Magmatic Province (CAMP) spewed forth huge amounts of lava and gas, including carbon dioxide, sulfur and methane. Now, a research team has determined that these eruptions occurred precisely when the extinction began, providing strong evidence that volcanic activity did indeed trigger the end-Triassic extinction.
Computer simulations of water under extreme pressure are helping geochemists understand how carbon might be recycled from hundreds of miles below the Earth's surface. Carbon compounds are the basis of life, provide most of our fuels and contribute to climate change. The cycling of carbon through the oceans, atmosphere, and shallow crust of the Earth has been intensively studied, but little is known about what happens to carbon deep in the Earth.
Using advanced seafloor electromagnetic imaging technology, scientists with Scripps Institution of Oceanography and Woods Hole Oceanographic Institution imaged a 25-km-thick layer of partially melted mantle rock below the edge of the Cocos plate where it moves beneath Central America. The finding of this layer, which may be responsible for the sliding motions of the planet’s massive tectonic plates, could have far-reaching implications to our understanding of geologic processes.
Large chunks of an ancient tectonic plate that slid under North America millions of years ago are still present under parts of central California and Mexico, according to new research led by Brown University geophysicists. Called the Isabella anomaly—a large mass of cool, dehydrated material about 100 km beneath central California—is in fact a surviving slab of the ancient Farallon oceanic plate driven deep into the Earth’s mantle about 100 million years ago.
Drilling into a rock near its landing spot, the Curiosity rover has answered a key question about Mars: The red planet long ago harbored some of the ingredients needed for primitive life to thrive. Topping the list is evidence of water and basic elements that teeny organisms could feed on, scientists said Tuesday.
A new analysis of data from NASA’s Lunar Orbiter Laser Altimeter shows that molten rock may have been present on the Moon more recently and for longer periods than previously thought. Differentiation—a settling out of rock layers as liquid rock cools—would require thousands of years and a fluid rock sea at least six miles deep.
All living organisms rely on iron as an essential nutrient. In the ocean, iron’s abundance or scarcity means all the difference as it fuels the growth of plankton. A new study from the Woods Hole Oceanographic Institution identifies an unexpectedly large source of iron to the North Atlantic—meltwater from glaciers and ice sheets, which may stimulate plankton growth. This source is likely to increase as melting of the Greenland ice sheet escalates under a warming climate.
A rough, whitish block recovered from an Elizabethan shipwreck may be a sunstone, the fabled crystal believed by some to have helped Vikings and other medieval seafarers navigate the high seas, researchers say. That's because of a property known as birefringence, which splits light beams in a way that can reveal the direction of their source with a high degree of accuracy.