Researchers at the University of Bonn found that majorite minerals act as oxygen reservoirs, releasing stored oxygen to form water and sustain life on Earth. This mechanism helps prevent the Earth from becoming as dry and inhospitable as Mars.
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A team of scientists led by Sébastien Merkel found that post-perovskite, a high-pressure silicate mineral, doesn't fit what is known about the mysterious layer D
Seismologists have directly measured heat flowing from the molten core into a region of the lower mantle for the first time. The new temperature measurements provide insight into the geodynamo and tectonic plate movement, helping scientists understand the Earth's internal dynamics.
Researchers develop protocols to identify promising molecule/mineral pairs, building on previous findings that many biomolecules can adhere to mineral surfaces. The study uses DNA microarrays and Time-of-Flight Secondary Ion Mass Spectrometry to discover which molecules stick to specific mineral surfaces.
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Asteroid Itokawa's surface composition was determined by Brown University researcher Takahiro Hiroi, who linked it to LL chondrites, a common class of stony meteorites. The team also described the asteroid's diverse terrain, suggesting it may be an earlier stage of asteroid evolution and formation.
Researchers have discovered a new property of the very deep Earth, which challenges the prevailing thought that ultralow velocity zones contain liquid. The study found that iron-rich post-perosvkite can explain these zones' properties, suggesting an alternative explanation to partial melting.
Robert Downs is almost halfway to creating a library of spectral fingerprints for all the Earth's minerals, with over 1,500 cataloged so far. The associate professor of geosciences is collaborating with colleagues to develop a pocket-sized Raman spectrometer for use on Mars and handheld instruments for identifying gemstones on Earth.
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Researchers at the University of Minnesota have discovered post-perovskite in the D'' layer surrounding Earth's core, explaining its unusual seismic properties. This finding sheds new light on the Earth's evolution and aging processes, offering insights into the planet's history.
The Penn State Earth and Mineral Sciences Library launched a geocache treasure hunt as an orientation tool for freshmen. Participants used GPS coordinates to locate the cache, which was hidden in plain sight within the library. The hunt incorporated library knowledge, including the Library of Congress classification system.
A new study by Arizona State University reveals Mars' surface minerals using THEMIS and TES data, yielding surprising results in localized areas. The findings show that Mars has evolved and continues to evolve beneath its surface, similar to Earth, with diverse igneous mineral types rivaling those found on our planet.
Researchers found evidence of a failed rift in the ancient continent Nunavutia, dating back 3.9 billion years, with minerals suggesting significant diamond exploration potential. The discovery sheds light on Earth's history and evolution, offering insights into plate tectonics in the Archean era.
Researchers have discovered that the breakdown of mineral serpentine can trigger earthquakes in Earth's deeply buried crust. At pressures above a few tens of kilometers, scientists expected faulting instability only if volume change during serpentine breakdown was positive. However, experiments have shown that even with a strongly nega...
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Researchers found that a sugar called ribose can be formed from interstellar dust clouds using borate minerals like colemanite. This discovery sheds light on the 3-billion-year-old mystery of how life on Earth began and could have implications for disease diagnostics and therapy.
Researchers at Washington University in St. Louis found evidence that hot and dry Venus could have had water in its past due to the chemical stability of tremolite at extreme temperatures. This discovery could help scientists determine if they should investigate hydrous minerals on Venus.
Scientists have discovered a wealth of green minerals, including olivine, on the Martian surface, indicating low levels of chemical weathering by water. This suggests that Mars has remained cold and dry for most of its geologic history, contradicting previous theories about a warm, wet past.
The Mars Global Surveyor's Thermal Emission Spectrometer has mapped the mineral composition of Mars' surface, revealing a primarily volcanic surface with distinct differences between southern and northern hemispheres. The survey provides valuable insights into Martian geology and may help explain changes in the planet's interior.
Yale researchers develop a hypothesis linking rock metamorphism and earthquake generation. They show that rapid release of water from rocks within fault zones can lead to high internal fluid pressures, decreased rock strength, and induced rock failure, potentially triggering repeated earthquakes.
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Researchers predict significant changes in mineral behavior and crystal structures under high pressure, affecting the Earth's magnetic field. The study investigates the properties of materials containing iron, manganese, cobalt, and nickel at extreme conditions.
Researchers at Penn State found that laboratory experiments on soil mineral weathering do not match natural processes, with molecules dissolving in groundwater forming coatings or wearing away. The team is monitoring conditions in the field to better understand the mechanisms underway in the soil and develop more accurate models.