Using x-rays as a new diagnostic tool for monitoring space weather
Peer-Reviewed Publication
Updates every hour. Last Updated: 22-Jul-2025 10:10 ET (22-Jul-2025 14:10 GMT/UTC)
Earth’s magnetosphere protects us from charged particles constantly emitted by the Sun, but intense conditions can breach it through a process called magnetic reconnection. Now, researchers from Japan propose a novel method using soft X-ray imaging to remotely measure the reconnection rate, a key parameter in magnetic reconnection. This study showcases a powerful tool for forecasting hazardous space weather events, paving the way to safer near-Earth space applications and exploration.
Kyoto, Japan -- During the midday Friday prayer hours on 28 March 2025, a magnitude 7.7 earthquake struck central Myanmar along the Sagaing Fault. With an epicenter close to Mandalay, the country's second-largest city, it was the most powerful earthquake to strike Myanmar in more than a century and the second deadliest in its modern history.
The cause was a strike-slip fault, in which two masses of earth "slip" past each other horizontally along a vertical fault plane. To an observer, it would look like the ground were split in two along a defined line, with both sides being wrenched past each other in opposite directions.
Previous seismological studies have inferred pulse-like rupture behavior and curved slip paths from the analysis of seismic data. However, because the recording instruments were at a considerable distance from the fault itself, these findings were indirect.
A new study from the University of Missouri sheds light on how exceptional fossil preservation at Mazon Creek captured the diversity of life across land, delta and sea.
A pesky fish may be the culprit behind bleached tropical coral off the coast of the Florida Keys, according to research from the University of Georgia.
Chinese researchers have recently challenged the long-held belief that "all life depends on sunlight." In a study published in Science Advances, the researchers identified how microbes in deep subsurface areas can derive energy from chemical reactions driven by crustal faulting, offering critical insights into life deep below Earth's surface.