Organizational announcements and stories about our work and the science we support.
We want scientific inquiries to face as few speedbumps as possible, enabling you to do more with less time invested. Let’s talk a little about the way we’re structuring data storage to help make that happen.
A recent paper used DAS on Rhône Glacier in the Swiss Alps to infer the discharge of meltwater streams. We talked with one of the authors about how they wrangled this large dataset.
A set of studies explores questions pertaining to the rotation of the inner core relative to Earth’s mantle.
In East Greenland, a mysterious tsunami hit a military base on a remote island tucked into the fjords. At the same time, seismologists noticed a weird signal on seismic stations located around the world.
What can’t be explained by a delicious food metaphor? Maybe geophysical research in the cloud, but we’re going to try anyway.
When seismic sensors aren't detecting earthquakes, they’re picking up other vibrations—even shakes too subtle for people to feel. This ambient seismic noise might be able to tell scientists what’s happening at Mount St. Helens during times of activity and purported respite.
The National Science Foundation (NSF) has renewed funding for OpenTopography, a science gateway that provides online access to Earth science oriented high resolution topography data and processing tools.
A new paper using InSight data presents a noteworthy conclusion—seismic velocity data is best explained by the presence of liquid water.
Over the past few years, the Rainier Lahar Detection System has been upgraded with 25 new stations to better detect volcanic hazards on the mountain.
We regret to inform you that the irisFetch Matlab-based client is not compatible with recently released Matlab versions 2023a and onward.
Geoscience as a degree pathway and career trajectory is becoming more popular as opportunities expand. Despite the successful examples of growth in the field, there are still barriers to overcome.
A new study uses the latest maps of the structure beneath Antarctica to see how important realistic crust and mantle information is to sea level rise. The answer? It’s pretty important.
