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Journal of Geophysical Research: Solid Earth

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Scanning electron microscope images of an underformed and a deformed ice sample that clearly show differences in grain sizes.
Posted inEditors' Highlights

Ice on a Deadline: More Stress Makes Ice Move Faster

by Nikolai Bagdassarov and Douglas R. Schmitt 19 October 202115 October 2021

Anyone seeing photographs of glacier and ice sheets from above clearly sees that they flow; recent laboratory tests on ice further reveal the conditions that control just how fast this happens.

Plot showing a compilation the virtual dipole moment of the geomagnetic field during the Ediacaran and Cambrian periods.
Posted inEditors' Highlights

A Dipole Field from the Ediacaran-Cambrian Transition Onward?

by Mark J. Dekkers 14 October 202114 March 2023

The Ediacaran features an instable magnetic field complicating paleogeographic reconstructions; a new paleointensity study on late Ediacaran rocks indicates a weak but stable dipolar field.

Several charts showing the results of hydrothermal flow modelling along a 26 km-long line located on 7-million-year-old Atlantic oceanic crust.
Posted inEditors' Highlights

Mechanisms of Hydrothermal Ocean Plate Cooling Revealed

by V. Sallarès 28 September 202127 January 2023

A combination of waveform tomography and hydrothermal modelling allows characterizing the mechanisms and reach of fluid flux and ocean plate cooling near mid-ocean ridges with unprecedented detail.

The Bayside Picnic Area on Assateague Island National Seashore after Hurricane Sandy
Posted inResearch Spotlights

Long-Term Sea Level Cycle Affects Predictions of Future Rise

Sarah Stanley, Science Writer by Sarah Stanley 27 September 202126 October 2021

New research confirms the existence of a regular, long-term fluctuation in sea level, perhaps caused by processes in Earth’s core.

Two world maps with colored dots and stars denoting maximum mantle temperatures retrieved by the RevPET algorithm for the basaltic melts from the global submarine mid-ocean ridge system.
Posted inEditors' Highlights

A Novel Thermobarometer to Infer Mantle Melting Conditions

by Susanne Straub 16 September 20214 August 2023

The algorithm RevPET automatically reverses the complex multi-phase fractional crystallization path of oceanic basalts and offers new perspectives for advancing mantle thermobarometry.

Illustration of the transport of magmatic and meteoric fluids in the upper crust.
Posted inEditors' Highlights

Coupled Mechanisms of Fluid Transport Across the Crust

by Beatriz Quintal 14 September 202111 May 2022

Magmatic fluid moves up in the ductile zone through porosity waves, accumulates in high-porosity lenses, and migrates across the brittle zone in a convection pattern involving also meteoric fluid.

Series of six figures showing recovered fault geometry and slip models, from early to late stages in the inversion procedure.
Posted inEditors' Highlights

New Inversion Method Improves Earthquake Source Imaging

by Cécile Lasserre 30 August 202115 September 2026

A new method uses Bayesian inference to jointly invert for non-planar fault geometry and spatially variable slip (with associated uncertainties) in earthquake source modeling, based on geodetic data.

Viendo hacia afuera desde el Canion del Antílope Inferior, con el cielo cerca de la parte superior de la foto. La laminación característica de la arenisca es visible.
Posted inResearch Spotlights

La primera mirada de la meteorización a escala angstrom

Kate Wheeling, freelance science writer by Kate Wheeling 19 August 202124 February 2022

Investigadores observan cómo el vapor de agua y el líquido alteran las rocas sedimentarias a través de procesos físicos y químicos.

A view of Kīlauea’s summit lava lake
Posted inResearch Spotlights

Volcanic Tremor and Deformation at Kīlauea

Kate Wheeling, freelance science writer by Kate Wheeling 2 August 20216 March 2023

Two new studies investigate activity at Hawaii’s Kīlauea leading up to and following the 2018 eruption to better understand the volcano’s plumbing and behavior.

Sketch showing induced seismicity on critically stressed faults as a consequence of changes in pore pressure and related changes in stress due to anthropogenic activities
Posted inEditors' Vox

Understanding and Anticipating Induced Seismicity

by B. Müller, M.-L. Doan, T. H. Goebel, Yajing Liu, Patricia Martínez-Garzón, T. Mitchell and I. Zaliapin 30 July 20218 February 2023

A new special collection in JGR: Solid Earth and Earth and Space Science seeks papers from across disciplines that provide insights into induced seismicity at different spatial and temporal scales.

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Over a dark blue-green square appear the words Special Report: The State of the Science 1 Year On.

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The Geomagnetic Polarity Time Scale Revisited Once Again

22 October 202622 October 2026
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Opening Access to Earth Observation Data for Disaster Mitigation

21 October 202620 October 2026
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