• About
  • Special Reports
  • Topics
    • Climate
    • Earth Science
    • Oceans
    • Space & Planets
    • Health & Ecosystems
    • Culture & Policy
    • Education & Careers
    • Opinions
  • Projects
    • Postcards From the Field
    • ENGAGE
    • Editors’ Highlights
    • Editors’ Vox
    • Eos en Español
    • Eos 简体中文版
    • Print Archive: 2015–2025
  • Policy Tracker
  • Blogs
    • Research & Developments
    • The Landslide Blog
  • Newsletter
  • Submit to Eos
  • AGU.org
  • Career Center
  • Join AGU
  • Give to AGU
  • About
  • Special Reports
  • Topics
    • Climate
    • Earth Science
    • Oceans
    • Space & Planets
    • Health & Ecosystems
    • Culture & Policy
    • Education & Careers
    • Opinions
  • Projects
    • Postcards From the Field
    • ENGAGE
    • Editors’ Highlights
    • Editors’ Vox
    • Eos en Español
    • Eos 简体中文版
    • Print Archive: 2015–2025
  • Policy Tracker
  • Blogs
    • Research & Developments
    • The Landslide Blog
  • Newsletter
  • Submit to Eos
Skip to content
  • AGU.org
  • Career Center
  • Join AGU
  • Give to AGU
Eos

Eos

Science News by AGU

Support Eos
Sign Up for Newsletter
  • About
  • Special Reports
  • Topics
    • Climate
    • Earth Science
    • Oceans
    • Space & Planets
    • Health & Ecosystems
    • Culture & Policy
    • Education & Careers
    • Opinions
  • Projects
    • Postcards From the Field
    • ENGAGE
    • Editors’ Highlights
    • Editors’ Vox
    • Eos en Español
    • Eos 简体中文版
    • Print Archive: 2015–2025
  • Policy Tracker
  • Blogs
    • Research & Developments
    • The Landslide Blog
  • Newsletter
  • Submit to Eos

magnetic fields & magnetism

Two people, one wearing a yellow vest and one in a gray long-sleeved shirt, look up at a rock face.
Posted inResearch Spotlights

Where Was Baltica 616 Million Years Ago?

by Saima May Sidik 5 May 20265 May 2026

Disentangling magnetic signals in its ancient rocks gives an updated view of the paleocontinent’s position during the Ediacaran period.

Solar system diagram showing the Sun’s magnetic field lines and a shaded region representing the bubble of reduced cosmic rays, which sits at roughly a 45° angle extending ahead of and behind Earth as it orbits.
Posted inNews

Moon Mission Data Reveal Unexpected Cosmic Ray “Shadow”

by Matthew R. Francis 4 May 20264 May 2026

A particle detector on the Chang’e-4 lunar lander showed a surprising zone of reduced radiation stretching out from Earth at a strange angle, with potential implications for future astronauts.

A large, round, glowing yellow shape is shown at right (the Sun), and a smaller, reddish-brown sphere is at left (Mars). Pale yellow streaks and thicker curving white lines radiate from the Sun in all directions. Mars appears to disrupt the flow of the pale yellow streaks, which deflect around it like water flowing around a pebble in a stream.
Posted inResearch Spotlights

What Makes Mars’s Magnetotail Flap?

Sarah Stanley, Science Writer by Sarah Stanley 20 April 20261 May 2026

Spacecraft reveal a key driver of up-and-down motions of thin, current-carrying plasma sheets on the nightside of Mars.

A computer and keyboard on a desk sit next to a complex microscope that says “QDM” on the top.
Posted inResearch Spotlights

Navigating the Past with Ancient Stone Compass Needles

Aaron Sidder, freelance science writer by Aaron Sidder 16 April 20261 May 2026

The emerging field of magnetic microscopy allows scientists to reconstruct ancient magnetic fields from individual magnetic particles. A new study evaluates the accuracy of the technique.

Illustration of the Sun and Earth's magnetosphere.
Posted inEditors' Highlights

Timing of Geomagnetic Storms Shapes Their Impact

by Alberto Montanari 15 April 20261 May 2026

The impact of geomagnetic storms, which can disrupt satellites, GPS, and power grids, is shown to depend on their onset timing.

Two maps from the article.
Posted inEditors' Highlights

How Sediment Magnetism Captures the South Atlantic Anomaly

by Agnes Kontny 13 April 20261 May 2026

Magnetic data from an ODP core deposited during normal secular variation (65-41 thousand years ago) off the Chilean margin help clarify geomagnetic field behavior in the South Atlantic Anomaly region.

A gray, speckled rock sits on a metal plate. Above the rock is a sign showing the numerical label of the rock sample, 7225500.
Posted inNews

Apollo Samples Told a Conflicting Story About Lunar Magnetism, Until Now

by Grace van Deelen 19 March 202619 March 2026

Observations suggested the Moon had both a weak and strong magnetic field in the distant past. A new study presents a theory accommodating all the evidence.

Diagram from the article.
Posted inEditors' Highlights

Detecting Remagnetization with Quantum Diamond Microscopy

by Ramon Egli 15 January 20269 January 2026

Scientists reconstruct the magnetization timeline of serpentinized rocks from the Troodos ophiolite by investigating remanent magnetization-carrying structures with a Quantum Diamond Microscope.

The upper left image shows a clay pot. The lower part of the image is a chart showing age on the x axis and field intensity on the y axis. From about 1050 BCE until 700 BCE, the field intensity is high and has four spikes. After that, it falls until it reaches a low at about 200 CE before rising slightly and falling again at about 1800 CE. The spiky high is circled and labeled “Levantine Iron Age Anomaly” in red. The low from about 1800 to 2000 CE is circled in blue and labeled “Modern field.” A green line of the field intensity of the pot intersects the modern field. In the upper right corner is a large “FAKE” stamp.
Posted inNews

Credible or Counterfeit: How Paleomagnetism Can Help Archaeologists Find Frauds

by Alka Tripathy-Lang 16 December 202516 December 2025

Duplicating artifacts that preserve records from biblical times is a lucrative business. A method used for both dating artifacts and reconstructing Earth’s history could identify phony pieces.

A pale gray rock shows an impression of multiple curved lines.
Posted inNews

The Long and the Weak of It—The Ediacaran Magnetic Field

Katherine Kornei, Science Writer by Katherine Kornei 9 December 20259 December 2025

A roughly 70-million-year interval of anomalously weak magnetic field during the Ediacaran period could have triggered atmospheric changes that supported the rise of macroscopic life.

Posts pagination

1 2 3 … 34 Older posts
Over a dark blue-green square appear the words Special Report: The State of the Science 1 Year On.

Features from AGU Publications

Research Spotlights

How Much Will Western Wildfires Worsen Under Warming?

15 May 202615 May 2026
Editors' Highlights

A Digital Twin for Arctic Permafrost Beneath Roads

8 May 202612 May 2026
Editors' Vox

The Impact of Advocacy: American Geophysical Union’s Days of Action

14 May 202613 May 2026
Eos logo at left; AGU logo at right

About Eos
ENGAGE
Awards
Contact

Advertise
Submit
Career Center
Sitemap

© 2026 American Geophysical Union. All rights reserved Powered by Newspack