• About
  • Sections
  • Topics
    • Climate
    • Earth Science
    • Oceans
    • Space & Planets
    • Health & Ecosystems
    • Culture & Policy
    • Education & Careers
    • Opinions
  • Projects
    • ENGAGE
    • Editors’ Highlights
    • Editors’ Vox
    • Eos en Español
    • Eos 简体中文版
    • Print Archive
  • Blogs
    • Research & Developments
    • The Landslide Blog
  • Newsletter
  • Submit to Eos
  • AGU.org
  • Career Center
  • Join AGU
  • Give to AGU
  • About
  • Sections
  • Topics
    • Climate
    • Earth Science
    • Oceans
    • Space & Planets
    • Health & Ecosystems
    • Culture & Policy
    • Education & Careers
    • Opinions
  • Projects
    • ENGAGE
    • Editors’ Highlights
    • Editors’ Vox
    • Eos en Español
    • Eos 简体中文版
    • Print Archive
  • 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
  • Sections
  • Topics
    • Climate
    • Earth Science
    • Oceans
    • Space & Planets
    • Health & Ecosystems
    • Culture & Policy
    • Education & Careers
    • Opinions
  • Projects
    • ENGAGE
    • Editors’ Highlights
    • Editors’ Vox
    • Eos en Español
    • Eos 简体中文版
    • Print Archive
  • Blogs
    • Research & Developments
    • The Landslide Blog
  • Newsletter
  • Submit to Eos

Journal of Geophysical Research: Earth Surface

Visit the journal.

A large waterfall plunge pool system within the Seven Tea Cups, Dry Meadow Creek, California.
Posted inResearch Spotlights

Plunging into Waterfall Sediment Transport Modeling

Sarah Stanley, Science Writer by Sarah Stanley 7 June 20163 May 2022

A first-of-its-kind model describes how pools at the base of waterfalls adjust their depth to keep up with sediment flow.

The 25 May 2014 West Salt Creek landslide had a volume of 30 million cubic meters of rock and a runout of 4.5 kilometers (about 7 times its fall height).
Posted inResearch Spotlights

What Makes Long-Runout Landslides So Mobile?

Kate Wheeling, freelance science writer by Kate Wheeling 22 April 201628 March 2023

New research shows that acoustic waves rippling through some large landslides can reduce friction and allow slides to run out long distances.

water-eroded-hill-sedgwick-reserve-santa-barbara
Posted inResearch Spotlights

Hitting the Slopes

by W. Yan 24 March 201625 October 2022

Researchers investigate whether rain droplets alone can cause enough erosion to impact the shapes of hills.

Posted inResearch Spotlights

Water Waves Provide Insight into Landslides and Avalanche Models

by David Shultz 21 October 201511 February 2022

Boussinesq-type gravity waves appear to accurately describe vertical motion in granular flows found in geophysics.

Posted inResearch Spotlights

Efficiently Predicting Shallow Landslide Size and Location

by David Shultz 8 October 20156 February 2023

New mathematical approach lets researchers analyze potentially unstable slopes in three dimensions without testing every possible landslide shape.

Posted inResearch Spotlights

Ice-Penetrating Radar Reveals Age of Greenland Ice Sheet Layers

by Terri Cook 13 August 20159 February 2023

First comprehensive analysis of deep radar data gives insight into the dynamics and history of the Greenland Ice Sheet.

Posted inResearch Spotlights

Using Sound Waves to Study Grand Canyon Sediment

by E. Betz 13 July 20152 February 2022

New technology could help scientists understand how experimental floods from Glen Canyon Dam restore sandbars downstream.

Posted inResearch Spotlights

Researchers Track Moving Ice Shelves to Estimate Antarctic Ice Loss

by J. Rosen 14 May 201510 March 2023

A new method will help scientists monitor the basal melt of ice sheets in Antarctica.

Posted inResearch Spotlights

Bank Materials Strongly Influence River Valley Evolution

by J. Rosen 13 February 201511 February 2022

Models suggest that the shape of river valleys depends strongly on how meandering rivers interact with the sediment and bedrock of the banks.

Posted inResearch Spotlights

Wave Ripples Spaced by Flow Downstream of Ripple Peaks

by J. Rosen 12 February 20157 July 2025

The well-known ratio between sand ripple spacing and wave-driven flow oscillations may be dictated by flow dynamics downstream of ripple crests.

Posts pagination

Newer posts 1 … 8 9 10 11 12 Older posts
A view of a Washington, D.C., skyline from the Potomac River at night. The Lincoln Memorial (at left) and the Washington Monument (at right) are lit against a purple sky. Over the water of the Potomac appear the text “#AGU24 coverage from Eos.”

Features from AGU Publications

Research Spotlights

Abrupt Climate Shifts Likely as Global Temperatures Keep Rising

22 July 202522 July 2025
Editors' Highlights

New Insights into How Rocks Behave Under Stress

22 July 202522 July 2025
Editors' Vox

Groundwater Pollution in Karst Regions: Toward Better Models

22 July 202522 July 2025
Eos logo at left; AGU logo at right

About Eos
ENGAGE
Awards
Contact

Advertise
Submit
Career Center
Sitemap

© 2025 American Geophysical Union. All rights reserved Powered by Newspack