• 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
  • Science Policy Tracker
  • 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
  • Science 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
  • 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
  • Science Policy Tracker
  • Blogs
    • Research & Developments
    • The Landslide Blog
  • Newsletter
  • Submit to Eos

sediments

Antarctic research team scrapes sediment cores from 1200 meters below the seafloor near the Cosgrove Ice Shelf.
Posted inNews

Déjà Vu? Ocean Warmth Melted Ancient West Antarctic Ice Shelf

Sarah Derouin, Science Writer by Sarah Derouin 30 January 201713 December 2021

Clues in seafloor sediments reveal that relatively warm water beneath western Antarctic ice shelves, a major factor in today's massive ice sheet retreat, also fueled some past ice loss.

Researchers predict the movement of sediment in very steep streams.
Posted inResearch Spotlights

Boulders Limit Transport of Sand and Gravel in Steep Rivers

Alexandra Branscombe by A. Branscombe 6 January 20176 March 2023

Mountain rivers and streams actively reshape landscapes by eroding material from uplands and depositing it in lowlands. Scientists can now predict this transport in very steep streams.

Aerial view of Orakei basin, near Auckland, New Zealand, where a research team took core samples near the center of a maar, an ancient volcanic explosion crater.
Posted inScience Updates

Probing the History of New Zealand's Orakei Maar

by P. C. Augustinus 20 September 201623 September 2022

A team of scientists drilled into the bed within a northern New Zealand explosion crater lake to gain insights into volcanic hazards and past climates.

Pannonian-Basin-Miocene-extension-greater-than-previously-thought
Posted inResearch Spotlights

Unraveling the History of Central Europe's Pannonian Basin

by Terri Cook 12 August 201622 August 2023

A multidisciplinary model linking the sedimentary and tectonic histories of this structurally complex basin suggests that large amounts of extension occurred there between 20 and 9 million years ago.

The confluence of the Rees and Dart Rivers (New Zealand).
Posted inResearch Spotlights

The Mathematics of Braided Rivers

by David Shultz 10 June 201627 April 2022

River researchers find a mathematical relationship that predicts the average shape of a riverbed over a defined distance, opening the door to new ideas about modeling braided rivers.

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.

Satellite photo of Japan
Posted inResearch Spotlights

Earthquakes May Prevent Underwater Landslides

by David Shultz 4 April 201621 July 2022

Smaller quakes around the active edge of continental plates may contribute to increased stability by promoting compaction and solidifying the top 100 meters of seafloor sediment.

Posted inNews

Scientists Find the Point of No Return for Antarctic Ice Cap

JoAnna Wendel, freelance science writer and illustrator by JoAnna Wendel 10 March 201618 October 2022

Varying amounts of glacial debris in a core of ancient sediment show the ice cover grew and shrank until airborne carbon dioxide levels fell below 600 parts per million, spurring steady growth.

Posted inResearch Spotlights

Satellites Reveal Dynamics of Suspended Mineral Particles

by Terri Cook 18 February 20165 September 2023

A case study of the Irish Sea evaluates the use of ocean color data to measure the optical properties of sedimentary particles in offshore waters.

Posted inResearch Spotlights

How Sediment Transport Sways Wetland Stability

by L. Strelich 17 February 201616 February 2023

Scientists examine the role of variables like tides and suspended sediment concentration to improve methods of evaluating coastal wetlands and how they may respond to future sea level rise.

Posts pagination

Newer posts 1 … 18 19 20 21 22 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

Unveiling What’s Under the Hood in AI Weather Models

30 September 202530 September 2025
Editors' Highlights

New Evidence for a Wobbly Venus?

29 September 202525 September 2025
Editors' Vox

All Publish, No Perish: Three Months on the Other Side of Publishing

29 September 202525 September 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