Our March issue takes you on an epic journey with the rocks of Mount Everest, from seafloor to summit.
mountains
Posted inFeatures
How to Build the World’s Highest Mountain
The rocks of Mount Everest’s peak made an epic journey from seafloor to summit.
Posted inEditors' Highlights
Ice boost! Why Rock Avalanches Containing Ice Travel So Far
Researchers identify a new mechanism that allows avalanches containing a mixture of rock and ice to travel very long distances.
Posted inResearch Spotlights
Deep Beneath California’s Sierra Nevada, Earth’s Lithosphere May Be Peeling Away
Evidence for lithospheric foundering, or the process of denser material sinking into the mantle, is emerging.
Posted inThe Landslide Blog
Future increases in landslide hazard across the high mountains of Asia
The Landslide Blog is written by Dave Petley, who is widely recognized as a world leader in the study and management of landslides. In terms of human losses, the mountains of Asia remain the global hotspot for landslides. Whilst earthquake-induced landslides cause occasional, very high levels of loss (e.g. the 2005 Kashmir Earthquake and the […]
Posted inNews
Earthquakes May Lace Quartz Veins with Gold
Seismic activity may kick off chemical reactions that seed nuggets of gold.
Posted inNews
A Pirate River May Be Giving Mount Everest a Boost
Rapid erosion can cause mountains to rise—even the world’s tallest peak.
Posted inNews
Model Suggests Undersea Mountains Help Mix the Global Ocean
Seamounts may play a significant role in ocean turbulence and the upwelling of deep waters.
Posted inScience Updates
An Unprecedented Experiment to Map Kīlauea’s Summit Magma System
Dozens of researchers deployed nearly 2,000 seismic stations—and a T-Rex—to better illuminate subsurface structure and magma storage below the summit of the highly active volcano.
Posted inEditors' Highlights
Sediment Dampens the Impact of Glaciation on Cenozoic Denudation
Rates of continental-scale sediment flux and denudation are similar between glacial and interglacial periods when the aggradation of glacier-eroded sediment inhibits fluvial erosion downstream.