On May 12, 2008, the magnitude 7.9 Wenchuan Earthquake shook central China, its destructive tremors spreading from the flank of the Longmen Shan, or Dragon's Gate Mountains, along the eastern margin of the Tibetan Plateau.

Over 69,000 people died in the disaster, nearly a third are thought to be from geohazards like the more than 60,000 landslides that rushed down the slopes of the Longmen Shan.

After more than a decade and a half of work, scientists finally have an account of the fate of the landslide debris. Surveys of a reservoir downstream of the epicenter revealed how and how quickly the region’s major river moved this sediment, as well as the effect it had on the river channel itself. The results, published in Nature, suggest that the hazards caused by megaquakes may last long after the ground has settled. What’s more, they offer insights into a fundamental question of Earth science: How do earthquakes build mountains?

Harvard SEAS and University of Chicago researchers have tested and validated lightweight nanofabricated structures that can passively float in the mesophere, which is about 45 miles above Earth’s surface. The devices levitate via photophoresis, or sunlight-driven propulsion, which occurs in the low-pressure conditions of the upper atmosphere.

In a new study, archaeologists analyzed iron artifacts spanning more than 400 years of American colonial history using X-ray fluorescence spectroscopy. Their results show that differences in the purity of iron and the trace elements it contains can be reliably used as a diagnostic feature to identify iron artifacts from different time periods.

The scalar magnetometer conceived by Roland Lammegger and Christoph Amtmann at the Institute of Experimental Physics at Graz University of Technology opens up new possibilities in magnetic field measurement thanks to its further development.

Galactic Rosetta Stone: Magnetic Field Study of Sagittarius C

Study Overview

University of Chicago researchers, led by PhD student Roy Zhao, conducted a groundbreaking study of magnetic fields in the Sagittarius C (Sgr C) region near the center of the Milky Way. Using NASA's retired SOFIA flying telescope, the team mapped magnetic field orientations by analyzing polarized infrared light from dust grains aligned by the fields.