Origins of Earth’s magnetic field remain a mystery
The existence of a magnetic field beyond 3.5 billion years ago is still up for debate.
The existence of a magnetic field beyond 3.5 billion years ago is still up for debate.
Samuel Birch, a new Heising-Simons Foundation 51 Pegasi b Fellow at MIT, will investigate the surfaces of outer solar system objects.
MIT researchers describe factors governing how oceans and atmospheres move heat around on Earth and other planetary bodies.
Recovering and safely destroying the sources of these chemicals could speed ozone recovery and reduce climate change.
The average power of waves hitting a coastline can predict how fast that coast will erode.
Technique may help scientists more accurately map vast underground geologic structures.
Researchers in the Department of Earth, Atmospheric and Planetary Sciences will help direct Mars 2020 rover sample acquisition.
Study finds Earth’s oceans contain just the right amount of iron; adding more may not improve their ability to absorb carbon dioxide.
An advocate of international scientific cooperation, Press served as an MIT department head and lifetime MIT Corporation member.
Findings suggest the moon’s magnetic field was produced by the fallout of a crystallizing iron core.
Plate tectonics and mantle plumes set the lifespan of volcanic islands like Hawaii and the Galapagos.
A molecule that’s known for its smelly and poisonous nature on Earth may be a sure-fire sign of extraterrestrial life.
Scientists reveal the genes and proteins controlling the chemical structures underpinning paleoclimate proxies.
The Summons Lab compares lipids from Antarctic microbial communities to century-old samples.
Study finds even the tallest ice cliffs should support their own weight rather than collapsing catastrophically.