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    Observatories Director and Crawford M. Greenewalt Chair

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    Object 5 | Elizabeth Ramsey's Placental Circulation Diagram

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    February 11, 2026

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Earth and Planets Laboratory

Earth and Planets Laboratory
Chondrite image purchased from Shutterstock
January 26, 2023

Solar System formed from “poorly mixed cake batter,” isotope research shows

Tissint meteorite courtesy of Kurt Kracher, Museum of Natural History Vienna
January 11, 2023

Martian meteorite contains large diversity of organic compounds

Cover of final report
November 07, 2022

New Report Outlines a Major Initiative to Study Geologic Hazards Related to Subduction Zones

ouis and Lore Brown at an annual Carnegie celebration with scientists and members of the Board of Trustees.
September 22, 2022

Physicist’s Estate to Advance Geochemistry and Cosmochemistry at Carnegie

Nitrogen period table illustration purchased from Shutterstock
April 26, 2022

The Pathway To Pure Polynitrogen

A view over Fisher Caldera in the foreground, looking out to Shishaldin Volcano, at a distance in 2015. The gray and gloomy tone of the photo is characteristic of the weather in the Aleutian Island. Photo is courtesy of Daniel Rasmussen of the National Museum of Natural History. Photo taken under Alaska Maritime National Wildlife Refuge Research and Monitoring Special Use Permit #74500-15-011.

A view over Fisher Caldera in the foreground, looking out to Shishaldin Volcano, at a distance in 2015. The gray and gloomy tone of the photo is characteristic of the weather in the Aleutian Island. Photo is courtesy of Daniel Rasmussen of the National Museum of Natural History. Photo taken under Alaska Maritime National Wildlife Refuge Research and Monitoring Special Use Permit #74500-15-011.

March 10, 2022

Revealed: Water Determines Magma Depth

A diamond anvil cell crafted at Carnegie's Earth and Planets Laboratory
March 02, 2022

Discovered: An Easier Way To Create "Flexible Diamonds"

 Illustration of new eight-coordinated, intrinsically discorded mineral courtesy of Rajkrishna Dutta.

Working with magnesium germanate, Mg2GeO4, analogous to one of the mantle’s most abundant silicate minerals, the team was able to glean information about the potential mineralogy of super-Earths and other large, rocky exoplanets. Under about 2 million times normal atmospheric pressure a new phase emerged with a distinct crystalline structure that involves one germanium bonded with eight oxygens. The new eight-coordinated, intrinsically discorded mineral is expected to strongly affect the internal temperature and dynamics of these planets. Illustration is courtesy of Rajkrishna Dutta.

March 01, 2022

What’s Happening In The Depths Of Distant Worlds?

December 22, 2021

Tracking down the forces that shaped our Solar System’s evolution

March 31, 2021

Deep diamonds contain evidence of deep-Earth recycling processes

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