From its beginnings in the kitchen at Lamont Hall, the Geochemistry Division at Lamont-Doherty has built a proud tradition of working to understand Earth’s many complex and interconnected systems by pursuing studies of our planet’s history and the processes that have governed its past and present environment.
Mantel Convection Model Illustration: Jayne Doucette

Researchers examine samples of air, water, biological remains, rocks and even meteorites in order to address a broad range of scientific issues from determining the chemical composition of pollutant emitted by the collapse of the World Trade Center towers, to uncovering clues about past climate changes locked in the Earth’s glaciers and sea floors, to identifying the fundamental chemical and physical processes involved in the formation of the planet’s mantle and core.

Global Ocean Conveyer Belt graphic Illustration: W. Broecker
Hudson River Research Photo: Carlos Rene Perez

Lamont-Doherty’s geochemists also contribute to our understanding of socio-economic issues related to the environment, from the causes and remediation of arsenic in the groundwater in Bangladesh to the accumulation of carbon dioxide in the atmosphere.

By studying the Earth's chemical processes geochemists at Lamont-Doherty work to unlock the secrets of our planet's formation and future. The type and composition of rocks and gases that erupt from mid-ocean ridges and island arcs or volcanic islands (above) help scientists piece together a picture of how the Earth formed and how it continues to change.

Samples of sea floor sediment and water from the Earth's oceans have helped form a picture of they way surface processes such as the "great ocean conveyor belt" (right), which distributes heat around the world, govern our climate. Closer to home, Lamont-Doherty geochemists (left) also study the movement and mixing of water and sediment in the Hudson River.

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