Earth formed as part of our solar system more than 4.5 billion years ago. It has been shaped by powerful geologic forces over its entire history and will continue to change for billions of years to come. Societies depend on Earth’s vast mineral and energy resources and on a climate that allows life to flourish.
In the Mineral Galleries at the Peabody, you can learn more about the Solar System, how minerals are formed, gems and jewelry, and the history of mineralogy at Yale. David Friend Hall, the largest gallery, features artistic presentations of remarkable minerals from around the world.
Click to expand images below.
Quartz sandstone concretion
The undulating shape of sandstone concretions in the Fontainebleau quartz sand deposits southeast of Paris, France have for centuries fascinated humans.
Fulgurite
This 13-foot (4-meter) sand tube formed in an instant when lightning struck Miller's Beach on Congamond Lakes in Connecticut in 1949.
Photo credit: Andy Melien / Yale Peabody Museum unless otherwise noted.
"Fluorescent Minerals": credit: Harold Moritz