These web pages contain geologic information geared to park visitors. If you would like more indepth geologic information, the 2014 Geologic Inventory for John Day Fossil Beds is now available.
The geology at the John Day Fossil Beds can be split into two broad categories: physical and historical. Physical geology describes the processes that form rocks, faulting events, and other geologic occurrences. Historical geology examines the origins of the Earth and life’s adaptations to a dynamic planet. Both of these categories are utilized to find fossils as well as research and describe the landscapes that dominate the area.Sedimentary layers are deposited in a time sequence, with the oldest on the bottom and the youngest at the top. Think of layers of rock as being pages in a book. As you continue paging through the book, you work from the youngest layer in a time sequence to the oldest. Though the former is not always the case, sometimes older rock may overlie younger formations. Faulting events or unconformities (missing sections of geologic time) can often pit old rock against young where there ought to be horizontal time continuity of rock layers.
Fossils don’t just occur anywhere...
To have fossil bearing rock there needs to be a set of favorable conditions. Physical geologic occurrences allow fossils to be preserved. Most fossilized organisms had a durable skeleton or structure, and lived in an environment where sedimentation (deposition of solid materials including ash fall) occurred frequently or rapidly. The historical geology in the National Monument tells a story of plant progression and mammal evolution as climates changed from balmy swamps to arid steppe environments.
Use the links to the left or below to navigate the geologic formations within the National Monument, they are ordered youngest at the top to oldest at the bottom.