Drilling Projects By
Climate & Ecosystems
Sustainable Georesources
Natural Hazards
World
Geological Time
- Map of North and Central America
- Anadarko Basin (Oklahoma, U.S.A.)
- Bighorn Basin (U.S.A.)
- Blue Hole (Belize)
- Cape Cod (U.S.A.)
- Chesapeake Bay (U.S.A.)
- Chicxulub (Mexico)
- Chicxulub 2 (Mexico)
- Colorado (U.S.A.)
- Colorado 2 (U.S.A.)
- Death Valley (U.S.A.)
- Hawai'i (U.S.A.)
- Koolau (U.S.A.)
- Lake Chalco (Mexico)
- Lake Petén Itzá (Guatemala)
- Lead (U.S.A.)
- Long Valley (U.S.A.)
- Mallik (Canada)
- Newberry (U.S.A.)
- New Jersey (U.S.A.)
- Nicaragua
- Oklahoma (U.S.A.)
- San Andreas Fault (U.S.A.)
- Sevier Basin (U.S.A.)
- Snake River (U.S.A.)
- Sudbury (Canada)
Colorado Plateau Coring Project
Filling the Triassic Geochronologic Gap: A Continuous Cored Record of Continental Environmental Change in Western North America
The Triassic Period (~252-202 Ma) witnessed the evolutionary appearance of modern terrestrial biota, the origin and rise to ecological dominance of dinosaurs, and dramatic climate changes on the continents. The complex of epicontinental basins in western Pangea, now exposed on the Colorado Plateau, preserves a rich low-paleolatitude biotic and paleoenvironmental terrestrial record from the Triassic.
