Please wait...
About This Project
Sheeted clastic dikes offer geologists a new way to count the Missoula floods. The dikes formed coincident with flooding and grew larger with each flood event. Each flood is preserved as one or more fill bands in dikes. Each subbasin preserves a different flood count. Here we test whether clastic dikes grew larger in basins visited by more floods by documenting the number of fill bands in dikes at 300 sites throughout the Columbia Basin.
More Lab Notes From This Project
Browse Other Projects on Experiment
Related Projects
Excavating dinosaurs from the Late Cretaceous Almond Formation of Wyoming
In 2021 and 2023 we surveyed the Late Cretaceous Almond Formation of Wyoming for fossils. We discovered...
What factors affect the attractiveness of rivers to people?
Rivers are an important part of the natural environment. They provide habitat for fish, crayfish, insects...
Studying the World's Largest Invertebrate - the Colossal Squid, Mesonychoteuthis hamiltoni
We are launching a multi-year expedition to film a colossal squid in the deep sea for the first time off...