Caldwell B. answered 05/22/19
Tutor - Geology/ Ichnology
Age is best determined when an ash layer is deposited over a large area in a short amount of time to ensure that Zircon populations in the deposit are homogeneous for U/Pb dating. If radiometric dating is not available, shorter events can be used as lithostratigraphic marker beds and dated using biostratigraphy. A famous example of such an ash bed is the "X" Bentonite from the Graneros Shale (Cretaceous Western Interior Seaway).