The ages of some tsunami deposits can be determined by optical dating, a key requirement being that the deposits are derived from sediment that was reworked...
For any suite of optical dating samples two issues that must be considered are: do zero-age samples yield an optical age of zero, and are the optical ages...
Past aeolian activity was reconstructed at four dunefields in the prairie parkland and boreal forest of central Saskatchewan to elucidate landscape response to...
Center for Great Plains Studies, University of Nebraska-Lincoln
Geomorphological and archaeological evidence indicates potential linkages between Plains aboriginal occupation and dune activity in the Elbow Sand Hills of...
Geomorphic evidence and optical ages from seven locations indicate that widespread dune activity occurred within the last 200 years in the Great Sand Hills...
Late Wisconsinan dune activity was investigated within the present-day parkland and boreal forest regions to extend the spatial and temporal eolian record...
Late Wisconsinan dune activity is investigated within the present-day boreal forest and parkland regions of the northern Great Plains, Canada, to extend the...
The Holocene coastal landscape of northeastern Graham Island, British Columbia is reconstructed from ca. 9.5 ka to present based on surfi cial geology and...
Optical dating has now been established as a method that can be used to determine when quartz or feldspar grains in sediment were last exposed to sunlight. In...
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