
The Lecture:
Subduction-related late Quaternary tectonic uplift and sea-level change in the Pacific NW and around the Pacific Rim
In 1979, Seiya Uyeda and Hiroo Kanamori introduced a tectonic model with two end members of a subduction-boundary continuum: the “Chilean” type (shallow dip of the subducting plate, great thrust events, compression, and uplift of the overriding plate) and the “Mariana” type (steep dip of the subducting plate, no great thrust events, tension, and little or no uplift). The concept has been used to explain variable rates of Quaternary uplift around the Pacific Rim, and the paper has been cited over a thousand times since its publication in the Journal of Geophysical Research. We now have a sufficient number of dated late Quaternary marine terraces from around the Pacific Rim to test the veracity of this model. In this presentation, well-dated emergent shorelines of the Pacific Rim will be explored, from South America, North America, the Aleutians, Japan, and the Marianas.
About the Speaker
Dan Muhs is an emeritus scientist with the U.S. Geological Survey. He earned B.A. and M.S. degrees from the University of Illinois and a Ph.D. from the University of Colorado. He was a research geologist with the USGS from 1985 until his retirement in 2022. Despite his retirement, Dan remains an active researcher, lecturer, and writer.
Dan’s interests are in the fields of coastal and eolian geomorphology, Quaternary stratigraphy, soil genesis, and paleoclimatology. Most of his work has been in the US (Alaska, western US, and Great Plains), but he has also worked in Canada, Mexico, Caribbean, Spain, and western Pacific. Over the course of his career he has authored more than 150 scientific papers on a diverse range of subjects focused on the Quaternary period, including the origins and history of loess and dune fields, paleozoogeography of marine fossil invertebrates, tests of glacial isostatic adjustment models, and sea-level histories and tectonic uplift rates deduced from emergent marine terraces. Dan has received numerous awards and recognition, including the Geological Society of America Kirk Bryan Award.