@article {83047,
	title = {Characteristic scales of drainage reorganization in Cascadia},
	journal = {Geophysical Research Letters},
	volume = {48},
	number = {3},
	year = {2021},
	note = {The organization of river basins varies over geologic time.  Tectonic forces, uplift and erosion can cause a stream to be {\textquotedblleft}captured{\textquotedblright} by a neighboring river basin.  Stream captures are relatively common in the Oregon Coast Range.  In this most interesting article, the authors describe a process of modeling stream networks at different geographic scales. {\textquotedblleft}Integration of these {\textquoteleft}synthetic{\textquoteright} drainage networks into a margin-parallel river system, similar to the modern Willamette Valley, supports field observations of stream capture and river network reorganization. We propose that these methods are useful for predicting future drainage configurations and isolating the relevant tectonic processes responsible for changing river networks{\textquotedblright} (from the Abstract). This is an open-access article.},
	month = {2021, Feb.16 },
	pages = {e2020GL091413},
	keywords = {Columbia River, Cow Creek, geography, geology, Klamath River, mathematical modeling, paleosciences, Rogue River, Siletz River, South Umpqua River, topography, Umpqua River Basin, Yaquina River},
	doi = {https://doi.org/10.1029/2020GL091413},
	url = {https://www.sciencedirect.com/science/article/pii/S1470160X20311067?via\%3Dihub },
	author = {Struble, William T. and Roering, Joshua J. and Dorsey, Rebecca J. and Bendick, Rebecca}
}
@inbook {36901,
	title = {Geoarchaeological themes in a dynamic coastal environment, Lincoln and Lane Counties, Oregon},
	booktitle = {Volcanoes to vineyards : geologic field trips through the dynamic landscape of the Pacific Northwest},
	series = {Field Guide (Geological Society of America)},
	volume = {15},
	year = {2009},
	note = {"In many ways, the modern Oregon coastline bears little resemblence to that associated with prehistoric coastal peoples prior to 3000 years ago..." (from the abstract).  Examines how geological forces (earthquakes, sea level rise) have changed the landscape and obscured early peoples{\textquoteright} occupations of the area.  First stop on the tour is at the main HMSC parking lot, and the second stop is at Yaquina Head. Mentions Siletz, Yaquina, Alsea, Yachats and Siuslaw paleorivers.},
	pages = {p.319-336},
	publisher = {Geological Society of America},
	organization = {Geological Society of America},
	address = {Boulder, Colo.},
	keywords = {archeology, Florence dune sheet, Neptune State Park, Oregon State University Hatfield Marine Science Center, subsidence, tsunamis, Yaquina Bay, Yaquina Head},
	url = {https://www.researchgate.net/publication/290241966_Geoarchaeological_themes_in_a_dynamic_coastal_environment_Lincoln_and_Lane_Counties_Oregon},
	author = {Davis, Loren G. and Jenevein, Steven A. and Punke, Michele L. and Noller, Jay S. and Jones, Julia A. and Willis, Samuel C.},
	editor = {O{\textquoteright}Connor, Jim E. and Dorsey, Rebecca J. and Madin, Ian (eds.)}
}
