Megan Kenworthy is a hydrologist with the USGS Idaho Water Science Center in Boise, Idaho.
Megan joined the Idaho Water Science Center in 2022. Her research interests are centered on instream processes, including sediment transport, flow hydraulics, and understanding changes in stream channel morphology.
Professional Experience
Hydrologist, USGS Idaho Water Science Center, June 2022 - Present
Project Geomorphologist, Geomorphic Solutions, LLC, March 2019 - May 2022
Education and Certifications
M.S., Hydrology, 2011, Boise State University
B.A., Environmental Studies, 2004, University of Montana
Science and Products
Non-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
Estimating Spring Discharge to the Snake River, Milner Dam to King Hill, Southern Idaho
Science and Products
- Publications
Non-USGS Publications**
Yager, E.M., Kenworthy, M., and Monsalve, A., 2015. Taking the river inside: Fundamental advances from laboratory experiments in measuring and understanding bedload transport processes. Geomorphology, 244, pp. 21-32, https://doi.org/10.1016/j.geomorph.2015.04.002.Kenworthy, M.K., Rittenour, T.M., Pierce, J.L., Sutfin, N.A. and Sharp, W.D., 2014. Luminescence dating without sand lenses: An application of OSL to coarse-grained alluvial fan deposits of the Lost River Range, Idaho, USA. Quaternary Geochronology, 23, pp. 9-25.Kenwothy, M.K., 2011. Optically stimulated luminescence dating of Gravelly Alluvial Fan Deposits: Links Between Climate Change and Geomorphic Response in the Lost River Range, Idaho. Master’s thesis. Boise State University. http://scholarworks.boisestate.edu/td/249.**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
- Science
Estimating Spring Discharge to the Snake River, Milner Dam to King Hill, Southern Idaho
Groundwater discharges to the Snake River from numerous volcanic rock springs along the northern canyon wall between Milner Dam and King Hill. Water-resource managers need to be able to quantify the amount of this water to understand the eastern Snake River Plain aquifer's recharge, storage, and discharge. When completed, this study will provide the Idaho Department of Water Resources with an...