Published via the yankee Geophysical Union as a part of the Water technological know-how and alertness Series.
The Deschutes is a "peculiar" dammed river in Oregon. Its dramatic juxtaposition of geology, topography, and weather provides a digital textbook of landforms and geomorphic techniques revealing Quaternary, Holocene, and intensely fresh occasions of vast value. alongside the energetic volcanism and tectonism, the current riverine panorama displays this episodic geomorphic historical past, as remnants of fluviatle gains, large bars and boulders, mantle the panorama. A bizarre River: Geology, Geomorphology, and Hydrology of the Deschutes River, Oregon tells a desirable tale a few "striking, occasionally intimidating, panorama that serves to question generalities and is a laboratory within which to review specified landforms and the strategies that produce them."Content:
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Additional resources for A Peculiar River
Smith, G. D. , Oregon State University, Corvallis, Oregon, 1986. Smith, G. , The influence of explosive volcanism on fluvial sedimentation-the Deschutes Formation (Neogene) of central Oregon, J. Sed. , 57, 613-619, 1987a. Smith, G. , Geologic map of the Seekseequa Junction and a por tion of the Metolius Bench quadrangles, Jefferson County, Oregon, State of Oregon Dept. Geol. Min. Ind. Geol. Map Ser. GMS-44, Portland, Oregon, 1987b. , A field guide to depositional processes and facies geometry of Neogene continental volcaniclastic rocks, Deschutes basin, central Oregon, Oregon Geol, 53(1), 3-20, 1991.
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21-53, 1989. Robinson, P. T, G F. Brem, and E. H. McKee, John Day Formation of Oregon-a distal record of early Cascade volcanism, Geology, 12, 229-232, 1984. Roering, J. J, J. W. Kirchner, and W. E. Dietrich, Evidence for non linear, diffusive sediment transport on hillslopes and implications for landscape morphology, Wat. Resour. , 35, 853-870, 1999. Russell, I. S. Geol. Surv. Bull. , 1905. Sarna-Wojcicki, A. , and J. O. , Geol. Soc. , The geology of North America (K-2), edited by R. B. Morrison, pp.