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S. Hughes, E. Taylor (1986)
Geochemistry, petrogenesis, and tectonic implications of central High Cascade mafic platform lavasGeological Society of America Bulletin, 97
C. Yang (1971)
Potential Energy and Stream MorphologyWater Resources Research, 7
R. Marston (1982)
The Geomorphic Significance of Log Steps in Forest Streams1Annals of The Association of American Geographers, 72
Caning Caning (1986)
The Noon Hill Flash Floods, July 13, 1983: Hydrological and Geomorphological Aspects of a Major Formative Event in an Upland LandscapeInstitute of British Geographers Transactions, 11
R. Jarrett (1984)
Hydraulics of High-Gradient StreamsJournal of Hydraulic Engineering, 110
P. Allen, Rebecca Narramore (1985)
BEDROCK CONTROLS ON STREAM CHANNEL ENLARGEMENT WITH URBANIZATION, NORTH CENTRAL TEXASJournal of The American Water Resources Association, 21
B. Heede (1972)
Influences of a Forest on the Hydraulic Geometry of Two Mountain StreamsJournal of The American Water Resources Association, 8
Jarrett Jarrett (1990)
Hydrologic and Hydraulic Research in Mountain RiversWater Resources Bulletin, 26
Piest Piest, Bradford Bradford, Wyatt Wyatt (1975)
Soil Erosion and Sediment Transport from GulliesASCE, Journal of the Hydraulics Division, 101
C. Tuckfield (1973)
Seepage steps in the New Forest, Hampshire, EnglandWater Resources Research, 9
Allen Allen, Narramore Narramore (1985)
Bedrock Controls on Stream Channel Enlargement with Urbanization, North Central TexasWater Resources Bulletin, 21
Wertz Wertz (1966)
The Flood Cycle of Ephemeral Streams in the Southwestern U.SAnnals of the Association of American Geographers, 56
D. Bowman (1977)
Stepped-bed morphology in arid gravelly channelsGeological Society of America Bulletin, 88
J. Whittaker, M. Jaeggi (1982)
Origin of step-pool systems in mountain streamsJournal of Hydraulic Engineering, 108
G. Priest, B. Vogt (1983)
Geology and geothermal resources of the central Oregon Cascade Range. Special Paper 15
R. Jarrett (1990)
HYDROLOGIC AND HYDRAULIC RESEARCH IN MOUNTAIN RWERSJournal of The American Water Resources Association, 26
Whittaker Whittaker, Jaeggi Jaeggi (1982)
Origin of Step‐Pool Systems in Mountain Streams. Proceedings of the American Society of Civil EngineersJournal of the Hydraulics Division, 108
A. Clarke, C. Hansen (1988)
Geomorphology of Upper Palm Wash, Anza Borrego Desert, California
Kellerhals Kellerhals (1970)
Runoff Routing Through Steep Natural ChannelsProceedings of the American Society of Civil Engineer, Journal of the Hydraulic Division, 96
Heede Heede (1981)
Dynamics of Selected Mountain Streams in the Western USAZeitschrift für Geomorphologie, 25
A. Chin (1989)
Step pools in stream channelsProgress in Physical Geography, 13
C. Gardner, A. Sarna‐Wojcicki (1989)
Guidebook for field trip to the Mount Bachelor-South Sister-Bend area, central Oregon High Cascades
T. Gardner (1983)
Experimental study of knickpoint and longitudinal profile evolution in cohesive, homogeneous material: Discussion and replyGeological Society of America Bulletin, 95
Peterson Peterson, Mohanty Mohanty (1960)
Flume Studies of Some Flow in Steep, Rough ChannelsJournal of the Hydraulics Division, 86
J. Laronne, M. Carson (1976)
Interrelationships between bed morphology and bed‐material transport for a small, gravel‐bed channel*Sedimentology, 23
Harrison Harrison (1965)
Some Problems Concerning Flow Measurement in Steep RiversJournal of the Institute of Water Engineers, 19
Gardner Gardner (1983)
Experimental Study of Knickpoint and Longitudinal Profile Evolution in Cohesive, Homogeneous MaterialGeological Society of America Bulletin, 94
E. Robison, R. Beschta (1990)
Coarse woody debris and channel morphology interactions for undisturbed streams in southeast Alaska, U.S.A.Earth Surface Processes and Landforms, 15
Gary Smith, L. Snee, E. Taylor (1987)
Stratigraphic, sedimentologic, and petrologic record of late Miocene subsidence of the central Oregon High CascadesGeology, 15
Jacques Wertz (1966)
THE FLOOD CYCLE OF EPHEMERAL MOUNTAIN STREAMS IN THE SOUTHWESTERN UNITED STATESAnnals of The Association of American Geographers, 56
P. Carling (1986)
The Noon Hill flash floods; July 17th 1983. Hydrological and geomorphological aspects of a major formative event in an upland landscapeTransactions of the Institute of British Geographers, 11
Beltaos Beltaos (1982)
Dispersion in Tumbling Flow. Proceedings of the American Society of Civil EngineersJournal of the Hydraulics Division, 108
Cheadle Cheadle, Thorne Thorne (1988)
Flow Resistance in High Gradient StreamsAmerican Geophysical Union, EOS, 69
E. Keller, F. Swanson (1979)
EFFECTS OF LARGE ORGANIC MATERIAL ON CHANNEL FORM AND FLUVIAL PROCESSESEarth Surface Processes and Landforms, 4
C. O'loughlin (1969)
Streambed investigations in a small mountain catchmentNew Zealand Journal of Geology and Geophysics, 12
Ostrem Ostrem (1964)
A Method of Measuring Water Discharge in Turbulent StreamsGeographical Bulletin, 21
E. Keller, W. Melhorn (1978)
Rhythmic spacing and origin of pools and rifflesGeological Society of America Bulletin, 89
D. Peterson, P. Mohanty (1960)
Flume Studies of Flow in Steep, Rough ChannelsJournal of Hydraulic Engineering, 86
Jarrett Jarrett (1985)
Analyses of Vertical Velocity Profiles in High‐Gradient Streams in ColoradoAmerican Geophysical Union, EOS66
S. Beltaos (1982)
Dispersion in Tumbling FlowJournal of Hydraulic Engineering, 108
Heede Heede (1972)
Influence of a Forest on the Hydraulic Geometry of Two Mountain StreamsWater Resources Bulletin, 8
ABSTRACT: One‐hundred‐and‐sixty step pools were examined that have developed in andesitic, basaltic, or dacitic lavas or in glaciofluvial sediments along several reaches of Soda Creek in the Three Sisters Wilderness of the Oregon High Cascades to determine whether such systems exhibit similar morphology. Pool shapes, sizes, and spacing were measured, and the hydraulic head loss calculated for each pool surface. Lithologic variations among 15 shape categories were not significant, but size attributes ‐ length, depth, and area ‐ of pools were systematically different by rock type. The energy lost at hydraulic jumps did not differ significantly among the four lithologies, suggesting that perhaps step pools represent similar stream channel adjustments in steep terrain.
Journal of the American Water Resources Association – Wiley
Published: Feb 1, 1995
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