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Hydrology and Geomorphic Evolution of Basaltic Landscapes, High Cascades, OR
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About The Presenter
Anne Jefferson, Oregon State University, Department of Geosciences
About This Presentation
Running time: 42 minutes and 37 seconds.
Given: September 20, 2006, Ph.D. Defense.
Production by: M.J. Furniss and J. Guntle, Communications and Applications, PNW and PSW Research Stations
Topics covered:
- Hydrology and Geomorphic Evolution of Basaltic Landscapes—High Cascades—Oregon Geology
- Influences on Hydrology
- Some Ways It Might
- More Ways
- Cascades Geology and Streamflow Patterns
- Geologic Setting
- Western Cascades
- Subsurface Storm Flow
- Flows
- High Cascades
- Groundwater Flow
- High Cascade Springs
- Geology Predicts Summer Streamflow
- August Flow From Springs
- March Flow From Springs
- Volcanic History and Flow Patterns
- Study Area
- Flowpaths Do Not Follow Topography
- Stable Isotopes
- Springs Recharge in Young Lavas
- Recharge Areas
- Geology Trumps Topography
- Upper McKenzie Springs
- Remainder of Recharge
- Flowpaths and Ages
- Shallow Flowpaths
- How Old Is the Water?
- Ages Ranges From 3 to 14 Years
- Aquifer Volume
- Cracks in Volcanic Rock
- Aquifer Thickness
- Groundwater Velocity
- Hydraulic Conductivity
- Groundwater Flowpaths and Geologic History
- Hydrogeologic Controls
- Motivation: Warming Winters
- Study Watersheds
- Santiam Junction Precipitation
- Clear Lake Water Budget
- Temporal Centroid
- Autumn Minimum Discharge
- Sensitivity to Climate Variability
- Drainage Development
- Landscape Evolution
- Models of Drainage Evolution
- Depression Linkage
- Groundwater Seepage Erosion
- Knickpoint Migration
- Permeability Reduction
- Chronosequence of Landscapes
- Drainage Density Increases Over Time
- Chronosequence of Landscapes
- Major Springs Persist for =1 Ma
- Chronosequence of Landscapes
- Topographic form—end Members
- Topographic form—intermediates
- Processes that reduce Permeability
- Drainage Development on Permeable Landscapes
