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Tectonics, Geomorphology and Geologic Materials (The influence of the physical environment on watershed dynamics.) A Watershed Dynamics Tutorial © John F. Hermance February 9, 2003 (Images from Tasa Graphics among others) Contact information: Jack Hermance Environmental Geophysics/Hydrology Department of Geological Sciences Brown University, Providence, RI 02912-1846 Tel: 401-863-3830 e-mail: John_Hermance@Brown.Edu
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Regional tectonics can play a controlling role in local watershed dynamics. (Images from Tasa Graphics cannot be used without permssion of the company.)
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Plate tectonics drives current orogenic activity.
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Orogenic activity is enhanced at plate boundaries.
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How does the “rock cycle” determine local water decisions?
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Understanding the evolution of geologic features, generically or on a site specific basis, can give insight into watershed processes, hence water-related decisions.
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Igneous rocks
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Understanding the evolution of geologic features, generically or on a site specific basis, can give insight into watershed processes, hence water-related decisions. Metamorphic rocks
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Understanding the evolution of geologic features, generically or on a site specific basis, can give insight into watershed processes, hence water-related decisions. Sedimentary rocks
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The Northwest US.
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The “Rock Cycle” Exposed. The Northwest US.
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Igneous rocks
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Batholiths
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Intrusive igneous rocks
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Extrusive igneous rocks
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Metamorphic rocks
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Sedimentary rocks
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The Northwest US.
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The Western US. An Archetype Example
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The Western US. Physiographic Landforms
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The Western US. Basin & Range
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The Western US. Colorado Plateau
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The Western US. Snake River Plain
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The Western US. Cascades
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The Western US. Sierra Nevada
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The Western US. Southern Rockies
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The Western US. Northern Rockies
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The Western US. Rio Grande Rift
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The Western US. California Central Valley
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The Western US. Southern Basin & Range
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The Future (and the past).
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The Oldest Bedrock: Shield Areas of the World.
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“Basement”; then...
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“Basement”; now...
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Where or what is “basement”?
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Evolution of the crust
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Grand Canyon Exposure as a Microcosm of the North American Crust (From California to Massachusetts.)
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Next. we’ll look at the shallow unconsolidated section.
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We are interested in glacial features...
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... streambed features...
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... and fluvial deposits.
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Sedimentary sorting.
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(Back to metamorphism: Sediments are ephemeral.)
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(Metamorphic Grade.)
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A digression on glaciers.
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The Ice Age
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Maximum extent of glaciation.
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“Fossil” glacial features.
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(Moraines.)
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Glacial landforms.
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Glacial rebound.
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Present day mountain glaciers (or not) as “keys to the past”.
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Glacier in cross-section.
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Stresses in a glacier crossing a rock step.
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A tour of Canadian glacial forms.
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The Athabasca.
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A dry valley.
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A hanging glacier.
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A hanging glacier up-close.
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A trip up the Athabasca. (Note principal features.)
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The Ice Falls.
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The Ice Falls on approach.
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The Ice Falls on target.
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This is why we came here.
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(Radio waves through ice?)
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This is why we came here. (Radio waves through ice? What does this have to do with NASA, and the Lunar Lander (Apollo Program)?)
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“Fossil” glacial landforms.
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Stream morphology.
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Meanders.
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Meanders - Flooded.
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Meanders - Flooded - and buried.
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Stages of stream evolution.
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Deltas
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Drainage patterns driven by bedrock patterns.
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Current “geologic” processes can modify “current” hydrology.
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Mass movement can modify local hydrology & vice versa.
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Affect of subsurface water on mass movement.
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Evolution of bedrock.
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The paradigm for subsurface hydrology. Organic layer Leached layer Weathered bedrock Bedrock
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Physiography of North America.
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Groundwater regions of the US. (Note concordance with geology.)
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End of Presentation (Tectonics, Geomorphology and Geologic Materials) © John F. Hermance; February 9, 2003 Go to Soil & Water.
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