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Floodplain Management SESSION 2. Stream Systems on Dynamic Earth Geologic Framework Prepared By Donald R. Reichmuth, PhD. Geologic Framework. Objectives: Define Floodplains Describe Stream System Functions Explain Tectonic Plates Explain Vertical Plate Motion
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Floodplain ManagementSESSION 2 Stream Systems on Dynamic Earth Geologic Framework Prepared By Donald R. Reichmuth, PhD.
Geologic Framework Objectives: Define Floodplains Describe Stream System Functions Explain Tectonic Plates Explain Vertical Plate Motion Identify Tectonic Domains Summarize Glacial Behavior Compare Erosion Related Processes
River Basin Definition A region or area bounded by a topographic divide that contributes water to a particular stream channel (corridor) or other water body.
Floodplain Definition That portion of a Drainage Basin that is covered by Transported Sediment that was deposited in or near a stream channel.
FUCTIONS OF RIVER SYSTEMS • Removes Erosional Debris • Most Important • Acts Over Long Periods • Removes Excess Water • Importance Secondary • Acts Sporadically Over Short Periods • Provides Fresh Water Supply • Necessary To Sustain Life • Transports Chemicals & Nutrients
Geologic Framework • Tectonics • Passive Margins • Stable Platforms • Active Margins • Hot Spots • Glaciation • Alpine Glaciers • Continental Glaciers • Geomorphology • Surface Forming Processes • Water • Ice • Gravity • Wind
Stream Systems on Dynamic Earth BASIC TYPES OF PLATE INTERACTION
North America Structure • Craton • Shield • Stable Platform • Mobile Belts Tectonic Activity • Active Margin • Passive Margin
Karst TopographyExample • Solution Cavities In Limestone • Streams Have Subsurface Connections
Vertical Plate Motion Causes: Tectonic/Earthquake Activity Erosion & Sediment Loading Glaciation Human Activities
Himalayan Data Present Height --- 30,000 Ft (9,500 m) Tectonic Uplift Rate --- More Than 1 cm/yr Erosion Rate --- Now Equals Uplift Rate Sediment Yields Highest Known
Oceanic-Continental Convergence Oceanic Crust Subducts Ocean Trench Forms Lighter Melted Material Rises Volcanoes Form Lithosphere Plunges Into Asthenosphere
Active Margin Note: • Aleutian Trench • Canada • Strike-Slip Faulting • Mobile Belt Deposits • California • Strike-Slip Faulting
Active Margin • Ocean-Continent Subduction • Strike Slip Faulting
Passive Margin • Coastline Sinking • Drowned River Valleys • Numerous Near-shore Islands • Shoreline Migrating Landward
Northern Hemispheric GlacialAreas16,000 B.P. NOTE: Portions Of Alaska Are Ice Free
Pleistocene Glaciation Note: • Alpine Glaciers • Continental Glaciers • Ice Marginal Rivers • Alaska Ice Free Area
Preglacial Teays Basin Teays Basin Overrun By Ice Channel Buried Ohio River Forms Drains Basin
Western Glacial Lakes 15,000 B.P. • Climate Much Wetter Than Present • Large Basins Had Internal Drainage
Loess Wind Blown Silt From Glaciers Rock Flour Stream Banks Stand Vertical When Stable
Sea Level Changes 16,000 Years BP -- 120 Meters Lower 6,000 Years BP – Reached Present Level Near Future – Expected To Rise
HoloceneSea Level Changes Primarily Cause --- Glacial Melting In The Northern Hemisphere
Erosion In River Basins Controlling Factors: • Chemical vs. Mechanical Weathering • Temperature • Precipitation • Basin Gradient • Basin Soil/Bedrock Type • Tectonic Activity
CASE STUDIES • Columbia River • Mississippi River • Ohio River • Potomac River • Red River of the North • Rio Grande River • Santa Ana River
Slide PresentationPrepared ByGeomax, P.C.Dr. Donald R. Reichmuth, President1023 W. 30th Ave.Spokane, WA 99203-1324Phone & FAX – 509-838-6390E-mail – geomax@comcast.net