370 likes | 612 Views
General Geology: Raining Water. Instructor: Prof. Dr. Boris Natalin. Running water. Distribution of Earth water. All water reservoirs constitute the hydrosphere. The hydrologic cycle. Infiltration . Runoff. Rate of rain is greater than the rate of infiltration Sheet flow Rill Stream .
E N D
General Geology: Raining Water Instructor: Prof. Dr. Boris Natalin
Distribution of Earth water All water reservoirs constitute the hydrosphere
The hydrologic cycle Infiltration
Runoff • Rate of rain is greater than the rate of infiltration • Sheet flow • Rill • Stream
Streamflow • Laminar flow • Turbulent flow River system consists of 1) zone of erosion, 2) zone of sediment transport, and 3) zone of sediment deposition
Gradient The slope of the stream is expressed as a vertical drop over specific distance Discharge
Changes downstream • Head or headwaters and mouth • Longitudinal profile of a stream
Base level and graded stream profiles Sea level = base level = ultimate base level Local base level:Lakes Resistant rocksLarger streams
Stream erosion • Abrasion is the destruction by lifted particles (sandpaper)
Stream erosion Potholes are created by abrasive action of swirling particles
Transport of sediment by stream Streams sort transported rock fragments in accord with their sizes Types of sediment load transported by streams: 1) Dissolved load 2) Suspended load 3) Bed load
Bed load • Rolling • Sliding • Saltation (jumping)
Transport of sediment by stream • Capacity • Competence
Deposition of sediments by streams Material deposited by streams is called alluvium.
Deposition of sediments by streams Braided rivers
Stream valley Located closer to water heads • Vertical walls – canyons • V-shape
Stream valley: Wide valley (U-shape) • Erosional floodplain • Depositional floodplain
Incised Meanders and Terraces • Drop of base level • Terraces helps in studies of uplift history • Slip rate of the North Anatolian fault
Deposition of sediments by streams: Natural Levees • Fine grained sediment • Natural levees • Back swarms
Alluvial fans • Alluvial fans are formed at the abrupt drop in stream gradient
Stream piracy • River cuts through ridge or mountain • Antecedent valleys • Wind gaps
Stages of valley development • A – youth (V-shape) • B and C – maturity • D - old