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Lecture 4 Alluvial fans. What is an alluvial fan?. … a fan-shaped deposit of alluvium found where a stream flows out of a mountain onto flatter terrain. An alluvial fan in Death Valley. Narrow outlet (valley or gorge). Fan apex. Radial spreading alluvial fan. An alluvial fan in Death Valley.
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What is an alluvial fan? … a fan-shaped deposit of alluvium found where a stream flows out of a mountain onto flatter terrain.
An alluvial fan in Death Valley Narrow outlet (valley or gorge) Fan apex Radial spreading alluvial fan
An alluvial fan in Death Valley Coarse, channelized debris Sediments become finer-grained
Ok, back to alluvial fans….. The evolutionary stages of alluvial fans
Alluvial fans: Steeper gradient than “normal” river profiles, thus are often dominated by debris flow processes
Debris flows Shear stress vs. strain So flow is plug like and ceases as it reaches shallower surface, hence the velocity diminishes Flows also stop as they thin or lose water
Losing water and velocity caused the debris flow to become more viscous and stop, creating a very steep front
A closer view Note the existence of the “levees”
The radial deposition of alluvial fan Active depositional lobe
Period of active deposition, massive floods and debris flows
Facies relationships, a Devonian fan in Sweden, showing characteristic interfingering of depositional facies
Three small alluvial fans on Soda Lake Road Is there anything strange of these fans?