Part 8 ALLUVIAL FANS and DELTAS. Classic alluvial fan. Fans often develop where confined channels on steep gradients suddenly emerge from their canyons,

Slides:



Advertisements
Similar presentations
Erosion and Deposition
Advertisements

Landforms of the Fluvial System
Another Important Abiotic Factor
Another Important Abiotic Factor
Landforms Vocabulary Landform Vocabulary
Remote Sensing Lab, Part B Patterns of Deposition.
Stream Development.
Part 6 CLASSIC FLOOD PLAINS. FLOOD PLAINS Flood plains are those alluvial valleys that are periodically subject to inundation by flooding of a natural.
What landform am I? Canyon Which agent(s) changed me? Water Wind Ice.
Lab 8 Stream Processes. Channel Types Braided - steeper, large sediment supply Meandering - less steep, lower sediment supply.
Running Water Running water Water as an agent of erosion; water in streams, tributaries (larger streams) and rivers that flow down hill therefore changing.
Factors affecting erosion and deposition Velocity Gradient – rise over run Channel shape Channel roughness Discharge – amount of water flow per unit.
Stream Erosion & Deposition
Alluvial Fans By Tim Baker & Tom Coburn.
River Systems Earth Space Science Mr. Coyle. The Hydrologic Cycle Infiltration = Groundwater System Runoff = Surface Water System Runoff = Precipitation.
Chapter 4: Weathering and Erosion
Restoring Deltaic Functions on the Mississippi Harley S. Winer, Ph.D., P.E. Atkins, Metairie, LA Harley S. Winer, Ph.D.,
Surface Water Chapter 9 Notes.
EROSION- The transport of weathered materials….
Stream Erosion and Transport
Surface Water An Erosional-Depositional System. Running Water When running water is confined to a channel, it is called a stream Smaller streams called.
Streams: Transport to the ocean
River Systems. Objective  Students will describe factors that affect the erosive ability of a river and the evolution of a river system.
Erosion and Deposition
You have learned how to interpret how landforms are the result of a combination of constructive and destructive forces such as deposition of sediment and.
LANDFORMS VOCABULARY Clicker Presentation Created by: Cindy Jarrett Landform Vocabulary Clickers Interactive Presentation Created by: Cindy Jarrett Cindy.
Stream Erosion & Deposition Chapter 6 sections 1 and 2.
 Potholes are formed due to stream or river erosion which initiates by simple plucking out at the riverbed by hydraulic action.  These are variously.
TRANSPORTATION & DEPOSITION in a Stream System.
Rocks and Landforms I- 5/I-6 Review for Quiz. Question What is the shape of most rivers? What is the shape of most rivers?
Water Erosion “We’re changing Earth’s Surface!” A. Stream Erosion 1. Running Water 2. Energy 3. The water cycle -Most effective agent in wearing down.
River Transportation and Deposition
Objectives Describe some of the physical features of stream development. Explain the process of rejuvenation in stream development. –stream channel –stream.
Mississippi River. Names Great One Father of Waters “Great River” “Big River” Derived from the Ojibwe word misi-ziibi ("Great River") or gichi- ziibi.
Delta Environments Nile Delta Mississippi Delta.
Stages of River Development
RUNNING WATER.
Landforms Vocabulary Foss Science.
River Systems You will learn: Where do rivers begin?
River Terraces.
Chapter 11 The Flow of Fresh Water.
Chapter 13 Surface Water.
Erosion and Deposition
Stream/River Erosion & Deposition
River System Development
Things that BUILD UP and TEAR DOWN the Earth…
River Systems Part 3 Formation of Deltas Flooding.
Erosion and Deposition from Water
Running Water.
Landforms Vocabulary Landform Vocabulary
You have learned how to interpret how landforms are the result of a combination of constructive and destructive forces such as deposition of sediment and.
Chapter 18.
Stream Erosion.
Stream/River Erosion & Deposition
Erosion.
Gradient The land surrounding the river channel. Valley The middle section of the river. Upper Course The steepness of the river. Mid Course The part of.
Landforms made by Deposition
Stream/River Erosion & Deposition
NAME THAT LANDFORM!!!!!!.
Erosion and Deposition
Rivers and Running Water
Sedimentary Rocks A sedimentary rock is formed by the accumulation and compaction of sediments (rock pieces, minerals, animal parts, or chemical precipitates)
Stream/River Erosion & Deposition
Tributary.
Natural and Man-made features
You have learned how to interpret how landforms are the result of a combination of constructive and destructive forces such as deposition of sediment and.
Lots of tributaries joining 3rd order streams To travel across Quick or sudden Side view of the area showing the changing elevations Small 1st and.
Landforms Around the World
Stream/River Erosion & Deposition
Rivers features.
Presentation transcript:

Part 8 ALLUVIAL FANS and DELTAS

Classic alluvial fan. Fans often develop where confined channels on steep gradients suddenly emerge from their canyons, changing the flow regimen sufficiently to stimulate deposition.

River deltas are commonly built off a series of anastomotic distributary channels, such as that shown at lower right

The Mississippi and Atchafalaya Rivers have deposited enormous deltas over the past 6000 years; Delta # 7 being the youngest and #1 the oldest.

Abandoned distributaries of the Mississippi and Atchafalaya Rivers. The Metairie Ridge distributary channel, separating lower and upper New Orleans, is shown in red

Until the construction of jetties in the late 1870s, sand bars closed off the mouth of the Mississippi River each year for as much as 3 months at a time following high flows.