Top Banner
Part 8 Part 8 ALLUVIAL FANS ALLUVIAL FANS and DELTAS and DELTAS
6

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

Dec 20, 2015

Download

Documents

Welcome message from author
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
Page 1: Part 8 ALLUVIAL FANS and DELTAS. Classic alluvial fan. Fans often develop where confined channels on steep gradients suddenly emerge from their canyons,

Part 8Part 8

ALLUVIAL FANS ALLUVIAL FANS and DELTASand DELTAS

Page 2: Part 8 ALLUVIAL FANS and DELTAS. Classic alluvial fan. Fans often develop where confined channels on steep gradients suddenly emerge from their canyons,

• 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.

Page 3: Part 8 ALLUVIAL FANS and DELTAS. Classic alluvial fan. Fans often develop where confined channels on steep gradients suddenly emerge from their canyons,

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

Page 4: Part 8 ALLUVIAL FANS and DELTAS. Classic alluvial fan. Fans often develop where confined channels on steep gradients suddenly emerge from their canyons,

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

Page 5: Part 8 ALLUVIAL FANS and DELTAS. Classic alluvial fan. Fans often develop where confined channels on steep gradients suddenly emerge from their canyons,

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

Page 6: Part 8 ALLUVIAL FANS and DELTAS. Classic alluvial fan. Fans often develop where confined channels on steep gradients suddenly emerge from their canyons,

• 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.