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what is a floodplain
A flat area adjacent to the river carved out by rivers
why is it important to identify the location of a floodplain
- if you live in a floodplain you pay higher insurance rates
- building infrastructure: soil stability, soil erosion
hydrologic floodplain
every 1.5 yrs this area should experience flooding
Riparian zone
buffers formed b/w upland and aquatic zone
characteristics of a riparian zone
toe= organic rich
slope= fine grained
point bar
where active channel was, non horizontal
banks of flood plain act as
natural levees
levee
-highest elevation of floodplain
- sed. deposited near the channel edges
- restrict conductivity
first to be deposited when moving from high to low velocity
coarse grained
crevasse splay
- temporary delta when levee is breached
meander scrolls
former locations of the meander
oxbow lake
lake that forms in the bend of river where river no longer flows
Vertical accretion
-On top of floodplain deposits
- Can be colluvial or alluvial
-a Floodplain Process
Fluvial Terraces
abandoned floodplains formed when the river flowed at a higher level than at present; due to down-cuttings of river
Erosional terraces
- eroded down farther
- tread formed by lateral erosion
- when it occurs in Bedrock its called
• Bench, strath, or rock-cut terrace
depositional terraces
- River deposits build the river up
- Requires valley filling by something soft
-Subsequent incision
• Highest tread = highest elevation of valleyfloor
•
depositional terraces caused by
- Glacial outwash
- Climate change
- Change in sediment load, slope, or base level
Delta
A depositional plain where a stream enters a body of standing water
- The river supplies more sediment than can be redistributed
- have finer materials
- low gradient
-
fan
- Sediment eroded from the mountain is transported into a basin and deposited
- Coaser materials
- steeper
fan and delta similarities
- distributary channels
- fan shaped
- form by depositing sediments
What causes change in deltas?
- Sediment load
- Wave energy/turbulence
- Channel diversions through crevasses anddistributaries