LA-geography-Awesome-power-of-rivers

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Transcript LA-geography-Awesome-power-of-rivers

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Natural
Land
Regions
Coastal Marshes
Created when sediment
collected at the mouths of
rivers as they entered the
Gulf
Low wet grassland; usually
no trees
Exception: Cheniers:
ridges of high ground in the
marsh that run parallel to
the coastline; live oak trees
grow here
Saltwater, freshwater, or
brackish
Floodplains
 Low, flat valleys through
which rivers flow
 Include: Swamps,
sloughs, bayous, and
lakes
 Vegetation: Deciduous
trees (Cypress, Oak,
Hickory, Pecan, Magnolia,
Tupelo Gum, and
Cottonwood)
 sugarcane
Uplands
Areas with the highest elevation
Formed when magma pressure and
tectonic forces pushed the land upward
Erosion then washed away soft material,
leaving the hills
Vegetation: Some deciduous trees;
Dominated by coniferous trees
Coniferous: evergreen, cone-bearing
trees or shrubs
Contain ancient terraces (often called
hills)created by rivers
Sketch Louisiana landforms
Examples of Uplands
 Largest upland area – Piney Hills
 Piney Hills is the V-shaped region in the northern part of
the state that includes Driskill Mountain (rises 535 feet
above sea level)
 Uplands: Kisatchie National Forest, Dolet Hills, Florida
Parishes
Uplands
Did you know Louisiana once had
Prairies?
 Prairies: wide flat
areas where short
grasses flourish, but
few trees appear
 Common in
southwest Louisiana
 Large herds of
Buffalo used to roam
 Agriculture and
urban development
destroyed most of
the natural prairies
and animal life that
once existed
Awesome Power of Rivers
 Rivers’ sediment creates the land, and their movement
shapes it
 Louisiana Landforms: Floodplains, Meandering Streams,
Point Bars, Natural Levees, Terraces, Deltas, Coastal
Marshes, Barrier Islands, Cheniers
1. Floodplains
Floodplain: flat
valley floor covered
by excess water
caused by heavy
rains that spills over
the riverbanks
Reservoir: holds
excess water
2. Meandering Streams
 Meandering Streams:
winds its way back and
forth across the
floodplain in loops and
curves;
 Water always seeks the
path of least resistance
and goes around
obstacles
3. Point Bars
Point Bar: formed from
sediment falling to the
bottom of the river after
the current slows along
the inside of the meander
Oxbow lake: The
meander gets larger until
it creates nearly a full
circle around a narrow
neck of land;
the river eventually
straightens itself out by
cutting across the point
bar.
 The ends of the old
meander close up to form
an oxbow lake.
Oxbow lake
4. Natural levees
sediment builds
along the riverbank
forming strips of
elevated land.
5. Terraces
 Terraces: elevated ridges that
formed from the old riverbeds;
50-100 feet higher than the
surrounding floodplain.
 Ex. Terrace: Macon Ridge: 100
miles long and 20 miles wide;
Highland Road in Baton Rouge
 Loess: loamy wind-blown deposits
rest on terraces; behaves like
clay when wet; when the thick
layer of loess eroded it left the
region scarred with deep gullies
and high bluffs; ex. Vicksburg,
Mississippi
6. Deltas
Deltas: a landform shaped like a fan or a bird’s
foot where a river flows into the ocean; most
famous delta is the Miss. River Delta
Bar: underwater barrier of mud that interferes
with the river’s current; process continues
forming bird’s-foot shape.
7. Coastal Marshes
Coastal Marshes: wet
grasslands formed by
river sediment
deposited along the
coast during floods
Brackish: fresh and
saltwater mixed
together
Louisiana has the
largest marshland
area in the U.S.
8. Barrier Islands
Barrier Islands: created after a river
abandons its delta;
without fresh sediment to maintain it, the
delta erodes away;
sturdy bar that formed at the river’s mouth
remains.
Waves and tides deposit sand leaving a
crescent shape island.
Barrier Islands Importance:
1) absorb storms;
2) protect the mainland from erosion;
3) block saltwater from entering the marsh during storms;
4) home to thousands of birds, turtles, fish, and shellfish
Before and After Katrina
9. Cheniers
 Cheniers: ridges of high ground in the coastal marsh
that run paralles to the coastline; composed of shell and
sand; remnants of Gulf of Mexico beaches; 4 to 5 feet
high and several yards wide
 Example: Pecan Island and Holly Beach
 Chenier is French for “place of oaks”; live oaks thrive on
them
 Significance of a chenier: people live on them because
they do not flood; protect coastal marshes from
hurricanes
Other Land Forms
Rocks:
All native rock in
Louisiana is
sedimentary rock;
sediment compressed
into rock
Louisiana rock formed
between 2 and 66
million years ago

Hills
 After Gulf Coastal
Plain formed,
geologic forces
caused the land to
push upward
forming mountains
which eroded away
the forming hills
Salt Domes
 Reminders of the ancient sea that once covered
Louisiana
 Parts of the sea dried up leaving a layer of
salt and other minerals exposed
 Salt was covered by sediment and now lies
about 10 miles below the ground
 The weight exerted so much downward pressure
that in some places the salt squeezed upward like
toothpaste in tall vertical columns called salt
domes
 Louisiana has hundreds of salt domes
 They appear as wooded hills about 2 miles in
diameter
 Example: Five Islands: Jefferson Island, Avery
Island, Weeks Island, Cote Blanche, and Belle Isle


North Louisiana, salt domes do not protrude
above the earth’s surface; salt appears as a white
sandy crust
Salt mining is an important industry
 Mine shafts are dug into salt domes and the hard
rock-like salt is mined and brought to the surface
for crushing
 2nd largest salt mine in world is Belle Isle
 Salt Domes were once used as storage for oil
Salt Dome Locations
Salt Dome
Salt Dome
Aquifers
 Aquifer: underground water reservoir
 As sediment deposits slowly build up
the land, freshwater sometimes
becomes trapped between two layers
of sediment.
 Water Table: depth in the ground at
which water is located
 We are now drawing out more water
that is being replaced by nature.
 North Louisiana is facing a problem of
the falling water table of the Sparta
Aquifer
Sparta Aquifer
Avery Island Salt Dome