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Armored Beach
Shorelines protected by large rocks/boulders (sometimes man made)
Backwash
when waves go back from shore
Barrier Island
formed as waves rapidly deposit sediment
parallel to shore lines
start as a sandbar and grow over time (can also be taken away)
Beach Face
where waves are breaking
wet at high tide
dry at low tide
Beach renourishment
the process of dredging and pumping sediment from off the shore and brining it to the beach
increases width of the beach
man made- major storms take it away
has to be redone periodically
Berm Scarp
steep slope/drop off
created by waves hitting the same part
Berms
raised section of the sand
where we hangout
Brackish water
fresh water and salt water
cliff
steep rocky base
not always present
often leads to erosion
depositional coast
secondary coast
areas where more sediment is added to the shore, than is taken away
where beaches are growing
formed by waves, currents, tides, bring sediment to the shore line
have a gentle slope to them
dredging
the process of excavating sediments and debris from the bottom of waterways, like rivers, lakes, and harbors, to maintain navigability and improve water quality
Estuaries
behind barrier island
partially enclosed water
an ideal habitat
shallow water, lots of sunlight, lots of nutrients, many places for creatures to hide
Euryhaline
being able to tolerate a wide range of salinities, making organisms able to live in salt or fresh water
Fiddler Crab
have a big claw used for attracting mates, and fighting
Hook
sand spit that has a curve at the end, happens because of wave pattern
Inlet
a small arm of the sea, a lake, or a river
Jetties
interrupt/redirect the longshore currents
keep sandbars from filling in, why we have waterways
between barrier islands
build up of sediment on one side and erosion on the other
Longshore currents
an ocean current that moves parallel to the shoreline
Longshore drift
The movement of material, such as sand and stones, along a coastline caused by the movement of waves
Low tide terrace
only exposed during low tide
very gentle slope into the water
the end is like a “drop off”
Oyster reef
underwater ecosystems formed by dense aggregations of oysters that provide important habitat, filter water, and protect coastlines
Primary Coast
formed by land based processes, not by the ocean
made by things like rivers, volcanos, glaciers, tectonic plates
tides WON’T change these beaches
Salt marsh grasses
salt-tolerant plants, particularly grasses, that thrive in coastal areas where saltwater mixes with freshwater, like estuaries and along coastlines protected from strong waves
Sand bar
aka off shore bar
can be submerged or partially exposed
formed by sediments because of wave action
run parallel to the shore
Sand bubbler crab
filter food through sand, “clean” the beaches, make those little sand balls
seagrass bed
absorb nutrients from the water
stabilize the sea floor - MAJOR protective factor
help to clarify water both physically and chemically (absorb things out of water)
oysters, muscles, clams hangout here
Secondary coast
formed by waves, currents, marine life, and tides
oceans can reshape/change what they look like
often way older beaches
stenohaline
require a specific range of salinity for survival
Summer berm
formed by gentle waves
usually pretty wide
parallel to shore line
swash
when waves are approaching the shore, comes at an angle
tombolo
narrow strip of sand that connects an island to the mainland or one island to another
formed by waves and sediment
as waves approach land they loose energy
trough
a little dip right after the terrace
waves also break here
right before the first sand bar
turbidity
murky, cloudy
uplands
dry area above the beach, not being effected by waves/tides
boundary between land and sea
winter berm
stronger waves in winter
much thinner area
waves pull sand off of it