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54 Cards in this Set

  • Front
  • Back
serious coastal hazards?
rip currents
coastal erosion
tsunamis
tropical cyclones (P-typhoons/A-Hurricanes)
wave creation
wind blowing over the water produces friction, air is moving faster than water, moving air transfers energy into the water
size of waves depend on?
velocity, or speed of wind
duration of wind
distance that wind blows across the surface - fetch
wave height
difference between wave's trough and it peak
wave length
distance between successive peaks
wave period
time in seconds for successive waves to pass a reference point
swell
wave group that was generated by storms far out at sea
wave energy is approximately proportional to the square to...
wave height
beach
landform consisting of loose material, such as sand or gravel, that has accumulated by wave action at the shoreline
plunging breakers and spilling breakers
plunging at convergent
spilling at divergent
berms
flat backshore areas on beaches formed by deposition of sediment as waves rush up and expend the last of their energy
beach face
sloping portion of the beach below the berm
swash zone
part of the beach face that is exposed by the uprush and backwash of wave
surf zone
turbulent translational waves moves toward the shore after the incoming waves break
breaker zone
area where the incoming waves become unstable, peak and then break
longshore trough and longshore bar
elongated depression and adjacent ridge of sand produced by wave action
longshore sediment transport/littoral transport
process of transporting sand along beach
1. sand is transported along the coast
2. up and back movement of beach sand in the swash zone causes the sand to move along the beach in a zigzag pattern
rip currents/riptides/undertow
concentrated narow zones of water outflow
beach budget
input, storage and output of sand or larger sediment that may be found on the beach
sea cliff
steep bluff or cliff
* exposed to both wave action and land erosion processes such as running water and lanslides
erosion factors (seacliffs)
landslides
sea level dropping - seacliff base
urbanization along seacliff
hard stabilization
engineering structures to protect a shoreline from waves
soft stabilization
adding sand to a beach (beach nourishment)
managed retreat
living with beach erosion with perhaps a mixture of hard and soft
wetlands
large areas of coastal regions
- protected from waves and currents
- high biological productivity
- climate governs vegetation
estuaries
river valleys flooded by marine water
- mix of fresh and salt water
- modern estuaries and fjords
barrier islands/tidal flats
abundant sand areas;ephemeral
- elongate, linear sand bars
- very low topography
- tidal flats form in intertidal zones lacking strong waves
groins
linear structures placed perpendicular to the shore, usually in a group called groin fields
-designed to trap a portion of the sand that moves in the littoral transport system
beach nourishment
minimalizing beach erosion by artificially filling each groin
breakwaters
designed to intercept waves and provide a protected area, or harbor, for boat moorings
jetties
designed to stabilized the channel, prevent or minimize deposition of sediment in the channel and generally protect it from large waves
mid 1970's - Florida & U.S. Army Corps of Engineers
65 million
160,000 m3 of sand
barrier islands
long narrow islands separated from the mainland by a body of water
severity of erosion
presence or absence of a frontal dune system
- orientation of the coastline
- groundwater seepage
- existence of protective structures
storm surge
local rise in sea level that results when hurricane winds push water toward coast
setback
distance from the shoreline to where development such as homes are allowed
mineral resources
elements, compounds, minerals or rocks concentrated in a form that can be extracted to obtain a usuable commodity
mineral resource
concentration of a naturally occurring material in or on the crust of Earth in a form that can now or potentially be extracted at a profit
mineral reserve
portion of the resource that is identified and is currently available to be legally extracted at a profit
types of mineral resources
-elements that are used for metal and technological useage
-chemical engineering
-building material - aggregate
-agriculture
responses to limited availability
not actual exhaustion, is it worth the cost of mainting or mining
-find more sources
-find a substitute
-recycle what has already been obtained
-use less and make more efficient use of what we have
-do without
ore
useful metallic minerals that can be mined at a profit
concentration factor
measure of its concentration necessary for profitable mining
igneous processes
most of world ore deposits
disseminated - scattered through rocks (diamond)
hydrothermal deposits
hot chemically active fluid associated with magma that gives rise to a variety of hot minerals
metamorphic processes
cooling magma interacts with surrounding rock and often causes elevated heat and pressure - metamorphism
contact metamorphism
occurs on a local scale of a few meters to a few hundreds of meters from contact with magma
regional metamorphism
a regional scale of thousands of squre kilometers
sedimentary processes
resulting from physical or chemical processes
evaporite deposits
shallow marine basins or lakes dry up
placer deposits
stream deposits may concentrate a variety of heavy metals - gold
biological processes
accumulations of phosphate-rch fish bones and teeth form some of the richest phosphate deposits in the world
weathering processes
physical, chemical biochemical weathering processes may concentrate some materials to the points they can be extracted
residual deposits
intense weathering of rocks and soils that along with erosional processes, leaves behind the less soluble material with economic value