Coastal Systems & Wind Processes Flashcards

1
Q

How do coastal environments place in the geologic time scale?

A

relatively young

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2
Q

What interactions form coastal environments (5)?

A
  • land
  • ocean
  • atmosphere
  • sun
  • moon
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3
Q

What are the three zones of a coastal environment?

A
  • littoral zone: extends into the water until wave action does not affect sediment on the seafloor
  • shoreline: where the sea and land meet
  • coast: extends until the first major landform change
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4
Q

What is the mean sea level and how does it vary (4)?

A
  • based on average tidal levels recorded hourly over many years
  • varies around the world based on ocean currents, tides, temp. of air and ocean, air pressure, prevailing winds, gravity, and oceanic volume
  • sea levels change through climate change, tectonic activity, and glaciation
  • over the past 100 years, sea level has been increasing
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5
Q

What are tides (3)?

A
  • twice-daily osceillations in sea level
  • locations around the world experience different tidal fluctuation
  • exist in oceans and very large lakes
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6
Q

What causes tides (4)?

A
  • tidal bulge: water on Earth is pulled outward by the Sun and Moon
  • shift from high tide to low tide caused by Earth’s rotation through the tidal bulge
  • spring tide: higher tides occur when Earth and Moon align with the Sun and pull in the same direction
  • neap tide: lower tides occur when Earth and Moon are not aligned with the Sun, weakening gravitational force
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7
Q

What is tidal range?

A

the difference between consecutive high and low tides

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8
Q

What are waves and how do they vary in scale (2)?

A
  • form as a result of friction between wind and ocean surface
  • can be large and powerful or small and weak
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9
Q

What are swells (3)?

A
  • regular patterns of smooth, rounded waves that exist in the open ocean
  • swells compress and become top-heavy as they move closer to the coast
  • breaker waves form when the swell becomes too top-heavy and collapses over itself
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10
Q

What are tsunamis (4)?

A
  • form in the aftermath of an earthquake, landslide, or volcanic eruption below the ocean’s surface
  • movement displaces a huge amount of water, creating large waves
  • travel at a very fast rate
  • have a large wavelength but a low height
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11
Q

What are erosional coastlines (5)?

A
  • more erosion occurring
  • aka “emergent coastlines”
  • found along Pacific coast of U.S.
  • more common in areas with tectonic activity
  • waves act to erode away material and straighten coastline
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12
Q

What are seven features of erosional coastlines?

A
  • headlands: protruding landforms of erosion-resistant rock
  • refracted wave fronts: waves hit furthest point of headland and bend to attack the sides of that point, resulting in…
  • sea caves
  • sea arches
  • sea stacks
  • sea cliffs
  • wave-cut platforms
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13
Q

What are depositional coastlines (3)?

A
  • more deposition occurring
  • aka “submergent coastlines”
  • found along Gulf Coast and Atlantic Coast of U.S.
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14
Q

What are three features of depositional coastlines?

A
  • barrier spit: sandbar which extends parallel along shoreline in same direction as longshore drift; does not extend entirely along bay
  • lagoon: small body of water formed when the bay has been completely cut off by the barrier spit
  • tombolo: barrier spit which extends perpendicular to shoreline, connecting an off-shore island
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15
Q

What determines the material which makes up beaches?

A

the type of rock which makes up the coastline

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16
Q

What are barrier islands (5)?

A
  • long, narrow island which runs parallel to shoreline
  • absorb energy associated with wave activity
  • most common along depositional coastlines
  • popular for beach resorts (a bad idea)
  • creates swampy backbay area
17
Q

What is eolian erosion (4)?

A
  • wind erosion
  • less landforms associated
  • more common in arid environments
  • deflation vs abrasion
18
Q

What is deflation (2)?

A
  • removal and lifting of individual, loose particles

- forms desert pavement: larger particles cemented in place

19
Q

What are two explanations for desert pavement?

A
  • deflation hypothesis: wind removes fine particles, leaving larger materials to consolidate into pavement
  • sediment accumulation hypothesis: wind delivers fine particles that settle and wash downward as larger gravels migrate upward during cycles of swelling and shrinking, resulting in pavement
20
Q

What is abrasion (3)?

A
  • grinding of rock surfaces by tiny particles
  • yardang: elongated ridges created via abrasion
  • ventifact: irregular rock shape formed by irregular wind patterns (can also form via glacial erosion)
21
Q

What are the three types of eolian transportation?

A
  • suspension
  • saltation
  • surface creep
22
Q

What is suspension?

A

transportation of fine, wind-blown particles

23
Q

What is saltation (2)?

A
  • transportation of particles heavy enough to be moved via skipping motion along the surface
  • the most common form of eolian transportation
24
Q

What is surface creep?

A

transportation of larger particles which creep/roll along the surface

25
Q

What are the two formations associated with eolian deposition?

A
  • loess

- sand dune

26
Q

What is a loess (3)?

A
  • very fine, wind-blown glacial silt
  • common in Alaska, Great Plains, and Mississippi River Valley in U.S.
  • create fertile soil
27
Q

What is a sand dune (3)?

A
  • only a small portion of deserts consist of sand dunes
  • constantly moving hill of sand
  • migrate based on prevailing wind direction
28
Q

What are the three characteristics of a sand dune?

A
  • windward slope (gradual)
  • leeward slope (steep)
  • slipface: leeward slope of sand dune; constantly moving downward
29
Q

What are the five classes of sand dunes?

A
  • crescentic: curved shape with horns pointed downwind; found in areas with constant winds and little directional variability where limited sand is available
  • linear: straight, slightly sinuous, ridge-shaped dune aligned parallel with the wind direction
  • star: pyramidal-shaped structure with three or more sinuous, radiating arms extending outward from a central peak; results from effective winds shifting in all directions
  • parabolic: crescent-shaped dune with opening end facing upwind; U-shaped “blowout” and arms anchored by vegetation, which stabilizes dune form
  • dome: circular or elliptical dune with no slipface; sometimes modified into barchanoid forms, and sometimes stabilized by vegetation