Coastal and Marine Geology
Steven Dutch, Natural and Applied Sciences, University
of Wisconsin - Green Bay
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- Atolls may be described as:
- coral reefs paralleling a nearby coastline
- coral reefs surrounding a lagoon
- a flat-topped submerged seamount
- coral reefs separated from the mainland by a shallow lagoon
- a small reef growth in a lagoon
- Which of the following would you not
associate with turbidity currents?
- deposits of graded beds
- density current
- excavation of submarine canyons
- formation of seamounts
- sediment transport
- The scientist who correctly proposed the theory of atoll formation was:
- Kelvin
- Wegener
- Hutton
- Darwin
- none of these
- Which of the following is associated with mid-ocean ridges?
- rift zones
- mountainous topography
- greater heat flow than occurs in other parts of the ocean
- volcanic structures
- all of the above
- When waves reach shallow water, they are often bent and tend to become parallel to the shore. This process is termed:
- oscillation
- reflection
- refraction
- abrasion
- translation
- The movement of water parallel to the shore within the surf zone is termed:
- tidal current
- longshore current
- salinity current
- rip current
- beach drift
- Which one of the following is a landform created by wave erosion (as opposed to deposition)?
- spit
- sea arch
- estuary
- breakwater
- tombolo
- The movement of sand parallel to the shore:
- is created by waves approaching at an oblique angle
- may create spits
- is achieved by longshore currents
- is an important reason for the construction of groins
- all of the above
- When a breakwater is built beyond the surf zone offshore from a sandy beach:
- the area between the shore and the breakwater will probably be deepened by the intensified longshore current
- the area between the shore and the breakwater will probably begin filling in with sand
- the longshore current will not be affected
- none of the above
- The crests of mid-oceanic ridges:
- are heavily mantled with sediment
- lie at depths exceeding 6 kilometers
- are geologically young features
- have never been observed by man
- One result of wave refraction is that:
- wave energy is concentrated on headlands projecting into the water
- wave energy is concentrated in the recessed areas between headlands
- wave energy is largely dissipated before the waves reach the shore
- headlands are enlarged because sediment is deposited on their seaward side
- The zigzag movement of sand grains along a beach:
- is caused by obliquely breaking waves
- is called beach drift
- is very unusual and seldom occurs
- both a and b
- both b and c
- Within the continental margin, deep, steep-sided valleys known as ______ are found
- continental shelves
- submarine canyons
- continental slopes
- ocean basins
- continental rises
- The presence of which one of the following would indicate that the land had been uplifted or that sea level had fallen?
- an estuary
- a sea stack
- an elevated marine terrace
- a tombolo
- Chesapeake Bay and Delaware Bay:
- are associated with a submergent coast
- are former river valleys that were followed by a rise in sea level
- are excellent examples of large estuaries
- all of the above
- In the geologic past:
- the number of 24-hour days per year was greater than at present
- the earth rotated more rapidly than at present
- the number of hours in a day was greater than at present
- the earth was farther from the Sun
- all the above
- The gently sloping, shallowly-submerged surface extending from the shoreline toward the deep ocean is termed:
- continental shelf
- submarine canyon
- continental slope
- ocean basin
- continental rise
- Directly seaward of the continental shelf is a more steeply sloping region known as:
- continental shelf
- submarine canyon
- continental slope
- ocean basin
- continental rise
- Graded bedding is characterized by:
- an increase in sediment size from bottom to top
- a decrease in sediment size from bottom to top
- an unsorted mixture of many different sediment sizes
- sorting due to gentle wave action in shallow water
- Which of the following is
not
true of deep ocean trenches?
- they are long and narrow depressions
- they are sites where plates plunge back into the mantle
- they are geologically very stable
- they may act as sediment traps
- Which factors can make sea water more saline?
- freezing of sea ice
- evaporation
- both of the above
- none of the above
- Almost half of the sediment reaching the oceans comes from this continent:
- Asia
- South America
- Africa
- North America
- Australia
- Freak high waves sometimes encountered by ships at sea seem to be due to:
- Undersea volcanic eruptions
- Undersea landslides
- Tornado-like weather disturbances at sea
- Superposition and addition of waves of different frequencies
- Unusual tidal conditions
- A flat-topped submarine mountain
- guyot
- mesa
- cuesta
- horst
- A baymouth bar forms
- when a glacier builds a moraine across a bay
- when longshore drift causes a spit to be built across a
bay
- when a landslide dams a bay
- all of the above
- none of the above
- When waves break exactly parallel to a beach:
- the beach wears away
- the water returns to the sea in evenly-spaced flows call
rips
- the waves move sand along the shore
- deposition is greatest
- The highest known waves have occurred:
- as the result of earthquakes
- during hurricanes
- after volcanic eruptions
- when landslides dumped large amounts of material into small bodies of water
- An example of a secondary shoreline:
- the shore of an estuary
- the shore of a fiord
- a fault scarp which is partly submerged
- a barrier island
- When a wave changes direction in shallow water, the change in path is called:
- absorption
- refraction
- reflection
- erosion
- As an oceanic island sinks or is eroded, the fringing reef may be left behind as a circular ring called a(n):
- crater
- caldera
- atoll
- esker
- An isolated rock left behind as an island as a coast erodes:
- barrier reef
- stack
- dike
- atoll
- Beaches:
- tend to remain constant year-round
- tend to be eroded during stormy weather and deposited in calm weather
- tend to be deposited in stormy weather and eroded in calm weather.
- When are waves affected by the seafloor, that is, when do waves begin to "feel bottom"?
- when water depth is equal to one-half the wave length
- when water depth is equal to the wave length
- when water depth is twice as great as the wave length
- when water depth is three times a great as the wave length
- none of the above
- One of the following is not a requirement for coral reef growth:
- warm water
- shallow water
- abundant sunlight
- abundant amounts of suspended sediment
- A sea cliff
- retreats faster with time because the waves cut into softer rock
- retreats uniformly with time
- retreats more slowly because the waves cut into harder rock
- retreats more slowly because the wave-cut platform dissipates wave energy
- The salt in sea water plays little or no role in coastal erosion
- True
- False
- An isolated remnant of wave erosion is a:
- spit
- groin
- jetty
- tombolo
- sea stack
- A sand ridge connecting an island to the mainland or to another island is a:
- jetty
- tombolo
- sea stack
- none of the above
- breakwater
- A circular reef enclosing a lagoon is a(n):
- barrier reef
- guyot
- seamount
- atoll
- aseismic
- A flat, benchlike surface cut in rock by wave action is a:
- sea stack
- spit
- jetty
- none of the above
- tombolo
- Chesapeake Bay is an excellent example of a(n):
- coastal barrier
- fiord
- estuary
- primary coastline
- emergent coastline
- Which of these can be considered a fiord (even though the topography isn't
dramatic)?
- San Francisco Bay
- Chesapeake Bay
- Galveston Bay
- Puget Sound
- Biscayne Bay
- What did the city of Galveston do to try to prevent a repeat of the disaster
of 1900?
- Blocked the harbor
- Moved the city
- Built a seawall and raised parts of the city
- Banned shoreline construction
- Which is not a factor in shoreline subsidence in Louisiana?
- Dams capturing sediment upstream
- Delta buildup far offshore
- Compaction of sediment over time
- Prevention of course change by the Mississippi
- Wind erosion
- Which factor prevented Hurricane Katrina from being a much worse disaster?
- There was an unusually low tide
- The hurricane was not very strong
- Most levee failures happened after the peak of the storm
- Federal and local governments acted quickly
- If we allow the Mississippi River to change course:
- Wetlands along the Atchafalaya will be silted in
- Sediment will be trapped by the new flood plain
- Sediment will not be deposited under New Orleans
- All of the above
- Deltas on coasts with strong wave action:
- Build up long peninsulas into the sea
- Have smoothly curving fronts
- Consist of long parallel islands
- Are smeared out along the coast
- Deltas on coasts dominated by strong tidal action:
- Build up long peninsulas into the sea
- Have smoothly curving fronts
- Consist of long parallel islands
- Are smeared out along the coast
- Deltas where deposition dominates other processes:
- Build up long peninsulas into the sea
- Have smoothly curving fronts
- Consist of long parallel islands
- Are smeared out along the coast
- Deltas where deposition and wave action are roughly equal:
- Build up long peninsulas into the sea
- Have smoothly curving fronts
- Consist of long parallel islands
- Are smeared out along the coast
- Why do seawalls have a curving face?
- To take advantage of the Coriolis Effect
- To allow waves to dissipate their energy upward
- To save on construction material
- To keep them from tipping over
- How can sea floor spreading affect sea level?
- Fast-spreading ridges take up more room
- Slow-spreading ridges take up more room
- Rapid plate motions mean deeper ocean trenches
- Fast plate motions push the continents apart
- How are age and depth of sea floor related?
- Older sea floor is deeper
- Younger sea floor is deeper
- There is no relationship
- Crust older than 100 million years forms the floors of the trenches
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Created August 4, 1999; Last Update
07 November 2006
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