Exam 20: Coastal Processes and Terrain
Explain the origin, travel, and shoreline actions of a tsunami.
Tsunamis are generated by large underwater (usually) earthquakes. These send out much energy in very long wavelengths in ocean water. When the tsunami approaches the shore, the shallowing of the sea bottom interacts with the waveform sometimes translating it to very tall heights which disastrously crash on the shore.
People interfere with the natural flow of sediment in the coastal system. Explain two ways in which this is done.
For instance: 1) By nourishing beaches by dumping or pumping sand just up current from the beach so the beach becomes wider and protects the shore better or allows better recreation opportunities. 2) Place groins at right angles to the shoreline. This slows the wave action behind them allowing some additional sand to be deposited. Unfortunately, both of these actions are expensive and do not stop the basic problem of more beach erosion than deposition in some areas.
Which of the following is NOT a necessary condition needed for the growth of coral?
Which of the following is most closely associated with fjords?
________ is the longest barrier island along the coast of the United States.
Which of the following is a zone of active deposition of materials by waves?
Which of the following is most important to shoreline erosion?
Which of the following is most closely related to eustatic forces?
________ is the location of the highest tides in the world.
The oceanic tides rise and fall in a rhythmic cycle that takes place roughly once every ________ hours.
Stream outflow is important to coastal landscapes because streams provide ________ to the coastal environment.
Coral is usually localized in areas having relatively cool ocean currents in Tropical Latitudes.
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