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Geology/Geography/Oceanography/Atmospheric Sciences
Study Set
Earth Science An Introduction
Exam 16: Oceans and Coastlines
Path 4
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Question 1
Essay
What is the definition of salinity?
Question 2
Essay
Global sea level change, called eustatic sea level change, occurs by which three mechanisms?
Question 3
Short Answer
The circular motion of water caused by a passing wave diminishes with depth until it becomes negligible at the _______________.
Question 4
True/False
Because Earth's circumference is greatest at the equator and Earth rotates once each day, a point on the equator rotates much faster than a point near the North Pole.
Question 5
Short Answer
A sheltered body of water separated from the sea by a reef or barrier island is a(n) _______________.
Question 6
Short Answer
Any strip of shoreline washed by waves and tides is called a(n) _______________.
Question 7
True/False
The salinity of the oceans has been relatively constant throughout much of geologic time because salt has been removed from seawater at roughly the same rate at which it has been added.
Question 8
True/False
High and low tides occur at the same time every day.
Question 9
Multiple Choice
A wavelength is the ____.
Question 10
Short Answer
The bending of a wave that occurs when it approaches the shore at an angle and the end of the wave in shallow water slows down is called _______________.
Question 11
Essay
Define a spit and baymouth bar - how are they related?
Question 12
Multiple Choice
During an interval of 24 hours and 53 minutes, most coastlines experience ____ high tide(s) and ____ low tide(s) .
Question 13
Short Answer
What is the depth for the thermocline?
Question 14
Short Answer
Circular or elliptical currents in either water or air are called _______________.
Question 15
Multiple Choice
How does refraction affect wave erosion along irregular coasts?
Question 16
Multiple Choice
____ is the process by which surface water moved by wind drags the layer of ocean water below it, which in turn drags the layer below it, and so forth, with the direction of movement in each layer deflected by the Coriolis effect.