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Question
Extensive landscapes formed by the dissolution of limestone and other carbonate rock and characterized by pitted, bumpy surface topography, poor surface drainage, and well developed solutions channels are known asA) plains.
B) basins.
C) karst topography.
D) high tablelands.
Answer
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Related questions
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The basis for defining the length of a day is the fact that
A) Earth rotates east to west.
B) Earth moves through 365.25 days a year in its orbit about the Sun.
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D) Earth does not rotate; rather, it revolves.
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Predator/prey relationships are an example of
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Living systems are considered
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The key idea behind the scientific method is
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A) speculation
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The main methodology governing geographic inquiry
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"Geography" literally means
A) place memorization.
B) the study of rocks.
C) map making.
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Which map projection is best at reducing distortion?
A) All map projections distort.
B) Mercator projection.
C) Robinson projection.
D) Albers equal-area projection.
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A line of tangency (also called a standard line) is a line
A) that always corresponds to a great circle.
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The larger the scale of a map, the ________ the area covered by the map and the ________ detail it provides.
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B) larger; less
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Which type of map scale would be appropriate to use if the map were to be enlarged by photocopying?
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A) representative fraction.
B) graphic scale.
C) written scale.
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B) cone.
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A scale of 1 inch = 8 miles is an example of a
A) representative fraction.
B) graphic scale.
C) written scale.
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Earth's equator is an example of
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B) a great circle.
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D) a line of equal longitude.
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If City A is located 35 west of City B, the time at City A is ________ that at City B.
A) earlier than
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Scientific theories are capable of generating testing predictions.
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Pure science frequently involves the making of value judgments about the moral or political correctness of a fact, idea, or theory.
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Geography is a discipline primarily concerned with place names.
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The occurrence of contact metamorphism would be direct evidence for
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B) the local intrusion of magma.
C) regional plate collision.
D) lithification of clastics.