Answer:
This indicates a proximodistal pattern of growth
Explanation:
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Answer:
Stretched
Explanation:
Nevada and the western side of Utah are usually characterized by the formation of high mountain ranges that are oriented in the north-south direction. This is because of the effect of the transform plate boundary that is located towards the western boundary of the United States, which is commonly known as the San Andreas fault. The areas near to this region are being highly stretched apart because of the weakening of the crust due to the presence of a series of down-dropped fault blocks.
The Basin and the Range province areas in Utah, Nevada, Orogen are highly composed of numerous fault block mountainous ranges that are mostly bounded by the high angle-normal faults.
Thus, the crust here is actually stretched.
