<span>The Wasatch Fault sits in Utah and slips in a mainly vertical direction. It has mountains that rise relative to the floor of the valley. It is referred to as a normal fault. The Wasatch Mountains were slowly lifted up and tilted slightly east due to the fault moving. On average throughout history it has lifted roughly 1 millimeter per year thought there are signs that a rapid slip has occurred during the past few thousand years.</span>
Answer: Option (C)
Explanation:
A tombolo is a depositional feature that is formed when the longshore current, moving parallel to the sea shore, carries the sand long with them and deposits along the shoreline. After this, subsequent backwash carries the sands along with it and deposits at a right angle to the sea shore. This deposited sands and other materials connects the shore to an island and this features are known as tombolo.
Thus, the correct answer is option (C).