Final answer:
The mesas and buttes seen on the map of Cleopatra's Chair in Utah are erosional features, formed through the process of erosion. An example of erosional features can be seen in the Garden of the Gods in Colorado. Depositional features, on the other hand, are formed through the deposition of sediment or other material.
Step-by-step explanation:
The mesas and buttes seen on the map of Cleopatra's Chair in Utah are erosional features. Erosional features are formed through the process of erosion, which involves the wearing away of rock or soil by forces such as wind, water, or ice. In the case of mesas and buttes, they are formed when more resistant layers of rock are left behind after the surrounding softer rock is eroded.
An example of erosional features can be seen in the Garden of the Gods in Colorado, where sedimentary beds have been vertically tilted and faulted into fins by mountain-building forces.
On the other hand, depositional features are formed through the deposition of sediment or other material. An example of a depositional feature is the cross-bedded sandstone on Mars' Mount Sharp, where sediments carried by currents were deposited in lake water.