Final answer:
The salt, sand, and river gravel in Death Valley are most likely due to faulting and the ongoing deposition of materials from mountain erosion, shaped by long-term geological processes. The correct answer is option 2.
Step-by-step explanation:
Considering the provided information, the most likely explanation for the presence of salt, sand, and river gravel in the bottom of Death Valley is that the valley was dropped relative to the mountains by faulting, and rivers have been (and still are) carrying gravel, sand and salts down from the mountains into the valley. Death Valley lies near the boundary of tectonic plates, and the movements of these plates have created conditions for the development of the valley.
Over time, this tectonic activity coupled with wind and water erosion has filled the valley with sediment deposits from the surrounding mountains. These deposits are characterized by allu-vial fans, which are fan-shaped accumulations of sediment that have been transported by moving water from the mountains to the valley floor.
The sediment-filled basin of Death Valley is evidence of a dynamic Earth, where geological processes such as uplift, faulting, and erosion have transformed the landscape over millennia. The valley's extreme aridity and the rain shadow effect also contribute to its unique geographical features. These processes help explain why, despite historical borax mining operations, there is still an abundance of salt and other sediments in the valley.