ARCHVC_160716_055
Existing comment: Permian Period:
During Permian times, the Uncompahgre Uplift rose rapidly and became the source of sediments that completely filled the adjacent Paradox Basin. Streams deposited coarse material closer to the mountains as alluvial fans; finer materials were transported to the south, covering most of what is now southern Utah and northern Arizona.

275 Million Years Ago
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