Spires of Cedar Mesa Sandstone in Elephant Canyon (Needles District)
Deposited
Permian Period (245 to 286 million years ago)
Depositional Environment
Near-shore sand dunes interfingering with periodic floods that brought dark red sediments from the ancient Uncompahgre Mountains.
Appearance
Red and white layered sandstones forming cliffs, domes and spires.
Examples
Spires and canyons in the Needles and Maze Districts of Canyonlands.
Interactive Geologic Atlas Flash animations manage to simplify the story of Canyonlands. more...
Did You Know?
The Utah juniper, one of the most common trees in the southwest, has the ability to self-prune. During droughts, these trees will cut off fluids from one or more branches so that the rest of the tree can survive.
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