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Sundance Sea
From Wikipedia, the free encyclopedia
The Sundance Sea was an epeiric sea which existed in North America during the mid to late Jurassic Period of the Mesozoic Era.[1] It was an arm of what is now the Arctic Ocean, and extended through what is now western Canada into the central western United States. The sea receded when highlands to the west began to rise.
The Sundance Sea did not occur at a single time; geological evidence suggests that the Sea was actually a series of five successive marine transgressions--each separated by an erosional hiatus--which advanced and receded from the middle Jurassic onward.[1] The terrestrial sediments of the Morrison Formation--eroded from rising highlands to the west--were deposited on top of the marine Sundance sediments as the sea regressed for the last time late in the Jurassic.[2][3]
The sedimentary rocks which formed in and around the Sundance Sea are often rich in fossils.
- ^ a b Fanning, Suzette. Stratigraphy of the Sundance Formation. Retrieved on February 6, 2007.
- ^ Kuehn, Steve. Geology of the Mesozoic Era: 245 to 66 million years ago (PDF). Department of Physics, Physical Sciences, and Geology at California State University, Stanislaus. Retrieved on February 6, 2007.
- ^ Mesozoic Stratigraphy in the Thermopolis Area. Big Horn Basin Foundation. Retrieved on February 6, 2007.
