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Historical and Stratigraphic Analysis of the Grand Canyon By: Jake Halfhill

Historical and Stratigraphic Analysis of the Grand Canyon By: Jake Halfhill. Vishnu Schist. Tapeats Sandstone. Supai Group. Hermit Shale. Coconino, Toroweap, and Kaibab Units. In Conclusion: the Grand Canyon began to form 1.7 to 2 billion years ago

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Historical and Stratigraphic Analysis of the Grand Canyon By: Jake Halfhill

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  1. Historical and Stratigraphic Analysis of the Grand CanyonBy: Jake Halfhill

  2. Vishnu Schist

  3. Tapeats Sandstone

  4. Supai Group

  5. Hermit Shale

  6. Coconino, Toroweap, and Kaibab Units

  7. In Conclusion: • the Grand Canyon began to form 1.7 to 2 billion years ago • processes such as erosion and volcanism are causes of the topography of the Grand Canyon • the Colorado River has shaped the Grand Canyon • the stratigraphic sequence:

  8. There is then an unconformity of about 450 million years in which the rocks are missing. There is then another unconformity of about 250 million years in which new rock layers were probably laid down but were completely eroded away. The Tapeats Sandstone was then deposited around 550 million years ago along long vanished coastline. The Bright Angel Shale was deposited around 540 million years ago and indicates that the ocean was again advancing. The Muav Limestone was deposited around 530 million years ago at the bottom of a shallow sea. The thick layer of Redwall Limestone which began to deposited around 330 million years ago indicates that the land was submerged for a great deal of time.

  9. The Supai Group which rests atop the Redwall is dated at 300 million years ago and indicates that it was formed in an above water and coastal environment. The Hermit Shale which was deposited around 280 million years ago contains many plant fossils which indicate that it was also above water. The Coconino Sandstone represents the remains of a vast sea of sand dunes which was blown down from the north around 270 million years ago. The layers found within Toroweap Formation contains both sandstone and limestone, indicating that it was sometimes coastal and sometimes submerged. These layers date to around 260 million years. The Kaibab Limestone contains many marine fossils which indicate that it originated at the bottom of the sea. This layer is around 250 million years old.

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