The Tapeats Sandstone
Throughout the Grand Canyon area, the Great Unconformity represents at least 200 million years of time where no rocks were deposited. The seas retreated, leaving the basement rocks to erode away. But, 525 million years ago, the seas returned and the geologic record resumed.
The Tapeats Sandstone is the first unit on top of the Great Unconformity. The unit represents a shallow marine deposit, made up of sediments deposited in settings like modern-day sand bars, beaches, and channels.
The unit’s maximum thickness is about 250 meters, but he Tapeats actually isn’t deposited everywhere. In some places, the next unit up is actually deposited directly on top of the Grand Canyon Supergroup rocks. That means at the time of Tapeats deposition, there was substantial topography in the area. There were mesas and hills made up of the strong quartzites of the Supergroup and of the Vishnu Schist basement standing as islands amongst the channels where the sandstone was deposited.
The Tapeats also, as you see here being pointed at by this helpful person from Flickr, contains a variety of larger pebble and cobble-sized clasts. Many of these are made of familiar rocks; components of the Vishnu Schist and the Shunimo Quartzite, strong units deposited previously, are reworked into the Tapeats. The presence of these large clasts also suggests high-energy flows, like debris flows or turbidites, carried the clasts out to sea.
The Tapeats contains a variety of Cambrian-era fossils and trace fossils, including tracks of creatures like trilobites. It also contains the mineral glauconite, an iron-bearing mineral that forms sand-sized grains and also is likely a remnant of life, either of waste or of bodies after death. Various other sedimentary structures, like cross bedding and ripple marks are found as well.
As a strong, hard to erode sandstone, the Tapeats stands out and forms the strong platform around the central gorge in many areas of the Canyon. The Tapeats also marks the beginning of a long period of marine deposition both here and throughout the Western U.S. Although the rock types change slightly, sandstones correlative to the Tapeats can be found throughout the West, again as far north as Montana, all indicating the seas rising and beginning to claim the continent.
-JBB
Image credits (Creative Commons):
https://www.flickr.com/photos/alanenglish/3609981986
https://www.flickr.com/photos/ceedave/4647884862
References: http://3dparks.wr.usgs.gov/coloradoplateau/lexicon/tapeats.htm
http://geology.swau.edu/faculty/tapeats.html
http://hikearizona.com/dexcoder.php?PID=1942
Oh you have got to visit the Tapeats on Google Streetview.
https://www.google.com/maps/views/view/streetview/colorado-river/tapeats-sandstone/jXK-DOmUBE4PPqCz6A7CBw?gl=u&heading=263&pitch=107&fovy=75
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