Named by Noble (1914) Primary Sandstone, Conglomerate | Named for Tapeats Creek Thickness 70 m | |
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Region northern Arizona (Grand Canyon), central Arizona, southeast California, southern Nevada, and southeast Utah Country United States of America |
Features of the tapeats sandstone a sedimentary rock
The Cambrian Tapeats Sandstone is the lower geologic unit, about 230 feet (70 m) thick, at its maximum, of the 3-member Tonto Group.
Contents
- Features of the tapeats sandstone a sedimentary rock
- The formation of crossbedding in the tapeats sandstone
- Geologic sequence
- Popular Publications
- Gallery Tapeats Sandstone
- GalleryGreat Unconformity and angular unconformity
- References

The Tapeats Sandstone is the highly erosion-resistant unit laid upon the Vishnu Basement Rocks in the central, parts of east, and parts of west Grand Canyon, Arizona. The unit comprises the 'base horizontal unit' of the platform around Granite Gorge (Inner Gorge) on the Colorado River, and because of its hardness, creates the Tonto Platform upon which the two slope-forming, highly erodable units, the Muav Limestone, and Bright Angel Shale lie.

The Tapeats Sandstone and the Tonto Platform follow the Colorado River, and surrounding tributary canyons, creeks, watercourses, or washes, in a dendritic fashion, much like the branches of a tree.

The Tapeats unit is the bottom member of the Tonto Group, a typical marine transgression series of sandstone-(conglomerate)-shale-limestone, all part of a paleo sea, initially adjacent to land, the source of the Tapeats rocks-(conglomerates) and sand; (a regressing sequence has the reverse order). The Tapeats Sea at the early Devonian ceased to deposit more Muav Limestone, and a period of erosion ensued, a deposition unconformity.

The Tapeats Sandstone was laid upon the Vishnu Basement Rocks, after an unconformity of erosion, the Great Unconformity, of 1,000 million years (1.0 billion). Besides the erosion unconformity, the Unkar Group of the basement rocks are also at an angular unconformity, being an 8-member sequence tilted at 45 degrees.

The horizontal Tonto Platform has hiking trails that cross it from the South Rim to North Rim, Grand Canyon for instance. The extensive Tonto Trail lies on parts of the Tapeats Sandstone, and the platform on the south side of Granite Gorge.

The formation of crossbedding in the tapeats sandstone
Geologic sequence
The units of the Tonto Group:
Popular Publications

Gallery--Tapeats Sandstone
Examples of the deposition unconformity of time (550-800 million yrs), the Great Unconformity. The Tapeats approximately 200 ft thick.
Gallery—Great Unconformity and angular unconformity
Examples of the angular unconformity below the Tapeats Sandstone, (approx. 15 degrees).
