Esplanade Sandstone

The Lower Permian Esplanade Sandstone is a cliff-forming, resistant sandstone, dark red, geologic unit found in the Grand Canyon. The rock unit forms a resistant shelf in the west Grand Canyon, south side of the Colorado River, at the east of the Toroweap Fault, down-dropped to west, southeast of Toroweap Overlook, and west of Havasupai. The red, sandstone shelf, The Esplanade is about 20-mi long. At Toroweap Overlook region, Toroweap Valley with Vulcan's Throne, Uinkaret volcanic field, the resistant Esplanade Sandstone is described in access routes exploring the Toroweap Lake area.
The Esplanade Route–, of the east Grand Canyon is also named for the Esplanade Sandstone. The coeval sandstone geologic unit from eastern Utah is the Cedar Mesa Sandstone.

Isis Temple and Hermosa Group, Utah

In Grand Canyon, Isis Temple landform, north of Grand Canyon Village, contains a representative example of the Supai Group 'redbeds', and slope-former and cliff-former units that support the landform. The sequence of units below the white Coconino Sandstone prominence of Isis Temple are:

G – Coconino Sandstone–white prominence
F – Hermit Formation – grayish slopes
E – Supai Group –
* 4 – Esplanade Sandstone – cliff-former
* 3 – Wescogame Formation
* 2 – Manakacha Formation
* 1 – Watahomigi Formation
D – Redwall Limestone – large red cliff
C – Muav Limestone – grayish-cliff
B – – Bright Angel Shale
A – upon – Shinumo Quartzite

The Esplanade Sandstone is only found in Arizona, with the Hermosa Group being the equivalent coeval 'redbed' type geologic sequence found north and northeasterly in Utah –.

Geologic sequence

The Late Pennsylvanian–Early Permian geologic sequence of the Supai Group common in the Grand Canyon: The Pennsylvanian is the Late Carboniferous.

Supai Group
* Esplanade Sandstone
* Wescogame Formation
* Manakacha Formation
* Watahomigi Formation

The Supai Group members were created from marine sequences of marine transgression, and regression, thus the alternating sandstone, siltstones, conglomerate subsections ; the subsections are not always a continuous transition into the above section, mostly due to ocean levels, falling, or rising, glaciation, or regional subsidence– or uplift of land. Today's Wasatch Front is the approximate lineage, NNE to SSW of the western coast region of North America from where the oceans transgressed. The ancient Antler Mountains–, of ancient Nevada supplied material, from the west, off the 'ancestral' West Coast. The continent supplied material from the east, both directions supplying the offshore basin, the Cordilleran Basin which became part of the Basin and Range Province, in later epochs. Three other basins were involved in this history: southwest of the Ancestral Rocky Mountains was the Paradox Basin–, northeast was the Central Colorado Basin–; the Oquirrh Basin was north-northwest, at present day northwest Utah.

Supai Group and Hermosa Group, coeval units

The approximate coeval Supai and Hermosa Groups, Arizona, Utah, and northwest Colorado:
Because marine transgressions cover distances, over time, the coeval units are separated by distance, and type of deposition material; the local subsidence, or uplift, as well as glaciation, and sea level changes, can cause variations in the deposition sequences of transgression–regressions. The ocean was to the west of the proto-North American continent, but also northwest, or southwest.