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Formation · Jurassic · sandstone

Kayenta Formation

The dark-red, ledgy river sandstone of the Glen Canyon Group — the Early Jurassic stair-step that caps and protects the Wingate cliff, printed with dinosaur tracks.

Also known as: Kayenta

Jurassic — the golden age of dinosaurs

The world back then

Early Jurassic, about 190 million years ago. A break in the desert: shifting rivers wander a dry-to-semiarid plain, carrying red and lavender silt, leaving behind ledgy channel sands and dinosaur tracks. Wetter than the dunes above and below it, but not by much — a stripe of rivers in the middle of a drought. Braided streams under a hot, big sky.

Now it's the stair-stepping ledges between the Wingate cliff and the Navajo domes, and the current carries you the whole way and asks nothing back. That old stream could barely hold its water; yours does all the work while you loaf. A comfortable float past a fossil of a drier, harder world — the trade of the century.

Recognize it in the field

Typical color
red, maroon, brown, and lavender
Weathers as
Ledge- and bench-forming — thin-bedded, stair-stepping slabs that stand back between the Wingate cliff below and the Navajo slickrock above, often armoring the Wingate.
Grain
fine-grained, locally coarser and well-rounded in channels

Look for

  • dark-red to maroon/lavender ledgy band between two massive cliff units
  • lenticular fluvial channel sandstones interbedded with siltstone
  • abundant dinosaur trackways
  • interfingers with the overlying Navajo Sandstone near its top

How this rock was made

Braided-to-meandering river corridors crossing a dry Early Jurassic landscape, representing wetter conditions during the advance of the Navajo dune sea.

The setting: river (fluvial) — shifting streams of fluctuating volume on an arid-to-semiarid plain

About 330–390 ft (100–120 m) typical, to ~400 ft in Glen Canyon (Wikipedia). A New Mexico Geological Society guidebook cites a wider 140–350 ft range that was not independently verified here.

In the rock record

Part of the Glen Canyon Group.

↑ Younger — rests above

Navajo Sandstoneinterlocks like fingers (interfingering) · southwestern Utah (Cedar City / Tenney Canyon tongues intertongue with the Navajo)
Navajo Sandstoneblends into it (gradational) · Glen Canyon area and generally
Kayenta Formation you are here
Wingate Sandstoneno gap (conformable) · most of the Colorado Plateau
Moenave Formationsouthwestern Utah

↓ Older — sits beneath

See the full regional rock columns →

Where to see it

Regions: Colorado Plateau

Float past it: Westwater Canyon · Meander Canyon · Stillwater Canyon