VishnuPg

VISHNU COMPLEX Proterozoic Era, 1700 Million Years Old, Unknown Thickness Black rugged Inner Gorge with pink and white granite plutons Up to Layers Page Introduction Kaibab Formation Toroweap Formation Coconino Sandstone Hermit Formation Supai Group Redwall Limestone Tonto Group Muav Limestone Bright Angel Shale Tapeats Sandstone Vishnu Complex

The rocks at the bottom of the Canyon are the roots of an island archipelago perhaps similar to the Indonesian Islands of today. Grain by grain, creek by creek, landslide by landslide, the mountainous islands eroded down until at last they were at sea level. These are among the basement rocks of Arizona--the oldest rocks, upon which all other rocks are deposited. Prior to this time, Arizona and much of the Southwest did not exist.

The Vishnu Complex is schist, gneiss, and granite. The Vishnu mountains resulted from plate tectonic collision of ocean floor sediments and basalts with the North American continent. Under great pressure and heat, sedimentary and igneous rocks metamorphosed to form the black and silver mica schists of the Vishnu. White or pink granite plutons, dikes, and sills intruded the schist. After metamorphism, some granites became gneiss, a rock that looks like granite with wavy layering.

Here is a closer view of the Vishnu Schist, from the Clear Creek Trail.

All these stories pretend that people were alive when this formation was laid down. But all are way before people.
Our tribe in Vishnu time
We live on a barren island with large mountains. At sunrise our peaks glow pastel pink. Nothing but us has seen these mountains--eyes will not evolve for another 1,200 million years. Yet we are quite certain, in our tiny time frame, that these islands are everlasting. How could such great things ever disappear?

Up to Layers Page Introduction Kaibab Formation Toroweap Formation Coconino Sandstone Hermit Formation Supai Group Redwall Limestone Tonto Group Muav Limestone Bright Angel Shale Tapeats Sandstone Vishnu Complex