Geology of the Grand
Canyon
The history that can be
read through these layers is astounding but also complex given the age of the
rock layers, which date over one billion years. Briefly, the uppermost layers
of the Grand Canyon are Paleozoic rocks including the Kaibab formation, the
Hermit formation, Supai group and Redwall limestone, all easily seen from
canyon views. These tend to be the red rocks we think of when we think of canyonlands.
This is also the layer in which fossils are found. The next Proterozoic layer
is the Grand Canyon supergroup which is very difficult to see. Most of these
sedimentary rocks with some igneous have been worn away. But the Chuar group
and the Unkar group are viewable from the rim. The bottom and oldest Proterozoic
layer are the Vishnu basement rocks a mix of Schists and granite. The canyon
itself was uplifted and thus ripe for the continual wearing of the Colorado
River.
This USGS website is a great resource. The Map below is courtesy of USGS.