The Vishnu Schist was exposed when sedimentary layers above it were eroded
Vishnu Schist
The Vishnu Complex or Vishnu Metamorphic Complex is the basement metamorphic Paleoproterozoic schist and gneiss rock unit of the Grand Canyon of Arizona. It consists of two major units of rock, the dark-colored, fine-grained Vishnu Schist, metamorphosed Paleoproterozoic sedimentary rocks, that have been intruded by the second unit, a pink-colored gneiss that began as the Zoroaster Plutonic Complex. These complexes were named by CD Walcott in 1883. Scientists often use deity names to describe things. It is not intended to offend anyone.
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The Vishnu Schist rock at the bottom of the Grand Canyon.
Schist comes from shale. It is laminated , flaky, and found in parallel layers. The minerals in this rocks that have crystallized from the parent rock are visible.
Texture and metamorphic grade. Schist has visible crystals, while phyllite has crystals too small to be seen with the eye or barely seen. This is a result of schist having higher grade metamorphism.
The "newest" rocks that can be seen at the Grand Canyon are from the Paleozoic Era.
The Vishnu schist basement rock layer at the bottom of the Grand Canyon is roughly 1.8 billion years old.
Probably Kaibab limestone, Coconino sandstone, Hermit shale, Redwall limestone, Muav limestone, Vishnu Schist, and other layers.
No. Mica schist is a schist with a preponderance of mica minerals. There are also chlorite schists, talc schist, and so on.
No. Shale is the most common sedimentary rock exposed on the surface of Earth.
schist