Today, Schnebly Hill Formation is a topic that captures the attention of millions of people around the world. Whether due to its historical relevance, its impact on current society or its importance in everyday life, Schnebly Hill Formation has managed to occupy a prominent place in different areas of life. Since its appearance, Schnebly Hill Formation has aroused the interest of researchers, experts and the curious, who have dedicated time and effort to understanding and analyzing its implications. In this article, we will thoroughly explore Schnebly Hill Formation and its meaning in today's world, offering a global and detailed vision of this topic that has managed to transcend borders and cultures.
Schnebly Hill Formation | |
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Stratigraphic range: | |
Thickness | 800 feet (240 m) to 1,000 feet (300 m) |
Lithology | |
Primary | Sandstone |
Location | |
Region | Colorado Plateau |
Country | United States |
Type section | |
Named for | Sedona Schnebly |
Location | Arizona |
Thickness at type section | 800 feet (240 m) to 1,000 feet (300 m) |
The Schnebly Hill Formation is a section of red bed deposits found at the Colorado Plateau, near Sedona, Arizona. It is a dark red sandstone, from 800 feet (240 m) to 1,000 feet (300 m) thick. It lies between Coconino Sandstone and the older Hermit Formation. It is near the Supai Group.
The source of the name "Schnebly" is Sedona Schnebly, after whom the city of Sedona, Arizona, was named.
The formation traces to the Permian Age.
The formation is the most prominent layer of the red rocks of the Sedona area due the presence of hematite – iron-oxide, frankly, rust – giving the sandstone a red color. The Schnebly Hill Sandstone formation comprises three sections:
early Permian (Leonardian)