Wood Canyon Formation | |
---|---|
Stratigraphic range: Ediacaran-Cambrian | |
Type | Geologic formation |
Underlies | Zabriskie Quartzite Formation |
Overlies | Sterling Quartzite Formation |
Thickness | 0–2,500 feet (0–762 m) |
Location | |
Region | Mojave Desert, California and Nevada |
Country | United States |
The Wood Canyon Formation is a geologic formation in the northern Mojave Desert of Inyo County, California and Nye County and Clark County, Nevada. [1] [2]
It can be seen in the Panamint Range and Funeral Mountains adjoining Death Valley, within Death Valley National Park; and in the Spring Mountains in Clark County. [1]
The 570+ million years old formation underlies the Zabriskie Quartzite Formation, and overlies the Stirling Quartzite Formation. [1] [3]
It has members of quartzite, shale, sandstone, and dolomite. [1]
It preserves scattered olenellid trilobite and archaeocyathid fossils in upper part of formation, dating back to the Ediacaran period of the Neoproterozoic Era and Lower Cambrian Period of the Paleozoic Era. [1] [2] [4]
The Dunderberg Shale is a geologic formation in Nevada and Utah.
The Fish Haven Dolomite is an Ordovician period geologic formation in southern Idaho, northeastern Nevada, and northwestern Utah.
The Ely Springs Dolomite is an Ordovician period geologic formation in the Southwestern United States.
The Crystal Peak Dolomite is a geologic formation in the Wah Wah Mountains of western Utah. It preserves fossils dating to the Middle Ordovician period.
The Scott Canyon Formation is a geologic formation in Nevada. It preserves fossils dating back to the Cambrian period.
The Secret Canyon Shale is a geologic formation in Nevada. It preserves fossils dating back to the Cambrian period.
The Emigrant Springs Formation is a geologic formation in Nevada. It preserves fossils dating back to the Cambrian period.
The Harkless Formation is a geologic formation in Nevada and California. It preserves fossils dating back to the Cambrian period.
The Mule Spring Limestone is a geologic formation in the Saline Range of eastern California and Split Mountain and Goldfield Hills of Nevada.
The Campito Formation is a geologic formation in Nevada. It preserves fossils dating back to the Cambrian period.
The Deep Spring Formation is a geologic formation in Nevada. It preserves fossils dating back to the Cambrian period.
The Stirling Quartzite Formation is a geologic formation in the northern Mojave Desert of Inyo County, California and Nye County and Clark County, Nevada.
The Windfall Formation is a geologic formation in northeastern and southern Nevada.
The Saline Valley Formation is a geologic formation in the Mojave Desert, in Inyo County, California.
The Zabriskie Quartzite is a Cambrian Period geologic formation of the northern Mojave Desert, in Inyo County, California and Nye County, Nevada.
The Topanga Canyon Formation is a Miocene epoch geologic formation in the Santa Monica Mountains, Simi Hills, Santa Ana Mountains and San Joaquin Hills, in Los Angeles County, Ventura County, and Orange County, southern California. It is primarily composed of hard sandstone with some inter-bedded siltstone.
The Pomerado Conglomerate Formation is a geologic formation in southwestern San Diego County, California.
The Palm Spring Formation is a Pleistocene Epoch geologic formation in the eastern Colorado Desert of Imperial County and San Diego County County, Southern California.
The Ocotillo Formation is a Pliocene fluvial-alluvial fan geologic formation in the Colorado Desert of Southern California.
The Imperial Formation is the name of two distinct and unrelated geologic formations in North America, of different geologic Eras.