Approximately 600 million years ago in the Precambrian, the area was covered by a sea. As waters subsided and land masses began to appear 60 to 30 million years ago (between the Paleocene and Oligocene epochs), drainages such as Spearfish Canyon formed as softer rock was eroded away. Today, a National Scenic Byway, U.S. Highway 14A, winds through the canyon. This area is truly a crossroads, and trees and plants from Rocky Mountains, eastern woodlands, northern forests, and the Great Plains areas can be found here.
Flora and fauna
Of the 1,585 plant species found in South Dakota, 1,260 species are in the Black Hills, many of which can be found in Spearfish Canyon. Ponderosa pines are the most prominent vegetation in the Black Hills. As for bird species, turkeys, bluejays, woodpeckers, cliff swallows, chickadees, and golden or bald eagles are seen in the area. The canyon supports a cross-section of four-footed animal life. White-tail and mule deer can be found throughout the drive. Porcupines, raccoons, squirrels, and chipmunks might be spotted as well as a bobcat or a yellow-bellied marmot.
Geology
It is often studied by geologists due to the extreme old age of the Precambrian rocks exposed by the creek bed. The canyon's high walls are of three dominant rock types. The Cambrian to OrdovicianDeadwood Shale at the bottom lies on an unconformity above Precambrian rock and can be identified by its brown color. It is multi-layered in appearance and ranges from 10 feet (3.0 m) to 400 feet (120 m) thick. Englewood Limestone in the middle is pink to red colored and is 30 feet (9.1 m) to 60 feet (18 m) thick. The PaleogenePaha Sapa Limestone, the top layer, is the thickest (300 feet (91 m) to 600 feet (180 m)) and is buff-colored and weathered gray in appearance. Caves and fossils are frequently found in the Paha Sapa Limestone.
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