🚙 US-14A Mileage 2.1                 GPS Coordinates N 44.27.364   W 103.51.757    3,917 ft.
Lesson Guide: PRINT
The splendid cliffs that stand up tallÂ
Surround the canyon's rim
Adorned with limestone caves and moreÂ
The seas it formed within
No other geologic formation exemplifies the cliff-faced character of Spearfish Canyon more than the Pahasapa Limestone. In this exciting exploration you'll be introduced to its geologic story and be provided with an opportunity to peer into a roadside cave to examine some of the formation's amazing calcite crystals.Â
This pdf Lesson Guide contains the specific directions for reaching our featured site as well as a detailed explanation of its geologic story. Mileage and coordinates are provided in each document and roadmaps and other learning aids can be found at the Lesson Resources link in the sidebar menu. The document is most useful if taken with you to the lesson site. Exercise extreme caution at the lesson site and along roadways.
Are you ready. . . . Let's Go!                        S. V. Fogarty  &  W. R. Stevens
*Mileage starts at the intersection Colorado Bvd. and US 14A near Spearfish.
The Mississippian Pahasapa, is the thickest formation Spearfish Canyon and hosts most of the Black HIlls caves. Â Age and thickness are approximates.
This view is looking west from the parking turnout at the Lesson Site. The Pahasapa Formation is a buff-colored limestone that was deposited in the ancient Mississippian Sea some 300+ million years ago. See the Stratigraphic Column on the left for the position of the Pahasapa Limestone within the formations exposed here in Spearfish Canyon.
This small cave is located directly alongside the parking turnout. Caves, like this one, often form in layers of limestone and are common occurrences in the Pahasapa Formation.
A cautious scramble up to the cave for a look inside reveals a significant number of calcite crystals. Calcite is a pure form of limestone in crystalline form. Although the crystals resemble gemstones they are relatively soft and worthless. Many a miner, upon discovering calcite, has been fooled into thinking they've struck it rich. Keep your eyes open for other caves throughout Spearfish Canyon.
This photo was taken at arms length inside the small cave. The numerous calcite crystal that encrust the cave walls are a variety known as Dogtooth Spar.
Most of the taller, vertical cliffs you'll see throughout the canyon are exposures of the Pahasapa Formation, a vast layer of limestone that formed from the accumulated remains of hard-shelled invertebrates on the seafloor.Â
Note the dark mineral stains which are so common on the limestone cliff faces throughout the canyon.
Be sure to download our Onsite Geology Lesson PDF posted above for a detailed geologic investigation of this site.Â
Send comments to: partial.melting@gmail.com