Gravitation Greetings: The Kissing Rocks
 🚙 US-14A Mileage9.3                                                  GPS Coordinates N 44.23.577  W 103.54.715    4,796 ft.
Lesson Guide: PRINT
Field Exploration
Was that thunder I just heard or the sound of two giant boulders crashing into a riverbed? In this Spearfish Canyon exploration we take a look at the remnants of a rockfall event that took place in 1994. The sheer size of the boulders will amaze and the cause of the event will be investigated. Stay alert as you "Watch for Fallen Rock."
This pdf document contains the specific directions for reaching our featured Lesson Site as well as a detailed explanation of its geologic story. Mileage to the site as well as its specific coordinates are listed on the header above and also in the lesson document. Roadmaps and other learning aids can be found at the Lesson Resources link in the menu and are helpful to have handy in the field. Please print this document and take it with you or read it thoroughly before departing. 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 Kissing Rocks
Limestone boulders from the 1994 rockfall event came to rest alongside the highway in the Spearfish Creek channel.Â
The Kissing Rocks Viewed From Above
Drone photo taken at an altitude of ~175 ft. AGL. Compare boulders to highway for scale.
The Kissing Rocks Underpass
Spearfish Creek flows between the two large boulders creating a natural eyelet.
Note the lighter colored rock exposure in the upper cliff of Pahasapa Limestone. This marks the original location of the boulders before becoming detached and falling to the valley floor. Examination of the landslide chute shorty after the event revealed that an unfortunate deer had been caught directly in the path of the tumbling boulders.
Cliff Face Scar
Photo taken ~250ft. above the valley floor. Note the fresher-looking rock exposure near the lower center of the photo. This marks the attachment point of the boulders before falling. We personally don't know if one large mass fell and then fragmented upon impact or if each boulder broke off and fell independently. Fun to think about, though!
Be sure to download our Onsite Geology Lesson PDF posted above for a detailed geologic investigation of this site.Â
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