|MAYBE AGATE HUNTERS COULD GET A ROOM AT THE FAIRBURN HOTEL?|
If I were to quiz 10 rockhounds of the CSMS and ask them to name the two most “famous” agate types in the United States I suspect nine of them would list Lake Superior Agates and Fairburn Agates; I would agree. I first started looking for Fairburn Agates in South Dakota back when I was chasing fossils in 1966 for some of my research. In those long ago days the agates were not common, but were still available to the intrepid explorer willing to tramp around the exposures. I have a nice specimen collected in 1966, could not locate one during a hunt in 2009, but was again successful last summer.
|A COUPLE OF NICE FAIRBURNS.|
Fairburns are valued for their colorful fortification patterns with an abundance of reds (iron oxide), oranges (iron oxide) and blacks (manganese oxides). The derivation of their name comes from the small community of Fairburn, located south along I-90, ~25 miles, of Rapid City near SD 79. This area is also perhaps the easiest for collectors to locate. Agate hunters should travel east from Fairburn along French Creek Road (good gravel) for about 12 miles to a sign locating the original collecting area managed by the Buffalo Gap National Grasslands. Although known to collectors for decades, these Fairburn beds still yield an occasional agate, and as many colorful specimens of jasper, quartz and chalcedony as can be carried out in your collecting bag.
|ENOUGH MICROCRYSTALLINE QUARTZ TO FILL YOUR COLLECTING BAQ!|
The geology at the collecting site is as interesting as the specimens. French Creek has eroded the area and exposed the Cretaceous Pierre Shale, the Eocene/Oligocene Chadron Formation (White River Group—famous for producing mammals in Badlands National Park) and Tertiary terrace gravels (the original source of the microcrystalline quartz nuggets). However, rockhounds also will notice a very distinct red-orange-yellow “bed” between the Pierre and the Chadron. Originally named the Interior beds (for exposures near the village of Interior, SD), this “bed” is now known to be an ancient soil developed on the Pierre Shale in a tropical-like climate (warm and wet) during the Eocene.
|NOTE THE RED BURIED PALEOSOIL DEVELOPED ON THE PIERRE SHALE DURING TROPICAL TIMES OF THE EOCENE.|
The really interesting story about the Fairburns involves their relationship with the Teepee Canyon Agates in the Black Hills. This latter agate site, in the Paleozoic Minnelusa Formation, is located west of Custer, SD, along US 16 about two miles west of Jewel Cave National Monument, or perhaps 14 miles from Custer. Most geologists now believe that the Minnelusa Formation in the Black Hills is the source of the Fairburn Agates and the pebbles were transported out to the plains by Tertiary streams draining the Hills. These “high level” terrace gravels (from the streams) are evident at several localities surrounding the Hills and may be seen at the original Fairburn site. Further erosion of the terraces in the late Tertiary and Pleistocene winnowed out finer sediments and scattered the microcrystalline quartz pebbles over a wide area.
|YOU CAN'T GET LOST.|
If you plan on collecting at Teepee Canyon the agate “diggings” are very evident since prospectors must quarry out large pieces of limestone and then break out the cherty nodules, some large and some small. Large crack hammers, pry bars, leather gloves, and eye protection are required. The agate localities, both in Teepee Canyon and next door in Hell Canyon, are located on USFS land and are open to collectors, at least were open during my last visit.
|ROGER CLARK'S FAIRBURN AGATE BOOK.|
I would suggest that if you are interested in Fairburn Agates---pick up a book or three written by Roger Clark, the premier expert on the agates. Book one is South Dakota's Fairburn Agate is only available on the used book circuit. Book number two, Fairburn Agate: Gem of South Dakota, and number three, Fairburn Agate: South Dakota State Gemstone are in print and published by Silverwind Agates. The photos are just amazing.
|CHASING AGATES AND FOSSILS 1966|