The user is responsible to verify the limitations of the geospatial data and to use the data accordingly. The Shoofly lies at the margin of a lake basin and was buried to depths of 30 m or less beneath lake sediments and gravels derived from nearby volcanic rocks. The data are dynamic and may change over time. Abstract Intergranular pressure dissolution has occurred in the shallowly buried Plio-Pleistocene Shoofly oolite of the Glenns Ferry Formation in southwestem Idaho. Natural hazards may or may not be depicted on the data and maps, and land users should exercise due caution. The data and maps may not be used to determine title, ownership, legal descriptions or boundaries, legal jurisdiction, or restrictions that may be in place on either public or private land. This rare soil supports a high number of. These geospatial data and related maps or graphics are not legal documents and are not intended to be used as such. Got egg stones Shoofly Oolite is an unusual soil that can be found along the Mud Flat Road west of Bruneau, Idaho. The Diggings™ makes no warranty, expressed or implied, including the warranties of merchantability and fitness for a particular purpose, nor assumes any legal liability or responsibility for the accuracy, reliability, completeness or utility of these geospatial data, or for the improper or incorrect use of these geospatial data. There is also a little cemetery containing some of the original homesteaders there. It erodes strangely and makes for some great subjects. My father, a retired Geologist for the Sate of Idaho showed me this unique mineral called Oolite. The Diggings™ accepts no liability for the content of this data, or for the consequences of any actions taken on the basis of the information provided. South of Grandview Idaho just a bit is a collection of very unique and photographic elements. Shoofly Oolite Interpretive Trail (72) Twelve million years ago, the vast Lake Idaho drained in pretty much a huge whoosh when the Snake River punched through what is today Hell’s Canyon, leaving behind little egg-shaped grains of sedimentary limestone, called oolites. Also, if the weather is a little warmer, be sure to be vigilant of the pads of your dog's paws that can overheat easily in the sand.Information hosted on The Diggings™ is based on publicly available data through the Bureau of Land Management. The trail is off leash dog friendly, but there are no trash cans so please be sure to bag up and pack out the little land mines. Spring (through May) and fall are the best times to visit as summer is scorching hot and the desert becomes riddled with rattle snakes. Consider also walking along the oolite structures to see them all up close. For a view of the Owyhees, head up to the tallest dune from the oolite formations. Once you reach the top of the cliff, you'll be able to see along the stretch of rock formations and from there you can begin exploring. This uphill is all sand (oolites "granules" actually), so take your time. The hike from the parking area to the oolites is only a half mile, and about the last 1/8th of that portion is a steep uphill grade. These structures stretch on for as far as you can see, and only a minute portion are included in the article photography.Īccess to the trailhead is very easy any vehicle, even a Prius, can reach it as the road is chip-and-seal the entire route. Situated 200 feet up the interpretive trail stand the oolite rock structures. The two to three car parking area is situated at about and elevation of 3000 feet. Just north of the Owyhee mountain range, these little known oolite rocks have become stunning geological formations free for all to poke around and explore in otherwise flat surroundings. Oolite (egg stone) is a sedimentary rock formed from ooids, spherical grains composed of concentric layers - per Wikipedia.
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