It's 18 miles ahead to the primitive 2-track leading to the Shoofly Quick Loop trailhead. Go left at that junction, and then turn right at the signed turnoff for Mud Flat Road. Pick up any last-minute supplies at the gas station at the T-junction. You'll come to a stop sign, turn right on ID 167 and go to Grand View. Turn right on Simco and drive across the desert toward Grand View. How to get there: If you're coming from Boise, take I-84 east to Simco Road. Temps should be in the 50s next week.Īpproaching the little cabin, Perjue Canyon and W. The weather forecast for Grand View this weekend looks pretty promising with temperatures in the low 60s, partly cloudy skies and relatively light winds. Shoofly Quick Loop requires more cross-country travel, steeper climbing and descending, and backcountry navigation skills. It provides more of a loop experience with some cross-country hiking, while the BLM trail is an out-and-back experience, 2 miles each way or 4 miles total. When I first put together my Owyhee Canyonlands guidebook 10 years ago (can't believe it's been that long!), I pioneered a different route into Perjue Canyon called the Shoofly Quick Loop. I had a free afternoon on Tuesday, and I thought I'd try out the BLM trail that goes over to the West Fork of Shoofly Creek aka Perjue Canyon, accessed from Mud Flat Road, aka the Owyhee Canyonlands Scenic Backcountry Byway. One of my favorite early spring go-to hikes in the Owyhees is the Shoofly Creek area near Grand View. This spring-like weather we're enjoying this week will be temporary, but we have turned the page into March, and that means it's time to think about exploring the Owyhee Canyonlands.Īt this time of year, it's best to look at outdoor adventures in the lower elevations of the Owyhees to find trails that are drying out in the sunshine and wind, while the upper country is still wet and/or snowbound. This suggests the possibility that oil and gas accumulations are present along the shelf edge, although subsequent deformation may have allowed the hydrocarbons to escape.Cool rock outcropping at the saddle on the way over to Perjue Canyon. Throughout western and central Wyoming, shallow open-marine conditions prevailed.ĭespite differences in age and tectonic setting, the facies relations and the reconstructed paleogeography resemble the Permian shelf-basin sequence of West Texas. ![]() Restricted, shallow-marine conditions existed from the banks into western Wyoming. ![]() In eastern Idaho and westernmost Wyoming, carbonate mounds and oolite shoals lined the shelf edge. Red Peak-Thaynes correlations lead to the reconstruction of an average paleogeography for western and central Wyoming and adjacent Idaho. The writers demonstrate that the Alcova is an eastward-extending, marine tongue of a limestone in the upper part of the Thaynes, the "sandstone and limestone unit." This resolution of the problem is possible only by the combined use of surface and subsurface stratigraphic sections, sedimentary petrography, paleontology, bedding types and sedimentary structures. The principal marker bed in the Wyoming sequence, the Alcova Limestone Member, has been correlated variously with many different parts of the Thaynes, and even has been considered to be younger than the Thaynes. Stratigraphic relations between the shallow, generally open-marine deposits of the Triassic miogeosyncline in eastern Idaho (Thaynes Formation) and shelf deposits in Wyoming (Red Peak and Crow Mountain Formations) have been uncertain. Correlation and Stratigraphy of Triassic Red Peak and Thaynes Formations, Western Wyoming and Adjacent Idaho
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