Devil's Kitchen: Sedona's Collapsing Wonder

Devil's Kitchen, a captivating sinkhole in Sedona, Arizona, offers a unique look at the region's geological activity. The sinkhole's formation began long before Western presence, with the earliest signs of sinkage appearing on the southernmost wall. Significant collapses in the early 1880s and 1989 dramatically widened the hole, creating the impressive cavern visible today. The 1880s collapse was so powerful that residents reported dust filling the air all day.The sinkhole's geology is fascinating. It was formed by subsidence into caverns of paleokarst composed of Redwall Limestone. The upper walls consist of sandstone from the Schnebly Hill Formation, while the lower areas are made of shaly siltstone of the Hermit Formation. The southern wall displays rounded edges and manganese oxide, indicating exposure over hundreds of years, contrasting with the angular rocks on the northern side from more recent collapses.To reach Devil's Kitchen, hikers typically take the Soldier Pass Trail. This easy, short trail is suitable for all ages and skill levels. The trail also leads to the Seven Sacred Pools, another natural wonder worth exploring. The parking lot at the trailhead is small, accommodating only about 15 vehicles, so arriving early is highly recommended. An alternative is to park at the Posse Grounds Park & Ride and take the free Sedona Shuttle to the trailhead.