Owl Rock

Owl Rock is a red spire composed of Jurassic Wingate Sandstone which is a hard, fine-grained rock which is great for rock climbing, in contrast to the towers and buttes in nearby Monument Valley which have a different composition, de Chelly sandstone. Owl Rock stands atop Tyende Mesa which is formed of the Triassic Chinle Formation. The Owl Rock Member of the Chinle Formation, composed of cherty limestone and limestone conglomerate beds alternating with claystone, mudstone, and siltstone beds, forms the upper half of the mesa, and it overlays the Petrified Forest Member of the lower half.[7] The Owl Rock Member is best exposed at its type locality near the base of Owl Rock. Here the member crops out and the resistant limestone beds form a series of jutting ledges that serve partly in protecting the underlying strata. The limestone beds are very resistant to erosion, forming thin ledges interrupting the slopes weathered from the dominant siltstone interbeds. The Owl Rock Member ranges in thickness from approximately 120 to 166 feet, and at Owl Rock the member is 166 feet thick.[8]

Spring and fall are the most favorable seasons to visit Owl Rock. According to the Köppen climate classification system, it is located in a semi-arid climate zone with cold winters and hot summers. Summers average 54 days above 90 °F (32 °C) annually, and highs rarely exceed 100 °F (38 °C). Summer nights are comfortably cool, and temperatures drop quickly after sunset. Winters are cold, but daytime highs are usually above freezing. Winter temperatures below 0 °F (−18 °C) are uncommon, though possible. This desert climate receives less than 10 inches (250 millimeters) of annual rainfall, and snowfall is generally light during the winter.[9]

• Colorado Plateau
• List of rock formations in the United States

• Weather forecast: Owl Rock