Wingate Sandstone is a type of sedimentary rock primarily composed of quartz grains. It is known for its distinctive reddish-brown color, which is due to iron oxide. This rock formation is found mainly in the Colorado Plateau region of the United States, particularly in areas like Utah and Arizona. The Wingate Sandstone was formed during the Late Triassic to Early Jurassic periods, around 200 million years ago. It is characterized by its well-sorted, cross-bedded layers, which indicate that it was deposited by ancient windblown dunes. This formation is significant for both geological studies and as a source of natural resources.