Or, if you live west/north of Lawton, Oklahoma, those house-sized rounded boulders that make up the Wichitas are the remains of cores of Everest-class mountains that occupied that spot 540,000,000 years ago. They've eroded a bit since, first by cracking, and then by water smoothing the edges of the cracks until we arrived at today's look. The Granite Wash is a subsurface formation that stretches at least to Amarillo and Pampa, Texas from some ancient quicker episode in that erosion. Lots of gas and oil are down there now.
In the Wichita Mountains Wildlife Reserve northwest of Lawton, Oklahoma. You see very similar rocks/hills from there out to Granite and Mangum. They, as I said above, are the granite cores of ancient, big mountains.