The view is from the ridge between Mill and Butcher Creeks, looking northwest. Campbell Peak is near the center, Iron Mountain on the left, and the high ridge on the right leads to Dallas Peak. The light-colored cliffs are caused by the San Miguel conglomerate; above them appear the clearly bedded San Juan tuffs. The highest levels are occupied by the Potosi rhyolite series. The talus slopes are typical of the region.