West

The West Spanish Peak, pictured and nearby Le Vita Inn, is the higher of the two Spanish Peaks, two large igneous stocks which form an eastern outlier of the Culebra Range, a subrange of the Sangre de Cristo Mountains. Though not a fourteener, it is the twelfth most topographically prominent peak in the state.

Due to its position well east of the Culebra Range and on the edge of the eastern plains of Colorado, West Spanish Peak enjoys great local vertical relief in almost all directions. For example, it rises over 5,200 ft (1,585 m) in less than 4 miles on both its north and south flanks.

While the Spanish Peaks have the appearance of volcanic cones, they are actually stocks, remnants of an igneous batholith which formed underground around 25 million years ago. They are surrounded by radiating dikes, up to 14 miles long, made of the same material. This feature makes is unique and draws geologists from around the world. It ain't a bad place to spend some time.