Palisade History

Palisade, located in the eastern end of the Grand Valley, was named for the austere and dramatic palisades–steep cliffs of Mancos Shale bordering the town. The sculptured appearance was formed by various geologic uplifts in the area combined with localized erosion and down cutting by the Colorado River. Mancos Shale is mudrock that accumulated in marine environments of the Cretaceous Inland Sea which retreated about 75 million years ago. The Mesa Verde geologic sands were stripped from the mountains and built up as beach sands and river beds.

The Mesa Verde geologic formation is also known for its thick layers of coal. In Colorado, coal was formed in the middle Cretaceous Times (144-65 million years ago). In Palisade, the Mesa Verde formation provides abundant reserves of highly valuable low-sulfur bituminous coal.

At the turn of the 20th century, coal mining was a big business and as important to Palisade’s early development as fruit growing. More than a dozen coal mines operated in the area. John Nichols opened the Cameo Mine in 1885 which later provided coal for the Public Service Company power plant built on the former Cameo town site in 1957. Most of the mines closed in the late 1950s when natural gas replaced coal for heating.

For well over 10,000 years, Native Americans used the abundant waters flowing in the Grand Valley. When the area officially opened to white settlement in 1882, pioneers not disappointed by the Valley’s desolate appearance saw potential–if water from what was then the Grand River could be captured through dams, diversions, and canals. The subsequent irrigation projects transformed the desert into one of the most productive agricultural regions in Colorado and the Intermountain West.

By the mid 1880s, it was apparent Palisade’s unique geologic location protects crops from spring freezes. The local climate is often referred to as the “banana belt.” The mild climate and unique terrain create near-perfect peach growing conditions in the approximate 10-mile area stretching from the tip of Mt. Garfield to the south end of East Orchard Mesa. Wind moves 8 to 12 mph down-slope from the north and is focused by DeBeque Canyon. This “million dollar wind” is compressed and warms the air to prevent crop-killing frosts in the spring. As the katabatic wind moves west – down valley – it spreads out and its warming affect diminishes. In addition, the palisades absorb warmth and help prevent frost damage. The mild climate, a 182 day growing season, plenty of sunshine and water through elaborate irrigation systems, dams and canals, make Palisade the “Peach Capital.” Mineral-rich soil and our 4,700 foot altitude–which means warm days and cool nights–are also credited for Palisade’s great tasting peaches. Palisade makes Colorado the 7th largest peach producing state in the U.S.

Though a winter kill in 1962-63 wiped out most of the existing fruit trees, and a severe winter in 1989 again damaged the fruit trees and wine grapes, our growers bounced back. Palisade also largely survived pressure to convert prime irrigated land to high-density housing in response to a series of energy booms on the Western Slope. More recently, demand for locally-grown produce increased the number of fruit trees as well as expanded crops to include wine grapes, hops, and lavender. Palisade is a popular destination for fresh fruit, especially peaches, as well as 25 of Colorado’s 140 wineries. It is also the only wine grape growing region in the world more than 1,000 miles from an ocean and at 4,700 feet above sea level.

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