Watson Lake Park

Watson Lake was never natural. In the early 1900s the Chino Valley Irrigation District built a dam across Granite Creek to store water for farms down in the valley, and the creek backed up into the low ground among the Granite Dells to form the lake you see today. It is a compact reservoir, and because it flooded a boulder field rather than a smooth basin, it fills with islands and inlets and dead-end coves instead of an open sheet of water.

For decades the lake served its plain irrigation purpose, but the setting was too good to stay purely practical. In 1997 the City of Prescott bought the reservoir and the land around it to keep it as public recreation land rather than let it be developed, and that decision is why anyone can drive out today and put a boat in among rocks that predate almost everything on Earth.

The Granite Dells are the reason people photograph Watson Lake more than almost any other spot in central Arizona. They are a broad expanse of exposed bedrock and loose boulders of Precambrian granite, some dated to roughly 1.4 billion years old, weathered over that immense span into rounded, bulging, stacked forms that look nothing like the sharp cliffs most people picture when they think of Arizona rock.

The shapes come from spheroidal weathering. Granite fractures into a grid of joints as it cools and rises, and once water gets into those cracks it slowly rots the corners and edges faster than the flat faces, rounding every block a little more with each passing century. Multiply that by more than a billion years and you get the Dells: a landscape of smooth granite domes and toppled boulders, threaded with slots and hollows, that climbers, hikers, and paddlers now treat as an enormous natural playground.

One of the best ways into the Dells does not require a boat at all. The Peavine Trail follows the old railbed of the Santa Fe, Prescott and Phoenix Railway, a line that opened in 1893 and wound its way north from Prescott through the boulders toward Ash Fork. Railroaders nicknamed it the Peavine because its constant twisting curves, forced by the terrain, looked like the tendrils of a climbing pea plant.

Passenger trains ran the route for decades and made their last commemorative run in the early 1960s, and the line was finally abandoned in the 1980s. Rather than let it vanish, Prescott and its neighboring towns turned the corridor into the Peavine National Recreation Trail, part of the national rails-to-trails movement. The result is a nearly flat, wide, easy path that carries walkers, joggers, cyclists, and horseback riders straight through the heart of the Granite Dells, close enough to the rock that you can reach out and touch a billion years of weathering as you go.

Most first-time visitors come for the paddling, and it is worth building a trip around. Kayaks and canoes rented from local outfitters in the warm months let you nose into coves that the shoreline trails never reach, gliding between boulders that rise straight out of the water into little stone islands. It is calm, no-wake water, forgiving for beginners, and the scenery does all the work. Anglers fish the same water for bass, catfish, sunfish, and crappie, and the granite cliffs above the lake draw rock climbers who top-rope and lead-climb the faces.

On foot, the shoreline trails and the Watson Lake Loop scramble up and over open granite, marked mostly by painted dots on the rock, and reward the effort with high views back across the water. This is also a quietly excellent spot for birding, with herons, waterfowl, and raptors working the lake and the marshy Watson Woods nearby. Come at either end of the day if you can. When the low sun hits the boulders they glow gold and rose, the water goes still, and the whole strange basin looks like something dreamed up rather than dammed.

The closest Boutel™ stays, so you can turn this stop into an overnight. Each is an independently owned, editorially selected place to stay.