About Havasu Falls
Tucked deep within the remote red-rock side canyons of the Grand Canyon system lies Havasu Falls, one of the most famous and striking natural wonders in North America. Known for its brilliant turquoise-blue water contrasting vividly against fiery orange and crimson limestone cliffs, Havasu Falls drops approximately 90 to 100 feet into a series of inviting travertine plunge pools.
The extraordinary blue-green color of the water stems from high concentrations of dissolved calcium carbonate and magnesium, which reflect sunlight and continuously form dynamic mineral deposits that reshape the pools over time. Visitors must hike 10 miles from the trailhead at Hualapai Hilltop down through dusty desert canyons to reach the Havasupai Reservation village of Supai and the nearby campground.
Access is strictly controlled by the Havasupai Tribe, and visiting requires planning months or even years in advance. Swimming in the refreshing, year-round 70°F (21°C) waters after a arduous trek through the desert is an unforgettable bucket-list experience for outdoor enthusiasts worldwide.
History
The history of Havasu Falls is deeply tied to the Havasupai Tribe, whose name translates to 'People of the Blue-Green Waters.' The Havasupai have inhabited the Grand Canyon region for over 800 years, traditionally utilizing the canyon bottom for summer agriculture and moving up to the plateau Rim during the winter months.
In 1882, executive orders established a small reservation that severely restricted the ancestral territory of the tribe. Despite intense pressure from mining and government expansion, the Havasupai maintained their deep cultural bond with the land and water. In 1975, after decades of advocacy, the U.S. Congress passed legislation restoring over 185,000 acres of canyon land back to the sovereign control of the Havasupai Nation.
The physical structure of Havasu Falls has evolved dramatically due to periodic flash floods. Major flooding events in 1910, 1993, 2008, and 2018 altered the flow from a single wide curtain of water (formerly known as Bridal Veil Falls) into the present concentrated single drop and formed new travertine terraces downstream.