
Colorado River
The Colorado carves the deepest canyons of the Southwest — from Westwater's technical gorge to Cataract's flood-season violence to the 226-mile Grand Canyon traverse. · CO · UT · AZ · NV · CA
The Colorado River is the defining waterway of the American Southwest — 1,450 miles from the Rocky Mountain headwaters in Colorado to its historical terminus at the Gulf of California. The river carved the Grand Canyon, built the Canyonlands, and divided the Colorado Plateau into the architecture of high desert civilization. For boaters, it is a system of systems: the technical pool-drop of Westwater Canyon; the 40 miles of Cataract Canyon, where the whitewater concentrates in the first fourteen below the Confluence; the 226 miles of permit-controlled wilderness in the Grand Canyon; the quiet flatwater of Moab Daily and Meander Canyon between them. The Colorado is simultaneously one of the most over-allocated rivers in the world — every drop spoken for by compact law — and one of the most powerful wild experiences available to those who can access its permits. It flows through the ancient Precambrian basement of the Colorado Plateau, through a mile of exposed rock in the Grand Canyon, and through the heart of the most contested water politics in the Western United States.
Signature Experiences
- Cataract Canyon in high spring runoff — the Big Drops at Class IV–V
- 226-mile Grand Canyon traverse — a mile down, from 270-million-year-old Kaibab rim rock to 1.75-billion-year-old Vishnu basement
- Westwater Canyon technical Class IV in ancient Precambrian walls
- Meander Canyon quiet flatwater from Potash to the Confluence
- Moab Daily — accessible day floating through redrock canyon country
Colorado River Sections
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Ruby–Horsethief Canyon
25 mi Ruby–Horsethief Canyon is the Colorado Plateau's most welcoming multi-day float — 25 miles of... -

Westwater Canyon
17.2 mi Westwater compresses the entire Colorado River experience into a single day. The first six miles are... -

Cisco to Dewey Bridge
14 mi The quiet flatwater extension of a Westwater trip — 14 miles between Cisco and Dewey Bridge through... -

Dewey Bridge to Hittle Bottom
8 mi The most accessible mellow float above Moab — a redrock half-day on the Colorado with zero... -

Moab Daily
13 mi The 13-mile Hittle Bottom to Take Out Beach float — the most-run day section on the Colorado... -

Jackass Canyon
10 mi 10-mile Class I float from Take Out Beach through Moab to the US-191 Moab Bridge, with seven BLM... -

The Portal
17 mi 17-mile Class I flatwater through The Portal — where the Colorado exits the Moab Valley through a... -

Meander Canyon
48 mi Meander Canyon is the quiet before the storm — 48 miles of total flatwater through the heart of... -

Cataract Canyon
40 mi Cataract is two trips joined by a confluence. The first is a long, wind-bitten flatwater approach —... -

Narrow Canyon
7.5 mi Narrow Canyon is where Cataract Canyon exhales — tight walls, still water, and the eerie transition... -

Glen Canyon / Lake Powell
186 mi Lake Powell is 186 miles of drowned canyon country — a reservoir as vast and controversial as the... -

Glen Canyon Tailwaters
15 mi The 15-mile tailwater below Glen Canyon Dam — cold, clear water running down to Lees Ferry, where... -

Grand Canyon
226 mi Everything about the Grand Canyon operates at a scale that makes other river trips feel like... -

Diamond Creek to Pearce Ferry
51 mi
heavily regulated — Glen Canyon Dam (Lake Powell), Hoover Dam (Lake Mead), Davis, Parker, and many upstream diversions control flow throughout
Colorado River at Potash, UT
USGS gauge measuring discharge and gage height on the Colorado River at Potash, UT — downstream of the Moab valley and upstream of the Confluence. Reads the Colorado’s contribution at the Potash put-in; sum it with the Green at Mineral Bottom for the combined flow that reaches Cataract Canyon.
Current flow — Colorado River at Potash, UT
Colorado River Near Cisco, UT
Primary upstream Colorado River gauge used in Westwater, Moab Daily, and Cataract Canyon runoff interpretation.
Current flow — Colorado River Near Cisco, UT
Colorado River at Lees Ferry, AZ
The essential Grand Canyon planning gauge. Located at the historical put-in for Grand Canyon river trips, this gauge reflects Glen Canyon Dam release data and is the primary operational reference for all Grand Canyon river section planning.
Current flow — Colorado River at Lees Ferry, AZ
Best conditions vary dramatically by section. Cataract Canyon peaks in May–June runoff for big water; Grand Canyon is prime March–May and September–October; Westwater runs year-round with irrigation season (March–September) providing consistent flows. Summer (July–August) is viable but hot — 100°F+ in canyon bottoms. Spring runoff from Rocky Mountain snowmelt drives Cataract and upper sections. Fall offers ideal temperatures and lower crowds throughout.
The Colorado cuts through strata raised by the Laramide Orogeny, which lifted most of the Colorado Plateau between 70 and 40 million years ago, and by the Plateau's ongoing rise. In the Grand Canyon it exposes the Vishnu Schist and the granites of the Zoroaster complex — basement dated to about 1.75 billion years — beneath a rim of 270-million-year-old Kaibab Formation. The canyon is a mile deep, and the river cut it in roughly the last 5 to 6 million years. Through Cataract Canyon in Canyonlands, the river exposes Pennsylvanian and Permian strata: the Honaker Trail Formation at river level, Cutler red beds above. Westwater, farther upstream, cuts deeper in time than either — its inner gorge reaches the same Precambrian basement the river meets again in the Grand Canyon's Inner Gorge.
- Navajo SandstoneMassive cliff-former and rounded slickrock — domes, beehives, cuestas, and Zion's sheer walls; weathers into bald, cross-bedded rock.
- Wingate SandstoneMassive sheer vertical cliffs — the defining cliff-former of the Colorado Plateau. Joints control vertical breakage; differential erosion of softer underlying Chinle creates the characteristic 'undercut cliff' profile.
- Kayenta FormationLedge- and bench-forming — thin-bedded, stair-stepping slabs that stand back between the Wingate cliff below and the Navajo slickrock above, often armoring the Wingate.
- Hermit FormationSlope-former — a soft reddish-brown recessive slope beneath the Coconino cliff.
- Redwall LimestoneMassive cliff-former — the sheer 400–800 ft red cliff of the mid-canyon; the upper part is karstic (caves, overhangs).
- Tapeats SandstoneCliff-former — brown vertical cliffs above the basement; the transitional upper beds grade into the surface of the Tonto Platform.
- Vishnu SchistForms the dark, steep, polished walls of the Inner (Granite) Gorge.
Age range: Paleoproterozoic (~1.75 Ga basement) through Permian (Kaibab capstones, Grand Canyon rim) and Jurassic (Navajo capstones, upper river)
The Colorado River corridor supports four federally listed native fish — Colorado pikeminnow, razorback sucker, and bonytail, all endangered, and humpback chub, downlisted from endangered to threatened in 2021 — that evolved over millions of years in the warm, silt-laden, seasonally variable flows of the pre-dam river. Dams, diversions, and altered water temperatures have severely impacted native fish populations. Recovery programs operate throughout the system. Tamarisk, established throughout much of the riparian corridor since the mid-20th century, has displaced native cottonwood-willow communities across large reaches.
Notable Expeditions
- Powell Colorado River Expedition
- Powell Second Colorado River Expedition