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Colorado River
Colorado Plateau

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

Length 1450 miles
Class I–V (by section)
Sections 14
Season Apr, May, Jun, Sep, Oct
Gateway Moab, UT
Overview

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 47 miles of consequential Class IV–V whitewater through Cataract Canyon; 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 the deepest canyon on the continent, 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 through the deepest canyon in North America
  • 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
River Sections

14 sections, 1450 miles

Flows & Gauges

heavily regulated — Glen Canyon Dam (Lake Powell), Hoover Dam (Lake Mead), Davis, Parker, and many upstream diversions control flow throughout

Colorado River near Moab, UT

USGS gauge on the Colorado River near Moab, UT — a key reference point for the Moab area river sections including Ruby-Horsethief, Westwater Canyon downstream flows, and upper Cataract Canyon planning. Located upstream of the Dolores River confluence.

Current flow — Colorado River near Moab, UT

Updating… Provisional

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

Updating… Provisional

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

Updating… Provisional

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.

Geology

The Colorado River is the most geologically exposed river on Earth for a major drainage. It carved through sedimentary strata uplifted by the Laramide Orogeny (65–50 Ma) and the ongoing uplift of the Colorado Plateau. In the Grand Canyon, it exposes the Vishnu Schist and Zoroaster Granite — basement rocks dating to 1.7 billion years. The river carved roughly a mile (~5,000–6,000 feet) of canyon in approximately 5–6 million years. Through Cataract Canyon in Canyonlands, the river exposes Pennsylvanian and Permian strata — the same units that built the walls of Westwater Canyon farther upstream.

Rock types
sandstone limestone shale granite schist
Formations
Navajo Sandstone Wingate Sandstone Kayenta Formation Hermit Shale Redwall Limestone Tapeats Sandstone Vishnu Schist (Grand Canyon basement)

Age range: Paleoproterozoic (~1.75 Ga basement) through Permian (Kaibab capstones, Grand Canyon rim) and Jurassic (Navajo capstones, upper river)

Ecology

The Colorado River corridor supports four federally listed endangered native fish — Colorado pikeminnow, razorback sucker, humpback chub, and bonytail chub — 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.

Biomes
Colorado Plateau canyon desert Rocky Mountain montane (headwaters) Sonoran Desert (lower river) riparian cottonwood-willow gallery
Notable species
Colorado pikeminnow (Ptychocheilus lucius) — endangered razorback sucker (Xyrauchen texanus) — endangered humpback chub (Gila cypha) — threatened bonytail chub (Gila elegans) — endangered peregrine falcon (Falco peregrinus) desert bighorn sheep (Ovis canadensis nelsoni) ringtail cat (Bassariscus astutus) canyon wren (Catherpes mexicanus)
Invasive species
tamarisk / saltcedar (Tamarix ramosissima) — dominant in many riparian reaches Russian olive (Elaeagnus angustifolia)
History
Indigenous homelands
Ute Nation Navajo Nation (Diné) Havasupai Hualapai Hopi Southern Paiute Cocopah Yuma (Quechan)
Explorers
John Wesley Powell James White George Wheeler Frederick Dellenbaugh

Notable Expeditions

  • Powell Colorado River Expedition
  • Powell Second Colorado River Expedition
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