BRAUER, J. (2014). Druid Arch Sunset, Canyonlands.
The Three Districts of Canyonlands
Canyonlands is divided into three major districts, each separated by the Colorado and Green Rivers. While they share common geological origins, they each have unique characteristics.
Britnee, L (2022). Island in the Sky district. Canyonlands National Park.
1. Island in the Sky
Island in the Sky is a high mesa that rises over 1,000 feet above the surrounding landscape offering expansive views of the Colorado and Green River canyons.
The district’s elevation provides panoramic perspectives of the park’s layered rock formations and steep cliffs, with the White Rim Sandstone forming a distinctive shelf below the mesa.
Island in the Sky highlights the erosional forces at work, showcasing deep canyons and dramatic geological contrasts.
Britnee, L (2022). Needle district. Canyonlands National Park.
2. The Needles
Named for the towering, colorful sandstone spires that dominate the landscape, The Needles district offers a labyrinth of rock pinnacles, arches, and canyons.
The Needles district features formations created by erosion along natural rock joints.
The vertical cracks in Cedar Mesa Sandstone allowed weathering to carve the rock into tall, needle-like formations, showcasing bands of red and white rock.
Britnee, L (2022). Maze district. Canyonlands National Park.
3. The Maze
The Maze is the most remote and least accessible district in Canyonlands.
Famous for its complex system of twisting, narrow canyons, known for confusing early explorers, hence the name. Isolated by the Colorado and Green Rivers, The Maze has remained largely untouched by human activity, preserving its complex rock formations shaped by erosional processes.
This video will take you through a virtual tour of Canyonlands National Park and how it was created.
Levy, Y (2019). View from an Arch formation in Canyonlands National Park.
Britnee, L (2022). View from Above of Rivers and Canyons. Canyonlands National Park.
Rivers and Canyons
Rivers and Canyons are sculpted by the Colorado and Green Rivers over millions of years.
Erosion by rivers and seasonal flash floods created dramatic cliffs and winding channels.
Rivers and Canyons highlights the uplift of the Colorado Plateau and the park’s intricate geology.
Mesas and Buttes
Formed by differential erosion of flat-lying sedimentary rock layers.
Resistant sandstone forms cap rocks over eroding softer layers, creating flat-topped mesas.
Further erosion isolates smaller formations, forming buttes.
Reflects the “layer cake” geology of the Colorado Plateau.
Britnee, L (2022). View of the White Rim Trail. Canyonlands National Park.
White Rim Trail
Created from ancient sand dunes and tidal flats, uplifted during the Laramide Orogeny (~70 million years ago).
More resistant to erosion, leaving a distinct bench between towering cliffs and deep canyons.
White Rim Trail Offers insights into sedimentary deposition, tectonic uplift, and erosion.