The town Kanarraville
A creek town on the valley floor, right where the plateau breaks
Under the Hurricane Cliffs, where the plateau meets the valley.
Kanarraville sits at roughly 5,560 feet on the floor of Cedar Valley, tight against the base of the Hurricane Cliffs. The wall rises to the east and southeast, the valley opens west toward the Pine Valley Mountains, and Kanarra Creek runs cold down the middle of it all. This page is about that setting, and why the ground here looks the way it does.
By Scott Buehler, Southern Utah local
Updated September 2026
The short answer
Kanarraville is a small town on the floor of Cedar Valley, at its south end, tucked against the base of the Hurricane Cliffs at roughly 5,560 feet. The cliffs are the long, tilted wall that rises to the east and southeast of town, the raised and eroded edge of the Colorado Plateau. West of town the valley opens toward the Harmony Mountains and, beyond them, the Pine Valley Mountains. Kanarra Creek runs cold and year round down the middle of it, straight out of a slot canyon cut into the cliffs. Cedar City is about 20 minutes north on Interstate 15. That is the whole geography in a sentence: a creek town on flat valley ground, right where the plateau breaks and the land drops away to the west.
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The wall to the east
The cliffs, the creek, and the open valley.
Stand anywhere in Kanarraville, look east, and the horizon is a wall. The Hurricane Cliffs rise abruptly to the east and southeast, right at the edge of town, a long tan and rust colored escarpment topped by the higher ground of Kanarra Mountain and the Kolob Terrace behind it. The rock is not flat lying, either. The layers tilt and bend where you can see them, because the ground here was folded as well as lifted, and that gives the wall its stacked, ribbed look in the afternoon light.
Coming down out of that wall is Kanarra Creek. It runs out of a slot canyon carved straight into the cliffs east of town, cold and year round, and it flows right through the middle of Kanarraville before spreading into the irrigated ground along the valley floor. That canyon is the one people drive in for, the Kanarra Falls hike, but from town the creek is just the quiet green line that makes a high desert valley livable.
The other direction is the opposite of a wall. West and southwest the valley floor is flat and open, running toward the Harmony Mountains and, past them, the taller Pine Valley Mountains. Interstate 15 threads north to south through that open ground, so the town sits neatly between two things: the abrupt plateau edge on one side, and a wide valley with a long western horizon on the other. Sunset happens over the mountains to the west; first light hits the cliffs to the east.
Why the wall is there
The Hurricane Fault, and a plateau that broke.
The cliffs are not a coincidence of erosion. They mark the Hurricane Fault, a long north to south fault that runs from near Cedar City all the way south into northern Arizona. It is one of the major dividing lines in this part of the West: the boundary between the Colorado Plateau on the east, which stands high, and the lower Basin and Range country on the west. Along that line the western side dropped and the eastern side stayed up, and the raised, eroded edge of the high side is exactly the wall Kanarraville looks at every day.
So the town sits on the dropped side, on the valley floor, gazing up at the standing edge of the plateau. The rock around Kanarraville is also folded into what geologists call the Kanarra anticline, which is why the layers in the cliffs are so visibly tilted and bent rather than lying flat. Between the fault and the fold, this is one of the clearest places in Utah to actually read how the ground was pushed up, folded, and then broken, and it draws geology classes for exactly that reason.
The fault is still considered active, and it is studied for its long earthquake history. That is worth knowing as background rather than as a daily worry: it is the same seismic setting shared across much of southwestern Utah, and it is simply part of living against a young, still moving edge of the continent.
Seeing it for yourself
Where to actually take it in.
The easiest view is the drive itself. Come south on I-15 and get off at Exit 42, and the whole escarpment runs alongside you on the left, close enough that the tilted layers are obvious. From the streets of town the cliffs simply fill the eastern sky. If you want to stand right at their base, the Kanarra Falls trailhead in town puts you where the creek comes out of the rock.
For a closer look into the same uplifted plateau, Zion's Kolob Canyons entrance is about 15 minutes south. A paved scenic road climbs into the identical edge of the Colorado Plateau, where the gray lower rock gives way to the tall red Navajo sandstone that Zion is known for. It is the same geologic story as the wall above Kanarraville, just cut deeper and painted redder.
The slot canyon floods, so watch the weather. Kanarra Creek's canyon is narrow, and a summer thunderstorm miles away can push water through it fast. Check the forecast before going up, and stay out of the narrows any time rain is in the picture.
Scott Buehler
Moving Utah About Scott
Keep reading
More of Kanarraville on The Local.
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Read the guideThe permit hike
Kanarra Falls Permits
The fee, the daily cap, and why there is no walk-in office in town.
Read the guideThe canyon itself
Kanarra Creek Canyon
The ladder, the wading, and when the water makes it a bad idea.
Read the guideZion's quiet door
Kolob Canyons
A separate Zion entrance fifteen minutes south, and why locals treat it as an evening trip.
Read the guideMoving here
Living on Kanarra Creek
Three water systems, no subdivisions, and a market that moves slowly.
Read the guideThe companion
Kanarraville, from a local
The permit hike, the town underneath it, and the whole honest story in one place.
Read the pageQuick answers
The town, answered.
They are the long, tilted wall of rock that rises to the east and southeast of town, the eroded western edge of the Colorado Plateau. Kanarraville sits at their base, on the floor of Cedar Valley, so the cliffs are the first thing you see looking east from almost anywhere in town.
East and southeast. Kanarraville sits on the valley floor to the west of the cliffs, so the escarpment catches the morning and midday light, and the town looks up at it rather than down from it.
It is a long, north to south normal fault that runs from near Cedar City south into northern Arizona. It marks the boundary between the uplifted Colorado Plateau to the east and the dropped Basin and Range country to the west, and the Hurricane Cliffs are the raised, eroded edge it left behind.
The town sits at roughly 5,560 feet above sea level, on the floor of Cedar Valley. That elevation means real four season weather, with cool nights well into spring and genuine snow in winter, even though the low desert around St. George is only about an hour south.
It comes down out of a slot canyon cut into the Hurricane Cliffs east of town, running cold and year round, and it flows right through the middle of Kanarraville. That same canyon is the Kanarra Falls hike, which needs a permit.
The valley opens west and southwest toward the Harmony Mountains and, beyond them, the Pine Valley Mountains. The town sits between two very different kinds of high ground: the abrupt plateau wall on the east, and the more distant mountain ranges across the open valley to the west.
About 13 miles, or roughly 20 minutes north on Interstate 15 at Exit 42. Cedar City is where the groceries, schools, hospital and most jobs are, since Kanarraville itself has no stores or services inside town limits.
No. The town sits outside the park, but Zion's Kolob Canyons entrance is only about 15 minutes south, and it climbs into the same uplifted edge of the Colorado Plateau, so the red rock there is geologically the same story as the cliffs above Kanarraville.
Yes. It is considered an active fault, and geologists study it for its earthquake history, which is part of why the Kanarraville area is a well known place for reading the region's geology. For day to day life it is background, the same seismic setting shared across much of southwestern Utah.
A small town, a slow market, and water questions that actually matter.
The setting is the easy part to love. Kanarraville rarely has more than a few homes for sale at once, and out here the harder questions sit underneath the view: which water a property actually has, how the creek and the mountain springs figure in, and what the ground itself is doing. I walk buyers through all of it before they fall for the cliffs.
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