Checkerboard Mesa's distinctive crosshatched sandstone face rises dramatically above pine trees in Zion National Park, Utah.

Checkerboard Mesa: What You Are Actually Looking At

Zion Travel Team·

Driving Highway 9 through the eastern side of Zion, most visitors are focused on the Zion-Mount Carmel Tunnel ahead of them and glance right past one of the park's more distinctive formations. Checkerboard Mesa sits right at the roadside near the tunnel's east portal, and the grid pattern etched into its face is not a trick of the light, it is two entirely different geological processes overlapping on the same rock.

What Actually Causes the Grid Pattern

The crosshatch pattern comes from two completely independent sets of rock fractures working on the same sandstone face. The vertical lines are stress joints, cracks that opened as buried sandstone was gradually exposed to the surface and subjected to repeated cycles of heating, cooling, and water freezing over thousands of years.

The horizontal lines are a different story entirely. They trace the original cross-bedded layers of ancient Jurassic sand dunes, fossilized wind-blown sand from a desert that existed here roughly 180 million years ago. The softer interfaces between those ancient dune layers erode faster than the surrounding rock, carving horizontal grooves that follow the dune geometry rather than any modern weathering pattern. When both the vertical stress joints and the horizontal dune-layer grooves erode simultaneously, the result is the grid visible from the road today.

There Is No Trail to the Top

Checkerboard Mesa is a roadside viewpoint, not a hike. The pullout offers a direct view of the formation, but there is no trail leading to the summit and no facilities at the site itself. Visitors expecting a maintained path to climb are looking in the wrong place.

If you want to add an actual hike near this stop, Canyon Overlook Trail is the closest option, starting about 1 mile west at the east portal of the Zion-Mount Carmel Tunnel. It covers 1 mile round trip with 163 feet of elevation gain and requires no permit, making it an easy addition to a Checkerboard Mesa stop without adding much time to your day.

No Shuttle Access

The free Zion Canyon shuttle only operates on Zion Canyon Scenic Drive and does not serve Highway 9 east of the tunnel at all. Reaching Checkerboard Mesa requires your own vehicle, which means this stop is really only practical for visitors driving through the park on Highway 9, whether entering from the east entrance or passing through en route to somewhere beyond the park.

Entrance Fee Applies Like Anywhere Else in the Park

Checkerboard Mesa sits inside Zion National Park boundaries, so the standard park entrance fee applies: $35 per vehicle, valid for 7 consecutive days. The America the Beautiful annual pass is also accepted. International visitors 16 and older pay an additional $100 per person surcharge, card only, a detail worth knowing in advance if your group includes international travelers so nobody is caught without the right payment method at the gate.

When to Photograph It

Morning is the best window for photography here. The mesa face is roughly east-facing, so morning light hits it directly and shows the crosshatch pattern at maximum contrast, with the vertical and horizontal lines both clearly visible against each other. By mid-afternoon, the face falls into full shadow, and the grid pattern becomes noticeably harder to read in photos. If direct sun timing does not work with your schedule, overcast light is a solid second option, since it gives even exposure across the whole face without the harsh shadows a midday sun angle would create.

Browse Hiking on Zion Travel for the trails near this stop, and check Trip Planning for how to build a Highway 9 drive into the rest of your Zion visit.

Frequently Asked Questions

What caused the grid pattern on Checkerboard Mesa?

The crosshatch pattern comes from two completely independent sets of rock fractures. Vertical lines are stress joints that opened as buried sandstone was exposed and subjected to repeated heating, cooling, and water freezing over thousands of years. Horizontal lines trace the original cross-bedded layers of ancient Jurassic sand dunes — these softer interfaces erode faster, carving grooves that follow the dune geometry. When both sets erode simultaneously, the result is the grid you see from the road.

Is there a hiking trail to the top of Checkerboard Mesa?

No — the article is clear that the pullout at Checkerboard Mesa is a roadside viewpoint with no trail to the summit and no facilities. If you want to add a hike nearby, Canyon Overlook Trail starts about 1 mile west at the east portal of the Zion-Mount Carmel Tunnel and covers 1 mile round trip with 163 feet of elevation gain, with no permit required.

Does the Zion shuttle stop at Checkerboard Mesa?

No. The free Zion Canyon shuttle only operates on Zion Canyon Scenic Drive and does not serve Highway 9 east of the Zion-Mount Carmel Tunnel. You need your own vehicle to reach Checkerboard Mesa.

What is the entrance fee to see Checkerboard Mesa?

Checkerboard Mesa sits inside Zion National Park, so you pay the standard park entrance fee of $35 per vehicle, valid for 7 consecutive days. The America the Beautiful annual pass also covers entry. International visitors 16 and older pay an additional $100 per person surcharge, card only.

What is the best time of day to photograph Checkerboard Mesa?

Morning is best. The mesa face is roughly east-facing, so morning light hits it directly and shows the crosshatch pattern at maximum contrast. By mid-afternoon the face falls into full shadow and the lines are harder to read. Overcast light is also a good option for even exposure without harsh shadows.