Sinking Ship
A tilted rock spire that looks like it's slipping into the canyon
About
Sinking Ship is a tilted butte of Kaibab limestone and cream-colored Coconino sandstone on the South Rim, about 1.7 miles southeast of Grandview Point. The rock layers here were shifted upward at an angle by the Cremation Fault and the Grandview-Phantom monocline, so instead of the canyon's usual flat-lying strata, the whole formation leans hard to one side — from some angles it reads as three tilted spires, from others as a hull sliding into the depths. The effect is what earned it the name in 1932, replacing its earlier label, "Three Castles."
Where to see it
Moran Point, along Desert View Drive, is the recognized best vantage — the same formation that painter Thomas Moran sketched here in the 1800s. It's a rim-edge view, not a maintained trail to the formation itself, so most visitors take it in from the overlook rather than approaching on foot. The summit itself sees occasional Class 4 scrambling by experienced climbers, but that's a technical, unofficial route, not a park-maintained hike.
Best Time to View It
Moran Point is accessible year-round on Desert View Drive; the tilted rock layers show best in morning or late-afternoon light.
Good to Know
- The effect earned it the name in 1932, replacing its earlier label, "Three Castles."
- The summit itself sees occasional Class 4 scrambling by experienced climbers, but that's a technical, unofficial route, not a park-maintained hike.
- Most visitors take it in from Moran Point rather than approaching on foot.
Where to See Sinking Ship
Moran Point, along Desert View Drive, is the recognized best vantage — the same formation that painter Thomas Moran sketched here in the 1800s. It's a rim-edge view, not a maintained trail to the formation itself.
What You're Looking At: Sinking Ship
Sinking Ship is a tilted butte of Kaibab limestone and cream-colored Coconino sandstone on the South Rim, about 1.7 miles southeast of Grandview Point. The rock layers here were shifted upward at an angle by the Cremation Fault and the Grandview-Phantom monocline, so instead of the canyon's usual flat-lying strata, the whole formation leans hard to one side — from some angles it reads as three tilted spires, from others as a hull sliding into the depths.
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