Shumard Peak

Shumard Peak

Natural Attr
Last Updated: July 2026

Type

Geological Formation

Accessibility

Drive-up view only. No summit trail; scramble access is unmaintained, crosses private property, and is not recommended.

Best Season

October–November and March–April. Moderate temperatures, clear skies, minimal thunderstorm risk, excellent light for photography.

Busiest Season

March–May (spring break and Easter holidays). September–October (mild weather, fall tourism). Most crowds transit via Highway 62/180 rather than stopping.

Features

Permian reef limestone, tilted strata revealing tectonic uplift, 8,615 ft peak elevation, western escarpment position.

Elevation

8,615 ft

Overview

About This Attraction

From Highway 62/180, Shumard Peak's sharp ridge rises to 8,615 feet above the western escarpment—the third highest point in Texas, composed of ancient Permian reef limestone that accumulated 250 million years ago on a shallow tropical sea. The peak is named for George Getz Shumard, a geologist who discovered Permian fossils here during the 1852 Marcy-McClellan expedition. No maintained trail reaches the summit; the peak is best viewed from a distance at the Salt Basin Dunes or from the highway itself, where you can see the distinctive strata tilted upward by the collision that created the Guadalupes.

Quick Facts

Type

Geological Formation

Elevation

8,615 ft

Access

Drive-up view only. No summit trail; scramble access is unmaintained, crosses private property, and is not recommended.

Main Features

Permian reef limestone, tilted strata revealing tectonic uplift, 8,615 ft peak elevation, western escarpment position.

What You'll See

A sharp, ridge-like peak composed of light gray to tan limestone with visible horizontal stratification. The tilted angle of the layers is immediately apparent, revealing the collision that created the Guadalupe Mountains. Darker shale bands alternate with lighter limestone. From the Salt Basin Dunes, the peak dominates the eastern horizon.

What Makes It Special

Third highest point in Texas. Named for geologist George Getz Shumard (1823–1867) who discovered Permian fossils in the Guadalupes. Best example of the Permian reef formation's summit expression. Visible Permian reef strata tilted 70–80 degrees from horizontal.

Best Time to Visit

October through April. Avoid summer when midday thermals create turbulent viewing conditions and extreme heat makes any scramble attempt dangerous.

Safety Considerations

Drop cliffs on all sides of peak; do not attempt scramble without professional equipment. Lightning risk at altitude during thunderstorm season (July–September). Exposure to wind and sun—bring water and hat for roadside viewing. Terrain is unstable shale and limestone rubble; any climbing attempt risks rockfall onto yourself or others below.

Visitor Tips

  • The peak is best viewed from U.S. Highway 62/180 westbound or from the Salt Basin Dunes parking area (superior angle).
  • Look at the strata—the tilted limestone layers show the collision that uplifted the reef 75 million years ago.
  • Bring binoculars; the rock quality reveals horizontal laminations typical of shallow-water reef deposits.
  • Early morning provides the best light for photography and clarity; afternoon haze obscures detail.
  • Do not attempt a bushwhack to the summit without topographic map and GPS—no trail exists, terrain is unstable shale, and summit approach crosses private land.
ℹ️ Data Sources
📖 National Park Service — Shumard Peak (official page) (checked 2026-07-13) 📖 National Park Service — Guadalupe Mountains National Park fees, hours & conditions (checked 2026-07-05) 📖 Climate data: Pine Springs, Tx Us, 5,590 ft (NOAA 1991-2020 normals, station USC00417044) 📝 YourNPGuide Editorial

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