Natural Attraction“Around The Bend”
Forest transition zone on north slope; watch for nesting peregrine falcons above Pine Spring Canyon.

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.
Geological Formation
8,615 ft
Drive-up view only. No summit trail; scramble access is unmaintained, crosses private property, and is not recommended.
Permian reef limestone, tilted strata revealing tectonic uplift, 8,615 ft peak elevation, western escarpment position.
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.
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.
October through April. Avoid summer when midday thermals create turbulent viewing conditions and extreme heat makes any scramble attempt dangerous.
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.
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.
Active Permian reef exposure with visible K-T-era folding (Laramide orogeny). Stratigraphic record of shallow tropical seaway 280–250 million years ago. Visible reef-building organisms' calcareous skeletons (brachiopods, trilobites, corals) in exposed strata. Tilting angle (70–80°) documents collision dynamics during mountain building.
From Pine Springs Visitor Center, take U.S. Highway 62/180 west approximately 40 miles. Pull off at designated viewpoints along the highway or visit the Salt Basin Dunes area west of the park for a distance view of the peak.
No trails originate at Shumard Peak. Nearby trailheads: Salt Basin Dunes Trail (west, outside park), Guadalupe Peak Viewpoint area, Guadalupe Ridge Trail (GRT) access north.
No direct trails; however, Guadalupe Ridge Trail (GRT) network connects to higher elevations. Salt Basin Dunes Trail (outside park) accessible from western viewpoints.
U.S. Highway 62/180 west of the park (direct view). Salt Basin Dunes parking area provides superior distance perspective and photographic angles. El Capitan Viewpoint nearby also offers vistas.
Sunrise from Salt Basin Dunes captures alpenglow on the western face. Sunset provides warm sidelighting of the strata. Midday provides harsh contrast that emphasizes the ridge geometry.
Highway pullout 1.5 miles east of peak provides broad angle; Salt Basin Dunes parking offers dramatic distance silhouette; telephoto lens recommended for detail of strata.
Mule deer, javelina, occasional bighorn sheep on higher slopes. Raptors (golden eagles, red-tailed hawks) visible from a distance. Collared lizards on exposed rock.
Afternoon thunderstorms (July–September) create lightning hazard at high elevations. Winter storms bring snow; Highway 62/180 may experience icing but rarely closes. Wind accelerates dramatically above 8,000 ft; expect gusts >30 mph on exposed ridges.
Guadalupe Peak (8,749 ft, viewpoint and trail 20 miles north), El Capitan (8,085 ft, dramatic escarpment 15 miles south), Salt Basin Dunes (unusual gypsum dunes 10 miles west), Williams Ranch (historic homestead 25 miles southeast), Frijole Ranch Museum (cultural site 10 miles north).
Pine Springs Visitor Center (40 miles): restrooms, water, interpretive exhibits. Supplies: Whites City, New Mexico (50 miles), Van Horn, Texas (60 miles), Dell City, Texas (30 miles). Nearest fuel: Dell City.
Roadside viewing only; no paved trail access to peak. Highway 62/180 pullouts are accessible by standard vehicles. No wheelchair-accessible facilities at viewpoint.
Safe for families viewing from Highway 62/180 or Salt Basin Dunes—no scrambling required. Do not allow children to wander toward cliff edges or unstable terrain. Keep children close during high winds. Water and snacks essential in this remote area.
Guadalupe Peak Viewpoint (nearby restrooms). Pine Springs Campground (40 miles, water and restrooms). Pine Springs Visitor Center (interpretive exhibits, restrooms, water). No food service at viewpoint.
To Park Entrance
Approximately 40 miles from Pine Springs Visitor Center via Highway 62/180 west.
" Visitors appreciate Shumard Peak as a spectacular geological landmark visible from a major highway, requiring minimal effort to view. Most recognize the dramatic tilt of strata and the sharp ridge profile. However, many are initially disappointed that no summit trail exists; managing expectations (emphasizing the superior distance view from Salt Basin Dunes) improves satisfaction. Experienced geology enthusiasts praise the visible reef architecture and fossil-rich strata."
No. No maintained trail reaches the summit. A bushwhack scramble crosses private property and unstable shale; it is not recommended. The peak is legally and safely viewed from Highway 62/180 or the Salt Basin Dunes area to the west.
No. Guadalupe Peak (8,749 ft) is Texas's highest point, located 20 miles north in the same park. Shumard Peak is the third highest.
Limestone and dolomite formed from a Permian reef that grew in a shallow tropical sea 280–250 million years ago. The tilted angle reveals collision-driven uplift 75 million years ago, not water erosion.
Yes, for geology enthusiasts and photographers. The peak offers the best view of the Permian reef's summit expression. Budget 2 hours round trip; combine with Salt Basin Dunes and Guadalupe Peak viewpoint for a full day.
Wind gusts >30 mph occur regularly. Stay in your vehicle during high wind events. Use pullouts designed for viewing—never stop on the shoulder. Afternoon thunderstorms (July–September) pose lightning risk for exposed viewers.
6 listings
3 listings
Information is compiled from official sources, verified traveler reviews, and editorial research. Learn how YourNPGuide works →
We use basic, essential analytics to measure traffic. You can also allow deeper first-party analytics that help us improve our park guides. We never sell your data. Learn more
We use basic, essential analytics to measure traffic, plus optional deeper analytics to improve our park guides. We never sell your data. Choose what you allow. Learn more
Essential analytics that measure basic traffic stay on. The deeper, first-party analytics below are optional — turn on what you are comfortable with. We never sell your data. Read the notice
Site function plus basic visit counts via Google Analytics and Search Console — needed to see how many people visit. Always on.
How far you scroll, whether you finish an article, and which sections are read — so we know which guides to improve.
Clicks on links and buttons, and searches you run on the site — so we can fix confusing navigation and content gaps.