Mount Pennell Wilderness Study Area is a remote wilderness study area in Utah, characterized by its rugged and diverse terrain. This region encompasses significant elevation changes, from deep canyons to the slopes of Mount Pennell, the second-highest peak in the Henry Mountains at 11,413 feet (3,478 meters). The landscape features varied forests of oak, Ponderosa pine, and subalpine species, creating four distinct biological life zones that support numerous outdoor activities. Its geology, including Mount Pennell as a laccolith, contributes toβ¦
6
Routes
5
(2)
Average rating
41
People visited

3
hikers
24.8km
08:51
470m
470m
Hard hike. Very good fitness required. Sure-footedness, sturdy shoes and alpine experience required.

24.0km
09:01
400m
740m
Hard hike. Very good fitness required. Sure-footedness, sturdy shoes and alpine experience required.

5.0
(1)
16
hikers
15.2km
04:12
270m
260m
Moderate hike. Good fitness required. Easily-accessible paths. Suitable for all skill levels.

8
hikers
24.1km
06:33
350m
350m
Hard hike. Very good fitness required. Easily-accessible paths. Suitable for all skill levels.
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Mount Pennell Wilderness Study Area offers opportunities for outdoor activities, primarily hiking. The area is characterized by its rugged and remote terrain, with significant elevation changes and diverse natural features. Visitors can explore deep canyons and ascend to expansive viewpoints.
The terrain in Mount Pennell Wilderness Study Area is rugged and remote, featuring deep canyons and significant elevation changes. Mount Pennell itself rises to 11,413 feet (3,478 meters). The landscape includes varied forests of oak, Ponderosa pine, subalpine fir, spruce, Douglas fir, and aspen.
Yes, a komoot guide titled Hiking in Mount Pennell Wilderness Study Area is available. This guide provides information for those interested in exploring the area's trails. The region is known for its challenging and remote hiking environment.
Mount Pennell Wilderness Study Area features Mount Pennell, the second-highest peak in the Henry Mountains, and diverse forests across four distinct biological life zones. The area also includes deep canyons and offers expansive views. Mount Pennell is a notable geological laccolith formation.
The most favorable seasons for visiting Mount Pennell Wilderness Study Area are spring and fall. The region experiences a cold semi-arid climate. These seasons generally offer more moderate conditions for outdoor activities.
Mount Pennell Wilderness Study Area is home to a variety of wildlife. Portions of the area serve as summer range for the Henry Mountain bison herd, with bison frequently sighted near 'The Horn.' Other species include cougar, peregrine falcons, and bald eagles.
Komoot users have rated activities in Mount Pennell Wilderness Study Area with an average of 5.0 out of 5 stars. This rating is based on more than 2 reviews from over 40 visitors who have shared their experiences in the area.
Access to the Henry Mountains, including Mount Pennell Wilderness Study Area, is often limited. A four-wheel-drive vehicle is typically required due to generally steep, rocky, narrow, and natural-surface roads. Cell service in the area is unreliable.
Mount Pennell Wilderness Study Area is managed by the Bureau of Land Management (BLM). Visitors should contact the BLM for specific information regarding permits for camping or other activities. Regulations may vary and should be confirmed prior to a visit.
Mount Pennell Wilderness Study Area is managed by the Bureau of Land Management (BLM). The Henry Mountains Field Station can be reached at +1-435-542-3461. Additional information is available on the official BLM website for the area.
Mount Pennell is the second-highest peak in the Henry Mountains, reaching an elevation of 11,413 feet (3,478 meters). The wilderness study area encompasses significant elevation changes, with nearly 5,000 feet between its lowest and highest points.
Mount Pennell is geologically significant as a laccolith, a type of igneous rock intrusion. This geological term was first applied to formations in the Henry Mountains by geologist Grove Karl Gilbert in the late 19th century. This unique formation contributes to the area's distinct landscape.

