Unit 2

Chimney Rock and Hanging Rock anchor navigation in the mid-elevations, while The Wall and Chinese Wall ridge systems provide major terrain features visible across drainages. Fishhawk Glacier and surrounding alpine basins mark the highest terrain. Major stream corridors—Glacier Creek, Howell Fork, Rampart Creek, and Torrent Creek—serve as natural travel lines through the mountains.

Crow Creek Pass, Reservation Peak, and Sunlight Peak are prominent reference points. These features aid glassing opportunities and navigation through terrain that otherwise offers few obvious corridors.

Terrain transitions from creek-bottom valleys through dense conifer zones into open high alpine. The median elevation near 8,300 feet reflects predominantly subalpine and alpine habitat. Lower canyons feature spruce-fir forests with moderate canopy; these thin dramatically at higher elevations, yielding to scattered krummholtz, grassland benches, and exposed ridgelines.

Glacial basins like Glacier Basin and Silvertip Basin sit in the upper terrain, while lower meadows such as Grinnell and Eagle Creek Meadows provide openings in the forest. This layered elevation structure creates distinct seasonal corridors and pressure zones.

Nearly 500 miles of road exist in the unit, but density distribution favors lower valleys and canyon systems. Highway access via Wyoming 120 and approach roads to Wapiti and Pahaska Tepee provide staging areas, though terrain steepness means most roads concentrate in lower elevations. Fair accessibility to valley bottoms contrasts sharply with steep mountain sections requiring foot travel.

The complexity and remoteness of higher terrain likely draws lighter pressure than more accessible units, but canyon approaches funnel hunters into predictable corridors. Pressure concentrates where roads end.

Unit 2 encompasses the North Fork Shoshone River drainage and north-facing slopes of the Shoshone River watershed west of Highway 120, extending to include Mountain Creek and Escarpment Creek outside Yellowstone. The unit occupies high country on the western slope of the Absaroka Range, with the eastern boundary anchored by the Park itself. Lower elevations sit around 4,800 feet in the canyon bottoms and valleys; terrain climbs sharply into alpine ridges exceeding 12,000 feet.

The sheer elevation gain and rugged topography characterize this vast, wilderness-scale territory.

The North Fork Shoshone River and its tributaries—Glacier Creek, Howell Fork, Jones Creek, Torrent Creek—provide reliable water through the main valleys and lower elevations. However, above the subalpine zone, dependable water becomes scarce. Springs like De Maris Springs, Blue Springs, and Needle Hot Springs offer supplemental sources, though their seasonal reliability varies.

Buffalo Bill Reservoir lies adjacent in lower country. Higher basins and ridges require understanding spring locations and creek flow patterns. Water scarcity at elevation fundamentally shapes hunting strategy and camp placement.

Wolf presence defines this unit's context; tracking drainages where game congregates around water becomes critical. The steep terrain creates natural migration corridors—animals move vertically with season and weather, using lower valleys in late season and ridge systems in early fall. Creek bottoms like the North Fork and Shoshone offer travel corridors where predators and prey concentrate.

Higher basins provide escape terrain and summer range. Successful hunting requires understanding elevation movements, scout from ridges like The Wall and Chinese Wall for distant glassing, then commit to steep foot travel. Fitness and route-finding are prerequisites in terrain this complex and remote.