Unit 76

The Preuss Range and Webster Range anchor the eastern terrain, while the Fox Hills and Aspen Range provide relief throughout the unit. Notable passes including White Pass, Suicide Pass, Geneva Summit, and Freeman Pass serve as natural travel corridors and navigation landmarks. Mahogany Ridge and Tygee Ridge offer glassing platforms for surveying adjacent country.

Swan Lake and Merkley Lake mark water features visible from distance. The Ponds, Dingle Swamp, and numerous canyon systems including Rattlesnake Canyon and Wood Canyon create topographic character for route-finding and understanding movement corridors.

Elevations span from the mid-5700s to just under 10,000 feet, creating a landscape dominated by mid-elevation terrain. Lower basins feature sagebrush flats and grasslands, while ridges and slopes support moderate stands of aspen, lodgepole pine, and Douglas fir. Higher terrain above 8,500 feet transitions to more sparse, windswept forest and alpine meadows.

The moderate forest coverage means much of the country remains relatively open, particularly in the numerous valleys and basin floors, creating strong glassing country mixed with pockets of timber for cover and thermal refugia.

Over 2,300 miles of roads crisscross the unit, indicating well-distributed vehicle access and high connectivity. Towns including Dingle, Alton, Border, and Condaprovidlogistical support close to the unit. Road density supports fair public access to most ridges and valleys, though actual pressure depends on seasonal timing and weather.

The terrain's size and rolling nature means vehicle access doesn't guarantee crowding—many hunters concentrate near obvious trailheads and maintained roads, leaving quieter country for those exploring less obvious drainages and ridges away from main spines.

Unit 76 encompasses portions of Bear Lake and Caribou counties in southeastern Idaho, spanning the Bear Lake Plateau and surrounding mountain terrain. The unit occupies high plateau country—a vast rolling landscape defined by ridges, valleys, and basins rather than dramatic peaks. Geography here centers on the transition zone between the Bear Lake Valley to the west and higher mountain country to the east, with multiple gaps and passes providing natural travel corridors.

The terrain is substantial in scale and supports a network of ranches, small communities, and access roads throughout the footprint.

Water is reasonably reliable throughout the unit, with multiple springs including Woodall Spring, Formation Spring, and Cold Spring scattered across ridges and flats. Slug Creek, Fish Haven Creek, Paris Creek, and Dry Fork provide seasonal to perennial flow in major drainages. Sheep Creek Reservoir, Lakey Reservoir, Montpelier Reservoir, and Cranes Reservoir add static water sources on higher terrain.

Spring Creek and Montpelier Creek run reliable enough to support ranch operations. The moderate water rating reflects this distribution—water exists but requires understanding creek systems and spring locations rather than following obvious riparian corridors.

The Bear Lake Plateau supports elk, mule deer, and moose habitat across its elevation bands. Lower basin and foothill country favors mule deer in sagebrush and scattered timber, particularly during early and late seasons. Mid-elevation aspen and lodgepole forests provide thermal cover and summer range for elk.

Higher ridges above 8,500 feet can be productive during summer for migratory animals, though early winter weather can close high terrain quickly. The numerous water sources and moderate timber distribution create natural concentration points—glassing from ridge systems like Mahogany Ridge toward basins below remains a productive approach. Spring dispersal and fall migration patterns are key; this country funnels animals through specific valleys and drainages as seasons change.