Unit 390
3
Rolling foothill country between Canyon Ferry Reservoir and the Big Belts, moose habitat in scattered timber and creek drainages.
Hunter's Brief
Unit 390 spans rolling terrain along the Missouri River corridor and Canyon Ferry Reservoir, mixing open grasslands with moderate timber in the Big Belt foothills. Elevation ranges from reservoir level to nearly 9,500 feet on upper ridges, creating distinct habitat zones. Access via fair road network allows entry from multiple points, though terrain complexity and elevation change demand solid backcountry navigation. Limited water away from major streams and springs requires careful planning. Moose hunting focuses on riparian areas, willow-choked drainages, and high-country ponds accessed from ridgeline approaches.
- Compact: under 200 sq mi
- Moderate: 200 - 800 sq mi
- Vast: over 800 sq mi
- Few: under 25%
- Some: 25 - 60%
- Most: over 60%
- Limited: under 0.7 mi/mi² (backcountry)
- Fair: 0.7 - 1.5 mi/mi²
- Connected: over 1.5 mi/mi² (well-roaded)
- Flat: under 20% mountains
- Rolling: 20 - 55%
- Steep: over 55%
- Sparse: under 20%
- Moderate: 20 - 50%
- Dense: over 50%
- Limited: under 0.3% area
- Moderate: 0.3 - 2% area
- Abundant: over 2% area
Terrain Deep Dive
Landmarks & Navigation
Major navigational anchors include the Big Belt Mountains as the eastern spine, with recognizable summits like Black Butte Mountain, Cayuse Mountain, and Boulder Mountain providing orientation from both inside and outside the unit. Canyon Ferry Reservoir and the Missouri River form unmistakable western boundaries visible from most vantage points. Key drainages include Woods Creek, Spring Creek, and Sixteenmile Creek serving as natural travel corridors and moose habitat concentrations.
The Townsend Valley to the south and ridgeline systems like Windy Ridge help hunters establish position within complex terrain. These landmarks facilitate navigation in a unit where terrain complexity rewards good map reading.
Elevation & Habitat
The unit spans dramatic elevation change from reservoir level near 3,800 feet to peaks exceeding 9,400 feet. Lower elevations feature sagebrush-grass benches and scattered Douglas fir in the foothills; mid-elevations transition to moderate timber with ponderosa and lodgepole interspersed with meadows; upper reaches become increasingly dense forest with subalpine character. This vertical relief creates distinct hunting zones—open ridges and glassing slopes at mid-elevation, willow-lined creeks in valleys, and high-country parks and ponds where moose concentrate.
The rolling topography means terrain changes frequently over short distances, offering habitat diversity within a compact area.
Access & Pressure
Fair road access via 863 miles of roads provides multiple entry points but scattered distribution means pressure doesn't concentrate heavily anywhere. Populated places like Toston, Ringling, and Lombard serve as staging towns on the periphery. The Fairchild Ditch and other irrigation infrastructure near lower elevations marks developed areas where private land chunks exist.
Terrain complexity and rolling topography create natural compartmentalization—hunters can find solitude by moving away from obvious ridge-top access points into the creek drainages and bench country. Road density suggests moderate access without the heavily-hunted-area feel; hunters willing to navigate complexity encounter fewer competitors.
Boundaries & Context
Unit 390 occupies the transition zone between the Missouri River valley and the Big Belt Mountains across portions of Broadwater, Lewis and Clark, and Gallatin Counties. The unit's western boundary follows the Missouri River and Canyon Ferry Reservoir shoreline, while eastern limits reach into the Big Belt Range proper. Northern margins track the Lewis and Clark-Broadwater County line along ridge systems, and southern boundaries follow Sixteenmile Creek westward to the reservoir.
This geographic position creates a landscape of foothill benches, creek bottoms, and ascending ridge systems that funnel water and wildlife movement predictably.
Water & Drainages
The Missouri River and Canyon Ferry Reservoir dominate water access along western and southern boundaries, providing reliable water for base camps and consistent moose habitat. Interior water is more scattered but significant: Woods Creek, Spring Creek, and Sixteenmile Creek offer perennial flow through lower and mid-elevations, with willow concentrations attractive to moose. Multiple named springs—Franklin, Miller, Dixon, Moonshine, Hard Cash, Big Spring—provide backup water sources though some are seasonal.
Higher elevations contain unnamed ponds and seeps typical of mountain terrain. Water scarcity in mid-elevation benches means planning travel routes along drainage systems where moose naturally concentrate.
Hunting Strategy
Moose in Unit 390 concentrate in willow-choked creeks and riparian areas at lower to mid-elevations, particularly Woods Creek, Spring Creek, and the drainages feeding Sixteenmile Creek. Early season hunting focuses on high-country ponds and parks above 7,000 feet where moose move to escape heat and find better nutrition. Rut period (September-October) drives bulls into willow bottom habitat, making creek drainages and valley floors the target zones.
Ridge systems like Windy Ridge and the Big Belt summits provide excellent glassing platforms for spotting and stocking bulls in open parks and meadows. The rolling terrain demands careful wind reading and quiet stalking through timber; terrain complexity rewards hunters who study topography and use ridgelines for position rather than direct creek approaches. Limited water availability away from major drainages means moose movements are predictable around established springs and seeps.