The range has a north-south length of about 28 miles (45 km) .
The northeast has an off-lying triangular mountain section which causes the north of Beaver Valley to bifurcate.
East of the mountain section, I-15 transits to Sulphurdale.
The section contains many peaks, with the highest being Gillies Hill, 7,888 feet (2,404 m).
The southwest side of the section contains south-flowing Cunningham Wash.
The south-southeast side of the range is a straight stretch from Cunningham Wash, north and the Minersville Reservoir, south, a collection of numerous watercourses from Beaver Valley, and neighboring mountains.
Beaver River (Utah) enters the reservoir and leaves flowing due-west at the southern Mineral Mountains terminus.
The terminus of the range comes to a V-shaped point; the river stretch, and mountains, are only 4-mi wide from the outlet of the Beaver River at the reservoir.
The range then immediately turns into a stretch of southwest foothills, also a short stretch, only about 9-mi long.

The northwest stretch begins at that point, about 7 or 8-mi southeast of Milford; it transits to an east-west stretch at the north, which continues to the outlying mountain section east, and its junction with the west flank of the Pavant-Tushar Mountains massif.

A small, narrow 3-mile (4.8 km) wide ridgeline feeds north-northwest from the north stretch; it extends about 6-mi toward the Black Rock Desert volcanic field region, and contains Pinnacle Pass, and a highpoint of Antelope Mountain, 7,230 feet (2,200 m).
The range has a north-south length of about 28 miles (45 km) . The northeast has an off-lying triangular mountain section which causes the north of Beaver Valley to bifurcate. East of the mountain section, I-15 transits to Sulphurdale. The section contains many peaks, with the highest being Gillies Hill, 7,888 feet (2,404 m). The southwest side of the section contains south-flowing Cunningham Wash.
The south-southeast side of the range is a straight stretch from Cunningham Wash, north and the Minersville Reservoir, south, a collection of numerous watercourses from Beaver Valley, and neighboring mountains. Beaver River (Utah) enters the reservoir and leaves flowing due-west at the southern Mineral Mountains terminus. The terminus of the range comes to a V-shaped point; the river stretch, and mountains, are only 4-mi wide from the outlet of the Beaver River at the reservoir. The range then immediately turns into a stretch of southwest foothills, also a short stretch, only about 9-mi long.
The northwest stretch begins at that point, about 7 or 8-mi southeast of Milford; it transits to an east-west stretch at the north, which continues to the outlying mountain section east, and its junction with the west flank of the Pavant-Tushar Mountains massif.
A small, narrow 3-mile (4.8 km) wide ridgeline feeds north-northwest from the north stretch; it extends about 6-mi toward the Black Rock Desert volcanic field region, and contains Pinnacle Pass, and a highpoint of Antelope Mountain, 7,230 feet (2,200 m).
Mineral Mountains (Utah)