thumb|Mount Stuart and the Stuart Range
thumb|right|300px|Stuart Range from Cashmere Peak in the [[Wenatchee Mountains]]
thumb|right|300px|[[Argonaut Peak, left center; Colchuck Peak, center; Dragontail Peak, right center; from the southwest]]
The Stuart Range is a mountain range in central Washington, United States. The range lies within the eastern extent of the Cascade Range immediately southwest of Leavenworth and runs east–west. The western peaks make up a single sharp ridge. The eastern half of the range splits into two parallel ridges, the northern of which is known as the Enchantment Peaks. Between these ridges lies the Enchantment Basin, which holds the dozens of tarns known as the Enchantment Lakes.
- Sherpa Peak - -
- Argonaut Peak - -
- Colchuck Peak - -
- Dragontail Peak - -
Eastern peaks of south ridge
- Witches Tower - -
- Little Annapurna - -
- McClellan Peak - -
- Rocket Peak - -
- Gremlin Peak - -
Enchantment Peaks (eastern peaks of north ridge)
- Colchuck Balanced Rock - + -
- Cannon Mountain - -
- Enchantment Peak - + -
- Prusik Peak - -
- The Temple - -
Geology
The Mount Stuart batholith underlies the Stuart Range and the nearby Wenatchee Mountains. The batholith is about 13 by 16 miles in extent. Two plutonic masses are separated by a thin screen of Chiwaukum Schist and rocks of the Ingalls Complex. The more-eastern pluton is 93 million years old, while the more-western rock mass is between 83 and 86 million years old. Exposed rock tends to be quartz diorite and granodiorite.