— — the wall of granite that catches the last of the light.
“The east face of the Bitterroot rises straight from the valley floor west of Stevensville, glaciated canyons cut between the high points. The range marks the Idaho line and runs more than a hundred miles north to south. At Stevensville, the oldest town in Montana, the wall takes the evening light and holds it long after the valley below has cooled.
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The Bitterroot Range forms the western wall of the Bitterroot Valley and the Montana–Idaho border for more than one hundred and forty miles. The east face rises sharply from the valley floor near Stevensville, carved into a row of U-shaped canyons (Bass, Kootenai, Big, and Sweathouse) by Pleistocene glaciers. Trapper Peak, the high point at 10,157 feet, sits south of Stevensville. Stevensville itself was founded in 1841 around St. Mary's Mission by the Jesuit Pierre-Jean De Smet and is the oldest permanent settlement in Montana.
The range is built largely of the Idaho Batholith, a 70-million-year-old body of granite that crystallised deep underground and was lifted to the surface as the surrounding sedimentary rock eroded away. Glaciers in the last ice age carved the east face into a row of canyons separated by knife-edge ridges. The granite weathers slowly and holds its lines; climbers on the faces above Blodgett Canyon work some of the longest granite walls in the lower forty-eight outside of Yosemite.
The Bitterroot Valley runs north to south, and the range catches the late afternoon and evening light along its full east face. From Stevensville the wall sits about ten miles west across the valley floor at roughly 3,300 feet, while the ridges rise to over nine thousand feet. Alpenglow on the granite reads pink in late summer and orange in winter, and the last light often holds on the highest snow long after the valley itself has gone into shadow.