John Muir compared the area with
Yosemite Valley for its similar geology and glacial morphology. Light-colored
granite, about 50 to 70 million years old (
Eocene Epoch to
Cretaceous Period) has been sculpted by
glaciers that gouged deep U-shaped troughs throughout the monument. Many of the glacial valleys are filled with sea water and are called "canals", but they are not man-made in any way; the walls of these
fjords are near-vertical and often rise 2,000 to 3,000 feet (600 to 900 m) above sea level, and drop 1,000 feet (300 m) below it. Across from the Salmon River and Portland Canal and the settlement of
Hyder, Alaska, small glaciers occupy high areas of the northeast part of the monument. Soule and Through Glaciers cover high plateaus and valleys in the Lincoln and Seward Mountains, where one peak rises to 6,250 feet (1,900 m) above
sea level. Most mountain tops in the monument are in the 4,000 to 5,000 foot (1,200 to 1,500 m) elevation range. The
tree line is usually around 2,700 feet (800 m). ==Ecology==