Chapman Peak
Chapman Peak is located in the Livingston Range, Glacier National Park in the U.S. state of Montana. Chapman Peak is situated along the Continental Divide.Climate
Based on the Köppen climate classification, Chapman Peak has in a subarctic climate characterized by long, usually very cold winters, and short, cool to mild summers. Temperatures can drop below −10° F with wind chill factors below −30° F.Geology
Like other mountains in Glacier National Park, Chapman Peak is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks thick, wide and long over younger rock of the cretaceous period.
