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The soil of intermountain basins usually consists of clay, gravel, sand, silt, and volcanic ash, much of it laid down by lakes which covered the region during the Oligocene 33 to 23 million years ago.The glaciated plains are generally covered in clay, gravel, sand, and silt left by the proglacial Lake Great Falls or by moraines or gravel-covered former lake basins left by the Wisconsin glaciation 85,000 to 11,000 years ago.Flowers native to Montana include asters, bitterroots, daisies, lupins, poppies, primroses, columbine, lilies, orchids, and dryads.Several species of sagebrush and cactus and many species of grasses are common.
Other major reservoirs include Hungry Horse on the Flathead River; Lake Koocanusa on the Kootenai River; Lake Elwell on the Marias River; Clark Canyon on the Beaverhead River; Yellowtail on the Bighorn River, Canyon Ferry, Hauser, Holter, Rainbow; and Black Eagle on the Missouri River.The name Montana was added to a bill by the United States House Committee on Territories, which was chaired at the time by Rep.James Ashley of Ohio, for the territory that would become Idaho Territory.The watersheds divide at Triple Divide Peak in Glacier National Park.
The Pend Oreille River forms the outflow of Lake Pend Oreille.
The area west of the divide has a modified northern Pacific coast climate, with milder winters, cooler summers, less wind and a longer growing season.