Belt Supergroup
The Belt Supergroup of rocks is composed mainly of argillite, as well as other metamorphosed or semi-metamorphosed mudstones. This supergroup is mainly exposed in Western Montana, including the Bitterroot Valley and Bitterroot Mountains, Missoula area, Flathead Lake, and Glacier National Park, and is also exposed in parts of Northern Idaho, and British Columbia. Belt Supergroup rocks are also thought to be present in what is now Korea, Northeast China, and Eastern Siberia as well as possibly Australia. Glacier National Park in northwestern Montana and Wolf Creek Canyon along the US Interstate 15 in west-central Montana are well known for their exposed deep purple, wine red, red, blue, turquoise, and green argillites.
Read more about this topic: Argillite
Famous quotes containing the word belt:
“The shore is composed of a belt of smooth rounded white stones like paving-stones, excepting one or two short sand beaches, and is so steep that in many places a single leap will carry you into water over your head; and were it not for its remarkable transparency, that would be the last to be seen of its bottom till it rose on the opposite side. Some think it is bottomless.”
—Henry David Thoreau (1817–1862)