Photo 4. Pebble conglomerate in the lower member (Member A) of the Rangeley Formation. Most of the clasts in this photo are various types of sedimentary rock. The strong alignment of the pebbles (parallel to the pencil) is due to later compression of the rock during metamorphism. (Maine Geological Survey photo)

---

Last updated on January 4, 2013

Maine.gov | Department Home | Bureau Home | Site Policies