Fossils are the preserved remains or traces of ancient organisms. They are usually found in sedimentary rocks, which are formed when sediments containing remains are buried over time. Fossils form when an organism is buried rapidly in sediment before it can fully decay. The sediment hardens to rock and preserves a record of the organism. Index fossils are fossils used to date rock layers because they existed for a short, well-defined period of time. Nummulites are coin-shaped fossils that were commonly found in the Pyrenees mountains, indicating the presence of Tertiary-era sedimentary rocks formed during the Alpine orogeny.