In sedimentary sequences, a bed generally represents a single deposition event: a period of time in which the conditions of sedimentation in a basin remained constant, resulting in a layer with characteristic composition and structures that can be distinguished from the underlying and the overlying beds. Amalgamated beds are an exception. Amalgamation occurs in high-energy environments characterized by alternating phases of erosion and deposition, for example alluvial plains or turbidite fans. Amalgamated beds form when two or more layers with similar composition are merged together due to the presence of one (or more) erosional surfaces. The resulting amalgamated bed may apparently look as the result of a single deposition event, since it shows similar sedimentary structures, lithology, and grain size along its thickness. Amalgamated beds can be distinguished based on the recognition of erosional surfaces, sharp and sudden changes in grain size or inconsistent sequences of sedimentary structures within the same bed. Amalgamated beds are relatively common in coarse-grained sandstone and conglomerate sequences which deposit in high-energy environments.