Considerable research has been conducted on the upstream effects of dam installation, particularly sedimentation of reservoirs. The principal sedimentation processes in reservoirs is deposition of coarser sediment in the delta and deposition of fine sediment in the reservoir through either stratified or homogenous flow (depending on reservoir geometry and sediment concentration). Other processes such as landslides and shoreline erosion also play

a role in reservoir dynamics. Reservoir sedimentology and governing geomorphic processes forming various zones (headwater deltas, deep water fine-grained deposits, and turbidity currents) are generally well-characterized (Vischer and Hager, 1998 and Annandale, 2006), and quantified

(Morris and Fan, 1998 and Annandale, LGK-974 in vitro 2006). Despite significant advancements in the knowledge of downstream and upstream impacts of dams, they are often considered independent of one another. The current governing hypothesis is that the effects of dams attenuate in space and time both upstream and downstream of a dam INK128 until a new equilibrium is reached in the system. But given the extremely long distances required for attenuation this gradual attenuation may frequently be interrupted by other dams. Our GIS analysis of 66 major rivers in the US shows, however, that over 80% have multiple dams on the main stem of the river. The distance between the majority of these dams is much closer than the hundreds of kilometers that may be required for a downstream reach to recover from an upstream dam (Williams and Wolman, 1984, Schmidt and Wilcock, 2008 and Hupp et al., 2009). For example, Schmidt and Wilcock (2008) metrics for assessing downstream impacts predict degradation of the Missouri River near Bismark, ND, but aggradation has occurred because of backwater effects of the Niclosamide Oahe. We hypothesize that where dams that occur in a longitudinal sequence, their individual effects interact in unique and complex ways with distinct morphodynamic consequences. On the Upper Missouri River,

the Garrison Dam reduces both the supply and changes the size composition of the sediment delivered to the delta formed by the reservoir behind the Oahe Dam. Conversely, the backwater effects of the Oahe Dam cause deposition in areas that would be erosional due to the upstream Garrison Dam and stratifies the grain size deposition. These effects are further influenced by large changes in water levels and discharge due to seasonal and decadal changes in dam operations. This study introduces the concept of a distinct morphological sequence indicative of Anthropocene Streams, which is referred to as an Inter-dam sequence. Merritts et al. (2011) used the term ‘Anthropocene Stream’ to refer to—a stream characterized by deposits, forms and processes that are the result of human impacts.