Historically, the Mississippi River has replenished sediment across the lower deltaic plain, abating land loss. However, flood-control structures along the river now restrict this natural process and divert sediment from the modern delta offshore to the shelf break, thereby removing it from the coastal system. Localized crevasse splays, however, can deposit significant amounts of...
Authors
N.F. Ferina, J. G. Flocks, Jack L. Kingdinger, M.D. Miner, J. P. Motti, Paul C. Chadwick, James D. Johnston