sand spit and lagoon: a sandspit begins where there is a change in the direction of a coastline, long shore drift loses some of its energy and deposits material at a faster rate than it can be removed. gradually, these deposits build up, spit extends further across bay. if sand spit continues to grow, it will reach far side of bay to form a sandbar. a lagoon is formed. over time the lagoon begins to fill with silt and mud from rivers that may flow into it.