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There are several conspicuous dead or alive 5 ultimate parts to a beach that relate dead or alive 5 ultimate to the processes that form and dead or alive 5 ultimate shape it. The part mostly above water (depending upon tide), and more or dead or alive 5 ultimate less actively influenced by the waves at some point in the tide, dead or alive 5 ultimate is termed the beach berm. The berm is the dead or alive 5 ultimate deposit of material comprising the active shoreline. dead or alive 5 ultimate The berm has a crest (top) and a face—the latter dead or alive 5 ultimate being the slope leading down towards the water dead or alive 5 ultimate from the crest. At the very bottom of the face, there dead or alive 5 ultimate may be a trough, and further seaward one or more long shore bars: slightly raised, underwater embankments formed where the waves first start to break.

The sand deposit may extend well inland from the berm crest, where there may be evidence of one or more older crests (the storm beach) resulting from very large storm waves and beyond the influence of the normal waves. At some point the influence of the waves (even storm waves) on the material comprising dead or alive 5 ultimate the beach stops, and if the particles are small enough (sand size or smaller), winds shape the feature. Where wind is the force dead or alive 5 ultimate distributing the grains inland, the deposit behind the beach becomes a dune.

These geomorphic features dead or alive 5 ultimate compose what is called the beach profile. The beach profile changes seasonally due to the change in wave energy dead or alive 5 ultimate experienced during summer and winter months. In temperate areas where summer is characterised by dead or alive 5 ultimate calmer seas and longer periods between breaking wave crests, the beach profile is higher in summer. The gentle wave action during this season tends to dead or alive 5 ultimate transport sediment up the beach towards the berm where it is deposited and remains while the water dead or alive 5 ultimate recedes. Onshore winds carry it further inland forming and enhancing dunes.