Flood deltas, which form on the open sea side, are subject to the interaction between sea-waves and tidal processes. The tombolos may be simple or compound double or triple , depending on whether they are formed by one or more strands. Without exhumation, in general, there is no unconformity, since there is no hiatus. It corresponds to a significant of sea level fall, in which the eustatic absolute sea level parameter is very important. In strata or groups of successive dipping beds deposited on each other progradationally basinward lateral accretion or outbuilding , the lower terminations are downlaps.
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