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The spit bar of Calahonda (Granada), together with that one from Roquetas (Almer&#237;a), constitutes one of the best examples in south-eastern Spain. Its development is associated to the different Holocene sea-level oscillations occurred since the last eustatic maximum. Progradation of these spit bars occurs under certain climatic conditions, which have repeated cyclically during Holocene times, giving place to different morphosedimentary units recognized along the whole southern peninsular littoral. In Calahonda, the main development of the spit bar is associated to the second progradation phase, which takes place since ca. 2,400 years.  La flecha litoral de Calahonda (Granada) constituye, junto con la de Roquetas (Almer&#237;a), uno de los mejores ejemplos del sureste peninsular. Su desarrollo est&#225; asociado a las distintas oscilaciones del nivel del mar ocurridas durante el Holoceno, una vez alcanzado el m&#225;ximo eust&#225;tico. En general, se ha visto que la progradaci&#243;n de estas flechas se produce en unas condiciones favorables determinadas, que se han repetido c&#237;clicamente durante el Holoceno, y han quedado reflejadas como diferentes unidades morfosedimentarias, cuyo patr&#243;n de formaci&#243;n es reconocible en todo el sur peninsular. En Calahonda, el principal crecimiento de la flecha litoral est&#225; asociado a la segunda fase de progradaci&#243;n, desarrollada en los &#250;ltimos 2.400 a&#241;os

Fases de programación y evolución morfosedimentaria de la flecha litoral de Calahonda (Granada) durante el Holoceno