Ingression
In contrast to transgression, an ingression denotes a particularly slow, “tentative” advance of the sea onto the mainland. Ingressions arise from the rise in sea level or the lowering of land masses. Areas affected by ingressions are called ingression coasts . Characteristic for ingressions is a transition from freshwater ( limnic - fluvial ) and mainland sediments to marine sediments in the deposition sequence of sedimentary rocks without special transgression horizons such as e. B. Conglomerates have been handed down.
literature
- H. Murawski, W. Meyer: Geological dictionary. 10th edition, Enke-Verlag, Stuttgart 1998, 278 p., 82 fig., 7 tab.