Ingression

from Wikipedia, the free encyclopedia

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.