Флиш (геология) [Nature Category:
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“Флиш е поредица от морски седиментни скали, които са предимно с кластичен произход и се характеризират с редуване на няколко литологични слоя. Независимо от минералогичния състав на слоевете, гранулометричният им състав намалява нагоре по разреза. Общият капацитет на сериите обикновено е няколко хиляди метра. …” (Wikipedia) (Wikipedia translated)
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