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Stacking of fluvial channel filled by polygenic conglomerate encased within floodplain facies (Lower transgressive system tract). The Montserrat Conglomerate formation are a Middle Eocene Deposit (Upper Lutetian-Bartonian). Montserrat, Spain.
PhotoID401

Stacking of fluvial channel filled by polygenic conglomerate encased within floodplain facies (Lower transgressive system tract). The Montserrat Conglomerate formation are a Middle Eocene Deposit (Upper Lutetian-Bartonian). Montserrat, Spain.
PhotoID401

Photograph: D. Pieruccioni