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