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cf. Assilina sp., a genus of fossil marine foraminifera (family Nummulitidae) from the Eocene (Ascaso, Huesca, Spain).

Fossil male freshwater stingray from the eocene period found in the Green River Formation in Wyoming

Fish fossil on sand stone background

Fossil bat from the eocene period found in the Green River Formation in Wyoming

Turó Roig (Red Knoll), conglomerates deposited during the Eocene, Sant Llorenç i l’Obac Natural Park (Barcelona).

A mass of conglomerate deposited during the Eocene (Sant Llorenç i l’Obac Natural Park, Barcelona).

fossil leaf (Cedrelospermum linaetum), Eocene Epoch, Florissant, Colorado

Dramatic Eocene rock formations of the Cingles de Bertí escarpment, Barcelona, Catalonia

A mass of conglomerate deposited during the Eocene (Sant Llorenç i l’Obac Natural Park, Barcelona).

A mass of conglomerate deposited during the Eocene (Sant Llorenç i l’Obac Natural Park, Barcelona).

Fossil Fish from the Eocene Epoch.

Castellsapera rock face, a mass of conglomerate deposited during the Eocene (Sant Llorenç i l’Obac Natural Park, Barcelona).

fish fossil (Priscacara oxyprion)
Eocene Epoch
Warfield Springs Quarry
Kemmerer, Wyoming

Closeup of Middle Eocene highly fossiliferous, limestone representing a carbonate platform facies. It belongs to highly porous Fulra Limestone equivalent to Bassein limestone of Mumbai offshore.

fossil Dawn Redwood (Metasequoia occidentalis), Mid Eocene Epoch, Tranquille Shale, Cache Creek, BC, Canada

Ravines formed by the erosion of Middle Eocene marls (San Vicente Marls, Huesca, Spain).

Falconera Rock, a mass of gray polymictic conglomerate with carbonate conglomerates at the base, deposited during the Eocene (Sant Llorenç i l'Obac Natural Park, Barcelona).

Palaeotherium magnum steilhini, Left Hemimandibula, Upper Eocene, Sossis, Epicentre - Pallars Jussà Visitor Center, Tremp, Lleida, Catalonia, Spain

Ripple marks are sedimentary structures formed by the action of a water current on a substrate of loose sand in shallow water basins or on ancient beaches after waves or turbulence. Fossil ripple marks can be found in the marine Eocene sandstones of the Bages region (Barcelona).

Falconera Rock, a mass of gray polymictic conglomerate with carbonate conglomerates at the base, deposited during the Eocene (Sant Llorenç i l'Obac Natural Park, Barcelona).

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