Oxfordian

Intervalle géologique

5 image(s) · 0 Actualités

Voir la fiche

Galerie d'images

Upper Jurassic (Oxfordian) sedimentary rock layers at the base of a cliff at low tide at Filey Brigg in North Yorkshire, England.

Upper Jurassic (Oxfordian) sedimentary rock layers at the base of a cliff at low tide at Filey Brigg in North Yorkshire, England.

Royaume-Uni Jurassique Oxfordian
The Géoscope at the motorway service station, La Lozère, displays a collection of rocks found in Lozère. Each has a description.


Limestone (beige) Oxfordian
Provenance:La Canourgue, Lozère

The Géoscope at the motorway service station, La Lozère, displays a collection of rocks found in Lozère. Each has a description. Limestone (beige) Oxfordian Provenance:La Canourgue, Lozère

description Oxfordian
Cliff at Filey Brigg in North Yorkshire, England (at low tide). Soft Quaternary deposits lie on top of horizontal layers of Upper Jurassic (Oxfordian) sedimentary rocks.
Intervalles Oxfordian

Cliff at Filey Brigg in North Yorkshire, England (at low tide). Soft Quaternary deposits lie on top of horizontal layers of Upper Jurassic (Oxfordian) sedimentary rocks.

Royaume-Uni Jurassique Oxfordian Quaternaire
Partial skull and anterior cervical vertebrae of unidentified pliosaurid plesiosaurian (MPPL 18797) from the uppermost Callovian–middle Oxfordian of Kaberlaba (Asiago, Italy), in left lateral view. Photograph (A) and explanatory drawing (B). White, preserved bone surfaces; dark grey, preserved margins of skull fenestrae; light grey, eroded bone surface; cross hatching, broken bone.
Taxons Anguanax

Partial skull and anterior cervical vertebrae of unidentified pliosaurid plesiosaurian (MPPL 18797) from the uppermost Callovian–middle Oxfordian of Kaberlaba (Asiago, Italy), in left lateral view. Photograph (A) and explanatory drawing (B). White, preserved bone surfaces; dark grey, preserved margins of skull fenestrae; light grey, eroded bone surface; cross hatching, broken bone.

os dessin Italie Callovien +6
Oxfordian (Upper Jurassic) cyclic sediments at Péry-Reuchenette, near Tavannes, kanton Bern, Switzerland. Alternating layers are limestone (light, more competent) and marl/clay; dominant cycle is the 200.000 year-cycle.
Formations Reuchenette

Oxfordian (Upper Jurassic) cyclic sediments at Péry-Reuchenette, near Tavannes, kanton Bern, Switzerland. Alternating layers are limestone (light, more competent) and marl/clay; dominant cycle is the 200.000 year-cycle.

Suisse Reuchenette Jurassique Oxfordian