London Clay

1,018 distinct taxa, from 2,027 fossil occurrences the Paleobiology Database records under this name, spanning 56–34 Mya.

England, Kent, Hampshire, Sussex · UK

1,018 taxa · 2,027 fossils · 56–34 Mya

Filed under the Thames Group. Members recorded: Division C, Tilehurst, Middle Clay, Walton, division D-E, E, Swanscombe.

Macrostrat places this rock in the Thames Group, and dates it 56–48 Ma. Macrostrat’s own record

London Clay — 51.43°N, 2.00°WLondon Clay — 51.40°N, 0.83°ELondon Clay — 50.83°N, 0.78°WLondon Clay — 50.89°N, 1.28°WLondon Clay — 51.73°N, 0.48°ELondon Clay — 50.78°N, 0.65°WLondon Clay — 51.08°N, 1.17°WLondon Clay — 51.23°N, 0.85°WLondon Clay — 51.25°N, 0.75°ELondon Clay — 52.00°N, 0.82°ELondon Clay — 51.32°N, 0.90°ELondon Clay — 52.02°N, 1.43°ELondon Clay — 51.42°N, 0.75°WLondon Clay — 51.78°N, 1.17°ELondon Clay — 51.45°N, 0.13°WLondon Clay — 51.50°N, 0.75°ELondon Clay — 51.83°N, 1.25°ELondon Clay — 51.62°N, 0.32°WLondon Clay — 51.67°N, 0.40°WLondon Clay — 51.78°N, 2.27°WLondon Clay — 51.37°N, 1.13°ELondon Clay — 50.63°N, 3.47°WLondon Clay — 50.93°N, 1.48°WLondon Clay — 51.41°N, 0.53°ELondon Clay — 51.51°N, 0.24°ELondon Clay — 51.72°N, 0.79°ELondon Clay — 51.53°N, 0.31°ELondon Clay — 51.37°N, 1.14°WLondon Clay — 51.51°N, 0.19°WLondon Clay — 51.42°N, 0.90°ELondon Clay — 51.58°N, 0.05°WLondon Clay — 51.46°N, 0.30°WLondon Clay — 51.29°N, 1.05°WLondon Clay — 51.28°N, 0.99°WLondon Clay — 51.63°N, 0.16°WLondon Clay — 51.94°N, 1.27°ELondon Clay — 51.35°N, 1.21°WLondon Clay — 50.87°N, 0.95°WLondon Clay — 51.27°N, 0.40°WLondon Clay — 51.38°N, 0.24°WLondon Clay — 51.65°N, 0.07°ELondon Clay — 51.53°N, 0.70°ELondon Clay — 51.25°N, 0.93°WLondon Clay — 51.90°N, 1.62°WLondon Clay — 50.80°N, 1.67°WLondon Clay — 51.07°N, 1.74°WLondon Clay — 51.64°N, 0.78°ELondon Clay — 50.67°N, 1.33°WLondon Clay — 51.70°N, 0.27°ELondon Clay — 51.71°N, 0.74°ELondon Clay — 51.37°N, 1.04°ELondon Clay — 51.35°N, 1.00°ELondon Clay — 51.40°N, 0.70°ELondon Clay — 50.67°N, 1.57°W

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54 distinct localities, where the rock is now rather than where it was laid down. Tectonics draws the world it belonged to.

When

What has been found

The 40 most often recorded, of 1,018.

What else lived thenRank the rock of a period

Counts are of occurrence records, which measure the rock and the fieldwork together.