
(Oldhaven Beds) - 2005
The London Clay is exposed at the extreme West end of the bay, the exposures are not very good, although there are some excellent exposures further west at 'Seasalter'. The bay runs from youngest to the East to Oldest to the West.
West of the carpark, the Oldhaven beds are well exposed on the foreshore, these beds are marked by a pebble bed at the base. This pebble bed contains black flint pebbles in a buff yellow sandy matrix, which cuts down into the underlying Woolwich Beds.
The Woolwich and Reading beds are below this but are rarely exposed. Well-bedded clays are crowded with brackish water shells.
To the East of the bay, the Thanet beds are both exposed as clays on the foreshore and sands within the cliff section.

How Herne Bay looked during the Eocene - Green Turtle
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How Herne Bay looked during the Eocene - Sting Ray
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How Herne Bay looked during the Eocene - White Shark
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How Herne Bay looked during the Eocene - Grey Nurse Shark
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How Herne Bay looked during the Eocene
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Palaeogene |
Oligocene |
Chattian |
23.8 to 28.5 |
| Rupelian |
28.5 to 33.7 |
Eocene |
Priabonian |
33.7 to 35.5 |
| Bartonian |
35.5 to 40.5 |
| Lutetian |
40.5 to 49.5 |
| Ypresian |
49.5 to 54.8 |
Paleocene |
Thanetian |
54.8 to 57.0 |
| Selandian |
57.0 to 60.5 |
| Danian |
60.5 to 65.0 |
|
1:250 000 Geological Map of Herne Bay
Geological Maps are sold either Flat or Folded for Solid, or Seabed geology. Special editions may be available for certain locations. For a complete list click the link below.
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1: 50 000 Geological Map of Herne Bay
Geological Maps are sold either Flat or Folded for Solid, Drift or combined geology. Special editions may be available for certain locations. For a complete list of
1: 50 000 maps, click the link below.
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