East Mersea can be very popular in the summer, as it is a beautiful area, not far from Colchester. The foreshore is made up of London Clay, with a few sharks’ teeth to be found. This site is also well documented for OIS5 and OIS6 Pleistocene deposits, rich in (among other things) the teeth from small mammals and the shells of molluscs.
♦ Mersea Island is not that well signposted and the only practical way of getting there is through the middle of Colchester. Therefore maps and a GPS device are ideal for getting to and around the island. Once on the island, there is only two ways to go – west to the main town or east to the more scenic areas.
♦ Head east, following the road until you reach a bend with Cudmore Grove Country Park signposted ahead. Take this road and it will lead to a large car park. From here, walk to the foreshore and head southwest (to the right).
♦ 51.79041°N, 0.99496°E
FIND FREQUENCY: ♦♦♦♦ – Fossils from the London Clay are not that common, although collecting during spring and autumn scouring is quite productive. However, this location is well documented for small mammals from the Pleistocene deposits, especially if you wet sieve samples onsite or at home.
CHILDREN: ♦♦♦♦ – East Mersea is suitable for children. There is plenty of grass to play on, a picnic area, toilets and a sandy area on the beach. However, keep away from the mud flats.
ACCESS:♦♦♦ – Once on the island, there is good access to the fossil sites, with toilets, a cafe and a picnic area at the car park. Getting to the island through Colchester is the only challenge.
TYPE: – Most fossils are found on the foreshore by searching in the areas of shingle or in the London Clay mud flats. Some of these areas can be dangerous, so stick to the harder clay areas. Samples of sediments can be taken from the foreshore Pleistocene channels for sieving at home, which are rich in small mammals.
The vast majority of people visiting this site will be interested in the London Clay exposures at the western end of the cliff. As with all London Clay sites, the most common finds are sharks’ teeth, although the site is not particularly good in this respect.
However, East Mersea is also well documented for its Pleistocene deposits, which are rich in small mammals. These deposits form a channel near to Cudmore Grove Country Park on the foreshore and, if you sieve samples, you can find several rodent species. These are from an interglacial period during the Pleistocene and dating from OIS9. Freshwater molluscs are also common from these deposits. Further west, another deposit dating from OIS5 contains hippopotamus remains, but this is below the level of the beach. Keep an eye out for Bronze Age flint artefacts, which can also be found at East Mersea.
The foreshore at East Mersea has extensive deposits of London Clay (Eocene ~50 mya), forming the ‘Mersea Flats’, which are a haven for birds and other wildlife. East Mersea is also well documented for its Pleistocene interglacial sediments. A channel filled with these sediments dates from OIS9 and is exposed on the foreshore at Cudmore Grove Country Park. Further west, a second deposit from the OIS5 interglacial stage has yielded hippopotamus remains, but is beneath the level of the beach.
Common sense when collecting at all locations should be used and prior knowledge of tide times is essential. At East Mersea, the main danger is the mud flats. Take extra care when looking for fossils on the foreshore, as some areas are extremely muddy and it is easy to become stuck. Do not venture too far out. Generally, you can see the hard, safe areas, as the clay is well exposed, but there are sometimes areas of soft mud.
Most fossils are found simply by walking along the foreshore. Any larger bones you find may need a small spade to dig them out of the mud.
This site is a site of special scientific interest (SSSI). This means you can visit the site, but hammering the bedrock is not permitted. For full information about the reasons for the status of the site and restrictions, download the PDF from Natural England.