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Shakespeare Cliff (Samphire Hoe), Dover, Kent, England, UK

This page kindly sponsored by Sussex Mineral & Lapidary Society
 
Latitude & Longitude (WGS84): 51° 6' 28'' North , 1° 16' 56'' East
Latitude & Longitude (decimal): 51.1079766617, 1.28224987356
UK National Grid Reference:TR300393


Chalk boulders at the base of Shakespeare Cliff on beach to the east of the car park and Channel Tunnel works at Samphire Hoe.

This locality is frequently referred to as "Samphire Hoe", more for convenience than through accuracy. Samphire Hoe is 'reclaimed' land produced by dumping the waste rock from the digging of the Channel Tunnel, and this is mostly landscaped and enclosed within thick concrete and rock sea defences now.

However, the access tunnel and car park (£2 per day parking as of 2017) at Samphire Hoe do provide very convenient access for the beach areas to the east and west where mineral specimens and the occasional cretaceous fossil may be collected.

Generally the beach area under the cliffs immediately to the (north) east of the Samphire Hoe area is the best area for collecting. This beach cannot be accessed at high tide, and you must be careful not to go too far along the beach here in case you are caught by the tide turning.

The marker on the map shows the starting point on the beach where good material can be found. You do not need to go very far from this point to find things.

Due to the constant erosion there is a virtually unlimited supply of material.


Mineral List


4 valid minerals.

Rock Types Recorded

Entries shown in red are rocks recorded for this region.

Note: this is a very new system on mindat.org and data is currently VERY limited. Please bear with us while we work towards adding this information!

Geochronology

Mineralization age: Late Cretaceous : 100.5 Ma to 66.0 Ma

Important note: This table is based only on rock and mineral ages recorded below and is not necessarily a complete representation of the geochronology, but does give an indication of possible mineralization events relevant to this locality. As more age information is added this table may expand in the future. A break in the table simply indicates a lack of data entered here, not necessarily a break in the geologic sequence. Grey background entries are from different, related, localities.

Geologic TimeRocks, Minerals and Events
Phanerozoic
 Mesozoic
  Cretaceous
   Late Cretaceous
ⓘ ChalkLate Cretaceous
(66.0 - 100.5 Ma)


This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.
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