Chantry Mill
Also within
Condition (Natural England)
Favourable (1)
| Unit | Feature | Condition | Area (ha) | Assessed |
|---|---|---|---|---|
| TQ094138 | — | Favourable | 8.7 | 2023-02-03 |
Geology & landscape
Geological Period: Cretaceous
Description
Area, 8.6 ha. 21.3 ac. Description Chantry Mill provides the best available exposure of the unusual 'iron grit' horizon which characterises the Gault/ Folkestone Beds junction in this part of Sussex and which contrasts strongly with the type of transition seen between these formations elsewhere in south east England. The 'iron grit' represents a condensed deposit associated with prolonged non deposition over a structural axis, probably the northern margin of the major Portsdown Axis, which separated the Vectian and Wealden provinces in the Lower Cretaceous.