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1:250 000 Geological Map

This range of geological maps show the general geology of the area, they come in either folded (for taking on the field), or flat (for wall mounting)
Buy from UKGE

1: 50 000 Geological Map

This range of geological maps show the localised geology, they come in either folded (for taking on the field), or flat (for wall mounting)
Buy from UKGE

Cretaceous

GEOGRAPHY AND CLIMATE: Seas flood half the land, Great thickness of chalk, single-celled animals laid down. Land masses begin to move towards their present positions. Climate mild without
extremes.

TERRESTRIAL ANIMAL LIFE: Advanced dinosaurs such as duck-bills. Turtles, snakes,salamanders. Gulls and wading birds. Opossums & other mammals. All dinosaurs and many other large reptiles extinct by the end of the period.

PLANT LIFE: Gymnosperms, sequoias and cypresses. Flowering plants appear, magnolias and oaks.

SEA LIFE: Plankton, coral reefs, rudists, ammonites, calcareous algae. Marine reptiles and ammonites extinct by the end of the period.

Jurassic

GEOGRAPHY AND CLIMATE: Gondwanaland continues to break up, Graywacke, shale and siliceous sediments formed. Continued mountain building. mild, moist climates over most of the land.

TERRESTRIAL ANIMAL LIFE: Reptiles dominant with Crocodiles, turtles, lizards and dinosaurs. Pterosaurs and Archaeopteryx take to the air. Mammals begin to diversify. More advanced insects such as flies.

PLANT LIFE: Cycads, ginkos, conifers, ferns and tree ferns.

SEA LIFE: All major invertebrate groups well represented, ammonites and bivalves successful. Marine reptiles, Ichthyosaurs are Plesiosaurs.

 

Triassic

GEOGRAPHY AND CLIMATE: Sea levels very low. Graywacke shale, siliceous and Red desert sandstone deposits, arid climate over most of land Pangaea begins to split. Atlantic Ocean opens up.

TERRESTRIAL ANIMAL LIFE: Reptiles dominant, including the ancestors of the dinosaurs and mammals.

PLANT LIFE: Gymnosperms such as ferns, cycads, gingko's and conifers.

SEA LIFE: Ammonites dominate the seas, Bivalves and Brachiopods are locally abundant but generally rare. All other major invertebrate groups are rare of missing.

 


 

Geological Guide to Pinhay Bay


Geological succession at Pinhay Bay

The head of Pinhay Bay exposes Triassic rocks of the Penarth on the foreshore, the Contorta Shales from the Westbury Formation make up 5m here and crop out. A range of bivalves including Rhaotavicula contorta, Chlamys valonensis and Protocardia rhaetica can all be found.

The White Lias Langport member follows this, around 8m clearly seen in the cliff by its pale green or gray limestones. Walking West of Seven Rock Point, the higher and younger rocks can be seen. These overlying 19m of Blue Lias. The lowest beds are from the Penarth, this is only around 0.3m and are excluded from the Lias. At the base of the Jurassic, ammonites can be found.

Succession from Chapel Rock
Clay with Flints 1m
Upper Chalk 26m
Middle Chalk 44m
Lower Chalk 1m
Upper Greensand 25m
Gault 43m
Lower Lias 8m




Santonian
83 - 86 MYA
Newhaven Group
Old Nore
Brighton Marl
Splash Point
Buckle Marls
Micraster cortestudinarium Zone Beer Head
Pinhay Bay
Holaster (Sternotaxis) planus Zone

Beer Head
Pinhay Bay
Seaton

Seaford Chalk
Haven Brow

Turonian
89.0 to 93.0
Lewes Nodular Chalk
Navigation

Beachy Head
Dover

South Street

Beachy Head
Dover

Kingston

Beachy Head
Dover

Ringmer

Beachy Head
Dover

Caburn

Beachy Head
Dover

Glynde

Eastbourne
Beachy Head
Dover

New Pit Chalk member

Eastbourne
Beachy Head
Dover

St Margaret's Member
 
Ranscombe Member
 
Terebratulina lata Zone Hookend Cliff
Beer Head
Pinhay Bay
Inoceramus labiatus (Orbirhynchia cuvieri) Zone Hookend Cliff
Beer Head
Pinhay Bay
Holywell Nodular Chalk Member
Eastbourne
Beachy Head
(Middle Chalk)

Houghton Quarry
Swanage


Cenomanian
93 - 98.9 MYA
Zig Zag Chalk
Plenus Marls

Eastbourne
Yaverland
White Nothe
Swanage

Grey Chalk
Yaverland
Hunstanton
White Nothe
West Melbury Marly Chalk
Chalk Marl
Yaverland
Rocken End
Glauconitic Marl
Eastbourne
Yaverland
Rocken End
Beer Head Limestone Formation Hookend Cliff
Beer Head
Pinhay Bay
(Lower Chalk)

Houghton Quarry
Samphire Hoe


Albian
98.9 - 111 MYA
Late Albian
Upper Greensand

Folkestone
Charmouth
Golden Cap (Seatown)
Thorncombe Beacon
White Nothe
Chippel Bay
Eastbourne
Yaverland
Rocken End
Swanage
Lulworth Cove
Hookend Cliff
Beer Head
Pinhay Bay
Seaton

Red Chalk

Middle Albian

Gault

Folkestone
Charmouth
Golden Cap (Seatown)
Thorncombe Beacon
Eastbourne
Yaverland
Rocken End
Swanage
Lulworth Cove
Pinhay Bay

Carstone
Speeton Clay Formation (A-Bed) Speeton
Early Albian
Speeton Clay Formation (A-Bed) Speeton
Lower Greensand

Folkestone
Swanage
Lulworth Cove

Sandrock

Hettangian
201 to 205.7 MYA
E
A R
L
Y

L
I
A
S
Early Blue Lias

Watchet
Lilstock
Hinkley Point
Quantoxhead
Kilve
Chippel Bay
Doniford Bay
St Audries Bay
Blue Anchor
Pinhay Bay

Redcar Mudstone Formation Early Calcareous Shales  
Dunrobin Bay Formation Lady's Walk Shale Golspie
White Sandstone Golspie
Carbonaceous Siltstone Golspie

Rhaetian
206 - 210 MYA
P
E
N
A
R
T
H

G
R
O
U
P
Lilstock Formation Langport Member Lilstock
Blue Anchor
Cotham Member Lilstock
Blue Anchor
Westbury Formation Aust
Blue Anchor
White Lias Formation Pinhay Bay
Dunrobin Pier Conglomerate Golspie



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