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Bouldnor (Isle of Wight) Fossils

Fossil Collecting Code

Fossil Collecting Code

Location and directions

Directions: The beach is accessed via
the A3054, along 'Cranmore Avenue'.
Follow the track until you reach a
grassed area (see photo below) on the
right; there is room for several cars.
Follow the track north; see additional
direction notes below.

Key information

Geological period

Palaeogene (Oligocene epoch)

Approximate age

34 - 28 million years

Fossil diversity

Turtle, Mammal Bones / Teeth, Wood...

Find frequency

Below average

Dangers

Muddy and tidal

Equipment

A small steel probe

Accessibility

Easily accessible / brief walk

Local facilities

Parking and nothing else

Additional notes

Site of Special Scientific Interest (SSSI)

How would Bouldnor have looked 34 million years ago?

 

 

Introduction

 

The coast between Bouldnor and Cranmore stretches along the top-left corner of the Isle of Wight and is frequently visited by those interested in the geology of the area; as a result, over collecting often occurs, which makes finding good specimens during the summer months more of a challenge.  The best time to visit is following periods of stormy weather or during the winter, when the foreshore has been disturbed and new fossils exposed. Visiting on a low or retreating tide is recommended, as the majority of finds are made among the pebbles on the foreshore.

 

The following page is based on the coast between Bouldnor and Cranmore (a future visit is planned to examine the continuation of the coast towards Hamstead).

 

Access to the beach is made along Cranmore Avenue, at the top of which a limited amount of parking space is available (see photo below-left). Continue on foot along Sea View Road towards the coast until you reach a large private residence (see photo below-right). Alongside the seaward edge of the property is a public footpath leading directly to the beach; please note, during or after periods of wet weather the path becomes extremely muddy!

 

 

(Left) Parking is available on the grass along Cranmore Avenue. (Right) Access is made via a public footpath which runs alongside a large private residence.

 

One of the notable environmental processes at Hamstead is the rate of erosion, evident by the large number of trees and buildings littering the foreshore or surrounded by water! This occurs throughout the year and particularly during the winter, as the waves batter the soft clay cliffs. Some of the marooned features include a large building (see photo below-left), which in the spring of 2007 appeared to be approximately 80 meters off the high water mark!

 

 

(Left) The retreating cliff has turned former buildings into islands! (Right) One of many trees that have collapsed as the cliff has been eroded.

 

 

The geology of Hamstead

 

B.Daley and P.Balson, British Tertiary Stratigraphy 1999, describe the environment during this period as 'a sluggish fluvial / estuary / lagoonal complex occassionally subject to marine inundation.'.

 

During this time a variety of mammals including Entelodon (pig-like animal), Bothriodon and Brachyodus (grazers), and Caenotherium (small and deer-like) grazed the land close to the water; carnivores including Hyaenodon are also known to have hunted these areas.

 

  

Stratigraphy at Hamstead

 

Hamstead is the only site with a more or less complete succession of the Bouldnor Formation and the only place where the Hamstead and Cranmore Members are exposed.  Despite being heavily overgrown and reliant on very low tides, Hamstead is one of the best locations for evidence of sediments formed through periods of change, notably freshwater and brackish (semi-salty) environments, and low wave energy.

  

 

Where to look for fossils?

 

From the beach access point (described) fossils can be found in either direction. Moving westward along the beach, the volume of finds steadily increases for around half a mile, before reducing again (reflecting the reducing exposures of the Hamstead Formation);  very few fossils were found beyond the point indicated in the photo below-left. In reality, this stretch of coast is constantly changing, meaning a recently poor collecting area may become productive soon after.

 

 

(Left) Looking for fossils within the clay exposed on the foreshore at Bouldnor. (Right) Searching for fossils among the pebbles on the foreshore at Cranmore.

 

Fossils can be found in situ within the clay and within/among the flint pebbles on the foreshore. Whilst collecting from the clay provides the best opportunity to examine largely intact fossils, the vast majority of finds are made among the pebbles, some of which were of excellent quality (especially mammalian and reptilian). Whilst searching among the pebbles it's also worth keeping an eye out for flint fossils, these are much older (circa 85 million years old) than the local fossils and were sourced from chalk and transported to the area by glaciers during the last ice-age.

 

For more information about the features and processes controlling coastal fossil collecting locations click here.

 

 

What fossils might you find?

 

The fossils at Hamstead range from very large sections of tree trunks to tiny gastropods and can be found all year round, although in varying volume depending of the prevailing conditions (as outlined above).

 

The following photos illustrate the range of common finds at Hamstead, all of which were found during a single four hour visit.  

 

 

(Left) A large section of fossilised wood. (Right) A squashed gastropod shell.

 

 

(Left) A collection of bivalves in situ on the foreshore. (Right) A pyritised twisted twig.

 

 

Two pyritised gastropod shells

 

 

(Left) A concentration of small pyritised gastropod shells. (Right) A close-up.

 

 

Two large fragments of bone, possibly turtle.

 

 

(Left) A lovely piece of turtle carapace. (Right) Section of jaw, including teeth - Elomeryx porcinus (Identified by Danielle Schreve at the NHM London).

 

 

(Left) A large flint echinoid - Echinocorys. (Right) A small, partial echinoid Echinocorys within a flint pebble.

 

 

(Left) A large flint bivalve fragment. (Right) A bivalve impression in a flint pebble.

 

 

Protecting your finds

 

It's important to spend some time considering the best way to protect your finds onsite, in transit, on display and in storage. Prior to your visit, consider the equipment and accessories you're likely to need, as these will differ depending on the type of rock, terrain and prevailing weather conditions.

 

 

(Left) Fossil wrapped in newspaper, ready for transport. (Right) A small compartment box containing cotton wool is ideal for separating delicate specimens.

 

When you discover a fossil, examine the surrounding matrix (rock) and consider how best to remove the specimen without breaking it; patience and consideration are key. The aim of extraction is to remove the specimen with some of the matrix attached, as this will provide added protection during transit and future handling; sometimes breaks are unavoidable, but with care you should be able to extract most specimens intact. In the event of breakage, carefully gather all the pieces together, as in most cases repairs can be made at a later time...continued.

 

     

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Picture credits: Turtles from www.fundecoipa.com; Estuary from www.celebrating200years.noaa.gov.
 
References
: British Tertiary Stratigraphy, B.Daley and P.Balson.

  
Safety notice: Fossil hunting can at times pose a risk to personal safety, in particular within environments close to the coast, cliffs or in quarries and when using the tools and equipment illustrated. Discovering Fossils provides a free resource to inform you about this fascinating subject and does not accept any liability for decisions made using this information. We recommend all individuals abide by the 'National Fossil Hunting Code' and independently research the potential dangers before and during the visit.

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