The change in the strata over time illustrate the changing conditions and climate associated with this place. This is topped with up to 15 metres of brown sandy clay.
The sand grains making up the Boscombe Sands are generally rounded or sub angular grains of quartz. The head is 36 metres high at its highest point which is approximately a quarter of the way along or about metres from its most easterly point.
Warren Hill itself is composed of Tertiary Bracklesham Beds a mixture of clays and marls with overlying sandy and lignitic beds. Hengistbury Head had been subject erosion ever since the southerly chalk ridge, which stretched from the Needles in the Isle of Wight to the Old Harry rocks near Studland was breached by the sea.
The natterjack was last recorded on the headland in the s before its extinction, probably as the result of a lack of suitable ponds. I understand that some ironstones have been found embedded in it. This erosion was slowed, if not stopped, by the accumulation of hard iron stone boulders that were left from the erosion of the softer rocks in which they were embedded.
Until comparatively recent geological time Hengistbury Head was several kilometres inland. The deposits on the northerly shore line of Hengistbury Head are traditional river deposits leading to the building of salt marshes and reed beds. During the last Ice age about 12, years ago Hengistbury Head was several Kilometres inland.
These vary in size but are usually at least 1 metre across with some being 2 metres. The spit has a long association with shipbuilding with two large ships being built in the midth century, the Viscountess Canning of tons and the Enterprise tons.
He died from his injuries shortly after his fall. After the River Avon and Stour eroded their dividing ridge and joined in a confluence about 1 kilometre north west of the Hengistbury Head the old Stour bed, which used to route the river to the south of Hengistbury Head was initially abandoned and then adopted by the river Bourne.
The Balearic shearwaterconsidered critically endangered with extinction by the IUCN and seldom sighted in the UK, has been seen in the area. The final stretch of the river bed originally used by the River Stour was abandoned.
It is famous for having historic towers and has been an ancient site since Roman times — just like H. The whole mass is a sandy orange in colour. These sit about half way down the head on the northern escarpment.
About twenty pioneer aviators from around the world participated in various competitions including spot landing, altitude tests and speed trials both for the fastest and slowest circuit. All of the strata are inclined at about 3 degrees to the horizontal declining to the south east.
The normal slow erosion that had taken place had caused the Ironstones to form a natural reef off shore. The main nature reserve area faces Christchurch Harbourand is contiguous with the reed beds of Wick Fields.
In a channel was cut out to sea, whilst ironstone boulders from the head were used to create a pier.
It is possible that this river was actually the small River Bourne. While it was very acidic in the early years, since it has allowed the growth of a significant number of plant and insect species, as well as mallard and little grebe.
Reculver Towers — ancient site. These river deposits consist mainly of river gravel's and are some of the newest of the deposits at Hengistbury Head. What you might start to be realising is that perhaps H. Hengistbury Head is a sandstone headland forming part of Southbournewhich is a suburb of the town of Bournemouth to the west; the nearest major settlement is Christchurch to the north.
The clay lumps then became incorporated into the general make up of the stratum. Hengistbury Head. Declared a Local Nature Reserve inthe head and its surroundings form part of the Christchurch Harbour Site of Special Scientific Interest.
It is also a Special Area of Conservation, Special Protection Area, an Environmentally Sensitive Area and a Site of Nature Conservation Interest. Year 11 – this is the booklet for your controlled assessment fieldwork to Hengistbury Head.
Remember the booklet is for the fieldwork day and is to be completed in detail for you to refer back to when you complete the rest of the project.
Hengistbury Head. Hengistbury Head is a scenic and historic headland near the town of Bournemouth on the south coast of England. It stands mid way between Poole harbour and Hurst spit and forms the main division between Poole and Christchurch Bays.
To fulfil the needs of the GCSE syllabus we are undertaking coastal geography fieldwork at Hengistbury Head, Dorset. The aim of the fieldtrip is to collect data for the controlled assessment (coursework) aspect of the new GCSE. This controlled assessment represents 15% of the pupil’s final grade.
Hengistbury Head 18th September Although coursework and Controlled Assessments are no longer carried out as part of GCSE Geography exams, fieldwork remains essential in helping pupils understand the concepts they cover in class as well as build teamwork skills and apply research methods.
Hengistbury Head is in the county of Dorset and it is 2 miles away from Christchurch. Hengistbury Head is miles from London and Bournemouth centre is approximately 6 miles to the west of it.
The nature of Hengistbury head is that it's headland alinges west to east towards Mudeford.Hengistbury head coursework