the dorset coast (and a little bit of hampshire!) ~ a virtual field trip ~ i took this picture!

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The Dorset Coast (and a little bit of Hampshire!) ~ a virtual field trip ~ I took this picture!

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The Dorset Coast(and a little bit of Hampshire!)

~ a virtual field trip ~

I took this picture!

Where it is located

Day 2 – Lyme Regis to Ringstead Bay

Day 1– The journey to Dorset!

An aerial photo of Lyme Regis Bay, showing ‘The

Cobb’ (Harbour) and where the River Lim meets the sea

Groynes

Golden Cap

Lyme Regis ~ Charmouth ~ Golden Cap

The cliff top at Black Ven

Black Ven between Lyme Regis and Charmouth. Upper Greensand lies

over Lower Jurassic clays. The largest coastal

mudflow in Europe took place here in the winter of

1958/9

The coast is unstable because there are numerous situations where porous strata, principally the Chalk and Upper Greensand, lie over impermeable clays.

How Landslides occur

Chesil Beach

Isle of Portland

The Fleet West Bay (west)

Pebbles are ’sorted!’

Portland (east)

The gradient of the beach can get very steep

The Isle of Portland

When the island was uplifted, a series of massive fractures developed in the limestone.

Weymouth is a traditional seaside resort. It is protected by the Isle of Portland.

Portland Harbour (South of Weymouth)

Weymouth

White Nothe Headland from Ringstead Bay

Day 3 – Ringstead Bay to St. Alban’s head

Durdle Door ~ Lulworth Cove ~ Stair Hole ~ Warbarrow Bay ~ Tynham ~ Broad Bench ~ Kimmeridge ~ Winspit

Durdle Door ~ A Limestone Arch

Eventually the arch will collapse to

leave a sea stack

Limestone Headlands

Soft sand and clays

Chalk Hills stop the cove eroding any

further inland

Lulworth Cove

Small arch is only gap in the limestone.

Marine processes eroding further inland

Stair Hole

The formation of Lulworth Cove, Stair Hole and the future

Worbarrow Bay

Tyneham from Gadd Cliff

(Note the land use)

Broad Bench

Kimmeridge Bay – A wave cut platform

Chapmans Pool

St. Alban’s Head

Waves shape the coastline.

Winspit

Winspit (behind)

Day 4 – St. Albans Head to Sandbanks

Dancing Ledge

(+ tidal pool!)

Looking out to see from Anvil Point

Durlston Head

Peveril Point

Swanage Bay

Old Harry

Sandbanks

Studland

Anvil Point

Swanage Bay

Swanage

Old Harry Rocks – A stack

Stack

New cave forming

CollapsedUndercuttingmeans stack will collapse

Studland – Sand Dune System

Fieldwork (transects!)

Little Sea

3 Major dune ridges

Development of Studland – Blown Sands

Little Sea

View over dune slack with further vegetation

succession Younger dunes with Marram Grass

Actual fieldwork! Hmmmmmm!

Day 5 – Sandbanks to Barton on Sea and the Isle of White

Bournemouth

Sandbanks

Bournemouth Pier

Bournemouth

Groynes

Hengistbury Head

Long Groyne

Spit

Christchurch Harbour

Groynes

Sediment Build Up

Hengistbury Head

Gullies

Erosion

Unstable Cliffs

Salt Marsh

Groynes

Barton on Sea Landslides

House!

Landslip

Barton on Sea

Land UseEvidence of lanslides

Christchurch Bay

West Cowes

East Cowes

River Medina

To Newport

River Medina ~ A Ria Isle of Wight

Day 6 - Back to School

That’s it!