Download presentation
Presentation is loading. Please wait.
Published byJonas Jakobsen Modified over 5 years ago
1
The Dorset Coast (and a little bit of Hampshire!)
~ a virtual field trip ~ I took this picture!
2
Where it is located
3
Day 1– The journey to Dorset! Day 2 – Lyme Regis to Ringstead Bay
4
Groynes An aerial photo of Lyme Regis Bay, showing ‘The Cobb’ (Harbour) and where the River Lim meets the sea
5
Lyme Regis ~ Charmouth ~ Golden Cap
6
The cliff top at Black Ven
The coast is unstable because there are numerous situations where porous strata, principally the Chalk and Upper Greensand, lie over impermeable clays. 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 cliff top at Black Ven
7
How Landslides occur
8
The gradient of the beach can get very steep
Chesil Beach Isle of Portland The Fleet West Bay (west) Pebbles are ’sorted!’ Portland (east) The gradient of the beach can get very steep
9
The Isle of Portland When the island was uplifted, a series of massive fractures developed in the limestone.
10
Portland Harbour (South of Weymouth)
Weymouth is a traditional seaside resort. It is protected by the Isle of Portland. Portland Harbour (South of Weymouth)
11
White Nothe Headland from Ringstead Bay
12
Day 3 – Ringstead Bay to St. Alban’s head
Durdle Door ~ Lulworth Cove ~ Stair Hole ~ Warbarrow Bay ~ Tynham ~ Broad Bench ~ Kimmeridge ~ Winspit
13
Durdle Door ~ A Limestone Arch
Eventually the arch will collapse to leave a sea stack
14
Chalk Hills stop the cove eroding any further inland
Lulworth Cove Chalk Hills stop the cove eroding any further inland Soft sand and clays Limestone Headlands
15
Stair Hole Small arch is only gap in the limestone.
Marine processes eroding further inland
16
The formation of Lulworth Cove, Stair Hole and the future
17
Tyneham from Gadd Cliff
Worbarrow Bay Tyneham from Gadd Cliff (Note the land use) Broad Bench
18
Kimmeridge Bay – A wave cut platform
19
Waves shape the coastline.
St. Alban’s Head Winspit (behind) Chapmans Pool Waves shape the coastline. Winspit
20
Day 4 – St. Albans Head to Sandbanks
21
Looking out to see from Anvil Point
Dancing Ledge (+ tidal pool!) Sandbanks Studland Old Harry Swanage Bay Peveril Point Looking out to see from Anvil Point Durlston Head Anvil Point
22
Swanage Swanage Bay
23
Old Harry Rocks – A stack
Collapsed Undercuttingmeans stack will collapse New cave forming
24
Studland – Sand Dune System
3 Major dune ridges Little Sea Fieldwork (transects!)
25
Development of Studland – Blown Sands
Little Sea
26
View over dune slack with further vegetation succession
Younger dunes with Marram Grass Actual fieldwork! Hmmmmmm!
28
Day 5 – Sandbanks to Barton on Sea and the Isle of White
29
Bournemouth Sandbanks Bournemouth Bournemouth Pier Groynes
30
Hengistbury Head Christchurch Harbour Spit Groynes Long Groyne
Sediment Build Up
31
Hengistbury Head Unstable Cliffs Gullies Groynes Salt Marsh Erosion
32
Barton on Sea Landslides
House! Barton on Sea Landslides Landslip
33
Barton on Sea Christchurch Bay Evidence of lanslides Land Use
34
River Medina ~ A Ria Isle of Wight
East Cowes West Cowes River Medina To Newport
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.