'Biddulph high school' presentation slideshows

Longshore Drift

Longshore Drift. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash.

983 views • 57 slides

Longshore Drift

Longshore Drift. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash.

1.39k views • 56 slides

Longshore Drift

Longshore Drift. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash. Direction of swash.

741 views • 56 slides

Wave Refraction and Orthogonals

Wave Refraction and Orthogonals. Wave refraction and orthogonals. The physical geography of headlands and bays. Shallow water. Shallow water. Shallow water. Shallow water. wave. Shallow water. Shallow water. wave. Shallow water. Shallow water. wave. Shallow water.

1.39k views • 29 slides

What's it like in a Tropical Rainforest?

What's it like in a Tropical Rainforest?.

444 views • 27 slides

Coastal Erosion

Coastal Erosion. Learning objectives. To be able to define the five processes of marine coastal erosion . To be able to explain the factors affecting coastal erosion. To describe the difference between concordant and discordant coastlines. Homework. Answer the exam question:

661 views • 27 slides

Wave Scour

Wave Scour. How waves build beaches and can destroy them. Waves are reflected back from the sea wall, pulling sand out to sea. Wave scour undercuts the sea wall. Wall becomes unstable. Seawall collapse. Wave can now attack the coast.

402 views • 15 slides

Settlement Sites

P. PH. Settlement Sites. Village. Move the village until you think it is in the correct location on the settlement maps. Example: Burton upon Trent, Staffordshire and A38. Valley Site. River floodplain. Raised river terrace.

415 views • 12 slides

buttress roots

buttress roots. Wide roots stop these enormously tall trees from falling over. They also wind above the ground looking for food and nutrients rather than digging beneath the ground where nutrients are scarce. Parasitic plant. Pitcher plant - a carnivorous plant. slippery rim . tendril .

836 views • 12 slides

Cave Arch and Stack Formation

Cave Arch and Stack Formation. Waves attack the headland cutting caves on each side. Wave attack opens up the caves on each side of the headland until they join and form a natural arch. The arch enlarges until it collapses, leaving a standing rock called a stack. New arch forms.

97 views • 9 slides

Tropical rainforest models

Tropical rainforest models. Rainforest plants And the enormous the number of different species of plants grow in rainforests, with many species occurring only in one particular region. Unlike other forests, rain forests have an abundance of :

411 views • 8 slides

Stages in the Development of a River Valley

1.52k views • 8 slides

Limestone Pavements

Limestone Pavements. Karst Scenery. Limestone is an alkaline rock. It is a hard rock but it reacts with acidic rain and dissolves away. Little material is left on the surface to form soil. So it appears as bare rock. The landscape can look very barren.

385 views • 7 slides

Depression Formation

Depression Formation. A 3D Model. Cold wind. Warm wind. Cold wind. Warm wind. Cold wind. Warm wind. Cold wind.

176 views • 5 slides

Depression Formation

Depression Formation. A 3D Model. Cold wind. Warm wind. Cold wind. Warm wind. Cold wind. Warm wind. Cold wind.

52 views • 5 slides