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Coastal Landscapes in the UK: Deposition 🌊 GCSE Geography Learning & Revision

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Manage episode 479697771 series 3139505
Content provided by Seneca Learning Revision. All podcast content including episodes, graphics, and podcast descriptions are uploaded and provided directly by Seneca Learning Revision or their podcast platform partner. If you believe someone is using your copyrighted work without your permission, you can follow the process outlined here https://staging.podcastplayer.com/legal.

In this episode, we discuss coastal deposition.

Coastal deposition is the process where the sea deposits sediment at the coastline, causing coasts to expand when deposition exceeds erosion.

This primarily occurs when constructive waves break on the shore, leaving behind transported material.

The deposited sediment typically forms beaches, which can be sandy or shingle depending on the size of the particles.

Increased erosion in nearby areas can lead to greater deposition due to the larger amount of available sediment.

Sandy beaches are long and flat due to fine particles easily washed back, while shingle beaches are steep and short because larger pebbles are harder to move.

Don't miss out on subscribing for more educational content tailored to help you succeed in your exams. Perfect for AQA, OCR, Edexcel, CIE and WJEC exam boards.

⁠Click here to see all of our GCSE Geography content!

  continue reading

156 episodes

Artwork
iconShare
 
Manage episode 479697771 series 3139505
Content provided by Seneca Learning Revision. All podcast content including episodes, graphics, and podcast descriptions are uploaded and provided directly by Seneca Learning Revision or their podcast platform partner. If you believe someone is using your copyrighted work without your permission, you can follow the process outlined here https://staging.podcastplayer.com/legal.

In this episode, we discuss coastal deposition.

Coastal deposition is the process where the sea deposits sediment at the coastline, causing coasts to expand when deposition exceeds erosion.

This primarily occurs when constructive waves break on the shore, leaving behind transported material.

The deposited sediment typically forms beaches, which can be sandy or shingle depending on the size of the particles.

Increased erosion in nearby areas can lead to greater deposition due to the larger amount of available sediment.

Sandy beaches are long and flat due to fine particles easily washed back, while shingle beaches are steep and short because larger pebbles are harder to move.

Don't miss out on subscribing for more educational content tailored to help you succeed in your exams. Perfect for AQA, OCR, Edexcel, CIE and WJEC exam boards.

⁠Click here to see all of our GCSE Geography content!

  continue reading

156 episodes

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