Geography SL
Geography SL
10
Chapters
152
Notes
Option A - Freshwater – Drainage basins
Option A - Freshwater – Drainage basins
Option B - Oceans & coastal margins
Option B - Oceans & coastal margins
Option C - Extreme Environments
Option C - Extreme Environments
Option D - Geophysical Hazards
Option D - Geophysical Hazards
Option E - Leisure, Tourism And Sport
Option E - Leisure, Tourism And Sport
Option F - The Geography Of Food & Health
Option F - The Geography Of Food & Health
Option G - Urban Environments
Option G - Urban Environments
Unit 1 - Changing Population
Unit 1 - Changing Population
Unit 2 - Global Climate - Vulnerability & Resilience
Unit 2 - Global Climate - Vulnerability & Resilience
Unit 3 - Global Resource Consumption & Security
Unit 3 - Global Resource Consumption & Security
IB Resources
Option B - Oceans & coastal margins
Geography SL
Geography SL

Option B - Oceans & coastal margins

Unlock The Secrets of Coastal Erosion From Bays to Stacks

Word Count Emoji
620 words
Reading Time Emoji
4 mins read
Updated at Emoji
Last edited on 16th Oct 2024

Table of content

Introduction

Did you ever wonder how beautiful beaches and fascinating headlands are formed? Well, today's your lucky day! We'll walk through the wonderful world of erosion that sculpts our coastal landscapes. Remember, erosion is like an artist, sculpting the Earth's surface over thousands of years, turning boring rocks into scenic landscapes!

Bays and headlands

Just like us, rocks have their strengths and weaknesses. When waves go head to head with rocks, the weaker ones lose the battle and get eroded to form bays, while the harder rocks remain, forming headlands that stick out. Imagine a boxing match where waves are the heavyweight champion, and weaker rocks are the underdogs. Over time, the champ punches (erodes) the weaker rocks forming bays. An example of this is Maracas Bay and Tyrico Bay in northern Trinidad!

Wave refraction and bayhead beaches

Waves are smart; they distribute their energy evenly around the bay (a process known as wave refraction). But guess what? They still have a bit of a temper. They focus their energy on the flanks of headlands, like an angry gamer zeroing in on their opponent in a video game. Bayhead beaches form when friendly waves (constructive waves) drop sand between two headlands.

Sea caves, arches, stacks, & stumps

You won't believe what waves can do to rocks with weaknesses or faults! They can create sea caves, arches, stacks, and stumps. It's like the waves are playing a game of Minecraft, digging out caves, forming arches, and making stacks and stumps! Here's how:

  • Waves find a fault in the rock and start digging a sea cave.
  • If two caves meet, they form an arch (it's like a high-five between two caves!).
  • If the roof of the arch collapses, we get a stack.
  • Finally, if this stack is eroded, a stump is formed.

You can see these in action at Etretat in northern France and Dyrhólaey, southern Iceland.

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IB Resources
Option B - Oceans & coastal margins
Geography SL
Geography SL

Option B - Oceans & coastal margins

Unlock The Secrets of Coastal Erosion From Bays to Stacks

Word Count Emoji
620 words
Reading Time Emoji
4 mins read
Updated at Emoji
Last edited on 16th Oct 2024

Table of content

Introduction

Did you ever wonder how beautiful beaches and fascinating headlands are formed? Well, today's your lucky day! We'll walk through the wonderful world of erosion that sculpts our coastal landscapes. Remember, erosion is like an artist, sculpting the Earth's surface over thousands of years, turning boring rocks into scenic landscapes!

Bays and headlands

Just like us, rocks have their strengths and weaknesses. When waves go head to head with rocks, the weaker ones lose the battle and get eroded to form bays, while the harder rocks remain, forming headlands that stick out. Imagine a boxing match where waves are the heavyweight champion, and weaker rocks are the underdogs. Over time, the champ punches (erodes) the weaker rocks forming bays. An example of this is Maracas Bay and Tyrico Bay in northern Trinidad!

Wave refraction and bayhead beaches

Waves are smart; they distribute their energy evenly around the bay (a process known as wave refraction). But guess what? They still have a bit of a temper. They focus their energy on the flanks of headlands, like an angry gamer zeroing in on their opponent in a video game. Bayhead beaches form when friendly waves (constructive waves) drop sand between two headlands.

Sea caves, arches, stacks, & stumps

You won't believe what waves can do to rocks with weaknesses or faults! They can create sea caves, arches, stacks, and stumps. It's like the waves are playing a game of Minecraft, digging out caves, forming arches, and making stacks and stumps! Here's how:

  • Waves find a fault in the rock and start digging a sea cave.
  • If two caves meet, they form an arch (it's like a high-five between two caves!).
  • If the roof of the arch collapses, we get a stack.
  • Finally, if this stack is eroded, a stump is formed.

You can see these in action at Etretat in northern France and Dyrhólaey, southern Iceland.

Unlock the Full Content! File Is Locked Emoji

Dive deeper and gain exclusive access to premium files of Geography SL. Subscribe now and get closer to that 45 🌟