askvity

How Do Sea Stacks Form?

Published in Coastal Geology 2 mins read

Sea stacks are dramatic rock formations that rise from the ocean, resembling tall, solitary islands. They form through a fascinating process of coastal erosion.

The Formation Process: A Step-by-Step Guide

  1. Headland Erosion: The process begins with a headland, a section of resistant rock jutting out into the sea. Constant wave action, driven by powerful currents and storms, relentlessly attacks the headland, eroding weaker areas.

  2. Sea Cave Formation: Over time, waves carve out weaknesses in the headland, creating caves. These caves are often formed along joints or fractures in the rock, which provide pathways for the water to exploit.

  3. Sea Arch Development: As erosion continues, the caves may eventually erode through the headland, forming a sea arch. The arch’s stability depends entirely on the strength of the remaining rock structure.

  4. Arch Collapse and Stack Creation: The constant pounding of waves eventually weakens the roof of the sea arch. As described in the reference provided, "A sea stack forms when a sea arch continues to be eroded and widened until the rock becomes too weak to support the roof of the sea arch and collapses into the sea." The remaining isolated rock pillar is then called a sea stack.

  5. Further Erosion and Transformation: The newly formed sea stack itself is vulnerable to further erosion. Waves continue to sculpt the stack, potentially leading to its eventual collapse, leaving behind sea stumps or smaller remnants.

Examples of Famous Sea Stacks

Many stunning coastal areas around the world showcase magnificent sea stacks. Some notable examples include:

  • The Needles, Isle of Wight (UK): Famous chalk stacks that are a popular tourist attraction.
  • Old Man of Hoy, Orkney (Scotland): An iconic red sandstone stack.
  • Ball's Pyramid, Lord Howe Island (Australia): A towering volcanic remnant.

These examples highlight the diverse geological conditions that contribute to sea stack formation. The specific rock type, wave action, and other environmental factors influence the size, shape, and longevity of these incredible landforms.

Related Articles