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- Blowholes are formed in geography through the following process12:
- Sea caves grow landward and upward into vertical shafts.
- These caves expose themselves toward the surface.
- Hydraulic compression of seawater occurs, which is then released through a port from the top of the blowhole.
- The constant movement of waves at the bottom of cliffs weakens the rock and forces air into small fissures, creating blowholes on the surface.
Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.In geology, a blowhole or marine geyser is formed as sea caves grow landward and upward into vertical shafts and expose themselves toward the surface, which can result in hydraulic compression of seawater that is released through a port from the top of the blowhole.en.wikipedia.org/wiki/Blowhole_(geology)The constant movement of waves at the bottom of cliffs (or any solid structure at the shore) eats away at the area around the crack and renders it weak enough to create sea caves at the bottom. As if this wasn’t bad enough for the health of the rock, the movement of waves forces air into these small fissures, which are formed on the surface.www.scienceabc.com/nature/deconstructing-blowh… - People also ask
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