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  2. Blowholes are formed through the following process123:
    1. Sea caves grow landward and upward into vertical shafts.
    2. Zones of weakness in the cliff erode, creating cavities.
    3. Hydraulic pressure from waves enlarges these cavities.
    4. Eventually, holes are forced through the cave roof, allowing pressure to be released as a jet of spray.
    Learn more:
    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)
    Zones of weakness in the cliff give way under the force of the waves and are eroded out; these cavities are enlarged by the hydraulic pressure built up by each wave. Holes, commonly known as blowholes, may eventually be forced through the roof of the cave to allow the pressure created by each wave to be released as a jet of spray.
    www.britannica.com/science/blowhole-sea-cave
    A blowhole is a cavity formed when a joint between a sea cave (formed by erosion) and the land surface above the cave becomes enlarged. The sea cave and the land surface become conjoined when the roof of the cave collapses. Blowholes are formed by the process of erosion.
    en.wikipedia.org/wiki/Category:Blowholes
     
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