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  2. Natural arch - Wikipedia

    en.wikipedia.org/wiki/Natural_arch

    A natural arch, natural bridge, or (less commonly) rock arch is a natural landform where an arch has formed with an opening underneath. Natural arches commonly form where inland cliffs , coastal cliffs , fins or stacks are subject to erosion from the sea, rivers or weathering ( subaerial processes).

  3. Stack (geology) - Wikipedia

    en.wikipedia.org/wiki/Stack_(geology)

    Without the constant presence of water, stacks also form when a natural arch collapses under gravity, due to sub-aerial processes like wind erosion. Erosion causes the arch to collapse, leaving the pillar of hard rock standing away from the coast—the stack. Eventually, erosion will cause the stack to collapse, leaving a stump.

  4. List of rock formations of New Zealand - Wikipedia

    en.wikipedia.org/wiki/List_of_rock_formations_of...

    Wave erosion, sea stacks, and natural arch Notable for their well documented partial destruction from wave erosion. 38°49′07″S 174°34′52″E  /  38.81861°S 174.58111°E  / -38.81861; 174

  5. One of world’s most iconic sea arches could collapse at any ...

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  6. Hopewell Rocks - Wikipedia

    en.wikipedia.org/wiki/Hopewell_Rocks

    The Hopewell Rocks, also called the Flowerpot Rocks or simply the Rocks, are rock formations known as sea stacks caused by tidal erosion in the Hopewell Rocks Ocean Tidal Exploration Site at the Hopewell Rocks Provincial Park in New Brunswick, Canada. They stand 12–21 metres (40–70 ft) tall.

  7. Coastal erosion - Wikipedia

    en.wikipedia.org/wiki/Coastal_erosion

    Hampton-on-Sea is located in Kent, England. It was at one time very popular for its oyster fishing and was very reliant on the sea. Hampton-on-Sea has undergone the effects of coastal erosion since before the 1800s. Hampton-on-Sea's coastal erosion worsened with the increase in global warming and climate change.

  8. Marsden Rock - Wikipedia

    en.wikipedia.org/wiki/Marsden_Rock

    Marsden Rock was formed by erosion of less-resistant stone along the joints of the cliffs of Marsden Bay, resulting in an isolated stack of compacted limestone. [3] [4] A channel was carved through the rock by waves which formed a natural arch. [5] By the 1800s, the arch had become large enough for sailing boats to pass through at high tide. [6]

  9. Arch of Cabo San Lucas - Wikipedia

    en.wikipedia.org/wiki/Arch_of_Cabo_San_Lucas

    The Arch is accessible by land or boat from the beach of the last hotel on the Pacific. Access to the arch requires climbing large rocks. [2] [3] [4] Entering the arch in a small watercraft can be somewhat dangerous when the sea is running. The water level can significantly go up and down. Being close to the sides of the arch is not recommended.