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Geological Formation

Cathedral Cove

Erosional and Karst Formations

Cathedral Cove, on the Coromandel Peninsula of New Zealand's North Island, is a coastal formation centered on a large natural sea arch cut through a headland of pale, sheer volcanic rock known as Cathedral Cove Rhyolite. The arch was carved by long-term wave erosion acting on natural lines of weakness in the rhyolite, a hardened volcanic rock, which was progressively hollowed and widened by the sea into a tall, cathedral-like archway connecting two adjoining beaches, alongside a separate freestanding sea stack called Te Hoho Rock nearby. The formation remains an actively eroding coastal feature, part of the wider Te Whanganui-A-Hei Marine Reserve, and its dramatic sea arch has made it one of the best known coastal rock formations in New Zealand.

Facts
Classification
Protected Status
National Park or Reserve 1
Connections

Caused By

Erosion, Processes

In Discipline

In the Other Atlases
Sources
1. Cathedral Cove (Wikipedia)
Marine reserve lead sentence
Quote, Marine reserve lead sentence
Te Whanganui-o-Hei (Cathedral Cove) Marine Reserve is in the southern part of Mercury Bay on the Coromandel Peninsula in New Zealand covering an area of 840 hectares (2,100 acres).
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