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Geological Formation

Waitomo Caves

Karst Caves and Sinkholes

Waitomo Caves is a limestone cave system on the North Island of New Zealand, near the town of Waitomo in the Waikato region, carved into a thick Oligocene-to-Miocene marine limestone that was uplifted and then slowly dissolved by underground drainage over roughly the last two million years. The caves are best known for the Glowworm Grotto, where the ceiling and walls host dense colonies of the bioluminescent larvae of Arachnocampa luminosa, a fungus gnat found only in New Zealand, whose glowing threads mimic a night sky and attract the small insects the larvae feed on. The cave system was first explored and mapped in 1887 by local Maori chief Tane Tinorau together with English surveyor Fred Mace, and it has been open to visitors since 1889, making it one of New Zealand's longest-running tourist attractions.

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Protected Status
National Park or Reserve 1
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Source Wikidata: Waitomo Caves
Sources
1. UNEP-WCMC and IUCN, World Database on Protected Areas: Protected area record for Waitomo Caves
UNEP-WCMC and IUCN, World Database on Protected AreasWDPA record, field desig_eng
Quote, WDPA record, field desig_eng
"desig_eng": "Scenic Reserve"
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Wikidata: Waitomo Caves
Wikidata Q1071889, class allow-list match (w-wdresolver-0926)View the Source
Protected Planet (UNEP-WCMC and IUCN): Waitomo Caves
Protected Planet (UNEP-WCMC and IUCN)Protected area profile
Quote, Protected area profile
Protected Area Profile for Waitomo Caves from the World Database on Protected Areas
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Waitomo (Wikipedia)
In Group: Caves and Cave Systems, Lead sentence
Quote, In Group: Caves and Cave Systems, Lead sentence
There are several solutional cave systems in the area around the village, which are popular tourist attractions.
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