Kōrero: Hauraki–Coromandel region

Inshore islands and coast, Coromandel

Inshore islands and coast, Coromandel

Whanganui Island, in the middle distance, lies on the northern side of Coromandel Harbour. The inshore islands are a by-product of glaciation. During the ice age tens of thousands of years ago sea levels were lower than at present; with the end of the ice age sea levels rose and coastal features became islands. The Moehau Range, 892 m at its highest point, is in the distance.

Te whakamahi i tēnei tūemi

Te Ara - The Encyclopedia of New Zealand
Photograph by Janine Faulknor

Ngā whakaahua me ngā rauemi katoa o tēnei kōrero

Te tuhi tohutoro mō tēnei whārangi:

Paul Monin, 'Hauraki–Coromandel region - Geology and landscape', Te Ara - the Encyclopedia of New Zealand, http://www.TeAra.govt.nz/mi/photograph/30362/inshore-islands-and-coast-coromandel (accessed 7 December 2019)

He kōrero nā Paul Monin, updated 1 Apr 2016