Panmure Basin

In today's article we are going to delve into the fascinating world of Panmure Basin. From its origins to its impact on current society, Panmure Basin has been the object of study and interest in various areas of knowledge. Throughout history, Panmure Basin has played a crucial role in the evolution and development of humanity, influencing cultural, economic and social aspects. In this article, we will explore different facets of Panmure Basin, analyzing its importance and relevance in the current context. In addition, we will examine how Panmure Basin has marked a before and after in various areas, as well as its influence on people's daily lives. Join us on this journey of discovery and learning about Panmure Basin.

Panmure Basin
View of Panmure Basin from Maungarei
View of Panmure Basin from Maungarei / Mount Wellington
LocationAuckland, North Island
Coordinates36°54′18″S 174°50′57″E / 36.9049°S 174.8493°E / -36.9049; 174.8493
Typemaar lake
Primary outflowsTamaki River
Surface elevation0 m (0 ft)
Map

The Panmure Basin (traditionally known in Māori as Kaiahiku [1] or Te Kopua Kai-a-Hiku[2]), also sometimes known as the Panmure Lagoon, is a tidal estuary within a volcanic crater or maar in New Zealand's Auckland volcanic field. It is located to the south of Panmure town centre.

Geology

The narrow passage that connects Panmure Basin to the Tāmaki River

The volcano erupted approximately 25,200 years ago.[3] During the Last Glacial Maximum, the basin was a freshwater lake. When sea-levels rose, the estuarine waters of the Tāmaki River breached the lake, turning it into a tidal estuary.[4] A small scoria cone is found in the centre of the basin, obscured by layers of mud.[5]

History

The traditional name of the basin was Te Kai a Hiku. It features in traditional Tāmaki Māori stories as the eating place of the taniwha Moko-ika-hiku-waru.[4] The headland between the basin and the Tāmaki River was the location of the Ngāti Pāoa pā Mauināina (also known as Maunga-inaina and Taumata-inaina).[6]

In February 2008, scientists announced that drilling had discovered a scoria cone buried within the mud filling the explosion crater.[7] Although newspaper journalists inferred that the discovered scoria cone was a much younger and different volcano from Panmure Basin,[8] geologists consider that the scoria cone was produced as the second phase of the eruption of Panmure Basin explosion crater and tuff ring. The explosive phase was produced by the interaction of the magma with cold groundwater but once the water was used up the eruption switched to a dry phase of fire-fountaining producing the scoria cone from the same vent.[9] Thus Panmure Basin is no different from a number of other volcanoes in the Auckland volcanic field, such as the Auckland Domain Volcano, Māngere Lagoon Volcano, Waitomokia, Te Tatua-a-Riukiuta and Crater Hill (each with one or more scoria cones inside their explosion crater), except that Panmure Basin's small central scoria cone was buried.

See also

  • Volcanoes of Auckland: The Essential guide - Hayward, B.W., Murdoch, G., Maitland, G.; Auckland University Press, 2011.
  • Volcanoes of Auckland: A Field Guide. Hayward, B.W.; Auckland University Press, 2019, 335 pp. ISBN 0-582-71784-1.

References

  1. ^ Pegman, David M (August 2007). "The Volcanoes of Auckland" (PDF). Manukau City Council. Mangere Mountain Education Centre. Archived from the original (PDF) on 24 March 2012. Retrieved 6 October 2021.
  2. ^ Hayward, Bruce William; Jamieson, Alastair (2019). "Volcanoes of Auckland : a field guide". Auckland University Press. Retrieved 30 October 2022.
  3. ^ Hopkins, Jenni L.; Smid, Elaine R.; Eccles, Jennifer D.; Hayes, Josh L.; Hayward, Bruce W.; McGee, Lucy E.; van Wijk, Kasper; Wilson, Thomas M.; Cronin, Shane J.; Leonard, Graham S.; Lindsay, Jan M.; Németh, Karoly; Smith, Ian E. M. (3 July 2021). "Auckland Volcanic Field magmatism, volcanism, and hazard: a review". New Zealand Journal of Geology and Geophysics. 64 (2–3): 213–234. doi:10.1080/00288306.2020.1736102. hdl:2292/51323.
  4. ^ a b Cameron, Ewen; Hayward, Bruce; Murdoch, Graeme (2008). A Field Guide to Auckland: Exploring the Region's Natural and Historical Heritage (Revised ed.). Random House New Zealand. p. 225. ISBN 978-1-86962-1513.
  5. ^ Janssen, Peter (January 2021). Greater Auckland Walks. New Holland Publishers. p. 100-101. ISBN 978-1-86966-516-6. OL 34023249W. Wikidata Q118136068.
  6. ^ Ballara, Angela (2003). "Tāmaki-makau-rau (Auckland isthmus)". Taua: 'musket wars', 'land wars' or tikanga?: warfare in Maori society in the early nineteenth century. Auckland: Penguin. pp. 206–234. ISBN 9780143018896.
  7. ^ "Geologists find buried volcano inside Panmure Basin". Press release. GNS Science. 22 February 2008. Archived from the original on 19 February 2013. Retrieved 1 November 2011.
  8. ^ "New Auckland volcano discovered". The New Zealand Herald. NZPA. 22 February 2008. Retrieved 1 November 2011.
  9. ^ Hayward, B.W., Murdoch, G., Maitland, G. 2011. Volcanoes of Auckland: The essential guide. Auckland University Press.