Kogin Panmure
| Kogin Panmure | |
|---|---|
 | |
| General information | |
| Labarin ƙasa | |
 | |
| Tsarin Daidaiton Labarin Kasa | 36°54′18″S 174°50′57″E / 36.9049°S 174.8493°E |
| Kasa | Sabuwar Zelandiya |
| Territory |
Auckland Region (en)  |
| Hydrography (en) | |
| Inflow (en) |
duba
|
| Outflows (en) |
Tamaki River (en) |
Panmure Basin (wanda aka fi sani shi a cikin Māori kamar Kaiahiku [1] ko Te Kopua Kai-a-Hiku [2]), wanda wani lokacin ake kira Panmure Lagoon, wani tafki ne mai zurfi a cikin rami mai hasken wuta ko maar a filin dutsen wuta na Auckland na New Zealand. Tana kudu da tsakiyar garin Panmure.
Ilimin ƙasa
[gyara sashe | gyara masomin]
Dutsen ya fashe a kimanin shekaru 25,200 da suka gabata.[3] A lokacin Last Glacial Maximum, tafkin ya kuma kasance tafkin ruwa mai laushi. Lokacin da matakan teku suka tashi, ruwan Kogin Tāmaki ya karya tafkin, ya juya shi zuwa bakin teku.[4] Ana samun karamin ƙwayoyin ƙwayoyin cuta a tsakiyar kwandon, wanda aka rufe shi da laka.
Tarihi
[gyara sashe | gyara masomin]Sunan gargajiya na kogin shi ne Te Kai a Hiku . Yana nuni a cikin labarun gargajiya na Tāmaki Māori a matsayin wurin cin abinci na taniwha Moko-ika-hiku-waru . [1] Yankin da ke tsakanin kwandon da Kogin Tāmaki shine wurin Ngāti Pāoa pā Mauināina (wanda aka fi sani da Maunga-ina da Taumata-ina).[4].
A watan Fabrairun shekara ta 2008, masana kimiyya sun ba da sanarwar cewa hakowa ya gano wani sharar gida da aka binne a cikin laka da ke cika fashewar fashewa.[5] Kodayake 'yan jarida sun yi la'akari da cewa ƙwanƙolin da aka gano ƙarami ne kuma ya bambanta da dutsen wuta daga Panmure Basin, masu ilimin ƙasa suna la'akari cewa an samar da ƙwanƙwasawar ƙwanƙara a matsayin mataki na biyu na fashewar fashewar Panmure basin fashewa da zoben tuff. An kuma samar da fashewar ta hanyar hulɗar magma tare da ruwan sanyi amma da zarar an yi amfani da ruwa har zuwa fashewar wuta ta sauya zuwa wani lokaci mai bushe na tushen wuta wanda ke samar da ƙanƙara daga wannan iska. Don haka Panmure Basin ba ya bambanta da wasu tsaunuka masu fitattun wuta a cikin filin dutsen wuta na Auckland, kamar su Auckland Domain Volcano, Māngere Lagoon Volcano, Waitomokia, Te Tatua-a-Riukiuta da Crater Hill (kowane tare da ɗaya ko fiye da ƙwayoyin ƙwayoyin cuta a cikin fashewar su), sai dai an binne ƙaramin ƙwayoyin tsakiya na Panmure.
Dubi kuma
[gyara sashe | gyara masomin]- Dutsen wuta na Auckland: Jagoran Jagora - Hayward, B.W., Murdoch, G., Maitland, G.; Jami'ar Auckland, 2011.
- Dutsen wuta na Auckland: Jagoran filin. Hayward, B.W.; Auckland University Press, 2019, shafi na 335 .
Manazarta
[gyara sashe | gyara masomin]- ↑ 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.
- ↑ Hayward, Bruce William; Jamieson, Alastair (2019). "Volcanoes of Auckland : a field guide". Auckland University Press. Retrieved 2022-10-30.
- ↑ 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-access=requires|hdl=(help) - ↑ 4.0 4.1 Bruce Hayward. Missing
|author1=(help); Missing or empty|title=(help) Cite error: Invalid<ref>tag; name "FieldGuide2008" defined multiple times with different content - ↑ "Geologists find buried volcano inside Panmure Basin". Press release. GNS Science. 22 February 2008. Archived from the original on 2013-02-19. Retrieved 1 November 2011.
Haɗin waje
[gyara sashe | gyara masomin]- Hotuna na Panmure Basin da aka gudanar a cikin tarin kayan tarihi na Auckland.
- Hotuna na Panmure Basin da aka gudanar a cikin tarin kayan tarihi na Auckland War Memorial.