Lord Howe Seamount Chain
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| Lord Howe Seamount Chain | |
|---|---|
| Lua error in package.lua at line 80: module 'Module:InfoboxImage/data' not found. Topographic map of Zealandia with the Lord Howe Rise to the north west of New Zealand labelled. | |
| Lua error in package.lua at line 80: module 'Module:InfoboxImage/data' not found. Lord Howe Seamount Chain (yellow are seamounts, red islands) | |
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| Location | |
| Location | Coral and Tasman seas |
| Coordinates | Lua error: callParserFunction: function "#coordinates" was not found. |
| Geology | |
| Type | Seamount chain |
| Age of rock | |
The Lord Howe Seamount Chain formed during the Miocene. It features many coral-capped guyots and is one of the two parallel seamount chains alongside the east coast of Australia; the Lord Howe and Tasmantid seamount chains both run north-south through parts of the Coral Sea and Tasman Sea.[2][1] These chains have longitudes of approximately 159°E and 156°E respectively.[2]
Geography
The Lord Howe Seamount Chain has been known under a variety of different gazetted names, including the Lord Howe Seamounts, Lord Howe Guyots, Lord Howe Rise Guyots and the Middleton Chain.[3]
The Lord Howe Seamount Chain is on the western slope of Lord Howe Rise, a deep-sea elevated plateau which is a submerged part of Zealandia.[2][4] The Tasmantid and Lord Howe seamount chains are both broadly within the Tasman basin which is the abyssal plain between Lord Howe Rise and the Australian continental shelf. The two chains lie on opposite sides of the Dampier Ridge which is believed to be a submerged continental fragment, that is over 250 million years old, and had split from the Australian plate during Tasman Sea formation.[5] Earlier magnetic studies suggest that the Dampier Ridge is adjunct to the Tasman Sea's former extinct mid oceanic ridge,[6] and it had been postulated to be much younger.[2]
The Lord Howe Seamount Chain extends from north of the Chesterfield group of islands (17°S)[1] to Flinders Seamount (34.7°S).[7] It includes the officially named Nova Bank, Argo and Kelso seamounts, Capel and Gifford guyots, Middleton and Elizabeth reefs, Lord Howe Island and Ball's Pyramid.[2]
Geology
The Lord Howe and Tasmantid chains each resulted from the Indo-Australian Plate moving northward over a stationary hotspot; historically the hotspot for the Lord Howe chain was expected to presently be beneath Flinders Seamount.[8] but is now thought likely to be somewhat to the south of this, possibly beyond the Heemskerck and Zeehaen seamounts.[9] Indeed the dating of this chain has only been as far south as Lord Howe Island which erupted 6.5 million years ago and there are other gaps in relevant knowledge of this hotspot chain. The chain has now been characterised by compositional analysis to be related at 28 million years to the South Rennell Trough spreading center as its potential initiation point with lessening magma being erupted progressively as the younger seamounts of the hot spot were formed.[1][9] On the Australian mainland, a third north-south sequence of extinct volcanoes (which includes the Glass House Mountains) is likely to have the same origin.[8][10] The Lord Howe Seamount Chain includes the following features:
| Seamount | Location | Age | Notes |
|---|---|---|---|
| Zeehaen Seamount | Lua error: callParserFunction: function "#coordinates" was not found. | [11][12] | |
| Heemskerck Seamount | Lua error: callParserFunction: function "#coordinates" was not found. | [11] | |
| Flinders Seamount | Lua error: callParserFunction: function "#coordinates" was not found. | [11] | |
| Ball's Pyramid | Lua error: callParserFunction: function "#coordinates" was not found. | Island.[11] | |
| Lord Howe Island | Lua error: callParserFunction: function "#coordinates" was not found. | 6.9 to 6.4 Ma | Island.[11][12][13] |
| Elizabeth Reef | Lua error: callParserFunction: function "#coordinates" was not found. | Coral reef features are above sea level.[11] | |
| Middleton Reef | Lua error: callParserFunction: function "#coordinates" was not found. | Coral reef features are above sea level.[11] | |
| Gifford Guyot | Lua error: callParserFunction: function "#coordinates" was not found. | [11] Dating of seamount top sediments is consistent with expected seamount age progression[14] | |
| Capel Bank | Lua error: callParserFunction: function "#coordinates" was not found. | [11] Dating of seamount top sediments is consistent with expected seamount age progression[14] | |
| Kelso Bank | Lua error: callParserFunction: function "#coordinates" was not found. | [11] | |
| Argo Bank | Lua error: callParserFunction: function "#coordinates" was not found. | [11] | |
| Nova Bank | Lua error: callParserFunction: function "#coordinates" was not found. | 23 Ma | [11][13] |
| Chesterfield Plateau | Lua error: callParserFunction: function "#coordinates" was not found. | 28.1 ± 1.0 Ma | [1] |
| Horsehead Seamount | Lua error: callParserFunction: function "#coordinates" was not found. | 27.24 ± 0.24 Ma | [1] |
| South Rennell Trough | 28 Ma | [1] |
See also
References
Page Template:Reflist/styles.css has no content.
- ^ a b c d e f g Page Module:Citation/CS1/styles.css has no content.Seton, Maria; Williams, Simon; Mortimer, Nick; Meffre, Sebastien; Micklethwaite, Steven; Zahirovic, Sabin (2019-01-22). "Magma production along the Lord Howe Seamount Chain, northern Zealandia". Geological Magazine. 156 (9): 1605–1617. Bibcode:2019GeoM..156.1605S. doi:10.1017/S0016756818000912.
- ^ a b c d e Page Module:Citation/CS1/styles.css has no content.van der Linden, W. J. M. (1970). "Morphology of the Tasman sea floor". New Zealand Journal of Geology and Geophysics. 13: 282–291. Bibcode:1970NZJGG..13..282V. doi:10.1080/00288306.1970.10428218.
- ^ Page Module:Citation/CS1/styles.css has no content."Marine Gazetteer Placedetails". Retrieved 2017-02-20.
- ^ Page Module:Citation/CS1/styles.css has no content.Luyendyk, Bruce P. (April 1995). "Hypothesis for Cretaceous rifting of east Gondwana caused by subducted slab capture". Geology. 23 (4): 373–376. Bibcode:1995Geo....23..373L. doi:10.1130/0091-7613(1995)023<0373:HFCROE>2.3.CO;2.
- ^ Page Module:Citation/CS1/styles.css has no content.McDougall, I.; Maboko, M. A. H.; Symonds, P. A.; McCulloch, M. T.; Williams, I. S.; Kudrass, H. R. (1994). "Dampier Ridge, Tasman Sea, as a stranded continental fragment". Australian Journal of Earth Sciences. 41 (5): 395–406. doi:10.1080/08120099408728150.
- ^ Page Module:Citation/CS1/styles.css has no content.van der Linden, W. J. M. (1969). "Extinct mid-ocean ridges in the Tasman sea and in the Western Pacific". Earth and Planetary Science Letters. 6 (6): 483–490. Bibcode:1969E&PSL...6..483V. doi:10.1016/0012-821X(69)90120-4.
- ^ Przeslawski et al. Biogeography of the Lord Howe Rise region, Tasman Sea. Deep-Sea Research Part II 58 (2011) 959–969.
- ^ a b W. J. Morgan and J. P. Morgan. Plate velocities in hotspot reference frame: electronic supplement
- ^ a b Page Module:Citation/CS1/styles.css has no content.Hansma, Jeroen; Tohver, Eric (2020). "Southward Drift of Eastern Australian Hotspots in the Paleomagnetic Reference Frame Is Consistent With Global True Polar Wander Estimates". Frontiers in Earth Science. 8: 489. Bibcode:2020FrEaS...8..489H. doi:10.3389/feart.2020.544496.
- ^ Page Module:Citation/CS1/styles.css has no content.Knesel, Kurt M.; Cohen, Benjamin E.; Vasconcelos, Paulo M.; Thiede, David S. (August 2008). "Rapid change in drift of the Australian plate records collision with Ontong Java plateau". Nature. 454 (7205): 754–757. Bibcode:2008Natur.454..754K. doi:10.1038/nature07138. ISSN 0028-0836. PMID 18685705. S2CID 4427792.
- ^ a b c d e f g h i j k l Page Module:Citation/CS1/styles.css has no content."GEBCO Undersea Feature Names Gazetteer".
- ^ a b Page Module:Citation/CS1/styles.css has no content.Douglas (Smethurst), Amelia (2022). The East Australian, Tasmantid and Lord Howe volcanoes : exploring the origins of three, contemporaneous, parallel chains of volcanism. (PhD thesis and appendix) (Thesis). doi:10.7488/era/2805. Retrieved 2023-03-30.
- ^ a b Page Module:Citation/CS1/styles.css has no content.McDougall, I; Embleton, B; Stone, D (1981). "Origin and evolution of Lord Howe Island, southwest Pacific Ocean". Journal of the Geological Society of Australia. 28 (1–2): 155–76. Bibcode:1981AuJES..28..155M. doi:10.1080/00167618108729154.
- ^ a b Page Module:Citation/CS1/styles.css has no content.Quilty, Patrick G. (1993). "Tasmantid and Lord Howe seamounts: biostratigraphy and palaeoceanographic significance". Alcheringa: An Australasian Journal of Palaeontology. 17 (1): 27–53. Bibcode:1993Alch...17...27Q. doi:10.1080/03115519308619487.
