Tasmantid Seamount Chain
The Tasmantid Seamount Chain is a 2,000 km (1,200 mi) long chain of seamounts in the South Pacific Ocean. The chain consists of over 16 extinct volcanic peaks, many rising more than 4,000 m (13,000 ft) from the seabed.[1][2] It 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. These chains have longitudes of approximately 159°E and 156°E respectively.[3]
| Tasmantid Seamount Chain | |
|---|---|
![]() Topographic map of Zealandia that includes the unlabelled Tasmantid Seamount Chain (above the label Australia) off the east of Australia extending from the Coral Sea southwards into the Tasman Sea. | |
![]() Tasmantid Seamount Chain (click on location for individual names) | |
| Location | |
| Location | Coral and Tasman seas |
| Coordinates | 31°00′S 156°00′E |
| Geology | |
| Type | Seamount chain |
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Like its neighbour, the Tasmantid Seamount Chain has resulted from the Indo-Australian Plate moving northward over a stationary hotspot.[4] It ranges in age from 40 to 6 million years old.[1] Alternative names for the Tasmantid Seamount Chain include the Tasmantid Seamounts, Tasman Seamounts, Tasman Seamount Chain, Tasmantide Volcanoes or simply the Tasmantids.[5]
Features
The Tasmantid Seamount Chain includes the following:
- Barcoo Bank 32°35′00″S 156°15′00″E[6]
- Brisbane Guyot 26°59′00″S 155°05′00″E[6]
- Britannia Guyots 28°17′00″S 155°38′00″E[6]
- Cato Reef 23°13′S 155°34′E[6]
- Derwent Hunter Guyot 30°52′00″S 156°11′00″E[6]
- Fraser Seamount 24°26′00″S 155°17′00″E[6]
- Gascoyne Seamount 36°41′00″S 156°07′00″E[6]
- Kenn Reef 21°12′S 155°43′E[6]
- Moreton Seamount 26°01′00″S 154°58′00″E[6]
- Queensland Guyot 27°35′00″S 155°11′00″E[6]
- Recorder Guyot 25°12′00″S 154°56′00″E[6]
- Stradbroke Seamount 29°05′00″S 155°45′00″E[6]
- Taupo Bank 31°00′S 156°00′E[6]
- Wreck Reefs 22°11′S 155°20′E[6]
References
- "Tasmantid Seamounts of Australia". Retrieved 2017-02-20.
- Richards, F. D.; Kalnins, L. M.; Watts, A. B.; Cohen, B. E.; Beaman, R. J. (October 2018). "The Morphology of the Tasmantid Seamounts: Interactions Between Tectonic Inheritance and Magmatic Evolution" (PDF). Geochemistry, Geophysics, Geosystems. 19 (10): 3870–3891. doi:10.1029/2018GC007821. hdl:20.500.11820/10f58983-8003-4af7-8fdd-def2ed23b0be. S2CID 133360937.
- Van Der Linden, Willem J. M. (1970). "Morphology of the Tasman sea floor". New Zealand Journal of Geology and Geophysics. 13: 282–291. doi:10.1080/00288306.1970.10428218.
- W. J. Morgan and J. P. Morgan. Plate velocities in hotspot reference frame: electronic supplement.
- "Marine Gazetteer Placedetails". Retrieved 2017-02-20.
- "GEBCO Undersea Feature Names Gazetteer".


