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In
December 1882, however, a Lloyd's agent at Rarotonga reported that the Haymet rocks were supposed to exist about 150 miles (240 km) SSW of Rarotonga, and therefore right in the track of vessels bound from Auckland to that island, who always give this supposed position a wide berth. If this
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in 1887; the latter vessel spent three days in the search under favourable circumstances of wind and weather, running over some 253 miles (407 km) within a radius of from 20 to 25 miles (32 to 40 km) of the position assigned, and with no result. A depth of 68 fathoms (124 m) to the
55:. The rocks are said to extend over a space of about a quarter of a mile, to have been distinctly seen, and with apparently 7 or 8 feet (2.1 or 2.4 m) of water over them. Haymet gave their position as
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information is correct, these rocks are about 240 miles (385 km) NNW of the position as given by Haymet and still shown on the charts.
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195:"About the Cook Islands. Their Nomenclature and a Systematic Statement of Early European contacts"
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These rocks were unsuccessfully searched for, in the position given, by HMS
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Lost
Islands: The Story of Islands That Have Vanished from Nautical Charts
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It was suggested that the Haymet Rocks were a remnant of sunken island
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were reported by J.E. Haymet, master and owner of the cutter
241:. Vancouver: University of British Columbia Press. p.
97:in 1886, and again by the French Government vessel
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279:, a publication from 1900, now in the
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270:This article incorporates text from
199:Journal de la Société des océanistes
23:1924 map of Central Polynesia, with
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165:"THE MYSTERY OF TUANAKI ISLAND",
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302:Reefs of the Pacific Ocean
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193:Coppell, W. G. (1973).
168:Pacific Islands Monthly
175:(7): 104, 1952-02-01,
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283:in the United States.
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291:Categories
216:2018-01-18
205:(38): 46.
53:false keel
41:Will Watch
181:0030-8722
95:Satellite
88:Orne Bank
49:Rarotonga
233:(1984).
116:158°33′W
65:160°13′W
45:Auckland
25:Haymet R
146:Tuanaki
62:27°11′S
276:, v. 3
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113:24°7′S
104:Fabert
99:Fabert
29:Orne B
152:Notes
247:ISBN
177:ISSN
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
