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・ Tasmanian One Design
・ Tasmanian Open
・ Tasmanian opium poppy farming industry
・ Tasmanian pademelon
・ Tasmanian polar network
・ Tasmanian Ports Corporation
・ Tasmanian power referendum, 1981
・ Tasmanian pygmy possum
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・ Tasmanian Rugby League
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Tasmanian Seamounts
・ Tasmanian smelt
・ Tasmanian Softball Council
・ Tasmanian South East
・ Tasmanian Southern Ranges
・ Tasmanian state election, 1909
・ Tasmanian state election, 1912
・ Tasmanian state election, 1913
・ Tasmanian state election, 1916
・ Tasmanian state election, 1919
・ Tasmanian state election, 1922
・ Tasmanian state election, 1925
・ Tasmanian state election, 1928
・ Tasmanian state election, 1931
・ Tasmanian state election, 1934


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Tasmanian Seamounts : ウィキペディア英語版
Tasmanian Seamounts

The Tasmanian Seamounts (also ''Tasman Seamounts'' and ''Tasmania Seamounts'') are a group of seamounts (underwater volcanoes) located off the southern tip of Tasmania. The seamounts were created more than 55 million years ago by the Tasman hotspot. The seamounts are ecologically important, and harbor a lush marine ecosystem, but are threatened by overfishing. For this reason, part of the Tasmanian Seamounts were incorporated into a marine reserve in 1999.
== Geology ==
The Tasmanian Seamounts were created by the Tasman hotspot, a long mantle plume that is currently the active center of Mount Erebus in Antarctica.〔 The seamounts, created roughly 55 million years ago, are between deep, across, and tall.〔

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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