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赤尾嶼Chihwei Island

赤尾嶼Chihwei Island

文章Lohas 發表於 2008年 4月 11日, 11:02

圖檔
赤尾嶼具有典型之玄武岩柱狀構造、岩脈,類似小型火山噴口(具有放射狀與環狀構造),及珍奇海洋生物,漲潮時成一孤島,形勢孤立,極具研究與教育價值。

由於奎壁山附近海域地形相當特殊,海浪由兩側向往中間拍打,退潮時踏浪前往數百公尺遠的赤嶼,在3公尺寬的鵝卵石潮間帶踏浪前往赤嶼,那種循著落日向大海前進的感覺,讓人有一種時空錯亂之感。 不過旅客要注意踏浪時間,一般來說,滿潮開始退潮二小時左右的時間是奎壁山踏浪最好的時機。


Chihwei Island features classic basalt pillar formations, dikes, small volcano-like vents (radiating and circular structures) and unusual marine life. The area is considered of great research and educational value, and at high tide it becomes an island.
The waters near Mt. Kueibi are quite unusual as the waves come in from two sides to merge in the middle. At low tide, a 3m wide intertidal zone covered with pebbles appears, making it possible to walk to the Chih Island several hundred meters away. Walking into the sea at sunset here provides quite an otherworldly experience. Visitors should however pay attention to the surf walking times. Generally speaking it is best to begin the surf walk at Mt. Kueibi about two hours after the tide begins to go out.


赤尾嶼

類型:レジャースポット

區域:湖西郷

赤尾嶼には典型的な玄武岩の柱状構造や岩脈があり、小型噴火口様構造(放射状および環状構造)や珍しい海洋生物が見られます。満潮時には離れ小島となり、研究や教育的価値の高い地域と言えます。

Chihwei Island

Chihwei Island contains basalt of a typical columnar structure, so it is like a tiny volcanic orifice (with radial and ring structure). There are also substantial marine creatures in and around the islet. Chihwei Islandis an isolated islet during the rising tide, and because of its isolation, it is valuable for research and education.
Lohas
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文章: 9394
註冊時間: 2008年 3月 9日, 09:11
來自: 樂活澎湖灣

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