Spots:青灣柱狀玄武岩
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From PHSea
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| Revision as of 17:29, 1 April 2006 Ebee (Talk | contribs) ← Previous diff |
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| - | *'''景點：''' | + | *'''景點：'''青灣柱狀玄武岩 |
| - | **青灣柱狀玄武岩(201[[縣道]]上[[嵵裡沙灘]]到[[風櫃聽濤]]段的左邊的山頭) [[Image:青灣玄武岩.jpg]] | + | *'''位置'''：(201[[縣道]]上[[嵵裡沙灘]]到[[風櫃聽濤]]段的左邊的山頭) [[Image:青灣玄武岩.jpg|280px|thumb|right|藍天綠草輝映的青灣玄武岩就在往風櫃縣道上的左方，騎車經過時記得留神看看南環最美的玄武岩山壁]] |
| *'''介紹：''' | *'''介紹：''' | ||
| - | **澎湖群主要由玄武岩組成，係熔岩經過多次由地底裂隙湧出地表冷卻形成，目最早的火山熔岩，約在一千八百萬年前寧靜噴發，大概在800萬年前中止火山運動。澎湖由玄武岩構成了方山地形，四周岩壁陡峭，長期就過風化，風蝕以及海蝕作用後，便會發展出各種獨特的地形景觀，加上岩體常會因熔岩急速收縮冷卻而產生張力，使岩石產生多角柱狀的破裂，此破裂面稱為柱狀節理。有平直，彎曲或各種方向的傾斜，成為澎湖玄武岩景觀中最具特色的風貌。 | + | **澎湖群主要由玄武岩組成，係熔岩多次由地底裂隙湧出地表冷卻形成，目前最早的火山熔岩，約在一千八百萬年前寧靜噴發，大概在800萬年前中止火山運動。澎湖由玄武岩構成了方山地形，四周岩壁陡峭，長期經過風化、風蝕以及海蝕作用後，發展出各種獨特的地形景觀，加上岩體常會因熔岩急速收縮冷卻而產生張力，使岩石產生多角柱狀的破裂，此破裂面稱為柱狀節理。有平直、彎曲或各種方向的傾斜，成為澎湖玄武岩景觀中最具特色的風貌。 |
| - | **澎湖各地柱狀玄武岩以桶盤嶼柱狀玄武岩最為有名氣，而澎南地區則在青灣到風櫃間的馬路左手邊可以清楚看到一片山頭就是呈現柱狀玄武岩的分佈，藍天搭配黝黑的玄武岩巨石，氣勢滂薄，超脫獨立，右邊則是澎湖內海加上筆直無人的201[[縣道]]，風景渾然天成，騎車往風櫃的路途上不妨留意這一次青灣玄武岩。 | + | |
| + | **澎湖各地柱狀玄武岩以桶盤嶼柱狀玄武岩最有名氣，而澎南地區則在青灣到風櫃間的馬路左手邊可以清楚看到一片山頭就是呈現柱狀玄武岩的分佈，藍天搭配黝黑的玄武岩巨石，氣勢滂薄，超脫獨立，右邊則是澎湖內海加上筆直無人的201[[縣道]]，風景渾然天成，騎車往風櫃的路途上不妨留意這一次青灣玄武岩。 | ||
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| + | ! <h2 style="margin:0;background-color:#fff078;font-family:sans-serif;font-size:130%;font-weight:bold;border:1px solid #a3b0bf;text-align:left;color:#000;padding-left:0.4em;padding-top:0.2em;padding-bottom:0.2em;">我有問題要舉手發問： | ||
| + | *對於本文有任何問題，請前往站內[https://www.phsea.com.tw/phseaforum/forums/list.page 澎湖行程規劃討論區]提問 | ||
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Current revision
- 景點：青灣柱狀玄武岩
- 位置：(201縣道上嵵裡沙灘到風櫃聽濤段的左邊的山頭)
藍天綠草輝映的青灣玄武岩就在往風櫃縣道上的左方，騎車經過時記得留神看看南環最美的玄武岩山壁
- 介紹：
- 澎湖群主要由玄武岩組成，係熔岩多次由地底裂隙湧出地表冷卻形成，目前最早的火山熔岩，約在一千八百萬年前寧靜噴發，大概在800萬年前中止火山運動。澎湖由玄武岩構成了方山地形，四周岩壁陡峭，長期經過風化、風蝕以及海蝕作用後，發展出各種獨特的地形景觀，加上岩體常會因熔岩急速收縮冷卻而產生張力，使岩石產生多角柱狀的破裂，此破裂面稱為柱狀節理。有平直、彎曲或各種方向的傾斜，成為澎湖玄武岩景觀中最具特色的風貌。
- 澎湖各地柱狀玄武岩以桶盤嶼柱狀玄武岩最有名氣，而澎南地區則在青灣到風櫃間的馬路左手邊可以清楚看到一片山頭就是呈現柱狀玄武岩的分佈，藍天搭配黝黑的玄武岩巨石，氣勢滂薄，超脫獨立，右邊則是澎湖內海加上筆直無人的201縣道，風景渾然天成，騎車往風櫃的路途上不妨留意這一次青灣玄武岩。
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