玄武岩冷卻時,因氣體在岩漿中來不及逸出而聚集在玄武岩內,便成為含氣孔柱玄武岩。
本中心所收藏的標本採自西嶼鄉池西村。
玄武岩冷卻時,因氣體在岩漿中來不及逸出而聚集在玄武岩內,便成為含氣孔柱玄武岩。
本中心所收藏的標本採自西嶼鄉池西村。
When the basalt cools down, the gas may accumulate inside the basalt because it does not have time to escape,thus forming thepore-bearing columnar basalt.The specimens collected by this center are from Chixi Village of Siyu Township.