火山集塊岩是指岩漿經火山爆發碎裂成大於64mm的岩塊所膠結組成的岩石;若其出火山口時仍是液態,形成的顆粒呈圓滑狀,此種顆粒稱為「火山彈」;膠結所成的岩石稱集塊岩。主要出露在近火山口、噴發能力較強的火山,如赤嶼、煙屯山、鳥嶼北岸、東吉港旁海蝕平台等地區。本中心所收藏的標本來自東吉嶼。
火山集塊岩是指岩漿經火山爆發碎裂成大於64mm的岩塊所膠結組成的岩石;若其出火山口時仍是液態,形成的顆粒呈圓滑狀,此種顆粒稱為「火山彈」;膠結所成的岩石稱集塊岩。主要出露在近火山口、噴發能力較強的火山,如赤嶼、煙屯山、鳥嶼北岸、東吉港旁海蝕平台等地區。本中心所收藏的標本來自東吉嶼。
Volcanic agglomerates refer to the magma that is broken into rocks larger than 64mm by volcanic eruption. If the rock is still liquid when it comes out of the crater, it will form smooth particles, which are called “volcanic bomb”,the rocks formed by cementation are called agglomerates, which are mainly exposed in volcanic areas near the craterswith strong eruption capacity, such as Chiyu, Yantun Hill, the north shore of Niaoyu,the marine erosion platform next to Dongji Port. The specimens collected by this center are from Dongjiyu.