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石灰岩洞
Kaohsiung

壽山在180萬年前沉積形成最早的「古亭坑層」,為惡地地形,主要由深灰色泥岩所組成,插入一些細緻中粒的鬆散砂岩,易遇水軟化。約在125萬年前,壽山為淺水區域,生長大量之珊瑚、藻類、有孔蟲和貝殼,遺骸形成堅硬的石灰岩,覆蓋在古亭坑層上,形成所謂的「高雄石灰岩」,構成壽山的內部主體。後期侵蝕作用帶來大量泥沙沉積,珊瑚無法生存,珊瑚礁不再形成,此時形成砂岩及泥岩組成之「崎腳層」。後來岩層受到擠壓,發生隆起、褶皺、斷層和節理,高雄石灰岩崩落,岩塊堆積在壽山東南部,形成壽山石灰岩。經過風化、侵蝕和雨水的沖刷,帶走石灰岩旁的軟弱岩,使石灰岩更為突顯,造成壽山隨處可見嶙峋的礁岩、洞穴、峽谷、斷崖等地形。經歷長時間溶蝕的結果,使當地形成許多石灰岩洞,洞內可看到由碳酸鈣沉澱形成的鐘乳石、石筍、石柱,景觀十分奇特。

Copyright: Steven Ho
Type: Spherical
Resolution: 8192x4096
Taken: 31/10/2013
Geüpload: 03/02/2014
Published: 03/02/2014
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