Crocodile Rock Introduction
Crocodile Rock is formed by the accumulation of volcanic ejecta, shaped by the erosion of coral reefs and the movement of the Earth's crust. The rock's joints are fractured, resembling the rough skin of a crocodile, as it rises from the coastline with its mouth opened wide, displaying two rows of sharp teeth, thus earning its name. The geological layers of Lanyu mainly consist of andesitic lava containing amphibole and basaltic conglomerate, alongside Pleistocene red clay, uplifted coral reefs, and Holocene alluvial, colluvial deposits, and coastal skirt reefs. Through the natural processes of marine erosion and weathering, Lanyu's most intriguing rock formations have been sculpted. The Tao people (Yami) refer to Crocodile Rock as ji-macingeR, describing its elongated shape, like a waist that has been tightly bound, creating a slender appearance. Sheep are often seen grazing on Crocodile Rock, giving the impression of being swallowed by the wide-open mouth of a crocodile, creating a rather interesting scene. In addition to Crocodile Rock, Lanyu is also famous for other unique rock formations, including Red Head Rock, Battleship Fish Rock, Twin Lion Rock, Dragon Head Rock, Old Man Rock, Hen Rock, Jade Girl Rock, Five Holes Cave, Tank Rock, Steel Helmet Rock, and Steamed Bun Rock.
