Crocodile Rock Introduction
Crocodile Rock is formed by volcanic debris accumulation and is shaped by coral reef erosion and tectonic movements, resulting in the rock's fractures resembling the rough skin of a crocodile. The rock rises from the coastline with its mouth wide open, revealing two rows of sharp teeth, which is how it got its name. The geological layers of Lanyu consist mainly of hornblende andesite lava and basaltic agglomerate, along with Pleistocene red soil layers, uplifted coral reefs, as well as Holocene alluvial, colluvial, and coastal fringe deposits, all sculpted into Lanyu's most fascinating rock formations through natural sea erosion and weathering processes. The Tao people (Yami) refer to Crocodile Rock as ji-macingeR, describing its elongated shape that resembles a waist being tightly bound, giving it a slender appearance. Often, flocks of sheep can be seen climbing the rock, reminiscent of being swallowed by the open mouth of a crocodile, creating a rather amusing scene. In addition to Crocodile Rock, Lanyu is also famous for other remarkable rock formations, including Red Head Rock, Warship Fish Rock, Twin Lions Rock, Dragon Head Rock, Old Man Rock, Hen Rock, Jade Girl Rock, Five Holes Cave, Tank Rock, Helmet Rock, and Bun Rock.
