Chiyu (Moses' Crossing) Introduction
Chihyu Island, located southeast of Kueibishan, measures approximately 120 meters in length and 60 meters in width. It becomes an independent small island during high tide. At the base of the southeastern cliff of the island, there is a sedimentary layer composed of tuff, some of which has turned red due to iron oxidation, showcasing clear stratification. Within the stratification, tiny faults can be found, indicating historical movements of the rock layers. Chihyu Island features typical basalt columnar structures, veins, and resembles a small volcanic vent with radial and circular formations, as well as unique marine life. During high tide, it turns into an isolated island, making it highly valuable for research and education. The sea terrain around Kueibishan and Chihyu Island is quite special—during the ebb and flow of tides, waves crash towards the center from both sides. When the tide goes out, a pebble pathway about 500 meters long and 3 meters wide emerges, connecting Chihyu Island to the mainland. Walking along the basalt pebble pathway at the intertidal zone, one can enjoy the fun of splashing through the waves similar to the Exodus of Moses, without harming the ecosystem. It is highly recommended. For those planning to visit, be mindful of the timing and it's suggested to go about two hours after high tide begins to recede, as this is the best time to enjoy the tidal flats at Kueibishan. [Recommended stay time] 1 hour
Chihyu Islet
