Chih Yu (Moses Crossing) Introduction
Chiyu, located to the east of Kuibi Mountain in Beiliao, is approximately 120 meters long and 60 meters wide. It becomes an isolated small island at high tide. Beneath the southeastern cliff of the island, there is a sedimentary layer made of tuff, with some layers appearing red due to iron oxidation, showing clear stratification. Small faults can be found between the layers, indicating past movements. Chiyu features typical basalt columnar structures and veins, resembling a small volcanic vent (with radial and circular structures), as well as unique marine organisms. At high tide, it becomes an isolated island, making it valuable for research and education. The seabed terrain between Kuibi Mountain and Chiyu is quite special; when the tide rises and falls, waves hit the center from both sides. At low tide, a gravel path about 500 meters long and 3 meters wide connects Chiyu to the main island, allowing visitors to enjoy the fun of wading through waves in the intertidal zone without harming the ecology, making it highly recommendable. It is important to pay attention to the timing of wading, and it is suggested that the best time to wade at Kuibi Mountain is about two hours after high tide begins to recede. [Recommended stay time] 1 hour.
Chiyu Island
