Chiyu (Moses Crossing) Introduction
Chiyu, located to the east of Mt. Kueibi, measures approximately 120 meters in length and 60 meters in width. During high tide, it becomes an independent small island. At the southeastern cliffs of the island, there is a layer of sedimentary rock composed of tuff. Some of the rock layers appear red due to iron oxidation, with clear stratification, and tiny faults can be seen among the layers, indicating previous movements in the rock formations. Chiyu features typical basalt column structures, intrusions, resembling a small volcanic vent (with radial and circular formations) and unique marine life. At high tide, it becomes isolated, making it highly valuable for research and education. The nearby waters between Mt. Kueibi and Chiyu have a unique topography: when the tide rises and falls, the waves crash towards the center from both sides. During low tide, Chiyu reveals a gravel pathway about 500 meters long and 3 meters wide that connects it to the main island. Walking along the basalt pebble path during low tide is reminiscent of the fun of crossing the Red Sea, while posing no threat to the ecosystem, making it highly recommended. Visitors should be mindful of the timing when walking along the shore; it is suggested that the best time for exploring Mt. Kueibi is about two hours after high tide begins to recede. 【Recommended duration of stay】 1 hour.
Chiyu Island
