The reef platforms are formed from uplifted coral limestone, a geological process resulting from the tectonic activity of the Philippine Sea Plate.
The pools host a micro-ecosystem that remains insulated from the deeper, stronger currents of the Taiwan Strait.
Local ecological regulations prohibit the removal or disturbance of any marine organisms found within the intertidal zone.
The sharp, porous surface of the coral rock is formed by biological and chemical weathering over thousands of years.
Duziping is a coastal tide pool formation located on the southwestern shoreline of Xiaoliuqiu, characterized by its extensive intertidal reef platforms. The site consists of fossil-rich coral limestone that has been eroded by wave action to create shallow, protected pools. It serves as a primary site for observing diverse marine life including sea cucumbers, brittle stars, and colorful anemones during low tide. The area is geologically part of the elevated coral reef terrain that defines much of the island's coastline. Access to the pools is dictated by the tide cycle, which exposes the reef flat twice daily.
The edge of the reef platform looking toward the horizon at low tide provides the best wide-angle perspective.
Wear thick-soled water shoes to protect feet from sharp coral edges.
Consult the local tidal chart prior to arrival as the pools are fully submerged at high tide.
Use polarized sunglasses to better see through the water surface into the tide pools.
Do not attempt to walk on the reef flats during high tide or high wave conditions for safety reasons.
Access is restricted during severe weather conditions or typhoons when coastal areas are closed for safety.
Do not touch or remove any marine life; stay on marked paths to prevent trampling coral growth.
