The beach is formed by the rapid descent of sediments from the Liwu River and surrounding steep coastal mountains into the Pacific.
The water depth increases drastically within a few meters of the shore due to the immediate drop-off of the continental shelf.
The pebble composition is predominantly composed of marble and schist washed down from the Qingshui Cliff face.
The area is a recognized migration path for certain marine species due to the unique deep-sea topography near the coast.
Chongde Gravel Beach is characterized by its dramatic transition where the steep, towering cliffs of the Qingshui Cliff range meet the Pacific Ocean. The beach consists of smooth, multicolored pebbles rather than sand, resulting from the erosion of nearby mountains. It serves as a primary viewing point for the northern section of Taroko National Park's coastline. Strong ocean currents and deep water make this location strictly unsuitable for swimming. The site is a popular location for launching sunrise canoe expeditions. Its unique geological formation allows for high-contrast photography against the backdrop of the Central Mountain Range. The beach is exposed to high waves and shifting tides, which frequently rearrange the pebble patterns along the shore.
From the northern section of the beach looking southward toward the full span of the Qingshui Cliff range.
Wear sturdy, closed-toe footwear to navigate the unstable, loose pebble surface comfortably.
Stay well back from the shoreline as 'sneaker waves' are common and can pull visitors into deep water without warning.
Bring polarized sunglasses to reduce glare from the white marble pebbles and intense sunlight reflecting off the ocean.
Attempting to swim or wade in the water, as the steep underwater drop-off and strong undertows are extremely dangerous.
Do not remove pebbles from the beach, as this contributes to coastal erosion; stay within designated safety zones.
