The park's unique 'onion-like' weathering patterns are a rare geological feature in the Taipei basin.
The site was historically the primary source of raw materials for Taiwan's porcelain and brick-making industries.
In 1977, a major debris flow disaster triggered by Typhoon Thelma led to the government’s decision to transform the area into a soil conservation demonstration project.
The exposed geological layers represent a chronological sequence of sedimentary deposition spanning millions of years.
The park integrates engineering works like drainage channels and slope retaining walls directly into its walking paths.
The name 'Guizikeng' is derived from a local Hokkien term referring to the valley's history of clay extraction.
Guizikeng Soil and Water Conservation Education Park is a former clay mining site turned ecological educational area featuring distinct multi-colored geological strata. The park highlights the legacy of the Beitou ceramic industry, which relied on the local white kaolin clay deposits. Visitors can observe the 'Wuzhishan Formation,' a geological layer dating back 20 to 30 million years, which is exposed due to past open-pit mining. The site serves as a functional demonstration zone for soil conservation techniques, including check dams and drainage systems designed to prevent landslides. Extensive hiking trails connect the park to the larger Datun Mountain trail system. A small indoor exhibition hall provides context on regional geology and historical mining practices. The landscape is characterized by steep, rugged cliffs contrasted with man-made reservoirs and terraced forest restoration areas. It is an active facility for researchers and schools to study slope stability and watershed management.
The wide-angle vantage point looking up at the multi-colored sediment cliffs near the main reservoir.
Bring a portable fan and high-SPF sunscreen, as the exposed rocky areas offer very little shade during midday.
Wear hiking footwear with good grip, as the terrain consists of gravel, dirt paths, and occasional steep inclines.
Carry sufficient water, as there are no shops or convenience stores within the park boundaries.
Do not attempt to hike the connecting mountain trails during or immediately after heavy rain due to the high risk of slope instability.
Closed on Mondays for maintenance; the indoor visitor center may have restricted access during typhoons or extreme weather alerts.
Stay strictly on marked trails to prevent erosion; do not collect geological samples or remove rocks.
