The park preserves a portion of the 100-kilometer-long rupture line caused by the magnitude 7.3 Jiji earthquake.
The facility serves as an active research site for geologists studying tectonic shifts along the Chelungpu fault zone.
The exhibition hall was intentionally constructed to straddle the fault line rather than avoiding it, allowing for direct observation of the seismic scarring.
The park's design incorporates scientific monitors that record ongoing geological data from the surrounding terrain.
Chelungpu Fault Preservation Park is a specialized geological museum built directly over the surface rupture of the 1999 Chi-Chi earthquake in Taiwan. The primary exhibit is the preserved fault line itself, which remains exposed within the facility to demonstrate crustal deformation. The architecture features a distinct curved roof design intended to minimize environmental impact on the site. Exhibits utilize interactive displays to explain plate tectonics and seismic activity within the context of the island's unique geology. Visitors walk along elevated paths that traverse the physical evidence of the 2-meter vertical displacement caused by the quake. The facility is managed by the National Museum of Natural Science as a field station for earthquake research and public education.
The main exhibition hall catwalk provides the clearest, eye-level vantage point of the exposed fault scarp.
Wear comfortable, flat walking shoes to navigate the transition between outdoor park areas and indoor ramps.
Allocate time to view the introductory film, which provides essential context for interpreting the exposed fault line.
Combine your visit with the nearby 921 Earthquake Museum of Taiwan for a comprehensive understanding of the event.
Do not attempt to touch the exposed earth or geological formations, as the site is a protected research preservation zone.
Typically closed on Mondays.
