The site contains fossils and exotic rock fragments embedded in mudstone that originated deep within the ocean floor.
The 'Liji Melange' is a geological term for this specific mixture of crushed rock and mudstone formed by tectonic activity.
The area is prone to rapid transformation; the landscape appearance changes noticeably after every typhoon or heavy rain event.
Mudstone at this site has high sodium content, which prevents most plants from taking root in the soil.
The Beinan River, located adjacent to the park, is responsible for the ongoing downcutting that exposes the internal geological layers.
Liji Badland Geopark is a geological formation characterized by highly eroded mudstone slopes known as the Liji Melange. The landscape is defined by deep gullies and jagged ridges created by the rapid erosion of soft, clay-rich soil during heavy rainfall. It is located at the southern terminus of the Coastal Mountain Range. The area displays a distinct lack of vegetation due to the high salinity and unstable nature of the sediment. The site is a primary location for observing the collision boundary between the Eurasian Plate and the Philippine Sea Plate. It overlooks the Beinan River, which cuts through the valley and contributes to the surrounding silt-heavy topography. The park is managed as part of the East Rift Valley National Scenic Area.
The elevated observation platform providing a panoramic view of the mudstone gullies against the backdrop of the Beinan River.
Wear sturdy, closed-toe hiking shoes as the terrain is loose, dusty, and slippery when wet.
Bring a hat and high-SPF sunscreen, as there is almost no natural shade provided by trees or high structures.
Carry at least one liter of water, as the lack of vegetation makes the area significantly hotter than the surrounding region.
Do not attempt to hike or climb the mudstone slopes; they are extremely fragile and susceptible to collapse under human weight.
Stay on marked trails to avoid contributing to erosion and to prevent slipping on unstable slopes.
