The Zuriati Waterfall site, located in North Gorontalo Regency, has a beautiful natural panorama. The lithology that forms Zuriati Waterfall consists of three types of lithology, namely Vitric Tuff rocks, Crystalline Tuff rocks and Claystones. The geological unit in this area is equivalent to the Wobudu Breccia Unit (Tpwv) which is Pliocene in age, which is about 5.3 million years ago. The geological structure found at this site is fracture.
Figure 1. Zuriati Falls