Limestone karst setting
The falls are shaped by soluble limestone terrain, terraces, pools, and divided channels. The setting is different from basalt or granite waterfall records because karst structure controls much of the stepped form.
Stepped drops and border-river flow
River flow spreads across multiple lips and terraces, creating a broad waterfall complex rather than one clean vertical fall.
Rock
Limestone terraces
Karst surfaces shape the waterfall steps.
Water
Border river
The falls sit on an international river corridor.
Form
Segmented channels
Divided flow creates multiple cascades.