Ginga and Ryusei waterfalls descending side by side through basalt cliffs in Sounkyo Gorge, Hokkaido

Ginga and Ryusei waterfalls flowing side by side down the vertical basalt walls of Sounkyo Gorge in autumn

Ginga Falls (Sounkyo)

Water Feature

Ginga Falls is a multi-stream waterfall within Sounkyo Gorge, where numerous narrow flows descend down a vertical rock face into the valley below. The water separates into thin strands across the cliff, forming a broad, segmented cascade. The composition resolves through repetition of vertical water lines against the dark rock surface.

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Gallery

Ginga and Ryusei waterfalls flowing side by side down the vertical basalt walls …

Ginga Falls (left) and Ryusei Falls (right) descending through the vertical rock…

Ginga Falls descending in multiple streams through the vertical rock walls of So…

Ginga Falls spreading across the rock face in layered streams within the steep w…

Quick Facts

Access

Roadside / Step-out

0–5 min

Elevation Gain

5 m

Best Light

Overcast

Diffuse light reduces contrast between white water and dark rock, allowing individual streams to remain distinct without harsh shadow.

Season

Seasonally Distinct

Summer provides consistent water flow with clear separation between individual streams. Winter introduces freezing conditions that partially transform the falls into ice formations.

Crowds

Often Busy

Restrictions

Access is from a roadside viewing area; movement is limited to designated viewpoints near the base of the gorge.

Photography Notes

The falls read through segmented flow, with position controlling how individual streams align across the rock face. Slight lateral movement changes spacing between streams and affects how evenly they distribute within the frame. Lower positions emphasise the vertical drop, while stepping back clarifies the full width of the cascade.

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