
Bridalveil Fall descending through granite cliffs above the forested valley floor in afternoon light, Yosemite National Park, California.
Bridalveil Fall is a single-drop waterfall descending from the cliffs at the entrance to Yosemite Valley, forming a narrow stream that falls freely into the valley below. The fall is defined by its clean vertical drop and the way wind can disperse the water as it descends. The composition resolves through the vertical line of water against the surrounding rock face.
37.71681, -119.64677
Gallery
Quick Facts
Access
Roadside / Step-out
0–5 min
Elevation Gain
5 m
Best Light
Diffuse light reduces contrast between water and rock, allowing the fall to remain clearly defined without harsh shadow.
Why This Light
Season
Seasonally Distinct
Spring provides stronger water flow from snowmelt, creating a more continuous fall. In drier periods, reduced flow and wind can break the stream into dispersed mist.
Crowds
Often Busy
Restrictions
Access is via a short paved path from roadside parking; viewpoints are located near the base of the fall.