The name 'Nevada' is derived from the Spanish word for 'snowy,' referencing the white appearance of the water as it descends.
Nevada Fall is located approximately 1.5 miles upstream from the smaller Vernal Fall.
The water flow is significantly regulated by the snowpack, with peak volume typically occurring during late spring and early summer snowmelt.
The rock formation forming the fall is part of the extensive granitic batholith that defines the Yosemite region.
The Mist Trail, which leads to the waterfall, was constructed by the Sierra Club in the late 1890s.
The Merced River continues to carve the deep canyon beneath the falls, contributing to the park's ongoing geological transformation.
Nevada Fall is a 594-foot waterfall on the Merced River located within Yosemite National Park. The waterfall features a distinctive white, twisting appearance caused by the water sliding over a massive granite cliff face. It is a major landmark along the Mist Trail, which provides hikers direct access to the base and brink of the falls. The waterfall is fed by the drainage basin of the Little Yosemite Valley. It represents the second major drop in the Merced River as it exits Yosemite Valley to the east. The structure consists of a massive granite cliff that drops into the canyon below.
The metal footbridge crossing the Merced River just below the waterfall offers a clear, full-frontal view of the plunge.
Bring a waterproof jacket, as the spray from the falls can create heavy mist, particularly during peak runoff.
Use trekking poles to assist with stability on the steep, granite-heavy segments of the trail.
Carry extra water, as the climb is strenuous and provides little shade in exposed sections.
Attempting to swim or enter the water near the brink of the falls, as the current is extremely powerful and dangerous.
The Mist Trail is often closed during winter months due to hazardous icy conditions and avalanche risk.
Stay on marked trails to protect sensitive alpine vegetation and prevent erosion; pack out all trash.
