Multnomah Falls, Waterfall in Columbia River Gorge, United States.
Multnomah Falls drops about 540 feet (165 meters) in two separate tiers, with the upper cascade accounting for most of the height and the lower forming a shorter descent. The rock wall behind the falling water is made of several layers of volcanic basalt, clearly visible and formed over millions of years.
Simon Benson funded a stone footbridge in 1914 that allowed visitors to view both tiers of the waterfall from close range. The site opened to the public shortly after and quickly became a popular destination in the Pacific Northwest.
The name recalls the Multnomah tribe who lived along this section of the Columbia River before European settlers arrived. The Benson Bridge, which spans the waterfall, honors the businessman who had it built in the early twentieth century.
A paved path leads from the road to the viewing platform at the base, while a steeper trail climbs to the bridge and onward to the top rim. The lower platform is accessible without stairs, but higher areas require climbing steps and a longer ascent.
Underground springs feed the falls throughout the year, keeping a steady flow even during dry summer months. During colder winter temperatures, icicles often form along the rock wall, giving the place an entirely different appearance.
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