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The Geology of Walla Walla Wine Country

Discover how ancient floods, volcanic eruptions, and millions of years of geology helped shape one of the Columbia Basin's distinctive wine landscapes.

Did You Know?

Fascinating facts about Walla Walla's geological heritage

At peak flow, the Missoula Floods discharged roughly 10 times the combined flow of every river on Earth — a volume of water per second that dwarfs anything in the modern hydrological record.

mind blowing

Wind-blown loess deposits in some Walla Walla vineyards exceed 30 feet in depth — and in parts of the broader Columbia Basin, loess can reach over 100 feet.

statistic

The floods traveled at speeds up to 65 mph—faster than most rivers flow during major hurricanes.

comparison

The combination of basalt, loess, and flood deposits found beneath Walla Walla's vineyards is characteristic of the Columbia Basin — a geological foundation shared with the Yakima Valley, Horse Heaven Hills, and Pasco Basin.

wine connection

Some vineyards have vine roots extending 30+ feet deep through multiple geological layers.

wine connection

Geology Expertise

KP

Dr. Kevin R. Pogue

Dr. Kevin R. Pogue is a professor in the Department of Geology at Whitman College in Walla Walla, Washington. He also regularly contributes lectures and leads field trips for the Enology and Viticulture program at Washington State University.

Dr. Pogue's research focuses on variations in growing conditions related to vineyard topography, climate, and soil chemistry. He has authored petitions for federally sanctioned American Viticultural Areas and has been honored by the Washington State Wine Commission for his contributions to the Washington wine industry.

Plan Around the Landscape

Use geology as a planning lens for your Walla Walla visit. We can help connect vineyard districts, soil stories, and winery stops in a way that feels coherent.

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Plan a Geology-Focused Visit

We'll help you find the right mix of wineries, viewpoints, and educational context.