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Scientists Detect Something Bizarre in Subterranean Structures Under the Great Salt Lake

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Why This Matters

The discovery of a vast freshwater reservoir beneath the Great Salt Lake challenges previous assumptions about its composition and has significant implications for water resource management and environmental monitoring. This finding could influence future scientific research, conservation efforts, and regional water policies, highlighting the importance of advanced geophysical techniques in uncovering hidden natural resources.

Key Takeaways

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The Great Salt Lake is harboring an unexpected secret: a huge stash of water that’s decidedly not salty.

A team of researchers who x-rayed its subterranean structures discovered that lurking below its briny surface is a vast and miles-deep reservoir of freshwater.

The findings, detailed in a new study in the journal Scientific Reports, upend expectations that any freshwater presence would be small and relegated to the lake’s outskirts, dumped there by nearby mountains. In reality, it appears that possibly the entire saltwater lake is undergirded by freshwater.

“We were able to answer the question of how deep this potential reservoir is, and what its spatial extent is beneath the eastern lake margin. If you know how deep, you know how wide, you know the porous space, you can calculate the potential freshwater volume,” said lead author Michael Zhdanov, a geophysicist at the University of Utah, in a statement about the work.

Scientists had a sneaking suspicion that there was a hidden freshwater presence with the sudden appearance in the past few years of large mounds of reeds popping up in regions of dry exposed lakebed called playa.

To probe the depths beneath the lake, the researchers conducted what’s known as airborne electromagnetic surveys by flying over the saltwater body in a helicopter and pointing instruments that measure the electrical conductivity on the ground. The resulting signals help distinguish between salt and fresh water — salt makes the liquid it’s suspended in far more conductive — and tease out the composition of the rocks and soils.

Some 154 miles of flying later, the team had collected the data they were looking for. After using it to create a map of the lake, they found that spikes of resistive fresh water were turning up everywhere.

That clued them in to an even bigger find: a sudden drop in the lake’s subterranean layer called a basement, going from just a few hundred yards deep to over 2.5 miles. The freshwater appears to be saturating sediments trapped in this region, forming a deep reservoir.

Bill Johnson, a UT hydrologist and coauthor of the study, called the findings “unexpected.”

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