How did the Navajo Sandstone form in the western interior of North America?

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The Navajo Sandstone formed during the Early Jurassic period when the western interior of North America was covered by a vast sand sea, or erg. This massive accumulation of dune sands represents one of the largest such deposits in the geologic record and remains prominent today in locations such as Zion National Park in Utah.1

While the western interior was later characterized by marine incursions—specifically the Carmel and Sundance seas—during the Middle Jurassic, the Navajo Sandstone itself is associated with the earlier, arid desert environment that preceded these epicontinental seaways.21