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Around 30 million years ago, a flood basalt plateau began to form, piling layers upon layers of voluminous fissure-fed basaltic lava flows.
Most of the flows were tholeiitic, save for a thin layer of alkali basalts and minor amounts of felsic ( high-silica ) volcanic rocks, such as rhyolite.
In the waning stages of the flood basalt episode, large explosive caldera-forming eruptions also occurred.

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