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How does mountain belt loading affect foreland basins?

Foreland basins develop adjacent and parallel to mountain belts because the immense mass generated by crustal thickening forces the underlying lithosphere to bend through lithospheric flexure. This downward flexure creates the accommodation space necessary for thick layers of eroded sediment to accumulate. The exact width and depth of these basins depend heavily on the flexural rigidity of the lithosphere and the characteristics of the adjacent mountain belt.

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