Fig. 3 Upper Mississippi long-profile evolution.

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Presentation transcript:

Fig. 3 Upper Mississippi long-profile evolution. Upper Mississippi long-profile evolution. The Pliocene long profile was reconstructed by identifying ancient river courses and buried strath terraces in statewide depth-to-bedrock data and gridding these sparse elevation markers into a hydrologically consistent DEM (20). The modern mainstem alluvial surface lies above the bedrock long profile of the upper Mississippi, which includes the now-abandoned Princeton Channel–Illinois River course. The bedrock long profile may be split into three zones, as indicated on the figure. Downstream of the forebulge-induced overdeepening, a uniform incision signal dominates. Above the forebulge-induced overdeepening, buried bedrock elevations frequently align with the downstream bedrock long profile, indicating that forebulge incision created a narrow inner gorge that lies within a longer-occupied valley floor. Andrew D. Wickert et al. Sci Adv 2019;5:eaav2366 Copyright © 2019 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution License 4.0 (CC BY).