The Mississippi River records glacial-isostatic deformation of North America

The imprint of glacial isostatic adjustment has long been recognized in shoreline elevations of oceans and proglacial lakes, but to date, its signature has not been identified in river long profiles. Here, we reveal that the buried bedrock valley floor of the upper Mississippi River exhibits a 110-m...

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Detalles Bibliográficos
Autores principales: Wickert, Andrew D., Anderson, Robert S., Mitrovica, Jerry X., Naylor, Shawn, Carson, Eric C.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2019
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6353627/
https://www.ncbi.nlm.nih.gov/pubmed/30729164
http://dx.doi.org/10.1126/sciadv.aav2366

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6353627/
https://www.ncbi.nlm.nih.gov/pubmed/30729164
http://dx.doi.org/10.1126/sciadv.aav2366

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