Landscape Evolution of Continental-Scale River Systems

This book offers an in-depth analysis of North America's Pre-Pleistocene Bell River Basin, exploring the relationship between tectonic changes and sediment deposition, providing insights for geology and geomorphology researchers.

Landscape Evolution of Continental-Scale River Systems: A Case Study of North America's Pre-Pleistocene Bell River Basin offers an in-depth examination of a significant paleo-river system in North America. The book focuses on the Bell River Basin, utilizing detrital zircon provenance data to establish connections between the Grand Canyon's incision and the deposition of its erosional materials in a large drowned delta located in the Labrador Sea. This analysis is framed within the broader context of sedimentary source-to-sink processes and the changes in continental drainage that occurred during the Plio-Pleistocene era.

The author explores the tectonic transformations that influenced this paleo-river system, highlighting its global relevance. By comparing the Bell River Basin to other continental-scale river systems worldwide, the book provides valuable insights into the dynamics of river evolution and landscape change. This comparative approach allows readers to grasp the complexities of river systems and the various factors that contribute to their development over time.

This book serves as an essential resource for postgraduate students, academics, and researchers in geology, fluvial geomorphology, and related geosciences. It equips readers with a comprehensive understanding of how active tectonics in headwater regions can affect delta deposition in large river systems globally. Through this detailed case study, readers will gain a deeper appreciation of the interplay between geological processes and landscape evolution.