The long-term evolution of the Douro River as evidenced by strath terrace staircases located at NE Portugal (western Iberia)
In western Iberia, mechanisms that explain the transition from endorheic to exorheic continental-scale drainage reorganisation are foreland basin overspill, headwards erosion and capture by an Atlantic river, or a combination of both. To explore these controls we have investigated the Portuguese sec...
Main Author: | |
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Other Authors: | , , , , , , , , |
Format: | conferenceObject |
Language: | eng |
Published: |
2019
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Subjects: | |
Online Access: | http://hdl.handle.net/1822/72102 |
Country: | Portugal |
Oai: | oai:repositorium.sdum.uminho.pt:1822/72102 |