Share

Feedback

How do bends form in peat-land streams?

We propose a conceptual model to explain the origin of bends in peatland streams to better inform stream restoration.

Data-collection methods: Field survey measurements

Key goals:

Key locations: IJssel River (NL)

Spatial scale: Floodplain

Temporal scale: Periods of Earth history

Related outputs

Oblique aggradation: a novel explanation for sinuosity of low‐energy streams in peat‐filled valley systems

07/12/2016 by Jasper Candel

Contains: Dataset access Publication open access Storyline for practice

View output

Last modified: 12/06/2018

Open storyline

Details

Date
23/10/2017
Project
C1) Historical evolution of lowland rivers

Contact details

Jasper Candel

Wageningen University & Research