We use cookies to distinguish you from other users and to provide you with a better experience on our websites. Close this message to accept cookies or find out how to manage your cookie settings.
To save content items to your account,
please confirm that you agree to abide by our usage policies.
If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account.
Find out more about saving content to .
To save content items to your Kindle, first ensure no-reply@cambridge.org
is added to your Approved Personal Document E-mail List under your Personal Document Settings
on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part
of your Kindle email address below.
Find out more about saving to your Kindle.
Note you can select to save to either the @free.kindle.com or @kindle.com variations.
‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi.
‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.
This chapter considers the development of drainage basins and stream networks over geological timescales. It examines why a focus on river systems over geological timescales is important, how river channels form through surface and subsurface processes, and the differences between stream channels and hillslope erosional features, such as rills and gullies. It explores how drainage networks are related to properties of drainage basins and how stream networks develop, grow, and evolve over time. It also examines how channels are initiated on the landscape and how drainage-basin evolution and channel network evolution are intertwined. The spatial geometry and arrangement of river networks is reviewed along with the scaling properties of these networks.
Recommend this
Email your librarian or administrator to recommend adding this to your organisation's collection.