Abstract
A mathematical theory of erosion is developed along similar lines to the classical Fourier theory of heat flow in solids. The general theory is considered in some detail, and a few representative examples of its application to stream profiles and valley slopes are suggested in outline.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
