Abstract
AbstractIt is suggested that the evolution of morphology on a hard rock surface should be studied at a micro‐scale. At this scale there is a reasonable chance of establishing the relationship between the operation of process events and the progression of erosion rates. Micro‐erosion meters and micro‐weighed weight‐loss tablets make this possible. However, installation and disturbance factors make it difficult to approach the theoretical limits of the techniques and at the present stage only seasonal differences in erosion rates can be identified with any real certainty. Measurements on a smaller time scale of about one month have, however, been gained but these results should be interpreted with caution in the light of the problems involved.
Sign-in/Register to access full text options 
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.
