Abstract
In the area along the northern flank of the Mount Hutt Range, Canterbury, deposition of alluvial fans is initiated in three ways: the sudden release of large quantities of sediment from the stream headwaters, the truncation of earlier formed fans, and erosion at the fan apex in the course of the normal cycle of erosion. © 1966 Taylor & Francis Group, LLC. All rights reserved.
Cite
CITATION STYLE
APA
Carryer, S. J. (1966). A Note on the Formation of Alluvial Fans. New Zealand Journal of Geology and Geophysics, 9(1–2), 91–94. https://doi.org/10.1080/00288306.1966.10420197
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.
Already have an account? Sign in
Sign up for free