Proluvial facies are a type of terrestrial facies that commonly develop in arid or semi-arid regions. In mountainous areas, intermittent floods transport weathered materials of parent rocks to the valley mouth to form deposits. Abundant gravels, sand and silts transported by floods accumulate rapidly at the valley mouth to form a fan-shaped deposit, which is called a proluvial fan. The material is poorly sorted with unclear bedding. Particle gradation is remarkable in map view; a thick layer of coarse fragments mainly composed of gravels is located close to the fan, but towards the outer margin, the particles gradually transition to smaller sizes in the form of sand, silt and mud, and the thickness decreases gradually with the development of cross-bedding.
This is a preview of subscription content, log in via an institution.
Buying options
Tax calculation will be finalised at checkout
Purchases are for personal use only
Learn about institutional subscriptionsEditor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2020 Springer Nature Singapore Pte Ltd.
About this entry
Cite this entry
(2020). Proluvial Facies. In: Chen, A., Ng, Y., Zhang, E., Tian, M. (eds) Dictionary of Geotourism. Springer, Singapore. https://doi.org/10.1007/978-981-13-2538-0_1944
Download citation
DOI: https://doi.org/10.1007/978-981-13-2538-0_1944
Published:
Publisher Name: Springer, Singapore
Print ISBN: 978-981-13-2537-3
Online ISBN: 978-981-13-2538-0
eBook Packages: Earth and Environmental ScienceReference Module Physical and Materials ScienceReference Module Earth and Environmental Sciences