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Reconstruction of ancestral drainage patterns in an internally draining region, Fars Province, Iran

Reconstruction of ancestral drainage patterns in an internally draining region, Fars Province, Iran

This is a Preprint and has not been peer reviewed. The published version of this Preprint is available: https://doi.org/10.1017/S0016756814000685. This is version 1 of this Preprint.

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Authors

Jacqueline Lee

Abstract

Google Earth imagery is used here in conjunction with a Geographic Information System to identify transverse drainages and recreate paleodrainage in an internally draining region in Iran. At least thirty-five water gaps and thirty-four wind gaps are shown to exist in the region, as well as evidence for an integrated paleodrainage that originated north of the internally draining region and emptied into the Mand watershed to the west. The topographic characteristics of the transverse drainages suggest a strong control by local topography, and support formation of the internally draining region by basin filling and overflow. Both climatic and tectonic factors may have controlled the loss of external connectivity.

DOI

https://doi.org/10.31223/X5SF7P

Subjects

Earth Sciences, Physical Sciences and Mathematics

Keywords

internal drainage, endorheic basin, Iran, Fars, wind gaps, paleodrainage

Dates

Published: 2026-10-14 08:51

Last Updated: 2026-10-14 08:51

License

CC-By Attribution-NonCommercial-NoDerivatives 4.0 International

Additional Metadata

Conflict of interest statement:
None

Data Availability:
Data is publicly available

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