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Exploring the myth of Lake Saveh on the Iranian Plateau

The effects of climate change and civilizational evolution

Bibliographic Data

ID12265013
AuthorsHamid Nazari (0000-0002-0004-6303, UNESCO Chair on Coastal Geo-Hazards Analysis, Research Institute for Earth Sciences, Iran, corresponding author), Jean-François Ritz (0000-0002-7351-8877, UNESCO Chair on Coastal Geo-Hazards Analysis, Research Institute for Earth Sciences, Iran), Aram Fathian (0000-0001-8025-5692, UNESCO Chair on Coastal Geo-Hazards Analysis, Research Institute for Earth Sciences, Iran), Hassan Fazeli Nashli (0000-0002-0724-365X, UNESCO Chair on Coastal Geo-Hazards Analysis, Research Institute for Earth Sciences, Iran), Shannon Mahan (Denver Federal Center), Shannon A Mahan (0000-0001-5214-7774, Geosciences and Environmental Change Science Center, United States Geological Survey, Denver Federal Center, USA), Alireza Vaezi (0000-0003-2824-4923, UNESCO Chair on Coastal Geo-Hazards Analysis, Research Institute for Earth Sciences, Iran), Ara Avagyan (0000-0001-8737-2074, UNESCO Chair on Coastal Geo-Hazards Analysis, Research Institute for Earth Sciences, Iran)
Year2026
Volume36
Issue5-6
Pages499-516
Publication date2026-02-26
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publishing (PUBLISHER • US)
DOI10.1177/09596836251414037
OpenAlexW7131622233
LanguageEN
Citations received1
References cited70

This study presents a multidisciplinary reconstruction of a paleolake’s Holocene evolution in Iran’s Central Plateau, synthesizing sedimentological, geochronological, archeological, and historical evidence. Our findings confirm the existence of a large paleolake (~16–14 ka) in the northern plateau, with episodic desiccation and recharge. Lake levels declined by 250 m between 11.5 and 8.2 ka, stabilizing at ~850 m elevation. The 8.2 ka climatic cooling event triggered regional aridification, prompting human migration to warmer lowlands. We propose that the Masileh Basin, hydrologically active until the Sassanid era, represents the residual footprint of the mythologized Lake Saveh. By correlating Late Pleistocene–Holocene hydrological dynamics with settlement patterns, this work establishes a direct linkage between climatic forcing, tectonic controls, and anthropogenic responses. The integration of geological archives with archeological and historiographical data resolves long-standing ambiguities surrounding the lake’s existence while demonstrating how environmental transitions became encoded in cultural memory

Climate change · Environmental change · Environmental history · Holocene · Human settlement · Multidisciplinary approach · Period (music · Tectonics · Vegetation (pathology · Geology and Paleoclimatology Research · Marine and environmental studies · Transboundary Water Resource Management

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Citations per year1
Citation span2026 - 2026 (1)
Highly citedNo

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