from Part II - Regional Studies
Published online by Cambridge University Press: 30 April 2023
Centrally situated in France, hosting famous chateaus and vineyards yet oddly secluded, the extensive, diamond-shaped region known as Sologne is a geological elephant in the room. Nationally one of the last regions to be fully surveyed, this deceptively uniform yellow patch on small-scale geological maps is presented here and portrayed for the first time as a fluvial megafan. Its attributes are compiled and reviewed from a collection of reports, maps, handbooks and articles. Evidence shows that this ~ 100-m-thick Neogene accumulation of quartz-rich sand and clay was primarily generated by the Loire River and remained intermittently functional until early Quaternary time, whereupon dissection by the Loire River itself and by its fan-fed tributary streams prevailed. The ~ 120-km-long megafan was fed from the south by the rising volcanic swell of the Massif Central in a succession of pulses, relatively well-dated by different generations of accessory volcanic minerals. Sediment aggradation conforms to a pattern for which modern analogues may only exist in Africa, a continent hosting many dozens of swells of a similar nature to the Massif Central, with adjacent basins populated by very large megafans fed by swell-flank rivers. As such, the Loire megafan is a unique occurrence in Europe.
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