Rivers and creeks continue to flow underground when they dry up at the surface
Rivers and creeks that appear dry at the surface frequently maintain subterranean water flow and moisture within their hyporheic zones and subsurface sediments.
The claim is specific and empirically verifiable. Multiple retrieved papers, notably those studying intermittent rivers, ephemeral streams, and hyporheic zones, directly support the phenomenon where surface dry phases conceal ongoing subsurface water flow or moisture retention.
Soumaya Nabih, Ourania Tzoraki, Prodromos Zanis, Thanos Tsikerdekis, Dimitris Akritidis, Ioannis Kontogeorgos, Lahcen Benaabidate. Alteration of the Ecohydrological Status of the Intermittent Flow Rivers and Ephemeral Streams due to the Climate Change Impact (Case Study: Tsiknias River). 2021. https://doi.org/10.3390/hydrology8010043
Discusses how intermittent and ephemeral rivers maintain subsurface hyporheic and edaphic aquatic states when surface flows cease.
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DelVecchia AG, Shanafield M, Zimmer MA, Busch MH, Krabbenhoft CA, Stubbington R, Kaiser KE, Burrows RM, Hosen J, Datry T, Kampf SK, Zipper SC, Fritz K, Costigan K, Allen DC. Reconceptualizing the hyporheic zone for nonperennial rivers and streams.. 2022. https://doi.org/10.1086/720071
Explains that when surface water dries in nonperennial streams, flow or moisture is retained in the subsurface sediments of the hyporheic zone.
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