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Publikováno v:
Hydrogeology Journal. 28:921-939
Approximately 2 km2 of sand- and gravel-rich Pleistocene glacial-outburst megaflood sediment has accumulated in a series of five subparallel paleochannels that are an important component of a basalt-dominated aquifer system on the semiarid, ~450-km2
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::627afb31f5d195c91192702a2c61b5e2
https://doi.org/10.1007/s10040-019-02100-1
https://doi.org/10.1007/s10040-019-02100-1
