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The Eridanos began about 40 million years ago in the [[Eocene]]. By about 12 million years ago in the [[Miocene]], the Eridanos had reached the [[North Sea]] area, where sediments carried by the river built an immense [[river delta|delta]]. The Eridanos disappeared in the early Middle [[Pleistocene]], about 1 million years ago, when the Ice Age [[glacier]]s excavated the Baltic Sea bed.
The [[Neogene]] uplift of the [[South Swedish highlands|South Swedish Dome]] deflected the Eridanos river from its original path across south-central Sweden into a course south of Sweden in the [[Pliocene]].<ref name=Karna2017>{{cite journal |last1=Lidmar-Bergström |first1=Karna |last2=Olvmo |first2=Mats|last3=Bonow |first3=Johan M. |author-link=Karna Lidmar-Bergström|date=2017 |title=The South Swedish Dome: a key structure for identification of peneplains and conclusions on Phanerozoic tectonics of an ancient shield |journal=[[GFF (journal)|GFF]] |volume=139 |issue=4 |page=244 |doi=10.1080/11035897.2017.1364293 |bibcode=2017GFF...139..244L |s2cid=134300755 |url=http://urn.kb.se/resolve?urn=urn:nbn:se:miun:diva-31508 }}</ref>
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