Mineral-rich waters originating from the Apennine Mountains of Italy flowed through ancient Rome’s Anio Novus aqueduct and left behind a detailed rock record of past hydraulic conditions, researchers have said. Two studies characterizing layered limestone—called travertine—deposits within the Anio Novus are the first to document the occurrence of anti-gravity growth ripples and establish that these features lend clues to the history of ancient water conveyance and storage systems.
Click here for original story, Layered limestone deposits give unique insight to Roman aqueducts
Source: Phys.org