Editing Monte Bolca (section)

=== Spilecco ===
Spilecco, also known as Spilecco Hill, is largely made up of poorly-exposed reddish marly and grey-green [[Limestone|limestones]]. While the fossil content of the grey-green limestones is made up of various microfossils, macrofossils are found in the reddish marly limestones. The strata within Spilecco date from the Thanetian to lower Ypresian which make them the oldest shallow water deposits in the Lessini Shelf and would have been deposited after the first period of volcanic activity.<ref name=":2">{{Cite journal |last=Seghetti |first=Simone Matteo |last2=Georgalis |first2=Georgios L. |last3=Tschopp |first3=Emanuel |last4=Delfino |first4=Massimo |date=2022 |title=A historical overview of the reptile fauna from the Eocene Bolca Fossil-Lagerstätte (Italy) |journal=Bollettino della Società Paleontologica Italiana |volume=61 |issue=2}}</ref><ref name=":3">The  Bolca  Fossil-Lagerstätten: A  window  into  the  Eocene  World</ref>