Abstract
AbstractOver the course of studying stone products from the Roman colony of Emona (Regio X), stratigraphically undefined calcarenite that was used to make simple sepulchral and architectural stone products was detected. The calcarenite used is late Aptian to early Cenomanian in age. The corresponding facies were found in the Lower Flyschoid Formation outcropping near the town of Medvode, within the local radius of Emona. The Roman quarry was likely located in this area near the Sava River. According to the collected data, the quarry was in operation mainly in the 1st century.
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