20.500.12556/DiRROS-15310 Kamnolom apnenca v Podpeči pri Ljubljani in njegovi izdelki Limestone quarry at Podpeč near Ljubljana (Slovenia) and its products Kamnolom v naselju Podpeč pri Ljubljani velja za glavni kamnolom rimske kolonije Emone (Ljubljana). Obstoj antič-nega kamnoloma v Podpeči je bil do sedaj utemeljen le na podlagi makroskopske podobnosti med Členom litiotidnega apnenca, ki izdanja v Podpeči, in z njim povezanimi rimskimi spomeniki, odkritimi v Ljubljani. V okviru pričujočega dela smo skušali poiskati oprijemljive arheološke in geoarheološke dokaze za njegov obstoj. V skrajno severnem delu kamnoloma smo izvedli arheološko sondiranje, hkrati pa natančno določili sestavo apnenca na tem območju in v 288 izdelkih iz antične Emone. Sondiranje severno od modernega kamnoloma je odkrilo dobro ohranjene sledove rimsko-dobne kamnoseške dejavnosti. Hkrati je litološka analiza spomenikov iz Emone razkrila, da je kar 182 (ali 64 odstotkov) analiziranih spomenikov izdelanih iz apnenca, litološko identičnega različkom, ki izdanjajo v Podpeči. Ti različki se prostorsko grupirajo severno od modernega kamnoloma. Pri tem sicer ostaja odprto vprašanje pripadnosti nekaterih različkov apnenca v izdelkih, ki so brez diagnostičnih komponent in bi lahko pripadali tudi nekoliko starejšemu Členu krkinega apnenca. Rekonstrukcijo obsega starega kamnoloma omogoča primerjava faciesov izvornih litostratigrafskih enot in izdelkov, pa tudi historična analiza zgodnjih kartografskih in katastrskih dokumentov. Analiza najzgodnejših izdelkov je omogočila hipotezo o prihodu kamnosekov iz kamnoloma v Nabrežini. The quarry in Podpeč near Ljubljana is considered the main quarry of the Roman colony Iulia Emona (Ljubljana, Slovenia). The existence of an ancient quarry in Podpeč has been substantiated based solely on the macroscopic similarity between the Lithiotid Limestone Member outcropping in Podpeč and the associated Roman monuments discovered in Ljubljana. In the present work, we have attempted to find tangible archaeological and geoarchaeological evidence for its existence. Archaeological excavations in the form of three trenches were carried out in the northernmost part of the quarry. We determined the lithological composition of limestone discovered in the trenches and the limestone used for the 288 objects found in Ljubljana. The lithological analysis of the monuments from Emona revealed that as many as 182 (or 64%) of the analysed monuments were made of limestone, which is lithologically identical to the types of limestone outcropping in Podpeč. Lithologies represented in monuments also spatially group north of the modern quarry. However, the question of the affiliation of some of the varieties of limestone represented remains open. These limestone types lack diagnostic components and could also belong to the slightly older Krka Limestone Member. Reconstruction of the extent of the ancient quarry was enabled using microfacies comparison of lithostratigraphic source units and objects/products, as well as with the historical analysis of early cartographic and cadastral documents. Studying the forms of the earliest objects (stelae) also suggests that the earliest monuments were produced by stonemasons who came to the area from the quarry in Aurisina (Italy). Slovenija Podpeč Emona rimska doba litiotidni apnenec mikrofaciesna analiza rimski in novoveški kamnolom izdelki Slovenia Podpeč Emona Roman period Lithiotid Limestone microfacies analysis Roman and modern quarry stone products true false true Inštitut za arheologijo ZRC SAZU Slovenski jezik Angleški jezik Delo ni kategorizirano 2022-07-21 13:00:57 2022-07-21 13:15:18 2022-08-21 03:36:42 0000-00-00 00:00:00 2022 0 0 str. 155-198 letn. 73 2022 0000-00-00 Zaloznikova Objavljeno NiDoloceno 0000-00-00 0000-00-00 0000-00-00 904:679.85(497.451Podpeč) 0570-8966 10.3986/AV.73.06 112093955 Arheo_73.pdf Arheo_73.pdf 1 A4FC026841BE97A06393CF26C42537CD b1453d1702405fafc36aa008284868500cc67fb72684f17f8e6c22978dad8098 f89d99a3-17b6-11ed-b6b8-001a4af901a5 https://dirros.openscience.si/Dokument.php?lang=slv&id=20164 Geološki zavod Slovenije 0 0 0