Horizont ranog bronzanog doba na lokalitetu Rit

Abstract

U radu o eneolitskom periodu na lokalitetu Rit u ovom zborniku položaj ovog lokaliteta već je opisan, tako da ćemo ovde samo napomenuti da je reč o zabarenom aluvijumu, koji je bio konstantno pod vodom sve do polovine prošlog veka. Zanimljivo je da je lokalitet bio nastanjen samo krajem starijeg eneolita, u prvom kvartalu 4. milenijuma pre n.e. i u ranom bronzanom dobu, ne računajući usamljeni grob iz gvozdenog doba, koji je pomenut u radu o eneolitu. Ovo napominjemo jer je lokalitet Nad Klepečkom, sa kojim se Rit graniči, bio konstantno nastanjen u praistoriji, od eneolita do mlađeg gvozdenog doba. Po svemu sudeći, razlog je u tome što se Rit nalazi na niskim kotama između 69 i 70 m nadmorske visine i očito je bio često zabaren, osim u pomenutim periodima, za razliku od lokaliteta Nad Klepečkom, koji se nalazi na gredi na kotama između 75 i 90 m nadmorske visine i verovatno je konstantno bio iznad nivoa voda.

The exact position of the site is provided in the paper discussing the Eneolithic period at the site of Rit in this volume, and therefore we shall only mention that the location represents marshy alluvium, which was periodically flooded up to the second half of the 20th century. It is interesting that the site was inhabited exclusively during the Early Eneolithic, meaning the first quarter of the 4th millennium BC and during the Early Bronze Age, excluding the lone Iron Age grave which was also mentioned in the paper dealing with the Eneolithic period. We highlight this because the site of Nad Klepečkom, which borders the site of Rit was continuously inhabited in prehistory, from the Eneolithic to the Late Iron Age. The reason behind this is most likely the position of the site of Rit, which lies at altitude between 69 m and 70 m, and was often flooded, save for the aforementioned periods, in comparison to the site of Nad Klepečkom, which lies on a terrace at altitude between 75 m and 90 m, and was apparently positioned on a dry land.