The Demolition of the Roman Tetrapylon in Caerleon: An Erasure of Memory

Excavations in Caerleon, the headquarters of the Second Augustan Legion, have demonstrated the existence of a tetrapylon at the centre of the Roman fortress. Evidence indicates that the structure survived into the medieval period when it was undermined and demolished. A recent review of ceramic finds associated with the demolition horizon suggests that the tetrapylon was razed in the thirteenth century. While stone-robbing for reconstruction of the medieval castle in Caerleon may provide a partial explanation for the destruction, political circumstances at the time provided additional incentives. Association of the Roman remains with resurgent Welsh lordship appears to have created a political reason for removal of the structure.     

Distal cryptotephra found in a Viking boathouse: the potential for tephrochronology in reconstructing the Iron Age in Norway

Distal tephra deposits from Icelandic volcanic eruptions have been found in Norway and can be used to precisely date a variety of sedimentary environments. Tephrochronology has not yet been applied to archaeological investigations in Norway because tephra are generally not found as visible layers, but are present as very low concentrations of glass shards (i.e. cryptotephra). In this study, we present results from the analysis of cryptotephras found in an Iron Age boathouse in northern Norway. The boathouse was associated with the chieftain center at Borg on Vestvågøy in the Lofoten Islands. In 2003, a trench was excavated and the stratigraphy of the boathouse was described. Radiocarbon ages from cultural deposits show that it was constructed in the Early Iron Age c. AD 540–660 and the main period of use was at the end of the Iron Age between c. AD 1030 and AD 1270. Volcanic glass shards were isolated from sediment samples collected above and below the cultural deposit representing the main period of use. Electron microprobe analysis of the glass shards showed that the lower sample resembles the AD 860 Layer B tephra and the upper sample resembles tephra erupted from the Hekla volcanic system between AD 1104 and AD 1300. These tephrochronologic dates agree with the radiocarbon-derived dates and possibly further constrain the boathouse’s main period of use to c. AD 1030–1104. Our results demonstrate the value of using tephrochronology for archaeological studies in Norway and the potential for finding cryptotephra from other large explosive volcanic eruptions during the Iron Age.