Imaging skeletal remains with ground-penetrating radar: comparative results over two graves from Viking Age and Medieval churchyards on the St¨®ra-Seyla farm, northern Iceland

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• 作者：Brian N. Damiata^a ; ^{damiata@ucla.edu} ; John M. Steinberg^b ; Douglas J. Bolender^c ; Guð ; ný ; Zoë ; ga^d
• 关键词：Ground-penetrating radar ; Time-slice imaging ; Reflection coefficient ; Graves ; Skeletal remains ; Viking Age churchyard ; Iceland
• 刊名：Journal of Archaeological Science
• 出版年：2013
• 出版时间：January, 2013
• 年：2013
• 卷：40
• 期：1
• 页码：268-278
• 全文大小：2428 K

文摘

Detailed ground-penetrating radar surveys were conducted at separate Viking Age and Medieval churchyards on the St¨®ra-Seyla farm in Skagafj?reur, northern Iceland. Surveying over a previously unknown site (ca. AD 1000) that is located just a few meters above the Skagafj?reur valley bottom delineated the remnants of a buried circular turf wall that encloses a church structure and several graves. The radar profiles over the graves contain strong hyperbolic reflections that emanated from the skeletal remains. Over one of the graves, an air-filled void within the chest cavity had been detected as noted by reflections with normal polarity which indicated a boundary towards increasing microwave velocity. During excavation, the soil surrounding an intact rib cage collapsed thus confirming the presence of the void. In general, the skeletal remains were very well preserved and yielded strong reflections which permitted the orientation of the body to be determined. Conversely, the radar profiles over a grave from a more recent churchyard (ca. AD 1200) show ground disturbance but lack hyperbolic reflections. Upon excavation, only teeth were recovered. The poor preservation of the skeletal remains is attributed to increase contact with infiltrating groundwater from an overlying gravel layer. Interpretations were aided by time-slice overlay imaging, forward modeling and analysis of the reflection coefficient.