When a Local Legend Is (Mis)Appropriated in the Interpretation of an Archaeological Site

Context permitting, should public archaeologists allow “archaeologically incorrect” accounts of the past? In this paper I discuss this question through a case study based on the experience of myself and my colleagues at the excavation of the Villa of Augustus in Somma Vesuviana, Italy. In 2003 and 2004, we became aware that some visitors to the excavation interpreted the site by reference to a legend of the tunnel of Queen Giovanna, which had existed in Somma Vesuviana over the centuries. Although initially interested in this phenomenon, we soon realised that we needed to make certain judgements as to how to respond to local people asking whether the tunnel had been discovered in the excavation. We presented two different ways of interpreting the site, one based on archaeology and the other on the legend, and both as equally meaningful, while at the same time stressing what we as archaeologists believed, based on what we had found. In this process we decided to adhere to the principles of archaeology, even in embracing the multivocality of material remains.     

Introduction

The public are engaging more with archaeology today than ever before, whether this is through the plethora of television channels increasing access to and providing reinterpretations of archaeological sites and finds, or through the blockbuster exhibitions hosted by museums (see Holtorf 2005, 2007). However are the public just expected to be consumers or should they be encouraged to participate and help direct the archaeological work being undertaken through active engagement?     

Geomorphic reconstruction of formation and recession processes of waterfalls of the Kaminokawa river basin on Osumi Peninsula,southern Kyushu,Japan

To assess the geomorphological importance of waterfall recession in volcanic bedrock, we examined recession rates of six waterfalls in the lower reaches of Kaminokawa river basin on the Osumi Peninsula in southern Kyushu. The examination was performed with an empirical equation that uses a dimensionless parameter obtained by dimensional analysis of relevant measured factors, including erosive force, size of waterfall, and bedrock resistance. Welded Ata ignimbrite, formed at approximately 110 ka, may have played an initiating role to maintain such waterfalls because it resists weathering more than other local rocks. Estimated recession rates for the six waterfalls range from 0.2 to 3.0 cm/y, which compare with estimated rates for waterfalls in another region characterised by welded ignimbrite. Comparison of equation‐derived recession rates of waterfalls with actual recession distances from confluences supports the idea that an original waterfall will subsequently split into two distinct waterfalls when it recesses past an upstream junction of two channels. Our findings revealed that all six waterfalls likely would have been at almost the same point lower in the watershed in the past, marking the general site of the original waterfall. Moreover, the ancestral original waterfall is highly likely to have started from a point between the caldera rim and present river mouth. There, a knickpoint was likely caused by the river dropping into an inner part of the caldera, possibly just after the eruption of the Ata ignimbrite. The waterfall erodes upstream away from the caldera basin, and this happens to be to the east.     

Spinal degenerative lesions and spinal ligamentous ossifications in ancient Chinese populations of the Yellow River Civilization

Rheumatological diseases, whether inflammatory or degenerative, are ubiquitous among modern Asian people but very few palaeopathological studies have been performed in Asia on this subject. Since 1996, we have been carrying out a palaeoepidemiological survey of rheumatic diseases in ancient Chinese and Japanese skeletal populations. Findings on the spinal column in ancient Chinese populations (ca. 5000 bc –ad 1644) in Henan Province (centre of the Yellow River Civilization) are reported in this study. The examined number of the people over 20 years old was 365 (185 males, 169 females and 11 unsexed). Of these, 248 were young adults, 98 were middle adults and 19 were old adults. Crude prevalence (number/100) in total population of vertebral osteophytosis/facet osteoarthritis was 17.5/7.7, 17/3.7 and 44.6/21.1 at the cervical, thoracic and lumbar spine, respectively. That of ossified anterior longitudinal ligament (OALL) or Forestier's disease was around 3 at each of the cervical, thoracic and lumbar spine. Ossification of the posterior longitudinal ligament (OPLL) of the cervical spine was observed in five out of 114 skeletons with cervical spine preserved, while it did not exist in any thoracic and lumbar segment. Ossification of the ligamentum flavum (OLF) was predominantly observed in the thoracic spine, the crude prevalence of which was 36.7. Overall spinal degenerative lesions seemed to have been more prevalent and spinal ligament ossifications less prevalent in ancient Chinese populations than in modern people. None of the inflammatory lesions like rheumatoid spondylitis, as well as seronegative spondyloarthropathies, were detected. This is the first palaeopathological study in which the prevalence of OPLL and OLF, the two clinically important spinal ligamentous ossifications causing myelopathy in modern mankind, was surveyed in ancient skeletons. Copyright © 2000 John Wiley & Sons, Ltd.