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VSF 2010 Report - Nabo

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CORING AT HÁLSHÚS AND VATNSFJARÐASEL<br />

Céline Dupont-Hébert<br />

Université Laval<br />

Introduction<br />

Surveying the landscape by auguring<br />

fields and archaeological features have<br />

proven to be a productive way to<br />

evaluate the potential of archaeological<br />

sites. This means of probing site<br />

stratigraphy has been used in many<br />

different ways by archaeologists and<br />

geologists around the world but a typical<br />

procedure for archaeological use in<br />

Iceland does not exist. Most of the time,<br />

a strategy is elaborated in an ad hoc<br />

fashion according to the research<br />

objectives, landscape feature’s length<br />

and width, knowledge of the area and<br />

intuition of the archaeologist.<br />

Interpretation of core results and data<br />

synthesis are somehow open to<br />

misinterpretation. This matter will be<br />

discussed later.<br />

During the summer of <strong>2010</strong>, two<br />

auguring experiments were undertaken<br />

by the field school staff in the<br />

Vatnsfjörður area. The first one was<br />

done at the farm of Hálshús where an<br />

eroded profile showed archaeological<br />

deposits. The second experiment was<br />

done at Vatnsfjarðasel, a shieling– sel- that became an independent farm in the early<br />

modern period (Figure 1). This assessment will show the application of auguring in the<br />

evaluation process for both rescue and<br />

potential research using both Hálshús<br />

and Vatnsfjarðasel as examples.<br />

Borgarey<br />

Vatnsfjarðasel<br />

Vatnsfjörður<br />

Hálshús<br />

Figure 1. Location of archaeological sites under<br />

discussion in this assessment (modified map from<br />

Aldred 2008)<br />

Hálshús<br />

During the summer of <strong>2010</strong>, field staff at Vatnsfjörður were advised that severe erosion<br />

had occurred on a slope east of the farm of Hálshús, near the Vatnsfjörður farm. An<br />

exposed profile showed stratified deposits of peat ash, charcoal and faunal remains<br />

interpreted as a possible midden feature. In order to evaluate its extent, damage caused by<br />

the erosion, and to plan an eventual rescue excavation, the author and a student from the<br />

field school undertook the coring procedure around the possible midden.<br />

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