Soil erosion, agricultural terracing and site formation processes at Markiani, Amorgos, Greece

C A I French, 2000. https://doi.org/10.5284/1000343. How to cite using this DOI

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https://doi.org/10.5284/1000343
Sample Citation for this DOI

C A I French (2000) Soil erosion, agricultural terracing and site formation processes at Markiani, Amorgos, Greece [data-set]. York: Archaeology Data Service [distributor] https://doi.org/10.5284/1000343

Data copyright © Dr C A I French unless otherwise stated

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Dr C A I French
University of Cambridge
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Cambridge
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England

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Resource identifiers

Digital Object Identifiers

Digital Object Identifiers (DOIs) are persistent identifiers which can be used to consistently and accurately reference digital objects and/or content. The DOIs provide a way for the ADS resources to be cited in a similar fashion to traditional scholarly materials. More information on DOIs at the ADS can be found on our help page.

Citing this DOI

The updated Crossref DOI Display guidelines recommend that DOIs should be displayed in the following format:

https://doi.org/10.5284/1000343
Sample Citation for this DOI

C A I French (2000) Soil erosion, agricultural terracing and site formation processes at Markiani, Amorgos, Greece [data-set]. York: Archaeology Data Service [distributor] https://doi.org/10.5284/1000343

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Introduction

This dataset was deposited by Dr C.A.I. French of the University of Cambridge. The work was carried out with funding from the British Academy. The article that came from this archive is published in Geoarchaeology 14.

Soils and sediments of a terraced slope at an Early Bronze Age site on the Aegean island of Amorgos were examined micromorphologically to determine the nature and amount of erosion on the slope during the past 5,000 years, and how this had affected the formation of the surviving archaeological record. The deposits forming representative terraces were examined, as was the post-depositional sequence overlying the site, and a palaeosol preserved beneath terrace retaining walls at the break of slope. The buried, pre-terrace system 'red soil' was a reworked red palaeosol, much affected by downslope erosion processes, which probably commenced with clearance associated with the Early Bronze Age occupation of the site. Examination of this soil suggested that there were at least two pre-modern phases of use of the hill-side.


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