Roman Amphorae: a digital resource

University of Southampton, 2005. (updated 2014) https://doi.org/10.5284/1028192. How to cite using this DOI

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/10.5284/1028192
Sample Citation for this DOI

University of Southampton (2014) Roman Amphorae: a digital resource [data-set]. York: Archaeology Data Service [distributor] https://doi.org/10.5284/1028192

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Dr David Williams
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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/10.5284/1028192
Sample Citation for this DOI

University of Southampton (2014) Roman Amphorae: a digital resource [data-set]. York: Archaeology Data Service [distributor] https://doi.org/10.5284/1028192

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Dressel 43



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Dressel 43 Dressel 43 Dressel 43
Dressel 43 fabric

Visual characteristics

The fabric is a little variable but commonly occurs in a dense fine-textured hard fired clay, which is generally light red to buff in colour, or sometimes a lightish grey. The outer surface, which is often roughly finished, is often covered thin light coloured slip.

Petrology

There is some variety, as one should expect where there are several production sites. Commonly there are frequent subangular grains of quartz, usually below 0.3mm in size, together with flecks of mica, a little cryptocrystalline limestone and some red iron oxide. Occasionally small pieces of igneous and metamorphic rocks are also present.

 


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