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

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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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Primary contact

Dr David Williams
Dept of Archaeology
University of Southampton
Avenue Campus
Highfield
Southampton
SO17 1BJ
England
Tel: 080 593032

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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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Almagro 50

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details | characteristics | pictures | drawings | petrology | specimens | bibliography | 3D models

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Almagro 50 Almagro 50 Almagro 50 Almagro 50
Almagro 50 fabric

Visual characteristics

A fairly hard, rough sandy fabric containing small white inclusions of limestone, buff (7.5YR 7/4) colour throughout.

Petrology

We have examined one sample which shows frequent inclusions of limestone and quartz, with a few grains of pyroxene and flecks of mica. The pyroxene is significant and could suggest an origin not far removed from an outcrop of basic igneous rocks. Basalt outcrops occur in a long strip inland along the length of the Algarve (Peacock & Williams, 1986: Class 22).

 


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