THE PLOUGH PEBBLES OF IRELAND
By
Niall D. K. Brady
Introduction
The wear stones known as plough pebbles
have been studied since the early twentieth
century (Dauzat; Steensberg 1936,1963; Phil-
lips; Patte; Fenton; Lerche 1970a,b;
O’Kelly). They have realized a distribution
comprising the Auvergne and Loire regions
of France; Denmark; central and northern
Britain and parts of Ireland. Over the follow-
ing pages is presented an updated assessment
of the Irish assemblage and an appendix list-
ing all the known occurrences. In 1976
M. J. O’Kelly was working with fifteen peb-
bles from two sites from which he was unable
to find secure dating contexts. There are to-
day ninety-three examples from eighteen lo-
calities. Seven come from sealed archaeolog-
ical strata and a further ten from other usable
contexts. These indicate a narrow Medieval
time range centering on the thirteenth cen-
tury.
Form (figs. 2-4)
The Irish series conforms with the types
found elsewhere. Plough pebbles are essen-
tially worn stones. They are ordinary hard
field pebbles and in Ireland are predomin-
antly of quartz and flint. Two examples of
silicified mudstone and one of basalt also oc-
cur (Nos. 6, 67 and 93). They are small, on
average pebbles measure 35x25x30 mm
lengthxbreadthxdepth)1. Dauzat (482) rec-
orded that the French stones in Auvergne
were specially worked; however, there is no
evidence for such in the Irish series. The va-
riety of shapes suggests an entirely natural
form, the distinctiveness arising only from
wear. When in use, a very characteristic pat-
tern develops on one surface (figs. 1, 2). The
worn, or facetted, surface typically consists
of a smooth, slightly convex face with a
characteristically rounded edge directly op-
Fig. 1. Explanatory drawing of a plough pebble.
Drawn by N. B.
Darstellung eines Pflugkiesels mit Erlauterungen.
Gezeichnet von N. B.
By
Niall D. K. Brady
Introduction
The wear stones known as plough pebbles
have been studied since the early twentieth
century (Dauzat; Steensberg 1936,1963; Phil-
lips; Patte; Fenton; Lerche 1970a,b;
O’Kelly). They have realized a distribution
comprising the Auvergne and Loire regions
of France; Denmark; central and northern
Britain and parts of Ireland. Over the follow-
ing pages is presented an updated assessment
of the Irish assemblage and an appendix list-
ing all the known occurrences. In 1976
M. J. O’Kelly was working with fifteen peb-
bles from two sites from which he was unable
to find secure dating contexts. There are to-
day ninety-three examples from eighteen lo-
calities. Seven come from sealed archaeolog-
ical strata and a further ten from other usable
contexts. These indicate a narrow Medieval
time range centering on the thirteenth cen-
tury.
Form (figs. 2-4)
The Irish series conforms with the types
found elsewhere. Plough pebbles are essen-
tially worn stones. They are ordinary hard
field pebbles and in Ireland are predomin-
antly of quartz and flint. Two examples of
silicified mudstone and one of basalt also oc-
cur (Nos. 6, 67 and 93). They are small, on
average pebbles measure 35x25x30 mm
lengthxbreadthxdepth)1. Dauzat (482) rec-
orded that the French stones in Auvergne
were specially worked; however, there is no
evidence for such in the Irish series. The va-
riety of shapes suggests an entirely natural
form, the distinctiveness arising only from
wear. When in use, a very characteristic pat-
tern develops on one surface (figs. 1, 2). The
worn, or facetted, surface typically consists
of a smooth, slightly convex face with a
characteristically rounded edge directly op-
Fig. 1. Explanatory drawing of a plough pebble.
Drawn by N. B.
Darstellung eines Pflugkiesels mit Erlauterungen.
Gezeichnet von N. B.