“In 1760 the broch measured 30’ internally, with walls 12 1/2’ thick at base and battered externally, surviving to 15’ in height. ”
stolinskie
It’s a featured article
[Open access] This volume presents the result of three excavations and two field walking surveys in Aberdeenshire. They were intended to shed new light on the character, chronology and structural development of the distinctive recumbent stone circles which are such a feature of north-east Scotland. Although the monuments share certain elements with other traditions of prehistoric architecture, and, in particular, with the Clava Cairns of the inner Moray Firth, no excavations at these sites had been published since the 1930s and their wider contexts had not been investigated by field survey. The new project took advantage of techniques which had not been used before, including pollen analysis and soil micromorphology, in an attempt to interpret these monuments in their wider chronological and geographical contexts. In that respect this work was the sequel to an earlier investigation of the Clava Cairns.
PDF link for a pamphlet made by Aberdeenshire Council in 2022.
Key:
Pink = Recumbent Stone Circle
Blue = Four-poster or similar
Green = Ring Cairn
Black = Destroyed (no trace remains)
With links to Wikipedia articles via en.wikipedia.org/wiki/List_of_recumbent_stone_circles
View of stones from the north east. Original negative captioned ‘Frendraught Stone Circle Remains from the North East June 1915’.
Excavations at the findspot of the Deskford carnyx, a major piece of Iron Age decorated metalwork found in a bog in the early nineteenth century, revealed a special location with a long history. Early Neolithic activity on the adjacent ridge consisted of massive postholes and pits, suggesting a ceremonial site. An Early Bronze Age cremation became the focus for a feasting event in the Middle Bronze Age. Around this time, peat began to form in the valley, with vessels of pot and wood smashed and deposited there; these activities on ridge and bog may be connected. Activity in the bog intensified in the later Iron Age, when offerings included quartz pebbles, the dismantled carnyx head, and two unusual animal bone deposits. The ridge was cut off at this period by a complex enclosure system. This Iron Age activity is interpreted as communal rituals at a time of increasing social tension. The site’s significance in this period may stem from its unusual landscape character, with flowing water to one side and a bog to the other. The area saw occasional activity in the Early Medieval period, but its significance had waned.
Abstract
Geological research reveals that Stonehenge’s stones come from sources beyond Salisbury Plain, as recently demonstrated by the Altar Stone’s origins in northern Scotland more than 700 km away. Even Stonehenge’s huge sarsen stones come from 24 km to the north, while the bluestones can be sourced to the region of the Preseli Hills some 225 km away in west Wales. The six-tonne Altar Stone is of Old Red Sandstone from the Orcadian Basin, an area that extends from the Northern Isles of Orkney and Shetland to Inverness and eastwards to Banff, Turriff and Rhynie. Its geochemical composition does not match that of rocks in the Northern Isles, so it can be identified as coming from the Scottish mainland. Its position at Stonehenge as a recumbent stone within the southwest arc of the monument, at the foot of the two tallest uprights of the Great Trilithon, recalls the plans of recumbent stone circles of north-east Scotland. Unusually strong similarities in house floor layouts between Late Neolithic houses in Orkney and the Durrington Walls settlement near Stonehenge also provide evidence of close connections between Salisbury Plain and northern Scotland. Such connections may be best explained through Stonehenge’s construction as a monument of island-wide unification, embodied in part through the distant and diverse origins of its stones.
A long blogpost by David C. Weinczok for National Museums Scotland about Kilmartin Glen