|Elevation||111 m (364 ft)|
|Prominence||83 m (272 ft)|
|Topo map||OS Landranger 57|
The quartz-dolerite, being much harder than the surrounding coal measures, has been exposed due to erosion, including by glaciation. The characteristic crag and tail shape of the crag reflects this glacial shaping.
The hilltop was also defended during the Early Medieval Period, and features a vitrified hillfort, destroyed by fire in the 6th or 7th centuries AD and then refortified in 8th or 9th centuries AD, as demonstrated by two phases of archaeological excavation, the first by SUAT Archaeology in 2001 and the second by Murray Cook, Stirling Council's Archaeologist in 2012.
- "Abbey Craig". www.hill-bagging.co.uk.
- Loughlin, S. C. "Wallstane". Geological Conservation Review. 27. Archived from the original on 4 March 2016. Retrieved 24 February 2020.
- Ross, David. R. (1999). "Stirlin Bidge". On the Trail of William Wallace. Dundurn. ISBN 9780946487479. Retrieved 3 November 2019.
- Historic Environment Scotland. "Abbey Craig (47113)". Canmore. Retrieved 24 February 2020.
- "Prehistoric Archaeology Blog". prehistoricarch.blogspot.com. Archived from the original on 31 October 2019. Retrieved 31 May 2021.
- "Archived copy". Archived from the original on 16 March 2014. Retrieved 15 March 2014.CS1 maint: archived copy as title (link)
- "Abbey Craig". Hill Bagging.
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