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Alloway to the south, Newton-On-Ayr to the north and Wallacetown to the northeast are all considered suburbs of Ayr, but for this study on Ayr, the suburbs have been purposely separated herein due to their individual characteristics. Ayr is steeped in history with several famous names appearing in time that helped shape this wonderful area.
Ayr is and always was considered a market town. The description of the bedrock geology includes field observations recorded up to , together with earlier published and unpublished work on the area. The bulk of the rocks are sedimentary and Palaeozoic in age, with a succession extending from Ordovician to early Permian, punctuated by several volcanic and intrusive igneous episodes.
In Mid Ordovician times, about Ma ago, the district lay close to the southern edge of the Laurentian continent. Oceanic crust was thrust up when a volcanic arc collided with the microcontinental segment that formed the Midland Valley Terrane as it docked against Laurentia. Upper Ordovician to lower Silurian sediments were deposited in a forearc basin on the southern margin of this terrane and were deformed as the Southern Uplands accretionary prism was pushed up from the south during the Caledonian Orogeny.
The Lanark Group was later deposited, in Siluro-Devonian times, in a sequence of sandstones and conglomerates lain down in a semi-arid environment, prior to the Early Devonian calc-alkaline magmatic event which produced shallow intrusions and eruptions of predominantly basaltic andesite. By Mid Devonian times the Lanark Group had been weakly deformed and uplifted as a far-field effect of the late stage Acadian deformation event.