Chronological analysis reveals crucial insights into middle devonian geology in cromarty, suggesting new interpretations of fossil findings.
The Victorian stonemason and polymath Hugh Miller's seminal 1841 book The Old Red Sandstone continues to attract critical acclaim due to its engaging delivery to the reader, of the science of geology as it was then understood, in eloquent and descriptive prose. Since Miller's time the study and elucidation of geological data has become far more sophisticated and focussed but due to the comparative lack of rigour in the formative years of the science some of his explanations of the Middle Devonian geology and palaeontology of Cromarty, have either become misunderstood or would benefit greatly from a refresh. Here we a provide a chronology of Miller's early discoveries and his evolving understanding of Cromarty geology and how it impacted his contemporaries, and subsequent researchers and the history of geological science. In particular the work of his son, as a surveyor with the British Geological Survey is described in the context of his role in Cromarty geology. We re-evaluate the literature which, in concert with fieldwork dating back to 1991, provides an up to date reconciliation of the Middle Devonian geology of the Cromarty area generally, including its historically and scientifically important fossil bearing fishbeds.
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Davidson et al. (2025) studied this question.
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