Geographically nestled in between an elongated solitary limestone outcrop to its north-east ( The Mountain ) and a cluster of same to its south ( Quarry/The Heighties ) , the Bog sat silently for thousands of years. But human interference since the 19th Century has seen to its eventual transformation and ultimately its complete erasure. This article will detail its geological history up to present times.
1830
The OS maps above ( 1830s ) and below ( 1880s - 1915 ) are the earliest examples of modern day mapping of The Bog. The article will treat each map with Ai to give a photo realistic view of the area from their aerial perspectives and even their ground levels. Of particular note is the changes in just a few decades! The Bog actually traverses 2 Townlands ; Clashduff and Deanrock. It was not in the classical sense of the word a true Bog but more a waterlogged wetland which acted as the Glasheen River's natural flood plain. It was fed by several underground streamlets which emanated from the high ground of Clashduff though limestone fissures. It contained a natural spring which flowed alongside an Osiery and into the nearby Glasheen River. The land itself sat 30 feet above sea level with a gently sloping gradient to its north west. In the 19th Century , the landowner in lieu of draining the Bog , had a drainage channel cut out at a downward angle to meet up with the flow of the spring and widened its natural channel to aid significantly in carrying away moisture and rainfall to free up a greater part of the Bog for grazing purposes. The spring was capped in the late 1970s and the entire Bog was leveled and covered in topsoil in the 1990s and is in use as a recreational park to date ( see below ).
Stage 3 - Glacial Period ( Ice Age )
Stage 4 - Post Glacial Period
Stage 7 - 1951
The Bog - 1967
The Bog - Aerial photograph 1967
The Bog - 1969
The Bog - Aerial photograph 1969
The Bog - 1971
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