Portlethen Moss millennia of evaporation, further intensifying the soil acidity, fueled by organic matter decaying, with little drainage outlet. A layer of sphagnum moss would have developed at the benthic level of the bog, and additional sphagnum layers floated in mats atop the bog. At an intermediate level of evolution, thick peat layers formed from decay and carbonisation of the rotting sphagnum. Generations of carex and juncus flourished, leading to further decay of these materials and eventual heightening of the organic mass. Finally, secondary vegetation took root in the spongy sphagnum mats adding greater biomass to the bog.In some cases the heavy
Red Moss, Aberdeenshire Red Moss, Aberdeenshire Red Moss is a wetland bog in Aberdeenshire, Scotland, located at the northwestern edge of the village of Netherley. (Grid Reference NO 955 856) The moss is designated a national Site of Special Scientific Interest by Scottish Natural Heritage, due to its biodiversity and undisturbed character. The elevation of Red Moss is 113 metres above mean sea level. The upland areas above Red Moss are characterised as agricultural and woodland parcels which are generally attractive and separated by ancient drystone walls or hedgerows. The outlet to Red Moss with respect to drainage is the Crynoch Burn, which