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
Ford Moss Ford Moss Ford Moss is a Site of Special Scientific Interest (SSSI), containing a Scheduled Ancient Monument, located south-west of Berwick-upon-Tweed, Northumberland, England. The site is managed by the Northumberland Wildlife Trust and gained its SSSI status in 1968, and in 2005 it was designated a Special Area of Conservation. Ford Moss is bound to the south by the high Goatscrag Hill and the west by the Blackchester Hill, both of which are sandstone formations. It is one of two SSSIs located on the Ford & Etal estate which were originally two separate estates combined in 1908 when James Joicey,