Brown Moss of breeding birds at the site and many visitors, including wetland birds, such as Canada goose, mallard and great crested grebe. During the summer, froglets and dragonflies are found around water and woodland edges. Brown Moss is a flat site that was created at the end of the last Ice Age, over 10,000 years ago. As glaciers retreated, pools were formed by the stranded ice rocks, forming kettle holes Peat is still being created and Sphagnum moss – which is very important for the creation of peat – is found in abundance. This site contains a number of circular walks
Sphagnum cuspidatum branch leaves can sometimes be faintly serrated. "S. cuspidatum" is a dioecious species. The spores produced are 29-38 µm, covered with large papillae on both surfaces, and appear to be covered in small blisters (pusticulate). "S. cuspidatum" can be found on wet humus under forests and on the bases of trees forming a hummock-hollow complex; in or near bogs. Distinguishing "Sphagnum cuspidatum" from "Sphagnum viride" is sometimes difficult as both occur over a similar geographic range and both grow in wet carpets. "Sphagnum cuspidatum" has narrower branch leaves and usually a distinct red tinge at the branch bases within the