Orton Moss devil's-bit scabious, knapweed, meadowsweet and wild angelica are abundant. Small remnants of raised mire vegetation including sphagnum moss, bog rosemary and royal fern. Birds to be seen are willow tits, woodcock, great spotted woodpeckers and willow warblers. Orton Moss Orton Moss is a Site of Special Scientific Interest located west of the city of Carlisle in northwest England. Orton Moss is a former raised mire and divided into strips and fields which would traditionally have been used for peat cutting and grazing. Formerly noted for its butterflies, it was once the homes of the wood white, ("Leptidea sinapis"), the large
Moss Antarctica and Russia, and a case is put forwards for Carboniferous mosses. It has further been claimed that tube-like fossils from the Silurian are the macerated remains of moss calyptræ. Mosses also appear to evolve 2–3 times slower than ferns, gymnosperms and angiosperms. Recent research show that ancient moss could explain why the Ordovician ice ages occurred. When the ancestors of today's moss started to spread on land 470 million years ago, they absorbed CO from the atmosphere and extracted minerals by secreting organic acids that dissolved the rocks they were growing on. These chemically altered rocks in turn reacted