Soils derived from the Silurian sedimentary rocks of this southern part of the district are all rather poor and acid, because of the very high rainfall over the last 10,000 years, since the last glacial episode. This has leached out the soluble mineral elements such as calcium.
High Borrans is located within the Silurian (Ordovician) division, made up of Silurian Slates, Grits and Flags. The Silurian hills and valleys present a gentler than the central mountains (seen from the farm) of the Borrowdale Volcanic series. These rocks were originally deposited in an ocean that covered the southern part of the region after the volcanic episode.
Barn Owls, bats; fieldfares; snipe woodcock; partridge; pheasants; swifts, house-martins, swallows, little owl and red squirrels.
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There are wild cranberries and wild juniper among the heather. There are areas of bog-moss (Sphagnum) with cotton-sedge (Eriophorum).
Hedgerows, because of lack of management in the past have grown too tall. A grant to re-lay these hedges is being investigated.
There is one barn, part of which is much older than the rest. Jonathan and Cathy Hodgson are investigating funding sources for restoration.
There is an ice house within the farm.
35% from livestock
65% from environmental management payments.