TOWN HEAD FARM

GRASMERE

ENVIRONMENTAL FEATURES

Northern reaches of Grasmere Vale, at the foot of Dunmail Raise.

GEOLOGY

Great Langdale is part of the Borrowdale Volcanic Series which ‘poured and shot out of the vents above Skiddaw Slates in Ordovician times,  about 400 million years ago, and then  Silurian slaty beds were laid down on top of them. ..The Ordovician and Silurian rocks were first submerged in the ancient Carboniferous sea about 280 million years ago, and were then uplifted into the desert environment of the Triassic period…the Carboniferous rocks haved been stripped off by wind and weather and water from the mountain heart… Much of the mineral wealth of the rocks is made up of the results of later changes – the intrusion into the Borrowdale rocks of later masses of igneous rock…’ WH Pearsall, W. Pennington, The Lake District: A Landscape History, 1973, pp. 27, 30, 44, 45

SOIL TYPE(S)

‘Soils …are now all rather poor and acid, because in the course of the last ten thousand years, since the last glacial episode, the very high rainfall of this western mountain district has leached out of the soil most of the soluble mineral elements such as calcium…bracken on these fells indicates the presence of deep and comparatively well-drained soils of which the profile approximates to a brown earth.’ (Ibid, pp.121, 124)

If you'd like to know more about Geology and Soil types in Grasmere; see WH  Pearsall, W. Pennington, The Lake District: A Landscape History, 1973, chapters 2, 3, 7

FAUNA

Two barn owls in the barn; Buzzards, Peregrines, Herons, House Martins, and the Redstart, a summer migrant from Africa. Badgers, foxes, and deer.

In Greenburn (a valley above Town Head Farm) there are dragonflys.
Townhead farm