TILBERTHWAITE FARM

CONISTON

ENVIRONMENTAL FEATURES

Tilberthwaite Farm lies within the Cumbrian high fells which have a mosaic of high craggy peaks and screes, heaths, mires, peatland, heather moorland, acid grassland and bracken. 

The farm is located in a narrow valley bottom rising steeply to fells of rocks and crags.  Woodland is a distinctive feature with ancient woods in the valley, and a large display of Juniper can be seen from the valley of Little Langdale.

GEOLOGY

The farm sits on the Borrowdale Volcanic group. Mines and quarries on two areas of fell land on the farm have been designated as Sites of Special Scientific Interest (SSSI) for their rock outcrops, mine spoil and disused mine workings. 

Birk Fell Hawse Mine on the Tilberthwaite fells has also been designated as a Site of Special Scientific Interest (SSSI) for its mineral vein deposits which are typical of Lake District late Devonian copper veins.

More information about mining in the Lake District can be seen at Keswick Mining Museum (www.keswickminingmuseum.co.uk) and at Threlkeld Quarry and Mining Museum (Tel 017687 79747).

 

FLORA

heatherAs well as extensive areas of heather moorland on the fells, Tilberthwaite Gill has been designated as a SSSI for its “montane” habitat of tall herb vegetation growing on its cliffs.

The farm is noted for its stands of Juniper which is one of only 3 native conifers in Britain. 

The woodland in Close Hill Quarry and Close Hill Coppice is designated as “ancient and semi natural woodland”.

 

Levers Water