Geology and Mining
Barf is a part of the Loweswater Formation of Ordovician rocks. This is composed of Greywacke sandstone turbidities. The lower eastern slopes show outcropping of the Kirkstile Formation, the typical rock of the Skiddaw group.
There is evidence of historic mining activity on the north bank of Beckstones Gill, below the east face and also near Woodend. Small amounts of lead and zinc were raised between 1532 and 1891, the principal ores being blende, cerussite and galena.
Read more about this topic: Barf (Lake District)
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“It’s a mining town in lotus land.”
—F. Scott Fitzgerald (1896–1940)