Geology and Mining
Robinson’s summit area is composed of rocks of the Buttermere Formation. This is an olistostrome of disrupted, sheared and folded mudstone, siltstone and sandstone. West and north east of the summit are outcroppings of the Robinson Member. This comprises large olistoliths of greywacke sandstone, with interbedded mudstone and siltstone. The southern flanks are a large area of landslip.
There has been considerable mining activity in the vicinity, particularly at the Goldscope Mine, but this has all taken place beneath the slopes of neighbouring Hindscarth. The remains of a small reservoir can still be seen in Little Dale. Robinson itself has a pair of short levels driven for lead, near to the south east corner of Buttermere lake. They appear not to have progressed beyond trials.
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“In strict science, all persons underlie the same condition of an infinite remoteness. Shall we fear to cool our love by mining for the metaphysical foundation of this elysian temple? Shall I not be as real as the things I see? If I am, I shall not fear to know them for what they are.”
—Ralph Waldo Emerson (18031882)