Borrowdale

ValleysLake DistrictGeologyIndustrial HeritageCumbriaLiterature
4 min read

Sometime around the year 1500, a Cumbrian shepherd noticed that a black rock from the fells above Seathwaite would mark a sheep cleanly and stay marked through rain. He had no idea that the rock under his thumb was, by accident of deep geology, the only deposit of pure solid graphite ever found anywhere in the world. That single quirk of Ordovician volcanism would build the village of Keswick five miles down the valley into the pencil capital of Britain. The valley where it happened is Borrowdale - a narrow green corridor of stone walls, slate cottages and steep wooded crags, climbing from the southern shore of Derwentwater into the heart of the Lake District.

The Jaws and the Waters

Borrowdale is shaped like a bottle. The wide end opens at Derwentwater, where the River Derwent slides out of the valley and into the lake. The narrow neck, two miles upstream, squeezes between Castle Crag and Grange Fell in a tight rock-walled defile known locally as the Jaws of Borrowdale. South of the Jaws the valley opens again into a broader basin around the village of Rosthwaite, then forks. One arm climbs west toward Honister Pass and the slate mines. The other runs south to Seathwaite, statistically the wettest inhabited place in England, where rain piles off the surrounding fells and feeds the river. The waters of the Derwent here begin as drips from the highest ground in the country - Scafell Pike, Great End, the Glaramara ridge - and arrive at Derwentwater carrying the runoff of a small Welsh-scale wilderness.

Pure Black Rock

The Borrowdale graphite deposit is unique on Earth. Most graphite is impure and crumbly. The Seathwaite stuff was solid enough to be sawn into sticks - pure carbon, deposited around 400 million years ago in a single catastrophic geological event tied to the same Ordovician volcanism that built the surrounding peaks. The locals first used it as sheep-marker, then as a black pigment, then, by the late 16th century, as the heart of the world's first pencils. The Crown took notice. Borrowdale graphite was so valuable that the mine became a guarded national asset, with armed guards and a careful schedule of openings designed to keep prices high. Smugglers grew rich on stolen blocks. When the original vein was finally exhausted, German chemists worked out how to mix graphite powder with clay - a process still used today - and the pencil industry kept going. But the valley where it all started has never had a rival. The graphite find remains unique.

The Quiet Population

Borrowdale is not crowded. Despite welcoming a steady stream of walkers, climbers and tour buses, the civil parish itself recorded just 417 residents in the 2011 census, living in 128 households across the settlements of Grange, Rosthwaite, Seathwaite, Seatoller, Stonethwaite and Watendlath. The numbers are slowly falling. Stone cottages that once housed families of farm labourers now serve as holiday lets and guest houses. The valley still works - sheep on the fells, the slate mine at Honister, a working farm or two - but its dominant industry is hospitality. Visitors come for the walks, the youth hostels, the campsites, the wood-fired pubs and the certainty that someone, somewhere in the next ten miles, will sell them a pot of tea.

Walpole's Valley

In 1923 the novelist Hugh Walpole bought a house called Brackenburn, on the western slope above Derwentwater, with a view straight down into Borrowdale. He lived there until his death in 1941. The valley became the setting for his Herries Chronicles, a four-novel saga about a fictional family rooted in Borrowdale across three centuries. Walpole based the family seat - Herries - on Hazel Bank, the real-life home of his friends the Simpsons. He described the valley in sympathetic and accurate detail: the way mist clings to the crags after rain, the angle of light on the fells in autumn, the sound of the Derwent under a wooden footbridge. The novels are largely out of print now. The valley they were written about is still there, more or less unchanged, which is the kind of immortality Walpole would probably have preferred.

What the Light Does

There is a quality of light in Borrowdale that is hard to explain to anyone who has not stood at Grange on a clear morning. The valley faces north, the surrounding fells are dark with bracken and stone, the lake reflects whatever sky it is given. After rain - and there is always rain - the air clears to a hard brilliance that picks out every rock face, every wall, every white sheep on every hillside. The Borrowdale Volcanic Group, the geological formation that gives this whole region its bones, is named after this valley. Standing beside the Derwent and looking south up at Castle Crag, you are looking at the same andesitic ash and lava that built Scafell Pike. The pencil came from here. So did, in a sense, much of the modern Lake District itself.

From the Air

Borrowdale sits at 54.53 degrees north, 3.15 degrees west, in the central Lake District. From the air, the valley reads as a narrow green corridor running roughly south from the foot of Derwentwater, squeezed at the Jaws of Borrowdale between Castle Crag and Grange Fell, then opening into the broader Rosthwaite basin. The high ground south-west includes Scafell Pike (978 m), England's highest mountain, and Great Gable. Carlisle Lake District (EGNC) is roughly 28 nm north; Blackpool (EGNH) about 70 nm south. Mountain weather is fast-changing - what looks like clear sky over the valley can give way to low cloud on the fells within minutes. Cruise altitudes of 4,000-6,000 feet provide views over the Jaws and the southern Lake District peaks.

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