Dave Broom argues why historical sites such as Lindores and Kennetpans must be preserved.
‘Why aren’t we told about this stuff?’ my walking companion asked. I’d been pointing out the rickle of stones and the lines of lazy beds the slanting sunlight was picking out among the heather. The stones would have been a small township, the lazybeds its occupants’ strips for cultivation, fertilised by seaweed dragged up from the bay where we’d landed, spread on piles.
I’d started to explain that the abandonment was unlikely to have been optional. We were on South Uist – north-east South Uist to be precise. Between 1841 and 1851 the island’s population was halved as its then landlord, John Gordon of Cluny, embarked on brutal clearances of the island, Benbecula, and Barra. His former tenants were forcibly shipped to Canada and left abandoned on the dockside.
‘It’s a forgotten history,’ he said, shaking his head as we head along the moor towards the lighthouse. ‘It needs to be told, it explains so much about how people spread over the world.’
Ancient foundations: This South Uist rock pool is lined with impenetrable Lewisian gneiss
Maybe wandering, whether by choice or enforced, is in Scottish bones. Over a week’s expedition we’d followed the whale-road from Orkney to Loch Ewe, Rum, and now the Uists (an attempt to reach St. Kilda having been nixed thanks to stormy weather). On board the ship I gave talks, wandering through whisky’s roots, flavours, styles often picking up on what information we’d gleaned in the morning hikes with the attendant geologists, historians, and naturalists.
A new picture of Scotland was beginning to form. One rooted in rock and migration. A year ago I wrote of shearwaters, now they were on the waves once more getting ready to head south. We travelled, picking up knowledge, fitting pieces into this new frame. The Clearances were now part of it.
On one side, over the Minch, were the hills of Skye, to the north the shattered landscape of the Hebrides. We sat next to one of the pools which stud the Uist landscape, its dark brown waters lit by flashes of cornflower blue.
I picked up a fist-sized lump of rock, gritty, zebra-striped, kibbled with crystals. Lewisian gneiss. It is old, and I mean old. 3,000 million years, which is so absurd a number it is impossible to compute. It is so ancient it contains no fossils, just the sparkles of those early minerals. I hold the roughness of unimaginable time in my hand, a rendering of liquefied rock from the earth’s heart, warped and buckled over eons.
As tectonic plates shifted, these rocks were heaved out of the planet’s belly to its surface to cool. They drifted across the globe as the continents continued their slow dance, starting close to where Antarctica is now, then settling into what is now Canada, before splitting off and fusing with what is now England. Odd that the emigrants took the same journey, but in reverse. Wandering rock, people, ship.
Distant beginnings: Looking out from South Uist across to the Isle of Skye
When the gneiss appears we have reached the basement. It is the bedrock, obdurate, unchanging, impermeable, and because of this, water cannot penetrate hence the pools, and the boggy ground. Gneiss flares red on geological maps, which is appropriate enough for these boggy, oxygen-starved conditions, and means that peat starts to build up, and peat means fuel, and fuel means home.
The thin soils were suitable only for some crops: kale, potatoes, bere barley or oats. Basic sustenance, and also the roots of what we call whisky.
All that’s left behind are the stones, the lines in the turf and the lost memories of the songs they sang and the drink they made. The scent of peat gone as they started their wanderings. The memories fragile, worn away. It’s perhaps too neat a metaphor.
We’ve caught up with Chris Edwards, the expedition’s geologist. I ask him if this scoured landscape is the result of erosion, is this is what was left behind after people, rock and soil had been removed?
‘We don’t know fully, but what we can say is that this landscape now is what it would have been like just after the ice left,’ he replies. ‘Isn’t that amazing? How things stay the same, and yet change.’ Time seems to compress, the houses rebuilt, smoke through the thatch, boats in the bay, crops in the field, the buzz of bees and, who knows, a wee sensation of spirit after the day’s work is done.
This is how it started. This is whisky’s bedrock.
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