Braslauskiya azyory

This is glacial country in the most literal sense: everything visible was laid down or gouged out by the last ice sheet, which stalled here long enough to leave its whole vocabulary of landforms on the ground. The Braslav ridge is a belt of moraine hills, drumlins streamlined by the ice into long parallel whalebacks, eskers left by rivers that ran in tunnels under the glacier, and kames dumped where meltwater ponded. Between them lie the lakes — around seventy inside the park's boundary, linked in chains and separated by necks of hill sometimes only a few hundred metres wide. Belarus made it a national park in 1995.

The water dominates. Dryviaty, the largest at some thirty-six square kilometres and the shallowest of the big three at twelve metres, spreads south of Braslav town; Snudy and Strusta lie north of it, deeper and island-strewn — Snudy carries eleven islands, Strusta seven, strung along its axis into a labyrinth. This is the best of the group for birds: gull colonies on the low islets, and the only reliably known breeding ground in northern Belarus for greylag goose, ferruginous duck, oystercatcher and bearded reedling. From Mayak hill, the kame between the two lakes, the pattern reads all at once — water, hill, water, hill, out to the Latvian border — and since 2020 there has been a thirteen-metre tower on top to read it from.

People have used the position for as long as it has been habitable. Zamkavaya Hara, the castle mound in the middle of Braslav, carries the earthworks of a fortified settlement occupied from the ninth century to the fifteenth, its ramparts still standing four metres high and nine on the north-west; nothing of the castle itself survives. The town below is small, wooden in places, and built along an esker — the ridge between lakes Dryviaty and Novyata is a meltwater deposit, and the main street runs down the spine of it. Out in the district the traces are scattered: the neo-Romanesque church at Slobodka, finished in 1906, standing over its lake; the terraces and Gothic-revival crypt-chapel of Belmont at Achremaŭcy, where the palace was pulled down for building material in the 1940s; field boundaries that follow drumlin crests because nothing else would drain.

What's worth knowing before you go

Braslav is the base and effectively the only one; it sits on Dryviaty's northern shore with the park administration, boat and bicycle hire, and the visitor centre. Braslav's station building survives but its line does not, so the approach is by road — about four hours by bus from Minsk, rather less by marshrutka.

The season is genuinely short, and the park quantifies it more honestly than most: seventy-seven days a year above the comfortable-summer threshold, against ninety-five to a hundred of comfortable winter. Its winter is longer than its summer. July and early August fill the lakeside campsites, though swimmers should know that the park's own management plan flags Dryviaty and Snudy as a serious cercarial-dermatitis hazard — swimmer's itch, harmless and miserable, worst in warm shallow water. The last full week of July is worth avoiding altogether unless you came for it: the Viva Braslav festival puts something like three times the town's population on the beach at Dryviaty, and the park's campsite tariff goes up roughly sixfold for the duration. By late September the light goes long and gold across the ridges and the crowds are gone, which is the better trade.

The connoisseur's move is a boat among the islands of Strusta rather than a walk along the shore: the archipelago only makes sense from the water, and Chaichin — 1.6 square kilometres, the second-largest island in Belarus, named for its gulls — has a lake of its own inside it, a former channel left stranded as the water shallowed.