From the sea shore, the path had been rising steadily up the hillside, twisting and turning through thick forest, when suddenly it opened up on to a vast clearing of cobble-sized stones. I had spent the previous hour sweating up the mountainside, yet it felt as if I were back on the coast, staring across a rocky beach at low tide.
I wasn’t too far wrong: this was in fact an ancient seabed, one of many bizarre features of the Swedish High Coast – in the Gulf of Bothnia, the topmost part of the Baltic Sea, 500km north-east of Stockholm. It’s a wild and largely unsettled landscape of flat-topped mountains, dense evergreen forests, lakes and inlets that is, quite literally, on the rise.
During the most recent ice age, this region was crushed by a 3km-thick layer of ice. But when this began to melt 9,600 years ago, the land began to rise in a process called isostatic rebound. It has been growing at a rate of 8mm a year ever since, leading to an ever-evolving archipelago gradually emerging from the sea. It was declared a Unesco world heritage site in 2000. ....... keep reading ..... http://bit.ly/2DEnaUV
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