Slåttdalsskrevan
Västernorrlands län
Slåttdalsskrevan is a remarkable natural crevice approximately 200 meters long, 30 meters deep, and 7 meters wide, located in Ångermanland, Sweden. It divides the Slåttdalsberget mountain into two distinct parts and is one of the highest points within Skuleskogen National Park. The surrounding cliffs and the crevice walls are composed of red Nordingrå granite, a characteristic feature of the region's rugged landscape. Formed over a billion years ago, the crevice's unique geological history includes the intrusion of diabase magma that later eroded away, shaped further by multiple ice ages and land uplift processes. Slåttdalsskrevan is part of the famous Höga Kustenleden hiking trail, attracting nature enthusiasts seeking dramatic scenery. Although the passage through the crevice has been closed since June 2023 due to rockfall hazards, visitors can still experience and photograph the impressive formation from both the northern and southern ends via alternative routes. This natural monument is protected as a national conservation object, highlighting its ecological and geological importance in Sweden.
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Tip: The best time to visit Slåttdalsskrevan is during late spring to early autumn when hiking trails are accessible and weather conditions are favorable. Since the direct passage through the crevice is currently closed due to rockfall risks, visitors should use the alternative trail that circles around the crevice. It is advisable to check the latest trail conditions and possible restrictions on the official Skuleskogen National Park website before planning your visit. Booking guided tours or visiting during weekdays may help avoid crowds. Discounted access may be available for certain groups, so inquire locally.
Interesting facts
- •Slåttdalsskrevan splits Slåttdalsberget mountain into two separate parts.
- •The crevice is about 200 meters long, 30 meters deep, and 7 meters wide.
- •Its walls are made of distinctive red Nordingrå granite.
- •The formation was shaped by diabase intrusion around 1.2 billion years ago, later eroded by ice ages and land uplift.
- •It is a designated national conservation object in Sweden.
History
Slåttdalsskrevan's geological formation dates back approximately 1.2 billion years when diabase magma intruded into the red Nordingrå granite of Slåttdalsberget.
Over subsequent millennia, erosion processes, including multiple ice ages, removed the more fragile diabase, shaping the deep crevice seen today.
The area was later influenced by land uplift following the last ice age, further defining the landscape.
Recognized for its natural significance, Slåttdalsskrevan became a protected conservation site within Skuleskogen National Park, which was established to preserve the unique High Coast environment.
Contact
Phone: 0613-70 02 00