En del av de uppgifter som samlas in av denna leverantör är avsedda för personalisering och mätning av annonseringseffektivitet.
En del av de uppgifter som samlas in av denna leverantör är avsedda för personalisering och mätning av annonseringseffektivitet.
En del av de uppgifter som samlas in av denna leverantör är avsedda för personalisering och mätning av annonseringseffektivitet.
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Kinnekulle has a complete set of layers featuring all of the rocks found in the table mountains: basement, sandstone, alum shale, limestone, clay shale, and dolerite. The dolerite layer is very thin, however – only about 10 metres thick. That is why Kinnekulle has such a characteristic conical shape and lacks the big dolerite plateau that many of the other mountains have.
Learn more www.vastsverige.com/en/lacko-kinnekulle/kinnekulle
Layers of history — In the geopark we find geological phenomena and places that are only found here or in a few places in the world, such as; the peneplane (the bedrock surface) with its flat surface, the table mountains which with their unique rock layers rise from the plain landscape and ice age deposits that create an incomparable landscape. This geology has also created conditions for varied flora, species-rich fauna, exciting cultural and industrial history and active outdoor life. Platåbergens Geopark is a collaboration between nine municipalities; Trollhättan, Vänersborg, Grästorp, Lidköping, Götene, Skara, Falköping, Skövde och Mariestad.
Skaras stadshus
Södra kyrkogatan 2
532 88 Skara
SWEDEN
info@platabergensgeopark.se
Platåbergens Geopark is since 2022 Sweden’s first UNESCO Global Geopark. Today there are 213 geoparks across 48 countries. We collaborate with other geoparks over the world via the Global Geoparks Network and the European Geoparks Network, which aims to connect geoparks all around the world.
