At this position, one can see a steep normal fault in the mountain side. Normal faults occur when rock is subject of extensional movement and breaks. Further towards the airport, folding and faulting caused by compression is visible. Compressional and extensional structures are often related, with the compressional structures perpendicular to the main stress direction, and the extensional structures more or less parallel to it.
The Longyearbyen Field Guide
We are a group of scientists and Svalbardians who want to share our knowledge about the vicinity of Longyearbyen with you. This app is non-commercial and meant for locals, guides, tourists and everyone interested in science.
It is initially based on the book “The Geology of Longyearbyen” and supported by the Svalbard environmental protection fund, The University Centre in Svalbard, Store Norske Spitsbergen Kulkompani and HDpublish.
We appreciate all of the voluntary contributions and support from all authors and initiators for making this app possible.
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