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Maskevarri Ráhppát in Finnmark, northern Norway – is it an earthquake-induced landform complex?
Sami rahppat coarse boulders terrain new tectonic fault and earthquake
2015/1/6
The Sami word ráhppát means rough bouldery/stony terrain with sharp-relief topography in Finnmark, northern Norway. Ráhppát is a common name in the region of the Younger Dryas landforms, yet the origi...
Variations of soil profile characteristics due to varying time spans since ice retreat in the inner Nordfjord, western Norway
soil profile characteristics due varying time spans since ice retreat inner Nordfjord western Norway
2015/1/6
In the Erdalen and Bødalen drainage basins located in the inner Nordfjord in western Norway the soils were formed after deglaciation. The climate in the uppermost valley areas is sub-arctic ocean...
High resolution reflection seismic profiling over the Tjellefonna fault in the Møre-Trøndelag Fault Complex, Norway
refl ection seismic profi ling Tjellefonna fault
2015/1/4
The Møre-Trøndelag Fault Complex (MTFC) is
one of the most prominent fault zones of Norway, both onshore and offshore.
High resolution reflection seismic profiling over the Tjellefonna fault in the Møre-Trøndelag Fault Complex, Norway
High resolution reflection seismic profiling Tjellefonna fault More-Trondelag Fault Complex Norway
2015/1/4
The Møre-Trøndelag Fault Complex (MTFC) is one of the most prominent fault zones of Norway, both onshore and offshore. In spite of its importance, very little is known of the deeper structur...
Geophysical characterisation of two segments of the Møre-Trøndelag Fault Complex, Mid Norway
Geophysical characterisation two segments of the More-Trondelag Fault Complex Mid Norway
2014/12/31
The Møre-Trøndelag Fault Complex (MTFC) has controlled the tectonic evolution of Mid Norway and its shelf for the past 400 Myr through repeated reactivations during Palaeozoic, Mesozoic and ...