Glacial geomorphology in Utsjoki, Finnish Lapland proposes Younger Dryas fault-instability.

@article{Sutinen2009GlacialGI,
  title={Glacial geomorphology in Utsjoki, Finnish Lapland proposes Younger Dryas fault-instability.},
  author={Raimo Sutinen and Matti Piekkari and Maarit Middleton},
  journal={Global and Planetary Change},
  year={2009},
  volume={69},
  pages={16-28}
}
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References

SHOWING 1-10 OF 42 REFERENCES
Late Quaternary faulting and-paleoseismicity in northern Fennoscandia, with particular reference to the Lansjärv area, northern Sweden
Abstract Many fault scarps, interpreted as post- or late-glacial in age, occur in northern Sweden and adjacent parts of Finland and Norway. In the Lansjarv area in northern Sweden attempts have been…
LATE WEICHSELIAN SHEETFLOW DRAINAGE OF SUBGLACIAL LOKKA ICE LAKE
Sutinen, R., Jakonen, M., Liwata, P. & Hyvonen, E. 2007. Late Weichselian sheetfl ow drainage of subglacial Lokka ice lake. Applied Quaternary research in the central part of glaciated terrain.…
The Stuoragurra Fault, evidence of neotectonics in the Precambrian of Finnmark, northern Norway
on Finnmarksvidda. The faults appear as well defined, often linear steps in the otherwise smooth till cover. Northeast of the lake of Iejav'ri the fault crosscuts glaciofluvial deposits, indicating…
Postglacial uplift, neotectonics and seismicity in Fennoscandia
Neotectonic faulting in northern Norway; the Stuoragurra and Nordmannvikdalen postglacial faults
Seismo- and neotectonics in Finnmark, Kola Peninsula and the southern Barents Sea. Part 1: Geological and neotectonic framework
Holocene development of the Vaisjeäggi palsa mire, Finnish Lapland
A palsa mire in Finnish Lapland is studied by means of plant macrofossil analysis, physico‐chemical analysis and AMS radiocarbon dating of peat deposits in order to reconstruct its development.…
Possible triggering of Heinrich events by ice-load-induced earthquakes
North Atlantic sediments dating from the last ice age contain layers of rock fragments from northeastern Canada (so-called Heinrich layers). Like modern iceberg-borne sediments from Greenland, these…
Large Holocene landslides from Pylon Peak, southwestern British Columbia
Mount Meager massif, the northernmost volcano of the Cascade volcanic belt, has been the site of very large (>10 7 m 3 ) landslides in the Holocene Epoch. We document two complex landslides at Pylon…
Sediment anisotropy coincides with moraine ridge trend in south‐central Finnish Lapland
The morpho‐sedimentary anisotropy of a field of moraine ridges, classified previously as ribbed moraine, was studied by means of ASTER satellite data, airborne radiometric (AR) data, digital…
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