GLACIAL HISTORY AND PERMAFROST IN THE SVALBARD AREA

Figure 2.9 – Geoseismic profile showing the development of the glacigenic sequence in outer Bjørnøyrenna and the top of the prograding clastic wedge deposited at the western

Models project that autumn and winter temperatures in the Arctic will increase to 4–5°C above late 20 th century values before mid-century, under either a moderate or

The analysis has shown that the dominant storyline in the Western media was that the enforcement of formal regulations and regulatory pressure against Shell and BP was subject

(2018): Lateglacial and Holocene glacier activity in the Van Mijenfjorden area, western Svalbard. The aim of this study was to detail the Late Weichselian and Holocene glacial

One explanation for the increased FMW in the upper 10 cm of the sea ice observed in 2012, between sta- tion 3 and the ice edge (station 5), together with high salinity, [CO 3 2− ],

A major feature in the lateglacial sea-level history of western Norway is the YD transgression, representing a rise in relative sea level of 10 m.. It temporarily reversed the

All investigators have regarded the Palaeogene deposits developed within small isolated sectors on the west coast of Svalbard (except the Kongsfjorden area)

(B) A section from the lower part.of the lacustrine sediments (core 14) with sporadic lamination.. John lnge Suendsen and Jan Mongerud: Holocene glacial and climatic