Field guide - IUGS

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The termination of the deglaciation is related to the ice extinction in the western part of the region, about 9500 BP. Around 9500 years BP glaciomarine sediments were replaced by marine deposits in the Pechenga River valley (Bakhmutov et al., 1994). The Holocene (QBIVB, MIS 1) The Holocene sediments are everywhere represented by marine, lacustrine, alluvial, eluvialdeluvial, peaty and bog deposits, and by diatomite. 10
Fig. 1. Quaternary deposits of the Kola region (extract from Niemelä et al., 1993) 11
Page 1 and 2: 33 IGC excursion No 34, August 14 -
Page 3 and 4: Abstract Partisipants will examine:
Page 5 and 6: General introduction Kola Peninsula
Page 7 and 8: ESR-age of subfossil mollusk shells
Page 9: independent low active Ponoi Glacie
Page 13 and 14: EXCURSION STOPS Day 1: Arrive at Ap
Page 15 and 16: Day 2 Trip to the Lovozero Mountain
Page 17 and 18: 17 Fig. 2.3. Geomorphological map o
Page 19 and 20: 19 Fig. 2.5. U-shaped valley with S
Page 21 and 22: a b Fig. 2.7. Lateral meltwater cha
Page 23 and 24: Fig. 2.9. Kola recessive marginal b
Page 25 and 26: There are two opinions on the genes
Page 27 and 28: Fig. 2.14. Fragment of the dump mor
Page 29 and 30: Fig. 2.18. Orientation diagrams for
Page 31 and 32: een developed in a single field of
Page 33 and 34: Day 3: Trip along the Tersky Coast
Page 35 and 36: Stop 7. Quarry opening the glaciofl
Page 37 and 38: Fig. 3.5.The outcrop of the damp mo
Page 39 and 40: Fig. 3.7. Internal structure of fac
Page 41 and 42: On the Turii Peninsula profile (Fig
Page 43 and 44: Fig. 3.11. The prominent ridge(~30
Page 45 and 46: Day 4. Start in Varzuga village at
Page 47 and 48: and fine-grained sands, is exposed
Page 49 and 50: Fig. 4.3. Sediment and landforms in
Page 51 and 52: 51 Fig.4.6. Strel'na marine beds fr
Page 53 and 54: 53 Fig.4.8. Overview and scheme of
Page 55 and 56: possible earthquakes (6.5), obtaine
Page 57 and 58: Stop 13. Paleoseismic dislocation
Page 59 and 60: glacial formations occurred, positi
Page 61 and 62:
Fig. 5.4. Geological map of the Khi
Page 63 and 64:
Ice dammed lakes features are large
Page 65 and 66:
Fig. 5.8. Glaciofluvial delta and m
Page 67 and 68:
67 Fig. 5.10. Cirques of Tachtarvum
Page 69 and 70:
Fig. 5.14. Scenario of the glacier
Page 71 and 72:
Helmens, K.F., Räsänen, M.E., Joc
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Field guide - IUGS

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