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42 7,5-7,69 - gyttja dark brown, weakly laminated. 7,69-7,86 - dark brown to black laminated muddy gyttja. 7,86-7,97 - brown laminated muddy gyttja. 7,97-8,15 - laminated mud interrupted by a 1 cm thick, organic-rich layer, in interval 8.07-8.08 – shell fragments. 8,15-8,46 - laminated mud with shell fragments. 8,46-9,0 - mud weakly laminated. 9,00-9,37 - massive mud. 9,37-10,9 - dark green weakly laminated mud with more light impurities and shell fragments. 10,9 -11,27 - dark green massive mud with muddy “concretions” more light colour. 11,27-11,86 - dark green weakly laminated mud with more light impurities and shell fragments. 11,86-12,28 - dark green massive mud with muddy “concretions” more light colour and rich shell fragments. 12,28-12,75 - dark green weakly laminated mud with more light impurities and shell fragments. 12,75-12,77 - brown layer of mud and organic material (organic material ~25%). 12,77-13,53 - interbedding of mud and organic material (ratio of mud and organic material ~55:45%). 13,53-13,82 - blue laminated clay (varve clay). 13,82-14,47 - sand laminated. Fig. 3.10. Bottom-sediments litothostratigraphy of Umba area, lake3 with threshold of 30 m a.s.l (Fig. 3.8).
Fig. 3.11. The prominent ridge(~30 m a.s.l.) on the Turii Peninsula related to Tapes transgression Stop 10. Holocene coastal landforms on the Korabl ridge slope. Holocene coastal landforms on the slope of Korabl’ Mountain ridge (Kb in Fig. 3.6) are presented by numerous regular beach ridges, swales and terraces up to 55 m a.s.l. (Fig. 3.12) that formed by the regressing sea in Holocene. They differ from the similar coastal landforms on the Turii Peninsula in that beach ridges on Korabl’ Mountain ridge are formed by the coarse pebbles and boulders of the red sandstones (Fig. 3.13). As Figure 3.12 suggests, the High Basin Line is situated at 55 m a.s.l. This level corresponds to the Late Weichselian periglacial lake. High marine limit is located at 38-40 m a.s.l. Fig. 3.12. Geomorphological cross-sections of the beach features on the slope of the Korabl’ Mountain ridge. 43
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 and 10: independent low active Ponoi Glacie
Page 11 and 12: Fig. 1. Quaternary deposits of the
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: On the Turii Peninsula profile (Fig
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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