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63 Hyvärinen, rryvärinen, H., 1972. Flandrian regional regional pollen assemblage zones in eastern eastera Finland. Societas societas Scientiarum scientiarum Fennica, Commentationes commentationes Biologicae 59. b9. 25 p. Hyvärinen, H., 1973. The deglaciation deglaciation his history tory of eastern Fennoscandia - recent data from Finland. Boreas Boreas 2, 2,85-L02. 85-102. Hyyppä, Ifyyppä, E., 1936. Über die spätquartäre spätquartäre Entwicklung Entwicklung Nord-Finnlands mit Ergänzungen zur Kenntnis des spätglazialen spätglazialen Klimas. Klimas. Vorläufige vorläufige Mitteilung. Comptes Comptes Rendus Rendus de la Societe Soci6t6 Geologique Gdologique de Finlande 9; Bulletin de la Commission geologique g6ologique de Finlande 115, 401-465. 401-465. Hyyppä, E., 1966. I Salpausselän geologinen rakenne rakenne Lahden seudulla. Summary: On On the structure of the First Salpausselkä Salpausselkä at Lahti. Lahti. Geologi 18 (6), 73-76. 78-76. Ignatius, K.E.F., 1891. 1891. Finlands geografi. geografr. Handbok Handbok für ftir medborgare pä uppdrag af Finska Litteratur-sällskapet. I. Allmän Allmän öfverblick öfverblick af land och folk. Med kartor och illustrationer. Helsingfors: Finska Litteratursällskapets tryckeri. 594 bg4 p. Ignatius, H., II., Korpela, K. K. & & Kujansuu, Kr{ansuu, R., 1980. The The deglaciation ofFinland of Finland after 10000 10 000 B.P. Boreas 9, 9,217-228. 217-228. Jernström, Jernströn, A., A-, 1876. Om Om Qvartärbildningarna längs ltings Abo-Tavastehus-Tammerfors Abo-Tavastehus-Ta-merfors jenrvägslinie. jernvägslinie. Bidrag till kännedom af Finlands Finlands natur natur och folk 20. 77-115. Kilpi, S., 1937. Das Sotkamo-Gebiet in spätglazialer Zeit. Bulletin de la la Commission g6ologique geologique de Finlande Finlande 117, 1-118. Kqiansuu, Kujansuu, R., 1995. Sisä-Suomen reunamuodostuman syntyyn vaikuttaneista tekijöistä; kerrostumisolojen kuvastuminen kuvastuminen pohjasedimenteissä. pohjasedimenteissä. Summary: On the factors alfecting affecting the deposition of Central Finland ice-marginal formation; sedimentation sedimentation conditions reflected by bottom bottom sediments. sediments. Geologi 47 (9-lO),129-133. (9-10), 129-133. Krliansuu, Kujansuu, R. & Nenonen, K., 1987. Till Till stratigraphy and ice-flow directions in North Karelia. Geological Geological Survey of Finland. Special Paper 1,59-66. 1, 59-66. Krliansuu, Kujansuu, R. & Niemelä, J., J., 1984. Quaternar5r Quaternary deposits of Finland, Finland, 1:1 000 000000. 000. Espoo: Espoo: Geological Geological Survey of Finland. Finland. Kurimo, H., 1982. Ice-lobe lee-lobe formation and function during the deglaciation in m Finland and adjacent Soviet Karelia. Boreas 11, 59-78.
64 Lahermo, P. & Rainio, Rainio, H., II., 1976. 1976. Mellersta Mellersta Finlands Finlands randformation. randformation. Abstracts Abstracts av föredrag Iiiredrag vid XII Nordiska Geologvintermötet Göteborg Gäteborg 7-10 7- 10 J Januari, anuari, 1976. Göteborg: Geologiska institutionet. institutionet. Chalmers Chalmers tekniska tekniska högskola och Göteborgs Göteborgs universitet. Leiviskä, Leivishä,I., I., 1920. 1920. Der Salpausselkä. Fennia Fennia 41 41(3), (3), 1-388. Leiviskä, Leivishä, I., 1928. Über Über die die Ose Mittel-Finnlands. Die Entstehung Entstehung des Materials Materials und und der Formen Fomen der der Ose. Ose. Fennia Fennia 51 5L (4), 1-207. ]-2O7. Leiviskä, Leivishä, I., I., 1951. 1951. Drei Drei eiszeitliche Randmoränen. Fennia Fennia 74, 83 p. Lillja, Li\ia,.I. J. W., \ü., 1858. Geografisk Geogralisk och och historisk karta öfver Finland, Finland, till skolornas bruk. Abo: Abo: J J.W.Lillja .W.Lillja & & C:o C:o förlag. ftrlag. Lukashov, Lukashov, A., .d, Iljin, I[iin, V. V. & Ekman, Ekman, I., 1981. 1981. Marginal Marginal glacial formations formations of the Salpausselkä Salpausselkä stage in Soviet Karelia. Glacial deposits deposits and glacial glacial history in eastern Fennoscandia. Fennoscandia. Apatity: Academy os Sciences ofthe of the USSR, 128-139. Lukashov, A.D. A"D. & & Ekman, I.M., I.M., 1982. 1982. General information on geology geology and geogeomorphologymorphologT of the the Karelian ASSR, 4-17. Illustrations, Illustrations, 46-4 46-47(-56). 7( -56). In: In: International Union Union for for Quaternary research, XI XI Congress, Moscow, August August 1982. Guidebook for excursion excursion A-4, C-4. C-4. Moscow. Lundqvist, J., aI., 1987. 1987. Glaciodynamics of of the the Younger Younger Dryas Marginal Zone in Scandinavia. Scandinavia. Implications of of a a revised glaciationmodel. glaciationmodel. Geografiska Annaler 69A, 305-319. 305-319. Lundqvist, J., 1990. The Younger Dryas Dryas event event in Scandinavia. In: Termination of the Pleistocene. IGCP project 253. Lundqvist J. J . & Saaraisto, Saarnisto, M. (eds.). Field conference Norway-Sweden-Finland, Norway-Sweden-Finland, May May 9-16, 1990. Geological Survey of ofFinland. Finland. Guide 31, 3L,5-24. 5-24. Lundqvist,.I. Lundqvist, J. & Saarnisto, M., 1995. Summary of Project IGCP-253. Quaternary International 28, 9-18. Lyytikiünen, Lyytikäinen, A., 1980. Pohjois-Karjalan Pohjois-Karjalan ^{,., harjumaiseman haIjumaiseman kehitys, käyttti käyttö ja suojelu. Summar5l: Summary: The development, development, use and conservation of the the esker landscape in North Karelia, eastern eastern Finland. The Nation-Wide Nation-Wide Esker Esker Investigation, Report 14. 9 p. Lyytikiünen, Lyytikäinen, A, A., 1982. Pohjois-Karjalan Pohjois-KaIjalan harjumaiseman haIjumaiseman kehitys sekä nykyisen tilan ja maankäytön maankäytön yleispiirteet. summary: Summary: The development development and present present state of
Page 1 and 2:
LATE WEICHSELIAN END MORAINES AND D
Page 3 and 4:
Rainio, Heikki 1996. Late Weichseli
Page 6 and 7:
CONTENTS CON"IENTS Preface . . . .
Page 8 and 9:
The thesis is based on the followin
Page 10:
Joint publications 9 I Publications
Page 13 and 14: 20 km :l .,,I End Fnd moraines * /2
Page 15 and 16: L4 14 Obsen'ations Observations of
Page 17 and 18: 16 STI'DIES STUDIES ON ON THE SALPA
Page 19 and 20: 18 there via Riihimfi, Riihimäki,
Page 21 and 22: 20 the the notion, rejected rejecte
Page 23 and 24: 22 In 1920, Leiviskä Leiviska publ
Page 25 and 26: 24 24 According According to the in
Page 27 and 28: 26 In this zone, whieh which is elo
Page 29 and 30: 28 28 According to Berghell (1916),
Page 31 and 32: 30 Rainio (1972) (L972) proposed th
Page 33 and 34: s2 32 SALPAUSSEI.J(A SALPAUSSELKÄ
Page 35 and 36: 34 34 In the the light light of the
Page 37 and 38: 36 Rainio and Lahemo Lahermo togeth
Page 39 and 40: 38 11 II Rainio, H. H. 1985. 1985.
Page 41 and 42: 40 This This article presents new o
Page 43 and 44: v 42 V Rainio, Rainio,Il. H. 1993.
Page 45 and 46: 44 The conclusion is that that at a
Page 47 and 48: 46 In a zone zone about 10-km wide
Page 49 and 50: 48 The The relationship relationshi
Page 51 and 52: 50 Jaamankangas are composed of san
Page 53: 52 The The arguments presented pres
Page 56 and 57: 55 hummoeky hunmocky moraines that
Page 58 and 59: Closing words A hundred years ago,
Page 60 and 61: REFERENCES 59 Aario, R- & Forsströ
Page 62 and 63: 61 Ekman' r. & rliin, v., 1991. Deg
Page 66 and 67: 65 esker lands landscape cape of No
Page 68 and 69: 67 Rainio, H., 1978. 1978. Exkursio
Page 70 and 71: 69 Rainio, H., Saarnisto, M. & Ekma
Page 72 and 73: 71 7L Sauramo, Saurarno, M., 1928.
Page 74: 73 ?3 Wiik, wiik, F.J., 1876. Öfve
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