Bewegungen des Inlandeises im Lohja—Seebecken, Südfinnland

About 760 glacial striae measurements made on polished bedrock outcrops indicate variations in the direction of the movement of Fennoscandian ice-stream in the lake basin of Lohjanjärvi, South Finland. Three major ice-movements of different ages can be observed in the area. The oldest were westerly...

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Main Author: G. Glückert
Format: Article
Language:English
Published: Geological Society of Finland 1971-12-01
Series:Bulletin of the Geological Society of Finland
Online Access:http://www.geologinenseura.fi/bulletin/Volume43/sgs_bt_043_2_pages_173_184.pdf
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author G. Glückert
author_facet G. Glückert
author_sort G. Glückert
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description About 760 glacial striae measurements made on polished bedrock outcrops indicate variations in the direction of the movement of Fennoscandian ice-stream in the lake basin of Lohjanjärvi, South Finland. Three major ice-movements of different ages can be observed in the area. The oldest were westerly (240—290°) and the middle flow direction from NNW (320—350°). The youngest glacial movement advancing from a WNW direction (290—320°) was controlled more strongly by the topography than the others. The great NW—SE, N—S and ENE—WSW orientated depressions in the 59-m-deep basin of Lohjanjärvi represent tectonic fracture lines, and they have in a noticeable degree turned the direction of the ice flow in the basin. The lake is a preglacial depression. Its bedrock was originally formed by strong folding and fracturing of the Svecofennian mountain followed by weathering and hollow formation of gneissose limebearing zones and finally by glacial erosion of several ice ages. Two groups of small rock drumlins are formed in the direction of the main ice flow in plane areas at Vohloinen and Lohjansaari. The so-called »Zungenbecken» formations occur in some deep bays near the town of Lohja.
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spelling doaj.art-9c310ca082bb49b2a769d1846de7e2a92022-12-21T21:18:29ZengGeological Society of FinlandBulletin of the Geological Society of Finland0367-52111799-46321971-12-0143217318410.17741/bgsf/43.2.004Bewegungen des Inlandeises im Lohja—Seebecken, SüdfinnlandG. GlückertAbout 760 glacial striae measurements made on polished bedrock outcrops indicate variations in the direction of the movement of Fennoscandian ice-stream in the lake basin of Lohjanjärvi, South Finland. Three major ice-movements of different ages can be observed in the area. The oldest were westerly (240—290°) and the middle flow direction from NNW (320—350°). The youngest glacial movement advancing from a WNW direction (290—320°) was controlled more strongly by the topography than the others. The great NW—SE, N—S and ENE—WSW orientated depressions in the 59-m-deep basin of Lohjanjärvi represent tectonic fracture lines, and they have in a noticeable degree turned the direction of the ice flow in the basin. The lake is a preglacial depression. Its bedrock was originally formed by strong folding and fracturing of the Svecofennian mountain followed by weathering and hollow formation of gneissose limebearing zones and finally by glacial erosion of several ice ages. Two groups of small rock drumlins are formed in the direction of the main ice flow in plane areas at Vohloinen and Lohjansaari. The so-called »Zungenbecken» formations occur in some deep bays near the town of Lohja.http://www.geologinenseura.fi/bulletin/Volume43/sgs_bt_043_2_pages_173_184.pdf
spellingShingle G. Glückert
Bewegungen des Inlandeises im Lohja—Seebecken, Südfinnland
Bulletin of the Geological Society of Finland
title Bewegungen des Inlandeises im Lohja—Seebecken, Südfinnland
title_full Bewegungen des Inlandeises im Lohja—Seebecken, Südfinnland
title_fullStr Bewegungen des Inlandeises im Lohja—Seebecken, Südfinnland
title_full_unstemmed Bewegungen des Inlandeises im Lohja—Seebecken, Südfinnland
title_short Bewegungen des Inlandeises im Lohja—Seebecken, Südfinnland
title_sort bewegungen des inlandeises im lohja seebecken sudfinnland
url http://www.geologinenseura.fi/bulletin/Volume43/sgs_bt_043_2_pages_173_184.pdf
work_keys_str_mv AT ggluckert bewegungendesinlandeisesimlohjaseebeckensudfinnland