Akmens kelias į Lietuvą

Stones as solid individual pieces of rock are the main subject matter of the present paper. Their origin on the surface of the earth has been discussed by European field scientists since long ago. According to one of the persistent hypotheses, boulders were scattered by the waters of deluge. In the...

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Main Author: Baltrūnas, Valentinas
Format: Other/Unknown Material
Language:Lithuanian
Published: 2008
Subjects:
Online Access:https://www.vdu.lt/cris/bitstream/20.500.12259/127061/2/ISSN1822-7309_2008_T_6.PG_14-22.pdf
https://hdl.handle.net/20.500.12259/127061
id ftvytmagnusuniv:oai:portalcris.vdu.lt:20.500.12259/127061
record_format openpolar
spelling ftvytmagnusuniv:oai:portalcris.vdu.lt:20.500.12259/127061 2023-05-15T16:11:58+02:00 Akmens kelias į Lietuvą The path of stone to Lithuania Baltrūnas, Valentinas LT 2008 p. 14-22 text/xml application/pdf https://www.vdu.lt/cris/bitstream/20.500.12259/127061/2/ISSN1822-7309_2008_T_6.PG_14-22.pdf https://hdl.handle.net/20.500.12259/127061 lt lit Acta humanitarica universitatis Saulensis. Akmuo kultūroje. Šiauliai : Šiaulių universiteto leidykla, 2008, T. 6 IndexCopernicus 18227309 VDU02-000065583 https://www.vdu.lt/cris/bitstream/20.500.12259/127061/2/ISSN1822-7309_2008_T_6.PG_14-22.pdf https://hdl.handle.net/20.500.12259/127061 open access Lietuva Fenoskandija Akmuo Riedulys Ledynas Gamtos paminklas Lithuania Fennoscandia Stone Boulder Glacier Geological monument Geologija / Geology (N005) Straipsnis kitose duomenų bazėse / Article in other databases (S4) 2008 ftvytmagnusuniv 2021-02-16T00:43:44Z Stones as solid individual pieces of rock are the main subject matter of the present paper. Their origin on the surface of the earth has been discussed by European field scientists since long ago. According to one of the persistent hypotheses, boulders were scattered by the waters of deluge. In the course of time, a new hypothesis has developed. According to it, stones were scattered on the surface of the earth by icebergs. This hypothesis was proposed by a Scottish field scientist Ch. Lyell in 1830. Famous doctor and field scientist E. Eichwald (1830) also supported this point of view. He explained the appearance of boulders in the Vilnius region by iceberg activity. Some time later, exponents of the theory of glaciations took root in Europe. This opinion became popular in the Baltic countries in the second half of the 19th century (C. F. Schmidt, G. Berendt, A. Giedraitis, etc.). Yet only in 1911 a Finnish scientist J. Sederholm compiled and published a map demonstrating the cones (fans) of scattering of Fennoscandian indicator boulders in the northern part of Europe Vytauto Didžiojo universitetas Švietimo akademija Other/Unknown Material Fennoscandia Fennoscandian Vytautas Magnus University e-Publication Repository (VMU ePub) The Cones ENVELOPE(78.344,78.344,-68.635,-68.635)
institution Open Polar
collection Vytautas Magnus University e-Publication Repository (VMU ePub)
op_collection_id ftvytmagnusuniv
language Lithuanian
topic Lietuva
Fenoskandija
Akmuo
Riedulys
Ledynas
Gamtos paminklas
Lithuania
Fennoscandia
Stone
Boulder
Glacier
Geological monument
Geologija / Geology (N005)
spellingShingle Lietuva
Fenoskandija
Akmuo
Riedulys
Ledynas
Gamtos paminklas
Lithuania
Fennoscandia
Stone
Boulder
Glacier
Geological monument
Geologija / Geology (N005)
Baltrūnas, Valentinas
Akmens kelias į Lietuvą
topic_facet Lietuva
Fenoskandija
Akmuo
Riedulys
Ledynas
Gamtos paminklas
Lithuania
Fennoscandia
Stone
Boulder
Glacier
Geological monument
Geologija / Geology (N005)
description Stones as solid individual pieces of rock are the main subject matter of the present paper. Their origin on the surface of the earth has been discussed by European field scientists since long ago. According to one of the persistent hypotheses, boulders were scattered by the waters of deluge. In the course of time, a new hypothesis has developed. According to it, stones were scattered on the surface of the earth by icebergs. This hypothesis was proposed by a Scottish field scientist Ch. Lyell in 1830. Famous doctor and field scientist E. Eichwald (1830) also supported this point of view. He explained the appearance of boulders in the Vilnius region by iceberg activity. Some time later, exponents of the theory of glaciations took root in Europe. This opinion became popular in the Baltic countries in the second half of the 19th century (C. F. Schmidt, G. Berendt, A. Giedraitis, etc.). Yet only in 1911 a Finnish scientist J. Sederholm compiled and published a map demonstrating the cones (fans) of scattering of Fennoscandian indicator boulders in the northern part of Europe Vytauto Didžiojo universitetas Švietimo akademija
format Other/Unknown Material
author Baltrūnas, Valentinas
author_facet Baltrūnas, Valentinas
author_sort Baltrūnas, Valentinas
title Akmens kelias į Lietuvą
title_short Akmens kelias į Lietuvą
title_full Akmens kelias į Lietuvą
title_fullStr Akmens kelias į Lietuvą
title_full_unstemmed Akmens kelias į Lietuvą
title_sort akmens kelias į lietuvą
publishDate 2008
url https://www.vdu.lt/cris/bitstream/20.500.12259/127061/2/ISSN1822-7309_2008_T_6.PG_14-22.pdf
https://hdl.handle.net/20.500.12259/127061
op_coverage LT
long_lat ENVELOPE(78.344,78.344,-68.635,-68.635)
geographic The Cones
geographic_facet The Cones
genre Fennoscandia
Fennoscandian
genre_facet Fennoscandia
Fennoscandian
op_relation Acta humanitarica universitatis Saulensis. Akmuo kultūroje. Šiauliai : Šiaulių universiteto leidykla, 2008, T. 6
IndexCopernicus
18227309
VDU02-000065583
https://www.vdu.lt/cris/bitstream/20.500.12259/127061/2/ISSN1822-7309_2008_T_6.PG_14-22.pdf
https://hdl.handle.net/20.500.12259/127061
op_rights open access
_version_ 1765997182431789056