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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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 |