Degree of rock surface weathering on fjell summits in northern Finland: implications for the thermal regime of the last ice sheet

Measures of degree of rock surface weathering on three fjell summits in Finnish Lapland provide an independent test of the extent of continuously cold‐based ice during the Late Weichselian. The surface hardness of exposed surfaces is compared with that of surfaces that have remained covered and prot...

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Published in:Boreas
Main Authors: McCARROLL, DANNY, AUTIO, JYRKI, HEIKKINEN, OLAVI, KOUTANIEMI, LEO
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1996
Subjects:
Online Access:http://dx.doi.org/10.1111/j.1502-3885.1996.tb00830.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1996.tb00830.x
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spelling crwiley:10.1111/j.1502-3885.1996.tb00830.x 2024-06-02T08:06:28+00:00 Degree of rock surface weathering on fjell summits in northern Finland: implications for the thermal regime of the last ice sheet McCARROLL, DANNY AUTIO, JYRKI HEIKKINEN, OLAVI KOUTANIEMI, LEO 1996 http://dx.doi.org/10.1111/j.1502-3885.1996.tb00830.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1996.tb00830.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1996.tb00830.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Boreas volume 25, issue 1, page 1-7 ISSN 0300-9483 1502-3885 journal-article 1996 crwiley https://doi.org/10.1111/j.1502-3885.1996.tb00830.x 2024-05-03T11:00:30Z Measures of degree of rock surface weathering on three fjell summits in Finnish Lapland provide an independent test of the extent of continuously cold‐based ice during the Late Weichselian. The surface hardness of exposed surfaces is compared with that of surfaces that have remained covered and protected from subaerial weathering. Roughness measurements from granite gneiss surfaces are compared with results from similar lithologies that are known to have been eroded during the Late Weichselian. The results suggest that the summits have been covered and actively eroded by warm‐based ice and are difficult to reconcile with suggestions that large parts of Fennoscandia have not been glacially abraded since the Early Weichselian. Article in Journal/Newspaper Fennoscandia Ice Sheet Northern Finland Lapland Wiley Online Library Fjell ENVELOPE(14.526,14.526,67.181,67.181) Boreas 25 1 1 7
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Measures of degree of rock surface weathering on three fjell summits in Finnish Lapland provide an independent test of the extent of continuously cold‐based ice during the Late Weichselian. The surface hardness of exposed surfaces is compared with that of surfaces that have remained covered and protected from subaerial weathering. Roughness measurements from granite gneiss surfaces are compared with results from similar lithologies that are known to have been eroded during the Late Weichselian. The results suggest that the summits have been covered and actively eroded by warm‐based ice and are difficult to reconcile with suggestions that large parts of Fennoscandia have not been glacially abraded since the Early Weichselian.
format Article in Journal/Newspaper
author McCARROLL, DANNY
AUTIO, JYRKI
HEIKKINEN, OLAVI
KOUTANIEMI, LEO
spellingShingle McCARROLL, DANNY
AUTIO, JYRKI
HEIKKINEN, OLAVI
KOUTANIEMI, LEO
Degree of rock surface weathering on fjell summits in northern Finland: implications for the thermal regime of the last ice sheet
author_facet McCARROLL, DANNY
AUTIO, JYRKI
HEIKKINEN, OLAVI
KOUTANIEMI, LEO
author_sort McCARROLL, DANNY
title Degree of rock surface weathering on fjell summits in northern Finland: implications for the thermal regime of the last ice sheet
title_short Degree of rock surface weathering on fjell summits in northern Finland: implications for the thermal regime of the last ice sheet
title_full Degree of rock surface weathering on fjell summits in northern Finland: implications for the thermal regime of the last ice sheet
title_fullStr Degree of rock surface weathering on fjell summits in northern Finland: implications for the thermal regime of the last ice sheet
title_full_unstemmed Degree of rock surface weathering on fjell summits in northern Finland: implications for the thermal regime of the last ice sheet
title_sort degree of rock surface weathering on fjell summits in northern finland: implications for the thermal regime of the last ice sheet
publisher Wiley
publishDate 1996
url http://dx.doi.org/10.1111/j.1502-3885.1996.tb00830.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1996.tb00830.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1996.tb00830.x
long_lat ENVELOPE(14.526,14.526,67.181,67.181)
geographic Fjell
geographic_facet Fjell
genre Fennoscandia
Ice Sheet
Northern Finland
Lapland
genre_facet Fennoscandia
Ice Sheet
Northern Finland
Lapland
op_source Boreas
volume 25, issue 1, page 1-7
ISSN 0300-9483 1502-3885
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1111/j.1502-3885.1996.tb00830.x
container_title Boreas
container_volume 25
container_issue 1
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