Jens Esmark's mountain glacier traverse 1823 − the key to his discovery of Ice Ages

The discovery of Ice Ages is one of the most revolutionary advances made in the Earth sciences. In 1824 Danish‐Norwegian geoscientist Jens Esmark published a paper stating that there was indisputable evidence that Norway and other parts of Europe had previously been covered by enormous glaciers carv...

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Published in:Boreas
Main Author: Hestmark, Geir
Other Authors: Universitetet i Oslo
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2017
Subjects:
Online Access:http://dx.doi.org/10.1111/bor.12260
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fbor.12260
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spelling crwiley:10.1111/bor.12260 2024-09-15T18:07:52+00:00 Jens Esmark's mountain glacier traverse 1823 − the key to his discovery of Ice Ages Hestmark, Geir Universitetet i Oslo 2017 http://dx.doi.org/10.1111/bor.12260 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fbor.12260 https://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12260 en eng Wiley http://creativecommons.org/licenses/by-nc-nd/4.0/ Boreas volume 47, issue 1, page 1-10 ISSN 0300-9483 1502-3885 journal-article 2017 crwiley https://doi.org/10.1111/bor.12260 2024-07-25T04:18:47Z The discovery of Ice Ages is one of the most revolutionary advances made in the Earth sciences. In 1824 Danish‐Norwegian geoscientist Jens Esmark published a paper stating that there was indisputable evidence that Norway and other parts of Europe had previously been covered by enormous glaciers carving out valleys and fjords, in a cold climate caused by changes in the eccentricity of Earth's orbit. Esmark and his travel companion Otto Tank arrived at this insight by analogous reasoning: enigmatic landscape features they observed close to sea level along the Norwegian coast strongly resembled features they observed in the front of a retreating glacier during a mountain traverse in the summer of 1823. Which glacier they observed up close has however remained a mystery, and thus an essential piece of information in the story of this discovery has been missing. Based on previously unknown archive sources, supplemented by field study, I here identify the key locality as the glacier Rauddalsbreen. This is the northernmost outlet glacier from Jostedalsbreen, the largest glacier in mainland Europe. Here the foreland exposed by glacier retreat since the Little Ice Age maximum around AD 1750 contains a rich collection of glacial deposits and erosional forms. The point of enlightenment is more precisely identified to be a specific moraine and its distal sandur at 61°53′26″N, 7°26′43″E. In memory of Esmark's travel companion who possibly was the first to realise the analogy, it is proposed to name this moraine Otto Tank's Moraine, a pendant to the already famous Esmark Moraine at Forsand by the sea. Article in Journal/Newspaper glacier Wiley Online Library Boreas 47 1 1 10
institution Open Polar
collection Wiley Online Library
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language English
description The discovery of Ice Ages is one of the most revolutionary advances made in the Earth sciences. In 1824 Danish‐Norwegian geoscientist Jens Esmark published a paper stating that there was indisputable evidence that Norway and other parts of Europe had previously been covered by enormous glaciers carving out valleys and fjords, in a cold climate caused by changes in the eccentricity of Earth's orbit. Esmark and his travel companion Otto Tank arrived at this insight by analogous reasoning: enigmatic landscape features they observed close to sea level along the Norwegian coast strongly resembled features they observed in the front of a retreating glacier during a mountain traverse in the summer of 1823. Which glacier they observed up close has however remained a mystery, and thus an essential piece of information in the story of this discovery has been missing. Based on previously unknown archive sources, supplemented by field study, I here identify the key locality as the glacier Rauddalsbreen. This is the northernmost outlet glacier from Jostedalsbreen, the largest glacier in mainland Europe. Here the foreland exposed by glacier retreat since the Little Ice Age maximum around AD 1750 contains a rich collection of glacial deposits and erosional forms. The point of enlightenment is more precisely identified to be a specific moraine and its distal sandur at 61°53′26″N, 7°26′43″E. In memory of Esmark's travel companion who possibly was the first to realise the analogy, it is proposed to name this moraine Otto Tank's Moraine, a pendant to the already famous Esmark Moraine at Forsand by the sea.
author2 Universitetet i Oslo
format Article in Journal/Newspaper
author Hestmark, Geir
spellingShingle Hestmark, Geir
Jens Esmark's mountain glacier traverse 1823 − the key to his discovery of Ice Ages
author_facet Hestmark, Geir
author_sort Hestmark, Geir
title Jens Esmark's mountain glacier traverse 1823 − the key to his discovery of Ice Ages
title_short Jens Esmark's mountain glacier traverse 1823 − the key to his discovery of Ice Ages
title_full Jens Esmark's mountain glacier traverse 1823 − the key to his discovery of Ice Ages
title_fullStr Jens Esmark's mountain glacier traverse 1823 − the key to his discovery of Ice Ages
title_full_unstemmed Jens Esmark's mountain glacier traverse 1823 − the key to his discovery of Ice Ages
title_sort jens esmark's mountain glacier traverse 1823 − the key to his discovery of ice ages
publisher Wiley
publishDate 2017
url http://dx.doi.org/10.1111/bor.12260
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fbor.12260
https://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12260
genre glacier
genre_facet glacier
op_source Boreas
volume 47, issue 1, page 1-10
ISSN 0300-9483 1502-3885
op_rights http://creativecommons.org/licenses/by-nc-nd/4.0/
op_doi https://doi.org/10.1111/bor.12260
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