V. On hollow pyramidal ice crystals
I. The Lava Cavern, Surtshellir .—At a visit to the lava cavern, Surtshellir (Iceland), in June, 1892, the farthest recess, which contains ice stalactites and an ice pond, was found to be covered on walls and ceiling with ice crystals in the form of hollow hexagonal pyramids, analogous in shape to t...
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The Royal Society
1894
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Online Access: | http://dx.doi.org/10.1098/rspl.1894.0020 https://royalsocietypublishing.org/doi/pdf/10.1098/rspl.1894.0020 |
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crroyalsociety:10.1098/rspl.1894.0020 2024-06-02T08:09:16+00:00 V. On hollow pyramidal ice crystals 1894 http://dx.doi.org/10.1098/rspl.1894.0020 https://royalsocietypublishing.org/doi/pdf/10.1098/rspl.1894.0020 en eng The Royal Society https://royalsociety.org/journals/ethics-policies/data-sharing-mining/ Proceedings of the Royal Society of London volume 55, issue 331-335, page 113-115 ISSN 0370-1662 2053-9126 journal-article 1894 crroyalsociety https://doi.org/10.1098/rspl.1894.0020 2024-05-07T14:16:29Z I. The Lava Cavern, Surtshellir .—At a visit to the lava cavern, Surtshellir (Iceland), in June, 1892, the farthest recess, which contains ice stalactites and an ice pond, was found to be covered on walls and ceiling with ice crystals in the form of hollow hexagonal pyramids, analogous in shape to the well-known cubic crystals of rock salt. The hollow ice pyramids were, roughly speaking, built in the proportion of base 1 to height 2, and ranged up to about 1 in. diameter of base. They were attached to the wall by their apices, turning their hollow bases towards the interior of the cave. They were only found on those parts where stalactites did not occur. The temperature was +0.5° C. (+33° F.), and, as the cave forms a cul-de-sac , the air is perfectly calm. The crystals, having thus evidentia been formed from the moisture of the atmosphere, had to be considered as a kind of hour frost. Article in Journal/Newspaper Iceland The Royal Society Recess ENVELOPE(-61.516,-61.516,-64.500,-64.500) Proceedings of the Royal Society of London 55 331-335 113 115 |
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Open Polar |
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The Royal Society |
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crroyalsociety |
language |
English |
description |
I. The Lava Cavern, Surtshellir .—At a visit to the lava cavern, Surtshellir (Iceland), in June, 1892, the farthest recess, which contains ice stalactites and an ice pond, was found to be covered on walls and ceiling with ice crystals in the form of hollow hexagonal pyramids, analogous in shape to the well-known cubic crystals of rock salt. The hollow ice pyramids were, roughly speaking, built in the proportion of base 1 to height 2, and ranged up to about 1 in. diameter of base. They were attached to the wall by their apices, turning their hollow bases towards the interior of the cave. They were only found on those parts where stalactites did not occur. The temperature was +0.5° C. (+33° F.), and, as the cave forms a cul-de-sac , the air is perfectly calm. The crystals, having thus evidentia been formed from the moisture of the atmosphere, had to be considered as a kind of hour frost. |
format |
Article in Journal/Newspaper |
title |
V. On hollow pyramidal ice crystals |
spellingShingle |
V. On hollow pyramidal ice crystals |
title_short |
V. On hollow pyramidal ice crystals |
title_full |
V. On hollow pyramidal ice crystals |
title_fullStr |
V. On hollow pyramidal ice crystals |
title_full_unstemmed |
V. On hollow pyramidal ice crystals |
title_sort |
v. on hollow pyramidal ice crystals |
publisher |
The Royal Society |
publishDate |
1894 |
url |
http://dx.doi.org/10.1098/rspl.1894.0020 https://royalsocietypublishing.org/doi/pdf/10.1098/rspl.1894.0020 |
long_lat |
ENVELOPE(-61.516,-61.516,-64.500,-64.500) |
geographic |
Recess |
geographic_facet |
Recess |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
Proceedings of the Royal Society of London volume 55, issue 331-335, page 113-115 ISSN 0370-1662 2053-9126 |
op_rights |
https://royalsociety.org/journals/ethics-policies/data-sharing-mining/ |
op_doi |
https://doi.org/10.1098/rspl.1894.0020 |
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Proceedings of the Royal Society of London |
container_volume |
55 |
container_issue |
331-335 |
container_start_page |
113 |
op_container_end_page |
115 |
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1800754961451057152 |