Finger rafting: a generic instability of floating elastic sheets.

Colliding ice floes are often observed to form a series of interlocking fingers. We show that this striking phenomenon is not a result of some peculiar property of ice but rather a general and robust mechanical phenomenon reproducible in the laboratory with other floating materials. We determine the...

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Main Authors: Vella, D, Wettlaufer, J
Format: Journal article
Language:English
Published: 2007
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author Vella, D
Wettlaufer, J
author_facet Vella, D
Wettlaufer, J
author_sort Vella, D
collection OXFORD
description Colliding ice floes are often observed to form a series of interlocking fingers. We show that this striking phenomenon is not a result of some peculiar property of ice but rather a general and robust mechanical phenomenon reproducible in the laboratory with other floating materials. We determine the theoretical relationship between the width of the resulting fingers and the material's mechanical properties and present experimental results along with field observations to support the theory. The generality of this "finger rafting" suggests that analogous processes may be responsible for creating the large-scale structures observed at the boundaries between Earth's convergent tectonic plates.
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spelling oxford-uuid:96abc48e-f9ab-441f-92ed-243152aee25a2022-03-26T23:54:41ZFinger rafting: a generic instability of floating elastic sheets.Journal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:96abc48e-f9ab-441f-92ed-243152aee25aEnglishSymplectic Elements at Oxford2007Vella, DWettlaufer, JColliding ice floes are often observed to form a series of interlocking fingers. We show that this striking phenomenon is not a result of some peculiar property of ice but rather a general and robust mechanical phenomenon reproducible in the laboratory with other floating materials. We determine the theoretical relationship between the width of the resulting fingers and the material's mechanical properties and present experimental results along with field observations to support the theory. The generality of this "finger rafting" suggests that analogous processes may be responsible for creating the large-scale structures observed at the boundaries between Earth's convergent tectonic plates.
spellingShingle Vella, D
Wettlaufer, J
Finger rafting: a generic instability of floating elastic sheets.
title Finger rafting: a generic instability of floating elastic sheets.
title_full Finger rafting: a generic instability of floating elastic sheets.
title_fullStr Finger rafting: a generic instability of floating elastic sheets.
title_full_unstemmed Finger rafting: a generic instability of floating elastic sheets.
title_short Finger rafting: a generic instability of floating elastic sheets.
title_sort finger rafting a generic instability of floating elastic sheets
work_keys_str_mv AT vellad fingerraftingagenericinstabilityoffloatingelasticsheets
AT wettlauferj fingerraftingagenericinstabilityoffloatingelasticsheets