Geologic - geotechnical characteristics and preservation proposals for the Historic Site and Monument n° 38, Nordenskjöld’s Hut, Antarctica

The historic site and monument n° 38, Nordenskjöld Hut, is located on Snow Hill Island, James Ross archipelago, Antarctica. This is a place of a great historic and heritage value because there are very few centennial buildings in Antarctica. This building was built in February 1902 as a refuge by th...

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Language:unknown
Published: 2017
Subjects:
Ice
Online Access:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_03660176_v128_n1_p207_SilvaBusso
https://hdl.handle.net/20.500.12110/paper_03660176_v128_n1_p207_SilvaBusso
id ftunibueairesbd:paper:paper_03660176_v128_n1_p207_SilvaBusso
record_format openpolar
spelling ftunibueairesbd:paper:paper_03660176_v128_n1_p207_SilvaBusso 2023-05-15T13:42:26+02:00 Geologic - geotechnical characteristics and preservation proposals for the Historic Site and Monument n° 38, Nordenskjöld’s Hut, Antarctica 2017 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_03660176_v128_n1_p207_SilvaBusso https://hdl.handle.net/20.500.12110/paper_03660176_v128_n1_p207_SilvaBusso unknown https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_03660176_v128_n1_p207_SilvaBusso http://hdl.handle.net/20.500.12110/paper_03660176_v128_n1_p207_SilvaBusso Antarctica Historic site and monument Nordenskjöld hut Permafrost Snow hill island climate effect embankment erosion heritage conservation historic building monument preservation warming James Ross Island West Antarctica 2017 ftunibueairesbd https://doi.org/20.500.12110/paper_03660176_v128_n1_p207_SilvaBusso 2023-02-16T01:56:29Z The historic site and monument n° 38, Nordenskjöld Hut, is located on Snow Hill Island, James Ross archipelago, Antarctica. This is a place of a great historic and heritage value because there are very few centennial buildings in Antarctica. This building was built in February 1902 as a refuge by the Swedish expedition directed by Otto Nordenskjöld, between 1901 and1904. The building is located over an embankment with ice-rich permafrost, which produces unstable conditions for the foundation. In the past anthropic factors accelerated this process, for example the use of the hut as refuge and garage for other field campaigns. Intensive and potentially destructive signs are observed as a consequence of the thermokarst and erosion active processes in the last decades, in relation with climate warming. Around the embankment the erosion processes are connected with underground icethaw occurring in the top of the permafrost. The embankment area contains 17-20% of underground ice and the mean active layer depth is 1.2 m. A potential maximum settlement of the embankment top surface between 0.15-0.25m has been estimated. The above mentioned processes are consequence of ice thaw in the permafrost table. This would modify the natural surface and could produce significant damages. This study analyzes contingency and mitigation strategies to prevent or reduce the rate of settlement and avoid altering the top of the embankment. The goal is to protect the slopes and foundation from surface erosion and thermo-erosion. We propose increasing the thickness of the embankment, making a frame on the shoulder of the embankment and carrying out a retaining wall or socket in the foundation. © 2017, Instituto Geologico y Minero de Espana. All rights reserved. Other/Unknown Material Antarc* Antarctica Ice James Ross Island Otto Nordenskjöld permafrost Ross Archipelago Ross Island Snow Hill Island Thermokarst West Antarctica Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires) Hill Island ENVELOPE(76.070,76.070,-69.395,-69.395) Nordenskjöld ENVELOPE(-60.583,-60.583,-64.667,-64.667) Ross Archipelago ENVELOPE(167.000,167.000,-77.500,-77.500) Ross Island Snow Hill ENVELOPE(-57.183,-57.183,-64.466,-64.466) Snow Hill Island ENVELOPE(-57.183,-57.183,-64.466,-64.466) West Antarctica
institution Open Polar
collection Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires)
op_collection_id ftunibueairesbd
language unknown
topic Antarctica
Historic site and monument
Nordenskjöld hut
Permafrost
Snow hill island
climate effect
embankment
erosion
heritage conservation
historic building
monument
preservation
warming
James Ross Island
West Antarctica
spellingShingle Antarctica
Historic site and monument
Nordenskjöld hut
Permafrost
Snow hill island
climate effect
embankment
erosion
heritage conservation
historic building
monument
preservation
warming
James Ross Island
West Antarctica
Geologic - geotechnical characteristics and preservation proposals for the Historic Site and Monument n° 38, Nordenskjöld’s Hut, Antarctica
topic_facet Antarctica
Historic site and monument
Nordenskjöld hut
Permafrost
Snow hill island
climate effect
embankment
erosion
heritage conservation
historic building
monument
preservation
warming
James Ross Island
West Antarctica
description The historic site and monument n° 38, Nordenskjöld Hut, is located on Snow Hill Island, James Ross archipelago, Antarctica. This is a place of a great historic and heritage value because there are very few centennial buildings in Antarctica. This building was built in February 1902 as a refuge by the Swedish expedition directed by Otto Nordenskjöld, between 1901 and1904. The building is located over an embankment with ice-rich permafrost, which produces unstable conditions for the foundation. In the past anthropic factors accelerated this process, for example the use of the hut as refuge and garage for other field campaigns. Intensive and potentially destructive signs are observed as a consequence of the thermokarst and erosion active processes in the last decades, in relation with climate warming. Around the embankment the erosion processes are connected with underground icethaw occurring in the top of the permafrost. The embankment area contains 17-20% of underground ice and the mean active layer depth is 1.2 m. A potential maximum settlement of the embankment top surface between 0.15-0.25m has been estimated. The above mentioned processes are consequence of ice thaw in the permafrost table. This would modify the natural surface and could produce significant damages. This study analyzes contingency and mitigation strategies to prevent or reduce the rate of settlement and avoid altering the top of the embankment. The goal is to protect the slopes and foundation from surface erosion and thermo-erosion. We propose increasing the thickness of the embankment, making a frame on the shoulder of the embankment and carrying out a retaining wall or socket in the foundation. © 2017, Instituto Geologico y Minero de Espana. All rights reserved.
title Geologic - geotechnical characteristics and preservation proposals for the Historic Site and Monument n° 38, Nordenskjöld’s Hut, Antarctica
title_short Geologic - geotechnical characteristics and preservation proposals for the Historic Site and Monument n° 38, Nordenskjöld’s Hut, Antarctica
title_full Geologic - geotechnical characteristics and preservation proposals for the Historic Site and Monument n° 38, Nordenskjöld’s Hut, Antarctica
title_fullStr Geologic - geotechnical characteristics and preservation proposals for the Historic Site and Monument n° 38, Nordenskjöld’s Hut, Antarctica
title_full_unstemmed Geologic - geotechnical characteristics and preservation proposals for the Historic Site and Monument n° 38, Nordenskjöld’s Hut, Antarctica
title_sort geologic - geotechnical characteristics and preservation proposals for the historic site and monument n° 38, nordenskjöld’s hut, antarctica
publishDate 2017
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_03660176_v128_n1_p207_SilvaBusso
https://hdl.handle.net/20.500.12110/paper_03660176_v128_n1_p207_SilvaBusso
long_lat ENVELOPE(76.070,76.070,-69.395,-69.395)
ENVELOPE(-60.583,-60.583,-64.667,-64.667)
ENVELOPE(167.000,167.000,-77.500,-77.500)
ENVELOPE(-57.183,-57.183,-64.466,-64.466)
ENVELOPE(-57.183,-57.183,-64.466,-64.466)
geographic Hill Island
Nordenskjöld
Ross Archipelago
Ross Island
Snow Hill
Snow Hill Island
West Antarctica
geographic_facet Hill Island
Nordenskjöld
Ross Archipelago
Ross Island
Snow Hill
Snow Hill Island
West Antarctica
genre Antarc*
Antarctica
Ice
James Ross Island
Otto Nordenskjöld
permafrost
Ross Archipelago
Ross Island
Snow Hill Island
Thermokarst
West Antarctica
genre_facet Antarc*
Antarctica
Ice
James Ross Island
Otto Nordenskjöld
permafrost
Ross Archipelago
Ross Island
Snow Hill Island
Thermokarst
West Antarctica
op_relation https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_03660176_v128_n1_p207_SilvaBusso
http://hdl.handle.net/20.500.12110/paper_03660176_v128_n1_p207_SilvaBusso
op_doi https://doi.org/20.500.12110/paper_03660176_v128_n1_p207_SilvaBusso
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