The role of vegetation cover and slope angle in tephra layer preservation and implications for Quaternary tephrostratigraphy ...

Our aim is to understand the significance of slope position, slope angle and the interplay between slopes and vegetation in influencing the ways in which tephra layers may be preserved, thickened or thinned within the Quaternary stratigraphic record. This matters because tephra layers are used to re...

Full description

Bibliographic Details
Main Authors: Dugmore, AJ, Streeter, RT, Cutler, NA
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2018
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.18677
https://www.repository.cam.ac.uk/handle/1810/271689
id ftdatacite:10.17863/cam.18677
record_format openpolar
spelling ftdatacite:10.17863/cam.18677 2024-02-27T08:40:19+00:00 The role of vegetation cover and slope angle in tephra layer preservation and implications for Quaternary tephrostratigraphy ... Dugmore, AJ Streeter, RT Cutler, NA 2018 https://dx.doi.org/10.17863/cam.18677 https://www.repository.cam.ac.uk/handle/1810/271689 en eng Elsevier open.access Creative Commons Attribution Non Commercial No Derivatives 4.0 International Creative Commons Attribution Non Commercial No Derivatives 4.0 International Attribution-NonCommercial-NoDerivatives 4.0 International Attribution-NonCommercial-NoDerivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 http://purl.org/coar/access_right/c_abf2 Grímsvötn Eyjafjallajökull Mount St Helens biocrust isopach maps fallout volumes article-journal ScholarlyArticle JournalArticle Article 2018 ftdatacite https://doi.org/10.17863/cam.18677 2024-02-01T14:55:16Z Our aim is to understand the significance of slope position, slope angle and the interplay between slopes and vegetation in influencing the ways in which tephra layers may be preserved, thickened or thinned within the Quaternary stratigraphic record. This matters because tephra layers are used to reconstruct volumes of past volcanic eruptions and assess both past and future risks, hazards and impacts. This study uses modern data to better understand the formation of the palaeoenvironmental record and evaluates a data set of > 5,500 tephra layer thickness measurements across a range of slopes and vegetation types in Iceland and Washington State, USA. We measured tephra layers formed in October 1918, March 1947, May 1980, April 2010 and May 2011 across moderate slopes (< 35-37 °). Holding vegetation communities constant, location on slope had no systematic impact on mean tephra layer thickness. Holding slopes constant (< 5 °), we observed systematic modifications of initial fallout thickness in areas ... Article in Journal/Newspaper Eyjafjallajökull Iceland DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Grímsvötn
Eyjafjallajökull
Mount St Helens
biocrust
isopach maps
fallout volumes
spellingShingle Grímsvötn
Eyjafjallajökull
Mount St Helens
biocrust
isopach maps
fallout volumes
Dugmore, AJ
Streeter, RT
Cutler, NA
The role of vegetation cover and slope angle in tephra layer preservation and implications for Quaternary tephrostratigraphy ...
topic_facet Grímsvötn
Eyjafjallajökull
Mount St Helens
biocrust
isopach maps
fallout volumes
description Our aim is to understand the significance of slope position, slope angle and the interplay between slopes and vegetation in influencing the ways in which tephra layers may be preserved, thickened or thinned within the Quaternary stratigraphic record. This matters because tephra layers are used to reconstruct volumes of past volcanic eruptions and assess both past and future risks, hazards and impacts. This study uses modern data to better understand the formation of the palaeoenvironmental record and evaluates a data set of > 5,500 tephra layer thickness measurements across a range of slopes and vegetation types in Iceland and Washington State, USA. We measured tephra layers formed in October 1918, March 1947, May 1980, April 2010 and May 2011 across moderate slopes (< 35-37 °). Holding vegetation communities constant, location on slope had no systematic impact on mean tephra layer thickness. Holding slopes constant (< 5 °), we observed systematic modifications of initial fallout thickness in areas ...
format Article in Journal/Newspaper
author Dugmore, AJ
Streeter, RT
Cutler, NA
author_facet Dugmore, AJ
Streeter, RT
Cutler, NA
author_sort Dugmore, AJ
title The role of vegetation cover and slope angle in tephra layer preservation and implications for Quaternary tephrostratigraphy ...
title_short The role of vegetation cover and slope angle in tephra layer preservation and implications for Quaternary tephrostratigraphy ...
title_full The role of vegetation cover and slope angle in tephra layer preservation and implications for Quaternary tephrostratigraphy ...
title_fullStr The role of vegetation cover and slope angle in tephra layer preservation and implications for Quaternary tephrostratigraphy ...
title_full_unstemmed The role of vegetation cover and slope angle in tephra layer preservation and implications for Quaternary tephrostratigraphy ...
title_sort role of vegetation cover and slope angle in tephra layer preservation and implications for quaternary tephrostratigraphy ...
publisher Elsevier
publishDate 2018
url https://dx.doi.org/10.17863/cam.18677
https://www.repository.cam.ac.uk/handle/1810/271689
genre Eyjafjallajökull
Iceland
genre_facet Eyjafjallajökull
Iceland
op_rights open.access
Creative Commons Attribution Non Commercial No Derivatives 4.0 International
Creative Commons Attribution Non Commercial No Derivatives 4.0 International
Attribution-NonCommercial-NoDerivatives 4.0 International
Attribution-NonCommercial-NoDerivatives 4.0 International
https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode
cc-by-nc-nd-4.0
https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode
cc-by-nc-nd-4.0
http://purl.org/coar/access_right/c_abf2
op_doi https://doi.org/10.17863/cam.18677
_version_ 1792047421670293504