TY - JOUR
T1 - A consistent global approach for the morphometric characterization of subaqueous landslides
AU - Clare, Michael
AU - Chaytor, Jason
AU - Dabson, Oliver
AU - Gamboa, Davide
AU - Georgiopoulou, Aggeliki
AU - Eady, Harry
AU - Hunt, James
AU - Jackson, Christopher
AU - Katz, Oded
AU - Krastel, Sebastian
AU - León, Ricardo
AU - Micallef, Aaron
AU - Moernaut, Jasper
AU - Moriconi, Roberto
AU - Moscardelli, Lorena
AU - Mueller, Christof
AU - Normandeau, Alexandre
AU - Patacci, Marco
AU - Steventon, Michael
AU - Urlaub, Morelia
AU - Völker, David
AU - Wood, Lesli
AU - Jobe, Zane
N1 - This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/3.0/).
PY - 2018/3/28
Y1 - 2018/3/28
N2 - Landslides are common in aquatic settings worldwide, from lakes and coastal environments to the deep sea. Fast-moving, large-volume landslides can potentially trigger destructive tsunamis. Landslides damage and disrupt global communication links and other critical marine infrastructure. Landslide deposits act as foci for localized, but important, deep-seafloor biological communities. Under burial, landslide deposits play an important role in a successful petroleum system. While the broad importance of understanding subaqueous landslide processes is evident, a number of important scientific questions have yet to receive the needed attention. Collecting quantitative data is a critical step to addressing questions surrounding subaqueous landslides. Quantitative metrics of subaqueous landslides are routinely recorded, but which ones, and how they are defined, depends on the end-user focus. Differences in focus can inhibit communication of knowledge between communities, and complicate comparative analysis. This study outlines an approach specifically for consistent measurement of subaqueous landslide morphometrics to be used in the design of a broader, global open-source, peer-curated database. Examples from different settings illustrate how the approach can be applied, as well as the difficulties encountered when analysing different landslides and data types. Standardizing data collection for subaqueous landslides should result in more accurate geohazard predictions and resource estimation.
AB - Landslides are common in aquatic settings worldwide, from lakes and coastal environments to the deep sea. Fast-moving, large-volume landslides can potentially trigger destructive tsunamis. Landslides damage and disrupt global communication links and other critical marine infrastructure. Landslide deposits act as foci for localized, but important, deep-seafloor biological communities. Under burial, landslide deposits play an important role in a successful petroleum system. While the broad importance of understanding subaqueous landslide processes is evident, a number of important scientific questions have yet to receive the needed attention. Collecting quantitative data is a critical step to addressing questions surrounding subaqueous landslides. Quantitative metrics of subaqueous landslides are routinely recorded, but which ones, and how they are defined, depends on the end-user focus. Differences in focus can inhibit communication of knowledge between communities, and complicate comparative analysis. This study outlines an approach specifically for consistent measurement of subaqueous landslide morphometrics to be used in the design of a broader, global open-source, peer-curated database. Examples from different settings illustrate how the approach can be applied, as well as the difficulties encountered when analysing different landslides and data types. Standardizing data collection for subaqueous landslides should result in more accurate geohazard predictions and resource estimation.
UR - http://www.scopus.com/inward/record.url?scp=85076671865&partnerID=8YFLogxK
U2 - 10.1144/SP477.15
DO - 10.1144/SP477.15
M3 - Article
AN - SCOPUS:85076671865
SN - 0305-8719
VL - 477
SP - 455
EP - 477
JO - Geological Society Special Publication
JF - Geological Society Special Publication
IS - 1
ER -