Field
Value
Language
dc.contributor.author
Kusack, Kyle
datacite.creator.affiliationIdentifier
https://ror.org/0213rcc28
en_US
datacite.creator.affiliation
Simon Fraser University
en_US
datacite.creator.nameIdentifier
en_US
dc.contributor.author
Li, Tingan
datacite.creator.affiliationIdentifier
https://ror.org/0213rcc28
en_US
datacite.creator.affiliation
Simon Fraser University
en_US
datacite.creator.nameIdentifier
https://orcid.org/0000-0002-6006-7712
en_US
dc.contributor.author
Venditti, Jeremy
datacite.creator.affiliationIdentifier
https://ror.org/0213rcc28
en_US
datacite.creator.affiliation
Simon Fraser University
en_US
datacite.creator.nameIdentifier
https://orcid.org/0000-0002-2876-4251
en_US
dc.coverage.temporal
2020-09-01/2023-05-01
dc.date.accessioned
2023-05-30T15:41:53Z
dc.date.available
2023-06-29T06:00:00Z
dc.date.issued
2023-06-29
dc.identifier.uri
https://www.frdr-dfdr.ca/repo/dataset/e06be893-4db7-42ad-b75d-d9cbb37d2f25
dc.identifier.uri
https://doi.org/10.20383/102.0746
dc.description
Data used in experiments on constriction-pool-widening channel Morphology in Bedrock Canyons, including the morphology and flow in Black Canyon and Kelly Creek Canyon, the water and bed surface data, the morphology with and without gravel data, the cross-sectional morphology data, and erosion rate in our experiment. Bedrock canyons often exhibit a series of constriction-pool-widening morphology (CPW) that consists of a lateral constriction, a deeply scour pool formed downstream of the constriction, a channel widening at or near the pool exit. To explore how the CPWs are formed in bedrock canyons, we conducted an experiment in a flume channel with a forced lateral constriction at the canyon entrance. This dataset includes the CPWs observed in two natural bedrock canyons, Black Canyon and Kelly Creek Canyon, in British Columbia, and the CPWs formed in the flume experiments. The morphological data, water surface and bed surface data, and the erosion rate data (Excel files) can be found in the folder of Data for Figures. We presented the evolution of the three dimensional CPWs over time in the folder of Agisoft that can be viewed in the Agisoft software, and the evolution of the bed morphology with and without gravel cover over time in the folder of CloudCompare that can be viewed in the CloudCompare software. Using this dataset, our experiments show that a primary CPW can be formed by an initial lateral constriction, and more CPWs can be self-formed further downstream due to the lateral constriction formed at the downstream end of the primary CPW.
en_US
dc.publisher
Federated Research Data Repository / dépôt fédéré de données de recherche
dc.rights
Creative Commons Attribution 4.0 International (CC BY 4.0)
en_US
dc.rights.uri
https://creativecommons.org/licenses/by/4.0/
en_US
dc.subject
Bedrock Canyons
en_US
dc.subject
River Morphology
en_US
dc.subject
Bedrock Erosion
en_US
dc.subject
Flume Experiment
en_US
dc.title
Data for Experiments on Constriction-Pool-Widening Channel Morphology in Bedrock Canyons
en_US
globus.shared_endpoint.name
9e1bf1ee-8284-4f05-adf3-9ccd3cf24ca3
globus.shared_endpoint.path
/8/published/publication_741/
datacite.publicationyear
2023
datacite.contributor.DataCollector
Kyle Kusack
datacite.date.Collected
2021-09-01/2022-02-01
datacite.resourcetype
Dataset
en_US
datacite.geolocation.geolocationPoint
49.275700 -122.916737
datacite.geolocation.geolocationPlace
-;Burnaby;British Columbia;Canada
datacite.fundingReference.funderIdentifier
https://ror.org/01h531d29
en_US
datacite.fundingReference.funderName
Natural Sciences and Engineering Research Council of Canada
en_US
datacite.fundingReference.awardNumber
en_US
datacite.fundingReference.awardTitle
en_US
frdr.crdc.code
RDF1050601
en_US
frdr.crdc.group_en
Earth and related environmental sciences
en_US
frdr.crdc.class_en
Environmental geoscience
en_US
frdr.crdc.field_en
Geomorphology
en_US
frdr.crdc.group_fr
Sciences de la Terre et sciences de l'environnement connexes
fr_CA
frdr.crdc.class_fr
Géosciences de l'environnement
fr_CA
frdr.crdc.field_fr
Géomorphologie
fr_CA
datacite.description.other
Item exited embargo and became publicly available on 2023-06-29
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