Tracking rapid landscape change with repeated photography, Gros Morne National Park, Canada

At various coastal and inland sites in and around Gros Morne National Park in western Newfoundland, photographs taken periodically over many decades illustrate the physical stability of landforms. ἀese images provide a convenient, qualitative way to track the development of stone rings and patterned...

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Published in:Atlantic Geology
Main Author: Berger, Antony
Format: Article in Journal/Newspaper
Language:English
Published: Atlantic Geoscience Society 2017
Subjects:
Online Access:https://journals.lib.unb.ca/index.php/ag/article/view/24471
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spelling ftuninewbrunojs:oai:ojs.journals.lib.unb.ca:article/24471 2023-05-15T16:31:53+02:00 Tracking rapid landscape change with repeated photography, Gros Morne National Park, Canada Berger, Antony 2017-03-29 text/html application/pdf https://journals.lib.unb.ca/index.php/ag/article/view/24471 eng eng Atlantic Geoscience Society https://journals.lib.unb.ca/index.php/ag/article/view/24471/29613 https://journals.lib.unb.ca/index.php/ag/article/view/24471/29569 https://journals.lib.unb.ca/index.php/ag/article/view/24471 Copyright (c) 2017 Atlantic Geology Atlantic Geoscience; Vol. 53 (2017); 115 - 126 2564-2987 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 2017 ftuninewbrunojs 2022-07-11T11:42:13Z At various coastal and inland sites in and around Gros Morne National Park in western Newfoundland, photographs taken periodically over many decades illustrate the physical stability of landforms. ἀese images provide a convenient, qualitative way to track the development of stone rings and patterned ground, the movement of rocks along intertidal platforms, changes to marine estuaries and to alluvial rivers and fans, temporal trends in late-lying snow beds along mountain tops, and slope failure by landslides and rock falls. ἀis study has established a spatial and temporal photographic record of slope failures along the steep cliḀs of Western Brook Pond, showing that nearly all of the sites identiᴀed in earlier studies as high risk of failure have remained stable. In contrast, thin-skinned landslides along Winter House Brook have remained active for at least 100 years. Little evidence of physical changes in patterned ground features in Trout River Gulch was found, other than frost-heaving in soils disturbed by road construction. Fluctuations from year to year in the level of gravel beaches along parts of the coast are common, and blow-outs continue to modify coastal sand dunes. Apart from certain engineered sites where change was obviously driven by direct human activities, the immediate cause or “driver” of change was natural (non-human), the result of gravitational instability, heavy precipitation, wave and storm action, frost heaving, and other background processes of the sort that long pre-date the coming of people to the region. Continuation of this kind of inexpensive, non-invasive monitoring can assist in assessing ecological integrity, managing public safety, and interpreting landscape processes for Park visitors. Article in Journal/Newspaper Gros Morne National Park Newfoundland University of New Brunswick: Centre for Digital Scholarship Journals Canada Gulch ENVELOPE(-61.483,-61.483,-63.997,-63.997) Gros Morne National Park ENVELOPE(-57.531,-57.531,49.613,49.613) Western Brook ENVELOPE(-57.865,-57.865,49.833,49.833) Western Brook Pond ENVELOPE(-57.815,-57.815,49.767,49.767) Atlantic Geology 53 115 126
institution Open Polar
collection University of New Brunswick: Centre for Digital Scholarship Journals
op_collection_id ftuninewbrunojs
language English
description At various coastal and inland sites in and around Gros Morne National Park in western Newfoundland, photographs taken periodically over many decades illustrate the physical stability of landforms. ἀese images provide a convenient, qualitative way to track the development of stone rings and patterned ground, the movement of rocks along intertidal platforms, changes to marine estuaries and to alluvial rivers and fans, temporal trends in late-lying snow beds along mountain tops, and slope failure by landslides and rock falls. ἀis study has established a spatial and temporal photographic record of slope failures along the steep cliḀs of Western Brook Pond, showing that nearly all of the sites identiᴀed in earlier studies as high risk of failure have remained stable. In contrast, thin-skinned landslides along Winter House Brook have remained active for at least 100 years. Little evidence of physical changes in patterned ground features in Trout River Gulch was found, other than frost-heaving in soils disturbed by road construction. Fluctuations from year to year in the level of gravel beaches along parts of the coast are common, and blow-outs continue to modify coastal sand dunes. Apart from certain engineered sites where change was obviously driven by direct human activities, the immediate cause or “driver” of change was natural (non-human), the result of gravitational instability, heavy precipitation, wave and storm action, frost heaving, and other background processes of the sort that long pre-date the coming of people to the region. Continuation of this kind of inexpensive, non-invasive monitoring can assist in assessing ecological integrity, managing public safety, and interpreting landscape processes for Park visitors.
format Article in Journal/Newspaper
author Berger, Antony
spellingShingle Berger, Antony
Tracking rapid landscape change with repeated photography, Gros Morne National Park, Canada
author_facet Berger, Antony
author_sort Berger, Antony
title Tracking rapid landscape change with repeated photography, Gros Morne National Park, Canada
title_short Tracking rapid landscape change with repeated photography, Gros Morne National Park, Canada
title_full Tracking rapid landscape change with repeated photography, Gros Morne National Park, Canada
title_fullStr Tracking rapid landscape change with repeated photography, Gros Morne National Park, Canada
title_full_unstemmed Tracking rapid landscape change with repeated photography, Gros Morne National Park, Canada
title_sort tracking rapid landscape change with repeated photography, gros morne national park, canada
publisher Atlantic Geoscience Society
publishDate 2017
url https://journals.lib.unb.ca/index.php/ag/article/view/24471
long_lat ENVELOPE(-61.483,-61.483,-63.997,-63.997)
ENVELOPE(-57.531,-57.531,49.613,49.613)
ENVELOPE(-57.865,-57.865,49.833,49.833)
ENVELOPE(-57.815,-57.815,49.767,49.767)
geographic Canada
Gulch
Gros Morne National Park
Western Brook
Western Brook Pond
geographic_facet Canada
Gulch
Gros Morne National Park
Western Brook
Western Brook Pond
genre Gros Morne National Park
Newfoundland
genre_facet Gros Morne National Park
Newfoundland
op_source Atlantic Geoscience; Vol. 53 (2017); 115 - 126
2564-2987
op_relation https://journals.lib.unb.ca/index.php/ag/article/view/24471/29613
https://journals.lib.unb.ca/index.php/ag/article/view/24471/29569
https://journals.lib.unb.ca/index.php/ag/article/view/24471
op_rights Copyright (c) 2017 Atlantic Geology
container_title Atlantic Geology
container_volume 53
container_start_page 115
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