Dynamic Geomorphology of the Drumlin Coast of Southeast Cape Breton Island

The southeastern coast of Cape Breton Island from Gabarus Bay to Framboise Cove has been investigated as a typical example of a drumlin coast. Landforms have been mapped from ground observations and air photographs. Time series of coastal profiles of both beaches and eroding drumlin cliffs have been...

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Published in:Atlantic Geology
Main Authors: Wang, Ying, Piper, D. J. W.
Format: Article in Journal/Newspaper
Language:English
Published: Atlantic Geoscience Society 1982
Subjects:
Online Access:https://journals.lib.unb.ca/index.php/ag/article/view/1385
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spelling ftuninewbrunojs:oai:ojs.journals.lib.unb.ca:article/1385 2023-05-15T15:46:44+02:00 Dynamic Geomorphology of the Drumlin Coast of Southeast Cape Breton Island Wang, Ying Piper, D. J. W. 1982-01-01 application/pdf https://journals.lib.unb.ca/index.php/ag/article/view/1385 eng eng Atlantic Geoscience Society https://journals.lib.unb.ca/index.php/ag/article/view/1385/1753 https://journals.lib.unb.ca/index.php/ag/article/view/1385 Copyright (c) 2015 Atlantic Geology Atlantic Geoscience; Vol. 18 No. 1 (1982) 2564-2987 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1982 ftuninewbrunojs 2022-07-11T11:41:14Z The southeastern coast of Cape Breton Island from Gabarus Bay to Framboise Cove has been investigated as a typical example of a drumlin coast. Landforms have been mapped from ground observations and air photographs. Time series of coastal profiles of both beaches and eroding drumlin cliffs have been measured. Nearshore sediment distribution has been mapped. An analysis has been made of wind and wave frequency and direction data. Four coastal segments are distinguished: (1) the south coast of Gabarus Bay has rock-cored drum-11ns separated by small barrier beaches; (2) the coast around Winging Point has a relatively stable depositional tombolo coast; (3) Fourchu Bay and Framboise Cove are developed in an area of thick till drumlins, and consist of barrier bars backed by lagoons and drumlins; and (4) the Fourchu Head and Red Cape are rocky coastlines from which all till has been removed by marine erosion, The geomorphologlcal evolution is a consequence of the initial drumlin landscape, the availability of a wide range of sediment sizes, and the type and intensity of marine erosion processes including the effects of transgression. Two types of coast are developed: a) in irregular hilly areas, where the till is thin and occurs in rock-cored drumlins; and b) in valley areas, where thick till drumlins are found. In each of these types, three stages of coastal development are distinguished. These represent the effect of differing rate of maturation, dependent on the configuration of drumlins and varying type and intensity of marine erosion. RÉSUMÉ Depuis la baie de Gabarua jusqu'à l'anse Framboise, la côte sud-est de l'ile du Cap-Breton a été étudiée en tant qu'exemple type d'une côte à drumlins. Les formes de relief ont été cartographies à partlr d'observations sur le terrain et de photographies aériennes. On a mesure à différents intervalles de temps, des séries de ... Article in Journal/Newspaper Breton Island University of New Brunswick: Centre for Digital Scholarship Journals Breton Island ENVELOPE(141.383,141.383,-66.800,-66.800) Atlantic Geology 18 1
institution Open Polar
collection University of New Brunswick: Centre for Digital Scholarship Journals
op_collection_id ftuninewbrunojs
language English
description The southeastern coast of Cape Breton Island from Gabarus Bay to Framboise Cove has been investigated as a typical example of a drumlin coast. Landforms have been mapped from ground observations and air photographs. Time series of coastal profiles of both beaches and eroding drumlin cliffs have been measured. Nearshore sediment distribution has been mapped. An analysis has been made of wind and wave frequency and direction data. Four coastal segments are distinguished: (1) the south coast of Gabarus Bay has rock-cored drum-11ns separated by small barrier beaches; (2) the coast around Winging Point has a relatively stable depositional tombolo coast; (3) Fourchu Bay and Framboise Cove are developed in an area of thick till drumlins, and consist of barrier bars backed by lagoons and drumlins; and (4) the Fourchu Head and Red Cape are rocky coastlines from which all till has been removed by marine erosion, The geomorphologlcal evolution is a consequence of the initial drumlin landscape, the availability of a wide range of sediment sizes, and the type and intensity of marine erosion processes including the effects of transgression. Two types of coast are developed: a) in irregular hilly areas, where the till is thin and occurs in rock-cored drumlins; and b) in valley areas, where thick till drumlins are found. In each of these types, three stages of coastal development are distinguished. These represent the effect of differing rate of maturation, dependent on the configuration of drumlins and varying type and intensity of marine erosion. RÉSUMÉ Depuis la baie de Gabarua jusqu'à l'anse Framboise, la côte sud-est de l'ile du Cap-Breton a été étudiée en tant qu'exemple type d'une côte à drumlins. Les formes de relief ont été cartographies à partlr d'observations sur le terrain et de photographies aériennes. On a mesure à différents intervalles de temps, des séries de ...
format Article in Journal/Newspaper
author Wang, Ying
Piper, D. J. W.
spellingShingle Wang, Ying
Piper, D. J. W.
Dynamic Geomorphology of the Drumlin Coast of Southeast Cape Breton Island
author_facet Wang, Ying
Piper, D. J. W.
author_sort Wang, Ying
title Dynamic Geomorphology of the Drumlin Coast of Southeast Cape Breton Island
title_short Dynamic Geomorphology of the Drumlin Coast of Southeast Cape Breton Island
title_full Dynamic Geomorphology of the Drumlin Coast of Southeast Cape Breton Island
title_fullStr Dynamic Geomorphology of the Drumlin Coast of Southeast Cape Breton Island
title_full_unstemmed Dynamic Geomorphology of the Drumlin Coast of Southeast Cape Breton Island
title_sort dynamic geomorphology of the drumlin coast of southeast cape breton island
publisher Atlantic Geoscience Society
publishDate 1982
url https://journals.lib.unb.ca/index.php/ag/article/view/1385
long_lat ENVELOPE(141.383,141.383,-66.800,-66.800)
geographic Breton Island
geographic_facet Breton Island
genre Breton Island
genre_facet Breton Island
op_source Atlantic Geoscience; Vol. 18 No. 1 (1982)
2564-2987
op_relation https://journals.lib.unb.ca/index.php/ag/article/view/1385/1753
https://journals.lib.unb.ca/index.php/ag/article/view/1385
op_rights Copyright (c) 2015 Atlantic Geology
container_title Atlantic Geology
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