{"id":{"repo_id":"london-metro","oai_identifier":"oai:repository.londonmet.ac.uk:3069"},"canonical_url":"https://search.dev.ndltd.org/etd/london-metro/oai:repository.londonmet.ac.uk:3069","repository":{"repo_id":"london-metro","name":"London Metropolitan University","base_url":"https://repository.londonmet.ac.uk/cgi/oai2"},"display":{"title":"The stratigraphy and morphology of Pleistocene deposits in County Waterford (with special reference to the Ballyvoyle Till)","abstract":"The Ballyvoyle Till (Watts, 1959) was originally described by Wright and Muff (1904) as a boulder clay deposited by southerly-moving ice of Inland, northern origin. They regarded this advance as having post~dated one of Irish Sea origin along the south coast. While Watts (1959) considered that the two ice masses were broadly contemporaneous, Synge (1977) suggested that the glacigenic sequence predated the deposition of the underlying raised beach and was subsequently soliflucted downslope to Its present stratigraphic position overlying the raised beach unit.","abstract_html":"The Ballyvoyle Till (Watts, 1959) was originally described by Wright and Muff (1904) as a boulder clay deposited by southerly-moving ice of Inland, northern origin. They regarded this advance as having post~dated one of Irish Sea origin along the south coast. While Watts (1959) considered that the two ice masses were broadly contemporaneous, Synge (1977) suggested that the glacigenic sequence predated the deposition of the underlying raised beach and was subsequently soliflucted downslope to Its present stratigraphic position overlying the raised beach unit.","abstract_has_math":false,"creators":["Quinn, Irene M."],"institution":"Polytechnic of North London","degree_name":"phd","degree_level":"doctoral","degree_discipline":null,"degree_department":null,"school":null,"contributors":[],"advisors":[],"committee_chairs":[],"committee_members":[],"year":1987,"date_issued":"1987-12","date_published":"1987-12","updated_at":"2026-07-24T02:54:27Z","subjects":["550 - Earth Sciences"],"languages":[],"rights":[],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier.grantnumber","label":"Dc Identifier Grantnumber","values":["N/A"],"render_values":[{"text":"N/A","href":null,"code":true}]}]},"links":{"outbound_url":null,"outbound_label":null,"outbound_source":null},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor.sponsor","label":"Sponsor","values":["London Metropolitan University"]},{"key":"dc:creator","label":"Author","values":["Quinn, Irene M."]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["1987-12"]},{"key":"dc:date.issued","label":"Date","values":["1987-12"]},{"key":"dc:publisher.department","label":"Dc Publisher Department","values":["School of Human Sciences (SHSC)","Department of Geography"]},{"key":"dc:publisher.institution","label":"Dc Publisher Institution","values":["Polytechnic of North London"]},{"key":"dc:relation.isreferencedby","label":"Dc Relation Isreferencedby","values":["https://repository.londonmet.ac.uk/3069/"]},{"key":"dc:type","label":"Dc Type","values":["Thesis"]},{"key":"dc:type.qualificationlevel","label":"Dc Type Qualificationlevel","values":["doctoral"]},{"key":"dc:type.qualificationname","label":"Dc Type Qualificationname","values":["phd"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["550 - Earth Sciences"]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier.grantnumber","label":"Dc Identifier Grantnumber","values":["N/A"]},{"key":"dc:identifier.uri","label":"Identifier URI","values":["https://repository.londonmet.ac.uk/3069/1/380644.pdf"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description.abstract","label":"Abstract","values":["The Ballyvoyle Till (Watts, 1959) was originally described by Wright and Muff (1904) as a boulder clay deposited by southerly-moving ice of Inland, northern origin. They regarded this advance as having post~dated one of Irish Sea origin along the south coast. While Watts (1959) considered that the two ice masses were broadly contemporaneous, Synge (1977) suggested that the glacigenic sequence predated the deposition of the underlying raised beach and was subsequently soliflucted downslope to Its present stratigraphic position overlying the raised beach unit."]},{"key":"dc:format","label":"Dc Format","values":["text"]},{"key":"dc:title","label":"Title","values":["The stratigraphy and morphology of Pleistocene deposits in County Waterford (with special reference to the Ballyvoyle Till)"]}]}],"canonical_facts":{"dc:contributor.sponsor":["London Metropolitan University"],"dc:creator":["Quinn, Irene M."],"dc:date":["1987-12"],"dc:date.issued":["1987-12"],"dc:description.abstract":["The Ballyvoyle Till (Watts, 1959) was originally described by Wright and Muff (1904) as a boulder clay deposited by southerly-moving ice of Inland, northern origin. They regarded this advance as having post~dated one of Irish Sea origin along the south coast. While Watts (1959) considered that the two ice masses were broadly contemporaneous, Synge (1977) suggested that the glacigenic sequence predated the deposition of the underlying raised beach and was subsequently soliflucted downslope to Its present stratigraphic position overlying the raised beach unit."],"dc:format":["text"],"dc:identifier.grantnumber":["N/A"],"dc:identifier.uri":["https://repository.londonmet.ac.uk/3069/1/380644.pdf"],"dc:publisher.department":["School of Human Sciences (SHSC)","Department of Geography"],"dc:publisher.institution":["Polytechnic of North London"],"dc:relation.isreferencedby":["https://repository.londonmet.ac.uk/3069/"],"dc:subject":["550 - Earth Sciences"],"dc:title":["The stratigraphy and morphology of Pleistocene deposits in County Waterford (with special reference to the Ballyvoyle Till)"],"dc:type":["Thesis"],"dc:type.qualificationlevel":["doctoral"],"dc:type.qualificationname":["phd"]},"updated_at":"2026-07-24T02:54:27Z"}