{"id":{"repo_id":"vt","oai_identifier":"oai:vtechworks.lib.vt.edu:10919/64022"},"canonical_url":"https://search.dev.ndltd.org/etd/vt/oai:vtechworks.lib.vt.edu:10919/64022","repository":{"repo_id":"vt","name":"Virginia Tech","base_url":"https://vtechworks.lib.vt.edu/oai/request"},"display":{"title":"Marine offshore to alluvial plain transitions within the \"Chemung\"-Hampshire interval (Upper Devonian) of the southern central Appalachians","abstract":"The Upper Devonian \"Chemung\" and Hampshire Formations of the southern Central Appalachian basin constitute the upper strata of an eastward thickening wedge of elastic sediment. The sediments comprising the \"Chemung\" and Hampshire, deposited on a low-gradient marine shelf and alluvial plain, respectively, are syn- to post-orogenic (Acadian), and were derived from the erosion of the Acadian Mountains to the east. Facies of the \"Chemung\" indicate deposition within three major, laterally adjacent environments. The predominating facies assemblage constitutes upward-coarsening sequences interpreted as offshore to upper shoreface progradational successions. The sequences are storm- and wave-dominated and pass upward into storm- and wave-dominated shoal water delta facies or into low-energy subtidal to supratidal mudflat facies. The absence of beaches and tidal channels is indicative not only of low tidal ranges, but also of seaward dissipation of wave-energy within a very shallow intracratonic foreland basin. The easternmost sections of the Hampshire Formation are comprised of fluvial cycles interpreted as high-energy sheetflood deposits.This style of sedimentation developed in closest proximity to the source. The Hampshire of more western sections is constructed predominantly of cycles interpreted as low-sinuosity braided stream deposits with a lesser abundance of cycles deposited by high-sinuosity meandering streams and high-energy sheetfloods. Low depositional slopes were associated with the alluvial plain. Braiding, however, was probably due to high runoff associated with high rainfall in a tropical climate and inadequate floodplain stabilization by vegetation, resulting in periodic high discharge.","abstract_html":"The Upper Devonian "Chemung" and Hampshire Formations of the southern Central Appalachian basin constitute the upper strata of an eastward thickening wedge of elastic sediment. The sediments comprising the "Chemung" and Hampshire, deposited on a low-gradient marine shelf and alluvial plain, respectively, are syn- to post-orogenic (Acadian), and were derived from the erosion of the Acadian Mountains to the east. Facies of the "Chemung" indicate deposition within three major, laterally adjacent environments. The predominating facies assemblage constitutes upward-coarsening sequences interpreted as offshore to upper shoreface progradational successions. The sequences are storm- and wave-dominated and pass upward into storm- and wave-dominated shoal water delta facies or into low-energy subtidal to supratidal mudflat facies. The absence of beaches and tidal channels is indicative not only of low tidal ranges, but also of seaward dissipation of wave-energy within a very shallow intracratonic foreland basin. The easternmost sections of the Hampshire Formation are comprised of fluvial cycles interpreted as high-energy sheetflood deposits.This style of sedimentation developed in closest proximity to the source. The Hampshire of more western sections is constructed predominantly of cycles interpreted as low-sinuosity braided stream deposits with a lesser abundance of cycles deposited by high-sinuosity meandering streams and high-energy sheetfloods. Low depositional slopes were associated with the alluvial plain. Braiding, however, was probably due to high runoff associated with high rainfall in a tropical climate and inadequate floodplain stabilization by vegetation, resulting in periodic high discharge.","abstract_has_math":false,"creators":["McClung, Wilson S."],"institution":"Virginia Polytechnic Institute and State University","degree_name":"Master of Science","degree_level":"masters","degree_discipline":"Geological Sciences","degree_department":"Geological Sciences","school":null,"contributors":[],"advisors":[],"committee_chairs":[],"committee_members":[],"year":1983,"date_issued":"1983","date_published":"1983","updated_at":"2026-07-22T22:19:26Z","subjects":[],"languages":["en_US"],"rights":["In Copyright"],"rights_urls":["http://rightsstatements.org/vocab/InC/1.0/"],"identifier_entries":[]},"links":{"outbound_url":"http://hdl.handle.net/10919/64022","outbound_label":"Handle","outbound_source":"dc:identifier.uri"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor.department","label":"Department","values":["Geological Sciences"]},{"key":"dc:creator","label":"Author","values":["McClung, Wilson S."]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date.accessioned","label":"Dc Date Accessioned","values":["2015-11-13T19:06:47Z"]},{"key":"dc:date.available","label":"Dc Date Available","values":["2015-11-13T19:06:47Z"]},{"key":"dc:date.issued","label":"Date","values":["1983"]},{"key":"dc:publisher","label":"Institution","values":["Virginia Polytechnic Institute and State University"]},{"key":"dc:type","label":"Dc Type","values":["Thesis"]},{"key":"dc:type.dcmitype","label":"Dc Type Dcmitype","values":["Text"]},{"key":"thesis:degree_discipline","label":"Discipline","values":["Geological Sciences"]},{"key":"thesis:degree_level","label":"Degree Level","values":["masters"]},{"key":"thesis:degree_name","label":"Degree Name","values":["Master of Science"]},{"key":"thesis:institution_name","label":"Thesis Institution Name","values":["Virginia Polytechnic Institute and State University"]}]},{"id":"language_rights","label":"Language and Rights","entries":[{"key":"dc:language.iso","label":"Language (ISO)","values":["en_US"]},{"key":"dc:rights","label":"Dc Rights","values":["In Copyright"]},{"key":"dc:rights.uri","label":"Rights URI","values":["http://rightsstatements.org/vocab/InC/1.0/"]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier.uri","label":"Identifier URI","values":["http://hdl.handle.net/10919/64022"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description.abstract","label":"Abstract","values":["The Upper Devonian \"Chemung\" and Hampshire Formations of the southern Central Appalachian basin constitute the upper strata of an eastward thickening wedge of elastic sediment. The sediments comprising the \"Chemung\" and Hampshire, deposited on a low-gradient marine shelf and alluvial plain, respectively, are syn- to post-orogenic (Acadian), and were derived from the erosion of the Acadian Mountains to the east. Facies of the \"Chemung\" indicate deposition within three major, laterally adjacent environments. The predominating facies assemblage constitutes upward-coarsening sequences interpreted as offshore to upper shoreface progradational successions. The sequences are storm- and wave-dominated and pass upward into storm- and wave-dominated shoal water delta facies or into low-energy subtidal to supratidal mudflat facies. The absence of beaches and tidal channels is indicative not only of low tidal ranges, but also of seaward dissipation of wave-energy within a very shallow intracratonic foreland basin. The easternmost sections of the Hampshire Formation are comprised of fluvial cycles interpreted as high-energy sheetflood deposits.This style of sedimentation developed in closest proximity to the source. The Hampshire of more western sections is constructed predominantly of cycles interpreted as low-sinuosity braided stream deposits with a lesser abundance of cycles deposited by high-sinuosity meandering streams and high-energy sheetfloods. Low depositional slopes were associated with the alluvial plain. Braiding, however, was probably due to high runoff associated with high rainfall in a tropical climate and inadequate floodplain stabilization by vegetation, resulting in periodic high discharge."]},{"key":"dc:description.degree","label":"Dc Description Degree","values":["Master of Science"]},{"key":"dc:format.mimetype","label":"Dc Format Mimetype","values":["application/pdf"]},{"key":"dc:title","label":"Title","values":["Marine offshore to alluvial plain transitions within the \"Chemung\"-Hampshire interval (Upper Devonian) of the southern central Appalachians"]}]}],"canonical_facts":{"dc:contributor.department":["Geological Sciences"],"dc:creator":["McClung, Wilson S."],"dc:date.accessioned":["2015-11-13T19:06:47Z"],"dc:date.available":["2015-11-13T19:06:47Z"],"dc:date.issued":["1983"],"dc:description.abstract":["The Upper Devonian \"Chemung\" and Hampshire Formations of the southern Central Appalachian basin constitute the upper strata of an eastward thickening wedge of elastic sediment. The sediments comprising the \"Chemung\" and Hampshire, deposited on a low-gradient marine shelf and alluvial plain, respectively, are syn- to post-orogenic (Acadian), and were derived from the erosion of the Acadian Mountains to the east. Facies of the \"Chemung\" indicate deposition within three major, laterally adjacent environments. The predominating facies assemblage constitutes upward-coarsening sequences interpreted as offshore to upper shoreface progradational successions. The sequences are storm- and wave-dominated and pass upward into storm- and wave-dominated shoal water delta facies or into low-energy subtidal to supratidal mudflat facies. The absence of beaches and tidal channels is indicative not only of low tidal ranges, but also of seaward dissipation of wave-energy within a very shallow intracratonic foreland basin. The easternmost sections of the Hampshire Formation are comprised of fluvial cycles interpreted as high-energy sheetflood deposits.This style of sedimentation developed in closest proximity to the source. The Hampshire of more western sections is constructed predominantly of cycles interpreted as low-sinuosity braided stream deposits with a lesser abundance of cycles deposited by high-sinuosity meandering streams and high-energy sheetfloods. Low depositional slopes were associated with the alluvial plain. Braiding, however, was probably due to high runoff associated with high rainfall in a tropical climate and inadequate floodplain stabilization by vegetation, resulting in periodic high discharge."],"dc:description.degree":["Master of Science"],"dc:format.mimetype":["application/pdf"],"dc:identifier.uri":["http://hdl.handle.net/10919/64022"],"dc:language.iso":["en_US"],"dc:publisher":["Virginia Polytechnic Institute and State University"],"dc:rights":["In Copyright"],"dc:rights.uri":["http://rightsstatements.org/vocab/InC/1.0/"],"dc:title":["Marine offshore to alluvial plain transitions within the \"Chemung\"-Hampshire interval (Upper Devonian) of the southern central Appalachians"],"dc:type":["Thesis"],"dc:type.dcmitype":["Text"],"thesis:degree_discipline":["Geological Sciences"],"thesis:degree_level":["masters"],"thesis:degree_name":["Master of Science"],"thesis:institution_name":["Virginia Polytechnic Institute and State University"]},"updated_at":"2026-07-22T22:19:26Z"}