Surficial sands deposited in the Chesapeake Bay are a mixture of sands derived from the bay's shorelines, from offshore, and from relict deposits. Direct fluvial input is probably minor except from the James River, which may serve as a local source of sands in the Thimble Shoals area. Sands in the western half of the bay are primarily derived from the erosion of the adjacent shoreline. In contrast, the eastern half of the bay has two major sources of sand. Shoreline erosion is the dominant source north of the town of Eastville, Virginia, while the offshore is the major source south of this area.
Some surficial sands in the Chesapeake Bay are relict. Sands in the upper mid-bay channel are the result of reworked deposits from the Paleo-Susquehanna River. Preservation of this older material is probably the result of its location in the deeper portions of the bay, where depositional rates are low.
","abstract_html":"<p>Surficial sands deposited in the Chesapeake Bay are a mixture of sands derived from the bay's shorelines, from offshore, and from relict deposits. Direct fluvial input is probably minor except from the James River, which may serve as a local source of sands in the Thimble Shoals area. Sands in the western half of the bay are primarily derived from the erosion of the adjacent shoreline. In contrast, the eastern half of the bay has two major sources of sand. Shoreline erosion is the dominant source north of the town of Eastville, Virginia, while the offshore is the major source south of this area.</p> <p>Some surficial sands in the Chesapeake Bay are relict. Sands in the upper mid-bay channel are the result of reworked deposits from the Paleo-Susquehanna River. Preservation of this older material is probably the result of its location in the deeper portions of the bay, where depositional rates are low.</p>","abstract_has_math":false,"creators":["Council, Edward Augustus, III"],"institution":null,"degree_name":"Master of Science (MS)","degree_level":"Thesis","degree_discipline":"Ocean & Earth Sciences","degree_department":null,"school":null,"contributors":["Dennis A. Darby","Joseph H. Rule","Ronald E. Johnson","R. J. Bryne"],"advisors":[],"committee_chairs":[],"committee_members":[],"year":1987,"date_issued":"1987-04-01T08:00:00Z","date_published":"1987-04-01T08:00:00Z","updated_at":"2026-07-24T03:35:08Z","subjects":["Sand","Sedimentation analysis","Chesapeake Bay","Deposits","Geology"],"languages":[],"rights":["In Copyright. URI: http://rightsstatements.org/vocab/InC/1.0/ This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).
"],"rights_urls":[],"identifier_entries":[]},"links":{"outbound_url":"https://digitalcommons.odu.edu/oeas_etds/105","outbound_label":"Repository record","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor","label":"Contributor","values":["Dennis A. Darby","Joseph H. Rule","Ronald E. Johnson","R. J. Bryne"]},{"key":"dc:creator","label":"Author","values":["Council, Edward Augustus, III"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date.available","label":"Dc Date Available","values":["2019-09-13T07:00:00Z"]},{"key":"thesis:degree_discipline","label":"Discipline","values":["Ocean & Earth Sciences"]},{"key":"thesis:degree_level","label":"Degree Level","values":["Thesis"]},{"key":"thesis:degree_name","label":"Degree Name","values":["Master of Science (MS)"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["Sand","Sedimentation analysis","Chesapeake Bay","Deposits","Geology"]}]},{"id":"language_rights","label":"Language and Rights","entries":[{"key":"dc:rights","label":"Dc Rights","values":["In Copyright. URI: http://rightsstatements.org/vocab/InC/1.0/ This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).
"]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier","label":"Identifier","values":["https://digitalcommons.odu.edu/oeas_etds/105"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description.abstract","label":"Abstract","values":["Surficial sands deposited in the Chesapeake Bay are a mixture of sands derived from the bay's shorelines, from offshore, and from relict deposits. Direct fluvial input is probably minor except from the James River, which may serve as a local source of sands in the Thimble Shoals area. Sands in the western half of the bay are primarily derived from the erosion of the adjacent shoreline. In contrast, the eastern half of the bay has two major sources of sand. Shoreline erosion is the dominant source north of the town of Eastville, Virginia, while the offshore is the major source south of this area.
Some surficial sands in the Chesapeake Bay are relict. Sands in the upper mid-bay channel are the result of reworked deposits from the Paleo-Susquehanna River. Preservation of this older material is probably the result of its location in the deeper portions of the bay, where depositional rates are low.
"]},{"key":"dc:title","label":"Title","values":["Provenance of Sands Within the Lower Chesapeake Bay Based on Ilmenite Composition"]}]}],"canonical_facts":{"dc:contributor":["Dennis A. Darby","Joseph H. Rule","Ronald E. Johnson","R. J. Bryne"],"dc:creator":["Council, Edward Augustus, III"],"dc:date.available":["2019-09-13T07:00:00Z"],"dc:description.abstract":["Surficial sands deposited in the Chesapeake Bay are a mixture of sands derived from the bay's shorelines, from offshore, and from relict deposits. Direct fluvial input is probably minor except from the James River, which may serve as a local source of sands in the Thimble Shoals area. Sands in the western half of the bay are primarily derived from the erosion of the adjacent shoreline. In contrast, the eastern half of the bay has two major sources of sand. Shoreline erosion is the dominant source north of the town of Eastville, Virginia, while the offshore is the major source south of this area.
Some surficial sands in the Chesapeake Bay are relict. Sands in the upper mid-bay channel are the result of reworked deposits from the Paleo-Susquehanna River. Preservation of this older material is probably the result of its location in the deeper portions of the bay, where depositional rates are low.
"],"dc:identifier":["https://digitalcommons.odu.edu/oeas_etds/105"],"dc:rights":["In Copyright. URI: http://rightsstatements.org/vocab/InC/1.0/ This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).
"],"dc:subject":["Sand","Sedimentation analysis","Chesapeake Bay","Deposits","Geology"],"dc:title":["Provenance of Sands Within the Lower Chesapeake Bay Based on Ilmenite Composition"],"thesis:degree_discipline":["Ocean & Earth Sciences"],"thesis:degree_level":["Thesis"],"thesis:degree_name":["Master of Science (MS)"]},"updated_at":"2026-07-24T03:35:08Z"}