{"id":{"repo_id":"mo-state","oai_identifier":"oai:bearworks.missouristate.edu:theses-1792"},"canonical_url":"https://search.dev.ndltd.org/etd/mo-state/oai:bearworks.missouristate.edu:theses-1792","repository":{"repo_id":"mo-state","name":"Missouri State University","base_url":"https://bearworks.missouristate.edu/do/oai/"},"display":{"title":"The Geology of Cedar County, Missouri: a Guide For Planners","abstract":"Cedar County is located on the northwest flank of the Ozark Uplift. The rock units have a regional dip of less than one degree to the west. This has been modified locally by three northwest-southeast trending faults, two anticlines, and two synclines. Dolomite, limestone, and sandstone of Ordovician, Mississippian and Pennsylvanian age occur in the county. These units are a source of limestone, sand and gravel, and coal. The geology was used to determine potential areas of geologic hazards, flooding, solid waste disposal, and wastewater disposal. Recommendations to avoid faulted ares, abandoned coal mines and limestone quarries, and flood-prone areas are discussed and should be considered prior to future development.","abstract_html":"Cedar County is located on the northwest flank of the Ozark Uplift. The rock units have a regional dip of less than one degree to the west. This has been modified locally by three northwest-southeast trending faults, two anticlines, and two synclines. Dolomite, limestone, and sandstone of Ordovician, Mississippian and Pennsylvanian age occur in the county. These units are a source of limestone, sand and gravel, and coal. The geology was used to determine potential areas of geologic hazards, flooding, solid waste disposal, and wastewater disposal. Recommendations to avoid faulted ares, abandoned coal mines and limestone quarries, and flood-prone areas are discussed and should be considered prior to future development.","abstract_has_math":false,"creators":["Neill, Jerry R."],"institution":null,"degree_name":"Master of Science in Geospatial Sciences","degree_level":"Masters","degree_discipline":"Geography, Geology, and Planning","degree_department":null,"school":null,"contributors":["Kenneth Thomson"],"advisors":[],"committee_chairs":[],"committee_members":[],"year":1987,"date_issued":"1987-05-01T07:00:00Z","date_published":"1987-05-01T07:00:00Z","updated_at":"2026-07-24T03:15:48Z","subjects":["Earth Sciences"],"languages":[],"rights":["© Jerry R Neill"],"rights_urls":[],"identifier_entries":[]},"links":{"outbound_url":"https://bearworks.missouristate.edu/theses/791","outbound_label":"Repository record","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor","label":"Contributor","values":["Kenneth Thomson"]},{"key":"dc:creator","label":"Author","values":["Neill, Jerry R."]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"thesis:degree_discipline","label":"Discipline","values":["Geography, Geology, and Planning"]},{"key":"thesis:degree_level","label":"Degree Level","values":["Masters"]},{"key":"thesis:degree_name","label":"Degree Name","values":["Master of Science in Geospatial Sciences"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["Earth Sciences"]}]},{"id":"language_rights","label":"Language and Rights","entries":[{"key":"dc:rights","label":"Dc Rights","values":["© Jerry R Neill"]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier","label":"Identifier","values":["https://bearworks.missouristate.edu/theses/791"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description.abstract","label":"Abstract","values":["Cedar County is located on the northwest flank of the Ozark Uplift. The rock units have a regional dip of less than one degree to the west. This has been modified locally by three northwest-southeast trending faults, two anticlines, and two synclines. Dolomite, limestone, and sandstone of Ordovician, Mississippian and Pennsylvanian age occur in the county. These units are a source of limestone, sand and gravel, and coal. The geology was used to determine potential areas of geologic hazards, flooding, solid waste disposal, and wastewater disposal. Recommendations to avoid faulted ares, abandoned coal mines and limestone quarries, and flood-prone areas are discussed and should be considered prior to future development."]},{"key":"dc:title","label":"Title","values":["The Geology of Cedar County, Missouri: a Guide For Planners"]}]}],"canonical_facts":{"dc:contributor":["Kenneth Thomson"],"dc:creator":["Neill, Jerry R."],"dc:description.abstract":["Cedar County is located on the northwest flank of the Ozark Uplift. The rock units have a regional dip of less than one degree to the west. This has been modified locally by three northwest-southeast trending faults, two anticlines, and two synclines. Dolomite, limestone, and sandstone of Ordovician, Mississippian and Pennsylvanian age occur in the county. These units are a source of limestone, sand and gravel, and coal. The geology was used to determine potential areas of geologic hazards, flooding, solid waste disposal, and wastewater disposal. Recommendations to avoid faulted ares, abandoned coal mines and limestone quarries, and flood-prone areas are discussed and should be considered prior to future development."],"dc:identifier":["https://bearworks.missouristate.edu/theses/791"],"dc:rights":["© Jerry R Neill"],"dc:subject":["Earth Sciences"],"dc:title":["The Geology of Cedar County, Missouri: a Guide For Planners"],"thesis:degree_discipline":["Geography, Geology, and Planning"],"thesis:degree_level":["Masters"],"thesis:degree_name":["Master of Science in Geospatial Sciences"]},"updated_at":"2026-07-24T03:15:48Z"}