{"id":{"repo_id":"montana-tech","oai_identifier":"oai:scholarworks.umt.edu:etd-2298"},"canonical_url":"https://search.dev.ndltd.org/etd/montana-tech/oai:scholarworks.umt.edu:etd-2298","repository":{"repo_id":"montana-tech","name":"Montana Technology","base_url":"https://scholarworks.umt.edu/do/oai/"},"display":{"title":"Lithofacies and Microfacies of a Fossil Hot Spring System: McGinness Hills, Nevada","abstract":"Ertel, Bonnie, M.S., Spring 2009 Geology Microfacies and Morphology of a Fossil Hot Spring System, McGinness Hills, Nevada Chairperson or Co-Chairperson: Dr. Nancy Hinman The Miocene McGinness Hills sinters are a well-preserved, fossil hot spring system in Nevada. The sinter in McGinness Hills is comparable with the fossil hot spring system in the Drummond Basin, Queensland, Australia (Farmer and Hinman, 1998), Artist Point in Yellowstone National Park (Hinman and Walter, 2005) and with modern systems in Yellowstone. Further The purpose of this study was to further our understanding microfacies preserved in hot springs systems after diagenesis thus facilitating the identification of epithermal systems in which exposure is limited. It is possible to recognize a range of paleo-hot spring environments from near-vent stratiform geyserite, outflow channels and terraces and distal marsh facies. McGinness Hills is a ‘decapitated’ system in which hydrothermal, eruption breccia is exposed on top of the sinter mound. Based on lithology, macro-features and micro-features the sinter at McGinness Hills was divided into seven microfacies, hydrothermal breccia, massive chalcedonic sinter, flat-laminated sinter, stromatolitic sinter, palisade sinter, palisade sinter, sinter breccia and marsh sinter. The microfacies followed a general bulls-eye pattern with hydrothermal breccia and massive chalcedonic sinter in the center, grading out to the opaline, low temperature marsh facies. Hydrothermal eruption breccia is normally a subsurface feature confined within the throat of the geyser (Browne and Lawless, 2001) hence the breccia at McGinness Hills provides a glimpse into the inner workings of a geyser.","abstract_html":"Ertel, Bonnie, M.S., Spring 2009 Geology Microfacies and Morphology of a Fossil Hot Spring System, McGinness Hills, Nevada Chairperson or Co-Chairperson: Dr. Nancy Hinman The Miocene McGinness Hills sinters are a well-preserved, fossil hot spring system in Nevada. The sinter in McGinness Hills is comparable with the fossil hot spring system in the Drummond Basin, Queensland, Australia (Farmer and Hinman, 1998), Artist Point in Yellowstone National Park (Hinman and Walter, 2005) and with modern systems in Yellowstone. Further The purpose of this study was to further our understanding microfacies preserved in hot springs systems after diagenesis thus facilitating the identification of epithermal systems in which exposure is limited. It is possible to recognize a range of paleo-hot spring environments from near-vent stratiform geyserite, outflow channels and terraces and distal marsh facies. McGinness Hills is a ‘decapitated’ system in which hydrothermal, eruption breccia is exposed on top of the sinter mound. Based on lithology, macro-features and micro-features the sinter at McGinness Hills was divided into seven microfacies, hydrothermal breccia, massive chalcedonic sinter, flat-laminated sinter, stromatolitic sinter, palisade sinter, palisade sinter, sinter breccia and marsh sinter. The microfacies followed a general bulls-eye pattern with hydrothermal breccia and massive chalcedonic sinter in the center, grading out to the opaline, low temperature marsh facies. Hydrothermal eruption breccia is normally a subsurface feature confined within the throat of the geyser (Browne and Lawless, 2001) hence the breccia at McGinness Hills provides a glimpse into the inner workings of a geyser.","abstract_has_math":false,"creators":["Ertel, Bonnie Jean"],"institution":"University of Montana","degree_name":"Master of Science (MS)","degree_level":null,"degree_discipline":null,"degree_department":null,"school":null,"contributors":[],"advisors":[],"committee_chairs":[],"committee_members":[],"year":2009,"date_issued":"2009-01-01T08:00:00Z","date_published":"2009-01-01T08:00:00Z","updated_at":"2026-07-24T03:14:30Z","subjects":["geyserite","hydrothermal breccia","microfacies","sinter"],"languages":[],"rights":[],"rights_urls":[],"identifier_entries":[]},"links":{"outbound_url":"https://scholarworks.umt.edu/etd/1279","outbound_label":"Repository record","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:creator","label":"Author","values":["Ertel, Bonnie Jean"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:publisher","label":"Institution","values":["University of Montana"]},{"key":"dc:type","label":"Dc Type","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":["geyserite","hydrothermal breccia","microfacies","sinter"]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier","label":"Identifier","values":["https://scholarworks.umt.edu/etd/1279"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description.abstract","label":"Abstract","values":["Ertel, Bonnie, M.S., Spring 2009 Geology Microfacies and Morphology of a Fossil Hot Spring System, McGinness Hills, Nevada Chairperson or Co-Chairperson: Dr. Nancy Hinman The Miocene McGinness Hills sinters are a well-preserved, fossil hot spring system in Nevada. The sinter in McGinness Hills is comparable with the fossil hot spring system in the Drummond Basin, Queensland, Australia (Farmer and Hinman, 1998), Artist Point in Yellowstone National Park (Hinman and Walter, 2005) and with modern systems in Yellowstone. Further The purpose of this study was to further our understanding microfacies preserved in hot springs systems after diagenesis thus facilitating the identification of epithermal systems in which exposure is limited. It is possible to recognize a range of paleo-hot spring environments from near-vent stratiform geyserite, outflow channels and terraces and distal marsh facies. McGinness Hills is a ‘decapitated’ system in which hydrothermal, eruption breccia is exposed on top of the sinter mound. Based on lithology, macro-features and micro-features the sinter at McGinness Hills was divided into seven microfacies, hydrothermal breccia, massive chalcedonic sinter, flat-laminated sinter, stromatolitic sinter, palisade sinter, palisade sinter, sinter breccia and marsh sinter. The microfacies followed a general bulls-eye pattern with hydrothermal breccia and massive chalcedonic sinter in the center, grading out to the opaline, low temperature marsh facies. Hydrothermal eruption breccia is normally a subsurface feature confined within the throat of the geyser (Browne and Lawless, 2001) hence the breccia at McGinness Hills provides a glimpse into the inner workings of a geyser."]},{"key":"dc:title","label":"Title","values":["Lithofacies and Microfacies of a Fossil Hot Spring System: McGinness Hills, Nevada"]}]}],"canonical_facts":{"dc:creator":["Ertel, Bonnie Jean"],"dc:description.abstract":["Ertel, Bonnie, M.S., Spring 2009 Geology Microfacies and Morphology of a Fossil Hot Spring System, McGinness Hills, Nevada Chairperson or Co-Chairperson: Dr. Nancy Hinman The Miocene McGinness Hills sinters are a well-preserved, fossil hot spring system in Nevada. The sinter in McGinness Hills is comparable with the fossil hot spring system in the Drummond Basin, Queensland, Australia (Farmer and Hinman, 1998), Artist Point in Yellowstone National Park (Hinman and Walter, 2005) and with modern systems in Yellowstone. Further The purpose of this study was to further our understanding microfacies preserved in hot springs systems after diagenesis thus facilitating the identification of epithermal systems in which exposure is limited. It is possible to recognize a range of paleo-hot spring environments from near-vent stratiform geyserite, outflow channels and terraces and distal marsh facies. McGinness Hills is a ‘decapitated’ system in which hydrothermal, eruption breccia is exposed on top of the sinter mound. Based on lithology, macro-features and micro-features the sinter at McGinness Hills was divided into seven microfacies, hydrothermal breccia, massive chalcedonic sinter, flat-laminated sinter, stromatolitic sinter, palisade sinter, palisade sinter, sinter breccia and marsh sinter. The microfacies followed a general bulls-eye pattern with hydrothermal breccia and massive chalcedonic sinter in the center, grading out to the opaline, low temperature marsh facies. Hydrothermal eruption breccia is normally a subsurface feature confined within the throat of the geyser (Browne and Lawless, 2001) hence the breccia at McGinness Hills provides a glimpse into the inner workings of a geyser."],"dc:identifier":["https://scholarworks.umt.edu/etd/1279"],"dc:publisher":["University of Montana"],"dc:subject":["geyserite","hydrothermal breccia","microfacies","sinter"],"dc:title":["Lithofacies and Microfacies of a Fossil Hot Spring System: McGinness Hills, Nevada"],"dc:type":["Thesis"],"thesis:degree_name":["Master of Science (MS)"]},"updated_at":"2026-07-24T03:14:30Z"}