{"id":30,"date":"2024-11-06T15:39:39","date_gmt":"2024-11-06T15:39:39","guid":{"rendered":"https:\/\/mupages.marshall.edu\/sites\/caudillm\/?page_id=30"},"modified":"2024-11-12T16:08:21","modified_gmt":"2024-11-12T16:08:21","slug":"research","status":"publish","type":"page","link":"https:\/\/mupages.marshall.edu\/caudillm\/research\/","title":{"rendered":"Research"},"content":{"rendered":"\n<h2 class=\"wp-block-heading has-text-align-center\">Research Interests<\/h2>\n\n\n\n<p><strong>Contribution of Ohio River islands to Floodplain Growth in Upper Ohio River Valley<\/strong><\/p>\n\n\n\n<div class=\"wp-block-media-text has-media-on-the-right is-stacked-on-mobile\"><div class=\"wp-block-media-text__content\">\n<p>Ohio River Islands are temporary features. The upper valley contains example of islands in various stages of accretion to the floodplain. The focus of this work is to:<\/p>\n\n\n\n<p>1) delineate islands that have already been added to the floodplain.<\/p>\n\n\n\n<p>2) understand the timing and processes involved in island accretion.<\/p>\n<\/div><figure class=\"wp-block-media-text__media\"><img loading=\"lazy\" decoding=\"async\" width=\"924\" height=\"538\" src=\"http:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research1-OhioRIver-1.jpg\" alt=\"\" class=\"wp-image-42 size-full\" srcset=\"https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research1-OhioRIver-1.jpg 924w, https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research1-OhioRIver-1-300x175.jpg 300w, https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research1-OhioRIver-1-768x447.jpg 768w\" sizes=\"auto, (max-width: 924px) 100vw, 924px\" \/><\/figure><\/div>\n\n\n\n<p><strong>Microfacies of Ancient Lake Deposits of the Teays Valley and Assessment of the Paleoclimate and Paleoenvironment Archives<\/strong><\/p>\n\n\n\n<div class=\"wp-block-media-text has-media-on-the-right is-stacked-on-mobile\" style=\"grid-template-columns:auto 15%\"><div class=\"wp-block-media-text__content\">\n<p><\/p>\n\n\n\n<p>This work focuses on extracting evidence of paleoclimate and paleoenvironmental changes during the MIS 22-21 glacial-interglacial cycle recorded by the deposits of ancient Lake Tight which occupied the former Teays River valley roughly 800,000 years ago. &nbsp;The primary goal is to exploit this high-resolution record to delineate short-term trends of decadal, centennial, and potentially millennial scales. To this end, geochemical climate proxies are used in tandem with assessments of sediment sources, depositional processes, and intra-seasonal events. This is a cooperative project with Dr. El-Shazly.<\/p>\n<\/div><figure class=\"wp-block-media-text__media\"><img loading=\"lazy\" decoding=\"async\" width=\"194\" height=\"501\" src=\"https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research2-Microfacies-1.png\" alt=\"\" class=\"wp-image-62 size-full\" srcset=\"https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research2-Microfacies-1.png 194w, https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research2-Microfacies-1-116x300.png 116w\" sizes=\"auto, (max-width: 194px) 100vw, 194px\" \/><\/figure><\/div>\n\n\n\n<p><strong>Relict Pattern Ground and Thermokarst Features along Pleistocene Glacial Margins<\/strong><\/p>\n\n\n\n<figure class=\"wp-block-image aligncenter size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"437\" src=\"http:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research3-RelictPatternGlacier-1-1024x437.jpg\" alt=\"\" class=\"wp-image-66\" srcset=\"https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research3-RelictPatternGlacier-1-1024x437.jpg 1024w, https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research3-RelictPatternGlacier-1-300x128.jpg 300w, https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research3-RelictPatternGlacier-1-768x327.jpg 768w, https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research3-RelictPatternGlacier-1.jpg 1433w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n\n\n\n<p>In southcentral and east central Ohio French and Millar (2014) indicate a narrowing of the width permafrost belt of last glacial maximum. Here the permafrost belt appears to have been narrower that any area in the Midwest lying between the Mississippi River and Appalachian Mtns. Here, the very limited width of permafrost zone in this area from south central Ohio to southwestern Ohio has been attributed to 1) lack of through field investigations and 2) a strong environmental gradient in this region. To better define the ancient permafrost zone, my research uses Google Earth images to identify and map the distribution of relict patterned ground, a feature characteristic of permafrost zones, along the front of the Wisconsin glacier at maximum extent in Ohio.<\/p>\n\n\n\n<p><strong>Weathering Durability of Upper Paleozoic Mudrocks of the Appalachian Plateau<\/strong><\/p>\n\n\n\n<div class=\"wp-block-media-text has-media-on-the-right is-stacked-on-mobile\"><div class=\"wp-block-media-text__content\">\n<p>The resistance of argillaceous rocks to weathering is an important engineering concern for geotechnical projects of many types. Many approaches have been proposed for assessing this important attribute. This work compares the results of two newer methods developed by Bryson, et.al. (2012, 2019), the Loss Slake Index (LSI) and Electrical Jar Slake test (ESJ).&nbsp; It focuses on testing and applying these methods for assessment of Pennsylvanian and Permian mudrocks of the Appalachian Plateau.<\/p>\n<\/div><figure class=\"wp-block-media-text__media\"><img loading=\"lazy\" decoding=\"async\" width=\"1025\" height=\"289\" src=\"http:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research4-WeatheringDurability.png\" alt=\"\" class=\"wp-image-45 size-full\" srcset=\"https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research4-WeatheringDurability.png 1025w, https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research4-WeatheringDurability-300x85.png 300w, https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research4-WeatheringDurability-768x217.png 768w\" sizes=\"auto, (max-width: 1025px) 100vw, 1025px\" \/><\/figure><\/div>\n\n\n\n<p><strong>Origin of Relict Landslide Assemblages and Associated Colluvial Lithofacies<\/strong><br><br><p class=\"MsoNormal\"><span style=\"font-size:12.0pt;line-height:107%;color:black\"><\/span><\/p><\/p>\n\n\n\n<div class=\"wp-block-media-text has-media-on-the-right is-stacked-on-mobile\"><div class=\"wp-block-media-text__content\">\n<p>A large assemblage (50+) of paleo-slumps have been identified in one small watershed of southeastern Ohio a few 10s of miles south of the Pleistocene glacial fronts. Dating of soils buried on the tops of ancient slump blocks suggest initial movement occurred more 7800 years ago. Work continues and is focused on; 1) using OSL dating to further constrain age of the slumping event(s), 2) identify the colluvial process which buried ancient soils on the slump block top to depths of 7+ ft, and 3) evaluate the extrinsic trigger(s) of slumping.<\/p>\n<\/div><figure class=\"wp-block-media-text__media\"><img loading=\"lazy\" decoding=\"async\" width=\"984\" height=\"556\" src=\"http:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research5-RelictLandslide.jpg\" alt=\"\" class=\"wp-image-46 size-full\" srcset=\"https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research5-RelictLandslide.jpg 984w, https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research5-RelictLandslide-300x170.jpg 300w, https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research5-RelictLandslide-768x434.jpg 768w\" sizes=\"auto, (max-width: 984px) 100vw, 984px\" \/><\/figure><\/div>\n\n\n\n<div class=\"wp-block-kadence-spacer aligncenter kt-block-spacer-30_4dfdd1-9f\"><div class=\"kt-block-spacer kt-block-spacer-halign-center\"><hr class=\"kt-divider\" \/><\/div><\/div>\n\n\n\n<div class=\"wp-block-kadence-column kadence-column30_138b0c-41\"><div class=\"kt-inside-inner-col\">\n<h2 class=\"wp-block-heading has-text-align-center\">Recent Student Research<\/h2>\n<\/div><\/div>\n\n\n\n<p>The projects listed here were conducted to meet the Capstone course requirement for the Geology program. They include both in-house internships and senior theses. Some were supported by WV NASA Undergraduate Fellowships.<\/p>\n\n\n\n<p><strong>Survey of Relict Pattern Ground Periglacial Features along Wisconsin Glacial Maximum in<\/strong> <strong>Portions of Ohio<\/strong>: Madeleine Tisler, 2026<\/p>\n\n\n\n<figure class=\"wp-block-image aligncenter size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"884\" height=\"715\" src=\"http:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research6-SurveyRelict.jpg\" alt=\"\" class=\"wp-image-47\" srcset=\"https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research6-SurveyRelict.jpg 884w, https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research6-SurveyRelict-300x243.jpg 300w, https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research6-SurveyRelict-768x621.jpg 768w\" sizes=\"auto, (max-width: 884px) 100vw, 884px\" \/><\/figure>\n\n\n\n<p><\/p>\n\n\n\n<div class=\"wp-block-media-text has-media-on-the-right is-stacked-on-mobile\"><div class=\"wp-block-media-text__content\">\n<p><strong>Micromorplogy of Varves of mid-Pleistocene Lake Tight, Teays Valley WV; Sedimentation Rates and Paleoenvironmental Change<\/strong><\/p>\n\n\n\n<p> Zach Sparks, 2025. <\/p>\n\n\n\n<p>(Funded by WV NASA Undergraduate Summer Fellowship)<\/p>\n<\/div><figure class=\"wp-block-media-text__media\"><img loading=\"lazy\" decoding=\"async\" width=\"380\" height=\"408\" src=\"http:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research7-Micromorphology.png\" alt=\"\" class=\"wp-image-48 size-full\" srcset=\"https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research7-Micromorphology.png 380w, https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research7-Micromorphology-279x300.png 279w\" sizes=\"auto, (max-width: 380px) 100vw, 380px\" \/><\/figure><\/div>\n\n\n\n<div class=\"wp-block-kadence-spacer aligncenter kt-block-spacer-30_8ee613-54\"><div class=\"kt-block-spacer kt-block-spacer-halign-center\"><hr class=\"kt-divider\" \/><\/div><\/div>\n\n\n\n<div class=\"wp-block-media-text has-media-on-the-right is-stacked-on-mobile\"><div class=\"wp-block-media-text__content\">\n<p><strong>Durability of Pennsylvanian Red Beds Using Electric Jar Slake Test Method.<\/strong><\/p>\n\n\n\n<p>&nbsp;Jamie Ward, 2024<\/p>\n<\/div><figure class=\"wp-block-media-text__media\"><img loading=\"lazy\" decoding=\"async\" width=\"567\" height=\"664\" src=\"http:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research8-LossSlakeDurability.jpg\" alt=\"\" class=\"wp-image-49 size-full\" srcset=\"https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research8-LossSlakeDurability.jpg 567w, https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research8-LossSlakeDurability-256x300.jpg 256w\" sizes=\"auto, (max-width: 567px) 100vw, 567px\" \/><\/figure><\/div>\n\n\n\n<div class=\"wp-block-kadence-spacer aligncenter kt-block-spacer-30_c41095-38\"><div class=\"kt-block-spacer kt-block-spacer-halign-center\"><hr class=\"kt-divider\" \/><\/div><\/div>\n\n\n\n<div class=\"wp-block-media-text has-media-on-the-right is-stacked-on-mobile\"><div class=\"wp-block-media-text__content\">\n<p><strong>Durability of Pennsylvanian Red Beds Using Electric Jar Slake Test Method<\/strong><\/p>\n\n\n\n<p>&nbsp;Jamie Ward, 2024<\/p>\n<\/div><figure class=\"wp-block-media-text__media\"><img loading=\"lazy\" decoding=\"async\" width=\"615\" height=\"330\" src=\"http:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research9-RedBedDurability.png\" alt=\"\" class=\"wp-image-50 size-full\" srcset=\"https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research9-RedBedDurability.png 615w, https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research9-RedBedDurability-300x161.png 300w\" sizes=\"auto, (max-width: 615px) 100vw, 615px\" \/><\/figure><\/div>\n\n\n\n<div class=\"wp-block-kadence-spacer aligncenter kt-block-spacer-30_486734-af\"><div class=\"kt-block-spacer kt-block-spacer-halign-center\"><hr class=\"kt-divider\" \/><\/div><\/div>\n\n\n\n<div class=\"wp-block-media-text has-media-on-the-right is-stacked-on-mobile\"><div class=\"wp-block-media-text__content\">\n<p><strong>Loss Slake Index of Middle Pennsylvanian Mudrocks of the Appalachian Plateau in&nbsp; West Virginia<\/strong><\/p>\n\n\n\n<p>Jack Pennington, 2024<\/p>\n\n\n\n<p>(Funded by WV NASA Undergraduate Fellowship)<\/p>\n<\/div><figure class=\"wp-block-media-text__media\"><img loading=\"lazy\" decoding=\"async\" width=\"476\" height=\"358\" src=\"http:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research10-LossSlake.png\" alt=\"\" class=\"wp-image-51 size-full\" srcset=\"https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research10-LossSlake.png 476w, https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research10-LossSlake-300x226.png 300w\" sizes=\"auto, (max-width: 476px) 100vw, 476px\" \/><\/figure><\/div>\n\n\n\n<div class=\"wp-block-kadence-spacer aligncenter kt-block-spacer-30_757118-b4\"><div class=\"kt-block-spacer kt-block-spacer-halign-center\"><hr class=\"kt-divider\" \/><\/div><\/div>\n\n\n\n<div class=\"wp-block-media-text has-media-on-the-right is-stacked-on-mobile\"><div class=\"wp-block-media-text__content\">\n<p><strong>Assessment of the Electric Slake Jar method for Determining Weathering Susceptibility of an Upper Pennsylvanian \u201cRedbed\u201d, central Appalachian Plateau<\/strong> <strong>of West Virginia<\/strong><\/p>\n\n\n\n<p>Jackelyn McClanahan, 2023<\/p>\n<\/div><figure class=\"wp-block-media-text__media\"><img loading=\"lazy\" decoding=\"async\" width=\"730\" height=\"482\" src=\"http:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research11-ElectricSlake.jpg\" alt=\"\" class=\"wp-image-52 size-full\" srcset=\"https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research11-ElectricSlake.jpg 730w, https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research11-ElectricSlake-300x198.jpg 300w\" sizes=\"auto, (max-width: 730px) 100vw, 730px\" \/><\/figure><\/div>\n\n\n\n<div class=\"wp-block-kadence-spacer aligncenter kt-block-spacer-30_1b10a8-5b\"><div class=\"kt-block-spacer kt-block-spacer-halign-center\"><hr class=\"kt-divider\" \/><\/div><\/div>\n\n\n\n<div class=\"wp-block-media-text has-media-on-the-right is-stacked-on-mobile\"><div class=\"wp-block-media-text__content\">\n<p><strong>Analysis and Applications of USGS Water Quality Online Data with Respect to Specific Conductivity Levels in Ten West Virginia Streams<\/strong><\/p>\n\n\n\n<p> Kelley Cusick, 2022<\/p>\n<\/div><figure class=\"wp-block-media-text__media\"><img loading=\"lazy\" decoding=\"async\" width=\"690\" height=\"347\" src=\"http:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research12-WaterQuality.png\" alt=\"\" class=\"wp-image-53 size-full\" srcset=\"https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research12-WaterQuality.png 690w, https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research12-WaterQuality-300x151.png 300w\" sizes=\"auto, (max-width: 690px) 100vw, 690px\" \/><\/figure><\/div>\n\n\n\n<div class=\"wp-block-kadence-spacer aligncenter kt-block-spacer-30_d96587-8c\"><div class=\"kt-block-spacer kt-block-spacer-halign-center\"><hr class=\"kt-divider\" \/><\/div><\/div>\n\n\n\n<div class=\"wp-block-media-text has-media-on-the-right is-stacked-on-mobile\"><div class=\"wp-block-media-text__content\">\n<p><strong>Modified Slake Durability Index and Loss Slake Index Determination of Upper Pennsylvanian, Monongahela Group Strata for Better Weathering Susceptibility Classification of Mudrock Samples<\/strong><\/p>\n\n\n\n<p>Matt Shaffer, 2021<\/p>\n<\/div><figure class=\"wp-block-media-text__media\"><img loading=\"lazy\" decoding=\"async\" width=\"605\" height=\"807\" src=\"http:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research13-SlakeDurability.jpg\" alt=\"\" class=\"wp-image-54 size-full\" srcset=\"https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research13-SlakeDurability.jpg 605w, https:\/\/mupages.marshall.edu\/caudillm\/wp-content\/uploads\/sites\/110\/2024\/11\/Research13-SlakeDurability-225x300.jpg 225w\" sizes=\"auto, (max-width: 605px) 100vw, 605px\" \/><\/figure><\/div>\n\n\n\n<div class=\"wp-block-kadence-spacer aligncenter kt-block-spacer-30_414991-8e\"><div class=\"kt-block-spacer kt-block-spacer-halign-center\"><hr class=\"kt-divider\" \/><\/div><\/div>\n\n\n\n<div class=\"wp-block-kadence-column kadence-column30_540236-3f\"><div class=\"kt-inside-inner-col\">\n<h2 class=\"wp-block-heading has-text-align-center\">Selected Research<\/h2>\n<\/div><\/div>\n\n\n\n<h3 class=\"wp-block-heading has-text-align-center\">Professional Consulting Reports<\/h3>\n\n\n\n<p><strong>Caudill, M.R.<\/strong>, 2017, Soils and Geomorphic Analysis, Deep Test Archaeological Assessment, St. Albans, WV, Wastewater Treatment Facility; ACS Group Inc. Columbus, Ohio.<\/p>\n\n\n\n<p><strong>Caudill, M.R.<\/strong>, 2016, Soils and Geomorphic Analysis, Deep Test Archaeological Assessment, High Carpenter Bridge, Middle Island, St. Mary\u2019s, WV; ACS Group Inc. Columbus, Ohio.<\/p>\n\n\n\n<p><strong>Caudill, M.R.<\/strong>, 2015, Soils and Geomorphic Analysis, Deep Test Archaeological Assessment, Mouth of Seneca Bridge Site, Seneca Rocks, WV; ACS Group Inc. Columbus, Ohio.<\/p>\n\n\n\n<p><strong>Caudill, M.R.<\/strong>, Soils and Geomorphic Analysis, Deep Test Archaeological Assessment, New Ohio River Bridge Site, Wellsburg, WV; ACS Group Inc. Columbus, Ohio.<\/p>\n\n\n\n<p><strong>Caudill, M.R.<\/strong>, 2011, Soils and Geomorphic Analysis, Deep Test Archaeological Assessment, Mid-Ohio Valley Technical School, St. Mary\u2019s, WV; ACS Group Inc. Columbus, Ohio.<\/p>\n\n\n\n<p><strong>Caudill, M.R.<\/strong>, 2010, Soils and Geomorphology Analysis, Deep Test Archaeological Assessment, Carver Career Center, Charleston, WV, ACS Group Inc. Columbus, Ohio.<\/p>\n\n\n\n<p><strong>Caudill, M.R.<\/strong>, 2008, Soils and Geomorphology Analysis, Deep Test Archaeological Assessment, Development Site, Williamstown WV; ACS Group Inc. Columbus, Ohio.<\/p>\n\n\n\n<p><strong>Caudill, M.R.<\/strong>, 2007, Soils and Geomorphology Analysis Deep Test Archaeological Assessment, Municipal Waterline Extension Project, ACS Group Inc. Columbus, Ohio.<\/p>\n\n\n\n<p><strong>Caudill, M.R<\/strong>., 1998, Alleghenian Coal Resources of western Pennsylvania, East Fairfield Coal Company, Lisbon, OH.<\/p>\n\n\n\n<h3 class=\"wp-block-heading has-text-align-center\">Referred Publications<\/h3>\n\n\n\n<p>Driese, S.G., <strong>Caudill, M.R.<\/strong>, and Srinivasan, K., 1998, Late Mississippian paleokarst in east-central Tennessee: field, petrographic, and stable isotope evidence. Southeastern Geolofy, 37, 4, 189-204.<\/p>\n\n\n\n<p><strong>Caudill, M.R.<\/strong>, Driese, S.G., and Mora, C.I., 1997, Compaction of vertic paleosols: Implications for burial diagenesis and paleo-precipitation estimates. Sedimentology, 44, 4, 673-686.<\/p>\n\n\n\n<p><strong>Caudill, M.R.<\/strong>, Driese, S.G., and Mora, C.I., 1996, Preservation of a paleo-Vertisol and an estimate of Late Mississippian paleoprecipitation. Journal of Sedimentary Research, A66, 58-70<\/p>\n\n\n\n<p><strong>Caudill, M.R.<\/strong>, 1990, Lithostratigraphy of Conemaugh marine zones (Pennsylvanian); Steubenville, Ohio -Weirton, West Virginia. Southeastern Geolofy, 31, 3, 1-10.<\/p>\n\n\n\n<p><strong>Caudill, M.R.<\/strong> and Schumacher, G.S., 1989, Ohio Blattoid(Insecta) Fossil Locality, Rediscovered. Journal of Paleontology, 60, 1, 121-124.<\/p>\n\n\n\n<h3 class=\"wp-block-heading has-text-align-center\">Abstracts<\/h3>\n\n\n\n<p>Shafer, C.M. and <strong>Caudill, M.R<\/strong>., 2022, Loss Slake Index of an Upper Pennsylvanian mudrock,&nbsp; Appalachian Plateau, West Virginia. NC-SE GSA Mtg Absts. with Prog., 54, 4.<\/p>\n\n\n\n<p><strong>Caudill, M.R.,<\/strong> 2021, Preliminary Mapping and Assessment of Landslide Assemblage, Minkers Run Area, Athens County, southeastern Ohio. NC-SC GSA Absts. with Prog., 53, 3.<\/p>\n\n\n\n<p><strong>Caudill, M.R.<\/strong> and Driese, S.G., 1999, Paleokarst conduit sediments and the origin of conglomerates in Upper Mississippian paleosols of the Cumberland Plateau, Tennessee. GSA Absts. with Prog., 31, A7.<\/p>\n\n\n\n<p><strong>Caudill, M.R.<\/strong> and Driese, S.G., 1998 (invited), Transgression-driven rises in ancient, coastal groundwater tables: Evidence from vertic paleosols of Late Pennsylvanian (lower Conemaugh Group) cyclothems. Appalachian Cyclothems Symposium, GSA Absts. with Prog., 30, 2, 9.<\/p>\n\n\n\n<h3 class=\"wp-block-heading has-text-align-center\">Maps<\/h3>\n\n\n\n<p>Slucher, E.R., Swinford, E.M., Larsen, G.E., Schumacher, G.A., Shrake, D.L., Rice, C.L., <strong>Caudill, M.R., <\/strong>and Rea, R.G., 2006, Bedrock Geologic Map of Ohio. Ohio Geological Survey, BG-1.<\/p>\n\n\n\n<p>Slucher, E.R., <strong>Caudill, M.R.,<\/strong> and Swinford, E.M., 1992, Bedrock Geology of the Powell quad. Ohio Geological Survey, BGC4B1.<\/p>\n\n\n\n<p><strong>Caudill, M.R.,<\/strong> 1991, Bedrock Geology of the Knoxville quad. Ohio Geological Survey, BGC1D6<\/p>\n\n\n\n<p><strong>Caudill, M.R.,<\/strong> 1991, Bedrock Geology of the Wellsville quad. Ohio Geological Survey, BGC1E6<\/p>\n\n\n\n<p><strong>Caudill, M.R.,<\/strong> 1991, Bedrock Geology of the Weirton quad. Ohio Geological Survey, BGC1D5.<\/p>\n\n\n\n<p><strong>Caudill, M.R.,<\/strong> 1991, Bedrock Geology of the Richmond quad. Ohio Geological Survey, BGC1D7 1990<\/p>\n\n\n\n<p><strong>Caudill, M.R.<\/strong> and Slucher, E.R., 1990, Bedrock Geology of the Salineville quad. Ohio Geological<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Research Interests Contribution of Ohio River islands to Floodplain Growth in Upper Ohio River Valley Ohio River Islands are temporary features. The upper valley contains example of islands in various stages of accretion to the floodplain. The focus of this work is to: 1) delineate islands that have already been added to the floodplain. 2) [&hellip;]<\/p>\n","protected":false},"author":257,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false,"footnotes":""},"class_list":["post-30","page","type-page","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/mupages.marshall.edu\/caudillm\/wp-json\/wp\/v2\/pages\/30","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/mupages.marshall.edu\/caudillm\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/mupages.marshall.edu\/caudillm\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/mupages.marshall.edu\/caudillm\/wp-json\/wp\/v2\/users\/257"}],"replies":[{"embeddable":true,"href":"https:\/\/mupages.marshall.edu\/caudillm\/wp-json\/wp\/v2\/comments?post=30"}],"version-history":[{"count":35,"href":"https:\/\/mupages.marshall.edu\/caudillm\/wp-json\/wp\/v2\/pages\/30\/revisions"}],"predecessor-version":[{"id":102,"href":"https:\/\/mupages.marshall.edu\/caudillm\/wp-json\/wp\/v2\/pages\/30\/revisions\/102"}],"wp:attachment":[{"href":"https:\/\/mupages.marshall.edu\/caudillm\/wp-json\/wp\/v2\/media?parent=30"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}