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Hamilton County Ohio
The American upper Ordovician standard, XVII; areal variation of limestone frequencies in the Kope and Fairview formations, Hamilton County, Ohio
The American upper Ordovician standard; XIV, Markov analysis of typical Cincinnatian sedimentation, Hamilton County, Ohio
American Upper Ordovician Standard. IX. Bedrock Geology of Eastern Hamilton County, Ohio
Cincinnatian Geology in Southwest Hamilton County, Ohio
Middle Devonian bone beds of Ohio
Paleoecologic Associations and Secondary Tiering of Cornulites on Crinoids and Bivalves in the Upper Ordovician (Cincinnatian) of Southwestern Ohio, Southeastern Indiana, and Northern Kentucky
Escape traces associated with Rafinesquina alternata , an Upper Ordovician strophomenid brachiopod from the Cincinnati Arch Region
LATE ORDOVICIAN JAWED POLYCHAETE FAUNAS OF THE TYPE CINCINNATIAN REGION, U.S.A
A PALEOECOLOGIC COMPARISON OF TWO EDRIOASTEROID (ECHINODERMATA) ENCRUSTED PAVEMENTS FROM THE UPPER ORDOVICIAN CORRYVILLE FORMATION OF FLORENCE, KENTUCKY AND THE MIAMITOWN SHALE OF SHARONVILLE, OHIO, U.S.A
Comparative Taxonomic Richness and Abundance of Late Ordovician Gastropods and Bivalves in Mollusc-rich Strata of the Cincinnati Arch
Sediment supply versus storm winnowing in the development of muddy and shelly interbeds from the Upper Ordovician of the Cincinnati region, USA This article is one of a series of papers published in this Special Issue on the theme The dynamic reef and shelly communities of the Paleozoic. This Special is in honour of our colleague and friend Paul Copper .
Remarkable preservation of shell microstructures from the Late Ordovician of the Cincinnati Arch region, USA, and the success of nacre among Ordovician mollusks
EXCEPTIONAL PYRITIZED CYANOBACTERIAL MATS ENCRUSTING BRACHIOPOD SHELLS FROM THE UPPER ORDOVICIAN (KATIAN) OF THE CINCINNATI, OHIO, REGION
GIANTS AMONG MICROMORPHS: WERE CINCINNATIAN (ORDOVICIAN, KATIAN) SMALL SHELLY PHOSPHATIC FAUNAS DWARFED?
LNAPL Removal from Unsaturated Porous Media Using Surfactant Infiltration
Unlike other informal sites, fossil parks provide visitors collecting opportunities that result in ownership of a small number of fossils. In 2003, we investigated the first three identified U.S. fossil parks at Hamburg, New York; Sylvania, Ohio; and Rockford, Iowa. Case study analyses determined the opportunities to learn geobiology at each site. Data collection proceeded through lived learning experiences, and included field notes, photographic records, informal conversations with park participants, brochures, and on-site signage. Through constant comparative methods, six variable categories converged for fossil park development: (1) informative previsit Web site, (2) authentic collecting in situ, (3) authentic collecting tools, (4) accessibility, (5) fossil identification, and (6) visitor education. These variables were optimized in a model of fossil park design. In 2005, fossil parks at Sharonville, Ohio, and Fossil, Oregon, were investigated in phase 2 of our study, and in 2006, our third case study researched fossil parks in Aurora, North Carolina, and Republic, Washington. Analysis of the seven U.S. fossil park data sets resulted in the emergence of key variables that affected the visitors' opportunities to learn geobiology concepts at fossil parks: (1) authenticity of experience, (2) age of fossils, (3) fossil-collection training and facilities, (4) availability of on-site paleontological mentors, (5) fossil identification via signage and brochures, (6) site organization and wayfinding signs, and (7) accessibility of site, including safety. The seven U.S. fossil parks were ranked against these variables according to their effectiveness as informal science education sites. We conclude that fossil parks can provide valuable informal geobiology education that can contribute to the public's geobiological literacy.