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NARROW
Format
Article Type
Journal
Publisher
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Canada
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Western Canada
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British Columbia
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Princeton British Columbia (3)
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North America
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Kootenay Arc (1)
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North American Cordillera (1)
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Okanogan Range (5)
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Omineca Belt (1)
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United States
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Colorado
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Park County Colorado (1)
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Iowa
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Floyd County Iowa (1)
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Kansas
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Ellsworth County Kansas (1)
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New York
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Erie County New York (1)
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North Carolina
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Beaufort County North Carolina (1)
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North Dakota
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Slope County North Dakota (1)
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Ohio
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Butler County Ohio (1)
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Hamilton County Ohio (1)
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Oregon
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Utah
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Uintah County Utah (1)
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Washington
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Western U.S. (1)
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commodities
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metal ores
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gold ores (1)
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elements, isotopes
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metals
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rare earths (1)
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fossils
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Chordata
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Vertebrata
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Pisces
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Osteichthyes
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Actinopterygii
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Teleostei (2)
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Tetrapoda
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Aves
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Neornithes (1)
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ichnofossils (1)
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Invertebrata
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Arthropoda
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Insecta
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Coleoptera (1)
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Hymenoptera (1)
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palynomorphs
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pollen (1)
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Betula (2)
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Hamamelididae (1)
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Rosidae (1)
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Monocotyledoneae
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Palmae (1)
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Gymnospermae
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Coniferales
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Pinaceae
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Abies (2)
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geochronology methods
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K/Ar (2)
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U/Pb (1)
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U/Th/Pb (1)
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geologic age
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Cenozoic
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Quaternary
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Tertiary
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Florissant Lake Beds (1)
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Paleogene
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Eocene
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Green River Formation (2)
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lower Eocene
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Ypresian (1)
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middle Eocene
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Laney Shale Member (1)
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Mesozoic
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Cretaceous
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Dakota Formation (1)
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Upper Cretaceous
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Hell Creek Formation (1)
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Paleozoic
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Cambrian
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Lardeau Group (1)
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lower Paleozoic (1)
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Permian (1)
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igneous rocks
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hypabyssal rocks (1)
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granodiorites (1)
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porphyry (1)
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basalts (1)
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dacites (1)
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framework silicates
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iron silicates (1)
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orthosilicates
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nesosilicates
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sheet silicates
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mica group
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biotite (2)
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sulfides
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pyrrhotite (1)
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Primary terms
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absolute age (2)
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biogeography (3)
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Canada
-
Western Canada
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British Columbia
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Princeton British Columbia (3)
-
-
-
-
Cenozoic
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Quaternary
-
Pleistocene
-
Lake Missoula (1)
-
-
-
Tertiary
-
Florissant Lake Beds (1)
-
Paleogene
-
Eocene
-
Green River Formation (2)
-
lower Eocene
-
Ypresian (1)
-
-
middle Eocene
-
Laney Shale Member (1)
-
-
-
-
-
-
Chordata
-
Vertebrata
-
Pisces
-
Osteichthyes
-
Actinopterygii
-
Teleostei (2)
-
-
-
-
Tetrapoda
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Aves
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Neornithes (1)
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-
-
-
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crust (1)
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education (1)
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faults (2)
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foliation (1)
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geochemistry (1)
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geochronology (2)
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geomorphology (1)
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geophysical methods (1)
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glacial geology (1)
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ichnofossils (1)
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igneous rocks
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hypabyssal rocks (1)
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plutonic rocks
-
granites (1)
-
granodiorites (1)
-
-
porphyry (1)
-
volcanic rocks
-
andesites (1)
-
basalts (1)
-
dacites (1)
-
rhyolites (1)
-
-
-
inclusions (1)
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intrusions (2)
-
Invertebrata
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Arthropoda
-
Mandibulata
-
Insecta
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Pterygota
-
Neoptera
-
Endopterygota
-
Coleoptera (1)
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Hymenoptera (1)
-
Mecoptera (1)
-
Neuroptera (1)
-
-
-
-
-
-
-
-
magmas (2)
-
Mesozoic
-
Cretaceous
-
Dakota Formation (1)
-
Upper Cretaceous
-
Hell Creek Formation (1)
-
-
-
-
metal ores
-
gold ores (1)
-
-
metals
-
rare earths (1)
-
-
metamorphic rocks
-
gneisses (2)
-
metasedimentary rocks (2)
-
mylonites (1)
-
-
metamorphism (1)
-
metasomatism (1)
-
North America
-
Kootenay Arc (1)
-
North American Cordillera (1)
-
Okanogan Range (5)
-
Omineca Belt (1)
-
-
paleoclimatology (4)
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paleoecology (5)
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paleogeography (5)
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paleontology (4)
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Paleozoic
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Cambrian
-
Lardeau Group (1)
-
-
lower Paleozoic (1)
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Permian (1)
-
-
palynomorphs
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miospores
-
pollen (1)
-
-
-
paragenesis (1)
-
petrology (2)
-
phase equilibria (1)
-
Plantae
-
Pteridophyta (1)
-
Spermatophyta
-
Angiospermae
-
Dicotyledoneae
-
Alnus (3)
-
Betula (2)
-
Hamamelididae (1)
-
Rosidae (1)
-
-
Monocotyledoneae
-
Palmae (1)
-
-
-
Gymnospermae
-
Coniferales
-
Pinaceae
-
Abies (2)
-
-
-
-
-
-
sedimentary rocks
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carbonate rocks (1)
-
-
sedimentary structures
-
planar bedding structures
-
rhythmic bedding (1)
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rhythmite (1)
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varves (1)
-
-
-
sedimentation (2)
-
sediments
-
clastic sediments
-
clay (1)
-
-
-
stratigraphy (1)
-
structural geology (1)
-
tectonics (4)
-
tectonophysics (1)
-
United States
-
Colorado
-
Park County Colorado (1)
-
-
Iowa
-
Floyd County Iowa (1)
-
-
Kansas
-
Ellsworth County Kansas (1)
-
-
New York
-
Erie County New York (1)
-
-
North Carolina
-
Beaufort County North Carolina (1)
-
-
North Dakota
-
Slope County North Dakota (1)
-
-
Ohio
-
Butler County Ohio (1)
-
Hamilton County Ohio (1)
-
-
Oregon
-
Wheeler County Oregon (1)
-
-
Utah
-
Uintah County Utah (1)
-
-
Washington
-
Ferry County Washington (25)
-
Okanogan County Washington (3)
-
Stevens County Washington (4)
-
Whatcom County Washington (1)
-
-
Western U.S. (1)
-
Wyoming
-
Lincoln County Wyoming (1)
-
-
-
-
rock formations
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Fort Union Formation (1)
-
-
sedimentary rocks
-
sedimentary rocks
-
carbonate rocks (1)
-
-
-
sedimentary structures
-
sedimentary structures
-
planar bedding structures
-
rhythmic bedding (1)
-
rhythmite (1)
-
varves (1)
-
-
-
-
sediments
-
sediments
-
clastic sediments
-
clay (1)
-
-
-
GeoRef Categories
Era and Period
Epoch and Age
Date
Availability
Ferry County Washington
Early Eocene (Ypresian) birds from the Okanagan Highlands, British Columbia (Canada) and Washington State (USA)
BIOFILMS MEDIATE THE PRESERVATION OF LEAF ADPRESSION FOSSILS BY CLAYS
Biotic processes in the Okanagan Highlands floras: possible evidence of hybridization in plants adapting to a temperate forest
The Eocene Apex of Panorpoid Scorpionfly Family Diversity
A Diverse New Assemblage of Green Lacewings (Insecta, Neuroptera, Chrysopidae) from the Early Eocene Okanagan Highlands, Western North America
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.