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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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North America
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Appalachians
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Appalachian Plateau (1)
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United States
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Ohio River (1)
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Pennsylvania
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Allegheny County Pennsylvania
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Pittsburgh Pennsylvania (1)
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commodities
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clay deposits (1)
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coal deposits (1)
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construction materials
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building stone (1)
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dimension stone (1)
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granite deposits (1)
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limestone deposits (1)
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marble deposits (1)
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metal ores
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iron ores (1)
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geologic age
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Paleozoic
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Carboniferous
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Pennsylvanian
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Conemaugh Group (1)
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Middle Pennsylvanian
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Allegheny Group (1)
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Monongahela Group (1)
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Dunkard Group (1)
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Permian (1)
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Primary terms
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clay deposits (1)
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coal deposits (1)
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construction materials
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building stone (1)
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dimension stone (1)
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foundations (1)
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granite deposits (1)
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limestone deposits (1)
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marble deposits (1)
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metal ores
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iron ores (1)
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North America
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Appalachians
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Appalachian Plateau (1)
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-
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Paleozoic
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Carboniferous
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Pennsylvanian
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Conemaugh Group (1)
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Middle Pennsylvanian
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Allegheny Group (1)
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Monongahela Group (1)
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Dunkard Group (1)
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Permian (1)
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sedimentary rocks
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chemically precipitated rocks
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chert (1)
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coal (1)
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United States
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Ohio River (1)
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Pennsylvania
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Allegheny County Pennsylvania
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Pittsburgh Pennsylvania (1)
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sedimentary rocks
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sedimentary rocks
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chemically precipitated rocks
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chert (1)
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coal (1)
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Abstract This guidebook chapter outlines a walking tour that provides an introduction to the geological, archaeological, and historical setting of Pittsburgh, with an emphasis on the use of local and imported geologic materials and resources in the eighteenth and nineteenth centuries. The focus is on downtown Pittsburgh, the low-lying triangle of land where the Monongahela and Allegheny Rivers join to form the Ohio River, and Coal Hill (Mount Washington), the escarpment along the Monongahela River to its south. Topics include the importance of—and concomitant effect of—historic coal use; use of local and imported geologic materials, including dimension stone used for buildings and gravestones, and chert used for gunflints and millstones; the frontier forts built at the site; and the ubiquitous landslides along Coal Hill.