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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Southern Africa
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South Africa
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Eastern Cape Province South Africa
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Cape Town South Africa (1)
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Commonwealth of Independent States
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Russian Federation
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Europe
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dimension stone (2)
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granite deposits (7)
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ornamental materials (2)
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geologic age
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Paleozoic
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Carboniferous
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Conemaugh Group (1)
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Precambrian
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igneous rocks
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metamorphic rocks
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metamorphic rocks
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hornfels (1)
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slates (1)
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Primary terms
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Africa
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Southern Africa
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South Africa
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Eastern Cape Province South Africa
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Cape Town South Africa (1)
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Asia
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Far East
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Singapore (1)
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Middle East
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Turkey
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Istanbul Turkey (1)
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Canada
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Eastern Canada
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Newfoundland and Labrador
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Newfoundland
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Burin Peninsula (1)
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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 (3)
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crushed stone (1)
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dimension stone (2)
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crust (1)
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earthquakes (1)
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Europe
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Leningrad Oblast Russian Federation
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Saint Petersburg Russian Federation (1)
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Southern Europe
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Iberian Peninsula
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Spain
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Galicia Spain (1)
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Western Europe
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Scandinavia
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Finland (1)
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granite deposits (7)
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ground water (1)
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igneous rocks
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plutonic rocks
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granites
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rapakivi (1)
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intrusions (2)
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limestone deposits (2)
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magmas (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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metamorphic rocks
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hornfels (1)
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slates (1)
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metamorphism (1)
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mining geology (1)
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North America
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Appalachians
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Appalachian Plateau (1)
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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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petrology (1)
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Precambrian
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upper Precambrian
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Proterozoic
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Neoproterozoic (1)
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rock mechanics (1)
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sandstone deposits (1)
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sedimentary rocks
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chemically precipitated rocks
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chert (1)
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clastic rocks
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sandstone (1)
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coal (1)
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sediments
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clastic sediments
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dust (1)
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tectonics (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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waste disposal (1)
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weathering (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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clastic rocks
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sandstone (1)
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coal (1)
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sediments
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sediments
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clastic sediments
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dust (1)
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granite deposits
Rapakivi granite in the architecture of St Petersburg: a potential Global Heritage Stone from Finland and Russia
Abstract Rapakivi granites were in use during the Middle Ages in Finland. Their most spectacular use, however, was for structures built in St Petersburg between 1760 and 1917. Remarkable examples are the majestic and slender Alexander Column and the 112 columns of St Isaac's Cathedral. All Rapakivi granite was extracted from the Wiborg Rapakivi granite batholith in several quarries around the municipality of Virolahti in SE Finland (old Russia). Today, the 1640 Ma-old Wiborg batholith is the most important area for natural stone production in Finland and in the Leningrad region, Russian Federation. The main quarried stone varieties of Rapakivi granite (Baltic Brown, Baltic Green, Carmen Red, Karelia Red, Eagle Red and Balmoral Red) are regularly produced in large quantities in Finland for the global stone market due to the stone's unique qualities. Examples of applications in Rapakivi granite from Finland can be found in the USA, China, South Africa, the UK, Italy, Austria, Ireland, Spain and Germany as well as in Scandinavia and Russia. There are also quarries near Vyborg, the Russian Federation: Vozrozhdenie and Ala-Noskua.
Abstract Cape Town was founded in 1652 and many of its historical buildings are constructed of local natural stone. Malmesbury Group slate was exploited from 1666 and used to build Cape Town Castle, which is the oldest building in Cape Town. Two other local stones, Cape granite and Table Mountain sandstone were utilized for buildings from 1850. A medium-grained granite named Paarl Grey was exploited from an area adjacent to the town of Paarl, 50 km east of Cape Town, from 1890. This granite is the most extensively-used natural stone in Cape Town. The resource fields of natural stone near Cape Town, namely Malmesbury Group slate, Cape granite and Table Mountain sandstone, lie within the Table Mountain National Park and Robben Island World Heritage Site and can no longer be exploited, but similar resource fields occur outside Cape Town. Paarl Grey granite is still extracted at one quarry and, despite part of the resource field lying within the Paarl Mountain Nature Reserve, there are still sufficient quantities of stone available. From an international perspective, the heritage stones of Cape Town, South Africa, are best considered as having national significance.
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.