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Primary terms
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Africa
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East Africa
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Kenya
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absorption
Visible-Near Infrared–Short-Wave Infrared Spectroscopy and Mineral Mapping of Hydrothermal Alteration Zones at the Brejuí W-Mo Skarn Deposit, Seridó Mobile Belt, Borborema Province, Brazil
Wave vector and field vector orientation dependence of Fe K pre-edge X-ray absorption features in clinopyroxenes
Thomsen-type parameters and attenuation coefficients for constant- Q transverse isotropy
Hidden hydrosphere under the Caspian Sea: Geophysical evidence and sea-level influence
Muttalip green clay and its ultraviolet and infrared absorption and reflection
Cryogenic heat capacity measurements and thermodynamic analysis of lithium aluminum layered double hydroxides (LDHs) with intercalated chloride
Functional Montmorillonite/Polymer Coatings
Water in omphacite fingerprints the thermal history of eclogites
Some Features of Quantitative Analysis of Rock-Forming Minerals Using a JXA-8230 Electron Probe Microanalyzer
Synthesis, Characterization, and Performance Evaluation of Starch-Based Degradable Temporary Plugging Agent for Environmentally Friendly Drilling Fluid
Impact Assessment of Artificial Recharge Structures on Kakatiya University Campus, Warangal Urban District, Telangana
Removing tar and nicotine from mainstream cigarette smoke using sepiolite-modified filter tips
Python Earth Engine API as a new open-source ecosphere for characterizing offshore hydrocarbon seeps and spills
Abstract By virtue of its use in iconic monuments and historic buildings in the USA, Cockeysville marble, a dolomitic to calcitic lower Paleozoic (Cambrian/Ordovician) marble quarried in Baltimore County and adjacent areas in Maryland, is proposed as a potential Global Heritage Stone Resource. The most important use of this stone was for the Washington Monument in Washington, DC whose construction began in 1848; the second most important use was for the 108 columns of the United States Capitol's wings, completed in 1868. It was also used for two of the oldest major marble monuments in the USA, Baltimore's Battle Monument (dedicated in 1827) and Washington Monument (completed in 1829), as well as Baltimore's City Hall, Buffalo's Adkins Art Museum, Detroit's Fisher Building and parts of St Patrick's Cathedral in New York City. During the nineteenth century white Cockeysville was most desired, but a colourful variety, Mar Villa marble, was also used in the first decades of the twentieth century. Cockeysville marble is no longer quarried for dimension stone. All Cockeysville used outdoors has weathered to a lesser or great extent, but early testing indicating that the dolomitic marble would be more durable has proved to be true.
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.