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- W2316231755 abstract "The nodule to which this paper refers was discovered at Kinghornness during the excavations rendered necessary by the fortifications at present being raised for the defence of the Firth of Forth.The material was enclosed in a nest or nodule, and was found at a depth of 15 feet from the surface of the ground, and embedded 5 feet in hard trap-rock.The rock in which the nodule was obtained was sound, there being no crack or fissure observable for several feet round the nest, but at a point some distance below the nodule the section shows a series of small veins or fissures running through the rock in various directions, and averaging ![Graphic][1] of an inch in breadth. The analysis of the rock gave the following results, calculated to percentages:—1. On treating the pulverised sample with hydric chloride (HCl), and subjecting the mixture to a prolonged low heat, it was found that 29.73 per cent. of the substance dissolved in the acid. The detailed results of the analysis of this solution are as follows:—2. The portion insoluble in acids was then fused with a flux and the following results obtained from the after-solution in acid:—The rocks lying next to the trap were also analysed, and gave results as stated below:—1. Soluble in Hydric Chloride (HCl)—2. Matter insoluble in Hydric Chloride (HCl), fused with flux and then treated with acid—The nodule when broken consisted of—1. An outer coating of hard rock;2. An inner lining [1]: /embed/inline-graphic-1.gif" @default.
- W2316231755 created "2016-06-24" @default.
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- W2316231755 date "1879-01-01" @default.
- W2316231755 modified "2023-09-29" @default.
- W2316231755 title "On the chemical composition of a nodule of ozokerite found at Kinghornness" @default.
- W2316231755 doi "https://doi.org/10.1144/transed.3.2.272" @default.
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