Oolitic ironstone – Stanion Lane Railway
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Fact sheet
Description: 

Northampton Sand Ironstone is a sedimentary rock unit of Jurassic age that extends from Lincoln to Towcester in Northamptonshire, and this sample is from Stanion Lane railway, near Corby. This rock was a major source of iron ore for the steel manufacturing towns of Corby and Kettering. The ironstone has been secondarily enriched by weathering which caused dissolution of calcium and iron carbonate, and oxidation of the iron minerals to limonite, increasing the iron content of the rock.

In thin section this oolitic ironstone is composed of spherical concretions (ooids), cemented by fine grained sparry calcite. Note that several of the ooliths were lost during the preparation of the thin section. The ooliths formed in shallow, well-stirred water in which chemical precipitation of iron compounds predominated. Ooliths consist of concentric growths around a nucleus, which may be a shell fragment, quartz grainor algal pellet. The mineral chamosite is the most common constituent of the ooliths. Siderite and limonite are secondary iron-rich species that replace chamosite, and also authigenic magnetite and pyrite, contributing to the elevated iron content of the rock.

In Place
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Location description: 
Stanion railway line near Corby, Northamptonshire
Accuracy:
Location precision: 
Good
Timescale:
Timescale: 
Jurassic
Ma = Millions of years ago
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sedimentary
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