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- W2142377820 abstract "The towered 'pagoda' rock formations of the north-western Blue Mountains, west of Sydney, have a heartland of about 600 km2, mostly at around 1000 metres altitude in Banks Wall and Burra Moko Head Sandstones. The pagodas are of two types: the 'platy pagodas' are generally stepped-cones in shape, with semi-regular ironstone bands, whereas the 'smooth pagodas' display less ironstone bands and are similar to many slickrock slopes found elsewhere. The platy pagodas however are an uncommon and significant geomorphic landscape feature, and are distinguished by the extent and regularity of their ironstone banding. The formation of the ironstone banding has involved the movement of iron in solution and its precipitation to form resistant bands, swirls and pipes. Questions remain as to how the ironstone banding formed, however 'roll fronts' of reaction between reduced Fe2+-rich water and oxygenated water may best explain the amazing ironstone shapes. The geoheritage value of the pagodas is significant, but is threatened by activities such as longwall coal mining. The pagodas and the associated slot canyons of the Blue Mountains are ideal candidates for future geological and geomorphological research." @default.
- W2142377820 created "2016-06-24" @default.
- W2142377820 creator A5030286684 @default.
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- W2142377820 date "2011-01-01" @default.
- W2142377820 modified "2023-09-26" @default.
- W2142377820 title "The geoheritage and geomorphology of the sandstone pagodas of the North-western Blue Mountains Region (NSW)" @default.
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