Abstract
The role which soil plays as an indicator of landscape stability is discussed. The influential model and concepts developed by Butler (1959) are used as the framework through which soils of the past can be studied. Although only a relatively few Quaternary depositional sequences are observable on the Maltese Islands almost without exception, they all contain palaeosoil material. The specific sites discussed (Marfa ridge, Santa Maria Bay (Comino), St. Thomas Bay, Għar Lapsi and Ċirkewwa) reveal how palaeosoils can be used to provide insights into differing aspects of landscape history. In addition, buried materials can also provide information about the nature of soil.
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Farres, P. (2019). Palaeosoils: Legacies of Past Landscapes, with a Series of Contrasting Examples from Malta. In: Gauci, R., Schembri, J. (eds) Landscapes and Landforms of the Maltese Islands. World Geomorphological Landscapes. Springer, Cham. https://doi.org/10.1007/978-3-030-15456-1_12
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