Publication: Charcoal fragments of Alpine soils as an indicator of landscape evolution during the Holocene in Val di Sole (Trentino, Italy)
Charcoal fragments of Alpine soils as an indicator of landscape evolution during the Holocene in Val di Sole (Trentino, Italy)
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Favilli, F., Cherubini, P., Collenberg, M., Egli, M., Sartori, G., Schoch, W., & Haeberli, W. (2010). Charcoal fragments of Alpine soils as an indicator of landscape evolution during the Holocene in Val di Sole (Trentino, Italy). Holocene, 20(1), 67–79. https://doi.org/10.1177/0959683609348850
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Subalpine and Alpine soils in Val di Sole (Trentino, Italy) have been investigated in order to reconstruct vegetation changes and human impact during the Holocene period. Archaeological findings have demonstrated that Alpine sites have been populated since pre-historical times. Humans have had a great impact on the natural landscape evolution. One of the most-used tools has been fire. The use of fire has enabled the landscape to be cleared to provide new pastures for grazing and also to allow it to be used for agricultural purposes. T
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Favilli, F., Cherubini, P., Collenberg, M., Egli, M., Sartori, G., Schoch, W., & Haeberli, W. (2010). Charcoal fragments of Alpine soils as an indicator of landscape evolution during the Holocene in Val di Sole (Trentino, Italy). Holocene, 20(1), 67–79. https://doi.org/10.1177/0959683609348850