Portal de Periódicos da CAPES

Tin Mining and Sediment Supply to the Ringarooma River, Tasmania, 1875–1979

1987; Wiley; Volume: 25; Issue: 1 Linguagem: Inglês

10.1111/j.1467-8470.1987.tb00540.x

1467-8470

A. D. Knighton,

Soil erosion and sediment transport

Tin mining, based largely on alluvial tin deposited along the line of the ancestral Ringarooma, began in 1875 and reached a peak in the period 1905‐9. Output declined thereafter and, following a brief recovery during the Second World War, had virtually ceased by 1981. Neither the methods, location nor level of production remained constant during the mining era. The widespread use of hydraulic sluicing and the proximity of many mines to the main river were major factors contributing to the high rate of sediment supply, with the Briseis mine at Derby being the dominant source. Based on data from published and unpublished papers, and mine records, the variable nature of that supply was estimated using a procedure which takes account of the effects of storage and changing practices. Many input points supplied material but the overall pattern is one in which downstream reaches made later starts and reached later peaks, suggesting that they will continue to experience the effects of an increased sediment load for some time.