Abstract
HE GEOCHEMICAL DIVERSITY OF LACUSTRINE SEDIMENTS OF THE SUCHEDNIÓW WATER RESERVOIR (ŚWIĘTOKRZYSKIE VOIVODESHIP, POLAND) - PRELIMINARY RESULTS
Highlights
The Holy Cross Mountains area is known from the Prehistorical metallurgical activity during the Roman period [1], [2], as well in the modern period [3]
In the Middle Ages, many forges and water mills were built on the Holy Cross Mountains rivers, on which many smaller ponds were built as the part of hydrotechnical structure
The Suchedniów water reservoir was built on the former forge industrial pond area (Fig. 2) and part of the former Kamionka floodplain
Summary
The Holy Cross Mountains area is known from the Prehistorical metallurgical activity during the Roman period [1], [2], as well in the modern period [3]. In the Middle Ages, many forges and water mills were built on the Holy Cross Mountains rivers, on which many smaller ponds were built as the part of hydrotechnical structure. The ore was processed in blast furnances and forges that operated in the Old Polish Industrial District area. In Kamionka, as on many other rivers of this region, they were created anthropogenic small-scale water retention system (ASWRS)[5]. In the place of some of the old ponds were built bigger reservoirs, just like at Suchedniów [6]. The Suchedniów water reservoir was built in 1974 in the middle section of Kamionka
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