A three-year study (1991-1993) on the chemistry of streams was carried out in two valleys of different bedrock in the Polish Tatra Mountains. Significant seasonal fluctuations in the concentration of most of the studied elements of the granitic Waksmundzki and carbonate Miętusi Streams were observed. The chemistry of the Miętusi Stream was dominated by calcium and magnesium ions and the Waksmundzki Stream by sulphate ions. The drawing of general conclusions on changes in the stream chemistry over the last 30 years is impossible because of the different analytical methods used and only a single samplings of the stream water taken by the investigation carried out in the 60’s.
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