Left/Top: Crnica, eastern Serbia. Right/Bottom: River Itchen Channel, Itchen Stoke, Hampshire. Photograph by Peter Trimming, 22 October 2011. CC BY-SA 2.0. Wikimedia Commons.
There is something about certain limestone spring creeks that has always reminded me of the English chalk streams. Perhaps it is the exceptionally clear water, the limestone surroundings, or the quiet character of a stream whose life begins underground.
I have often wondered how closely a small spring creek in eastern Serbia, in a landscape I know intimately, might resemble celebrated English rivers such as the Test and the Itchen. The simplest place to start is pH.
Published measurements from my favourite limestone spring in eastern Serbia give pH values between 7.16 and 7.50, which means water that is close to neutral or mildly alkaline. English chalk streams generally run a little higher, often around 7.4-8.0, though seasonal fluctuations can be considerable. The ranges overlap more than I expected, and the upper end of the Serbian spring reaches the lower end of the chalk streams. pH is only one measure, but it is a revealing first one.
The similarity makes sense, because both types of water are shaped by carbonate geology. Chalk streams draw their chemistry from water moving through chalk aquifers, while Balkan karst springs emerge from extensive limestone formations. In both, dissolved calcium and bicarbonate give the water its mineral-rich character.
Of course, a karst spring creek is not a chalk stream in the geological sense. The aquifers, landscapes, and hydrology are different.
Both kinds of stream also begin underground. Rain soaks into carbonate rock and returns to the surface as spring water. Chalk is itself a soft, porous form of limestone, so the two rocks are close relatives, although a karst aquifer, with its fissures and channels, tends to react to rain more quickly than chalk does. On this stream, the rise does not come at once. There is a lag after the rain, and how long it lasts and how high the water climbs depend on how much has fallen. Still, this groundwater origin gives both streams their clarity and a temperature that stays cooler in summer and milder in winter than that of rain-fed rivers.
I find this comparison particularly appealing. In a remote corner of the Balkans, surrounded by forests and limestone mountains, one can find some of the same fundamental qualities that make the English chalk streams so distinctive. Perhaps we should look beyond geographical labels when thinking about rivers, since two very different landscapes can produce waters with surprisingly similar character.
For a fisherman who has spent much of his life beside limestone spring creeks, the Crnica among them, discovering these connections is another reminder of how much there is still to learn from the waters we know best.









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