When Rob Cunningham was rising up in Norfolk, England, he would generally go fishing with a pal on the banks of a river the place the water was crystal clear. “I used to be a garbage fisherman,” he says. “I by no means actually caught any, however I’d see a great deal of trout.” The spot on the River Wensum was idyllic, he says, with strands of water-crowfoot—a sort of ranunculus—blooming on the water’s floor.

It was solely years later, as Cunningham was finding out environmental science in one other area of England, that he would come to understand how uncommon rivers just like the Wensum actually are. Generally known as “chalk streams”—a globally uncommon kind of waterway discovered nearly solely in England—these rivers’ particular options each create uncommon biodiverse habitats and make them uniquely weak.
At the moment, because the director of The Nature Conservancy’s Resilient Watersheds program in Europe, Cunningham is attempting to guard rivers like these all through Norfolk by way of a water fund.
Launch in 2024, the Norfolk Water Fund is a collaboration of a number of native and regional companions that pairs traders, residents and companies to finance tasks designed to guard the amount and high quality of the world’s water. (Learn extra concerning the water fund within the newest problem of Nature Conservancy journal.)
However what precisely are the chalk streams that run by way of that area?

Burbling up from aquifers fashioned in chalk layers that date again to the Cretaceous Interval, these rivers exist solely the place chalk sits near the Earth’s floor. That’s why of the 200-odd recognized chalk streams on the earth, practically all of them are present in England, the place 66 million years in the past a shallow seabed collected the skeletons of aquatic creatures—the makings of chalk.
About 15,000 years in the past retreating glaciers carved channels into this previous layer of chalk. Rainfall seeped into this chalk aquifer and ultimately emerged as springs that also right now present a lot of the water in these streams.

“It could take something from a matter of years to a long time for rainwater to maneuver by way of the chalk after which emerge into the river,” Cunningham says. “So that you’ve obtained this large filtration system.” The consequence, when the streams are wholesome, is obvious water, low vitamins, remarkably constant temperatures and a gravel creek backside left over from the retreat of glaciers within the final Ice Age.
These circumstances have made these rivers very best habitats for trout and at one time, Atlantic salmon too. The endangered water vole makes use of chalk streams and bugs just like the banded demoiselle thrive close to them. In the summertime, blooming water-crowfoot point out a wholesome chalk stream. In southern England, some chalk streams have turn out to be world-renowned for his or her flyfishing alternatives. They are often, as Cunningham put it, idyllic and sluggish.

“We frequently take into consideration rivers being formed by storm occasions and floods,” he says. “However with a chalk stream, all of that carving occurred on the Ice Age. They’re truly actually low power, in order that they don’t have sufficient power to reshape themselves.”
All of these elements make them weak to air pollution and improvement. The lack of bushes alongside riverbanks and the rise in intensive agriculture close by has led to extra water working into the streams, carrying silt and vitamins from inorganic fertilizers. As a result of the aquifers maintain a lot clear water, they’ve been over-exploited. And in contrast to many rivers that, although straightened, carve new paths by way of erosion, chalk streams aren’t robust sufficient to return to their unique paths on their very own.


Restoring these chalk streams includes utilizing historic maps to study the place the rivers as soon as traveled. “It’s primarily like a detective story,” Cunningham says, “an actual mixture of artwork and science and historical past.”
Chalk stream restorers use these maps to assist plan the place to “re-wiggle” artificially straightened streams. In addition they use hydrological fashions to assist resolve how deep to dig a channel. In some circumstances, they’ll take soil cores to establish the unique channels: As a result of the streambeds have been first dug 50,000 years in the past as glaciers left behind gravel, some restorers have recognized these unique channels partly by discovering that gravel once more.
In Norfolk this restoration work includes TNC together with residents, the water utility, the native council and lots of different companions. It includes creating panorama buffers, holding water in “leaky” ponds the place soil overlays a chalk aquifer, planting bushes and extra.
The method can look worse earlier than it will get higher. “There’ll be mud in every single place and it seems such as you’ve created a catastrophe,” Cunningham says. “However then it’s superb how shortly life comes again.”
