| Riserva Naturale dei Calanchi di Atri |
|
|
|
|
The calanchi ('badlands') in the WWF nature reserve at Atri represent one of the most fascinating landscapes on the Adriatic Sea. They are also called 'Bolge' or 'Scrimoni' and they are a geomorphological phenomenon which is due to continuous soil erosion. Deforestation in the past as well as climatic factors like aridity and hydric stress lead to the erosion of the soil that consists of clay, silt and sand. The so-called 'badlands' are dry areas with sparse vegetation that are characterized by high rates of erosion which creates narrow ravines, gullies, knife-sharp ridges and crests and interesting sculptures and pinnacles.
The following prerequisites are important for the evolution of a calanco:
Clay is dry and powder-like with lots of cracks on the surface. When it gets wet, you can easily form it. The existing minerals don't provide many nutrients for the plants which can hardly develop on this ground. That's why the drops of heavy rainfalls cause the detachment of small clay particles. The water quickly flows from the surface into the cracks and carries away these clay particles creating small water channels that become larger and deeper. In the course of time they form a miniature hydrographic network of channels and gullies which finally furrow and erode the whole surface of the slope. The small and light clay particles, washed away by the rain, accumulate at the foot of the calanco and are finally taken to the sea by the water.
|





