Browse

The most recent glacial period span in the interval 110,000 to 10,000 years ago. Recent geomorphologic studies in the Eastern Thracian plane have shown significant change in the sedimentation rates since the Younger Driass (between 10,800 and 9500 BC), which may provide a new inside on the climatic evol ution of the region. It was found that all local rivers are in an aggradation phase, depositing up to 3 m thick mudstone deposits on top of a colder climate’s well-washed, coarse sandstones. The aggradation resul...

A horizon of carbonate minerals underlies the organic soils of the Thracian plane. This horizon has irregular thickness, density and mineral composition. In the world scientific literature, such horizons are usually described as pedogenic calcretes. The growth of the carbonate layer depends on many factors; among them are the global climate change, the acidity of the atmospheric precipitates and the agricultural practices. The carbonate layer is very significant to the biological productivity of the soil. It tends...