Where are pedocals typically found?

Pedocals are soil types that are notably found in drier regions, particularly in grasslands and brush areas of Western North America. These soils generally develop in environments characterized by limited moisture and are often associated with regions that experience low rainfall. The accumulation of calcium carbonate is a key feature of pedocals, resulting from the process of evaporation and the leaching of nutrients, which occurs in these semi-arid conditions. This specific climate contributes to the formation and characteristics of pedocals, making them specifically suited to the grasslands and brush ecosystems found in this region.