The term refers to a soil type characterized by a balanced composition of sand, silt, and clay, sought after in a localized geographic area. This soil blend typically comprises approximately 40-50% sand, less than 20% clay, and the remaining portion as silt. A sample exhibiting these characteristics would drain well yet retain sufficient moisture to support plant growth.
Its balanced properties make it desirable for agriculture and horticulture. The presence of significant sand content prevents waterlogging, while the clay and silt fractions provide nutrient retention. Historically, regions with this soil composition have often been centers of agricultural productivity due to its favorable attributes for a wide range of crops.
