What best describes fissured soil?

Fissured soil refers to soil that has cracks or breaks in its structure. This fissuring typically occurs due to factors such as drying, shrinking, or significant changes in moisture content. Such breaks in the soil can result in poor stability and can affect its ability to retain moisture and nutrients, making it less suitable for certain agricultural applications and potentially hazardous in construction settings.

Understanding the characteristics of fissured soil is important in evaluating soil stability and determining appropriate site management practices, particularly in the context of construction and safety standards. Recognizing that fissured soil is prone to breaking up helps in assessing conditions that could pose risks in both agricultural and construction environments.