Which of the following statements regarding Type A soils is true?

Type A soils are characterized by their high infiltration rates and low runoff potential. This is primarily due to their fine texture and structure, which allows water to percolate through them more easily. The high infiltration capacity reduces the likelihood of surface runoff, making these soils effective in managing water and minimizing erosion. Understanding the characteristics of Type A soils is essential for effective erosion control and sedimentation management, as these soils can help in retaining water and reducing the impact of runoff in landscapes.

Contextually, the other options describe attributes not typically associated with Type A soils. For instance, soils with low infiltration rates and high runoff potential would be more representative of clayey Type C soils, which tend to hold water and create surface runoff. The mention of moderate infiltration rates and variable runoff potential aligns more closely with Type B soils, which possess intermediate characteristics. Lastly, while Type A soils can indeed be found in various locations, describing them as typically found in urban areas does not accurately reflect their natural occurrence, as they are more commonly associated with undisturbed, natural landscapes. Understanding these distinctions is crucial for application in sedimentation and erosion control practices.