Which soil type would likely be found in areas with high annual precipitation and poor drainage?

The correct answer is wet-climate soil because it forms in environments characterized by high levels of annual precipitation. In such regions, the abundance of rainfall contributes to saturated conditions that inhibit proper drainage. As a result, organic matter and minerals can accumulate in the soil, leading to the development of specific characteristics associated with wet-climate soils. These soils often have a darker color due to organic content and can exhibit gleying—a process that occurs when waterlogged conditions limit oxygen availability, affecting the soil's chemical properties.

While other soil types may also have certain features that may be observed in high precipitation areas, they do not encompass the defining traits of wet-climate conditions as effectively. For example, dry-climate soils are typically found in arid regions and are characterized by low moisture, making them unsuitable for areas of high rainfall. Clayey soils, while they can retain water due to their fine texture, do not specifically indicate high precipitation zones without consideration for surrounding drainage conditions. Sandy soils drain quickly and are commonly found in drier environments, which further emphasizes their incompatibility with high precipitation and poor drainage scenarios.