Here's a breakdown of the different types of transported soils:

* Alluvial soil: This is the most common type of transported soil. It's formed from sediment deposited by rivers, streams, or floods. Alluvial soils are typically fertile and well-drained due to the constant movement of water. They're often found in river valleys and floodplains.

* Eolian soil: This type of soil is formed from sediment transported by wind. It's often found in deserts and other dry areas where wind erosion is prevalent. Eolian soils can be sandy, loamy, or clay-like, depending on the size of the transported particles.

* Glacial till: This soil is formed from sediment deposited by glaciers. It's typically a mixture of rock fragments, sand, silt, and clay. Glacial till is often poorly sorted and can be very heavy.

* Colluvial soil: This soil is formed from sediment transported by gravity, often down slopes. Colluvial soils are typically found at the base of hills and mountains.

The specific characteristics of a transported soil depend on several factors, including:

* Source of the sediment: The composition of the parent material will influence the soil's texture, nutrient content, and pH.

* Mode of transport: The way the sediment is transported (e.g., water, wind, gravity) will affect the sorting and size of the particles.

* Climate: The climate of the region will influence the weathering and decomposition processes that occur in the soil.

* Time: Over time, transported soils can develop unique characteristics as they mature.

Overall, transported soils are important for agriculture and human development because they often have good drainage, fertility, and depth. They're also essential for supporting ecosystems in various environments.