What can be said about New England soils?

New England soils can generally be classified as young due to their geological history and formation processes. The region has been influenced by glacial activity which shaped the landscape and deposited various types of sediments. These processes have not allowed for extensive soil development over time, particularly in terms of horizon formation and significant mineral weathering that typically characterize older soils.

Young soils are typically characterized by their mineral composition and the relatively recent deposition of these materials. In New England, you can find a range of soil types, but many of them are formed from glacial till or outwash, which means they may show signs of limited weathering relative to older soils found in more stable landscapes. Thus, considering this geological context, it is accurate to classify New England soils as generally young.