Right off the bat I’ll give three examples of what I have seen described as the most fertile soils, the best soils, or the most ideal soils out there.
- Volcanic soil
Typically in Mediterranean or tropical climates (parts of Italy, Hawaii), but sometimes in the subtropics and temperate zones (eg. parts Japan and New Zealand).
Volcanic soil is touted as superior due to several different factors. The soils are geologically extremely young, so they are highly chemically active, both being still rapidly weathering and having a high cation exchange capacity. Additionally, the soils are very “light.” Relatively large particle size, combined with a high proportion of glasses and similar materials and an extremely high amount of porosity, mean that the soils are physically light, drain very quickly, but still hold a lot of water.
- Chernozem
Some areas of the US and Canada, and vast areas in Ukraine and Russia, with scattered smaller areas Patagonia, China, etc. Always in cold temperate zones.
Chernozem (Russian, чернозем, literally just meaning “black soil”) has the highest level of organic matter of any commonly occurring soil outside of wetlands and certain alpine environments. These soils have very high nutrient loading and availability, can hold enormous amounts of water, and are typically extremely deep. They are not, however, especially well-drained, and can remain water-logged for long periods of time.
- Juniper Level Botanic Garden
A special mention. Juniper Level Botanic Garden, just outside of Raleigh, NC, is an interesting case study in soil conditioning: they grow slightly over 21,000 species and varieties of plants, all using the exact same soil mixture and pH. That mixture is 50% permatill (expanded slate), 25% compost, 25% native soil, kept at a pH of 6.2 to 6.5. They, in the same soil, are growing orchids, agaves, proteas, ericaceous plants, bananas, cacti, and pitcher plants, among others.
Some food for thought.