How would you describe soil with a high degree of 'very friable' consistence?

A soil described as having a high degree of "very friable" consistence is characterized by its ability to break apart easily under minimal pressure. This means that when a small amount of force is applied, such as when it is squeezed between fingers, the soil readily separates into smaller pieces. This property indicates that the soil is loose, crumbly, and well-aerated, which generally supports good root growth and drainage.

The term "friable" specifically refers to the texture and structure of the soil that allows for this easy breakdown. Friable soils tend to have more porous structures, which enhance water infiltration and root penetration. This characteristic is especially beneficial in agricultural practices, as it allows for efficient planting and cultivation.

In contrast, soils that clump together strongly, remain solid under pressure, or require significant pressure to change are indicative of different consistencies, such as compacted or heavy clay soils, which do not exhibit the same desirable properties as friable soils.