topsoil
The dark, top layer of soil where most plants grow.
Topsoil is the uppermost layer of soil, usually the top 2 to 8 inches, where most of the earth's biological activity happens. This dark, crumbly layer is where plants sink their roots, where earthworms tunnel and aerate the ground, and where fallen leaves and dead plants break down into nutrients that feed new growth.
What makes topsoil special is that it's rich in organic matter, the decomposed remains of plants and animals that make soil fertile. Without good topsoil, farmers can't grow crops successfully, and forests can't sustain themselves. A single handful of healthy topsoil contains more living organisms than there are people on Earth: bacteria, fungi, tiny insects, and microscopic creatures all working together.
Topsoil forms incredibly slowly, often taking 500 years to create just one inch through the natural process of rock weathering and organic material decomposing. That's why farmers and gardeners work hard to protect it. When heavy rains wash topsoil away, or when wind blows it off bare fields (a problem called erosion), that precious layer can disappear in a season, even though it took centuries to form. Plants help hold topsoil in place with their roots, which is one reason why forests and grasslands are so important to healthy land.