The deepest soil horizon is typically the C horizon, also known as the "parent material." This layer is composed of unweathered rock or partially weathered rock from which the upper layers of soil are formed. Below the C horizon lies the bedrock, which is not considered a soil layer but rather the solid rock underlying the soil profile.
it is the deepest soil found and is below horizon a and b
The parent material horizon (C horizon) is typically the thickest soil horizon, as it consists of the unconsolidated material from which the soil develops over time. It is often the deepest layer and can vary greatly in thickness depending on the location and the type of parent material.
The C horizon is the unconsolidated parent material from which the R horizon (bedrock) forms over time. The R horizon is a consolidated layer of rock that lies beneath the C horizon. Both horizons are part of the soil profile, with the R horizon being the deepest layer.
The deepest horizon layer of the Earth is the inner core, which is located at a depth of about 5,150 kilometers (3,200 miles) beneath the Earth's surface. The inner core is primarily composed of solid iron and nickel, with temperatures reaching up to 5,700 degrees Celsius (10,300 degrees Fahrenheit).
The D horizon is the deepest soil layer in the soil profile. It consists of partially weathered bedrock or unconsolidated material. This layer is typically located below the C horizon and represents the transition between soil and the underlying parent material.
The C horizon is the weathered parent material from which soil originates. It typically consists of partially weathered rock material and may contain clay minerals, iron oxides, and other elements. It is the deepest layer of the soil profile and lies beneath the B horizon.
The 6 layers of soil from top to bottom are: 1. Organic layer (O horizon) - decomposing plant matter, 2. Topsoil (A horizon) - mixture of minerals, organic matter, and living organisms, 3. Eluviated layer (E horizon) - leached of minerals and clay, 4. Subsoil (B horizon) - accumulation of minerals and clay, 5. Parent material (C horizon) - partially weathered rock, and 6. Bedrock (R horizon) - unweathered rock.
The C horizon forms from the weathering and decomposition of rock materials over a long period of time. It is the deepest layer of soil and consists of partially weathered parent material, with little to no organic matter present. It is characterized by a lack of structure and is often the least developed soil layer.
The A horizon, the uppermost layer in the soil profile, often is called the surface soil. It is the part of the soil in which life is most abundant in such forms as plant roots, bacteria, fungi, and small animals. It is the part in which organic matter is most abundant. The B horizon lies immediately beneath the A horizon and often is called the subsoil. Lying between the A and C horizons, it utilizes the properties of both. Living organisms are fewer than in the A horizon but more abundant than in the C horizon. THE C horizon is the deepest of the three major horizons. It consists of the loose and partly decayed rock beneath the A and B horizons. The rock material in the C horizon is of the same kind which now forms the bulk of the soil above it.
a horizon
The deepest part of the heart is the ventricle, and the deepest part of the ventricle is the apex.
Deepest Fish - SnailfishPseudoliparis amblystomopsis