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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 last layer of soil to form a horizon is called Horizon C. This layer is often referred to as the parent material, as it is made up of weathered rock fragments that have not yet fully decomposed into soil. Horizon C is the layer closest to the bedrock and has the least amount of organic matter.
Bedrock is typically found in the C horizon of the soil profile. The C horizon is the layer of partially weathered parent material that lies beneath the topsoil (A horizon) and subsoil (B horizon). It is composed of loosely packed rock fragments and minerals.
The correct order of soil horizons, from top to bottom, is O horizon, A horizon, E horizon, B horizon, C horizon, and R horizon. It is important to note that not all soils have all these horizons, as they can vary depending on the specific conditions of the soil.
The correct order of soil horizons from top to bottom is O, A, E, B, C. The O horizon is organic matter on the surface, the A horizon is topsoil with organic material mixed with mineral particles, the E horizon is a zone of leaching, the B horizon is subsoil with accumulated minerals, and the C horizon is weathered parent material.
The B horizon is rich in minerals leached from the A horizon above and can exhibit a higher clay content. The A horizon is the topmost layer commonly consisting of organic matter mixed with mineral particles. The C horizon is a layer of weathered and broken rock material beneath the B horizon.