BEDROCK ~@P3X~
The O horizon, also known as the organic horizon, contains the most organic material. It is made up of decomposing organic matter like leaves, plant debris, and other organic materials.
The parent material horizon, also known as C horizon, is chemically most similar to the underlying bedrock or unaltered sediment. This horizon is largely unaffected by the processes of soil formation and represents the original material from which the soil developed over time.
The top layer of soil, known as the organic horizon or O horizon, contains the most decayed organic material. This layer consists of partially decomposed plant and animal matter, such as leaves, twigs, and dead organisms.
The layer that contains the most organic material in the diagram is the top layer, known as the O horizon or organic horizon. This layer is made up of decomposing organic matter such as leaf litter and other plant debris.
Weathering occurs most rapidly in the O horizon, which is the organic-rich surface layer. This layer contains a high amount of plant material and microorganisms that contribute to the breakdown of rocks and minerals through biological and chemical processes.
In comets
It is the O horizon. The A horizon is the mineral horizon and does include a large amount of organic material but the O horizon contains the most abundant amount of organic matter. The O horizon overlies the A horizon.
The O horizon, also known as the organic horizon, contains the most organic material. It is made up of decomposing organic matter like leaves, plant debris, and other organic materials.
The parent material horizon, also known as C horizon, is chemically most similar to the underlying bedrock or unaltered sediment. This horizon is largely unaffected by the processes of soil formation and represents the original material from which the soil developed over time.
The top layer of soil, known as the organic horizon or O horizon, contains the most decayed organic material. This layer consists of partially decomposed plant and animal matter, such as leaves, twigs, and dead organisms.
The layer that contains the most organic material in the diagram is the top layer, known as the O horizon or organic horizon. This layer is made up of decomposing organic matter such as leaf litter and other plant debris.
organic
most likely RNA
The O horizon contains the most organic matter. The O horizon overlies the A horizon which is known as the mineral horizon. O - organic A - mineral E - elluviation B - illuviation C - parent material R - bedrock This is the order in which you will see standard soil horizons.
Weathering occurs most rapidly in the O horizon, which is the organic-rich surface layer. This layer contains a high amount of plant material and microorganisms that contribute to the breakdown of rocks and minerals through biological and chemical processes.
Venus is the most likely, however, Saturn will be low on the horizon.
The three horizons of a mature residual soil are the A horizon (topsoil), B horizon (subsoil), and C horizon (weathered rock material). The A horizon contains organic matter and is the most fertile layer for plant growth. The B horizon is rich in minerals leached from the topsoil. The C horizon is the least weathered and consists of partially weathered bedrock.