* Horizon, A: a surface soil mineral horizon characterized by a highly humified organic matter content intimately mixed with the mineral fraction. The A Horizon may have properties resulting from cultivation, pasturing or similar kinds of disturbance.
* Horizon, B: the horizon usually below the A or E Horizon that is generally a horizon of maximum accumulation (illuviation) of iron, aluminum, or organic matter. A dark reddish brown to a yellowish-brown color may be evident in the more developed horizons.
[RIGHT ARROW] Subordinate Distinction "h" (Bh): alluvial accumulations of organic matter. This symbol is used with "B" to indicate the accumulation of dispersible organic matter - and to a lesser extent, sesquioxide complexes (iron and aluminum compounds).
[RIGHT ARROW] Subordinate Distinction 's" (Bs): illuvial accumulation of iron, aluminum and organic matter. This symbol is used with "B" and may also be combined with "h" as "Bhs".
* Horizon, C: soil horizons that have been very little affected by the soil forming process. Most are mineral, but C horizons can also be found in organic soils. They can be either like or unlike the soil material above them.
* Horizon, E:a layer of maximum leaching (eluviation) of iron, aluminum, and organic matter. The E horizon is usually lighter in color than the overlying or underlying horizons. An E Horizon is commonly near the surface below an A Horizon and above a B Horizon.
* Horizon, O: a Layer usually found on top of the mineral soil material comprised entirely or mostly of organic matter in various stages of decomposition. O horizons may contain small percentages of mineral matter, generally comprising less than half of its weight.
The term Major Water Body/Course includes, but is not limited to, the following:
10-144 C.M.R. ch. 241, § 1