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New River Mining

The coal mined along the New River, a tributary of the Elk River in West Virginia, is of excellent quality for power-generating facilities or for direct heating, depending upon the final destination of the coal. Coal is commonly divided into two types, bituminous and sub-bituminous, but the chemical composition of the two is essentially the same. The average quality coal in the Lower New River region is about 93% bituminous and 7% sub-bituminous, with very little anthracite. In the easternmost parts of New River Region, the coal is about 40% bituminous and 60% sub-bituminous. Economic conditions drive the production of minerals, not important qualities, such as the percentage of bituminous coal. The best fuel coal is bituminous. Hence, these valleys are noted for their lower amount of anthracite, which is used for steel making.

There are generally four distinct strata in the New River formation, from base to top. The upper coal zone is usually known as the New River Formation, and the three lower zones are subdivisions of it, described in the following:

The New River Formation consists of the lowest part of the strip formation and the New River Trough. This zone varies in thickness from about 10 to 60 feet, and in some districts its thickness may reach a little beyond 100 feet. Its thickness is greater overlying relatively impermeable rocks than where it does not exist. The overall thickness of the New River Formation ranges from less than 200 feet in the trough of the river to about 200 feet over the north-central part of the river valley, and in some places the thickness exceeds 800 feet. In the valley of the Scioto River the thickness ranges from less than 100 feet to more than 400 feet.

The upper New River and the lower Scioto formations are part of the Middle Anthracite coal-bearing division. On the basis of the average thickness of the New River Formation, this zone varies in depth from about 200 to 800 feet. It is a relatively impermeable formation, although sometimes more or less permeable at or near the surface. This division is divided into several major sub-divisions.

The upper New River Trough or Middle Anthracite zone is approximately 10

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