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Location: 120 km S from Charleston, West Virginia, United States
250 West Main St. Ste. 1900LexingtonKentucky, United States40507
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The uppermost coal seams of interest (Jawbone and Tiller seams) within the Berwind Complex belong to the Norton Formation in Virginia of Early Pennsylvanian Age, which is stratigraphically equivalent to the Lower Kanawha and New River formations in southwestern West Virginia. The lower and primary coal seams of interest (Pocahontas and Squire Jim seams) belong to the Lee Formation of the Pottsville Group (Lower Pennsylvanian). The depositional setting for these seams is complex and thought to be upper delta plain, with subsidence controlling the sedimentation rate. The Lower Pennsylvania (Pottsville) sedimentary strata of the coal-bearing rocks of the Pocahontas Formation rest uncomformably on the Mississippian Bluestone Formation of the Mauch Chunk Group.The coal seams of interest within the Berwind Complex are in the Southwest Virginia Coal Field and the Southern Coal Field in West Virginia. These coalseams are known for very high calorific value (Btu/lb)and high through low-volatile metallurgical coal characteristics, with high fluidity, low ash content, and low-sulfur content.The primary coal seams of interest on the Berwind Property, in descending stratigraphic order, are the Tiller, Pocahontas No. 6, Pocahontas No. 5, Pocahontas No. 4, Pocahontas No. 3 and Squire Jim. All of the coal seams of interest outcrop on the property. The Canebrake Fault passes through the Berwind Property, however, it is not anticipated to adversely affect mining activities.Deposit TypeThe Berwind Complex resource area is a relatively flat-lying, sedimentary deposit of Pennsylvanian Age. The 34 coal seams in the Lee Formation and the overlying Norton Formation (Virginia nomenclature) account for approximately 3,000 feet of geologic section.