AGS / Energy / Lignite / Geology

Lignite occurs at shallow depths (less than 300 feet) in sedimentary strata of Eocene age in the West Gulf Coastal Plain and along Crowley’s Ridge in the Mississippi River Alluvial Plain. These rocks are divided, from oldest to youngest, into the Wilcox, Claiborne and Jackson Groups (Figure 1). These units contain sediments which were deposited in fluvial, deltaic and marine environments. Overlying these Eocene age units in many areas are gravels, sands, silts and clays of Quaternary age.

The Wilcox Group is exposed in outcrops trending southwest from northwestern Lonoke County to northern Miller County and along Crowley’s Ridge in Craighead, Greeene, and Clay Counties of northeastern Arkansas. The Wilcox is as much as 850 feet thick in Arkansas and has a maximum outcrop width of 21 miles in southern Hot Spring and Dallas Counties. The sediments dip less than 1 degree to the southeast. In the subsurface the Wilcox is found in the Gulf Coastal Plain from Clay County southward to Chicot County and from Chicot westward to southern Miller County.

The group is composed predominantly of fine to very-fine sands, silty sands, and clays. The sands are generally light gray when unweathered. The clays are generally light shades of gray or brown and contain varying amounts of fine sand and silt. The sands and clays frequently contain enough carbonaceous material to make them dark brown to black. Lignite occurs in beds up to 10 feet thick and is generally lenticular in shape. The larger, more important lignite beds appear to be in the lower and middle Wilcox, while thinner beds are scattered throughout. The Wilcox is thought to be deposited in a fluvial environment.

Outcrops of the Claiborne Group occur from eastern Saline to western Miller County and from southern Pulaski southward to western Ashley County. The Claiborne is also exposed in outcrops along the Crowley’s Ridge in St. Francis, Cross, Poinsett and southern Craighead Counties in northeastern Arkansas. In the subsurface the Claiborne is found from Craighead County southward to Ashley and Chicot Counties, and central Grant County eastward to the Mississippi River. The Claiborne generally dips to southeast at less than 1 degree.

The Claiborne is as much as 1,200 feet thick in Arkansas and consists predominantly of silty clays, fine to very-fine sands, and silts. The clays are light to dark gray, blue-gray and usually very silty or sandy. The sands are medium to dark gray when unweathered and alter to white, brown and red when weathered. The silts are medium to dark gray and clayey. Lignite beds in the Claiborne are lenticular, generally of limited areal extent, with a maximum reported thickness of over 10 feet. The lignite in the Claiborne was deposited in deltaic to near shallow marine environments which affected the areal distribution and the chemistry of the lignite.

The Jackson Group crops out in eastern Grant, Cleveland and Bradley Counties and western Jefferson, Lincoln and Drew Counties in southeastern Arkansas. Outcrops of the Jackson Group also occur along the flank of the Crowley’s Ridge in St. Francis County in eastern Arkansas. The Jackson Group attains a reported maximum thickness of 450 feet in the subsurface. It is composed of fossiliferous, calcareous, glauconitic clays, glauconitic fine-grained sands, and carbonaceous silts and clays. The Jackson Group was deposited in a marine environment. No commercial deposits of lignite are known to exist in the Jackson Group.

Figure 1. Generalized stratigraphic column of the Eocene and associated strata, southern and eastern Arkansas

During the period of 1975-1985 the Arkansas Geological Commission (now the Arkansas Geological Survey) underwent a lignite project to (1) determine the geographical and geological distribution of lignite in Arkansas at mineable depths and (2) obtain heating values and chemical analyses of lignite. 1,843 test holes were drilled to an average depth of 157 feet for a total of over 290,400 feet. Of this total footage, 246,000 feet were drilled in lignite-bearing units.

Based on 590 drill holes, with an average depth of 161 feet, and 95,000 feet of section drilled, lignite in the Wilcox Group represents 0.93% of all the Wilcox sediments drilled.

Fifty-two (52) lignite samples from the Wilcox Group were collected for chemical analyses. Proximate and ultimate analyses show that on an as-received basis Wilcox lignites average 35.7% moisture, 17.6% ash, 0.57% sulfur and 5,759 Btu/1b. Moisture-free analyses show an average of 27% ash, 0.9% sulfur and 9,004 Btu/1b. On a moisture- and ash-free basis the Wilcox lignites have 1.2% total sulfur, and 12,226 Btu/1b. Total fixed carbon averages 44% with 56% volatile matter. Based on a moist, mineral-matter-free basis Wilcox lignites average 7,100 Btu/1b and are of Lignite A rank.

The Arkansas Geological Commission lignite project drilled 1,003 test holes into Claiborne Group sediments. Based on an average depth of 150 feet per hole, the lignite in the Claiborne Group represents 0.15% of all of the Claiborne sediments drilled. The major lignite deposits in the Claiborne occur approximately in the middle of the stratigraphic section.

Fifty (50) lignite samples from the Claiborne Group were analyzed in this project. Proximate and ultimate analyses show that on an as-received basis Claiborne lignites average 38.7% moisture, 17.9% ash, 0.62% sulfur and 5,467 Btu/1b. Moisture-free values average 28% ash, 1.03% sulfur and 9,008 Btu/1b. On a moisture- and ash-free basis the Claiborne lignites have 1.48% total sulfur, and 12,524 Btu/1b. Based on a moist, mineral-matter-free basis Claiborne lignites average 6,764 Btu/1b and are of Lignite A rank.