Difference between revisions of "Cardiff coal bed"
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Nelson, W.J., , Pennsylvanian Subsystem in Illinois: Illinois State Geological SurveyBulletin (in press).
Latest revision as of 16:30, 9 February 2022
The Cardiff coal is demoted from a formal member to an informal name and is considered to be the Survant Coal Member.
Nelson, W.J., P.H. Heckel and J.M. Obrad, 2022, Pennsylvanian Subsystem in Illinois: Illinois State Geological Survey, Bulletin (in press).
Cady (1915) referred informally to the “big vein” or “Cardiff coal” mined underground at Cardiff in northeastern Livingston County, Illinois. With a map and cross sections, Cady illustrated how the coal lies in a “small, channel-like basin” shaped like a crescent and 1,000 to 1,200 ft (300 to 360 m) wide. Peppers (1970) formally identified the unit as the Cardiff Coal Member.
Cardiff, Illinois, was settled by coal miners from Wales and named for the Welsh city that formerly was a major coal-mining center (Callary 2009).
Mining people knew this seam as the “big vein.”
None. Mines that extracted this coal have been sealed or backfilled. Numerous drill-hole records exist, but only drillers’ logs are available.
As Cady (1915) recognized, the Cardiff coal, like the Kerton Creek coal bed and Roodhouse coal bed, is a highly localized deposit filling channels that locally cut into the Colchester Coal. Peppers (1970, p. 49) concluded that the Cardiff is “an earlier abandoned channel phase of deposition of the Lowell [Survant] Coal” that may be slightly older than the Survant elsewhere in the basin, based on its spore composition. Willman et al. (1975) did not elucidate, but their chart shows the Cardiff as a lentil of coal near the base of the Francis Creek Shale. Jacobson (1985, figure 4) illustrated the same relationship. Although Baird et al. (1985b) did not discuss the Cardiff coal, they presented a schematic representation of the “Mazonian delta complex” (their figure 15) showing what appears to be thick peat filling an abandoned distributary channel within the Francis Creek Shale.
A generalized columnar section of the Cardiff area (Figure 4-37) is based on drilling records from the Cardiff Coal Company, circa 1989–1902. These records may have been based on cores because thicknesses are stated to the inch, but they read like drillers’ logs and use quaint terminology, such as “soapstone” and “coal stone.” Accordingly, a fair amount is left to the imagination. My correlations agree with those of Jacobson (1985, plate 5) but differ from those of Smith (1970), who identified the coal at the top of the column as the Summum (Houchin Creek). I interpret the Cardiff coal to be overthickened Wheeler (lower Survant) coal that partially filled a channel incised into the Purington and Francis Creek Members during a brief eustatic lowstand. The Cardiff is partly correlative to the Kerton Creek, Roodhouse, and unnamed examples elsewhere in the Illinois Basin.
The Cardiff coal is hereby demoted from a formal member to an informal name useful to discuss the deposit near Cardiff. The Cardiff coal is considered to be the Survant Coal Member.
Extent and thickness
The Cardiff coal is a channel-fill deposit. Drilling and mine records near Cardiff portray the seam running east to northeast in a belt that varies from a few hundred feet to about one-half mile (~100 to 800 m) wide (Cady 1915). Coal having the same characteristics was encountered in surface mining at Clarke City, on the eastern edge of Grundy County, about 7 mi (11 km) north-northeast of Cardiff (Smith et al. 1970). Whether the Cardiff and Clarke City deposits connect is unknown. In cross-section, the coal body is crescent-shaped, concave upward. Coal reaches 12 ft (3.6 m) thick and the total seam thickness (with interbedded clastics) attains 19 ft (5.8 m). In some places, the seam terminates abruptly at the margins; elsewhere, it interfingers or grades out to shale.
As outlined by Cady (1915) and Smith (1970) and by drilling records, the Cardiff coal includes thick layers of shale and claystone. Cady reported “sandstone and pebble conglomerate” in the floor, evidently a channel lag deposit. The roof is normally medium to dark gray shale, but one borehole log reported “dark fossiled shale” immediately overlying the coal.
Detailed descriptions are not available. The lower contact probably is erosive in places; elsewhere, coal grades downward to channel-lag sandstone and conglomerate. The upper contact apparently is gradational, intertonguing with shale.
Well log characteristics
No geophysical log showing the Cardiff coal is known.
Summarizing the spore composition of the Cardiff, Peppers (1970, p. 49) stated, “The Cardiff Coal is interpreted as an earlier abandoned channel phase of deposition of the Lowell [Survant] Coal. It may actually be a little older than the Lowell Coal of other parts of the Illinois Basin because the spore assemblage has some aspects of the No. 2 [Colchester] Coal assemblage. This is not surprising because Cady (1915, p. 35) reported that the Cardiff coal in places rests on top of the No. 2 Coal. On the other hand, the ecological conditions in a coal swamp forest growing in a narrow channel-like depression must have been somewhat different from conditions in a more shallow, wide depression. Therefore, the differences in spore content that exist between the Cardiff and more typical Lowell Coal may be more a reflection of the differences of environment than of geological age.”
The U.S. Geological Survey has a small collection (locality number 4150), made by David White in 1906, of fossil plants from shale overlying the Cardiff coal in the Cardiff Coal Company mine. Arden Bashforth of the Natural History Museum of Denmark (written communication, July 27, 2017) identified from photographs Laveineopteris rarinervis, cf. Neuropteris vermicularis, cf. Neuropteris flexuosa, and aff. Mariopteris occidentalis.
Age and correlation
The Cardiff coal is here interpreted to be part of the Survant Coal Member.
Environments of deposition
The Cardiff coal originated as peat accumulating in an abandoned channel. This feature must have been abandoned shortly after it was cut; only a thin lag deposit underlies the peat (coal).
This bed supported a few local underground mines. Reserves have not been estimated.
- Baird, G.C., C.W. Shabica., J.L. Anderson, and E.S. Richardson Jr., 1985b, Biota of a Pennsylvanian muddy coast: Habitats within the Mazonian delta complex, northeast Illinois: Journal of Paleontology, v. 59, no. 2, p. 253–281.
- Cady, G.H., 1915, Coal resources of District I (longwall): Illinois State Geological Survey, Coal Mining Investigations Bulletin 10, 149 p.
- Callary, E., 2009, Place names of Illinois: Urbana, University of Illinois Press, 425 p.
- Jacobson, R.J., 1985, Coal resources of Grundy, La Salle, and Livingston Counties, Illinois: Illinois State Geological Survey, Circular 536, 58 p., 6 pls.
- Peppers, R.A., 1970, Correlation and palynology of coals in the Carbondale and Spoon Formations (Pennsylvanian) of the northeastern part of the Illinois Basin: Illinois State Geological Survey, Bulletin 93, 173 p.
- Smith, W.H., 1970, Lithology and distribution of the Francis Creek Shale in Illinois, in W.H. Smith, R.B. Nance, M.E. Hopkins, R.G. Johnson, and C.W. Shabica, eds., Depositional environments in parts of the Carbondale Formation—Western and northern Illinois: Francis Creek Shale and associated strata and Mazon Creek biota: Illinois State Geological Survey, Guidebook Series 8, p. 34–42.
- Smith, W.H., R.B. Nance, M.E. Hopkins, R.G. Johnson, and C.W. Shabica, eds., 1970, Depositional environments in parts of the Carbondale Formation—western and northern Illinois: Francis Creek Shale and associated strata and Mazon Creek biota: Illinois State Geological Survey, Guidebook Series No. 8, 125 p.
- Willman, H.B., E. Atherton, T.C. Buschbach, C. Collinson, J.C. Frye, M.E. Hopkins, J.A. Lineback, and J.A. Simon, 1975, Handbook of Illinois stratigraphy: Illinois State Geological Survey, Bulletin 95, 261 p.
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