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Fig. 16.4 Fluvial to estuarine facies in rhythmites from southern
Illinois. ( a ) Low angle planar forsets in medium-grained sandstone.
Foresets are delineated by sand- and silt-sized accumulations
of coalified plant debris. Sample from immediately above
Murphysboro Coal in southwestern Illinois. ( b ) conglomerate
within lower part of IVF sequence consisted of locally derived
clasts of limestone ( light colored ), poorly cemented sandstone,
sideretic chips. From lower IVF in Tonganoxie Sandstone,
east-central Kansas. ( c ) Outcrop in southern Illinois of Abbott
Formation exhibiting mostly planar forests delineated by iron-
cemented zone (originally mud drapes). Cyclicity within this
outcrop has been described by Kvale and Archer ( 1991 ) and
Archer ( 1996a )
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