AGS / Geology / Stratigraphy / Ozark Plateaus / Mississippian
ST. JOE LIMESTONE/MEMBER OF THE BOONE FORMATION
Age: Early Mississippian Period
Distribution: Northern Arkansas, Ozark Plateaus; Oklahoma, southern Missouri
Geology: The St. Joe Limestone is a fine-grained, crinoidal limestone that may occasionally contain some smoothly bedded chert. Some beds may display a coarse bioclastic texture. The limestones (and cherts) are frequently gray, but may also be red, pink, purple, brown, or amber. The fossil clasts are generally white in contrast to the matrix. Some thin calcareous shales are found in the sequence (top, lower middle, and base). The base of the St. Joe Limestone is generally marked by a phosphatic, greenish shale or conglomerate. It is a frequent bluff former. A formation rank has been suggested by some workers for the St. Joe Member of the Boone Formation. Crinoids, brachiopods, bryozoa, conodonts, blastoids, ostracods, and rugose coral have been noted in the unit. The basal contact is considered disconformable in most places, but some workers suggest a conformable lower contact with the Chattanooga Shale. The St. Joe Limestone ranges from a feather edge to over 110 feet in thickness.
At various localities a sandstone is present at the base of the St. Joe Limestone. Excerpt from Fiftysix quadrangle description: The basal sandstone is a fine to medium-grained, moderately sorted, sub-rounded to rounded, iron or quartz-cemented sandstone. White to light gray and tan on fresh surface but sometimes blotchy due to iron. Weathers dark gray, tan, or black. Thin to thick bedded but most often seen as float. Contains phosphate pebbles and angular white and light gray chert fragments. The greatest thickness (approx 12 ft.) of this sandstone is near Gayler Crossing in the NE1/4, SW1/4, Sec 21, T15N, R11W. This unit yields abundant conodonts. 0 - approx. 12 ft. thick.
Original Reference: T. C. Hopkins, 1893, Annual Report of the Geological Survey of Arkansas for 1890, v. 4.
Type locality: Named for exposures near St. Joe, Searcy County, Arkansas; principal reference section in a quarry two miles northwest of St. Joe (NE, NW, Sec.18, T16N, R17W)
Red St. Joe Limestone near St. Joe Arkansas.
Contact (center of picture) between cherty Boone and St. Joe Limestone/Member.
St. Joe Member along Highway 71 north of Bella Vista.
Age: Early and Middle Mississippian Period
Distribution: Northern Arkansas, Ozark Plateaus; southwestern Missouri and eastern Oklahoma
Geology: The Boone Formation consists of gray, fine- to coarse-grained fossiliferous limestone interbedded with chert. Some sections may be predominantly limestone or chert. The cherts are dark in color in the lower part of the sequence and light in the upper part. The quantity of chert varies considerably both vertically and horizontally. The sequence includes an oolite member (Short Creek Member) near the top of the Boone Formation in western exposures and the generally chert-free St. Joe Member at its base. The Boone Formation is well known for dissolutional features, such as sinkholes, caves, and enlarged fissures. Crinoids are the most common fossil found in the formation, but brachiopods, bryozoa, mollusks, corals, shark material, trilobites, conodonts, and others fossils are known. The lower contact of the Boone Formation is considered disconformable in most places, but some workers suggest a conformable lower contact with the Chattanooga Shale; the contact with the St. Joe Member is conformable. The thickness of the Boone Formation is 300 to 350 feet in most of northern Arkansas, but as much as 390 feet has been reported.
Original reference: J. C. Branner and F. W. Simonds, 1891, Arkansas Geol. Survey Ann. Rept. 1888, v. 4, p. xiii, 27-37.
Type locality: Named for extensive development in Boone County, Arkansas
|Boone Formation along Highway 65 at Marshall, AR.||Boone Formation at Pfieffer, Arkansas.|
Boone Formation forming “buttresses” north of Marshall along Bear Creek.
Boone Formation at Bella Vista exhibiting karstic weathering.
Age: Late Mississippian Period
Distribution: Central northern Arkansas, Ozark Plateaus; central eastern Oklahoma
Geology: The Moorefield Shale in the Batesville area consists of a lower member of black, calcareous shale and siliceous limestone and an upper member of dark, fissile clay shale. The unit listed as the Ruddell Shale on the state geologic map is usually considered part of the Moorefield Formation and is equivalent to the upper member listed here. The formation is sparsely fossiliferous in much of the sequence, but locally may contain an abundant fauna dominated by cephalopods and brachiopods. The lower boundary is sharp and considered unconformable by most workers. The thickness ranges from a thin edge to 300 feet.
Original reference: G. I. Adams, 1904, U. S. Geol. Survey Prof. Paper 24, p. 26.
Type locality: Named for Moorefield, Independence County, Arkansas.
|Moorefield Shale in Marshall, Arkansas.||Moorefield Shale near Mt. View, Arkansas.|
Age: Late Mississippian Period
Distribution: Central northern Arkansas, Ozark Plateaus
Geology: The Ruddell Shale is described as dark-gray to greenish-gray fissle clay shales with some dark-gray to black limestone concretions. The Ruddell as indicated on the state geologic map is usually considered part of the Moorefield Formation by most geologists and is equivalent to its upper member. See the listing for the Moorefield Formation.
Original reference: Mackenzie Gordon Jr., 1944, AAPG Bull., v. 28, n. 11, p. 1631-1634.
Type locality: West end of Ruddell Hill (NE, NE, Sec. 13, T7N, R13W), Independence Co., Arkansas.
Age: Late Mississippian Period
Distribution: Northern Arkansas, Ozark Plateaus; southern Missouri and northeastern Oklahoma
Geology: The Batesville Sandstone is often a flaggy, fine- to coarse-grained, cream-colored to brown sandstone with thin shales. A limestone member, the Hindsville Member, found mostly in western outcrops, is a crystalline, fossiliferous limestone that, when present, usually occurs at the base of the formation. In western Arkansas the Hindsville Member may be the only representative of this unit. Fossils are somewhat common in the Hindsville Member, but generally sparse in the sand facies. The basal contact is unconformable and often marked by a chert (Boone Formation) conglomerate. The thickness of the Batesville Formation is quite variable, ranging from a feather edge to over 200 feet. The thickest sections are in Independence County.
Original reference: J. C. Branner and F. W. Simonds, 1891, Arkansas Geol. Survey Ann. Rept. 1888, v. 4, p. xiii, 26, 49-53.
Type locality: Named for Batesville, Independence County, Arkansas
|Batesville Sandstone near Rosie, Arkansas.||Batesville Sandstone above Moorefield Shale near Mt.View, Arkansas.
Hindsville Member (upper half of picture), consisting of a conglomeratic limestone, above the cherty Boone Limestone
Age: Late Mississippian Period
Distribution: Northern Arkansas, Ozark Plateaus; southern Missouri, eastern Oklahoma
Geology: The Fayetteville Shale is a black, fissile, concretionary, clay shale. Dark-gray, fine-grained limestones commonly are interbedded with the shales in north-central Arkansas. The Wedington Sandstone Member, known from west Arkansas outcrops, is composed of gray to brown, fine-grained, sometimes calcareous sandstone. Septarian concretions are common in lower beds of the Fayetteville, but may be found throughout the formation. Fossils are abundant in some intervals and in local areas. Most of the fauna recovered is pyritic, but some silicified material is found. The formation is considered to rest conformably on the Batesville Sandstone (and Hindsville Member). The Fayetteville Shale ranges in thickness from 10 to 400 feet.
Original reference: F. W. Simonds, 1891, Arkansas Geol. Survey Ann. Rept. 1888, v. 4, p. 26, 42-49.
Type locality: Named for Fayetteville, in the valley of the West Fork of White River, Washington County, Arkansas
The lower portion of the Fayetteville Shale, Witts Springs Quadrangle.
|The upper portion of the Fayetteville Shale on Blue Mountain, near Oxley.|
Age: Late Mississippian Period
Distribution: Northern Arkansas, Ozark Plateaus; eastern Oklahoma
Geology: The Pitkin Limestone is usually a fine- to coarse-grained, oolitic, bioclastic limestone. Sequences of black shale interbedded with the limestone occur in the eastern outcrop area, minor chert is sometime present near either the top or bottom of the interval, and minor sandstone has been reported near the top of the unit in the northwest. The unit becomes more shaly to the south. Fossils are common and include crinoids, brachiopods, bryozoa, corals, bivalves, gastropods, cephalopods, trilobites, conodonts, and shark teeth. The bryozoan Archimedes is a good marker fossil for this unit but does occur in other subjacent formations. The basal contact of the formation is conformable. The thickness of the Pitkin Limestone ranges from a thin edge to over 400 feet. The average thickness is about 50 feet in the west and about 200 feet in the east.
Original reference: G. I. Adams and E. O. Ulrich, 1904, U. S. Geol. Survey Prof. Paper 24, p. 27, 109.
Type locality: Named for exposures near Pitkin post office in Washington County, Arkansas
Mapping since 2007 in areas east of western Searcy County has differentiated a unit of latest Mississippian age that has been informally designated the Imo shale member of the Pitkin Formation. Its lower contact is placed above the uppermost continuous limestone bed of the Pitkin Limestone in the Pitkin Formation, and below the lowest continuous unit of interbedded sandstone/siltstone/shale of the Cane Hill Member in the Hale Formation. This upper contact is most likely shale on shale so is difficult to distinguish in the field. A description from the Canaan quadrangle follows:
Imo shale (Upper Mississippian, Chesterian) – consists of several shale units with intervening sandstone units. The lowest unit is a light-gray, calcareous or dark-gray, non-calcareous, fissile shale with interbedded, discontinuous sandstone and limestone. This limestone commonly takes the form of small, yellowish, platy concretions encrusted with fossils, especially Chonetes, or light-gray, lenticular, septarian concretions. Locally, loosely accreted, cigar-sized crinoid stems weather out. Above this shale is a persistent, fine- to medium-grained, thin- to massive- and locally cross-bedded sandstone. Fresh surfaces are buff to tan and locally mottled or banded with dark-red iron blebs. Weathers dark-orangey-brown to gray, and blocky. Commonly exhibits pronounced stylolites, liesegang banding, and honeycomb weathering. Unit thickness ranges from approximately 15-60 feet (5-18 meters). Above this sandstone is a fossil–bearing, dark-gray to black, fissile shale. Fossils are abundant and include bivalves (commonly nuculoids), cephalopods (commonly conical nautiloids), solitary corals (commonly rugose), crinoids, brachiopods, gastropods, trilobites and plant material. Typically contains lenticular, orange to dark-red, fossiliferous limestone tempestites, rounded, non-fossiliferous ironstone concretions, and secondary, fibrous calcite partings. Additional discontinuous, thin-bedded sandstone and limestone beds are interbedded within this upper shale unit. The limestone beds are dark-gray on fresh surfaces and weather dark-red. They are fine- to coarse-grained, oolitic and fossiliferous. Conformable with the underlying Pitkin. Ranges from approximately 40-140 feet (12-43 meters) in thickness.
|The contact (black line) between the Pitkin Limestone (above) and the Fayetteville Shale (below) along highway 65 near Marshall.|
Pitkin Limestone at West Fork Arkansas.
An upper Mississippian age sequence mapped on the Geologic Map of Arkansas as the lower part of the Cane Hill Member of the Hale Formation in north-central Arkansas has been offered as a separate unit called the Imo Formation (Original reference: M. Gordon, Jr., 1964, U. S. Geol. Survey Prof. Paper 460, p. 34; Type locality: Sulphur Springs Hollow, SE, SE, Sec. 3 & NW, NW, Sec. 11, T13N, R17W; Searcy County, AR.). This sequence is a fossiliferous gray to black shale with some fine- to coarse-grained, phosphatic sandstone and conglomeratic limestone. Upper-most Mississippian age fossils are common in some intervals and include bivalves, gastropods, cephalopods, brachiopods, crinoids, trilobites, palynomorphs, plant material, and others. The upper boundary is poorly defined and may be a shale on shale contact while the base appears to be conformable with the Pitkin Limestone. The maximum thickness of this sequence cannot be determined without a clear definition of its contacts, but descriptions have indicated a range from 200 to 340 feet. This unit was mapped on the Witts Springs Quadrangle by Smith and Hutto, 2007as the Imo Member of the Pitkin Formation.
Excerpt description from Witts Springs Quadrangle: Imo Member (Upper Mississippian, Chesterian) – consists primarily of a dark-gray to black, fissile, clay shale with interbedded discontinuous sandstone, limestone, and conglomerate. The shale weathers dark gray to brown, ranges from calcareous to non-calcareous, and often contains platy fossiliferous to non-fossiliferous concretionary intervals. Fossils are common in the shale and include bivalves, gastropods, cephalopods (including Rayonnoceras, Reticycloceras, and Tylonautilus), brachiopods, crinoids, trilobites, corals (solitary and colonial) and plant material. The sandstone is typically brown to gray in color, fine to medium-grained, thin to medium-bedded, lenticular to platy, and sometimes cross-bedded. The limestone is typically dark gray, fine to coarse-grained, very thin to medium-bedded, and fossiliferous. A conglomerate that is gray to black on fresh surfaces, and orange-tan on weathered surfaces is present in Piney Branch. It is a fine-grained to bioclastic, fossiliferous, oncolitic, limonitic, limestone-pebble conglomerate with clasts up to 3 inches (76 mm) in diameter. The conglomerate also contains abundant calcite veining and reaches a maximum thickness of about 2 feet (0.7 meters). Overall, this upper unit appears to have been deposited in an east-west trending basin formed on the Pitkin south of the 35° 50’ latitude which may extend eastward to the Peyton Creek locality and beyond. The lower contact is placed at the top of a continuous limestone bed in the Pitkin, and the upper contact (the Missisippian/Pennsylvanian boundary) is placed beneath the first continuous sandstone in the Cane Hill. Due to the similarity in lithology between the units at this contact, it is not completely certain and is therefore drawn as a dashed line. Approximate thickness ranges 0 - 140 feet (0 – 43 meters).
Cane Hill (thin bedded sandstone) above Imo Member (black shale) of Pitkin Formation in Bear Creek, Witts Springs Quadrangle.