Tuesday, December 18, 2018

L79

Location   
36.336256,-93.630954 (Google Map)
Site name       
None
Type
Natural outcrop or old road cut
Age/Formation/Unit  (in stratigraphic order)
Ordovician / Everton (Cotter?)
Features of interest
Complex lateral relationships between limestone and local shale development, depositional dips, massive units and thin laminated units.
Lithology present
Dolomite, Shale, limestone, sandstone?
State/County    
AR / Carroll County
Access         
AR 221 4.25 mi south of 324 intersection
Support material available
Photos (26 iPhone)
Site visit history
C. Liner 2/24/2013




Flow structures

Minor chert in probable burrow casts



L13

Location   
36.565040, -94.353329 (Google Map)
Site name       
None
Type
Road cut
Age/Formation/Unit  (in stratigraphic order)
Features of interest
Long road cut along Little Sugar Creek with vertical section of 60+ ft and one cut back terrace.  Boone/St Joe contact with angular contact, local unconformity? Dark layered chert (Reed Springs facies) at base of Boone. Tripolite at top of exposure. Good geophysical access on terrace.
Lithology present
Limestone, white chert, tripolitic chert, layered dark chert
State/County    
AR / Benton County
Access         
West side of US71
Support material available
Photos (35 iPhone)
Site visit history
C. Liner 11/14/2012, 6/18/2013



Detail of section showing angular contact

Area in read box of previous figure with lateral squeeze to exaggerate dips. Left image is uninterpreted. Right figure shows St. Joe/Boone angular contact.  The opening angle between blue and red lines is 6.7 degrees.



L5

Location   
36.450172, -94.240090 (Google Map)
Site name       
None
Type
Natural outcrop
Age/Formation/Unit  (in stratigraphic order)
Features of interest
Vertical section of 80+ ft and two cut back terrace.  Devonian/Mississippian contact. Fractures in Chattanooga Shale. Tripolite appearance near top. Fresh and rust weathered pyrite in St. Joe section. Good geophysical access to contact. 
Lithology present
Shale, limestone, white chert, tripolitic chert, pyrite
State/County    
AR / Benton County
Access         
East side of US71
Support material available
Photos (13 iPhone)
Site visit history
C. Liner 11/14/2012, 4/28/2013 w Mac McGilvery

Wide view with formation names and contacts. View is not on level so some rock section present is not shown in the photo. Light tan probable tripolite is seen at the top of the exposure.

Fracture planes in Chattanooga Shale section.





Wednesday, August 10, 2016

L18

Location   
36.211043, -94.771736 (Google Map)
Site name       
None
Type
Road cut approximately 0.53 miles long
Age/Formation/Unit  (in stratigraphic order)
Vertical section of 30+ ft.  Exposure of Miss/Dev contact with 'Reed Springs"-style chert in lower Boone. Gentle anticline with probable N-S axis and S plunge.
Lithology present
Limestone, shale, hard black bedded chert
State/County    
OK / Delaware County
Access         
US412 north side 0.5 mi east of OK10 intersection. Access from westbound lane.
Support material available
Photos (90 iPhone, 265 Nikon, section measuring video using ImageJ)
Site visit history
C. Liner 11/19/2012, 6/3/2014


Broad view of location showing formations, broad anticline and 4 ft scale bar (orange)

Detail

Detail of Miss/Dev boundary



Tuesday, July 5, 2016

L145

Location   
35.777717, -93.587150 (at base of section along roadway)

Site name       
Spoke Plant

Type
Exposures along well-maintained gravel county road and in nearby ravines in Boston Mountains.  Horizontal length is approximately 2900’.  Strata are horizontal.    

Age/Formation/Unit (in stratigraphic order)

Features of interest
Vertical section of approximately 170 ft.  Section is noteworthy for presence of accessible, well-developed outcrops of both the “Middle Bloyd sandstone” (Parthenon Member) and the Basal Atoka sandstone.  The lower beds of both units are massive, medium- to coarse-grained, low-stand fluvial sandstones.  At isolated exposures across the Boston Mountains, the identities of these units can easily be confused.  

Lithology present
Sandstone, shale 

State/County    
AR / Madison County

Access         
Madison County Road 4845, along east side of Spoke Plant Hollow, Sections 18 and 19, T13N-R24W, Ozark National Forest (Boston Quadrangle), 4.8 miles southeast of Arkansas Highway 16 intersection at Pettigrew.  

Support material available
Illustrated geology note (text, photos, site map, stratigraphic section, wireline log from nearby well)

Site contributed by
M. R. Shinn, 7/4/16.  Site visits by Shinn in 2013-16

Figure 1.  Spoke Plant site map (base from Boston 7.5-minute topographic quadrangle, 40’ CI).  Triangle symbols denote locations of outcrop photos in Figures 2-5.

Figure 2.  Outcrop of “Middle Bloyd sandstone” (Parthenon Member) along Madison 4845, GPS 35.778, -93.587.  Freshly exposed road-cut outcrop is 21 feet thick and consists of massive, tan, medium- to coarse-grained, porous sandstone.  The unit is a gas pay zone in Johnson and Franklin Counties (“Cannon”, “Brentwood”).

Figure 3.  Outcrop of “Middle Bloyd sandstone” in ravine, 260’ east of Madison 4845, GPS 35.776230, -93.586156.  Outcrop is 24 feet thick.

Figure 4.  Kessler Member (Bloyd Formation) and Basal Atoka sandstone along Madison 4845, GPS 35.781083, -93.584783.  Freshly-exposed outcrop of upper Kessler is 15 feet thick and consists of 5 feet of thick-bedded, upper fine- to coarse-grained, clay-cemented, porous sandstone and 10 feet of overlying shale, with sandstone interbeds.  Limestone facies of Kessler is absent here, as in most of eastern Madison County.  (Basal Atoka bluff at this spot is on private residential property.)

Figure 5.  Basal Atoka fluvial sandstone in ravine, 700’ east of Madison 4845, GPS 35.776464, -93.584750.  Total outcrop is 27 feet thick, massive, cross-bedded, siliceous, clay-cemented, porous, medium-grained with quartz granules.  The unit is a gas pay zone across the eastern Arkoma Basin (“Spiro”, “Orr”, “Kelly”, “Barton A”).

Tuesday, June 28, 2016

L144

Location   
35.459917, -92.865050 (at base of exposed section)

Site name       
Evans Mountain Road

Type
Exposure along National Forest Service gravel road and in nearby ravine in Boston Mountains.  Horizontal length approximately 2600 ft.   

Age/Formation/Unit (in stratigraphic order)

Features of interest
Vertical section of 220 ft.  Marine high-stand sandstones and shales of upper Bloyd Formation (expanded Kessler Member) are overlain unconformably by basal Atoka fluvial and shallow marine sandstones, which are correlative with “Barton A” gas pay zone in the eastern Arkoma subsurface.

Lithology present
Sandstone, shale

State/County    
AR / Pope County

Access         
Evans Mountain Road (NFM 1304) and nearby ravine, Sec 1, T9N-R18W and Sec 36, T10N-R18W,  Ozark National Forest, 2.5 miles north of Arkansas Highway 124 intersection at Appleton (Jerusalem Quad). 

Support material available
Illustrated geology note (field guide text, photos, site map, stratigraphic section)

Site contributed by
M. R. Shinn, 6/22/16.  Site visits by Shinn in 2012-13


Figure 1.  Evans Mountain Road site map (base from Jerusalem 7.5-minute topographic quadrangle, 20’ CI)

Figure 2. Outcrops of Lower Kessler sandstone (Bloyd Formation) occur along NFM 1304 at elevations 988’-1052’ ASL. Thick bedded, upper fine- to lower medium-grained, abundant fossil molds (crinozoans, bryozoans), calcareous, friable, porous, with clay pebbles.  This marine sandstone is correlative to the restricted “Kessler limestone” of type Bloyd area.


Figure 3. Upper Kessler sandstone (Bloyd Formation) outcrops occur, along NFM 1304 road side at elevations 1121’-1152’ ASL.  Thick to medium-bedded, lower medium-grained, with fossil molds.  These rocks are the uppermost marine sandstones preserved beneath the Morrowan-Atokan unconformity in Pope County and are absent in the type Bloyd area. 


Figure 4. Massive, trough cross-stratified basal Atoka fluvial sandstone, unconformably overlying mostly-covered shales of the upper Kessler Member of the Bloyd Formation. Outcrop is along stream, approximately 600 feet northwest of NFM 1304.  The incised fluvial facies, here approximately 21 feet thick, is absent at the NFM 1304 roadway exposures.


Figure 5. Transgressive facies near top of basal Atoka sandstone. Unit outcrops along NFM 1304 road side at elevations 1175-1208’ ASL. Sandstones are medium to thick bedded, upper fine-grained, siliceous and friable, with minor marine fossil molds. Interpreted as shoreface deposits.