ogq-17 geologic map of the adamson 7.5' quadrangle
TRANSCRIPT
AFEET FEET
A'
Arco 3 Edith Richards
N icor 4 P. Bowman
Arco 5 P au line Bowman
G u lfstream 1 Du ran
G u lfstream 1 Neig hbors
Adamson Anticline
Gaines Creek
G u lfstream 1-7 Adamson Townsite
G as U nit
Coqu ina 1 Tobe
Buffalo Creek
Bend in Section
Hamilton 1-31 Winship Browne
Sans Bois Syncline
Bu ffalo Mou ntainS nee & Eberly 1 Oneth
Bend in Section
Ash Creek
Eberly & Meade 4-18 Gladys Vau ghn
O xley 1 Argie Vau ghn
Burning Spring
Anticline
-16000
-14000
-12000
-10000
-8000
-6000
-4000
-2000
S EA LEV EL
2000
-16000
-14000
-12000
-10000
-8000
-6000
-4000
-2000
S EA LEV EL
2000
(?)
P svu (u ndivided S avanna Form ation). P bbju (u ndivided Member of Bog g y Formation) and P bu (u ndivided Bog g y Form ation above P bbju ) inclu de sandstone and shale u nits. Cross-section based on su rface g eolog y and well-log interpretation
S andstone beds (stippled) diag ramatic to show stru ctu re
P wu (W apanu ka Formation u ndifferentiated)(not exposed in qu adrang le)
S -W
S -WS -W
PROBABLE SUB-WAPANUCKA UNITS (S-W) (not exposed in qu adrang le)
SUB-WAPANUCKA UNITS (not exposed in qu adrang le)
10,700' T D
16,300' T D
10,927' T D
12,210' T D
5,950' T D6,005' T D
10,438' T D
11,226' T D
8,400' T D
3,203' T D3,000' T D
8,000' T D
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Lower HartshorneCoal
Upper HartshorneCoal
unnamed coal
Keefton (?)
McAlester coal
Lower Witteville coal
Secor CoalSecor Rider Coal
Correlation of Map Units
Quaternary
Pennsylvanian
DESCRIPTION OF UNITS
ALLU V IU M (QU AT ERN ARY)— G ravel, sand, silt, and clay on flood plains of present-day streams. TERRACE DEP O S IT S (QU AT ERN ARY)— S u bang u lar to su brou nded cobbles, g ravel, sand, and silt, forming a veneer,
g enerally abou t 4-10 ft thick, on the su rfaces of terraces that stand abou t 15-50 ft above the beds of present-day streams.G ERT Y S AN D (QU AT ERN ARY)— U nsolidated g ravel, sand, silt, and clay in abandoned river channel fou nd at elevations well above modern flood plains. Main constitu ents of the sand and g ravel are qu artz, qu artzite, chert, flint, jasper, and silicified wood. T hickness varies from an estimated maximu m of 50 ft to a thin veneer. In places (su ch as parts of sec. 14, T. 6 N ., R. 16 E.), siliceou s, well-rou nded pebbles from the G erty are scattered on weathered S avanna Formation, bu t the deposits are too thin to map as G erty.BO G G Y FO RMAT IO N (P EN N S YLV AN IAN )— P redominantly sandy, silty g rayish black (N 2) to olive g ray (5Y4/1) to dark yellowish brown (10YR4/2) shales and siltstones (P b) with several mappable, scarp-forming , fine- to very fine g rained sandstones (P bbj, P b2, P b3, and P b4). At the base is the Blu ejacket S andstone Member (P bbj), mostly moderate yellowish brown (10YR5/4), abou t 150-200 ft thick. T he Blu ejacket contains a lower, very fine g rained, silty, shaly, thin-bedded, parallel-bedded, ripple-marked, biotu rbated sandstone u nit 25-50 ft thick; a middle silty shale u nit (g enerally covered), abou t 50-100 ft thick; and an u pper fine-g rained, mediu m- to thick-bedded sandstone u nit abou t 25-75 ft thick, containing larg e-scale trou g h cross-bedding , abu ndant soft-sediment-deformation featu res, and stacked-channel sequ ences. A thin (0.05-0.4 ft) coal bed (Lower W itteville) is present in the middle shale u nit of the Blu ejacket Member. It is exposed in the ditch along S tate Hig hway 31 in the S W /4 of sec. 15, T. 6 N ., R. 16 E., and in a cu t along the trail in the S E/4 of sec. 36, T. 6 N ., R. 16 E. P b2-P b4 are predominantly dark yellowish brown (10YR4/2) to g rayish orang e (10YR7/4) to lig ht brown, (5YR5/2), very fine g rained, noncalcareou s sandstones with abu ndant sedimentary stru ctu res su ch as ripples, cross-stratification, sole marks, and soft sediment deformation featu res. T he S ecor coal occu rs in the shale interval between P bbj and P b2. It is of minable thickness in the northwestern part of the qu adrang le where it is >2 ft thick. T he S ecor Rider coal is ~1 ft thick in this same area, and occu rs -40 ft above the S ecor bed. P b2 is discontinu ou s, or thin bedded and g enerally u nmappable on the flanks of Bu ffalo Mou ntain. However, the u nit is mappable in sees. 16, 21, 22, 27, and 28, T. 6 N ., R. 16 E., where it is mostly thin-bedded, shaly, and g enerally not more than -5 ft thick. P b3 is a prominent thick, ledg e-forming u nit that is mapped as P b3a and P b3b at hig her elevations on Bu ffalo Mou ntain and on the hig h hill in sec. 28, T 6 N ., R. 16 E. In those areas it is divided into two parts by a mappable shale u nit (P b). P b4 is preserved only on the hig hest elevations on Bu ffalo Mou ntain. Top of formation eroded. T hickness: 700-800 ft.S AV AN N A FO RMAT IO N (P EN N S YLV AN IAN )— P redominantly pale yellowish brown (10YR6/2) to olive-g ray (5Y3/2) to mediu m dark g ray (N 4) shales (P sv) with several mappable moderate brown (5YR4/4) to g rayish orang e (10YR7/4) to moderate reddish brown (10R4/6), fine- to very fine g rained, noncalcareou s sandstone u nits (P sv1, P sv2, P sv3, P sv4, P sv5, P sv6, P sv7).T he sandstones are massive to thin-bedded and shaly. T hey commonly are cross bedded and ripple marked and in places _contain abu ndant soft-sediment deformation featu res, S oJe marks (trace fossils; bru sh and prod ""marks; flu te, g roove, and load casts) at the base of some sandstone beds are locally common. P sv1 marks the base of the formation throu g hou t the map area. It locally g rades u pward into a fossilifer-ou s, sandy limestone. P sv1-P sv7 are all mapped as sing le u nits, bu t g enerally contain shale beds of varying thicknesses. In sees. 1 and 2, T. 5 N ., R. 16 E.; and sees. 35 and 36, T. 6 N ., R. 16 E., P sv5, P sv6, and P sv7 are u ndifferentiated in a stru ctu rally complex area. In the extreme sou thwest corner of the map, P sv2, P sv3 and P sv4 are mapped as a sing le, u ndifferentiated u nit, as are P sv5 and P sv6. Most shales in the S avanna inclu de thin, u nmappable sandstone u nits. T hickness: 1400-1500 ft.McALES T ER FO RMAT IO N (P EN N S YLV AN IAN )— P redominantly dark g ray (N 3) to black (N 1), blocky shales containing abu ndant ironstone concretions. McCu rtain S hale Member (P mm) at the base is~~ -600 ft thick. A coal bed, -1 ft thick, crops ou t in the N /2 of sec. 30, T. 5 N ., R. 17 E., in the u pper part of the McCu rtain S hale Member. T he W arner S andstone Member (P mw) overlies the McCu rtain S hale Member. It is a resistant, moderate reddish brown (10R4/6) to g rayish orang e (10YR7/4) to moderate yellowish brown (10YR5/4), fine-g rained, cross-bedded sandstone of variable thickness. W here exposed in the area east of Dow, it is mapped as P mw (I), a thick sandstone u nit containing intervening shales, a middle shale u nit, P mw, and an u pper sandstone u nit, P mw (u ). A thin coal (0.2 ft) crops ou t within P mw (u ) at the crest of the ridg e along the road in the northern part of sec. 8, T. 5 N ., R. 17 E. T his coal bed may be equ ivalent to the Keefton coal of Mu skog ee Cou nty and Haskell Cou nty. T hree named, moderate brown (5YR3/4), very fine g rained, thin-bedded sandstone u nits occu r in the shale (P m) above the W arner S andstone Member: Lequ ire S andstone Member (P ml); Cameron S andstone Member (P mc); and Keota S andstone Member (P mk). T he McAlester coal, abou t 2.0-3.5 ft thick, occu rs in the shale interval above the Cameron S andstone Member. It has been extensively mined east and west of Adamson as well as in the Dow area. T hickness: 1,750-2,000 ft.
HART S HO RN E FO RMAT IO N (P EN N S YLV AN IAN )— G rayish orang e (1O YR7/4) to moderate reddish orang e (10R6/6) to very lig ht g ray (N 8), very fine g rained, ripple-marked, biotu rbated, thin-bedded to massive sandstone interbedded with silty, mediu m-g ray (N 5) shale. Contains the Lower and U pper Hartshorne coal beds. T he Lower Hartshorne coal rang es in thickness from 2.5 ft to 6.0 ft — averag e thickness is -4.0 ft; the U pper Hartshorne coal rang es in thickness from 2.3 ft to 3.5 ft — averag e thickness is -3 ft. Both coals are exposed in the N E/4 of sec. 7, T. 5 N ., R. 17 E., in a road cu t, ju st sou theast of Adamson. T hickness: approximately 250-300 ft.
AT O KA FO RMAT IO N (P EN N S YLV AN IAN )— P redominantly silty, mediu m dark g ray (N 4) to olive black (5Y2/1) noncalcerou s shale (P a) with thin, brownish g ray (5YR3/4) siltstone beds. Locally inclu des discontinu ou s, ridg e-forming , moderate yellowish brown (10YR5/4) to dark yellowish orang e (10YR6/ 6), very fine g rained, dirty, micaceou s sandstone (P ass) containing plant frag ments and trace fossils.
Approximately 2,000 ft of u pper part exposed in the map area. Total thickness in su bsu rface in S ans Bois Mou ntains: ~12,000 ft
11
1
1
LIST OF WELLS SPUDDED BEFORE JUNE 1,1995MAP NO. OPERATOR LEASE DATE __________________________________________________________________________________________________________________
SPUD TOTAL DEPTH (ft)1234567891011121313141415161718192020212223232425262728293031323334353637373839404142434444454647484950515253545556575859606162636465666768686970717273747576777879808182838485868687888990919293949596
O xley P etroleu m Co.O xley P etroleu m Co.O xley P etroleu m Co.O xley P etroleu m Co.S u n ray DX O il Co.O xley P etroleu m Co.S W AB Corp. (Bonanza P etroleu m, Inc.)S nee & EberlyS nee & EberlyS nee & EberlyEberly & Meade, Inc.Eberly & Meade, Inc.Eberly & Meade, Inc.Eberly & Meade, Inc. (work over)O xley P etroleu m Co.O xley P etroleu m Co. (work over)O xley P etroleu m Co.O xley P etroleu m Co.O xley P etroleu m Co.Cities S ervice G as Co.O xley P etroleu m Co.Mark Resou rces Corp.Mark Resou rces Corp. (work over)W alter Du ncanO xley P etroleu m Co.King Resou rces Co.King Resou rces Co. (work over)Eberly & Meade, Inc. Eberly & Meade, Inc.O ld Dominion O il Corp.S nee & EberlyS nee & EberlyU nit P etroleu m Co.S amson Resou rcesARCO O il & G as Co.Mag nolia P etroleu m Co.S nee & EberlyHamilton Brothers O il Co.Mu stang P rodu ction Co.Coqu ina O il Corp.Hamilton Brothers O il Co.Hamilton Brothers O il Co. (work over)G u lfstream P etroleu m Corp.G u lfstream P etroleu m Corp. G u lfstream P etroleu m Corp. Tenneco O il Co. Hanna O il & G as Co. T XO P rodu ction Corp.Midwest O il Corp.Midwest O il Corp. (work over) Tenneco O il Co. S amson Resou rces Co.Zinke & T ru mbo, Ltd.T XO P rodu ction Corp.G u lfstream P etroleu m Corp.G u lfstream P etroleu m Corp.T XO P rodu ction Corp. S amson Resou rces Co.Dyco P etroleu m Corp.Intex O il Co. & Midway P remier O il Co.Intex O il Co.S amson Resou rces Co.S hamrock O il & G as Corp.Atlantic Richfield Co.V astar Resou rces, Inc.D-P EX O perating Co. AMO CO P rodu ction Co. S u n O il Co.Kaiser-Francis O il Co.S amson Resou rces Co.AMO CO P rodu ction Co.O ryx Energ yS u n O il Co. - DX Div.Exxon Corp.Exxon Corp. (work over)Hu mble O il & Refining Co.Exxon Corp.ARCO O il & G as Co.Atlantic Richfield Co.S inclair O il & G as Co.N icor Exploration Co.ARCO O il & G as Co.U nit P etroleu m Co.V astar Resou rces, Inc.S inclair O il & G as Co.Au stin Drilling Co.S amson Resou rces Co.S amson Resou rces Co.V astar Resou rces, Inc.ARCO O il & G as Co.Atlantic Richfield Co.Daniel-P rice ExplorationMarathon O il Co.Marathon O il Co. (work over)ARCO O il & G as Co.V astar Resou rces, Inc.JMC ExplorationS inclair O il & G as Co.V astar Resou rces, Inc.V astar Resou rces, Inc.ARCO O il & G as Co.V astar Resou rces, Inc. inclair O il & G as Co.ARCO O il & G as Co.
1 W ard B2 W ard B1 Baptist 1-15 W ard 1 Mary W hite 1 Du retta 1-14 Baldwin 1 Baldwin A 1 Ing ram 1 V au g hn2-13V au g hn3-13 V au g hn 3-18 Arg ie V au g hn 3-18 Arg ie V au g hn 1 Arg ie V au g hn1 Arg ie V au g hn2 Arg ie V au g hn1 Erie W hite2 Erie W hite 1 J.R. Hu g hes1 Dolly Harrison2 Toone 2 Toone 1 Toone U nit 1 Lu cy Mae S mith 1 E.G . Mckenzie 1 E.G . Mckenzie 1-24 O neth 4-18 G ladys V au g hn 1 Debbie 1-21 Clifton 1 O neth 1 Fu g itt 1 Browne1 Browne 1 Manschrick 1-27Cirar1-31 W inship-Browne 1-33 Brown 1Tobe1-10 Bernardi-Jones 1-10 Bernardi-Jones 1 -7 Adamson Townsite G asU nit 1-9M.A. Randel 1 Raspotnik C Coal & Coke Corp. 1 Martha Cook 1 Cook K 1 Barnes 1 Barnes 1-13 Moss A 1 W eberlAW m.W eber1 W eber A1 Du ran 1 N eig hbors1 Beatrice 1 Bowman U nit1 Bowman 1 McEvoy1 Emery Estate U nit1 Bobo U nit1 Joe Emery, Jr., et al.1 Lillie W elch U T2 Lillie W elch U nit 1 Randel1 Clyde Monroe 1 Ernest L. Cook 1 -23 Bru shy1 McBee U nit2 G eorg e P eden3 G eorg e P eden1 G eorg e P eden2 K. Anderson2 K. Anderson1 Kathleen Anderson U nit3 Anderson5 P au line Bowman2 P au line Bowman/sec. 20/U T1 P au line Bowman/sec. 204 P. Bowman3 P au line Bowman2 Bowman3-21 Bowman1 P au line Bowman U nit1-28 Monroe1 Monroe U nit1 Honea3-27 U .S . G overnment2 U .S . G overnment 271 R.A. King U nit1 Miller2 Mass U nit2 Mass U nit3 Edith Richards4-30 Edith Richards3 P.O . Bowman1 P.O . Bowman U nit5-29 P.O . Bowman4-28 U S A2 U S A S ec. 283-28 U S A 1 U S A S ec. 28 U nit2 Alfred P arker
10/18/92 12/01/92 08/19/92 06/27/89 06/21/66 01/24/90 11/24/81 03/04/71 12/18/71 07/05/63 12/17/88 12/20/92 11/16/89 11/16/89 12/31/72 12/31/72 04/28/84 06/22/73 07/13/84 11/28/30 09/15/73 11/23/76 11/23/76 06/03/71 12/14/81 11/20/68 11/20/68 09/12/91 08/31/93 12/13/81 08/06/75 02/25/74
04/24/75 09/24/79 11/15/74 08/15/73 08/27/79 08/27/7903/24/8104/06/81 11/01/78 03/01/82 11/27/77 10/04/81 03/26/61 02/23/63 03/19/81 11/16/8112/30/9006/11/8701/13/7908/25/7906/17/8307/11/8101/25/75
04/02/7808/19/6703/21/7608/10/9005/23/7403/10/7012/11/9012/02/8409/30/9307/20/8704/12/9108/23/6808/31/9412/29/9104/23/76 04/09/67 08/26/89 09/16/87 02/11/91 11/21/94 06/08/66 08/05/77 02/09/81 01/04/90 12/01/94 09/14/79 12/28/70 10/16/8610/23/82 10/23/82 02/28/86 10/19/94 03/15/92 02/04/67 02/05/95?04/23/88 07/24/94 02/15/66 07/11/87
08/01/90 ?09/02/89?/?/54
11/19/4905/15/59
01/30/89
06/09/77
05/03/69
7,4007,3027,2008,0003,2707,5007,2008,0047,6102,6252,7501,8502,8052,8058,0008,0002,5007,9002,4972,2852,4656,2106,2218,0057,9879,853-8,0853,2033,0003,1008,0008,4008,175?14,18012,9158,00011,22610,95010,43811,91711,9176,00512,81512,37011,4006,90212,45011,79911,9599,50610,10010,100 9,80012,21Q_ 5,950 5,500 9,56712,759 3,014 8,000 9,79911,626 6,811 7,42011,315 7,00011,485 6,750 9,18510,545 9,705 9,407 9,875 9,875 9,10011,20010,9275,8219,39116,3009,46011,10011,2509,7607,82311,05011,3187,60010,2009,4609,6259,8859,88510,70011,50010,05010,68610,850?12,24711,6509,81311,937
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416 14
302533185
3225
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17281521 27
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20 1920
2321
20
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4032
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293133
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3338 36
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2419 25 25
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4253 40 41
88 90 90 90 89 84
3726
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63863 90 90 30
90 32 27 40 3832 41 32 44
4140 43
35 453940
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LowerW ittevilleCoal
LowerW ittevilleCoal
S ecor Coal
S ecor Coal
S ecor Coal
McAlesterCoal
McAlesterCoal
LowerW ittevilleCoal
LowerHarthshorneCoal
U nnam ed Coal
U nnam ed Coal
LowerHarthshorneCoal
LowerHarthshorne
Coal
Keefton(?)Coal
#
#
###
##
#
UD
UD
U D
?
S ecor Coal
McAlester Coal
Adamson Fau ltAdamson Anticline
Bu rning Spring s An
ticline
S ans Bois S yncline
GEOLOGIC MAP OF THE ADAMSON 7.5' QUADRANGLE,LATIMER AND PITTSBURG COUNTIES, OKLAHOMA
ByLeRoy A. Hemish, 1995
*sv7
#
#
A
A'
G eolog y mapped in 1994-95.Dig itized by Jacob Hernandez, 2014P rodu ced in cooperation with the U .S . G eolog ical S u rvey,
N ational G eolog ic Mapping P rog ram. P artial fu nding from U S G SS T AT EMAP P rog ram Assistance Award N o. 1434-94-A-1249.
O KLAHO MA G EO LO G ICAL S U RV EYCharles J. Mankin, Director
O klahoma G eolog ic Qu adrang le OGQ-17Geologic Map of the Adamson 7.5' Quadrangle
(previou sly O pen-File Report O F4-95)
SYMBOLS CO N T ACT — Dashed where approximately locatedCO AL BO U N DARY— Approximate ou tcrop bou ndary of coal bed (nam ed on map); qu eried where probable; triang le indicates exposu re of coalT HRU S T FAU LT — S awteeth on u pper plate; dashed where approximately _ located; dotted where concealed ~~FAU LT — Arrows show relative horizontal movement; dashed where approximately located; dotted where concealed; qu eried where probableFAU LT — Dashed where inferred; dotted where concealed; U , u pthrown side; D, downthrown sideAN T ICLIN E— S howing crestline; arrow shows direction of plu ng e; dashed where approximately located; dotted where concealedS Y N CLIN E— S howing trou g hline; arrow shows direction of plu ng e; dashed where approximately located; dotted where concealedM IN O R S Y N CLIN E— S howing plu ng e
S U RFACE CO AL MIN E— Abandoned or area reclaimed
S trike and dip of beds, u prig htU ndu latory beds, averag e dipV ertical beds, ball indicates top of bedsHorizontal bedsU ndu latory, bu t more or less horizontal, beds
Completion not reported as of Ju ne 1,1995Dry hole, abandonedG as well
ABAN DO N ED S MALL CO AL MIN EABAN DO N ED S T O N E QU ARRY O R O P EN S HALE P ITABAN DO N ED S HAFTS P O IL P ILES FRO M ABAN DO N ED CO AL MIN E _
S T RIKE AN D DIP O F BEDS
O IL AN D G AS W ELLS
70
(
UD
AT O KA
P U S HMATAHA
LEFLO RE
McCU RTAIN
HAS KELL
P IT T S BU RG
LAT IMER
CO AL
IN DEX T O QU ADRAN G LES AN D CRO S S S ECT IO N S
Atoka
McAlester
P oteau
HeavenerW ilbu rtonHartshorne
IMBRICATE ZONE
OUACHITA MOUNTAINS
CHO CTAW
ARKOMA
FRONT
OKLA
HOMA
ARKA
NSAS
59271
271
27175
69
259
271
59
69
SUMMEE D
RFIL
HEAVENERNTU
BBY
HOHODN
GEWISTER
LEFLORE SE
BLACKJACK
RIDGE
LEFLRE
O
TIHI
ALNA
REOD AK
BAKERMO
NTAINU
PANOLA
WILRTO
BUN
DAMON
GEN
OWHIGGINS
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ON
HARTSHORNE
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SLO
VING AR
KANS
AS