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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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72
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119
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878
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335
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1566
10122615 36
1211
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202212 37
416 14
302533185
3225
60
20
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17
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0 0
17281521 27
19
212019
22
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20 1920
2321
20
22
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4032
32 35
2532
293133
2521
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35303230
3338 36
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25 28 26 24
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303233
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21 22 2325
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1921
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23 2524
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34 25 2625
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2419 25 25
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39343040
3750
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22171417
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4253 40 41
88 90 90 90 89 84
3726
4690 90 56 80 83 88
41
63863 90 90 30
90 32 27 40 3832 41 32 44
4140 43
35 453940
55 52
65
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14 15
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66
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2721242525
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30 30 2933 26 26
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202016
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15
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3
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
SADAM
ON
HARTSHORNE
BATE
SLO
VING AR
KANS
AS
