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Geologic Map of the Buckeystown Quadrangle, Frederick and Montgomery Counties, Maryland, and Loudoun County, Virginia

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Geologic Map of the Buckeystown Quadrangle, Frederick and Montgomery Counties, Maryland, and Loudoun County, Virginia U.S. DEPARTMENT OF THE INTERIOR Prepared in cooperation with the GEOLOGIC QUADRANGLE MAP U.S. GEOLOGICAL SURVEY MARYLAND GEOLOGICAL SURVEY BUCKEYSTOWN QUADRANGLE, MARYLAND AND VIRGINIA 77°30′ 77°22′30″ MAP GQ–1800 39°22′30″ 39°22′30″ S Qt _fl 21 80 85 E 77 CORRELATION OF MAP UNITS REFERENCES CITED A 54 _a 22 45 82 16 4 L 17 21 5 33 F E 1 2 1 1 2 1 82 Cenozoic surficial deposits E 20 4 4 V 6 8 0 8 2 2 0 6 15 _fa E _ 0 h 0 0 0 0 0 0 0 0 0 E Brezinski, D.K., 1992, Lithostratigraphy of the western Blue Ridge cover rocks in 0 T 0 0 0 0 0 0 0 0 0 L 85 81 73 34 _fr Qal 36 26 Holocene B Qal Maryland: Maryland Geological Survey Report of Investigations 55, 69 p. 16 25 Ogu 30 37 S 4 A 11 20 72 QUATERNARY 0 u 27 79 Holocene and 0 r Qt Burton, W.C., Froelich, A.J., Pomeroy, J.S., and Lee, K.Y., 1995, Geologic map of f Qc Qr Qt i f 40 c 27 e 26 25 84 _frs Pleistocene i e the Waterford and Virginia portion of the Point of Rocks quadrangles, Virginia: a 82 42 t l ^bs 11 QUATERNARY = 82 Pleistocene and d 1 29 71 22 QTt e U.S. Geological Survey Bulletin 2095, 30 p. 2 52 ^ Qc _fa late Tertiary AND TERTIARY p 61 2 62 o 81 _ b h 5 m s 74 Clark, F.W., 1924, The data of geochemistry: U.S. Geological Survey Bulletin 770, l Unconformity i O_gl 54 42 t e 71 79 69 s 70 Qal 72 t ^mt 22 e 10 841 p. n ^ 20 9 Qt Qal _ r Qal O gl 86 o 50 Early Jurassic JURASSIC s Jd m t 65 71 s Cloos, Ernst, and Cooke, C.W., 1953, Geologic map of Montgomery County and the s 10 u 45 _ t ^ frs h bl r 37 f 80 o a Intrusive contacts c w 60 District of Columbia: Baltimore, Maryland Department of Geology, Mines, and Wa- e ^mp 23 n 15 81 21 76 Culpeper basin ter Resources, scale 1:62,500. 61 51 80 Qr 77 81 54 Drake, A.A., Jr., and Lee, K.Y., 1989, Geologic map of the Vienna quadrangle, Fair- 12 52 29 11 78 43 55 51 ^bl Qc 17 39 F _a 65 76 _ar fax County, Virginia, and Montgomery County, Maryland: U.S. Geological Survey 25 22 70 ^bs ^tm Geologic Quadrangle Map GQ–1670, scale 1:24,000. ? _fr 61 32 Newark lower part of 25 Upper Triassic TRIASSIC 55 Supergroup Culpeper Group Drake, A.A., Jr., Sinha, A.K., Laird, Jo, and Guy, R.E., 1989, The Taconic orogen, ^ Qt 58 18 41 60 ^mp b 82 11 22 in Hatcher, R.D., Jr., Thomas, W.A., and Viele, G.W., eds., The Appalachian-Oua- s QTt _fr 45 15 60 77 41 ^mt ^mr chita orogen in the United States: Boulder, Colo., Geological Society of America, 23 51 17 _fl 40 50 80 The Geology of North America, v. F–2, p. 101–177. 62 61 35 Unconformity 85 72 _ 75 Jd Route 180 40 _ frs _frs 25 Edwards, Jonathan, 1986, Geologic map of the Union Bridge quadrangle, Carroll and 41 Ogu fr western Piedmont 43 67 71 42 57 Blue Ridge- Frederick Valley Sugarloaf Mountain Westminster Frederick Counties, Maryland: Baltimore, Maryland Geological Survey, scale 39 20 80 F 23 Qt South Mountain synclinorium anticlinorium terrane 1:24,000. 72 14 22 40 17 ^ 35 62 70 anticlinorium m Qc 15 ———1988, Geologic map of the Woodsboro quadrangle, Carroll and Frederick 9 _fl 25 81 37 p 67 Ogu Lower Ordovician ORDOVICIAN Counties, Maryland: Baltimore, Maryland Geological Survey, scale 1:24,000. ^ _fa 72 m 25 21 77 F 42 31 46 Lower Ordovician ORDOVICIAN Evans, N.H., and Milici, R.C., 1994, Stratigraphic relations and structural chaos on t 81 19 65 79 45 60 O_gl 42 66 81 75 _frs 82 and Upper Cambrian AND CAMBRIAN 52 37 the southeastern limb of the Blue Ridge anticlinorium and points east, central Vir- 22 Qt 52 80 86 43 _fl ginia Piedmont, in Schultz, Art, and Henika, Bill, eds., Fieldguides to southern Ap- 49 39 Qc ^mt 80 85 palachian structure, stratigraphy, and engineering geology: Virginia Tech Depart- 31 70 _fa Upper Cambrian Qr 39 63 82 ment of Geological Sciences Guidebook Number 10, p. 31–64. 62 28 O_gl 72 ^bl 62 _fr _frs Fauth, J.L., 1968, Geology of the Caledonia Park quadrangle area, South Mountain, _ 39 35 a 11 42 81 ? 75 Pennsylvania: Pennsylvania Geological Survey, 4th Series, Atlas 129a, 132 p. r Middle and ? _ar 53 79 _fr 75 _Zi Lower Cambrian Fisher, G.W., 1978, Geologic map of the New Windsor quadrangle, Carroll County, 62 _fl Maryland: U.S. Geological Survey Miscellaneous Investigations Series Map I–1037, 42 32 65 59 _t 80 scale 1:24,000. Qc ^ 47 59 Jd Tuscarora Creek bs 12 65 _fl _a Lower Cambrian CAMBRIAN ? Froelich, A.J., 1975, Bedrock map of Montgomery County, Maryland: U.S. Geologi- _frs Chilhowee Jd 42 Qt Group cal Survey Miscellaneous Investigations Series Map I–920–D, scale 1:62,500. 9 25 _h 40 79 Qal 33 Goddard, E.N., Trask, P.D., DeFord, R.K., Rove, R.N., Singewald, J.T., and Over- _ 60 57 80 40 _ul f 15 78 _ar _u r 37 45 85 Qal _uq beck, R.M., 1948, Rock-color chart: Washington, D.C., National Research Coun- 39 87 56 72 A 67 75 _ cil, 6 p. [reprinted by Geological Society of America, 1951, 1963, 1970]. ^ 33 55 ar _su mp 7 _fa 55 57 79 Lower Cambrian(?) Hopson, C.A., 1964, The crystalline rocks of Howard and Montgomery Counties, in 45 21 65 ^mt _sm 22 42 The geology of Howard and Montgomery Counties: Baltimore, Maryland Geologi- ^mp 21 Qt cal Survey, p. 27–215. _ Qr _fr 84 65 sl B 28 65 31 Horton, J.W., Jr., Drake, A.A., Jr., and Rankin, D.W., 1989, Tectonostratigraphic 17 _uq 27 Ogu 24 T _Zi Lower Cambrian(?) 17 71 L CAMBRIAN AND terranes and their Paleozoic boundaries in the central and southern Appalachians, 62 31 U and 11 _fa A LATE PROTEROZOIC in Dallmeyer, R.D., ed., Terranes in the Circum-Atlantic Paleozoic orogens: Geo- B&O Railroad 57 F _Zs Late Proterozoic(?) _ 25 11 59 _frs logical Society of America Special Paper 230, p. 213–245. f 59 85 Jd a ^mt 27 21 T S Hoy, R.B., and Schumacher, R.L., 1956, Fault in Paleozoic rocks near Frederick, U 22 T 23 Jd R L Maryland: Geological Society of America Bulletin, v. 67, no. 11, p. 1521–1528. Jd 25 75 H 37 U 70 T A 11 81 ? F Jonas, A.I., 1924, Pre-Cambrian rocks of the western Piedmont of Maryland: Geo- ? ^ bl 21 logical Society of America Bulletin, v. 35, no. 2 p. 355–363. Qr 22 17 C 70 I 30 New Design Road 10 Jd T 1 T ———1927, Geologic reconnaissance in the Piedmont of Virginia: Geological Soci- 32 R S A sl U 21 81 69 61 £ ety of America Bulletin, v. 38, no. 4, p. 837–846. 62 M 42 58 R 29 Ogu 57 10 H 80 T Jonas, A.I., and Stose, G.W., 1938a, Geologic map of Frederick County and adjacent _ 10 75 32 f Qc 77 73 Qt parts of Washington and Carroll Counties: Baltimore, Maryland Geological Survey, r 65 s ^bl 39 27 _uq Qr 62 21 70 72 37 IC DESCRIPTION OF MAP UNITS scale 1:62,500. 80 69 42 T Antietam Formation of Chilhowee Group (Lower Cambrian)—Light- R _a 10 _fr 78 ———1938b, New formation names used on the geologic map of Frederick County, 13 7 27 17 10 A [Color designations, in parentheses, are from Goddard and others (1948)] olive-gray (5 Y 6/1) to olive-gray (5 Y 4/1), medium- to coarse-grained, 19 65 10 M _ 12 46 52 _fr 71 60 u Maryland: Washington Academy of Sciences Journal, v. 28, no. 8, p. 345–348. _fr 81 _ 75 medium-bedded, locally ferruginous, micaceous, silty metasandstone in- Qt fa 35 _ 11 Keith, Arthur, 1894, Harpers Ferry Folio, Va.-Md.-W. Va.: U.S. Geological Survey F 70 R 78 CENOZOIC SURFICIAL DEPOSITS terbedded with very fine grained, silty metasandstone to sandy metasilt- f 23 Qal E 60 l D 59 11 Geologic Atlas of the United States, Folio 10, scale 1:125,000, 11 p. E 20 34 65 _ar 70 25 R 13 7 78 stone. Poorly exposed. Thickness estimated at 300 ft I ^bs 77 C 21 Alluvium (Holocene)—Unconsolidated mixture of clay, silt, sand, gravel, O Qal Keyes, C.R., 1890, Discovery of fossils in the limestones of Frederick County, Mary- K 35 53 _Zi V _ _fr 80 A 10 57 81 38 67 cobbles, and some boulders underlying flood plains of Potomac and Harpers Formation of Chilhowee Group (Lower Cambrian)—Brownish- L g 75 Jd _ land: Johns Hopkins University Circular 10, p. 32. L 28 h E Qt l Y Monocacy Rivers and their tributaries. Includes alluvial terraces as gray (5 YR 6/1) to dark-greenish-gray (5 G 4/1), silty, phyllitic metashale ———1891, A geological section across the Piedmont Plateau in Maryland: Geologi- S _ 81 Y 45 _frs N Ogu 69 80 f much as 10 ft above stream channels, and fine colluvial debris from ad- to highly sheared, phyllitic metasiltstone containing intervals of brownish- C ^ cal Society of America Bulletin, v.
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