LEADER 02365oam 2200433zu 450 001 9910830952503321 005 20210807004625.0 010 $a1-118-66821-9 035 $a(CKB)3450000000004188 035 $a(SSID)ssj0001033983 035 $a(PQKBManifestationID)12452793 035 $a(PQKBTitleCode)TC0001033983 035 $a(PQKBWorkID)11006708 035 $a(PQKB)11778324 035 $a(NjHacI)993450000000004188 035 $a(PPN)189691468 035 $a(EXLCZ)993450000000004188 100 $a20160829d2013 uy 101 0 $aeng 135 $aur||||||||||| 181 $ctxt 182 $cc 183 $acr 200 00$aUltramafite-Associated Cu-Fe-Co-Ni-Zn Deposits of the Sykesville District, Maryland Piedemont: Sykesville, Maryland, July 17 1989 210 31$a[Place of publication not identified]$cAmerican Geophysical Union$d2013 215 $a1 online resource (239 pages) 300 $aBibliographic Level Mode of Issuance: Monograph 311 $a0-87590-595-1 330 $aThis trip will make only one stop, the abandoned workings of the Mineral Hill Mine which is located on state land surrounding the Liberty Reservoir, Carroll County, Maryland. The mine is located approximately 40 miles north of Washington, D.C. in the Piedmont Province. The Piedmont consists of gently rolling hills with thick soil cover and few outcrops. As we leave Washington, D.C., we will travel mainly on the coastal Plain until we turn west-northwest on Rt. 32 (Figure 1). We will travel across the Towson terrain traversing the Clarksville gneiss dome and enter the Liberty Complex as we turn northward. Just before we stop, we will cross the bridge over the Morgan Run Arm of the Liberty Reservoir where the old mine road comes out onto Rt. 32. Parking is available on the right side of the road. If you will look across the water to the east on the right side of the bus, you will be able to see the tailings pile of the Mineral Hill Mine. 606 $aZinc compounds 615 0$aZinc compounds. 676 $a546.66 702 $aWylie$b Ann G 702 $aCandela$b Philip A 801 0$bPQKB 906 $aBOOK 912 $a9910830952503321 996 $aUltramafite-Associated Cu-Fe-Co-Ni-Zn Deposits of the Sykesville District, Maryland Piedemont: Sykesville, Maryland, July 17 1989$92267779 997 $aUNINA