Named for Cardiff, Harford Co., northeastern MD. Present in strongly synclinal basin with greatest depth in vicinity of Cardiff, MD. Consists of somewhat intermittent, poorly developed, quartzitic conglomerate. Underlies Peach Bottom slates; overlies Wissahickon phyllite, mica schist, and mica gneiss.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Cardiff Metaconglomerate designated a formation of Glenarm Series. Underlies Wissahickon Formation (quartzite facies); overlies Peach Bottom Slate. Includes rocks previously assigned to metaconglomerate lithofacies (here abandoned) of Wissahickon (Southwick and Fisher, 1967). Age of Cardiff changed from Ordovician(?) to latest Precambrian.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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