A FIELD METHOD OF DEFINING AND MAPPING EARLY PLEISTOCENE SEQUENCES USING GEOPROBE CORES – SURRY PALEOSHORELINE COMPLEX, COASTAL PLAIN, NORTH CAROLINA
Geoprobe cores were collected along key transects using the continuous, discrete sampling method. Cores were acquired incrementally in 4 ft tubes. Maximum penetration depth was 72 ft; recovery was >80%. Tubes were split lengthwise and core was processed on site. Core tops were sliced off with piano wire. Core surfaces were washed to enhance stratigraphy and air dried. A graphic log was sketched in the field book (0.5 in = 4 ft) using a standardized method of textural classification (Farrell and others, 2013) that is independent from composition. Recent cores (Fall 2015) were photographed in the field using a cell phone camera; the results were remarkable. After transport to home base, cores are reprocessed, photographed with a digital camera, and logged in detail. For archiving purposes, high-resolution photomosaics provide a composite image of the whole core.
This method of coring provides an excellent record of Quaternary strata: recovery is high and cores are relatively undisturbed. Graphic logs constructed in the field permit on site identification of facies and stratigraphic boundaries, and tentative correlations between adjacent cores.