Bloomsburg paleosol "cycles" consist of a basal, sharp marine erosional surface that truncates the subjacent paleosol, followed by a red interval that includes symmetrical wave ripple-laminated sandstone and bioturbated siltstone, which is then succeeded upward by red claystone with abundant pedogenic slickensides. Cycle 6 at the North Milton locality is designated North Milton paleosol. Soil is a 3.4-m-thick claystone. Age of the Bloomsburg and its North Milton paleosol is Late Silurian.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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