ACID SULFATE SOILS - Sawgal.umd.edu - University of Maryland
ACID SULFATE SOILS - Sawgal.umd.edu - University of Maryland
ACID SULFATE SOILS - Sawgal.umd.edu - University of Maryland
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pr<strong>of</strong>ile and a midden landscape when the soil was tilled from that site appear<br />
on page 67 in the Fanning and Fanning (1989) book.<br />
Picture X1. Carol Gordon, (now, 2011, Carol Loopstra) who is a short<br />
person, holding a tiling spade (sharp shooter) standing on top <strong>of</strong> Native<br />
American oyster shell kitchen midden exposed on low cliff above tidal<br />
Potomac River just a short distance (50 meters) upriver from where the trail<br />
from the Loyola Retreat House reaches the river thru a creek valley to the<br />
right <strong>of</strong> where Carol is standing.<br />
This site will also afford an opportunity to view other parts <strong>of</strong> the cliff face<br />
to see the oxidized vs. un-oxidized parts <strong>of</strong> the soil-geologic column that are<br />
in marine sediments <strong>of</strong> Miocene (probably Calvert formation) and/or Eocene<br />
(probably Nanjemoy formation) age. We are hoping to get out to this site<br />
for a further look before we bring the tour group here. One <strong>of</strong> the interesting<br />
features that occurs in the cliff face are what we think are petrified<br />
(silicified) tree logs that have petrified worm burrows within them – see the<br />
picture, X2, on the following page.<br />
An acid sulfate weathering pr<strong>of</strong>ile with its lower part in the un-oxidized<br />
Nanjemoy (Eocene) formation was studied on a 6 meter high cliff about a<br />
mile farther up river from the Retreat House cliff on the Mt. Air estate<br />
(Wagner, 1982). There the cliff was in a cut river terrace. At the Retreat<br />
33