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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

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