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Report of the Archaeological Investigations of the New Castle Court ...

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NEW CASTLE COURT HOUSE PLAZA<br />

NEW CASTLE, DELAWARE<br />

3.0 FIELD RESULTS<br />

with <strong>the</strong> 1845 wing construction; while <strong>the</strong> second disturbance relates to <strong>the</strong> westward expansion<br />

<strong>of</strong> <strong>the</strong> circa 1820 plaza. The third group <strong>of</strong> intrusive features relates to a number <strong>of</strong> post holes,<br />

some <strong>of</strong> which may relate to <strong>the</strong> 1845 construction. However, a number <strong>of</strong> <strong>the</strong>se post holes are<br />

located a significant distance from <strong>the</strong> newly constructed wing and may signify <strong>the</strong> periodic<br />

renovation <strong>of</strong> <strong>the</strong> circa 1732 block.<br />

3.2.3 SILT LOAM DEPOSIT (SU J)<br />

A total <strong>of</strong> 138 artifacts were recovered from this layer including one prehistoric ceramic and six<br />

flakes. Additional recovered items include bone, oyster shell fragments, a gold cuff link, ball clay<br />

pipe bowl and stem fragments, tin glazed ear<strong>the</strong>nware, buff-bodied ear<strong>the</strong>nware, redware,<br />

imported gray stoneware, porcelain, unidentified bottle glass, nails, brick fragments, and window<br />

glass. This layer’s occupation date range was 1709.6 to 1776.5 and a TPQ <strong>of</strong> 1779 was assigned<br />

based on <strong>the</strong> recovery <strong>of</strong> three pearlware sherds from EU 18.<br />

3.2.4 SUBSOIL – B HORIZON (SU K)<br />

This represents <strong>the</strong> unexcavated subsoil within <strong>the</strong> western section <strong>of</strong> <strong>the</strong> circa 1820 plaza.<br />

3.3 1845 PLAZA STRATIGRAPHIC UNITS<br />

The stratigraphy underlying <strong>the</strong> western-most section <strong>of</strong> plaza, a measured distance <strong>of</strong> 14 ft. from<br />

<strong>the</strong> interior edge <strong>of</strong> <strong>the</strong> 1845 capstone, exhibited a very different stratigraphic construction<br />

sequence than seen elsewhere in <strong>the</strong> plaza. Four distinct fill layers overlie <strong>the</strong> historic ground<br />

surface, corresponding to <strong>the</strong> north pr<strong>of</strong>iles <strong>of</strong> EUs 20 to 22 (Table 3; Figure 8; Plate 3). As seen<br />

previously, <strong>the</strong> uppermost layer corresponded to accumulated organic debris that had collected<br />

between <strong>the</strong> brick plaza surface. This spoil consisted <strong>of</strong> black (10YR 2/1) to very dark grayish<br />

brown (10YR 3/2) loam. Immediately underlying <strong>the</strong> extant brick pavers was a very thin<br />

foundation sand, measuring less than 0.24 ft. in thickness, comprised <strong>of</strong> brown (10YR 5/3) sand<br />

to yellowish brown (10YR 5/4) loamy sand with less than 30 percent pea gravel. Beneath this<br />

primary foundation material was a second, relatively thin deposit, with a maximum depth <strong>of</strong> .23<br />

ft. This layer consisted <strong>of</strong> brown (10YR 5/3) to pale brown (10YR 6/3) sandy clay loam<br />

containing brick and mortar inclusions. Although not uniformly present within <strong>the</strong>se units, it<br />

appears to represent a transition between <strong>the</strong> overlying foundation sand and <strong>the</strong> underlying<br />

demolition layer. The third layer measuring 0.39 to approximately 1.5 ft. in depth comprised <strong>the</strong><br />

bulk <strong>of</strong> <strong>the</strong> fill material within <strong>the</strong> 1845 plaza and appears to constitute a brick and mortar<br />

demolition deposit, containing more than 90 percent brick and mortar by volume. This layer<br />

appears to represent <strong>the</strong> destruction material associated with <strong>the</strong> pre-1845 western addition. What<br />

little soil was present within this layer consisted <strong>of</strong> brown (7.5YR 4/3, 10YR 4/3) loamy sand.<br />

Underlying this demolition layer, adjacent to <strong>the</strong> circa 1820 foundation wall and overlying <strong>the</strong><br />

original ground surface, appeared to be <strong>the</strong> final fill deposit. This layer, comprised <strong>of</strong> dark olive<br />

brown (2.5Y 3/3) sandy loam, may represent a transition between <strong>the</strong> overlying brick/mortar<br />

demolition layer and <strong>the</strong> underlying horizon. The lowest excavated level corresponded to <strong>the</strong><br />

historic ground surface. This buried surface appears to represent a plowzone, or Ap horizon,<br />

based on <strong>the</strong> presence <strong>of</strong> an abrupt lower boundary at <strong>the</strong> base <strong>of</strong> <strong>the</strong> layer. Hue and chroma for<br />

this horizon consisted <strong>of</strong> olive brown (2.5Y 4/4) sandy loam with pockets <strong>of</strong> brownish yellow<br />

(10YR 6/6) silt loam. Unexcavated Subsoil, or B horizon, was composed <strong>of</strong> yellowish brown<br />

(10YR 5/4) silt loam to sandy clay loam with a 40 percent mottle <strong>of</strong> pale brown (10YR 6/3) silt<br />

loam. The density <strong>of</strong> artifacts from this plaza section was quite low. In fact, only one diagnostic<br />

27

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