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Rappahannock Landing Archaeological Survey ... - Fauquier County

Rappahannock Landing Archaeological Survey ... - Fauquier County

inches. Its parent

inches. Its parent material is alluvium derived from igneous and metamorphic rock (NRCS 2008). Montalto and Haymarket soils, 7 to 15 percent slopes, is found in ten percent of the project area. It is a deep, well drained soil found on the backslope or shoulder and crest of interfluves. It is composed of residuum weathered from diabase and/or basalt. Twenty percent of the project area is composed of minor soils. Sowego loam, 2 to 7 percent slopes, is a moderately deep, moderately well drained soil. Frequently flooded, it is located on the toeslopes and base slopes of drainageways. It is composed of colluvium over residuum weathered from shale and siltstone. Oakhill-Rock outcrop complex, 15 to 45 percent slopes, is a shallow, well drained soil. Comprising residuum weathered from basalt, it is located on the back and sides of hillslopes. Ashburn silt loam, 2 to 7 percent slopes, is a shallow, moderately well drained soil found on the shoulder and summit of interfluves. It is formed from reworked alluvium over residuum weathered from sandstone and shale (NRCS 2008). Ott-Catlett complex and Panorama silt loam, both 2 to 7 percent slopes, are each found on less than 1 percent of the project area. Ott-Catlett complex is a shallow, well drained soil composed of residuum weathered from metamorphic rock. Panorama silt loam is a moderately deep, well drained soil composed of residuum weathered from shale and siltstone (NRCS 2008). 6

Rappahannock River Figure 3: Location of the Project Area on the 1984 USGS 7.5 Minute Remington Topographic Quadrangle (USGS 1984). 7 Project Area N

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