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Facility Audit: Deer Park, TX - Clean Harbors

Facility Audit: Deer Park, TX - Clean Harbors

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Figure 1. STRATIGRAPHIC SECTION OF THE DEER PARK, TEXAS AREA<br />

SYSTEM SERIES FORMATION AQUIFER<br />

Quaternary Holocene Alluvium Chicot Upper<br />

Beaumont<br />

Lower<br />

Pleistocene<br />

Lissie Montgomery Evangeline<br />

Willis<br />

Goliad<br />

Tertiary Pliocene Fleming<br />

Miocene<br />

Burkeville<br />

Jasper<br />

Review of lithologic/textural descriptions from exploratory borings, monitoring well installation<br />

logs, and other such information indicates that the subsurface at the facility consists of sediments<br />

of the regional Beaumont Formation, with the surface soils consisting mainly the Beaumont<br />

Clay. These sediments are generally highly-plastic clays, separated by interbedded, lenticular<br />

deposits of sandy clay, clayey silt, and silty sand. The silt and sand sediments represent periods<br />

of fluvial activity, whereas the clays are mainly of marginal-marine origin.<br />

Based on differences in physical properties, the upper 140 to 150 feet of the subsurface can be<br />

divided into six distinct units. These units are referred to as Strata 1, 2, 3, 4, 5, and 6, in order of<br />

decreasing depth. Figure 2 on the next page provides general unit descriptions of these six strata.<br />

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