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facilities renewal master plan - National Zoo - Smithsonian Institution

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FACILITIES MASTER PLAN ENVIRONMENTAL ASSESSMENT<br />

At the end of each section when applicable, SI provides information on mitigation<br />

measures that would be employed to help avoid, minimize, or mitigate an adverse impact<br />

on a given resource.<br />

A. Natural and Biological Resources<br />

A.1 Soils, Geology, and Topography<br />

The soils of the <strong>National</strong> <strong>Zoo</strong> are classified as urban land soils, which are soils that have<br />

been previously excavated and filled with other soil materials. Some of the site soils<br />

have been historically disturbed for construction, and covered with impervious materials<br />

such as asphalt, concrete, and building materials. In steeply sloped areas of the site, soils<br />

may be mixed with bluestone for stabilization. In other areas, extensive fill may have<br />

been used to create level surface areas for construction of structures. Therefore, the depth<br />

to undisturbed soils on the site varies; the natural soils overlie bedrock at depths of 12 to<br />

15 feet below the natural soil surface. The source of historical fill material has not been<br />

documented in most instances; however, previous excavations in fill materials at the<br />

<strong>National</strong> <strong>Zoo</strong> have not detected any signs of contamination.<br />

The <strong>National</strong> <strong>Zoo</strong> lies within the physiographic province of the Eastern Piedmont Region.<br />

The underlying rocks in this province consist primarily of granite, gneiess and schist.<br />

The depth to bedrock on the site is approximately 12 to 15 feet below the natural soil<br />

surface (USGS, 2008).<br />

The topography of the <strong>National</strong> <strong>Zoo</strong> consists of a moderate to steeply sloping basin<br />

descending eastward from the Connecticut Avenue entrance, at approximately 210 feet in<br />

elevation to mean sea level, to the eastern boundary at Rock Creek, at approximately 55<br />

feet in elevation. The natural topography of the site has been modified over time by the<br />

introduction of fill material to create level surfaces areas for built structures. One unique<br />

aspect of the topography on site is that Olmsted’s design utilized the natural ridge line<br />

affecting the placement of many of the exhibits and circulation.<br />

Impacts to Soils, Topography, and Geology<br />

No-Action Alternative<br />

Additional exhibit <strong>plan</strong>ning outside of the on-going Elephant Trails project would<br />

continue on a site-by-site basis without the availability of large land tracts, preferable for<br />

new exhibits. Other small scale site improvements would continue for site<br />

improvements, building rehabilitation, and <strong>facilities</strong> updates related to safety, health, and<br />

maintenance. The impacts to soils, topography, and geology from exhibit <strong>renewal</strong> and<br />

other improvements would be localized to small areas. With erosion and sediment control<br />

measures to minimize soil runoff and loss, impacts to soils would be minor and shortterm.<br />

There would be no impact to topography or geology because construction activities<br />

such as surface grading, drilling, pile driving, etc. would not occur; therefore, there would<br />

be no change to existing topography or geology.<br />

SMITHSONIAN INSTITUTION – NATIONAL ZOOLOGICAL PARK 40 | P a g e

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