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Chapters 1 - U.S. Fish and Wildlife Service

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Chapter 4 <br />

With the exception of the area restored by the Port of Long Beach in 1990, the configuration of the<br />

marsh plain <strong>and</strong> associated tidal channels protected within the Refuge boundary remains much the<br />

same as it was in the 1800s (refer to Figure 4-5). Although wider in some places <strong>and</strong> more<br />

constricted in others, the tidal creeks remain in essentially the same locations, as does the<br />

extensive marsh plain. Habitat quality has however been compromised to some degree by a<br />

reduction in the marsh’s tidal prism following the completion of Huntington Harbour, as well as by<br />

the significant reduction in seasonal freshwater flows that once flowed into the marsh. The volume<br />

of freshwater entering the marsh was significantly reduced following the flood of 1862, which<br />

changed the course of the Santa Ana River, diverting the floodway well to the south of Anaheim<br />

Bay. As a result of this <strong>and</strong> other major flood events, the watershed upstream of Anaheim Bay<br />

continued to be altered through the construction of flood control channels, including the<br />

construction of the Bolsa Chica <strong>and</strong> East Garden Grove-Wintersburg flood control channels.<br />

These channels divert essentially all of the freshwater flow from the streams <strong>and</strong> creeks upstream<br />

of Anaheim Bay. Instead of following through the marsh, these flows follow a man-made channel<br />

around the eastern edge of NWSSB <strong>and</strong> empty directly into the western end of Anaheim Bay<br />

(Figure 4-6). Despite the changes that have occurred in Anaheim Bay over the past 100 years, 748<br />

acres of the marsh remain essentially intact <strong>and</strong> represent some of the best quality coastal wetl<strong>and</strong><br />

habitat remaining in southern California. This is due in large part to regular, unobstructed tidal<br />

influence that supports a diversity of plants, fish, birds, <strong>and</strong> other coastal dependent organisms.<br />

4.2 Physical Environment<br />

Elements of the physical environment include topography, visual quality, geology/soils,<br />

agricultural resources, mineral resources, paleontology, hydrology/water quality, climate/climate<br />

change/sea level rise, air quality, greenhouse gas emissions, contaminants, <strong>and</strong> noise.<br />

The Quaternary alluvium floodplains that dominant the area included within the Seal Beach NWR<br />

were formed during recent times, therefore the potential for the presence of paleontological<br />

resources beneath the surface is very low, particularly in the upper levels of the formation. Fossils<br />

have however been found at greater depths in nearby areas underlain by the same geological<br />

formations. Because of the low potential for paleontological resources <strong>and</strong> the limited potential for<br />

significant ground disturbing activity on the Refuge, no effects to paleontological resources are<br />

anticipated; therefore, this topic is not addressed any further in the EA. Similarly, the Seal Beach<br />

NWR is not located in proximity to any sensitive noise receptors (e.g., housing, hospitals, libraries),<br />

therefore, there is no potential for adverse noise impacts to such uses as a result of activitities<br />

occurring on the Refuge. No further discussion related to noise is therefore required.<br />

4.2.1 Topography/Visual Quality<br />

The elevations within the 965-acre Refuge range from -2.0 feet below mean sea level (MSL) to just<br />

over 9.0 feet above MSL. The majority of the Refuge, approximately 793 acres, supports tidal<br />

channels, associated mud flats, <strong>and</strong> extensive areas of salt marsh (Figure 4-7). The areas restored<br />

as part of the Port of Long Beach mitigation project include 116 acres divided among four tidal<br />

basins <strong>and</strong> several feeder channels that facilitate tidal exchange within the basins. Forrestal <strong>and</strong><br />

Perimeter ponds support open water habitat, while Case Road Pond <strong>and</strong> 7 th Street Pond support a<br />

combination of open water, salt marsh, <strong>and</strong> periodically exposed mudflats. The Case Road <strong>and</strong> 7 th<br />

Street Ponds also include constructed isl<strong>and</strong>s that support a range of intertidal habitats. These<br />

isl<strong>and</strong>s average about 1.7 feet above MSL. The easternmost isl<strong>and</strong> in the Case Road Pond includes<br />

several mounds that achieve an elevation of approximately four feet above MSL.<br />

4-8 Seal Beach National <strong>Wildlife</strong> Refuge

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