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Resilience - University of Miami School of Architecture

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environmental history<br />

As is typical <strong>of</strong> barrier islands, Virginia Key is a naturally dynamic enty whose<br />

form and character fluctuates over me. Anthropogenic changes to the Biscayne<br />

Bay ecosystem have supplanted hurricanes and natural dal fluctua-<br />

ons as the major cause <strong>of</strong> landscape change. Peter Harlem’s 1979 analysis<br />

<strong>of</strong> historical aerial photography provides a comprehensive review <strong>of</strong> changes<br />

to the structure <strong>of</strong> Biscayne Bay which parallel the urbanizaon <strong>of</strong> the region<br />

over the 20th century. The <strong>Miami</strong> mainland consists <strong>of</strong> a limestone ridge which<br />

separates the Everglades from the Bay and the Atlanc Ocean. Key Biscayne<br />

forms the southernmost part <strong>of</strong> a second limestone ridge underlying the chain<br />

<strong>of</strong> sandy barrier islands which protect the mainland coast (Harlem 16).<br />

Like other islands, Virginia Key was once covered predominantly with Mangrove<br />

which anchored sediment deposited by fluctuang current and dal ac-<br />

vity (Harlem 26). In the 1930’s dredging and wall construcon began to alter<br />

current flow in the Bay. Sediment began to accrete to the north <strong>of</strong> the island<br />

providing area for expansion <strong>of</strong> the mangrove swamp. By the 1950’s the island<br />

had expanded to the north by almost a half mile. The eastern third <strong>of</strong> this<br />

new area was dredged to provide fill for the sewage treatment plant which<br />

was constructed throughout the mid 1950’s. The dredged area created a sink<br />

for sand eroding <strong>of</strong>f Virginia Key Beach to the south. By the mid 1970’s jees<br />

had been constructed to slow erosion <strong>of</strong> Virginia Key beach. The northern p<br />

<strong>of</strong> the Key was surrounded by levees in the mid 1960’s and the area was used<br />

as a sanitary landfill (figures 4,5)(Harlem 94). The landfill area is now an EPA<br />

superfund site. The northwestern poron <strong>of</strong> the island was altered by the<br />

construcon <strong>of</strong> the Marine Stadium lagoon. The southern poron <strong>of</strong> the island<br />

was cleared for the Seaquarium, RSMAS campus, and federal facilies by the<br />

end <strong>of</strong> the 1950’s (figure 6).<br />

5. Virginia Key Aerials, Harlem<br />

4. Biscayne Bay in green, frame on<br />

study area, adapted from Harlem<br />

8

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