The Herbert Hoover Dyke stands as the primary engineering feature in this region of southern Florida, reflecting the massive hydrological management systems designed to control water flow around Lake Okeechobee. This landscape is defined by its artificial watercourses and wetlands, where the Harney Pond Canal cuts through the terrain to facilitate drainage and navigation. The presence of Cabbage Island and the winding path of Gator Slough suggest the original marshy character of the Glades before modern reclamation efforts. While the area is largely characterized by open space and water management infrastructure, the network of local roads and ramps indicates a landscape managed for both flood control and accessibility in the early twenty-first century.
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This is the sole edition of this map. No revisions or reprints were ever made.
1953 · Brighton NW
USGS Topo · 1:24,000
1953 · Brighton SW
USGS Topo · 1:24,000
1953 · Brighton
USGS Topo · 1:24,000
1953 · Brighton SE
USGS Topo · 1:24,000
1953 · Childs
USGS Topo · 1:24,000
1956 · West Palm Beach
USGS Topo · 1:250,000
1956 · Fort Pierce
USGS Topo · 1:250,000
1957 · West Palm Beach
USGS Topo · 1:250,000
1957 · Venus
USGS Topo · 1:24,000
1958 · Fort Pierce
USGS Topo · 1:250,000