marked the
line between Spanish La Florida and French La Louisiane. Thirty-one years
later, the United States accepted and then surveyed the 31° border under the
Treaty of San Lorenzo of 1795 (Pinckney’s Treaty). Final y, in 1822, when
Congress organized the Territory of Florida, it used the Perdido River to
mark its western boundary.
The Spanish mariners who first saw the shores of La Florida encountered
what appeared to their untutored eyes to be unbroken forests of pines and
mixed pines and hardwoods running from the sea to the great stands of
fire-tolerant longleaf pine trees that marked the edges of the piedmont in
the Carolinas and Georgia and covered the northern highlands of the pen-
insula. Along the shore and on the backs of coastal islands were hammocks
of live oaks where soils were appropriate. The river valleys that ran to the
sea were thickly grown with multiple hardwood species. On the piedmont,
the oak-pine-hickory forest appeared, while on some slopes of the Appala-
chian Mountains the dominant forest was the oak-hickory-elm association
now largely lost to Dutch elm disease. Appearing uniform, these vast bands
of forest were in fact mosaics of many floristic communities, communi-
ties determined by soils, rainfal , drainage, temperature, and the shaping of
the forests by lightning fires, insects, and Native American agricultural and
proof
hunting practices, including the use of fire. Faunal diversity accompanied
this floral diversity, although most species were too small for use as food.2
Less clearly in peninsular Florida than farther north along the coastal
plain, the rising and retreating of the Atlantic and the warping of the North
American geologic plate have shaped as many as a dozen step-like, if dis-
continuous, “terraces” in what geologists classify as three sections (lower or
outer, middle, and upper or inner) of the coastal plain. The soils on these
coastal terraces were once back barrier marsh surfaces, bay bottoms, and/or
areas of al uvial deposition and are general y acidic sands of low fertility and
high moisture content during the rainy season. In general, they are classified
as Aquults, although areas of Humaquepts occur along the Georgia coast.3
Inland swamps, marshes, and low areas that flood during the rainy season
reflect this geologic history. Hardpans (horizons of nearly impermeable
clay) underlay some areas, notably on the east and west coasts of Florida
where the soils are Aquods. These hardpans result in rainy-season flooding
and the famous pine flatwoods that some British-era “planters” exploited
for naval stores and that today support the pulpwood industry where sub-
divisions have not sprung up. Scarps or even sand hills (in Georgia and
the Carolinas) mark the edges of the terraces and provide gradations in
44 · Paul E. Hoffman
moisture from wetter (close to the water) to drier on the uplands, gradations
that define ecotones where floral and faunal diversity is greater than on the
terrace below or above. Ecotones can also be found around ponds and lakes
and along stream beds, especial y in central Florida.4
The Piedmont has a similar topography of terraces although the soils are
more fertile and better drained by numerous small streams flowing into the
rivers that drain to the east or south. In general, the soils are mostly reddish
Udults. Native Americans and modern farmers used and use the friable,
quality soils of the valley floodplains associated with the smaller streams.
De Soto’s men (1539–40) and Juan Pardo’s soldiers (1566–68) recognized
these areas as places suitable for Spanish agricultural settlement.5 Histo-
rian Eugene Lyon believes that had Pedro Menéndez de Avilés lived long
enough, he would have claimed the upper Wateree River Valley (explored
by Pardo) as part of the marquisate Philip II had promised him if he success-
ful y settled La Florida.6 Had Spanish settlement developed in this