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The great majority of conifer genera and species are evergreen, retaining their leaves for several (2–40) years before falling, but unusual deciduous conifers occur in five genera (Larix, Pseudolarix, Glyptostrobus, Metasequoia and Taxodium), shedding their leaves in autumn and leafless through the winter.
The dark appearance of the spruce–fir canopy in contrast to the bright green canopy of the deciduous forest is the root of numerous mountain names across the southern Appalachians, most notably the Black Mountains, as well as individual summits such as Old Black in the Great Smokies. [16]
Similarly, the Southeastern conifer forests occupy the Gulf coastal plain to the south. Higher, and to the north and west, are the Appalachian-Blue Ridge forests and the Appalachian mixed mesophytic forests of the Appalachian Mountains. [2] Small stands of these forests extend into north Florida.
In terms of biodiversity, the only comparable temperate deciduous forest regions in the world are in central China, Japan, and in the Caucasus Mountains.Both the Appalachians (along with the neighbouring Appalachian mixed mesophytic forests ecoregion) and central China contain relict habitats of an ancient forest that was once widespread over the Northern Hemisphere.
Appalachian mixed mesophytic forests images at bioimages.vanderbilt.edu; Owen, Wayne (2002). "Chapter 2 (TERRA–2): The History of Native Plant Communities in the South". Southern Forest Resource Assessment Final Report. U.S. Department of Agriculture, Forest Service, Southern Research Station
In 1969, Harold and Josephine Hatcher retired to Spartanburg, South Carolina and began developing the land behind their home on Briarwood Road. Over the next thirty years they acquired property totaling 10 acres (40,000 m 2). Much of the land was in ruin: erosion from the former cotton fields had robbed the soil of its nutrients.
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The Mountains of South Carolina refers to the Blue Ridge Mountains, a province of the larger Appalachian Mountains, that stretches from Maine to Alabama. It is the smallest geographical region in the whole state. In South Carolina, this regions consists mostly of igneous and metamorphic rocks of Precambrian age.