| COUNTRY United States of America - Tennessee
NAME Great Smoky Mountains National Park
IUCN MANAGEMENT CATEGORY
II (National Park)
Biosphere Reserve
Natural World Heritage Site - Criteria i, ii, iii, iv
BIOGEOGRAPHICAL PROVINCE 1.05.05 (Eastern Forest)
GEOGRAPHICAL LOCATION Lies at the southern end
of the Appalachian Mountains in eastern Tennessee and western North Carolina.
Bounded by the Little Tennessee River to the south, French Broad River
to the north and Pigeon River to the east. Surrounded by parts of several
national forests, an Indian reservation, a Tennessee Valley Authority
lake and numerous private holdings. Gatlinburg (Tennessee) lies close
to the north entrance and Cherokee (North Carolina), the south entrance.
35°26'-35°47'N, 83°45'-84°00'W
DATE AND HISTORY OF ESTABLISHMENT Gazetted a
national park on 22 May 1926 (44 Stat. 616). Accepted as a biosphere reserve
in 1976, and in November 1988 was incorporated in the Southern Appalacian
Biosphere Reserve; a distinct biosphere reserve cluster comprising Great
Smoky Mountains National Park, Coweeta Hydrological Laboratory and Oak
Ridge National Environmental Park. Two additional units were added to
the cluster in 1992, namely Mount Mitchell State Park and Grandfather
Mountain, making the total area 6,416,545ha. Inscribed on the World Heritage
List in 1983.
AREA 209,000ha
LAND TENURE Federal government
ALTITUDE Ranges from 259m to 2,025m
PHYSICAL FEATURES The park's dominant topographic
feature is the Great Smoky Mountains range with peaks over 1,818m. In
a broader aspect, the topography comprises moderately sharp-crested, steep-sided
ridges separated by deep V-shaped valleys. Many of the mountain ridges
branch and subdivide from the central ridgeline, creating a complex of
drainage systems with 3,057km of fast-flowing clear mountain streams.
The park contains 45 watersheds and the water table is near the surface
in almost all sections. Precambrian metamorphic rocks consisting of gneisses
and schists, and sedimentary rocks of the Precambrian Ocoee series are
predominant, while younger sedimentary rocks are found in the Appalachian
Valley.
CLIMATE Mean annual temperature for Gatlinburg
is 13.7°C, but the average temperature is 5°-10°C cooler at higher altitudes,
with warm humid summers and relatively mild winters. Mean annual precipitation
is 1625mm, although differences in average annual precipitation of more
than 600mm have been recorded between a peak and valley only 15km apart.
Snow accumulations may reach 1.2m at 1,500m, but are negligible below
1,000m.
VEGETATION The deeply dissected landscape present
at the southern end of the Appalachian chain provided a refuge for a host
of temperate and boreal species during Pleistocene glaciation. This has
resulted in a rich vegetation mosaic comprising approximately 1,500 species
of flowering plants, including 130 trees, and an estimated 2,200 cryptogamous
taxa. Approximately 20% of the park's forest is high in 'virgin' attributes
(National Park Service, pers. comm., 1995). Areas which were farmed or
logged have been recovering for varying periods of time and now represent
a range of successional stages. Deciduous broad-leaved and evergreen coniferous
forests predominate, but treeless grass and heath balds, open wet meadows
and cliffs communities also occur. Vegetation changes continuously with
elevation, slope, aspect and topographic position.
Fourteen major forest types are currently recognised
within the park. On mesic sites, low and mid-elevation cove hardwood (mixed
mesophytic) and hemlock-hardwood forest grade, with increasing elevation,
into northern hardwoods and finally, at about 1,500m, into spruce-fir.
On a gradient from mesic to xeric, the cove hardwoods are replaced by
mixed oak, xeric oak, and oak-pine. Heath balds represent the xeric extreme
at higher elevations and are dominated by ericaceous shrubs such as Rhododenron
catawbiense, R. minus, Kalmia latifolia and Leiophyllum
buxfolium. Perhaps the most notable forest types are cove hardwood
and spruce-fir. The former may contain over 20 different species in the
canopy at any one site. Dominants often include Liriodendron tulipifera,
Halesia carolina, Acer saccharum, Aesculus octandra
and Prunus serotina. One single tenth-hectare plot may support
in excess of 50 species throughout the year. Spruce-fir forest type only
occurs at the highest elevations and contains the largest contiguous block
of virgin Picea rubens on earth. About 75% of all Southern Appalachian
spruce-fir occurs within the park. Additionally, grass balds, ridges,
cliffs and landslide scars within these high elevation forests support
the growth of rare regional endemics. Fifteen plants are listed as candidates
for federal protection as threatened or endangered species. Moreover,
120 species are recognised as rare enough to be of managerial concern.
A similar number of bryophytes, lichens and fungi are also considered
rare at either the regional, national, or global level.
FAUNA Reflecting the richness of the flora,
the diverse fauna includes at least 50 native mammals. With the exception
of black bear Ursus americanus, white-tailed deer Odocoileus
virginianus and introduced wild boar Sus scrofa, large mammals
are not encountered. However, there are many medium sized mammals including
red fox Vulpes fulva, grey fox Urocyon cinereoargenteus,
racoon Procyon lotor, opossum Didelphis marsupialis, woodchuck
Marmota monax and bobcat Lynx rufus. Several squirrels are
seen including eastern chipmunk Tamias striatus, red squirrel Tamiasciurus
hudsonicus, grey squirrel Sciurus carolinensis and two types
of flying squirrel, the southern Glaucomys volans and the northern
endangered subspecies Carolina flying squirrel G. sabrinus coloratus
(E). Other smaller mammals include muskrat Ondatra zibethicus,
cottontail rabbit Sylvilagus floridanus, and a number of mice,
mole and shrew species. Beaver Castor canadensis, apparently once
common here, are beginning to reappear in several valleys. Mustelids include
long-tailed weasel Mustela frenata, mink M. vision, and
skunks. River otter Lutra canadensis has beensuccessfully reintroduced.
Several species of bats inhabit the park; the threatened Indiana bat Myotis
sodalis (V) is known to use at least three of the park's caves as
a winter roost. There have been several recent, but unconfirmed, sightings
of puma Felis concolor. Bison Bison bison and elk or wapiti
Cervus elaphus were extirpated by the early 1800's. Although there
are no plans at present to reintroduce bison, preliminary work has been
initiated to determine the feasibility of reintroducing elk. Grey wolf
Canis lupus (V), fisher Martes pennanti and red wolf Canis
rufus (E) formerly occurred here, and the latter is currently being
reintroduced (National Park Service, pers. comm., 1995). Recently, coyote
Canis latrans has migrated naturally to the park.
Over 200 species of birds have been observed, including
many species of warblers, flycatchers and other migratory songbirds. Over
60 permanent residents including ruffed grouse Bonasa umbellus
and wild turkey Meleagris gallopavo can be seen all year round.
Peregrine falcon Falco peregrinus has been reintroduced. Red-cockaded
woodpecker Picoides borealis had been observed nesting, but has
not been seen since the early 1980's and the species has probably become
extinct due to fire supression. Some habitats in the park contain bird
communities with an unusually high percentage of species that are neo-tropical
migrants, a group that has declined significantly in North America in
recent decades. As the largest unfragmented forest left in the eastern
U.S., park bird populations may be stable, in part due to avoidance of
cowbird Molothrus ater, a prolific nest parasite (National Park
Service, pers. comm., 1995).
Reptile species include seven turtles, eight lizards
and 23 snakes. Heavy precipitation and numerous streams make the mountains
ideal for a wide variety of amphibian species including about 30 salamander,
two toads and at least ten frogs. For its size, the park has one of the
richest salamander faunas in the world with species that vary from the
endemic pigmy salamander Desmognathus wrightii, to the aquatic
hellbender Cryptobranchus alleganiensis. Over 40 species of native
fish inhabit the streams, including eastern brook trout Salvelinus
fontalis (the park's population may be a separate and threatened subspecies)
(National Park Service, pers. comm., 1995). Other threatened fish species
include smoky madtom Noturus baileyi, yellow-fin madtom N. flavipinnis
(V) and spotfin chub Hybopsis nonacha, which are currently being
reintroduced into the park.
The park also contains a diversity of invertebrates,
especially land snails, spiders, insects and other arthropods, that are
not well known. The park is thought to be a regional or continental centre
of diversity for several of these groups. Over 100 species of caddisflies
and stoneflies are found, including stonefly endemics such as Megaloptera
williamsi, Hansonoperla appalachia, several Capnia species
and Acroneuria lycorias (found only in Sevier County). Over 800
Lepidopteran species have been recorded. Most groups reveal a complex
assortment of forms that often include species endemic to the park and/or
new to science.
CULTURAL HERITAGE Archaeological sites support
the theory that prehistoric people (15,000 years ago) were hunters and
gatherers. Present historical and cultural interpretation in the park
is based mainly on structures dating from the middle 1800s to 1920, including
the finest collection of log buildings in the United States. The National
Register of Historic Places includes three historic districts, four structures
and 29 buildings.
LOCAL HUMAN POPULATION No information
VISITORS AND VISITOR FACILITIES The park records
about 8.8 million recreational visits each year and is the most visited
national park in the country (National Park Service, pers. comm., 1995).
Use of camping grounds, trailer parks, hotels and other infrastructure
are now encouraged outside the park. Facilities within the park include
three visitor centres, ten campgrounds (three primitive), and 18 shelters
along the Appalachian Trail and other back country trails (668km), ten
picnic areas, numerous backcountry campsites and over 1,448km of trails.
The parks conducts an active visitor services programme which primarily
interprets the natural and cultural resources of the area and provides
visitor information. There are six amphitheatres and one campfire circle.
A wide variety of publications and interpretive literature about the park
is made available by the Great Smoky Mountains Natural History Association.
This association also operates the Great Smoky Mountains Institute, which
is a live-in facility that accommodates 120 people and offers environmental
education programmes for school groups, teacher workshops, adult programmes,
elderhostels etc.
SCIENTIFIC RESEARCH AND FACILITIES Many scientific
inventories are planned or underway, and the park is setting up a long-term
monitoring program for selected species and communities focused on biodiversity
issues. Numerous research projects are undertaken each year by academic
institutions, other agencies and co-operators. A career research scientist,
from the National Biological Service, is stationed in the park to conduct
and assist in the co-ordination of research (National Park Service, pers.
comm., 1995).
CONSERVATION VALUE The region is a Pleistocene
refuge and includes remnants of a diverse Arcto-Tertiary geoflora, with
a large number of temperate species. Great Smokey Mountains also contains
the finest collection of log buildings in the USA, dating from the mid-1800s
to 1920.
CONSERVATION MANAGEMENT The park is particularly
valued by visitors for the seemingly endless vistas of forested mountains.
A limited area contains visitor, maintenance and administrative facilities
and the park also contains Cades Cove, Noah Ogle and Roaring Forks historic
districts and Oconaluftee archaeological district. The remaining area
has been allowed to revert to a forest state through natural plant succession
processes and much management effort is directed at keeping human impact
to a minimum. The park has a general management plan and a resource management
plan supported by a variety of natural resource action plans developed
to mitigate specific threats to the park's resources. The system of zoning
comprises natural zone (92%), historic zone (1%) and development zone
(7%). Generally, the collection of natural resources is not permitted.
Exceptions are by scientific permit, fishing permit (mostly for non-native
species) and fruits, nuts, berries and certain mushrooms when picked by
hand for personal use only (National Park Service, pers. comm., 1995).
MANAGEMENT CONSTRAINTS Several road systems
pass through the park as well as over 1,280km of horse and foot trails
which dissect the high country. The three historical zones have open fields
of grass and Cades Cove supports a cattle operation. Subsistence farming
and commercial logging have been practised in the past, and logging railroads
were built. Some of the park's 1,200 historical structures have been removed,
destroyed or allowed to deteriorate. Over 20 non-native plant and several
animal species are known to cause significant impacts to natural resources.
Management strategies for exotic plants are being actively applied. Non-native
forest insects and diseases, mostly from Europe and EastAsia are devastating
certain tree species, shifting natural communities and reducing formerly
abundant species to rare ones. Wild boar has been controlled since the
mid-1950s and are removed regularly. In order to protect and perpetuate
rapidly declining native brook trout populations, control efforts have
been conducted against two competitive non-native trout species. Continuing
problems include visitor abuse of backcountry resources; poaching of wildlife,
particulary native brook trout, deer, black bear and American ginseng
Panax quinquefolius. Other significant threats include air pollution,
since high elevations receive some of the highest acid depositions in
North America, and ozone levels are elevated to the point of injury to
some plant species. Since inception of park management, total suppression
of all wild fires has accounted for unnatural accumulation of fuels and
changes in the forest mosaic, which in unfavourable to fire-dependent
plant and animal species (National Park Service, pers. comm., 1995).
STAFF 255 (214 full-time, and part-time employees
and 41 temporary employees) (National Park Service, pers. comm., 1995).
BUDGET The financial statement for 1995 was
approximately US$10.3 million (National Park Service, pers. comm., 1995).
LOCAL ADDRESSES
Superintendent, Great Smoky Mountains National Park,
107 Park Headquarters Road, Gatlinburg, Tennessee 37738 (Tel: (615) 436
1705)
REFERENCES
The park library has numerous reference documents, and
there are numerous publications relating to the park. A full bibliography
of scientific study has been published by the Southern Appalachian Research/
Resources Management Cooperative and Western Carolina University (1982,
US MAB Report No. 4, Washington DC) which also published a history of
scientific study in the area (1982, US MAB Report No. 5, Washington, DC).
Campbell, C.C. (1960). Birth of a National park in
the Great Smoky Mountains.
Maps: 1:125,000 Great Smoky Mountains National Park
and Vicinity, US Geological Survey.
USDI/NPS (1977 to present). Research/Resource Management
Report Series. National Park Service, Southeast Region, US Department
of the Interior/National Park Service.
USDI/NPS (1982). General Management Plan - Great Smoky
Mountains National Park, North Carolina-Tennessee. (1982) US Department
of the Interior, National Park Service, Denver Service Center, Denver,
CO. 70pp.
DATE August 1982, revised August 1986,
May 1990, July 1995
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