LITTLE RIVER CANYON NATIONAL PRESERVE
"The Grand Canyon of the South"


All photos by CDaniels unless noted otherwise

The Little River and its canyon are located on the Cherokee and Dekalb County lines in Alabama and is one of the newest of the national preserves.  The National Park Service recently bought about 9,000 acres of land from the Alabama Power Company to form the Little River Canyon National Preserve.  Adjacent to the preserve is the state-owned DeSoto State Park.  It is a national preserve since it allows hunting while a national park does not.  Hunting is regulated by the Alabama Game and Fish Division and monitored by the Game and Fish and National Park Service Rangers.  Along with the river and canyon, there is a backcountry accessible only by 19 miles of dirt road with three primitive campsites open from February through September.  There are no charges at the whole preserve except a $2.00/vehicle parking charge at the mouth of the canyon.

  Map: Courtesy of USGS

TEACHER ACTIVITIES:

*Teachers will have the opportunity to photoshoot throughout the canyon/river trip.  They will follow the Little River as it traverses through the canyon stopping at several overlooks and walking just a short distance, up to a mile, wherever the terrain permits safe passage.  Each teacher will be instructed on how to make a primitive walking staff from broken tree branches.  They will be encouraged to use the staff while hiking to allow easier walking through the woods and to push poison ivy from their path.  At the end of the canyon they will be seining the river at the mouth of the canyon and snorkling to collect  data on the river's aquatic inhabitants.

 
 

FACTS TO KNOW:

Also known as "The Little Grand Canyon," or "The Grand Canyon of the South", Little River Canyon is one of the deepest gorges east of the Mississippi River.

The canyon was formed over the eons, by the rushing waters of the Little River as it carved its way through the soft sandstone slabs of the Cumberland Plateau section of the Appalachian Plateaus Province.  The Cumberland is a giant geological formation that covers much of Tennessee and juts into Alabama from the northeast as far south as Tuscaloosa County. Its highest point is the northern end of Lookout Mountain in De Kalb County, about 2,000 feet above sea level.  From here the plateau slopes down to about 500 feet in the south.


Courtesy of National Park Service.  Unpaginated.  Jamestown, ND:
     Northern Prairie Wildlife Research Center Home Page.
     http://www.npwrc.usgs.gov/resource/othrdata/chekbird/r4/info.htm
     (Version 22MAY98)

Courtesy of National Park Service.  Unpaginated.  Jamestown, ND:
     Northern Prairie Wildlife Research Center Home Page.
     http://www.npwrc.usgs.gov/resource/othrdata/chekbird/r4/info.htm
     (Version 22MAY98).

The Little River and the canyon it has formed are two of the most unique geologic features in Alabama.  It is among the longest rivers in the United States that forms and flows most of its entire length on top of a mountain.  It begins at 1900 feet above sea level and traverses on top of Lookout Mountain.  The Little River then plunges off the Cumberland Plateau at the head of the canyon and ends up at Weiss Lake at 650 feet above sea level.  The canyon's elevations range from 560 to 1752 feet above sea level.  When you stand at the edge of the rim of the canyon and peer down, you will see Little River as a narrow ribbon of water zig-zagging through the canyon.  The canyon is more than 20 miles and plunges 900 feet down at its deepest point.  Its width varies from one half mile to a mile and a half.

Some of the rocks show the effects of compressional forces buckling and changing the shape of the layers.  Lookout Mountain is a syncline!!  Its strata on the mountainous areas are synclinal, bending downward, while the valley areas are anticlinal, with the strata bending upward.  This is due to the fact that uplifting has raised the whole area  but more erosion has occurred on the anticlines which now form the valleys below!!

Courtesy of National Park Service

Lookout Mountain area is within the Appalachian Plateaus and the Ridge and Valley systems.  Mountain ridges and valleys trending in a northeast-southwest direction characterize the Ridge and Valley Province and this is where stratified rocks are highly inclined.  Along the magins of Lookout Mountain, some of the strata are sharply upturned.  The valley structure results from the folding and faulting of the Paleozoic rocks that form the base of Lookout Mountain.  The bulk of the area which falls in the Appalachian Plateau province exhibits only minor deformation.


Erosion has formed expanses of unique rock formations, benches, canyon rims and bluffs.
Needle Eye Rock or Mushroom Rock is a natural rock formation in the middle of Hwy. 176.









Little River is free-flowing, its flow being under the direct control of the amount of precipitation on the mountain.  There are no dams, anthropogenic channels or other man-made structures influencing the flow of water in the canyon.  During some dry summers, the water flow could be just a trickle.  But a little bit of rain in these mountains means a lot of water rushing through the narrow canyon walls.  And a lot of rainfall can quickly change the white caps of the water into a thunderous surging river.

According to Park Ranger Larry Beane,  Little River is noted for being pure and unpolluted.  It begins its journey along the top of Lookout Mountain through an upland forest then it plunges 45 feet at the Little River Falls just south of the bridge at Ala. 35. . The canyon begins at the falls where we started our trip.  As it starts its descent down the mountain, the river picks up speed and carves its way through one of the deepest gorges in the eastern United States.  It continues to carve the sandstone even today.

The river and canyon have become a unique habitat for many endangered and threatened species.   Most of it is protected as the Little River Canyon National Preserve when Congress added the canyon and river  to the National Park  System in 1992.  The preserve covers 14,000 mountainous acres and protects 35 miles of the Little River and its surrounding feeder streams and gorges.  The Little River watershed covers 199 square miles of critical habitat for unique species of plants and animals such as carnivorous green pitcher plants, green salamanders, the endangered blue shiner fish, and Kral's water plantains, an aquatic herb only found in this river ecosystem.

The views along the canyon is spectacular any time of year.  The uplands and canyon slopes are covered with hardwoods such as American Beach, hickories, yellow poplar,  black gum, and oaks.  Under the canopy are under story trees including flowering dogwood, huckleberries, sourwood, and sassafras. 

On the forest floor, ferns and mosses abound.


Wildflowers can be found blooming for most of the year.
Depending on the time of year, you may see cascades of  fall colors, brilliant golden and white daisies, wild azaleas, mountain laurel or Catawba rhodondendron. 
 








The canyon and river ecosystems support many migrant and temperate zone birds, including the Southern bald eagle and other predatory birds.  According to the National Park Service, there are close to 100 bird species found in the preserve, many of which are threatened or endangered.

The American peregrine falcon,  vultures and hawks can be seen flying over Hawk's Glide overlook. In the early evening, the Indiana bat may be observed.

 The climate is mild, humid, and temperate having four distinct seasons.  Average temperature hovers at 60 degrees Fahrenheit.  Average annual rainfall for the Little River area is about 54 inches.  Winter months bring more rain and higher levels of water in the river.  January is the wettest month (6.7 inches).   October is the driest with less than 3.5 inches.  The summers have moderately hot days and fairly cool nights.  Winters are mild and pleasant. The temperature on occasion falls below freezing during the night and may remain below freezing for 1 to 3 days. Snow is not common and averages about 3 inches per year but does not stay long, melting away as the sun shines.
One of the most popular activities here is paddling the river's water.  Kayaks and canoes abound in the 25 or so miles of  water in the canyon especially in the spring when rains bring the river's level high enough for such names as "Suicide Run" and "Devil's Curve".   In the summer, the deciduous forest canopy is emerald but the leaf-color-changes in the fall rival those in the Northeast.  People forget they are in the South.


  Within the gorge one can find a number of sandstone walls measuring from 30 to 80 feet.  The angle of overhang varies from just over vertical (say 75 to 80 degrees) to really overhanging (45 to 30 degrees).











 Upstream in the canyon, a series of falls restrict fish movement, so the fish community there is not very diverse.  In  the river below the canyon, however, the fish fauna is quite diverse including an excellent population of the federally threatened blue shiner.  The snorkeling here is quite good.

Snorkling on a clear day should allow us to see  longnose gar, Alabama blue and tricolor shiners, Mobile logperch, and freshwater drum.  The sein net should give us a greater glimpse of the biodiversity of this aquatic ecosystem.  We should be able to see several species of darters, minnows, shiners, sculpin, stoneroller, sunfish and bass.


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