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Last updated: October 11, 2002
South Florida Restoration Science Forum

Our Coastal Ecosystems

The Southwest Florida Project Coordination Team:

How are we expanding the science needed for effective resource management?


National Park Service

Big Cypress
National Preserve

Everglades
National Park

Restoration of the Turner River

By Bob Sobczak,
Hydrologist, Big Cypress National Preserve


 
  
Canoests and kayakers typically access Turner River off the Tamiami Trail, about 5 miles east of Barron River Road (CR29).
Turner River is a meandering stream that originates in the mixed cypress swamp of Big Cypress National Preserve and empties into Chokoloskee Estuary of Everglades National Park.  Maintaining the river's health is important because it meanders through many of the reasons behind the establishment of the Preserve.
Turner River meanders for 9 miles from its headwater pools in Big Cypress National Preserve to its estuarine tailwaters in Everglades National Park.
map of Turner River

(Click on image above for larger version.)

Importance of the river

arrows
It is part of the upstream watershed that delivers freshwater discharge to the shallow coastal waters of Everglades National Park.
illustration of trees and river
Its corridor provides a continuity between the range of freshwater and saltwater habitats of the region. Its headwaters form in mixed cypress swamp and its tail-waters meander through mangrove tunnels.
illustration of canoest
Its channel provides canoe and kayak access for visitors to explore the diversity and solitude of the swamp away from roadways and without the assistance of a motorized off-road vehicle.
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The river has been restored by the efforts of the National Park Service in cooperation with state and county officials.  It is a true success story of how a resource can be recovered from the brink of extinction.


How the river dried up

illustration of landscape

(Click on image above for larger version.)
Seemingly minor alterations to the landscape can have drastic consequences to natural hydrologic and vegetation patterns in south Florida.  As shown in the figure to the left, elevated roadbeds block sheetflow movement and canals redirect water away from its natural drainages.
note: colored asterisks * in the text and figures below correspond with colored asterisks in the timeline at the end of this page
*Before it was disturbed, water levels and flows in Turner River naturally fluctuated in concert with its upstream watershed.  During the summer rainy season, water levels would rise until a shallow "sheetflow" covered the landscape.  This sheetflow then fed into the headwaters of the river and flowed to sea.

As shown in the above figure, *construction of Turner River Road cut the river off from its contributing watershed.  The elevated roadbed blocked sheetflow from the river and the roadside canal drained most of the water away from the headwater pools of the river.

This drastically altered the ecology of the river corridor; including:  (1) reduced water levels and flows, (2) altered timing of flow to its estuarine tailwaters, (3) unnatural vegetation growth in the channel and river corridor, (4) displacement of wildlife, and (5) displacement of canoests and kayakers to the canal because of lack of flow and too much vegetation in the river.


How the river was restored

Establishment of Big Cypress National Preserve in 1974 brought the Turner River and its watershed under the single jurisdication of the National Park Service.

In 1980, a restoration plan was devised for getting water back into the river's headwaters.  The plan called for (1) a series of earthen dams (or plugs) to prevent water from draining down the canal and (2) a series of culverts to re-route water under the elevated roadbed. Plugs are coded red and culverts are coded green on the lower left map. The plan was implemented in 1988.

In 1996, the southernmost mile and a half of the Turner River Canal was filled in by pushing the adjacent berm back into the canal. This is shown in the zoom view below. This action was needed because water was continuing to flow around the plugs and down the canal. Results were (1) increased flow in the river and (2) discontinuation of canoe and kayaking in the canal.

Additional actions are still necessary.  Water continues to bypass around plugs in some locations as shown below and to the right.  Actions are also needed to improve recreational opportunities such as marking and clearing parts of the channel.

*This map shows the 1980 plan for getting water back into the river. The basic idea was to put culverts under the roadbeds and plugs in the canals.
maps

(Click on image above for larger version.)
 
*In 1996, the southernmost stretch of the canal was filled in.  This action redirected both water and canoests back to the river.
*Water continues to sneak around the plugs during high water conditions, as shown in the figure to the right. Additional actions to improve instream flow and recreational use of the river are being considered in a Turner River Management Plan. illustration of landscape

Click on image below for a full-sized version.

Turner River Timeline

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U.S. Department of the Interior, U.S. Geological Survey, Center for Coastal Geology
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Last updated: 11 October, 2002 @ 09:42 PM (KP)