The Forked Deer River system is the main drainage of the central portion of West Tennessee.
The Forked Deer consists of various streams designated "Forked Deer" and their tributaries. Much of the Forked Deer basin was initially wetlands; however much of this area has been drained and most Forked Deer tributaries have been channelized for agricultural In the mid 20th century much of this was done under the auspices of the Obion-Forked Deer Basin Authority, a Tennessee state agency. Environmental concerns have led to the cessation of channelization on a widespread basis; the federal government's "no net loss" policy regarding wetlands means that further channelization must be offset by creating new wetlands, called "mitigation lands", elsewhere.
Much of the channelized flow is routed into the Obion River just above the mouth of that river into the Mississippi, other streams related to the system have their own mouths into the Mississippi. It should be noted that in some areas where the historic channels are left in place even after the bulk of the flow has been routed into new ones that the historic channels at times still demonstrate considerable flow, especially after heavy rains.
The South Fork of the ForkedDeerRiver at Jackson, Tennessee
The ForkedDeerRiver system is the main drainage of the central portion of West Tennessee.
Much of the ForkedDeer basin was initially wetlands; however much of this area has been drained and most ForkedDeer tributaries have been channelized for agricultural In the mid 20th century much of this was done under the auspices of the Obion-Forked Deer Basin Authority, a Tennessee state agency.
The Big Sandy River of Tennessee rises about five miles (eight km) northwest of Lexington, Tennessee, county seat of Henderson County, Tennessee, in the same vicinity as two other important rivers of West Tennessee, the Beech River and the Middle Fork of the ForkedDeerRiver.
Like the Beech (and unlike the ForkedDeer, which flows to the MississippiRiver), the Big Sandy flows to the Tennessee River.
Despite the extensive channelization activity, much of what the river must have been like prior to this can be seen in the wetlands surrounding it near the Interstate 40 bridge and also along State Route 69 between Camden and Paris.