FLOOD CONTROL PROJECT FOR THE
JACKSON METROPOLITAN AREA
Flood Elevations
Benefits
Flood Frequency
Lake Map
This is a proposal intended to solve the flooding problems in the
Jackson area in such a manner that the attractiveness and growth potential of the
metropolitan area would also be enhanced. Flood levels would be permanently lowered in the
Byram to Jackson area by providing a better flow course for the passage of water and by
reducing the rate of flow in the river . The graph below shows the profile of the flood
levels that occurred in the 1979 flood. On this graph a person can see the extra water
that had been backed up into the area north of Jackson. The curve also shows what both the
1979 flood and the 100 year frequency flood are projected to be after the proposed lake
has been constructed and the improved reservoir discharge plan has been implemented (The
better flow course would enable the reservoir to develop an improved discharge plan).

A person whose home or
business flooded during the 1979 flood can use the following chart to determine what level
of protection his structure would derive from the implementation of this plan. If a person
has an accurate water mark on his structure made by the 1979 flood, that person could
determine whether the structure would receive water in another 1979 flood by measuring
down to his slab level from this mark. Column 2 shows where the new 1979 flood level would
be. A person whose structure would still receive water in a 1979 flood (a 200 year flood)
may be protected from a 100 year flood. This could be determined by using column 3. The
best way to determine the level of protection for any structure would be to survey the
elevation of the structures slab and refer to column 1.
FLOOD ELEVATION
|
Present Condition |
Effect of lake |
Change due to lake |
Column 1 effect of lake plus
improved discharge |
Change due to improved discharge |
Column 2 distance from 1979 flood
mark down to new 1979 level |
Column 3 distance from 1979 flood
mark down to a 100 yr frequency flood |
| Byram 1979 |
264.9 |
265.2 |
+0.3 |
264.1 |
-1.1 |
-0.8 |
|
| Byram 100 yr |
263.6 |
263.8 |
+0.2 |
262.6 |
-1.2 |
|
-2.3 |
| Richland 1979 |
272.7 |
273.1 |
+0.4 |
271.8 |
-1.3 |
-0.9 |
|
| Richland 100 yr |
271.5 |
271.7 |
+0.2 |
270.4 |
-1.3 |
|
-2.3 |
| Lynch Creek 1979 |
276.6 |
273.8 |
-2.8 |
272.6 |
-1.2 |
-4.0 |
|
| Lynch Creek 100 yr |
275.0 |
272.3 |
-2.7 |
270.7 |
-1.6 |
|
-5.9 |
| Towncreek 1979 |
277.7 |
274.0 |
-3.7 |
272.7 |
-1.3 |
-5.0 |
|
| Towncreek 100 yr |
276.1 |
272.3 |
-3.8 |
270.8 |
-1.5 |
|
-6.9 |
| Highway 468 1979 |
284.7 |
275.5 |
-9.2 |
274.6 |
-0.9 |
-10.1 |
|
| Highway 468 100 yr |
282.0 |
274.7 |
-7.3 |
273.7 |
-1.0 |
|
-11.0 |
| Lakeland 1979 |
284.7 |
275.5 |
-9.2 |
274.6 |
-0.9 |
-10.1 |
|
| Lakeland 100 yr |
282.0 |
274.7 |
-7.3 |
273.7 |
-1.0 |
|
-11.0 |
| Hanging Moss Crk 1979 |
286.5 |
276.2 |
-10.3 |
275.1 |
-1.1 |
-11.4 |
|
| Hanging Moss Crk 100 yr |
283.4 |
275.3 |
-8.1 |
274.2 |
-1.1 |
|
-12.3 |
MAXIMUM BENEFITS THAT
WILL RESULT FROM THE
FLOOD CONTROL LAKES ALONE WITH NO ADDITIONAL BENEFIT
FROM RESERVOIR REGULATION
Flood benefits at 1979 Flow Rate
350 Year Probability
| Position |
1979 Actual |
Flood Lake |
Difference |
|
|
|
|
| 1. Richland Flood Plain |
272.9 |
273.3 |
+ 0.4 feet |
| 2. Lynch Creek |
276.6 |
273.8 |
- 2.8 |
| 3. Town Creek |
277.7 |
274.2 |
- 3.5 |
| 4. Island South End |
281.0 |
275.0 |
- 6.0 |
| 5. Island North End |
283.7 |
275.2 |
- 8.5 |
| 6. The Quarter |
283.7 |
275.2 |
- 8.5 |
| 7. Twin Lake Subdivision |
284.0 |
275.7 |
- 9.2 |
| 8. Canterbury Court SBV |
285.8 |
276.0 |
- 9.8 |
| 9. Hanging Moss Creek |
286.4 |
276.1 |
-10.3 |
| 10. McLeod SBV |
286.8 |
276.3 |
-10.5 |
| 11. Canton Club SBV |
287.1 |
276.5 |
-10.6 |
| 12. Dam |
288.4 |
277.0 |
-11.4 |
MAXIMUM BENEFITS THAT CAN BE DERIVED BY
SUBTRACTING AN
ADDITIONAL 1.25 FEET THAT WILL RESULT FROM IMPROVED
REGULATION OF THE RESERVOIR
Renefits derived from reservoir regulation will be discounted
according to the consistency with which reservoir inflow can
be predicted from rainfall as it is measured on the ground.
This discount value will be applied to the chart below when a
computer model for inflow projection has been completed.
| Position |
1979 Actual |
Flood Lake |
Difference |
|
|
|
|
| 1. Richland Flood Plain |
272.9 |
272.0 |
- 0.9 feet |
| 2. Lynch Creek |
276.6 |
272.6 |
- 4.0 |
| 3. Town Creek |
277.7 |
272.9 |
- 4.8 |
| 4. Island South End |
281.0 |
273.9 |
- 7.1 |
| 5. Island North End |
283.7 |
274.2 |
- 9.5 |
| 6. The Quarter |
283.7 |
274.2 |
- 9.5 |
| 7. Twin Lake Subdivision |
284.0 |
274.7 |
-10.2 |
| 8. Canterbury Court SBV |
285.8 |
275.0 |
-10.8 |
| 9. Hanging Moss Creek |
286.4 |
275.1 |
-11.3 |
| 10. McLeod SBV |
286.8 |
275.3 |
-11.5 |
| 11. Canton Club SBV |
287.1 |
275.5 |
-11.6 |
| 12. Dam |
288.4 |
276.0 |
-12.48 |

The 1979 flood was rated as a 500 year event by the
USGS in a 1982 study. The inclusion of another large flood in 1982 had the effect of
reducing the rating of the 1979 flood to a 350 year frequency event.

All the structures that flooded in the 1979 flood
should be protected from a 100 year flood by the new lake and the improved reservoir
discharge procedure. Additionally, the plan would provide that surveying be conducted in
order to determine what structures exist in the various flood prone areas that would not
be protected from the 1979 flood (a 200 year flood). If any structures exist that need
protection, auxiliary plans would be considered and if warranted, additional protection
would be extended to these structures.
The improved flow course for the river would be
created by removing the trees from the very lowest level of the river flood plain (the
river bottomland). This level would then be lowered approximately five feet with dredges
and/or trackhoes and earth moving equipment and then the entire eleven mile river course
opposite Jackson would be made into a permanent lake. (See following map of lower level
flood control lakes). A lake would be necessary to prevent the redistribution of sand and
silt and to prevent the regrowth of trees in the river flow course.
It would be necessary to remove very large amounts
of sand from beneath the numerous railroad and highway structures south of downtown
Jackson. This is needed to provide the proper flow course thru this area of the river. The
levees and bridges are presently blocking the river’s flow and backing water up into
Jackson homes and businesses. In order to have some place to put this sand the Flowood
levee would be moved to the east and the excavated material would then be put in the
middle of the newly formed lake. This would create a 600 acre island opposite downtown
Jackson. North of Lakeland the dredged material would be placed on the east side of the
newly formed lake.

The following map shows how the dredged material could be turned
into an asset. This would be accomplished by accessing the newly created land with bridges
and by constructing interchanges, parkways and city streets over it and along the entire
length of the three thousand acre lake. Many of the roads and bridges are needed at this
time to alleviate the metropolitan areas traffic congestion. Both the traffic and flooding
problems could be solved at once and at less cost than plans for previous flood control,
roads and bridges. This is because the newly created land would offer no impediment to
construction.
Any flood control plan, to be successful, must pass
the give and take considerations of the many communities that it will have an effect upon.
The Jackson area has four distinct areas that will be effected in different ways by any
flood control plan. We hope that the features of this plan that might be objectionable to
a given area can be overcome by the good features that it contributes to that area.
Reservoir people would expect that on two or three
occasions each year the water’s level, over a period of a day and a half, will fall
one foot then rise again to its original level. Once every 25 years they would be warned
to untie moorings and move boats because the level will be taken down below 295 feet. On
the positive side, they would enjoy an extra one half to one foot of water in their boat
slips.
Some people in northeast Jackson who appreciate
hiking in the existing river bottom areas and who want to preserve the wetlands that exist
there would be compensated by knowing that two thousand of their neighbors will never have
to worry about their homes and businesses flooding again.
A few people in downtown Jackson built metal
buildings at very low elevations and will not be protected from another 1979 flood, but
they will be compensated by having protection from a 100 year flood on structures that
probably will not last 100 years.
People who own land and camps on the river south of
Jackson would experience one or two river bottom floods that they would not have had
otherwise but they would be compensated by the assurance that the reservoir would have the
capacity to take one foot of elevation off of every major flood that could occur in the
area. One foot off of the 1979 flood would have prevented much of the flooding that these
people’s neighbors suffered in 1979.
Anyone reading this proposal is reminded that we intend to change it
in any way possible to overcome their concerns. Please let us hear from you.
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