Over
the last 30 years, pollution in the Neponset River
has been cleaned up, the buildings along its shores have been
converted to residential and commercial rather than industrial
use and its banks have been opened up and improved for
recreation. All of these changes have dramatically increased
the river’s importance as an aesthetically pleasing backdrop
that people can enjoy as they go about their daily business.
Without question, any dam removal project changes the
appearance of a river, although the change often is not as
dramatic as one might imagine. Aesthetic concerns also are the most subjective issue
to be evaluated when
considering dam removal. NepRWA believes that dam removal presents a unique
opportunity to enhance the river’s aesthetics.
The
first and most challenging task in evaluating river aesthetics
post-dam removal, is to accurately visualize the change before
it occurs.
What would a free-flowing
Neponset
River
look like?
A
free-flowing
Neponset
River
will look, more or less, like the parts of the Neponset
River
that are free flowing already.
When a dam is removed, the water levels behind the dam will
drop vertically, and in most cases the river will become narrower
than the previous mill pond (e.g., the pooled water
behind the dam). However, removing the dam does
not change the amount of water that flows down
the river every day, so although the depth and width of
the former impoundment will change, the river itself will not
dry up. The amount by which the depth and width of the river
will change depends on the shape of the riverbed, both across
its width and along its length.
A mill pond typically presents a slow-moving, lake-like
appearance. Furthermore, most mill ponds create at least the
appearance of a more or less constant depth and width
throughout the seasons. By contrast, a free-flowing stream
presents a more dynamic appearance, as the river meanders back
and forth and works its way over or around obstacles. The
appearance of a free-flowing river typically varies
considerably across the four seasons as water flow varies from spring snowmelt to summer dry periods.
Another critical factor in determining the appearance of a
free-flowing river is the slope of the riverbed. The steeper
the riverbed, the faster the water moves. Free-flowing rivers
with a shallow slope tend to be slower moving, wider, deeper,
meandering and marshy, with soft, muddy bottoms. A steeper
riverbed translates into faster moving water and a narrower,
shallower channel. The faster moving water also tends to scour away
fine muddy deposits, leaving behind a streambed of coarse
sand, gravel or boulders and producing the proverbial
“babbling brook” or even a white-water rapid.
Natural processes tend to produce rivers that change character
at regular intervals, from upstream to
downstream. Rather than being all slow moving or all rapids,
rivers tend to adopt a natural variation with a slow moving
“pool” followed by a fast moving “riffle,” and then a
smoothly flowing “run.” This pattern is so common that it
is referred to as the “riffle, run, pool” pattern. This
variation creates visual as well as auditory interest. It also
creates a diverse array of micro-habitats that host a tremendous diversity of plant and animal species.
Note
that in a dam
removal context, it is possible to partially control the
formation of riffles, runs and pools by intentionally
configuring the riverbed.
Because dam removal makes the river narrower, it also creates
new areas along the river's edge that will be colonized by a
variety of plants and some of which will become wetlands. The
character of these “new riverbanks” will vary depending on
the steepness of the riverbank. In some areas where the
riverbanks are very steep, the width of the river will hardly
change at all and there will be no new vegetation. More gently sloping
areas will tend to be marshy or
grassy if they are inundated during much of the year, shrubby if they
get flooded at least a few times per year, and wooded in areas
that are generally inundated less than every other year.
The “new” riverbanks created following a dam removal will
re-vegetate rapidly, even without any active replanting. The pattern of vegetation can be controlled by
adjusting the shape of the stream channel or by periodic
pruning in drier areas. The newly exposed areas will not smell
unless there is pollution getting into the stream, in which
case the mill pond would have smelled, too.
The best way to really understand how these visual changes
might play out is to take a tour of the Neponset
River
as it exists right now, and see with fresh eyes what the river
really looks like in areas where it is and is not dammed.
Who can see the river now?
Under existing conditions, there is virtually no visual access
to the T&H Dam and very little visual access to its mill
pond. Access to the T&H Dam is obstructed by
the former paper mill on the
Boston
side of the river and by abandoned industrial land and locked
gates on the
Milton
side. The impoundment is largely fenced off, and can be seen
only by a few abutting homeowners and from a few locations
such as near the
Martini
Shell Park along Truman Parkway, and where bridges
span the river. Because of this
limited visual access, there has been no objection to removal of
the T&H Dam based on aesthetic concerns.
There is significantly more visual access to the Baker Dam and
its impoundment. During the winter and early spring, the Baker
Dam can be seen by looking upstream from Adams Street,
at Lower Mills. However, during the summer, foliage obscures the
Baker Dam from view
on the Adams St. bridge. The Baker Dam and its
mill pond can be seen from the Neponset Greenway Trail, and the public can approach the dam
itself from there. In addition, some units of the Baker Square Condominiums have a view of the
mill pond and/or the Baker Dam.
December
2009