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How Sinkholes Develop
There are many detailed, scholarly reports that are
available for those desiring a more thorough and highly
technical discussion of this topic. What follows here is
intended only to be a brief “consumer friendly” summation of
sinkhole development.
Sinkholes are depressions or holes in the land surface. They
can be shallow or deep, small or large, but all are the
result of the dissolving of the underlying limestone.
Hydrologic conditions, including lack of rainfall, lowered
water levels, or conversely, excessive rainfall in a short
period of time (especially after a drought) can all
contribute to sinkhole development. New construction, new
roads, and any diversion of water flow are also common
culprits.
Solution activity within the limestone is greatest along
localized fractures, joints, or bedding planes, since these
features represent preferential paths that concentrate the
flow of water into the formation. This activity is
accelerated where the volume of flow increases. In Florida,
especially, infiltration rates are very high; sometimes
upwards of 75%, and this increased volume transports soil
into the voids and speeds the dissolving of the limestone
rock. The dissolution of the limestone can be accelerated
even more if the rainwater permeates through vegetation.
This makes it more acidic. Obviously, the closer to the
surface the limestone is, the more likely that a sinkhole
can occur, although there are many that are very deep.
Despite many so-called insurance
company experts, many sinkholes occur below layers of clay.
Sinkholes occur naturally, and it is estimated that the
majority of all lakes in Florida are a result of sinkhole
activity. Sinkholes are common where the rock below the land
surface is limestone and other carbonate rock, which can
naturally be dissolved by water. As the rock dissolves, the
ceiling of the cavern becomes thinner. When the land above
the cavern becomes too heavy for the ceiling to support, a
depression or collapse of the land surface can occur. The
damage can be minor or significant depending upon what
structure is immediately above the sinkhole activity and how
much ground is disturbed. Abrupt collapse sinkholes have
become more common over the past several decades,
proportionate to the increased activity of humans, which
involves building, withdrawal of ground water, diversion of
surface water, and etc. Even the “repair” of some sinkholes
by grouting can cause more damage and create new sinkholes
by the added weight to the soil and from the diversion of
the current water flow.
Spotting the Signs of a Sinkhole
Just
as there are several different types of sinkholes and all
different types of homes and landscapes, sinkholes may
appear very differently.
If you think you may have sinkhole damage to your
home, the first thing that is done is determining whether or
not it’s actually a sinkhole, as defined by
Florida
law.
Roads,
driveways, sidewalks or other pavements may be cracked or
sitting at funny angles.
Floors might be off level in the house.
This can be checked by setting a ball in the middle
of a room and watching if it rolls in a way it hadn’t
before. Such
activity can easily crack the underlying concrete slab.
You may
notice your doors no longer hang correctly in their frames
and won’t close or lock.
Windows can even break in their frames or refuse to
work properly anymore.
Large gaps in between the house and the door or
window frames can appear -- sometimes large enough to see
thorough or let critters in. Cracks in the wall at the
corners of doors and windows are a common result of sinkhole
activity.
Inside,
if your water comes from a well, it might come out the tap
discoloured when the soil movement causes pipes to break and
let dirty water seep in.
If so, it’s very possible those pipes are leaking
water back into the soil, and the problem might be getting
worse by the moment.
If
the sinkhole under your house or other structures is large
enough, you may find some disturbing changes in the building
itself. These
can manifest as large cracks that form in lines that point
toward the middle of the hole or, zig-zags as along bricks,
known as “stair-step” cracking.
Generally
speaking, it’s a good idea to periodically check around
garages, barns, swimming pools and any other development on
your property. A
sinkhole can open up anywhere.
The condition of buildings, vegetation and the ground
itself can be quickly surveyed by eye.
When professionals come in to scientifically verify a
sinkhole, they may use one of several techniques to get a
“picture” of the rock below.
Of these techniques, taking a simple drill core is
the crudest and often yields poor results.
Other devices create a 3-D map of the property using
radar or other sonic technology.
One
of the more obvious sign of sinkhole activity is the
appearance of a round hole on your property where there
wasn’t one before.
Often these are filled with the soil that fell in and
water, but they may be filled with dissolved rock that looks
like sludgy water and other debris, too.
Sometimes, if the water table is higher than the lip of the
new hole, the water can gush out like a spring, causing even
more water to work on the soil beneath.
Such sinkholes are very dangerous, because they tend
to get bigger for some time before they stabilize and can be
repaired.
However,
even if you don’t have a gaping chasm on your property yet,
there are signs that you can look for that will alert you to
the conditions that mean sinkhole formation may be imminent.
These clues may be on the ground, affecting the
vegetation and structures upon the land or already causing
damage to the building itself.
On
the ground there are some obvious changes in the way water
moves through your soil that impact the things living or
just sticking in it.
For instance, you may find a circle of wilted plants.
As water drains way into the hole, it can starve the
plants above of water – especially if they are annual plants
with shallow root systems.
Sometimes trees will begin to lean over – sometimes
dangerously. It
may happen so slowly you don’t notice until someone else
points it out.
Often, upon inspection, you’ll find their roots are exposed
as if they’re being pushed out of the ground.
This is an especially ominous sign if there is a ring
of such damage around a central area of wilting vegetation.
Items
that are in the ground, such as poles or fence posts may
also begin to lean or tip over.
One may also find the ground loosened around such
objects, as if someone had been pushing and pulling in an
effort to remove it.
The ground itself may form observable cracks.
These will often appear in either a circular pattern
or along radial lines.
The
soil around your house or other building may become
unsettled and prone to shifting.
This will be evident by a sudden change in the
texture of the soil around the foundation and perhaps by a
change in the vegetation found there.
Small
ponds of any size may form where they normally don’t.
Clear water is just groundwater filling a hole in,
whereas mucky water may represent a type of sinkhole that
contains a high concentration of the dissolved rock in the
collected water.
This type is especially common where soils are very thin.
Such holes often continue to fill and sink over time,
eventually collapsing.
If
you observe the signs of sinkhole activity on your property,
contact a professional and your insurance company
immediately.
Changes to Florida
law that take effect after June 1, 2007, will make it much
harder, if not impossible, to claim sinkhole damages after
that time. If
your house appears to be succumbing to sinkhole activity,
make a claim with your insurance company immediately.
Depending on the extent of the damage, it may be
dangerous to remain in your home.
Keeping an eye out for such damage could mean the
difference between safety and harm for your family.
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