The History Behind The District's Creation
It was in the early 1900's
that the Houston area began to see the first true signs of
human-induced land subsidence -- initially attributed to the
extraction of oil and gas from beneath the surface, and
relegated to the land immediately in and around the center of
the oil fields. But the future would hold a much more
widespread and insidious cause for subsidence in our area -
expanding industry and a growing population's water needs.
Houston was growing and
it was growing fast. Increased oil production and the
establishment of the Port of Houston in 1925 were creating an
industrial and population "boom". The area's plentiful supply
of fresh groundwater helped to fuel the massive growth, but
ultimately, the community's need outpaced the aquifer's
ability to safely sustain their demand for water.
In the early 1940's,
new studies began to identify problems due to groundwater
extraction. Original land-subsidence benchmarks, established
just after the turn of the century, were releveled in the
40's, and the results verified that subsidence was occurring.
In the 1950's and
1960's, community leaders finally began to link the increased
frequency and severity of flooding to subsidence. In the
sub-tropical, low-lying areas of Houston/Galveston -- where
tropical storms and hurricanes were a probability, not just a
possibility-- flooding was real and could be severe. In 1961,
when Hurricane Carla hit, our worst fears about the impact of
subsidence were confirmed. The storm had been horrific and
some water damage was not surprising, but the flooding that
occurred was beyond what was, in the past, expected from a
hurricane of this size. As a result, local area governments
began to analyze the serious and very real impact subsidence
could have on the area's potential economic growth and quality
of life, and, just as important, began to determine what
exactly could be done about it.
With a number of
studies linking groundwater withdrawal to subsidence -- and
ongoing measurements confirming those findings -- groups of
citizens began to work for a reduction in groundwater use in
the late 1960's. By 1973, the City of Galveston had begun
converting to surface water supplied from Lake Houston, and in
May of 1975, the Texas Legislature created the
Harris-Galveston Subsidence District (HGSD), the
first of its kind in the United States. Authorized as a
regulatory agency created to "end subsidence" and armed with
the power to restrict groundwater withdrawals, the Subsidence
District immediately went to work on a plan to positively
impact the critical situation in the coastal areas.
By 1976, the District
had begun the process of compiling hydrologic information on
the characteristics of the Chicot and Evangeline aquifers,
engineering planning information on water usage and water
supply in Harris and Galveston counties, and implementing
regulatory procedures associated with their first groundwater
regulatory plan. By converting industries on the Houston Ship
Channel to surface water supplied from the recently completed
Lake Livingston reservoir, subsidence in the Baytown-Pasadena
area was dramatically improved, and has since been largely
halted.
But as subsidence was
stabilizing in the coastal areas, groundwater levels in inland
areas north and west of Houston were rapidly declining. In the
Evangeline aquifer, measurements recorded a decline of more
than 100 feet between 1977 and 1997.
As a result of the
increasing threat subsidence posed to these areas, the HGSD
adopted a series of regulatory plans to reduce groundwater
pumpage, and ultimately mandated, in their 1999 plan, a
reduction to only 20% reliance on groundwater by 2030. With
the help of the North Harris County Regional Water Authority
(NHCRWA) and the West Harris County Regional Water Authority
(WHCRWA), both created by the Texas Legislature to transition
the areas to surface water in the allotted timeframe, a fair
and equitable contract with the City of Houston to supply
surface water from Lake Houston was successfully negotiated
and construction is already underway in both Authority areas.
It is our goal that the same dramatic improvements will occur
in these areas as were experienced south and east of Houston
years ago.
The HGSD, along with
numerous utility districts and other public and private
partners, have also worked hard to educate the public on water
conservation, for one very simple reason: The future of our
water supply not only depends on where we get it, but on how
EFFICIENTLY we are able to use it. (Please take a moment to go
through our web site and read about our highly successful
Waterwise program).
Water is an element
that has no substitute, and our need for it will always be
there. The population in our area will only continue to grow,
and our need for water will grow right along with it. It is
the responsibility of the HGSD -- as well as those of us
fortunate enough to live in this wonderful area -- to treat
our precious natural resources as the treasures they are-- not
only for us, but for those who will be here long after us.
This is a responsibility we take very seriously and we
appreciate your interest and support in achieving this goal.
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1906: |
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Documented
land-subsidence elevations initially established |
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1925: |
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U.S. Army Corps of Engineers completes dredging of the
Houston Ship Channel. Houston becomes a deep-water port.

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1926: |
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Pratt and Johnson
present first report drawing a correlation between fluid
withdrawal and subsidence ("Local subsidence of the
Goose Creek Oil Field")


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1930: |
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City of Houston and the U.S. Geological Survey (USGS)
begin collection of the hydrological characteristics of
the Chicot and Evangeline aquifers |
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Early 1940’s:
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Benchmark
relevelings performed - verify that subsidence is
occurring (Baytown area had subsided 3.2 feet; Texas
City area had subsided 1.6 feet) |
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1950's: |
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Continued documentation of substantial additional
subsidence |
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1954: |
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Lake Houston
completed and canals constructed to supply surface water
to the City of Houston's East Water Purification Plant
and to industry in the eastern portion of Harris County. |
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1958: |
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The
first extensometer specifically for the measurement of
subsidence is constructed by USGS at the City of
Houston's East-End well field. |
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1950’s & 60’s:
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Several studies
released linking the relationship between groundwater
withdrawal and subsidence (1954: Winslow and Doyle;
1959: Winslow and Wood; 1969: Gabrysch) |
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1961:
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Hurricane Carla hits area - brings realization to the
region that there is an increased likelihood of flooding
due to subsidence.

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1975: |
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The Harris-Galveston
Subsidence District created by the 64th
Legislature |
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1984: |
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Devastating flood on Brays Bayou renews concern about
the effects of subsidence in inland areas |
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1987: |
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A network of 82
benchmarks installed – distributed throughout the
districts to determine elevation changes using the
Global Positioning System (GPS). |
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1989: |
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Fort Bend Subsidence District created in legislative
session to manage and control subsidence in Fort Bend
County |
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1999: |
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Harris-Galveston
Subsidence District adopts its most recent
regulatory plan establishing an ultimate groundwater
reduction goal for north and west Harris - to reduce
groundwater pumpage to 20% of total water demand by
2030. |
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2003: |
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Fort Bend Subsidence
District adopts new regulatory plan establishing
groundwater reduction requirements for certain
permitees of 30% by 2013 and 60% by 2025. |
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