About the District
The Fort Bend Subsidence District was created by the Texas Legislature in 1989 as a conservation and reclamation district (Act of May 26, 1989, 71st Leg., R.S., ch. 1045, 1989 Tex. Gen. Laws 4251). The District’s purpose is to regulate the withdrawal of groundwater within the District to prevent subsidence that contributes to flooding and infrastructure damages. The District’s boundary is defined as all the territory within Fort Bend County. Although Fort Bend County experienced minor amounts of subsidence prior to the 1980’s, several characteristics of the area raised concern about the potential for increasing subsidence in the future such as:
- Rapid growth
- Water supply dependent almost entirely on groundwater
- Proximity to significant water-level declines in Harris county
Currently, total water use in the District comprises about 50% groundwater and 50% alternative water, which is primarily sourced through surface water and waste water reuse. The District was formed to address measured impacts from the predominant use of groundwater. In addition to the moderate, but noticeable, amounts of subsidence, the heavy dependence of groundwater has resulted in declining water levels. Groundwater levels in wells drawing from the Chicot/Evangeline Aquifer in the northern part of the District have declined in excess of 160 feet from 1990 to 2021. (Source: 2020 Annual Groundwater Report) These declines have resulted in increased operational costs to well users and increased subsidence throughout the area. The District regularly analyzes the adequacy of the current District Regulatory Plan and Rules to assure they continue to meet the District’s legislative mandate.
News & Updates
Revised Office Hours for November 18-22, 2024
Our office hours for the week of November 18, [...]
Office Closure – November 11, 2024 for Veterans Day
The Fort Bend Subsidence District will be closed on [...]
Subsidence in Fort Bend and Surrounding Counties
The Fort Bend Subsidence District operates GPS stations in Fort Bend county. These stations are part of a dense GPS network in the Houston-Galveston region called HoustonNet, which includes a collaboration of local and state agencies to monitor the land surface elevation. The HoustonNet comprises GPS stations operated by the following agencies.
GPS observations/data are collected at the GPS station for approximately seven days every two months. The University of Houston processes the raw GPS data and produces a time series displacement plot. The linear regression (i.e., best fit line) of the ellipsoidal height component, which essentially measures the land surface elevation, is used to determine the subsidence rate. Other collaborators include the United States Geological Survey (USGS) and the National Geodetic Survey (NGS). A network of extensometers is maintained by the USGS to provide key insight into aquifer compaction. The NGS has been an integral partner in establishing the District’s monitoring program since the 1990s.