Land-surface subsidence in the area of Moses Lake near Texas City, Texas

Water-Resources Investigations Report 76-32
Prepared in cooperation with the U.S. Army Corps of Engineers
By:  and 

Links

Abstract

Removal of water, oil, and gas from the subsurface in Harris and Galveston Counties has caused declines in fluid pressures, which in turn have resulted in subsidence of the land surface. Subsidence of the land surface at Moses Lake in due principally to the removal of ground water in adjacent areas. Significant subsidence of the land surface at Moses Lake began after 1900, and as much as 1.8 feet of subsidence had occurred in the ara by 1973.

Probable future subsidence was calculated by two methods for two loading situations. In the first loading situation, the artesian head in the middle Chicot aquifer, in the Alta Loma Sand (Rose, 1943), and in the Evangeline aquifer would continue to decline at respective rates of 1, 3, and 3 feet per year until 1980 and then cease. In the second loading situation, the artesian head in the middle Chicot aquifer, in the Alta Loma Sand, and in the Evangeline aquifer would continue to decline at respective rates of 1, 3, and 3 feet per year until 1990 and then cease. 

Study Area

Publication type Report
Publication Subtype USGS Numbered Series
Title Land-surface subsidence in the area of Moses Lake near Texas City, Texas
Series title Water-Resources Investigations Report
Series number 76-32
DOI 10.3133/wri7632
Year Published 1976
Language English
Publisher U.S. Geological Survey
Publisher location Austin, TX
Contributing office(s) Texas Water Science Center
Description v, 42 p.
Country United States
State Texas
Other Geospatial Moses Lake
Online Only (Y/N) N
Additional Online Files (Y/N) N
Google Analytic Metrics Metrics page
Additional publication details