Remote sensing for lineaments in the Mississippi Embayment
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Abstract
A recurrence of an 1811-12 type earthquake in the Mississippi Valley would pose severe problems to construction in the valley. As William Stauder has stated in the preceding article, a particular difficulty in understanding the seismicity of this area is that, whereas various surface manifestations of the 1811-12 earthquakes have been well documented (for example, sandblows and sunken lands), active fault zones have never been recognized. There may be different reasons for this.
Study Area
Publication type | Article |
---|---|
Publication Subtype | Journal Article |
Title | Remote sensing for lineaments in the Mississippi Embayment |
Series title | Earthquake Information Bulletin (USGS) |
Volume | 9 |
Issue | 1 |
Year Published | 1977 |
Language | English |
Publisher | U.S Geological Survey |
Description | 5 p. |
First page | 14 |
Last page | 18 |
Country | United States |
Other Geospatial | Mississippi embayment |
Online Only (Y/N) | N |
Additional Online Files (Y/N) | N |
Google Analytic Metrics | Metrics page |