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.
Suggested Citation
O'Leary, D., 1977, Remote sensing for lineaments in the Mississippi Embayment: Earthquake Information Bulletin (USGS), v. 9, no. 1, p. 14-18.
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 |