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 |