Late Holocene faulting and earthquake recurrence in the Reelfoot Lake area, northwestern Tennessee
Journal Article
·
· Geol. Soc. Am., Bull.; (United States)
Faults, folds, and sand dikes have been identified in late Holocene sediments exposed in an exploratory trench excavated across Reelfoot scarp in northwestern Tennessee. In excess of 3 m of vertical displacement believed to be of deep-seated origin occurs across a 0.5-m-wide zone of east-dipping normal faults near the scarp base. The zone includes the only faults of probable tectonic origin known to cut Holocene sediments in the upper Mississippi embayment. Stratigraphic and geomorphic relationships suggest, however, that little (< 0.5 m) or no near-surface fault movement occurred across the zone during the high-magnitude New Madrid earthquakes of 1811 to 1812. Numerous faults having only minor displacements were mapped elsewhere in the trench. Geologic relationships between the faults and sand dikes indicate that the faults formed contemporaneously with the dikes during high-magnitude earthquakes. Crosscutting geologic features and local geomorphic history suggest that at least two periods of faulting predate sediments deposited before A.D. 1800. Thus historical data and the sediments in the trench record a history of three earthquakes near the trench site strong enough to liquefy sediments and generate faulting. Carbon-14 dates obtained on fresh-water shells indicate that the trench sediments have a maximum age of about 2000 radiocarbon years. A recurrence interval of approx. 600 y or less is suggested for large earthquakes in the New Madrid area. 5 figures.
- Research Organization:
- Geological Survey, Denver, CO
- OSTI ID:
- 6563860
- Journal Information:
- Geol. Soc. Am., Bull.; (United States), Journal Name: Geol. Soc. Am., Bull.; (United States) Vol. 90:2; ISSN BUGMA
- Country of Publication:
- United States
- Language:
- English
Similar Records
Recurrent faulting in the vicinity of Reelfoot Lake, northwestern Tennessee
Deformation along the central Reelfoot scarp and Lake County uplift, northwestern Tennessee
Tectonic deformation revealed in baldcypress trees at Reelfoot Lake, Tennessee
Journal Article
·
Wed Oct 31 23:00:00 EST 1979
· Geol. Soc. Am., Bull.; (United States)
·
OSTI ID:6805752
Deformation along the central Reelfoot scarp and Lake County uplift, northwestern Tennessee
Conference
·
Sun Feb 28 23:00:00 EST 1993
· Geological Society of America, Abstracts with Programs; (United States)
·
OSTI ID:7069787
Tectonic deformation revealed in baldcypress trees at Reelfoot Lake, Tennessee
Technical Report
·
Mon Jul 01 00:00:00 EDT 1991
·
OSTI ID:5667361
Related Subjects
58 GEOSCIENCES
580100* -- Geology & Hydrology-- (-1989)
580201 -- Geophysics-- Seismology & Tectonics-- (1980-1989)
CENOZOIC ERA
EARTHQUAKES
GEOLOGIC AGES
GEOLOGIC FAULTS
GEOLOGIC STRUCTURES
GEOLOGY
GROUND MOTION
MOTION
NORTH AMERICA
QUATERNARY PERIOD
SEISMIC EVENTS
SOUTHEAST REGION
STRATIGRAPHY
TENNESSEE
USA
580100* -- Geology & Hydrology-- (-1989)
580201 -- Geophysics-- Seismology & Tectonics-- (1980-1989)
CENOZOIC ERA
EARTHQUAKES
GEOLOGIC AGES
GEOLOGIC FAULTS
GEOLOGIC STRUCTURES
GEOLOGY
GROUND MOTION
MOTION
NORTH AMERICA
QUATERNARY PERIOD
SEISMIC EVENTS
SOUTHEAST REGION
STRATIGRAPHY
TENNESSEE
USA