Late hologene episodes of deformation along the central reelfoot scarp, Lake County, Tennessee
In. U.S. Central United States Earthquake Consortium (CUSEC). Hazard assessment preparedness, awareness, and public education emergency response and recovery socioeconomic and public policy impacts : Proceedings. Memphis, Tennessee, U.S. Central United States Earthquake Consortium (CUSEC), 1993. p.195-203, mapas.
Monography
in En
| Desastres -Disasters-
| ID: des-6598
Responsible library:
CR3.1
Localization: CR3.1; DES
ABSTRACT
This research is desinged to assess Holocene tectonic defornmation in the Lake County uplift region, and to evaluate the recurrence of large - magnitude earthquakes in the Central New Madrid seismic zone. A 90-m long trench across the central reelfoot scarp exposed fluvial levee and overbank deposits overlain by colluvial deposits at the base of the scarp. Liquefaction related features include unweathered sand dikes and sills that intrude into the fluvial deposits. We interpret that the sand dikes and sills are results of the A.D. 1811-12 earthquakes, and that the colluvial deposits along the scarp estimated that the time between the two most - recent earthquakes large enough to produce liquefaction and/or surface deformation along the scarp is about 200 to 600 years (AU)
Full text:
Available
Collection:
Tematic databases
Health context:
SDG3 - Target 3D Strengthen the capacity for early warning, risk reduction and management of national and global health risks
Health problem:
Hydrometeorological and Geophysical Hazards
Database:
Desastres -Disasters-
Main subject:
Risk Assessment
/
Earthquakes
Type of study:
Etiology study
/
Risk factors
Country/Region as subject:
North America
Language:
English
Year:
1993
Document type:
Congress and conference
/
Monography