This field guide describes three accessible sites along the Dandridge-Vonore fault zone in the Eastern Tennessee seismic zone. These sites reveal bedrock faulted against Quaternary river sediments, including (1) a thrust fault on the Little River near Alcoa, Tennessee; (2) a series of thrust faults exposed in a drainage ditch that thrust Conasauga Shale against Quaternary colluvium in the footwall; and (3) a normal fault at Tellico Lake near Vonore, Tennessee, with Quaternary sediments faulted against Conasauga Shale
A series of high-resolution seismic reflection surveys was carried out in 2008, 2010, and 2011, prov...
Two reflection seismic profiles at English Hill, across the southern edge of the Benton Hills escarp...
Bureau Publication GC8001 - to purchase a print copy please go to: https://store.beg.utexas.edu/geol...
The eastern Tennessee seismic zone (ETSZ) is the second-most active seismic zone in the eastern Unit...
A geologic investigation of the city of Memphis and southern Shelby County, Tennessee reveals Quater...
The southeastern Reelfoot Rift margin is expressed as a series of collinear scarps across western Te...
The East Tennessee seismic zone (ETSZ) is the second most active in the eastern United States, but r...
Approximately 320 km of deep seismic-reflection profiles in northwestern Tennessee r veal the struct...
The New Madrid seismic zone of the central United States is an intraplate seismic zone with blind st...
The Reelfoot reverse fault, a major northwest-striking and southwest-dipping fault within the New Ma...
The stratigraphy and structure beneath Dyer County, Tennessee, were mapped using lignite exploration...
A geologic investigation of the city of Memphis and south-ern Shelby County, Tennessee r veals Quate...
Basement structures and their relationship to the Alleghanian thrust system in the vicinity of the N...
Geophysical and drill-hole data within the Reelfoot rift of Arkansas, Tennessee, Missouri, and Kentu...
A newly recognized thrust and nearby asymmetric anticline crop out 40 km north of Memphis, Tennessee...
A series of high-resolution seismic reflection surveys was carried out in 2008, 2010, and 2011, prov...
Two reflection seismic profiles at English Hill, across the southern edge of the Benton Hills escarp...
Bureau Publication GC8001 - to purchase a print copy please go to: https://store.beg.utexas.edu/geol...
The eastern Tennessee seismic zone (ETSZ) is the second-most active seismic zone in the eastern Unit...
A geologic investigation of the city of Memphis and southern Shelby County, Tennessee reveals Quater...
The southeastern Reelfoot Rift margin is expressed as a series of collinear scarps across western Te...
The East Tennessee seismic zone (ETSZ) is the second most active in the eastern United States, but r...
Approximately 320 km of deep seismic-reflection profiles in northwestern Tennessee r veal the struct...
The New Madrid seismic zone of the central United States is an intraplate seismic zone with blind st...
The Reelfoot reverse fault, a major northwest-striking and southwest-dipping fault within the New Ma...
The stratigraphy and structure beneath Dyer County, Tennessee, were mapped using lignite exploration...
A geologic investigation of the city of Memphis and south-ern Shelby County, Tennessee r veals Quate...
Basement structures and their relationship to the Alleghanian thrust system in the vicinity of the N...
Geophysical and drill-hole data within the Reelfoot rift of Arkansas, Tennessee, Missouri, and Kentu...
A newly recognized thrust and nearby asymmetric anticline crop out 40 km north of Memphis, Tennessee...
A series of high-resolution seismic reflection surveys was carried out in 2008, 2010, and 2011, prov...
Two reflection seismic profiles at English Hill, across the southern edge of the Benton Hills escarp...
Bureau Publication GC8001 - to purchase a print copy please go to: https://store.beg.utexas.edu/geol...