Tiptonville Household Pharmacy 650 Carl Perkins Pkwy, Tiptonville Tn 38079
The datasets generated for this study is not going to be made publicly obtainable. The datasets are geologic interpretations made by the corresponding creator and coauthor. The actual knowledge are within the form of boring nicely logs or geophysical survey lines. All data in addition to the lignite logs are non-proprietary and are housed throughout the respective organizations. The lignite logs are housed on the University of Memphis. RV has access to those logs and can be contacted if a reader wishes to review the boring logs.
The inset map also reveals the New Madrid seismic zone of northwest Tennessee, southeast Missouri, and northeast Arkansas within the northern Mississippi embayment [modified from Pryne et al. ]. Cross-Section B-B’ is a NW-SE oriented section via the center of Lake County and crosses the Axial, Cottonwood Grove, and Ridgely faults. Ridgely ridge appears to be a tilted, asymmetric horst on all mapped stratigraphic tops. The obvious down-to-the-west displacement on the highest of the Eocene throughout the AF is interpreted to be due to Mississippi River erosion.
A handful of faculties within the county are running a pilot program, “Life Check Systems,” a way to higher monitor on-campus activity. A COCORP deep reflection profile throughout the buried Reelfoot rift, south-central United States. Surface geology of Lake County, Tennessee and floor layer of the 3-D Quaternary Model in Figure 12. Individual alluvial 5 ft (1.three m) layers are in Weathers . Two cross-sections were made for each cross-section line; one unfaulted and one faulted.
Locally owned businesses are located in Tiptonville as nicely. Sherry’s Kuntry Kupboard and El Potrillo Mexican Restaurant are positioned alongside Carl Perkins Parkway. Located a short glen r dawson distance from the town are a quantity of parks such because the Reelfoot State Park and Gayoso Bend Conservation Area.
The 3-D Lake County Geologic Model graphically illustrates the subsurface construction to the top of the Paleozoic. This model and Figure three illustrate where and what sense of displacement has occurred across the Lake County faults. Perhaps more meaningful to the residents of Lake County is that Figures three, 8, 9, 10 illustrate the place and what sense of motion might occur throughout a future major earthquake. Further, it is strongly recommended that shallow seismic reflection profiles be acquired throughout these faults to better document their Quaternary displacements. Although not a focus of this research, we imagine that our Quaternary Mississippi River alluvium maps and 3-D alluvium model provide valuable subsurface information for Lake County farmers. Lake County irrigation wells pump water from shallow wells drilled into sand and gravel horizons within the Mississippi River flood plain alluvium.