California faults are nearer the surface. It makes nice artwork. Many structures in Memphis, Tenn., St. Louis, Mo., and other communities in the central Mississippi River Valley region are vulnerable and at risk from severe ground shaking. Fuller talks about the environmental impact of the quakes. City above marked Caruthersville, should be Sikeston. https://mrdata.usgs.gov/services/wfs/sgmc2. Show in Google Earth or other KML viewer: https://mrdata.usgs.gov/services/sgmc2 (WMS, version 1.3.0), https://mrdata.usgs.gov/services/wfs/sgmc2 (WFS, version 1.1.0), Preliminary integrated geologic map databases for the United States : Alabama, Florida, Georgia, Mississippi, North Carolina, and South Carolina, Detailed report of standardization procedures, Methods used to create several styles for lithology or geologic time. Likely from David Stewart. However, it wasn’t until the discovery of the Cascadia Fault in the 1960s th… Lewis & Clark found the Shawnee village north of Cape Girardeau in 1803 and said it numbered 400 inhabitants. They got the canal finished about the same time they decided to sneak one, then another gunboat past island 10. more. Memphis was not available for European settlement until after 1812, and an agreement with the Chickasaw Indians. The Yanks had several iron-sided gunboats waiting just upriver for three weeks. Caruthersville is near Tiptonville. Area is now northern Cape Girardeau County. The New Madrid Seismic Zone , sometimes called the New Madrid Fault Line, is a major seismic zone and a prolific source of intraplate earthquakes (earthquakes within a tectonic plate) in the Southern and Midwestern United States, stretching to the southwest from New Madrid, Missouri. Benton Hills, Bloomfield Hills, Western Lowlands, Eastern Lowlands, Sikeston Ridge, Oran-Bell City Gap Share. Clicking a map will usually take you to its source. above shows connection of Wabash Fault and New Madrid Faults. Moore, William Halsell, 1969, reprinted 1985, Geologic Map of Mississippi, Compiled by Bicker, A. R., Jr., a revision of the geologic map published by the MS Geological Survey in 1945 in cooperation with the USGS, revised from data submitted by Dr. E. E. Russell of MS State University from published reports of the MS Geological Survey and from field revisions, Mercury Maps Inc., Jackson, MS. Water polygons that are generated when standard state base map is used. Many quakes are 5-10 miles underground, but some are more than 100. There is broad agreement in the scientific community that a continuing concern exists for a major destructive earthquake in the New Madrid seismic zone. Until 10,000 years ago the Ohio flowed a bit north of its current route across Southern Illinois, then along the south side of the Benton Hills. Point Pleasant had some Civil War involvement, but the main Civil War activity was just to the right of Google map. The levee makes a slight detour to include the new town, and 30-40 people who currently live there. Fuller's book, made from horseback observation 100 years ago, is regarded as authoritative. Map pages 1 | 2 | 3 | 4 | 5 | 6 | 7 | aerials | sitemap. An online map of United States Quaternary faults (faults that have been active in the last 1.6 million years) is available via the Quaternary Fault and Fold Database. The white area just upriver on Google Earth map is current site of power and aluminum plants. At 8 a.m. January 23, 1812, another big shake struck, north of Caruthersville. The Yanks dug a shallow canal that came out just east of New Madrid, to bypass Island 10 and move supplies. The hatched regions are plutons. Many scientists now consider these quakes high 7's. Many tribes even left the region permanently. Thinner northwest trending lines denote the approximate lateral extent of the Missouri batholith. See topography- The Thebes gap of the Mississippi River is relatively young, about 10,000 years old, probably helped by earthquakes along the Commerce Lineament. There is an interactive map application to view the faults online and a separate database search function. Map and info below come from book "On Shaky Ground: The New Madrid Earthquakes of 1811-1812" By Norma Hayes Bagnall 1996. The upper 30 meters of sediment within the embayment includes sand, silt, and clay deposited by the Mississippi, Ohio, St. Francis, and White Rivers and their tributaries over the past 60,000 years. A GIS database of geologic units and structural features in Mississippi, with lithology, age, data structure, and format written and arranged just like the other states. Compare this picture to the quake diagrams, models of one section being forced underneath another. The town of Point Pleasant, southeast of Marston, on a point of land sticking into the Mississippi River, completely crashed into the river and was swept away without a trace. This is a Corps of Engineers map from about 1944, from Cape Girardeau Mo to Donaldsonville, La. By the time Lewis and Clark arrived on the West Coast in 1805, it had been 105 years since the Cascadia Subduction Zone last ruptured, sending a large portion of the Pacific Ocean roaring toward the coast. The few remaining Native Americans in the area spoke of the earth shaking and ocean rising to consume the land. Thick lines denote the boundary of the Reelfoot rift. This is how some of it might appear. The older Richter scale measurements saturate at higher levels. http://www.amnh.org/nationalcenter/youngnaturalistawards/1999/hagenauer.html. This map came from Close environmental. The Rebs had 30 guns on Island 10 at bottom of river loop. By Nina Godlewski On 12/12/18 at 10:03 AM EST . The townspeople had all fled, a month earlier, because of the tremors. Triangles are seismic stations. Then a gap developed between the Benton Hills and Bloomfield Hills (Crowley's Ridge), allowing the river to flow through the "eastern lowlands" -- the Oran - Bell City gap, just west of Sikeston Ridge. In Fig. The white line on Google Earth map above shows one mile. The Mississippi embayment is a broad trough filled with marine sedimentary rocks about 50-100 millions years old and river sediments less than 5 millions years old. KML (Google Earth-type) files and GIS shape files are also available for download from the site. The town was rebuilt, perhaps a mile west of the original location. The illustration shows how the Mississippi River has meandered over the centuries. Fault Line Map in United States: USGS Facts After Tennessee Earthquake. Benton Hills, Bloomfield Hills, Western Lowlands, Eastern Lowlands, Sikeston Ridge, Oran-Bell City Gap. This photo shows a section of the San Andreas fault alongside a road in Palmdale, California, an hour north of Los Angeles. 1.4 the Mississippi River, during the first part of the age of glaciers, flowed from the top inlet of the map (Cape Girardeau), to the "western lowlands" near Poplar Bluff, before spilling out across the bootheel and eastern Arkansas. Memphis was built on/near the "fourth Chickasaw bluffs (just north of town). The New Madrid Fault is well below the surface and none of it is visible. Map originally from State of Missouri Handbook 1945-1946. This assessment is based on decades of research on New Madrid earthquakes and related phenomena by d… Moore, William Halsell, 1969, reprinted 1985, Geologic Map of Mississippi, Compiled by Bicker, A. R., Jr., a revision of the geologic map published by the MS Geological Survey in 1945 in cooperation with the USGS, revised from data submitted by Dr. E. E. Russell of MS State University from published reports of the MS Geological Survey and from field revisions, Mercury Maps Inc., Jackson, MS.
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