This report is preliminary and has not be en reviewed for conformity
with U.S. Geological Survey editorial standards or with the North
American Stratigraphic Code. Any use of trade, product, or firm names
is for descriptive purposes only and does not imply endorsement by the
U.S. Government.
This database, identified as mf2264, has been approved for release and
publication by the Director of the USGS. Although the database has
been subjected to rigorous review and is substantially complete, the
USGS reserves the right to revise the data pursuant to further
analysis and review. Furthermore, it is released on condition that
neither the USGS nor the United States Government may be held liable
for any damages resulting from its authorized or unauthorized use.
Digital_Form:
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Format_Version_Number: 7.x
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Earthquake locations, faults, well locations, and other geographic features shown on the printed maps
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Format_Information_Content: COCORP seismic reflection line traces
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Format_Information_Content: graticule for the map
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Format_Information_Content: point cover of all the .1250 interval tics in the 2x2grat area
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Format_Information_Content: axial gravity anomaly (Langenheim, 1995)
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selected hydrography, selected on the basis of significant ground-shaking or liquefaction potential
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Bootheel Lineament as observed on low-altitude photos and transferred to 1:24,000 scale topographic maps (Schweig and others 1992)
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Format_Information_Content: Bootheel Lineament as observed on landsat images
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Format_Information_Content: selected cities
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Format_Information_Content: state and county borders in the map area
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locations of probable subsurface ruptures of the 1811-12 earthquakes, as defined by sandblow distribution (Obermeier, 1989)
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damaging earthquakes (moment magnitude ? 5.0) since 1811-12 as defined by EPRI (Johnston, 1994)
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earthquakes located by the St. Louis University from July 1974 to December 1992, Taylor and others (1991)
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Format_Information_Content: locations of faults identified by geologic observation
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Format_Information_Content: locations of Global Positioning System monuments
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structures identified from gravity-field data (Langenheim,1995)
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Format_Information_Content: locations of ground-water anomalies (Brahana and Mesko, 1994)
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intrusive complexes defined by aeromagnetic studies (Hildenbrand and Hendricks, 1995)
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P-velocity contours for depths 5 - 14 km (Al-Shukri and Mitchell, 1987)
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P-velocity contours for depths 0 - 5 km (Al-Shukri and Mitchell, 1987)
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landslides along the Chickasaw Bluffs, mapped by Jibson and Keefer (1988) at 1:62,500 scale
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Format_Information_Content: depth to magnetic basement (Hildenbrand and Hendricks, 1995)
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polygon coverage of the Mississippi River extracted from basehyd
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Format_Information_Content: Fischer and Schumm's (1995) locations of historical centerlines
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Fischer and Schumm's (1995) locations of historical shorelines of the Mississippi River from 1765 to 1960
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Reelfoot Graben structures interpreted from magnetotelluric data
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Format_Information_Content: paleozoic surface depth contours from Dart (1995)
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control points for defining the paleozoic surface from Dart (1995)
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Format_Information_Content: subcrop contacts on the paleozoic surface from Dart (1995)
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Format_Information_Content: polygons of the 1:24000 scale topographic maps in the area
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Format_Information_Content: railroads on the 100k DLG's
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Format_Information_Content: class 1 and 2 roads (major 4-lane and principle 2-lane roads)
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Format_Information_Content: structures identified in seismic reflection research
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river anomalies throughout the New Madrid region identified by Fischer and Schumm (1995)
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outlines of Obermeier's (1989) definitions of areas covered by greater than 1% and greater than 25% sandblows from the 1811-12 earthquakes
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Format_Information_Content: selected wells from Dart (1992)
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significant structures visible at the surface in the vicinity of New Madrid
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locations of seismograph stations that have operated in the New Madrid region since July 1974
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Format_Information_Content: arcs from cnty with bndytype = 1; see cnty for description
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stress orientations either from borehole breakouts or earthquake focal mechanism solutions updated in Ellis (1994)
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Format_Information_Content: strong motion seismometers
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trenches examined for prehistoric earthquakes and a report has been published
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wells from Dart (1992) in the map area. See selwell for wells used in MF-2264
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