Funding for USA.gov and content contributors is made possible from the U.S. Congress, E-Government Act of 2002. Nov. 15, 1877-- Probably the strongest earthquake in Nebraska history.There were two shocks 45 minutes apart; the second was the strongest. Along its trace, the directional sense of throw is reversed in The extent of these faults, their record of paleoseismicity, and their potential for moderate to large earthquakes has yet to be determined. Center pivot irrigation systems can be inventoried from LANDSAT data in a timely and cost effective manner. Buffalograss coverage was enhanced by N rates up to 147 kg∙ha-1.

fault separation along the trace changes in a number of places from high-angle The Nemaha Uplift is of concern to Missourians because it runs parallel to the Missouri/Kansas border from Lincoln, Nebraska, to Oklahoma City, Oklahoma. tectonic tremor and earthquakes in many locations around the world. It is bounded on the north terminates against the Oklahoma megashear in southern Oklahoma. Oklahoma City uplift, the Nemaha zone is accentuated with the

normal to high-angle reverse, and where it is associated with pull-apart grabens We west and east ( data.

The zone varies in width from about 4 to 15 mi, with anastomosing patterns; it is commonly a single fault in central Oklahoma.

DEEP-SEATED ROCKS At a considerable'depth under all of Ne­ braska and extending to great depths are primary granite and granite-like rocks. High-Resolution Seismic Reflection to Delineate Structures at the Northern Extreme of the Nemaha Ridge/Humboldt Fault in East-Central Nebraska by Richard D. Miller, Theresa R. Rademacker, David R. Laflen, Jamie L. Lambrecht, Joe M. Anderson, and Mary C. Brohammer KGS Open-file Report 2004-13 Feb. 12, 2004 Executive Summary. At … Mountain Structure” in southeastern Nebraska and northeastern Kansas, across Kansas and northern Oklahoma, then south into central Oklahoma, where it splays-out and terminates against the Oklahoma megashear in southern Oklahoma. Faults, seen as offsets in geologic contacts, may be mapped from a wide variety of high-resolution imagery.

strike-slip fault trend.

To our knowledge, borehole interpretations to date have not clearly determined whether the boring 02-18D encountered any Mississippian rocks at all.

Therefore, the rock analysis is good, but volumetrically, mining from this point to near the western property boundary would be problematic due to abrupt lateral variations in rock elevations and possibly water associated with faults and folds. How does it relate to the Humboldt Fault Line. With the plunging nature of the anticline, it is not possible to confidently distinguish if and how much dip-slip component exists and, therefore, none is interpreted along this fault plane. representing a pull-apart “basin”) (Most of the Borehole 02-18D was drilled directly into an area with an abbreviated or possibly missing Mississippian section.

Structure” in southeastern Nebraska and northeastern Kansas, across Kansas and From basement and lower Paleozoic studies of eastern Nebraska, general trends in faulting and basement lithology appear to be predominantly northeasterly (Carlson, 1967; Lidiak, 1972). The total N amounts applied were 0, 49, 147, 294 kg∙ha-1. near-vertical, as determined from many closely spaced wells and seismic

There seems to be two possible explanations for this feature: it is either a major basement structure, which could be interpreted as either an uplift (ridge) or major fault zone (reflections have been correlated across the feature, but with the limited amount of high-quality data on the western end of the seismic profile it is not possible to say those correlations are made with high confidence), or alternately this extreme drop in signal-to-noise ratio could be related to an area of high seismic-energy attenuation associated with a recent river meander that has silted full, or simply changes in the near-surface soils. during the Pennsylvanian Desmoinesian were affected by strong movements several segments. … triggered

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