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Volume , Issues 3—4 , 10 September , Pages Ouachita, Appalachian, and Ancestral Rockies deformations recorded in mesoscale structures on the foreland Ozark plateaus Author links open overlay panel Randel TomCox Show more https: The two earliest episodes can be assigned to progressive northwestward docking of the Ouachita terrane with North America. This suggests development of a slip-line deformation field in response to minor northeastward lateral escape of lithospheric blocks away from the northwestward-moving Ouachita terrane’s leading edge, which acted as an indenter in western Arkansas, southeastern Oklahoma, and Texas. Deformation episodes are localized along basement fault zones, particularly at major bends, suggesting minor restraining-bend uplifts along strike-slip faults. Geometries of conjugate normal fault and hybrid shear joint arrays indicate localized areas of high differential stress consistent with basement block uplift at these bends. High-angle faults reactivated in a reverse sense and bedding-parallel veins suggest tensile minimum stresses and pore fluid pressures exceeding lithostatic stress, consistent with brine pulses driven into the midcontinent during Late Paleozoic orogeny as proposed by other authors. Previous article in issue.
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Overview[ edit ] States that permit localities to go dry[ edit ] 33 states have laws which allow localities to prohibit the sale and in some cases, consumption and possession of liquor. Still, many of these states have no dry communities. Three states, Kansas , Mississippi , and Tennessee , are entirely dry by default: Alabama specifically allows cities and counties to elect to go dry by public referendum.
Kansas is dry by default; counties have to choose to allow liquor sales in order for liquor to be sold at all in the county. It is however allowed for local jurisdictions to elect to go dry by public referendum.
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He was born on June 21, , in Detroit, MI. In addition, he enjoyed travel with his family to visit historical landmarks all over the United States. He is survived by his wife Linda Trevino Martin, daughters Andrea Martin and Rachel Martin, sister Kathy Barton of Texas, and his aunts, uncles, nieces, nephews, and cousins, along with his brothers- and sisters-in-law. He was preceded in death by his parents, Adrian J. A Memorial Service will be held at 1 p.
The family will receive friends at the funeral home from 11 a. Private burial will take place at a later date. Memorial contributions may be made to the family.
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The base contributed greatly to the economic and intellectual growth of the primarily agricultural county until it closed in The base was originally a 2, acre army air field installation used by the U. Mississippi County was a prime location because of its close proximity to the Mississippi River , where supplies could easily be shipped in.
The flight school closed in October after the war ended.
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Place a small block on the top of the sand, and gradually saturate the sand with water. The block still rests on the surface. Now, strike the bucket sharply, and watch the block of wood quickly drop. This is called “liquefaction”. The same can happen to houses built, as the Bible says, ” like a foolish man who built his house on sand.
Paleoseismologists can learn a great deal by studying them. The USGS used the above illustration to diagram a sand blow. The Enigma paper says Bootheel sand blows are commonly 1. Portions of roads in the Bootheel could disappear entirely as the soft, sandy soil shakes and the heavy roads sink. Memphis’ Pyramid Memphis’ city and county government in built a story pyramid on its riverfront. In the city started considering earthquake construction standards.
The pyramid sits smack dab on a Mississippi River sandbar. Guess what could happen to 20, spectators in the event of a major quake. It is being remodeled into a huge sporting goods store.
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Health Departments Blytheville Marriage License Offices Marriage License Offices are responsible for processing marriage license applications, issuing marriage licenses, and recording marriage certificates. Marriage License Offices maintain records on marriage licenses they issue, in addition to filing marriage certificates. In many locations, Marriage License Offices provide online search tools and request forms to access marriage records. Mississippi County Marriage License West Walnut Street Blytheville AR Blytheville Clerk Offices Clerks file important documents and preserve vital records for a county or local government, and the Clerk’s Office makes these records available to the public.
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Grand Prairie[ edit ] Rice field near Stuttgart The underlying impermeable clay layer in the Stuttgart soil series that allowed the region to be a flat grassland plain initially appeared to stunt the region’s growth relative to the rest of the Delta. But in , William Fuller began cultivating rice, a crop that requires inundation, to the region with great success. Rice cultivation still features prominently in the region’s economy and culture today.
Riceland Foods , the world’s largest rice miller and marketer, is based in Stuttgart, Arkansas on the Grand Prairie. History of Arkansas Early history and frontier Arkansas[ edit ] In the earth’s history, after the Gulf of Mexico withdrew from what was Missouri, many floods occurred in the Mississippi River Delta, building up alluvial deposits.
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Volume 44, Issues 1—4 , October , Pages Research paper Use of liquefaction-induced features for paleoseismic analysis — An overview of how seismic liquefaction features can be distinguished from other features and how their regional distribution and properties of source sediment can be used to infer the location and strength of Holocene paleo-earthquakes Author links open overlay panel Stephen F.
Obermeier1 Show more https: These features include dikes, craters, vented sand, sills, and laterally spreading landslides. The relatively high seismic shaking level required for their formation makes them particularly valuable as records of strong paleo-earthquakes. This state-of-the-art summary for using liquefaction-induced features for paleoseismic interpretation and analysis takes into account both geological and geotechnical engineering perspectives.
The driving mechanism for formation of the features is primarily the increased pore-water pressure associated with liquefaction of sand-rich sediment.
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