The purpose of this study was to determine whether differences existed in academic achievement, attitude toward school, and self-concept of seventh and eighth grade junior high school students in comparison to seventh and eighth grade middle school students who changed from a junior high school or an elementary school to a middle school in Jonesboro, Arkansas. A further concern of the study was to determine middle school principles of the Jonesboro Middle Schools.The subjects who furnished data for the study were 808 randomly selected seventh and eighth grade students. The students participated as control seventh and eighth grade junior high school students during the first year of the study (197576), or as experimental middle school seventh and eighth grade students during the second year of the study (1976-77). Five groups were formed for each grade. Two groups of each grade participated as the control groups, and the remaining three groups of each grade served as experimental groups.The Gordon How I See Myself Scale and the McElhinney Middle School Questionnaire Pupil Attitude Toward School scale were administered to accommodate a separate-sample-pretest-posttest control group design. Data from the Metropolitan Achievement Test and the SRA Achievement Test were used to fit a nonequivalent control group design. The data pertaining to self-concept and attitude toward school were analyzed by a multivariate analyses of variance technique. Achievement data were analyzed by multivariate analysis of covariance. On-site interviews were conducted to determine the Jonesboro-actual-middle school principles.Six null hypotheses were tested at the .05 level of statistical significance. Hypotheses one and two were stated to compare mean achievement scores of seventh and eighth grade Junior high school students to seventh and eighth grade middle school students. No statistically significant difference was found between the seventh grade junior high and middle school students. A statistically significant difference was found between the eighth grade junior high school and middle school students. The difference favored the junior high school students.Hypotheses three and four were stated to compare self-concept mean scores of seventh and eighth grade junior high school students to seventh and eighth grade middle school students. No statistically significant difference was found between mean scores of either grade.Hypotheses five and six were stated to compare mean scores on attitude toward school between seventh and eighth grade junior high and middle school students. No statistically significant difference was found between mean scores of either grade.The results of the interviews indicated elimination of "inappropriate" social and physical activities, more emphasis on intramural activities, and development of extensive exploratory programs as strengths of the Jonesboro Middle Schools. The lack of provision for continuous progress, team teaching, independent study, planned gradualism and use of multi media material appeared to be weaknesses.Conclusions drawn from the findings were:1. Students who experience a rigid academic schedule of a junior high school may tend to score significantly higher on achievement tests than students who attend less rigid middle schools.2. Students who have experienced the junior high school may tend to form some negative feelings toward school if placed in a middle school, but not to a statistically significant degree.3. The attitude and self-concept of seventh and eighth grade students appeared to be unaffected by the reduction of "inappropriate" social and physical activities.4. Little change in instructional procedures of classroom teachers appeared to be apparent.5. The major change seemed to be the addition of exploratory programs in middle schools.6. During the in-service program too much emphasis may have been placed on exemplary middle school programs at the expense of providing emphasis on the best middle school for Jonesboro.

A largely quantitative view of the institution of slavery in Hempstead County, Arkansas, this work does not describe the everyday lives of slaveholders and slaves. Chapters examine the origins, expansion, economics, and demise of slavery in the county. Slavery was established as an important institution in Hempstead County at an early date. The institution grew and expanded quickly as slaveholders moved into the area and focused the economy on cotton production. Slavery as an economic institution was profitable to masters, but it may have detracted from the overall economic development of the county. Hempstead County slaveholders sought to protect their slave property by supporting the Confederacy and housing Arkansas's Confederate government through the last half of the war.

This empirical study focused on the level of application of strategic planning by senior colleges and universities in Arkansas. The study was designed to examine, analyze, and describe the extent of strategic planning practices by Arkansas higher education institutions, as reflected in the opinions and perceptions of the institutions' chief executive officers and based on the profile of characteristics validated by twenty experts in the strategic planning literature.

The primary purpose of this study is to survey the attitudes of Arkansas speech teachers toward the oral interpretation events in the Arkansas State Speech Festival. The secondary purpose is to trace the development of oral interpretation from its inception in the festival to the present time. The thesis contains four chapters: I--an explanation of the purposes and procedures followed in the study; II--a history of the interpretation events and present structure of the festival; III--a compilation of the results of a questionnaire mailed to seventy-one Arkansas teachers; IV--a summary of the attitudes reflected in the questionnaires and recommendations for change in the current structure of the Arkansas State Speech Festival.

The primary purposes of this study were to assess the understanding and attitudes of teachers, to determine the interaction effects of certain variables, and to determine if there is a correlation between understanding of economic concepts and attitude toward economic education. The problem of the study was an assessment of the attitudes toward and understanding of economic concepts held by secondary school teachers in Arkansas who taught economics or economics-related subjects.

The purpose of this study was to examine the relationships between religiosity, marital satisfaction, sexual behaviors, and sexual satisfaction of married persons who attended a church affiliated university. Data were collected from 56 married individuals who attended a conservative, church-affiliated university located in the south-central United States. The sample was mostly caucasian, heterosexual, upper-middle income, college educated, divided equally by gender, and ranged. in age from 27 to 83 (M=age 46). Participants had been married between 4 and 54 years (M=22 years), and most (90%) participants were in their first and only marriage. Religiosity was operationalized by Rohrbaugh and Jessor's (1975) religiosity scale. Marital satisfaction was operationalized using the Kansas Marital Satisfaction Scale (Hatch, James, & Schumm, 1986). Sexual satisfaction was operationalized from global sexual satisfaction questions (Darling & Davidson, 1987). / Ph. D.

This study examines the county courthouses of Arkansas with the purpose of discovering certain qualities which they possess as architecture. Stylistic influences are identified, as are influential architects, periods of building activity, and characteristics of age and condition. An historical overview provides information concerning nationwide trends in public architecture over the last century, allowing observations as to the effects which national and regional tastes had on Arkansas' county courthouse builders. It is concluded that Arkansas' county courthouses reflect, to some extent, the stylistic preferences and backwardness of southern and rural courthouses, respectively. The Georgian Revival is identified as the most popular style for courthouses still in use, although the most active building period is found to be the 1930s, when WPA design specifications dominated Arkansas courthouse architecture.

I have studied syntectonic veins from shales and coarse calcareous sands of the Ordovician Womble Shale, Benton uplift, Arkansas. All veins are composed of calcite with minor quartz and trace feldspar and dolomite or high-Mg calcite in the coarser veins. All host lithologies have a pressure-solution cleavage, more closely spaced in the fine-grained shale beds. The vein internal fabrics are coarsely to finely fibered, with a strong host-rock grain size control on fiber width. The finest fibers are in veins with shale host and the coarsest in the coarse-grained calcareous sandstone. Fiber aspect ratio is inversely proportional to host grain size; more equant vein grains are found in the veins hosted in the coarse host fraction. Within one outcrop, the δ13C and δ18O compositions of the host lithologies range from 1.5 to -3.0 per mil and 7.5 to -14.0 per mil (VPDB), respectively. By contrast, the δ18O composition of the veins is remarkably constant (-13.5 per mil) among veins of starkly different fabrics. This composition is identical to that of the coarse calcareous sandstone lithology in the outcrop. No cathodoluminescence or stable isotope zoning was observed in the veins. In addition, there were no gradients in Ca or Si in the vicinity of the veins, suggesting either that the host did not contribute these elements or that diffusion was not the rate-limiting step to vein formation. In any case, the wide variety of veins was probably formed from meter-scale migration of fluid derived from local calcite-rich layers in calcareous sandstone.

This study is a statistical analysis of the sandstone distribution within the Arkansas Jackfork Group which is a passive margin fan complex. Passive margin fan systems are typically associated with long fluvial transport, fed by deltas, wide shelf, efficient basin transport, that result in a bypassing system. Passive margin fans are generally fine-grained, mud rich, and well sorted. These fans can be separated into three units (upper, middle, and lower fan) based on their location within the fan and how the sediments are deposited. Five outcrops from the Arkansas Jackfork Group have been chosen for this study and each were divided into different facies dependent on sandstone percentages in certain bed sets. The amount of sandstone for each facies was calculated and a statistical approximation for each outcrop was determined. Sandstone distribution curves were made for each outcrop to show a graphic representation of how the sandstone is dispersed. After analyzing different upper, middle, and lower fan outcrops, it is clear there is an obvious change in the sandstone percentage and distribution. The upper fan deposit has an overall sandstone percentage of approximately 77.5% and is deposited in beds that are mainly amalgamated; 10-30m thick. Sandstone is deposited moderately even and is quite concentrated throughout the exposure. The middle fan outcrops contain approximately 72.6% sandstone and show similar patterns, except that the amalgamated sandstone beds are not as thick, 5-15m and contain more shale in between layers. As expected the lower fan outcrop is completely different in both sandstone percentage and distribution. The lower fan has approximately 65.4% sandstone. The distribution of sandstone is more concentrated in each of the individual units, or systems, but the overall complex has two systems separated by a massive marine shale bed, 33.5 m, that contains virtually no sand.

I have studied syntectonic veins from shales and coarse calcareous sands of the Ordovician Womble Shale, Benton uplift, Arkansas. All veins are composed of calcite with minor quartz and trace feldspar and dolomite or high-Mg calcite in the coarser veins. All host lithologies have a pressure-solution cleavage, more closely spaced in the fine-grained shale beds. The vein internal fabrics are coarsely to finely fibered, with a strong host-rock grain size control on fiber width. The finest fibers are in veins with shale host and the coarsest in the coarse-grained calcareous sandstone. Fiber aspect ratio is inversely proportional to host grain size; more equant vein grains are found in the veins hosted in the coarse host fraction. Within one outcrop, the δ13C and δ18O compositions of the host lithologies range from 1.5 to -3.0 per mil and 7.5 to -14.0 per mil (VPDB), respectively. By contrast, the δ18O composition of the veins is remarkably constant (-13.5 per mil) among veins of starkly different fabrics. This composition is identical to that of the coarse calcareous sandstone lithology in the outcrop. No cathodoluminescence or stable isotope zoning was observed in the veins. In addition, there were no gradients in Ca or Si in the vicinity of the veins, suggesting either that the host did not contribute these elements or that diffusion was not the rate-limiting step to vein formation. In any case, the wide variety of veins was probably formed from meter-scale migration of fluid derived from local calcite-rich layers in calcareous sandstone.