This dissertation explores the University of Kentucky’s efforts to develop and implement an “action program” in eastern Kentucky in the 1960s. By the late 1950s, Kentucky’s political, business, and academic leaders had identified eastern Kentucky as the state’s problem area, and they sought strategies to bring the region into the economic and cultural mainstream. This generation of post-war leaders had an uncompromising faith in the power of knowledge, technology, and planning, and University leaders saw their action program as a university-wide effort to address what most would argue was Kentucky’s ugliest problem. This study begins with an examination of the rushed and disorganized Kellogg Foundation-funded Eastern Kentucky Resource Development Project (EKRDP) in 1960. With the national “rediscovery” of Appalachia in the early 1960s and the passage of the Equal Opportunity Act (EOA) and the Appalachian Regional Development Act (ARDA) in 1964 and 1965, University leaders reframed their thinking about how to engage eastern Kentucky in the midst of a War on Poverty. Institutional support for the EKRDP dwindled, and administrators tried to shift the responsibility of the eastern Kentucky program to the newly developed Center for Developmental Change (CDC). However, the leadership of the CDC lacked stability, the faculty who had been the driving force behind the Center did not want to be tied down to Appalachian projects, and the changing expectations for faculty ushered in by the “Oswald Revolution” did not reward interdisciplinary work.

The Berea Sandstone is a Late Devonian, tight oil and gas reservoir that intertongues with the Bedford Shale in eastern Kentucky. In order to evaluate the Bedford-Berea interval in the subsurface, 555 well logs from the Kentucky Geological Survey’s oil and gas database were used to construct structure maps, isopach maps, and cross sections of the interval and its possible hydrocarbon source rocks. Gamma-ray logs were compared to known cores in order to separate Bedford from Berea lithologies. Maps and cross sections were compared to known basement structures to evaluate possible structural influences on the interval. The Bedford-Berea interval is thickest along a north-south elongate trend which extends from Lewis to Pike Counties and cuts across basement structures. Along this trend, the interval is thickest and the percentage of Berea lithologies is greatest on known basement highs. The interval is thinnest and dominated by Bedford shales above structural lows and west of the main trend. Several wells are also reported in which the Bedford-Berea thickens on the down-thrown side of major faults. Also, in northeastern Kentucky, where the Berea is thickest, possible submarine channel facies are identified which cut into the underlying Cleveland Shale near the Waverly Arch.

Groundwater in the Kentucky Appalachian region is constrained by physiography and lithology. Lithostratigraphy, groundwater flow, and chemistry were delineated in the alluvial aquifer along the Cumberland River at H.L. Disney Training Center. To assess groundwater-river interactions and water quality, 11 monitoring wells were installed and sampled quarterly, plus the river and an existing bedrock well. Analytical results were evaluated for temporal and spatial trends. Collected soil cores were analyzed for bulk chemistry and grain size. Solute speciation and saturation indices were calculated and hydraulic conductivity estimated from grain-size analyses. Pumping and slug tests were performed to estimate hydraulic conductivity and hydraulic head was monitored using logging transducers for river stage comparison. Site lithology consists of loamy soils underlain by silty clay, transitioning downward to clayey-fine sands on friable sandstone/shale. Alluvium becomes finer-grained and has lower hydraulic conductivities with proximity to the river (10-9–10-2 cm/s). Meteoric recharge drives local groundwater flow from ridges toward rivers. Hydraulic head fluctuates with stage and temporary gradient reversals occur. Groundwater does not appear to be impacted by current land use. Wells have elevated iron and manganese concentrations; post-treatment, the alluvial aquifer may provide sufficient quality and rates of water to support onsite military activities.

Thesis advisor: Marc K. Landy / Education - and rural education - was on LBJ’s mind when he declared “War on Poverty” from the front porch of a family cabin in Inez, Kentucky. In 2021, Lyndon Johnson would find his Great Society did not fully come to fruition. In this work, I explore how responsive federal, state, and local bodies of government are to the needs of underresourced schools in Eastern Kentucky’s rural, economically distressed coal counties. National Assessment of Educational Progress (NEAP) scores demonstrate that Eastern Kentucky’s students are behind from the starting-line, thanks to economic, health, and developmental disparities. However, some school districts feature rates of improvement between fourth and eighth grade that exceed the national average, while others stay behind. This project’s central finding is that local investment is the variable most correlated with school improvement. Today, Appalachia remains a place where “working people, and those who wish there was work...battle for dignity and security, for themselves and for their children.” That battle for dignity and security, for better schools and better quality of life, has gone on for decades and continues today. / Thesis (BA) — Boston College, 2020. / Submitted to: Boston College. College of Arts and Sciences. / Discipline: Departmental Honors. / Discipline: Scholar of the College. / Discipline: Political Science.

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