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Morehead State University

1991

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Full-Text Articles in Higher Education and Teaching

Cooperation In Resource Management Planning: A Model Process For Promoting Partnerships Between Resource Managers And Private Service Providers, Curt Schatz, Leo H. Mcavoy, David W. Lime Jan 1991

Cooperation In Resource Management Planning: A Model Process For Promoting Partnerships Between Resource Managers And Private Service Providers, Curt Schatz, Leo H. Mcavoy, David W. Lime

Faculty Research at Morehead State University

This study presents a modified transactive planning process intended to improve communication and cooperation between public sector resource managers and private sector businesses that serve visitors to an outdoor recreation resource. The elements of the transactive planning process are illustrated and applied in a case study approach with the U.S. Forest Service and commercial outfitters adjacent to a forest recreation area. Outcomes of the planning process indicate that public managers and private businesses share many of the same management goals and concerns. They also agree they can and should address these concerns cooperatively. Results of the study indicate that this …


The Silurian Of Central Kentucky, U.S.A.: Stratigraphy, Palaeoenvironments And Palaeoecology, Charles E. Mason, F. R. Ettensohn, C. E. Andrews Jan 1991

The Silurian Of Central Kentucky, U.S.A.: Stratigraphy, Palaeoenvironments And Palaeoecology, Charles E. Mason, F. R. Ettensohn, C. E. Andrews

Faculty Research at Morehead State University

Silurian rocks in Kentucky are exposed on the eastern and western flanks of the Cincinnati Arch, a large-wavelength cratonic structure separating the Appalachian foreland basin from the intracratonic Illinois Basin. The Cincinnati Arch area experienced uplift during latest Ordovician-early Silurian time, so that the exposed Silurian section is relatively thin due to onlap and post-Silurian erosional truncation on the arch. On both flanks of the arch, dolomitic carbonates predominate, but the section on the eastern side reflects a more shale-rich ramp that faced eastern Appalachian source areas. In the Silurian section on the western side of the arch, which apparently …