Fire, logging, livestock grazing, and insect outbreaks are disturbances that have significantly influenced both the historic and present fire regimes. The composition and structure of vegetation communities within Great Smoky Mountains National Park (GSMNP) have likely changed in response to these disturbances. Two study sites (CRX, the near site, and CRT, the far site) were chosen along the Cooper Road Trail based on topographic separation, presence of mixed oak-pine communities, presence of fire-scarred yellow pine trees, and GSMNP land acquisition records. To quantify and evaluate fire regimes, individual fire histories were developed for each site from fire-scarred yellow pine trees, and two 1000 m2 (0.1 ha) study plots were established for vegetation surveys. Fire history analysis yielded mean fire intervals of 6.2 years at the near site, 3.4 years at the far site, and 3.2 years when combined. Spatial analysis showed significant differences in fire activity between study sites. Temporal analysis showed significant differences in mean fire intervals between the pre-settlement (1720–1818) and post-settlement periods (1819–1934). Superposed epoch analysis showed the over-riding influence of climate at these sites. At the near site, trees displayed greater species diversity, larger diameter, and older age. Eastern white pine, pitch pine, red maple, and black gum were the dominant species. At the far site, tree species diversity was lower and trees were generally younger. Mixed oak-pine communities are succeeding to a canopy dominated by shade-tolerant, fire-sensitive species such as eastern white pine and red maple. Without fire disturbance, yellow pine communities will cease to regenerate, as will oak species that prefer a fire-maintained habitat.

World-wide amphibian declines sparked concern and encouraged investigation into potential causes beginning in the 1980’s. Infectious disease has been identified as one of the major potential contributors to amphibian declines. For example, Ranavirus has caused amphibian die-offs throughout the United States. Investigators isolated Ranavirus from dead or moribund amphibians during large-scale die-offs of amphibians in the Cades Cove area of Great Smoky Mountains National Park in 1999-2001. In 2009, after nearly a decade without follow-up monitoring, I undertook an investigation to determine if the virus persisted in the area, and if so, to assess spatial, temporal, and taxonomic patterns in prevalence. Three amphibian breeding ponds, including Gourley Pond, the site of these earlier mortality events, were monitored for Ranavirus during the 2009 amphibian breeding season. A peak in prevalence occurred at Gourley Pond corresponding to a massive amphibian die-off. Prevalence varied among three different taxonomic groups during this mortality event with the highest prevalence, 84%, detected in larval Ambystomatids, 44.4% prevalence in adult Newts, and no virus detected in adult Plethodontids. I did not detect virus at either of the other two breeding ponds despite equivalent sampling effort, similar community composition, and close proximity to Gourley Pond. These results suggest that the severity and spatial extent of Ranavirus in Cades Cove remains unchanged since its initial detection a decade ago. Also, despite the observed massive die-offs there is no evidence of local amphibian extinction at Gourley Pond.

Three outstanding problems related to the tectonic evolution of the Western Blue Ridge in the eastern Great Smoky Mtns. (GSM) include: (1) the nature of the Greenbrier Fault, previously interpreted as a younger over older pre-Taconic thrust fault with ~24 km of displacement between the Snowbird and Great Smoky Groups; (2) the relationship of regional metamorphism, expressed by the growth of porphyroblastic index minerals, to folding and foliation development in pelitic metasediments; (3) the relation of deformation to regional Taconian metamorphism. These problems were addressed in previous studies that did not have detailed mapping and petrography as a context. By using 1:24000 bedrock mapping in the eastern GSM in the area of the Greenbrier Fault and where regional metamorphic isograds are telescoped as a context, it can be concluded that: (1) the Greenbrier Fault exhibits an unconstrainable amount of post-metamorphic slip along the contact of the Great Smoky and Snowbird Groups and is not a major tectonic feature within the western Blue Ridge; (2) there is no direct spatial/coeval relationship between porphyroblast growth and foliation formation/matrix deformation that is consistent throughout the study area; (3) further work and mapping outside of the study area (S and SE) is needed when considering the relation of deformation to regional Taconian metamorphism, because of the non-pelitic nature of the Great Smoky and Snowbird Groups.

Thesis (M.S.)--University of Tennessee, Knoxville, 2008. / Title from title page screen (viewed on Mar. 12, 2009). Thesis advisor: Carol Harden. Vita. Includes bibliographical references.

Thesis (M.S.)--University of Tennessee, Knoxville, 2007. / Title from title page screen (viewed on Sept. 24, 2008). Thesis advisor: Randall Gentry. Vita. Includes bibliographical references.

Thesis (M.S.)--University of Tennessee, Knoxville, 2009. / Title from title page screen (viewed on Nov. 3, 2009). Thesis advisor: Joseph Clark. Vita. Includes bibliographical references.

The hemlock-silverbell (Tsuga canadensis-Halesia tetraptera) forest type is known to exist in only two places, the Great Smoky Mountains National Park (GRSM) and the Joyce Kilmer National Memorial Forest. The hemlock component of this forest type is currently threatened by the hemlock woolly adelgid (Adelgis tsugae), an invasive aphid-like insect native to Japan. This current status has given rise to the need to investigate the ecological resources of this rare forest type before the hemlock component dies out. The objectives of this study were to determine the nature of the plant/environment and plant/plant associations within this forest type. Within this forest type hemlock was negatively related to protection, aspect, and slope steepness and silverbell was positively related to aspect and slope steepness. This study also identified some interspecific associations such as the negative relationship in the understory between hemlock and striped maple, and provided evidence that understory stems are exhibiting a growth response to hemlock decline in these stands. The information obtained from this study characterizing the plant/environment interactions and even the structural and species components of this forest type will serve as a baseline of data from which to measure change and will provide insight into the mechanisms of species distribution and perhaps into short term scenarios of forest response to hemlock decline and mortality.

Debris-slides are one of the most frequently occurring geological hazards in metasedimentary rocks of the Anakeesta ridge in Great Smoky Mountains National Park (GRSM), which often depends on the influence of multiple causing factors or geo-factors such as geological structures, slope, topographic elevation, land use, soil type etc. or a combination of these factors. The main objective of the study was to understand the control of geo-factors in initiating debris-slides using different knowledge and data-driven methods in GIS platform. The study was performed in three steps: (1) Evaluation of geometrical relationship between geological discontinuity and topographic orientation in initiation of debris-slides, (2) Preparation of knowledge-driven debris-slide susceptibility model, and (3) Preparation of data-driven debris-slide susceptibility models and compare their efficacy. Performance of the models were evaluated mostly using area under Receiver Operating Characteristic (ROC) curve, which revealed that the models were statistically significant.

No description available.

Great Smoky Mountains National Park (GRSM) provides quality education programs to local schools. In order to continue this success and expand programs to reach more middle and high school students, a mixed methods study was conducted to help better understand why local middle and high school teachers participate or not in park educational programs. Using the Theory of Planned Behavior, teacher surveys measured factors that influence teacher intentions to participate in park programs to best predict their likelihood of future involvement. In addition, school administrators were interviewed to understand their perceptions of teacher involvement. Results provided insight to how GRSM can better provide valuable services to local middle and high schools. The best predictors of teachers' intentions to participate in future programs were their perceptions of whether programs would enhance academic achievement, how easily and comfortably they could incorporate the programs into their pre-existing curricula, and whether the experience would be a fun experience in nature for both their students and themselves. Future communications with teachers should therefore emphasize that Park programs are fun, relevant learning experiences that address academic requirements for various subjects and are relatively easy to incorporate into pre-existing curricula. / Master of Science