Spelling suggestions: "subject:"monongahela"" "subject:"monnahela""
1 |
Understanding the Occupational History of the Monongahela Johnston Village Site through Total Artifact DesignMitchell, Seth Thomas 03 August 2011 (has links)
The period after A.D. 1100 in western Pennsylvania was a dynamic period in history occupied by diverse populations with rapidly changing social interactions. The Johnston site located in Indiana County represents one of the most important village sites during this period. Through a combination of ceramic analyses and radiocarbon dating previous hypotheses posited about this site are investigated. Archaeologists have relied on final twist direction of cordage impressions on shell-tempered and cord-marked ceramics to argue for population amalgamation between social groups from northwestern and southwestern Pennsylvania. In addition, ceramics recovered from the site have been used to define the date range for occupation at the site and for the Johnston phase of the late Middle Monongahela period. By combining radiocarbon dating and ceramic analyses these previous hypotheses are investigated. Specifically the usefulness of using cordage twist as a sole attribute to define social groups at the intrasite level is challenged. / Dr. Sarah Neusius
Dr. Beverly Chiarulli
Dr. Phillip Neusius
|
2 |
Forest songbird abundance and viability at multiple scales on the Monongahela National Forest, West VirginiaDeMeo, Thomas E. January 1999 (has links)
Thesis (Ph. D.)--West Virginia University, 1999. / Title from document title page. Document formatted into pages; contains xi, 149 p. : ill. (some col.), map. Vita. Includes abstract. Includes bibliographical references.
|
3 |
Petrographic and Geochronologic Provenance Analysis of Upper Pennsylvanian Fluvial Sandstones of the Conemaugh and Monongahela Groups, Athens County, OhioDodson, Scott A. 25 September 2008 (has links)
No description available.
|
4 |
Identifying structural differences in mixed mesophytic and northern hardwood forests on the Monongahela National Forest using remote sensing dataBender, John Richard, January 1999 (has links)
Thesis (M.A.)--West Virginia University, 1999. / Title from document title page. Document formatted into pages; contains viii, 55 p. : ill. (some col.), maps. Includes abstract. Includes bibliographical references (p. 44-48).
|
5 |
An assessment of Monongahela National Forest management indicator speciesMoseley, Kurtis R. January 1900 (has links)
Thesis (Ph. D.)--West Virginia University, 2008. / Title from document title page. Document formatted into pages; contains xiv, 258 p. : ill., maps. Includes abstract. Includes bibliographical references.
|
6 |
Stream fish metacommunity and metapopulation ecology in a mined Appalachian watershedMartin, Roy Worth. January 1900 (has links)
Thesis (Ph. D.)--West Virginia University, 2010. / Title from document title page. Document formatted into pages; contains xii, 492 p. : ill. (some col.), maps. Includes abstract. Includes bibliographical references.
|
7 |
The Prehistoric Diet and Nutritional Status of the Wylie Site InhabitantsValko, Amanda Lee January 2001 (has links)
No description available.
|
8 |
Fluvial Architecture of the Interval Spanning the Pittsburgh and Fishpot Limestones (Late Pennsylvanian), Southeastern OhioKing, M. Ryan 25 April 2008 (has links)
No description available.
|
9 |
Acid deposition effects on soil chemistry and forest growth on the Monongahela National ForestElias, Patricia Elena 29 August 2008 (has links)
Acid deposition (AD) results largely from the combustion of fossil fuels, and has been found to negatively impact forest ecosystems. AD may acidify soils through base cation leaching or Al mobilization, may cause accumulation of nitrates and sulfates in soils, and in some cases has been related to forest decline. The Monongahela National Forest (MNF) lies downwind from many sources of AD pollution, and average deposition pH is around 4.4. Therefore, managers are concerned about the possible deleterious effects of AD on the forest ecosystem. During the 2006 Forest Plan revision, evaluation of site sensitivity to acidification was specifically stated as a step in the Forest's adaptive management process. To meet this management objective, forest practitioners must understand the effects AD has on the forest, prescribe appropriate practices, and be able to monitor for future changes.
To address the needs of MNF managers we used Forest Inventory and Analysis (FIA) sites to evaluate forest growth patterns on the Forest and determined the relationship between growth and key indicators of soil acidity. Furthermore, we used those relationships to create a map of site resistance to acidification across the MNF. To further develop a monitoring scheme we assessed two soil sampling protocols and two soil analysis methods for their suitability for monitoring AD-related changes in soil chemistry. Additionally, we evaluated the utility of dendrochronological and foliar sampling as AD-specific monitoring methods.
Across all FIA sites on the MNF periodic mean annual volume increment (PMAVI) ranged from -9.5 m³ha⁻¹yr¹ to 11.8 m³ha⁻¹yr¹, suggesting lower-than-expected growth on two-thirds of the sites. Growth was compared to soil indicators of acidity on 30 FIA sites. In the surface horizon, effective base saturation (+), Ca concentration (+), base saturation (+), K concentration (+), Fe concentration (-), Ca/Al molar ratio (+), and Mg/Al molar ratio (+), were correlated with PMAVI (p ≤ 0.1). In the subsurface horizon pH<sub>(w)</sub> (+), effective base saturation (+), Al concentration (-), and K concentration (-) were correlated with PMAVI. Site resistance to acidification was mapped based on site parent material, aspect, elevation, soil depth, and soil texture. There was a significant (p ≤ 0.1) positive correlation between PMAVI and a resistance index developed using five soil and site factors. Resistance was also compared with key soil indicators of AD-induced decline on 28 sites across the forest, and pH, effective base saturation, and Al content were found to be the best indicators related to resistance index. Resistance index was used to create a map of the MNF, of which 14% was highly resistant (RI ≥ 0.7), 57% was moderately resistant (0.7 > RI > 0.45) and 29% was slightly resistant (RI ≤ 0.45).
The first of our monitoring program evaluations compared soil sampling and analysis methods on 30 FIA plots. Analyses of variance showed that soil pH, effective base saturation, Ca/Al molar ratio, and sum of bases varied significantly with sampling protocol. We also compared lab analyses methods and found that if sampling by horizon, a linear relationship can be used to estimate Ca/Al<sub>SrCl₂</sub> ratio using NH₄Cl extractions. The second monitoring approach evaluated the utility of a northern red oak (Quercus rubra L.) dendrochronology on two FIA plots. This analysis suggests that pollution on the MNF caused a decrease in growth rate during the 50-year period from 1940 to 1990. There were no differences among ring width increment and basal area increment between the two sites. From 1900 to 2007 the two sites showed 58.5% similarity in growth trends, but these could not be attributed to a dissimilar influence of AD. The third monitoring approach evaluated the relationship between foliar and soil chemical indicators. Across FIA plots, nutrient concentrations varied by tree species. The first year results from a potted-seedling study suggest that soil acidity influences growth, and foliar concentrations are related to growth rates.
This evaluation of the effects of AD on the MNF can be used to develop adaptive management plans and a monitoring program that will meet the AD-related objectives of the 2006 Forest Management plan. / Master of Science
|
10 |
Pittsburgh's Identity: Investigating the Relationship between Geography, Geology and the City's Social DevelopmentKirsch, Alexandra N. 07 May 2020 (has links)
No description available.
|
Page generated in 0.0301 seconds