Thesis (M.S.)--Oregon State University, 1988. / Typescript (photocopy). Includes bibliographical references (leaves 93-99). Also available on the World Wide Web.

A first-order approximation is made of the frequency and magnitude of bedload transport downstream of the Pelton-Round Butte Dam Complex, lower Deschutes River, Oregon with implications for salmonid spawning habitat. Field measurements of channel hydraulics, geometry, and particle size were combined with one-dimensional hydraulic and bedload transport models to determine the streamflow needed to move the channel bed material and to predict how much material would move once bedload transport was initiated. Inflows and outflows from the Dam Complex, and the predicted bedload carried by each, were compared to evaluate the effect of the Dam Complex on downstream discharge and bedload transport. Predicted critical discharges were equaled or exceeded very infrequently during the 72-year streamflow record. In addition, discharges capable of transporting bed material exceeded threshold conditions by very little. This has resulted in low predicted rates and amounts of bedload transport over the period of record. The Pelton-Round Butte Dam Complex was found to slightly increase the magnitude of flood peaks and associated predicted bedload transport for post-dam transport events exceeding threshold transport conditions. An exception to this pattern was the effect of the Dam Complex on the flood of December 1964, the second largest flood on record. This large flood occurred under unique circumstances -- while the reservoir of Round Butte Dam was filling for the first time. Since none of the transport events that occurred after the reservoir finished filling were affected by the Dam Complex in the same way as the 1964 event, the influence of the Complex on the 1964 flood is considered unique. The two largest floods on record (1964 and 1996), despite their relatively large sizes with respect to all other recorded flood events, did not cause major morphological changes to the lower Deschutes River. This observation, along with other independently derived information, supports the conclusion that the lower Deschutes is a very stable river. / Graduation date: 1998

Thesis--University of Chicago. / Bibliography: p. 135-139.

McKinney Butte, a late Tertiary andesite vent and flow complex, is located near the town of Sisters, Oregon, in the upper Deschutes Basin, and is situated along the structural trend that forms the eastern margin of the High Cascades graben (Sisters fault zone and Green Ridge). Rapid development and over appropriated surface water resources in this area have led to an increased dependence upon groundwater resources. A primary concern of resource managers is the potential impact of expanding groundwater use on stream flows and spring discharge. Two sets of springs (McKinney Butte Springs and Camp Polk Springs) discharge to Whychus Creek along the east flank of McKinney Butte, and during low-flow conditions supply a substantial component of the total flow in the creek. Despite their contribution to Whychus Creek, the springs along McKinney Butte are small-scale features and have received less attention than larger volume (> 2 m³/s) springs that occur in the basin (i.e., Metolius Spring and Lower Opal Springs). This study used discharge measurements in Whychus Creek upstream and downstream of the springs, and mixing models using measurements of electrical conductivity and temperature in the springs and Whychus Creek to determine the contribution of the springs to the creek. Isotopic, thermal, and geochemical signatures for the McKinney Butte and Camp Polk Springs, and local streams (Whychus Creek and Indian Ford Creek) and springs (Metolius Spring, Paulina Spring, Alder Springs, and Lower Opal Spring) were assessed to determine the source(s) of the McKinney Butte and Camp Polk Springs. The discharge and hydrochemical data along with hydraulic head data from local wells were used in the development of a conceptual model of groundwater flow for the McKinney Butte area. Discharge from the McKinney Butte Springs supplies the majority of water to Whychus Creek on the east flank of McKinney Butte (~0.20 m³/s), provides up to 46% of the flow in the creek, and is relatively stable throughout the year. Discharge from the Camp Polk Springs is less than 0.05 m³/s. Isotopic, thermal, and geochemical signatures indicate distinct sources for the McKinney Butte and Camp Polk Springs. Groundwater discharged at the McKinney Butte Springs is depleted in heavy stable isotopes (δD and δ¹⁸O) relative to the Camp Polk Springs. Recharge elevations inferred from stable isotope concentrations are 1800-1900 m for the McKinney Butte Springs and 950-1300 m for the Camp Polk Springs. Elevated water temperature in the McKinney Butte Springs relative to the average air temperature at the inferred recharge elevation indicates the presence of geothermal heat and implies deep circulation in the flow system. The temperature in the Camp Polk Springs is not elevated. The Camp Polk Springs, though not the McKinney Butte Springs, contain elevated concentrations of ions Cl, SO₄, and NO₃ that are indicative of contamination. The study results indicate the source of the Camp Polk Springs is shallow groundwater whereas the McKinney Butte Springs discharge water that has circulated deep in the groundwater flow system. Additionally, the hydrochemical traits of the McKinney Butte Springs are similar to Metolius Spring, suggesting discharge from the McKinney Butte Springs is controlled by the structural trend that forms the eastern margin of the High Cascades graben. The significant difference in discharge between the McKinney Butte Springs and Metolius spring may be related to the size of faults that occur locally.

Thesis (M.S.)--Oregon State University, 1991. / Typescript (photocopy). Includes bibliographical references (leaves 143-152). Also available on the World Wide Web.

The prehistory of Central Oregon is explored through the examination of six archaeological sites and two isolated finds from the Upper Deschutes River Basin. Inquiry focuses on the land use, mobility, technological organization, and raw material procurement of the aboriginal inhabitants of the area. Archaeological data presented here are augmented with ethnographic accounts to inform interpretations. Eight stone tool assemblages and three debitage assemblages are analyzed in order to characterize technological organization. Diagnostic projectile points recovered from the study sites indicate the area was seasonally utilized prior to the eruption of ancient Mt. Mazama (>6,845 BP), and continuing until the Historic period (c. 1850). While there is evidence of human occupation at the study sites dating to between >7,000-150 B.P., the range of activities and intensity of occupation varied. Source characterization analysis indicates that eight different Central Oregon obsidian sources are represented at the sites. Results of the lithic analysis are presented in light of past environmental and social phenomena including volcanic eruptions, climate change, and human population movements. Chapter One introduces the key questions that directed the inquiry and defines the theoretical perspective used. Chapter Two describes the modem and ancient environmental context of study area. Topics of discussion include physiography, fauna, vegetation, geology, and climate. Chapter Three introduces the aboriginal inhabitants of the Upper Deschutes River Basin and summarizes past archeological investigations in the area. Hunter-gatherer land use and lithic technology are discussed in Chapter Four. The methods used to collect and analyze the data used in this study are presented in Chapter Five. Chapter Six summarizes the results of the technological lithic analysis and geochemical sourcing. The final chapter, Discussion and Conclusions, interprets the results with respect to cultural chronology, site function and distribution, land use and mobility, lithic technology, and raw material procurement. / Graduation date: 2003

The Quartz Mountain Obsidian Quarry is located in the Southeast corner of the Bend Fort Rock Ranger District in central Oregon, approximately forty-five miles southeast of Bend, Oregon. The research of the Quartz Mountain Obsidian Quarry began with a literature search of other quarry sites in the area and the use of aerial photos to determine the survey area. After the survey area was established a ground survey was conducted. Following the survey several key areas were chosen for surface collections that could answer key questions: What types of core reductions were being used on Quartz Mountain?; and What types of materials were being utilized? (red/black obsidian found in rhyolite veins, red/black obsidian found in fist sized and larger nodule form, or large block black obsidian). In order to answer these questions three collection units were established. The lithic material from the units was collected and analyzed and the information placed into a database, which was then grouped for statistical analysis, and generated into charts and tables. The resulting data was then compared to the information found from an extensive literature search to see how the material that I collected compared to those found at other quarry sites. From this information I was able to determine that two different core reduction methods were being used on Quartz Mountain: blade core and bifacial core. Along with the different core reduction methods a mobility strategy also came into play. In this thesis I will use the data gathered to determine the different core reduction methods and the mobility strategies that are associated with them. / Graduation date: 1998

Private land conservation provides an opportunity to address problems of habitat fragmentation and biodiversity loss caused by an increase in the development and parcelization of private land. Conservation easements (CEs) are an innovative tool used by land trusts to protect significant natural qualities of private land in perpetuity, while also allowing the land to remain in private ownership. Traditionally, property represents an individualistic relationship, however, CEs redefine this relationship by seeking to maximize the overlap in private and public goods in property. In this study, I explore the relationship between the common good and private property through an analysis of landowner attitudes and interest in conveying CEs. To address my research objectives I implemented a mixed-mode survey to 664 private landowners in the Whychus Creek Watershed in Deschutes County, OR. I received 257 survey responses, yielding a response rate of 41%. The first layer of this study focuses on landowner attitudes towards CEs (Chapter 2). The results of an exploratory factor analysis suggest there are two dimensions to landowner attitudes towards CEs--internal and external dimension. I constructed logistic regression models to predict positive internal and external attitudes and found that external attitudes are primarily influenced by environmental beliefs, whereas internal attitudes are influenced by a suite of factors including financial beliefs and perceived risk to private ownership. Furthermore, landowner knowledge and awareness of CEs may play a role in attitude development. I found that as awareness increased the number of landowners perceiving low risk also increased. Additionally, I found that those who learned about CEs from a peer were more likely to have an extreme positive or negative attitude towards CEs. The second part of this study focuses on landowner interest in conveying a CE (Chapter 3). The results of a multinomial logistic regression analysis suggest that positive external and internal attitudes towards CEs provide the foundation for CE, while personal incentives and connections to the social and/or natural community serve as the motivation driving CE conveyance. Although the results of this study are only representative of landowners in the Whychus Creek Watershed I argue that some of the findings may be more broadly applicable. Contributing to our conceptual understanding of CEs, I discuss how CEs may be beneficial in reintegrating the common good into private property. Further, I highlight that landowner connections to both the social community and natural environment are important characteristics of CE conveyance as well as private land conservation in general.

Thesis (M.S.)--Oregon State University, 1998. / Typescript (photocopy). Includes bibliographical references (leaves 103-107). Also available online.

Thesis (M.S.)--Oregon State University, 1998. / Typescript (photocopy). Includes bibliographical references (leaves 82-85). Also available via the World Wide Web.