Excerpt: Driven by parents’ beliefs that home- school learning environments can be superior to those of public or private schools, as well as a desire by parents to spend more time together as a family, Nevada homeschooling has undergone remarkable growth during the past decade.

The Mormon Church has for years been given credit by historians for the settlement of Carson Valley. Prior to 1854 the LDS Church actually had no connection with that valley except that it was part of the Utah Territory, which the Church controlled. When political dissension against the Mormons developed in Carson Valley, Brigham Young decided to organize the area into a county in 1854. The following year he sent Orson Hyde and other officials there to organize the county government. Within a year Hyde so influenced Young that he agreed to send 250 colonists to Carson Valley in order to bring that area under the control of the Mormon Church. During the next eighteen months the colony failed to live up to its several objectives. When the Utah War broke out the Mormon leaders decided to abandon the colonial effort and instructed the missionaries to return to Salt Lake City. This hardship Hyde and Young could have spared the Saints had they foreseen the difficulties of establishing the colony in the midst of non-Mormons, an experience the Church had previously undergone in the East.

Since this writer has been confused by what seems to her to be radically different attitudes toward marriage and divorce in her own home town (Las Vegas, Nevada) and in Utah communities where she has been residing for the past five years, the social adjustment of female divorcees in these two locations was studied. The purpose was to begin to build knowledge about postdivorce adjustment, and it is hoped that future students of the family will be inspired to further investigate postdivorce problems.

An increasing amount of evidence suggests that as temperatures increase, montane animals are moving upward in elevation (IPCC 2007, Parmesan and Yohe 2003). As suitable habitats rise in elevation and then disappear altogether, these animals could be pushed to extinction. The American pika, Ochotona princeps, is a montane mammal that lives in western North America, usually at elevations above 1500 m (Smith and Weston 1990). Recent evidence suggests that pika population numbers are dropping in response to rising temperatures (Beever et al. 2010). The pika is a small herbivorous lagomorph, a relative of hares and rabbits. Its habitat is tightly restricted to talus slopes (rockfields) and the surrounding vegetation (Grayson 2005). Pikas have a high tolerance for cold temperatures, and do not hibernate during the long montane winter. However, they have very little tolerance for even mildly warm temperatures, and have been found to die when confined above ground at 25.5˚ C (Smith 1974b). To better understand pika persistence, we resurveyed 17 historic pika sites in the Lassen Peak region of northern California in August and September, 2009. Six of the historic sites were abandoned, as well as an additional 11 of 17 new sites surveyed. At each site we collected habitat information, and analyzed the data for factors that were correlated with site occupancy. We also installed 38 iButton thermal dataloggers in abandoned and occupied pika use sites, to determine if temperature affects occupancy. The dataloggers remained in pika sites for 14 months and recorded temperature every 1.5 hours. Abandoned pika sites had higher average temperatures and more days below 0˚ C. They also had greater shrub cover, less forb and graminoid cover, and a greater percentage of litter substrate. These findings suggest that the current warming trend may be having a negative impact on pikas in the Lassen Peak Region. As temperatures rise, pikas may be declining due to unsuitable temperatures and altered vegetative communities. In addition to the Lassen surveys, I investigated pika behavior in different temperature regimes in the Sierra Nevada. If pikas are able to adapt to climate change, it is possible that populations of pikas in different temperature regimes may exhibit behavioral plasticity, or have evolved genetic differences, such that these populations have different daily activity schedules. To determine if there is a difference in pika behavior at different elevations I observed pikas in one low and one high elevation site within the Bishop Creek drainage system in the Sierra Nevada. I conducted behavioral observations of pikas in four time blocks throughout the day in August and September, 2010. I recorded specific behaviors, such as foraging and haying (vegetation collecting), and compared these activities between low and high elevation pikas at different times of day. In August, pikas in the low elevation site exhibited a different activity profile than those in the high elevation site. Low elevation pikas were significantly more crepuscular (most active at dawn and dusk) during this month. I also observed more foraging behavior in the high elevation than the low elevation site, in both August and September. Reduced activity at higher temperatures may have negative impacts on pikas as temperatures increase. Low elevation pikas may be stressed due to reduced time spent foraging and haypile (overwinter vegetation cache) gathering. However, if pikas were able to switch their activity schedules to a more nocturnal schedule, they could escape higher daytime temperatures. To detect the possibility of nocturnal behavior in low elevation pikas, I set up four infra-red remote cameras in the low elevation site. I had variable success in capturing pika behavior with the cameras, and detected no evidence of nocturnal behavior. More research on the possibility of nocturnal behavior in pikas would be worthwhile, in part to determine what chance, if any, pikas have of adapting to rising global temperatures.

The problem to which this study is directed is the need for a better understanding of the current status of the salaries of ministers and their significance in the life of the individual minister, the local churches they serve, and the conference of which they are a part. The study was limited to the California-Nevada Conference of the Methodist Church and its antecedent, the California Conference, during the period 1941 to 1952. The author is a minister in this conference.

The place of counseling in the pastor's task has been the subject of much research and study during the past few decades. The consensus of those concerned with defining the pastor's task seems to be that counseling is a vital need of parishioners in all churches and that responsibility for counseling usually lies with the pastor. In a sincere attempt to meet the needs of their people many pastors are genuinely trying to equip themselves to provide counseling services. The problem that naturally needs evaluation is: The Present Status of Pastoral Counseling. The objectives that ultimately evolve in this investigation are: To provide for ministers and other interested persons information regarding the present status of pastoral counseling of the ministers of the California Nevada Conference of the Methodist Church. To furnish possible basis for revision and improvement of such counseling services as are now offered in various churches.

The purpose of this paper is to present in brief form, far too brief for the wealth of material available, an account of the history of the town of Elko, Nevada. There has been no attempt to include in these pages all the interesting events which are traditional in the gossip of the town. Every effort has been made to include only such material as can be readily verified either by the memories of those still living who remember the events or, in cases where this has bailed or there has been an evident conflict of stories, by resort to the written records. It is fortunate, indeed, that there are so many still living who were present in the early days, especially since the written records are not so complete as might be desired. Because of the limitations of space, the history has been limited to the years 1868-1890.

This thesis focuses on the comprehensive study of controlling a customized Active Magnetic Bearing (AMB) installed on Bently Nevada’s RK4 rotor kit in Cal Poly’s Vibrations and Rotordynamics Lab. The AMB was uniquely designed and manufactured by a Cal Poly senior project team to fit Bently’s rotor kit and the results of this research are distinctive to the custom system. To achieve practical functionality of the AMB system, we designed a controller a Virtual Instrument (VI) using the National Instrument software, LabVIEW. From the experimental study, we calibrated the programming to find unknown parameters of the AMB system and validated the design using a well-established industrial rotordyanmics software, Bentley Nevada System 1. The development of the control programming consists of theoretical analysis (MATLAB/ Simulink) and simulation validation (MSC ADAMS View). Both linear and non-linear models were implemented in MATLAB and Simulink to effectively tune a Proportional-Integral-Derivative (PID) control developed for various AMB models. To validate the theoretical results, we compared them to results from a co-simulation using MSC Adams VIEW, a multi-body dynamics simulation, and Simulink. From experimental trial and error at a shaft rotational speed of 2800 rpm, a 16% decrease in shaft orbit was achieved. These results demonstrate the practicality of the control program and custom AMB rotor kit that can be used for further research.

No description available.

Indiana University-Purdue University Indianapolis (IUPUI) / The Antler and Sonoma orogenies occurred along the southwest-trending passive Pacific margin of North America during the Paleozoic concluding with the accretion of the McCloud Arc. A southeast-trending sinistral transform fault truncated the continental margin in the Permian, becoming a locus for initiation of an east-dipping subduction zone creating the Sierran magmatic arc. Constrained in age between two early Triassic tuff layers, the volcanic clasts in the breccia of Frog Lakes represent one of the earliest records of mafic magmatism in the eastern Sierra Nevada. Tholeiitic rock clasts found in the breccia of Frog Lakes in the Saddlebag Lake pendant in the east central Sierra Nevada range in composition from 48% to 63% SiO2. Boninites produced by early volcanism of subduction initiation by spontaneous nucleation at the Izu-Bonin-Mariana arc are more depleted in trace element concentrations than the clasts while andesites from the northern volcanic zone of the Andes produced on crust 50 km thick have similar levels of enrichment and provide a better geochemical modern analogue. Textural analysis of the breccia of Frog Lakes suggest a subaqueous environment of deposition from a mature magmatic arc built on continental crust > 50 km thick during the Triassic. The monzodiorites of Saddlebag and Odell Lakes are temporal intrusive equivalents of the breccia of Frog Lakes and zircon geochemistry indicates a magmatic arc petrogenesis.