Riding the crest of the torrent of verbal altruism which flooded in the New Deal came a malnurtured little fellow, the consumer-the same timid, mistreated, gullible little fellow with the battered derby hat whom cartoonists have so aptly pictured on the stool peering meekly over the counter at the big bruiser, the producer, who stood behind it. Put now he was to be such rejuvenated personage. The hair shirt in which one writer has so smartly dresed him was to be miraculously transformed into finest armor of an impregnable protective allogy which was to be composed of nemerous ethical abstractions. Prominent among these was to be thorough education as to his enemies' methods of attack and manners of exploitation, which was to include insturction in the arts and practies of the skull-duggery of advertising, which is perhaps the most effective weapon of his adversary.

The goal of this study was to determine if watering and fertilizing would help maintain favorable vegetation conditions on forested recreation sites. Sunrise Campground on the Cache National Forest in northern Utah was the study site. Treatment applications of water and nitrogen- phosphorous fertilizer were made from 1964 through 1968. Covariance analysis of variables indicated that all treatments produced significantly greater amounts of ground cover vegetation than control plots. Ground cover response to treatments was greater under aspen than under coniferous overstory, and treatments under aspen produced differences in appearance of vegetation . There were no significant differences in diameter growth of overstory trees. The results showed that watering and fertilizing are effective management tools for maintaining ground cover.

During the eighteenth and nineteenth centuries, the xii Shoshones of Cache Valley evolved from scattered pedestrian hunter-gatherers to large, armed, mounted bands that hunted and gathered from the Great Basin to the Plains. Trade with European Americans helped initiate this evolution. However, Shoshones did not respond passively to the presence of European Americans. Shoshones actively sought change, and incorporated trade goods into their culture within a Shoshone context. They adapted to each wave of European Americans that they encountered. When Mormons dispossessed them of their land, Cache Valley Shoshones resisted by going on the offensive. Finally overwhelmed, the remnants of the Cache Valley Shoshones submitted--physically but not spiritually--to European-American oversight.

The Smithfield 7.5' quadrangle is located about 13.8 kilometers (8.6 miles) south of the Utah-Idaho State Line and occupies the central portion of the eastern side of Cache Valley, Utah. The mapped area contains more than 55 square miles. The Bear River Range on the eastern side of the quadrangle contains stratigraphic units ranging from Precambrian to Quaternary age. Cache Valley contains deposits of Tertiary and Quaternary age. Quaternary units in the Smithfield quadrangle are subdivided into thirty-two map units based on age and genesis. Five ages of Quaternary units are identified, and these units are assigned to one of fourteen genetic types. The East Cache fault zone is mapped along the western edge of the Bear River Range. Early Quaternary time was principally a period of pediment formation, followed by normal faulting, erosion, and alluvial-fan deposition. Cache Valley was later occupied by a pre-Bonneville cycle lake which is tentatively correlated with the Little Valley lake cycle. This lacustrine cycle was followed by more erosion and alluvial-fan deposition. The current Cache Valley landscape is dominated by the sediments and geomorphic features of Pleistocene Lake Bonneville. Alluvial-fan deposition has been the principal geologic process in post-Lake Bonneville time. Geologic hazards in the Smithfield quadrangle include flooding, landslides, debris flows, rock fall, problem soils, shallow ground water, earthquake ground shaking, surface fault rupture, and liquefaction. Some of the areas affected by these hazards and measures for mitigating the hazards are identified. Bonneville lake cycle fine-grained offshore deposits and the Tertiary Salt Lake Formation are the primary geologic units susceptible to landsliding.

National English Committees insist that composition content is of first importance; organization of ideas, second; and form third. The writer agrees with this point of view, but believes that a large proportion of class time in English, all through the grades, is spent in trying to establish knowledge and skill in the use of grammar, punctuation, capitalization, and mechanics generally.

Alzheimer’s disease is a progressive disease that impairs cognitive and functional abilities. Currently, there is no cure and it is estimated there will be 81 million cases of Alzheimer’s disease by 2040. Life for the individual with Alzheimer’s disease, and their family, changes drastically when the affected individual experiences significant impairments in cognitive or functional ability (severe dementia), is placed in a skilled nursing home facility (institutionalization), or passes away (death). Until a cure is discovered, it will be important to identify modifiable factors that influence progression to severe dementia, institutionalization, and death. Three hundred thirty-five participants who were living in the community were followed after the onset of Alzheimer’s disease and continued until they left the study or the study period ended. Participants completed neuropsychological assessments at each visit. Visits occurred as close to every 6 months as possible and the mean number of visits was 5.32 (SD = 3.46). Outcomes of interest were severe dementia, institutionalization, and death. Predictor variables were hypertension, stroke, congestive heart failure, number of prescription medications being taken, General Medical Health Rating (GMHR) score, and Charlson Comorbidity Index score. Cox Regression was utilized to identify associations with progression to the specified outcomes. GMHR score, congestive heart failure, and number of prescription medications were associated with progression to severe dementia. The number of prescription medications was also associated with nursing home placement. GMHR score, stroke, and number of prescription medications were associated with death. These findings are important because they contribute to a better understanding of how measures of medical health, certain medical conditions, and potentially their prevention or treatment may help those with Alzheimer’s disease sustain a higher quality of life.

The present investigation examined the current water demand characteristics and the future water demand of Cache Valley, Utah for the time period of 1990-2010. The demand attributable to agriculture and seven nonagricultural economics sectors was determined and forecasts were performed based on those demand values. Linear regression, extrapolation, and alternative futures forecasting methods were applied and the various results compared against each other. Three different scenarios were calculated for residential demand to represent different sources and composition of demand information. It was determined that consideration of water demand data excluding Logan City provided the best statistical description of water demand. A discussion of the probable changes in the three water demand components, agriculture, industrial and residential, addressed issue of conservation and change of use patterns which would impact on the need for future development of new water supplies to meet the forecast demand for Cache Valley, Utah.

Meat is important in the American diet. Money spent for meat ranks as the largest single item in the family food dollar. Various studies indicate that the proportion of the food dollar spent for meat ranges from 25 to 30 percent. Such foods as dairy products and fresh and frozen fruits and vegetables calculated as separate groups account for a smaller single percentage than meat. Dairy products, the one of next importance to meat, account for approximately 18 percent of the consumer's food dollar.

A series of five east-west and two north-south hydrostratigraphic cross sections were drawn from drillers' logs of water wells within the southern half of Cache Valley, Utah. These cross-sections demonstrate that ground water flow to streams is restricted by a continuous low- II permeability layer, nearly 100-feet thick. This layer was correlated to the lake-bottom deposits of the Bonneville (30,000 -13,000 years ago) and Little Valley (140,000 - 90,000 years ago) cycles of the ancient Lake Bonneville. The most productive aquifers in the valley, collectively termed the principal aquifer , are in the southeast corner , approximately between Smithfield and Hyrum, and between the eastern valley margin and the valley center. Sands and gravels of the principal aquifer were deposited as alluvial fans and deltas by streams draining the Bear River Range. Ground water chemistry in the principal aquifer system is of the calcium-magnesium bicarbonate type with total dissolved solids (TDS) averaging about 300 ± 100 mg/L. TDS and the relative proportions of sodium, potassium, and chloride increase down flowpath, from recharge areas in the east to discharge areas in the west. Oxygen-18 (18O) and deuterium (D) analyses were performed on precipitation samples at three locations on the east valley benches, four surface water samples from streams entering the valley, and fourteen ground water samples from either wells or springs. Precipitation and surface water values generally plotted along the Global Meteoric Water Line (GMWL), although the precipitation values plotted significantly lower on the GMWL than the surface water values. Of the ground water samples, twelve from the principal aquifer generally clustered near the surface water data points, suggesting that water from streams, rather than infiltrating precipitation, recharges the principal aquifer. Twelve ground water samples were analyzed for tritium. The tritium values of eight samples from wells or springs in the principal aquifer suggest recharge after 1952. Two samples with tritium values dating prior to 1952 are from wells in the principal aquifer, and two are from wells west of the principal aquifer. Four samples were analyzed for 14C. Two of these wells were completed in the principal aquifer and two west of it. Correcting for partial carbon dilution, the age difference between the different areas is on the order of tens of thousands of years.

The alfalfa weevil, Hypera postica (Gyllenhal), was first found in the United States in Salt Lake City, Utah, during 1904 (Titus, 1910b). It spread form this point of original introduction and partially infested Cache Valley by 1912 (Titus, 1913). The alfalfa weevil has become one of the more important insect problems currently affecting American agriculture. Recently, this problem has attracted national attention because of the development of resistance to insecticides by the alfalfa weevil, the outlawing of certain pesticides for use on forage crops and the rapid spread of the alfalfa weevil to new areas. With this increased attention, many discrepancies have appeared in different reports of the alfalfa weevil's biology. The results of studies in the eastern United States often do not agree with those of studies which were made in Utah and vicinity during the early part of this century. In order to investigate the discrepancies or differences, and to determine the behavior patterns of the alfalfa weevil in Cache Valley, this study was undertaken. It was conducted from June, 1965 to August, 1966. The main topics investigated were the adult alfalfa weevil's flight activities, reproduction, daily field activities, seasonal history including diapause, and respiration under controlled conditions.