The junior college athletic program at College of Southern Utah commenced in 1923. The facilities were barely satisfactory, and the construction of better facilities began in 1926. A new gymnasium was constructed and was rated as one of the better facilities in the state. The football stadium was relocated in 1928 and constructed almost entirely by donated labor , materials and equipment from community residents. A new and larger gymnasium was constructed in 1949. Football was inaugrated in 1928 on a full-time basis and has maintained this status, except during World War II The College of Southern Utah won the league championship only once and never did go through a season undefeated. Basketball was always the big s port, having its beginning in 1923. The basketball teams won the league title for many years and went on to higher honors by winning the intermountain championship and participating in the Western States Tournaments. On one occasion, a basketball team entered the National Junior College Tournament and placed sixth. Wrestling was tried on several occasions, but it failed to take hold and was not permanent until 1959. This team won the league championship. Baseball was sporadic because of the unpredictable spring weather, and did not become a strong program until 1950. The team of 1963 finished in third place in the National Junior College Tournament. Track and field had little success until 1946. The teams from 1946 to 1951 did not lose a dual meet and won the conference championship each year, a league record. Tennis was a hit and miss sport and never did obtain a full schedule. Eleven men have served as head coach at College of Southern Utah with the first six serving alone and handling all the coaching duties. The coaching duties were split and two coaches were hired in 1946, one for football and one for basketball. This policy has remained constant since then.

The mapped area, in north-central Utah, is centered about 22.6 miles south of Logan, Utah. It measures about 3.8 miles in the north-south direction and 6.6 miles in the east-west direction. Stratigraphic units of Precambrian and Cambrian age underline most of the area. The Precambrian units are as follows: (1) Maple Canyon Formation, (2) Kelley Canyon Formation, (3) Orthoquartzite unit, (4) Argillite unit, (5) Mutual Formation, and (6) Volcanic unit. The Brigham Formation, which overlies the Precambrian volcanic unit, is probably of Cambrian age; however, the lower part may be Precambrian. The overlying Cambrian carbonate unit is not differentiated. The Salt Lake Formation of Tertiary age overlaps older rocks in the valley north of James Peak. The western part of James Peak, east of a major normal fault, consists of east-dipping Precambrian units. The oldest unit, which crops out on the eastern side of Broadmouth Canyon, is the Maple Canyon Formation. The rocks of the eastern part of James Peak also dip generally eastward. A continuous stratigraphic section extends from the Kelley Canyon Formation, exposed in Wolf Creek Canyon, northeastward to the Brigham Formation. The Cambrian carbonate unit seems to overlie the Brigham in normal stratigraphic succession. A thrust fault, which has about 1,000 feet of displacement, is present on the eastern side of James Peak. Another thrust fault, on the southeastern side of James Peak, places the Cambrian carbonate unit on Precambrian units. A block of the Brigham Formation, near the southeastern corner of the area, is thrust over the carbonate unit and the Brigham. The thrust faulting is part of the Laramide Orogeny that occurred late in the Mesozoic Era and early in the Teritary Period. Movement was generally eastward. Normal faulting began early in the Tertiary Period and continues at the present time.

No description available.

No description available.

Inclusive education is a recent phenomenon in the education system in Papua New Guinea. It is about giving equal educational opportunities to all children, whether with disabilities or not in the regular school or classroom. Schools are considered as social institutions that should endeavour to enhance all children's lives through appropriate teaching and learning practices. However, the school culture, which is generally defined as 'how things are done here' is vital for the promotion of inclusive practices. The main aim of this study was to identify the school cultural features and practices that influenced or did not influence inclusive education, and the impact on inclusion. Teachers and school administrators appeared to play a vital role in enhancing inclusive practices through their practices. The study was based on an interpretive/naturalistic research paradigm, the qualitative research approach and the case study methodology. Four schools were studied and categorised as rural and urban settings. The main purpose of categorisation was to identify some similarities and differences in terms of how inclusion was promoted in these schools. Teachers and school administrators were chosen as the main participants. The primary source of data collection was semi-structured interviews. Interview questions were developed for both teachers and school administrators respectively. A non-participant observation method was used as a support instrument to collect more data from selected research participants based on the preliminary interview data. The results suggested the existence of four broad school cultural features and practices. These included staff understanding of special and inclusive education concepts, leadership and organisation, school cultural features/practices and implications for staff, and policies. Teachers and school administrators appeared to have limited knowledge and understanding about what constitutes special and inclusive education practices. However, the school leadership, collaboration and inspection practices minimally influenced inclusive practices. At the same time other school cultural features such as the outcomes-based education curriculum and ecological assessment seemed to have the potential to influence the outcomes of the process of inclusion. The results suggest the value of Callan Services as a school support service agency to influence inclusive education in the Southern Highlands Province. It was noted that children with disabilities were already part of the education system. Though the teachers and school administrators claimed this to be inclusive education, according to the literature this was a manifestation of functional mainstreaming practices. The teachers and school administrators and the Department of Education at the provincial and national levels appeared to take less responsibility in disseminating information pertaining to inclusive practices. The teachers and school administrators received limited support and information from the national and provincial Departments of Education. Therefore, the special education policies developed at the national level had not trickled down to the school level. This situation created a gap between inclusive education policy and practice. One of the major channels of communication and connection was through the inspectors and their inspection practices, but this appeared to have been under-utilised.

A multi-decadal survey program undertaken at the Collaroy-Narrabeen embayment in SE Australia identifies medium-term (~2-7 year) cycles of both erosion and accretion across the entire embayment ('beach oscillation') and at its two extremities ('beach rotation'). These cycles have been observed to respond to phase shifts in the El Ni??o/Southern Oscillation (ENSO). To investigate wave and climate controls of embayment variability in finer detail, this study combines historical surveys with 45 years of wave data from the ERA-40 reanalysis and four years of high-resolution beach measurements using RTK-GPS and image-derived survey techniques. ENSO and Southern Annular Mode (SAM) controls of wave variability in the Sydney region are first explored. In general, wave heights increase/decrease and wave directions become more easterly/southerly during La Ni??a/El Ni??o phases. A positive correlation is observed between the SAM and summer wave heights, and a negative correlation between the SAM and winter wave directions. Storm variability is observed to be modified by the ENSO, but not the SAM. In particular, La Ni??a phases are generally associated with longer duration, higher energy events from a more easterly direction when compared to those during El Ni??o phases. Wave controls of embayment variability are subsequently investigated. In the short-term (days - months), beach oscillation/rotation is observed to be the most dominant process, accounting for approx. 60%/20% of overall embayment variability. Beach oscillation is related to changes in wave height and storms, whereas beach rotation is related to changes in wave direction and/or wave period. An empirical model that estimates the beach response to individual storm events is developed. In the longer-term (months - years), beach rotation is observed to respond to both wave heights and directions. Larger waves are sheltered somewhat at the southern end, creating an apparent clockwise rotation under energetic wave conditions. Clockwise/anticlockwise rotations are also observed to follow southerly/easterly wave shifts at lags of up to 12 months. Comparisons between the ENSO and beach oscillation/rotation agree with previous observations that El Ni??o/La Ni??a phases are associated with an overall accretion/erosion and clockwise/anticlockwise rotation of the embayment. In general, the SAM shows little influence on embayment variability. While it is clear that beach oscillation is driven by cross-shore processes, to what extent beach rotation is a longshore and/or cross-shore phenomena requires further investigation.

An investigation of the geological resources of the Southern Highlands was undertaken and over two hundred samples were collected and examined for possible use as stoneware ceramic ingredients. Thirty four of these samples were tested for possible use as clay body ingredients, while sixty five samples were selected for assessment as glaze ingredients. A wood fired kiln was built from firebricks produced from a local deposit of a white bauxite related material. Materials selected as a result of these tests were combined to create ceramic objects fired at stoneware temperatures. The most interesting result of the investigation was the discovery of a number of small weathered dykes and sills, samples from which were developed into workable ceramic clay bodies and glazes using a simple empirical testing procedure. A previously unknown excellent white translucent native porcelain stone or ‘bai tunze’ was discovered and developed into a workable porcelain body. Some iron stained porcelain bodies that ‘flashed’ red in the wood firing kiln were also developed. Exhibitions of the creative work produced were shown in the ‘Legge Gallery’, a Fine Art gallery in Sydney. Two critical reviews of those shows appeared in the magazine Craft Arts International, No. 64, 2005, pp 106-107 and The Journal of Australian Ceramics, Vol 46 #1 pp 21-24. Several papers were published detailing various aspects of the research: “The Search for Raw Materials in the Southern Highlands” in The Journal of Australian Ceramics, Vol 41#3, pp 22-23; “Flotation – A method of refining useful minerals”, in The Journal of Australian Ceramics, Vol 41#3, pp 24-25; “Magic Dirt” in The Journal of Australian Ceramics, Vol 46 #1 pp 76-79; “New work from an old landscape”, in Ceramics Technical, 24, 2007. pp 45-52;“From the ground up”, in Ceramic review, issue 222, 2006, pp 54-55. The research concludes that the Southern Highlands of New South Wales is geologically rich in suitable materials for the production of stoneware ceramics and that there are a few specific bai tunze like materials that are very interesting and have considerable aesthetic potential. The research determined that these bai tunze like materials are potentially capable of being developed into clay bodies and glazes of great beauty. / Doctor of Philosophy (PhD)

Little is known about the strain and consequences of very prolonged and sustained exercise lasting multiple days. This thesis comprises two multi-day exercise field studies and a 24-h, controlled-trial field/laboratory study. The field studies were undertaken using international adventure races (2003 and 2004 Southern Traverses: 86-120 h) to profile exercise intensity and associated physiological and psychophysical strain, and physical and cognitive performance. The 2003 study showed that exercise intensity (from heart rate range) averaged 64% during the first 12 h, dropped to 41% by 24 h, and remained so thereafter. Body core temperature (gastrointestinal pills), throughout racing (n=8) was relatively stable (min 36.0�C and only briefly >39�C), despite widely varying endogenous and exogenous thermal stress. Blood samples obtained before (n=34), during (n=11) and after (n=34) racing revealed a large plasma volume expansion (24%), with stable [sodium]plasma (n=6). Acute (15-30 h) and chronic (96-120 h) elevation of neutrophil, monocyte and lymphocyte numbers were observed across the race. Standardised exercise tests (rest, 25 and 50% peak power output (PPO)) before and after racing (n=9) revealed an extreme shift toward fat utilisation, consistent with lowered fat mass (11%; n=44) and high [free fatty acids]plasma (up 370%; n=9) at race-finish, although [HAD]muscle was unchanged. Muscle glycogen was only 50% lower post-race (290 nmol�kg⁻�d.w.). Complex cognitive performance (Stroop test) impairment was attenuated during 50% PPO post-race. Perceived exertion uncoupled from HR at standardised workloads. Explosive power (jump test; n=24) and anaerobic power (30-s Wingate; n=27) were modestly (<10%) impacted. Strength reduction of arms (11%) and legs (17%) was equivalent (p=0.17). The 2004 study (n=4) involved dissimilar terrain, vegetation, and sequence of exercise modes, yet the profile of exercise intensity was similar: first 12 h 65%, then 45% by 24 h and thereafter. Thus, athletes reliably attain sustainable, low-to-moderate exercise intensity by 24 h. Plasma volume, neutrophil and monocyte responses were reliable across races, whereas lymphocytes were not. Plasma [IL-6] and [S100β] were elevated, substantially in some individuals (IL-6: 223 pg�mL⁻�; S100β: 113 pg�mL⁻�), during racing. A 24-h adventure race simulation (n=9) was then undertaken to investigate physiological and psychophysical factors influencing exercise intensity, autonomic function and orthostatic tolerance. Tests were at 0, ~7, ~15 and 24 h. The 24-h HR profile matched that observed during racing: first 12 h 58% (including 3-h testing), remainder 41%. The shift toward fat utilisation was almost complete within 7 h, and similar to that following 2003 race. The perceived exertion-to-HR uncoupling was also similar; being complete within 15 h. Plasma [noradrenaline] for rest and 12-km�h⁻� run was elevated post-simulation. Plasma [IL-6] peaked by 7 h, although not as high as field observations. The timeframe of metabolic change and perceived exertion uncoupling coincided with that of pace reduction, and may be important regulatory components of very prolonged exercise intensity. Orthostatic intolerance was evident during the simulation (n=6/9), as was cerebral hypo-perfusion (15 h & 24 h). Autonomic function (baroreflex sensitivity, sympathetic activation, parasympathetic withdrawal) was altered only at 7 h, whereas postural-induced hypotension (via impaired venous response) and hypocapnia were always present.

An investigation of the geological resources of the Southern Highlands was undertaken and over two hundred samples were collected and examined for possible use as stoneware ceramic ingredients. Thirty four of these samples were tested for possible use as clay body ingredients, while sixty five samples were selected for assessment as glaze ingredients. A wood fired kiln was built from firebricks produced from a local deposit of a white bauxite related material. Materials selected as a result of these tests were combined to create ceramic objects fired at stoneware temperatures. The most interesting result of the investigation was the discovery of a number of small weathered dykes and sills, samples from which were developed into workable ceramic clay bodies and glazes using a simple empirical testing procedure. A previously unknown excellent white translucent native porcelain stone or ‘bai tunze’ was discovered and developed into a workable porcelain body. Some iron stained porcelain bodies that ‘flashed’ red in the wood firing kiln were also developed. Exhibitions of the creative work produced were shown in the ‘Legge Gallery’, a Fine Art gallery in Sydney. Two critical reviews of those shows appeared in the magazine Craft Arts International, No. 64, 2005, pp 106-107 and The Journal of Australian Ceramics, Vol 46 #1 pp 21-24. Several papers were published detailing various aspects of the research: “The Search for Raw Materials in the Southern Highlands” in The Journal of Australian Ceramics, Vol 41#3, pp 22-23; “Flotation – A method of refining useful minerals”, in The Journal of Australian Ceramics, Vol 41#3, pp 24-25; “Magic Dirt” in The Journal of Australian Ceramics, Vol 46 #1 pp 76-79; “New work from an old landscape”, in Ceramics Technical, 24, 2007. pp 45-52;“From the ground up”, in Ceramic review, issue 222, 2006, pp 54-55. The research concludes that the Southern Highlands of New South Wales is geologically rich in suitable materials for the production of stoneware ceramics and that there are a few specific bai tunze like materials that are very interesting and have considerable aesthetic potential. The research determined that these bai tunze like materials are potentially capable of being developed into clay bodies and glazes of great beauty. / Doctor of Philosophy (PhD)

[Abstract]: Universities have traditionally focused their efforts on recruiting new students and increasing participation rates. However, higher retention and progression rates of students are likely to have a beneficial effect on the overall performance of universities in terms of their student-based income. The majority of previous studies addressing student retention have largely been focused on younger undergraduate on-campus students therefore this research seeks to investigate the factors which affect the retention and progression of postgraduate business students undertaking their studies by distance education. This study is based on a qualitative exploratory research design comprising twenty semi-structured in-depth interviews conducted with current and former students and university staff members. The key findings of this study indicate that a combination of situational, institutional and dispositional factors impact upon the retention and progression of postgraduate business distance education students. The employment and family commitments of students, whether students believed that their studies would benefit their career goals and the design of the distance education program appear to be the most important factors impacting upon student retention and progression. In contrast to the majority of services marketing literature, it would appear that student satisfaction is not a key factor impacting upon student retention and progression in this context. This research also provides a range of managerial implications and recommendations for postgraduate distance education providers.