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Academic literature on the topic 'The Hut Central Valley'

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Published: 10 December 2022
Last updated: 19 February 2023

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Journal articles on the topic "The Hut Central Valley"

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Lee, Yun-Young, and Richard Grotjahn. "California Central Valley Summer Heat Waves Form Two Ways*." Journal of Climate 29, no. 3 (February 1, 2016): 1201–17. http://dx.doi.org/10.1175/jcli-d-15-0270.1.

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Abstract California Central Valley (CCV) heat waves are grouped into two types based on the temporal and spatial evolution of the large-scale meteorological patterns (LSMPs) prior to onset. The k-means clustering of key features in the anomalous temperature and zonal wind identifies the two groups. Composite analyses show different evolution prior to developing a similar ridge–trough–ridge pattern spanning the North Pacific at the onset of CCV hot spells. Backward trajectories show adiabatic heating of air enhanced by anomalous sinking plus horizontal advection as the main mechanisms to create hot lower-tropospheric air just off the Northern California coast, although the paths differ between clusters. The first cluster develops the ridge at the west coast on the day before onset, consistent with wave activity flux traveling across the North Pacific. Air parcels that arrive at the maximum temperature anomaly (just off the Northern California coast) tend to travel a long distance across the Pacific from the west. The second cluster has the ridge in place for several days prior to extreme CCV heat, but this ridge is located farther north, with heat anomaly over the northwestern United States. This ridge expands south as air parcels at midtropospheric levels descend from the northwest while lower-level parcels over land tend to bring hot air from directions ranging from the hot area to the northeast to the desert areas to the southeast. These two types reveal unexpected dynamical complexity, hint at different remote associations, and expand the assessment needed of climate models’ simulations of these heat waves.
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Yang, Yan, Jiwen Fan, L. Ruby Leung, Chun Zhao, Zhanqing Li, and Daniel Rosenfeld. "Mechanisms Contributing to Suppressed Precipitation in Mt. Hua of Central China. Part I: Mountain Valley Circulation." Journal of the Atmospheric Sciences 73, no. 3 (February 15, 2016): 1351–66. http://dx.doi.org/10.1175/jas-d-15-0233.1.

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Abstract A significant reduction in precipitation in the past decades has been documented over many mountain ranges such as those in central and eastern China. Consistent with the increase of air pollution in these regions, it has been argued that the precipitation trend is linked to the aerosol microphysical effect on suppressing warm rain. Rigorous quantitative investigations on the reasons responsible for the precipitation reduction are lacking. In this study, an improved Weather Research and Forecasting (WRF) Model with online coupled chemistry (WRF-Chem) is applied and simulations are conducted at the convection-permitting scale to explore the major mechanisms governing changes in precipitation from orographic clouds in the Mt. Hua area in central China. It is found that anthropogenic pollution contributes to a ~40% reduction of precipitation over Mt. Hua during the 1-month summertime period. The reduction is mainly associated with precipitation events associated with valley–mountain circulation and a mesoscale cold-front event. In this paper (Part I), the mechanism leading to a significant reduction for the cases associated with valley–mountain circulation is scrutinized. It is found that the valley breeze is weakened by aerosols as a result of absorbing aerosol-induced warming aloft and cooling near the surface as a result of aerosol–radiation interaction (ARI). The weakened valley breeze and the reduced water vapor in the valley due to reduced evapotranspiration as a result of surface cooling significantly reduce the transport of water vapor from the valley to mountain and the relative humidity over the mountain, thus suppressing convection and precipitation in the mountain.
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Karavaev, G. F., and S. V. Sudakov. "Hot electron plasma instability in semiconductors with a nonparabolic central valley." Soviet Physics Journal 32, no. 3 (March 1989): 182–86. http://dx.doi.org/10.1007/bf00897380.

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Zhenhua, Ren, Zhou Xun, Yang Miaolin, Wang Xiaocui, Zheng Yuhui, Li Xiaolu, and Shen Ye. "Hydrochemical Characteristics and Formation of the Madeng Hot Spring in Yunnan, China." Geofluids 2018 (July 2, 2018): 1–11. http://dx.doi.org/10.1155/2018/2368246.

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The Madeng hot spring emerges in the central river valley in the northeastern Lanping Basin in Jianchuan county of Yunnan Province in China. Quaternary sand and gravel occur in the valley which is underlain by the red beds consisting of sandstone and mudstone. The temperature of the hot spring is 42.1°C. The spring water has a pH value of 6.41, TDS of 3.98 g/L, F contents of 3.08 mg/L, and H2SiO3 of 35.6 mg/L. The hot water is of SO4•Cl-Na•Ca type. There is a slight hydrogen sulfide odor in the spring water. Stable hydrogen and oxygen isotopes indicate that the hot water is of meteoric origin. It is estimated that the elevation of the recharge area of the hot spring is approximately 3800 m, the age of the hot water is some 140 years, the temperature of the geothermal reservoir is 75°C–80°C, the mixture ratio of cold water is approximately 80%, and the circulation depth of the thermal groundwater is 1870 m. After receiving recharge from infiltration of precipitation in the mountainous recharge areas, the groundwater undergoes a deep circulation, obtains heat from the heat flow, flows upward along the fractured zone, and emerges as an upflow spring through the Quaternary sand and gravel in the central low-lying river valley.
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BAI, LIN, BRUCE MASLIN, and NIANHE XIA. "Senegalia propinqua (Leguminosae: Mimosoideae), a new species from the Yuanjiang dry-hot valley in south-central Yunnan Province, China." Phytotaxa 522, no. 1 (October 5, 2021): 38–46. http://dx.doi.org/10.11646/phytotaxa.522.1.4.

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Senegalia propinqua (Leguminosae: Mimosoideae), a new species from the Yuanjiang dry-hot valley in south-central Yunnan Province, China is described and illustrated. It is compared with S. kunmingensis, S. macrocephala and S. teniana. A distribution map of the four species is provided.
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Stevens, D. R., and J. P. Garden. "Challenges facing the farmers of Central Otago." Proceedings of the New Zealand Grassland Association 76 (January 1, 2014): 25–28. http://dx.doi.org/10.33584/jnzg.2014.76.2957.

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The Central Otago region, with its cold winters and hot summers, and valley floors with uplift mountains is definitely "a world of difference". At the NZGA conference in Alexandra in 1966 John Hercus stated "Central Otago has a lure which sets it apart from the rest of New Zealand. Its characteristics of geology, topography and climate, its history of occupation and exploitation, its scenery at once forbidding and yet strangely fascinating - these features combine to cast a spell which few who have been exposed, can ever fully escape" (Hercus 1966). The region and its high country have an iconic status epitomised by the "Southern Man" stereotype. This places Central Otago deep in the psyche of the nation. With this goes a unique and significant set of conditions under which farming must take place. Not only does the region have the biophysical challenges of soils, water and climate to contend with, but a wider set of values, often imposed from elsewhere. Fifty years after that first conference we remain challenged. What are the opportunities in front of us and how should we best accommodate the challenge of maintaining a viable enterprise and at the same time, respecting the intense public and customer interest in our use of land and livestock? Central Otago and the associated high country of the Lakes district and McKenzie basin can be divided into three farming types. These are the valley floor irrigable type, the flat and downland dryland regions, and the high country. Each of these has challenges that are at times unique, but often overlap with problems faced in other regions.
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Sarna-Wojcicki, Andrei M., Charles E. Meyer, Harry R. Bowman, N. Timothy Hall, Paul C. Russell, Marta J. Woodward, and Janet L. Slate. "Correlation of the Rockland Ash Bed, a 400,000-Year-Old Stratigraphic Marker in Northern California and Western Nevada, and Implications for Middle Pleistocene Paleogeography of Central California." Quaternary Research 23, no. 2 (March 1985): 236–57. http://dx.doi.org/10.1016/0033-5894(85)90031-6.

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Outcrops of an ash bed at several localities in northern California and western Nevada belong to a single air-fall ash layer, the informally named Rockland ash bed, dated at about 400,000 yr B.P. The informal Rockland pumice tuff breccia, a thick, coarse, compound tephra deposit southwest of Lassen Peak in northeastern California, is the near-source equivalent of the Rockland ash bed. Relations between initial thickness of the Rockland ash bed and distances to eruptive source suggest that the eruption was at least as great as that of the Mazama ash from Crater Lake, Oregon. Identification of the Rockland tephra allows temporal correlation of associated middle Pleistocene strata of diverse facies in separate depositional basins. Specifically, marine, littoral, estuarine, and fluvial strata of the Hookton and type Merced formations correlate with fluvial strata of the Santa Clara Formation and unnamed alluvium of Willits Valley and the Hollister area, in northwestern and west-central California, and with lacustrine beds of Mohawk Valley, fluvial deposits of the Red Bluff Formation of the eastern Sacramento Valley, and fluvial and glaciofluvial deposits of Fales Hot Spring, Carson City, and Washoe Valley areas in northeastern California and western Nevada. Stratigraphic relations of the Rockland ash bed and older tephra layers in the Great Valley and near San Francisco suggest that the southern Great Valley emerged above sea level about 2 my ago, that its southerly outlet to the ocean was closed sometime after about 2 my ago, and that drainage from the Great Valley to the ocean was established near the present, northerly outlet in the vicinity of San Francisco Bay about 0.6 my ago.
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Lee, Yun-Young, and Richard Grotjahn. "Evidence of Specific MJO Phase Occurrence with Summertime California Central Valley Extreme Hot Weather." Advances in Atmospheric Sciences 36, no. 6 (April 12, 2019): 589–602. http://dx.doi.org/10.1007/s00376-019-8167-1.

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Daci, A., G. Kaza, T. Deda, and S. Hoti. "The environmental impact of the Copper industry in the Fani River Valley (Repsi "Hot spot") Mirdita, Albania." Bulletin of the Geological Society of Greece 40, no. 3 (June 5, 2018): 1387. http://dx.doi.org/10.12681/bgsg.16970.

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For more than 40 years, full cycle Copper industry has exercised its activity in central Mirdita, as one of the priorities for the economic development of this zone. Copper deposits have been discovered in many parts of the territory of central Mirdita, whereas the main activity of the mining and processing industry is located in the Fan iriver valley. The interruption of industrial activity after the years '90, could not stop the negative environmental impact. The presence of dumps in Fani river banks (as in Repsi, Rresheni and Rubiku) and numerous mining works· (addits) in Spaçi and Kodër Spaçi slopes, from which many acid waters drain, including also the natural leaching of surface outcrops of mineralized zones, make up a serious danger to the biodiversity of this area. Several recommendations to reduce the environmental impact of the tailings and copper ores in the dumps in Fani river valley are given in this paper
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Whitman, Christopher J. "STRAW BALES, A POSSIBLE SOLUTION FOR HYGRO-THERMALLY COMFORTABLE DWELLINGS IN CHILE'S CENTRAL VALLEY: PHYSICAL TEST CHAMBERS AND IN SITU MEASUREMENTS." Journal of Green Building 9, no. 2 (July 2014): 161–81. http://dx.doi.org/10.3992/1943-4618-9.2.161.

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Dwellings in a Mediterranean climate, such as that of Chile's Central Valley, must provide hygro-thermal comfort both during the cold winters, and the hot days and cool summer nights. Straw, once a material common in Chile's indigenous and vernacular architecture, could meet these demands when coupled with sufficient thermal mass in the form of earth renders and floor finishes. This article presents measurements of dry bulb temperatures and relative humidity, both in physical test chambers and Chilean straw bale homes. The results of these measurements confirm that straw bale construction could provide hygro-thermal comfort with heating demands 28% less than those of constructions that meet the Chilean thermal building regulations. Straw bale, therefore, could provide a viable solution for comfortable, energy efficient, rural dwellings in Chile's Central Valley. Whilst over 40 private straw bale projects have been completed in Chile to date, restrictions applying to projects receiving government subsidies prevent this technology being available to those who need it most.
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Dissertations / Theses on the topic "The Hut Central Valley"

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Walters, Eric L. "Habitat and space use of the Red-naped Sapsucker, Sphyrapicus nuchalis, in the Hat Creek valley, south-central British Columbia." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk2/tape16/PQDD_0014/MQ32698.pdf.

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Marquez, Lizbeth. "Central Valley Promise| Creating a K-16 College and Career Pipeline for Central Valley Students." Thesis, California State University, Fresno, 2019. http://pqdtopen.proquest.com/#viewpdf?dispub=13424463.

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Degree completion has been a topic of debate in higher education institutions. Although efforts have been made to raise the rate of completion, the number of students completing college remains low. Low rates may lead to wasted time and money as students often take unnecessary coursework as a result of not having a well-developed plan for completion. To combat this problem, programs have been implemented at community colleges that are designed to meet student needs, develop tailored educational plans, and help students set goals. One such program is the Central Valley Promise (CVP) program, which offers a solution that could meet the specific needs students of the Central Valley of California. Upon meeting the entrance requirements, students are eligible to receive free tuition for one semester and the promise of support to completion for all students. Because CVP has the potential to affect many incoming students, it was important to examine whether it is achieving its goal. This study sought to gain understanding of student transition and career readiness. A survey was given to 402 CVP students during their first semester of college. A comparison group of 112 students also received the survey. All participants were incoming community college freshmen. Also, observations were conducted during three CVP events. Findings included an increased satisfaction and confidence level in academic performance, social life, and choosing a college major among CVP students. Recommendations include continued support for students, adding a mentorship component, and hiring faculty to exclusively work with CVP students.

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Peterson, Kaj. "Agriculture and Groundwater Overdraft in California’s Central Valley : Lantbruk och grundvatten-övertrassering i Kaliforniens Central Valley region." Thesis, KTH, Industriell ekologi, 2016. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-189046.

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Agriculture in California’s Central Valley is important to the US economy and food supply. High reliance on groundwater (GW) for irrigation has led to GW overdraft. Among the consequences is that the GW level is lowered, increasing the energy requirements and cost of GW extraction. This is assessed in a case study of the Turlock subbasin, as well as a simplified Cost-Benefit Analysis (CBA), in which the profitability of strategies for avoiding groundwater overdraft is compared to Business As Usual (BAU) for the years 2001 and 2050, using a high and low energy cost estimate. Climate projections are applied to the year 2050. An overdraft of 95 million m3 in 2001 is found to lower the GW level by 19.3cm, leading to an increase in energy requirements and cost of GW extraction of 0.320 Wh/m3 and 0.416 cents/m3, respectively. A reduction in production was found to be less profitable than BAU in all cases except for the year 2050, using high cost estimates. Crop replacement was found to be profitable in all cases. The use of desalinated water was found to be unprofitable in all cases. It is concluded that climate change and irrigation costs will have one or more of the following outcomes: decreased production, a shift towards higher $/m3 crops, and/or increased food prices.
Lantbruk I Kaliforniens Central Valley region är viktig för den Amerikanska ekonomin och livsmedelsförsörjningen. Stort beroende av grundvatten till konstbevattning har lett till grundvatten-övertrassering. Bland dess konsekvenser är att grundvatten nivån sjunker, vilket gör det mer energi-krävande och kostsamt att pumpa grundvattnet. Detta analyseras i fallstudiet, Turlock subbasin, där det även utförs en förenklad kostnads-nytto analys, i vilken lönsamheten av strategier för att undvika grundvatten-övertrassering jämförs med Business As Usual (BAU) för åren 2001 och 2050, baserad på en hög och en låg uppskattning av energi kostnader. Året 2050 beräknas inklusive förväntade förändringar i klimatet. En övertrassering på 95 miljoner m3 i 2001 visar sig resultera i att grundvatten nivån sjunker 19,3 cm, vilket ökar energibehovet och kostnaden av att pumpa grundvatten med 0,32 Wh/m3 respektivt 0,416 cents/m3. Att minska produktionen visar sig att endast vara lönsamt i ett fall: år 2050 med höga energi uppskattningar. Att byta grödor visar sig vara lönsamt i alla fall. Att förbruka desalinerat vatten visar sig vara olönsamt i alla fall. Det dras slutsatsen att förändringar i klimatet och kostnader av konstbevattning kommer att leda till en eller fler av följande utfall: förminskad produktion, ett skift mot högre $/m3 grödor, och/eller förhöjda matpriser.
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Pool, Donald Robert 1955. "Hydrogeology of McMullen Valley, west-central Arizona." Thesis, The University of Arizona, 1987. http://hdl.handle.net/10150/191959.

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The hydrogeology of McMullen Valley, west-central Arizona, was investigated using geologic, geophysical, and hydrologic data and a numerical model of the ground-water system. Geologic information and gravity modeling indicate that the main structure of McMullen Valley is a syncline. Basin fill that accumulated in the structural depression is the main aquifer and is divided into upper and lower units. A fine-grained facies in separates the aquifer into shallow and deep systems. A numerical model was used to analyze the ground-water system for both steady-state and transient conditions. The steady-state model aided in evaluating the distribution of hydraulic properties. The transient model was used to analyze system response to pumping stress. Water-level declines are controlled by the distribution of pumpage, specific-yield, and the fine-grained facies of lower basin fill. Significant water-level declines may extend to aquifer boundaries in most of the basin.
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Bieker, Chelsea Jean. "Out the Valley." PDXScholar, 2012. https://pdxscholar.library.pdx.edu/open_access_etds/349.

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The following eight stories make up Out the Valley, a collection of short fiction. Each story stands independently as a single work, though together they are bound by ties to California's Central Valley. The places the characters inhabit range widely in socio-economic class systems, from the gang-ruled streets of Fresno in Beautiful, Smart, Talented, to upper middle class suburbia, looking back over one man's life in My Mary. Each character is dealing with their own set of deficiencies, so to speak. In Dominoes, Ross recalls his first love from prison. In Be Thou My Vision, a mother takes a trip to understand the life of her daughter in the wake of her murder. The Bare of Our Chests circles truth in a series of frames as the main character, Maynard, tries to confront the past while mourning his mother. A More Interesting Story shows Joni attempt to find freedom in her world of mental restrictions. In A Well Matched Man, Ephram's superficiality keeps him from finding and recognizing love. The title story, Deficiencies, follows a college-aged young man, Erol, as he learns to write despite dyslexia and the onslaught of obsessive love for his tutor. These are stories that the main characters wish they were not telling--events they cannot face in truth, and so view instead through their own flawed lenses.
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Nash, Linda Lorraine. "Transforming the Central Valley : body, identity, and environment in California, 1850-1970 /." Thesis, Connect to this title online; UW restricted, 2000. http://hdl.handle.net/1773/10414.

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Anderson, Darcy J., and Darcy J. Anderson. "Central Avra Valley storage and recovery project geochemical modeling study." Thesis, The University of Arizona, 2000. http://hdl.handle.net/10150/626879.

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The chemical and isotopic characteristics of the groundwater in A vra Valley, Arizona, were investigated, and existing hydrologic information was compiled to determine processes affecting groundwater chemistry in this area. The characteristics of Central Arizona Project (CAP) water, the surface water source for recharge operations in the Central Avra Valley Storage and Recovery Project (CAVSARP), were investigated for comparison. The changes that occurred over time in the chemistry of the groundwater were evaluated with respect to vadose zone processes and mixing with CAP water during recharge operations. Two major vadose zone processes were identified: flushing of perched water remaining from historical agricultural irrigation, and cation exchange as recharged CAP water infiltrated through clay layers at the site. Geochemical modeling using PHREEQC was conducted for groundwater, CAP water and mixtures of the two waters to determine processes that could affect recharge rates and the chemical composition of groundwater that will be recovered for delivery to customers. The results of the modeling were used to infer the likelihood that mineral precipitation and ion exchange occurred during the study period of January 1998 to December 1999. Based on the modeling results, significant mineral precipitation and subsequent decreases in recharge rates seems unlikely. Cation exchange processes will continue to alter the chemical composition of the CAP water between the recharge basin and its arrival at the water table.
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Wischusen, John David Henry School of Biological Earth &amp Environmental Sciences UNSW. "Hydrogeology, hydrochemistry and isotope hydrology of Palm Valley, Central Australia." Awarded by:University of New South Wales. School of Biological, Earth and Environmental Sciences, 2005. http://handle.unsw.edu.au/1959.4/32925.

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The Palm Valley oasis in arid central Australia is characterised by stands of palm trees (Livistona mariae). How these unique plants, separated by nearly a 1000 kilometres of arid country from their nearest relatives persist, has long fascinated visitors. Defining the hydrogeology of the Hermannsburg Sandstone, a regionally extensive and thick Devonian sequence of the Amadeus Basin that underlies Palm Valley, is the major thrust of investigation. Appraisal of drilling data shows this aquifer to be a dual porosity fractured rock aquifer which, on a regional scale, behaves as a low permeability, hydraulically continuous resource. Groundwater is low salinity (TDS <1000 mg/L) and bicarbonate rich. Slight variations in cation chemistry indicate different flow paths with separate geochemical histories have been sampled. Stable isotope (????H, ???????O) results from Palm Valley show groundwater to have a uniform composition that plots on or near a local meteoric water line. Radiocarbon results are observed to vary from effectively dead (< 4%) to 87 % modern carbon. To resolve groundwater age beyond the radiocarbon window the long lived radioisotope 36Cl was also used. Ratios of 36Cl/Cl range from 130 to 290 x 10-15. In this region atmospheric 36Cl/Cl ratio is around 300 x 10-15. Thus an age range of around 300 ka is indicated if, as is apparent, radioactive decay is the only significant cause of 36Cl/Cl variation within the aquifer. A review of previous, often controversial, 36Cl decay studies shows results are usually ambiguous due to lack of certainty when factoring subsurface Cl- addition into decay calculations. Apparently, due to the thickness of the Hermannsburg Sandstone, no subsurface sources of Cl- such as aquitards or halites, are encountered along groundwater flow paths, hence the clear 36Cl decay trend seen. The classic homogenous aquifer with varying surface topography, the "Toth" flow model, is the simplest conceptual model that need be invoked to explain these isotope data. Complexities, associated with local topography flow cells superimposed on the regional gradient, signify groundwater with markedly different flow path lengths has been sampled. The long travel times (> 100 ka) indicate groundwater discharge would endure through arid phases associated with Quaternary climate oscillations. Such a flow system can explain the persistence of this arid zone groundwater-dependent ecosystem and highlight the possibility that Palm Valley has acted as a flora refuge since at least the mid- Pleistocene.
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Coleman, Margaret E. (Margaret Emily). "The tectonic evolution of the central Himalya, Marsyandi Valley, Nepal." Thesis, Massachusetts Institute of Technology, 1996. http://hdl.handle.net/1721.1/10663.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 1996.
Folded map in pocket following text.
Includes bibliographical references.
by Margaret E. Coleman.
Ph.D.
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Pena, Kyle. "PALEOSEISMOLOGY OF THE CENTRAL GARLOCK FAULT IN SEARLES VALLEY, CALIFORNIA." CSUSB ScholarWorks, 2019. https://scholarworks.lib.csusb.edu/etd/956.

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In this study, a paleoseismic trench with limited age constraints that was previously excavated in 1990 across the central Garlock Fault near Christmas Canyon, in Searles Valley, California, was reopened to take advantage of new advances in luminescence dating techniques to investigate potential temporal variability in earthquake recurrence on the Garlock fault and to analyze previously unexposed older earthquake evidence. The trench exposed interbedded alluvial sand and pebble-gravels, with well-sorted, rounded, lacustrine sand from the most recent highstand of pluvial Lake Searles present at the base of the trench. Preliminary findings suggest at least 10 surface rupturing earthquake events occurred during the 10 k.y. time period exposed in the trench. To provide age constraints on the paleo-surface-rupturing events from the new trench, 54 luminescence samples were collected and the single-grain luminescence dating technique post- - was employed. The ages indicated that 7 events have occurred in the past ~7.2 ka, with at least 3 additional events in the more poorly stratified deeper section of the trench. This suggests a recurrence interval of ~1000 years. Event pattern seen at this trench did not exactly replicate the same pattern at other paleoseismic sites along the Garlock Fault. The most recent event seen at this trench occured within the same time period as the most recent events seen at the other paleoseismic sites on the central Garlock Fault.
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Books on the topic "The Hut Central Valley"

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Authority, California High-Speed Rail. Final Bay Area to Central Valley high-speed train (HST) program environmental impact report/environmental impact statement (EIR/EIS). Sacramento, CA: California High-Speed Rail Authority, 2008.

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Orfield, Myron. Central Valley metropatterns: Regional challenges in California's Central Valley. Minneapolis, MN (1313 5th Street SE, Suite 108): Metropolitan Area Research Corp., 2000.

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McCormack, Don. Alameda County & Central Valley 2006. Martinez, Calif: McCormack's Guides, 2005.

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Schweinsberg, Allen R. Birds of the Central Susquehanna Valley. [Lewisburg, Pa.]: A.R. Schweinsberg, 1988.

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A, Morse Phyllis, ed. Archaeology of the central Mississippi Valley. Tuscaloosa: University of Alabama Press, 2009.

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W, Haslam Gerald, and Dawson Robert 1950-, eds. The great central valley: California's heartland. Berkeley: University of California Press, 1993.

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Moffat, Amy. 2020: Visions for the Central Valley. Berkeley, Calif: Heyday Books, 2010.

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H, McNutt Charles, ed. Prehistory of the Central Mississippi Valley. Tuscaloosa: University of Alabama Press, 1996.

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Obermeier, Stephen F. Liquefaction potential in the central Mississippi Valley. [Washington, D.C.]: U.S. G.P.O., 1988.

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Pool, D. R. Hydrogeology of McMullen Valley, west-central Arizona. Tucson, Ariz: Dept. of the Interior, U.S. Geological Survey, 1987.

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Book chapters on the topic "The Hut Central Valley"

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Reid, F. A., D. Fehringer, R. Spell, K. Petrik, and M. Petrie. "Wetlands of California’s Central Valley (USA)." In The Wetland Book, 1–7. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6173-5_119-1.

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Reid, Frederic A., Daniel Fehringer, Ruth Spell, Kevin Petrik, and Mark Petrie. "Wetlands of California’s Central Valley (USA)." In The Wetland Book, 697–703. Dordrecht: Springer Netherlands, 2018. http://dx.doi.org/10.1007/978-94-007-4001-3_119.

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Crow, Charles L. "Regions of California: The Great Central Valley." In A Companion to the Regional Literatures of America, 379–96. Oxford, UK: Blackwell Publishing Ltd, 2007. http://dx.doi.org/10.1002/9780470999080.ch23.

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Abazov, Rafis. "Border Disputes in the Farghona Valley." In The Palgrave Concise Historical Atlas of Central Asia, 106–7. New York: Palgrave Macmillan US, 2008. http://dx.doi.org/10.1057/9780230610903_48.

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Lancaster, N. "Paleoenvironments in the Tsondab Valley, Central Namib Desert." In Palaeoecology of Africa, 411–19. London: Routledge, 2022. http://dx.doi.org/10.1201/9780203744512-38.

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Otorbaev, Djoomart. "The Fergana Valley and Its Conflicts." In Central Asia's Economic Rebirth in the Shadow of the New Great Game, 281–92. London: Routledge, 2022. http://dx.doi.org/10.4324/9781003360728-16.

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Russell, David J., Hans Schick, and Dietrich Nährig. "Reactions of soil Collembolan communities to inundation in floodplain ecosystems of the Upper Rhine Valley." In Wetlands in Central Europe, 35–70. Berlin, Heidelberg: Springer Berlin Heidelberg, 2002. http://dx.doi.org/10.1007/978-3-662-05054-5_3.

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Evans, Mark A., and Steven Wojtal. "Day five - Shenandoah Valley." In Geometry and Deformation Fabrics in the Central and Southern Appalachian Valley and Ridge and Blue Ridge: Frederick, Maryland to Allatoona Dam, Georgia July 20–27, 1989, 44–48. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft357p0044.

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Balfour, William M. "The Contact Caves of Central Greenbrier County." In Caves and Karst of the Greenbrier Valley in West Virginia, 207–30. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-65801-8_11.

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Doctor, Daniel H., and Wil Orndorff. "Hypogene Caves of the Central Appalachian Shenandoah Valley in Virginia." In Hypogene Karst Regions and Caves of the World, 691–707. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-53348-3_46.

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Conference papers on the topic "The Hut Central Valley"

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Peterson, Lloyd E., and Paul Fujitani. "The Central Valley Operations Office Monthly Spreadsheet Model." In Operations Management Conference 2006. Reston, VA: American Society of Civil Engineers, 2006. http://dx.doi.org/10.1061/40875(212)2.

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Day, Stephanie S., Charles Idell Nixon, Carrie Jennings, Karen B. Gran, Stephen B. DeLong, Whitney M. DeLong, Megan Ostrand, Samuel D. Marolt, Victoria Elizabeth Halvorson, and Micheal Sullivan. "LANDSLIDES IN THE RED RIVER VALLEY, MINNESOTA." In 54th Annual GSA North-Central Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020nc-348211.

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Krippner, Kiara, Matt Allison, Laura D. Triplett, Julie K. Bartley, Stephen B. DeLong, Whitney M. DeLong, Zachary Engle, Karen B. Gran, Carrie Jennings, and Andrew D. Wickert. "LANDSLIDE CHARACTERIZATION IN THE LOWER MINNESOTA RIVER VALLEY." In 54th Annual GSA North-Central Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020nc-348146.

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René, R. M. "Gravimetry of the Anderson Bedrock Valley of Central Indiana." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2004. Environment and Engineering Geophysical Society, 2004. http://dx.doi.org/10.4133/1.2923328.

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René, R. M. "Gravimetry Of The Anderson Bedrock Valley Of Central Indiana." In 17th EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems. European Association of Geoscientists & Engineers, 2004. http://dx.doi.org/10.3997/2214-4609-pdb.186.00_addendum.

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Thompson, Ren, Amy K. Gilmer, Kate Souders, and Daniel P. Miggins. "MIOCENE MAGMATISM OF THE CENTRAL DEATH VALLEY RHOMBOCHASM, USA." In Joint 118th Annual Cordilleran/72nd Annual Rocky Mountain Section Meeting - 2022. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022cd-374142.

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Broaddus, Carson L., Kimberly A. Hannula, and Robert W. Krantz. "THE EFFECT OF FAULT GOUGE ON FLUID FLOW, LISBON VALLEY, UT." In Joint 53rd Annual South-Central/53rd North-Central/71st Rocky Mtn GSA Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019sc-327376.

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Morgan, Tanner F., Kimberly A. Hannula, and Robert W. Krantz. "MAPPING SURFACE GEOCHEMICAL DATA WITH GIS IN LOWER LISBON VALLEY, UTAH." In Joint 53rd Annual South-Central/53rd North-Central/71st Rocky Mtn GSA Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019sc-327381.

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Layzell, Anthony L., and Rolfe D. Mandel. "HOLOCENE LANDSCAPE EVOLUTION IN THE REPUBLICAN RIVER VALLEY, SOUTH-CENTRAL NEBRASKA." In Joint 53rd Annual South-Central/53rd North-Central/71st Rocky Mtn GSA Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019sc-327447.

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Phillips, Andrew C. "GEOMORPHIC MAP OF THE LOWER WABASH VALLEY, IL-IN-KY." In 50th Annual GSA North-Central Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016nc-275448.

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Reports on the topic "The Hut Central Valley"

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Wandeler, Christian, and Steve Hart. The Central Valley Transportation Challenge. Mineta Transportation Institute, December 2022. http://dx.doi.org/10.31979/mti.2022.2029.

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The Central Valley Transportation Challenge provides underserved minority students, who are primarily from rural areas, with high quality transportation-related educational experiences so that they learn about transportation-related topics and opportunities in transportation careers. The CVTC is a project-based learning program that brings university faculty and students to K–12 classrooms in rural areas. The project operated with three main objectives: (1) support K–12 teachers’ understanding and implementation of the CVTC programs; (2) connect K–12 students with university faculty and students, and transportation professionals through the CVTC program; and (3) develop an online hub with transportation-related lesson plans and sequences. The results of this study are reported as five case studies and a description of the online hub. The case studies illustrate how different pedagogical approaches and uses of technology were implemented and how the project connections between the schools, community members and professionals from transportation-related fields were developed. In addition, to support the sustainability of transportation-related learning across subsequent years, the research team created an online transportation resource repository. This hub was populated with lessons and units developed by pedagogical and content experts. The lessons cover the grades K–12 and range from brief lessons to very engaging and holistic two-week-long lesson sequences. The CVTC has proven to be a highly flexible and adaptive model due to the use of technology and the teachers’ experience and pedagogical expertise. The timing of the program during the COVID-19 pandemic also provided the students that were learning from home with an engaging learning experience and some relief for teachers who were already dealing with a lot of adjustments. In that sense, the program reached traditionally underserved students, but did so in a critical time where these students faced even more obstacles.
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BECHTEL NEVADA and NNSA NEVADA SITE OFFICE. POST CLOSURE INSPECTION AND MONITORING REPORT FOR CORRECTIVE ACTION UNIT 417: CENTRAL NEVADA TEST AREA - SURFACE, HOT CREEK VALLEY, NEVADA, FOR CALENDAR YEAR 2004. Office of Scientific and Technical Information (OSTI), April 2005. http://dx.doi.org/10.2172/850249.

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Plouffe, A., V. Levson, and T. Giles. Quaternary stratigraphy of Taseko valley, south-central British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207418.

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Water Management Institute, International. Sharing water equitably in the Ferghana Valley, Central Asia. International Water Management Institute (IWMI), 2010. http://dx.doi.org/10.5337/2011.0038.

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Bardoux, M. The Kelowna detachment zone, Okanagan Valley, south-central British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/120179.

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Keller, G., G. Matile, H. Thorleifson, and Z. Malolepszy. 3D geological model of the Red River Valley, central North America. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2006. http://dx.doi.org/10.4095/221885.

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Huntley, D. Geoart in the south-central Mackenzie River valley region, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2006. http://dx.doi.org/10.4095/222391.

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Cockburn, Myles. Prostate Cancer and Pesticide Exposure in Diverse Populations in California's Central Valley. Fort Belvoir, VA: Defense Technical Information Center, December 2008. http://dx.doi.org/10.21236/ada494594.

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Huntley, D., and A. Duk-Rodkin. Landslide processes in the south-central Mackenzie River valley region, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2006. http://dx.doi.org/10.4095/222392.

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Huntley, D., A. Duk-Rodkin, and C. Sidwell. Landslide inventory of the south-central Mackenzie River valley region, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2006. http://dx.doi.org/10.4095/222393.

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