Relevant bibliographies by topics / Overland Lake

Academic literature on the topic 'Overland Lake'

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Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "Overland Lake"

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Motiee, Homayoun, and Edward McBean. "An assessment of long-term trends in hydrologic components and implications for water levels in Lake Superior." Hydrology Research 40, no. 6 (November 1, 2009): 564–79. http://dx.doi.org/10.2166/nh.2009.061.

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The combination of climate change and natural periodicities in meteorological variables are demonstrating significant impacts on the water resources of Lake Superior within the Laurentian Great Lakes system of North America. Statistical analyses of long-term records are used to demonstrate how changes over time may be interpreted very differently, depending upon the timeframe over which the analyses are made. Non-linear regression modelling shows that, while increasing trends in overland and overlake precipitation, flows and runoff occurred during the first decades of the twentieth century, very different trends are apparent for the period 1970–2005. For this latter period, increasing rates of air overlake temperature and lake evaporation are occurring but all other parameters are demonstrating decreasing trends. The result is a decline in water levels in Lake Superior at the rate of approximately 1 cm per year over the last 35 years. The results are used to show that to avoid decreasing water levels in Lake Superior, the discharge through St Mary's River must be decreased to approximately one-half the long-term annual average, the results of which will have dramatic implications for ships' cargo levels and hydroelectric energy generation.
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Tuheteru, Edy Jamal, Rudy Sayoga Gautama, Ginting Jalu Kusuma, Arno Adi Kuntoro, Kris Pranoto, and Yosef Palinggi. "Water Balance of Pit Lake Development in the Equatorial Region." Water 13, no. 21 (November 4, 2021): 3106. http://dx.doi.org/10.3390/w13213106.

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In recent years, Indonesia has become the largest coal exporter in the world, and most of the coal is being mined by means of open-pit mining. The closure of an open-pit mine will usually leave a pit morphological landform that, in most cases, will be developed into a pit lake. One of the main issues in developing a pit lake is the understanding of the pit lake filling process. This paper discusses the hydrological model in filling the mineout void in a coal mine in Kalimantan which is located close to the equatorial line. The J-void is a mineout coal pit that is 3000 m long and 1000 m wide, with a maximum depth of 145 m. The development of the J-void pit lake after the last load of coal had been mined out experienced a dynamic process, such as backfilling activities with an overburden as well as pumping mine water from the surrounding pits. There are two components in the model, i.e., overland/subsurface and pit area. The overland zone is simulated using the Rainfall-Runoff NRECA Hydrological Model approach to determine the runoff and groundwater components, whereas the pit area is affected by direct rainfall and evaporation. The model is validated with the observation data. The main source of water in the J-void pit lake is rainwater, both from the surrounding catchment area as well as direct rainfall. As this coal mine area is characterized as a multi-pit area and, consequently, several pit lakes will be formed in the future, the result of the hydrological model is very useful in planning the future pit lakes.
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Salisbury, Michael, Todd DeMunda, and Nicole Walker. "DEVELOPMENT AND VALIDATION OF A STORM SURGE AND WAVE MODEL FOR LAKE HURON (GREAT LAKES, USA)." Coastal Engineering Proceedings, no. 36 (December 30, 2018): 79. http://dx.doi.org/10.9753/icce.v36.waves.79.

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The Federal Emergency Management Agency (FEMA) is tasked with developing flood insurance rate maps along coastlines and major water bodies within the United States, which includes the U.S. portion of the Great Lakes shoreline. Previous flood studies have developed storm surge and wave models of the Great Lakes (including Lake Huron) in support of FEMA’s efforts; however, an independent technical review of those previous coastal flood studies in Lake Huron revealed technical deficiencies in the methods and tools used to generate the wave conditions needed to support overland mapping. Most paramount of these was the fact that starting wave conditions for one dimensional (1D) transformation from a two-dimensional (2D) model were taken from deep water. Using 1D methods to shoal and refract waves to the coastline for runup and/or overland wave analysis may fail to capture the more complex nature of wave refraction/diffraction that 2D wave models can capture. Further, this method omits the development of the directional wave spectra in the nearshore region. To address this concern, a coupled 2D wave and water level model (ADCIRC+SWAN) was developed to hindcast historical storms that have occurred in Lake Huron. These model results will be used to drive the 1D methods to assess nearshore wave hazards from locations near the surfzone limit.
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Kuhn, Catherine, and David Butman. "Declining greenness in Arctic-boreal lakes." Proceedings of the National Academy of Sciences 118, no. 15 (April 5, 2021): e2021219118. http://dx.doi.org/10.1073/pnas.2021219118.

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The highest concentration of the world’s lakes are found in Arctic-boreal regions [C. Verpoorter, T. Kutser, D. A. Seekell, L. J. Tranvik, Geophys. Res. Lett. 41, 6396–6402 (2014)], and consequently are undergoing the most rapid warming [J. E. Overland et al., Arctic Report Card (2018)]. However, the ecological response of Arctic-boreal lakes to warming remains highly uncertain. Historical trends in lake color from remote sensing observations can provide insights into changing lake ecology, yet have not been examined at the pan-Arctic scale. Here, we analyze time series of 30-m Landsat growing season composites to quantify trends in lake greenness for >4 × 105 waterbodies in boreal and Arctic western North America. We find lake greenness declined overall by 15% from the first to the last decade of analysis within the 6.3 × 106-km2 study region but with significant spatial variability. Greening declines were more likely to be found in areas also undergoing increases in air temperature and precipitation. These findings support the hypothesis that warming has increased connectivity between lakes and the land surface [A. Bring et al., J. Geophys. Res. Biogeosciences 121, 621–649 (2016)], with implications for lake carbon cycling and energy budgets. Our study provides spatially explicit information linking climate to pan-Arctic lake color changes, a finding that will help target future ecological monitoring in remote yet rapidly changing regions.
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Otley, Helen M., Sarah A. Munks, and Mark A. Hindell. "Activity patterns, movements and burrows of platypuses (Ornithorhynchus anatinus) in a sub-alpine Tasmanian lake." Australian Journal of Zoology 48, no. 6 (2000): 701. http://dx.doi.org/10.1071/zo99010.

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Adult male and female platypuses were radio-tracked in summer and winter at Lake Lea, north-western Tasmania. They appeared to exhibit greater diurnality, particularly during winter months, a greater degree of overland movement and more frequent use of non-earth refuge sites than do animals inhabiting mainland water bodies. Individuals foraged continuously for up to 16 h, with longer foraging bouts observed during the winter tracking period. Foraging range varied between 2 and 58 ha, with no significant differences observed between the sexes or seasons. All platypuses foraged predominantly in the lake; however, a number of animals were observed moving overland to and from waterbodies and burrows. Burrows were located on lake, creek and pool edges. A high percentage of burrows (25%) were located within dense sedge tussocks and scrub vegetation. Both the terrestrial activity and more opportunistic burrow-site selection may be related to reduced predation pressure in Tasmania.
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DELAFOSSE, PETER H. "West from Salt Lake City: Diaries from the Central Overland Trail." Utah Historical Quarterly 81, no. 1 (January 1, 2013): 92–93. http://dx.doi.org/10.2307/45063394.

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Li, Leilei, Jintao Yang, and Jin Wu. "A Method of Watershed Delineation for Flat Terrain Using Sentinel-2A Imagery and DEM: A Case Study of the Taihu Basin." ISPRS International Journal of Geo-Information 8, no. 12 (November 26, 2019): 528. http://dx.doi.org/10.3390/ijgi8120528.

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Accurate watershed delineation is a precondition for runoff and water quality simulation. Traditional digital elevation model (DEM) may not generate realistic drainage networks due to large depressions and subtle elevation differences in local-scale plains. In this study, we propose a new method for solving the problem of watershed delineation, using the Taihu Basin as a case study. Rivers, lakes, and reservoirs were obtained from Sentinel-2A images with the Canny algorithm on Google Earth Engine (GEE), rather than from DEM, to compose the drainage network. Catchments were delineated by modifying the flow direction of rivers, lakes, reservoirs, and overland flow, instead of using DEM values. A watershed was divided into the following three types: Lake, reservoir, and overland catchment. A total of 2291 river segments, seven lakes, eight reservoirs, and 2306 subwatersheds were retained in this study. Compared with results from HydroSHEDS and Arc Hydro, the proposed method retains crisscross structures in the topology and prevented erroneous streamlines in large lakes. High-resolution Sentinel-2A images available on the GEE have relatively greater merits than DEMs for precisely representing drainage networks and catchments, especially in the plains area. Because of the higher accuracy, this method can be used as a new solution for watershed division in the plains area.
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Maftei, Carmen, Constantin Buta, and Ionela Carazeanu Popovici. "The Impact of Human Interventions and Changes in Climate on the Hydro-Chemical Composition of Techirghiol Lake (Romania)." Water 12, no. 8 (August 12, 2020): 2261. http://dx.doi.org/10.3390/w12082261.

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The aim of this study is to establish the potential effect of changes in climate and anthropic interventions made over time on the hydro-chemical properties of the Techirghiol Lake. Located in the littoral region of the Black Sea, Techirghiol Lake is the most hypersaline lake of Romania—well-known for the therapeutic properties of the saline water and sapropelic mud. Long-term time series of salinity and water level were investigated in relation to the lake water inputs (precipitation, overland flow and groundwater), to chemical parameters (pH, DO and BOD5) and also to the hydraulic works designed and built in the region. The obtained results reveal a degradation of this ecosystem in the period of 1970–1998, when the extensive irrigation practice in the proximity of the lake had a negative effect on the water budget of Techirghiol Lake (an increased freshwater input through runoff and seepage), followed by a major decrease of the lake’s salinity.
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Curry, B. Brandon. "Paleochemistry of Lakes Agassiz and Manitoba based on ostracodes." Canadian Journal of Earth Sciences 34, no. 5 (May 1, 1997): 699–708. http://dx.doi.org/10.1139/e17-056.

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The ionic composition and salinity of Lake Manitoba and its late-glacial precursor, Lake Agassiz, changed significantly over the past 11 000 years. The paleochemical record reported here is based on modern analog environments of ostracodes identified in a new 14.5 m core from southern Lake Manitoba. The ionic composition of Lake Manitoba today is dominated by Na+, Cl−, and HC03−, with much less Ca2+, Mg2+, and K+. Evaporative concentration of modern Lake Manitoba water would lead to greater salinity and the near depletion of Ca2+ due to continued precipitation of calcite. During periods of highest salinity in the Holocene, however, Lake Manitoba supported Limnocythere staplini. Today this species inhabits waters in which [Ca2+] > [HCO3−], including springs associated with groundwater in Paleozoic bedrock discharging into Lake Winnipegosis (and eventually, after much dilution, into Lake Manitoba). Further complicating the Holocene record are intervals containing Limnocythere friabilis that suggest periodic influxes of dilute water, probably from the Assiniboine River, which bypasses Lake Manitoba today. The variations in Holocene paleochemistry indicated by the ostracode record imply changes in the proportion of overland flow plus precipitation relative to groundwater inputs to Lake Manitoba, independent of changes in evaporation relative to precipitation.
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Marston, Richard. "Changes in Geomorphic Processes in the Snake River Following Impoundment of Jackson Lake and Potential Changes Due to 1988 Fires in the Watershed." UW National Parks Service Research Station Annual Reports 15 (January 1, 1991): 152–54. http://dx.doi.org/10.13001/uwnpsrc.1991.3003.

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The purpose of this three-year study is to describe, explain and predict changes in the geomorphology of the Snake River (from Jackson Lake Dam to Moose) and related changes in riparian vegetation due to Jackson Lake Dam and 1988 fires in the watershed. Specific objectives are to determine changes over time and space in: 1) sediment mobilization on hillslopes from rainsplash and overland flow; 2) sediment delivery to streams from slope failures; 3) equilibrium condition and relative stability of the Snake River; and 4) extent of various riparian vegetation communities in the Snake River floodplain.
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Dissertations / Theses on the topic "Overland Lake"

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Krueger, Sarah E. "Cooperative Overlap, Gender, and Identity in Late Night Talk Show Interviews." Case Western Reserve University School of Graduate Studies / OhioLINK, 2019. http://rave.ohiolink.edu/etdc/view?acc_num=case1554483565830578.

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Whittaker, Clare C. Weickert. "Enclosed Elk and Bison in Land Between The Lakes, Kentucky: Dietary Overlap." OpenSIUC, 2011. https://opensiuc.lib.siu.edu/theses/626.

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I evaluated the potential for interspecific competition for forage between elk (Cervus elaphus) and bison (Bison bison) in the 265.5-ha Elk & Bison Prairie enclosure at Land Between The Lakes National Recreation Area in western Kentucky. I studied diet composition of elk and bison based on microhistological analysis of fecal samples collected monthly for 36 months from September 1996 through August 1999. Elk diet was more variable than that of bison, but no significant seasonal differences in diet composition were found for either species throughout the study. As expected, elk and bison differed significantly in their feeding habits. As seen in studies of wild sympatric populations, bison consumed more graminoids, less browse and fewer forbs than did elk, regardless of season. Dietary overlap varied considerably, but with little apparent seasonal pattern. Overlap did not consistently increase during winter, when quantity and quality of available forage might be reduced. Competition between elk and bison for available forage may have been alleviated by supplemental feeding and the ability of elk to adapt to alternative forages.
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Vaghani, Vimalkumar. "Flood Impact Analysis using GIS : A case study for Lake Roxen and Lake Glan - Sweden." Thesis, Linköping University, Department of Computer and Information Science, 2005. http://urn.kb.se/resolve?urn=urn:nbn:se:liu:diva-4206.

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Floods are common natural disaster occurring in most parts of the world. This results in damage to human life and deterioration of environment. There have been immense uses of technology to mitigate measures of flood disaster i.e. structurally and non-structurally. Undoubtedly, structural measures are very expensive and time consuming which involves physical work like construction of dams, reservoirs, bridges, channel improvement, river diversion and other embankments to keep floods away from people. Whereas non-structural measures is concerned with planning like flood forecasting and warning, flood plain zoning, relief and rehabilitation for reducing the risk of flood damage to keep people away from floods. Thus, non-structural measures involve analysis, planning providing spatial information on maps with high accuracy in less time. Non-structural measures can help decision maker to plan an effective emergency response towards flood disaster. A one of the good way to plan non-structural measures is to analyze impact of flood in the flood prone areas. The thesis tries to analyze impact of flood on environment along the demarcated flood prone areas of Lake Roxen and Lake Glan in Östergötland County, Sweden. The thesis also proposes how to use current flood information during flood emergency utilizing geographical information system. This provides spatial information for area in the flood zone for assessment regarding flood vulnerability.

Using map overlay analysis in GIS software (ArcGIS); flood prone areas and topographic data along Lake Roxen and Lake Glan were digitized from PDF maps. Thus, the thesis work is an effort to analyze impact of flood when areas along Lake Roxen and Lake Glan are flooded. ESRI® GIS software Arc Map 9 and Arc View 3.3 is used for data preparation, integrating, analyzing, and spatial data with attribute table information. Finally, to show GIS can be an effective tool for development of flood emergency system as a part of disaster preparedness by the decision makers.

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Lane, Rachel Clare. "The mediating effect of locus of control between role overload, job satisfaction and turnover intention / Rachel Clare Lane." Thesis, North-West University, 2007. http://hdl.handle.net/10394/1653.

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Marschner, Caroline A. "ANALYSIS OF DIETARY OVERLAP BETWEEN YELLOW PERCH (PERCA FLAVESCENS) AND ROUND GOBY (NEOGOBIUS MELANOSTOMUS) IN WESTERN LAKE ERIE THROUGH GUT AND STABLE ISOTOPE ANALYSES." Miami University / OhioLINK, 2003. http://rave.ohiolink.edu/etdc/view?acc_num=miami1069365415.

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Fang, Fang. "Gain-of-function mutations in SCN5A gene lead to type-3 long QT syndrome." Cleveland State University / OhioLINK, 2012. http://rave.ohiolink.edu/etdc/view?acc_num=csu1354056382.

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Carvalho, Cristiane. "Decomposição de Potamogeton pectinatus e Chara zeylanica: estrutura de habitat e sobreposição espacial na colonização por invertebrados." reponame:Repositório Institucional da FURG, 2013. http://repositorio.furg.br/handle/1/6106.

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Em lagos as macrófitas aquáticas são importantes fontes de matéria orgânica detrital, aumentam a complexidade do hábitat proporcionando vários nichos ecológicos a uma diversidade de espécies animais. Durante do processo de decomposição, a colonização dos detritos passa por uma sucessão ecológica entre fungos, bactérias e invertebrados, sendo seu papel fundamental para promover a circulação dos nutrientes. Assim, essa dissertação objetivou: (1) analisar os coeficientes de decomposição e a composição química dos detritos de duas macrófitas, a fim de verificar os efeitos dessas características sobre a biomassa fúngica e invertebrados; (2) analisar se o local de incubação das bolsas dos detritos influencia o recurso de hábitat e sobreposição espacial, interferindo na estrutura funcional da comunidade colonizadora. Para tanto foram realizados dois experimentos. Para o experimento 1 (setembro à dezembro de 2011), incubamos 24 bolsas de Potamogeton pectinatus e 24 de Chara zeylanica e retiradas em 1, 7, 20, 40, 60 e 80 dias. O material foi lavado, seco e triturado para análises químicas e determinação dos coeficientes de decomposição. A biomassa fúngica foi avaliada através do conteúdo de ergosterol. Para o experimento 2 (janeiro de 2012), foram incubadas 60 bolsas aleatoriamente divididas em 4 tratamentos, onde 15 bolsas contendo detritos de P. pectinatus foram incubadas em meio ao próprio estande (PP); 15 bolsas no estande de C. zeylanica (PC); 15 bolsas com detritos de C. zeylanica (CC) incubadas em meio ao seu estande e 15 no estande de P. pectinatus (CP), sendo retiradas em 5, 10 e 20 dias. Em ambos os estudos, os invertebrados foram classificados em grupos tróficos funcionais e determinadas a riqueza e abundância. As características químicas explicaram 59% da variação na abundância de invertebrados. A biomassa fúngica nos detritos não diferiu. A maior abundância e riqueza de invertebrados ocorreram nos detritos de P. pectinatus para o experimento 1 e nos detritos incubados em meio ao seu próprio estande (experimento 2). Houve diferença na perda de massa entre os tratamentos e entre detritos. A maior abundância na composição funcional foi de coletores - catadores e predadores, em ambos os estudos. Houve menor sobreposição espacial entre os grupos tróficos nos tratamentos em relação a PP. Nosso estudo demonstrou que os as características químicas e os coeficientes de decomposição interferem na colonização de invertebrados, relacionado ao tempo de incubação dos detritos. Além disso, o local de incubação afetou os coeficientes de decomposição e a estruturação da comunidade de invertebrados, relacionado à disponibilidade de hábitat oferecido pelos tratamentos.
In lakes the macrophytes are important sources of detrital organic matter, increase the complexity of providing various habitat niches to a variety of animal species. During the colonization process of decomposition of the waste undergoes an ecological succession among fungi, bacteria and invertebrates, and its key role in promoting the circulation of nutrients. Thus, this thesis aimed to: (1) analyze the decomposition rates and chemical composition of the detritus of two macrophytes in order to verify the effects of these characteristics on the fungal biomass and invertebrates, (2) examine if the site of the bags of incubation detritus influences the use and habitat overlap of space, affecting the functional structure of the settler community. Therefore, we performed two experiments. For experiment 1 (September to December, 2011), incubated 24 bags of Potamogeton pectinatus and 24 Chara zeylanica and withdrawn at 1, 7, 20, 40, 60 and 80 days. The material was washed, dried and ground for chemical analyzes and determination of the coefficients of decomposition. The fungal biomass was evaluated through the content of ergosterol. For experiment 2 (January, 2012), 60 bags were incubated randomly assigned to 4 treatments, where 15 bags of debris containing P. pectinatus were incubated in medium to own booth (PP); 15 scholarships in booth C. zeylanica (PC), 15 bags of detritus C. zeylanica (CC) incubated in the midst of its stand and 15 at the P. pectinatus (CP) and taken in 5, 10 and 20 days. In both studies, the invertebrates were classified into functional trophic groups and certain richness and abundance. The chemical characteristics explained 59% of variation in abundance of invertebrates. The fungal biomass in waste did not differ. The greatest abundance and diversity of invertebrates occurred in the debris of P. pectinatus for experiment 1 and incubated debris amidst its own booth (experiment 2). Was no difference in weight loss between treatments and among detritus. The highest abundance was in the functional composition of collectors - scavengers and predators, in both studies. There was a lower spatial overlap between trophic groups in treatments against PP. Our study demonstrated that the chemical characteristics and the coefficients of decomposition interfere with colonization of invertebrates, related to incubation time of detritus. Furthermore, the location of incubation affected the decomposition rates and invertebrate community structure, related to the availability of habitat offered by the treatments.
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Beck, Martina. "Feeding and Habitat Preferences of Non-Native Smallmouth Bass (Micropterus dolomieui) in Lakes Throughout British Columbia." Thesis, 2013. http://hdl.handle.net/1828/4752.

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Characterization of smallmouth bass (Micropterus dolomieu) interaction with native species assemblages, especially salmonids, in lakes throughout BC is prerequisite to identification of high-risk systems warranting on-going monitoring. Therefore this project addresses the following issues: How does smallmouth bass (SMB) trophic profile overlap with native species and does it vary across time and space? Schoener’s index of dietary overlap was not significant between SMB and rainbow trout (Oncorhynchus mykiss; α=0.406, 0.257), or cutthroat trout (Oncorhynchus clarkia; α=0.145, 0.29). Prey fish levels (Ei =35.4%) and the total energetic density (14.91±4.74J/g) of the cutthroat trout diet from Weston Lake (SMB free) were significantly higher compared to the diet of cutthroat trout from Cusheon Lake (Ei =3.3% and 7.69±1.93J/g) where non-native SMB have been introduced. Within the Vancouver Island study lakes, gut-content analysis revealed available signal crayfish serve as an important prey resource in the SMB diet (Ei =34%). What capacity do SMB have to take advantage of seasonal pulses of forage? SMB displayed the ability to rapidly (within 24hrs.) alter their diet and consumption levels (4.7 times higher) to maximize on pulses of rainbow trout fry following a stocking event. SMB did not spatially overlap with spring peaks in salmonid fry runs in the Okanagan lakes, as water temperature remained around the 10°C threshold when SMB are not yet active. Kokanee (Oncorhynchus nerka) fry did however make up Ei =83% of the yellow perch (Perca flavescens) diet. SMB are thriving in locations suspected to be on the limit for their environmental suitability through increased size at age for SMB in the Cariboo region in order to adapt to a longer (by 62 days) winter starvation period. SMB are a generalist predator able to adapt and thrive in very different systems; high vs. low productivity, few or many fish species, crayfish or no crayfish. The likely impacts of this in BC could include shifts in the diet of other fish species and increased costs associated with only stocking larger catchable sized trout in lakes containing non-native SMB. Policy recommendations based on our findings are that SMB introductions into systems that have rainbow/cutthroat trout are likely to cause the highest impacts on our native fisheries in BC if the systems are; highly productive, contain a high diversity of small bodied fish and invertebrate species, lack signal crayfish and large lakes with predominant littoral zones and complex shorelines.
Graduate
0793
0329
0792
mbeck@uvic.ca
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9

Müllerová, Světlana. "Vztahy mezi staroseverskými adjektivními výpůjčkami a jejich staroanglickými protějšky ve střední angličtině." Master's thesis, 2020. http://www.nusl.cz/ntk/nusl-436595.

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CHARLES UNIVERSITY - FACULTY OF ARTS DEPARTMENT OF ENGLISH LANGUAGE AND ELT METHODOLOGY Relationships between the borrowed Old Norse adjectives in English and their Old English counterparts MA THESIS Supervisor: prof. PhDr. Jan Čermák, CSc. Author: Světlana Müllerová Abstract: The aim of this MA thesis is to examine the relationship between six word pairs, each comprising an Old Norse adjectival borrowing in Middle English and its Old English counterpart along with its Middle English reflex for further reference. The inquiry into their relationship involves an analysis of: their (i) formal aspects, (ii) syntactic properties, (iii) semantic fields and (iv) external factors possibly contributing to their obsolescence or survival, such as the restriction to certain text types or geographic localization, as suggested by the individual linguistic profiles in the Linguistic Atlas of Early Middle English and Linguistic Atlas of Late Mediaeval English. The description of individual semantic fields of the given words is based on their semantic classification within the Historical Thesaurus of English. This analysis is based on the occurrences of the individual words as taken from the dictionaries Middle English Dictionary and Dictionary of Old English, and related corpora Dictionary of Old English Corpus and...
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Books on the topic "Overland Lake"

1

West from Salt Lake: Diaries from the central overland trail. Norman, Okla: Arthur H. Clark Co., 2012.

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The trail: A bibliography of the travelers on the overland trail to California, Oregon, Salt Lake City, and Montana during the years 1841-1864. Albuquerque: University of New Mexico Press, 1987.

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O'Brien, Mary Barmeyer. Across Death Valley: The pioneer journey of Juliet Wells Brier : a novel. Guilford, Conn: TwoDot, 2009.

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Hafen, Le Roy Reuben, 1893- and Hafen Ann W. 1893-1970, eds. Journals of Forty-niners: Salt Lake to Los Angeles : with diaries and contemporary records of Sheldon Young, James S. Brown, Jacob Y. Stover, Charles C. Rich, Addison Pratt, Howard Egan, Henry W. Bigler, and others. Lincoln: University of Nebraska Press, 1998.

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Richard, Burton. The city of the Saints and across the Rocky Mountains to California. Niwot, Colo: University Press of Colorado, 1990.

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Uhlmeyer, Jeffrey Scott. NovaChip: SR-17, City of Soap Lake milepost 75.44 to milepost 76.15. [Olympia, Wash.]: Washington State Dept. of Transportation, 2003.

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Montana, Dept of Fish Wildlife and Parks. Environmental assessment for access road overlay and widening, shoreline stabilization, and boat sewage dump station at Flathead Lake State Park-Finley Point in Lake County. Kalispell, MT: The Dept., 1993.

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Goodell, Jotham. A winter with the Mormons: The 1852 letters of Jotham Goodell. Salt Lake City, Utah: Tanner Trust Fund, Marriott Library, University of Utah, 2001.

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Sprawson, Warwick. Hiking the Overland Track : Tasmania: Cradle Mountain-Lake St Clair National Park. Cicerone Press, 2020.

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Sprawson, Warwick. Hiking the Overland Track : Tasmania: Cradle Mountain-Lake St Clair National Park. Cicerone Press, 2020.

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Book chapters on the topic "Overland Lake"

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Childress, R. Brooks, Leon A. Bennun, and David M. Harper. "Population changes in sympatric Great and Long-tailed Cormorants (Phalacrocorax carbo and P. africanus): the effects of niche overlap or environmental change?" In Lake Naivasha, Kenya, 163–70. Dordrecht: Springer Netherlands, 2002. http://dx.doi.org/10.1007/978-94-017-2031-1_16.

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Roche, Kennedy. "Spatial overlap of a predatory copepod, Acanthocyclops robustus, and its prey in a shallow eutrophic lake." In Intrazooplankton Predation, 163–83. Dordrecht: Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-009-2067-5_16.

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Museth, Jon, Reidar Borgstrøm, and John E. Brittain. "Diet overlap between introduced European minnow (Phoxinus phoxinus) and young brown trout (Salmo trutta) in the lake, Øvre Heimdalsvatn: a result of abundant resources or forced niche overlap?" In The subalpine lake ecosystem, Øvre Heimdalsvatn, and its catchment: local and global changes over the last 50 years, 93–100. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-9388-2_9.

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Helenius, Dan. "Nordic and European Judicial Cooperation in Criminal Matters." In Ius Gentium: Comparative Perspectives on Law and Justice, 133–49. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-74851-7_8.

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AbstractJudicial cooperation in criminal matters between the Nordic states has traditionally been extensive. This cooperation has included matters of extradition, legal assistance in regard to evidence, transfer of the enforcement of punishments and transfer of criminal proceedings and criminal jurisdiction. Since the late twentieth century and the early twenty-first century, the Nordic cooperation agreements have to a rather significant degree been replaced or complemented by EU legislation. Nevertheless, the Nordic agreements continue to be of relevance in many aspects, which gives rise to a rather complicated system of interwoven legal frameworks. This contribution aims to point out legal similarities and differences as well as overlaps between these frameworks, but also to elaborate on the characteristics of the Nordic cooperation as compared to the EU regulated cooperation system. It is specifically argued that the reason for the success of the Nordic cooperation is the mutual trust that the Nordic states share. However, this trust differs somewhat from the trust that is presumed to exist also between the EU Member States.
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Agostini, Domenico, and Samuel Thrope. "On the Nature of Lakes." In The Bundahišn, 67. Oxford University Press, 2020. http://dx.doi.org/10.1093/oso/9780190879044.003.0020.

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Chapters 12 lists the principal lakes of the known world; this list overlaps in part with the list of seas in chapter 10. Some of lakes mentioned can be tentatively identified with modern bodies of water, including Lake Urumieh, Lake Sōwar, Čašma-yi Sabz in Afghanistan, Aral Sea, and Gaud-i Zira in the Sistan region.
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Schmelz, Peter J. "Popular Music, the Devil, and Aerobics." In Sonic Overload, 141–94. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780197541258.003.0006.

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This chapter advances the argument of Sonic Overload by turning to the interactions between art and popular music in Schnittke’s Symphony No. 1, Requiem (1975), Concerto Grosso No. 1 (1977), Piano Concerto (1979), Symphony no. 3 (1976–81), and Faust Cantata (Seid nüchtern und wachet, 1983), as well as several of his film scores. It considers for the first time Schnittke’s ongoing negotiations between high and low across his entire career, giving careful scrutiny to his declaration in the late 1980s that “pop culture is a good disguise for any kind of devilry.” Schnittke’s change of heart, from embracing popular music—and specifically jazz and rock—from the late 1960s through the 1970s, to expressing grave concerns about its effects a decade later, mirrored the sentiments of many. In the turbulent final years of the Soviet Union, rock supplanted poetry as the conscience of the nation yet it still inspired deep anxiety among those embracing traditional Soviet conceptions of being “cultured.” Schnittke’s apprehensions about popular music in the 1980s stemmed from its growing presence in the fragmented late-Soviet soundscape and its growing prestige among newly influential tastemakers, chief among them younger intellectuals and other cultural figures. The elevation of pop music in the USSR (as in the West) expanded a growing generational divide. Schnittke’s own rejection of popular music seems to have been instigated in part by his son, Andrey, who in the early 1980s was a member of the noted Moscow rock group Center (Tsentr), a fact overlooked by previous scholars.
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Schmelz, Peter J. "Legacies of Polystylistic Tendencies (Today, Tomorrow, Yesterday)." In Sonic Overload, 332–47. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780197541258.003.0011.

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Chapter 11 takes account of Alfred Schnittke’s posthumous reception as well as of Valentin Silvestrov’s works from the late 1980s to the present. Schnittke’s death in 1998 marked, for many, the end of an era. Yet his polystylism in both theory and practice still influences many composers in Russia today. Silvestrov has continued composing, beginning around 2000 a new style he calls the bagatelle. The chapter ends by addressing the musical and sociocultural manifestations of polystylism today in the countries of the former USSR and in the global post-Soviet diaspora. Among them are the works of Vladimir Martynov and Lera Auerbach.
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Schmelz, Peter J. "Silvestrov the Centaur and Polystylism in the 1970s." In Sonic Overload, 69–84. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780197541258.003.0004.

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Chapter 4 examines Valentin Silvestrov’s journey from avant-garde enfant terrible to neoromantic. It looks at Silvestrov’s goal of musical “unity” or “oneness” in the late 1960s and early 1970s as it developed as a specific inflection of polystylism, influenced by the theories of both Boris Asafyev and Yakov Druskin. This chapter also begins to distinguish Silvestrov’s polystylism from Schnittke’s. It concludes by positioning Silvestrov’s and Schnittke’s first polystylistic works against the reception of polystylism and collage by Soviet critics, composers, and audiences in the 1970s. Among the most potent examples came from an older composer: Dmitriy Shostakovich’s Symphony no. 15, which critics used as a testing ground for the viability of polystylism in the Soviet Union.
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Schmelz, Peter J. "Schnittke’s Path to Polystylism." In Sonic Overload, 47–68. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780197541258.003.0003.

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Chapter 3 draws on unpublished correspondence and archival documents to offer a fuller accounting of the sources and development of Alfred Schnittke’s evolving concept of polystylism in the late 1960s and early 1970s. It explores the first expressions of polystylism in his film scores for Elem Klimov and Andrey Khrzhanovsky. It also offers a close reading of Schnittke’s seminal 1971 polystylism manifesto, “Polystylistic Tendencies of Modern Music.” This analysis is based on a contextualization and comparison of all known existing sources of the essay. It considers Schnittke’s influences from the contemporary soundscape as well as the essay’s larger implications for understanding his goals for writing music, music that balanced innovation with familiar socialist realist demands for accessibility and “democratization.” It also returns to Schnittke’s Violin Sonata no. 2, “Quasi una Sonata,” further discussing it as an example of his early polystylistic practice.
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Schniedewind, William M. "The Emergence of Scribal Education in Ancient Israel." In The Finger of the Scribe, 1–22. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780190052461.003.0001.

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This chapter first sketches out the history of scholarship on scribal education. The chapter summarizes new archaeological discoveries that point to the overlap between the Late Bronze Age cuneiform scribal culture and the emergence of early alphabetic writing in Canaan/Israel. This overlap provides a vector of transmission from cuneiform to early alphabetic education. Tangible evidence of this vector of transmission is found in cuneiform school texts dating to the Late Bronze Age, which is the only time such school texts are known in the southern Levant. Thus, scribal training in cuneiform overlaps the emergence of the alphabet in the southern Levant. Parallels of the borrowing from cuneiform and development of alphabetic school curriculum can also be adduced from the Ugaritic alphabetic tradition.
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Conference papers on the topic "Overland Lake"

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Taylor, Chris. "Great Salt Lake Exploration Platform." In 2016 ACSA International Conference. ACSA Press, 2016. http://dx.doi.org/10.35483/acsa.intl.2016.28.

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The Great Salt Lake Exploration Platform is a creative machine built to foster visual and performative research within the vastly under explored situated locale of the Great Salt Lake. GLSEP is a modular, flexibly deployable craft for a small group of people to remain upon the lake for limited durations of time, make work, and not die. Given the remote severity of this landscape the qualifier is significant. Storms appear quickly and can generate ten to twelve foot waves in tight oscillation. Coupled with the water’schemical density the lake is known to literally tear boats apart. Rather than being built and powered as a boat, with need of a marina to launch and a geometry to accommodate overland travel, the GSLEP is a deployable assembly providing necessary life support and research infrastructure (shade, fresh water, food and waste storage, solar power, communications,and evacuation provisions) to researchers operating on the Great Salt Lake, akin to off planet missions with immanent dangers and very limited rescue opportunities.
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JIA, YAFEI, LINDSEY YASARER, ROBERT WELLS, MARTIN LOCKE, RICHARD LIZOTTE, and RON BINGNER. "NUMERICAL SIMULATIONS OF OVERLAND FLOW AND SOIL EROSION IN THE BEASLEY LAKE WATERSHED." In 38th IAHR World Congress. The International Association for Hydro-Environment Engineering and Research (IAHR), 2019. http://dx.doi.org/10.3850/38wc092019-1084.

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Negri, Paolo. "La difesa dei territori dell’Ossola, sul corridoio spagnolo delle Fiandre, negli ultimi decenni del secolo XVII." In FORTMED2020 - Defensive Architecture of the Mediterranean. Valencia: Universitat Politàcnica de València, 2020. http://dx.doi.org/10.4995/fortmed2020.2020.11362.

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The defense of Ossola territories, on the Spanish passageway to Flanders, in the late seventeenth centuryThe Ossola territories, in the area to the northwest of Milan, have constituted the western border most in contact with the nordic and tens-alpine world, ever since the first establishment of the Duchy of Milan. It is already known from G. Parker’s monography on the camino español that one of the common routes, which allowed overland redeployment of Spanish troops headed towards Flanders, from the Liguria region across central Europe, would go through Ossola and cross the Simplon Pass or the Gries Pass. During the turbulent historical period of the Thirty Years’ War and the following one, the changing fortunes of the Duchy of Milan in Spanish hands led to the fast and strategic conquest of Piedmontese cities (1639) and their equally rapid loss on the western border. Especially in the second half of the seventeenth century, the Franco-Savoy advance threw the Piedmontese borders into a severe crisis and the Spanish governors of Milan accordingly adopted all the military measures needed to address the issue. Fearing incursions from the north, through Romandie, Valais and Ossola, in the late seventeenth century, many field engineers among whom Beretta and Formenti, arranged the transformation of Domodossola, the outermost military stronghold only equipped with obsolete medieval walls at the time, into a “modern” rampart city (1687-1690). The engineers produced an accurate study of the territory, preserved today in the Historical Civic Archive and at the Trivulziana library in Milan in a cartographic manuscript series of all the Ossola valleys and the Swiss territory from Brig to Lake Leman.
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Fontenault, Jeremy, Tara Franey, and Matt Horn. "Assessing Potential Impacts to Waterways From Small Volume Releases Originating From Facilities or Equipment." In 2020 13th International Pipeline Conference. American Society of Mechanical Engineers, 2020. http://dx.doi.org/10.1115/ipc2020-9377.

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Abstract The pipeline industry strives for continuous improvement and reaching zero incidents. The risks associated with below grade pipelines are typically assessed in detail as part of operators’ pipeline integrity management program. However, the level of risk associated with above grade facilities and equipment is often not investigated to the same level. As part of an effort, with an anonymous pipeline operator, to refine the calculated risks associated with these facilities and valve sites, a focus was made on enhancing the consequence calculations with more accurate site-specific information. An approach was developed to assess whether smaller volume releases from these locations may impact nearby waterways following a release. The operator identified 150 sites throughout North America where releases had the potential to contaminate a waterbody. In order to confirm/disprove this potential impact to water, hypothetical releases of multiple hydrocarbon products were simulated using oil spill modeling tools to assess the potential overland and downstream transport and fates of the released products. Hypothetical release scenarios were simulated until all of the modeled oil had been released and had either adhered to the land surface, filled a depression in the land surface, and/or evaporated to the atmosphere; or when oil was predicted to enter a perennial waterbody (stream or lake). The goal was to assess the potential for each release to reach a waterbody. A single release was simulated for each site based on a historical maximum volume for a release associated with the specific equipment type (e.g. valves) that could be released over a 24-hour period. Releases were simulated using conditions selected to produce reasonable, conservative results to maximize the potential for the largest volume of oil to enter a waterbody. These conditions were based on the spring season, where rivers and streams would be under some of the highest flow conditions, intermittent streams and waterbodies would contain water feeding larger water bodies, cool air temperatures would reduce evaporative losses, and no snow cover maximize overland transport. This screening level analysis allowed for identification of each location’s potential to reach a nearby waterbody under the conservative set of conditions and assumptions. By eliminating sites where oil would not reach a waterbody, the operator was able to focus efforts on the highest consequence areas in order to complete more detailed field-level analysis. In regard to spill modeling, more detailed analyses could be conducted in the future to predict the range of possible outcomes from other types of releases and using more site-specific and season-specific data. As an example, slower releases/leak rates, enhanced evaporative losses, a range of environmental conditions, and/or losses to infiltration could be assessed to bound the range of potential impacts.
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Peris, Antonio Delgado, Jose M. Hernandez, and Eduardo Huedo. "Distributed scheduling and data sharing in late-binding overlays." In 2014 International Conference on High Performance Computing & Simulation (HPCS). IEEE, 2014. http://dx.doi.org/10.1109/hpcsim.2014.6903678.

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Colleoni Couto, Julia, Olimar Teixeira Borges, and Duncan Dubugras Ruiz. "Automatized Bioinformatics Data Integration in a Hadoop-based Data Lake." In 9th International Conference on Artificial Intelligence and Applications (AIAPP 2022). Academy and Industry Research Collaboration Center (AIRCC), 2022. http://dx.doi.org/10.5121/csit.2022.120912.

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When we work in a data lake, data integration is not easy, mainly because the data is usually stored in raw format. Manually performing data integration is a time-consuming task that requires the supervision of a specialist, which can make mistakes or not be able to see the optimal point for data integration among two or more datasets. This paper presents a model to perform heterogeneous in-memory data integration in a Hadoop-based data lake based on a top-k set similarity approach. Our main contribution is the process of ingesting, storing, processing, integrating, and visualizing the data integration points. The algorithm for data integration is based on the Overlap coefficient since it presented better results when compared with the set similarity metrics Jaccard, Sørensen-Dice, and the Tversky index. We tested our model applying it on eight bioinformatics-domain datasets. Our model presents better results when compared to an analysis of a specialist, and we expect our model can be reused for other domains of datasets.
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Wang, Zhong, Edwin H. M. Sha, and Yuke Wang. "Optimal partitioning and balanced scheduling with the maximal overlap of data footprints." In the 11th Great Lakes Symposium. New York, New York, USA: ACM Press, 2001. http://dx.doi.org/10.1145/368122.368155.

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Ajder, Vitalie, and Silvia Ursul. "The inventory of the ornitofauna of Sarata Noua lake, Leova county, Republic of Moldova from 2016 – 2021." In Xth International Conference of Zoologists. Institute of Zoology, Republic of Moldova, 2021. http://dx.doi.org/10.53937/icz10.2021.49.

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The Republic of Moldova is a small European country where long-term studies have been more of an exception than a rule. Being an agrarian country, the mosaic of natural and artificial habitats is found on a smaller scale, namely in the Sărata river meadow, and in Sărata Nouă lake and surrounding. The Sărata River is a right tributary of the Prut River in the Republic of Moldova, having a quiet plain character, with a mosaic of natural and artificial habitats which are traditionally managed. The area overlaps with the East-Elbic migration route, the short distance to the Prut River and being located in the northern part of the Bugeac steppe, ensures a great diversity both in winter and nesting, and especially in the migration period. During 2016-2021, we registered the presence of 126 bird species, which represent 46% of the total species encountered in the Republic of Moldova.
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Iskandar, Dadang, Sigit Pranowo Hadiwardoyo, Raden Jachrizal Sumabrata, and Hendra Ariyapijati. "Overlay maintenance on road heavy vehicle lane by non-destructive test method." In EXPLORING RESOURCES, PROCESS AND DESIGN FOR SUSTAINABLE URBAN DEVELOPMENT: Proceedings of the 5th International Conference on Engineering, Technology, and Industrial Application (ICETIA) 2018. AIP Publishing, 2019. http://dx.doi.org/10.1063/1.5112420.

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Torregrosa, Tess, Larry Fennigkoh, and Jordan Weston. "Fabrication of a nursing manikin overlay for simulation of chest drainage management." In 2015 IEEE Great Lakes Biomedical Conference (GLBC). IEEE, 2015. http://dx.doi.org/10.1109/glbc.2015.7158299.

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Reports on the topic "Overland Lake"

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Phan, Long T., Donald N. Slinn, and Shaun W. Kline. Introduction of wave set-up effects and mass flux to the sea, lake, and overland surges from hurricanes (slosh) model. Gaithersburg, MD: National Institute of Standards and Technology, 2010. http://dx.doi.org/10.6028/nist.ir.7689.

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DeSantis, John, and Jeffery Roesler. Longitudinal Cracking Investigation on I-72 Experimental Unbonded Concrete Overlay. Illinois Center for Transportation, February 2022. http://dx.doi.org/10.36501/0197-9191/22-002.

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A research study investigated longitudinal cracking developing along an experimental unbonded concrete overlay (UBOL) on I-72 near Riverton, Illinois. The project evaluated existing literature on UBOL (design, construction, and performance), UBOL case studies, and mechanistic-empirical design procedures for defining the mechanisms that are contributing to the observed distresses. Detailed distress surveys and coring were conducted to assess the extent of the longitudinal cracking and faulting along the longitudinal lane-shoulder joint. Coring over the transverse contraction joints in the driving lane showed stripping and erosion of the dense-graded hot-mix asphalt (HMA) interlayer was the primary mechanism initiating the longitudinal cracks. Cores from the lane-shoulder joint confirmed stripping and erosion was also occurring there and leading to the elevation difference between the driving lane and shoulder. Field sections by surrounding state departments of transportation (DOTs), such as Iowa, Michigan, Minnesota, Missouri, and Pennsylvania, with similar UBOL design features to the I-72 section were examined. Site visits were performed in Illinois, Michigan, Minnesota, and Pennsylvania, while other sections were reviewed via state DOT contacts as well as Google Earth and Maps. Evidence from other DOTs suggested that HMA interlayers, whether dense graded or drainable, could experience stripping, erosion, and instability under certain conditions. An existing performance test for interlayers, i.e., Hamburg wheel-tracking device, and current models reviewed were not able to predict the distresses on I-72 eastbound. Adapting a dynamic cylinder test is a next step to screen HMA interlayers (or other stabilized layers) for stripping and erosion potential. To slow down the cracking and faulting on I-72 eastbound, sealing of the longitudinal lane-shoulder joint and driving lane transverse joints is suggested. To maximize UBOL service life, an HMA overlay will minimize water infiltration into the interlayer system and significantly slow down the HMA stripping and erosion mechanism that has led to longitudinal cracking and lane-shoulder faulting.
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Cecile, M. P., B. S. Norford, G. S. Nowlan, and T. T. Uyeno. Lower Paleozoic stratigraphy and geology, Richardson Mountains, Yukon (with stratigraphic and paleontological appendices). Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329454.

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The Richardson Trough was a rift basin on the southern margin of an ancestral Iapetus Ocean. It was part of a complex paleogeography that included at least two major rift basins on western Franklinian and northern Cordilleran continental shelves. This paleogeography included the Ogilvie Arch, Porcupine Platform, Blackstone 'supra-basin', Babbage Basin, Husky Lakes Arch, Richardson Trough, Mackenzie Arch, Lac des Bois Platform, and the White Mountains and Campbell uplifts. The Richardson Trough was the failed arm of a triple rift system that formed when an early Paleozoic Iapetus Ocean developed north of the trough. The Richardson Trough displays a classic 'steer's head' profile with two rift fill cycles. The first features late early to middle late Cambrian rifting and late late Cambrian to late Early Ordovician post-rift subsidence; the second, late Early Ordovician to early Silurian rifting and late early Silurian to early Middle Devonian post-rift subsidence. Lower Paleozoic strata exposed in the Richardson Trough range in age from middle Cambrian to early Middle Devonian and are similar to strata in their sister rift, the Misty Creek Embayment. Before this study, the stratigraphic units defined for the Richardson Trough were the Slats Creek Formation and the Road River Formation. Here, the Slats Creek Formation and a new Road River Group are recognized. In order, this group consists of the middle and/or late Cambrian to Early Ordovician Cronin Formation; the early Early Ordovician to latest early Silurian Mount Hare Formation; the early Silurian to late Silurian Tetlit Formation; and the late Silurian to early Middle Devonian Vittrekwa Formation. These Road River Group strata are unconformably overlain by the late Middle to Late Devonian Canol Formation (outcrop) and by the Early Devonian Tatsieta Formation (subsurface).
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Kellett, D. A., and A. Zagorevski. Overlap assemblages: Laberge Group of the Whitehorse Trough, northern Canadian Cordillera. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/326064.

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The Laberge Group was deposited during the Early to Middle Jurassic in a marginal marine environment, in the northern Canadian Cordillera. It occurs as a narrow, elongated siliciclastic unit along more than 600 km of strike length, overlapping the Intermontane terranes of southern Yukon and northwestern British Columbia. The Laberge Group was deposited on the Late Triassic Stuhini and Lewes River groups, a volcano-plutonic complex of the Stikine terrane (Stikinia), and, locally, the Kutcho Arc. It is overlain by Middle Jurassic to Cretaceous clastic units. The variations in clast composition and detrital zircon populations among these units indicate major changes in depositional environment, basin extent, and sources during the latest Triassic to Middle Jurassic. Detrital zircon populations are dominated by near contemporary Stuhini-Lewes River arc grains, consistent with dissection of an active arc. Detrital rutile and muscovite data show rapid cooling and exhumation of metamorphic rocks during the Early Jurassic. Thermochronological data indicate that basin thermal evolution was domainal, with at least five regional temperature-time histories.
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Zaleski, E., R. L'Heureux, N. Duke, L. Wilkinson, and W J Davis. Komatiitic and felsic volcanic rocks overlain by quartzite, Woodburn Lake group, Meadowbank River area, western Churchill Province, Northwest Territories (Nunavut). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210167.

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Turner, E. C. Mesoproterozoic Borden Basin, northern Baffin Island. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/321825.

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The unmetamorphosed and nearly undeformed late Mesoproterozoic Borden Basin on northern Baffin Island exhibits sag, rift, and foreland-basin-like phases. A thin, partly subaqueous basal basalt is overlain by mature shallow-marine quartz arenite, upward-deepening siltstone and shale (marking the beginning of rifting), a complex suite of rift-delineated carbonate units containing two dramatic internal unconformities, and a flysch-molasse-like succession containing evidence of sediment derivation from the Grenville Orogen. Geochronological data indicate that deposition of most of the succession took place ca. 1100 to 1050 Ma. One of the carbonate intervals, Nanisivik Formation, is the main host of regional Zn-Pb showings including the past-producing Nanisivik orebody, which formed in the late Mesoproterozoic from low-temperature fluids, and which was emplaced under strong structural and stratigraphic controls. Minimal postdepositional deformation is limited to the emplacement of mafic dykes ca. 720 Ma and repeated reactivation of basement-rooted normal faults.
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Bleeker, W. The ca. 2680 Ma Raquette Lake Formation and correlative units across the Slave Province, Northwest Territories: evidence for a craton-scale overlap sequence. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/212072.

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Midwinter, D., T. Hadlari, and K. Dewing. Upper Triassic to Lower Jurassic stratigraphy along the northeastern margin of the Sverdrup Basin, Axel Heiberg and Ellesmere islands, Nunavut: new data from measured sections. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329398.

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Two stratigraphic sections were measured through Late Triassic - Early Jurassic aged strata in the Blue Mountains map area (NTS 340-B/11) on Ellesmere Island and the Depot Point map area (NTS 049-G/7) on Axel Heiberg Island. These sections are subdivided in terms of established member and formation names based on previous mapping along the north-eastern margin of the Sverdrup Basin. The lowermost strata in the Heiberg Formation, the Romulus Member (510-575 m thick), is a coarsening-upward succession of mudstone to fine-grained sandstone from a prodelta to delta plain environment. The overlying Fosheim Member (317-425 m) is a coal-bearing and sandstone-rich interval from a mixed alluvial-marine environment, such as a delta plain. It is overlain by the Remus Member (100-112 m); a sandstone-rich unit representative of shallow marine deposits. The Heiberg Formation at Depot Point is of similar thickness (1009 m) to the Blue Mountains (1035 m) and may represent a marginally more distal basinal setting with a thinner Fosheim Member but a slightly thicker Romulus and Remus members.
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Chen, Stanley, Yaobin Chen, Renran Tian, Lingxi Li, Donglin Liu, Jue Zhou, and Dan Shen. Alternate Interchange Signing Study for Indiana Highways. Purdue University, 2022. http://dx.doi.org/10.5703/1288284317439.

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The main objectives of this research were to (1) understand signing issues from the perspective of drivers and (2) develop recommendations for improving interchange signing in Indiana to aid driver understanding and increase the safety and efficiency of highway traffic operations. An online survey with specific questions was designed and distributed through email, social media, online newspapers, and a survey company with the goal of better understanding driver thinking when approaching decision-making areas on the interstate. The analysis of the survey results revealed the following. •Drivers usually do not know the interchange types as they approach an interchange on the freeway. •Drivers are most interested in which lanes they should be in when approaching an interchange, even in advance of typical signing locations. •Drivers do not like signs that require cognitive work since it will delay their driving decision by creating uncertainty. •Different drivers need different types of information from signs, such as cardinal direction, destination name, road name, and lane assignments. Therefore, a perfect sign for one driver may be confusing or information overload for another driver. •In some instances, a driver who is familiar with the area is confused by the signs because the sign information contradicts the driver’s knowledge.
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Kontak, D. J., S. Paradis, Z. Waller, and M. Fayek. Petrographic, fluid inclusion, and secondary ion mass spectrometry stable isotopic (O, S) study of Mississippi Valley-type mineralization in British Columbia and Alberta. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/327994.

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Abstract:
A comprehensive study of Mississippi Valley-type base-metal deposits across the Canadian Cordillera was done to compare and contrast their features. Extensive dissolution of host rocks is followed by multiple generations of dolomite cements from early, low-temperature, fine-grained to coarser, higher temperature types that overlap with Zn-Pb sulfide minerals; late-stage calcite occludes residual porosity. Dolomite is generally chemically stoichiometric, but ore-stage types are often rich in Fe (<1.3 weight per cent FeO) with small sphalerite inclusions. Sphalerite-hosted fluid inclusions record ranges for homogenization temperatures (77-214°C) and fluid salinity (1-28 weight per cent equiv. NaCl±CaCl2). These data suggest fluid mixing with no single fluid type related to all sulfide mineralization. In situ secondary ion mass spectrometry (SIMS) generated delta-18OVSMOW values for carbonate minerals (13-33 permille) reflect dolomite and calcite formation involving several fluids (seawater, basinal, meteoric) over a large temperature range at varying fluid-rock ratios. Sphalerite and pyrite SIMS delta-34SVCDT values vary (8-33 permille) but in single settings have small ranges (<2-3 permille) that suggest sulfur was reduced via thermochemical sulfate reduction from homogeneous sulfur reservoirs. Collectively, the data implicate several fluids in the mineralizing process and suggest mixing of a sulfur-poor, metal-bearing fluid with a metal-poor, sulfide-bearing fluid.
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