Public Personnel Administration And Collective Bargaining

Public Personnel Administration and Collective Bargaining. In chapter five, the author retrospectively revises the roots of the various reforms applied to managing human capital in the public sector. Since 1789 there have been three comprehensive periods that divide the progress of personnel practice in the United States. 1- The era of the â€Å"gentlemen† that occurred from 1789 until 1828. This era began with President Washington’s first administration and ended with the appointment of President Jackson in 1829. President Washington understood that his administration would be setting the standards in all aspects of public sector administration, therefore he focused on giving administrative roles to those who he considered of great character. Even when these appointees had little political experience. These selected candidates were usually upper class, their character and integrity made them models for others and even with little expertise in public administrative roles, they proved to be fast learners and talented. President Washington learned as time went by, that skills and integrity were not enough, so he started to look for political loyalty among the candidate’s characteristics. In 1801 during his administration, President Jefferson sought to appoint political roles equita bly to create a balance between Republicans and federalists. 2- The â€Å"spoiler system† was institutionalized by President Jackson and went from 1829 until 1882. President Jackson articulated uponShow MoreRelatedLabor And The Collective Bargaining Process978 Words   |  4 Pagesactors who are generally involved in the collective bargaining process are Management but more specifically, the owners and shareholders, executives and managers and the industrial and human resource people. 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Premarital Sex A Morally Issue Free Essays

Pre-marital sex, young Catholics know it is wrong. So why do they do it? Most teenagers have heard or coined the phrases â€Å"everyone†s doing it.† â€Å"If you loved me you†d do it† and also â€Å"It†s okay I have a condom. We will write a custom essay sample on Premarital Sex: A Morally Issue or any similar topic only for you Order Now † Sex before marriage can be harmful to your body, your future, but the scariest of all your eternity. In this paper we shall look more into the Catholic point of view on pre-marital bliss. The purpose of sex is to unite a married couple as one loving body in consummating a marriage, to leave the possibility of procreation open, and to and to educate a child. The purpose of sex is to unite a married couple as one loving body. This is because God†s intention in creating the first man and woman was for them to love and create more men and women. To do so a married couple must join as one loving body or to have sexual intercourse. In having intercourse the first time in a marriage you are consummating the marriage therefore making the marriage official in the eyes of God. The Catechism of the Catholic Church says: â€Å"the union of man and woman in marriage is a way of imitating the flesh in the creators generosity and fecundity: ‘Therefore . . . and they become one flesh† (Gen4:24) All human generations proceed from this union† (Catechism 2335). Sex is meant for mature individuals who are prepared to face the consequences of sex. Two of the biggest fears in premarital sex are STDs (sexually transmitted diseases) and unwanted pregnancy. A married individual normally does not have to deal with such problems. This is because at the average age of marriage most STDs are not common. Second, in a marriage a couple normally wants a child to care for. However, teenagers do not want these responsibilities. Which leads to common use of contraceptives in teen sex. Sex is meant to leave an opening for procreation. Contraceptives are commonly used in premarital sex. These are used to prevent unwanted pregnancy and STDs. How can one use a condom and leave an opening for a child to be conceived? The Bible says â€Å"God blessed man and woman with the words: ‘Be fruitful and multiply†Ã¢â‚¬  (GS 50). Condom, the most popular choice for a contraceptive, is a latex cover for the male phallus, which prevents the sperm from entering the vagina and making it†s way to the egg. In humans sexual reproduction is done through intercourse. When the sperm meets the egg. When a condom does fail there is a high risk of catching a STD or having an unwanted pregnancy. In the chance of a pregnancy there are alternatives such as raising the child on your own, giving it up for abortion, and the sinful way out, having an abortion. Abortion is a mortal sin because it is the death of an unborn child. The Catechism of the Catholic Church states: â€Å"By its very nature the institution of marriage and married love is ordered to the procreation and education of the offspring and is in them that it finds their crowning glory† (1652, 460). Raising a child on your own is not impossible however it is not easy. Finally, Sex is meant to aid in educating a child. Without sex there is no child. In the cases of teen-parents, it is not probable that the child will grow up with the proper education. This is most probable because the teens themselves are still learning. In the instances of single parent parenting, the education can be very tedious. It would be tedious because the single parent would have to play the role of the mother and the father as well. Such examples prove that sex inside of marriage is the simplest choice. One would not have as many issues to face and will be able to raise a family almost problem free. In parenting there will naturally be problems too, however when an adult is there to help their children they have the personal experience and moral guidance needed to lead the offspring off on the right foot. The Catechism of the Catholic Church states: † Parents are the principle and first educators of their children. In this sense the fundamental task of marriage and family is to be at the service of life† (1653, 461). When your child comes to you and tell you that their boy/girlfriend is pressuring them for sex you can be able to tell them to abstain. â€Å"Abstinence is the only safe and morally correct form of contraception†. In conclusion, sex is meant to unite a married couple as one loving body in consummating a marriage, to leave the possibility of procreation open and to and to educate a child. The previous information has shown sex to only be moral and truly worry free in a marriage. â€Å"Let the Hebrews marry, at the age fit for it, virgins that are free, and born of good parents. But if the damsel be convicted, as having been corrupted, and is one of the common people, let her be stoned, because she did not preserve her virginity till she were lawfully married; but if she were the daughter of a priest let her be burnt alive† (Pastor David, Virginity/Marriage, 1) How to cite Premarital Sex: A Morally Issue, Papers

Petroleum Potential of the Dutch North Sea (L15 Block)

Question: Describe the Petroleum Geology and Basin Analysis? Answer: 1. Abstract Here in this report the study is made on the petroleum drilling in the Dutch North Sea area and the drilling engineering is understood in this report. The report is mainly based on understanding the petroleum potential structure in the North Basin area. It has been found that the petroleum extracted from the North Sea area is facing price rise due to the advance technology introduced in the area. To understand the issue it is important to understand the entire structure or mechanism of drilling of petroleum. The entire report deals with that. Here in this report the geological setting of petroleum system in the North Sea basin is discussed, the tectonical structure and the stratigraphy structure of the basin is discussed. Further the study is made on the burial and thermal history of the basin. Then the discussion is done and the detailed study is presented on the petroleum potential structure of the North Sea Basin. The source rocks, reservoirs and the seals and traps are studied in this report. After all this studies a conclusion is drawn that represent the summary of the report and the detailed study made in this report. 2. Introduction The North Sea Basin spreads and region of 625,000 km2 and is lies north of the Netherlands and in the middle of Norway and Great Britain. In the north it is limited by the mainland rack edge. It is a geological low and can be partitioned into a few sub-bowls (A healthy North Sea ecosystem and a healthy North Sea fishery: two sides of the same regulation, 1994). The region has a dynamic tectonic history and statement has shifted between the diverse bowls. In this study the center will be on structural improvement and the stratigraphy from the Silesian (125 Ma) until later. A connection to the depositional history and the paleo environment will be made. This is carried out to have the capacity to show conceivable source shakes, repositories and seals for oil creation, the primary industry of the locale (Mayer-GuÃÅ'ˆrr, 1976). 2.1 Geologic Setting The present North Sea Basin, lies between three jumping massifs: the Norwegian Caledonides, the London Brabant Massif and the topographic high of Great Britain. The Norwegian Caledonides have been a topographic high since the Carboniferous, while the other two massifs were inspired above ocean level amid the Early Tertiary. The depositional setting for the late Pliocene to Pleistocene chilly and glaciomarine progression in the region is acquired from a long topographical history that influenced the basinal range and the dregs source zone. Tectonic action that created the present structural make up can be followed back to Permian and Carboniferous times (Mead, 2012). Three fundamental cracking stages happened amid Carboniferous to Permian, late Mid Jurassic to Early Cretaceous and late cretaceous to Early Eocene times. Albeit extensional tectonics in the North Sea and in contiguous areas of the North Sea started as ahead of schedule as the late Carboniferous, however the mainland divi sion in the middle of Greenland and Norway was launched first after the late Paleocene (A North Sea School of Architecture?: Nidaros Cathedral's Romanesque Transepts and North Sea Medieval Architecture, 2012). The Early Permian-Triassic breaking in the North Sea region is ineffectively compelled. Amid Jurassicearly Cretaceous, the North Sea locale endured huge breaking. This fracturing finished in the soonest Cretaceous and moved to the More, Voring and FaroeShetland bowls. After this period, the North Sea Basin thermally subsided and was loaded with silt sourced from the encompassing landmasses, intruded on intermittently by bowl reversal. Crustal augmentation stayed amid Late Paleozoic in the mainland outside layer fragment in the middle of Norway and Greenland, and proceeded in a few cracking scenes amid the Mesozoic. Crustal augmentation influenced external parts of the More and Voring bowls amid Late Cretaceous Paleocene, which later on moved towards the focal piece of the bowl s with the progression of the passage of time (North Sea oil: Women not at sea, 1985). 2.1.1 Tectonic history; how the basin formed 1. Caledonian geosynclinals stage (Cambrian-Devonian). Transformative and meddling rocks of Caledonian age structure the storm cellar unpredictable for a significant part of the North Sea region. The north-eastern limit of the Caledonian fold belt at this stage can't be characterized more nearly than as an evident pattern from the focal North Sea through northern Germany into Poland. 2. Variscan geosynclinals stage. Devonian and Carboniferous testimony transgressed from the south over the dissolved Caledonides and arrived at greatest thickness in the southern North Sea, a territory which framed piece of the Variscan fore deep (Alvarez, 1986).3. Permian-Triassic intracratonic stage. Taking after the Variscan orogeny vast parts of the North Sea were possessed by the quickly subsiding intracratonic Northern and Southern Permian bowls. These bowls contain a thick arrangement of clastic and evaporite stores.4. Cracking pathogenic stage. Advancement of the North Sea fracture framework began amid the Triassic and overwhelmed the pale geographic setting of the zone amid the Jurassic and Cretaceous (Pegrum, Rees and Naylor, 1975). The advancement of the North Sea crack is identified with the improvement of the Arctic North Atlantic break zone. The recent arrived at the phase of crustal division in the early Tertiary, at which time the North Sea break got to be idle.5. Ter tiary, post rifting phase of provincial bowl subsidence. With the end of fracturing developments in the North Sea the zone got to be liable to local subsidence prompting the advancement of a symmetrical, saucer-molded intracratonic bowl (Bottom irregularities in the North Sea, 1977). The late Tertiary Rhone-Rhine crack framework does not reach out into the North Sea and postdates the North Sea break. 2.1.2 Stratigraphy: how the basin was filled In Paleogene the Rogland Group was saved and is made out of the shallow marine shale, minimal marine sandstone and volcanic stores that are of Eocene age. The Neogene contains the Hordaland and Nordland bunches (Phelps and Lake, 1924). The lower Neogene progression speaks to the profound water sedimentation, as showed by the development of the contourite silt float over the sub marine unconformity. The upper Neogene speak to a time of provincial change that demonstrates a significant offshore move (progradation) of the mainland edge that could be because of subsidence. The building of the rack slant shows increment in silt supply because of inspire and disintegration (Reis, 1996). The Nordland Group of Early Miocene-Recent age is of prime criticalness in present study and its principle viewpoints as foundation for the present study is displayed underneath. Utsira formation: The Utsira Formation is of Middle-Late Miocene age and was stored in the northern North Sea range, predominantly inside the Norwegian segment, between the Jaeren High and the Tampen Spur. This arrangement demonstrates a complex depositional structural engineering which fluctuates with scope. Around 58 N in the southern Viking Graben, the arrangement structures goliath mounded sand framework with scattered interims of mud stone. This sand hill is squeezing primarily out both eastward and westward (Bradley and Gipson, 1987). Around 59 N the Utsira Formation is portrayed by square sandstone in lower part, while the upper part demonstrates an acceptable upward coarsening pattern in well logs. In the northern Viking Graben (60- 61 N), the Utsira Formation, spoke to by a mounded sandstone body, for the most part comprises of square sandstone with subordinate mud stone interims. In its northward augmentation to Tampen zone the Utsira Formation is shown by a think unit of glauconitic sand (Roberts, 1985). The Utsira Formation is considered time proportional to the Molo arrangement. The Naust Formation: The formation is made out of sand, residue, mud and infrequently coarse grained clastic silt. The arrangement speaks to Pliocene to Pleistocene strata on the Norwegian mainland rack. The Naust Formation is circulated everywhere throughout the Mid- Norwegian mainland rack. The arrangement is involved a westward ace reviewing thick progression of Plio-Pleistocene strata on the rack and comprises of a few unintelligible seismic units of till, glaciogenic flotsam and jetsam and slide stores (Russell and Bijaksana, 2012). The cold seismic units of the Naust Formation are bury stratified with entomb frosty stores. The Naust Formation down laps onto the Kai Formation and is in the eastward course limited beneath by the Molo Formation. A few ages have been appointed to the base of the Naust Formation, yet the age that has been most broadly utilized is 2.7 to 2.8 (Ma). This age has been allocated on the premise of the bio stratigraphic information related with the remote ocean boring centres (Brouwer and Shawcross, 1964). 3. Petroleum element within the basin The historical source of rocks is very important and litho logic character that attracts the eyes of the researchers in this field (The North Sea., 1976). The source rocks brings the definition of the petroleum system present in the North Sea Basin that includes several different basins that together makes the worlds most important petroleum source that provides supply of power generation to the entire globe. The petroleum system in the North Sea Basin includes the Moray Firth Ground, Viking Graben and the Central Graben. The petroleum system includes the Mandal Ekofisk petroleum system which is defined and described by the Cornford in the year 1994 (Buydos, n.d.). It was decided to treat the entire system of petroleum in the North Sea Basin as a single petroleum system because to make it simple and through the detailed study of the source rocks and hydrocarbons relationship, it was found that the properties of the entire system was almost same. Hence, it was decided to treat the ent ire system as a single petroleum system. The analysis of the properties in the North Sea Basin is discussed in details in the following points: 3.1 Source Rocks To know what petroleum is it is important to know the source of petroleum. Petroleum is formed from the organic substances that were buried under the soil for a long period since the Jurassic age (Walton, 2011). The marine shale of the Jurassic periods is important source of petroleum throughout the world. It was found that the sea level rose which led to the burring of the marine shale under the water. The high organic productive material got buried under the land and the water depth increased during the Jurassic period. This resulted in the anoxic bottom water in the areas of bathymetric basins. This further resulted in thick accumulation of organic hydrocarbon rich shale that led to the preservation of rich organic materials in the deep basins of the North Sea. During that period the rifting reached to its maximum and the organic materials started burring under the soil. Due to the rise of the water level the soil mudstones got buried under the sea water and the source rocks of pe troleum in this area came under the sea. Later in the man period this areas were discovered and the petroleum was extracted from this area. The basin contains a huge source rocks that are still yet not converted into petroleum and will need many more years to get converted into petroleum products (Churchill, 1977). Experiments and researches were done and it was found that this area includes source rocks that were similar in nature and the properties of the source rocks were almost same. This led to declare the entire basin as a single petroleum source and it was decided to treat it as a single petroleum system. 3.2 Reservoirs The entire petroleum system in the North Sea basin is made out of same type of source rocks. This area has huge reservoirs of petroleum that has been extracted since a number of years. These reservoirs are mainly found in the sea shores and few of it is found in the land areas. The entire Petroleum system includes the reservoirs mainly in the North Sea area (Warme, Douglas and Winterer, 1981). These reservoirs are mainly distributed in the area with time and space; the diverse characteristics of the reservoirs are the result of the complex geological structure in the area. The reservoirs are grouped into three main categories that are the pre rift reservoirs of the Jurassic age, pre rift reservoirs of the middle or early age and the post rift reservoirs. These reservoirs are distributed in the North Sea basin uniformly and are used for the extraction of petroleum and gas products that are the main source of energy for the entire globe in the present day. The most of the area in the N orth Sea Basin is covered with the Pre rift reservoirs of the Jurassic period, and then stands the pre rift reservoirs of the middle age and after that stand the Post rift reservoirs. The post rift reservoirs are situated in the 57 degree North in the Basin (Coakley and Stein, 2010). Figure: Burial curves for several location in the North Sea Basin (HARKER, STUART D., Occidental Petro, 1991) Figure: Showing the approximate depth of the craterous rocks in the North Sea Basin (HARKER, STUART D., Occidental Petro, 1991) 3.3 Seals traps In the areas near the Southern part of the North Sea area the Zechstein evaporates that serves as a source of several seals and traps in the central and northern North Sea area. This seals and traps areas are the source and accumulation of the hydrocarbons that are the source of energy for the globalized world. These hydrocarbons are matched by several different varieties of seals and tarps in the area (Gautier, 2005). Gas and Oil is found in the area of the North Sea Basin in the Pre Rift reservoirs that are found to be in tilted position that has fault in the blocks where seals are formed along with fine grained and post rift sedimentary sequences that are the part of the Jurassic structure in the area. If the examples are taken the Auk and the Argyll fields can be taken in consideration which has Rotliegend and Zechstein carbon sandstone in the reservoirs where traps are sealed by uncomfortably overlying craterous rocks during the Jurassic period (Cooper and Gaskell, 1966). These are the low permeability zones that have fine grained rocks of Triassic. In the areas of the Viking Graben Traps are sealed with vertically overlying craterous and Jurassic rocks. Here the traps and seals are result from the reservoirs fault in the contact of the sandstones and the juxtaposition of the shales. In several areas seals are equivalent to the Kimmeridge clay that are temporary in nature. In the Moray Firth Ground the seals are caused because of the shallow marine that has sandstones reservoirs that provides trapping mechanisms in that area. In the Central Graben area the seal are also temporary in nature and are equivalent to the reservoirs seals in the Fulmar and Ula regions (Cubitt, England and Larter, 2004). 4. Burial and thermal history of the basin To understand the structure of the petroleum system in the North Sea area it is important to understand the history of the Burial and Thermal nature of the petroleum reservoirs in the Basin Area. It is really important because without knowing the nature of the Petroleum, the Basin cannot be differentiated form other basins in the rest of the world (Cussler and Dirgo, 1996). In this section a detailed study is made to understand the burial and thermal history of the Basin in the North Sea region. This study is done with the help of Modeling and is the result of the modeling process. The analysis is discussed in the points below: 4.1 Burial History: The burial history of the North Sea Basin is predicted in the pre inversion techno stratigraphic units. This shows a huge difference in the observation along the cross sectional observation made for the Basin area. It includes the Variscan to the early rift techno graphic units that has reached to its maximum in the depth of burial which is prior to the cretaceous syncing version period. In this area the maximum depth is not present at present day in a small area of 50km along the cross sectional area of the Basin. In the southern part of the basin the units are pre inverse in nature and are structurally high in nature in the area of P9 (Demaison and Murris, 1984). The maximum burial depth is found in the southern Basin that extends southward up to 7 km and northward up to 10-20 km. But in the northern part of the actual basin the depth at the present point that extends up to 62-78km in the region of the Traissic rocks and carboniferous rocks is max. 4.2 Thermal History: It is important to understand the temperature and heat flow history of the petroleum reserves in the Basin area. It is stimulated by assuming the transient heat that has a flow condition and takes into account the time dependence of the bottom and top boundaries condition. It has been found that zero heat flows in the flow in the lateral boundary, radiogenic heat flow in the sediments and the porosity is dependent on the heat capacities and condition of the sediments (DeNatale, Troise and Sacchi, 2007). The thermal modeling also reveals the vertical and lateral variation of the flow of heat in the sediments in the cross sectional area of the basin. The figures are shown below to make it easy to understand. Figure: a. Tectonic curve, b. Evolution of heat flow, c. Evolution of sediment water temperatures (Verweij and Simmelink, 2002) 5. Discussion The Central North Sea (CNS) has been a center of hydrocarbon investigation and generation for a considerable length of time. Indeed now the region remains a hive of movement, with an expected 5 billion barrels of oil and gas undiscovered. Late revelations in the CNS incorporate the Culzean Gas and Condensate field by Maersk Oil, and the Shaw Discovery by Marubeni and Talisman in the year 2009. In 2010 Encore published the Catcher and Catcher East revelations with assessed stores of 300 Mmboe, speaking to one of the biggest disclosures in the Central North Sea for over 10 years. Petroleum Geo-Services (PGS) has been working in the Central North Sea for almost 20 years (Distribution of Holocene silicoflagellates in North Pacific sediments, 1977). Since 2002, the organization has been conveying united 3d seismic information known as the Mega Survey, which has mapped, in both provincial and prospect level detail, 60,000km of the Central North Sea. This has now been moved up to the Mega S urvey Plus; a pre-stack consolidation of almost 17,000 km of Central North Sea seismic which, with skyline understanding and highlighted AVO irregularities, permits fast provincial screening for prospect and lead distinguishing prospect and the major identification. Figure: Petroleum Projection in North Sea Basin The Central North Sea is a center of investigation for structural, stratigraphic and mix traps. Scopes of structural traps are introduced in the CNS, extending from tilted flaw pieces to crestal droops (Echo-traces from the north-eastern Atlantic, 1977). However as investigation and improvement has advanced, critical new structural terminations are progressively uncommon. The PGS Mega Survey Plus covers various substantial scale Cretaceous droops like the gainful Centurion field, speaking to another play sort in the CNS. Stratigraphic traps are thought to hold up to 75% of the undiscovered oil in the UK mainland rack. Stratigraphic traps range from on lap to squeeze outs, crossing single seal and poly-seal traps. The Forties sandstone stratigraphic trap in the Callanish Field is a case of profound water mounded turbidites that have endured differential compaction and squeeze out towards the southwest. Blend catching components consolidating structural and stratigraphic gimmicks are likewise display, for instance in the Britannia field in the Lower Cretaceous (Eddy kinetic energy in the deep western North Atlantic, 1977). Despite the fact that a scope of hydrocarbon play sorts exist in the CNS, this article centres upon profound water Paleocene and shallow to profound marine Jurassic plays. This article has quickly secured the late disclosures and plays of the Central North Sea and exhibits how the redesigned information scope of the Mega Survey Plus can help to recognize more leads and prospects with a level of certainty never conceivable previously (Eedler, 1978). With an expected five billion barrels of oil and gas undiscovered and huge in-situ framework, the Central North Sea is still an exceptionally alluring range to investigate and work. As investigation proceeds in this productive hydrocarbon region, exhaustive, condition of-the-craftsmanship information is fundamental for portraying prospects and decreasing danger. The application of pre stack seismic information consolidated with refined decently tied skylines and AVO peculiarities gives an abundance of data (Errant polychaete annelids from North Carolina, 1977). Besides, the future application of PGS' Geo Streamer (double sensor towed streamer engineering) will further upgrade information scope of the Central North Sea and keep on including worth at the supply level. North Sea is one of the major places of great importance because of the huge availability of the major natural resources of the world. The huge availability of the resources actually is of great importance. But along with the huge availability of the resources and important stuffs there are major uncertainties and from the largest is the climate change (Fischer, 1981). This is the major possible uncertainties and it is explained briefly below: Climate change: Environmental change will prompt changes in a few variables which can affect surge risk, including ocean level climb, changes in precipitation examples and profundities, and expanded temperatures which will modify examples of evaporation, transpiration and snow stockpiling (Goldberg, 1973). The nearby effect of these progressions differs fundamentally between regions inside the North Sea locale, so examinations utilizing territorially downscaled atmosphere projections and further displaying are obliged to focus their impact on surge danger. An environmental change projection for northern Europe demonstrates changes in both temperature and precipitation administrations later on that, in a few regions, will help an expanded risk from hydrological flooding. Likewise, the local impacts of worldwide ocean level climb and anticipated changes in examples of storm surge will likewise have a noteworthy impact on the probability and/or extent of surge immersion in numerous seas ide areas. There are, on the other hand, huge varieties between areas as to the effect of changed climatic administrations on surge danger (Healey, Force and Oslo and Paris Commissions, 1995). In vast parts of the Nordic area, for instance, a reduction in the general surge peril is anticipated for some bigger catchments, reflecting the anticipated abatement in the spring and early summer snowmelt surges which overwhelm crest streams in these catchments. At the same time, an increment in the event of great precipitation can improve the probability of surges in littler catchments and in urban zones in the same area. Lake flooding can increment in zones presently commanded by snowmelt flooding because of changes in regular spill over volumes in spite of an anticipated decrease in the greatest every day inflow to the lake (History of the North American Pinnipeds: a Monograph of the Walruses, Sea-Lions, Sea-Bears, and Seals of North America, 1881). Ocean level climb will likewise have va riable neighbourhood impacts all through northern Europe because of local contrasts in elevate coming about because of isostasy rather than area subsidence. In the event that one is to create direction for making note of environmental change in surge hazard administration, it is accordingly important to direct genuinely point by point local or nearby examinations. The North Sea Region Climate Change Assessment (NOSCCA) will archive the deductively real learning about past and conceivable future environmental change in the North Sea and neighbouring ranges for an extensive variety of subjects. It will be a complete environmental change appraisal from distributed investigative work with a territorial IPCC like assessment and a more extensive concentrate on marine and physical biology and fluxes of matter (Holstein and Lake, 2007). It is a global activity being proposed by the Institute for Coastal Research of the GKSS Research Center in Germany. 6. Conclusion The reproduction of this geographical history aides anticipate the area of conceivable oil supplies through the investigation of conceivable source, supply and seal rocks. The Kimmeridge Clay is a decent source rock and it is thickest in the North of the Central Graben and has been saved less in the Terschelling Basin. A decent store rock can be found in the permeable Scruff Greensand development, which has additionally been, which has been broadly kept all through the Central Graben, yet is thickest in the South (Jordan, 2004). A decent seal are the Cretaceous chalk arrangements that together with disfigurement because of (reversal) tectonics and salt diapirism can make flawless oil and gas traps. A large portion of these layers have been disintegrated in the focal point of the Central Graben however. So the oil potential (at this profundity) around there is bad. General the North Sea bowl has encountered a very intricate land history. Anyway, because of the substantial measure of h ydrocarbon collections it has been decently mulled over. In this paper just a concise history has been depicted (Junger, 1997). Likely the most critical tectonic stage in the North Sea has been the one of fracturing, the Kimmerian stages. Not just has the melancholy created by the fracturing guaranteed the affidavit of an exceptionally rich source rock; it has likewise delivered satisfactory structures to capacity as traps (Kell, Scott and Hunter, 2004). Towards the south, fundamentally in the Netherlands the Variscan stage and its related foreland have created a rich gas region. This was less because of the structures that created amid that tectonic stage, but instead because of the way of the foreland bowl which has made a practically immaculate source-repository seal progression (Lake and Fanchi, 2006). The last stage, the Alpine stage has from numerous points of view entangled the structures in the Southern North Sea and has had some negative ramifications for timing and spillage. However, it has likewise brought on new structures to structure that got to be fabulous traps. Since the North Sea is exceptionally developed, investigation insightful, new revelations ought to be looked for in tight oil and gas and in play levels that have not been decently investigated (Lake and Mitchell, 2006). The Pre Sillesian may have potential despite the fact that not a great deal of business aggregations has been found. Tertiary delta groupings and their conceivable sedimentary traps might likewise demonstrate effective if concentrated on in subtle element (MacGarvin, 1990). 7. References A North Sea School of Architecture?: Nidaros Cathedral's Romanesque Transepts and North Sea Medieval Architecture. (2012).Journal of the North Atlantic. A healthy North Sea ecosystem and a healthy North Sea fishery: two sides of the same regulation. (1994).Biological Conservation, 67(2), p.190. Alvarez, A. (1986).Offshore. Boston: Houghton Mifflin. Bottom irregularities in the North Sea. (1977).Deep Sea Research, 24(4), p.294. Bradley, H. and Gipson, F. (1987).Petroleum engineering handbook. Richardson, TX, U.S.A.: Society of Petroleum Engineers. Brouwer, L. and Shawcross, L. (1964).The North Sea. Ebbingford, Bude, Eng.: Geographical Pub. Buydos, J. (n.d.).Petroleum engineering. Churchill, R. (1977). Industrial island in the North Sea Report on the feasibility study The North Sea Island Group.Marine Policy, 1(2), pp.170-171. Coakley, B. and Stein, R. (2010). Arctic Ocean Scientific Drilling: The Next Frontier.Scientific Drilling, (9, April 2010). Cooper, B. and Gaskell, T. (1966).North Sea oil--the great gamble. London: Heinemann. Cubitt, J., England, W. and Larter, S. (2004).Understanding petroleum reservoirs. London: Geological Society. Cussler, C. and Dirgo, C. (1996).The sea hunters. New York: Simon Schuster. Demaison, G. and Murris, R. (1984).Petroleum geochemistry and basin evaluation. Tulsa, Okla.: American Association of Petroleum Geologists. DeNatale, G., Troise, C. and Sacchi, M. (2007). The Campi Flegrei Deep Drilling Project.Scientific Drilling, (4, March 2007). Distribution of Holocene silicoflagellates in North Pacific sediments. (1977).Deep Sea Research, 24(4), p.292. Echo-traces from the north-eastern Atlantic. (1977).Deep Sea Research, 24(4), p.197. Eddy kinetic energy in the deep western North Atlantic. (1977).Deep Sea Research, 24(4), p.212. Eedler, G. (1978). On the North Atlantic circulation.Deep Sea Research, 25(6), pp.584-585. Errant polychaete annelids from North Carolina. (1977).Deep Sea Research, 24(4), p.193. Fischer, D. (1981).North Sea oil, an environment interface. Bergen: Universitetsforlaget. Gautier, D. (2005).Kimmeridgian Shales Total Petroleum System of the North Sea Graben Province. Reston, VA: U.S. Geological Survey. Goldberg, E. (1973).North Sea science. Cambridge: MIT Press. HARKER, STUART D., Occidental Petro, (1991). Oxfordian-Kimmeridgian (Late Jurassic) Reservoir Sandstones in the Witch Ground Graben, U.K North Sea.Bulletin, 75. Healey, M., Force, N. and Oslo and Paris Commissions, (1995). North Sea Quality Status Report 1993.Estuaries, 18(1), p.316. History of the North American Pinnipeds: a Monograph of the Walruses, Sea-Lions, Sea-Bears, and Seals of North America. (1881).Nature, 23(586), pp.261-262. Holstein, E. and Lake, L. (2007).Petroleum engineering handbook. Richardson, TX: Society of Petroleum Engineers. Jordan, P. (2004).North Sea saga. Harlow, England: Pearson/Longman. Junger, S. (1997).The perfect storm. New York: Norton. Kell, L., Scott, R. and Hunter, E. (2004). Implications for current management advice for North Sea plaice: Part I. Migration between the North Sea and English Channel.Journal of Sea Research, 51(3-4), pp.287-299. Lake, L. and Fanchi, J. (2006).Petroleum engineering handbook. Richardson, TX: Society of Petroleum Engineers. Lake, L. and Mitchell, R. (2006).Petroleum engineering handbook. Richardson, TX: Society of Petroleum Engineers. MacGarvin, M. (1990).The North Sea. London: Collins Brown. Mayer-GuÃÅ'ˆrr, A. (1976).Petroleum engineering. New York: Wiley. Mead, S. (2012).Petroleum engineering. Delhi: Research World. North Sea oil: Women not at sea. (1985).Nature, 313(6000), pp.260-260. Pegrum, R., Rees, G. and Naylor, D. (1975).The North Sea. London: Graham Trotman Dudley. Phelps, R. and Lake, F. (1924).Petroleum engineering. Houston, Tex.: Gulf Pub. Co. Reis, J. (1996).Environmental control in petroleum engineering. Houston, Tex.: Gulf Publ. Roberts, G. (1985).Engineering the North Sea connection. University of Salford. Russell, J. and Bijaksana, S. (2012). Scientific Drilling.Scientific Drilling, (14, September 2012). The North Sea. (1976).BMJ, 1(6011), pp.705-706. Verweij, J. and Simmelink, H. (2002). Geodynamic and hydrodynamic evolution of the Broad Fourteens Basin (The Netherlands) in relation to its petroleum systems.Marine and Petroleum Geology, 19(3), pp.339-359. Walton, A. (2011). U.S. Continental Scientific Drilling Community Looks to the Future.Scientific Drilling, (11, March 2011). Warme, J., Douglas, R. and Winterer, E. (1981).The Deep Sea Drilling Project--a decade of progress. Tulsa, Okla.: Society of Economic Paleontologists and Mineralogists.

Women In Educational Administration The Glass Ceiling Is Still There Essay Example For Students

Women In Educational Administration: The Glass Ceiling Is Still There Essay WOMEN IN EDUCATIONAL ADMINISTRATIONTHE GLASS CEILING IS STILL THERESeveral people at the conference dealt with the problems women encounter in getting into administrative positions in schools and colleges and when they do, the obstacles they encounter in making their jobs successful. Their discussions brought home to me the reality of my own mother’s experience. As children we witnessed our mother struggling, summer after summer and during many school years in the evenings, with those courses required for an administrative license. The state gave her that license some twelve years ago, but she is still teaching mathematics in high school. We used to tease her when we were growing up calling her â€Å"principal mom† and â€Å"assistant principal mom† and the like and pretending that she called us into her office for punishment. We do not do that any more because we know it won’t be fun and games any more but it will be a cruel joke if we did that. What made her disillusioned about the career of an administrator in her school system in which she served nearly a quarter of a century?It has to do with what is known as a glass ceiling. Administrative positions are open to all qualified persons. They are up there within everyone’s view. All you have to do is qualify yourself with the appropriate education and skills. The law of the land makes every person eligible for them. All employers proclaim in their policy statements that they are â€Å"equal opportunity employers.† But when women reach for them, the invisible ceiling stops them. A cruel tease indeed!My mother said she would not talk to me about her own reluctance to pursue an administrative career, despite all the efforts she put in to qualify for it. She said I should talk with teachers or other personnel in the school systems who had no personal involvement in order to get objective observations. So I interviewed more than 25 people from Superintendents and Principal s through Vice Principals, Department Heads, Counselors, Teachers and Teachers’ Assistants to Security, Cafeteria and Maintenance Personnel, in two different school systems. My findings were quite revealing of the invisible glass ceiling. We will write a custom essay on Women In Educational Administration: The Glass Ceiling Is Still There specifically for you for only $16.38 $13.9/page Order now Let me start with the lowest level positions in the school systems—maintenance workers, security personnel and cafeteria workers. Strictly speaking, they cannot be called part of the education system. Their jobs do not have anything to do with the educational system, they could be in any other place than the school, but the way the heads of their departments are chosen will show how endemic gender discrimination is to the entire school systems, from bottom to top. In fact, it is ingrained in the culture of the school systems as it is in the culture of many other organizations in the public life. My innocent ears were offended hearing the tale of a woman security officer describe what was going on in the South Bend School Corporation at her level of employment. She has much more seniority than most of the chiefs of security in the school system, but the chief’s position along with all the benefits go to the men who, in her judgement, were less qualified, experienced and conscientious. She pointed out to her own chief, a pot-bellied man who sat by a closet and snacked all day, according to reports, which could not be far from the truth judging from his appearance. â€Å"Only men can handle the tough situations; he does all that sitting in that chair while I do the simple things like breaking up fights, confiscating guns and knives and searching out drug pushers,† she stated. Among maintenance workers there were only very few women. The chief janitor in one school, a fair man who has a couple of women in his staff, a rarity, said that women are intimidated by furnaces and electrical systems, so they don’t sign up for janitorial jobs. But he also added that â€Å"not that they are welcome either; I don’t mind them, but the guys in other schools will hire a women only if they can not even find a dead body.† I asked, â€Å"can a woman ever become the chief janitor?† The answer was a plain and clear â€Å"never.†The cafeteria was a completely different story. Practically all the workers in the cafeterias of all schools are women. I asked the head of the food service department in one high school, who I thought was a fair-minded lady, why it was that all cafeteria workers are women. She said men do not generally apply; cooking and serving food is a women’s job, they think. She also added, â€Å" We don’t want t hem anyway, you can hardly find one who is not sloppy and dirty.† But I observed, and she agreed, that there is no injustice involved. There is no built-in obstacle for men to be hired or promoted in food service. Leaving the support staff level and getting to the heart of the educational enterprise, we come to the teaching staff. Instantly, one notices that the elementary schools are mostly staffed by women teachers. However, the administrators by and large are men. The South Bend School Corporation, for example, has approximately 25 elementary schools. Of these, twenty of them have men principals while nearly 70% of teachers are women. I asked one of the male principals why there is such a disparity between male/female ratios of teachers and administrators in elementary schools. He said that it is the â€Å"mother thing,† women are more suited to teach little children and they are attracted towards the elementary age kids, that is as far as teaching is concerned. The administration, however, is another matter. There you need men. They, according to him, are better organizers, disciplinarians, and of course father figures. A woman principal had a different view. For her it is the †Å"old boys’ club at work. They simply do not want to give women top jobs even in elementary schools,† she said. When you go up to the Middle School level, the disparity worsens. Of the eight middle schools I visited, six had male principals while the teaching staff was fairly evenly divided. From what I could surmise from the conversations with teachers and administrators, there is no good reason for the disparate male/female ratio in the building administration, except the continuing resistance against women. .ub681905b1376466c19880d63548e3083 , .ub681905b1376466c19880d63548e3083 .postImageUrl , .ub681905b1376466c19880d63548e3083 .centered-text-area { min-height: 80px; position: relative; } .ub681905b1376466c19880d63548e3083 , .ub681905b1376466c19880d63548e3083:hover , .ub681905b1376466c19880d63548e3083:visited , .ub681905b1376466c19880d63548e3083:active { border:0!important; } .ub681905b1376466c19880d63548e3083 .clearfix:after { content: ""; display: table; clear: both; } .ub681905b1376466c19880d63548e3083 { display: block; transition: background-color 250ms; webkit-transition: background-color 250ms; width: 100%; opacity: 1; transition: opacity 250ms; webkit-transition: opacity 250ms; background-color: #95A5A6; } .ub681905b1376466c19880d63548e3083:active , .ub681905b1376466c19880d63548e3083:hover { opacity: 1; transition: opacity 250ms; webkit-transition: opacity 250ms; background-color: #2C3E50; } .ub681905b1376466c19880d63548e3083 .centered-text-area { width: 100%; position: relative ; } .ub681905b1376466c19880d63548e3083 .ctaText { border-bottom: 0 solid #fff; color: #2980B9; font-size: 16px; font-weight: bold; margin: 0; padding: 0; text-decoration: underline; } .ub681905b1376466c19880d63548e3083 .postTitle { color: #FFFFFF; font-size: 16px; font-weight: 600; margin: 0; padding: 0; width: 100%; } .ub681905b1376466c19880d63548e3083 .ctaButton { background-color: #7F8C8D!important; color: #2980B9; border: none; border-radius: 3px; box-shadow: none; font-size: 14px; font-weight: bold; line-height: 26px; moz-border-radius: 3px; text-align: center; text-decoration: none; text-shadow: none; width: 80px; min-height: 80px; background: url(https://artscolumbia.org/wp-content/plugins/intelly-related-posts/assets/images/simple-arrow.png)no-repeat; position: absolute; right: 0; top: 0; } .ub681905b1376466c19880d63548e3083:hover .ctaButton { background-color: #34495E!important; } .ub681905b1376466c19880d63548e3083 .centered-text { display: table; height: 80px; padding-left : 18px; top: 0; } .ub681905b1376466c19880d63548e3083 .ub681905b1376466c19880d63548e3083-content { display: table-cell; margin: 0; padding: 0; padding-right: 108px; position: relative; vertical-align: middle; width: 100%; } .ub681905b1376466c19880d63548e3083:after { content: ""; display: block; clear: both; } READ: What the difference is between strict and broad co EssayA veteran teacher told me that in all his memory he could not think of one female principal in any of the five South Bend public high schools. In the 1998-1999 school year, however, there are three female principals, a majority! But, they are relatively new appointments, two of them only a year ago and the third just this year, but she is only an acting principal. A female superintendent who is also relatively new made these appointments, though they were not very popular. As a result, one of the regular appointees has tended her resignation, the second is on the verge of doing so, and the acting principal’s fa te is hanging in the balance. One of the school staff related to me the reception the acting principal received when she came to take charge of the school and for a few weeks thereafter. To start with, she was appointed at the last minute, as a last resort when none of the candidates the school system offered the job to accepted it. When she came to the building for the first time, very few faculty persons greeted her. One of the two vice principals, a male who had applied for the principal’s job unsuccessfully, greeted her sitting on his chair and with his feet on his desk. He arrogated the principal’s authority to himself, calling faculty meetings, making policy decisions, addressing the school community through the public address system and complaining to the corporate administration about the acting principal. The department heads, counselors, and teachers also started to set their own rules. Being placed in such a tough situation, a weak person would have been totally broken, but the acting pri ncipal stood her ground, asserted her authority and established discipline within a few weeks. It was a superhuman task. In high schools, between the teachers and building administrators, stand the department heads. My curiosity peaked when I noticed that almost all department heads, other than home economics and special education, were men, in all five South Bend high schools. What I learned was that these were all appointees of men principals, hanging on to their jobs, wielding whatever little authority they could claim over their fellow teachers. The culture of male domination governed this low level of administration as well. Coming to the top level of administration, the South Bend School Corporation never had a woman superintendent in its entire history until five years ago when the present superintendent was appointed. She got the job by default when three outside finalists, all men, declined the offer. She had not been ranked among the finalists despite the fact that she had been a very successful principal in the corporation, with a national reputation as an educator. Being a woman and an African-American were two strikes against her. Her appointment divided the teachers and the community at large along racial lines. A prolonged and bitter teachers strike further divided the community. In spite of her accomplishments in bringing about fiscal discipline and solvency to the corporation, she barley got re-appointed for two short years after the first three-year term. Efforts are mounting to release her even before the two years are up. Resistance against the superintendent by the combined forces of anti feminist and anti-minority groups in the school system itself and the larger community have paralyzed her administration. Lack of discipline and moral within the schools result in the failure of the process of education itself. It is no surprise, therefore, that the South Bend students are among the lowest achievers on the ISTEP. The sad story of South Bend schools is a classic example of how damaging to the public good discrimination against women and minorities can be. It is also important for us to look beyond the local scene to the national picture to see what role is given to women and minorities in the administration of educational institutions. Several recent studies were able to unveil some hidden truths about women and minorities in the educational administration. The 1990 study by Patricia T. Whitfield entitled Status of Access of Women and Minorities to Administrative Positions in Idaho is a case in point. This study focused on the status of women and minorities in administrative positions in Idaho public schools. Statistically Whitfield documented that among administrators of Idaho public schools only approximately 20% were women and only about 7% minorities. She cites the â€Å"old boy network,† family responsibilities, lack of mentors or role models, a late entry into career tracks, and difficulty in gaining credibility as the reasons for this poor representation of women and minorities. As for the possible remedy for this situat ion, Whitfield received different responses from the administrators and members of the women and minority groups. While the administrators indicated that change/progress would come through their efforts, the women’s and minority groups felt that progress will come only through equal opportunity policies and legislation. I am sure that similar responses will be forthcoming from other comparable groups in all parts of the country. (Patricia T. Whitfield, Status of Women Minorities toAdministrative Positions in Idaho. ERIC TITLE NUMBER: ED 323907). It is also important to compare the status of women in administrative positions in higher education with what we have seen in the nation’s school systems. Let me start with a local women’s college, Saint Mary’s College of Notre Dame, Indiana. This is a college founded some 155 years ago exclusively for women by women religious of the Holy Cross Congregation. All major administrative positions were held by the Sisters of the Holy Cross up until 1967. This college was also the sister institution of the larger University of Notre Dame, across the road, founded about the same time exclusively for men by the Priests of the Holy Cross. In 1967, when the then president of Saint Mary’s died and another well-qualified nun was not available to fill the role, the sisters appointed Saint Mary’s first male president, a priest. In 1970, Notre Dame proposed a merger with Saint Mary’s. Fearing the total absorption of Saint Mary’s into larger Notre Dam e, the sisters withdrew from the merger. However, they inadvertently entered into another dangerous situation, the male domination of the school. This happened when they appointed the first layman president of the college, hoping that would bring Saint Mary’s in tune with the modern age. For the next 29 years, the administration of the college passed into almost exclusively male hands. Only in 1999 did they appoint a woman president and a female administrative team, after three decades of male domination. .uf6a157b5b801c4c47d73c2070ca6db5b , .uf6a157b5b801c4c47d73c2070ca6db5b .postImageUrl , .uf6a157b5b801c4c47d73c2070ca6db5b .centered-text-area { min-height: 80px; position: relative; } .uf6a157b5b801c4c47d73c2070ca6db5b , .uf6a157b5b801c4c47d73c2070ca6db5b:hover , .uf6a157b5b801c4c47d73c2070ca6db5b:visited , .uf6a157b5b801c4c47d73c2070ca6db5b:active { border:0!important; } .uf6a157b5b801c4c47d73c2070ca6db5b .clearfix:after { content: ""; display: table; clear: both; } .uf6a157b5b801c4c47d73c2070ca6db5b { display: block; transition: background-color 250ms; webkit-transition: background-color 250ms; width: 100%; opacity: 1; transition: opacity 250ms; webkit-transition: opacity 250ms; background-color: #95A5A6; } .uf6a157b5b801c4c47d73c2070ca6db5b:active , .uf6a157b5b801c4c47d73c2070ca6db5b:hover { opacity: 1; transition: opacity 250ms; webkit-transition: opacity 250ms; background-color: #2C3E50; } .uf6a157b5b801c4c47d73c2070ca6db5b .centered-text-area { width: 100%; position: relative ; } .uf6a157b5b801c4c47d73c2070ca6db5b .ctaText { border-bottom: 0 solid #fff; color: #2980B9; font-size: 16px; font-weight: bold; margin: 0; padding: 0; text-decoration: underline; } .uf6a157b5b801c4c47d73c2070ca6db5b .postTitle { color: #FFFFFF; font-size: 16px; font-weight: 600; margin: 0; padding: 0; width: 100%; } .uf6a157b5b801c4c47d73c2070ca6db5b .ctaButton { background-color: #7F8C8D!important; color: #2980B9; border: none; border-radius: 3px; box-shadow: none; font-size: 14px; font-weight: bold; line-height: 26px; moz-border-radius: 3px; text-align: center; text-decoration: none; text-shadow: none; width: 80px; min-height: 80px; background: url(https://artscolumbia.org/wp-content/plugins/intelly-related-posts/assets/images/simple-arrow.png)no-repeat; position: absolute; right: 0; top: 0; } .uf6a157b5b801c4c47d73c2070ca6db5b:hover .ctaButton { background-color: #34495E!important; } .uf6a157b5b801c4c47d73c2070ca6db5b .centered-text { display: table; height: 80px; padding-left : 18px; top: 0; } .uf6a157b5b801c4c47d73c2070ca6db5b .uf6a157b5b801c4c47d73c2070ca6db5b-content { display: table-cell; margin: 0; padding: 0; padding-right: 108px; position: relative; vertical-align: middle; width: 100%; } .uf6a157b5b801c4c47d73c2070ca6db5b:after { content: ""; display: block; clear: both; } READ: The Cherry Orchard Lopakhin EssayWhile Saint Mary’s College’s link with the Holy Cross Sisters made it easy for its board to revert to its traditional administration by women, what is happening nationwide in higher education is quite different. A 1982 study by Kathryn M. Moore documents the low status of women in administrative positions in higher education. Moore studied the career issues, educational concerns and the professional, educational and personal backgrounds of 2, 896 senior college administrators from all parts of the United States. The focus of her study was the status of women and minorities in educational administration. She discovered that wom en and minorities represented a shocking 20 and 8 percent of the sample, respectively. Even more disturbing was her discovery that women and minorities held only low level positions such as registrar, librarian, and financial aid director. In contrast, men held positions like President and Chief Financial Officer. Of the 653 deans in the survey only 90 (13.8%) were women. Half of these women deans were in the fields of nursing, home economics, arts and sciences, and continuing education. As for minorities, only 5.5% of them were among the deans. These statistics tell the cruel hoax American society still plays on its female citizens despite decades of equal opportunity enforcement. (Women and Minorities. Leaders in Transition: A National Study of Higher Education Administrators by Kathryn M. Moore. University Park, PA., Center for the Study of Higher Education, Pennsylvania State University, 1982. P.64.). Leaving the broad, nationwide survey, let us now take a closer look at one institution of higher learning, University of New Hampshire, an institution with a relatively high reputation. A 1993 study ordered by the university president on the status of women showed that out of 16 principal administrators (president, vice president, and deans) of the university, only one was a woman and she was only a temporary appointment. At the next level, the Academic Administration level, 27.3% were women. At the executive management level, women held only 21.8% of the positions. But at the management or supervisory level (support staff level) 60.8% of the employees were women. The story becomes even grimmer when we look at the compensation level of employers at the University of New Hampshire. Of those employees making $35,000-55,000, 54% were women. Of those making $55,000-66,000 only 31% were women. Of those making above $65, 000 only a meager 19% were women. When different groupings were emplo yed, the glaring and shameless fact came out, that is out of all the employees making less than $30,000, a towering 83.3% were women!The study also indicated that the situation at the University of New Hampshire was fairly typical of all universities in the country; only much worse in many other schools. (University of New Hampshire President’s Commission on the Status of Women, July 1993). The issues relating to the status of women were placed in a broader, national perspective by the Federal Glass Ceiling Commission in 1996. Rene Redwood, then Special Assistant to the Secretary of Labor, Robert Reich, summarized the findings of this commission in a speech she gave at the â€Å"Working Women’s Summit† held by Women in Technology International (WITI) in Philadelphia, Pennsylvania in September 1996. The most telling data she included in her speech was that in the top 1000 industrial and 500 service companies in the United States, 95% of senior level managers were men of which 95% were white. Of the 5% of those managers who were women, only 5% were minority women. This translated into a total of 2,100 senior women executives out of the 42,000 top-level executives. She also pointed out the disparity in salary levels between men and women on a national level. While non-Hispanic white males with bachelors degrees received an average salary of $47, 181, the females with bachelor’s degrees in the same ethnic group received only an average of $31, 338. Of those with masters’ degrees, non-Hispanic white males received an average of $57, 371, but females in the same ethnic group with master’ degrees received only an average $38, 391. Reliable statistics about the salary levels of other ethnic groups are not available but it is safe to assume that they are appallingly disparate. While statistics document the injustice of the system, they do not suggest solutions for the problem. Solutions can be found only if men and women of good will come together and seek them out. There are many organizations that address these issues on the local and national level. There are also laws on the book that could be brought to bear when institutions are insensitive to the issues of equality. However, in order to bring about fundamental changes, we have to work at the roots of our culture. This is where educators have an advantage. It is their hands that mold the next generation. They can change the whole outlook of society if they put their minds to it. Let us hope, therefore, in a generation or two, we can make the statistics look very different. NOTES ABOUT MY SOURCES1. For information about women in administration in local schools, I interviewed 25 individuals at various levels of employment, from maintenance staff and cafeteria workers to teachers, principals and Superintendents of South Bend, Mishawaka, and Penn-Harris-Madison School Systems. 2. For information on local colleges and universities, I interviewed 12 professors and administrators at Saint Mary’s College and the University of Notre Dame. 3. For information on the status of women in educational administration on the regional and national level, I used the following sources:a. Patricia T. Whitfield, Status of Access of Women and Minorities to Administrative Positions in Idaho. ERIC TITLE No. ED 323907. b. Kathryn M. Moore, Women and Minorities. Leaders in Transition: A National Study of Higher Education Administrators. ERIC TITLE No. ED 225459. c. University of New Hampshire President’s Commission on Status of Women. University of New Hampshire, 1993. d. Rene Redwood, The Glass Ceiling: The Findings and Recommendations of the Federal Glass Ceiling Commission. Washington, D.C. 1996. WOMEN IN EDUCATIONAL ADMINISTRATIONTHE GLASS CEILING IS STILL THEREANAND PULLAPILLYJULY 30, 1999Social Issues