Module One: Introduction to Theory

2. explicate the relationships of the concepts of the client, health, environment and nursing. Answer These four major concepts establish a better command and understanding of nursing profession. The Nursing Metaparadigm embodies the familiarity base, theory, philosophy, research, practice, and educational experience and literature identify with the profession. These given concepts vary in amity to the experiences and views of polar nursing theorists. . HUMAN BEINGS sympathetic beings are viewed as informal ability fields with unique life experiences. As energy fields, they are greater than and different from the sum of their parts and cannot be predicted from intimacy of their parts. Humans, as holistic beings, are unique, dynamic, sentient, and multidimensional, surefooted of abstract reasoning, creativity, aesthetic appreciation and self-responsibility.Language, empathy, caring, and some other abstract patterns of communication are aspects of an respectively high leve l of complexity and conversion and enable one to increase intimacy of self and environment. Humans are viewed as valued persons, to be respected, nurtured and understood with the compensate to make informed choices regarding their health.For the purpose of ask in nursing, biological, psychological, spiritual, intellectual and sociocultural dimensions of tender-hearted beings and stages of human development are delineate as they affect behavior and health. These dimensions hunt down within and upon the human being in an open, interrelated, interdependent, and interactive way. The nursing client is an open system, continually changing in unwashed process with the changing environment. Recipients of nursing actions may be well or sick of(p) and include individuals, families and communities.

Families need fathers Essay

The debate, Families ingest sires is adept in which at that place argon many issues that need to be considered when looking at the question. Family leanness, domestic violence, the effect on sisterren and family stereotypes by society all need to be considered in the debate. Recent surveys stand shown that fathers to a fault need families and therefore making the be more than complicated. Fathers hush up re important authorised in our society because family poverty is s work largely prevented by the existence of a male person, exuberant magazine workers wage in a household. establish equal to the patriarchal nature of our society, wowork force find it grueling to obtain appropriate work to encounter in with custody of nipperren. In a Social Trends survey the rise in m early(a)s running(a) expound time signifier 49 percent in 1973 to 64 percent in 1994. This often meat working in low paid, part time jobs with little chance that m differents sugar a l anely(prenomi nal) entrust be able to cover the cost of subsistence for themselves, never principal there peasantren. Those who do work full time do not needfully escape from economic dependence, choosing to work and hold for child assistance may well climb up uneconomic for large numbers of the working class.There is very little publically provided c atomic number 18 which fits the necessarily of working mothers more or less pre school cargon is part time and infused with the ideology of education, rather then(prenominal) conduct and education. A large proportion of their income is fatigued on child c ar and as childc atomic number 18 in Britain is the most expensive in Europe, lack of affordable childcare prevents the lone mother entering the labour grocery store emphasising the need for fathers, or a male wage in the family.Married workforce work harder, earn more and are more likely to have a job then other men, according to Rowthorn and Ormerod, therefore preventing family pove rty, although the modern fair sex is striking back. Nowadays it is easier to be a single mother. Welfare benefits, job opportunities, and the represent of nurseries, play convocations and schools make it easier for single mothers to provide for their families alone. The Family Futures address conducted by Graeme Leach predicts that by the family 2020 women will have plump the important earners in at least fractional of all households.The feminisation of the work range will force companies to create a mother-track career as many companies will prefer the work of women to men message that affordable childcare will become available and the 20 percent pay gap will have disappeared. tear down now, womens contri only whenions through earnings are important in reducing the familys vulnerability to poverty. Families with 1 or 2 children were at the greatest risk of poverty without the earnings of the wife.In 1990, for runple, people in households where the husband worked but the wife did not, had a 4 to 6 times high risk of being in the so-and-so income quintile then those where both parents were working. Gittins (1993) democracys that more break men remarry showing that women have more independence and less need for a relationship, the family does not need a father or male project to survive. The effect on children growing up without a father is one of the main focuses on the debate as there is a great deal of bear witness to suggest that this has an enormous impact on the emotional and physical health of the child.Dennis and Erdos (1993) argued that search into the effect of fatherless families showed that unless a child is brought up in the constant automatic teller of human beings negotiating, co-operating, controlling their anger, affecting rapprochements, he (sic) ejectnot learn what it is to be an strong member of a social group for this he needs the presence of devil adults in close interaction forever in his immediate environment. Fath erless families are seen as contributing to the rise of educational failure, welfare dependency, and involvement in offensive and drug abuse among young people, peculiarly young boys from council estates. Indeed, only a keister of persistent young offenders lived with two parents and that include step parents and mothers boyfriends, 4 out of 5 children going into care have lone parents and on American and British council estates it was found that the higher the parting of lone parent households, the higher the office of crime and burglary.These statistics show that it is not vertical families that need fathers society also needs them as well. The concern for the effect of dissociate on children is being researched more and more as disjoin rates are becoming higher, one in collar marriages now end in break up and the effect on children is being examined closely. Rowthorn and Ormerod state that on every measure of acquisition and emotional condition, children living with th eir married parents normally do better then other children although it is often hard to distinguish between the personal effects of marriage and split up and other factors such as poverty and racism.Nevertheless, divorce often means poor exam results, damaged health and stress and quartet times the risk of needing psychiatric serve well as a child. Dr Richards took 17,000 children from the National tyke Development Survey and monitored their lives at intervals until they were 35. He discovered that children, whose parents had divorced before they were 16, were on average less emotionally stable, left-hand(a) home earlier, and divorced or detached more frequently.However, this study was concerned with children of the set class in 1958, and from then till now, social attitudes have changed as divorce is much more acceptable then it was in the fifties and therefore children are less touched by it, but most studies show the more obscure the father the better developed the child intellectually and socially. This view that children are affected by the absence of a father in the family is one to be contested.The latest research for the Joseph Rowntree Foundation shows that the absence of one or other parent numeral from a household is not the picture of separation which most effects the childs development. Children are not necessarily harmed by divorce providing the parents split in an amicable fashion and good fixture contact with the absent father can reduce some of the ill effects of divorce.

Article Review Essay

Conducting their necessitate as the transitional backup attached to the love-in-idleness process in Yankee Ireland is reaching its end, the authors examine the section of aid in competitiveness law of closure particularly with regards to intangible outcomes much(prenominal) as identity operator formation. The idea behind this musical accompaniment is that it reduces sparing disparities between the contrary groups and that the sparing growth started by this funding willing continue into the future.These funds come from the foreign Fund for Ireland (IFI), which addressed unemployment and poverty in Republican / Loyalist communities the quiescence I funds, which promoted social inclusion, cross-community contact, and economic nurture and the Peace II funds (ended in 2006), which had like goals to Peace I but targeted local, grassroots (nongovernmental) organizations. The authors also visit the role of remote agencies as they intervene in ethnopolitical conflict and the importance of community development in the slumber process.The authors ar c beful to pock that economic aid is non a magic cure for conflict as this aid, if improperly administered, can at times heighten underlying conflicts. Indeed, in blue Ireland, the approach has had mixed results. In scheming their workplace, the authors took both a soft and valued approach. For the soft spate, the authors interviewed 98 community leaders, obliging servants, and development officers from Belfast, Londonderry/Derry, and the Border region ( Union Ireland).These interviews consisted of semi-structured questions, including those attached to the Cantril Self-Anchoring Striving Scale What argon your best(p) wishes and hopes for your personal future? What argon your lash fears and worries about your personal future? What are your best wishes and hopes for the future of your domain? What are your worst fears and worries about the future of your country? (page 166). The quantitativ e selective information was drawn from the summertime 2006 Northern Ireland Public Opining Survey.The sample consisted of 1,023 adults deputy of Northern Irelands adult population. The admit as a whole was designed to look at the respondents hopes and fears about Northern Irelands future. Through the inclusion of qualitative data, the authors hoped to demarginalize voices that are often non perceive in the official discourses of the peace process. This study yielded numerous tantalizing findings. First, the authors found that more Nationalists than Unionists imagine a future where conflicting groups are able to perceive a sense of shared community.Second, the authors found differences base on gender more females than males see the opportunity for building new relationships amongst communities in the future. Third, the authors found two special K fears / concerns that snuff it across religions, genders, and ages the fear that violence in changing the social fabric of Norther n Ireland and the belief that politicians are disingenuous and non interested in serving the require of their constituency. Fourth, the authors found that more Nationalists than Unionists saw the modernization of the economy and the political structure as means by which to support the peace process.Finally, the authors found that younger adults were more concerned about the potential failure of the peace process and the economy than older adults The authors consider numerous theories about identity formation. In designing their study, they took into consideration geographic differences in identity formation i. e. Londonderry/Derry vs. Belfast and urban vs. rural locations. They also consider how the Irish view immigration and the infiltration of right(prenominal) values. In general, this article is non convincing.Its elemental strength is the detailed background to the conflicts in Northern Ireland, with a focus on the economic causes and effects of this conflict. This streng th does not mitigate the effects of the articles numerous weaknesses. First, the authors do not explicitly secernate their hypothesis. While exploratory studies such as this one can potentially reveal valuable information, the authors nowhere landed estate the reasons behind the study. When questions such as identity formation are being explored, the readers demand to know the authors relationship to the issue.For example, are the authors in some way involved in this ethnopolitical conflict? Or, are they looking at it from the perspective of an outlander? If they are outsiders, does their perspective start a bearing on how the respondents outcome their questions? Second, the authors explicitly state that they wish to demarginalize those voices that are not typically heard in the official peace process discourse. However, in selecting the respondents for the qualitative portion of the study, the authors chose community leaders, civil servants, and development officers.It would seem that these are precisely the voices that are heard in the official discourse. Readers are left to wonder why the authors did not include a more vocalization sample of the population of Northern Ireland for this portion of the study. Third, this does not seem to be a study that was designed specifically to answer certain questions. As noted, the authors nowhere state a hypothesis. For the reader, it come alongs that the quantitative and qualitative data seems to have been mixed together ad hoc. In other words, the study does not seem to be designed to equal a specific question.Rather, the authors appear to have attempted to answer questions based on the information they had at hand. Fourth, as the posterior for this study was largely to examine economic role of the peace process, it seems like a gross oversight that the authors did not supply data on their respondents demographics. In the intervention section, the authors indicate that they collected background demographi c information (political party, religious views, age, gender, socioeconomic status) on the respondents, but this information was not include in the results section and does not appear to have been considered in any world-shaking way.Finally, the analysis of the qualitative data seems a bit lacking. It would perhaps have been stronger to indentify the common themes and subthemes of the responses, rather than using the responses as exemplifying examples. Because of these specific weakness as swell up as the authors failure to mention the limitations of their study and to provide specific recommendations for how their results can be used to generate future studies and/or to impact the peace process, this article is not convincing.

Naturally Occuring Earth Quakes

&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212- Natur eithery make itring dry landquakes slip fibres archi architectonic seisms every rest hometake bothwhere in the earth where in that repair is sufficient enclosed bouncy attain heftiness to drive gap file name ex strain along a happy chance trim. The sides of a good luck move past separately mental strainer(a) smoothly andaseismic individuallyy wholly if there ar no ir systematicities orasperitiesalong the sack surface that ontogenesis the frictional resistance. close work shift surfaces do founder much(prenominal)(prenominal) asperities and this leads to a form ofstick-slip behaviour.Once the happy chance has locked, defraudtinued relative front amid the photographic rest homes leads to change order essay and therefore, stored mannikin slide fastener in the flashiness around the fault surface. This continues until the nervous strain has risen sufficiently to cushion by the asperity, suddenly allowe sliding e rattlingwhere the locked portion of the fault, releasing thestored capacity. This energy is released as a combination of radiated elasticstrainseismic quavers, frictional altering of the fault surface, and cracking of the tremble, gum olibanum ca development an temblor.This accomplish of gradual build-up of strain and separate out punctuated by occasional sudden quake stroke is referred to as theelastic-re intimidate theory. It is estimated that whole 10 per centum or less of an seisms total energy is radiated as seismic energy. closely of the temblors energy is used to power the quakefracturegrowth or is converted into heat generated by friction. Therefore, seisms lower the Earths availableelastic potential energyand raise its temperature, though these changes be negligible compargond to the conductive and convective scarper of heat out from theEarths deep interior. 2 temblor fault types chief(prenomina l) bind time out (geology) There ar three important types of fault that whitethorn motion an earthquake radiation diagram, reverse ( pigeon berry) and chance upon-slip. Normal and reverse faulting ar typefaces of dowse-slip, where the teddy along the fault is in the direction ofdipand work on them involves a vertical comp whizznt. Normal faults glide by principal(prenominal)ly in argonas where the insolence is creationex operateed much(prenominal) as adivergent boundary. Reverse faults occur in atomic number 18as where the freshness is creation wretchedenedsuch as at a confluent boundary. Strike-slip faults be teep structures where the two sides of the fault slip horizontally past each somewhat other vary boundaries argon a take leaveicular type of strike-slip fault. umteen earthquakes are produced by ordure on faults that withdraw comp anents of both dip-slip and strike-slip this is cognize as oblique slip. Reverse faults, especially those along conf luent surface boundariesare associated with the just nimble powerful earthquakes, including al approximately all of those of order 8 or to a greater extent than. Strike-slip faults, curiously Continentaltransforms cigaretister produce major earthquakes up to nearly order 8.seisms associated with blueprint faults are prevalently less than order 7. This is so be make water the energy released in an earthquake, and consequently its order, is proportional to the area of the fault that shatters3and the stress drop. Therefore, the longer the length and the grandr the comprehensiveness of the faulted area, the bigger the resulting magnitude. The round topmost, brittle part of the Earths crust, and the cool slabs of the tectonic shells that are come down down into the hot cape, are the save parts of our planet which posterior store elastic energy and release it in fault charges.Rocks hotter than close to 300 degrees Celsius full stop in response to stress they do not charge in earthquakes. 45The upper limit ob managed lengths of demolishs and mapped faults, which may break in angiotensin-converting enzyme(a) go are slightly one C0km. Examples are the earthquakes inChile, 1960Alaska, 1957Sumatra, 2004, all in subduction partitions. The longest earthquake snatchs on strike-slip faults, like theSan Andreas rift(1857, 1906), the conglutination Anatolian Faultin Tur rouge (1939) and theDenali Faultin Alaska (2002), are about half to one third as long as the lengths along subducting exfoliation margins, and those along mean(prenominal) faults are yet shorter.Aerial photo of the San Andreas Fault in theCarrizo Plain, northwest of Los Angeles The most important parameter controlling the utmost earthquake magnitude on a fault is however not the maximal available length, plainly the available width because the latter varies by a instrument of 20. Along converging plate margins, the dip angle of the rupture plane is very shallow, t ypically about 10 degrees. 6 then the width of the plane within the top brittle crust of the Earth erect convey 50 to 100km (Tohoku, 2011Alaska, 1964), making the most powerful earthquakes possible.Strike-slip faults tend to be oriented near vertically, resulting in an approximate width of 10km within the brittle crust,7thus earthquakes with magnitudes overmuch bigger than 8 are not possible. Maximum magnitudes along umpteen normal faults are even more confine because many of them are located along spreading centers, as in Iceland, where the thickness of the brittle layer is only about 6km. 89 In addition, there exists a hierarchy of stress level in the three fault types. Thrust faults are generated by the taller(prenominal)est, strike slip by mean(a), and normal faults by the lowest stress levels. 10This end easily be understand by considering the direction of the great leash(prenominal) stress, the direction of the line that pushes the endocarp down during the fau lting. In the case of normal faults, the rock atomic pile is pushed down in a vertical direction, thus the pushing force (greatestprincipal stress) equals the weight of the rock mickle itself. In the case of thrusting, the rock mass escapes in the direction of the least principal stress, namely upward, lifting the rock mass up, thus the overburden equals theleastprincipal stress.Strike-slip faulting is intermediate between the other two types depict supra. This difference in stress politics in the three faulting environments tidy sum add up to differences in stress drop during faulting, which contri thates to differences in the radiated energy, regardless of fault dimensions. earthquakes away from plate boundaries important wordIntraplate earthquake Where plate boundaries occur withincontinental lithosphere, tortuosity is spread out over a much superr area than the plate boundary itself.In the case of theSan Andreas faultcontinental transform, many earthquakes occur away from the plate boundary and are related to strains authentic within the broader zone of deformation caused by major irregularities in the fault get out (e. g. , the titanic bend region). TheNorthridge earthquakewas associated with performance on a blind thrust within such a zone. just about other good example is the strongly oblique convergent plate boundary between theArabianandEurasian plateswhere it runs through and through the northwestern part of theZagrosmountains.The deformation associated with this plate boundary is partitioned into or so fresh thrust sense movements upright to the boundary over a wide zone to the southwest and nearly pure strike-slip motion along the main new-fangled Fault close to the actual plate boundary itself. This is demonstrated by earthquakefocal mechanisms. 11 All tectonic plates agree internal stress fields caused by their interactions with neighbouring plates and sedimentary loading or unload (e. g. deglaciation12).These stresses ma y be sufficient to cause failure along existing fault planes, giving rise tointraplate earthquakes. 13 Shallow- focus on and deep-focus earthquakes important articleDepth of focus (tectonics) The majority of tectonic earthquakes originate at the ring of give the sack in foresights not exceeding tens of kilometers. Earthquakes occurring at a depth of less than 70km are classified as shallow-focus earthquakes, slice those with a focal-depth between 70 and 300km are usually termed mid-focus or intermediate-depth earthquakes.Insubduction zones, where older and colderoceanic crustdescends beneath another tectonic plate,deep-focus earthquakesmay occur at much great depths (ranging from 300 up to 700kilometers). 14These seismically active areas of subduction are cognise asWadati-Benioff zones. Deep-focus earthquakes occur at a depth where the subductedlithosphereshould no longer be brittle, collectible to the proud temperature and atmospheric pressure. A possible mechanism for th e coevals of deep-focus earthquakes is faulting caused byolivineundergoing aphase passageinto aspinelstructure. 15 Earthquakes and vol keisteric bodily function Earthquakes a good deal occur in volcanic regions and are caused there, both bytectonicfaults and the movement ofmagmainvolcanoes. Such earthquakes can serve as an early pattern of volcanic eruptions, as during theMount St. Helenseruption of 1980. 16Earthquake spuds can serve as markers for the attitude of the flowing magma throughout the volcanoes. These swarms can be bear witnessed by seismometers andtiltmeters(a device that measures scope slope) and used as sensors to predict close at hand(predicate) or upcoming eruptions. 17 breakage dynamicsA tectonic earthquake begins by an initial rupture at a point on the fault surface, a process cognise as nucleation. The outstrip of the nucleation zone is uncertain, with some evidence, such as the rupture dimensions of the slimest earthquakes, nominateing that it is little than 100 m while other evidence, such as a piece of tail component revealed by low- relative frequency spectra of some earthquakes, suggest that it is wider. The possibility that the nucleation involves some sort of dressing process is punted by the observation that about 40% of earthquakes are preceded by fore infracts.Once the rupture has initiated it begins to propagate along the fault surface. The mechanics of this process are seriously unders excessivelyd, partly because it is difficult to re compel the high sliding velocities in a laboratory. similarly the effectuate of strong prime motion make it very difficult to record information close to a nucleation zone. 18 Rupture propagation is generally modeled apply afracture mechanicsapproach, equate the rupture to a propagating mixed mode shear crack. The rupture stop number is a function of the fracture energy in the volume around the crack tip, increasing with decreasing fracture energy.The stop number of rupture propagation is orders of magnitude swift than the shifting velocity crossways the fault. Earthquake ruptures typically propagate at velocities that are in the range 7090% of the S- gesticulate velocity and this is independent of earthquake size. A dispirited subset of earthquake ruptures appear to have propagated at speedings greater than the S-wave velocity. Thesesupershear earthquakeshave all been sight during large strike-slip events. The unusually wide zone of coseismic scathe caused by the2001 Kunlun earthquakehas been attri plainlyed to the set up of thesonic boom genuine in such earthquakes.Some earthquake ruptures excursion at unusually low velocities and are referred to asslow earthquakes. A oddly dangerous form of slow earthquake is thetsunami earthquake, observed where the relatively low snarl intensities, caused by the slow propagation speed of some great earthquakes, fail to jocund the population of the neighbouring coast, as in the1896 Meiji-Sanr iku earthquake. 18 tidal forces See besidesEarthquake farsightednessTides Research work has shown a spicy correlation between small tidally spend a penny forces and non-volcanic tremor activity. 19202122 Earthquake clusters Most earthquakes form part of a sequence, related to each other in terms of location and time. 23Most earthquake clusters consist of small tremors that cause little to no damage, but there is a theory that earthquakes can recur in a regular warning. 24 Aftershocks Main articleAftershock An subsequentlyshock is an earthquake that occurs later a previous earthquake, the mainshock. An aftershock is in the alike region of the main shock but always of a smaller magnitude.If an aftershock is larger than the main shock, the aftershock is redesignated as the main shock and the original main shock is redesignated as aforeshock. Aftershocks are formed as the crust around the displacedfault planeadjusts to the personal effects of the main shock. 23 Earthquake swarms Main articleEarthquake swarm Earthquake swarms are sequences of earthquakes striking in a specific area within a short period of time. They are different from earthquakes followed by a series ofaftershocksby the fact that no single earthquake in the sequence is obviously the main shock, therefore none have remark higher magnitudes than the other.An example of an earthquake swarm is the 2004 activity atYellowstone National Park. 25 Earthquake storms Main articleEarthquake storm some clock a series of earthquakes occur in a sort ofearthquake storm, where the earthquakes strike a fault in clusters, each triggered by the shaking or stress redistribution of the previous earthquakes. Similar toaftershocksbut on adjacent segments of fault, these storms occur over the hang of years, and with some of the later earthquakes as detrimental as the early ones.Such a pattern was observed in the sequence of about a dozen earthquakes that struck theNorth Anatolian Faultin Turkey in the twentie th cytosine and has been inferred for older paradoxical clusters of large earthquakes in the Middle East. 2627 &8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212- size of it and frequency of occurrence It is estimated that around 500,000 earthquakes occur each year, detectable with current instrumentation. slightly 100,000 of these can be felt. 2829Minor earthquakes occur nearly constantly around the military personnel in places likeCaliforniaandAlaskain the U. S. , as well as nMexico,Guatemala,Chile,Peru,Indonesia,Iran,Pakistan, theAzoresinPortugal,Turkey,New Zealand,Greece,Italy, andJapan, but earthquakes can occur almost anywhere, includingNew York City,London, andAustralia. 30bigger earthquakes occur less frequently, the relationship beingexponential for example, roughly ten times as many earthquakes larger than magnitude 4 occur in a particular time period than earthquakes larger than magnitude 5. In the (low seismicity) United Kingdom, for ex ample, it has been calculated that the total recurrences are an earthquake of 3. 4. 6 every year, an earthquake of 4. 75. 5 every 10years, and an earthquake of 5. 6 or larger every 100years. 31This is an example of theGutenberg-Richter law. TheMessina earthquakeand tsunami took as many as 200,000 lives on December 28, 1908 inSicilyandCalabria. 32 The number of seismic stations has increase from about 350 in 1931 to many thousands today. As a result, many more earthquakes are reported than in the past, but this is because of the spacious extenuatement in instrumentation, rather than an increase in the number of earthquakes.TheUnited States geologic look backestimates that, since 1900, there have been an average of 18 major earthquakes (magnitude 7. 07. 9) and one great earthquake (magnitude 8. 0 or greater) per year, and that this average has been relatively stable. 33In recent years, the number of major earthquakes per year has decreased, though this is probably a statistical mutant rather than a systematic trend. citation needed more than detailed statistics on the size and frequency of earthquakes is available from theUnited States Geological Survey(USGS). 34A recent increase in the number of major earthquakes has been noted, which could be explained by a cyclical pattern of periods of deep tectonic activity, interspersed with longer periods of low-intensity. However, accurate recordings of earthquakes only began in the early 1900s, so it is too early to categorically state that this is the case. 35 Most of the worlds earthquakes (90%, and 81% of the largest) take place in the 40,000km long, horseshoe-shaped zone called the circum-Pacific seismic belt, know as thePacific Ring of Fire, which for the most part bounds thePacific Plate. 3637 great earthquakes tend to occur along other plate boundaries, too, such as along theHimalayan Mountains. 38 With the rapid growth ofmega-citiessuch asMexico City,TokyoandTehran, in areas of highseismic risk, some se ismologists are warning that a single quake may claim the lives of up to 3 one million million slew. 39 &8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212- induce seismicity Main articleInduced seismicity While most earthquakes are caused by movement of the Earthstectonic plates, human activity can besides produce earthquakes.Four main activities contribute to this phenomenon storing large measuring sticks of water behind adam(and possibly twist an extremely heavybuilding), drilling and injecting bland intowells, and by blacken miningand embrocate drilling. 40Perhaps the best known example is the2008 Sichuan earthquakein ChinasSichuan Provincein May this tremor resulted in 69,227 fatalities and is thenineteenth deadliest earthquake of all time. TheZipingpu Damis believed to have fluctuated the pressure of the fault 1,650 feet (503m) away this pressure probably increased the power of the earthquake and accelerated the rate of movement for the fault. 41The greatest earthquake in Australias history is also claimed to be induced by humanity, through coal mining. The city of Newcastlewas built over a large sector of coal mining areas. The earthquake has been reported to be spawned from a fault that reactivated due to the millions of tonnes of rock removed in the mining process. 42 &8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212- measuring stick and locating earthquakes Main articleSeismology Earthquakes can be enter by seismometers up to great places, becauseseismic waves transit through the wholeEarths interior.The absolute magnitude of a quake is conventionally reported by numbers on theMoment magnitude scale(formerly Richter scale, magnitude 7 create serious damage over large areas), whereas the felt magnitude is reported using the modifiedMercalli intensity scale(intensity IIXII). all tremor produces different types of seismic waves, which travel through rock with different velocities * lo ngitudinalP-waves(shock- or pressure waves) * TransverseS-waves(both physiologic structure waves) * Surface waves (RayleighandLovewaves) Propagation velocityof the seismic waves ranges from approx. km/s up to 13km/s, depending on the slow-wittednessandelasticityof the medium. In the Earths interior the shock- or P waves travel much faster than the S waves (approx. relation 1. 7 1). The differences intravel timefrom theepicentreto the scout are a measure of the distance and can be used to picture show both sources of quakes and structures within the Earth. Also the depth of thehypocentercan be computed roughly. In self-coloured rock P-waves travel at about 6 to 7km per succor the velocity increases within the deep mantle to 13km/s.The velocity of S-waves ranges from 23km/s in light sediments and 45km/s in the Earths crust up to 7km/s in the deep mantle. As a consequence, the for the first time waves of a distant earthquake move in at an observatory via the Earths mantle. Rule of pitch On the average, the kilometer distance to the earthquake is the number of seconds between the P and S wavetimes 8. 43Slight deviations are caused by inhomogeneities of subsurface structure. By such analyses of seismograms the Earths core was located in 1913 byBeno Gutenberg.Earthquakes are not only categorised by their magnitude but also by the place where they occur. The world is split up into 754Flinn-Engdahl regions(F-E regions), which are based on governmental and geographical boundaries as well as seismic activity. More active zones are divided into smaller F-E regions whereas less active zones belong to larger F-E regions. &8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212- Effects of earthquakes 1755 shit engraving depictingLisbonin ruins and in flames after the1755 Lisbon earthquake, which killed an estimated 60,000 people. Atsunamioverwhelms the ships in the harbor.The effects of earthquakes include, but are not confine to, the following Shaking and shew rupture Damaged buildings inPort-au-Prince,Haiti, January 2010. Shaking and nation rupture are the main effects created by earthquakes, principally resulting in more or less knockout damage to buildings and other rigid structures. The severity of the local anesthetic effects depends on the complex combination of the earthquakemagnitude, the distance from theepicentre, and the local geologic and geomorphological conditions, which may amplify or reducewave propagation. 44The basis-shaking is measured byground acceleration.Specific local geological, geomorphological, and geostructural features can induce high levels of shaking on the ground surface even from low-intensity earthquakes. This effect is called spot or local amplification. It is principally due to the transfer of theseismicmotion from intemperately deep soils to soft superficial soils and to effects of seismic energy focalization owing to typical geometrical setting of the deposits. grounds rupture is a visible suspension and displacement of the Earths surface along the run along of the fault, which may be of the order of several(prenominal) metres in the case of major earthquakes.Ground rupture is a major risk for large engineering structures such asdams, bridge andnuclear power stationsand requires calculated mapping of existing faults to identify any which are likely to break the ground surface within the living of the structure. 45 landslips and avalanches Main articleLandslide Earthquakes, along with severe storms, volcanic activity, coastal wave attack, and wildfires, can produce slope instability leash to landslides, a major geological hazard. Landslide danger may persist while emergency personnel are attempting rescue. 46 FiresFires of the1906 San Francisco earthquake Earthquakes can causefiresby negativeelectrical poweror flatulence lines. In the event of water mains rupturing and a prejudice of pressure, it may also become difficult to stop the sprea d of a fire once it has started. For example, more deaths in the1906 San Francisco earthquakewere caused by fire than by the earthquake itself. 47 Soil liquefaction Main articleSoil liquefaction Soil liquefaction occurs when, because of the shaking, water-saturatedgranular square (such as sand) temporarily loses its strength and transforms from asolidto aliquid.Soil liquefaction may cause rigid structures, like buildings and bridges, to tilt or sink into the liquefied deposits. This can be a devastating effect of earthquakes. For example, in the1964 Alaska earthquake, soil liquefaction caused many buildings to sink into the ground, in the end collapsing upon themselves. 48 Tsunami The tsunami of the2004 Indian Ocean earthquake A large ferry boat rests midland amidst destroyed houses after a 9. 0earthquakeand subsequent tsunami struck Japan in March 2011. Main articleTsunami Tsunamis are long-wavelength, long-period sea waves produced by the sudden or abrupt movement of large volum es of water.In the render ocean the distance between wave crests can surpass 100 kilometers (62mi), and the wave periods can vary from five proceeding to one min. Such tsunamis travel 600-800kilometers per hour (373497 miles per hour), depending on water depth. Large waves produced by an earthquake or a torpedo landslide can overrun nigh coastal areas in a function of minutes. Tsunamis can also travel thousands of kilometers across open ocean and wreak final stage on far shores hours after the earthquake that generated them. 49 Ordinarily, subduction earthquakes under magnitude 7. on the Richter scale do not cause tsunamis, although some instances of this have been preserve. Most destructive tsunamis are caused by earthquakes of magnitude 7. 5 or more. 49 Floods Main articleFlood A flood is an overflow of any amount of water that reaches land. 50Floods occur usually when the volume of water within a eubstance of water, such as a river or lake, exceeds the total capacity of t he formation, and as a result some of the water flows or sits outside of the normal perimeter of the body. However, floods may be secondary effects of earthquakes, if dams are damaged.Earthquakes may cause landslips to dam rivers, which crush and cause floods. 51 The terrain below theSarez LakeinTajikistanis in danger of catastrophic flood if thelandslide damformed by the earthquake, known as theUsoi Dam, were to fail during a approaching earthquake. Impact projections suggest the flood could be active roughly 5million people. 52 human being reachs An earthquake may cause wound and loss of life, road and bridge damage, generalproperty damage(which may or may not be cover byearthquake insurance), and collapse or destabilization (potentially leading to future collapse) of buildings.The slipstream may bringdisease, lack of staple necessities, and higher insurance premiums. &8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212- Major earthquakes Earthqu akes of magnitude 8. 0 and greater since 1900. The apparent 3D volumes of the bubbles are linearly proportional to their various(prenominal) fatalities. 53 Main articleList of earthquakes one(a) of the most devastating earthquakes in recorded history occurred on 23 January 1556 in theShaanxiprovince, China, killing more than 830,000 people (see1556 Shaanxi earthquake). 54Most of the population in the area at the time lived inyaodongs, artificial caves inloesscliffs, many of which collapsed during the catastrophe with great loss of life. The1976 Tangshan earthquake, with a death toll estimated to be between 240,000 to 655,000, is believed to be the largest earthquake of the 20th century by death toll. 55 The1960 Chilean Earthquakeis the largest earthquake that has been measured on a seismograph, reaching 9. 5 magnitude on 22 May 1960. 2829Its epicenter was near Canete, Chile.The energy released was approximately in two ways that of the next most powerful earthquake, the commodity Friday Earthquake, which was centered inPrince William Sound, Alaska. 5657The ten largest recorded earthquakes have all beenmegathrust earthquakes however, of these ten, only the2004 Indian Ocean earthquakeis simultaneously one of the deadliest earthquakes in history. Earthquakes that caused the greatest loss of life, while powerful, were deadly because of their proximity to either heavily populated areas or the ocean, where earthquakes often createtsunamisthat can devastate communities thousands of kilometers away.Regions most at risk for great loss of life include those where earthquakes are relatively antiquated but powerful, and poor regions with lax, unenforced, or innocent seismic building codes. &8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212- Prediction Main articleEarthquake prediction Many methods have been substantial for predicting the time and place in which earthquakes will occur. Despite considerable research efforts byseismologists , scientifically uniform predictions cannot yet be made to a specific day or month. 58However, for well-understood faults the chance that a segment may rupture during the next few decades can be estimated. 59 Earthquake warning systemshave been developed that can provide regional poster of an earthquake in progress, but out front the ground surface has begun to move, potentially allowing people within the systems range to seek shelter before the earthquakes impact is felt. &8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212- Preparedness The bearing ofearthquake engineeringis to foresee the impact of earthquakes on buildings and other structures and to design such structures to minimize the risk of damage.Existing structures can be modified byseismic retrofittingto improve their resistance to earthquakes. Earthquake insurancecan provide building owners with financial surety against losses resulting from earthquakes. Emergency managementstrategies c an be employed by a government or organization to mitigate risks and prepare for consequences. &8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212- Historical views An image from a 1557 book From the lifetime of the Greek philosopherAnaxagorasin the 5th century BCE to the 14th century CE, earthquakes were usually attributed to air (vapors) in the cavities of the Earth. 60Thalesof Miletus, who lived from 625547 (BCE) was the only documented person who believed that earthquakes were caused by tension between the earth and water. 60Other theories existed, including the Greek philosopher Anaxamines (585526 BCE) beliefs that short incline episodes of dryness and wetness caused seismic activity. The Greek philosopher Democritus (460371 BCE) blamed water in general for earthquakes. 60Pliny the Eldercalled earthquakes underground thunderstorms. 60 &8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212&8212- Earthquakes in culture Mythology and religionInNorse novelology, earthquakes were explained as the knock-down-and-drag-out struggling of the godLoki. When Loki,godof hurt and strife, murderedBaldr, god of beauty and light, he was punished by being bound in a cave with a poisonous serpent placed above his head dripping venom. Lokis wifeSigynstood by him with a bowl to catch the poison, but whenever she had to empty the bowl the poison dripped on Lokis face, forcing him to jerk his head away and work against his bonds, which caused the earth to tremble. 61 InGreek mythology,Poseidonwas the cause and god of earthquakes.When he was in a bad mood, he struck the ground with atrident, causing earthquakes and other calamities. He also used earthquakes to punish and inspect fear upon people as revenge. 62 InJapanese mythology,Namazu(? ) is a giant lancetfishwho causes earthquakes. Namazu lives in the mud beneath the earth, and is watch over by the godKashimawho restrains the fish with a stone. When Kashima lets his gu ard fall, Namazu thrashes about, causing violent earthquakes. usual culture In modern habitual culture, the portrayal of earthquakes is shaped by the repositing of great cities laid waste, such asKobe in 1995orSan Francisco in 1906. 63 sham earthquakes tend to strike suddenly and without warning. 63For this reason, stories about earthquakes generally begin with the disaster and focus on its immediate race, as inShort Walk to Daylight(1972),The rag Edge(1968) orAftershock Earthquake in New York(1998). 63A notable example is Heinrich von Kleists classic novella,The Earthquake in Chile, which describes the dying of Santiago in 1647. Haruki Murakamis short apologue collectionafter the quakedepicts the consequences of the Kobe earthquake of 1995.The most popular single earthquake in fiction is the hypothetical Big One expected ofCaliforniasSan Andreas Faultsomeday, as depicted in the novelsRichter 10(1996) and pass California(1977) among other works. 63Jacob M. Appels widely anthol ogized short story,A Comparative Seismology, features a con artist who convinces an elderly woman that an revelatory earthquake is imminent. 64InPleasure ride in Lituya Bay, one of the stories inJim Shepards desire Youd Understand, Anyway, the Big One leads to an even more devastating tsunami.In the film2012(2009), solar flares (geologically implausibly) touch on the Earths core caused massive destabilization of the Earths crust layers. This created closing planet-wide with earthquakes and tsunamis, foreseen by theMayanculture and myth surrounding the last year noted in theMesoamerican calendar2012. modern-day depictions of earthquakes in film are variable star in the manner in which they radiate human psychological reactions to the actual suffering that can be caused to directly disconcert families and their loved ones. 65Disaster mental health response research emphasizes the need to be aware of the different roles of loss of family and key community members, loss of home and well-known(prenominal) surroundings, loss of essential supplies and services to carry survival. 6667Particularly for children, the clear availability of caregiving adults who are able to protect, nourish, and clothe them in the aftermath of the earthquake, and to help them make sense of what has befallen them has been shown even more important to their emotional and physical health than the simple giving of provisions. 68As was observed after other disasters involving destruction and loss of life and their media depictions, such as those of the 2001 World Trade Center Attacks or Hurricane Katrinaand has been recently observed in the2010 Haiti earthquake, it is also important not to pathologize the reactions to loss and displacement or disruption of governmental cheek and services, but rather to validate these reactions, to support constructive problem-solving and reflection as to how one might improve the conditions of those affected. 69

Orlando Garcia, Jr. vs. Ranida and Ramon Salvador Essay

Orlando Garcia, Jr. (Community diagnostics reduce) vs. Ranida and Ramon Salvador G.R. No. 168512 parade 20, 2007FACTSanswerer Ranida Salvador underwent a medical enquiry at the Community Diagnostics Center (CDC) as a prerequisite for repair employment. Garcia, a medical technologist, conducted the HBs Ag (Hepatitis B Surface Antigen) block out. On October 22, 1993, CDC issued the essay conduct indicating that Ranida was HBs Ag Reactive. The result bore the material body and signature of Garcia as examiner and the good-for-nothing stamp signature of Dr. Castro as diagnostician. When Ranida submitted the foot race result to Dr. Sto. Domingo, the partnership mendelevium, the latter apprised her that the findings indicated that she is ugly from Hepatitis B, a liver disease.Thus, based on the medical report submitted by Sto. Domingo, the Company terminated Ranidas employment for helplessness the physical examination. It was later determined that on that point was an error in the previous examination and that the respondent was not suffering from Hepatitis B. Respondent was rehired by the company. ISSUEWhether Garcia (CDC) is liable for restoration to the respondents for issuing an incorrect HBsAG test result. HELDThe cost held that CDC was negligent because there was no pass physician in CDC as need by law. CDC is not administered, directed and superintend by a accredited physician as required by law, unless by Ma. Ruby C. Calderon, a licensed Medical Technologist. In the License to pass on and Operate a Clinical science laboratory for the years 1993 and 1996 issued by Dr. Juan R. Naagas, M.D., Undersecretary for health Facilities, Standards and Regulation, defendant-appellee Castro was named as the head of CDC. However, defendant pathologist is not the owner of the Community Diagnostic Center nor an employee of the same nor the employer of its employees.Defendant pathologist comes to the Community Diagnostic Center when and where a proble m is referred to him. Castros infrequent trounce to the clinical laboratory barely qualifies as an effective administrative supervision and run across over the activities in the laboratory. Supervision and instruction means the authority to act instantaneously whenever a specific function is entrusted by law or regulation to a subordinate direct the performance of handicraft restrain the commission of acts review, approve, revise or modify acts and decisions of subordinate officials or units. Moreover, Garcia conducted the HBsAG test of respondent Ranida without the supervision of defendant-appellee Castro. Lastly, the disputed HBsAG test result was released to respondent Ranida without the authorization of defendant-appellee Castro.

Diabetes as Disorder

DESCRIPTIONDiabetes pertains to a metabolous disorder that is associated with the lack or absence seizure seizure of insulin, a protein that transports glucose into the cells of the physical structure. Glucose, likewise simply know as dulcorates, is considered as the first stock of dynamism for the daily activities performed by the clement body, such as walking and standing.In addition, glucose besides serves as the main resource for the energy that is required to fuel cellular processes at bottom the body, including that of growth and repair of cells and tissues. The pabulum items consumed by an individual generally contain glucose and therefromly the presence of insulin is important for the transport of this supermolecule to the appropriate regions of the body.Insulin is mainly produced by the pancreas, which is a digestive organ that is st locategically laid next to the small intestines, where digestion commonly occurs. erstwhile the process of digestion has been co mpleted in the intestines, the glucose molecules transported into cells through with(predicate) and through the help of insulin. In traffic pattern individuals, the substance of insulin produced by the pancreas is enough to transport the glucose that is correspond in the meal consumed.On the former(a) hand, individuals with diabetes testify a lack or absence of insulin secreted by the pancreas, thus preventing the transport of the glucose molecules into the cells. Glucose is whence left outside the cells and these remain move in the blood. The continuous accumulation of glucose un slight extends from the blood to the urine, which in turn ar samples employed for the diagnostics of diabetes.CAUSES OF DIABETESDiabetes is generally caused by a number of factors, depending on the graphic symbol of diabetes that has been positively diagnosed in an individual. theatrical role 1 diabetes, overly known as insulin-dependent diabetes mellitus (NIDDM), pertains to an autoimmune ana tomy that involves the incapacity of the body to combat infections (NIH, 2010a).In this case, the immune system of an individual causes the ending of the cells of the pancreas, thus decreasing and possibly preventing the business of insulin for glucose transport. The actual mechanism that triggers the destruction of the pancreatic cells by the immune system is dormant unknown and there ar sprightly efforts in the field of biomedical explore that be attempting to elucidate this reaction.Type 2 diabetes, also known as non-insulin dependent diabetes mellitus (NIDDM), pertains to an add-on in the direct of glucose in the body due to aging, obesity or transmittable inheritance of the condition (NIH, 2010b). Type 2 diabetes is therefore more commonly observe among elderly individuals, as their metabolic rate generally slows down as they age. round individuals tend to develop diabetes because their food choices are often different from the recommended daily diet, thus chan ge magnitude the likelihood that sugar-rich foods would be consumed on a regular basis.Gestational diabetes pertains to the subjoin in the blood glucose level of a muliebrityish during pregnancy. This occurrence is usually linked to the establish in the total body charge of a woman during pregnancy, as wellhead as the decrease in the physical activity of the woman as she progresses through the entire gestational period of 36 weeks or 9 months. Unlike causes 1 and 2 diabetes, gestational diabetes often disappears once the woman has given birth. The disappearance of the features of diabetes are possibly linked to the loss in the total body weight later on birth, as well as the increase in the physical activity of the woman after delivery.EPIDEMIOLOGY OF DIABETESType 1 diabetes generally affects both(prenominal) males and females, yet there are certain(a) characteristics that strongly associated with this metabolic disease. According to the demesne Health Organization, type 1 diabetes is more common among whites and is considered as a grand disease among non-white populations of Africa and Asia. Type 2 diabetes, on the other hand, is commonly diagnosed in elderly individuals.Moreover, elderly individuals who are overweight are more likely to develop type 2 diabetes because these individuals tend to be less active in physical activities. trusted populations are thus associated with type 2 diabetes, including those of African and Asian ethnicities. In the get together States alone, there are 24 meg individuals with the age of 20 years hoary and above that have been diagnosed with diabetes (NIDDK, 2007). On the other hand, there are 12 meg elderly individuals who have been diagnosed with diabetes in the join States.TREATMENT OF DIABETESType 1 diabetes is generally treated with the organisation of insulin on a daily basis. diligent are therefore taught how to inject insulin everyday, in order to maintain a normal level of insulin in their blood. Type 2 diabetes is usually treated with medications that assist in the digestion of glucose from the food items consumed. This medication is given on a daily basis utilise a tablet or enclose format. In addition to medications, a rosy diet is highly recommended to diabetic patients. This includes food items that are low in sugar content, such as green, leafy vegetables and fiber-rich fruits and grains.Exercise is also recommended for diabetic patients, as this assists in increasing the metabolic rate of the body. Diabetic patients are also educated on the condition of hypoglycemia, which is the extreme lowering of the blood glucose level of the body, resulting in fainting and a decrease in the arterial blood pressure. A dietitian therefore plays an important role in the design of the dietary regimen of diabetic patients. A regular check-up should also be performed every 3 to 6 months, wherein the temperance blood sugar levels are determined, in order to evaluate the progress of the patient with the current dietary regimen.REFERENCESNational Institute of Diabetes and digestive and Kidney Diseases. (2007). National Diabetes Statistics, 2007. Downloaded from http//diabetes.niddk.nih.gov/dm/pubs/statistics/DM_Statistics.pdf on July 8, 2010.National Institutes of Health. (2010a). Type 1 diabetes cardinal years of progress. Downloaded from http//www.nih.gov/ to the highest degree/researchresultsforthepublic/Type1Diabetes.pdf on July 8, 2010.National Institutes of Health. (2010b). Type 2 diabetes Thirty years of progress. Downloaded from http//www.nih.gov/about/researchresultsforthepublic/Type2Diabetes.pdf on July 8, 2010.

Plato, Descartes, and The Matrix Essay

Consider this, Is what we weigh to be strong and true hearty and true? In the moving-picture show The Matrix, modern is a ready reckoner programer by day and hacker by night. He senses that something is wrong with the human race moreoer insists what he know he feels. When he woolgathers, he isnt sure if it was hearty or just a dream just as Descartes believes he potty non self-confidence his senses to announce him whether or not he is still dreaming. neo meets with Morpheus and Morpheus gives modern the natural selection of knowing the equity. According to Morpheus the arena isnt real, it is an illusion and offers modern a feel altering choice. To take a check that will give him the truth.The truth Morpheus refers to is that the world Neo believes in is just an illusion. What Neo perceives as real by his senses is cipher more than a computer generating ideas in his head without any real experiences. Morpheus gives Neo the option of continuing to live his sustena nce in the shadows and the port he perceives it or to rule the light and the truth. This closely resembles the simile of the cave by Pluto. Plato invites us to animadvert humans being held captives, with no liberty to move or see get out what is directly in front of them in the form of shadows. This is the prisoners macrocosm.This is what they come to believe is real. When in-fact on that point is another world just beyond their reality. It is solo after one prisoner escapes the shackles and chains and finds that the actual world is not just shadows but a world with the light of the sun. The prisoner has difficulty adjusting his eye to the brightness, but eventually does. This experience parallels to what Neo experiences. Descartes poses the questions in his work Meditations of First Philosophy, 1961, of how we cannot for certain(p) that the world he experiences isnt not the product of an illusion forced upon him by an infernal demon.He questions what he believes is real because of what he sees and feels while dreaming and indeed cant trust his senses to tell him if 2he is still dreaming. When Neo requires the red tabloid and his perception of his biography slips a way of life when he realizes that the human race is held in containers, unconscious, with a computer generating their thoughts and experiences. Humans invented Artificial knowledge and in turn the AI took over mankind and enslaved them using them for the energy they postulate to stay alive.Neo realizes what Descartes proposed, that Neos life was just controlled by an evil demon, the Matrix. But Descartes went on to contend the existence of God, saying a wide-cut God would not let an evil demon control us. Neo struggles with this newfound truth because he didnt believe in fate because he didnt like the idea he wasnt in control of life. Neo life as he knew it is gone, and he is set about with the new reality and he struggles with the incompatible emotions first of shock, fear an d disbelief and wherefore acceptance.He joins the group of dissidents to help others see the truth and reality of life. Knowing the truth doesnt necessarily set you desolate as we find out. A lad dissident Cypher discovers the truth is unassailable and decides that ignorance is bliss. He negotiates a finagle to deliver Morpheus in turn for his old life. For Cypher, the truth was too oftentimes to handle, he liked the illusion of his introductory life. Once Neo gains knowledge of he Matrix, he is able to discern mingled with the truth and illusion and ascends to a high level of understanding.He realizes that he can no longer blindly accept information received through his senses, but must requires answers to his questions. He like Descartes comes to the conclusion I think, therefore I am. The difference between the Matrix and Plato and Descartes is the movie gives Neo a way screen to the physical real world whereas Plato and Descartes only suggest there is another reality and we are dreaming but doesnt give us a way back. None of the notables address God inwardly the realm of truth. God states he is the way of the light and the truth. We are challenged in our nonchalant lives to live a real life.