The Fundamentals Motives and Traits free essay sample

When you think of these three words; motives, goals, traits, what is the first thing that comes to mind? Are there similarities? How about differences? Before we discuss the differences between these three words, I believe Its Important to understand their meanings. Motive Is defined as the reason for doing or behaving In a certain way. Goal Is defined as something you want to achieve. Lastly, traits can be defined as a characteristic that distinguishes a person.So what are the differences between motives, goals, and traits? I believe traits are characteristics that stick with a person. A trait is almost a defining feature, something strict that allows you to remember a person. You may remember your friends by certain traits they have, whether it be height, hair color, or personality. It is possible for a trait to be subdued for a moment in time, but they never change for good. We will write a custom essay sample on The Fundamentals Motives and Traits or any similar topic specifically for you Do Not WasteYour Time HIRE WRITER Only 13.90 / page On the other hand, motives and goals can change on a day to day basis. These two can actually work together at times. You may set a goal to graduate from college, or receive a promotion at work. You can use positive motivation to work towards those goals. Unlike traits, these two may not stick with you forever. I believe motives and goals are perfect examples of characteristic adaptations. Characteristic adaptations come about In time, situation, and social roles.Some characteristic adaptations may change over time; they define the details of human individuality. The same goes for motives and goals. No one person has the same aspirations in life. We all create our own path and decided how we are going to get where we want to go. I hope that this has given you some insight into the deference between your goals, motives, and traits. You should now be able to find a clear definition of what your own personal traits are, and how to define your motives and goals.

What Is the PreACT

What Is the PreACT SAT / ACT Prep Online Guides and Tips Finally, a practice test from the ACT with a name that doesn't include a corny inspirational verb! That's right - the ACT is rolling out a new test called the PreACT this upcoming school year. It's similar to its SAT counterpart, the PSAT, although not exactly the same. In this article, I'll tell you what's on the PreACT, how its different from the PSAT, and what it means for you as a student. What Is the PreACT? The ACT recently announced that it will be adding a new test to its repertoire: the PreACT. It's a multiple-choice test aimed at preparing 10th grade students for the ACT. This new test seems poised to emerge as a competitor for the PSAT, although the ACT claims this was not the intention behind its creation. The ACT retired the ACT Explore (for 8th and 9th graders) and ACT Plan (for 10th graders) tests in 2014 to make way for the new ACT Aspire program (which is a set of standardized tests spanning grades 3-10).The PreACT is different from ACT Aspire tests because it serves as a way for students to see direct score predictionsbased on the same scale and content as the regular ACT. The PreACT has the same four multiple-choice sections as the regular ACT: English, Math, Reading, and Science. There is no Writing section. The test is also scored the same way as the regular ACT, on a scale from 1-36. The main difference is that it's considerably shorter. While the regular ACT is 2 hours and 55 minutes long (3 hours 35 minutes if you add the Writing section), the PreACT is only 1 hour and 55 minutes long. The questions on the exam will be questions from past ACTs that have been reformulated, so the difficulty level of the test is on par with the regular ACT. The point of the test is to help students get a better sense of where they would score on the real ACT and how much more they need to prepare before taking it. The PreACT will debut in the 2016-2017 school year. Schools and districts can choose to administer the test anytime between September 1st and June 1st. The changing of the seasons has no bearing on the PreACT. It is timeless. It is all around us. How Is the PreACT Different from the PSAT? The PreACT is different from the PSAT in a couple of significant ways. First of all, there's no scholarship competition associated with the PreACT. Its sole purpose is to prepare students for the ACT; scores will not have any direct effects on the college admissions process. It's genuinely just a practice tool. Another difference is that the test wil cost slightly less than the PSAT - it's $12 per student rather than $15. The SAT and the ACT are currently in a contentious battle for a greater share of the standardized testing market, so this move appears to be an attempt to further undercut the dominance of the PSAT. Schools can also administer the PreACT whenever they want during the year, whereas the PSAT has a specific October testing date with only one alternate date available. Offering greater flexibility is most likely another appeal to students and school districts who might be frustrated with the rigidity of the PSAT testing schedule. Students will be able to see the original PreACT questions and their answers within two weeks of taking the test. This is a much faster turnaround than the PSAT, which typically doesn't release scores until six weeks after the test. Your results will be piping hot when they're delivered. Don't burn your tongue. Remember, eating the score report is the only way to truly eliminate your mistakes. What Does This Mean for You? Ok, there's a new official practice test for the ACT. So what? Well, if you plan on taking the ACT as a junior, you might consider taking the PreACT in 10th grade to augment your prep efforts. Since it's made up of actual ACT questions, it will give you an accurate estimate of your score level and help diagnose your weaknesses so you can study strategically. Based on what we know about the PreACT so far, however, you should view it as an option rather than a necessity. If you're a motivated studier, you can take timed ACT practice tests, assess your mistakes, and get the same information about your strengths and weaknesses without handing over the cash equivalent of two Chipotle burritos. If you're more of a procrastinator, it might be a good idea to sign up for the PreACT. It will help you get familiar with the format of the ACT earlier than you would otherwise, and it does the grunt work of assessing your areas of weakness so you can start fixing them. Dust off that tool kit sitting in the back of your brain, and create a DIY masterpiece. What's Next? Do you really have to start preparing for standardized tests this early?Find out whether you should start studying for the ACT in 10th grade or hold off until a bit later. If you plan on taking the SAT instead of the ACT, you actually have two practice test options in 10th grade. Learn more about the difference between the PSAT 10 and the PSAT/NMSQT. When should you take the ACT for the first time? This article will give you the tools to decide on the best test date for your ACT debut. Want to improve your ACT score by 4+ points? Download our free guide to the top 5 strategies you need in your prep to improve your ACT score dramatically.

John Wayne Gacy Murder Trial Essay Example | Topics and Well Written Essays - 750 words

John Wayne Gacy Murder Trial - Essay Example Repetitive patterns were evident in his criminal acts. John Gacy’s criminality and psychopathy did not arise from nothing; possibly, there are development issues and life experiences that would have caused them. John Wayne Gacy Murder Trial Introduction John Wayne Gacy was an American who was convicted for murder and sexual assaults. Evidence indicated that between 1972 and 1978, he murdered and sexually assaulted at least 33 young men and teenage boys. Due to his serial killing he earned the tag â€Å"Killer Clown†. Also, evidence indicates that the defendant was living a double life; that of committing murders and that of engaging in political and charitable activities. Murder trials show that he was convicted of more murders than any other person in the American history. Based upon this historic murder trial, therefore, this paper will analyze the case and document and respond to a number of issues relating to the case (Mendenhall, 1996). Specific psychological chara cteristics and patterns that might be inferred about the individual Since the offences that the defendant committed were â€Å"unusual†, it is important to understand the specific psychological characteristics and patterns that might be inferred about him. The testimony that was made during the trial indicated that Gacy had psychological characteristics and patterns that to a greater extent depicted his atrocious actions. Those who worked for him testified that he was violent and in most cases showed intention to commit sexual assaults; actually, they testified that they had survived sexual and violent encounters with him (Amirante and Broderick, 2011). Friends, family and his former employees also testified that Gacy had mood swings and was â€Å"awfully tricky†, a trait he used to succeed in handcuffing them. Most of the sixty witnesses who testified during trial took notice of these characteristics and patterns. Since such characteristics are often associated with t he insane, this was not the case with Gacy as psychologists had confirmed that he was sane, and he committed the offences while in sound mind. Psychologists and medical experts who testified for the defense agreed that he was very intelligent and generous. However, they also noted that he was schizophrenic; that is, he had antisocial behaviors or suffered from manifold personality disorder (Peck and Allan, 2001). A review of the individual’s signature and modus operandi In order to effectively execute his actions, John Gacy adopted his own specific signature and modus operandi. His signature and modus operandi enabled him to execute his actions with â€Å"efficient and effective† ease before he was eventually arrested. He admitted that his signature characteristic was to keep the people he had killed beneath his bed or in the attic for a number of hours prior to burying them later on (Kozenczak, 2003). His modus operandi is what enabled him to lure his victims easily a nd even sometimes manage to effortlessly trick them into being handcuffed so that he can execute his intentions. He would promise his victims employment opportunities in his construction company and then follow them up with alcohol. Once they were drunk, he would chloroform them and tie them to a chair. It should be noted that all his victims were male aged between 9 and 27 years. He sexually assaulted them, strangled them, or stuffed underwear into their mouths (Amirante and Broderick, 2011). When not using that tactic, he would drive around the town in search of

Taj Mahal Essay Example | Topics and Well Written Essays - 750 words

Taj Mahal - Essay Example Taj Mahal is one of the most visited places of interests in India by all tourists, especially foreigners for whom it is on top of their priority list. When you enter to see its front view - it is so ravishing that you are mesmerized. It seems as if a palace in brilliant architecture made in white marble is standing high in the sky before you. There is a story of true love behind the building of this monument. The fifth Mughal king Shah Jehan made this monument out of love for his beloved second wife, Mumtaz Mahal, to fulfil her wish on deathbed. She wanted the King to build a monument of their love to show it to the whole world. King Shah Jehan fulfiled her wish by building a miracle of white marble in the loving memory of his beloved wife. History says that the monument took 22 years to complete in 1653. That time, it cost 32 Million Rupees. The guide informs that it took twenty thousand workmen and expert craftsmen from countries like Persia, France, Iran, Italy and Turkey to build the Taj Mahal under the supervision of a Persian architect, Ustad Isa. As we are entering the main gateway, the guide informs that the length and width of the Taj Mahal complex measures 590x300m, including the main gateway called Darwaza, the equally proportioned garden measuring 300x300m, the Masjid or mosque, the Naqqar Khanna means rest house and the Rauza or the Taj Mahal mausoleum.

Etty Hillesum & Religion & Holocaust Research Paper

Etty Hillesum & Religion & Holocaust - Research Paper Example The theory that it was God's fault, Etty explained, was an easy way out. Man created this world (1940's) and its atrocities, because of lack of faith in God. Her faith and belief in God helped many get through the horrible times before being transferred to Auschwitz. She did feel life was absurd though there were things each individual person could gain. Religion was not wishful thinking. She had a special religious vocation which was beyond the understanding of the times and a little bit more comprehensible today. "Fear created the first Gods". Perhaps, Etty considered that fear also took spirituality away from most. "Moreover, life itself contradicts the most basic of human aspirations: to live without suffering and cruelty because most are not prepared in "healing the soul". Life require work on the soul. This sound trite as a phrase but it was her aspiration in turning suffering and cruelty into an experience where some benefit could begotten. She made a transition in 1943, as sh e actually felt it was not fair that she did not share the suffering of others and volunteered to be transferred.. There are different explanations of the Holocaust but non like Etty Hillesum. Her diaries written from 1941-1943 give an incredible outlook to how one young women dealt with the atrocities from looking within. She shared her inspirations with others. She inspired many. Ester Hillesum was born in the Netherlands January 15, 1914. She died in Auschwitz November 30 1943. One of the most influential person in her short life taught her the value of looking within for the necessary answers of one's problems . Julias Spier, a psycho-chirologist, studied with Carl Jung the technique of analyzing the lines of the hand. Etty met him in 1941 at a conference and then in therapy. He showed her the value of writing as a part of her therapy. In her letters, she refers to him as .S. Etty became his good friend and secretary. She continued writing her diaries for 3 years. They are writt en in the forms of letters representing a spiritual journey. She wished to become a journalist 'if she made it after the war'. S woke the God in her. She saw that God was omnipresent in all aspects of life. She had two tendencies in her letters: to write of the God within her; and to write of the God of creation and creatures. Towards the end of the diary she converges these two thoughts. "For once you have begun to walk with God, you need only keep on walking with Him and all of life becomes on long stroll ...such a marvellous feeling....(14/07/1942). She continued writing about God until the end of her life. God is within man. Because God could do nothing with what man was doing at this time in life (WWII), she said it was time for man to help God. Take care of his presence. Don't just offer him your tears and sadness but make his time he has with you as agreeable as possible. Hatred and anger are the easy route to take though you have every right to do so. Any element of moral in dignation touches the soul. One element of hatred, one atom more of hatred added to this world renders it even more disagreeable. Life is absurd, but man still has libre-arbitre over his proper soul. "This hatred and animosity which exist in others is also in us. I don't see any other solution other than cleaning our souls of this rot. We cannot improve the outside world without having made progress within ourselves. There is one lesson that can be learned from the war, the need to look within". A lite comparison done in 2011 would be going to a cancer waiting room, seeing everyone with sour faces. Bring a box of chocolates, or tell a joke for

Petrogenesis of the Basalts From Lanjiafan Formation

Petrogenesis of the Basalts From Lanjiafan Formation Chapter 5: Petrogenesis of the basalts from Lanjiafan Formation and Evaluation of Tectonic setting Most trends on variation diagrams are the result of mixing. Below consider some of the more important mixing process. 5.1 Alteration It is observed from the field evidence as well as petrography that the studied basalts are experienced varying degrees of alteration, which were observed by the presence of the secondary minerals such as calcite and a larger LOI varying from 3.87wt%-13wt%. Elements which are mobile during alteration include SiO2, CaO, Na2O, K2O, indicating that these major elements easily migrate with alteration occurs and low strength elements (Humphris et al., 1978). However, the high field strength elements (HFSE, such as Nb, Ta, Zr, Hf, Th, U, and Y) and the rare earth elements (REE) are relatively immobile in all even the most severe hydrothermal alteration (Pearce, 1975). In contrast, large LILE (LILEs, such as Cs, Rb, Sr, Rb, Pb and Ba) show no linear relation with zirconium. For this reason only high field strength elements Ti, Zr, Y, Nb, Ta, Hf, Th and REE have been used in the discussion of the source properties and petrogenesis of these mafic volcanic rocks. 5.2 Fractional crystallization Fractional crystallization is a major process in the evolution of many igneous rocks, and is frequently the cause of trends seen on variation diagrams for igneous rocks, especially basalts rocks. However, the basalts from the Lanjiafan Formation have Mg# varying from 46.2 to 89.3, slightly higher than those of the primitive mantle derived magmas (about 70-72; Irving and Green 1976; Frey et al., 1987). Besides, they are relatively low in Cr (0.68-37.8) and Ni (14-123), indicating a fractional crystallization to a certain degree in the magmatic chambers or during the ascending processes of the parental magma most likely of plagioclase (Xu et al., (2015). Accordingly, the petro graphical observations show the presence of plagioclase as the dominant mineral. For the alkaline basalts, the weak Eu and Sr anomalies imply a minor fraction crystallization of plagioclase, (Frey et al., 1978). For sub alkaline basalts, the negative Eu (0.58Niu et al, 2009, suggest fractionation crystallization. Therefore, in both alkaline and sub alkaline rocks experienced fractional crystallization. 5.3 Crustal contamination Generally, the compositional variation of magma is subject to different degrees of contamination by different crustal components during their ascent to the surface through continental crust, which changes the composition of magma (Manikyamba et al., 2014). Although it is difficult to assess crustal contamination without having isotope data, some critical geochemical characters may help to identify possible involvement of crustal material during emplacement of alkaline magmas. The basalts samples show a depletion in Nb, Ti, and Ta and a positive Pb anomaly, and some samples show an enrichment of LREE, indicating these samples may have been subjected to crustal contamination (Hawkesworth., 1984) or derived from the enriched lithospheric mantle (Wang et al., 2008). Nb-Ta and neighboring elements (Th, U and La) are not fractionated from each other during partial melting or fractional crystallization (Hofman., 1988), but the enrichment of the mantle source and the crustal contamination can significantly increase LILLE and LREE content and decrease HFSE/LILLE or HFSE/LREE ratios. For alkaline basalts, the higher Nb/Th (11.43-12.84), Nb/U (12.41-54.58) and Nb/La (1.28-1.89) ratios than those of the primitive mantle (Nb/Th=8.4; Nb/U=34; Nb/La=1.04; Sun and McDonough, 1989) values reflect the primary signature of the mantle sources with a significant involvement of crustal contamination in the alkaline basalts (fig 5.3.1). Thus, the alkaline basalts from Lanjiafan Formation were likely derived from a relatively less depleted mantle, and the alkali basaltic magmas were assimilated with minor crustal components. However, sub alkaline basalts show crust-like characteristics with obvious enrichment in Th, U, LREE and depletion in Nb, Ta (La/Nb>1), they have Nb/Th Although, sample D26-11 exhibit no visible HFSE depletion (La/Nb2.5ppm) and Th-U positive anomaly indicate contamination with upper crustal materials (fig 4.6 and 5.3.1). We consider that the primary magma must have experienced significant crustal contamination. Indeed, Fig 5.3.1 shows a general trend toward more crustal contribution from alkaline basalts. Trace-element ratio-ratio plots (fig 5.3.2) for these basalts show a good hyperbolic correlations between Lu/Hf and Hf/Yb, Lu/Hf and Zr/Yb, also indicating crustal contamination in the form of a binary mixing (Wang et al., 2008). 5.4 Nature of the mantle sources The basaltic magmas mainly originated in the continental lithospheric mantle or asthenospheric mantle. Turner et al (1995) presented the statistics of the worldwide continental flood basalts, the CaO/Al2O ratios for the basalts from the continental lithospheric mantle are less than 0.7 while those from the asthenospheric mantle are greater than 0.7. The basalts from western USA (Fitton et al., 1988) have La/Nb ratios greater than 1.5 if the basaltic magmas are derived from the lithospheric mantle, whereas those that originated from the asthenospheric mantle have ratios less than 1.5. As for the analyzed samples in this study, except for sample D26-7 and D26-8 with lower LOI, all of samples have CaO/Al2O ratios between 0.13 and 0.53 with a mean of 0.34 and La/Nb ratios from 0.53 to 0.85, indicating an asthenospheric mantle source. In addition, the La/Ta ratios (>30 for the lithospheric mantle) may also be considered as the discriminating index for the basaltic magmas (Deng et al., 2013). The La/Ta ratios for all of the analyzed samples from Lanjiafan Formation vary from 11.89 to 25.22, with an average of 15.44, indicating an asthenospheric mantle source as well. Although, differences in the degree of melting of mantle peridotite can lead to variation of TiO2 content in basal. Ewart et al., (1998) showed the basaltic magma from the asthenosphere has a relatively high Ti content (mean value of TiO2 in OIB’s is 2.86), while Ti content of basaltic magma from the lithosphere mantle is relatively low. High TiO2 content in alkali basalts rocks (2.46%-3.66%), mainl y comes from the asthenosphere mantle, except for D26-10 sample. For the tholeiitic samples TiO2 (0.44%-0.56%) content is low. 5.5. Evaluation of Tectonic setting Basaltic magmas are known to be emplaced in a variety of tectonic settings including intraplate continental or oceanic environments, intraplate rift zone settings, fast and slow spreading mid-oceanic ridges, island arcs, and back-arc basins (Pearce et al., 1973; Manikyamba et al., 2014). It is further demonstrated that, the Dabieshan orogenic belt has a complex evolution history, and different tectonic settings occurred in its southern and northern slopes in the Early Paleozoic (Ma et al., 2005). The enrichment in HFSE and LREE of the alkaline basalts may be directly derived from the asthenospheric mantle such as ocean island basalts (OIB) like source or the small degree partial melting of a normal-type MORB. On the other hand, contents of the basalts from Lanjiafan Formation suggest that the basaltic protoliths might have been derived from an enriched mantle source. The positive Eu anomaly points to the early plagioclase phenocryst accumulation in the magma chamber, may suggest that they originated from the plagioclase-bearing mantle reservoir and experienced the low degree of partial melting (Frey et al., 1987). As a result, the primary magma of the alkaline suite is possibly generated from the partial melting of the asthenospheric mantle caused by a mantle plume. However, the high contents of HFSE (e.g. Nb, Ti and Ta) relatively high Ti/Y (mostly >350), except for four samples (D26-7, D26-8, D26-10 and D26-11) and low Hf/Ta (mostly Even, the ratios of Zr/Y (10.00-12.47ppm) and Zr/Sm (29.20-34.38ppm) are similar to many intra-plate basalts (Zr/Y>3.5 and Zr/Sm So the alkali basalts from Lanjiafan Formation exhibit some characteristics of the within-plate basalts, they may have been derived from ocean floor, ocean plateau or mature back-arc basin basalts, because they have significant positive Nb anomalies (Floyd, 1989) (fig 4.6a). Most of oceanic island are generally considered to be related ascending plumes of hot mantle (Wilson, 1989). In conclusion the basalts from Lanjiafan Formation are likely formed in an extension-related within-plate environment probably induced by a mantle plume, rather than the supra-subduction zone. Chapter 6: Conclusion and Suggestions 6.1. Conclusion In summary, the Lanjiafan Formation is widely dominated by basaltic rocks, which are mostly alkaline rocks. These basalts contain basanite, trachyte, and rhyodacite. Through advanced Zircon dating method, we first obtained the ages of the of set of these basalts in the southwest Suizhou tectonic zone 459.5-464.4 Ma, which belong to the middle Ordovician, suggesting that a tectono-magma event affected the study area during Paleozoic, which might be the response to occurred of alkaline basalts in the Lanjiafan Formation. The CL images of zircon show that the zircons from the basaltic rocks are off magmatic type and most of them are euhedral. The basalts contain plagioclase phenocryst altered, magnetite, and calcite and pyroxene minerals. Geochemically, the analyzed basalts, which have a large variation of LOI, indicate that the basalts rocks from Lanjiafan Formation experienced of the strong alteration. These alkaline basalts present a weak Eu and Sr anomalies imply minor fraction crystallization of plagioclase, and suggesting that they undergone significant crustal contamination. Thus, the basalts from Lanjiafan Formation were likely derived from a relatively less depleted mantle, and the alkaline basaltic magmas were assimilated with minor crustal components. For sub alkaline basalts, the high Th content (>2.5ppm) and Th-U positive anomaly indicate contamination with upper crustal materials. The basalts from Lanjiafan Formation may be formed in an extension-related within-plate environment probably induced by a mantle plume. Being part of the South Qinling-South Dabieshan Paleozoic alkaline rock belt, the basalts from Lanjiafan Formation result from the Paleozoic extension-initial rifting in the northern margin of the Yangtze Craton.

A Reflection On Herman Melvilles Accomplishments :: essays research papers fc

A Reflection On Herman Melville's Accomplishments "As an author Melville both courted failure and scorned success."(pg. 613, A Companion to Melville Studies). How many famous legends in time have existed to know no fame. How many remarkable artist have lived and died never receiving due credit for there work. Herman Melville is clearly an artist of words. Herman Melville is certainly a prodigy when it comes to writing. Herman Melville never received hardly any credit for any of his works. Melville wrote such novels as Moby-Dick, and Billy Budd. Melville wrote about things that he knew about. He wrote about his own experiences. The one thing that he loved, and knew the most about was whaling. Herman Melville was born in 1819, the son of Allan and Maria Melville. He was one of a Family of eight children - four boys and four girls - who was raised comfortably in a nice neighborhood in New York City. Herman Melville came from a famous blood line out of Albany, NY. Melville's grandfather, General Peter Gansevoort, was a hero. Even though the General died six years before Melville was born, Melville still put him in his book, Pierre. On the outer side of the blood line there was Major Melville. The Major was a wealthy Boston merchant who was one of the famous "Mohawks" who boarded the ship of the East India Company that night of 1773, and dumped the cargo in to the Boston Harbor. Later Major Melville became the Naval Officer of The Port of Boston, a post given to him by Gorge Washington. It is like the two blood lines fitted together perfectly to create Herman Melville. Herman had the strength of the General, and the crazy hart of the Major. Herman Melville was "hardly more than a boy" when he ran out to sea after his fathers death. A young Melville sighed up as a boy on the St. Lawrence to Liverpool and back to New York. Many of the events that show up in Melville's Redburn are actuarial events that happened of his first voyage. After returning home and finding his mothers family fortune gone, Melville decided to take a journey over land this time to the Mississippi river to visit his Uncle Thomas. Through out all of Melville's work the image of inland landscapes, of farms, prairies, rivers, lakes, and forest recur as a counterpoint to the barren sea. Also in Moby-Dick Melville tells how he was a "Vagabond" on the Erie Canal, which was the way Melville returned. Melville wrote that it was not the lakes or forest that sank in as much