Three men in a boat summary Essay Example for Free

Three men in a boat summary Essay Pampady is a beautiful village in the Kottayam district of Kerala, India. Majority of the people there belonged to Orthodox Syrian Christian Denomination. Karinganamattom Family is one such old time, famous Orthodox Syrian Christian Family, a branch of which is the Moolakara Family into which Our Thirumeni was born. Parents of Thirumeni: Avira, Thirumenis paternal grandfather had two sons Kuruvilla and Chacko. Chacko married Ilachi from the Velukottu family from Veloor. They had four sons and six daughters. Thirumeni was the fifth child among the nine of them. He was born on 1060 Meenam, 24th according to the Malayalam System or on April 5th, 1885 (Sunday) according to the English Calendar. Thirumenis baptismal name is Kuriakose. Though our Thirumenis parents were not very rich, it never hindered their prayerful life. Thirumenis father used to teach the young Kuriakose prayers by making him sit on the fathers lap. Thirumenis mother taught him Psalms from his childhood days. All these instilled Thirumeni to lead a prayerful life from the very young days. House Of Thirumeni: Thirumenis father Chacko, built a house in the Pezhamattathu Plot. This was at the place called Patham Mile (10th Mile), North Of K. K. Road (Kottayam Kumily Road) around 20 km away from Kottayam town. This house was later donated to the Church to built a Kurishum Thotty (Cross) by the family members after the Heavenly Abode of Thirumeni. Now a big cross in the name of Pampady Thirumeni stands in the place where initially the house of Thirumeni was situated. Education: As per the usual custom that prevailed during those times, it was at the age of 5 (1890) that Thirumeni first started his official education. There was at that time, a small school at Karakuzha on the side of K K Road. Later this was moved near to the small church at Pampady. Hence from then on it came to be known as Pallivathulkal School (School near the Church Gate). At that time, a very famous teacher (Aashan) by the name of Madathil Raman Pilla Aashan was teaching there. There were two classes in this school with around 100 students. Class 1 was under Kushumbil Krishna  Pillai from Erivaloor. Class 2 was under Madathil Aashan. But, Madathil Aashan made it a point to look after the well being of all these 100 students of both these classes.Pallivathulkal School All that was taught in this school was the basic arithmetic and to read and write. Those who wanted to go for higher studies had to go to Kottayam, which was not possible at that time due to lack of conveyance. If a person studies for 4-5 years under Madathil Aashan, he would be proficient in all the required knowledge. Our Thirumeni was a very good student who had a craving for knowledge. He keenly listened to all that was taught in the class. Since he was an obedient and a quite child, he was liked by all. Madathil Aashan was well versed in Tamil. Thus most of his students also learned the same. Among them was our Thirumeni. This is the reason why Thirumeni maintained a good collection of Tamil books later. Character Of Thirumeni: 1890 was a time when caste system was at its peak. Many Nair students also studied with Thirumeni. They never used to go out for lunch as they were not supposed to touch or interact with the lower caste people. Thirumeni used to take Coconut and Molasses (Sharkara Thenga) for these students from home, so that they neednt stay hungry. Thus from the younger days Thirumeni had the habit of feeding all those who were hungry. This continued even when he grew up. Thirumeni was known for his hospitality far and wide. Never a person who came to see Thirumeni, returned empty handed!! Prayerful Influence Of Grandma: During the times when he studied under Madathil Aashan, Thirumeni stayed in the Moolakara Family with his Paternal Grandma Unnichi at his home in Pezhamatathu. His Grandma was a devoted servant of God who followed the prayers and lent religiously. She made it a point to tell Thirumeni devotional stories of Mother Mary and Parables of Jesus Christ. Thirumeni used to listen to all of them intensely. This created in Thirumeni a love for the prayerful life. Thirumeni and the Church: From the very young days, Thirumeni loved taking part in the Qurbana. He used to stand right in front of the church to have a full view of the Mass and even jostled his way up. He longed to serve on the madhbaha and take part  in the Holy Mass. The parish priests at that time: Rev Father Parapurathu, Rev Father Kochukulathil and Rev Father Aykarapadavil, helped Thirumeni fulfil his wish. He was so devoted in his duties that the achens decided to ordain him as a Priest. Many church fathers, including Kadavil Mar Athanasius Thirumeni told this news to Pampady Thirumenis father Chacko. But owing to financial difficulties at home, Chacko did not approve of the idea in the beginning. This denial of the offer led to several mishaps at their home, including Kuriakose nearly incapacitating his right hand in a crusher when he was feeding sugar cane into it. Thirumenis right hand had a slight handicap which led him to be a Left Hander. This made Chacko realize that Gods will was the supreme and it was not right to go against the Lord Gods decision. Realising his mistake, Chacko sent word of his willingness to have his son ordained. Kadavil Poulose Mar Athanasius Thirumeni Sub-Deaconship on 5 Feb, 1899 (Age of 14) Thirumeni was made the Sub-Deacon and given title of the Korooyo (sub-deacon) at the Pamapady Church on 5 Feb, 1899 at the age of fourteen by Poulose Mar Athanasios, who was in charge of the Kottayam diocese. Along with Thirumeni at that time itself, Rev Father O.C. Kuriakose of Kandathil and Alexanthrayose Kor Episcope of Kadavumbhagam was given the Sub -deaconship. Later he was elevated to the order of SHAMSHONO (Full-Deacon) Life as a Deacon: Immediately after he was made the Deacon, Thirumeni proceeded to the Old Seminary for his theological studies. The main Malpan (Teacher) at that time was Vattasheril Geevarghese Malpan. Scaria Malpan of Ilavanamannil, Alexanthrayose Malpan of Mattaykal and P. P Joseph Kathanar (Fr Joseph) of Chakkarakadavil were the other main teachers of Thirumeni. Every Monday morning Thirumeni would walk to Kottayam along with other Pastoral students and would return back on Friday. It was routine for Thirumeni to invite his friends home on Fridays. He enjoyed treating them with tasty food. This hospitality of Thirumeni is well known far and wide and continued till his last days. Slowly the young Deacon became well versed in Syriac Language, Biblical Knowledge and mastered theological treaties and sacraments. He was  a very good student who always respected his teachers and other scholars. His simple life style, discipline, humility and hard work made him a favourite among his teachers. Vattasseril Geevarghese Mar Dionysius (Main teacher of Pamapady Thirumeni) The First Miracle: The young deacon used to stay in Pampady when the seminary closed for vacation. He usually stayed in the Church and always took care to follow the Church Rituals. He used to regularly pray and fast. One year the villagers faced severe famine. All ponds and rivers dried up. All ran here and there in search of water. All crops were destroyed. During this time, on a Sunday after the Holy Mass, the young deacon declared that everyone should pray intensely for three days. Many of the devotees fasted and prayed for rain. But, some unbelievers took this as an opportunity to mock the young deacon. On the third day of the prayer, while congee (kanji / rice porridge) was being served to the poor people on the Northern side of the Church at the Chethimattom Field, the sky darkened and heavy down pour started!!! People had to move to the nearby homes to have their food. The deluge was so heavy that the vessels, like the Chempu (cauldron), in which the congee was made had to be tied to the nearby coconut trees so that they were not swept away in the torrent.Intense prayer of Thirumeni brought forth Heavy Rain Stay in Parumala Church: The young deacon stayed in Parumala seminary as per the instructions of his Holy Malpan, Vattasseril Geevarghese Mar Dionysius. He used to accompany the Malpan to various places. Some time after which Thirumeni got the deaconship, his father Chacko passed away. His father used to constantly worry about the young deacon due to lack of money. Thirumeni himself has told in many occasions that it was very difficult for him to buy even a pair of dress to be used in the Holy Mass. Thirumeni made it a routine to give clothes to the poor on the day of his fathers demise every year (29th of Kanni Masam). Parumala Seminary Ordination as Priest and Ramban: Vattasseril Malpan was impressed by the young deacons prayerful and disciplined life. He felt that the young deacon was apt to be ordained as  the Metropolitan. But before that he needed to be ordained as the Ramban. Thus on 8th July, 1906 the young deacon was ordained as the Kassisso (Full-Priest) by H.G Murimattathu Poulose Mar Ivanios (the first Catholicose of Malankara). The next day the Catholicose ordained him as the Ramban. Thus Pampady Thirumeni was consecrated as the Ramban (Rabban in Syriac) on 9th July, 1906 by the Catholicose H.G.Poulose Mar Ivanios at the Pampady Church. The next day Ramban solemnised his first Holy Mass. H.G Murimattathu Poulose Mar Ivanios (The first Catholicose of Malankara, who ordained Pampady Thirumeni as Kassisso and Ramban) Ramban in Pampady Church After being ordained as the Ramban on 9th July, 1906 by the Catholicose H.G. Poulose Mar Ivanios, Ramban stayed at the Pampady Church. It was during this time that the Pampady Church was rebuilt and the second floor was built to the Nadakashala. The beautiful paintings now seen in the Madbaha of the Church were also drawn during this time. Ramban used to announce in the Church about the planned work and the devotees used to gather together to do these work, which got over very quickly due to the united effort. Ramban was very particular that all the workers should be fed well. The people used to present Ramban with many eatables and harvests when they visited him. And all these were given away to the devotees who used to come to see Ramban. It should be noted that the more he gave, the more he used to get back. Rambans first teacher, Madathil Aashan still continued teaching in the Pallivathulkal school, adjacent to the church. It was Rambans another main hobby to present the students there with eatables. Thus Ramban was loved by one and all.Pampady Church Ramban in Parumala Seminary At this time, as per the instruction of Rambans Malpan H G Vattasseril Thirumeni, Ramban shifted to the Parumala seminary. There he served as the assistant of Kallasheril Punnose Ramban. The stay at Parumala Seminary, where Parumala Thirumenis body was laid to rest was indeed a spiritual renovation for the Ramban. His desire to follow the sanctified foot steps of Parumala Thirumeni raised the Ramban to great heights. He was also appointed to teach Syriac to the church scholars at Parumala Seminary. Vattasseril Thirumeni used to make Ramban write replies for his letters  from foreign lands like Sheema. Rambans Syriac letters were very beautiful and hence his hand writing very impressive. One day, His Grace Abdulla Patriarch, who was staying at the seminary asked Ramban to celebrate the Holy Qurbana. Though initially Ramban was a bit hesitant to Celebrate the Holy Mass in Syriac in front of the Patriarch, it finally resulted in everyone praising Ramban. Pampady Thirumeni as a Ramban Disciples Of Ramban During his stay in Parumala Seminary, Ramban got two disciples: Vattamala Abraham Deacon and Mannukaduppil Kuriakose Deacon. Ramban with the First Catholicose: When the First Catholicose, H.G Murimattathu Poulose Mar Ivanios was not well and was resting at Parumala Seminary, Ramban used to look after him with due care and love. The Catholicose used to term Ramban lovingly as My Ramban (Ente Rambachan). The Bava Thirumeni used to love Ramban so much. Bava played a major role in forcing the Ramban to become the Catholicose, when Vakathanam Kaaruchira Pilaksinos Metropolitan disagreed to continue as the Catholicose.Second Catholicose (Vakathanam Bava / Vailcattu Bava) Pothenpuram Hill Pothenpuram is a beautiful hill which interlocks the places Pampady and Meenadom. Pampady lies in the Eastern region of the hill and the rest is Meenadom. It was told that a deep hum was heard if someone stamps the Hill, and hence the origin of the name Pothenpuram. It is also believed that the name originated because there were many Bisons during that time and hence the name Pothenpuram. (A literal translation may well be Bison Back). Pigs, porcupines and bisons used to roam freely along this tract. Mar Kuriakose Dayara and the Church is situated on the raised plateau, amidst this hill.Pampady Dayara, amidst Pothenpuram Hill Placed centrally between Meenadom and Pampady, it invites co-operative effort from both Meenadom and Pampady region for its all round development. The mile long hill is skirted by fertile paddy fields yielding a rich harvest of mundakan and viruppu varieties of paddy. Till well into the 20th century human inhabitation was limited to the fringes of these paddy fields, it is said. The land was ideal for coconut and areca nut farms. Treated and processed areca nut found ready market in bordering Tamil Nadu areas. Traders from Tamil Nadu used to come and stay in Pothenpuram to deal in  Korappakku giving the name adakkakalom to one of the plain stretches on the hill. The Pothenpuram Hill was initially in the hands of an ancient aristocratic Nair family (Karthavu Family), who resided at a place called Kothala in Pampady. Later this family grew financially weak and hence the various regions of the Hill was sold to different people. Thus the place where the Dayara lies came in the hands of Madathil Aashan, the revered teacher of Pampady Thirumeni.Madathil Aashan Reason for the establishment of Dayara: In the mean time, Pampady Church was closed due to the fight between the two factions. This disturbed Rambans prayerful and pious life. It came to the extent that Ramban had to move away from the Church. It was indeed painful for Ramban to leave behind Pampady Church where he was staying the past ten years and which was his home church. One day, on the way to the Pallithazham school, Madathil Aashan visited Ramban. Seeing the grief-stricken face of Ramban, Aashan understood the situation. Ramban explained about the fight and the result of the same in a sorrowful tone. Aashan comforted the Ramban by suggesting that the Ramban make an ashram and a Church and to move over there. Ramban wanted to know how it could be done, as there was no money. Aashan assured that he would give the land and that the rest would all take place without any worry. Ramban conceded to his beloved masters advice. Ramban invited Cheriya Madathil Velyachan (Valiya Yacob Kathanar) also to see the place. Hence along with the Achan and Aashan, Ramban went and saw Pothenpuram. They liked it immensely and the registration took place on 15 Chingam, 1087. Construction of the Well: The construction of a well was started on 8th Idavom, 1089. Ramban used to come from Pampady to inspect the work. On 25th of that month, Ramban built a tent. On 31st, water was seen in the well. On 1st Midhunam, Ramban started staying in the tent there. After the construction of the well was over, Ramban thought about constructing the Dayara. But due to lack of money, it did not proceed. Instead Ramban decided to rent a house. But due to unavailability of a suitable house, even that idea was abandoned. Slowly Ramban, with the help of a few others started collecting money for the construction of Dayara from the people of Meenadom and Pampady. Construction of the Church: Ramban decided to build a temporary church there at the earliest. Thus the church was built at the place of the current Nadakashala of the Church. Ramban celebrated the Holy Mass for the first time here on 15th Makaram, 1090 along with the celebration of Mother Marys Festival of Seeds (vithu vila perunnal). Many people attended this function. Karinganamattathil Chacko used to stay with Ramban during this time, as a token of his love and respect for the Ramban.Church at Pampady Dayara Ramban: A Guardian for all Ramban soon became a guardian for those in and around the place. He used to take Syriac classes for the children and devoted his time in prayers. Everyday devotees used to bring fruits and other crops to the Dayara. All these were given away to those who came to visit Ramban. Ramban made it a point to show hospitality to who ever came to visit him and gave them food till their stomachs were full!! The same was the case with social service and alms giving.Ramban: Kuriakose Mar Gregorios Thabore Dayara: Soon after the church construction was over, on 13th Medom 1090, Vattasseril Mar Dionysius Thirumeni visited the Dayara. He liked the place very much and stayed there for three days and later proceeded to the Pazhaya Seminary. He christened the Dayara as Thabore Dayara. Ramban: A strict teacher Ramban was a very strict teacher. He used to beat even the best students if they showed lack in studies or indiscipline. Afterwards Ramban used to feel sad about the incident. He used to apply oil and hot water bags to the hurt areas. He also used to buy eatables and present to his disciples later. Church Re-Construction: The stone laying function of todays Dayara Church took place on 28th May, 1920. This was conducted by Yuyakim Mar Ivanios Metropolitan of Kandanad diocese. When the central pillar of the church was constructed, many witnessed a shining star in the sky. This took place in the after noon. The Church was consecrated on 20th January, 1923 by Geevarghese Mar Dionysius Thirumeni and Vakathanathu Mar Pilaksinos Thirumeni. Only very few know who and what Thomas the deaf and dumb, but remarkably loyal servant of Rambachan was or his daily chores in the service of his beloved master. Thomas came on Mithunam 18, 1090, as Rambachans cook. He belonged to the Ooppootil family of Veloor Karickamattom. His father was a regular help for the late Palampadom Vakil. Thomas has spoken at length, of course, in sign language to P.C Yohannan Ramban. Pottan as Thomas was called by some, was very intelligent and had a grasp of most things happening around him. He would take his part whenever he could contribute meaningfully. The way he pictured in sign language personages like Mahatma Gandhi, the Viceroy, Patriarch Bava, Wattacheril Thirumeni, Kurichi Valiya Bava Thirumeni and Julius Metropolitan has been quite memorable. He seemed to pose as though the whole of Pothenpuram was his own. Every tall coconut palm you see on the hill slopes was indeed planted by him, watered by him from the pond of Charothuparambil and Kizhakkemuri. Because they were fruits of his labour he would not part with any of the produce that Pothenpuram yielded. He would express himself without any reserve to anyone. In fact people around had some respect for his temper. He wouldnt even spare Pampady Thirumeni! Thirumenis devoted Pottan

Research on Altered Granites

Research on Altered Granites Visible yellow radial U- minerals (up to 1 % U )was recorded coating the fractures in the sheared granites, border on the two sides by milky quartz veins, which play as septa for U- minerals migration. From the mineralogical point of view, the sheared granite rich in; a) uranium (meta-autunite, kasolite and phurcalite) , b) thorium (uranothorite) and c) base metals (wolframite, columbite, fergusonite and Plumbopyrochlore minerals) in addition to zircon, allanite, rutile, fluorite, fluro-apatite, phlogopite and iron oxide minerals (hematite, ilmenite, goethite and magnetite )(Table.1).Meta-autunite occurs as lemon-yellow to greenish yellow, subhedral crystals formed as dehydration pseudomorphs after autunite (Fig,6a) and usually associated with kasolite. Phurcalite occurs as light brown subhedral to anhedral crystals of calcium uranium phosphate (Fig,6b) and usually associated with iron oxides. The altered granites are enriched in most major oxides (Fe2O3, Tio2, ,Mn, Mg, CaO and P2O5,) except SiO2 and Na2O than fresh granites (Fig.7) manifesting ferrugination, calcification ,desilicification and illitization .Also the fresh granites are depleted in most trace elements (Ni, Cr, Sr, Zr, Y, Ga, Zn, Pb, and Cu) except Nb than altered ones. Based on major element data, the main characteristic features of the studied altered granites are higher in Fe/Mg ratio (15 av.), lower in SiO2(av.52.8 %)andNa2O /K2O ( av.0.16) than fresh granites Table 2 ) . Fig. 6: Photomicrographs showing; a) meta-autunite crystal surrounded by phurcalite mineral in altered granites. C.N., X=40 and b) phurcalite mineral associated with iron oxide in altered granites. C.N., X=40. Table (1): Shows the result of minerals occurrences in the study area. Minerals group Rock types Minerals Uranium minerals Altered granite Meta-autunite, Phurcalite and Kasolite Thorium minerals Uranothorite Base Metals Altered granite Wolframite Black Jasper Cassiterite, Wolframite, Zincite, Ni-chromite and Cr-spinel Red Jasper Ni-Chromite and Cr-spinel Milky quartz Galena, Pyrite, pyrrhotite and Sphalerite Copper Minerals Milky quartz covellite, bornite Red Jasper crysocolla Black Jasper Atacamite, Paratacamite, and cuprite Native minerals Black Jasper and Milky quartz Gold and Nickel Nb-Ta minerals Altered granites Plumbopyrochlore, Columbite and Fergusonite REEs-Bearing Minerals Alkali feldspar granites Zircon, Fluorite syenogranites Zircon, allanite Altered granites Zircon, Allanite, Rutile and Fluorite Stream sediments Zircon, Monazite Black Jasper Xenotime Red Jasper Iron Minerals Altered granites Hematite, Ilmenite, Goethite and Magnetite Black Jasper Hematite, Magnetite Red Jasper Hematite, Magnetite and Goethite Milky quartz Hematite Fig.( 7 ) The enrichment and depletion of major oxides and trace elements of altered granites to the fresh granites samples. Fig.( 8 ) Bar- diagram showing the trace elements distribution of red and black jasper. The content of HFSE in both fresh and altered granites (Nb (36-10 ppm), Zr (316- 759 ppm), Y(69- 220 ppm) ,U (8-ppm) respectively as well as low Rb/Sr ratio (1.04-0.45) and K/ Rb ratio (0.03-0.04) (Table 2) suggest that the fresh granites are primarily derived from felsic source .On the other side, these criteria in the altered granites are critical for uranium exploration . The black jasper more richer than red one in Ni (av.1004 -81ppm),Cr(av.8575 -853ppm),Zn (av.144 -80 ppm), Cu(av.1106- 35 ppm), Co(av.371-0.0 ppm), Au(1.04 -0.5 ppm) and U(40- 8800ppm)respectively (Table 2,Fig.8 ). The latest event invades the WNW-ESE shear zone was the intrusion of silica and jasper veins with different magnitude. The excess of released quartz can migrate as colloidal silica to precipitate later in the tension fractures as jasperoid vein at upper structural levels under low temperature condition .Silicification along the main shear zone has a noticeable amount of liberated secondary silica occurs as fine crystals associated with the large primary quartz crystals and characterized by the existence of three generations of silica veins differ in color, mineralization and age. 1)The milky quartz veins are the first phase (the youngest one), mainly barren, running WNW and dipping 70 °/ SSW direction, highly brecciated (2-5 Km in length, 0.25-3 m in width)and common only at the southern border of the shear zone. 2) The red jasper veins(second phase) have E-W ,WNW,NW and NE trends (Fig.5), dipping 50-75/N or S , 45 °/ SSW, SW and SE direction respectively. They fractured, fragmented, discontinuous, brecciated,(7km in length, 0.30-3 m in width) and rich in Cr, , Ni, Sn, Zn and Cu- mineralization (Fig.6) (some parts of red jasper are rich by vugs (physical tap) that are filled by mineralization. These veins exhibit combinations of more than one style; orbicular and brecciated. Brecciated red jasper (Plate 4.a) can vary from soft swirls of color to dramatically fragmented shades of rich brown, brick red and cream colors. Deeply integrated colors come from organic materials and iron oxides imbedded in the stones. Ore microscopic investigation reveals that; quartz crystals occur as anhedral cryptocrystalline associated and stained by iron oxide. Sometimes cryptocrystalline crystals of amorphous silica form banding. Iron oxide occurs as black crystalline minerals and staining of quartz. 3) The black jasper(oldest one) is represented by 1.8 km in length, 0.5-10 m in width, trending N45 °W ,dipping 50 °-65 ° /SW (Figs.5), and rich in Cr, Ni, Cu and Au mineralization, Fig.7).They are concentrated only in the eastern part of G. Um Bakra shear zone and less abundant in length than milky and red veins. The black jasper are vuggy than milky and red silica veins and these vugs filled by calcite minerals. The apical parts of the veins are intensely weathered, oxidized, brecciated fragments (Plate.4b) and decomposed to forming gossans. Petrographically, quartz occurs as cryptocrystalline and polycrystalline forming spherulitic texture and associated with iron oxide. Iron oxide associated with quartz and sometimes forming network or needle (Plate .4c). Cr- spinel with blood red color was observed and having darker boundaries with quartz (Plate.4d).Ore microscopic study reveals the presence of gold, chromite and magnetite minerals. Fire assay for gold content give 1.04 g/ton .Chromite occurs as anhedral crystal associated with magnetite (Plate.4e). Chromite existed in different forms; zoned veinlet or disseminated specks (Plate. 4 fg). Black minerals filling fracture and associated with quartz (Plate.4h) . Fig. (6): showing different types of copper minerals in red and black jasper ,a) atacamite mineral, b) paratacamite mineral, c) cuprite mineral and d) crysocolla mineral . Fig. (7): Photograph showing copper minerals from black jasper of the study area. Alterations Two phases of hydrothermal alterations; acid and alkaline were distinguished in the shear zone resulting in Kaolinization and ferrugination processes as illustrated below: Kaolinization indicates that the rocks were affected by acidic solution with low temperature varying from 200 to 250  °C (Helgeston 1974). Kaolinitization process causes an increase in alumina (18.2%) at the expense of the other major oxides (Table2).Kaolinization affects sheared granites in the shear zone are characterized by the formation of clay minerals and adsorbed secondary U- minerals( meta-autunite, Kasolite and Phurcalite) (Table1). Acidic alteration of biotite produces illite+quartz ,while magnesium, iron, oxygen, and fluorine are dissolved in hydrothermal fluids (Pirajno,1992). These solution caused the alteration of the feldspars and micas to clay minerals (Fig.8) are produced by an acidic fluid and it liberates silica and K+ according to Pirajno,(1992). Similarly, the anorthite component of plagioclase is transformed to (clay minerals) (Hemley and Jones, 1964; Pirajno1992) and frees Ca2+ ions transported also by the hydrothermal solution. The free Al+3 increase the alumina in the clay mineral. This kind of alteration by acid solution is responsible for transported and redeposited uranium and base metals mineralization in WNW-ESE shear zone which acts as a good trap. carbonitization:The common presence of calcite manifesting carbonitization process along the shear zone (Fig.8).Also both of ultramafic -mafic rocks and intrusive gabbros are rich by carbonate minerals. Ferrugination causes increase in total Fe2O3 content (FeOt= 4.7%. to 32.7%) at the expense of other oxides. The strong alkaline solution may precipitate Fe+3 and U+6 within the shear zones in the form of iron oxy-hydroxides rich in uranium (Cuney, et al., 1984). Sheared granite samples stained by Fe oxides adsorb U minerals at the main shear zone. Ferrugination is represented mainly by hematite and goethite minerals (table1, Fig.9).Oxygen may combine with iron to produce hematite forming hematitic alteration. Plate 4: Photomicrographs showing; a) brecciated red jasper vein, C.N., X=40., b ) brecciated black jasper vein with vugs, c) black silica vein showing hematitization in quartz, iron oxide occurs as needles in quartz. C.N., X=40, d) blood red, Cr spinel having darker boundaries in BJV (PPL), X=20., e) chromite (cr) in rim and magnetite (mag) in core in BJV. X =40, f) veinlet of chromite and groundmass of magnetite in BJV. X=40, g) disseminated specks of chromite in BJV. X= 40, h) red jasper vein showing iron oxide present as black crystalline minerals and staining of quartz. C.N., X=20 fluoritization :Fluorite was emplaced through the fractures and fissures in altered granite along the shear zone. The released 3Ca2+and 6 Fà ¢Ã‹â€ Ã¢â‚¬â„¢ during illitization of the anorthite and biotite may combine together forming fluorite which is observed within the shear zone associate with U- minerals. Acknowledgements Our sincere thanks and gratitude should be provided to Dr.I, Hassan and Dr.W. El-Gazlawy, NMA, for their help during field work. Discussion Conclusion 1-To form a hydrothermal deposit in Um Bakra- Um Samra WNW-ESE shear zone requires: (1) a magma source of fluid, (2) dissolved metals in the magmatic fluids, , (3) heat source and activate tectonic, causes the migration of à ¯Ã‚ ¬Ã¢â‚¬Å¡uid and (4) Presence of channel ways, layering and physical cavities, to precipitates the metals or minerals. 2-G. Um Samra -G. Um Bakra shear zone strikes N-80 ° and dipping 45 ° /SSW and ranges from 30 to 500 m in thickness and extends 10 km in length. The host rock (syenogranites)is highly altered, fine -grained,ferruginous ,reddish pink and grayish pink to grayish in color. Two opposite N-S strike-slip faults and NNE and NNW strike-slip faults dextral and sinistral sense of movement(good channel ways) forming grabben and horst structures respectively (6 km in length, 30 m in width, dipping 10 °-20 ° towards E or W) cut the shear zone. 3-Three generations of silica veins differ in color, mineralization and age are common. The first phase (youngest),is barren milky quartz veins, running WNW and dipping 70 °/ SSW direction , highly brecciated (2-5 Km in length, 0.25-3 m in width. The red jasper(second phase) has N 60 °-76 ° W trend, dipping 45 °/ SSW direction, fractured, fragmented, discontinuous, brecciated, (7km in length, 0.30-3 m in width) and rich in Cr, Ni, Sn, Zn and Cu- mineralization) .The third phase (oldest one) is represented by black jasper (1.8 km in length, 0.5-10 m in width, trends N75W ,dipping 50 °-65 ° /SSW and rich in Cr, Ni, and Au mineralization). 4-The black jasper more richer than red one in Ni (av.1004 -81ppm),Cr(av.8575 -853ppm),Zn (av.144 -80 ppm), Cu(av.1106- 35 ppm), Co(av.371-0.0 ppm), Au(1.4 -0.5 ppm) and U(av, à ¢Ã¢â€š ¬Ã‚ ¦Ãƒ ¢Ã¢â€š ¬Ã‚ ¦.ppm)respectively (Table ). 5-The presence of clay mineral (dickite:Al2Si2O5(OH)4) in quartz and jasper veins indicates a temperature environment higher than 200 °C. The mixing of volatile fluids with meteoric water and fluid- wall rock interaction result in changes in pH and oxygen activity and deposition of base metals. 6- Precipitation of hematite in shear zone and red jasper veins probably decreased the pH of the solution and rising acidic fluids. The sudden change in the pH and temperature of the fluids will lead to destabilization of base metal complexes favouring their deposition (Alexandrov et al., 1985). 7-The cooling of the hydrothermal solution decreases the solubility of the metals. Cooling can take place when hot magmatic à ¯Ã‚ ¬Ã¢â‚¬Å¡uids enter cooler wall rocks or when two à ¯Ã‚ ¬Ã¢â‚¬Å¡uids mix, Similar reactions can take place between hydrothermal solutions and wall rock; a solution containing dissolved sulà ¯Ã‚ ¬Ã‚ de might contact a rock containing magnetite, to convert the magnetite to pyrite by a process called sulà ¯Ã‚ ¬Ã‚ dation.Or, a solution containing Cu might react with a rock containing pyrite to form Cu sulà ¯Ã‚ ¬Ã‚ des. 8- The base metals mineralization are accumulate in the residual melt of the late fractionate alkali feldspar granites (Bright, 1974) especially upward in the magmatic system (Smith,1979). During the emplacement of the basic and intermediate dikes (olivine basalt, andesite and dolerite dikes) which accompanied with high temperature and Co2), the base metals(galena, pyrite, sphalerite and cassiterite) were precipitated from saline and reduced fluids as sulfides due to cooling, fluid mixing and wall rock reaction. 9-The banded texture in jasper veins is common in epithermal base metals, indicating of boiling event and rapid deposition (Hedenquist et al.,1995).Most epithermal deposits consist of numerous separate, largely vertical veins that form a conjugate set, sometimes reà ¯Ã‚ ¬Ã¢â‚¬Å¡ecting regional tectonic stress. Low-temperature hydrothermal solutions ( 10- The non-sulfide ore deposits are classified into two major types; supergene and hypogene deposits (Hitzman et. al., 2003). (a) Supergene deposits form primarily from the oxidation of sulfide-bearing deposits and are formed principally zinc carbonate or silicates, and (b) hypogene deposits consist dominantly of zinc silicates and oxides, and they commonly result from mixing of a reduced, Zn-rich, with an oxidized, sulfur-poor fluid. Um Bakra-Um Samra shear zone containing zinc oxides (hypogene deposits). 11-Pyrite presents in two generations, disseminated and along fractures. The occurrence of covellite, bornite and magnetite are related to the oxidation product of disseminated pyrite, whereas the second type of pyrite transformed into pyrrhotite. 12-The chloritization process is the last phase of alteration in the shear zone, where fluids became rich in Mg/Fe most probably due to the decomposition of ferromagnesian minerals from the basic and intermediate dikes. Fig.( 8) :Showing Kaolinization map for Um Bakra -Um Samra area. Fig.( 9) showing ferrugination map for Um Bakra -Um Samra area. Table ( 2 ) chemical analysis of major oxides and trace elements of Um Samra-Um Bakra area. Trace elements (ppm) Fresh Altered Red Black Ni Range 0.0-55 0-18095 0-409 314-1501 Average 10 2322 81 1004 Cr Range 233-485 113-2409 294-2689 3490-12898 Average 296 798 853 8575 Rb Range 83-210 0-392 0.0-1161 0.0 Average 147. 128 289 0.0 Sr Range 17-507 73-58 8-127 0-17 Average 142 278 74 7 Zr Range 89-659 196-1873 0-466 0.0 Average 316 759 238 0.0 Y Range 16-102 84-512 0-79 0-142 Average 69 220 38 77 Nb Range 14-56 0-62 0-35 0.0 Average 36 10 11 0.0 Ga Range 22-45 0-151 0-59 0.0 Average 32 73 24 0.0 Zn Range 16-145 0-2409 32-169 56-281 Average 78 528 80 144 Pb Range 0-52 0-684 0-173 0.0 Average 16 157 45 0.0 Cu Range 0-32 0-210 0-80 431-2045 Average 4 26 35 1107 Co Range 0.0 0.0 0.0 0-558 Average 0.0 0.0 0.0 371 Mo Range 0.0 0.0 0-127 0.0 Average 0.0 0.0 25 0.0 As Range 0.0 0.0 0-2098 0.0 Average 0.0 0.0 419 0.0 U Range 0.0 0-7640 0.0 0.0 Average 0.0 1749 0.0 0.0 Major oxides % Fresh Altered Red Black SiO2 Range 69.22-75.33 23.14-72.09 70.3-92.53 72.93-91.27 Average 72.9 52.8 84.2 82.7 TiO2 Range 0.01-0.29 0.28-2.46 0.01-0.22 0.0 Average 0.2 1.08 0.2 0.0 Al2O3 Range 12.35-15.4 10.37-18.02 0.69-14.85 0.69 Average 13.7 12.7 6.8 0.8 Fe2O3 Range 0.08-2.91 2.10-45-77 1.39-4.97 4.46-22.54 Average 1.9 19.8 3.4 13.4 MnO Range 0-0.08 0-0.75 0.01-0.03 0.01-0.04 Average 0.03 0.1 0.03 0.03 MgO Range 0.13-0.65 0.24-7.23 0.29-1.75 0.19-0.60 Average 0.31 1.32 0.806 0.442 CaO Range 0.45-2.55 1.26-4.4 0.31-0.76 0.01-1.74 Average 1.1 2.6 0.6 0.5 Na2O Range 3.15-4.34 0.12-3.34 0.05-2.2 0.05-0.12 Average 3.7 0.8 0.6 0.08 K2O Range 4-6.70 1.84-7.78 0.1-6.96 0.04-0.09 Average 5 5 3 0.06 P2O5 Range 0.020.16 0.01-1.23 0.07-0.48 0.02-0.04 Average 0.08 0.39 0.224 0.032 L.O.I. Range 0.04-0.85 0.8-2.80 Average 0.31 1.43 Total Range 99.73-99.9 93.22-99.91 99.36-99.92 97.45-99.01 Average 100 98.42 99.7 98.288 References Abdalla, H. M., Matsueda, H., Obeid, M., A. and Takahashi., R., (2008): Chemistry of cassiterite in rare metal granitoids and the associated rocks in Eastern Desert, Egypt. Journal of Mineralogical and petrological sciences, 103, 318-326. Abdalla, H. M. and Mohamed, F. H., (1999): Mineralogical and geochemical investigation of emerald and beryl mineralization, Pan-African Belt of Egypt genetic and exploration aspects: J. Afr Earth Sci, 28,3, 581-598. Bakhit, F.S., 1978 geology and radioactive mineralization of Gabal El-Missikat area,Eastern Desert of Egypt, A.R.E. Ph.D. thesis, Fac. Sci., Ain Shams Univ., Cairo, Egypt, 289 p. Bakhit, F.S., and Meleik, M.L.,1990. Application of autocorrelation function to structural lineaments in radioactive sample area in the Central Eastern Desert of Egypt. Int. G. Remote Sensing, 11, No. 10,1919. El Ramly, M.F. (1972): A new geological map for the basement rocks rocks in the South Western Desert of Egypt. Ann. Geol. Surv. Egypt.2, 1-18. Gharieb A.G.

Moving To America Essays -- Personal Narrative Essays

I walked around unsteadily all day like a lost baby, far away from its pack. Surrounded by unfamiliar territory and uncomfortable weather, I tried to search for any signs of similarities with my previous country. I roamed around from place to place and moved along with the day, wanting to just get away and go back home. This was my first day in the United States of America. A few months before all of this I was pleased with my calm life in a local city of Taiwan. I settled there at the age of two with my family, and things were going well so far. Because I lived there for ten years, the longest time that I ever spent living in one place, I had made really good friends and was not looking forward to any significant changes although my mom had told me a long time ago, we might move to USA to settle with our uncle and grandma. My mom also told me that the other reason we move is for a better education and life there but I was not listening at that time. I thought she was just joking around because my brother and I have always expected to have a vacation to other countries. By the time I finished my first year of middle school I knew that this was nearly impossible. My family was already packing up, cleaning out the house, and reserving four airplane tickets to USA. The day that I discovered my parents' future plans was one that seemed like a normal day for a twelve-year old. I got up, had my breakfast, and then proceeded to hang around with my friends. Later on that day I went out to play basketball at the school along with my older brother. After we went home, my mom was making dinner and talking to our uncle. After my mom finished the call, she tried to casually approach me and then said in Taiwanese, ?Judy, we are moving i... ... and I started to realize some of the good effects that moving has had. I now understand that this experience has changed me in positive ways as well. Soon I would have friends in different places in the world that I can visit. I would have many places where I could go and feel like home. Most importantly, I would learn that one can adapt to every town and its people and that friends can be made everywhere. Every place has its conveniences and its problems. Every town has its generous and heartless citizens. I live now more secure and bold, like a lion with increased mass and knowledge, not with one, but many packs. I can roam territory that is unfamiliar without feeling lost and alone. Instead, I search for the best way to take advantage of my position in a foreign territory. I can visit recognizable lands and feel at home. This is my, not so new, way of life.

A Time Of Prosperous Change :: essays research papers

A Time of Prosperous Change In the early nineteen hundreds when women used to be treated as objects who were only good for cooking and cleaning. These women were expected to stay home and do nothing but take care of the children. Authors were rarely women .Now in the present day a women is thought of as having a mind of her own. She is thought of as a independent, an individual who has a peace of mind of her own who is allowed to work and make a living as she pleases. Even we don't think of Weldon every time someone mentions a popular contemporary author we know she deserves to be mentioned. Both in the Critical Survey of Long Fiction and in Love and Marriage in the Novels of Anita Brookner and Fay Weldon Weldon is mentioned with great honor and respect. Anna Ericson uses more past situations in Fay Weldon's own life while contrasting her to Anita Brookner while in contrast the Critical Survey of Long Fiction criticizes the works without much comparison to others. Both the Magill and Anna Ericson have strong points on a women's individualism but Anna Ericson proves Weldon's choice of personality for the main character was one reflecting Weldon's own thoughts and morals. In the The Life and Loves of a She Devil Ruth is a character who is well developed who one can feel one with because of the fact that the author creates great depth to her as a character. In the Critical Survey of Long Fiction the author states that "In her fiction, Fay Weldon explores women's lives with wit and humor. She is caustic in her implicit condemnation of injustice but avoids preaching by characters say and what they do"(Magill 3474). On the other hand Ericson has more of a formula to Weldon's novels unlike the Critical Survey of Long Fiction. "The Weldon narrator is usually omniscient; she is wise, sad and cynical"(Ericson 1). which shows that the characters must be well developed to have such a personified personality. Magill rarely states how Ruth's personality had come about in The Life and Loves of a She Devil. Love was not an issue to Weldon when writing this novel this may be due to the lack of love in her very own life. Love was never thought of importance in the Critical Survey of Long Fiction. On the other hand in Love and Marriage in the Novels of Anita Brookner and Fay Weldon Ericson uses the subject of lack of love as the focus of his theories and that

Post Traumatic Stress Disorder vs Generalized Anxiety Disorder Essay

It may be shocking to learn that 21% of American adults suffer from some sort of anxiety disorder(National Institute of Mental Health Statistics). Do you know the differences between the two major types of anxiety disorder? The two major types of anxiety are Post Traumatic Stress Disorder (PTSD) and Generalized Anxiety Disorder (GAD). While many may think PTSD and GAD are one in the same, you may be surprised that they vastly differ in cause and symptoms with their only similarity being their treatment. According to the PTSD Fact Sheet †PTSD was once considered a psychological condition of combat veterans who were â€Å"shocked† by and unable to face their experiences on the battle field† (Fact Sheet Page 1). Over the years with additional research and discoveries PTSD has now become a much more common diagnosis for many anxiety sufferers. According to the National Center for PTSD â€Å"Anyone who has gone through a life-threatening even can develop PTSD. These events can include: combat or military exposure, child sexual or physical abuse, terrorist attacks, sexual or physical assault, serious accidents such as a car wreck, or natural disasters.† (National Center for PTSD). Each individual is different and not everyone who lives through a traumatic event will developed PTSD. Some of the determination factors if an individual will develop PTSD vary based on how intense a trauma was, if the individual lost someone they were close with, how strong the individuals reaction was and how much support the individual received after the event. (National Center for PTSD) Unlike PTSD, Generalized Anxiety Disorder (GAD) is not necessarily associated with a particular event and therefore can appear to come from nowhere. Accordi... ...cess rate. Works Cited Greist John H MD, Jefferson James W. MD. â€Å"Generalized Anxiety Disorder.† Merck Manual Professional. Aug 2007. Haby Michelle, Donnelly Maria, Corry Justine, Vos Theo â€Å"Cognitive behavioral therapy for depression, panic disorder and generalized anxiety disorder: a meta-regression of factors that may predict outcome.† Australian and New Zealand Journal of Psychiatry. 2006. Print. Pages 9-19. National Center for PTSD. â€Å"What is PTSD?† United States Department of Veterans Affairs†. Web. 01 Jan 2007. Web. 26 June 2011. National Institute of Mental Health Statistics. Web. 26 June, 2011. Post-Traumatic Stress Disorder (PTSD) Fact Sheet. â€Å"National Institutes of Health†. Oct 2010. Web. 26 June 2011. Van der kolk Bessel A MD, van der Hart Onno PH.D, Burbridge, Jennifer M.A. â€Å"Approaches to the Treatment of PTSD†. Print. 1995.

Introduction to International Relations

In the context of the idea of â€Å"Nationalism†, what are the differences between the Scottish National Party and the British National Party? BODY OF WORK Being today a central issue of the modern world, Nationalism, a term from nasci which means â€Å"to be born†, has most of the time been considered as a 19th century phenomenon, connected to the development and creation of nation-states .While seen by a large number of critics as outdated in other word old, not just because it is inherently expansionist but also destructive, others in meantime see it as a strength to re-enforce order and solve conflict. Thus, the issue of nationalism will therefore depend on a system every country adopts. If we take the United Kingdom(UK),a constitutional monarchy and unitary states which is composed of four(4) countries :England(London),Northern Ireland(Belfast),Wales(Cardiff) and Scotland(Edinburgh) has been governed by a Parliamentary system.However,it is argued that nationalism w ithin the UK is both reactionary and progressive . The simply reason of this statement is that in different parts of UK,the notion of nationalism has components of both looking towards the future inclusively and progressively but ,also looking to their past regressively thus hoping to bring back their historical period.Britain and Scotland, being among these parts of UK, have for a centuries had political parties sometimes based on similar ideas but most of the time different from each others. The British nationalism referring to the nationalist ideas and policies’ application to the United Kingdom tends to promote the UK as a goal for national identity, social movements, comprises political and sentiment inspired by the love of British language, culture , history and ot forgotten the pride of being British. Supported ,politically from the Euro scepticism of the conservative United Kingdom Independence Party and far-right British national party to the centre-right conservativ e Party and the left-centrist Liberal Democrats, British nationalism has had a progressive cause characterised by â€Å"a powerful but ambivalent force in British politics†.From this British nationalism, a party called the British national party will be one of our aim studies in this topic. As for Scotland, Nationalism being a political ideology and created in 1921 as primarily body based in London and largely influenced by Sinn Fein ,has most of the time supported greater autonomy for Scotland as part of the United Kingdom, but also the creation of a sovereign state.In which case Scottish nationalism can be referred to three (3) main elements: -The Scottish Independence with the advocacy of Scotland becoming a sovereign state -The Scottish national party with the main political party that support Scottish Independence. -The Scottish home rule, an organisation knew before the Devolved Scottish Parliament was created in 1999 that had for purpose to give Scotland the autonomy w ithin the British Empire. From this nationalism , derived a national party called the Scottish national party.It is therefore in the process Nationalism that, our aim target will be to identify the differences between the two major national parties in the United Kingdom known as the British National Party (BNP) and the Scottish National To begin with, we should start by saying that the Scottish National Party (SNP), a civic party with strong democratic leanings and non-nationalist was first created in (1934) having as aim to promote justice, caring and enterprising community by making Scottish potential as an independent nation in the mainstream of modern Europe.Wishing to be completely independent from Britain, the Scottish national party has always wanted to be a separate state making its own decisions not just in Europe but throughout the world, this is why Scottish political parties such as, the SNP encourage progressive attitudes that are principally based on two main(2) things :the long term desire to become but also the ambition to be entirely inclusive with global organisation such as Europe . While the British National Party, reated in (1982) by a group of the National Front with John Tyndall, is a far-right, fascist political party combined with a white supremacy organisation that stands for anti-non british,because it believes that there are significant differences between races, one of the party’s main objectives is to restore by legal methods white ethnicity, which existed prior to 1948 in a way that anything that does not fit their narrow stereotype is meant to be kept away from the party.Adding to this, it has to be said that the British national party adoring men like Adolf Hitler of German Nazi is almost claimed to be a Nazi political party as well. Another reason that makes the difference between the two parties is that, the Scottish national party has always wanted an open door to all races and nationalities in the sense that even non- Scottish people have been accepted to be members of the party without forgetting the fact that this was the first party to have a Muslim MSP as member.After independence, anyone living in Scotland could claim a Scottish citizenship under the SNP constitution with an open door policy on immigration compared to Britain ,where immigration still a dominant issue thus blaming immigrants for any possible problem . It is even believed that the British national party has for wish to put the white British- born before immigrants and non- british,stopping immigration and repatriate people of different races, presently living in the UK to the respective countries .In a speech given by Nick Griffin ,the actual leader of the British national party(BNP),he declared that â€Å"it is probably now too late to anticipate a return to the status quo ante 1948 â€Å" therefore suggested a new model of â€Å"milti-culturalism†. This model was meant to lead by a policy of cultural and biological separation ,not by principles of integration, this could allow people to enjoy each other’s culture and tradition but each staying on their own in order to avoid â€Å"diversity† which could be but a short –lived stepping stone to nothingness.An expected outcome of the method as Tyndall said, was going to be in the image of a south-African apartheid-style system with like he said â€Å"separate communities of people –Indian ,Pakistani, Bangladeshi(Hindu and Muslim),African and Afro-Caribbean and heaven knows what else-living side by side in Britain in separate enclaves†. This is to show that although immigrations issues were trying to be solved there were nevertheless still based on strict principles that had to be followed. Principles that were completely different from the one the Scottish national party made.These days, the Scottish national party does not have a lot to deal with national parties in eastern and central Europe particularly becaus e most of them are rather right wing ,among them men like, Michal Kaminski of the polish law and justice party. Also, in the European parliament for Freedom and fatherland party, it will be noticed that men like David Cameron will definitely be comfortable to sit with Latvia whereas it would be hard if not never for the Scottish party to Roberts Zile from the FFF to the next Bannockburn shindig.This is to prove that racism is not a big concern in Scottish nationalism because there is no race problem in Scotland. Moreover, there are also differences regarding the concern of the British and Scottish public as a whole. While Scotland is much more concerned about the unemployment as a big problem to face, Britain on its side is more worried about the economic field which is very frequent nowadays.In the other hand, crime, law and order are very serious matters in Britain than in Scotland where it is more likely to be concerned about the education. Furthermore ,another difference between the British national party and the Scottish one is that, the Scottish national party, being left wing is very focused on what people living in Scotland will be in the future regardless what the religion or skin colour are, while the British national, being right wing wants to go back to their old values.In terms of Military issue, providing that it is the government in Westminster that is in charge to send soldiers at war, Scotland plays a very small part in sending soldiers for defence ,war and terrorism compared to Britain that is more concerned about this issue. To conclude with this topic, it shall be said that although, these two are different parties in different countries, the differences between them is all about Racism, Immigrations and Political issues.In terms of racism, the British national party states that their constitution has for purpose, the preservation of the ethnic and national typical character of the British people themselves . David Blackburn writes for the spectator coffee house that â€Å"the BNP is no longer a racist party, but a party of racists† in respond to the news that the British national party membership look to vote in favour of allowing the non-whites and non-British to join the party while the Scottish national party has always wanted an open door to all races and nationalities no matter colour, gender and creed there are.In terms of political issues, Scotland is a minority within the UK (United Kingdom) which means the decision-making process stays in the goal of the majority included Britain . Therefore; policies that suit Scotland are often not taken into consideration. In terms of immigrations issues, differences have also been seen above with the British national party wanting to repatriate all immigrants or sometimes create strict principles that have to be followed by all immigrants. Whereas, the Scottish national party has and still fighting against immigration, thus giving citizenship to those claiming for it.So basically, these are some of the differences in brief between the British national party and the Scottish national party, although there could others points according to different points of viReferences and Bibliography David B. , Nick G. ,†Changing course or changing Clothes? †Reflection on the ideological evolution of the British national party 1999-2006 , pp81 Iain M. , gardian. co. uk, Monday 8 June 2009 14. 00 BST IN Last night was the SNP’s night Arthur A. ,†Nationalism, Devolution and the Challenge to the United Kingdom

Philippine Literature During Japanese Period Essay

During the Japanese Occupation, when Tagalog was favored by the Japanese military authority, writing in English was consigned to limbo. It picked up after the war, however, with a fervor and drive for excellence that continue to this day. Stevan Javellana’s â€Å"Without Seeing the Dawn† (1947), the first postwar novel in English, was published in the United States. In 1946, the Barangay Writers Project was founded to help publish books in English. Against a background marked by political unrest and government battles with Hukbalahap guerrillas, writers in English in the postwar period honed their sense of craft and techniques. Among the writers who came into their own during this time were: Nick Joaquin, NVM Gonzalez, Francisco Arcellana, Carlos Bulosan, F. Sionil Jose, Ricaredo Demetillo, Kerima Polotan Tuvera, Carlos Angeles, Edilberto K. Tiempo, Amador Daguio, Estrella Alfon, Alejandrino Hufana, Gregorio Brillantes, Bienvenido Santos, Dominador Ilio, T.D. Agcaoili, Alejandro R. Roces, Sinai C. Hamada, Linda Ty-Casper, Virginia Moreno, Luis Dato, Gilda Cordero-Fernando, Abelardo and Tarrosa Subido, Manuel A. Viray, Vicente Rivera Jr., and Oscar de Zuà ±iga, among many others. Fresh from studies in American universities, usually as Fulbright or Rockefeller scholars, a number of these writers introduced New Criticism to the country and applied its tenets in literature classes and writing workshops. In this way were born the Silliman Writers Summer Workshop (started in 1962 by Edilberto K. Tiempo and Edith L. Tiempo) and the U.P. Writers Summer Workshop (started in 1965 by the Department of English at the U.P.). To this day, these workshops help discover writing talents and develop them in their craft.