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Tips to print PDF document using Acrobat or Reader. Wondering why this page appeared? You probably clicked a button when trying to print. If you aren't looking for printing tips, simply close this window and return to printing. If you are having problems printing, try this quick fix first. Problem printing comments in word 2010. Microsoft Office > Word IT Pro. Printing to PDF, then printing the PDF. But the right-hand column is empty -- no comments. Unlike most other operating systems, Windows still doesn’t include first-class support for printing to PDFs. However, PDF printing is still fairly simple — you can quickly install a free PDF printer or use the support. If you are using Acrobat 9. Printing problems . See this troubleshooting article for additional solutions, such as updating your printer driver and copying your file to your hard drive. Forums have discussions about issues similar to yours. To participate in a community forum, type the description of your issue in the search box on the Acrobat or Adobe Reader forum, or the Acrobat. Users. com Printing & Prepress forum. When posting on forums, include your operating system and your product's version number. Print even pages first, reload the pages, and then print odd pages. You sometimes have to print some pages in reverse order to get the correct page sequence. If you have Acrobat, use the Edit Document Text tool (Acrobat X) or Touch.
Printing PDF files Top issues. Below is a list of support documents related to printing Adobe PDF files. If you don't find the information you're looking for, try searching in the support knowledgebase or the User to User forum. Printing comments on adobe pdf Print PDF comments, print in-place comments in print swf files pdf PDF, print pop-up comments in PDF, print all comments in PDF, print a list of comments in PDF, print a summary. Print PDF files in various ways such as double-sided, posters and banners, color and black and white, multiple pages per sheet, PDF comments, pages of mixed sizes,, and booklet. Up Text tool (Acrobat 9) to change the color of text. To learn more about editing text, go to Edit Text. The creator of the PDF did not embed the fonts used in the document. Embedding prevents font substitution when you view or print the document, and ensures that you see the text in its original font. If you don't have the original fonts installed on your computer, a substitute font is temporarily used for any font not embedded in the PDF. To learn more, see Font embedding and substitution. The Print dialog box does not provide an option to change only the font size. You can do any of the following to enlarge the font: Scale the entire PDF out to the page margins. See Print a portion of a page.(Acrobat only) To change the font size for a specific page or the entire document, use the Edit Document Text tool (Acrobat X) or Touch. Up Text tool (Acrobat 9). To learn more, see Edit text. Most printers provide options to save ink. Click Properties in the Print dialog box to find printer- specific options. To learn more, see the video Printing documents in Acrobat and Reader X. 5.1 Weathering Mechanical weathering occurs when physical forces break rock into smaller and smaller pieces Mechanical Weathering without changing the rock’s. Engineering Characteristics of Soils and Weathered Rocks of Fairfax County and Vicinity, Virginia. UNESCO – EOLSS SAMPLE CHAPTERS EARTH SYSTEM: HISTORY AND NATURAL VARIABILITY - Vol. II - Weathering and Development of Chemically Mature Soils - Nicolas Fedoroff. Weathering - Wikipedia, the free encyclopedia. A natural arch produced by erosion of differentially weathered rock in Jebel Kharaz (Jordan)Weathering is the breaking down of rocks, soil and minerals as well as wood and artificial materials through contact with the Earth's atmosphere, waters and biological organisms. Weathering occurs in situ, roughly translated to: . Mechanical or physical weathering involves the breakdown of rocks and soils through direct contact with atmospheric conditions, such as heat, water, ice and pressure. The second classification, chemical weathering, involves the direct effect of atmospheric chemicals or biologically produced chemicals also known as biological weathering in the breakdown of rocks, soils and minerals. However, both types of weathering occur together, and each tends to accelerate the other. For example, physical abrasion (rubbing together) decreases the size of particles and therefore increases their surface area, making them more susceptible to rapid chemical reactions. The various agents act in concert to convert primary minerals (feldspars and micas) to secondary minerals (clays and carbonates) and release plant nutrient elements in soluble forms. The materials left over after the rock breaks down combined with organic material creates soil. The mineral content of the soil is determined by the parent material; thus, a soil derived from a single rock type can often be deficient in one or more minerals needed for good fertility, while a soil weathered from a mix of rock types (as in glacial, aeolian or alluvial sediments) often makes more fertile soil. In addition, many of Earth's landforms and landscapes are the result of weathering processes combined with erosion and re- deposition. Physical weathering. The primary process in physical weathering is abrasion (the process by which clasts and other particles are reduced in size). However, chemical and physical weathering often go hand in hand. Physical weathering can occur due to temperature, pressure, frost etc. For example, cracks exploited by physical weathering will increase the surface area exposed to chemical action, thus amplifying the rate of disintegration. Abrasion by water, ice, and wind processes loaded with sediment can have tremendous cutting power, as is amply demonstrated by the gorges, ravines, and valleys around the world. In glacial areas, huge moving ice masses embedded with soil and rock fragments grind down rocks in their path and carry away large volumes of material. Plant roots sometimes enter cracks in rocks and pry them apart, resulting in some disintegration; Burrowing animals may help disintegrate rock through their physical action. However, such influences are usually of little importance in producing parent material when compared to the drastic physical effects of water, ice, wind, and temperature change. Rates of weathering Weathering 1 Weathering, Erosion, and Soils Weathering vs. Soil can be defined as the solid material on the Earth’s surface that results from the interaction of weathering and biological activity on the. Rock Weathering and Soil Development OCN 401 -Biogeochemical Systems 30 August 2012 Reading: Schlesinger, Chapter 4. Biological processes are known to play significant roles in soil formation and surficial weathering. However, the contributions of biological activity to regolith and. This page last updated on 10-Sep-2015 EENS 1110 Physical Geology Tulane University Prof. Nelson Weathering and Soils Earth is covered by a thin “veneer. Weathering, Soil and Erosion Study Guide 1. Mass movement is caused by what force? Landslides, mudflows, slump, and creep are all examples of what type of. Physical weathering is also called mechanical weathering or disaggregation. Thermal stress. For example, heating of rocks by sunlight or fires can cause expansion of their constituent minerals. As some minerals expand more than others, temperature changes set up differential stresses that eventually cause the rock to crack apart. Because the outer surface of a rock is often warmer or colder than the more protected inner portions, some rocks may weather by exfoliation . This process may be sharply accelerated if ice forms in the surface cracks. When water freezes, it expands with a force of about 1. Mg/m^2, disintegrating huge rock masses and dislodging mineral grains from smaller fragments. Thermal stress weathering comprises two main types, thermal shock and thermal fatigue. Thermal stress weathering is an important mechanism in deserts, where there is a large diurnal temperature range, hot in the day and cold at night. The process of peeling off is also called exfoliation. Although temperature changes are the principal driver, moisture can enhance thermal expansion in rock. Forest fires and range fires are also known to cause significant weathering of rocks and boulders exposed along the ground surface. Intense localized heat can rapidly expand a boulder. The thermal heat from wildfire can cause significant weathering of rocks and boulders, heat can rapidly expand a boulder and thermal shock can occur. The differential expansion of a thermal gradient can be understood in terms of stress or of strain, equivalently. At some point, this stress can exceed the strength of the material, causing a crack to form. If nothing stops this crack from propagating through the material, it will result in the object's structure to fail. Frost weathering. These processes include frost shattering, frost- wedging and freeze- thaw weathering. Severe frost shattering produces huge piles of rock fragments called scree which may be located at the foot of mountain areas or along slopes. Frost weathering is common in mountain areas where the temperature is around the freezing point of water. Certain frost- susceptible soils expand or heave upon freezing as a result of water migrating via capillary action to grow ice lenses near the freezing front. The ice accumulations grow larger as they attract liquid water from the surrounding pores. The ice crystal growth weakens the rocks which, in time, break up. An example of rocks susceptible to frost action is chalk, which has many pore spaces for the growth of ice crystals. This process can be seen in Dartmoor where it results in the formation of tors. When water that has entered the joints freezes, the ice formed strains the walls of the joints and causes the joints to deepen and widen. When the ice thaws, water can flow further into the rock. Repeated freeze- thaw cycles weaken the rocks which, over time, break up along the joints into angular pieces. The angular rock fragments gather at the foot of the slope to form a talus slope (or scree slope). The splitting of rocks along the joints into blocks is called block disintegration. The blocks of rocks that are detached are of various shapes depending on rock structure. Ocean waves. They are under tremendous pressure because of the overlying rock material. When erosion removes the overlying rock material, these intrusive rocks are exposed and the pressure on them is released. The outer parts of the rocks then tend to expand. The expansion sets up stresses which cause fractures parallel to the rock surface to form. Over time, sheets of rock break away from the exposed rocks along the fractures, a process known as exfoliation. Exfoliation due to pressure release is also known as . These salt crystals expand as they are heated up, exerting pressure on the confining rock. Salt crystallization may also take place when solutions decompose rocks (for example, limestone and chalk) to form salt solutions of sodium sulfate or sodium carbonate, of which the moisture evaporates to form their respective salt crystals. The salts which have proved most effective in disintegrating rocks are sodium sulfate, magnesium sulfate, and calcium chloride. Some of these salts can expand up to three times or even more. It is normally associated with arid climates where strong heating causes strong evaporation and therefore salt crystallization. It is also common along coasts. An example of salt weathering can be seen in the honeycombed stones in sea wall. Honeycomb is a type of tafoni, a class of cavernous rock weathering structures, which likely develop in large part by chemical and physical salt weathering processes. Biological effects on mechanical weathering. Lichens and mosses grow on essentially bare rock surfaces and create a more humid chemical microenvironment. The attachment of these organisms to the rock surface enhances physical as well as chemical breakdown of the surface microlayer of the rock. On a larger scale, seedlings sprouting in a crevice and plant roots exert physical pressure as well as providing a pathway for water and chemical infiltration. Biogeochemical weathering. Chemical weathering is a gradual and ongoing process as the mineralogy of the rock adjusts to the near surface environment. New or secondary minerals develop from the original minerals of the rock. In this the processes of oxidation and hydrolysis are most important. Chemical weathering is enhanced by such geological agents as the presence of water and oxygen, as well as by such biological agents as the acids produced by microbial and plant- root metabolism. The process of mountain block uplift is important in exposing new rock strata to the atmosphere and moisture, enabling important chemical weathering to occur; significant release occurs of Ca. In unpolluted environments, the rainfall p. H is around 5. 6. Acid rain occurs when gases such as sulfur dioxide and nitrogen oxides are present in the atmosphere. These oxides react in the rain water to produce stronger acids and can lower the p. H to 4. 5 or even 3. Sulfur dioxide, SO2, comes from volcanic eruptions or from fossil fuels, can become sulfuric acid within rainwater, which can cause solution weathering to the rocks on which it falls. Some minerals, due to their natural solubility (e. Carbonation occurs on rocks which contain calcium carbonate, such as limestone and chalk. This takes place when rain combines with carbon dioxide or an organic acid to form a weakcarbonic acid which reacts with calcium carbonate (the limestone) and forms calcium bicarbonate. This process speeds up with a decrease in temperature, not because low temperatures generally drive reactions faster, but because colder water holds more dissolved carbon dioxide gas. Carbonation is therefore a large feature of glacial weathering. The reactions as follows: CO2 + H2. O . This process is most effective along the joints, widening and deepening them. Hydration. For example, iron oxides are converted to iron hydroxides and the hydration of anhydrite forms gypsum. 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Pear (2. 00. 3) berpendapat bahawa tingkah laku juga merangkumi aktiviti aksi, prestasi, bertindakbalas, tindakan dan reaksi dari segi teknik, aktiviti yang melibatkan otot- otot, kelenjar dan aktiviti eletrik oleh setiap organ. Mengikut (PL9. 4- 1. Tingkah laku atau gangguan emosi yang serius merujuk kepada keadaan di mana ciri- ciri yang berikut berlaku dalam tempoh yang lama, pada darjat yang ketara dan keadaan ini menjejaskan pembelajaran. Tingkah laku terbahagi kepada dua iaitu tingkah laku positif dan tingkah laku negatif. DEFINISI PENGURUSAN TINGKAH LAKUPengurusan tingkah laku satu perancangan untuk mengubah tingkah laku bermasalah ke satu tingkah laku matlamat yang ditetapkan dengan teknik yang sesuai. Sebagai guru, kita hendaklah membimbing tingkah laku positif dan menghentikan tingkah laku negatif. Tingkah laku bermasalah positif merangkumi tingkah laku ingin tahu, tingkah laku cepat belajar, tingkah laku pintar cerdas, dan tingkah laku proaktif. Tingkah laku bermasalah negatif pula merangkumi tingkah laku yang menghalang (bergantung). Tingkah laku ini merupakan tingkah laku yang boleh membahayakan diri. Ia merujuk kepada rasa kebimbangan iaitu sentiasa berasa takut, menunjukkan reaksi bimbang, tiada keyakinan diri, selain itu, rasa pergantungan berlebihan iaitu terlalu mengharapkan pertolongan atau bantuan dari orang lain terutama ibu bapa atau orang yang rapat dengannya, terlalu manja, tidak boleh berdikari. Selain itu, rasa pengunduran diri iaitu malu untuk menunjukkan kebolehan, teragak- agak memberi pendapat atau idea, tidak yakin pada kebolehan diri, sering menggangap orang lebih baik dari dirinya. Selain itu juga, rasa pengasingan diri iaitu tidak suka bergaul atau berkomunikasi dengan kawan- kawan, sikap rendah diri yang terlalu tinggi, perasaan malu pada kawan- kawan. Selain itu juga, ia merangkumi tingkah laku yang mengganggu ( disruptif ). Tingkah laku ini merupakan tingkah laku yang boleh membahayakan orang lain. Ia merujuk kepada hiperaktif iaitu kelakuan atau bertingkah laku yang tersangat agresif. Selain itu ia merujuk kepada kelakuan nakal iaitu suka menggangu kawan- kawan, membuli atau menyakat kawan- kawan sekelas. Selain itu, bising iaitu kanak- kanak yang menganggu ketenteraman bilik darjah, banyak bercakap . Selain itu, sikap yang ditonjolkan ialah ketawa kuat misalnya ketawa dengan suara yang nyaring dan kuat tanpa menghiraukan orang yang berada di sekelilingnya. Selain itu juga, sikap yang ditonjolkan ialah agresif secara lisan atau fizikal misalnya menggunakan kata- kata kasar, lucah, kurang ajar, tidak sopan. Selain itu, tingkah laku bermasalah merangkumi tingkah laku anti sosial (distruktif). Tingkah laku ini merupakan tingkah laku yang boleh membahayakan diri, sekolah dan masyarakat. Tingkah laku ini merujuk kepada permusuhan nyata iaitu suka bergaduh, berlawan, bertumbuk, mencari pasal dengan mana- mana murid terutama rakan sebaya. Selain itu, vandalisme iaitu suka merosakkan harta benda awam seperti menconteng dinding menggunakan pen, pensil, marker atau tapak kaki, mematahkan alat pengepam tandas, memecahkan kerusi atau meja di dalam bilik darjah, menggores atau menconteng meja. Selain itu, kumpulan liar yang melibatkan kanak- kanak yang terlibat dengan kumpulan tidak bermoral. Selain itu, lik iaitu kanak- kanak yang mempunyai hubungan dengan beberapa orang yang mempunyai perangai atau tabiat yang sama tetapi lebih kepada tingkah laku tidak baik. Selain itu juga, geng iaitu kanak- kanak yang menubuhkan kumpulan tertentu di dalam sekolah, kumpulan yang ditakuti atau digeruni oleh murid- murid lain, bertindak membuli atau menakut- nakutkan murid- murid lain. Tingkah laku anti- sosial lebih menjurus kepada masalah tingkah laku berbentuk jenayah. Di dalam sebuah sekolah, ia lebih difokuskan kepada masalah disiplin. Tingkah laku murid sebegini harus diberi perhatian khusus oleh guru- guru rendah kerana bibit- bibit jenayah pada peringkat ini jika dibiarkan akan menular dan merebak dan menjadi masalah besar pada peringkat akan datang. PENGURUSAN BILIK DARJAH DAN TINGKAH LAKUKONSEP PENGURUSAN BILIK DARJAHDefinisi. Download free song lyrics and chords. License. Trial version. Language. English. Platformwindows. Professional music composition software .. Is there anyway of adding more browsers to the option where you select IE where you can turn on and off the tab that lets you download. Sites to Download Online Videos Free. Guitar, bass and drum tabs & chords with free online tab player. One accurate tab per song. Huge selection of 500,000 tabs. Music is getting less expensive with each year. Today you don’t need to buy CDs or tracks on iTunes or Amazon in order to listen to your favorite music. You may simply go to YouTube and download YouTube music with a free. 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Fordham University is ranked third in the New York metropolitan area and 34th in the nation for the number of students we send abroad each year; Fordham University offers over 125 study abroad programs in 52 countries, on 6.Fordham University - Wikipedia, the free encyclopedia. Fordham University. Latin: Universitas Fordhamensis. Former names. St. Mc. Shane, S. J. Academic staff. Summer Study Abroad Fordham 2016. Summer Study Fordham University in New York City. Study Abroad and Travel Summer Programs for High School Students and Middle School Students. Study Abroad and Related Opportunities. Opportunities abound for study in many of the world’s most dynamic regions for either a summer, a semester or a year. Fordham Law School also. Learn more about Summer Study Programs. Study Abroad; Language Schools; Degrees Abroad; High School Study Abroad; Intern. You might also be interested in these other programs. Check the boxes to inquire. It was founded by the Catholic Diocese of New York in 1. St. John's College, placed in the care of the Society of Jesus shortly thereafter, and has since become an independent institution under a lay board of trustees, which describes the university as . It enrolls approximately 1. New York State: Rose Hill in the Bronx, Lincoln Center in Manhattan and Westchester in West Harrison. In addition to these campuses, the university maintains a study abroad center in the United Kingdom and field offices in Spain and South Africa. Fordham awards the Bachelor of Arts, Bachelor of Science, and Bachelor of Fine Arts degrees, as well as various master's and doctoral degrees. News and World Report lists Fordham as a . John's College, 1. Fordham was founded as St. John's College in 1. Irish- born coadjutor bishop (later archbishop) of the Diocese of New York, the Most Reverend John J. The college was the first Catholic institution of higher education in the northeastern United States. In September 1. 84. Hughes purchased most of Rose Hill Manor in Fordham, New York, for slightly less than $3. St. Joseph's Seminary following the model of Mount Saint Mary's University of which he was an alumnus. The seminary was paired with St. John's College, which opened at Rose Hill with a student body of six on June 2. The Reverend John Mc. Closkey (later archbishop of New York and eventually the first American cardinal) was the school's first president, and the faculty were secular priests and lay instructors. The college presidency went through a succession of four diocesan priests in five years, including the Rev. James Roosevelt Bayley, a distant cousin of Theodore and Franklin D. Roosevelt and a nephew of St. In 1. 84. 5, the seminary church, Our Lady of Mercy, was built. The same year, Bishop Hughes convinced several Jesuit priests from the St. Mary's Colleges in Maryland and Kentucky to staff St. Bishop Hughes deeded the college over but retained title to the seminary property, about nine acres. In 1. 84. 7, Fordham's first school in Manhattan opened. The school became the independently chartered College of St. Francis Xavier in 1. It was also in 1. American poet Edgar Allan Poe arrived in the village of Fordham and began a friendship with the college Jesuits that would last throughout his life. In 1. 84. 9, he published his famed work . John's curriculum consisted of a junior division (i. Colonel Robert Gould Shaw, famed commander of the all- black. Massachusetts Volunteer Infantry American Civil War regiment, attended the junior division. An Artium Baccalaureus degree was earned for completion of both curricula, and an additional year of philosophy would earn a Magister Artium degree. In 1. 85. 5, the first student stage production, Henry IV, was presented. The seminary was closed in 1. Jesuits in 1. 86. John's bringing a cadet corps to campus. From 1. 88. 5 to 1. U. S. Squires, built a cadet battalion to a strength of 2. ROTC unit at Fordham. The college built a science building in 1. In addition, a three- year Bachelor of Science degree was created. In 1. 89. 7, academic regalia for students at Commencement was first adopted. John's College, c. Woolworth Building at night c. Fordham schools in Manhattan at the time. With the addition of law and medical schools in 1. St. John's College became Fordham University in 1. The name Fordham refers to the village of Fordham, in which the original Rose Hill campus is located. The village, in turn, drew its name from its location near a shallow crossing of the Bronx River (. When Fordham and several other Westchester County towns were consolidated into the Bronx at the turn of the twentieth century, the village became the borough's Fordham neighborhood. Still in existence today, it is located just to the west of the Rose Hill campus. Not requiring its students to obtain bachelor's degrees until the late 1. Jewish student body, and in recognition of that, the students were exempted from the then- required course in Catholic theology. The school's longtime dean, Jacob Diner, was also Jewish. Francis Xavier was closed in 1. Fordham colleges were opened at the Woolworth Building in Manhattan to fill the void, beginning an unbroken string of instruction in Manhattan that became what is now Fordham College at Lincoln Center. They were later moved to 3. Broadway. Fordham football played on some of the largest stages in sports, including games in front of sellout crowds at the Polo Grounds and Yankee Stadium, a Cotton Bowl appearance and a Sugar Bowl victory, as well as producing the famed Seven Blocks of Granite (including Vince Lombardi). On September 3. 0, 1. Fordham participated in the world. The university discontinued the program during World War II, reinstating it in 1. However, it proved much less successful and too expensive to maintain, and was again discontinued in 1. NCAA Division III team in 1. Division I team in 1. Eisenhower unveils the Lincoln Center project, including the Fordham campus seen on the upper- right of the image in the foreground. In 1. 96. 1, the Lincoln Center campus opened as part of the Lincoln Square Renewal Project. The School of Law was the first to occupy the new campus, but the academic programs at 3. Broadway were moved to the new location in 1. At Rose Hill, the all- female Thomas More College began instruction in 1. During this period, students routinely organized protests and class boycotts and used psychoactive drugs on campus open spaces. An experimental college with no set requirements and no grades, it was studied by a wide array of educators and reported on by such large- circulation publications of the day as Look, Esquire, and the Saturday Review. The school closed in 1. In 1. 96. 9, students organized a sit- in on the main road leading to Rose Hill in response to an announcement that President Richard Nixon would be speaking on campus. The College of Pharmacy closed due to declining enrollment in 1. Fordham College at Rose Hill merged with Thomas More College in 1. It became legally independent in 1. Rose Hill campus; however, the school remains connected to the university in many ways. In 1. 99. 6, the campus's undergraduate college changed its name to . The school had been steeped in financial hardship since the 1. Located 2. 5 miles (4. Manhattan in Tarrytown, New York, the college remained open, and its campus received a branch of the School of Professional and Continuing Studies as well as extensions of the graduate schools for education, social service, and business administration. In 2. 00. 5, Fordham announced that Marymount College would be phased out; it awarded degrees to its final undergraduate class in May 2. University administrators indicated that the campus would remain open for Fordham graduate programs in several disciplines. In the autumn of 2. Marymount campus. Administrators stated that the expenses required to support the programs at the campus far exceeded their demand. University officials estimated that the revenue gained from the proposed sale would not be greater than the expenses incurred maintaining and improving the campus since the merger with Marymount. President Mc. Shane stated that the university's decision was nonetheless a . Fordham then indicated its intention to move the remaining programs from the Marymount campus to a new location in Harrison, New York by the autumn of 2. On February 1. 7, 2. EF Schools, a chain of private language instruction schools. It recently completed a new building for The Law School, as well as an undergraduate dormitory. The former law school building is being renovated to give the Gabelli School of Business a home in Manhattan, and long- term plans are under consideration for a new library building, as well as buildings to house the Graduate School of Social Service and the Graduate School of Education. Academics. The university promotes the Jesuit principles of cura personalis, which fosters a faculty and administrative respect for the individual student and all of his or her gifts and abilities; magis, which encourages students to challenge themselves and strive for excellence in their lives; and homines pro aliis, which intends to inspire service among members of the Fordham community. Based on the curriculum established by the Society of Jesus in the sixteenth century, the Core is shared by Jesuit schools all over the world and is intended to provide a sound liberal arts education. Nevertheless, the university continues its tradition of medical education through a collaboration with the Albert Einstein College of Medicine at Yeshiva University. The partnership allows Fordham undergraduate and graduate science students to take classes, conduct research, and pursue early admission to select programs of Einstein. In addition, it involves a physician mentoring program, which permits students to shadow an attending physician at Einstein's Montefiore Medical Center. Walsh Family Library, ranked in 2. Quinn Library and the Leo T. Kissam Memorial Law Library at the Lincoln Center campus, and the Media Center at the Westchester campus. In addition to the university's formal libraries, several academic departments, research institutes, and student organizations maintain their own literary collections. The Fordham Museum of Greek, Etruscan, and Roman Art is located at the Rose Hill campus and contains more than 2. Classical antiquity. A gift from alumnus William D. Walsh, it is the largest collection of its kind in the New York metropolitan area. Most honors students are inducted into the programs upon admission to the university, though some are invited at the end of their first year. Each program has a designated study space for its members, including Alpha House for the Fordham College Honors Program and the honors wing of Hughes Hall for the Global Business Honors Program. |
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