Test Prep SAT Test Exam Prep
Scholastic Assessment Test: Reading, Writing and Language, Mathematics (Page 10 )

For the last hour I have been watching President Lincoln and General McClellan as they sat together in earnest conversation on the deck of a steamer closer to us. I am thankful, I am happy, that the President has come `" has sprung across the dreadful intervening Washington, and come to see and hear and judge for his own wise and noble self.
While we were at dinner someone said, `Why, there's the President!` and he proved to be just arriving on the Ariel, at the end of the wharf. I stationed myself at once to watch for the coming of McClellan. The President stood on deck with a glass, with which, after a time, he inspected our boat, waving his handkerchief to us. My eyes and soul were in the direction of the general headquarters, over which the great balloon was slowly descending. As used in the passage, the word glass means:

For the last hour I have been watching President Lincoln and General McClellan as they sat together in earnest conversation on the deck of a steamer closer to us. I am thankful, I am happy, that the President has come `" has sprung across the dreadful intervening Washington, and come to see and hear and judge for his own wise and noble self.
While we were at dinner someone said, `Why, there's the President!` and he proved to be just arriving on the Ariel, at the end of the wharf. I stationed myself at once to watch for the coming of McClellan. The President stood on deck with a glass, with which, after a time, he inspected our boat, waving his handkerchief to us. My eyes and soul were in the direction of the general headquarters, over which the great balloon was slowly descending. The `great balloon was slowly descending` is apparently:

Big earthquakes are naturally occurring events well outside the powers of humans to create or stop. An earthquake is caused by a sudden slip on a fault. Stresses in the earth's outer layer push the side of the fault together. The friction across the surface of the fault holds the rocks together so they do not slip immediately when pushed sideways. Eventually enough stress builds up and the rocks slip suddenly, releasing energy in waves that travel through the rock to cause the shaking that we feel during an earthquake. Earthquakes typically originate several tens of miles below the surface of the earth. It takes many years `" decades to centuries `" to build up enough stress to make a large earthquake, and the fault may be tens to hundreds of miles long. The scale and force necessary to produce earthquakes are well beyond our daily lives. Likewise, people cannot prevent earthquakes from happening or stop them once they've started `" giant nuclear explosions at shallow depths, like those in some movies, won't actually stop an earthquake. The two most important variables affecting earthquake damage are the intensity of ground shaking cased by the quake and the quality of the engineering of structures in the region. The level of shaking, in turn, is controlled by the proximity of the earthquake source to the affected region and the types of rocks that seismic waves pass through en route (particularly those at or near the ground surface). Generally, the bigger and closer the earthquake, the stronger the shaking. But there have been large earthquakes with very little damage either because they caused little shaking or because the buildings were built to withstand that shaking. In other cases, moderate earthquakes have caused significant damage either because the shaking was locally amplified or more likely because the structures were poorly engineered. The word fault means?

Big earthquakes are naturally occurring events well outside the powers of humans to create or stop. An earthquake is caused by a sudden slip on a fault. Stresses in the earth's outer layer push the side of the fault together. The friction across the surface of the fault holds the rocks together so they do not slip immediately when pushed sideways. Eventually enough stress builds up and the rocks slip suddenly, releasing energy in waves that travel through the rock to cause the shaking that we feel during an earthquake. Earthquakes typically originate several tens of miles below the surface of the earth. It takes many years `" decades to centuries `" to build up enough stress to make a large earthquake, and the fault may be tens to hundreds of miles long. The scale and force necessary to produce earthquakes are well beyond our daily lives. Likewise, people cannot prevent earthquakes from happening or stop them once they've started `" giant nuclear explosions at shallow depths, like those in some movies, won't actually stop an earthquake. The two most important variables affecting earthquake damage are the intensity of ground shaking cased by the quake and the quality of the engineering of structures in the region. The level of shaking, in turn, is controlled by the proximity of the earthquake source to the affected region and the types of rocks that seismic waves pass through en route (particularly those at or near the ground surface). Generally, the bigger and closer the earthquake, the stronger the shaking. But there have been large earthquakes with very little damage either because they caused little shaking or because the buildings were built to withstand that shaking. In other cases, moderate earthquakes have caused significant damage either because the shaking was locally amplified or more likely because the structures were poorly engineered. The amount of shaking during an earthquake is determined by:

Big earthquakes are naturally occurring events well outside the powers of humans to create or stop. An earthquake is caused by a sudden slip on a fault. Stresses in the earth's outer layer push the side of the fault together. The friction across the surface of the fault holds the rocks together so they do not slip immediately when pushed sideways. Eventually enough stress builds up and the rocks slip suddenly, releasing energy in waves that travel through the rock to cause the shaking that we feel during an earthquake. Earthquakes typically originate several tens of miles below the surface of the earth. It takes many years `" decades to centuries `" to build up enough stress to make a large earthquake, and the fault may be tens to hundreds of miles long. The scale and force necessary to produce earthquakes are well beyond our daily lives. Likewise, people cannot prevent earthquakes from happening or stop them once they've started `" giant nuclear explosions at shallow depths, like those in some movies, won't actually stop an earthquake. The two most important variables affecting earthquake damage are the intensity of ground shaking cased by the quake and the quality of the engineering of structures in the region. The level of shaking, in turn, is controlled by the proximity of the earthquake source to the affected region and the types of rocks that seismic waves pass through en route (particularly those at or near the ground surface). Generally, the bigger and closer the earthquake, the stronger the shaking. But there have been large earthquakes with very little damage either because they caused little shaking or because the buildings were built to withstand that shaking. In other cases, moderate earthquakes have caused significant damage either because the shaking was locally amplified or more likely because the structures were poorly engineered. This passage was most likely written to:

Big earthquakes are naturally occurring events well outside the powers of humans to create or stop. An earthquake is caused by a sudden slip on a fault. Stresses in the earth's outer layer push the side of the fault together. The friction across the surface of the fault holds the rocks together so they do not slip immediately when pushed sideways. Eventually enough stress builds up and the rocks slip suddenly, releasing energy in waves that travel through the rock to cause the shaking that we feel during an earthquake. Earthquakes typically originate several tens of miles below the surface of the earth. It takes many years `" decades to centuries `" to build up enough stress to make a large earthquake, and the fault may be tens to hundreds of miles long. The scale and force necessary to produce earthquakes are well beyond our daily lives. Likewise, people cannot prevent earthquakes from happening or stop them once they've started `" giant nuclear explosions at shallow depths, like those in some movies, won't actually stop an earthquake. The two most important variables affecting earthquake damage are the intensity of ground shaking cased by the quake and the quality of the engineering of structures in the region. The level of shaking, in turn, is controlled by the proximity of the earthquake source to the affected region and the types of rocks that seismic waves pass through en route (particularly those at or near the ground surface). Generally, the bigger and closer the earthquake, the stronger the shaking. But there have been large earthquakes with very little damage either because they caused little shaking or because the buildings were built to withstand that shaking. In other cases, moderate earthquakes have caused significant damage either because the shaking was locally amplified or more likely because the structures were poorly engineered. You can conclude from this passage that:

Oliver Goldsmith (1730`"1774) wrote criticism, plays, novels, biographies, travelogues, and nearly every other conceivable kind of composition. This good- humored essay is from a series published in the Public Ledger and then in book form as The Citizen of the World (1762). Were we to estimate the learning of the English by the number of books that are every day published among them, perhaps no country, not even China itself, could equal them in this particular. I have reckoned not less than twenty-three new books published in one day, which, upon computation, makes eight thousand three hundred and ninety-five in one year. Most of these are not confined to one single science, but embrace the whole circle. History, politics, poetry, mathematics, metaphysics, and the philosophy of nature, are all comprised in a manual no larger than that in which our children are taught the letters. If then, we suppose the learned of England to read but an eighth part of the works which daily come from the press and surely non can pretend to learning upon less easy terms), at this rate every scholar will read a thousand books in one year. From such a calculation, you may conjecture what an amazing fund of literature a man must be possessed of, who thus reads three new books every day, not one of which but contains all the good things that ever were said or written. And yet I know not how it happens, but the English are not, in reality so learned as would seem from this calculation. We meet but few who know all arts and sciences to perfection; whether it is that the generality are incapable of such extensive knowledge, or that the authors of those books are not adequate instructors. In China, the Emperor himself takes cognizance of all the doctors in the kingdom who profess authorship. In England, every man may be an author, that can write; for they have by law a liberty, not only of saying what they please, but of being also as dull as they please. Yesterday, as I testified to my surprise, to the man in black, where writers could be found in sufficient number to throw off the books I saw daily crowding from the press. I at first imagined that their learned seminaries might take this method of instructing the world. But, to obviate this objection, my companion assured me that the doctors of colleges never wrote, and that some of them had actually forgot their reading. `But if you desire,` continued he, `to see a collection of authors, I fancy I can introduce you to a club, which assembles every Saturday at seven ...` I accepted his invitation; we walked together, and entered the house some time before the usual hour for the company assembling. My friend took this opportunity of letting me into the characters of the principal members of the club... `The first person,` said he, `of our society is Doctor Nonentity, a metaphysician. Most people think him a profound scholar, but, as he seldom speaks, I cannot be positive in that particular; he generally spreads himself before the fire, sucks his pipe, talks little, drinks much, and is reckoned very good company. I'm told he writes indexes to perfection: he makes essays on the origin of evil, philosophical inquiries upon any subject, and draws up an answer to any book upon 24 hours' warning...` Goldsmith believes that:

Oliver Goldsmith (1730`"1774) wrote criticism, plays, novels, biographies, travelogues, and nearly every other conceivable kind of composition. This good- humored essay is from a series published in the Public Ledger and then in book form as The Citizen of the World (1762). Were we to estimate the learning of the English by the number of books that are every day published among them, perhaps no country, not even China itself, could equal them in this particular. I have reckoned not less than twenty-three new books published in one day, which, upon computation, makes eight thousand three hundred and ninety-five in one year. Most of these are not confined to one single science, but embrace the whole circle. History, politics, poetry, mathematics, metaphysics, and the philosophy of nature, are all comprised in a manual no larger than that in which our children are taught the letters. If then, we suppose the learned of England to read but an eighth part of the works which daily come from the press and surely non can pretend to learning upon less easy terms), at this rate every scholar will read a thousand books in one year. From such a calculation, you may conjecture what an amazing fund of literature a man must be possessed of, who thus reads three new books every day, not one of which but contains all the good things that ever were said or written. And yet I know not how it happens, but the English are not, in reality so learned as would seem from this calculation. We meet but few who know all arts and sciences to perfection; whether it is that the generality are incapable of such extensive knowledge, or that the authors of those books are not adequate instructors. In China, the Emperor himself takes cognizance of all the doctors in the kingdom who profess authorship. In England, every man may be an author, that can write; for they have by law a liberty, not only of saying what they please, but of being also as dull as they please. Yesterday, as I testified to my surprise, to the man in black, where writers could be found in sufficient number to throw off the books I saw daily crowding from the press. I at first imagined that their learned seminaries might take this method of instructing the world. But, to obviate this objection, my companion assured me that the doctors of colleges never wrote, and that some of them had actually forgot their reading. `But if you desire,` continued he, `to see a collection of authors, I fancy I can introduce you to a club, which assembles every Saturday at seven ...` I accepted his invitation; we walked together, and entered the house some time before the usual hour for the company assembling. My friend took this opportunity of letting me into the characters of the principal members of the club... `The first person,` said he, `of our society is Doctor Nonentity, a metaphysician. Most people think him a profound scholar, but, as he seldom speaks, I cannot be positive in that particular; he generally spreads himself before the fire, sucks his pipe, talks little, drinks much, and is reckoned very good company. I'm told he writes indexes to perfection: he makes essays on the origin of evil, philosophical inquiries upon any subject, and draws up an answer to any book upon 24 hours' warning...` Why does Goldsmith calculate the number of books published in England?