Question is based on the following passage. This passage is from Charlotte Brontë, The Professor, originally published in 1857. No man likes to acknowledge that he has made a mistake in the choice of his profession, and every man, worthy of the name, will row long against wind and tide before he allows himself to cry out, “I am 5 baffled!” and submits to be floated passively back to land. From the first week of my residence in X— felt my occupation irksome. The thing itself—the work of copying and translating business-letters— was a dry and tedious task enough, but had that been 10 all, I should long have borne with the nuisance; I am not of an impatient nature, and influenced by the double desire of getting my living and justifying to myself and others the resolution I had taken to become a tradesman, I should have endured in 15 silence the rust and cramp of my best faculties; I should not have whispered, even inwardly, that I longed for liberty; I should have pent in every sigh by which my heart might have ventured to intimate its distress under the closeness, smoke, monotony, and 20 joyless tumult of Bigben Close, and its panting desire for freer and fresher scenes; I should have set up the image of Duty, the fetish of Perseverance, in my small bedroom at Mrs. King’s lodgings, and they two should have been my household gods, from which 25 my darling, my cherished-in-secret, Imagination, the tender and the mighty, should never, either by softness or strength, have severed me. But this was not all; the antipathy which had sprung up between myself and my employer striking deeper root and 30 spreading denser shade daily, excluded me from every glimpse of the sunshine of life; and I began to feel like a plant growing in humid darkness out of the slimy walls of a well. Antipathy is the only word which can express the 35 feeling Edward Crimsworth had for me—a feeling, in a great measure, involuntary, and which was liable to be excited by every, the most trifling movement, look, or word of mine. My southern accent annoyed him; the degree of education evinced in my language 40 irritated him; my punctuality, industry, and accuracy, fixed his dislike, and gave it the high flavour and poignant relish of envy; he feared that I too should one day make a successful tradesman. Had I been in anything inferior to him, he would not 45 have hated me so thoroughly, but I knew all that he knew, and, what was worse, he suspected that I kept the padlock of silence on mental wealth in which he was no sharer. If he could have once placed me in a ridiculous or mortifying position, he would have 50 forgiven me much, but I was guarded by three faculties—Caution, Tact, Observation; and prowling and prying as was Edward’s malignity, it could never baffle the lynx-eyes of these, my natural sentinels. Day by day did his malice watch my tact, hoping it 55 would sleep, and prepared to steal snake-like on its slumber; but tact, if it be genuine, never sleeps. I had received my first quarter’s wages, and was returning to my lodgings, possessed heart and soul with the pleasant feeling that the master who had 60 paid me grudged every penny of that hard‑earned pittance—(I had long ceased to regard Mr. Crimsworth as my brother—he was a hard, grinding master; he wished to be an inexorable tyrant: that was all). Thoughts, not varied but strong, 65 occupied my mind; two voices spoke within me; again and again they uttered the same monotonous phrases. One said: “William, your life is intolerable.” The other: “What can you do to alter it?” I walked fast, for it was a cold, frosty night in January; as I 70 approached my lodgings, I turned from a general view of my affairs to the particular speculation as to whether my fire would be out; looking towards the window of my sitting-room, I saw no cheering red gleam. Q. Which choice best summarizes the passage?

A character describes his dislike for his new joband considers the reasons why.

Two characters employed in the same officebecome increasingly competitive.

A young man regrets privately a choice that hedefends publicly.

A new employee experiences optimism, thenfrustration, and finally despair.

Question is based on the following passage. This passage is from Charlotte Brontë, The Professor, originally published in 1857. No man likes to acknowledge that he has made a mistake in the choice of his profession, and every man, worthy of the name, will row long against wind and tide before he allows himself to cry out, “I am 5 baffled!” and submits to be floated passively back to land. From the first week of my residence in X— felt my occupation irksome. The thing itself—the work of copying and translating business-letters— was a dry and tedious task enough, but had that been 10 all, I should long have borne with the nuisance; I am not of an impatient nature, and influenced by the double desire of getting my living and justifying to myself and others the resolution I had taken to become a tradesman, I should have endured in 15 silence the rust and cramp of my best faculties; I should not have whispered, even inwardly, that I longed for liberty; I should have pent in every sigh by which my heart might have ventured to intimate its distress under the closeness, smoke, monotony, and 20 joyless tumult of Bigben Close, and its panting desire for freer and fresher scenes; I should have set up the image of Duty, the fetish of Perseverance, in my small bedroom at Mrs. King’s lodgings, and they two should have been my household gods, from which 25 my darling, my cherished-in-secret, Imagination, the tender and the mighty, should never, either by softness or strength, have severed me. But this was not all; the antipathy which had sprung up between myself and my employer striking deeper root and 30 spreading denser shade daily, excluded me from every glimpse of the sunshine of life; and I began to feel like a plant growing in humid darkness out of the slimy walls of a well. Antipathy is the only word which can express the 35 feeling Edward Crimsworth had for me—a feeling, in a great measure, involuntary, and which was liable to be excited by every, the most trifling movement, look, or word of mine. My southern accent annoyed him; the degree of education evinced in my language 40 irritated him; my punctuality, industry, and accuracy, fixed his dislike, and gave it the high flavour and poignant relish of envy; he feared that I too should one day make a successful tradesman. Had I been in anything inferior to him, he would not 45 have hated me so thoroughly, but I knew all that he knew, and, what was worse, he suspected that I kept the padlock of silence on mental wealth in which he was no sharer. If he could have once placed me in a ridiculous or mortifying position, he would have 50 forgiven me much, but I was guarded by three faculties—Caution, Tact, Observation; and prowling and prying as was Edward’s malignity, it could never baffle the lynx-eyes of these, my natural sentinels. Day by day did his malice watch my tact, hoping it 55 would sleep, and prepared to steal snake-like on its slumber; but tact, if it be genuine, never sleeps. I had received my first quarter’s wages, and was returning to my lodgings, possessed heart and soul with the pleasant feeling that the master who had 60 paid me grudged every penny of that hard‑earned pittance—(I had long ceased to regard Mr. Crimsworth as my brother—he was a hard, grinding master; he wished to be an inexorable tyrant: that was all). Thoughts, not varied but strong, 65 occupied my mind; two voices spoke within me; again and again they uttered the same monotonous phrases. One said: “William, your life is intolerable.” The other: “What can you do to alter it?” I walked fast, for it was a cold, frosty night in January; as I 70 approached my lodgings, I turned from a general view of my affairs to the particular speculation as to whether my fire would be out; looking towards the window of my sitting-room, I saw no cheering red gleam. Q. The main purpose of the opening sentence of the passage is to

establish the narrator’s perspective on a controversy.

provide context useful in understanding the narrator’s emotional state.

offer a symbolic representation of Edward Crimsworth’s plight.

contrast the narrator’s good intentions with his malicious conduct.

Question is based on the following passage. This passage is from Charlotte Brontë, The Professor, originally published in 1857. No man likes to acknowledge that he has made a mistake in the choice of his profession, and every man, worthy of the name, will row long against wind and tide before he allows himself to cry out, “I am 5 baffled!” and submits to be floated passively back to land. From the first week of my residence in X— felt my occupation irksome. The thing itself—the work of copying and translating business-letters— was a dry and tedious task enough, but had that been 10 all, I should long have borne with the nuisance; I am not of an impatient nature, and influenced by the double desire of getting my living and justifying to myself and others the resolution I had taken to become a tradesman, I should have endured in 15 silence the rust and cramp of my best faculties; I should not have whispered, even inwardly, that I longed for liberty; I should have pent in every sigh by which my heart might have ventured to intimate its distress under the closeness, smoke, monotony, and 20 joyless tumult of Bigben Close, and its panting desire for freer and fresher scenes; I should have set up the image of Duty, the fetish of Perseverance, in my small bedroom at Mrs. King’s lodgings, and they two should have been my household gods, from which 25 my darling, my cherished-in-secret, Imagination, the tender and the mighty, should never, either by softness or strength, have severed me. But this was not all; the antipathy which had sprung up between myself and my employer striking deeper root and 30 spreading denser shade daily, excluded me from every glimpse of the sunshine of life; and I began to feel like a plant growing in humid darkness out of the slimy walls of a well. Antipathy is the only word which can express the 35 feeling Edward Crimsworth had for me—a feeling, in a great measure, involuntary, and which was liable to be excited by every, the most trifling movement, look, or word of mine. My southern accent annoyed him; the degree of education evinced in my language 40 irritated him; my punctuality, industry, and accuracy, fixed his dislike, and gave it the high flavour and poignant relish of envy; he feared that I too should one day make a successful tradesman. Had I been in anything inferior to him, he would not 45 have hated me so thoroughly, but I knew all that he knew, and, what was worse, he suspected that I kept the padlock of silence on mental wealth in which he was no sharer. If he could have once placed me in a ridiculous or mortifying position, he would have 50 forgiven me much, but I was guarded by three faculties—Caution, Tact, Observation; and prowling and prying as was Edward’s malignity, it could never baffle the lynx-eyes of these, my natural sentinels. Day by day did his malice watch my tact, hoping it 55 would sleep, and prepared to steal snake-like on its slumber; but tact, if it be genuine, never sleeps. I had received my first quarter’s wages, and was returning to my lodgings, possessed heart and soul with the pleasant feeling that the master who had 60 paid me grudged every penny of that hard‑earned pittance—(I had long ceased to regard Mr. Crimsworth as my brother—he was a hard, grinding master; he wished to be an inexorable tyrant: that was all). Thoughts, not varied but strong, 65 occupied my mind; two voices spoke within me; again and again they uttered the same monotonous phrases. One said: “William, your life is intolerable.” The other: “What can you do to alter it?” I walked fast, for it was a cold, frosty night in January; as I 70 approached my lodgings, I turned from a general view of my affairs to the particular speculation as to whether my fire would be out; looking towards the window of my sitting-room, I saw no cheering red gleam. Q. During the course of the first paragraph, the narrator’s focus shifts from

recollection of past confidence to acknowledgment of present self-doubt.

reflection on his expectations of life as a tradesman to his desire for another job.

generalization about job dissatisfaction to the specifics of his own situation.

evaluation of factors making him unhappy to identification of alternatives.

Question is based on the following passage. This passage is from Charlotte Brontë, The Professor, originally published in 1857. No man likes to acknowledge that he has made a mistake in the choice of his profession, and every man, worthy of the name, will row long against wind and tide before he allows himself to cry out, “I am 5 baffled!” and submits to be floated passively back to land. From the first week of my residence in X— felt my occupation irksome. The thing itself—the work of copying and translating business-letters— was a dry and tedious task enough, but had that been 10 all, I should long have borne with the nuisance; I am not of an impatient nature, and influenced by the double desire of getting my living and justifying to myself and others the resolution I had taken to become a tradesman, I should have endured in 15 silence the rust and cramp of my best faculties; I should not have whispered, even inwardly, that I longed for liberty; I should have pent in every sigh by which my heart might have ventured to intimate its distress under the closeness, smoke, monotony, and 20 joyless tumult of Bigben Close, and its panting desire for freer and fresher scenes; I should have set up the image of Duty, the fetish of Perseverance, in my small bedroom at Mrs. King’s lodgings, and they two should have been my household gods, from which 25 my darling, my cherished-in-secret, Imagination, the tender and the mighty, should never, either by softness or strength, have severed me. But this was not all; the antipathy which had sprung up between myself and my employer striking deeper root and 30 spreading denser shade daily, excluded me from every glimpse of the sunshine of life; and I began to feel like a plant growing in humid darkness out of the slimy walls of a well. Antipathy is the only word which can express the 35 feeling Edward Crimsworth had for me—a feeling, in a great measure, involuntary, and which was liable to be excited by every, the most trifling movement, look, or word of mine. My southern accent annoyed him; the degree of education evinced in my language 40 irritated him; my punctuality, industry, and accuracy, fixed his dislike, and gave it the high flavour and poignant relish of envy; he feared that I too should one day make a successful tradesman. Had I been in anything inferior to him, he would not 45 have hated me so thoroughly, but I knew all that he knew, and, what was worse, he suspected that I kept the padlock of silence on mental wealth in which he was no sharer. If he could have once placed me in a ridiculous or mortifying position, he would have 50 forgiven me much, but I was guarded by three faculties—Caution, Tact, Observation; and prowling and prying as was Edward’s malignity, it could never baffle the lynx-eyes of these, my natural sentinels. Day by day did his malice watch my tact, hoping it 55 would sleep, and prepared to steal snake-like on its slumber; but tact, if it be genuine, never sleeps. I had received my first quarter’s wages, and was returning to my lodgings, possessed heart and soul with the pleasant feeling that the master who had 60 paid me grudged every penny of that hard‑earned pittance—(I had long ceased to regard Mr. Crimsworth as my brother—he was a hard, grinding master; he wished to be an inexorable tyrant: that was all). Thoughts, not varied but strong, 65 occupied my mind; two voices spoke within me; again and again they uttered the same monotonous phrases. One said: “William, your life is intolerable.” The other: “What can you do to alter it?” I walked fast, for it was a cold, frosty night in January; as I 70 approached my lodgings, I turned from a general view of my affairs to the particular speculation as to whether my fire would be out; looking towards the window of my sitting-room, I saw no cheering red gleam. Q. The references to “shade” and “darkness” at the end of the first paragraph mainly have which effect?

They evoke the narrator’s sense of dismay.

They reflect the narrator’s sinister thoughts.

They capture the narrator’s fear of confinement.

They reveal the narrator’s longing for rest.

Question is based on the following passage. This passage is from Charlotte Brontë, The Professor, originally published in 1857. No man likes to acknowledge that he has made a mistake in the choice of his profession, and every man, worthy of the name, will row long against wind and tide before he allows himself to cry out, “I am 5 baffled!” and submits to be floated passively back to land. From the first week of my residence in X— felt my occupation irksome. The thing itself—the work of copying and translating business-letters— was a dry and tedious task enough, but had that been 10 all, I should long have borne with the nuisance; I am not of an impatient nature, and influenced by the double desire of getting my living and justifying to myself and others the resolution I had taken to become a tradesman, I should have endured in 15 silence the rust and cramp of my best faculties; I should not have whispered, even inwardly, that I longed for liberty; I should have pent in every sigh by which my heart might have ventured to intimate its distress under the closeness, smoke, monotony, and 20 joyless tumult of Bigben Close, and its panting desire for freer and fresher scenes; I should have set up the image of Duty, the fetish of Perseverance, in my small bedroom at Mrs. King’s lodgings, and they two should have been my household gods, from which 25 my darling, my cherished-in-secret, Imagination, the tender and the mighty, should never, either by softness or strength, have severed me. But this was not all; the antipathy which had sprung up between myself and my employer striking deeper root and 30 spreading denser shade daily, excluded me from every glimpse of the sunshine of life; and I began to feel like a plant growing in humid darkness out of the slimy walls of a well. Antipathy is the only word which can express the 35 feeling Edward Crimsworth had for me—a feeling, in a great measure, involuntary, and which was liable to be excited by every, the most trifling movement, look, or word of mine. My southern accent annoyed him; the degree of education evinced in my language 40 irritated him; my punctuality, industry, and accuracy, fixed his dislike, and gave it the high flavour and poignant relish of envy; he feared that I too should one day make a successful tradesman. Had I been in anything inferior to him, he would not 45 have hated me so thoroughly, but I knew all that he knew, and, what was worse, he suspected that I kept the padlock of silence on mental wealth in which he was no sharer. If he could have once placed me in a ridiculous or mortifying position, he would have 50 forgiven me much, but I was guarded by three faculties—Caution, Tact, Observation; and prowling and prying as was Edward’s malignity, it could never baffle the lynx-eyes of these, my natural sentinels. Day by day did his malice watch my tact, hoping it 55 would sleep, and prepared to steal snake-like on its slumber; but tact, if it be genuine, never sleeps. I had received my first quarter’s wages, and was returning to my lodgings, possessed heart and soul with the pleasant feeling that the master who had 60 paid me grudged every penny of that hard‑earned pittance—(I had long ceased to regard Mr. Crimsworth as my brother—he was a hard, grinding master; he wished to be an inexorable tyrant: that was all). Thoughts, not varied but strong, 65 occupied my mind; two voices spoke within me; again and again they uttered the same monotonous phrases. One said: “William, your life is intolerable.” The other: “What can you do to alter it?” I walked fast, for it was a cold, frosty night in January; as I 70 approached my lodgings, I turned from a general view of my affairs to the particular speculation as to whether my fire would be out; looking towards the window of my sitting-room, I saw no cheering red gleam. Q. The passage indicates that Edward Crimsworth’s behavior was mainly caused by his

impatience with the narrator’s high spirits.

scorn of the narrator’s humble background.

indignation at the narrator’s rash actions.

jealousy of the narrator’s apparent superiority

Question is based on the following passage. This passage is from Charlotte Brontë, The Professor, originally published in 1857. No man likes to acknowledge that he has made a mistake in the choice of his profession, and every man, worthy of the name, will row long against wind and tide before he allows himself to cry out, “I am 5 baffled!” and submits to be floated passively back to land. From the first week of my residence in X— felt my occupation irksome. The thing itself—the work of copying and translating business-letters— was a dry and tedious task enough, but had that been 10 all, I should long have borne with the nuisance; I am not of an impatient nature, and influenced by the double desire of getting my living and justifying to myself and others the resolution I had taken to become a tradesman, I should have endured in 15 silence the rust and cramp of my best faculties; I should not have whispered, even inwardly, that I longed for liberty; I should have pent in every sigh by which my heart might have ventured to intimate its distress under the closeness, smoke, monotony, and 20 joyless tumult of Bigben Close, and its panting desire for freer and fresher scenes; I should have set up the image of Duty, the fetish of Perseverance, in my small bedroom at Mrs. King’s lodgings, and they two should have been my household gods, from which 25 my darling, my cherished-in-secret, Imagination, the tender and the mighty, should never, either by softness or strength, have severed me. But this was not all; the antipathy which had sprung up between myself and my employer striking deeper root and 30 spreading denser shade daily, excluded me from every glimpse of the sunshine of life; and I began to feel like a plant growing in humid darkness out of the slimy walls of a well. Antipathy is the only word which can express the 35 feeling Edward Crimsworth had for me—a feeling, in a great measure, involuntary, and which was liable to be excited by every, the most trifling movement, look, or word of mine. My southern accent annoyed him; the degree of education evinced in my language 40 irritated him; my punctuality, industry, and accuracy, fixed his dislike, and gave it the high flavour and poignant relish of envy; he feared that I too should one day make a successful tradesman. Had I been in anything inferior to him, he would not 45 have hated me so thoroughly, but I knew all that he knew, and, what was worse, he suspected that I kept the padlock of silence on mental wealth in which he was no sharer. If he could have once placed me in a ridiculous or mortifying position, he would have 50 forgiven me much, but I was guarded by three faculties—Caution, Tact, Observation; and prowling and prying as was Edward’s malignity, it could never baffle the lynx-eyes of these, my natural sentinels. Day by day did his malice watch my tact, hoping it 55 would sleep, and prepared to steal snake-like on its slumber; but tact, if it be genuine, never sleeps. I had received my first quarter’s wages, and was returning to my lodgings, possessed heart and soul with the pleasant feeling that the master who had 60 paid me grudged every penny of that hard‑earned pittance—(I had long ceased to regard Mr. Crimsworth as my brother—he was a hard, grinding master; he wished to be an inexorable tyrant: that was all). Thoughts, not varied but strong, 65 occupied my mind; two voices spoke within me; again and again they uttered the same monotonous phrases. One said: “William, your life is intolerable.” The other: “What can you do to alter it?” I walked fast, for it was a cold, frosty night in January; as I 70 approached my lodgings, I turned from a general view of my affairs to the particular speculation as to whether my fire would be out; looking towards the window of my sitting-room, I saw no cheering red gleam. Q. Which choice provides the best evidence for the answer to the previous question?

Lines 28-31 (“the antipathy... life”)

Lines 38-40 (“My southern... irritated him”)

Lines 54-56 (“Day... slumber”)

Lines 61-62 (“I had... brother”)

Question is based on the following passage. This passage is from Charlotte Brontë, The Professor, originally published in 1857. No man likes to acknowledge that he has made a mistake in the choice of his profession, and every man, worthy of the name, will row long against wind and tide before he allows himself to cry out, “I am 5 baffled!” and submits to be floated passively back to land. From the first week of my residence in X— felt my occupation irksome. The thing itself—the work of copying and translating business-letters— was a dry and tedious task enough, but had that been 10 all, I should long have borne with the nuisance; I am not of an impatient nature, and influenced by the double desire of getting my living and justifying to myself and others the resolution I had taken to become a tradesman, I should have endured in 15 silence the rust and cramp of my best faculties; I should not have whispered, even inwardly, that I longed for liberty; I should have pent in every sigh by which my heart might have ventured to intimate its distress under the closeness, smoke, monotony, and 20 joyless tumult of Bigben Close, and its panting desire for freer and fresher scenes; I should have set up the image of Duty, the fetish of Perseverance, in my small bedroom at Mrs. King’s lodgings, and they two should have been my household gods, from which 25 my darling, my cherished-in-secret, Imagination, the tender and the mighty, should never, either by softness or strength, have severed me. But this was not all; the antipathy which had sprung up between myself and my employer striking deeper root and 30 spreading denser shade daily, excluded me from every glimpse of the sunshine of life; and I began to feel like a plant growing in humid darkness out of the slimy walls of a well. Antipathy is the only word which can express the 35 feeling Edward Crimsworth had for me—a feeling, in a great measure, involuntary, and which was liable to be excited by every, the most trifling movement, look, or word of mine. My southern accent annoyed him; the degree of education evinced in my language 40 irritated him; my punctuality, industry, and accuracy, fixed his dislike, and gave it the high flavour and poignant relish of envy; he feared that I too should one day make a successful tradesman. Had I been in anything inferior to him, he would not 45 have hated me so thoroughly, but I knew all that he knew, and, what was worse, he suspected that I kept the padlock of silence on mental wealth in which he was no sharer. If he could have once placed me in a ridiculous or mortifying position, he would have 50 forgiven me much, but I was guarded by three faculties—Caution, Tact, Observation; and prowling and prying as was Edward’s malignity, it could never baffle the lynx-eyes of these, my natural sentinels. Day by day did his malice watch my tact, hoping it 55 would sleep, and prepared to steal snake-like on its slumber; but tact, if it be genuine, never sleeps. I had received my first quarter’s wages, and was returning to my lodgings, possessed heart and soul with the pleasant feeling that the master who had 60 paid me grudged every penny of that hard‑earned pittance—(I had long ceased to regard Mr. Crimsworth as my brother—he was a hard, grinding master; he wished to be an inexorable tyrant: that was all). Thoughts, not varied but strong, 65 occupied my mind; two voices spoke within me; again and again they uttered the same monotonous phrases. One said: “William, your life is intolerable.” The other: “What can you do to alter it?” I walked fast, for it was a cold, frosty night in January; as I 70 approached my lodgings, I turned from a general view of my affairs to the particular speculation as to whether my fire would be out; looking towards the window of my sitting-room, I saw no cheering red gleam. Q. At the end of the second paragraph, the comparisons of abstract qualities to a lynx and a snake mainly have the effect of

contrasting two hypothetical courses of action.

conveying the ferocity of a resolution.

suggesting the likelihood of an altercation.

illustrating the nature of an adversarial relationship

Question is based on the following passage. This passage is from Charlotte Brontë, The Professor, originally published in 1857. No man likes to acknowledge that he has made a mistake in the choice of his profession, and every man, worthy of the name, will row long against wind and tide before he allows himself to cry out, “I am 5 baffled!” and submits to be floated passively back to land. From the first week of my residence in X— felt my occupation irksome. The thing itself—the work of copying and translating business-letters— was a dry and tedious task enough, but had that been 10 all, I should long have borne with the nuisance; I am not of an impatient nature, and influenced by the double desire of getting my living and justifying to myself and others the resolution I had taken to become a tradesman, I should have endured in 15 silence the rust and cramp of my best faculties; I should not have whispered, even inwardly, that I longed for liberty; I should have pent in every sigh by which my heart might have ventured to intimate its distress under the closeness, smoke, monotony, and 20 joyless tumult of Bigben Close, and its panting desire for freer and fresher scenes; I should have set up the image of Duty, the fetish of Perseverance, in my small bedroom at Mrs. King’s lodgings, and they two should have been my household gods, from which 25 my darling, my cherished-in-secret, Imagination, the tender and the mighty, should never, either by softness or strength, have severed me. But this was not all; the antipathy which had sprung up between myself and my employer striking deeper root and 30 spreading denser shade daily, excluded me from every glimpse of the sunshine of life; and I began to feel like a plant growing in humid darkness out of the slimy walls of a well. Antipathy is the only word which can express the 35 feeling Edward Crimsworth had for me—a feeling, in a great measure, involuntary, and which was liable to be excited by every, the most trifling movement, look, or word of mine. My southern accent annoyed him; the degree of education evinced in my language 40 irritated him; my punctuality, industry, and accuracy, fixed his dislike, and gave it the high flavour and poignant relish of envy; he feared that I too should one day make a successful tradesman. Had I been in anything inferior to him, he would not 45 have hated me so thoroughly, but I knew all that he knew, and, what was worse, he suspected that I kept the padlock of silence on mental wealth in which he was no sharer. If he could have once placed me in a ridiculous or mortifying position, he would have 50 forgiven me much, but I was guarded by three faculties—Caution, Tact, Observation; and prowling and prying as was Edward’s malignity, it could never baffle the lynx-eyes of these, my natural sentinels. Day by day did his malice watch my tact, hoping it 55 would sleep, and prepared to steal snake-like on its slumber; but tact, if it be genuine, never sleeps. I had received my first quarter’s wages, and was returning to my lodgings, possessed heart and soul with the pleasant feeling that the master who had 60 paid me grudged every penny of that hard‑earned pittance—(I had long ceased to regard Mr. Crimsworth as my brother—he was a hard, grinding master; he wished to be an inexorable tyrant: that was all). Thoughts, not varied but strong, 65 occupied my mind; two voices spoke within me; again and again they uttered the same monotonous phrases. One said: “William, your life is intolerable.” The other: “What can you do to alter it?” I walked fast, for it was a cold, frosty night in January; as I 70 approached my lodgings, I turned from a general view of my affairs to the particular speculation as to whether my fire would be out; looking towards the window of my sitting-room, I saw no cheering red gleam. Q. Which choice provides the best evidence for the answer to the previous question?

Lines 17-21 (“I should... scenes”)

Lines 21-23 (“I should... lodgings”)

Lines 64-67 (“Thoughts... phrases”)

Lines 68-74 (“I walked... gleam”)

Question is based on the following passage and supplementary material. This passage is adapted from Geoffrey Giller, “Long a Mystery, How 500-Meter-High Undersea Waves Form Is Revealed.” ©2014 by Scientific American. Some of the largest ocean waves in the world are nearly impossible to see. Unlike other large waves, these rollers, called internal waves, do not ride the ocean surface. Instead, they move underwater, 5 undetectable without the use of satellite imagery or sophisticated monitoring equipment. Despite their hidden nature, internal waves are fundamental parts of ocean water dynamics, transferring heat to the ocean depths and bringing up cold water from below. 10 And they can reach staggering heights—some as tall as skyscrapers. Because these waves are involved in ocean mixing and thus the transfer of heat, understanding them is crucial to global climate modeling, says Tom 15 Peacock, a researcher at the Massachusetts Institute of Technology. Most models fail to take internal waves into account. “If we want to have more and more accurate climate models, we have to be able to capture processes such as this,” Peacock says. 20 Peacock and his colleagues tried to do just that. Their study, published in November in Geophysical Research Letters, focused on internal waves generated in the Luzon Strait, which separates Taiwan and the Philippines. Internal waves in this region, thought to 25 be some of the largest in the world, can reach about 500 meters high. “That’s the same height as the Freedom Tower that’s just been built in New York,” Peacock says. Although scientists knew of this phenomenon in 30 the South China Sea and beyond, they didn’t know exactly how internal waves formed. To find out, Peacock and a team of researchers from M.I.T. and Woods Hole Oceanographic Institution worked with France’s National Center for Scientific Research 35 using a giant facility there called the Coriolis Platform. The rotating platform, about 15 meters (49.2 feet) in diameter, turns at variable speeds and can simulate Earth’s rotation. It also has walls, which means scientists can fill it with water and create 40 accurate, large-scale simulations of various oceanographic scenarios. Peacock and his team built a carbon-fiber resin scale model of the Luzon Strait, including the islands and surrounding ocean floor topography. Then they 45 filled the platform with water of varying salinity to replicate the different densities found at the strait, with denser, saltier water below and lighter, less briny water above. Small particles were added to the solution and illuminated with lights from below in 50 order to track how the liquid moved. Finally, they re-created tides using two large plungers to see how the internal waves themselves formed. The Luzon Strait’s underwater topography, with a distinct double-ridge shape, turns out to be 55 responsible for generating the underwater waves. As the tide rises and falls and water moves through the strait, colder, denser water is pushed up over the ridges into warmer, less dense layers above it. This action results in bumps of colder water trailed 60 by warmer water that generate an internal wave. As these waves move toward land, they become steeper—much the same way waves at the beach become taller before they hit the shore—until they break on a continental shelf. 65 The researchers were also able to devise a mathematical model that describes the movement and formation of these waves. Whereas the model is specific to the Luzon Strait, it can still help researchers understand how internal waves are 70 generated in other places around the world. Eventually, this information will be incorporated into global climate models, making them more accurate. “It’s very clear, within the context of these [global climate] models, that internal waves play a role in 75 driving ocean circulations,” Peacock says. Q. The first paragraph serves mainly to

explain how a scientific device is used.

note a common misconception about an event.

describe a natural phenomenon and address itsimportance.

present a recent study and summarize itsfindings.

Question is based on the following passage and supplementary material. This passage is adapted from Geoffrey Giller, “Long a Mystery, How 500-Meter-High Undersea Waves Form Is Revealed.” ©2014 by Scientific American. Some of the largest ocean waves in the world are nearly impossible to see. Unlike other large waves, these rollers, called internal waves, do not ride the ocean surface. Instead, they move underwater, 5 undetectable without the use of satellite imagery or sophisticated monitoring equipment. Despite their hidden nature, internal waves are fundamental parts of ocean water dynamics, transferring heat to the ocean depths and bringing up cold water from below. 10 And they can reach staggering heights—some as tall as skyscrapers. Because these waves are involved in ocean mixing and thus the transfer of heat, understanding them is crucial to global climate modeling, says Tom 15 Peacock, a researcher at the Massachusetts Institute of Technology. Most models fail to take internal waves into account. “If we want to have more and more accurate climate models, we have to be able to capture processes such as this,” Peacock says. 20 Peacock and his colleagues tried to do just that. Their study, published in November in Geophysical Research Letters, focused on internal waves generated in the Luzon Strait, which separates Taiwan and the Philippines. Internal waves in this region, thought to 25 be some of the largest in the world, can reach about 500 meters high. “That’s the same height as the Freedom Tower that’s just been built in New York,” Peacock says. Although scientists knew of this phenomenon in 30 the South China Sea and beyond, they didn’t know exactly how internal waves formed. To find out, Peacock and a team of researchers from M.I.T. and Woods Hole Oceanographic Institution worked with France’s National Center for Scientific Research 35 using a giant facility there called the Coriolis Platform. The rotating platform, about 15 meters (49.2 feet) in diameter, turns at variable speeds and can simulate Earth’s rotation. It also has walls, which means scientists can fill it with water and create 40 accurate, large-scale simulations of various oceanographic scenarios. Peacock and his team built a carbon-fiber resin scale model of the Luzon Strait, including the islands and surrounding ocean floor topography. Then they 45 filled the platform with water of varying salinity to replicate the different densities found at the strait, with denser, saltier water below and lighter, less briny water above. Small particles were added to the solution and illuminated with lights from below in 50 order to track how the liquid moved. Finally, they re-created tides using two large plungers to see how the internal waves themselves formed. The Luzon Strait’s underwater topography, with a distinct double-ridge shape, turns out to be 55 responsible for generating the underwater waves. As the tide rises and falls and water moves through the strait, colder, denser water is pushed up over the ridges into warmer, less dense layers above it. This action results in bumps of colder water trailed 60 by warmer water that generate an internal wave. As these waves move toward land, they become steeper—much the same way waves at the beach become taller before they hit the shore—until they break on a continental shelf. 65 The researchers were also able to devise a mathematical model that describes the movement and formation of these waves. Whereas the model is specific to the Luzon Strait, it can still help researchers understand how internal waves are 70 generated in other places around the world. Eventually, this information will be incorporated into global climate models, making them more accurate. “It’s very clear, within the context of these [global climate] models, that internal waves play a role in 75 driving ocean circulations,” Peacock says. Q. According to Peacock, the ability to monitor internal waves is significant primarily because

it will allow scientists to verify the maximum height of such waves.

it will allow researchers to shift their focus to improving the quality of satellite images.

the study of wave patterns will enable regions to predict and prevent coastal damage.

the study of such waves will inform the development of key scientific models.

Question is based on the following passage and supplementary material. This passage is adapted from Geoffrey Giller, “Long a Mystery, How 500-Meter-High Undersea Waves Form Is Revealed.” ©2014 by Scientific American. Some of the largest ocean waves in the world are nearly impossible to see. Unlike other large waves, these rollers, called internal waves, do not ride the ocean surface. Instead, they move underwater, 5 undetectable without the use of satellite imagery or sophisticated monitoring equipment. Despite their hidden nature, internal waves are fundamental parts of ocean water dynamics, transferring heat to the ocean depths and bringing up cold water from below. 10 And they can reach staggering heights—some as tall as skyscrapers. Because these waves are involved in ocean mixing and thus the transfer of heat, understanding them is crucial to global climate modeling, says Tom 15 Peacock, a researcher at the Massachusetts Institute of Technology. Most models fail to take internal waves into account. “If we want to have more and more accurate climate models, we have to be able to capture processes such as this,” Peacock says. 20 Peacock and his colleagues tried to do just that. Their study, published in November in Geophysical Research Letters, focused on internal waves generated in the Luzon Strait, which separates Taiwan and the Philippines. Internal waves in this region, thought to 25 be some of the largest in the world, can reach about 500 meters high. “That’s the same height as the Freedom Tower that’s just been built in New York,” Peacock says. Although scientists knew of this phenomenon in 30 the South China Sea and beyond, they didn’t know exactly how internal waves formed. To find out, Peacock and a team of researchers from M.I.T. and Woods Hole Oceanographic Institution worked with France’s National Center for Scientific Research 35 using a giant facility there called the Coriolis Platform. The rotating platform, about 15 meters (49.2 feet) in diameter, turns at variable speeds and can simulate Earth’s rotation. It also has walls, which means scientists can fill it with water and create 40 accurate, large-scale simulations of various oceanographic scenarios. Peacock and his team built a carbon-fiber resin scale model of the Luzon Strait, including the islands and surrounding ocean floor topography. Then they 45 filled the platform with water of varying salinity to replicate the different densities found at the strait, with denser, saltier water below and lighter, less briny water above. Small particles were added to the solution and illuminated with lights from below in 50 order to track how the liquid moved. Finally, they re-created tides using two large plungers to see how the internal waves themselves formed. The Luzon Strait’s underwater topography, with a distinct double-ridge shape, turns out to be 55 responsible for generating the underwater waves. As the tide rises and falls and water moves through the strait, colder, denser water is pushed up over the ridges into warmer, less dense layers above it. This action results in bumps of colder water trailed 60 by warmer water that generate an internal wave. As these waves move toward land, they become steeper—much the same way waves at the beach become taller before they hit the shore—until they break on a continental shelf. 65 The researchers were also able to devise a mathematical model that describes the movement and formation of these waves. Whereas the model is specific to the Luzon Strait, it can still help researchers understand how internal waves are 70 generated in other places around the world. Eventually, this information will be incorporated into global climate models, making them more accurate. “It’s very clear, within the context of these [global climate] models, that internal waves play a role in 75 driving ocean circulations,” Peacock says. Q. Which choice provides the best evidence for the answer to the previous question?

Lines 4-6 (“they... equipment”)

Lines 24-26 (“Internal... high”)

Question is based on the following passage and supplementary material. This passage is adapted from Geoffrey Giller, “Long a Mystery, How 500-Meter-High Undersea Waves Form Is Revealed.” ©2014 by Scientific American. Some of the largest ocean waves in the world are nearly impossible to see. Unlike other large waves, these rollers, called internal waves, do not ride the ocean surface. Instead, they move underwater, 5 undetectable without the use of satellite imagery or sophisticated monitoring equipment. Despite their hidden nature, internal waves are fundamental parts of ocean water dynamics, transferring heat to the ocean depths and bringing up cold water from below. 10 And they can reach staggering heights—some as tall as skyscrapers. Because these waves are involved in ocean mixing and thus the transfer of heat, understanding them is crucial to global climate modeling, says Tom 15 Peacock, a researcher at the Massachusetts Institute of Technology. Most models fail to take internal waves into account. “If we want to have more and more accurate climate models, we have to be able to capture processes such as this,” Peacock says. 20 Peacock and his colleagues tried to do just that. Their study, published in November in Geophysical Research Letters, focused on internal waves generated in the Luzon Strait, which separates Taiwan and the Philippines. Internal waves in this region, thought to 25 be some of the largest in the world, can reach about 500 meters high. “That’s the same height as the Freedom Tower that’s just been built in New York,” Peacock says. Although scientists knew of this phenomenon in 30 the South China Sea and beyond, they didn’t know exactly how internal waves formed. To find out, Peacock and a team of researchers from M.I.T. and Woods Hole Oceanographic Institution worked with France’s National Center for Scientific Research 35 using a giant facility there called the Coriolis Platform. The rotating platform, about 15 meters (49.2 feet) in diameter, turns at variable speeds and can simulate Earth’s rotation. It also has walls, which means scientists can fill it with water and create 40 accurate, large-scale simulations of various oceanographic scenarios. Peacock and his team built a carbon-fiber resin scale model of the Luzon Strait, including the islands and surrounding ocean floor topography. Then they 45 filled the platform with water of varying salinity to replicate the different densities found at the strait, with denser, saltier water below and lighter, less briny water above. Small particles were added to the solution and illuminated with lights from below in 50 order to track how the liquid moved. Finally, they re-created tides using two large plungers to see how the internal waves themselves formed. The Luzon Strait’s underwater topography, with a distinct double-ridge shape, turns out to be 55 responsible for generating the underwater waves. As the tide rises and falls and water moves through the strait, colder, denser water is pushed up over the ridges into warmer, less dense layers above it. This action results in bumps of colder water trailed 60 by warmer water that generate an internal wave. As these waves move toward land, they become steeper—much the same way waves at the beach become taller before they hit the shore—until they break on a continental shelf. 65 The researchers were also able to devise a mathematical model that describes the movement and formation of these waves. Whereas the model is specific to the Luzon Strait, it can still help researchers understand how internal waves are 70 generated in other places around the world. Eventually, this information will be incorporated into global climate models, making them more accurate. “It’s very clear, within the context of these [global climate] models, that internal waves play a role in 75 driving ocean circulations,” Peacock says. Q. Based on information in the passage, it can reasonably be inferred that all internal waves

reach approximately the same height even though the locations and depths of continental shelves vary.

may be caused by similar factors but are influenced by the distinct topographies of different regions.

can be traced to inconsistencies in the tidal patterns of deep ocean water located near islands.

are generated by the movement of dense water over a relatively flat section of the ocean floor.

Question is based on the following passage and supplementary material. This passage is adapted from Geoffrey Giller, “Long a Mystery, How 500-Meter-High Undersea Waves Form Is Revealed.” ©2014 by Scientific American. Some of the largest ocean waves in the world are nearly impossible to see. Unlike other large waves, these rollers, called internal waves, do not ride the ocean surface. Instead, they move underwater, 5 undetectable without the use of satellite imagery or sophisticated monitoring equipment. Despite their hidden nature, internal waves are fundamental parts of ocean water dynamics, transferring heat to the ocean depths and bringing up cold water from below. 10 And they can reach staggering heights—some as tall as skyscrapers. Because these waves are involved in ocean mixing and thus the transfer of heat, understanding them is crucial to global climate modeling, says Tom 15 Peacock, a researcher at the Massachusetts Institute of Technology. Most models fail to take internal waves into account. “If we want to have more and more accurate climate models, we have to be able to capture processes such as this,” Peacock says. 20 Peacock and his colleagues tried to do just that. Their study, published in November in Geophysical Research Letters, focused on internal waves generated in the Luzon Strait, which separates Taiwan and the Philippines. Internal waves in this region, thought to 25 be some of the largest in the world, can reach about 500 meters high. “That’s the same height as the Freedom Tower that’s just been built in New York,” Peacock says. Although scientists knew of this phenomenon in 30 the South China Sea and beyond, they didn’t know exactly how internal waves formed. To find out, Peacock and a team of researchers from M.I.T. and Woods Hole Oceanographic Institution worked with France’s National Center for Scientific Research 35 using a giant facility there called the Coriolis Platform. The rotating platform, about 15 meters (49.2 feet) in diameter, turns at variable speeds and can simulate Earth’s rotation. It also has walls, which means scientists can fill it with water and create 40 accurate, large-scale simulations of various oceanographic scenarios. Peacock and his team built a carbon-fiber resin scale model of the Luzon Strait, including the islands and surrounding ocean floor topography. Then they 45 filled the platform with water of varying salinity to replicate the different densities found at the strait, with denser, saltier water below and lighter, less briny water above. Small particles were added to the solution and illuminated with lights from below in 50 order to track how the liquid moved. Finally, they re-created tides using two large plungers to see how the internal waves themselves formed. The Luzon Strait’s underwater topography, with a distinct double-ridge shape, turns out to be 55 responsible for generating the underwater waves. As the tide rises and falls and water moves through the strait, colder, denser water is pushed up over the ridges into warmer, less dense layers above it. This action results in bumps of colder water trailed 60 by warmer water that generate an internal wave. As these waves move toward land, they become steeper—much the same way waves at the beach become taller before they hit the shore—until they break on a continental shelf. 65 The researchers were also able to devise a mathematical model that describes the movement and formation of these waves. Whereas the model is specific to the Luzon Strait, it can still help researchers understand how internal waves are 70 generated in other places around the world. Eventually, this information will be incorporated into global climate models, making them more accurate. “It’s very clear, within the context of these [global climate] models, that internal waves play a role in 75 driving ocean circulations,” Peacock says. Q. Which choice provides the best evidence for the answer to the previous question?

Lines 29-31 (“Although... formed”)

Lines 56-58 (“As the... it”)

Lines 61-64 (“As these... shelf”)

Lines 67-70 (“Whereas... world”)

Question is based on the following passage and supplementary material. This passage is adapted from Geoffrey Giller, “Long a Mystery, How 500-Meter-High Undersea Waves Form Is Revealed.” ©2014 by Scientific American. Some of the largest ocean waves in the world are nearly impossible to see. Unlike other large waves, these rollers, called internal waves, do not ride the ocean surface. Instead, they move underwater, 5 undetectable without the use of satellite imagery or sophisticated monitoring equipment. Despite their hidden nature, internal waves are fundamental parts of ocean water dynamics, transferring heat to the ocean depths and bringing up cold water from below. 10 And they can reach staggering heights—some as tall as skyscrapers. Because these waves are involved in ocean mixing and thus the transfer of heat, understanding them is crucial to global climate modeling, says Tom 15 Peacock, a researcher at the Massachusetts Institute of Technology. Most models fail to take internal waves into account. “If we want to have more and more accurate climate models, we have to be able to capture processes such as this,” Peacock says. 20 Peacock and his colleagues tried to do just that. Their study, published in November in Geophysical Research Letters, focused on internal waves generated in the Luzon Strait, which separates Taiwan and the Philippines. Internal waves in this region, thought to 25 be some of the largest in the world, can reach about 500 meters high. “That’s the same height as the Freedom Tower that’s just been built in New York,” Peacock says. Although scientists knew of this phenomenon in 30 the South China Sea and beyond, they didn’t know exactly how internal waves formed. To find out, Peacock and a team of researchers from M.I.T. and Woods Hole Oceanographic Institution worked with France’s National Center for Scientific Research 35 using a giant facility there called the Coriolis Platform. The rotating platform, about 15 meters (49.2 feet) in diameter, turns at variable speeds and can simulate Earth’s rotation. It also has walls, which means scientists can fill it with water and create 40 accurate, large-scale simulations of various oceanographic scenarios. Peacock and his team built a carbon-fiber resin scale model of the Luzon Strait, including the islands and surrounding ocean floor topography. Then they 45 filled the platform with water of varying salinity to replicate the different densities found at the strait, with denser, saltier water below and lighter, less briny water above. Small particles were added to the solution and illuminated with lights from below in 50 order to track how the liquid moved. Finally, they re-created tides using two large plungers to see how the internal waves themselves formed. The Luzon Strait’s underwater topography, with a distinct double-ridge shape, turns out to be 55 responsible for generating the underwater waves. As the tide rises and falls and water moves through the strait, colder, denser water is pushed up over the ridges into warmer, less dense layers above it. This action results in bumps of colder water trailed 60 by warmer water that generate an internal wave. As these waves move toward land, they become steeper—much the same way waves at the beach become taller before they hit the shore—until they break on a continental shelf. 65 The researchers were also able to devise a mathematical model that describes the movement and formation of these waves. Whereas the model is specific to the Luzon Strait, it can still help researchers understand how internal waves are 70 generated in other places around the world. Eventually, this information will be incorporated into global climate models, making them more accurate. “It’s very clear, within the context of these [global climate] models, that internal waves play a role in 75 driving ocean circulations,” Peacock says. Q. Which concept is supported by the passage and by the information in the graph?

Internal waves cause water of varying salinity to mix.

Internal waves push denser water above layers of less dense water.

Internal waves push bands of cold water above bands of warmer water.

Internal waves do not rise to break the ocean’s surface.

Question is based on the following passage and supplementary material. This passage is adapted from Geoffrey Giller, “Long a Mystery, How 500-Meter-High Undersea Waves Form Is Revealed.” ©2014 by Scientific American. Some of the largest ocean waves in the world are nearly impossible to see. Unlike other large waves, these rollers, called internal waves, do not ride the ocean surface. Instead, they move underwater, 5 undetectable without the use of satellite imagery or sophisticated monitoring equipment. Despite their hidden nature, internal waves are fundamental parts of ocean water dynamics, transferring heat to the ocean depths and bringing up cold water from below. 10 And they can reach staggering heights—some as tall as skyscrapers. Because these waves are involved in ocean mixing and thus the transfer of heat, understanding them is crucial to global climate modeling, says Tom 15 Peacock, a researcher at the Massachusetts Institute of Technology. Most models fail to take internal waves into account. “If we want to have more and more accurate climate models, we have to be able to capture processes such as this,” Peacock says. 20 Peacock and his colleagues tried to do just that. Their study, published in November in Geophysical Research Letters, focused on internal waves generated in the Luzon Strait, which separates Taiwan and the Philippines. Internal waves in this region, thought to 25 be some of the largest in the world, can reach about 500 meters high. “That’s the same height as the Freedom Tower that’s just been built in New York,” Peacock says. Although scientists knew of this phenomenon in 30 the South China Sea and beyond, they didn’t know exactly how internal waves formed. To find out, Peacock and a team of researchers from M.I.T. and Woods Hole Oceanographic Institution worked with France’s National Center for Scientific Research 35 using a giant facility there called the Coriolis Platform. The rotating platform, about 15 meters (49.2 feet) in diameter, turns at variable speeds and can simulate Earth’s rotation. It also has walls, which means scientists can fill it with water and create 40 accurate, large-scale simulations of various oceanographic scenarios. Peacock and his team built a carbon-fiber resin scale model of the Luzon Strait, including the islands and surrounding ocean floor topography. Then they 45 filled the platform with water of varying salinity to replicate the different densities found at the strait, with denser, saltier water below and lighter, less briny water above. Small particles were added to the solution and illuminated with lights from below in 50 order to track how the liquid moved. Finally, they re-created tides using two large plungers to see how the internal waves themselves formed. The Luzon Strait’s underwater topography, with a distinct double-ridge shape, turns out to be 55 responsible for generating the underwater waves. As the tide rises and falls and water moves through the strait, colder, denser water is pushed up over the ridges into warmer, less dense layers above it. This action results in bumps of colder water trailed 60 by warmer water that generate an internal wave. As these waves move toward land, they become steeper—much the same way waves at the beach become taller before they hit the shore—until they break on a continental shelf. 65 The researchers were also able to devise a mathematical model that describes the movement and formation of these waves. Whereas the model is specific to the Luzon Strait, it can still help researchers understand how internal waves are 70 generated in other places around the world. Eventually, this information will be incorporated into global climate models, making them more accurate. “It’s very clear, within the context of these [global climate] models, that internal waves play a role in 75 driving ocean circulations,” Peacock says. Q. How does the graph support the author’s point that internal waves affect ocean water dynamics?

It demonstrates that wave movement forces warmer water down to depths that typically are colder.

It reveals the degree to which an internal wave affects the density of deep layers of cold water.

It illustrates the change in surface temperature that takes place during an isolated series of deep waves.

It shows that multiple waves rising near the surface of the ocean disrupt the flow of normal tides.

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