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Direction: Read the passage carefully and answer the questions
The last ice age has left its telltales written quite clearly across the landscape. When Louis Agassiz first promulgated his theory that ice had once covered the Swiss countryside, he looked to the valleys there that retain glaciers to this day. Like other observers, he noted the presence of strange boulders, called "erratics, " tossed down in valleys like flotsam after a flood had drained away. He saw the strange polish along the bedrock—a sheen imparted as if by some massive swipe of sandpaper; he saw the debris of rocks and boulders fringing the margin of existing glaciers. He saw what can be seen still, markings in stone that indicated that ice once flowed over vast stretches of land now clear and verdant.
The first great glaciations must have scored the earth as deeply in their turn, and, in principle, we ought to be able to track the history of the early ice ages by following the same reasoning Agassiz used to persuade himself and his contemporaries that ice once covered the earth. But the marks left by these earlier glaciations are quite subtle, tracks turned ghostly with great age. There are, however, telltale deposits of ancient rocks that strongly suggest that they had been ground together and laid down by the spread of ice.
The Australian climate historian L.A. Frakes has prospected through various theories proposed to account for those early ice ages. He isn't terribly enthusiastic about any of the possible culprits, but his choice for the least unlikely of them all emerges out of the recent revival of what was once a radically unorthodox idea: that continents drift over the face of the planet. Frakes argues that the glaciers originated at sites near the poles and that the ice ages began because the continents of the early earth had drifted to positions that took more and more of their land nearer to the polar regions.
More land near the poles meant that more precipitation fell as snow and could be compacted on land to form glaciers. With enough glaciers, the increase in the amount of sunlight reflected back into space off the glistening white sheen of the ice effectively reduced the amount by which the sun warmed the earth, creating the feedback loop by which the growth of glaciers encouraged the growth of more glaciers. Rocks have been found in North America, Africa and Australia whose ages appear to hover around the 2.3 billion—year—old mark. That date and their spread are vague enough, however, to make it almost impossible to determine just how much of the earth was icebound during the possible range of time in which each of the glacial deposits was formed.
Uncertainties about both the timing and the extent of these glaciers also muddy the search for the cause of the ancient ice ages. The record is so spotty that geologists are not sure whether areas near the equator or nearer the poles were the coolest places on earth. It's also possible that volcanic eruptions had tossed enough dust into the atmosphere to screen out sunlight and cool the earth. While some of the glacial records in the rocks do indeed contain evidence of volcanic activity prior to the buildup of glacial debris, others do not.
Such traces are the currency of science—data—and like money, a richness of data both buys you some credibility and ties you down, eliminating at least some theoretically plausible explanations. For this early period, theorists have come up with a variety of ideas to explain the ancient ice ages, all elegant and mostly immune to both proof and criticism. For example, a change in the earth's orbit could have reduced the amount of sunlight reaching the planet. However, the only physical signature of such an event that would show in the rocks would be the marks of the glaciers themselves.
Q. Suppose paleobotanists discover that during geological periods of reduced sunlight, ancient forests died away, leaving fossilized remains. What is the relevance of this information to the passage?
  • a)
    It supports the claim that dust from volcanic eruptions caused the ice ages.
  • b)
    It weakens the claim that dust from volcanic eruptions caused the ice ages.
  • c)
    It supports the claim that ice ages were accompanied by widespread loss of vegetation.
  • d)
    It weakens the claim that the only evidence of a change in orbit would be glacier marks.
Correct answer is option 'D'. Can you explain this answer?
Most Upvoted Answer
Direction: Read the passage carefully and answer the questionsThe las...
Explanation:

Relevance of the Information:
- The information provided by paleobotanists about ancient forests dying away during periods of reduced sunlight is relevant to the passage because it pertains to the discussion surrounding the potential causes of ancient ice ages.
- This information can help in assessing the validity of the claim that a change in the Earth's orbit, resulting in reduced sunlight reaching the planet, could have been a factor contributing to the ice ages.

Weakening the Claim:
- If paleobotanists discover that ancient forests died away during periods of reduced sunlight, leaving fossilized remains, it would weaken the claim that the only physical signature of a change in orbit would be the marks of glaciers themselves.
- Fossilized remains of ancient forests would provide additional evidence supporting the notion that changes in sunlight reaching the Earth could have had broader ecological impacts beyond just the formation of glaciers.

Conclusion:
- Therefore, the discovery of fossilized remains of ancient forests during periods of reduced sunlight would weaken the argument that the only evidence of a change in orbit would be glacier marks, opening up the possibility for a more comprehensive understanding of the factors contributing to ancient ice ages.
Community Answer
Direction: Read the passage carefully and answer the questionsThe las...
What would cause reduced sunlight? Only an orbital change. Think back on what the author says about the orbital change theory: its only evidence is the glaciation itself. This new evidence would therefore weaken the author's argument about the orbital theory: (D).
Wrong answers:
(A): Out of Scope. Though volcanic eruptions can lead to a reduction in the amount of sunlight that reaches earth, it isn't necessarily the case here.
(B): Out of Scope. As above. This evidence is outside the scope of the volcanic theory.
(C): Opposite. The author never makes this claim.
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Direction: Read the passage carefully and answer the questionsThe last ice age has left its telltales written quite clearly across the landscape. When Louis Agassiz first promulgated his theory that ice had once covered the Swiss countryside, he looked to the valleys there that retain glaciers to this day. Like other observers, he noted the presence of strange boulders, called "erratics, " tossed down in valleys like flotsam after a flood had drained away. He saw the strange polish along the bedrock—a sheen imparted as if by some massive swipe of sandpaper; he saw the debris of rocks and boulders fringing the margin of existing glaciers. He saw what can be seen still, markings in stone that indicated that ice once flowed over vast stretches of land now clear and verdant.The first great glaciations must have scored the earth as deeply in their turn, and, in principle, we ought to be able to track the history of the early ice ages by following the same reasoning Agassiz used to persuade himself and his contemporaries that ice once covered the earth. But the marks left by these earlier glaciations are quite subtle, tracks turned ghostly with great age. There are, however, telltale deposits of ancient rocks that strongly suggest that they had been ground together and laid down by the spread of ice.The Australian climate historian L.A. Frakes has prospected through various theories proposed to account for those early ice ages. He isn't terribly enthusiastic about any of the possible culprits, but his choice for the least unlikely of them all emerges out of the recent revival of what was once a radically unorthodox idea: that continents drift over the face of the planet. Frakes argues that the glaciers originated at sites near the poles and that the ice ages began because the continents of the early earth had drifted to positions that took more and more of their land nearer to the polar regions.More land near the poles meant that more precipitation fell as snow and could be compacted on land to form glaciers. With enough glaciers, the increase in the amount of sunlight reflected back into space off the glistening white sheen of the ice effectively reduced the amount by which the sun warmed the earth, creating the feedback loop by which the growth of glaciers encouraged the growth of more glaciers. Rocks have been found in North America, Africa and Australia whose ages appear to hover around the 2.3 billion—year—old mark. That date and their spread are vague enough, however, to make it almost impossible to determine just how much of the earth was icebound during the possible range of time in which each of the glacial deposits was formed.Uncertainties about both the timing and the extent of these glaciers also muddy the search for the cause of the ancient ice ages. The record is so spotty that geologists are not sure whether areas near the equator or nearer the poles were the coolest places on earth. It's also possible that volcanic eruptions had tossed enough dust into the atmosphere to screen out sunlight and cool the earth. While some of the glacial records in the rocks do indeed contain evidence of volcanic activity prior to the buildup of glacial debris, others do not.Such traces are the currency of science—data—and like money, a richness of data both buys you some credibility and ties you down, eliminating at least some theoretically plausible explanations. For this early period, theorists have come up with a variety of ideas to explain the ancient ice ages, all elegant and mostly immune to both proof and criticism. For example, a change in the earth's orbit could have reduced the amount of sunlight reaching the planet. However, the only physical signature of such an event that would show in the rocks would be the marks of the glaciers themselves.Q. There is an implicit assumption in the statement that geologists don't know whether the coolest places on earth were near the poles or near the equator. The assumption is that

Direction: Read the passage carefully and answer the questionsThe last ice age has left its telltales written quite clearly across the landscape. When Louis Agassiz first promulgated his theory that ice had once covered the Swiss countryside, he looked to the valleys there that retain glaciers to this day. Like other observers, he noted the presence of strange boulders, called "erratics, " tossed down in valleys like flotsam after a flood had drained away. He saw the strange polish along the bedrock—a sheen imparted as if by some massive swipe of sandpaper; he saw the debris of rocks and boulders fringing the margin of existing glaciers. He saw what can be seen still, markings in stone that indicated that ice once flowed over vast stretches of land now clear and verdant.The first great glaciations must have scored the earth as deeply in their turn, and, in principle, we ought to be able to track the history of the early ice ages by following the same reasoning Agassiz used to persuade himself and his contemporaries that ice once covered the earth. But the marks left by these earlier glaciations are quite subtle, tracks turned ghostly with great age. There are, however, telltale deposits of ancient rocks that strongly suggest that they had been ground together and laid down by the spread of ice.The Australian climate historian L.A. Frakes has prospected through various theories proposed to account for those early ice ages. He isn't terribly enthusiastic about any of the possible culprits, but his choice for the least unlikely of them all emerges out of the recent revival of what was once a radically unorthodox idea: that continents drift over the face of the planet. Frakes argues that the glaciers originated at sites near the poles and that the ice ages began because the continents of the early earth had drifted to positions that took more and more of their land nearer to the polar regions.More land near the poles meant that more precipitation fell as snow and could be compacted on land to form glaciers. With enough glaciers, the increase in the amount of sunlight reflected back into space off the glistening white sheen of the ice effectively reduced the amount by which the sun warmed the earth, creating the feedback loop by which the growth of glaciers encouraged the growth of more glaciers. Rocks have been found in North America, Africa and Australia whose ages appear to hover around the 2.3 billion—year—old mark. That date and their spread are vague enough, however, to make it almost impossible to determine just how much of the earth was icebound during the possible range of time in which each of the glacial deposits was formed.Uncertainties about both the timing and the extent of these glaciers also muddy the search for the cause of the ancient ice ages. The record is so spotty that geologists are not sure whether areas near the equator or nearer the poles were the coolest places on earth. It's also possible that volcanic eruptions had tossed enough dust into the atmosphere to screen out sunlight and cool the earth. While some of the glacial records in the rocks do indeed contain evidence of volcanic activity prior to the buildup of glacial debris, others do not.Such traces are the currency of science—data—and like money, a richness of data both buys you some credibility and ties you down, eliminating at least some theoretically plausible explanations. For this early period, theorists have come up with a variety of ideas to explain the ancient ice ages, all elegant and mostly immune to both proof and criticism. For example, a change in the earth's orbit could have reduced the amount of sunlight reaching the planet. However, the only physical signature of such an event that would show in the rocks would be the marks of the glaciers themselves.Q. Suppose that an advocate of the "change in orbit " theory of the ancient ice ages criticizes a defender of the "volcanic eruption " theory on the grounds that only some of the glacial records contain evidence of prior volcanic activity. The defender might justifiably counter this attack by pointing out that

Direction: Read the passage carefully and answer the questionsThe last ice age has left its telltales written quite clearly across the landscape. When Louis Agassiz first promulgated his theory that ice had once covered the Swiss countryside, he looked to the valleys there that retain glaciers to this day. Like other observers, he noted the presence of strange boulders, called "erratics, " tossed down in valleys like flotsam after a flood had drained away. He saw the strange polish along the bedrock—a sheen imparted as if by some massive swipe of sandpaper; he saw the debris of rocks and boulders fringing the margin of existing glaciers. He saw what can be seen still, markings in stone that indicated that ice once flowed over vast stretches of land now clear and verdant.The first great glaciations must have scored the earth as deeply in their turn, and, in principle, we ought to be able to track the history of the early ice ages by following the same reasoning Agassiz used to persuade himself and his contemporaries that ice once covered the earth. But the marks left by these earlier glaciations are quite subtle, tracks turned ghostly with great age. There are, however, telltale deposits of ancient rocks that strongly suggest that they had been ground together and laid down by the spread of ice.The Australian climate historian L.A. Frakes has prospected through various theories proposed to account for those early ice ages. He isn't terribly enthusiastic about any of the possible culprits, but his choice for the least unlikely of them all emerges out of the recent revival of what was once a radically unorthodox idea: that continents drift over the face of the planet. Frakes argues that the glaciers originated at sites near the poles and that the ice ages began because the continents of the early earth had drifted to positions that took more and more of their land nearer to the polar regions.More land near the poles meant that more precipitation fell as snow and could be compacted on land to form glaciers. With enough glaciers, the increase in the amount of sunlight reflected back into space off the glistening white sheen of the ice effectively reduced the amount by which the sun warmed the earth, creating the feedback loop by which the growth of glaciers encouraged the growth of more glaciers. Rocks have been found in North America, Africa and Australia whose ages appear to hover around the 2.3 billion—year—old mark. That date and their spread are vague enough, however, to make it almost impossible to determine just how much of the earth was icebound during the possible range of time in which each of the glacial deposits was formed.Uncertainties about both the timing and the extent of these glaciers also muddy the search for the cause of the ancient ice ages. The record is so spotty that geologists are not sure whether areas near the equator or nearer the poles were the coolest places on earth. It's also possible that volcanic eruptions had tossed enough dust into the atmosphere to screen out sunlight and cool the earth. While some of the glacial records in the rocks do indeed contain evidence of volcanic activity prior to the buildup of glacial debris, others do not.Such traces are the currency of science—data—and like money, a richness of data both buys you some credibility and ties you down, eliminating at least some theoretically plausible explanations. For this early period, theorists have come up with a variety of ideas to explain the ancient ice ages, all elegant and mostly immune to both proof and criticism. For example, a change in the earth's orbit could have reduced the amount of sunlight reaching the planet. However, the only physical signature of such an event that would show in the rocks would be the marks of the glaciers themselves.Q. Based on the passage, with which of the following statements would the author most likely NOT disagree?

Direction: Read the passage carefully and answer the questionsThe last ice age has left its telltales written quite clearly across the landscape. When Louis Agassiz first promulgated his theory that ice had once covered the Swiss countryside, he looked to the valleys there that retain glaciers to this day. Like other observers, he noted the presence of strange boulders, called "erratics, " tossed down in valleys like flotsam after a flood had drained away. He saw the strange polish along the bedrock—a sheen imparted as if by some massive swipe of sandpaper; he saw the debris of rocks and boulders fringing the margin of existing glaciers. He saw what can be seen still, markings in stone that indicated that ice once flowed over vast stretches of land now clear and verdant.The first great glaciations must have scored the earth as deeply in their turn, and, in principle, we ought to be able to track the history of the early ice ages by following the same reasoning Agassiz used to persuade himself and his contemporaries that ice once covered the earth. But the marks left by these earlier glaciations are quite subtle, tracks turned ghostly with great age. There are, however, telltale deposits of ancient rocks that strongly suggest that they had been ground together and laid down by the spread of ice.The Australian climate historian L.A. Frakes has prospected through various theories proposed to account for those early ice ages. He isn't terribly enthusiastic about any of the possible culprits, but his choice for the least unlikely of them all emerges out of the recent revival of what was once a radically unorthodox idea: that continents drift over the face of the planet. Frakes argues that the glaciers originated at sites near the poles and that the ice ages began because the continents of the early earth had drifted to positions that took more and more of their land nearer to the polar regions.More land near the poles meant that more precipitation fell as snow and could be compacted on land to form glaciers. With enough glaciers, the increase in the amount of sunlight reflected back into space off the glistening white sheen of the ice effectively reduced the amount by which the sun warmed the earth, creating the feedback loop by which the growth of glaciers encouraged the growth of more glaciers. Rocks have been found in North America, Africa and Australia whose ages appear to hover around the 2.3 billion—year—old mark. That date and their spread are vague enough, however, to make it almost impossible to determine just how much of the earth was icebound during the possible range of time in which each of the glacial deposits was formed.Uncertainties about both the timing and the extent of these glaciers also muddy the search for the cause of the ancient ice ages. The record is so spotty that geologists are not sure whether areas near the equator or nearer the poles were the coolest places on earth. It's also possible that volcanic eruptions had tossed enough dust into the atmosphere to screen out sunlight and cool the earth. While some of the glacial records in the rocks do indeed contain evidence of volcanic activity prior to the buildup of glacial debris, others do not.Such traces are the currency of science—data—and like money, a richness of data both buys you some credibility and ties you down, eliminating at least some theoretically plausible explanations. For this early period, theorists have come up with a variety of ideas to explain the ancient ice ages, all elegant and mostly immune to both proof and criticism. For example, a change in the earth's orbit could have reduced the amount of sunlight reaching the planet. However, the only physical signature of such an event that would show in the rocks would be the marks of the glaciers themselves.Q. According to the passage, which of the following is most likely to be true about the relationship between the amount of data one has about a phenomenon and the number of theoretically plausible explanations?

British colonial policy . . . went through two policy phases, or at least there were two strategies between which its policies actually oscillated, sometimes to its great advantage. At first, the new colonial apparatus exercised caution and occupied India by a mix of military power and subtle diplomacy, the high ground in the middle of the circle of circles. This, however, pushed them into contradictions. For, whatever their sense of the strangeness of the country and the thinness of colonial presence, the British colonial state represented the great conquering discourse of Enlightenment rationalism, entering India precisely at the moment of its greatest unchecked arrogance. As inheritors and representatives of this discourse, which carried everything before it, this colonial state could hardly adopt for long such a self-denying attitude. It had restructured everything in Europe—the productive system, the political regimes, the moral and cognitive orders—and would do the same in India, particularly as some empirically inclined theorists of that generation considered the colonies a massive laboratory of utilitarian or other theoretical experiments. Consequently, the colonial state could not settle simply for eminence at the cost of its marginality; it began to take initiatives to introduce the logic of modernity into Indian society. But this modernity did not enter a passive society.Sometimes, its initiatives were resisted by pre-existing structural forms. At times, there was a more direct form of collective resistance.Therefore the map of continuity and discontinuity that this state left behind at the time of independence was rather complex and has to be traced with care.Most significantly, of course, initiatives for modernity came to assume an external character. The acceptance of modernity came to be connected, ineradicably, with subjection. This again points to two different problems, one theoretical, the other political. Theoretically, because modernity was externally introduced, it is explanatorily unhelpful to apply the logical format of the ‘transition process’ to this pattern of change. Such a logical format would be wrong on two counts. First, however subtly, it would imply that what was proposed to be built was something like European capitalism. (And, in any case, historians have forcefully argued that what it was to replace was not like feudalism, with or without modificatory adjectives.) But, more fundamentally, the logical structure of endogenous change does not apply here. Here transformation agendas attack as an external force. This externality is not something that can be casually mentioned and forgotten. It is inscribed on every move, every object, every proposal, every legislative act, each line of causality. It comes to be marked on the epoch itself. This repetitive emphasis on externality should not be seen as a nationalist initiative that is so well-rehearsed in Indian social science. . . .Quite apart from the externality of the entire historical proposal of modernity, some of its contents were remarkable. . . . Economic reforms, or rather alterations . . . did not foreshadow the construction of a classical capitalist economy, with its necessary emphasis on extractive and transport sectors. What happened was the creation of a degenerate version of capitalism —what early dependency theorists called the ‘development of underdevelopment’.Q. All of the following statements, if true, could be seen as supporting the arguments in the passage, EXCEPT:( c)  the change in British colonial policy was induced by resistance to modernity in Indian society.

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Direction: Read the passage carefully and answer the questionsThe last ice age has left its telltales written quite clearly across the landscape. When Louis Agassiz first promulgated his theory that ice had once covered the Swiss countryside, he looked to the valleys there that retain glaciers to this day. Like other observers, he noted the presence of strange boulders, called "erratics, " tossed down in valleys like flotsam after a flood had drained away. He saw the strange polish along the bedrock—a sheen imparted as if by some massive swipe of sandpaper; he saw the debris of rocks and boulders fringing the margin of existing glaciers. He saw what can be seen still, markings in stone that indicated that ice once flowed over vast stretches of land now clear and verdant.The first great glaciations must have scored the earth as deeply in their turn, and, in principle, we ought to be able to track the history of the early ice ages by following the same reasoning Agassiz used to persuade himself and his contemporaries that ice once covered the earth. But the marks left by these earlier glaciations are quite subtle, tracks turned ghostly with great age. There are, however, telltale deposits of ancient rocks that strongly suggest that they had been ground together and laid down by the spread of ice.The Australian climate historian L.A. Frakes has prospected through various theories proposed to account for those early ice ages. He isn't terribly enthusiastic about any of the possible culprits, but his choice for the least unlikely of them all emerges out of the recent revival of what was once a radically unorthodox idea: that continents drift over the face of the planet. Frakes argues that the glaciers originated at sites near the poles and that the ice ages began because the continents of the early earth had drifted to positions that took more and more of their land nearer to the polar regions.More land near the poles meant that more precipitation fell as snow and could be compacted on land to form glaciers. With enough glaciers, the increase in the amount of sunlight reflected back into space off the glistening white sheen of the ice effectively reduced the amount by which the sun warmed the earth, creating the feedback loop by which the growth of glaciers encouraged the growth of more glaciers. Rocks have been found in North America, Africa and Australia whose ages appear to hover around the 2.3 billion—year—old mark. That date and their spread are vague enough, however, to make it almost impossible to determine just how much of the earth was icebound during the possible range of time in which each of the glacial deposits was formed.Uncertainties about both the timing and the extent of these glaciers also muddy the search for the cause of the ancient ice ages. The record is so spotty that geologists are not sure whether areas near the equator or nearer the poles were the coolest places on earth. It's also possible that volcanic eruptions had tossed enough dust into the atmosphere to screen out sunlight and cool the earth. While some of the glacial records in the rocks do indeed contain evidence of volcanic activity prior to the buildup of glacial debris, others do not.Such traces are the currency of science—data—and like money, a richness of data both buys you some credibility and ties you down, eliminating at least some theoretically plausible explanations. For this early period, theorists have come up with a variety of ideas to explain the ancient ice ages, all elegant and mostly immune to both proof and criticism. For example, a change in the earth's orbit could have reduced the amount of sunlight reaching the planet. However, the only physical signature of such an event that would show in the rocks would be the marks of the glaciers themselves.Q. Suppose paleobotanists discover that during geological periods of reduced sunlight, ancient forests died away, leaving fossilized remains. What is the relevance of this information to the passage?a)It supports the claim that dust from volcanic eruptions caused the ice ages.b)It weakens the claim that dust from volcanic eruptions caused the ice ages.c)It supports the claim that ice ages were accompanied by widespread loss of vegetation.d)It weakens the claim that the only evidence of a change in orbit would be glacier marks.Correct answer is option 'D'. Can you explain this answer?
Question Description
Direction: Read the passage carefully and answer the questionsThe last ice age has left its telltales written quite clearly across the landscape. When Louis Agassiz first promulgated his theory that ice had once covered the Swiss countryside, he looked to the valleys there that retain glaciers to this day. Like other observers, he noted the presence of strange boulders, called "erratics, " tossed down in valleys like flotsam after a flood had drained away. He saw the strange polish along the bedrock—a sheen imparted as if by some massive swipe of sandpaper; he saw the debris of rocks and boulders fringing the margin of existing glaciers. He saw what can be seen still, markings in stone that indicated that ice once flowed over vast stretches of land now clear and verdant.The first great glaciations must have scored the earth as deeply in their turn, and, in principle, we ought to be able to track the history of the early ice ages by following the same reasoning Agassiz used to persuade himself and his contemporaries that ice once covered the earth. But the marks left by these earlier glaciations are quite subtle, tracks turned ghostly with great age. There are, however, telltale deposits of ancient rocks that strongly suggest that they had been ground together and laid down by the spread of ice.The Australian climate historian L.A. Frakes has prospected through various theories proposed to account for those early ice ages. He isn't terribly enthusiastic about any of the possible culprits, but his choice for the least unlikely of them all emerges out of the recent revival of what was once a radically unorthodox idea: that continents drift over the face of the planet. Frakes argues that the glaciers originated at sites near the poles and that the ice ages began because the continents of the early earth had drifted to positions that took more and more of their land nearer to the polar regions.More land near the poles meant that more precipitation fell as snow and could be compacted on land to form glaciers. With enough glaciers, the increase in the amount of sunlight reflected back into space off the glistening white sheen of the ice effectively reduced the amount by which the sun warmed the earth, creating the feedback loop by which the growth of glaciers encouraged the growth of more glaciers. Rocks have been found in North America, Africa and Australia whose ages appear to hover around the 2.3 billion—year—old mark. That date and their spread are vague enough, however, to make it almost impossible to determine just how much of the earth was icebound during the possible range of time in which each of the glacial deposits was formed.Uncertainties about both the timing and the extent of these glaciers also muddy the search for the cause of the ancient ice ages. The record is so spotty that geologists are not sure whether areas near the equator or nearer the poles were the coolest places on earth. It's also possible that volcanic eruptions had tossed enough dust into the atmosphere to screen out sunlight and cool the earth. While some of the glacial records in the rocks do indeed contain evidence of volcanic activity prior to the buildup of glacial debris, others do not.Such traces are the currency of science—data—and like money, a richness of data both buys you some credibility and ties you down, eliminating at least some theoretically plausible explanations. For this early period, theorists have come up with a variety of ideas to explain the ancient ice ages, all elegant and mostly immune to both proof and criticism. For example, a change in the earth's orbit could have reduced the amount of sunlight reaching the planet. However, the only physical signature of such an event that would show in the rocks would be the marks of the glaciers themselves.Q. Suppose paleobotanists discover that during geological periods of reduced sunlight, ancient forests died away, leaving fossilized remains. What is the relevance of this information to the passage?a)It supports the claim that dust from volcanic eruptions caused the ice ages.b)It weakens the claim that dust from volcanic eruptions caused the ice ages.c)It supports the claim that ice ages were accompanied by widespread loss of vegetation.d)It weakens the claim that the only evidence of a change in orbit would be glacier marks.Correct answer is option 'D'. Can you explain this answer? for CAT 2025 is part of CAT preparation. The Question and answers have been prepared according to the CAT exam syllabus. Information about Direction: Read the passage carefully and answer the questionsThe last ice age has left its telltales written quite clearly across the landscape. When Louis Agassiz first promulgated his theory that ice had once covered the Swiss countryside, he looked to the valleys there that retain glaciers to this day. Like other observers, he noted the presence of strange boulders, called "erratics, " tossed down in valleys like flotsam after a flood had drained away. He saw the strange polish along the bedrock—a sheen imparted as if by some massive swipe of sandpaper; he saw the debris of rocks and boulders fringing the margin of existing glaciers. He saw what can be seen still, markings in stone that indicated that ice once flowed over vast stretches of land now clear and verdant.The first great glaciations must have scored the earth as deeply in their turn, and, in principle, we ought to be able to track the history of the early ice ages by following the same reasoning Agassiz used to persuade himself and his contemporaries that ice once covered the earth. But the marks left by these earlier glaciations are quite subtle, tracks turned ghostly with great age. There are, however, telltale deposits of ancient rocks that strongly suggest that they had been ground together and laid down by the spread of ice.The Australian climate historian L.A. Frakes has prospected through various theories proposed to account for those early ice ages. He isn't terribly enthusiastic about any of the possible culprits, but his choice for the least unlikely of them all emerges out of the recent revival of what was once a radically unorthodox idea: that continents drift over the face of the planet. Frakes argues that the glaciers originated at sites near the poles and that the ice ages began because the continents of the early earth had drifted to positions that took more and more of their land nearer to the polar regions.More land near the poles meant that more precipitation fell as snow and could be compacted on land to form glaciers. With enough glaciers, the increase in the amount of sunlight reflected back into space off the glistening white sheen of the ice effectively reduced the amount by which the sun warmed the earth, creating the feedback loop by which the growth of glaciers encouraged the growth of more glaciers. Rocks have been found in North America, Africa and Australia whose ages appear to hover around the 2.3 billion—year—old mark. That date and their spread are vague enough, however, to make it almost impossible to determine just how much of the earth was icebound during the possible range of time in which each of the glacial deposits was formed.Uncertainties about both the timing and the extent of these glaciers also muddy the search for the cause of the ancient ice ages. The record is so spotty that geologists are not sure whether areas near the equator or nearer the poles were the coolest places on earth. It's also possible that volcanic eruptions had tossed enough dust into the atmosphere to screen out sunlight and cool the earth. While some of the glacial records in the rocks do indeed contain evidence of volcanic activity prior to the buildup of glacial debris, others do not.Such traces are the currency of science—data—and like money, a richness of data both buys you some credibility and ties you down, eliminating at least some theoretically plausible explanations. For this early period, theorists have come up with a variety of ideas to explain the ancient ice ages, all elegant and mostly immune to both proof and criticism. For example, a change in the earth's orbit could have reduced the amount of sunlight reaching the planet. However, the only physical signature of such an event that would show in the rocks would be the marks of the glaciers themselves.Q. Suppose paleobotanists discover that during geological periods of reduced sunlight, ancient forests died away, leaving fossilized remains. What is the relevance of this information to the passage?a)It supports the claim that dust from volcanic eruptions caused the ice ages.b)It weakens the claim that dust from volcanic eruptions caused the ice ages.c)It supports the claim that ice ages were accompanied by widespread loss of vegetation.d)It weakens the claim that the only evidence of a change in orbit would be glacier marks.Correct answer is option 'D'. Can you explain this answer? covers all topics & solutions for CAT 2025 Exam. Find important definitions, questions, meanings, examples, exercises and tests below for Direction: Read the passage carefully and answer the questionsThe last ice age has left its telltales written quite clearly across the landscape. When Louis Agassiz first promulgated his theory that ice had once covered the Swiss countryside, he looked to the valleys there that retain glaciers to this day. Like other observers, he noted the presence of strange boulders, called "erratics, " tossed down in valleys like flotsam after a flood had drained away. He saw the strange polish along the bedrock—a sheen imparted as if by some massive swipe of sandpaper; he saw the debris of rocks and boulders fringing the margin of existing glaciers. He saw what can be seen still, markings in stone that indicated that ice once flowed over vast stretches of land now clear and verdant.The first great glaciations must have scored the earth as deeply in their turn, and, in principle, we ought to be able to track the history of the early ice ages by following the same reasoning Agassiz used to persuade himself and his contemporaries that ice once covered the earth. But the marks left by these earlier glaciations are quite subtle, tracks turned ghostly with great age. There are, however, telltale deposits of ancient rocks that strongly suggest that they had been ground together and laid down by the spread of ice.The Australian climate historian L.A. Frakes has prospected through various theories proposed to account for those early ice ages. He isn't terribly enthusiastic about any of the possible culprits, but his choice for the least unlikely of them all emerges out of the recent revival of what was once a radically unorthodox idea: that continents drift over the face of the planet. Frakes argues that the glaciers originated at sites near the poles and that the ice ages began because the continents of the early earth had drifted to positions that took more and more of their land nearer to the polar regions.More land near the poles meant that more precipitation fell as snow and could be compacted on land to form glaciers. With enough glaciers, the increase in the amount of sunlight reflected back into space off the glistening white sheen of the ice effectively reduced the amount by which the sun warmed the earth, creating the feedback loop by which the growth of glaciers encouraged the growth of more glaciers. Rocks have been found in North America, Africa and Australia whose ages appear to hover around the 2.3 billion—year—old mark. That date and their spread are vague enough, however, to make it almost impossible to determine just how much of the earth was icebound during the possible range of time in which each of the glacial deposits was formed.Uncertainties about both the timing and the extent of these glaciers also muddy the search for the cause of the ancient ice ages. The record is so spotty that geologists are not sure whether areas near the equator or nearer the poles were the coolest places on earth. It's also possible that volcanic eruptions had tossed enough dust into the atmosphere to screen out sunlight and cool the earth. While some of the glacial records in the rocks do indeed contain evidence of volcanic activity prior to the buildup of glacial debris, others do not.Such traces are the currency of science—data—and like money, a richness of data both buys you some credibility and ties you down, eliminating at least some theoretically plausible explanations. For this early period, theorists have come up with a variety of ideas to explain the ancient ice ages, all elegant and mostly immune to both proof and criticism. For example, a change in the earth's orbit could have reduced the amount of sunlight reaching the planet. However, the only physical signature of such an event that would show in the rocks would be the marks of the glaciers themselves.Q. Suppose paleobotanists discover that during geological periods of reduced sunlight, ancient forests died away, leaving fossilized remains. What is the relevance of this information to the passage?a)It supports the claim that dust from volcanic eruptions caused the ice ages.b)It weakens the claim that dust from volcanic eruptions caused the ice ages.c)It supports the claim that ice ages were accompanied by widespread loss of vegetation.d)It weakens the claim that the only evidence of a change in orbit would be glacier marks.Correct answer is option 'D'. Can you explain this answer?.
Solutions for Direction: Read the passage carefully and answer the questionsThe last ice age has left its telltales written quite clearly across the landscape. When Louis Agassiz first promulgated his theory that ice had once covered the Swiss countryside, he looked to the valleys there that retain glaciers to this day. Like other observers, he noted the presence of strange boulders, called "erratics, " tossed down in valleys like flotsam after a flood had drained away. He saw the strange polish along the bedrock—a sheen imparted as if by some massive swipe of sandpaper; he saw the debris of rocks and boulders fringing the margin of existing glaciers. He saw what can be seen still, markings in stone that indicated that ice once flowed over vast stretches of land now clear and verdant.The first great glaciations must have scored the earth as deeply in their turn, and, in principle, we ought to be able to track the history of the early ice ages by following the same reasoning Agassiz used to persuade himself and his contemporaries that ice once covered the earth. But the marks left by these earlier glaciations are quite subtle, tracks turned ghostly with great age. There are, however, telltale deposits of ancient rocks that strongly suggest that they had been ground together and laid down by the spread of ice.The Australian climate historian L.A. Frakes has prospected through various theories proposed to account for those early ice ages. He isn't terribly enthusiastic about any of the possible culprits, but his choice for the least unlikely of them all emerges out of the recent revival of what was once a radically unorthodox idea: that continents drift over the face of the planet. Frakes argues that the glaciers originated at sites near the poles and that the ice ages began because the continents of the early earth had drifted to positions that took more and more of their land nearer to the polar regions.More land near the poles meant that more precipitation fell as snow and could be compacted on land to form glaciers. With enough glaciers, the increase in the amount of sunlight reflected back into space off the glistening white sheen of the ice effectively reduced the amount by which the sun warmed the earth, creating the feedback loop by which the growth of glaciers encouraged the growth of more glaciers. Rocks have been found in North America, Africa and Australia whose ages appear to hover around the 2.3 billion—year—old mark. That date and their spread are vague enough, however, to make it almost impossible to determine just how much of the earth was icebound during the possible range of time in which each of the glacial deposits was formed.Uncertainties about both the timing and the extent of these glaciers also muddy the search for the cause of the ancient ice ages. The record is so spotty that geologists are not sure whether areas near the equator or nearer the poles were the coolest places on earth. It's also possible that volcanic eruptions had tossed enough dust into the atmosphere to screen out sunlight and cool the earth. While some of the glacial records in the rocks do indeed contain evidence of volcanic activity prior to the buildup of glacial debris, others do not.Such traces are the currency of science—data—and like money, a richness of data both buys you some credibility and ties you down, eliminating at least some theoretically plausible explanations. For this early period, theorists have come up with a variety of ideas to explain the ancient ice ages, all elegant and mostly immune to both proof and criticism. For example, a change in the earth's orbit could have reduced the amount of sunlight reaching the planet. However, the only physical signature of such an event that would show in the rocks would be the marks of the glaciers themselves.Q. Suppose paleobotanists discover that during geological periods of reduced sunlight, ancient forests died away, leaving fossilized remains. What is the relevance of this information to the passage?a)It supports the claim that dust from volcanic eruptions caused the ice ages.b)It weakens the claim that dust from volcanic eruptions caused the ice ages.c)It supports the claim that ice ages were accompanied by widespread loss of vegetation.d)It weakens the claim that the only evidence of a change in orbit would be glacier marks.Correct answer is option 'D'. Can you explain this answer? in English & in Hindi are available as part of our courses for CAT. Download more important topics, notes, lectures and mock test series for CAT Exam by signing up for free.
Here you can find the meaning of Direction: Read the passage carefully and answer the questionsThe last ice age has left its telltales written quite clearly across the landscape. When Louis Agassiz first promulgated his theory that ice had once covered the Swiss countryside, he looked to the valleys there that retain glaciers to this day. Like other observers, he noted the presence of strange boulders, called "erratics, " tossed down in valleys like flotsam after a flood had drained away. He saw the strange polish along the bedrock—a sheen imparted as if by some massive swipe of sandpaper; he saw the debris of rocks and boulders fringing the margin of existing glaciers. He saw what can be seen still, markings in stone that indicated that ice once flowed over vast stretches of land now clear and verdant.The first great glaciations must have scored the earth as deeply in their turn, and, in principle, we ought to be able to track the history of the early ice ages by following the same reasoning Agassiz used to persuade himself and his contemporaries that ice once covered the earth. But the marks left by these earlier glaciations are quite subtle, tracks turned ghostly with great age. There are, however, telltale deposits of ancient rocks that strongly suggest that they had been ground together and laid down by the spread of ice.The Australian climate historian L.A. Frakes has prospected through various theories proposed to account for those early ice ages. He isn't terribly enthusiastic about any of the possible culprits, but his choice for the least unlikely of them all emerges out of the recent revival of what was once a radically unorthodox idea: that continents drift over the face of the planet. Frakes argues that the glaciers originated at sites near the poles and that the ice ages began because the continents of the early earth had drifted to positions that took more and more of their land nearer to the polar regions.More land near the poles meant that more precipitation fell as snow and could be compacted on land to form glaciers. With enough glaciers, the increase in the amount of sunlight reflected back into space off the glistening white sheen of the ice effectively reduced the amount by which the sun warmed the earth, creating the feedback loop by which the growth of glaciers encouraged the growth of more glaciers. Rocks have been found in North America, Africa and Australia whose ages appear to hover around the 2.3 billion—year—old mark. That date and their spread are vague enough, however, to make it almost impossible to determine just how much of the earth was icebound during the possible range of time in which each of the glacial deposits was formed.Uncertainties about both the timing and the extent of these glaciers also muddy the search for the cause of the ancient ice ages. The record is so spotty that geologists are not sure whether areas near the equator or nearer the poles were the coolest places on earth. It's also possible that volcanic eruptions had tossed enough dust into the atmosphere to screen out sunlight and cool the earth. While some of the glacial records in the rocks do indeed contain evidence of volcanic activity prior to the buildup of glacial debris, others do not.Such traces are the currency of science—data—and like money, a richness of data both buys you some credibility and ties you down, eliminating at least some theoretically plausible explanations. For this early period, theorists have come up with a variety of ideas to explain the ancient ice ages, all elegant and mostly immune to both proof and criticism. For example, a change in the earth's orbit could have reduced the amount of sunlight reaching the planet. However, the only physical signature of such an event that would show in the rocks would be the marks of the glaciers themselves.Q. Suppose paleobotanists discover that during geological periods of reduced sunlight, ancient forests died away, leaving fossilized remains. What is the relevance of this information to the passage?a)It supports the claim that dust from volcanic eruptions caused the ice ages.b)It weakens the claim that dust from volcanic eruptions caused the ice ages.c)It supports the claim that ice ages were accompanied by widespread loss of vegetation.d)It weakens the claim that the only evidence of a change in orbit would be glacier marks.Correct answer is option 'D'. Can you explain this answer? defined & explained in the simplest way possible. Besides giving the explanation of Direction: Read the passage carefully and answer the questionsThe last ice age has left its telltales written quite clearly across the landscape. When Louis Agassiz first promulgated his theory that ice had once covered the Swiss countryside, he looked to the valleys there that retain glaciers to this day. Like other observers, he noted the presence of strange boulders, called "erratics, " tossed down in valleys like flotsam after a flood had drained away. He saw the strange polish along the bedrock—a sheen imparted as if by some massive swipe of sandpaper; he saw the debris of rocks and boulders fringing the margin of existing glaciers. He saw what can be seen still, markings in stone that indicated that ice once flowed over vast stretches of land now clear and verdant.The first great glaciations must have scored the earth as deeply in their turn, and, in principle, we ought to be able to track the history of the early ice ages by following the same reasoning Agassiz used to persuade himself and his contemporaries that ice once covered the earth. But the marks left by these earlier glaciations are quite subtle, tracks turned ghostly with great age. There are, however, telltale deposits of ancient rocks that strongly suggest that they had been ground together and laid down by the spread of ice.The Australian climate historian L.A. Frakes has prospected through various theories proposed to account for those early ice ages. He isn't terribly enthusiastic about any of the possible culprits, but his choice for the least unlikely of them all emerges out of the recent revival of what was once a radically unorthodox idea: that continents drift over the face of the planet. Frakes argues that the glaciers originated at sites near the poles and that the ice ages began because the continents of the early earth had drifted to positions that took more and more of their land nearer to the polar regions.More land near the poles meant that more precipitation fell as snow and could be compacted on land to form glaciers. With enough glaciers, the increase in the amount of sunlight reflected back into space off the glistening white sheen of the ice effectively reduced the amount by which the sun warmed the earth, creating the feedback loop by which the growth of glaciers encouraged the growth of more glaciers. Rocks have been found in North America, Africa and Australia whose ages appear to hover around the 2.3 billion—year—old mark. That date and their spread are vague enough, however, to make it almost impossible to determine just how much of the earth was icebound during the possible range of time in which each of the glacial deposits was formed.Uncertainties about both the timing and the extent of these glaciers also muddy the search for the cause of the ancient ice ages. The record is so spotty that geologists are not sure whether areas near the equator or nearer the poles were the coolest places on earth. It's also possible that volcanic eruptions had tossed enough dust into the atmosphere to screen out sunlight and cool the earth. While some of the glacial records in the rocks do indeed contain evidence of volcanic activity prior to the buildup of glacial debris, others do not.Such traces are the currency of science—data—and like money, a richness of data both buys you some credibility and ties you down, eliminating at least some theoretically plausible explanations. For this early period, theorists have come up with a variety of ideas to explain the ancient ice ages, all elegant and mostly immune to both proof and criticism. For example, a change in the earth's orbit could have reduced the amount of sunlight reaching the planet. However, the only physical signature of such an event that would show in the rocks would be the marks of the glaciers themselves.Q. Suppose paleobotanists discover that during geological periods of reduced sunlight, ancient forests died away, leaving fossilized remains. What is the relevance of this information to the passage?a)It supports the claim that dust from volcanic eruptions caused the ice ages.b)It weakens the claim that dust from volcanic eruptions caused the ice ages.c)It supports the claim that ice ages were accompanied by widespread loss of vegetation.d)It weakens the claim that the only evidence of a change in orbit would be glacier marks.Correct answer is option 'D'. Can you explain this answer?, a detailed solution for Direction: Read the passage carefully and answer the questionsThe last ice age has left its telltales written quite clearly across the landscape. When Louis Agassiz first promulgated his theory that ice had once covered the Swiss countryside, he looked to the valleys there that retain glaciers to this day. Like other observers, he noted the presence of strange boulders, called "erratics, " tossed down in valleys like flotsam after a flood had drained away. He saw the strange polish along the bedrock—a sheen imparted as if by some massive swipe of sandpaper; he saw the debris of rocks and boulders fringing the margin of existing glaciers. He saw what can be seen still, markings in stone that indicated that ice once flowed over vast stretches of land now clear and verdant.The first great glaciations must have scored the earth as deeply in their turn, and, in principle, we ought to be able to track the history of the early ice ages by following the same reasoning Agassiz used to persuade himself and his contemporaries that ice once covered the earth. But the marks left by these earlier glaciations are quite subtle, tracks turned ghostly with great age. There are, however, telltale deposits of ancient rocks that strongly suggest that they had been ground together and laid down by the spread of ice.The Australian climate historian L.A. Frakes has prospected through various theories proposed to account for those early ice ages. He isn't terribly enthusiastic about any of the possible culprits, but his choice for the least unlikely of them all emerges out of the recent revival of what was once a radically unorthodox idea: that continents drift over the face of the planet. Frakes argues that the glaciers originated at sites near the poles and that the ice ages began because the continents of the early earth had drifted to positions that took more and more of their land nearer to the polar regions.More land near the poles meant that more precipitation fell as snow and could be compacted on land to form glaciers. With enough glaciers, the increase in the amount of sunlight reflected back into space off the glistening white sheen of the ice effectively reduced the amount by which the sun warmed the earth, creating the feedback loop by which the growth of glaciers encouraged the growth of more glaciers. Rocks have been found in North America, Africa and Australia whose ages appear to hover around the 2.3 billion—year—old mark. That date and their spread are vague enough, however, to make it almost impossible to determine just how much of the earth was icebound during the possible range of time in which each of the glacial deposits was formed.Uncertainties about both the timing and the extent of these glaciers also muddy the search for the cause of the ancient ice ages. The record is so spotty that geologists are not sure whether areas near the equator or nearer the poles were the coolest places on earth. It's also possible that volcanic eruptions had tossed enough dust into the atmosphere to screen out sunlight and cool the earth. While some of the glacial records in the rocks do indeed contain evidence of volcanic activity prior to the buildup of glacial debris, others do not.Such traces are the currency of science—data—and like money, a richness of data both buys you some credibility and ties you down, eliminating at least some theoretically plausible explanations. For this early period, theorists have come up with a variety of ideas to explain the ancient ice ages, all elegant and mostly immune to both proof and criticism. For example, a change in the earth's orbit could have reduced the amount of sunlight reaching the planet. However, the only physical signature of such an event that would show in the rocks would be the marks of the glaciers themselves.Q. Suppose paleobotanists discover that during geological periods of reduced sunlight, ancient forests died away, leaving fossilized remains. What is the relevance of this information to the passage?a)It supports the claim that dust from volcanic eruptions caused the ice ages.b)It weakens the claim that dust from volcanic eruptions caused the ice ages.c)It supports the claim that ice ages were accompanied by widespread loss of vegetation.d)It weakens the claim that the only evidence of a change in orbit would be glacier marks.Correct answer is option 'D'. Can you explain this answer? has been provided alongside types of Direction: Read the passage carefully and answer the questionsThe last ice age has left its telltales written quite clearly across the landscape. When Louis Agassiz first promulgated his theory that ice had once covered the Swiss countryside, he looked to the valleys there that retain glaciers to this day. Like other observers, he noted the presence of strange boulders, called "erratics, " tossed down in valleys like flotsam after a flood had drained away. He saw the strange polish along the bedrock—a sheen imparted as if by some massive swipe of sandpaper; he saw the debris of rocks and boulders fringing the margin of existing glaciers. He saw what can be seen still, markings in stone that indicated that ice once flowed over vast stretches of land now clear and verdant.The first great glaciations must have scored the earth as deeply in their turn, and, in principle, we ought to be able to track the history of the early ice ages by following the same reasoning Agassiz used to persuade himself and his contemporaries that ice once covered the earth. But the marks left by these earlier glaciations are quite subtle, tracks turned ghostly with great age. There are, however, telltale deposits of ancient rocks that strongly suggest that they had been ground together and laid down by the spread of ice.The Australian climate historian L.A. Frakes has prospected through various theories proposed to account for those early ice ages. He isn't terribly enthusiastic about any of the possible culprits, but his choice for the least unlikely of them all emerges out of the recent revival of what was once a radically unorthodox idea: that continents drift over the face of the planet. Frakes argues that the glaciers originated at sites near the poles and that the ice ages began because the continents of the early earth had drifted to positions that took more and more of their land nearer to the polar regions.More land near the poles meant that more precipitation fell as snow and could be compacted on land to form glaciers. With enough glaciers, the increase in the amount of sunlight reflected back into space off the glistening white sheen of the ice effectively reduced the amount by which the sun warmed the earth, creating the feedback loop by which the growth of glaciers encouraged the growth of more glaciers. Rocks have been found in North America, Africa and Australia whose ages appear to hover around the 2.3 billion—year—old mark. That date and their spread are vague enough, however, to make it almost impossible to determine just how much of the earth was icebound during the possible range of time in which each of the glacial deposits was formed.Uncertainties about both the timing and the extent of these glaciers also muddy the search for the cause of the ancient ice ages. The record is so spotty that geologists are not sure whether areas near the equator or nearer the poles were the coolest places on earth. It's also possible that volcanic eruptions had tossed enough dust into the atmosphere to screen out sunlight and cool the earth. While some of the glacial records in the rocks do indeed contain evidence of volcanic activity prior to the buildup of glacial debris, others do not.Such traces are the currency of science—data—and like money, a richness of data both buys you some credibility and ties you down, eliminating at least some theoretically plausible explanations. For this early period, theorists have come up with a variety of ideas to explain the ancient ice ages, all elegant and mostly immune to both proof and criticism. For example, a change in the earth's orbit could have reduced the amount of sunlight reaching the planet. However, the only physical signature of such an event that would show in the rocks would be the marks of the glaciers themselves.Q. Suppose paleobotanists discover that during geological periods of reduced sunlight, ancient forests died away, leaving fossilized remains. What is the relevance of this information to the passage?a)It supports the claim that dust from volcanic eruptions caused the ice ages.b)It weakens the claim that dust from volcanic eruptions caused the ice ages.c)It supports the claim that ice ages were accompanied by widespread loss of vegetation.d)It weakens the claim that the only evidence of a change in orbit would be glacier marks.Correct answer is option 'D'. Can you explain this answer? theory, EduRev gives you an ample number of questions to practice Direction: Read the passage carefully and answer the questionsThe last ice age has left its telltales written quite clearly across the landscape. When Louis Agassiz first promulgated his theory that ice had once covered the Swiss countryside, he looked to the valleys there that retain glaciers to this day. Like other observers, he noted the presence of strange boulders, called "erratics, " tossed down in valleys like flotsam after a flood had drained away. He saw the strange polish along the bedrock—a sheen imparted as if by some massive swipe of sandpaper; he saw the debris of rocks and boulders fringing the margin of existing glaciers. He saw what can be seen still, markings in stone that indicated that ice once flowed over vast stretches of land now clear and verdant.The first great glaciations must have scored the earth as deeply in their turn, and, in principle, we ought to be able to track the history of the early ice ages by following the same reasoning Agassiz used to persuade himself and his contemporaries that ice once covered the earth. But the marks left by these earlier glaciations are quite subtle, tracks turned ghostly with great age. There are, however, telltale deposits of ancient rocks that strongly suggest that they had been ground together and laid down by the spread of ice.The Australian climate historian L.A. Frakes has prospected through various theories proposed to account for those early ice ages. He isn't terribly enthusiastic about any of the possible culprits, but his choice for the least unlikely of them all emerges out of the recent revival of what was once a radically unorthodox idea: that continents drift over the face of the planet. Frakes argues that the glaciers originated at sites near the poles and that the ice ages began because the continents of the early earth had drifted to positions that took more and more of their land nearer to the polar regions.More land near the poles meant that more precipitation fell as snow and could be compacted on land to form glaciers. With enough glaciers, the increase in the amount of sunlight reflected back into space off the glistening white sheen of the ice effectively reduced the amount by which the sun warmed the earth, creating the feedback loop by which the growth of glaciers encouraged the growth of more glaciers. Rocks have been found in North America, Africa and Australia whose ages appear to hover around the 2.3 billion—year—old mark. That date and their spread are vague enough, however, to make it almost impossible to determine just how much of the earth was icebound during the possible range of time in which each of the glacial deposits was formed.Uncertainties about both the timing and the extent of these glaciers also muddy the search for the cause of the ancient ice ages. The record is so spotty that geologists are not sure whether areas near the equator or nearer the poles were the coolest places on earth. It's also possible that volcanic eruptions had tossed enough dust into the atmosphere to screen out sunlight and cool the earth. While some of the glacial records in the rocks do indeed contain evidence of volcanic activity prior to the buildup of glacial debris, others do not.Such traces are the currency of science—data—and like money, a richness of data both buys you some credibility and ties you down, eliminating at least some theoretically plausible explanations. For this early period, theorists have come up with a variety of ideas to explain the ancient ice ages, all elegant and mostly immune to both proof and criticism. For example, a change in the earth's orbit could have reduced the amount of sunlight reaching the planet. However, the only physical signature of such an event that would show in the rocks would be the marks of the glaciers themselves.Q. Suppose paleobotanists discover that during geological periods of reduced sunlight, ancient forests died away, leaving fossilized remains. What is the relevance of this information to the passage?a)It supports the claim that dust from volcanic eruptions caused the ice ages.b)It weakens the claim that dust from volcanic eruptions caused the ice ages.c)It supports the claim that ice ages were accompanied by widespread loss of vegetation.d)It weakens the claim that the only evidence of a change in orbit would be glacier marks.Correct answer is option 'D'. Can you explain this answer? tests, examples and also practice CAT tests.
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