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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. Based on the passage, with which of the following statements would the author most likely NOT disagree?a)Recent geological events can be substantially easier to investigate than ancient ones.b)Deposits of ground—up rocks always indicate that an ice age occurred.c)Discovering the cause of the ancient ice ages will have important practical consequences.d)Each of the early ice ages had a different proximate cause.Correct answer is option 'A'. 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. Based on the passage, with which of the following statements would the author most likely NOT disagree?a)Recent geological events can be substantially easier to investigate than ancient ones.b)Deposits of ground—up rocks always indicate that an ice age occurred.c)Discovering the cause of the ancient ice ages will have important practical consequences.d)Each of the early ice ages had a different proximate cause.Correct answer is option 'A'. 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. Based on the passage, with which of the following statements would the author most likely NOT disagree?a)Recent geological events can be substantially easier to investigate than ancient ones.b)Deposits of ground—up rocks always indicate that an ice age occurred.c)Discovering the cause of the ancient ice ages will have important practical consequences.d)Each of the early ice ages had a different proximate cause.Correct answer is option 'A'. 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. Based on the passage, with which of the following statements would the author most likely NOT disagree?a)Recent geological events can be substantially easier to investigate than ancient ones.b)Deposits of ground—up rocks always indicate that an ice age occurred.c)Discovering the cause of the ancient ice ages will have important practical consequences.d)Each of the early ice ages had a different proximate cause.Correct answer is option 'A'. 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. Based on the passage, with which of the following statements would the author most likely NOT disagree?a)Recent geological events can be substantially easier to investigate than ancient ones.b)Deposits of ground—up rocks always indicate that an ice age occurred.c)Discovering the cause of the ancient ice ages will have important practical consequences.d)Each of the early ice ages had a different proximate cause.Correct answer is option 'A'. 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. Based on the passage, with which of the following statements would the author most likely NOT disagree?a)Recent geological events can be substantially easier to investigate than ancient ones.b)Deposits of ground—up rocks always indicate that an ice age occurred.c)Discovering the cause of the ancient ice ages will have important practical consequences.d)Each of the early ice ages had a different proximate cause.Correct answer is option 'A'. 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. Based on the passage, with which of the following statements would the author most likely NOT disagree?a)Recent geological events can be substantially easier to investigate than ancient ones.b)Deposits of ground—up rocks always indicate that an ice age occurred.c)Discovering the cause of the ancient ice ages will have important practical consequences.d)Each of the early ice ages had a different proximate cause.Correct answer is option 'A'. 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. Based on the passage, with which of the following statements would the author most likely NOT disagree?a)Recent geological events can be substantially easier to investigate than ancient ones.b)Deposits of ground—up rocks always indicate that an ice age occurred.c)Discovering the cause of the ancient ice ages will have important practical consequences.d)Each of the early ice ages had a different proximate cause.Correct answer is option 'A'. 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. Based on the passage, with which of the following statements would the author most likely NOT disagree?a)Recent geological events can be substantially easier to investigate than ancient ones.b)Deposits of ground—up rocks always indicate that an ice age occurred.c)Discovering the cause of the ancient ice ages will have important practical consequences.d)Each of the early ice ages had a different proximate cause.Correct answer is option 'A'. Can you explain this answer? tests, examples and also practice CAT tests.