Hi. Sorry about the wait.
I have looked up the passage. Page 464 of the OG 2025-2026.
The passage has been modified slightly (seems superficially) but very interesting that it has been modified the way it was. I will see if I can put them side by side and compare.
OLD
Years before the advent of plate tectonics―the widely accepted theory, developed in the mid-1960's, the holds that the major features of Earth's surface are created by the horizontal motions of Earth's outer shell, or lithosphere―a similar theory was rejected by the geological community. In 1912, Alfred Wegener proposed, in a widely debated theory that came to be called continental drift, that Earth's continents were mobile. To most geologists today, Wegener's The origin of Continents and Oceans appears an impressive and prescient document, containing several of the essential presumptions underlying plate tectonics theory: the horizontal mobility of pieces of Earth's crust; the essential difference between oceanic and continental crust; and a causal connection between horizontal displacements and the formation of mountain chains. Yet despite the considerable overlap between Wegener's concepts and the later widely embraced plate tectonics theory, and despite the fact that continental drift theory presented a possible solution to the problem of the origin of mountains at a time when existing explanations were seriously in doubt, in its day Wegener's theory was rejected by the vast majority of geologists.
Most geologists and many historians today believe that Wegener's theory was rejected because of its lack of an adequate mechanical basis. Stephen Jay Gould, for example, argues that continental drift theory was rejected because it did not explain how continents could move through an apparently solid oceanic floor. However, as Anthony Hallam has pointed out, many scientific phenomena, such as the ice ages, have been accepted before they could be fully explained. The most likely cause for the rejection of continental drift―a cause that has been largely ignored because we consider Wegener's theory to have been validated by the theory of plate tectonics―is the nature of the evidence that was put forward to support it. Most of Wegener's evidence consisted of homologies―similarities of patterns and forms based on direct observations of rocks in the field, supported by the use of hammers, hand lenses, and field notebooks. In contrast, the data supporting plate tectonics were impressively geophysical―instrumental determinations of the physical properties of Earth garnered through the use of seismographs, magnetometers, and computers.
NEW
Years before the advent of plate tectonics-the widely accepted theory, developed in the mid-1960s, that holds the major features of Earth's surface are created by the horizontal motions of Earth's outer shell, or lithosphere-a similar theory was rejected by the geological community. In 1912, Alfred Wegener proposed, in a widely debated theory that came to be called continental drift, that Earth's continents were mobile. To most geologists today, Wegener's The Origin of Continents and Oceans appears an impressive and prescient document, containing several of the essential presumptions underlying plate tectonics theory: the horizontal mobility of pieces of Earth's crust; the essential difference between oceanic and continental crust; and a causal connection between horizontal displacements and the formation of mountain chains.
Yet despite the considerable overlap between Wegener's concepts and the later widely embraced plate tectonics theory, and despite the fact that continental drift theory presented a possible solution to the problem of the origin of mountains at a time when existing explanations were seriously in doubt, in its day Wegener's theory was rejected by the vast majority of geologists.
Most geologists and many historians today believe Wegener's theory was rejected because of its lack of an adequate mechanical basis. A group of researchers argues continental drift theory was rejected because it did not explain how continents could move through an apparently solid oceanic floor. However, as Anthony Hallam has pointed out, many scientific phenomena, such as the ice ages, have been accepted before they could be fully explained. The most likely cause for the rejection of continental drift—a cause that has been largely ignored because we consider Wegener's theory to have been validated by the theory of plate tectonics— is the nature of the evidence that was put forward to support it. Most of Wegener's evidence consisted of homologies-similarities of patterns and forms based on direct observations of rocks in the field, supported by the use of hammers, hand lenses, and field notebooks. In contrast, the data supporting plate tectonics were impressively geophysical: instrumental determinations of the physical properties of Earth garnered through the use of seismographs and magnetometers.
I have bolded the differences. The OA for the 5th Question The author of the passage most likely discusses the "essential presumptions" of the Origins of Continents and Oceans in order to (see lines 12-13) has been changed from D to B
B) Show why Wegener's theory os now regarded as prescient.D) Cite features of the theory of continental drift for which no evidence was available in Wegener's dayExplanation: The context of the phrase "essential presumptions" indicates that the author's purpose is to show how Wegener anticipated some of the important ideas in plate tectonics and was therefore prescient.
GMATNinjaTwo, let me know if you figure out this mystery!
GMATNinjaTwo
inesip
Hi - question 5 correct answer appear to be D instead of B, I don't understand why it is not B?
bb
Question #5 in the latest OG, OA switched from B to D. It is a mystery.
bb, weird! Did they change the explanation as well? (I don't yet have the new OG to check myself.)
I would stand by eliminating (D) because there was in fact evidence for Wegener's theory: "Most of Wegener's evidence consisted of homologies―similarities of patterns and forms based on direct observations of rocks in the field, supported by the use of hammers, hand lenses, and field notebooks".
(B) on the other hand seems like a good fit based on this part: "To most geologists today, Wegener's The origin of Continents and Oceans appears an impressive and prescient document, containing several of the essential presumptions underlying plate tectonics theory...".
