K
Khách

Hãy nhập câu hỏi của bạn vào đây, nếu là tài khoản VIP, bạn sẽ được ưu tiên trả lời.

8 tháng 4 2018

Chọn A

Kiến thức: Sự hòa hợp giữa chủ ngữ và động từ

Giải thích:

Khi chủ ngữ là N1 + of + N2, ta phải chia động từ theo N1. Ở đây động từ chia là "is" nên N1 phải là danh từ số ít.

Sửa lại: shelves => shelf

Tạm dịch: Thềm lục địa ở khu vực nông của đáy đại dương là gần lục địa nhất

8 tháng 10 2017

Đáp án D

 Kiến thức: Sửa lỗi sai

Giải thích:

closest to => far from

Câu này sai về kiến thức trên thực tế, đáy đại dương cách xa lục địa, chứ không phải gần nhất với lục địa

Tạm dịch: Thềm lục địa là khu vực bóng tối của đại dương cách xa các lục địa.

Read the following passage and mark the letter A, B, C, or D on your answer sheet to indicate the correct answer to each of the questions. Continents and ocean basins represent the largest identifiable bodies on Earth. On the solid portions of the planet, the second most prominent features are flat plains, elevated plateaus, and large mountain ranges. In geography, the term "continent" refers to the surface of continuous landmasses that together comprise about 29.2% of the planet's surface. On...
Đọc tiếp

Read the following passage and mark the letter A, B, C, or D on your answer sheet to indicate the correct answer to each of the questions.

Continents and ocean basins represent the largest identifiable bodies on Earth. On the solid portions of the planet, the second most prominent features are flat plains, elevated plateaus, and large mountain ranges. In geography, the term "continent" refers to the surface of continuous landmasses that together comprise about 29.2% of the planet's surface. On the other hand, another definition is prevalent in the general use of the term that deals with    extensive main lands, such as Europe or Asia, that actually represent one very large landmass. Although all continents are bounded by the water bodies or high mountain ranges,

 

isolated main lands, such as Greenland and India-Pakistan areas are called subcontinents. In some circles, the distinction between continents and large islands lies almost exclusively in the size of a particular landmass.

The analysis of compression and tension in the earth's crust has determined that continental structures are composed of layers that underlie continental shelves. A great deal of disagreement among geologists surrounds the issue of exactly how many layers underlie each landmass because of their distinctive mineral and chemical composition. It's also quite possible that the ocean floor rests on top of unknown continents that have not yet been explored. The continental crust is believed to have been formed by means of a chemical reaction when lighter materials separated from heavier ones, thus settling at various levels within the crust. Assisted by the measurements of the specifics within crust formations by means of monitoring earthquakes, geologists can speculate that a chemical split occurred to form the atmosphere, sea water and the crust before it solidified many centuries ago.

Although each continent has its special features, all consist of various combinations of components that include shields, mountain belts, intra - cratonic basins, margins, volcanic plateaus, and block-vaulted belts. The basic differences among continents lie in the proportion and the composition of these features relative to the continent size. Climatic zones have a crucial effect on the weathering and formation of the surface features, soil erosion, soil deposition, land formation, vegetation, and human activities.

Mountain belts are elongated narrow zones that have a characteristic folded sedimentary organization of layers. They are typically produced during substantial crustal movements, which generate faulting and mountain building. When continental margins collide, the rise of a marginal edge leads to the formation of large mountain ranges, as explained by the plate tectonic theory. This process also accounts for the occurrence of mountain belts in ocean basins and produces evidence for the ongoing continental plate evolution.

According to the passage, what are the differences in the structure of continents?

A. The distinctive features of their elements. 

B. Ratios of major components and their comparative size. 

C. Climatic zones and their effect on the surface features. 

D. The proportional size of continents to one another.

1
23 tháng 3 2019

Chọn B

Theo đoạn văn, cấu trúc của các lục địa khác nhau như thế nào?

A. Tính chất riêng biệt của các thành phần cấu thành.

B. Tỉ lệ thành phần cấu thành chủ yếu và kích cỡ của chúng.

C. Vùng khí hậu và tác động của nó đối với đặc điểm bề mặt.

D. Kích cỡ của lục địa này so với lục địa khác.

Dẫn chứng: “The basic differences lie in the proportion and the composition of these features (components) relative to the continent size.”

Tạm dịch: Điểm khác biệt cơ bản nằm ở tỉ trọng của thành phần cấu thành so với kích cỡ của lục địa.

Read the following passage and mark the letter A, B, C, or D on your answer sheet to indicate the correct answer to each of the questions.Continents and ocean basins represent the largest identifiable bodies on Earth. On the solid portions of the planet, the second most prominent features are flat plains, elavated plateaus, and large moutain ranges. In geography, the term "continent" refers to the surface of continuous landmasses that together comprise about 29.2% of the planet's surface. On...
Đọc tiếp

Read the following passage and mark the letter A, B, C, or D on your answer sheet to indicate the correct answer to each of the questions.

Continents and ocean basins represent the largest identifiable bodies on Earth. On the solid portions of the planet, the second most prominent features are flat plains, elavated plateaus, and large moutain ranges. In geography, the term "continent" refers to the surface of continuous landmasses that together comprise about 29.2% of the planet's surface. On the other hand, another definition is prevalent in the general use of the term that deals with extensive mainlands, such as Europe or Asia, that actually represent one very large landmass. Although all continents are bounded by the water bodies or high mountain ranges, isolated mainlands, such as Greenland and India-Pakistan areas are called subcontinents. In some circles, the distinction between continents and large islands lies almost exclusively in the size of a particular landmass.

The analysis of compression and tension in the earth's crust has determined that continental structures are composed of layers that underlie continental shelves. A great deal of disagreement among geologists surrounds the issue of exactly how many layers underlie each landmass because of their distintive mineral and chemical composition. It's also quite possible that the ocean floor rests on top of unknown continents that have not yet been explored. The continental crust is believed to have been forrmed by means of a chemical reaction when lighter materials separated from heavier ones, thus settling at various levels within the crust. Assisted by the measurements of the specifics within crust formations by means of monitoring earthquakes, geologists can speculate that a chemical split occured to form the atmosphere, sea water and the crust before it solidified many centuries ago.

Although each continent has its special features, all consist of various combinations of components that include shields, moutain belts, intracratonic basins, margins, volcanic plateaus, and blockvaulted belts. The basic differences among continents lie in the proportion and the composition of these features relative to the continent size. Climatic zones have a crucial effect on the weathering and formation of the surface features, soil erosion, soil deposition, land formation, vegetation, and human activities.

Mountain belts are elongated narrow zones that have a characteristic folded sedimentary organization of layers. They are typically produced during substabtial crustal movements, which generate faulting and moutain building. When continental margins collide, the rise of a marginal edge leads to the formation of large moutain ranges, as explained by the plate tectonic theory. This process also accounts for the occurrence of mountain belts in ocean basins and produces evidence for the ongoing continental plate evolution.

According to the passage, what are the differences in the structure of continents?

A. The distinctive features of their elements.

B. Ratios of major components and their comparative size.

C. Climatic zones and their effect on the surface features.

D. The proportional size of continents to one another.

1
7 tháng 6 2017

Đáp án B

Kiến thức: đọc hiểu

Tạm dịch: Theo đoạn văn, sự khác biệt trong cấu trúc lục địa là gì?

A. Các cấu trúc riêng biệt của các yếu tố của chúng.

B. Tỷ lệ các thành phần chính và kích thước tương đối của chúng.

C. Các vùng khí hậu và ảnh hưởng của chúng đến các cấu trúc bề mặt.

D. Kích thước tỷ lệ của các lục địa với nhau.

Thông tin: The basic differences among continents lie in the proportion and the composition of these features relative to the continent size.

Read the following passage and mark the letter A, B, C, or D on your answer sheet to indicate the correct answer to each of the questions.Continents and ocean basins represent the largest identifiable bodies on Earth. On the solid portions of the planet, the second most prominent features are flat plains, elavated plateaus, and large moutain ranges. In geography, the term "continent" refers to the surface of continuous landmasses that together comprise about 29.2% of the planet's surface. On...
Đọc tiếp

Read the following passage and mark the letter A, B, C, or D on your answer sheet to indicate the correct answer to each of the questions.

Continents and ocean basins represent the largest identifiable bodies on Earth. On the solid portions of the planet, the second most prominent features are flat plains, elavated plateaus, and large moutain ranges. In geography, the term "continent" refers to the surface of continuous landmasses that together comprise about 29.2% of the planet's surface. On the other hand, another definition is prevalent in the general use of the term that deals with extensive mainlands, such as Europe or Asia, that actually represent one very large landmass. Although all continents are bounded by the water bodies or high mountain ranges, isolated mainlands, such as Greenland and India-Pakistan areas are called subcontinents. In some circles, the distinction between continents and large islands lies almost exclusively in the size of a particular landmass.

The analysis of compression and tension in the earth's crust has determined that continental structures are composed of layers that underlie continental shelves. A great deal of disagreement among geologists surrounds the issue of exactly how many layers underlie each landmass because of their distintive mineral and chemical composition. It's also quite possible that the ocean floor rests on top of unknown continents that have not yet been explored. The continental crust is believed to have been forrmed by means of a chemical reaction when lighter materials separated from heavier ones, thus settling at various levels within the crust. Assisted by the measurements of the specifics within crust formations by means of monitoring earthquakes, geologists can speculate that a chemical split occured to form the atmosphere, sea water and the crust before it solidified many centuries ago.

Although each continent has its special features, all consist of various combinations of components that include shields, moutain belts, intracratonic basins, margins, volcanic plateaus, and blockvaulted belts. The basic differences among continents lie in the proportion and the composition of these features relative to the continent size. Climatic zones have a crucial effect on the weathering and formation of the surface features, soil erosion, soil deposition, land formation, vegetation, and human activities.

Mountain belts are elongated narrow zones that have a characteristic folded sedimentary organization of layers. They are typically produced during substabtial crustal movements, which generate faulting and moutain building. When continental margins collide, the rise of a marginal edge leads to the formation of large moutain ranges, as explained by the plate tectonic theory. This process also accounts for the occurrence of mountain belts in ocean basins and produces evidence for the ongoing continental plate evolution.

The word "evidence" in the last line is closest in meaning to _____.

A. confirmation

B. eventuality

C. challenge

D. exemplification

1
13 tháng 1 2018

Đáp án A

Kiến thức: đọc hiểu

Giải thích: evidence (n): bằng chứng

A. confirmation (n): xác nhận               B. eventuality (n): sự ngẫu nhiên  

C. challenge (n): thử thách                    D. exemplification (n): minh họa

=> confirmation = evidence

Dịch bài đọc:

Các lục địa và các lưu vực đại dương đại diện cho bộ phậm có thể nhận dạng lớn nhất trên trái đất. Trên phần rắn của trái đất, các cấu trúc nổi bật thứ hai là đồng bằng, cao nguyên, và dãy núi lớn. Trong địa lý, thuật ngữ "lục địa" đề cập đến bề mặt của các liên lục địa liên tục chiếm khoảng 29,2% bề mặt của hành tinh. Mặt khác, một định nghĩa khác phổ biến trong việc sử dụng chung thuật ngữ liên quan đến các lục địa rộng lớn, chẳng hạn như châu Âu hoặc châu Á, thực sự đại diện cho một vùng đất rất lớn. Mặc dù tất cả các lục địa bị bao phủ bởi các vùng nước hoặc các dãy núi cao, các lục địa bị cô lập, chẳng hạn như vùng Greenland và Ấn Độ- Pakistan, được gọi là tiểu lục địa. Trong một số vòng tròn, sự phân biệt giữa các lục địa và các hòn đảo lớn hầu như chỉ có quy mô của một vùng đất cụ thể.

Việc phân tích sức ép và sức nén trong lớp vỏ trái đất đã xác định rằng cấu trúc lục địa bao gồm các lớp nằm dưới lớp thềm lục địa. Rất nhiều bất đồng giữa các nhà địa chất xung quanh vấn đề xác định chính xác có bao nhiêu lớp nền tảng cho từng vùng đất do khoáng chất và thành phần hóa học riêng biệt của chúng. Cũng có thể là đại dương nằm trên những lục địa chưa biết chưa được khám phá. Lớp vỏ lục địa được cho là đã bị tràn ngập bởi phản ứng hóa học khi các vật liệu nhẹ tách ra khỏi các lớp nặng hơn, do đó lắng xuống các mức độ khác nhau trong lớp vỏ. Các nhà địa chất học có thể suy đoán rằng một sự phân tách hóa học xảy ra để tạo thành bầu khí quyển, nước biển và vỏ trái đất trước khi nó đông lại nhiều thế kỷ trước.

Mặc dù mỗi châu lục có các đặc điểm đặc biệt, tất cả đều bao gồm các kết hợp các thành phần bao gồm khiên, đai cao su, các lưu vực intracratonic, lề, cao nguyên núi lửa, và các đai bị chặn. Sự khác biệt cơ bản giữa các châu lục nằm trong tỷ lệ và thành phần của các đặc tính này liên quan đến kích cỡ lục địa. Các vùng khí hậu có ảnh hưởng quan trọng đến thời tiết và sự hình thành các đặc tính bề mặt, xói mòn đất, lắng đọng đất, hình thành đất đai, thực vật và các hoạt động của con người.

Vành đai núi trải dài qua các vùng rộng lớn có các tổ hợp trầm tích đặc trưng của lớp. Chúng thường được sản xuất trong quá trình chuyển động vỏ trái đất, gây ra sự xây dựng đứt gãy và xây dựng. Khi biên giới lục địa va chạm, sự gia tăng của cạnh biên tạo ra các dãy núi lớn như đã giải thích bởi lý thuyết kiến tạo mảng. Quá trình này cũng giải thích cho sự xuất hiện của các vành đai núi trong các lưu vực đại dương và tạo ra bằng chứng cho sự phát triển của lục địa đang diễn ra.

  Read the following passage and mark the letter A, B, C, or D on your answer sheet to indicate the correct answer to each of the questions.   Continents and ocean basins represent the largest identifiable bodies on Earth. On the solid portions of the planet, the second most prominent features are flat plains, elevated plateaus, and large mountain ranges. In geography, the term "continent" refers to the surface of continuous landmasses that together comprise about 29.2% of the planet's...
Đọc tiếp

 

Read the following passage and mark the letter A, B, C, or D on your answer sheet to indicate the correct answer to each of the questions.

 

Continents and ocean basins represent the largest identifiable bodies on Earth. On the solid portions of the planet, the second most prominent features are flat plains, elevated plateaus, and large mountain ranges. In geography, the term "continent" refers to the surface of continuous landmasses that together comprise about 29.2% of the planet's surface. On the other hand, another definition is prevalent in the general use of the term that deals with    extensive main lands, such as Europe or Asia, that actually represent one very large landmass. Although all continents are bounded by the water bodies or high mountain ranges,

 

isolated main lands, such as Greenland and India-Pakistan areas are called subcontinents. In some circles, the distinction between continents and large islands lies almost exclusively in the size of a particular landmass.

The analysis of compression and tension in the earth's crust has determined that continental structures are composed of layers that underlie continental shelves. A great deal of disagreement among geologists surrounds the issue of exactly how many layers underlie each landmass because of their distinctive mineral and chemical composition. It's also quite possible that the ocean floor rests on top of unknown continents that have not yet been explored. The continental crust is believed to have been formed by means of a chemical reaction when lighter materials separated from heavier ones, thus settling at various levels within the crust. Assisted by the measurements of the specifics within crust formations by means of monitoring earthquakes, geologists can speculate that a chemical split occurred to form the atmosphere, sea water and the crust before it solidified many centuries ago.

Although each continent has its special features, all consist of various combinations of components that include shields, mountain belts, intra - cratonic basins, margins, volcanic plateaus, and block-vaulted belts. The basic differences among continents lie in the proportion and the composition of these features relative to the continent size. Climatic zones have a crucial effect on the weathering and formation of the surface features, soil erosion, soil deposition, land formation, vegetation, and human activities.

Mountain belts are elongated narrow zones that have a characteristic folded sedimentary organization of layers. They are typically produced during substantial crustal movements, which generate faulting and mountain building. When continental margins collide, the rise of a marginal edge leads to the formation of large mountain ranges, as explained by the plate tectonic theory. This process also accounts for the occurrence of mountain belts in ocean basins and produces evidence for the ongoing continental plate evolution.

According to the passage, how do scientists define continents?

 

A. As masses of land without divisions

B. As extensive bodies of land.

C. As surficial compositions and ranges.

D. As the largest identifiable features.

1
24 tháng 4 2019

Chọn A

Theo đoạn văn, các nhà khoa định nghĩa lục địa như thế nào?

A. Là các mảnh đất lớn, không có sự chia cắt.

B. Là vùng đất mở rộng.

C. Là cấu tạo trên bề mặt và dãy.

D. Là thực thể lớn nhất từng thấy.

Dẫn chứng: “In geography, the term “continent” refers to the surface of continuous landmasses.”

Tạm dịch: Trong địa lý, lục địa là những mảnh đất lớn với bề mặt liền mạch.

Read the following passage and mark the letter A, B, C, or D on your answer sheet to indicate the correct answer to each of the questions.Continents and ocean basins represent the largest identifiable bodies on Earth. On the solid portions of the planet, the second most prominent features are flat plains, elavated plateaus, and large moutain ranges. In geography, the term "continent" refers to the surface of continuous landmasses that together comprise about 29.2% of the planet's surface. On...
Đọc tiếp

Read the following passage and mark the letter A, B, C, or D on your answer sheet to indicate the correct answer to each of the questions.

Continents and ocean basins represent the largest identifiable bodies on Earth. On the solid portions of the planet, the second most prominent features are flat plains, elavated plateaus, and large moutain ranges. In geography, the term "continent" refers to the surface of continuous landmasses that together comprise about 29.2% of the planet's surface. On the other hand, another definition is prevalent in the general use of the term that deals with extensive mainlands, such as Europe or Asia, that actually represent one very large landmass. Although all continents are bounded by the water bodies or high mountain ranges, isolated mainlands, such as Greenland and India-Pakistan areas are called subcontinents. In some circles, the distinction between continents and large islands lies almost exclusively in the size of a particular landmass.

The analysis of compression and tension in the earth's crust has determined that continental structures are composed of layers that underlie continental shelves. A great deal of disagreement among geologists surrounds the issue of exactly how many layers underlie each landmass because of their distintive mineral and chemical composition. It's also quite possible that the ocean floor rests on top of unknown continents that have not yet been explored. The continental crust is believed to have been forrmed by means of a chemical reaction when lighter materials separated from heavier ones, thus settling at various levels within the crust. Assisted by the measurements of the specifics within crust formations by means of monitoring earthquakes, geologists can speculate that a chemical split occured to form the atmosphere, sea water and the crust before it solidified many centuries ago.

Although each continent has its special features, all consist of various combinations of components that include shields, moutain belts, intracratonic basins, margins, volcanic plateaus, and blockvaulted belts. The basic differences among continents lie in the proportion and the composition of these features relative to the continent size. Climatic zones have a crucial effect on the weathering and formation of the surface features, soil erosion, soil deposition, land formation, vegetation, and human activities.

Mountain belts are elongated narrow zones that have a characteristic folded sedimentary organization of layers. They are typically produced during substabtial crustal movements, which generate faulting and moutain building. When continental margins collide, the rise of a marginal edge leads to the formation of large moutain ranges, as explained by the plate tectonic theory. This process also accounts for the occurrence of mountain belts in ocean basins and produces evidence for the ongoing continental plate evolution.

According to tha passage, how do scientists define continents?

A. As masses of land without divisions.

B. As extensive bodies of land.

C. As surficial compositions and ranges.

D. As the largest identifiable features.

1
7 tháng 6 2018

Đáp án A

Kiến thức: đọc hiểu

Tạm dịch: Theo đoạn văn này, các nhà khoa học xác định các lục địa như thế nào?

A. Là một khối lượng đất lớn không chia tách.      B. Là các vùng đất rộng lớn.

C. Là thành phần bề mặt và các dãy núi.      D. Là cấu trúc có thể nhận diện lớn nhất.

Thông  tin:  In  geography,  the  term  "continent"  refers  to  the  surface  of  continuous  landmasses  that  together comprise about 29.2% of the planet's surface.

Read the following passage and mark the letter A, B, C, or D on your answer sheet to indicate the correct answer to each of the questions.Continents and ocean basins represent the largest identifiable bodies on Earth. On the solid portions of the planet, the second most prominent features are flat plains, elavated plateaus, and large moutain ranges. In geography, the term "continent" refers to the surface of continuous landmasses that together comprise about 29.2% of the planet's surface. On...
Đọc tiếp

Read the following passage and mark the letter A, B, C, or D on your answer sheet to indicate the correct answer to each of the questions.

Continents and ocean basins represent the largest identifiable bodies on Earth. On the solid portions of the planet, the second most prominent features are flat plains, elavated plateaus, and large moutain ranges. In geography, the term "continent" refers to the surface of continuous landmasses that together comprise about 29.2% of the planet's surface. On the other hand, another definition is prevalent in the general use of the term that deals with extensive mainlands, such as Europe or Asia, that actually represent one very large landmass. Although all continents are bounded by the water bodies or high mountain ranges, isolated mainlands, such as Greenland and India-Pakistan areas are called subcontinents. In some circles, the distinction between continents and large islands lies almost exclusively in the size of a particular landmass.

The analysis of compression and tension in the earth's crust has determined that continental structures are composed of layers that underlie continental shelves. A great deal of disagreement among geologists surrounds the issue of exactly how many layers underlie each landmass because of their distintive mineral and chemical composition. It's also quite possible that the ocean floor rests on top of unknown continents that have not yet been explored. The continental crust is believed to have been forrmed by means of a chemical reaction when lighter materials separated from heavier ones, thus settling at various levels within the crust. Assisted by the measurements of the specifics within crust formations by means of monitoring earthquakes, geologists can speculate that a chemical split occured to form the atmosphere, sea water and the crust before it solidified many centuries ago.

Although each continent has its special features, all consist of various combinations of components that include shields, moutain belts, intracratonic basins, margins, volcanic plateaus, and blockvaulted belts. The basic differences among continents lie in the proportion and the composition of these features relative to the continent size. Climatic zones have a crucial effect on the weathering and formation of the surface features, soil erosion, soil deposition, land formation, vegetation, and human activities.

Mountain belts are elongated narrow zones that have a characteristic folded sedimentary organization of layers. They are typically produced during substabtial crustal movements, which generate faulting and moutain building. When continental margins collide, the rise of a marginal edge leads to the formation of large moutain ranges, as explained by the plate tectonic theory. This process also accounts for the occurrence of mountain belts in ocean basins and produces evidence for the ongoing continental plate evolution.

The word "bounded" is closest in meaning to

A. covered

B. convened

C. dominated

D. delimited

1
25 tháng 12 2017

Đáp án D

Kiến thức: đọc hiểu, từ vựng

Giải thích: to bound (v): vạch biên giơ i

to cover: bao phủ                                 to convene: nhóm họp

to dominate: thống trị               to delimit: phân biên giới

Read the following passage and mark the letter A, B, C, or D on your answer sheet to indicate the correct answer to each of the questions. Continents and ocean basins represent the largest identifiable bodies on Earth. On the solid portions of the planet, the second most prominent features are flat plains, elevated plateaus, and large mountain ranges. In geography, the term "continent" refers to the surface of continuous landmasses that together comprise about 29.2% of the planet's surface. On...
Đọc tiếp

Read the following passage and mark the letter A, B, C, or D on your answer sheet to indicate the correct answer to each of the questions.

Continents and ocean basins represent the largest identifiable bodies on Earth. On the solid portions of the planet, the second most prominent features are flat plains, elevated plateaus, and large mountain ranges. In geography, the term "continent" refers to the surface of continuous landmasses that together comprise about 29.2% of the planet's surface. On the other hand, another definition is prevalent in the general use of the term that deals with    extensive main lands, such as Europe or Asia, that actually represent one very large landmass. Although all continents are bounded by the water bodies or high mountain ranges,

 

isolated main lands, such as Greenland and India-Pakistan areas are called subcontinents. In some circles, the distinction between continents and large islands lies almost exclusively in the size of a particular landmass.

The analysis of compression and tension in the earth's crust has determined that continental structures are composed of layers that underlie continental shelves. A great deal of disagreement among geologists surrounds the issue of exactly how many layers underlie each landmass because of their distinctive mineral and chemical composition. It's also quite possible that the ocean floor rests on top of unknown continents that have not yet been explored. The continental crust is believed to have been formed by means of a chemical reaction when lighter materials separated from heavier ones, thus settling at various levels within the crust. Assisted by the measurements of the specifics within crust formations by means of monitoring earthquakes, geologists can speculate that a chemical split occurred to form the atmosphere, sea water and the crust before it solidified many centuries ago.

Although each continent has its special features, all consist of various combinations of components that include shields, mountain belts, intra - cratonic basins, margins, volcanic plateaus, and block-vaulted belts. The basic differences among continents lie in the proportion and the composition of these features relative to the continent size. Climatic zones have a crucial effect on the weathering and formation of the surface features, soil erosion, soil deposition, land formation, vegetation, and human activities.

Mountain belts are elongated narrow zones that have a characteristic folded sedimentary organization of layers. They are typically produced during substantial crustal movements, which generate faulting and mountain building. When continental margins collide, the rise of a marginal edge leads to the formation of large mountain ranges, as explained by the plate tectonic theory. This process also accounts for the occurrence of mountain belts in ocean basins and produces evidence for the ongoing continental plate evolution.

The word "bounded" is closest in meaning to    

A. covered

B. convened

C. dominated

D. delimited

1
4 tháng 7 2019

Chọn D

Từ “bounded” gần nghĩa với từ nào nhất?

A. covered: bao chùm

B. convened: triệu tập

C. dominated: thống trị

D. delimited: giới hạn = bound

Read the following passage and mark the letter A, B, C, or D on your answer sheet to indicate the correct answer to each of the questions. Continents and ocean basins represent the largest identifiable bodies on Earth. On the solid portions of the planet, the second most prominent features are flat plains, elevated plateaus, and large mountain ranges. In geography, the term "continent" refers to the surface of continuous landmasses that together comprise about 29.2% of the planet's surface. On...
Đọc tiếp

Read the following passage and mark the letter A, B, C, or D on your answer sheet to indicate the correct answer to each of the questions.

Continents and ocean basins represent the largest identifiable bodies on Earth. On the solid portions of the planet, the second most prominent features are flat plains, elevated plateaus, and large mountain ranges. In geography, the term "continent" refers to the surface of continuous landmasses that together comprise about 29.2% of the planet's surface. On the other hand, another definition is prevalent in the general use of the term that deals with    extensive main lands, such as Europe or Asia, that actually represent one very large landmass. Although all continents are bounded by the water bodies or high mountain ranges,

 

isolated main lands, such as Greenland and India-Pakistan areas are called subcontinents. In some circles, the distinction between continents and large islands lies almost exclusively in the size of a particular landmass.

The analysis of compression and tension in the earth's crust has determined that continental structures are composed of layers that underlie continental shelves. A great deal of disagreement among geologists surrounds the issue of exactly how many layers underlie each landmass because of their distinctive mineral and chemical composition. It's also quite possible that the ocean floor rests on top of unknown continents that have not yet been explored. The continental crust is believed to have been formed by means of a chemical reaction when lighter materials separated from heavier ones, thus settling at various levels within the crust. Assisted by the measurements of the specifics within crust formations by means of monitoring earthquakes, geologists can speculate that a chemical split occurred to form the atmosphere, sea water and the crust before it solidified many centuries ago.

Although each continent has its special features, all consist of various combinations of components that include shields, mountain belts, intra - cratonic basins, margins, volcanic plateaus, and block-vaulted belts. The basic differences among continents lie in the proportion and the composition of these features relative to the continent size. Climatic zones have a crucial effect on the weathering and formation of the surface features, soil erosion, soil deposition, land formation, vegetation, and human activities.

Mountain belts are elongated narrow zones that have a characteristic folded sedimentary organization of layers. They are typically produced during substantial crustal movements, which generate faulting and mountain building. When continental margins collide, the rise of a marginal edge leads to the formation of large mountain ranges, as explained by the plate tectonic theory. This process also accounts for the occurrence of mountain belts in ocean basins and produces evidence for the ongoing continental plate evolution.

The word "evidence" in the last line is closest in meaning to_______.

A. confirmation

B. eventuality

C. challenge

D. exemplification

1
7 tháng 6 2017

Chọn A

Từ “evidence” ở dòng cuối gần nghĩa với từ nào nhất?

A. sự khẳng định = evidence (n): chứng cứ

B. sự cuối cùng

C. thử thách

D. sự soi chiếu