5 bài mẫu phần đọc hiểu trong đề ôn thi THPT quốc gia 2022 môn Anh
Phần Đọc hiểu trong đề ôn thi THPT quốc gia 2022 môn Anh thường là phần khó kiếm điểm do dài và có nhiều từ mới. Tuy nhiên nếu bạn đã làm quen dạng bài này bạn sẽ tự mình rút ra được một vài mẹo nhỏ khi chọn đáp án cho các câu hỏi. Dưới đây là 5 bài mẫu giúp bạn luyện tập thêm. Cùng thử sức xem sao nhé!
5 BÀI MẪU TRONG PHẦN ĐỌC HIỂU
CÂU 1:
Read the following passage and mark the letter A, B, C or D on you answer sheet to indicate the correct answer to each of the questions.
Glaciers are large masses of ice on land that show evidence of past or present movement. They grow by the gradual transformation of snow into glacier ice. A fresh snowfall is a fluffy mass of loosely packed snowflakes, small delicate ice crystals grown in the atmosphere. As the snow ages on the ground for weeks or months, the crystals shrink and become more compact to form firm, a much whole mass becomes squeezed together into a more dense form, granular snow. As new snow falls and buries the older snow, the layers of granular snow further compact to form firm, a much denser kind of snow, usually a year or more old, which has little pore space. Further burial and slow cementation- a process by which crystals become bound together in a mosaic of intergrown ice crystals- finally produce solid glacial ice. In this process of recrystallization, the growth of new crystals at the expense of old ones, the percentage of air is reduced from about 90 percent for snowflakes to less than 20 percent for glacier ice. The whole process may take as little as a few years, but more likely ten or twenty years or longer. The snow is usually many meters deep by the time the lower layers are converted into ice.
In cold glaciers those formed in the coldest regions of the Earth, the entire mass of ice is at temperatures below the melting point and no free water exists. In temperate glaciers, the ice is at the melting point at every pressure level within the glaciers, and free water is present as small drops or as larger accumulations, in tunnels within or beneath the ice. Formation of a glacier is complete when ice has accumulated to a thickness (and thus weight) sufficient to make it move slowly under pressure, in much the same way that solid rock deep within the Earth can change shape without breaking. Once that point is reached, the ice flows downhill, either as a tongue of ice filling a valley or as thick ice cap that flows out in directions from the highest central area where the most snow accumulates. The up down leads to the eventual melting of ice
Which of the following does the passage mainly discuss?
A. Damage from glaciers
B. The location of glaciers
C. The effect of glaciers on climate
D. Glacier formation
CÂU 2:
Read the following passage and mark the letter A, B, C or D on you answer sheet to indicate the correct answer to each of the questions.
Glaciers are large masses of ice on land that show evidence of past or present movement. They grow by the gradual transformation of snow into glacier ice. A fresh snowfall is a fluffy mass of loosely packed snowflakes, small delicate ice crystals grown in the atmosphere. As the snow ages on the ground for weeks or months, the crystals shrink and become more compact to form firm, a much whole mass becomes squeezed together into a more dense form, granular snow. As new snow falls and buries the older snow, the layers of granular snow further compact to form firm, a much denser kind of snow, usually a year or more old, which has little pore space. Further burial and slow cementation- a process by which crystals become bound together in a mosaic of intergrown ice crystals- finally produce solid glacial ice. In this process of recrystallization, the growth of new crystals at the expense of old ones, the percentage of air is reduced from about 90 percent for snowflakes to less than 20 percent for glacier ice. The whole process may take as little as a few years, but more likely ten or twenty years or longer. The snow is usually many meters deep by the time the lower layers are converted into ice.
In cold glaciers those formed in the coldest regions of the Earth, the entire mass of ice is at temperatures below the melting point and no free water exists. In temperate glaciers, the ice is at the melting point at every pressure level within the glaciers, and free water is present as small drops or as larger accumulations, in tunnels within or beneath the ice. Formation of a glacier is complete when ice has accumulated to a thickness (and thus weight) sufficient to make it move slowly under pressure, in much the same way that solid rock deep within the Earth can change shape without breaking. Once that point is reached, the ice flows downhill, either as a tongue of ice filling a valley or as thick ice cap that flows out in directions from the highest central area where the most snow accumulates. The up down leads to the eventual melting of ice
Which of the following will cause density within the glacier to increase?
A. Pressure from the weight of new snow
B. Increased water and air content
C. Long periods of darkness and temperature variations
D. Movement of the glacier
CÂU 3:
Read the following passage and mark the letter A, B, C or D on you answer sheet to indicate the correct answer to each of the questions.
Glaciers are large masses of ice on land that show evidence of past or present movement. They grow by the gradual transformation of snow into glacier ice. A fresh snowfall is a fluffy mass of loosely packed snowflakes, small delicate ice crystals grown in the atmosphere. As the snow ages on the ground for weeks or months, the crystals shrink and become more compact to form firm, a much whole mass becomes squeezed together into a more dense form, granular snow. As new snow falls and buries the older snow, the layers of granular snow further compact to form firm, a much denser kind of snow, usually a year or more old, which has little pore space. Further burial and slow cementation- a process by which crystals become bound together in a mosaic of intergrown ice crystals- finally produce solid glacial ice. In this process of recrystallization, the growth of new crystals at the expense of old ones, the percentage of air is reduced from about 90 percent for snowflakes to less than 20 percent for glacier ice. The whole process may take as little as a few years, but more likely ten or twenty years or longer. The snow is usually many meters deep by the time the lower layers are converted into ice.
In cold glaciers those formed in the coldest regions of the Earth, the entire mass of ice is at temperatures below the melting point and no free water exists. In temperate glaciers, the ice is at the melting point at every pressure level within the glaciers, and free water is present as small drops or as larger accumulations, in tunnels within or beneath the ice. Formation of a glacier is complete when ice has accumulated to a thickness (and thus weight) sufficient to make it move slowly under pressure, in much the same way that solid rock deep within the Earth can change shape without breaking. Once that point is reached, the ice flows downhill, either as a tongue of ice filling a valley or as thick ice cap that flows out in directions from the highest central area where the most snow accumulates. The up down leads to the eventual melting of ice
The word “bound” in paragraph 1 is closest in meaning to ________.
A. chosen
B. covered
C. held
D. planned
CÂU 4:
Read the following passage and mark the letter A, B, C or D on you answer sheet to indicate the correct answer to each of the questions.
Glaciers are large masses of ice on land that show evidence of past or present movement. They grow by the gradual transformation of snow into glacier ice. A fresh snowfall is a fluffy mass of loosely packed snowflakes, small delicate ice crystals grown in the atmosphere. As the snow ages on the ground for weeks or months, the crystals shrink and become more compact to form firm, a much whole mass becomes squeezed together into a more dense form, granular snow. As new snow falls and buries the older snow, the layers of granular snow further compact to form firm, a much denser kind of snow, usually a year or more old, which has little pore space. Further burial and slow cementation- a process by which crystals become bound together in a mosaic of intergrown ice crystals- finally produce solid glacial ice. In this process of recrystallization, the growth of new crystals at the expense of old ones, the percentage of air is reduced from about 90 percent for snowflakes to less than 20 percent for glacier ice. The whole process may take as little as a few years, but more likely ten or twenty years or longer. The snow is usually many meters deep by the time the lower layers are converted into ice.
In cold glaciers those formed in the coldest regions of the Earth, the entire mass of ice is at temperatures below the melting point and no free water exists. In temperate glaciers, the ice is at the melting point at every pressure level within the glaciers, and free water is present as small drops or as larger accumulations, in tunnels within or beneath the ice. Formation of a glacier is complete when ice has accumulated to a thickness (and thus weight) sufficient to make it move slowly under pressure, in much the same way that solid rock deep within the Earth can change shape without breaking. Once that point is reached, the ice flows downhill, either as a tongue of ice filling a valley or as thick ice cap that flows out in directions from the highest central area where the most snow accumulates. The up down leads to the eventual melting of ice
The word “converted” in paragraph 1 is closest in meaning to _________.
A. delayed
B. changed
C. promoted
D. dissolved
CÂU 5:
Read the following passage and mark the letter A, B, C or D on you answer sheet to indicate the correct answer to each of the questions.
Glaciers are large masses of ice on land that show evidence of past or present movement. They grow by the gradual transformation of snow into glacier ice. A fresh snowfall is a fluffy mass of loosely packed snowflakes, small delicate ice crystals grown in the atmosphere. As the snow ages on the ground for weeks or months, the crystals shrink and become more compact to form firm, a much whole mass becomes squeezed together into a more dense form, granular snow. As new snow falls and buries the older snow, the layers of granular snow further compact to form firm, a much denser kind of snow, usually a year or more old, which has little pore space. Further burial and slow cementation- a process by which crystals become bound together in a mosaic of intergrown ice crystals- finally produce solid glacial ice. In this process of recrystallization, the growth of new crystals at the expense of old ones, the percentage of air is reduced from about 90 percent for snowflakes to less than 20 percent for glacier ice. The whole process may take as little as a few years, but more likely ten or twenty years or longer. The snow is usually many meters deep by the time the lower layers are converted into ice.
In cold glaciers those formed in the coldest regions of the Earth, the entire mass of ice is at temperatures below the melting point and no free water exists. In temperate glaciers, the ice is at the melting point at every pressure level within the glaciers, and free water is present as small drops or as larger accumulations, in tunnels within or beneath the ice. Formation of a glacier is complete when ice has accumulated to a thickness (and thus weight) sufficient to make it move slowly under pressure, in much the same way that solid rock deep within the Earth can change shape without breaking. Once that point is reached, the ice flows downhill, either as a tongue of ice filling a valley or as thick ice cap that flows out in directions from the highest central area where the most snow accumulates. The up down leads to the eventual melting of ice
In temperate glaciers, where is water found?
A. In a thin layer below the firm
B. In pools at various depths
C. Only near the surface
D. In tunnels
ĐÁP ÁN
Câu 1:
Đoạn văn chủ yếu bàn về nội dung nào sau đây?
- Thiệt hại do sông băng B. Vị trí của sông băng
C. Ảnh hưởng của sông băng đến khí hậu D. Sự hình thành sông băng
Thông tin: Glaciers are large masses of ice on land that show evidence of past or present movement. They grow by the gradual transformation of snow into glacier ice. A fresh snowfall is a fluffy mass of loosely packed snowflakes, small delicate ice crystals grown in the atmosphere.
Tạm dịch: Sông băng là những khối băng lớn trên đất liền cho thấy bằng chứng về sự di chuyển trong quá khứ hoặc hiện tại. Chúng phát triển bởi sự biến đổi dần dần của tuyết thành băng của sông băng. Một trận tuyết mới rơi là một khối bông tuyết mềm xốp lỏng lẻo, những tinh thể băng nhỏ tinh tế được hình thành trong khí quyển.
Chọn D
Câu 2:
Cái nào sau đây sẽ khiến mật độ trong sông băng tăng lên?
Áp lực từ trọng lượng của tuyết mới B. Tăng hàm lượng nước và không khí
Thời gian dài của bóng tối và sự thay đổi nhiệt độ D. Chuyển động của sông băng
Thông tin: As new snow falls and buries the older snow, the layers of granular snow further compact to form firm, a much denser kind of snow, usually a year or more old, which has little pore space.
Tạm dịch: Khi tuyết mới rơi xuống và vùi lấp lớp tuyết cũ hơn, các lớp tuyết dạng hạt sẽ nén chặt hơn nữa để tạo thành khối cứng, một loại tuyết dày đặc hơn, thường là một năm tuổi trở lên, có rất ít lỗ rỗng.
Chọn A
Câu 3:
Từ “bound” (liên kết) trong đoạn 1 gần nghĩa nhất với ________.
chosen: được chọn B. covered: được bao phủ
held: được tổ chức D. planned: được lên kế hoạch
Thông tin: Further burial and slow cementation- a process by which crystals become bound together in a mosaic of intergrown ice crystals- finally produce solid glacial ice.
Tạm dịch: Quá trình chôn lấp sâu hơn và quá trình xi măng hóa chậm – một quá trình mà các tinh thể liên kết với nhau trong một bức tranh khảm các tinh thể băng xen kẽ nhau – cuối cùng tạo ra băng rắn.
Chọn C
Câu 4:
Từ “converted” (chuyển thành) trong đoạn 1 gần nghĩa nhất với ________.
delayed: trì hoãn B. changed: thay đổi
promoted: thúc đẩy, xúc tiến D. dissolved: giải thể
Thông tin: The snow is usually many meters deep by the time the lower layers are converted into ice.
Tạm dịch: Tuyết thường sâu nhiều mét vào thời điểm các lớp bên dưới chuyển thành băng.
Chọn B
Câu 5:
Trong các sông băng ôn đới, nước được tìm thấy ở đâu?
Trong một lớp mỏng bên dưới lớp cứng B. Trong các vũng ở các độ sâu khác nhau
Chỉ gần bề mặt D. Trong đường hầm
Thông tin: In temperate glaciers, the ice is at the melting point at every pressure level within the glaciers, and free water is present as small drops or as larger accumulations, in tunnels within or beneath the ice.
Tạm dịch: Ở các sông băng ôn đới, băng ở điểm tan chảy ở mọi mức áp suất bên trong sông băng và nước tự do tồn tại dưới dạng những giọt nhỏ hoặc tích tụ lớn hơn, trong các đường hầm bên trong hoặc bên dưới băng.
Chọn D
Mặc dù phần đọc hiểu trong đề ôn thi THPT quốc gia 2022 môn Anh là phần thi khó và mất thời gian do dài và khó dịch. Tuy nhiên đừng lo lắng, bạn hãy nắm bắt nhanh các ý chính trong câu hỏi và đối chiếu vào phần bài đọc để tìm ra đáp án đúng nhé. Chúc bạn làm thật tốt!
