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TOEFL Reading Test

Authored by Mohammad Nur Hadiyansyah

English

University

Used 508+ times

TOEFL Reading Test
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50 questions

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1.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

Questions 1- 10

Precipitation, commonly referred to as rainfall, is a measure of the quantity of water in the form of either rain, hail, or snow which reaches the ground. The average annual precipi- tation over the whole of the United States is thirty-six inches. It should be understood however, that a foot of snow is not equal to a foot of precipitation. A general formula for

Line (5) computing the precipitation of snowfall is that ten inches of snow is equal to one inch of pre- cipitation. In New York State, for example, twenty inches of snow in one year would be recorded as only two inches of precipitation. Forty inches of rain would be recorded as forty inches of precipitation. The total annual precipitation would be recorded as forty-two inches. The amount of precipitation is a combined result of several factors, including location,

Line (10) altitude, proximity to the sea, and the direction of prevailing winds. Most of the precipitation in the United States is brought originally by prevailing winds from the Pacific Ocean, the Gulf of Mexico, the Atlantic Ocean, and the Great Lakes. Because these prevailing winds generally come from the West, the Pacific Coast receives more annual precipitation than the Atlantic Coast. Along the Pacific Coast itself, however, altitude causes some diversity in rain-

Line (15) fall. The mountain ranges of the United States, especially the Rocky Mountain Range and the Appalachian Mountain Range, influence the amount of precipitation in their areas. East of the Rocky Mountains, the annual precipitation decreases substantially from that west of the Rocky Mountains. The precipitation north of the Appalachian Mountains is about 40 percent

less than that south of the Appalachian Mountains.


What does this passage mainly discuss?

Precipitation

Snowfall

New York State

A general formula

2.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

Questions 1- 10

Precipitation, commonly referred to as rainfall, is a measure of the quantity of water in the form of either rain, hail, or snow which reaches the ground. The average annual precipi- tation over the whole of the United States is thirty-six inches. It should be understood however, that a foot of snow is not equal to a foot of precipitation. A general formula for

Line (5) computing the precipitation of snowfall is that ten inches of snow is equal to one inch of pre- cipitation. In New York State, for example, twenty inches of snow in one year would be recorded as only two inches of precipitation. Forty inches of rain would be recorded as forty inches of precipitation. The total annual precipitation would be recorded as forty-two inches. The amount of precipitation is a combined result of several factors, including location,

Line (10) altitude, proximity to the sea, and the direction of prevailing winds. Most of the precipitation in the United States is brought originally by prevailing winds from the Pacific Ocean, the Gulf of Mexico, the Atlantic Ocean, and the Great Lakes. Because these prevailing winds generally come from the West, the Pacific Coast receives more annual precipitation than the Atlantic Coast. Along the Pacific Coast itself, however, altitude causes some diversity in rain-

Line (15) fall. The mountain ranges of the United States, especially the Rocky Mountain Range and the Appalachian Mountain Range, influence the amount of precipitation in their areas. East of the Rocky Mountains, the annual precipitation decreases substantially from that west of the Rocky Mountains. The precipitation north of the Appalachian Mountains is about 40 percent

less than that south of the Appalachian Mountains.


Which of the following is another word that is often used in place of precipitation?

Humidity

Wetness

Rainfall

Rain-snow

3.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

Questions 1- 10

Precipitation, commonly referred to as rainfall, is a measure of the quantity of water in the form of either rain, hail, or snow which reaches the ground. The average annual precipi- tation over the whole of the United States is thirty-six inches. It should be understood however, that a foot of snow is not equal to a foot of precipitation. A general formula for

Line (5) computing the precipitation of snowfall is that ten inches of snow is equal to one inch of pre- cipitation. In New York State, for example, twenty inches of snow in one year would be recorded as only two inches of precipitation. Forty inches of rain would be recorded as forty inches of precipitation. The total annual precipitation would be recorded as forty-two inches. The amount of precipitation is a combined result of several factors, including location,

Line (10) altitude, proximity to the sea, and the direction of prevailing winds. Most of the precipitation in the United States is brought originally by prevailing winds from the Pacific Ocean, the Gulf of Mexico, the Atlantic Ocean, and the Great Lakes. Because these prevailing winds generally come from the West, the Pacific Coast receives more annual precipitation than the Atlantic Coast. Along the Pacific Coast itself, however, altitude causes some diversity in rain-

Line (15) fall. The mountain ranges of the United States, especially the Rocky Mountain Range and the Appalachian Mountain Range, influence the amount of precipitation in their areas. East of the Rocky Mountains, the annual precipitation decreases substantially from that west of the Rocky Mountains. The precipitation north of the Appalachian Mountains is about 40 percent

less than that south of the Appalachian Mountains.


The term precipitation includes

only rainfall

rain, hail, and snow

rain, snow, and humidity

rain, hail, and humidity

4.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

Questions 1- 10

Precipitation, commonly referred to as rainfall, is a measure of the quantity of water in the form of either rain, hail, or snow which reaches the ground. The average annual precipi- tation over the whole of the United States is thirty-six inches. It should be understood however, that a foot of snow is not equal to a foot of precipitation. A general formula for

Line (5) computing the precipitation of snowfall is that ten inches of snow is equal to one inch of pre- cipitation. In New York State, for example, twenty inches of snow in one year would be recorded as only two inches of precipitation. Forty inches of rain would be recorded as forty inches of precipitation. The total annual precipitation would be recorded as forty-two inches. The amount of precipitation is a combined result of several factors, including location,

Line (10) altitude, proximity to the sea, and the direction of prevailing winds. Most of the precipitation in the United States is brought originally by prevailing winds from the Pacific Ocean, the Gulf of Mexico, the Atlantic Ocean, and the Great Lakes. Because these prevailing winds generally come from the West, the Pacific Coast receives more annual precipitation than the Atlantic Coast. Along the Pacific Coast itself, however, altitude causes some diversity in rain-

Line (15) fall. The mountain ranges of the United States, especially the Rocky Mountain Range and the Appalachian Mountain Range, influence the amount of precipitation in their areas. East of the Rocky Mountains, the annual precipitation decreases substantially from that west of the Rocky Mountains. The precipitation north of the Appalachian Mountains is about 40 percent

less than that south of the Appalachian Mountains.


What is the average annual rainfall in inches in the United States?

Thirty-six inches

Thirty-eight inches

Forty inches

Forty-two inches

5.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

Questions 1- 10

Precipitation, commonly referred to as rainfall, is a measure of the quantity of water in the form of either rain, hail, or snow which reaches the ground. The average annual precipi- tation over the whole of the United States is thirty-six inches. It should be understood however, that a foot of snow is not equal to a foot of precipitation. A general formula for

Line (5) computing the precipitation of snowfall is that ten inches of snow is equal to one inch of pre- cipitation. In New York State, for example, twenty inches of snow in one year would be recorded as only two inches of precipitation. Forty inches of rain would be recorded as forty inches of precipitation. The total annual precipitation would be recorded as forty-two inches. The amount of precipitation is a combined result of several factors, including location,

Line (10) altitude, proximity to the sea, and the direction of prevailing winds. Most of the precipitation in the United States is brought originally by prevailing winds from the Pacific Ocean, the Gulf of Mexico, the Atlantic Ocean, and the Great Lakes. Because these prevailing winds generally come from the West, the Pacific Coast receives more annual precipitation than the Atlantic Coast. Along the Pacific Coast itself, however, altitude causes some diversity in rain-

Line (15) fall. The mountain ranges of the United States, especially the Rocky Mountain Range and the Appalachian Mountain Range, influence the amount of precipitation in their areas. East of the Rocky Mountains, the annual precipitation decreases substantially from that west of the Rocky Mountains. The precipitation north of the Appalachian Mountains is about 40 percent

less than that south of the Appalachian Mountains.


If a state has 40 inches of snow in a year, by how much does this increase the annual precipitation?

By two feet

By four inches

By four feet

By 40 inches

6.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

Questions 1- 10

Precipitation, commonly referred to as rainfall, is a measure of the quantity of water in the form of either rain, hail, or snow which reaches the ground. The average annual precipi- tation over the whole of the United States is thirty-six inches. It should be understood however, that a foot of snow is not equal to a foot of precipitation. A general formula for

Line (5) computing the precipitation of snowfall is that ten inches of snow is equal to one inch of pre- cipitation. In New York State, for example, twenty inches of snow in one year would be recorded as only two inches of precipitation. Forty inches of rain would be recorded as forty inches of precipitation. The total annual precipitation would be recorded as forty-two inches. The amount of precipitation is a combined result of several factors, including location,

Line (10) altitude, proximity to the sea, and the direction of prevailing winds. Most of the precipitation in the United States is brought originally by prevailing winds from the Pacific Ocean, the Gulf of Mexico, the Atlantic Ocean, and the Great Lakes. Because these prevailing winds generally come from the West, the Pacific Coast receives more annual precipitation than the Atlantic Coast. Along the Pacific Coast itself, however, altitude causes some diversity in rain-

Line (15) fall. The mountain ranges of the United States, especially the Rocky Mountain Range and the Appalachian Mountain Range, influence the amount of precipitation in their areas. East of the Rocky Mountains, the annual precipitation decreases substantially from that west of the Rocky Mountains. The precipitation north of the Appalachian Mountains is about 40 percent

less than that south of the Appalachian Mountains.


The phrase "proximity to" in line 10 is closest in meaning to

communication with

dependence on

nearness to

similarity to

7.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

Questions 1- 10

Precipitation, commonly referred to as rainfall, is a measure of the quantity of water in the form of either rain, hail, or snow which reaches the ground. The average annual precipi- tation over the whole of the United States is thirty-six inches. It should be understood however, that a foot of snow is not equal to a foot of precipitation. A general formula for

Line (5) computing the precipitation of snowfall is that ten inches of snow is equal to one inch of pre- cipitation. In New York State, for example, twenty inches of snow in one year would be recorded as only two inches of precipitation. Forty inches of rain would be recorded as forty inches of precipitation. The total annual precipitation would be recorded as forty-two inches. The amount of precipitation is a combined result of several factors, including location,

Line (10) altitude, proximity to the sea, and the direction of prevailing winds. Most of the precipitation in the United States is brought originally by prevailing winds from the Pacific Ocean, the Gulf of Mexico, the Atlantic Ocean, and the Great Lakes. Because these prevailing winds generally come from the West, the Pacific Coast receives more annual precipitation than the Atlantic Coast. Along the Pacific Coast itself, however, altitude causes some diversity in rain-

Line (15) fall. The mountain ranges of the United States, especially the Rocky Mountain Range and the Appalachian Mountain Range, influence the amount of precipitation in their areas. East of the Rocky Mountains, the annual precipitation decreases substantially from that west of the Rocky Mountains. The precipitation north of the Appalachian Mountains is about 40 percent

less than that south of the Appalachian Mountains.


Where is the annual precipitation highest?

The Atlantic Coast

The Great Lakes

The Gulf of Mexico

The Pacific Coast

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