Pretes TOEFL Reading Test

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

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

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

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

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

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

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

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 was NOT mentioned as a factor in determining the amount of precipitation that an area will receive?

• Mountains

• Latitude

• The sea

• Wind

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 word "substantially" in line 17 could best be replaced by

• fundamentally

• slightly

• completely

• apparently

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 word "that" in line 19 refers to

• decreases

• precipitation

• areas

• mountain ranges