The Most Famous: Old Faithful
Probably the world’s most famous geyser is Old Faithful, located in the Upper Geyser Basin in Yellowstone National Park in Wyoming. There are over 300 geysers in the Basin, the largest concentration of geysers in the world, and over 700 in Yellowstone Park. Before the earthquake of 1959, Old Faithful’s eruptions came almost like clockwork, every 60 to 65 minutes. Since that earthquake, eruptions have been as few as 30 minutes apart or as long as 120 minutes apart.
An eruption of Old Faithful is a spectacular sight, one which has been drawing tourists to Yellowstone since the 1870s. The geyser usually gives a warning: a short burst of steam. Then a graceful jet of steam and boiling water rises up to 60 meters in the air, unfurling in the sunlight with the colors of the rainbow playing across it. Each eruption lasts from one and a half to five minutes. When it erupts, it sprays up to 32,000 liters of water in the air.
The eruption is only the visible part of the spectacle. In order for a geyser to erupt, there are four necessary conditions that must exist. First, there must be an abundant supply of water. Old Faithful is supplied with water from groundwater and rainfall, but other geysers in Yellowstone are partly supplied from creeks and rivers.
Second, there must be a heat source. All geyser fields are located over recently active volcanic areas. In the Upper Geyser Basin, a steady supply of heat is provided by hotspots of molten lava as little as 5 kilometers below the surface. When water trickles down to the hotspots, it heats up.
However, the water would never be ejected from the geysers with such tremendous force if it were not for geyserite, a material that is mainly composed of the mineral silicon dioxide. The presence of geyserite is the third necessary condition. Geyserite is dissolved from the rocks and deposited on the walls of the geyser’s plumbing system and around the surface of the geyser. These deposits make the plumbing system pressure-tight. This allows the water to be carried all the way to the surface rather than leaking out into the loose rock, sand, and soil that surrounds the plumbing system.
The final condition is a special underground plumbing system. Geysers have various types of plumbing systems, but all have a narrow spot, a constriction point near the surface. The water in this narrow spot acts like a valve or a lid that allows pressure to build up in the water below, causing the eruption. A geological feature that has water, geyserite, and heat but no special plumbing will be a hot spring, not a geyser. Geologists studying Old Faithful theorized that it had a relatively simple plumbing system composed of an underground reservoir connected to the surface by a long, narrow tube that grows even narrower near the surface. In 1992, a probe equipped with a video camera and heat sensors was lowered into the geyser and confirmed the existence of a constriction, a narrow shaft, and a cavern about the size of a large automobile 15 meters beneath the surface.
As water fills Old Faithful’s plumbing system, it is heated in the reservoir like water in a teakettle. But while water in a kettle rises because of convection, the water in the tube and the constriction above prevents free circulation. Therefore, the water in the upper tube is cooler than the water at the bottom. The weight of the water puts pressure on the water below, raising the boiling point of the water in the reservoir. Eventually, enough pressure builds to push water past the constriction point and out of the mouth of the geyser. The pressure drops as the water is released, and a sudden, violent boiling takes place through the length of the tube. A tremendous amount of steam is produced, and the water roars out of the geyser in a superheated mass. This is the eruption, and it continues until the reservoir is emptied or the steam runs out.
There are two main types of geyser. A columnar geyser (also called a cone geyser) such as Old Faithful shoots a fairly narrow jet of water from a formation of geyserite that looks like a miniature volcano. A fountain geyser has an open pool at the surface that fills with water before or during the eruption. When a fountain geyser erupts, water sprays in all directions but does not reach the height of the jet from a columnar geyser.
Choose the correct letter A, B, C, or D.
Write the correct letter in the appropriate box on your answer sheet.
1. According to the introduction, the earthquake of 1959 made Old Faithful erupt…
2. Old Faithful would not erupt at all if…
3. What is true of the material geyserite?
4. According to fourth paragraph, compared to Old Faithful, many other geysers
5. Old Faithful does NOT have
The Most Famous: Old Faithful
Probably the world’s most famous geyser is Old Faithful, located in the Upper Geyser Basin in Yellowstone National Park in Wyoming. There are over 300 geysers in the Basin, the largest concentration of geysers in the world, and over 700 in Yellowstone Park. Before the earthquake of 1959, Old Faithful’s eruptions came almost like clockwork, every 60 to 65 minutes. Since that earthquake, eruptions have been as few as 30 minutes apart or as long as 120 minutes apart.
An eruption of Old Faithful is a spectacular sight, one which has been drawing tourists to Yellowstone since the 1870s. The geyser usually gives a warning: a short burst of steam. Then a graceful jet of steam and boiling water rises up to 60 meters in the air, unfurling in the sunlight with the colors of the rainbow playing across it. Each eruption lasts from one and a half to five minutes. When it erupts, it sprays up to 32,000 liters of water in the air.
The eruption is only the visible part of the spectacle. In order for a geyser to erupt, there are four necessary conditions that must exist. First, there must be an abundant supply of water. Old Faithful is supplied with water from groundwater and rainfall, but other geysers in Yellowstone are partly supplied from creeks and rivers.
Second, there must be a heat source. All geyser fields are located over recently active volcanic areas. In the Upper Geyser Basin, a steady supply of heat is provided by hotspots of molten lava as little as 5 kilometers below the surface. When water trickles down to the hotspots, it heats up.
However, the water would never be ejected from the geysers with such tremendous force if it were not for geyserite, a material that is mainly composed of the mineral silicon dioxide. The presence of geyserite is the third necessary condition. Geyserite is dissolved from the rocks and deposited on the walls of the geyser’s plumbing system and around the surface of the geyser. These deposits make the plumbing system pressure-tight. This allows the water to be carried all the way to the surface rather than leaking out into the loose rock, sand, and soil that surrounds the plumbing system.
The final condition is a special underground plumbing system. Geysers have various types of plumbing systems, but all have a narrow spot, a constriction point near the surface. The water in this narrow spot acts like a valve or a lid that allows pressure to build up in the water below, causing the eruption. A geological feature that has water, geyserite, and heat but no special plumbing will be a hot spring, not a geyser. Geologists studying Old Faithful theorized that it had a relatively simple plumbing system composed of an underground reservoir connected to the surface by a long, narrow tube that grows even narrower near the surface. In 1992, a probe equipped with a video camera and heat sensors was lowered into the geyser and confirmed the existence of a constriction, a narrow shaft, and a cavern about the size of a large automobile 15 meters beneath the surface.
As water fills Old Faithful’s plumbing system, it is heated in the reservoir like water in a teakettle. But while water in a kettle rises because of convection, the water in the tube and the constriction above prevents free circulation. Therefore, the water in the upper tube is cooler than the water at the bottom. The weight of the water puts pressure on the water below, raising the boiling point of the water in the reservoir. Eventually, enough pressure builds to push water past the constriction point and out of the mouth of the geyser. The pressure drops as the water is released, and a sudden, violent boiling takes place through the length of the tube. A tremendous amount of steam is produced, and the water roars out of the geyser in a superheated mass. This is the eruption, and it continues until the reservoir is emptied or the steam runs out.
There are two main types of geyser. A columnar geyser (also called a cone geyser) such as Old Faithful shoots a fairly narrow jet of water from a formation of geyserite that looks like a miniature volcano. A fountain geyser has an open pool at the surface that fills with water before or during the eruption. When a fountain geyser erupts, water sprays in all directions but does not reach the height of the jet from a columnar geyser.
Do the following statements agree with the information given in Reading Passage 1?
In boxes 6–9 on your answer sheet, write
TRUEif the statement agrees with the information
FALSEif the statement contradicts the information
NOT GIVENif there is no information on the given statement
6. The first eruption of Old Faithful occurred in the 1870s.
7. The duration of an eruption has been reduced from one and a half hours to five minutes since the nineteenth century.
8. One of the necessary factors in the formation of hot springs and geysers is geyserite.
9. The jet from a columnar geyser reaches higher than that from a fountain geyser.
The Most Famous: Old Faithful
Probably the world’s most famous geyser is Old Faithful, located in the Upper Geyser Basin in Yellowstone National Park in Wyoming. There are over 300 geysers in the Basin, the largest concentration of geysers in the world, and over 700 in Yellowstone Park. Before the earthquake of 1959, Old Faithful’s eruptions came almost like clockwork, every 60 to 65 minutes. Since that earthquake, eruptions have been as few as 30 minutes apart or as long as 120 minutes apart.
An eruption of Old Faithful is a spectacular sight, one which has been drawing tourists to Yellowstone since the 1870s. The geyser usually gives a warning: a short burst of steam. Then a graceful jet of steam and boiling water rises up to 60 meters in the air, unfurling in the sunlight with the colors of the rainbow playing across it. Each eruption lasts from one and a half to five minutes. When it erupts, it sprays up to 32,000 liters of water in the air.
The eruption is only the visible part of the spectacle. In order for a geyser to erupt, there are four necessary conditions that must exist. First, there must be an abundant supply of water. Old Faithful is supplied with water from groundwater and rainfall, but other geysers in Yellowstone are partly supplied from creeks and rivers.
Second, there must be a heat source. All geyser fields are located over recently active volcanic areas. In the Upper Geyser Basin, a steady supply of heat is provided by hotspots of molten lava as little as 5 kilometers below the surface. When water trickles down to the hotspots, it heats up.
However, the water would never be ejected from the geysers with such tremendous force if it were not for geyserite, a material that is mainly composed of the mineral silicon dioxide. The presence of geyserite is the third necessary condition. Geyserite is dissolved from the rocks and deposited on the walls of the geyser’s plumbing system and around the surface of the geyser. These deposits make the plumbing system pressure-tight. This allows the water to be carried all the way to the surface rather than leaking out into the loose rock, sand, and soil that surrounds the plumbing system.
The final condition is a special underground plumbing system. Geysers have various types of plumbing systems, but all have a narrow spot, a constriction point near the surface. The water in this narrow spot acts like a valve or a lid that allows pressure to build up in the water below, causing the eruption. A geological feature that has water, geyserite, and heat but no special plumbing will be a hot spring, not a geyser. Geologists studying Old Faithful theorized that it had a relatively simple plumbing system composed of an underground reservoir connected to the surface by a long, narrow tube that grows even narrower near the surface. In 1992, a probe equipped with a video camera and heat sensors was lowered into the geyser and confirmed the existence of a constriction, a narrow shaft, and a cavern about the size of a large automobile 15 meters beneath the surface.
As water fills Old Faithful’s plumbing system, it is heated in the reservoir like water in a teakettle. But while water in a kettle rises because of convection, the water in the tube and the constriction above prevents free circulation. Therefore, the water in the upper tube is cooler than the water at the bottom. The weight of the water puts pressure on the water below, raising the boiling point of the water in the reservoir. Eventually, enough pressure builds to push water past the constriction point and out of the mouth of the geyser. The pressure drops as the water is released, and a sudden, violent boiling takes place through the length of the tube. A tremendous amount of steam is produced, and the water roars out of the geyser in a superheated mass. This is the eruption, and it continues until the reservoir is emptied or the steam runs out.
There are two main types of geyser. A columnar geyser (also called a cone geyser) such as Old Faithful shoots a fairly narrow jet of water from a formation of geyserite that looks like a miniature volcano. A fountain geyser has an open pool at the surface that fills with water before or during the eruption. When a fountain geyser erupts, water sprays in all directions but does not reach the height of the jet from a columnar geyser.
Complete the sentences below.
Choose NO MORE THAN TWO WORDS from the text for each answer.
10. The water of Old Faithful is provided from () unlike other geysers in Yellowstone.
11. Geyserite that has accumulated around the surface of the geyser makes the () pressure-tight.
12. In order to confirm their theory about Old Faithful, the geologists submerged the () into the geyser.
13. Old Faithful is a type of (), which shoots a very narrow jet of water.
Toward Immortality: The Social Burden of Longer Lives
Reading Passage 2 has eleven paragraphs, A–K.
Choose the correct heading for paragraphs A, B, E, F, I, and K from the list of headings below.
Drag and drop the correct number i–viii in boxes 14–19 on the answer sheet.
Toward Immortality: The Social Burden of Longer Lives
Complete the chart below.
Write NO MORE THAN TWO WORDS for each answer.
Effects of the Doubled Lifespan |
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Toward Immortality: The Social Burden of Longer Lives
Match the statement with Gregory Stock (S), Daniel Callahan (C), Richard Kalish (K), or Chris Hackler (H).
24. Life extension will make multiple marriages the norm.
25. Longer life will not contribute to solving the problem of war and poverty.
26. A large age difference between siblings will create different social relationships.
27. Life extension will increase economic productivity.
The Importance of the Social Environment
Reading Passage 3 has eight paragraphs, A–H.
Choose the correct heading for paragraphs A~H from the list of headings below.
Write the correct number i–viii in boxes 28~35 on the answer sheet.
The Importance of the Social Environment
Determine whether the following statements agree with the claims of the writer in Reading Passage 3.
In boxes 36–40 on your answer sheet, write
YESif the statement agrees with the information
NOif the statement contradicts the information
NOT GIVENif there is no information on the given statement
36. People agree with the opinion that we inherit temperamental traits, including a tendency to behave in a certain way.
37. Temperamental traits are changed by the environment where you are brought up.
38. The “wild boy” found in 1797 is an example to prove the importance of social learning in improving potential ability.
39. Children deprived of any human contact will eventually die because good care is essential for their survival.
40. Specialized socialization plays an important role in determining what we achieve in life.