Title: Universe Eighth Edition
1UniverseEighth Edition
i?clicker Questions
- Chapter 11
- Mercury, Venus, and Mars Earthlike yet Unique
2At greatest eastern elongation (see diagram)
Mercury is visible
- just before sunrise.
- just after sunset.
- at midnight directly overhead.
- at midnight toward the south.
- at midnight in the west.
Q11.1
3At greatest eastern elongation (see diagram)
Mercury is visible
- just before sunrise.
- just after sunset.
- at midnight directly overhead.
- at midnight toward the south.
- at midnight in the west.
A11.1
4The structure of Mercury is
- a rocky mantle surrounding a large iron core that
is 75 of the planets diameter. - a rocky mantle surrounding a small iron core that
is much less than half the diameter of the
planet. - a frozen icy mantle surrounding a rocky core.
- a frozen icy mantle surrounding an iron core.
- a rocky core beneath an iron shell.
Q11.2
5The structure of Mercury is
- a rocky mantle surrounding a large iron core that
is 75 of the planets diameter. - a rocky mantle surrounding a small iron core that
is much less than half the diameter of the
planet. - a frozen icy mantle surrounding a rocky core.
- a frozen icy mantle surrounding an iron core.
- a rocky core beneath an iron shell.
A11.2
6The rotation of Mercury on its axis is unusual in
that
- it has the slowest rotation of all the planets.
- it rotates extremely rapidly.
- it rotates retrograde.
- it rotates three times on its axis in the time it
takes to make two orbits around the Sun. - it rotates two times on its axis in the time it
takes to make three orbits around the Sun.
Q11.3
7The rotation of Mercury on its axis is unusual in
that
- it has the slowest rotation of all the planets.
- it rotates extremely rapidly.
- it rotates retrograde.
- it rotates three times on its axis in the time it
takes to make two orbits around the Sun. - it rotates two times on its axis in the time it
takes to make three orbits around the Sun.
A11.3
8Why is the surface of Mercury cooler than the
surface of Venus?
- Mercury moves too rapidly around the Sun to be
heated up significantly. - Mercury, unlike Venus, does not have an
atmosphere and there is no greenhouse effect. - Mercury is a very reflective body, so most of the
electromagnetic radiation incident on it is not
absorbed. - Mercury is much smaller than Venus.
- Mercurys magnetic field deflects some solar
radiation.
Q11.4
9Why is the surface of Mercury cooler than the
surface of Venus?
- Mercury moves too rapidly around the Sun to be
heated up significantly. - Mercury, unlike Venus, does not have an
atmosphere and there is no greenhouse effect. - Mercury is a very reflective body, so most of the
electromagnetic radiation incident on it is not
absorbed. - Mercury is much smaller than Venus.
- Mercurys magnetic field deflects some solar
radiation.
A11.4
10The Moon and Mercury are similar in that they
both
- are about the same size and are heavily cratered.
- are heavily cratered and lack an atmosphere.
- lack an atmosphere and have large flat maria.
- have a weak magnetic field and a tenuous
atmosphere. - have a weak magnetic field and numerous mountains.
Q11.5
11The Moon and Mercury are similar in that they
both
- are about the same size and are heavily cratered.
- are heavily cratered and lack an atmosphere.
- lack an atmosphere and have large flat maria.
- have a weak magnetic field and a tenuous
atmosphere. - have a weak magnetic field and numerous mountains.
A11.5
12Venus has a high surface temperature because
- of continual volcanic eruptions.
- radioactive elements heat its surface.
- of heating from the solar wind.
- the dense carbon dioxide atmosphere produces a
very strong greenhouse effect. - the dense nitrogen atmosphere produces a very
strong greenhouse effect.
Q11.6
13Venus has a high surface temperature because
- of continual volcanic eruptions.
- radioactive elements heat its surface.
- of heating from the solar wind.
- the dense carbon dioxide atmosphere produces a
very strong greenhouse effect. - the dense nitrogen atmosphere produces a very
strong greenhouse effect.
A11.6
14The surface of Venus
- exhibits plate tectonic activity similar to that
seen on Earth. - exhibits a crust that has not broken up into
moving plates but does exhibit hotspot volcanism.
- is relatively smooth and featureless.
- exhibits no tectonic activity as far as we can
tell. - has not yet been studied due to the dense cloud
cover, so we do not know if there is any tectonic
activity.
Q11.7
15The surface of Venus
- exhibits plate tectonic activity similar to that
seen on Earth. - exhibits a crust that has not broken up into
moving plates but does exhibit hotspot volcanism.
- is relatively smooth and featureless.
- exhibits no tectonic activity as far as we can
tell. - has not yet been studied due to the dense cloud
cover, so we do not know if there is any tectonic
activity.
A11.7
16How did Venus acquire its dense carbon dioxide
atmosphere?
- It captured carbon dioxide from space.
- Oxygen reacted with carbon on the surface to
produce carbon dioxide after Venus formed and
cooled. - Volcanic eruptions supplied carbon dioxide.
- It captured asteroids, which contain carbon
dioxide. - Solar radiation caused chemical reactions in the
surface rocks.
Q11.8
17How did Venus acquire its dense carbon dioxide
atmosphere?
- It captured carbon dioxide from space.
- Oxygen reacted with carbon on the surface to
produce carbon dioxide after Venus formed and
cooled. - Volcanic eruptions supplied carbon dioxide.
- It captured asteroids, which contain carbon
dioxide. - Solar radiation caused chemical reactions in the
surface rocks.
A11.8
18Venus and Earth differ significantly in several
ways. Earth has broken cloud cover and an
atmosphere consisting mostly of nitrogen, whereas
Venus has
- unbroken cloud cover with a much denser carbon
dioxide atmosphere. - broken cloud cover with a much denser carbon
dioxide atmosphere. - unbroken cloud cover with a much denser nitrogen
atmosphere. - broken cloud cover with a much denser nitrogen
atmosphere. - unbroken cloud cover with little atmospheric
nitrogen and a great deal of oxygen.
Q11.9
19Venus and Earth differ significantly in several
ways. Earth has broken cloud cover and an
atmosphere consisting mostly of nitrogen, whereas
Venus has
- unbroken cloud cover with a much denser carbon
dioxide atmosphere. - broken cloud cover with a much denser carbon
dioxide atmosphere. - unbroken cloud cover with a much denser nitrogen
atmosphere. - broken cloud cover with a much denser nitrogen
atmosphere. - unbroken cloud cover with little atmospheric
nitrogen and a great deal of oxygen.
A11.9
20Venus and Earth have similar
- mass, density, and magnetic field.
- mass and density.
- rotation rate, density, and atmosphere.
- magnetic field, surface temperature, and
atmosphere. - mass, density, and surface temperature.
Q11.10
21Venus and Earth have similar
- mass, density, and magnetic field.
- mass and density.
- rotation rate, density, and atmosphere.
- magnetic field, surface temperature, and
atmosphere. - mass, density, and surface temperature.
A11.10
22Why do volcanoes on Venus tend to be fewer and
larger than those on Earth?
- Venus has a much more tectonically active surface
than the Earth. - Erosion quickly reduces the size of any volcanoes
on the Earth. - Lava is much hotter on Venus than on Earth.
- Volcanoes on Venus grow in one spot only because
the crustal plates do not move, whereas on Earth
the movement of the crustal plates forms a chain
of volcanoes. - Venus is closer to the sun.
Q11.11
23Why do volcanoes on Venus tend to be fewer and
larger than those on Earth?
- Venus has a much more tectonically active surface
than the Earth. - Erosion quickly reduces the size of any volcanoes
on the Earth. - Lava is much hotter on Venus than on Earth.
- Volcanoes on Venus grow in one spot only because
the crustal plates do not move, whereas on Earth
the movement of the crustal plates forms a chain
of volcanoes. - Venus is closer to the sun.
A11.11
24Compared to Earth, Venus has a very weak magnetic
field. The most likely reason for this is that
- there is no liquid in the core.
- the intense solar radiation destroys the magnetic
field before it can form. - Venus rotates so slowly that no electric currents
are set up in its core. - the magnetic field is in the process of
reversing. - Venus is closer to the Sun.
Q11.12
25Compared to Earth, Venus has a very weak magnetic
field. The most likely reason for this is that
- there is no liquid in the core.
- the intense solar radiation destroys the magnetic
field before it can form. - Venus rotates so slowly that no electric currents
are set up in its core. - the magnetic field is in the process of
reversing. - Venus is closer to the Sun.
A11.12
26Which of the following have not been found on
Mars?
- Moving tectonic plates
- Wispy clouds
- Dust storms
- Ancient river beds
- Advancing and receding polar icecaps
Q11.13
27Which of the following have not been found on
Mars?
- Moving tectonic plates
- Wispy clouds
- Dust storms
- Ancient river beds
- Advancing and receding polar icecaps
A11.13
28About 4 billion years ago Martian volcanoes were
active. How did these active volcanoes affect
the atmosphere of Mars?
- They supplied large amounts of oxygen to the
atmosphere. - They supplied large amounts of carbon dioxide, a
greenhouse gas, to the atmosphere. - Their heat kept the surface of Mars warm so that
water could exist in vapor form. - They supplied large amounts of nitrogen, a
greenhouse gas, to the atmosphere. - They supplied large amounts of methane, a
greenhouse gas, to the atmosphere.
Q11.14
29About 4 billion years ago Martian volcanoes were
active. How did these active volcanoes affect
the atmosphere of Mars?
- They supplied large amounts of oxygen to the
atmosphere. - They supplied large amounts of carbon dioxide, a
greenhouse gas, to the atmosphere. - Their heat kept the surface of Mars warm so that
water could exist in vapor form. - They supplied large amounts of nitrogen, a
greenhouse gas, to the atmosphere. - They supplied large amounts of methane, a
greenhouse gas, to the atmosphere.
A11.14
30We now know that water exists on Mars. This
water is in the form of
- liquid in rivers only.
- atmospheric water vapor only.
- underground reservoirs of liquid water.
- ice in polar icecaps only.
- permafrost, polar icecaps, and a small amount of
atmospheric vapor.
Q11.15
31We now know that water exists on Mars. This
water is in the form of
- liquid in rivers only.
- atmospheric water vapor only.
- underground reservoirs of liquid water.
- ice in polar icecaps only.
- permafrost, polar icecaps, and a small amount of
atmospheric vapor.
A11.15
32The Mars Pathfinder mission carried a robotic
vehicle, Sojourner, to Mars. Sojourner discovered
rocks that appeared to be layered like
sedimentary rock. This is evidence that
- standing water once existed on Mars.
- flowing water was once present on Mars.
- atmospheric winds operating for millions of years
deposited many layers of rock. - volcanoes caused the layering.
- meteors brought sedimentary rocks to Mars.
Q11.16
33The Mars Pathfinder mission carried a robotic
vehicle, Sojourner, to Mars. Sojourner discovered
rocks that appeared to be layered like
sedimentary rock. This is evidence that
- standing water once existed on Mars.
- flowing water was once present on Mars.
- atmospheric winds operating for millions of years
deposited many layers of rock. - volcanoes caused the layering.
- meteors brought sedimentary rocks to Mars.
A11.16
34On Mars the greenhouse effect is weaker than it
is on Earth and far weaker than it is on Venus.
Which of the following explains this?
- The Martian atmosphere contains large amounts of
nitrogen, which is not a greenhouse gas. - Mars is too far from the Sun for the greenhouse
effect to be important. - The Martian atmosphere is very thin and traps
less infrared radiation from the surface. - There is no plant life on Mars.
- Mars once had water.
Q11.17
35On Mars the greenhouse effect is weaker than it
is on Earth and far weaker than it is on Venus.
Which of the following explains this?
- The Martian atmosphere contains large amounts of
nitrogen, which is not a greenhouse gas. - Mars is too far from the Sun for the greenhouse
effect to be important. - The Martian atmosphere is very thin and traps
less infrared radiation from the surface. - There is no plant life on Mars.
- Mars once had water.
A11.17
36The moons of Mars, shown in this photo, are
similar to what other objects in our solar system?
- Comets
- Asteroids
- The Earths Moon
- Small planets like Mercury
- Large planets like Uranus
Q11.18
37The moons of Mars, shown in this photo, are
similar to what other objects in our solar system?
- Comets
- Asteroids
- The Earths Moon
- Small planets like Mercury
- Large planets like Uranus
A11.18