51
Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

Embed Size (px)

Citation preview

Page 1: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

Chapter 24 Clickers

ConceptualIntegrated Science

Second Edition

© 2013 Pearson Education, Inc.

Earth'sSurface—Landand Water

Page 2: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

How much of the globe is covered by dry land rather than (liquid or solid) water?

a) 30%

b) 50%

c) 75%

d) 15%

Page 3: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

How much of the globe is covered by dry land rather than (liquid or solid) water?

a) 30%

b) 50%

c) 75%

d) 15%

Explanation:

About 75% of Earth is covered by ocean and 10% of the land surface is topped by ice. Exposed dry land is relatively scarce.

Page 4: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Which of the following is NOT one of the tectonic stresses experienced by Earth's crust?

a) Compression.

b) Tension.

c) Erosion.

d) Shear.

Page 5: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Which of the following is NOT one of the tectonic stresses experienced by Earth's crust?

a) Compression.

b) Tension.

c) Erosion.

d) Shear.

Explanation:

Erosion is a process that shapes Earth by acting at the planet's surface; erosion is NOT a result of plate tectonics. By contrast, the movement of tectonic plates DOES produce compressional, tensional, and shear stress.

Page 6: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

When rock deforms elastically,

a) it is permanently deformed after stress is removed.

b) it returns to its original size and shape after stress is removed.

c) it stretches irreversibly, even after stress is removed.

d) it fractures along planes of weakness when stress is applied.

Page 7: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

When rock deforms elastically,

a) it is permanently deformed after stress is removed.

b) it returns to its original size and shape after stress is removed.

c) it stretches irreversibly, even after stress is removed.

d) it fractures along planes of weakness when stress is applied.

Explanation:

Elastic means behavior like a rubber band—it returns to original size and shape after stressed and released.

Page 8: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

When rock deforms plastically,

a) it is permanently deformed after stress is removed.

b) it returns to its original size and shape after stress is removed.

c) it stretches irreversibly, even after stress is removed.

d) it fractures along planes of weakness when stress is applied.

Page 9: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

When rock deforms plastically,

a) it is permanently deformed after stress is removed.

b) it returns to its original size and shape after stress is removed.

c) it stretches irreversibly, even after stress is removed.

d) it fractures along planes of weakness when stress is applied.

Explanation:

Plastic means behavior like chewing gum—it stays deformed when stressed and released.

Page 10: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

When rock is stressed beyond its elastic limit,

a) minerals undergo retrograde metamorphism.

b) the rock loses heat.

c) a new elastic limit is established.

d) it deforms plastically or breaks.

Page 11: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

When rock is stressed beyond its elastic limit,

a) minerals undergo retrograde metamorphism.

b) the rock loses heat.

c) a new elastic limit is established.

d) it deforms plastically or breaks.

Explanation:

Folds and faults form when the elastic limit is surpassed. Cold rock is more brittle than warm rock, so warm rock deforms plastically to produce folds, and cold rock breaks to produce faults. Confining pressure also plays a role in determining elastic and plastic limits.

Page 12: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Rock in the center (or core) of a syncline is

a) younger than rock horizontally away from the center.

b) the same age as rock horizontally away from the center.

c) older than rock horizontally away from the center.

d) younger or older than rock horizontally away from the center.

Page 13: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Rock in the center (or core) of a syncline is

a) younger than rock horizontally away from the center.

b) the same age as rock horizontally away from the center.

c) older than rock horizontally away from the center.

d) younger or older than rock horizontally away from the center.

Explanation:

Think of a syncline as being shaped like a bowl. Sedimentary rocks are deposited horizontally with newer, younger rock on top of older rock. Flatten out the bowl by squishing and spreading it out. If the bowl was layered rock, can you see that younger rock forms the outside or "upper" part (deposited last)?

Page 14: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Rock in the center (or core) of an anticline is

a) younger than rock horizontally away from the center.

b) the same age as rock horizontally away from the center.

c) older than rock horizontally away from the center.

d) younger or older than rock horizontally away from the center.

Page 15: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Rock in the center (or core) of an anticline is

a) younger than rock horizontally away from the center.

b) the same age as rock horizontally away from the center.

c) older than rock horizontally away from the center.

d) younger or older than rock horizontally away from the center.

Explanation:

Think of an anticline as shaped like an "A" or an upside-down bowl. Sedimentary rocks are deposited horizontally with newer, younger rock on top of older rock. Flatten out the "A" by squishing and spreading it out. If the "A" was layered rock, can you see that younger rock forms the outside or "upper" part (deposited last)?

Page 16: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Normal faults are the result of

a) compression.

b) tension.

c) shear.

d) a combination of compression, tension, and shear.

Page 17: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Normal faults are the result of

a) compression.

b) tension.

c) shear.

d) a combination of compression, tension, and shear.

Explanation:

The production of normal faults is one way that Earth's crust stretches.

Page 18: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Reverse faults are the result of

a) compression.

b) tension.

c) shear.

d) a combination of compression, tension, and shear.

Page 19: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Reverse faults are the result of

a) compression.

b) tension.

c) shear.

d) a combination of compression, tension, and shear.

Explanation:

The production of reverse faults is one way that Earth's crust thickens.

Page 20: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

For a normal fault, the hanging wall moves

a) sideways.

b) obliquely.

c) up.

d) down.

Page 21: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

For a normal fault, the hanging wall moves

a) sideways.

b) obliquely.

c) up.

d) down.

Explanation:

A block of rock of a certain size will be lengthened horizontally if a fault forms and the hanging wall moves down. Normal faults are the result of tension.

Page 22: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

For a reverse fault, the hanging wall moves

a) sideways.

b) obliquely.

c) up.

d) down.

Page 23: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

For a reverse fault, the hanging wall moves

a) sideways.

b) obliquely.

c) up.

d) down.

Explanation:

A block of rock of a certain size will be shortened horizontally if a fault forms and the hanging wall moves up. Reverse faults are the result of compression.

Page 24: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Mountains are grouped into all the following classifications EXCEPT

a) normal-thrust mountains.

b) folded mountains.

c) upwarped mountains.

d) fault-block mountains.

Page 25: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Mountains are grouped into all the following classifications EXCEPT

a) normal-thrust mountains.

b) folded mountains.

c) upwarped mountains.

d) fault-block mountains.

Page 26: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Which of the following is NOT one of the three main types of volcanoes?

a) Composite cone.

b) Shield volcano.

c) Cinder cone.

d) Ash cone.

Page 27: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Which of the following is NOT one of the three main types of volcanoes?

a) Composite cone.

b) Shield volcano.

c) Cinder cone.

d) Ash cone.

Page 28: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Composite cones are formed by the eruption of

a) fluid basaltic lava.

b) alternating layers of lava, ash, and mud.

c) ash, cinders, glass, and lava fragments.

d) massive amounts of ash.

Page 29: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Composite cones are formed by the eruption of

a) fluid basaltic lava.

b) alternating layers of lava, ash, and mud.

c) ash, cinders, glass, and lava fragments.

d) massive amounts of ash.

Explanation:

A composite cone is so named because it consists of layers of differing consistency.

Page 30: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Plains and plateaus are both flat landforms. How do they differ from one another?

a) Elevation

b) Geologic history

c) Elevation and geologic history

d) Geographical location

Page 31: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Plains and plateaus are both flat landforms. How do they differ from one another?

a) Elevation

b) Geologic history

c) Elevation and geologic history

d) Geographical location

Explanation:

Plains are located at the bases of the mountain ranges that produce the sediment that composes them. Plateaus are pieces of crust that have been tectonically uplifted.

Page 32: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Where is most of Earth's fresh water found?

a) Lakes.

b) Ice caps and glaciers.

c) Rivers.

d) Underground.

Page 33: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Where is most of Earth's fresh water found?

a) Lakes.

b) Ice caps and glaciers.

c) Rivers.

d) Underground.

Explanation:

79% of Earth's fresh water is currently locked up in ice! Less than 21% has the potential for use by land-based life.

Page 34: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

What is the source of the energy that drives the hydrologic cycle?

a) The Sun, through the process of condensation.

b) The Sun, through the process of precipitation.

c) The Sun, through the process of warming.

d) The Sun, through the process of evaporation.

Page 35: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

What is the source of the energy that drives the hydrologic cycle?

a) The Sun, through the process of condensation.

b) The Sun, through the process of precipitation.

c) The Sun, through the process of warming.

d) The Sun, through the process of evaporation.

Explanation:

To drive the water cycle, billions of tons of water must of lifted into the sky. This involves breaking the hydrogen bonds between liquid water molecules as well as lifting them up. All this takes energy! The Sun supplies it. The energy pumped into the evaporated water is spent by the water when it falls back to Earth, as it moves across and reworks the land.

Page 36: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

The continental rise is

a) the elevated land next to a beach.

b) the sloping region between the continental shelf and deep ocean.

c) areas just barely above sea level.

d) the wedge of sediment at the base of the continental slope.

Page 37: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

The continental rise is

a) the elevated land next to a beach.

b) the sloping region between the continental shelf and deep ocean.

c) areas just barely above sea level.

d) the wedge of sediment at the base of the continental slope.

Explanation:

The continental rise is created by submarine "landslides" called turbidity currents.

Page 38: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

The Earth's longest topographical feature is the

a) Ocean trench system

b) Himalayan mountain range

c) Midocean Ridge

d) Mid-Atlantic Ridge

Page 39: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

The Earth's longest topographical feature is the

a) Ocean trench system

b) Himalayan mountain range

c) Midocean Ridge

d) Mid-Atlantic Ridge

Page 40: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

The compound that constitutes the majority of dissolved substances in ocean water is

a) sodium sulfate.

b) magnesium chloride.

c) sodium chloride.

d) sodium fluoride.

Page 41: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

The compound that constitutes the majority of dissolved substances in ocean water is

a) sodium sulfate.

b) magnesium chloride.

c) sodium chloride.

d) sodium fluoride.

Page 42: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Precipitation that does not infiltrate becomes

a) groundwater.

b) the water table.

c) soil moisture.

d) runoff.

Page 43: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

Precipitation that does not infiltrate becomes

a) groundwater.

b) the water table.

c) soil moisture.

d) runoff.

Explanation:

If water does not infiltrate, it stays on the surface and flows downslope.

Page 44: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

The maximum amount of water a particular soil can hold is determined by the

a) porosity.

b) permeability.

c) degree of saturation.

d) amount of recharge.

Page 45: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

The maximum amount of water a particular soil can hold is determined by the

a) porosity.

b) permeability.

c) degree of saturation.

d) amount of recharge.

Explanation:

Porosity is the percentage of open space in a soil. Water can only occupy open spaces—the higher the porosity, the larger the amount of water that can be held.

Page 46: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

The maximum amount of water that can flow through a particular soil is determined by the

a) porosity.

b) permeability.

c) degree of saturation.

d) amount of recharge.

Page 47: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

The maximum amount of water that can flow through a particular soil is determined by the

a) porosity.

b) permeability.

c) degree of saturation.

d) amount of recharge.

Page 48: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

The Antarctic Ice Sheet is

a) a continental glacier.

b) contains about 90% of the glacial ice on the planet.

c) nearly covers a continent.

d) All of the above

Page 49: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

The Antarctic Ice Sheet is

a) a continental glacier.

b) contains about 90% of the glacial ice on the planet.

c) nearly covers a continent.

d) All of the above

Page 50: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

An example of nonpoint water pollution is

a) heat from a nuclear power plant.

b) arsenic from a mine.

c) plastic bags in the ocean.

d) dead fish downstream from a factory.

Page 51: Chapter 24 Clickers Conceptual Integrated Science Second Edition © 2013 Pearson Education, Inc. Earth's Surface—Land and Water

© 2013 Pearson Education, Inc.

An example of nonpoint water pollution is

a) heat from a nuclear power plant.

b) arsenic from a mine.

c) plastic bags in the ocean.

d) dead fish downstream from a factory.

Explanation:

Plastic bags come from a multitude of sources. Pollution from distributed, hard-to-pinpoint sources is non-point pollution.