Unit 2: Earth Science Review

Unit 2 Exam Review!.pdf |
These are the core ideas that you should understand for your exam. If you thoroughly understand all of these concepts, you are in excellent shape for the exam.
Past Units
The following information learned in past units will be especially helpful to you in understanding this new material:
You should know how to:
You should understand:
You should know how to:
- Calculate density given mass and volume.
You should understand:
- The basic concept of density.
- Why objects sink or float.
- The concept of buoyant force and how it relates to sinking/floating.
- The concept of heat transfer.
- How density changes with temperature.
- How density changes with pressure.
Earth At A Glance
You should be able to:
- Calculate distance between two points on a scaled map based on the actual distance and the scaling factor.
- Identify cylindrical, cylindrical equal-area, oval, interrupted, and perspective maps based on their appearance.
- Identify political, physical, and topographical maps based on their appearance.
You should understand:
- The pros and cons of cylindrical, cylindrical equal-area, oval, interrupted, and perspective maps and globes
- Be able to recognize and define polar distortion
- The pros and cons of political, physical, and topographical maps.
Layers of the Earth
You should be able to
You should understand:
- Name the layers of the Earth in order of how they are arranged.
- Describe the composition of the layers (what they are made of).
You should understand:
- How/why the Earth has layers: differentiation/particle sorting (sinking of denser objects) and gravity (heavier objects being pulled toward the center)
- How/why temperature varies between the layers.
- How density changes between layers and why density follows this pattern.
- The unique properties of some the layers and the phenomena they give rise to:
- Movement of the mantle due to convection (cycling of hot/cold magma) and carbon dioxide escape causing movement of the plates above them
- Movement in the outer part of Earth’s iron core causing magnetic field
- Atmosphere: see atmosphere lesson
- Movement of the mantle due to convection (cycling of hot/cold magma) and carbon dioxide escape causing movement of the plates above them
Plate Tectonics
You should be able to:
You should understand:
- Identify convergent, divergent, and transform boundaries.
- Identify the events that occur at convergent, divergent, and transform boundaries
You should understand:
- Understand how and why those specific events occur at the boundaries where they do
- Understand why plates move, including why the mantle beneath them moves.
- Understand the principle of continental drift, including that it is still happening and that the continents were once one large supercontinent called Pangea
Rocks and Minerals
You should be able to:
You should understand:
- Classify rocks as sedimentary, metamorphic, igneous, or minerals (rather than rocks) based on their physical appearance.
You should understand:
- The difference between rocks and minerals.
- How sedimentary, metamorphic, and igneous rocks form.
- The general trend of density among sedimentary, metamorphic, and igneous rocks, as well as minerals (i.e., which of these is most dense? Least? Can we always know for sure based on the classification alone?).
- Why density follows this trend.
Particle Sorting
You should be able to:
You should understand:
- Predict how a particle will sort in still water, given a certain density or size (when the other is held constant/similar)
- Predict how a particle will sort in moving water (i.e., on a shoreline), given a certain density or size (when the other is held constant/similar)
You should understand:
- The patterns of particle sorting in still water (i.e., rocks sinking), moving water (i.e., a wave depositing rocks on the shore), and dry mixtures (i.e., sand seeping through cracks).
- How particle sorting in each of these scenarios is related to size/density, surface area, and density.
- The underlying principles of particle sorting in all of these scenarios: be able to explain why particles sort the way the do in a variety of circumstances, beyond just being able to identify the general trend of where they end up.
The Atmosphere
You should be able to:
You should understand:
- Name the layers of the atmosphere and in order of how they are arranged.
- Identify a unique property of or phenomenon present in each of the layers (e.g., where airplanes fly, where clouds form, etc.)
- Name the gases that make up the majority of the atmosphere and approximately what percentage of the atmosphere they comprise.
You should understand:
- How density varies through the atmosphere; be able to identify the general trend and explain why that trend is present.
- How/why temperature varies through the atmosphere in each of the layers.
- The general trend of how earth’s lifeforms have shaped the atmosphere from the early days of Earth (especially cyanobacteria and plants producing oxygen).
- How earth’s lifeforms allow the atmosphere to maintain a constant composition through the carbon and nitrogen cycles. You do not need to know the precise details of these cycles, beyond:
- Carbon cycle: plants use carbon dioxide and make oxygen, while animals use oxygen and make carbon dioxide.
- Nitrogen cycle: plants and animals make nitrogen waste products, which bacteria turn into atmospheric nitrogen.
- Carbon cycle: plants use carbon dioxide and make oxygen, while animals use oxygen and make carbon dioxide.
- The impact of climate change on the environment in the short and long term, including its effect on severe weather patterns.
- The causes of climate change and how these relate to the greenhouse effect.
- The basic principles of what causes a thunderstorm, a hurricane, and a tornado. You should have a sense of the extent of damage that each of these can cause.
- The consequences of pollution (smog, acid rain, and ozone depletion) for humans and/or other species.
- The role of ozone in the atmosphere.