Standards - Science

SC15.5.3

Examine matter through observations and measurements to identify materials (e.g., powders, metals, minerals, liquids) based on their properties (e.g., color, hardness, reflectivity, electrical conductivity, thermal conductivity, response to magnetic forces, solubility, density).

Unpacked Content

Scientific and Engineering Practices

Planning and Carrying out Investigations

Crosscutting Concepts

Scale, Proportion, and Quantity

Knowledge

Students know:
  • Materials have different properties-color, hardness, reflectivity, electrical conductivity thermal conductivity, solubility, and density.
  • Measurements of a variety of properties can be used to identify materials.
  • Measurements should be made in standard units (e.g., grams & liters).

Skills

Students are able to:
  • Identify the phenomenon through observations about materials, including color, hardness, reflectivity, electrical conductivity, thermal conductivity, response to magnetic forces, and solubility.
  • Identify the evidence and collect data about the observed objects in standard units (e.g., grams, liters).
  • Collaboratively plan the investigation.
  • Identify materials based on their properties.

Understanding

Students understand that:
  • Standard units are used to measure and describe physical quantities of materials such as weight, time, temperature, and volume. These measurements will assist in the identification of the materials ( e.g. powders, metals, minerals, and liquids).

Vocabulary

  • color
  • hardness
  • reflectivity
  • electrical conductivity
  • thermal conductivity
  • response to magnetic forces
  • solubility
  • density
  • measurement (quantitative and qualitative)
  • data
  • observable properties
  • standard units
  • conductors
  • nonconductors
  • magnetic
  • nonmagnetic

SC15.5.4

Investigate whether the mixing of two or more substances results in new substances (e.g., mixing of baking soda and vinegar resulting in the formation of a new substance, gas; mixing of sand and water resulting in no new substance being formed).

Unpacked Content

Scientific and Engineering Practices

Planning and Carrying out Investigations

Crosscutting Concepts

Cause and Effect

Knowledge

Students know:
  • When two or more different substances are mixed, a new substance with different properties may be formed.

Skills

Students are able to:
  • From a given investigation plan, describe the phenomenon under investigation, including the mixing of two or more substances.
  • Identify the purpose of the investigation.
  • Describe the evidence from data that will be collected, including quantitative and qualitative properties of the substances to be mixed and the resulting substances.
  • Collaboratively plan an investigation and describe the data to be collected, including: how quantitative and qualitative properties of the two or more substances to be mixed will be determined and measured, number of trials for the investigation, how variables will be controlled to ensure a fair test.
  • Collect necessary data.

Understanding

Students understand that:
  • Cause and effect relationships are identified and used to explain changes like those that occur when two or more substances are mixed together.

Vocabulary

  • variables
  • states of matter
  • properties of matter
  • chemical change
  • physical change
  • evidence
  • temperature

SC15.5.5

Construct explanations from observations to determine how the density of an object affects whether the object sinks or floats when placed in a liquid.

Unpacked Content

Scientific and Engineering Practices

Constructing Explanations and Designing Solutions

Crosscutting Concepts

Cause and Effect

Knowledge

Students know:
  • Objects are made of many tiny particles to small to be seen.
  • Some objects have many tiny particles compacted close together that causes the object to sink while other objects the same size may float because their tiny particles are less compact.
  • Some objects of the same size sink when others float.
  • Buoyancy is the ability of an object to float.

Skills

Students are able to:
  • Predict the results of different types of objects being placed in water. Test the objects and communicate the results.
  • Use appropriate tools (Scale, balance, ruler, or graduated cylinder) to measure the weight, mass, and/volume of an object.
  • Construct an explanation to describe the observed relationship between density and the ability of an object to sink or float.
  • Identify the evidence that supports the explanation that density affects the ability of an object to sink or float.

Understanding

Students understand that:
  • Cause and effect relationships are routinely identified and used to explain phenomenon like sinking and floating.

Vocabulary

  • density
  • volume
  • buoyancy
  • data
  • observe
  • explain
  • sink
  • float
  • mass

SC15.5.6

Construct an explanation from evidence to illustrate that the gravitational force exerted by Earth on objects is directed downward towards the center of Earth.

Unpacked Content

Scientific and Engineering Practices

Constructing Explanations and Designing Solutions

Crosscutting Concepts

Cause and Effect

Knowledge

Students know:
  • The Earth's shape is spherical.
  • That objects dropped appear to fall straight down.
  • That people live all around the spherical Earth, and they all observe that objects appear to fall straight down.

Skills

Students are able to:
  • Construct an explanation of observed relationships.
  • Use evidence to illustrate the relationship between gravity and objects on Earth.

Understanding

Students understand that:
  • If Earth is spherical, and all observers see objects near them falling directly "down" to the Earth's surface, then all observers would agree that objects fall toward the Earth's center.
  • Since an object that is initially stationary when held moves downward when it is released, there must be a force (gravity) acting on the object that pulls the object toward the center of the Earth.

Vocabulary

  • construct
  • explanation
  • gravitational force
  • evidence
  • illustrate
  • spherical

SC15.5.7

Design and conduct a test to modify the speed of a falling object due to gravity (e.g., constructing a parachute to keep an attached object from breaking).*

Unpacked Content

Scientific and Engineering Practices

Constructing Explanations and Designing Solutions

Crosscutting Concepts

Cause and Effect

Knowledge

Students know:
  • The gravitational force exerted by Earth on objects is directed downward towards the center of Earth.
  • How an engineering design process is used to design and conduct a test.
  • The properties (surface area, substance, weight) of different materials used to modify the speed of a falling object will affect the fall.

Skills

Students are able to:
  • Apply scientific ideas to solve design problems.
  • Generate and compare multiple solutions to a problem based on how well they meet the criteria and constraints of the design solution.

Understanding

Students understand that:
  • A device added to a falling object can cause the speed to be modified.

Vocabulary

  • gravity
  • design
  • conduct
  • gravitational force

SC15.5.8

Defend the position that plants obtain materials needed for growth primarily from air and water.

Unpacked Content

Scientific and Engineering Practices

Engaging in Argument from Evidence

Crosscutting Concepts

Energy and Matter

Knowledge

Students know:
  • How plants obtain nutrients.
  • How to measure growth of a plant.

Skills

Students are able to:
  • Collect and analyze evidence about plant growth.
  • Determine whether evidence supports the claim that plants do not acquire most of the material for growth from soil.
  • Use reasoning to connect the evidence to support the claim. A chain of reasoning should include the following:
    • During plant growth in soil, the weight of the soil changes very little over time, but the weight of the plant changes a lot. Additionally, some plants grow without soil at all.
    • Because some plants don't need soil to grow, and others show increases in plant matter but not accompanying decreases in soil matter, the material from the soil must not enter the plant in sufficient quantities to be the chief contributor to plant growth.
    • Therefore, plants do not acquire most of the material fro growth from soil.
    • A plant cannot grow without water or air. Because both air and water are matter and are transported into the plant system, they can provide the materials plants need for growth.
    • Since soil cannot account for the change in weight as a plant grows and since plants take in water and air, both of which could contribute to the increase in weight during plant growth, plant growth must come chiefly from water and air.

Understanding

Students understand that:
  • Matter, including air and water, is transported into, out of, and within plant systems.

Vocabulary

  • claim
  • evidence
  • hydroponic

SC15.5.9

Construct an illustration to explain how plants use light energy to convert carbon dioxide and water into a storable fuel, carbohydrates, and a waste product, oxygen, during the process of photosynthesis.

Unpacked Content

Scientific and Engineering Practices

Constructing Explanations and Designing Solutions

Crosscutting Concepts

Energy and Matter

Knowledge

Students know:
  • What plants need to survive.
  • Parts of plants and their functions in the process of photosynthesis.
  • The sun is the source of energy.
  • Plants are producers.

Skills

Students are able to:
  • Construct an illustration to explain the scientific phenomenon of photosynthesis.

Understanding

Students understand that:
  • Plants are producers of energy through the process of photosynthesis.

Vocabulary

  • convert
  • carbohydrates
  • waste product
  • photosynthesis
  • carbon dioxide
  • produces
  • oxygen

SC15.5.10

Construct and interpret models (e.g., diagrams, flow charts) to explain that energy in animals’ food is used for body repair, growth, motion, and maintenance of body warmth and was once energy from the sun.

Unpacked Content

Scientific and Engineering Practices

Developing and Using Models

Crosscutting Concepts

Energy and Matter

Knowledge

Students know:
  • The energy released [from] food was once energy from the sun that was captured by plants in the chemical process that forms plant matter (from air and water).
  • Food provides animals with the materials they need for body repair and growth and the energy they need to maintain body warmth and for motion.

Skills

Students are able to:
  • Use models to describe a phenomenon that includes the idea that energy in animals' food was once energy from the sun. Students identify and describe the components of the model that are relevant for describing the phenomenon, including the following:
    • Energy.
    • The sun.
    • Animals, including their bodily functions (e.g., body repair, growth, motion, body warmth maintenance).
    • Plants.
  • Identify and describe the relevant relationships between components, including the following:
    • The relationship between plants and the energy they get from sunlight to produce food.
    • The relationship between food and the energy and materials that animals require for bodily functions (e.g., body repair, growth, motion, body warmth maintenance).
    • The relationship between animals and the food they eat, which is either other animals or plants (or both), to obtain energy for bodily functions and materials for growth and repair.
  • Use the models to describe causal accounts of the relationships between energy from the sun and animals' needs for energy, including that:
    • Since all food can eventually be traced back to plants, all of the energy that animals use for body repair, growth, motion, and body warmth maintenance is energy that once came from the sun.
    • Energy from the sun is transferred to animals through a chain of events that begins with plants producing food then being eaten by animals.

Understanding

Students understand that:
  • Energy can be transferred in various ways and between objects.

Vocabulary

  • Model
  • Energy
  • Repair
  • Growth
  • Motion
  • Maintenance
  • Animal
  • Plant

SC15.5.11

Create a model to illustrate the transfer of matter among producers; consumers, including scavengers and decomposers; and the environment.

Unpacked Content

Scientific and Engineering Practices

Developing and Using Models

Crosscutting Concepts

Systems and System Models

Knowledge

Students know:
  • The food of almost any kind of animal can be traced back to plants.
  • Organisms are related in food webs in which some animals eat plants for food and other animals eat the animals that eat plants.
  • Some organisms, such as fungi and bacteria, break down dead organisms (both plants or plants parts and animals) and therefore operate as "decomposers."
  • Decomposition eventually restores (recycles) some materials back to the soil.
  • Organisms can survive only in environments in which their particular needs are met.
  • A healthy ecosystem is one in which multiple species of different types are each able to meet their needs in a relatively stable web of life.
  • Newly introduced species can damage the balance of an ecosystem.
  • Matter cycles between the air and soil and among plants, animals, and microbes as these organisms live and die. Organisms obtain gases, and water, from the environment, and release waste matter (gas, liquid, or solid) back into the environment.

Skills

Students are able to:
  • Develop a model to describe a phenomenon that includes the movement of matter within an ecosystem, identifying the relevant components such as matter, plants, animals, decomposers, and environment.
  • Describe the relationships among components that are relevant for describing the phenomenon, including the relationships in the system between organisms that consume other organisms, including the following:
    • Animals that consume other animals.
    • Animals that consume plants.
    • Organisms that consume dead plants and animals.
    • The movement of matter between organisms during consumption.
  • Use the model to describe the following:
    • The cycling of matter in the system between plants, animals, decomposers, and the environment.
    • How interactions in the system of plants, animals, decomposers, and the environment allow multiple species to meet their needs.
    • That newly introduced species can affect the balance of interactions in a system (e.g., a new animal that has no predators consumes much of another organism's food within the ecosystem).
    • That changing an aspect (e.g., organisms or environment) of the ecosystem will affect other aspects of the ecosystem.

Understanding

Students understand that:
  • A system can be described in terms of its components, like producers, consumers, and the environment, and their interactions, like the cycling of matter.

Vocabulary

  • Model
  • Transfer
  • Matter
  • Producer
  • Consumer
  • Decomposer
  • Environment

SC15.5.12

Defend the claim that one factor determining the apparent brightness of the sun compared to other stars is the relative distance from Earth.

Unpacked Content

Scientific and Engineering Practices

Engaging in Argument from Evidence

Crosscutting Concepts

Scale, Proportion, and Quantity

Knowledge

Students know:
  • The sun and other stars are natural bodies in the sky that give off their own light.
  • The sun is a star that appears larger and brighter than other stars because it is closer.
  • Stars range greatly in their distance from Earth.
  • A luminous object close to a person appears much brighter and larger than a similar object that is very far away from a person (e.g., nearby streetlights appear bigger and brighter than distant streetlights).

Skills

Students are able to:
  • Identify a given claim to be supported about a given phenomenon. The claim includes the idea that the apparent brightness of the sun and stars is due to their relative distances from Earth.
  • Describe the evidence, data, and/or models that support the claim, including the following:
    • The sun and other stars are natural bodies in the sky that give off their own light.
    • The apparent brightness of a variety of stars, including the sun.
    • A luminous object close to a person appears much brighter and larger than a similar object that is very far away from a person (e.g., nearby streetlights appear bigger and brighter than distant streetlights).
    • The relative distance of the sun and stars from Earth (e.g., although the sun and other stars are all far from the Earth, the stars are very much farther away; the sun is much closer to Earth than other stars).
  • Evaluate the evidence to determine whether it is relevant to supporting the claim, and sufficient to describe the relationship between apparent size and apparent brightness of the sun and other stars and their relative distances from Earth.
  • Use reasoning to connect the relevant and appropriate evidence to the claim with argumentation. Describe a chain of reasoning that includes the following:
    • Because stars are defined as natural bodies that give off their own light, the sun is a star.
    • The sun is many times larger than Earth but appears small because it is very far away.
    • Even though the sun is very far from Earth, it is much closer than other stars.

Understanding

Students understand that:
  • Natural objects, like the sun and stars, exist from the very small to the immensely large.

Vocabulary

  • Defend
  • Claim
  • Factor
  • Evidence
  • Apparent Brightness
  • Relative Distance
  • Sun
  • Stars
  • Earth
  • Reasoning
  • Argumentation

SC15.5.13

Analyze data and represent with graphs to reveal patterns of daily changes in length and direction of shadows, day and night, and the seasonal appearance of some stars in the night sky (e.g., shadows and the position and motion of Earth with respect to the sun, visibility of select stars only in particular months).

Unpacked Content

Scientific and Engineering Practices

Analyzing and Interpreting Data

Crosscutting Concepts

Patterns

Knowledge

Students know:
  • The orbits of Earth around the sun and of the moon around Earth, together with the rotation of Earth about an axis between its North and South poles, cause observable patterns.
  • These include day and night; daily changes in the length and direction of shadows; and different positions of the sun, moon, and stars at different times of the day, month, and year.
  • The apparent motion of the sun from east to west results in patterns of change in length and direction of shadows throughout a day as Earth rotates on its axis.
  • The length of the day gradually changes throughout the year as Earth orbits the sun, with longer days in the summer and shorter days in the winter.
  • Some stars and/or groups of stars (constellations) can be seen in the sky all year, while others appear only at certain times of the year.

Skills

Students are able to:
  • Using graphical displays (e.g., bar graphs, pictographs), organize data pertaining to daily and seasonal changes caused by the Earth's rotation and orbit around the sun. Organize data that include the following:
    • The length and direction of shadows observed several times during one day.
    • The duration of daylight throughout the year, as determined by sunrise and sunset times.
    • Presence or absence of selected stars and/or groups of stars that are visible in the night sky at different times of the year.
  • Use the organized data to find and describe relationships within the datasets.
  • Use the organized data to find and describe relationships among the datasets, including the following:
    • Similarities and differences in the timing of observable changes in shadows, daylight, and the appearance of stars show that events occur at different rates (e.g., Earth rotates on its axis once a day, while its orbit around the sun takes a full year).

Understanding

Students understand that:
  • Similarities and differences in patterns can be used to sort, classify, communicate and analyze daily changes in length and direction of shadows, day and night, and the seasonal appearance of some stars in the night sky.

Vocabulary

  • Data
  • Graph
  • Bar Graph
  • Pictograph
  • Pie Chart
  • Line Graph
  • Analyze
  • Shadow
  • Seasonal
  • Sun
  • Star

SC15.5.14

Use a model to represent how any two systems, specifically the atmosphere, biosphere, geosphere, and/or hydrosphere, interact and support life (e.g., influence of the ocean on ecosystems, landform shape, and climate; influence of the atmosphere on landforms and ecosystems through weather and climate; influence of mountain ranges on winds and clouds in the atmosphere).

Unpacked Content

Scientific and Engineering Practices

Developing and Using Models

Crosscutting Concepts

Systems and System Models

Knowledge

Students know:
  • Earth's major systems are the geosphere (solid and molten rock, soil, and sediments), the hydrosphere (water and ice), the atmosphere, and the biosphere (living things, including humans).
  • These systems interact in multiple ways to affect Earth's surface materials and processes.
  • The ocean supports a variety of ecosystems and organisms, shapes landforms, and influences climate.
  • Winds and clouds in the atmosphere interact with the landforms to determine patterns of weather.

Skills

Students are able to:
  • Develop a model, using a specific given example of a phenomenon, to describe ways that the geosphere, biosphere, hydrosphere, and/or atmosphere interact. In the model, identify the relevant components of their example, including features of two of the following systems that are relevant for the given example:
    • Geosphere (i.e., solid and molten rock, soil, sediment, continents, mountains).
    • Hydrosphere (i.e., water and ice in the form of rivers, lakes, glaciers).
    • Atmosphere (i.e., wind, oxygen).
    • Biosphere [i.e., plants, animals (including humans)].
  • Identify and describe relationships (interactions) within and between the parts of the Earth systems identified in the model that are relevant to the example (e.g., the atmosphere and the hydrosphere interact by exchanging water through evaporation and precipitation; the hydrosphere and atmosphere interact through air temperature changes, which lead to the formation or melting of ice).
  • Use the model to describe a variety of ways in which the parts of two major Earth systems in the specific given example interact to affect the Earth's surface materials and processes in that context. Use the model to describe how parts of an individual Earth system:
    • Work together to affect the functioning of that Earth system.
    • Contribute to the functioning of the other relevant Earth system.

Understanding

Students understand that:
  • Systems, like the atmosphere, biosphere, geosphere, and hydrosphere, can be described in terms of their components and their interactions.

Vocabulary

  • Atmosphere
  • Hydrosphere
  • Geosphere
  • Biosphere
  • Model
  • Phenomenon
  • System
  • Earth

SC15.5.15

Identify the distribution of freshwater and salt water on Earth (e.g., oceans, lakes, rivers, glaciers, ground water, polar ice caps) and construct a graphical representation depicting the amounts and percentages found in different reservoirs.

Unpacked Content

Scientific and Engineering Practices

Using Mathematics and Computational Thinking

Crosscutting Concepts

Scale, Proportion, and Quantity

Knowledge

Students know:
  • Nearly all of Earth's available water is in the ocean.
  • Most fresh water is in glaciers or underground; only a tiny fraction is in streams, lakes, wetlands, and the atmosphere.

Skills

Students are able to:
  • Graph the given data (using standard units) about the amount of salt water and the amount of fresh water in each of the following reservoirs, as well as in all the reservoirs combined, to address a scientific question:
    • Oceans.
    • Lakes.
    • Rivers.
    • Glaciers.
    • Ground water.
    • Polar ice caps.
  • Use the graphs of the relative amounts of total salt water and total fresh water in each of the reservoirs to describe that:
    • The majority of water on Earth is found in the oceans.
    • Most of the Earth's fresh water is stored in glaciers or underground.
    • A small fraction of fresh water is found in lakes, rivers, wetlands, and the atmosphere.

Understanding

Students understand that:
  • Standard units are used to measure and describe physical quantities such as the amounts of salt water and fresh water in various reservoirs.

Vocabulary

  • Fresh water
  • Salt water
  • Oceans
  • Lakes
  • Rivers
  • Glaciers
  • Ground water
  • Polar ice caps
  • Reservoir
  • Graph

SC15.5.16

Collect and organize scientific ideas that individuals and communities can use to protect Earth’s natural resources and its environment (e.g., terracing land to prevent soil erosion, utilizing no-till farming to improve soil fertility, regulating emissions from factories and automobiles to reduce air pollution, recycling to reduce overuse of landfill areas).

Unpacked Content

Scientific and Engineering Practices

Obtaining, Evaluating, and Communicating Information

Crosscutting Concepts

Systems and System Models

Knowledge

Students know:
  • Human activities in agriculture, industry, and everyday life can have major effects, both positive and negative, on the land, vegetation, streams, ocean, air, and even outer space.
  • Individuals and communities are doing things to help protect Earth's resources and environments.

Skills

Students are able to:
  • Obtain and combine information from books and/or other reliable media to explain how individuals and communities can protect Earth's natural resources and its environment.

Understanding

Students understand that:
  • Individual communities interact with components of environmental systems and can have both positive and negative effects.

Vocabulary

  • Natural Resource
  • Scientific idea
  • Individual
  • Community
  • Terracing
  • Erosion
  • Soil
  • No-till farming
  • Fertility
  • Emissions
  • Pollution
  • Recycling
  • Landfill

SC15.5.17

Design solutions, test, and revise a process for cleaning a polluted environment (e.g., simulating an oil spill in the ocean or a flood in a city and creating a solution for containment and/or cleanup).*

Unpacked Content

Scientific and Engineering Practices

Constructing Explanations and Designing Solutions

Crosscutting Concepts

Systems and System Models

Knowledge

Students know:
  • Human activities in agriculture, industry, and everyday life can have major effects, both positive and negative, on the land, vegetation, streams, ocean, air, and even outer space.
  • Individuals and communities are doing things to help protect Earth's resources and environments.
  • Research on a problem should be carried out before beginning to design a solution.
  • Testing a solution involves investigating how well it performs under a range of likely conditions.
  • At whatever stage, communicating with peers about proposed solutions is an important part of the design process, and shared ideas can lead to improved designs.

Skills

Students are able to:
  • Use grade-appropriate information from research about a given problem, including the causes and effects of the problem and relevant scientific information.
  • Generate at least two possible solutions to the problem based on scientific information and understanding of the problem.
  • Specify how each design solution solves the problem.
  • Share ideas and findings with others about design solutions to generate a variety of possible solutions.
  • Describe the necessary steps for designing a solution to a problem, including conducting research and communicating with others throughout the design process to improve the design [note: emphasis is on what is necessary for designing solutions, not on a step-wise process].

Understanding

Students understand that:
  • Engineers improve existing technologies or develop new ones to: increase benefits, decrease known risks, and/or meet societal demands.

Vocabulary

    Design
  • Solution
  • Test
  • Revise
  • Polluted
  • Environment
  • Engineer
  • Technology

SC15.6.1

Create and manipulate models (e.g., physical, graphical, conceptual) to explain the occurrences of day/night cycles, length of year, seasons, tides, eclipses, and lunar phases based on patterns of the observed motions of celestial bodies.

Unpacked Content

Scientific and Engineering Practices

Developing and Using Models

Crosscutting Concepts

Patterns

Knowledge

Students know:
  • Earth rotates on its tilted axis once in approximately 24 hours; this rotation is considered an Earth day. Due to the rotation of the Earth, the side of the Earth facing the sun experiences light (day); the side of the Earth facing away from the sun experiences dark (night).
  • The Earth-moon system revolves around the sun once in approximately 365 days; this revolution is considered an Earth year.
  • The distance between Earth and the sun stays relatively constant throughout the Earth's orbit.
  • The Earth's rotation axis is tilted with respect to its orbital plane around the sun. Earth maintains the same relative orientation in space, with its North Pole pointed toward the North Star throughout its orbit.
  • Solar energy travels in a straight line from the sun and hits different parts of the curved Earth at different angles — more directly at the equator and less directly at the poles.
  • Because the Earth's axis is tilted, the most direct and intense solar energy occurs over the summer months, and the least direct and intense solar energy occurs over the winter months.
  • The change in season at a given place on Earth is directly related to the orientation of the tilted Earth and the position of Earth in its orbit around the sun because of the change in the directness and intensity of the solar energy at that place over the course of the year.
  • Summer occurs in the Northern Hemisphere at times in the Earth's orbit when the northern axis of Earth is tilted toward the sun.
  • Summer occurs in the Southern Hemisphere at times in the Earth's orbit when the southern axis of Earth is tilted toward the sun.
  • Winter occurs in the Northern Hemisphere at times in the Earth's orbit when the northern axis of Earth is tilted away from the sun.
  • Winter occurs in the Southern Hemisphere at times in the Earth's orbit when the southern axis of Earth is tilted away from the sun.
  • A tide is the daily rise and fall of sea level.
  • Low tide is the lowest sea level at a particular time and place on Earth.
  • High tide is the highest sea level at a particular time and place on Earth.
  • Tides occur as a result of the moon's gravitational pull on the Earth.
  • Solar energy is prevented from reaching the Earth during a solar eclipse because the moon is located between the sun and Earth.
  • Solar energy is prevented from reaching the moon (and thus reflecting off of the moon to Earth) during a lunar eclipse because Earth is located between the sun and moon.
  • Because the moon's orbital plane is tilted with respect to the plane of the Earth's orbit around the sun, for a majority of time during an Earth month, the moon is not in a position to block solar energy from reaching Earth, and Earth is not in a position to block solar energy from reaching the moon.
  • A lunar eclipse can only occur during a full moon.
  • The moon rotates on its axis approximately once a month.
  • The moon orbits Earth approximately once a month.
  • The moon rotates on its axis at the same rate at which it orbits Earth so that the side of the moon that faces Earth remains the same as it orbits.
  • The moon's orbital plane is tilted with respect to the plane of the Earth's orbit around the sun.
  • Solar energy coming from the sun bounces off of the moon and is viewed on Earth as the bright part of the moon.
  • The visible proportion of the illuminated part of the moon (as viewed from Earth) changes over the course of a month as the location of the moon relative to Earth and the sun changes. This change in illumination is known as the lunar phase.
  • The moon appears to become more fully illuminated until "full" and then less fully illuminated until dark, or "new," in a pattern of change that corresponds to what proportion of the illuminated part of the moon is visible from Earth.
  • The lunar phase of the moon is a result of the relative positions of the Earth, sun, and moon.

Skills

Students are able to:
  • Develop a model of the Sun-Earth-Moon systems and identify the relevant components.
  • Describe the relationships between components of the model.
  • Use patterns observed from their model to provide causal accounts for events and make predictions for events by constructing explanations.

Understanding

Students understand that:
  • Patterns in the occurrences of day/night cycles, length of year, seasons, tides, eclipses, and lunar phases can be observed and explained using models based on observed motion of celestial bodies.

Vocabulary

  • Model
  • Earth
  • Moon
  • Sun
  • Orbit
  • Rotation
  • Axis
  • Tilted
  • Day
  • Night
  • Hour
  • Revolution
  • Constant
  • Orbital plane
  • Orientation
  • Solar Energy
  • Equator
  • Poles
  • Northern Hemisphere
  • Southern Hemisphere
  • Winter
  • Summer
  • Tides
  • Gravitational pull
  • Low tide
  • High tide
  • Eclipse
  • Solar eclipse
  • Lunar Eclipse
  • Lunar phases (new moon, waxing crescent, first quarter, waxing gibbous, full moon, waning gibbous, third quarter, waning crescent)
  • Illumination

SC15.6.2

Construct models and use simulations (e.g., diagrams of the relationship between Earth and man-made satellites, rocket launch, International Space Station, elliptical orbits, black holes, life cycles of stars, orbital periods of objects within the solar system, astronomical units and light years) to explain the role of gravity in affecting the motions of celestial bodies bodies (e.g., planets, moons, comets, asteroids, meteors) within galaxies and the solar system.

Unpacked Content

Scientific and Engineering Practices

Developing and Using Models

Crosscutting Concepts

Systems and System Models

Knowledge

Students know:
  • The solar system is a collection of bodies, including the sun, planets, moons, comets, asteroids, and meteors.
  • A galaxy is any of the very large groups of stars and associated matter that are found throughout the universe.
  • The Earth's solar system is one of many systems orbiting the center of the larger system of the Milky Way galaxy.
  • Gravity is an attractive force between solar system and galaxy objects.
  • Gravity increases as the mass of the interacting objects increases.
  • Gravity decreases as the distances between objects increases.
  • Gravity affects the orbital motion of objects in our solar system (e.g., moons orbit around planets, all objects within the solar system orbit the sun).
  • Gravity is a predominantly inward-pulling force that can keep smaller/less massive objects in orbit around larger/more massive objects.
  • Gravity causes a pattern of smaller/less massive objects orbiting around larger/more massive objects at all system scales in the universe.
  • Gravitational forces from planets cause smaller objects (e.g., moons) to orbit around planets.
  • The gravitational force of the sun causes the planets and other bodies to orbit around it, holding the solar system together.
  • The gravitational forces from the center of the Milky Way cause stars and stellar systems to orbit around the center of the galaxy.
  • The hierarchy pattern of orbiting systems in the solar system was established early in its history as the disk of dust and gas was driven by gravitational forces to form moon-planet and planet-sun orbiting systems.
  • Objects too far away from the sun do not orbit it because the sun's gravitational force on those objects is too weak to pull them into orbit.
  • Without gravity smaller planets would move in straight paths through space, rather than orbiting a more massive body.

Skills

Students are able to:
  • Develop a model and identify the relevant components including gravity and celestial bodies.
  • Describe the relationships and interactions between the components of the solar and galaxy systems.
  • Use the model to describe gravity and its effects.

Understanding

Students understand that:
  • Gravity is an attractive force between solar system and galaxy objects.
  • Gravity causes a pattern of smaller/less massive objects orbiting around larger/more massive objects at all systems scales in the universe.

Vocabulary

  • Model
  • Simulation
  • Gravity
  • Gravitational force
  • Solar system
  • Galaxy
  • Milky Way galaxy
  • Sun
  • Planets
  • Moons
  • Asteroids
  • Asteroid belt
  • Stars
  • Celestial bodies
  • Elliptical orbit

SC15.6.3

Develop and use models to determine scale properties of objects in the solar system (e.g., scale model representing sizes and distances of the sun, Earth, moon system based on a one-meter diameter sun).

Unpacked Content

Scientific and Engineering Practices

Developing and Using Models

Crosscutting Concepts

Scale, Proportion, and Quantity

Knowledge

Students know:
  • A (scale) model is a representation or copy of an object that is larger or smaller than the actual size of the object being represented.
  • Measurements may be multiplied or divided to correctly scale objects in a model.
  • Charts and data tables may be analyzed to find patterns in data.
  • Patterns can be used to describe similarities and differences in objects in the solar system.
  • Systems and their properties may be described using more than one scale.

Skills

Students are able to:
  • Develop a model of objects in the solar system and identify the relevant components.
  • Describe that different representations illustrate different characteristics of objects in the solar system, including differences in scale.
  • Use mathematics and computational thinking to determine scale properties.
  • Describe that two objects may be similar when viewed at one scale but may appear to be quite different when viewed at a different scale.

Understanding

Students understand that:
  • The solar system consists of the sun and a collection of objects, including planets, their moons, and asteroids that are held in orbit around the sun by its gravitational pull on them.
  • Space phenomena can be observed at various scales using models to study systems that are too large or too small.

Vocabulary

  • Model
  • Scale
  • Scale model
  • Properties
  • Size
  • Distance
  • Diameter
  • Solar system
  • Planet
  • Moon
  • Sun
  • Asteroid
  • Asteroid belt
  • Celestial body

SC15.6.4

Construct explanations from geologic evidence (e.g., change or extinction of particular living organisms; field evidence or representations, including models of geologic cross-sections; sedimentary layering) to identify patterns of Earth’s major historical events (e.g., formation of mountain chains and ocean basins, significant volcanic eruptions, fossilization, folding, faulting, igneous intrusion, erosion).

Unpacked Content

Scientific and Engineering Practices

Constructing Explanations and Designing Solutions

Crosscutting Concepts

Patterns

Knowledge

Students know:
  • Major events in Earth's history include natural and catastrophic events.
  • Natural events may include formations of mountain chains, formations of ocean basins, fossilization, folding, faulting, igneous intrusion, and erosion.
  • Catastrophic events may include significant volcanic eruptions or asteroid impacts,
  • The geologic time scale interpreted from rock strata provides a way to organize Earth's history.
  • Analyses of rock strata and the fossil record provide only relative dates, not an absolute scale.
  • Rock strata are layers of rock visually distinguishable from other layers of rock.
  • Rocks are the solid mineral materials forming part of the surface of the Earth and other similar planets.
  • Fossils are a trace or print of the remains of a plant or animal of a past age preserved in plant or rock.
  • Unless they have been disturbed by subsequent activity, newer rock layers sit on top of older rock layers, allowing for a relative ordering in time of the formation of the layers (i.e., older sedimentary rocks lie beneath younger sedimentary rocks).
  • Any rocks or features that cut existing rock strata are younger than the rock strata that they cut (e.g., a younger fault cutting across older, existing rock strata).
  • The fossil record can provide relative ages based on the appearance or disappearance of organisms (e.g., fossil layers that contain only extinct animal groups are usually older than fossil layers that contain animal groups that are still alive today, and layers with only microbial fossils are typical of the earliest evidence of life).
  • Specific major events (e.g., extensive lava flows, volcanic eruptions, asteroid impacts) can be used to indicate periods of time that occurred before a given event from periods that occurred after it.

Skills

Students are able to:
  • Articulate a statement that relates a given phenomenon to a scientific idea, including that geologic evidence can be used to identify patterns of Earth's major historical events.
  • Identify and use multiple valid and reliable sources of evidence to construct an explanation identifying patterns of Earth's major historical events.
  • Use reasoning to connect the evidence and support an explanation of patterns in Earth's major historical events.

Understanding

Students understand that:
  • The geologic time scale interpreted from rock strata provides a way to organize Earth's history. Analyses of rock strata and the fossil record provide only relative dates, not an absolute scale.
  • Using a combination of the order of rock layers, the fossil record, and evidence of major geologic events, the relative time ordering of events can be constructed as a model for Earth's history, even though the timescales involved are immensely vaster than the lifetimes of humans or the entire history of humanity.

Vocabulary

  • Natural event
  • Catastrophic event
  • Mountain chain
  • Ocean basin
  • Fossilization
  • Folding
  • Faulting
  • Igneous intrusion
  • Erosion
  • Volcano
  • Volcanic eruption
  • Asteroid impact
  • Geologic time scale
  • Rock
  • Rock strata
  • Fossil record
  • Relative age
  • Mineral
  • Fossil
  • Sedimentary rock
  • Lava flow

SC15.6.5

Use evidence to explain how different geologic processes shape Earth’s history over widely varying scales of space and time (e.g., chemical and physical erosion; tectonic plate processes; volcanic eruptions; meteor impacts; regional geographical features, including Alabama fault lines, Rickwood Caverns, and Wetumpka Impact Crater).

Unpacked Content

Scientific and Engineering Practices

Constructing Explanations and Designing Solutions

Crosscutting Concepts

Scale, Proportion, and Quantity

Knowledge

Students:
  • The planet's systems interact over scales that range from microscopic to global in size, and they operate over fractions of a second to billions of years. These interactions have shaped Earth's history and will determine its future.
  • Processes change Earth's surface at time and spatial scales that can be large (such as slow plate motions or the uplift of large mountain ranges) or small (such as rapid landslides or microscopic geochemical reactions).
  • Many geologic processes that change Earth's features (such as earthquakes, volcanoes, and meteor impacts) usually behave gradually but are punctuated by catastrophic events.
  • The composition of Earth's layers and their properties affect the surface of Earth.
  • Geologic processes that have changed Earth's features include events like surface weathering, erosion, and deposition by the movements of water, ice, and wind.
  • Surface weathering, erosion, movement, and the deposition of sediment range from large to microscopic scales (e.g., sediment consisting of boulders and microscopic grains of sand, raindrops dissolving microscopic amounts of minerals).
  • Water's movements—both on the land and underground—cause weathering and erosion, which change the land's surface features and create underground formations.
  • The motion of the Earth's plates produces changes on a planetary scale over a range of time periods from millions to billions of years. Evidence for the motion of plates can explain large-scale features of the Earth's surface (e.g., mountains, distribution of continents) and how they change.
  • Catastrophic changes can modify or create surface features over a very short period of time compared to other geologic processes, and the results of those catastrophic changes are subject to further changes over time by processes that act on longer time scales (e.g., erosion of a meteor crater).

Skills

Students are able to:
  • Articulate a statement that relates a given phenomenon to a scientific idea, including that geologic processes have shaped the Earth's history over widely varying scales of space and time.
  • Identify the corresponding timescales for each identified geoscience process.
  • Identify and use multiple valid and reliable sources of evidence to construct an explanation that changes occur on very large or small spatial and/or temporal scales.
  • Use reasoning to connect the evidence and support an explanation for how geologic processes have changed the Earth's surface at a variety of temporal and spatial scales.

Understanding

Students understand that:
  • The planet's systems interact over scales that range from microscopic to global in size, and they operate over fractions of a second to billions of years. These interactions have shaped Earth's history and will determine its future.
  • A given surface feature is the result of a broad range of geoscience processes occurring at different temporal and spatial scales.
  • Surface features will continue to change in the future as geoscience processes continue to occur.

Vocabulary

  • Evidence
  • Geology
  • Geologic process
  • Scale
  • System
  • Microscopic
  • Global
  • Time scale
  • Spatial scale
  • Uplift
  • Landslide
  • Geochemical reaction
  • Earthquake
  • Catastrophic event
  • Composition
  • Property
  • Deposition
  • Sediment
  • Surface features
  • Underground formations
  • Erosion
  • Chemical erosion
  • Physical erosion
  • Tectonic plates
  • Tectonic plate processes
  • Continent
  • Continental drift theory
  • Volcano
  • Volcanic eruption
  • Meteor
  • Meteor impact
  • Impact crater
  • Weathering
  • Fault line
  • Cavern

SC15.6.6

Provide evidence from data of the distribution of fossils and rocks, continental shapes, and seafloor structures to explain past plate motions.

Unpacked Content

Scientific and Engineering Practices

Constructing Explanations and Designing Solutions

Crosscutting Concepts

Patterns

Knowledge

Students:
  • Fossils are a trace or print of the remains of a plant or animal of a past age preserved in plant or rock.
  • Rocks are the solid mineral materials forming part of the surface of the Earth and other similar planets.
  • A continent is any of the world's main continuous expanses of land (i.e.,, Africa, Antarctica, Asia, Australia, Europe, North America, and South America).
  • The continental shelf is the part of a continent that lies under the ocean and slopes down to the ocean floor.
  • Regions of different continents that share similar fossils and similar rocks suggest that, in the geologic past, those sections of continent were once attached and have since been separated.
  • The shapes of the continents roughly fit together like pieces in a jigsaw puzzle, suggesting that those land masses were once joined and have since separated.
  • The hypothetical land mass that existed when all the continents were joined is called Pangea.
  • The separation of continents by the sequential formation of new seafloor at the center of the ocean is inferred by age patterns in the oceanic crust that increase in age from the center of the ocean to the edges of the ocean.
  • The distribution of seafloor structures (e.g., volcanic ridges at the centers of oceans, trenches at the edges of continents) combined with the patterns of ages of the seafloor (youngest ages at the ridge, oldest ages at the trenches) supports the interpretation that new crust forms at the ridges and then moves away from the ridges as new crust continues to form and that the oldest crust is being destroyed at seafloor trenches.
  • Ridges are underwater mountain systems formed by plate tectonics.
  • Trenches are long, narrow, steep-sided depressions in the ocean floor.
  • The Theory of Continental Drift was first proposed by Alfred Wegener and proposes that part of the Earth's crust slowly drifts atop a liquid core.
  • The Theory of Plate Tectonics states that the outer rigid layer of the Earth is divided into a couple of dozen "plates" that move around across the Earth's surface relative to each other.
  • The layers of the Earth include, from outmost to innermost, the crust, mantle, outer core, and inner core. The crust and upper mantle are broken into moving plates called the lithosphere. The asthenosphere is located below the lithosphere. In the asthenosphere, there is relatively low resistance to plastic flow and convection occurs, causing plates to move.
  • The three types of plate tectonic boundaries include divergent, convergent, and transform plate boundaries.
  • Divergent boundaries occur when two tectonic plates move away from each other.
  • Convergent boundaries occur when two tectonic plates come together.
  • Transform plate boundaries occur when two plates slide past one another.

Skills

Students are able to:
  • Articulate a statement that relates a given phenomenon to a scientific idea, including that past plate motions can be described with data from the distribution of fossils and rocks, continental shapes, and seafloor structures.
  • Organize given data in a way that facilitates analysis and interpretation.
  • Analyze the data to identify relationships between the data and Earth's past plate motions.
  • Identify and use multiple valid and reliable sources of data.
  • Use evidence and reasoning to construct an explanation for the given phenomenon, which involves past plate motions.

Understanding

Students understand that:
  • Maps of ancient land and water patterns, based on investigations of rocks and fossils, make clear how Earth's plates have moved great distances, collided, and spread apart.

Vocabulary

  • Evidence
  • Data
  • Fossils
  • Rock
  • Continent
  • Continental shelf
  • Geologic past
  • Pangea
  • Ridges
  • Volcanic ridges
  • Trenches
  • Theory of Continental Drift
  • Theory of Plate Tectonics
  • Crust
  • Mantle
  • Core
  • Lithosphere
  • Asthenosphere
  • Convection
  • Divergent boundary
  • Convergent boundary
  • Transform plate boundary
  • Seafloor
  • Seafloor structures
  • Alfred Wegener
  • Plastic flow

SC15.6.7

Use models to construct explanations of the various biogeochemical cycles of Earth (e.g., water, carbon, nitrogen) and the flow of energy that drives these processes.

Unpacked Content

Scientific and Engineering Practices

Developing and Using Models

Crosscutting Concepts

Stability and Change

Knowledge

Students:
  • The cycle of atoms between living and non-living things is known as a biogeochemical cycle.
  • Biogeochemical cycles interact through biotic and abiotic processes.
  • Biotic involves living or once living things such as plants, animals, and bacteria.
  • Abiotic involves nonliving things like air, rocks, and water.
  • Biogeochemical cycles may include, but are not limited to, the water, carbon, and nitrogen cycles.
  • The water cycle is the continuous process by which water is circulated throughout the earth and the atmosphere.
  • Water is a chemical compound made up of the elements hydrogen and oxygen.
  • Global movements of water and its changes in form are propelled by sunlight and gravity.
  • Energy from the sun drives the movement of water from the Earth (e.g., oceans, landforms, plants) into the atmosphere through transpiration and evaporation.
  • Water vapor in the atmosphere can cool and condense to form rain or crystallize to form snow or ice, which returns to Earth when pulled down by gravity.
  • Water continually cycles among land, ocean, and atmosphere via transpiration, evaporation, condensation and crystallization, and precipitation, as well as downhill flows on land.
  • Gravity causes water on land to move downhill (e.g., rivers and glaciers) and much of it eventually flows into oceans.
  • Some liquid and solid water remains on land in the form of bodies of water, glaciers and ice sheets or can be stored below ground in aquifers.
  • Some water remains in the tissues of plants and other living organisms, and this water is released when the tissues decompose. Water is also released by plants through transpiration and by other living organisms through respiration.
  • Carbon is an element found in the oceans, air, rocks, soil and all living organisms.
  • Carbon is the fundamental building block of life and an important component of many chemical processes.
  • In a process called the carbon cycle, carbon is exchanged among Earth's oceans, atmosphere, ecosystem, and geosphere.
  • Carbon is present in the atmosphere primarily attached to oxygen in a gas called carbon dioxide (CO2), but is also found in other less abundant but climatically significant gases, such as methane (CH4).
  • With the help of the Sun, through the process of photosynthesis, carbon dioxide is pulled from the air to make plant food.
  • Through food chains, the carbon that is in plants moves to the animals that eat them. When an animal eats another animal, the carbon is transferred.
  • When plants and animals die, their bodies, wood, and leaves decay bringing the carbon into the ground. Some become buried miles underground and will become fossil fuels in millions and millions of years.
  • Organisms release carbon dioxide gas through a process called respiration.
  • When humans burn fossil fuels to power factories, power plants, cars and trucks, most of the carbon quickly enters the atmosphere as carbon dioxide gas.
  • The oceans, and other bodies of water, soak up some carbon from the atmosphere.
  • Nitrogen is an element found in living things like plants and animals.
  • Nitrogen is also an important part of non-living things like the air and the soil.
  • Nitrogen atoms move slowly between living things, dead things, the air, soil and water.
  • The continuous process by which nitrogen is exchanged between organisms and the environment is called the nitrogen cycle.
  • Most of the nitrogen on Earth is in the atmosphere as molecules of nitrogen gas (N2).
  • All plants and animals need nitrogen to make amino acids, proteins, and DNA, but the nitrogen in the atmosphere is not in a form that they can use.
  • The molecules of nitrogen in the atmosphere can become usable for living things when they are broken apart during lightning strikes or fires, by certain types of bacteria, or by bacteria associated with bean plants.
  • Most plants get the nitrogen they need to grow from the soils or water in which they live. Animals get the nitrogen they need by eating plants or other animals that contain nitrogen.
  • When organisms die, their bodies decompose bringing the nitrogen into soil on land or into ocean water. Bacteria alter the nitrogen into a form that plants are able to use. Other types of bacteria are able to change nitrogen dissolved in waterways into a form that allows it to return to the atmosphere.
  • Certain actions of humans can cause changes to the nitrogen cycle and the amount of nitrogen that is stored in the land, water, air, and organisms.
  • The use of nitrogen-rich fertilizers can add too much nitrogen in nearby waterways as the fertilizer washes into streams and ponds. The waste associated with livestock farming also adds large amounts of nitrogen into soil and water. The increased nitrate levels cause plants to grow rapidly until they use up the supply and die. The number of plant-eating animals will increase when the plant supply increases and then the animals are left without any food when the plants die.

Skills

Students are able to:
  • Use a model of the various biogeochemical cycles and identify the relevant components.
  • Describe the relationships between components of the model including the flow of energy.
  • Articulate a statement that relates a given phenomenon to a scientific idea, including the various biogeochemical cycles of Earth and the flow of energy that drives these processes.

Understanding

Students understand that:
  • The transfer of energy drives the motion and/or cycling of matter of the various biogeochemical cycles.

Vocabulary

  • Biogeochemical
  • Biotic
  • Abiotic
  • Atom
  • Water cycle
  • Carbon cycle
  • Nitrogen cycle
  • Chemical compound
  • Hydrogen
  • Oxygen
  • Gravity
  • Atmosphere
  • Water vapor
  • Crystallize
  • Transpiration
  • Evaporation
  • Condensation
  • Precipitation
  • Glacier
  • Aquifer
  • Ice sheet
  • Organism
  • Decompose
  • Respiration
  • Element
  • Chemical process
  • Ecosystem
  • Geosphere
  • Carbon dioxide
  • Methane
  • Photosynthesis
  • Fossil fuel
  • Nitrogen
  • Carbon
  • Amino acid
  • Protein
  • DNA
  • Molecule
  • Bacteria
  • Fertilizer
  • Livestock
  • Nitrate

SC15.6.8

Plan and carry out investigations that demonstrate the chemical and physical processes that form rocks and cycle Earth’s materials (e.g., processes of crystallization, heating and cooling, weathering, deformation, and sedimentation).

Unpacked Content

Scientific and Engineering Practices

Planning and Carrying out Investigations

Crosscutting Concepts

Energy and Matter

Knowledge

Students know:
  • Rocks are the solid mineral materials forming part of the surface of the Earth and other similar planets.
  • Different Earth processes (melting, sedimentation, crystallization) drive matter cycling (from one type of Earth material to another) through observable chemical and physical changes.
  • Chemical changes are changes that result in the formation of new chemical substances.
  • Physical changes involve changes into new forms or shapes in which the chemical identity of the substance is not changed.
  • Melting is a physical change in which a solid changes to a liquid as a result of exposure to heat.
  • Sedimentation is a process in which material (like rock or sand) is carried to the bottom of a body of water and forms a solid layer. Sedimentary rock consists of cemented sediment.
  • Crystallization is the process of the formation of crystals from a liquid. Igneous rocks are the result of crystallizing magma.
  • Deformation is a physical change in a rock's shape or size. Rocks become deformed when the Earth's crust is stretched, compressed, or heated.
  • Metamorphic rock was once one form of rock but changed to another under the influence of heat or pressure.
  • Energy from Earth's interior and the sun drive Earth processes that together cause matter cycling through different forms of Earth materials.
  • The movement of energy that originates from the Earth's hot interior causes the cycling of matter through the Earth processes of melting, crystallization, and deformation.
  • Energy from the sun causes matter to cycle via processes that produce weathering, erosion, and sedimentation (e.g., wind, rain).
  • Weathering is the chemical or physical breaking down or dissolving of rocks and minerals on Earth's surface.
  • Erosion is the act in which Earth is worn away, often by wind, water, or ice.

Skills

Students are able to:
  • Identify the phenomena under investigation, which includes the chemical and physical processes of Earth.
  • Identify the purpose of the investigation, which includes demonstrating the chemical and physical processes that form rocks and cycle Earth materials.
  • Develop a plan for the investigation individually or collaboratively.
  • Describe factors used in the investigation including appropriate units (if necessary), independent and dependent variables, controls and number of trials for each experimental condition.
  • Perform the investigation as prescribed by the plan.
  • Use data from the investigation to provide an causal account of the relationship between chemical and physical processes and the formation of rocks and the cycling of Earth materials.

Understanding

Students understand that:
  • All Earth processes are the result of energy flowing and matter cycling within and among the planet's systems. This energy is derived from the sun and Earth's hot interior. The energy that flows and matter that cycles produce chemical and physical changes in Earth's materials.

Vocabulary

  • Rock
  • Melting
  • Sedimentation
  • Crystallization
  • Chemical change
  • Physical change
  • Deformation
  • Interior energy
  • Cycling
  • Weathering
  • Erosion
  • Solar energy
  • Sedimentary rock
  • Igneous rock
  • Metamorphic rock

SC15.6.9

Use models to explain how the flow of Earth’s internal energy drives a cycling of matter between Earth’s surface and deep interior causing plate movements (e.g., mid-ocean ridges, ocean trenches, volcanoes, earthquakes, mountains, rift valleys, volcanic islands).

Unpacked Content

Scientific and Engineering Practices

Developing and Using Models

Crosscutting Concepts

Energy and Matter

Knowledge

Students know:
  • The layers of the Earth include, from outmost to innermost, the crust, mantle, outer core, and inner core.
  • The crust and upper mantle are broken into moving plates called the lithosphere. These plates are known as tectonic plates and fit around the globe like puzzle pieces.
  • The asthenosphere is located below the lithosphere. The asthenosphere is hotter and more fluid than the lithosphere. Convection occurs in the asthenosphere.
  • Convection is the transfer of heat by the actual movement of the heated material.
  • Through convection, movements deep within the Earth, which carry heat from the hot interior to the cooler surface, cause the plates to move very slowly on the surface.
  • The Theory of Plate Tectonics states that the outer rigid layer of the Earth is divided into a couple of dozen "plates" that move around across the Earth's surface relative to each other.
  • The areas where plates interact are called plate boundaries.
  • The three types of plate tectonic boundaries include divergent (dividing), convergent (colliding), and transform (grinding past each other).
  • Because ocean plates are denser than continental plates, when these two types of plates converge, the ocean plates are subducted beneath the continental plates. Subduction zones and trenches are convergent margins.
  • Subduction zones form when plates crash into each other, spreading ridges form when plates pull away from each other, and large faults form when plates slide past each other.
  • A divergent boundary occurs when two tectonic plates move away from each other. Along these boundaries, lava spews from long fissures and geysers spurt superheated water. Frequent earthquakes strike along the rift. Beneath the rift, magma—molten rock—rises from the mantle. It oozes up into the gap and hardens into solid rock, forming new crust on the torn edges of the plates. Magma from the mantle solidifies into basalt, a dark, dense rock that underlies the ocean floor. Thus at divergent boundaries, oceanic crust, made of basalt, is created.
  • When two plates come together, it is known as a convergent boundary. The impact of the two colliding plates buckles the edge of one or both plates up into a rugged mountain range called a mid-ocean ridge, and sometimes bends the other down into an ocean trench. Trenches are long, narrow, steep-sided depressions in the ocean floor. A chain of volcanoes often forms parallel to the boundary, to the mountain range, and to the trench. Powerful earthquakes shake a wide area on both sides of the boundary. If one of the colliding plates is topped with oceanic crust, it is forced down into the mantle where it begins to melt. Magma rises into and through the other plate, solidifying into new crust. Magma formed from melting plates solidifies into granite, a light colored, low-density rock that makes up the continents. Thus at convergent boundaries, continental crust, made of granite, is created, and oceanic crust is destroyed.
  • Two plates sliding past each other forms a transform plate boundary. Rocks that line the boundary are pulverized as the plates grind along, creating a rift valley or undersea canyon. As the plates alternately jam and jump against each other, earthquakes rattle through a wide boundary zone. In contrast to convergent and divergent boundaries, no magma is formed. Thus, crust is cracked and broken at transform margins, but is not created or destroyed.

Skills

Students are able to:
  • Use a model of the flow of Earth's internal energy and the resulting plate movements and identify the relevant components.
  • Describe the relationships between components of the model including how the flow of Earth's internal energy drives a cycling of matter between Earth's surface and deep interior causing plate movements.
  • Articulate a statement that relates a given phenomenon to a scientific idea, including how the flow of Earth's internal energy drives a cycling of matter between Earth's surface and deep interior causing plate movements.

Understanding

Students understand that:
  • The flow of Earth's internal energy drives a cycling of matter between Earth's surface and deep interior. This cycling of matter causes plate movements.

Vocabulary

  • Crust
  • Mantle
  • Outer core
  • Inner core
  • Lithosphere
  • Plates
  • Tectonic plates
  • Ocean plate
  • Continental plate
  • Asthenosphere
  • Convection
  • Convection current
  • Magma
  • Divergent plate boundary
  • Theory of Plate Tectonics
  • Convergent plate boundary
  • Transform plate boundary
  • Fault
  • Lava
  • Fissure
  • Geyser
  • Rift
  • Basalt
  • Granite
  • Density
  • Ocean trench
  • Subduction
  • Subduction zone
  • Earthquake
  • Mid-ocean ridge
  • Mountain
  • Rift valley
  • Volcano
  • Volcanic island
  • Undersea canyon

SC15.6.10

Use research-based evidence to propose a scientific explanation regarding how the distribution of Earth’s resources such as minerals, fossil fuels, and groundwater are the result of ongoing geoscience processes (e.g., past volcanic and hydrothermal activity, burial of organic sediments, active weathering of rock).

Unpacked Content

Scientific and Engineering Practices

Constructing Explanations and Designing Solutions

Crosscutting Concepts

Cause and Effect

Knowledge

Students know:
  • Humans depend on Earth's land, ocean, atmosphere, and biosphere for many different resources.
  • These resources are distributed unevenly around the planet as a result of past geoscience processes.
  • The water cycle, the rock cycle, and plate tectonics are examples of geoscience processes that distribute Earth's resources.
  • The environment or conditions that formed the resources are specific to certain areas and/or times on Earth, thus identifying why those resources are found only in those specific places/periods.
  • The extraction and use of resources by humans decreases the amounts of these resources available in some locations and changes the overall distribution of these resources on Earth
  • As resources as used, they are depleted from the sources until they can be replenished, mainly through geoscience processes.

Skills

Students are able to:
  • Articulate a statement that relates a given phenomenon to a scientific idea, including that ongoing geoscience processes have caused the distribution of the Earth's resources.
  • Identify and use multiple valid and reliable sources of evidence to construct a scientific explanation of the phenomenon.
  • Use reasoning to connect the evidence and support an explanation of the distribution of Earth's resources.

Understanding

Students understand that:
  • The Earth's resources are formed as a result of past and ongoing geoscience processes.
  • These resources are distributed unevenly around the planet as a result of past and ongoing geoscience processes.
  • The extraction and use of resources by humans decreases the amounts of these resources available in some locations and changes the overall distribution of these resources on Earth.
  • Because many resources continue to be formed in the same ways that they were in the past, and because the amount of time required to form most of these resources (e.g., minerals, fossil fuels) is much longer than timescales of human lifetimes, these resources are limited to current and near-future generations. Some resources (e.g., groundwater) can be replenished on human timescales and are limited based on distribution.

Vocabulary

  • Natural resources
  • Minerals
  • Fossil Fuels
  • Groundwater
  • Geoscience processes
  • Distribution
  • Extraction
  • Depletion
  • Water cycle
  • Rock cycle
  • Plate tectonics

SC15.6.11

Develop and use models of Earth’s interior composition to illustrate the resulting magnetic field (e.g., magnetic poles) and to explain its measureable effects (e.g., protection from cosmic radiation).

Unpacked Content

Scientific and Engineering Practices

Developing and Using Models

Crosscutting Concepts

Cause and Effect

Knowledge

Students know:
  • The Earth's interior consists of rock and metal. It is made up of four main layers:
    1. the inner core: a solid metal core,
    2. the outer core: a liquid molten core,
    3. the mantle: dense and mostly solid rock, and
    4. the crust: thin rock material.
  • The temperature in the core is hotter than the Sun's surface. This intense heat from the inner core causes material in the outer core and mantle to move around.
  • It is possible that the movements of material deep within the Earth generate the Earth's magnetic field, called the magnetosphere.
  • The Earth has a magnetic field with north and south poles. The Earth's magnetic field reaches 36,000 miles into space.
  • The magnetosphere prevents most of the particles from the sun, carried in solar wind, from hitting the Earth.
  • Cosmic radiation, which includes solar radiation, is energy from space transmitted in the form of waves or particles.
  • The Sun and other planets have magnetospheres, but the Earth has the strongest one of all the rocky planets.
  • The Earth's north and south magnetic poles reverse at irregular intervals of hundreds of thousands of years.
  • Conditions inside the magnetosphere can create "space weather" that can affect technological systems and human activities. Technological systems that can be impacted may include the operations of satellites, the orbits of low-altitude Earth orbiting satellites, communication and navigations systems.

Skills

Students are able to:
  • Develop a model of Earth's internal composition and identify the relevant components.
  • Describe the relationships between components of the model.
  • Use observations from the model to provide causal accounts for events and make predictions for events by constructing explanations.

Understanding

Students understand that:
  • The composition of Earth's interior may produce a magnetic field with effects that can be measured.

Vocabulary

  • Interior
  • Inner Core
  • Outer Core
  • Mantle
  • Crust
  • Molten
  • Magnetic field
  • Magnetosphere
  • Magnetic poles
  • Particles
  • Solar wind
  • Cosmic radiation
  • Solar radiation
  • Waves

SC15.6.12

Integrate qualitative scientific and technical information (e.g., weather maps; diagrams; other visualizations, including radar and computer simulations) to support the claim that motions and complex interactions of air masses result in changes in weather conditions.

Unpacked Content

Scientific and Engineering Practices

Obtaining, Evaluating, and Communicating Information; Analyzing and Interpreting Data

Crosscutting Concepts

Cause and Effect

Knowledge

Students know:
  • Qualitative scientific and technical information may include weather maps, diagrams, and visualizations, including radar and computer simulations.
  • Qualitative scientific information may be obtained through laboratory experiments.
  • Weather is the condition of the atmosphere as defined by temperature, pressure, humidity, precipitation, and wind.
  • An air mass is a large body of air with uniform temperature, moisture, and pressure.
  • Air masses flow from regions of high pressure to low pressure, causing weather at a fixed location to change over time.
  • Sudden changes in weather can result when different air masses collide.
  • The distribution and movement of air masses can be affected by landforms, ocean temperatures, and currents.
  • Relationships exist between observed, large-scale weather patterns and the location or movement of air masses, including patterns that develop between air masses (e.g., cold fronts may be characterized by thunderstorms).
  • Due to the complexity and multiple causes of weather patterns, probability must be used to predict the weather.*Local atmospheric conditions (weather) may be monitored by collecting data on temperature, pressure, humidity, precipitation, and wind.
  • Instruments may be used to measure local weather conditions. These instruments may include, but are not limited to, thermometers, barometers, and anemometers.
  • Weather events, specifically severe weather, can be predicted based on weather patterns.
  • Severe weather may include, but is not limited to, fronts, thunderstorms, hurricanes, tornadoes, blizzards, ice storms, and droughts.

Skills

Students are able to:
  • Make a claim, to be supported by evidence, to support or refute an explanation or model for a given phenomenon, including the idea that motions and complex interactions of air masses result in changes in weather conditions.
  • Identify evidence to support the claim from the given materials including qualitative scientific and technical information.
  • Evaluate the evidence for its necessity and sufficiency for supporting the claim.
  • Determine whether the evidence is sufficient to determine causal relationships between the motions and complex interactions of air masses and changes in weather conditions.
  • Consider alternative interpretations of the evidence and describe why the evidence supports the claim they are making, as opposed to any alternative claims.
  • Use reasoning to connect the evidence and evaluation to the claim that motions and complex interactions of air masses result in changes in weather conditions.
  • Use instruments to collect local weather data.
  • Monitor local weather data.
  • Use patterns observed from collected data to provide causal accounts for weather events and make predictions.

Understanding

Students understand that:
  • The complex patterns of the changes and the movement of water in the atmosphere, determined by winds, landforms, and ocean temperatures and currents, are major determinants of local weather patterns. Because these patterns are so complex, weather can only be predicted based on probability.
  • Instruments may be used to monitor local weather.
  • Weather patterns can be used to predict weather events.

Vocabulary

  • Integrate
  • Qualitative scientific information
  • Technical information
  • Weather map
  • Radar
  • Visualization
  • Weather
  • Air mass
  • Temperature
  • Pressure
  • Humidity
  • Precipitation
  • Wind
  • Uniform
  • Temperature
  • Moisture
  • Landform
  • Current
  • Probability
  • Atmosphere
  • Monitor
  • Instruments
  • Predict
  • Weather patterns
  • Severe weather
  • Temperature
  • Moisture
  • Pressure
  • Humidity
  • Precipitation
  • Wind
  • Atmosphere

SC15.6.12a

Use various instruments (e.g., thermometers, barometers, anemometers, wet bulbs) to monitor local weather and examine weather patterns to predict various weather events, especially the impact of severe weather (e.g., fronts, hurricanes, tornados, blizzards, ice storms, droughts).

SC15.6.13

Use models (e.g., diagrams, maps, globes, digital representations) to explain how the rotation of Earth and unequal heating of its surface create patterns of atmospheric and oceanic circulation that determine regional climates.

Unpacked Content

Scientific and Engineering Practices

Developing and Using Models

Crosscutting Concepts

Systems and System Models

Knowledge

Students know:
  • Radiation from the sun (solar energy) introduces heat (thermal energy) into Earth's atmosphere, water, land, and ice.
  • Thermal energy exists in the atmosphere, water, land, and ice as represented by temperature.
  • Thermal energy moves from areas of high temperature to areas of lower temperature either through the movement of matter, via radiation, or via conduction of heat from warmer objects to cooler objects.
  • Absorbing or releasing thermal energy produces a more rapid change in temperature on land compared to in water.
  • Absorbing or releasing thermal energy produces a more rapid change in temperature in the atmosphere compared to either on land or in water so the atmosphere is warmed or cooled by being in contact with land or the ocean.
  • The rotation of Earth and unequal heating of its surface create patterns of atmospheric and oceanic circulation.
  • Patterns of atmospheric and oceanic circulation vary by latitude, altitude, and geographic land distribution.
  • Higher latitudes receive less solar energy per unit of area than do lower latitudes, resulting in temperature differences based on latitude.
  • A general latitudinal pattern in climate exists where higher average annual temperatures are found near the equator and lower average annual temperatures are at higher latitudes.
  • Latitudinal temperature differences are caused by more direct light (greater energy per unit of area) at the equator (more solar energy) and less direct light at the poles (less solar energy).
  • A general latitudinal pattern of drier and wetter climates caused by the shift in the amount of air moisture during precipitation from rising moisture-rich air and the sinking of dry air.
  • In general, areas at higher altitudes have lower average temperatures than do areas at lower altitudes. Because of the direct relationship between temperature and pressure, given the same amount of thermal energy, air at lower pressures (higher altitudes) will have lower temperatures than air at higher pressures (lower altitudes).
  • Features on the Earth's surface, such as the amount of solar energy reflected back into the atmosphere or the absorption of solar energy by living things, affect the amount of solar energy transferred into heat energy.
  • Landforms affect atmospheric flows (e.g., mountains deflect wind and/or force it to higher elevation, known as the rain shadow effect).
  • The geographical distribution of land limits where ocean currents can flow.
  • The Earth's rotation causes oceanic and atmospheric flows to curve when viewed from the rotating surface of Earth (Coriolis force).
  • Fluid matter (i.e., air, water) flows from areas of higher density to areas of lower density (due to temperature or salinity). The density of a fluid can vary for several different reasons (e.g., changes in salinity and temperature of water can each cause changes in density). Differences in salinity and temperature can, therefore, cause fluids to move vertically and, as a result of vertical movement, also horizontally because of density differences.
  • Ocean circulation is dependent upon the transfer of heat by the global ocean convection cycle, which is constrained by the Coriolis effect and the outlines of continents.
  • Because water can absorb more solar energy for every degree change in temperature compared to land, there is a greater and more rapid temperature change on land than in the ocean. At the centers of landmasses, this leads to conditions typical of continental climate patterns.
  • Climates near large water bodies, such as marine coasts, have comparatively smaller changes in temperature relative to the center of the landmass. Land near the oceans can exchange thermal energy through the air, resulting in smaller changes in temperature. At the edges of landmasses, this leads to marine climates.
  • Variations in density due to variations in temperature and salinity drive a global pattern of interconnected ocean currents.
  • Radiation is the transfer of heat energy by electromagnetic wave motion. The transfer of energy from the sun across nearly empty space is accomplished primarily by radiation.
  • Radiation from the sun (solar energy) introduces heat (thermal energy) into Earth's atmosphere, water, land, and ice.
  • Convection is the transfer of heat by a current and can occur in a liquid or a gas.
  • When air near the ground is warmed by heat radiating from Earth's surface. The warm air is less dense, so it rises. As it rises, it cools. The cool air is dense, so it sinks to the surface. This creates a convection current.
  • Convection is the most important way that heat travels in the atmosphere.
  • Convection in the atmosphere is responsible for the redistribution of heat from the warm equatorial regions to higher latitudes and from the surface upward.

Skills

Students are able to:
  • Use a model of Earth and identify the relevant components of Earth's system, including inputs and outputs.
  • Describe the relationships between components of the model including how the rotation of Earth and unequal heating of its surface create patterns of atmospheric and oceanic circulation.
  • Articulate a statement that relates a given phenomenon to a scientific idea, including how the rotation of Earth and unequal heating of its surface create patterns of atmospheric and oceanic circulation.
  • Identify and describe the phenomenon under investigation, which includes how energy is distributed between Earth's surface and its atmosphere.
  • Identify and describe the purpose of the investigation, which includes providing evidence that energy from the sun is distributed between Earth's surface and its atmosphere by convection and radiation.
  • Collect and record data, according to the given investigation plan.
  • Evaluate the data to determine how energy from the sun is distributed between Earth's surface and its atmosphere by convection and radiation.

Understanding

Students understand that:
  • Weather and climate are influenced by interactions involving sunlight, the ocean, the atmosphere, ice, landforms, and organisms. These interactions vary with latitude, altitude, and local and regional geography, all of which can affect oceanic and atmospheric flow patterns.
  • The ocean exerts a major influence on weather and climate by absorbing energy from the sun, releasing it over time, and globally redistributing it through ocean currents.
  • Radiation from the sun (solar energy) introduces heat (thermal energy) into Earth's atmosphere, water, land, and ice and is represented by temperature. Thermal energy moves from areas of high temperature to areas of lower temperature on Earth's surface and in its atmosphere either through radiation or convection.

Vocabulary

  • Model
  • Diagram
  • Map
  • Globe
  • Digital representation
  • Rotation
  • Heat
  • Pattern
  • Atmosphere
  • Atmospheric circulation
  • Ocean
  • Oceanic circulation
  • Climate
  • Regional climate
  • Radiation
  • Sun
  • Solar energy
  • Thermal energy
  • Water
  • Land
  • Ice
  • Temperature
  • Matter
  • Conduction
  • Latitude
  • Altitude
  • Geography
  • Geographic land distribution
  • Precipitation
  • Absorption
  • Landform
  • Atmospheric flow
  • Mountain
  • Rain shadow effect
  • Coriolis force
  • Fluid
  • Density
  • Salinity
  • Global ocean convection cycle
  • Landmass
  • Marine
  • Coast
  • Variation
  • Radiation
  • Electromagnetic wave
  • Space
  • Convection
  • Current
  • Liquid
  • Gas
  • Equator

SC15.6.13a

Use experiments to investigate how energy from the sun is distributed between Earth’s surface and its atmosphere by convection and radiation (e.g., warmer water in a pan rising as cooler water sinks, warming one’s hands by a campfire).

SC15.6.14

Analyze and interpret data (e.g., tables, graphs, maps of global and regional temperatures; atmospheric levels of gases such as carbon dioxide and methane; rates of human activities) to describe how various human activities (e.g., use of fossil fuels, creation of urban heat islands, agricultural practices) and natural processes (e.g., solar radiation, greenhouse effect, volcanic activity) may cause changes in local and global temperatures over time.

Unpacked Content

Scientific and Engineering Practices

Analyzing and Interpreting Data

Crosscutting Concepts

Stability and Change

Knowledge

Students know:
  • Natural processes and/or human activities may have affected the patterns of change in global temperatures over the past century, leading to the current rise in Earth's mean surface temperature (global warming).
  • Natural processes may include factors such as changes in incoming solar radiation, the greenhouse effect, or volcanic activity.
  • Human activities may include factors such as fossil fuel combustion, the creation of urban heat islands, and agricultural activity.
  • Natural processes and/or human activities may lead to a gradual or sudden change in global temperatures in natural systems (e.g., glaciers and arctic ice, and plant and animal seasonal movements and life cycle activities).
  • Natural processes and/or human activities may have led to changes in the concentration of carbon dioxide and other greenhouse gases in the atmosphere over the past century.
  • Patterns in data connect natural processes and human activities to changes in global temperatures over the past century.
  • Patterns in data connect the changes in natural processes and/or human activities related to greenhouse gas production to changes in the concentrations of carbon dioxide and other greenhouse gases in the atmosphere.
  • Reducing the level of climate change and reducing human vulnerability to whatever climate changes do occur depend on the understanding of climate science, engineering capabilities, and other kinds of knowledge, such as understanding of human behavior and on applying that knowledge wisely in decisions and activities.

Skills

Students are able to:
  • Organize given data on various human activities, natural processes, and changes in local and global temperatures to allow for analysis and interpretation.
  • Analyze the data to identify possible causal relationships between human activities and natural processes and changes in local and global temperature over time.
  • Interpret patterns observed from the data to provide causal accounts for events and make predictions for events by constructing explanations.

Understanding

Students understand that:
  • Human activities and natural processes may affect local and global temperatures over time.

Vocabulary

  • Natural processes
  • Human activities
  • Global temperatures
  • Mean surface temperature
  • Global warming
  • Solar radiation
  • Greenhouse Effect
  • Volcanic activity
  • Fossil fuels
  • Combustion
  • Urban heat islands
  • Agriculture
  • Natural systems
  • Carbon dioxide (gases)
  • Greenhouse gases
  • Concentration
  • Atmosphere
  • Climate change

SC15.6.15

Analyze evidence (e.g., databases on human populations, rates of consumption of food and other natural resources) to explain how changes in human population, per capita consumption of natural resources, and other human activities (e.g., land use, resource development, water and air pollution, urbanization) affect Earth’s systems.

Unpacked Content

Scientific and Engineering Practices

Analyzing and Interpreting Data

Crosscutting Concepts

Cause and Effect

Knowledge

Students know:
  • Increases in the size of the human population or in the per capita consumption of a given population cause increases in the consumption of natural resources.
  • Natural resources are any naturally occurring substances or features of the environment that, while not created by human effort, can be exploited by humans to satisfy their needs or wants.
  • Per capita consumption is the average use per person within a population.
  • Natural resource consumption causes changes in Earth systems.
  • Engineered solutions alter the effects of human populations on Earth systems by changing the rate of natural resource consumption or reducing the effects of changes in Earth systems.
  • All human activity draws on natural resources and has both short and long-term consequences, positive as well as negative, for the health of people and the natural environment.
  • The consequences of increases in human populations and consumption of natural resources are described by science, but science does not make the decisions for the actions society takes.

Skills

Students are able to:
  • Organize given evidence regarding changes in human population, changes in per capita consumption of natural resources, human activities, and Earth's systems to allow for analysis and interpretation.
  • Analyze the data to identify possible causal relationships between changes in human population, changes in per capita consumption of natural resources, human activities, and Earth's systems.
  • Interpret patterns observed from the data to provide causal accounts for events and make predictions for events by constructing explanations.

Understanding

Students understand that:
  • Human population growth affects natural resource consumption and natural resource consumption has an effect on Earth systems; therefore, changes in human populations have a causal role in changing Earth systems.
  • Typically as human populations and per-capita consumption of natural resources increase, so do the negative impacts on Earth unless the activities and technologies involved are engineered otherwise.

Vocabulary

  • Population
  • Per capita
  • Consumption
  • Natural resource
  • Environment
  • Earth's systems
  • Consequences

SC15.6.16

Implement scientific principles to design processes for monitoring and minimizing human impact on the environment (e.g., water usage, including withdrawal of water from streams and aquifers or construction of dams and levees; land usage, including urban development, agriculture, or removal of wetlands; pollution of air, water, and land).*

Unpacked Content

Scientific and Engineering Practices

Constructing Explanations and Designing Solutions

Crosscutting Concepts

Cause and Effect

Knowledge

Students know:
  • Human activities have significantly altered the environment, sometimes damaging or destroying natural habitats and causing the extinction of other species.
  • Changes to Earth's environments can have different positive and negative impacts for different living things.
  • Typically as human populations and per-capita consumption of natural resources increase, so do the negative impacts on Earth unless the activities and technologies involved are engineered otherwise.
  • Technology is anything man-made that solves a problem or fulfills a desire.
  • Technology can be an object, system, or process.
  • Engineering is a systematic and often iterative approach to designing objects, processes, and systems to meet human needs and wants.
  • The Engineering Design Process (EDP) is a series of steps engineers use to guide them as they solve problems.
  • The EDP may include the following cyclical steps: ask, imagine, plan, create, and improve.
  • Scientific information and principles regarding human impact on the environment must be used to design a process or solution that addresses the results of a particular human activity.
  • Scientific information and principles regarding human impact on the environment must be used to design a process or solution that incorporates technologies that can be used to monitor negative effects that human activities have on the environment.
  • Scientific information and principles regarding human impact on the environment must be used to design a process or solution that incorporates technologies that can be used to minimize negative effects that human activities have on the environment.
  • Causal and correlational relationships between the human activity and the negative environmental impact must be distinguished to facilitate the design of the process or solution.
  • Criteria and constraints for the solution must be defined and quantified to include individual or societal needs or desires and constraints imposed by economic conditions (e.g., costs of building and maintaining the solution).
  • Criteria are the principles or standards by which the process or solution is judged.
  • Constraints are the limitations or restrictions on the process or solution.
  • The process or solution must meet the criteria and constraints.
  • Limitations of the use of technologies exist.

Skills

Students are able to:
  • Use scientific information and principles to generate a design solution for a problem related to human impact on the environment.
  • Identify relationships between the human activity and the negative environmental impact based on scientific principles.
  • Distinguish between causal and correlational relationships to facilitate the design of the solution.
  • Define and quantify, when appropriate, criteria and constraints for the solution.
  • Describe how well the solution meets the criteria and constraints, including monitoring or minimizing a human impact based on the causal relationships between relevant scientific principles about the processes that occur in, as well as among, Earth systems and the human impact on the environment.
  • Identify limitations of the use of technologies employed by the solution.

Understanding

Students understand that:
  • A process or solution must meet criteria and constraints, including monitoring or minimizing a human impact based on the causal relationships between relevant scientific principles about the processes that occur in, as well as among, Earth systems and the human impact on the environment.

Vocabulary

  • Habitat
  • Extinction
  • Species
  • Human Impact
  • Population
  • Per-capita consumption
  • Technology
  • Object
  • System
  • Process
  • Engineer
  • Engineering Design Process (EDP)
  • Monitor
  • Minimize
  • Solution
  • Causal and correlational relationships
  • Criteria
  • Constraints
  • Limitations

SC15.7.1

Engage in argument from evidence to support claims of the cell theory.

Unpacked Content

Scientific and Engineering Practices

Engaging in Argument from Evidence

Crosscutting Concepts

Structure and Function

Knowledge

Students know:
  • The presence or absence of cells in living and nonliving things.
  • The presence of cells in a variety of organisms, including unicellular and multicellular organisms.
  • Different types of cells within one multicellular organism.
  • Cells only arise from preexisting cells by division.
  • The cell is the structural and functional unit of all living things.

Skills

Students are able to:
  • Make a claim about a given explanation or model for a phenomenon, including the cell theory .
  • Identify and describe the given evidence that supports the claim.
  • Evaluate the evidence and identify its strengths and weaknesses.
  • Use reasoning to connect the necessary and sufficient evidence and construct the argument.
  • Present oral or written arguments to support or refute the given explanation or model for the phenomenon.

Understanding

Students understand that:
  • The three components of the cell theory:
  • All life forms are made from one or more cells.
  • Cells only arise from pre-existing cells.
  • The cell is the smallest unit of life.

Vocabulary

  • Cell
  • Cell theory
  • Unicellular
  • Multicellular
  • Living
  • Non-living
  • Organism
  • Evidence
  • Scientific argument
  • Claims

SC15.7.2

Gather and synthesize information to explain how prokaryotic and eukaryotic cells differ in structure and function, including the methods of asexual and sexual reproduction.

Unpacked Content

Scientific and Engineering Practices

Obtaining, Evaluating, and Communicating Information

Crosscutting Concepts

Structure and Function

Knowledge

Students know:
  • Prokaryotic cells are microscopic, single-celled organisms that have neither a distinct nucleus with a membrane nor other specialized organelles.
  • Prokaryotes include the bacteria and cyanobacteria.
  • The function of prokaryotic cells.
  • The reproductive methods of prokaryotic cells.
  • Eukaryotic cells consist of a cell or cells in which the genetic material is DNA in the form of chromosomes contained within a distinct nucleus.
  • Eukaryotes include all living organisms other than the eubacteria and archaebacteria.
  • The function of eukaryotic cells.
  • The reproductive methods of eukaryotic cells.

Skills

Students are able to:
  • Obtain information about cells, including structure, function, and method of reproduction, from published, grade-level appropriate material from multiple sources.
  • Determine and describe whether the gathered information is relevant.
  • Use information to explain how prokaryotic and eukaryotic cells differ.

Understanding

Students understand that:
  • Prokaryotic and eukaryotic cells differ in structure and function, as well as method of reproduction.

Vocabulary

  • Cell
  • Prokaryotic cells
  • Eukaryotic cells
  • Structure
  • Function
  • Asexual reproduction
  • Sexual reproduction
  • Mitosis
  • Meiosis
  • Chromosome
  • DNA
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