Physical Geology
Other Ohio Science - Extended Learning Standards sets
Other Ohio Science - Extended Learning Standards sets
Minerals
- 1
Atoms and elements PG.M.1
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Complexity a
- a
Identify parts of an atom (e.g., protons, neutrons, electrons).PG.M.1.a
- a
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Complexity b
- b
Identify a diagram or model of an atom.PG.M.1.b
- b
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Complexity c
- c
Identify that all matter is made of atoms.PG.M.1.c
- c
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Learning Progression
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Build or recognize a model of an atom including protons, neutrons or electrons. PG.M.1.lp.a
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Identify that protons have a positive charge, neutrons are neutral, and electrons have a negative charge.PG.M.1.lp.b
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Recognize that valence electrons are in the outside layer of an atom. PG.M.1.lp.c
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Identify the valence electrons on a drawing or model on an atom.PG.M.1.lp.d
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Place labels (protons, neutrons, electrons) on a drawing of an atom.PG.M.1.lp.e
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Select the diagram that shows an atom from a set of drawings.PG.M.1.lp.f
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Engage with models or various visual representations of an atom.PG.M.1.lp.g
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- 2
Chemical bonding (ionic, covalent, metallic)PG.M.2
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Complexity a
- a
Represent a chemical compound with a ball-and-stick model or chemical formula.PG.M.2.a
- a
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Complexity b
- b
Recognize that a model (balland-stick or molecular geometries) or chemical formula represents a chemical compound.PG.M.2.b
- b
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Complexity c
- c
Identify that two elements combine to form a compound.PG.M.2.c
- c
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Learning Progression
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Use an atomic model and/or video to investigate that atoms interact to achieve 8 valence electrons (view the product).PG.M.2.lp.a
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Recognize that different atoms react in different ways (ionic and covalent bonding).PG.M.2.lp.b
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Recognize an ion as an atom that has gained or lost valence electrons (which changes their electrical charge).PG.M.2.lp.c
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Recognize that ionic bonding is an attraction between oppositely charged ions.PG.M.2.lp.d
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Recognize that in covalent bonding atoms share valence electrons so that each have 8.PG.M.2.lp.e
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Identify common minerals that are bonded ionically and covalently.PG.M.2.lp.f
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Recognize that an atom’s reactivity is based on its valence electrons. PG.M.2.lp.g
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Identify the valence electrons on a drawing or model on an atom.PG.M.2.lp.h
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Recognize that valence electrons are in the outside layer of an atom.PG.M.2.lp.i
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Engage with a model of an atom to locate the valence (outermost) electrons.PG.M.2.lp.j
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- 3
Crystallinity (crystal structure)PG.M.3
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Learning Progression
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Complex and advanced learning standards in Ohio’s New Learning Standards are not included in the extended standards.
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- 4
Criteria of a mineral (crystalline solid, occurs in nature, inorganic, defined chemical composition) PG.M.4
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Complexity a
- a
Match minerals with rock types in which they are commonly found.PG.M.4.a
- a
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Complexity b
- b
Identify a common mineral in a common rock.PG.M.4.b
- b
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Complexity c
- c
Recognize that minerals can be found in rocks.PG.M.4.c
- c
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Learning Progression
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Use a crystal growing kit to illustrate how crystals form.PG.M.4.lp.a
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Examine a variety of rocks and note the size of the crystals in the structure.PG.M.4.lp.b
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Watch videos that show how minerals are formed in a variety of rocks.PG.M.4.lp.c
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- 5
Properties of minerals (hardness, luster, cleavage, streak, crystal shape, fluorescence, flammability, density/specific gravity, malleability)PG.M.5
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Complexity a
- a
Sort minerals by cleavage, streak, hardness and fracture.PG.M.5.a
- a
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Complexity b
- b
Identify hardness and fracture as two characteristics to identify a mineral.PG.M.5.b
- b
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Complexity c
- c
Match minerals by properties (e.g., cleavage, streak, magnetism).PG.M.5.c
- c
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Learning Progression
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Investigate a sample rock and determine its identity by testing its properties.PG.M.5.lp.a
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Match a sample rock to its origin given a set of characteristics (e.g., using pictures, maps, illustrations, etc.).PG.M.5.lp.b
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Manipulate rocks to identify textural characteristics of each.PG.M.5.lp.c
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Engage with rocks by feeling the surface of each.PG.M.5.lp.d
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Igneous, Metamorphic and Sedimentary Rocks
- 1
Igneous • Mafic and felsic rocks and minerals • Intrusive (igneous structures: dikes, sills, batholiths, pegmatites) • Earth’s interior (inner core, outer core, lower mantle, upper mantle, Mohorovičić [Moho] discontinuity, crust) • Magnetic reversals and Earth’s magnetic field • Thermal energy within Earth • Extrusive (volcanic activity, volcanoes: cinder cones, composite, shield) • Bowen’s Reaction Series (continuous and discontinuous branches)PG.IMS.1
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Complexity a
- a
Compare how different environments change the type of igneous rock that is formed.PG.IMS.1.a
- a
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Complexity b
- b
Describe the properties of igneous rocks.PG.IMS.1.b
- b
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Complexity c
- c
Identify environments in which igneous rocks are formed.PG.IMS.1.c
- c
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Learning Progression
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Look at samples of igneous rock (e.g., granite, basalt), identify differences and recognize that they were formed in different environments.PG.IMS.1.lp.a
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Identify that granite makes up much of continental crust and basalt makes up much of our ocean floors.PG.IMS.1.lp.b
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View images or videos of volcanoes at various locations (e.g., edges of continents, mid-ocean spreading centers, hotspots).PG.IMS.1.lp.c
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Recognize that the cooled lava from volcanoes forms igneous rock (e.g., Hawaii).PG.IMS.1.lp.d
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View videos of volcanoes erupting.PG.IMS.1.lp.e
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- 2
Metamorphic • Pressure, stress, temperature, and compressional forces • Foliated (regional), nonfoliated (contact) • Parent rock and degrees of metamorphism • Metamorphic zones (where metamorphic rocks are found)PG.IMS.2
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Complexity a
- a
Compare how different environments change the type of metamorphic rock that is formed.PG.IMS.2.a
- a
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Complexity b
- b
Describe the properties of metamorphic rocks.PG.IMS.2.b
- b
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Complexity c
- c
Identify environments in which metamorphic rocks are formed.PG.IMS.2.c
- c
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Learning Progression
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Look at samples of metamorphic rocks and the rocks they formed from (e.g., slate from shale, marble from limestone), note the differences and similaritiesPG.IMS.2.lp.a
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Recognize that heat and pressure cause things to change. (e.g., examine a slice of white bread (crust removed), describe its properties, roll and squish it into a small ball, describe how its properties have changed, relate this to metamorphic rocks changing from other existing rocks (heat and pressure from your hand). PG.IMS.2.lp.b
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- 3
Sedimentary • Division of sedimentary rocks and minerals (chemical, clastic/physical, organic) • Depositional environmentsPG.IMS.3
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Complexity a
- a
Compare how different environments change the type of sedimentary rock that is formed.PG.IMS.3.a
- a
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Complexity b
- b
Describe the properties of sedimentary rocks.PG.IMS.3.b
- b
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Complexity c
- c
Identify environments in which sedimentary rocks are formed.PG.IMS.3.c
- c
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Learning Progression
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Predict what would happen if lots of pressure squeezed the sediments (they would cement together).PG.IMS.3.lp.a
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Describe locations where sedimentary rocks can form (e.g., desserts, oceans).PG.IMS.3.lp.b
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Build a model of the formation of sedimentary rock (e.g., shake sand and dirt in a jar of water, let it sit and describe what happens (settles to the bottom), relate this to sediments falling to the bottom of an ocean).PG.IMS.3.lp.c
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- 4
Ocean • Tides (daily, neap, and spring) • Currents (deep and shallow, rip and longshore) • Thermal energy and water density • Waves • Ocean features (ridges, trenches, island systems, abyssal zone, shelves, slopes, reefs, island arcs) • Passive and active continental margins • Transgressing and regressing sea levels • Streams (channels, streambeds, floodplains, cross-bedding, alluvial fans, deltas)PG.IMS.4
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Complexity a
- a
Use data to see how the sea level changes with the tides in a given location.PG.IMS.4.a
- a
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Complexity b
- b
Describe how the tides are controlled by the moon. PG.IMS.4.b
- b
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Complexity c
- c
Identify a reason for a change in sea level. (e.g., tides, currents, waves, etc.).PG.IMS.4.c
- c
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Learning Progression
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Given a tide table, identify the pattern (amount of time) that occurs between high and low tide and high tide to next high tide.PG.IMS.4.lp.a
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Watch videos on ocean currents (e.g., NASA, NOAA, Bill Nye) to look at patterns; understand that ocean currents move materials around the ocean and affect the climate on Earth.PG.IMS.4.lp.b
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View time lapse videos of tides in the ocean, recognize that the water level changes due to the tides.PG.IMS.4.lp.c
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Recognize that tides are controlled by the gravitational attraction between the moon and Earth. PG.IMS.4.lp.d
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Engage by watching convection in a tub of water to observe how temperature differences make water move in currents (heat a tub of water under one side only, sprinkle in pepper and watch the circulation pattern).PG.IMS.4.lp.e
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Earth’s History
- 1
The geologic rock record • Relative and absolute age • Principles to determine relative age • Original horizontality • Superposition • Cross-cutting relationships • Absolute age • Radiometric dating (isotopes, radioactive decay) • Correct uses of radiometric dating • Combining relative and absolute age data • The geologic time scale • Comprehending geologic time • Climate changes evident through the rock record • Fossil recordPG.EH.1
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Complexity a
- a
Describe how technology assists in determining the age of rocks (e.g., radiometric dating).PG.EH.1.a
- a
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Complexity b
- b
Identify that in a cross-section of rock, the layer on top is the youngest layer and the layer on the bottom is the oldest (assuming no geological process has shifted the layers).PG.EH.1.b
- b
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Complexity c
- c
Identify changes across layers (crosssection) of rocks.PG.EH.1.c
- c
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Learning Progression
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Explain that radiometric dating traces radioactive materials in the rock to determine age. PG.EH.1.lp.a
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Recognize that there are a variety of methods to determine the age of rock.PG.EH.1.lp.b
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Given a cross section of rock determine the relative age in an undisturbed section. PG.EH.1.lp.c
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Model the formation of rock layers and relate the age of the layers to the Law of Superposition.PG.EH.1.lp.d
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Identify the layers that can be seen within a cross section (e.g., highway cut, Grand Canyon).PG.EH.1.lp.e
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Engage with a model of a cross section of a highway cut or rock layers.PG.EH.1.lp.f
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Plate Tectonics
- 1
Internal Earth • Seismic waves • S and P waves • Velocities, reflection, refraction of wavesPG.PT.1
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Complexity a
- a
Analyze which earthquake was larger based on a seismographic report or readout.PG.PT.1.a
- a
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Complexity b
- b
Describe how a Richter scale is used as a tool to measure the seismic waves of an earthquake.PG.PT.1.b
- b
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Complexity c
- c
Recognize that a Richter scale is a tool used to measure intensity of earthquakes.PG.PT.1.c
- c
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Learning Progression
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Recognize that the “wiggles” on the seismograph represents energy waves traveling through Earth.PG.PT.1.lp.a
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Given two seismograms choose the one that represents a stronger earthquake.PG.PT.1.lp.b
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Compare seismograms, recognize that large “wiggles” mean more shaking of the ground.PG.PT.1.lp.c
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Recognize that the Richter scale uses numbers to describe the strength of earthquakes (larger numbers are 10 times stronger than the number before).PG.PT.1.lp.d
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Recognize that earthquakes have different strengths.PG.PT.1.lp.e
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Watch video footage of small and large earthquakes. PG.PT.1.lp.f
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- 2
Structure of Earth (Note: specific layers were part of grade 8) • Asthenosphere • Lithosphere • Mohorovičić (Moho) boundary • Composition of each of the layers of Earth • Gravity, magnetism and isostasy • Thermal energy (geothermal gradient and heat flow)PG.PT.2
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Learning Progression
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Complex and advanced learning standards in Ohio’s New Learning Standards are not included in the extended standards.
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- 3
Historical review (Note: this would include a review of continental drift and sea-floor spreading found in grade 8) • Paleomagnetism and magnetic anomalies • PaleoclimatologyPG.PT.3
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Learning Progression
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Complex and advanced learning standards in Ohio’s New Learning Standards are not included in the extended standards.
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- 4
Plate motion (Note: introduced in grade 8) • Causes and evidence of plate motion • Measuring plate motion • Characteristics of oceanic and continental plates • Relationship of plate movement and geologic events and features • Mantle plumesPG.PT.4
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Complexity a
- a
Describe how the continents used to be connected in one super continent of Pangaea and have moved due to tectonic forces.PG.PT.4.a
- a
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Complexity b
- b
Recognize that the shape of the continents is evidence of plate motion (e.g., they fit together like puzzle pieces).PG.PT.4.b
- b
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Complexity c
- c
Identify the crust as the location of the continental plates. PG.PT.4.c
- c
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Learning Progression
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Recognize that plate motion has caused the continents to shift. Use video footage of Hawaii to illustrate this type of activity.PG.PT.4.lp.a
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Use cut outs of the modern continents, try to fit them together like a puzzle, understand that the fact they fit is evidence they were once joined.PG.PT.4.lp.b
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Review maps of Earth’s continents over the past 300,000 years to identify changes.PG.PT.4.lp.c
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Recognize that the surface of Earth has changed.PG.PT.4.lp.d
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Identify the name of the previous supercontinent as Pangaea.PG.PT.4.lp.e
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Watch a video of a flower blooming or a glacier moving in real time and in fast motion, recognize that sometimes movement is too slow to see.PG.PT.4.lp.f
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Earth’s Resources
- 1
Energy resources • Renewable and nonrenewable energy sources and efficiency • Alternate energy sources and efficiency • Resource availability • Mining and resource extractionPG.ER.1
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Complexity a
- a
Identify factors to consider before mining for mineral resources (e.g., cost, pollution, effects on wildlife).PG.ER.1.a
- a
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Complexity b
- b
Identify the effect that mining for a mineral resource has on an area.PG.ER.1.b
- b
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Complexity c
- c
Recognize that minerals are a resource.PG.ER.1.c
- c
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Learning Progression
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Provide pictures of mining sites and describe the changes to the environment. Describe how those changes impact wildlife. PG.ER.1.lp.a
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Understand that renewable means more can be made is a short period of time.PG.ER.1.lp.b
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Understand that nonrenewable means that once it is used there is no way to get more in a reasonable time frame.PG.ER.1.lp.c
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Recognize that minerals are a nonrenewable resource.PG.ER.1.lp.d
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Recognize that minerals are extracted through mining.PG.ER.1.lp.e
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Recognize that minerals are used in our everyday materials.PG.ER.1.lp.f
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Observe and manipulate various minerals.PG.ER.1.lp.g
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- 2
Air • Primary and secondary contaminants • Greenhouse gasesPG.ER.2
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Complexity a
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Describe how greenhouse gas effects the atmosphere.PG.ER.2.a
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Complexity b
- b
Identify a cause and effect of specific air pollution problem (e.g., smoke from a factory causes haze in the air).PG.ER.2.b
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Complexity c
- c
Identify an air contaminant.PG.ER.2.c
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Learning Progression
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Identify greenhouse gases (e.g., carbon dioxide, water vapor) and how they can impact the atmosphere and environment.PG.ER.2.lp.a
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Use Google Earth to view a local area to determine what exists in an area and what products are produced and how that impacts an area (e.g., farms, housing developments, industries, nature reserves).PG.ER.2.lp.b
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Identify an effect of a primary and secondary contaminant.PG.ER.2.lp.c
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Identify sources of air pollution.PG.ER.2.lp.d
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Recognize when there is a change in the air (hot, cold, odor, scent, humid).PG.ER.2.lp.e
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Engage with the air by taking a deep breath and exhaling.PG.ER.2.lp.f
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- 3
Water • Potable water and water quality • Hypoxia, eutrophicationPG.ER.3
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Complexity a
- a
Describe why it is important to have clean drinking water.PG.ER.3.a
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Complexity b
- b
Identify a water contaminant. PG.ER.3.b
- b
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Complexity c
- c
Identify a drinking water source.PG.ER.3.c
- c
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Learning Progression
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Sort water sources as potable and nonpotable.PG.ER.3.lp.a
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Describe characteristics of potable and nonpotable water or factors that make it potable/non potable.PG.ER.3.lp.b
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In your region, identify where your water originates.PG.ER.3.lp.c
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Recognize that the water used for drinking has to be processed to be used.PG.ER.3.lp.d
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Recognize that some water is potable and some is not.PG.ER.3.lp.e
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Identify various sources of water.PG.ER.3.lp.f
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Actively participate in a discussion about water that is good for drinking versus water that would not be. PG.ER.3.lp.g
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- 4
Soil and sediment • Desertification • Mass wasting and erosion • Sediment contaminationPG.ER.4
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Complexity a
- a
Describe how erosion can change an environment.PG.ER.4.a
- a
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Complexity b
- b
Identify a reason for erosion. PG.ER.4.b
- b
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Complexity c
- c
Define erosion as the movement of Earth’s materials.PG.ER.4.c
- c
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Learning Progression
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Identify the agents of erosion. PG.ER.4.lp.a
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Recognize a landform or area that resulted from erosion.PG.ER.4.lp.b
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Examine before and after images of erosion.PG.ER.4.lp.c
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Observe erosion (video) in action.PG.ER.4.lp.d
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Glacial Geology
- 1
Glaciers and glaciation • Evidence of past glaciers (including features formed through erosion or deposition) • Glacial deposition and erosion (including features formed through erosion or deposition) • Data from ice cores • Historical changes (glacial ages, amounts, locations, particulate matter, correlation to fossil evidence) • Evidence of climate changes throughout Earth’s history • Glacial distribution and causes of glaciation • Types of glaciers: continental (ice sheets, ice caps), alpine/valley (piedmont, valley, cirque, ice caps) • Glacial structure, formation, and movement PG.GG.1
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Complexity a
- a
Describe land features that were formed through either erosion or deposition from glaciers.PG.GG.1.a
- a
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Complexity b
- b
Identify land features in Ohio that were formed by glaciers.PG.GG.1.b
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Complexity c
- c
Identify that glaciers consist mainly of ice.PG.GG.1.c
- c
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Learning Progression
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Use a map to trace the movement of glaciers globally for the last 20 years.PG.GG.1.lp.a
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Identify features on a map that are a direct result of glaciation (e.g., the Great Lakes, glacial grooves on Kelleys Island).PG.GG.1.lp.b
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Use pictures to identify the different kinds of glaciers (e.g., valley, piedmont, glaciers, cirque, tidewater).PG.GG.1.lp.c
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Look at a series of pictures from around Ohio, sort them into glaciated and unglaciated areas.PG.GG.1.lp.d
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Actively engage in an activity that demonstrates movement and effects of a glacier. Push a large ice cube across a container of sand, dirt and pebbles, to recognize that ice blocks (glaciers) can move materials. Push down to make the ice cube dig a hole in the sand, relate this to the formation of the Great Lakes.PG.GG.1.lp.e
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Frequently asked questions
- What grade levels do these standards cover?
- Grade 9, Grade 10, Grade 11, and Grade 12
- Where can I read the official document?
- Ohio’s Learning Standards – Extended with Learning Progressions Science
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