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Teacher companion

A quick reference for using this book in a Regents Earth Science classroom: which interactive to project for each unit, and the misconceptions worth heading off before they take root. Everything here points back into the book.

This companion is written to sit alongside the New York State P-12 Science Learning Standards and the Earth and Space Sciences course. Reference Table page numbers throughout the book refer to the 2026 Revised Edition. Every chapter closes with key takeaways, Reference Table connections, and Regents-style practice; the cumulative review page and per-unit checkpoints let students self-assess.

Unit 1 · Measurement and Earth Science Skills

1.1 Observations and Measurement

Project in class

the float-or-sink density lab when introducing why ice floats and how density is independent of sample size

Common misconceptions

  • “Density changes with sample size.” it does not. A small and a large piece of the same rock have the same density. Cut the density lab specimen in half on the board to show the ratio holds.
  • “Percent deviation and percent are the same.” percent deviation is the difference between the measured and accepted values, divided by the accepted value and turned into a percent. The most common error is dividing by the measured value instead.
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Unit 2 · Mapping the Earth

2.1 Locating Points · 2.2 Topographic Maps

Project in class

the Polaris altitude lab to connect latitude to the altitude of Polaris in one move

the gradient lab right before assigning gradient calculations

Common misconceptions

  • “Contour lines can cross.” they never cross or branch; each line is one elevation.
  • “Streams flow downhill on the map any old way.” contour lines bend upstream (point toward higher elevation) where they cross a stream, so the V points upstream, opposite the flow.
  • “Longitude gives you latitude.” Polaris altitude gives latitude in the Northern Hemisphere; longitude comes from time difference from Greenwich at 15 degrees per hour.
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Unit 3 · Dynamic Earth (Tectonics)

3.1 Interior · 3.2 Plate Boundaries · 3.3 Earthquakes · 3.4 Volcanoes

Project in class

the Earth interior explorer to read temperature, pressure, and density at any depth against page 10

the boundary explorer and the live quake map to classify boundaries and see real seismicity

the hot spot island-chain visualization when explaining why island chains age away from the source

Common misconceptions

  • “The crust and the lithosphere are the same.” the lithosphere is crust plus the rigid top of the mantle, about 100 km thick.
  • “Convection happens in the liquid outer core.” mantle convection (in solid rock that flows slowly) drives the plates; the outer core convection drives the magnetic field.
  • “Deeper earthquakes happen everywhere.” deep-focus quakes only occur in subducting slabs, which is itself evidence of subduction.
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Unit 4 · Minerals, Rocks, and the Rock Cycle

4.1 Minerals · 4.2 Rock Families · 4.3 Rock Cycle

Project in class

the mineral ID lab to model using the page-16 properties chart with hardness and streak

the rock cycle journey to show that any rock can become any other with no fixed starting point

Common misconceptions

  • “The rock cycle is a fixed circle with a start.” it has no start or required order; a rock can take many paths.
  • “Bigger crystals mean the rock formed fast.” the opposite. Large crystals mean slow cooling deep underground (intrusive).
  • “Ice cannot be a mineral.” ice fits every rule: natural, inorganic, solid, definite composition, crystalline.
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Unit 5 · Surface Processes

5.1 Weathering and Soil · 5.2 Erosion and Deposition

Project in class

the weathering-climate lab to show how temperature and moisture drive chemical weathering rate

the stream velocity lab built on the page-6 velocity-particle graph

Common misconceptions

  • “Weathering and erosion are the same.” weathering breaks rock in place; erosion carries the pieces away.
  • “Faster water dissolves bigger rocks.” faster water carries bigger particles; it is about transport energy, not dissolving.
  • “Well-sorted and poorly-sorted look random.” water sorts by size as it slows; glaciers dump unsorted till. Sorting tells you the agent.
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Unit 6 · Landscapes

6.1 Landscape Development

Project in class

the region classifier lab to practice reading elevation and bedrock structure into a region type

Common misconceptions

  • “The Catskills are mountains.” they are a plateau: high but flat-lying, undistorted bedrock. This is the single most common New York landscape trap.
  • “Steep slopes always mean recent uplift.” arid climates keep slopes steep and angular; humid climates round them. Climate shapes slope form.
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Unit 7 · Geologic History

7.1 Reading the Rock Record

Project in class

the half-life lab to make radioactive decay and the parent-daughter ratio concrete

the superposition stepper to build a cross section event by event

Common misconceptions

  • “Half-life means the sample halves in age.” after one half-life, half the parent atoms remain; the elapsed time is one half-life, not half the age.
  • “Index fossils are just old fossils.” a good index fossil is widespread but short-lived, so it pins a narrow time.
  • “Carbon-14 dates dinosaur bones.” C-14 only reaches tens of thousands of years; dinosaurs need slow clocks like uranium-238.
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Unit 8 · Meteorology

8.1 Atmosphere and Moisture · 8.2 Pressure and Wind · 8.3 Fronts and Storms

Project in class

the humidity lab to link temperature, dew point, and relative humidity

the station model decoder to practice reading and building station models

Common misconceptions

  • “High relative humidity means a lot of water.” it means the air is near saturation for its temperature; cold saturated air holds little water.
  • “Wind blows from low toward high pressure.” air flows from high toward low pressure; the Coriolis effect then curves it.
  • “Fronts are storms.” a front is a boundary between air masses; the weather comes from what happens along it.
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Unit 9 · Climate

9.1 What Controls Climate

Project in class

the climate factor lab to isolate latitude, elevation, water, and mountains one at a time

Common misconceptions

  • “Weather and climate are the same.” weather is now; climate is the long-term average pattern.
  • “Coastal and inland places at the same latitude have the same climate.” water moderates temperature, so marine climates have smaller annual ranges than continental ones.
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Unit 10 · Astronomy

10.1 Motions and Seasons · 10.2 The Moon · 10.3 Gravity and the Solar System · 10.4 Stars and the Universe

Project in class

the seasons lab to show the noon sun altitude and daylight hours change through the year at our latitude

the moon phase machine the dual-panel orbit-and-phase view for why we see phases

the Scale of the Universe visualization to give students a felt sense of cosmic scale

Common misconceptions

  • “Seasons are caused by distance from the sun.” they are caused by the 23.5-degree axial tilt; Earth is actually closest to the sun in January.
  • “The moon has a permanently dark side.” it has a far side we never see from Earth, but every part gets sunlight over a month.
  • “Heavier objects fall or orbit faster.” gravity depends on mass and distance; orbital speed depends on distance from the central body, not the satellite mass.
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Unit 11 · Human Impact and Sustainability

11.1 People and Earth Systems

Project in class

the greenhouse effect lab to show CO2 concentration driving warming

Common misconceptions

  • “The greenhouse effect is inherently bad.” the natural greenhouse effect keeps Earth about 33 C-degrees warmer and livable; the concern is the human-driven increase.
  • “The ozone hole causes global warming.” they are separate issues; ozone depletion is about UV protection, warming is about heat-trapping gases.
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