Two phenomena — eclipses and seasons — both depend on the same Earth-Sun-Moon system, yet each involves a different combination of alignment, tilt, and shadow geometry that students often confuse until they build a model.
The key difference is whose shadow falls on what. In a solar eclipse the Moon blocks sunlight from reaching part of Earth. In a lunar eclipse Earth's shadow falls on the Moon. In both cases, the shadow has a dark inner zone — the umbra — and a lighter outer zone — the penumbra.
Students use a flashlight, ball, and globe to model how Earth's shadow creates a lunar eclipse, observing both the umbra and penumbra firsthand.
A reference poster labels the umbra and penumbra zones for a lunar eclipse, with a real photograph of the moon during totality.
Structured writing questions cover both solar and lunar eclipses, asking students to compare and explain using evidence from the model and readings.
A three-section foldable lets students organize what is unique to solar eclipses, what is unique to lunar eclipses, and what both types share.
Seasons are caused by Earth's axial tilt of 23.5°, not by distance from the Sun. As Earth orbits, the Northern and Southern Hemispheres take turns being tilted toward the Sun, receiving more direct sunlight and experiencing longer days.
A table-top model shows Earth tilted on its axis orbiting a light source, making the connection between axial tilt and seasonal sunlight angles visible and tangible.
A labeled diagram shows Earth at each solstice and equinox, with details on hours of sunlight, Arctic Circle conditions, and the dates for each position.
This page is one part of a full NGSS-aligned unit covering lunar phases, tides, eclipses, seasons, the Big Bang, gravity, galaxies, the solar system, planets, the geologic time scale, and more — with hands-on models, projects, and Check for Understanding pages throughout.
View the Full Unit on TPT