Unit Plan
CK-12 Foundation

Ck 12: Earth Science: Climate Change in Earth History

For Students 9th - 10th
[Free Registration/Login may be required to access all resource tools.] Traces changes in Earth's climate through Earth history, especially in the past 2,000 years.
Unit Plan
CK-12 Foundation

Ck 12: Earth Science: Geothermal Power

For Students 9th - 10th
[Free Registration/Login may be required to access all resource tools.] Presents the way geothermal energy is harnessed and some of its benefits and costs. Downloadable resources are also available.
Unit Plan
CK-12 Foundation

Ck 12: Earth Science: Effect of Atmospheric Circulation on Climate

For Students 9th - 10th
[Free Registration/Login may be required to access all resource tools.] Looks at how atmospheric circulation cells affect the climate of regions.
Unit Plan
CK-12 Foundation

Ck 12: Earth Science: Short Term Climate Change

For Students 9th - 10th
[Free Registration/Login may be required to access all resource tools.] Looks at how El Nino and La Nina affect the climate.
Unit Plan
CK-12 Foundation

Ck 12: Earth Science: Long Term Climate Change

For Students 9th - 10th
[Free Registration/Login may be required to access all resource tools.] Describes some factors that lead to long-term climate changes.
Unit Plan
CK-12 Foundation

Ck 12: Earth Science: Impacts of Hazardous Waste

For Students 9th - 10th
[Free Registration/Login may be required to access all resource tools.] Discusses the impacts of hazardous waste on the environment and human health, and the provisions of the Superfund Act.
Unit Plan
CK-12 Foundation

Ck 12: Earth Science: Effect of Continental Position on Climate

For Students 9th - 10th
[Free Registration/Login may be required to access all resource tools.] How close a region is to the ocean affects its climate.
Lesson Plan
Science Education Resource Center at Carleton College

Serc: Why Is the Earth Still Hot Inside?

For Teachers 11th - 12th
In this lesson, students conduct heat transfer experiments to investigate why the Earth is still hot at its core, even after billions of years since its formation. They will learn that the rate of heat transfer is dependent on an...