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Earth's Magnetic Field Lesson

Earth's Magnetic Field — Strength, Polarity & Pole Flips

GED Science Practice — Reading graphs, tables, and scientific passages

What is Earth's magnetic field?

Many people think of Earth's magnetic field as a stationary bubble that protects humans from harmful radiation and helps guide ships and airplanes. In actuality, the field is dynamic — meaning it undergoes continuous change or activity.

Key facts from the passage:

  • Earth's overall magnetic field strength has decreased by nearly 10% since it was first regularly measured around 1900
  • The current magnetic poles are moving — they are not fixed in place
  • Some scientists believe this signals the beginning of a magnetic pole flip
  • Pole flips have happened many times in Earth's past — there is solid geological evidence

Earth's magnetic field — animated diagram

Earth's magnetic field lines extend from pole to pole, forming a protective magnetosphere

Dynamic
In the passage, "dynamic" means continuous change or activity. The field is NOT stationary — it shifts in strength and direction over time.
Magnetosphere
The region around Earth controlled by its magnetic field. It shields us from harmful solar radiation — like an invisible force field.
Polarity (N/R)
Normal (N) = current direction. Reversed (R) = opposite direction. A "pole flip" changes N to R or R to N over thousands of years.
10²³ AM²
The unit for magnetic field strength in the data table. A very large number — these measurements describe the total strength of Earth's entire magnetic field.
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