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
Magnetic field strength — 20th century (1900–2000)
Tap any point on the chart to explore. This graph shows the data from the passage.
Magnetic Field Strength (10²³ AM²) measured from 1900 to 2000
What does the graph show?
Look carefully at the shape of the line. The GED question asks which statement correctly describes the graph.
GED Question 1 — Graph interpretation
"Which statement describes the graph's representation of magnetic field strength during the twentieth century?"
The line is NOT a straight diagonal — it changes slope at different periods. A constant rate would be a perfectly straight line.
The steepest drop is actually in the first half (1900–1940), not just the last half. The last quarter (1970–2000) is steep again, but "last half" is too broad.
The rate of decline changes — steep early, slower in the middle, steep again at the end. "Variable rates" perfectly describes a line that isn't straight but always goes down.
The graph shows a consistent decline. The field strength never increases during this period — the line only goes downward.
Earth's Magnetic Field Polarity Through Time
Data for the last 2 million years (my), sampled at 100,000-year intervals. N = Normal polarity. R = Reversed polarity.
| Age of Rock (my) | Mag. Field Strength (10²³ AM²) | Polarity |
|---|---|---|
| 0.1 | 0.8 | N |
| 0.2 | 0.9 | N |
| 0.3 | 0.8 | N |
| 0.4 | 0.8 | N |
| 0.5 | 0.6 | N |
| 0.6 | 0.8 | N |
| 0.7 | 0.6 | N |
| 0.8 | 0.4 | R |
| 0.9 | 0.8 | R |
| 1.0 | 0.4 | N |
| 1.1 | 0.6 | R |
| 1.2 | 0.2 | R |
| 1.3 | 0.6 | R |
| 1.4 | 0.6 | R |
| 1.5 | 0.8 | R |
| 1.6 | 0.8 | R |
| 1.7 | 0.8 | R |
How minerals record polarity
When volcanic rocks cool, minerals inside them are "frozen" into alignment with Earth's magnetic field at that moment — like a tiny compass needle locked in rock. By measuring these rocks, scientists can reconstruct Earth's magnetic history millions of years back.
What is a magnetic pole flip?
A magnetic pole flip (also called a geomagnetic reversal) is when Earth's magnetic north and south poles swap positions. This process:
- Takes place over the course of a few centuries to thousands of years
- During the flip, the field weakens significantly before rebuilding in the opposite direction
- Has happened hundreds of times in Earth's 4.5-billion-year history
- The last full reversal was about 780,000 years ago
- There is solid geological evidence in rock mineral alignment that this has occurred many times
GED Question 2 — Evidence for pole flip hypothesis
"Which piece of evidence supports the hypothesis that Earth is currently at the beginning of a magnetic pole flip?"
This is a fact from the table, but it does NOT support the hypothesis that a flip is beginning — if anything, it shows stability. Long normal periods can precede a flip, but this alone is not evidence a flip is starting now.
This explains HOW we know about past flips — it's a method of measurement, not evidence that a flip is currently beginning.
This describes what happens during a flip — it's a definition, not evidence that one is happening right now.
This directly supports the hypothesis. A weakening field + moving poles are the two observable signs that scientists associate with the beginning of a pole flip. This is current, measurable evidence — not historical data or definitions.
GED Question 3 — Vocabulary in context
"What is the meaning of dynamic as it relates to the magnetic field in paragraph 1?"
This is one definition of "dynamic" in everyday use, but the passage contrasts "dynamic" with "stationary" — so it's about change and movement, not energy level.
The passage says the field "is dynamic" right after saying people wrongly think of it as "stationary." The contrast makes the meaning clear: dynamic = always changing, not fixed.
While the magnetic field does exert force, this doesn't fit the context. The passage is describing the field's nature (changing vs. fixed), not what force it creates.
Again, this misses the stationary vs. changing contrast the passage is making. The word "dynamic" here specifically contrasts with "stationary bubble."
GED strategy — passage + graph + table questions
All three correct answers summarized
Q1 (Graph): "The strength had variable rates of decline during the twentieth century." — The line steepens, flattens, then steepens again. Not constant. Never increases.
Q2 (Evidence): "The overall strength has decreased by nearly 10% since 1900, and the poles are moving." — Current observable data directly supporting the pole-flip hypothesis.
Q3 (Vocabulary): "Continuous change or activity." — The passage contrasts "dynamic" with "stationary," making the meaning clear from context.
