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Laboratory Manual for Introductory Geology 4e

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strength, resulting in an observed magnetic field stronger than today’s field (a positive

anomaly). If the paleomagnetic polarity is reversed, the rock’s paleomagnetism

subtracts from the modern field strength, and the result is a measurement weaker

than today’s field (a negative anomaly) (FIG. 2.10).

FIGURE 2.10 Components of the Earth’s magnetic field strength that produce marine

magnetic anomaly stripes.

Earth’s current

magnetic field

(strength and

direction)

Earth

Paleomagnetism Anomalously Earth’s current Paleomagnetism

+

(strength and

high magnetic field (reversed

= +

direction) magnetic field

polarity)

strength

=

Seafloor

Positive

anomaly

Earth

Seafloor

Anomalously

low

magnetic field

strength

Negative

anomaly

+

=

+ =

This pattern of marine magnetic anomalies has now been found at every midocean

ridge, proving that the magnetic reversals are truly worldwide events. Geologists

determined that as lava erupting at mid-ocean ridges cools, it records the

magnetic field polarity in effect at that time. If the Earth’s polarity reverses, new lava

will adopt the new polarity, and the older lava will yield a negative magnetic anomaly,

as shown in Figure 2.9. Exercise 2.4 shows the reasoning by which geologists connected

marine magnetic anomaly stripes in the oceans with plate tectonics theory.

EXERCISE 2.4

Interpreting Magnetic Anomaly Stripes at Mid-Ocean Ridges

Name:

Course:

Section:

Date:

In Figure 2.9a, compare the orientation of the magnetic anomaly stripes near the Mid-Atlantic Ridge with the orientation

of the ridge crest (highlighted by the red line). In Figure 2.9b, do the same for the Juan de Fuca Ridge (shown in yellow)

and its associated magnetic anomaly stripes.

(a) Are the individual anomalies oriented randomly? Are they parallel to the ridge crests? Oblique (at an angle) to the

ridge crests?

(b) Explain how the process of seafloor spreading can produce these orientations and relationships.

(c) Some magnetic anomaly stripes are wider than others. Knowing what you do about seafloor spreading and magnetic

reversals, suggest an explanation.

2.4 MODERN EVIDENCE FOR PLATE TECTONICS

35

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