To determine the correct range of Earth's magnetic field strength, we need to examine measurements from geomagnetic observatories and scientific studies.
1. Measurement Units and Scale:
Earth's magnetic field is measured in microteslas (μT), where:
- 1 μT = 10-6 tesla
- This is equivalent to 1 nanotesla (nT) = 0.001 μT
2. Global Field Strength Measurements:
Scientific observations show:
- At the surface, field strength varies from 25 to 65 μT
- Equatorial regions: ~30-35 μT
- Polar regions: ~60-65 μT
- The field weakens with altitude (~0.3 μT at 1000 km)
3. Why This Range is Correct:
The 25-65 μT range accounts for:
- Latitudinal variations (stronger near poles)
- Local magnetic anomalies
- Temporal variations (daily and secular changes)
4. Ruling Out Other Options:
- 250-650 μT: Too strong (10× actual values)
- 2.5-6.5 μT: Too weak (10× smaller)
- 0.25-0.65 μT: Extremely weak (100× smaller)
5. Practical Examples:
For comparison:
- Typical fridge magnet: ~5000 μT
- MRI scanner: ~1,000,000 μT
- Earth's field is relatively weak but globally significant
Final Answer:
The Earth's magnetic field ranges between $\boxed{\text{25 and 65 microteslas}}$.