Difficulty distribution
How the classified questions are distributed by difficulty.
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Practice Magnetic Methods - Advanced topics in Geophysics - Geology & Geophysics previous year questions organised from real papers, with year-wise coverage and clear topic navigation.
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How the classified questions are distributed by difficulty.
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Top topics across the included previous year papers.
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Question coverage for the most populated papers. Every active PYP paper remains listed below.
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| Paper name | Year | Attempt | |
|---|---|---|---|
Geology and Geophysics - Geophysics (GG) 20262026 | 2026 |
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Geology & Geophysics (GG) 2025 [Session 1]2025 | 2025 | |
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Geology & Geophysics (GG) 2025 [Session 2]2025 | 2025 | |
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Geology & Geophysics (GG) 2024 [Session 1]2024 | 2024 | |
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Geology & Geophysics (GG) 2024 [Session 2]2024 | 2024 | |
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Geology & Geophysics (GG) 2023 [Session 2]2023 | 2023 | |
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Geology & Geophysics (GG) 20222022 | 2022 | |
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Geology & Geophysics (GG) 20212021 | 2021 | |
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Geology & Geophysics (GG) 20202020 | 2020 | |
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Geology & Geophysics (GG) 20192019 | 2019 | |
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Geology & Geophysics (GG) 20182018 | 2018 | |
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Geology & Geophysics (GG) 20172017 | 2017 | |
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Geology & Geophysics (GG) 20162016 | 2016 | |
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Geology & Geophysics (GG) 20152015 | 2015 | |
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Geology & Geophysics (GG) 20142014 | 2014 | |
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Geology & Geophysics (GG) 20132013 | 2013 | |
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Geology & Geophysics (GG) 20122012 | 2012 | |
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Geology & Geophysics (GG) 20112011 | 2011 | |
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Geology & Geophysics (GG) 20102010 | 2010 | |
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Geology & Geophysics (GG) 20092009 | 2009 | |
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Geology & Geophysics (GG) 20082008 | 2008 | |
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Geology & Geophysics (GG) 20072007 | 2007 | |
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Practice every matching question in batches of 20, with every available option.
The liquid used in the sensor of a Proton Precession Magnetometer should be rich in
A successful combination of geophysical methods for exploration of kimberlite pipe is
In magnetic prospecting scalar magnetometers are used. Then, the prime assumption involved in magnetic data acquisition is
The relative intensities of induced and remanent magnetization are commonly expressed in terms of
If in a magnetic dipole 'm' represents poles of equal strength and 'l' represents the distance between the two poles, then the magnetic moment of dipole is
Variation of the geomagnetic field observed over the last 500 years indicates that the dipole moment of earth’s magnetic field has been
In magnetic data reduction, the altitude correction at magnetic equator is 0.015 nT/m. Altitude correction (in nT/m) at the magnetic poles is

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