Free Course Image Introduction to Marine Magnetometry

Free online course Introduction to Marine Magnetometry

Duration of the online course: 46 minutes

New

Build skills in marine magnetometry: learn how seabed surveys detect anomalies, design better grids, and earn a free course certificate to boost your profile.

In this free course, learn about

  • Core principles and terminology of marine magnetometry
  • Main factor controlling magnetometer detection range for a target
  • How magnetic anomaly strength changes with target mass and distance (nT vs distance)
  • How objects distort Earth’s magnetic field and create measurable anomalies
  • Role of transverse radiometer in establishing/maintaining a survey grid
  • Key survey design considerations for marine magnetometer work (line spacing, altitude, speed)
  • Interpreting anomaly shapes and signatures for different target types
  • Expected magnetic anomaly characteristics for hollow objects in a survey grid

About the free online course

Marine magnetometry is a powerful way to read hidden patterns beneath the sea, from small man‑made objects to broader geological signals. In this free online course, you will learn how magnetometers work in marine settings and why the surrounding environment, instrument setup, and survey decisions can drastically affect what you detect and how confidently you interpret it. The focus is practical and concept-driven, helping you connect core geography and Earth science ideas to real survey outcomes.

You will explore what controls detection range and why distance matters so much when measuring magnetic anomalies. By building an intuitive grasp of field strength and how signals change with separation, you will be better prepared to judge what a magnetometer can realistically find during a survey and what may remain invisible. You will also learn how objects distort the Earth’s magnetic field and how that distortion shows up in measurements, which is essential for distinguishing meaningful anomalies from background variation.

Survey design is a central theme throughout the course. You will consider how to plan a survey grid, how spacing and coverage influence the chance of locating a target, and how to think about instruments used to support reliable mapping across transects. You will also work through common interpretive challenges, including how different object shapes and internal structures can change the anomaly you expect to observe, such as the signatures produced by hollow targets compared with solid ones.

Because the course includes targeted questions and exercises, you will not only absorb terminology but also practice applying it to realistic scenarios. This makes the learning useful for students of geography, marine science, and related school subjects, as well as anyone curious about how geophysical surveying supports marine research, underwater search, and environmental or archaeological investigations.

Course content

  • Video class: Introduction to Marine Magnetometry - part 1 09m
  • Exercise: What is the primary factor influencing how far a marine magnetometer can detect a target?
  • Video class: Introduction to Marine Magnetometry - part 2 05m
  • Exercise: What is the correct relationship between mass and nanotesla at different distances?
  • Video class: Introduction to Marine Magnetometry - part 3 08m
  • Exercise: How is the Earth's magnetic field distorted by objects?
  • Video class: Introduction to Marine Magnetometry - part 4 07m
  • Exercise: What is the primary function of a transverse radiometer in a survey grid?
  • Video class: Introduction to Marine Magnetometry - part 5-1 09m
  • Exercise: What is a key consideration for designing a survey with a magnetometer?
  • Video class: Introduction to Marine Magnetometry - part 5-2 05m
  • Exercise: What is the expected magnetic anomaly for a hollow object in the survey grid?

This free course includes:

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46 minutes of online video course

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Digital certificate of course completion (Free)

Icon for exercises to practice what you've learned

Exercises to train your knowledge

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100% free, from content to certificate

What determines the detection range of a marine magnetometer for an underwater target?

Detection range is primarily determined by the target's magnetic mass and its distance from the sensor; magnetic signals weaken rapidly with distance.

How do submerged objects distort the Earth's magnetic field?

Ferrous objects become magnetized by the Earth's field and create local magnetic anomalies that a marine magnetometer can measure.

Why is survey-grid design important in marine magnetometry?

Line spacing, sensor altitude, and survey direction must be planned to ensure magnetic anomalies are detected and accurately located.

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