Step 1: The Earth's magnetic field at any location can be represented as a vector quantity, which has both horizontal and vertical components relative to the Earth's surface.
Step 2: To fully describe the magnetic field, we use magnetic elements such as:
Declination (\( D \)): The angle between the geographic north (true north) and the horizontal component of the Earth's magnetic field. It indicates the direction of the magnetic north relative to true north.
Inclination or Dip (\( I \)): The angle made by the total magnetic field vector with the horizontal plane. It measures how much the magnetic field dips below or rises above the horizontal.
Step 3: These magnetic elements are essential for compass navigation, geophysical surveys, and for understanding the Earth's magnetosphere. They allow navigators and scientists to accurately map the Earth's magnetic field and correct compass readings accordingly.