Visualizing the Magnetic Meridian
Imagine you are standing on the Earth's surface, holding a magnetic compass. The vertical plane that perfectly aligns with the magnetic north and south poles is called the Magnetic Meridian. If you allow a magnetic needle to pivot vertically in this plane, the angle it makes with the horizontal is the true dip (ρ).
But what happens if you force the needle to pivot in a different vertical plane? Let's say this new plane is at an angle α to the magnetic meridian. The angle the needle makes with the horizontal in this new plane is called the apparent dip (ρ′).
The Master Equation
To understand the relationship between true and apparent dip, we need to look at the components of the Earth's magnetic field. When we shift to a new vertical plane, the vertical component of the magnetic field (BV) remains exactly the same. However, the horizontal component (BH) changes because we are only looking at its projection in the new plane.
The new horizontal component is given by:
BH′=BHcosα
Now, let's write the equations for the dip angles. For the true dip, the tangent of the angle is the ratio of the vertical to the horizontal component:
tanρ=BHBV
Similarly, for the apparent dip:
tanρ′=BH′BV′
Final Calculation
Let's substitute our known values into the apparent dip equation. Since
BV′=BV and
BH′=BHcosα, we get:
tanρ′=BHcosαBV
We can rewrite this using our true dip equation:
tanρ′=cosαtanρ
Here is the crucial mathematical catch: the value of
cosα is always less than or equal to
1. This means that
cosα1 is always greater than or equal to
1. Therefore:
tanρ′≥tanρ
Since the tangent function is strictly increasing for angles between
0∘ and
90∘, it directly implies that:
ρ′≥ρ
This means the true dip is always less than or equal to the apparent dip. The correct option is (b).