If θ1 and θ2 be the apparent angles of dip observed in two vertical planes at right angles to each other, then the true angle of dip θ is given by:
A
cot2θ=cot2θ1+cot2θ2
B
tan2θ=tan2θ1+tan2θ2
C
cot2θ=cot2θ1−tan2θ2
D
tan2θ=tan2θ1−tan2θ2
Step-by-Step Solution
True Dip (θ): The true angle of dip is related to the vertical component (V) and horizontal component (H) of Earth's magnetic field in the magnetic meridian by tanθ=HV or cotθ=VH.
Apparent Dip: In a vertical plane making an angle α with the magnetic meridian, the effective horizontal component is H′=Hcosα, while the vertical component V remains the same. The apparent dip θ1 is given by:
tanθ1=HcosαV⇒cotθ1=VHcosα=cotθcosαcosα=cotθcotθ1
Second Plane: Since the second plane is perpendicular to the first, it makes an angle (90∘−α) with the meridian. The apparent dip θ2 is:
tanθ2=Hcos(90∘−α)V=HsinαV⇒cotθ2=VHsinα=cotθsinαsinα=cotθcotθ2
Derivation: Using the identity sin2α+cos2α=1:
(cotθcotθ2)2+(cotθcotθ1)2=1cot2θcot2θ2+cot2θ1=1cot2θ=cot2θ1+cot2θ2
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