The Earth’s Magnetism and Magnetic Instruments
PHXII05:MAGNETISM and MATTER

360661 The angle between the magnetic meridian and geographical meridian is called

1 Angle of declination
2 Angle of dip
3 Power of magnetic field
4 Magnetic moment
PHXII05:MAGNETISM and MATTER

360662 Isogonic lines on magnetic map joins the places having

1 Same angle of dip
2 Zero angle of dip
3 Same angle of declination
4 Zero angle of declination
PHXII05:MAGNETISM and MATTER

360663 If \(\theta_{1}\) and \(\theta_{2}\) are the apparent angles of dip observed in two vertical planes at right angles to each other, then the true angle of dip \(\theta\) is given by :-

1 \(\tan ^{2} \theta=\tan ^{2} \theta_{1}+\tan ^{2} \theta_{2}\)
2 \(\cot ^{2} \theta=\cot ^{2} \theta_{1}+\cot ^{2} \theta_{2}\)
3 \(\tan ^{2} \theta=\tan ^{2} \theta_{1}-\tan ^{2} \theta_{2}\)
4 \(\cot ^{2} \theta=\cot ^{2} \theta_{1}-\cot ^{2} \theta_{2}\)
PHXII05:MAGNETISM and MATTER

360664 A dip circle shows apparent dip of \(60^{\circ}\) at a place where the true dip is \(45^{\circ}\). If the dip circle is rotated by \(90^{\circ}\) the apparent dip will be equal to

1 \(\tan ^{-1} \sqrt{\dfrac{2}{3}}\)
2 \(\sin ^{-1} \sqrt{\dfrac{2}{3}}\)
3 \(\cos ^{-1} \sqrt{\dfrac{2}{3}}\)
4 \(\cot ^{-1} \sqrt{\dfrac{2}{3}}\)
PHXII05:MAGNETISM and MATTER

360665 If a magnet is suspended at angle \(30^{\circ}\) to the magnetic meridian, the dip needle makes angle of \(45^{\circ}\) with the horizontal. The real dip is

1 \(\tan ^{-1}(\sqrt{3} / 2)\)
2 \(\tan ^{-1}(\sqrt{3})\)
3 \(\tan ^{-1}\left(\dfrac{3}{\sqrt{2}}\right)\)
4 \(\tan ^{-1}\left(\dfrac{2}{\sqrt{3}}\right)\)
PHXII05:MAGNETISM and MATTER

360661 The angle between the magnetic meridian and geographical meridian is called

1 Angle of declination
2 Angle of dip
3 Power of magnetic field
4 Magnetic moment
PHXII05:MAGNETISM and MATTER

360662 Isogonic lines on magnetic map joins the places having

1 Same angle of dip
2 Zero angle of dip
3 Same angle of declination
4 Zero angle of declination
PHXII05:MAGNETISM and MATTER

360663 If \(\theta_{1}\) and \(\theta_{2}\) are the apparent angles of dip observed in two vertical planes at right angles to each other, then the true angle of dip \(\theta\) is given by :-

1 \(\tan ^{2} \theta=\tan ^{2} \theta_{1}+\tan ^{2} \theta_{2}\)
2 \(\cot ^{2} \theta=\cot ^{2} \theta_{1}+\cot ^{2} \theta_{2}\)
3 \(\tan ^{2} \theta=\tan ^{2} \theta_{1}-\tan ^{2} \theta_{2}\)
4 \(\cot ^{2} \theta=\cot ^{2} \theta_{1}-\cot ^{2} \theta_{2}\)
PHXII05:MAGNETISM and MATTER

360664 A dip circle shows apparent dip of \(60^{\circ}\) at a place where the true dip is \(45^{\circ}\). If the dip circle is rotated by \(90^{\circ}\) the apparent dip will be equal to

1 \(\tan ^{-1} \sqrt{\dfrac{2}{3}}\)
2 \(\sin ^{-1} \sqrt{\dfrac{2}{3}}\)
3 \(\cos ^{-1} \sqrt{\dfrac{2}{3}}\)
4 \(\cot ^{-1} \sqrt{\dfrac{2}{3}}\)
PHXII05:MAGNETISM and MATTER

360665 If a magnet is suspended at angle \(30^{\circ}\) to the magnetic meridian, the dip needle makes angle of \(45^{\circ}\) with the horizontal. The real dip is

1 \(\tan ^{-1}(\sqrt{3} / 2)\)
2 \(\tan ^{-1}(\sqrt{3})\)
3 \(\tan ^{-1}\left(\dfrac{3}{\sqrt{2}}\right)\)
4 \(\tan ^{-1}\left(\dfrac{2}{\sqrt{3}}\right)\)
PHXII05:MAGNETISM and MATTER

360661 The angle between the magnetic meridian and geographical meridian is called

1 Angle of declination
2 Angle of dip
3 Power of magnetic field
4 Magnetic moment
PHXII05:MAGNETISM and MATTER

360662 Isogonic lines on magnetic map joins the places having

1 Same angle of dip
2 Zero angle of dip
3 Same angle of declination
4 Zero angle of declination
PHXII05:MAGNETISM and MATTER

360663 If \(\theta_{1}\) and \(\theta_{2}\) are the apparent angles of dip observed in two vertical planes at right angles to each other, then the true angle of dip \(\theta\) is given by :-

1 \(\tan ^{2} \theta=\tan ^{2} \theta_{1}+\tan ^{2} \theta_{2}\)
2 \(\cot ^{2} \theta=\cot ^{2} \theta_{1}+\cot ^{2} \theta_{2}\)
3 \(\tan ^{2} \theta=\tan ^{2} \theta_{1}-\tan ^{2} \theta_{2}\)
4 \(\cot ^{2} \theta=\cot ^{2} \theta_{1}-\cot ^{2} \theta_{2}\)
PHXII05:MAGNETISM and MATTER

360664 A dip circle shows apparent dip of \(60^{\circ}\) at a place where the true dip is \(45^{\circ}\). If the dip circle is rotated by \(90^{\circ}\) the apparent dip will be equal to

1 \(\tan ^{-1} \sqrt{\dfrac{2}{3}}\)
2 \(\sin ^{-1} \sqrt{\dfrac{2}{3}}\)
3 \(\cos ^{-1} \sqrt{\dfrac{2}{3}}\)
4 \(\cot ^{-1} \sqrt{\dfrac{2}{3}}\)
PHXII05:MAGNETISM and MATTER

360665 If a magnet is suspended at angle \(30^{\circ}\) to the magnetic meridian, the dip needle makes angle of \(45^{\circ}\) with the horizontal. The real dip is

1 \(\tan ^{-1}(\sqrt{3} / 2)\)
2 \(\tan ^{-1}(\sqrt{3})\)
3 \(\tan ^{-1}\left(\dfrac{3}{\sqrt{2}}\right)\)
4 \(\tan ^{-1}\left(\dfrac{2}{\sqrt{3}}\right)\)
PHXII05:MAGNETISM and MATTER

360661 The angle between the magnetic meridian and geographical meridian is called

1 Angle of declination
2 Angle of dip
3 Power of magnetic field
4 Magnetic moment
PHXII05:MAGNETISM and MATTER

360662 Isogonic lines on magnetic map joins the places having

1 Same angle of dip
2 Zero angle of dip
3 Same angle of declination
4 Zero angle of declination
PHXII05:MAGNETISM and MATTER

360663 If \(\theta_{1}\) and \(\theta_{2}\) are the apparent angles of dip observed in two vertical planes at right angles to each other, then the true angle of dip \(\theta\) is given by :-

1 \(\tan ^{2} \theta=\tan ^{2} \theta_{1}+\tan ^{2} \theta_{2}\)
2 \(\cot ^{2} \theta=\cot ^{2} \theta_{1}+\cot ^{2} \theta_{2}\)
3 \(\tan ^{2} \theta=\tan ^{2} \theta_{1}-\tan ^{2} \theta_{2}\)
4 \(\cot ^{2} \theta=\cot ^{2} \theta_{1}-\cot ^{2} \theta_{2}\)
PHXII05:MAGNETISM and MATTER

360664 A dip circle shows apparent dip of \(60^{\circ}\) at a place where the true dip is \(45^{\circ}\). If the dip circle is rotated by \(90^{\circ}\) the apparent dip will be equal to

1 \(\tan ^{-1} \sqrt{\dfrac{2}{3}}\)
2 \(\sin ^{-1} \sqrt{\dfrac{2}{3}}\)
3 \(\cos ^{-1} \sqrt{\dfrac{2}{3}}\)
4 \(\cot ^{-1} \sqrt{\dfrac{2}{3}}\)
PHXII05:MAGNETISM and MATTER

360665 If a magnet is suspended at angle \(30^{\circ}\) to the magnetic meridian, the dip needle makes angle of \(45^{\circ}\) with the horizontal. The real dip is

1 \(\tan ^{-1}(\sqrt{3} / 2)\)
2 \(\tan ^{-1}(\sqrt{3})\)
3 \(\tan ^{-1}\left(\dfrac{3}{\sqrt{2}}\right)\)
4 \(\tan ^{-1}\left(\dfrac{2}{\sqrt{3}}\right)\)
PHXII05:MAGNETISM and MATTER

360661 The angle between the magnetic meridian and geographical meridian is called

1 Angle of declination
2 Angle of dip
3 Power of magnetic field
4 Magnetic moment
PHXII05:MAGNETISM and MATTER

360662 Isogonic lines on magnetic map joins the places having

1 Same angle of dip
2 Zero angle of dip
3 Same angle of declination
4 Zero angle of declination
PHXII05:MAGNETISM and MATTER

360663 If \(\theta_{1}\) and \(\theta_{2}\) are the apparent angles of dip observed in two vertical planes at right angles to each other, then the true angle of dip \(\theta\) is given by :-

1 \(\tan ^{2} \theta=\tan ^{2} \theta_{1}+\tan ^{2} \theta_{2}\)
2 \(\cot ^{2} \theta=\cot ^{2} \theta_{1}+\cot ^{2} \theta_{2}\)
3 \(\tan ^{2} \theta=\tan ^{2} \theta_{1}-\tan ^{2} \theta_{2}\)
4 \(\cot ^{2} \theta=\cot ^{2} \theta_{1}-\cot ^{2} \theta_{2}\)
PHXII05:MAGNETISM and MATTER

360664 A dip circle shows apparent dip of \(60^{\circ}\) at a place where the true dip is \(45^{\circ}\). If the dip circle is rotated by \(90^{\circ}\) the apparent dip will be equal to

1 \(\tan ^{-1} \sqrt{\dfrac{2}{3}}\)
2 \(\sin ^{-1} \sqrt{\dfrac{2}{3}}\)
3 \(\cos ^{-1} \sqrt{\dfrac{2}{3}}\)
4 \(\cot ^{-1} \sqrt{\dfrac{2}{3}}\)
PHXII05:MAGNETISM and MATTER

360665 If a magnet is suspended at angle \(30^{\circ}\) to the magnetic meridian, the dip needle makes angle of \(45^{\circ}\) with the horizontal. The real dip is

1 \(\tan ^{-1}(\sqrt{3} / 2)\)
2 \(\tan ^{-1}(\sqrt{3})\)
3 \(\tan ^{-1}\left(\dfrac{3}{\sqrt{2}}\right)\)
4 \(\tan ^{-1}\left(\dfrac{2}{\sqrt{3}}\right)\)