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

360687 At a point \(A\) on the earth's surface the angle of dip, \(\delta=+25^{\circ}\). At a point \(B\) on the earth's surface the angle of dip, \(\delta=-25^{\circ}\). We can interpret that:

1 \(A\) and \(B\) are both located in the northern hemisphere.
2 \(A\) is located in the southern hemisphere and \(B\) is located in the northern hemisphere.
3 \(A\) is located in the northern hemisphere and \(B\) is located in the southern hemisphere.
4 \(A\) and \(B\) are both located in the southern hemisphere.
PHXII05:MAGNETISM and MATTER

360688 Assertion :
A dip circle (used for dip measurement) is taken to geomagnetic equator. The needle is allowed to move in a vertical plane. The needle will stay in any direction when it is released.
Reason :
At geomagnetic equator \(B_{v}=0\).

1 Both Assertion and Reason are correct and Reason is the correct explanation of the Assertion.
2 Both Assertion and Reason are correct but Reason is not the correct explanation of the Assertion.
3 Assertion is correct but Reason is incorrect.
4 Assertion is incorrect but reason is correct.
PHXII05:MAGNETISM and MATTER

360689 At certain place, the horizontal component of earth's magnetic field is 3.0\(G\) and the angle of dip at that place is \(30^{\circ}\). The magnetic field of earth at that location

1 4.5\(G\)
2 5.1\(G\)
3 3.5\(G\)
4 6.0\(G\)
PHXII05:MAGNETISM and MATTER

360690 The angles of dip at the Earth's magnetic poles and the equator respectively are

1 \(30^{\circ}, 60^{\circ}\)
2 \(90^\circ ,0^\circ \)
3 \(30^{\circ}, 90^{\circ}\)
4 \(0^\circ ,0^\circ \)
PHXII05:MAGNETISM and MATTER

360687 At a point \(A\) on the earth's surface the angle of dip, \(\delta=+25^{\circ}\). At a point \(B\) on the earth's surface the angle of dip, \(\delta=-25^{\circ}\). We can interpret that:

1 \(A\) and \(B\) are both located in the northern hemisphere.
2 \(A\) is located in the southern hemisphere and \(B\) is located in the northern hemisphere.
3 \(A\) is located in the northern hemisphere and \(B\) is located in the southern hemisphere.
4 \(A\) and \(B\) are both located in the southern hemisphere.
PHXII05:MAGNETISM and MATTER

360688 Assertion :
A dip circle (used for dip measurement) is taken to geomagnetic equator. The needle is allowed to move in a vertical plane. The needle will stay in any direction when it is released.
Reason :
At geomagnetic equator \(B_{v}=0\).

1 Both Assertion and Reason are correct and Reason is the correct explanation of the Assertion.
2 Both Assertion and Reason are correct but Reason is not the correct explanation of the Assertion.
3 Assertion is correct but Reason is incorrect.
4 Assertion is incorrect but reason is correct.
PHXII05:MAGNETISM and MATTER

360689 At certain place, the horizontal component of earth's magnetic field is 3.0\(G\) and the angle of dip at that place is \(30^{\circ}\). The magnetic field of earth at that location

1 4.5\(G\)
2 5.1\(G\)
3 3.5\(G\)
4 6.0\(G\)
PHXII05:MAGNETISM and MATTER

360690 The angles of dip at the Earth's magnetic poles and the equator respectively are

1 \(30^{\circ}, 60^{\circ}\)
2 \(90^\circ ,0^\circ \)
3 \(30^{\circ}, 90^{\circ}\)
4 \(0^\circ ,0^\circ \)
PHXII05:MAGNETISM and MATTER

360687 At a point \(A\) on the earth's surface the angle of dip, \(\delta=+25^{\circ}\). At a point \(B\) on the earth's surface the angle of dip, \(\delta=-25^{\circ}\). We can interpret that:

1 \(A\) and \(B\) are both located in the northern hemisphere.
2 \(A\) is located in the southern hemisphere and \(B\) is located in the northern hemisphere.
3 \(A\) is located in the northern hemisphere and \(B\) is located in the southern hemisphere.
4 \(A\) and \(B\) are both located in the southern hemisphere.
PHXII05:MAGNETISM and MATTER

360688 Assertion :
A dip circle (used for dip measurement) is taken to geomagnetic equator. The needle is allowed to move in a vertical plane. The needle will stay in any direction when it is released.
Reason :
At geomagnetic equator \(B_{v}=0\).

1 Both Assertion and Reason are correct and Reason is the correct explanation of the Assertion.
2 Both Assertion and Reason are correct but Reason is not the correct explanation of the Assertion.
3 Assertion is correct but Reason is incorrect.
4 Assertion is incorrect but reason is correct.
PHXII05:MAGNETISM and MATTER

360689 At certain place, the horizontal component of earth's magnetic field is 3.0\(G\) and the angle of dip at that place is \(30^{\circ}\). The magnetic field of earth at that location

1 4.5\(G\)
2 5.1\(G\)
3 3.5\(G\)
4 6.0\(G\)
PHXII05:MAGNETISM and MATTER

360690 The angles of dip at the Earth's magnetic poles and the equator respectively are

1 \(30^{\circ}, 60^{\circ}\)
2 \(90^\circ ,0^\circ \)
3 \(30^{\circ}, 90^{\circ}\)
4 \(0^\circ ,0^\circ \)
PHXII05:MAGNETISM and MATTER

360687 At a point \(A\) on the earth's surface the angle of dip, \(\delta=+25^{\circ}\). At a point \(B\) on the earth's surface the angle of dip, \(\delta=-25^{\circ}\). We can interpret that:

1 \(A\) and \(B\) are both located in the northern hemisphere.
2 \(A\) is located in the southern hemisphere and \(B\) is located in the northern hemisphere.
3 \(A\) is located in the northern hemisphere and \(B\) is located in the southern hemisphere.
4 \(A\) and \(B\) are both located in the southern hemisphere.
PHXII05:MAGNETISM and MATTER

360688 Assertion :
A dip circle (used for dip measurement) is taken to geomagnetic equator. The needle is allowed to move in a vertical plane. The needle will stay in any direction when it is released.
Reason :
At geomagnetic equator \(B_{v}=0\).

1 Both Assertion and Reason are correct and Reason is the correct explanation of the Assertion.
2 Both Assertion and Reason are correct but Reason is not the correct explanation of the Assertion.
3 Assertion is correct but Reason is incorrect.
4 Assertion is incorrect but reason is correct.
PHXII05:MAGNETISM and MATTER

360689 At certain place, the horizontal component of earth's magnetic field is 3.0\(G\) and the angle of dip at that place is \(30^{\circ}\). The magnetic field of earth at that location

1 4.5\(G\)
2 5.1\(G\)
3 3.5\(G\)
4 6.0\(G\)
PHXII05:MAGNETISM and MATTER

360690 The angles of dip at the Earth's magnetic poles and the equator respectively are

1 \(30^{\circ}, 60^{\circ}\)
2 \(90^\circ ,0^\circ \)
3 \(30^{\circ}, 90^{\circ}\)
4 \(0^\circ ,0^\circ \)