This is true due to the difference in gravitational pull between the poles and the equator. At the poles, the Earth's rotation causes a slightly smaller centrifugal force, making gravity slightly stronger compared to the equator. This results in objects weighing slightly more at higher latitudes.
used by spinning motion of the earth around its axis passing through the poles...the force being max at the equator...since at tym of formation, earth was in fluid state, the force of cohesion was small & could not balance the centrifugal force...hence it bulged out at the equator
No, Earth's magnetic poles are not located exactly on its geographical poles. The magnetic poles are located slightly off-axis and can shift over time due to changes in the Earth's magnetic field.
The gravitational acceleration will decrease slightly as you move from the equator to the poles due to the Earth's shape (oblate spheroid). This is because the centrifugal force is greater at the equator compared to the poles, which causes a slight decrease in the net gravitational force experienced at the equator.
The Earth's magnetic poles do not align perfectly with the geographic North and South poles due to the planet's molten iron core generating a magnetic field that is not perfectly symmetrical. This causes the magnetic poles to shift and be slightly off from the true geographic poles.
This slight bulging is due to the Earth's rotation. The centrifugal force generated as the Earth spins causes the equator to bulge out slightly, making it wider than the poles. This shape is known as an oblate spheroid.
It is measured around the surface of the earth. The atmosphere has its own measurement excluded from that of the Earth. The Equator is bulged, and the Poles slightly flattened. The figure given is for sea level, and ignores any mountains. The Poles are about 21.4 km closer to the centre of the Earth than the Equator is.
This is true due to the difference in gravitational pull between the poles and the equator. At the poles, the Earth's rotation causes a slightly smaller centrifugal force, making gravity slightly stronger compared to the equator. This results in objects weighing slightly more at higher latitudes.
used by spinning motion of the earth around its axis passing through the poles...the force being max at the equator...since at tym of formation, earth was in fluid state, the force of cohesion was small & could not balance the centrifugal force...hence it bulged out at the equator
earth
The Earth is an oblate spheroid, which means it is mostly spherical but slightly flattened at the poles and bulging at the equator due to its rotation. It is not a perfect sphere, but rather slightly squashed.
used by spinning motion of the earth around its axis passing through the poles...the force being max at the equator...since at tym of formation, earth was in fluid state, the force of cohesion was small & could not balance the centrifugal force...hence it bulged out at the equator
The true shape of the earth is oblate spheriod. This means that the Earth is slightly flattened at the poles and slightly bulging at the Equator.
A body will have the least weight at the Earth's poles due to the effect of centrifugal force and the Earth's oblate spheroid shape. This is because the radius at the poles is slightly larger than at the equator, resulting in slightly weaker gravity.
No, Earth's magnetic poles are not located exactly on its geographical poles. The magnetic poles are located slightly off-axis and can shift over time due to changes in the Earth's magnetic field.
The rotation of the Earth causes it to bulge slightly at the equator, making it slightly flattened at the poles and slightly wider at the equator. This shape is known as an oblate spheroid.
The gravitational acceleration will decrease slightly as you move from the equator to the poles due to the Earth's shape (oblate spheroid). This is because the centrifugal force is greater at the equator compared to the poles, which causes a slight decrease in the net gravitational force experienced at the equator.