Physical geography miscellaneous
- Equator represents
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An equator is the intersection of a sphere’s surface with the plane perpendicular to the sphere’s axis of rotation and containing the sphere’s center of mass. Notably, the Equator refers to the Earth’s equator, per above: an imaginary line on the Earth’s surface equidistant from the North Pole and South Pole, dividing the Earth into the Northern Hemisphere and Southern Hemisphere. Other planets and spherical astronomical bodies have equators similarly defined. The length of the Equator is roughly 40,075 kilometres.
Correct Option: B
An equator is the intersection of a sphere’s surface with the plane perpendicular to the sphere’s axis of rotation and containing the sphere’s center of mass. Notably, the Equator refers to the Earth’s equator, per above: an imaginary line on the Earth’s surface equidistant from the North Pole and South Pole, dividing the Earth into the Northern Hemisphere and Southern Hemisphere. Other planets and spherical astronomical bodies have equators similarly defined. The length of the Equator is roughly 40,075 kilometres.
- The scale that measures the intensity of earthquakes is called as
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An earthquake is measured by its Magnitude and Intensity. The Magnitude indicates the amount of energy released at the source (or epicenter) and is measured by the open-ended Richter Scale. The intensity of an earthquake at a particular locality indicates the violence of earth motion produced there by the earthquake. It is computed with the help of Modified Mercalli Scale (MMS).
Correct Option: E
An earthquake is measured by its Magnitude and Intensity. The Magnitude indicates the amount of energy released at the source (or epicenter) and is measured by the open-ended Richter Scale. The intensity of an earthquake at a particular locality indicates the violence of earth motion produced there by the earthquake. It is computed with the help of Modified Mercalli Scale (MMS).
- What is the epicentre of an Earthquake?
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The epicenter is the point on the Earth's surface that is directly above the hypocenter or focus, the point where an earthquake or underground explosion originates. In the case of earthquakes, the epicenter is directly above the point where the fault begins to rupture, and in most cases, it is the area of greatest damage.
Correct Option: D
The epicenter is the point on the Earth's surface that is directly above the hypocenter or focus, the point where an earthquake or underground explosion originates. In the case of earthquakes, the epicenter is directly above the point where the fault begins to rupture, and in most cases, it is the area of greatest damage.
- Prime Meridian passes through
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A prime meridian is a meridian, i.e. a line of longitude, at which longitude is defined to be 0°. An international conference in 1884 decided the prime meridian passes through the Royal Observatory, Greenwich in southeast London, United Kingdom, known simply as the prime meridian.
Correct Option: B
A prime meridian is a meridian, i.e. a line of longitude, at which longitude is defined to be 0°. An international conference in 1884 decided the prime meridian passes through the Royal Observatory, Greenwich in southeast London, United Kingdom, known simply as the prime meridian.
- The greatest erosive power of a river is associated with
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Erosive power of a stream is proportional to the square of the velocity. Thus, when discharge increases, the depth increases and the velocity increases, resulting in dramatic increase of erosive
power. As the volume flowing in a stream increases, the stream's erosive power also increases. At a bend in a stream the water's momentum carries the mass of the water against the outer bank. The greater depth on the outer side of the bend also leads to higher velocity at the outer bank. The greater velocity combined with the greater inertial force on the outer bank erodes a deeper channel. The result of all these actions is a meanderCorrect Option: B
Erosive power of a stream is proportional to the square of the velocity. Thus, when discharge increases, the depth increases and the velocity increases, resulting in dramatic increase of erosive
power. As the volume flowing in a stream increases, the stream's erosive power also increases. At a bend in a stream the water's momentum carries the mass of the water against the outer bank. The greater depth on the outer side of the bend also leads to higher velocity at the outer bank. The greater velocity combined with the greater inertial force on the outer bank erodes a deeper channel. The result of all these actions is a meander