The frigid zone refers to the regions near the North and South Poles, where the climate is extremely cold. It includes areas within the Arctic Circle in the Northern Hemisphere and the Antarctic Circle in the Southern Hemisphere. The frigid ...
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The Earth’s axis is an imaginary line that runs from the North Pole to the South Pole, around which the Earth rotates. The axis is tilted at an angle of 23.5°, which is significant because it causes the changing of ...
A map legend, also known as a map key, is a small box or section on a map that explains the meaning of the symbols, colors, and lines used on the map. It helps readers understand what different symbols represent, ...
The Equator is an imaginary line that divides the Earth into two equal halves: the Northern Hemisphere and the Southern Hemisphere. It is located at 0° latitude and is the longest parallel of latitude. The Equator is equidistant from the ...
Time zones deviate from straight lines to accommodate the boundaries of countries and regions. Although time zones are based on lines of longitude, they are adjusted to ensure that neighboring areas within a country or region share the same time. ...
Local time is the time observed at a specific place, based on the position of the sun in the sky. It is determined by the local meridian, which is the line of longitude passing through that place. As the Earth ...
A globe is better for geographical accuracy because it represents the Earth in its true shape—a sphere. Unlike maps, which are flat and can distort distances, areas, and shapes, a globe accurately shows the relative positions of continents, countries, and ...
The 180° longitude is significant because it marks the location of the International Date Line (IDL), an imaginary line running from the North Pole to the South Pole. The IDL is where the date changes, moving from one calendar day ...
The scale of a map affects how much of the Earth’s surface is represented on the map. It shows the ratio between distances on the map and the actual distances on the ground. A larger scale map (e.g., 1 cm ...
The Earth is not a perfect sphere; it is slightly flattened at the poles and bulging at the equator, making it an oblate spheroid. This shape occurs because the Earth’s rotation causes it to slightly stretch around the middle. The ...