
The imaginary lines on the globe that are parallel to the equator are called _____________.
A. Latitudes
B. Longitudes
C. Imaginary Lines
D. All of these
Answer
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Hint: It is the estimation of distance north or south of the Equator. It is estimated with 180 nonexistent lines that structure hovers around the Earth east-west, corresponding to the Equator. These lines are known as equals. A hover of it is a nonexistent ring connecting all focuses sharing an equal.
Complete step-by-step solution:
In geography, the latitude is a geographic organization that indicates the north-south situation of a point on the Earth's surface. Latitude is a point (characterized beneath) which goes from $0^\circ $ at the Equator to $90^\circ $ (North or South) at the poles. Lines of consistent latitude, or equals, run east-west as circles corresponding to the equator. Latitude is utilized along with longitude to determine the exact area of highlights on the outside of the Earth. All alone, the term latitude should be taken to be the geodetic latitude as characterized beneath. Quickly, geodetic latitude at a point is the point-shaped by the vector opposite (or ordinary) to the ellipsoidal surface starting there, and the tropical plane. Likewise characterized are six assistant latitudes that are utilized in unique applications. The graticule is framed by the lines of consistent latitude and steady longitude, which are developed concerning the turn hub of the Earth. The essential reference focuses are where the pivot of a turn of the Earth crosses the reference surface. Planes that contain the revolution pivot converge the surface at the meridians, and the point between anyone’s meridian plane and that through Greenwich (the Prime Meridian) characterizes the longitude: meridians are lines of constant longitude. The plane through the focal point of the Earth and opposite to the revolution hub meets the surface at an incredible circle called the Equator. Planes corresponding to the central plane meet the surface around and around of consistent latitude; these are the equals. The Equator has a latitude of $0^\circ $, the North Pole has a latitude of $90^\circ $ North (composed $90^\circ {\text{N}} $ or $ + 90^\circ $), and the South Pole has a latitude of $90^\circ $ South (composed $90^\circ {\text{S}} $ or $ - 90^\circ $). The latitude of a self-assertive point is the point between the central plane and the typical to the surface by then: the ordinary to the outside of the circle is along the spanning vector. The latitude, as characterized in this path for the circle, is frequently named the circular latitude, to evade vagueness with the geodetic latitude and the assistant latitudes characterized in resulting segments of this article.
Thus, option (A) is correct.
Note: Other valuable, however nonexistent, lines around Earth that are corresponding to the Equator are called lines of scope. They are numbered from $0^\circ $ to $90^\circ $.
Complete step-by-step solution:
In geography, the latitude is a geographic organization that indicates the north-south situation of a point on the Earth's surface. Latitude is a point (characterized beneath) which goes from $0^\circ $ at the Equator to $90^\circ $ (North or South) at the poles. Lines of consistent latitude, or equals, run east-west as circles corresponding to the equator. Latitude is utilized along with longitude to determine the exact area of highlights on the outside of the Earth. All alone, the term latitude should be taken to be the geodetic latitude as characterized beneath. Quickly, geodetic latitude at a point is the point-shaped by the vector opposite (or ordinary) to the ellipsoidal surface starting there, and the tropical plane. Likewise characterized are six assistant latitudes that are utilized in unique applications. The graticule is framed by the lines of consistent latitude and steady longitude, which are developed concerning the turn hub of the Earth. The essential reference focuses are where the pivot of a turn of the Earth crosses the reference surface. Planes that contain the revolution pivot converge the surface at the meridians, and the point between anyone’s meridian plane and that through Greenwich (the Prime Meridian) characterizes the longitude: meridians are lines of constant longitude. The plane through the focal point of the Earth and opposite to the revolution hub meets the surface at an incredible circle called the Equator. Planes corresponding to the central plane meet the surface around and around of consistent latitude; these are the equals. The Equator has a latitude of $0^\circ $, the North Pole has a latitude of $90^\circ $ North (composed $90^\circ {\text{N}} $ or $ + 90^\circ $), and the South Pole has a latitude of $90^\circ $ South (composed $90^\circ {\text{S}} $ or $ - 90^\circ $). The latitude of a self-assertive point is the point between the central plane and the typical to the surface by then: the ordinary to the outside of the circle is along the spanning vector. The latitude, as characterized in this path for the circle, is frequently named the circular latitude, to evade vagueness with the geodetic latitude and the assistant latitudes characterized in resulting segments of this article.
Thus, option (A) is correct.
Note: Other valuable, however nonexistent, lines around Earth that are corresponding to the Equator are called lines of scope. They are numbered from $0^\circ $ to $90^\circ $.
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