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Definition of parallel: On a globe, a circle parallel to the equator.
The parallels are the trajectories formed by the rotation of the earth at a point on the earth's surface. All the parallels are parallel to each other and perpendicular to the meridians, which indicate the east-west direction. The weft is shaped as a circle.
The size of the weft coil varies, with the equator being the largest latitude coil, and gradually shrinking from the equator to the poles, and then to the north and south poles to the points. The meridians and parallels were drawn on globes and maps in order to determine the position and direction on the earth, and there were no latitude and longitude lines on the ground.
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Parallel: The trajectory formed by the rotation of the earth at a point on the earth's surface.
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The thread perpendicular to the warp is called the weft. The weft is a circle of varying lengths.
The longest coil of latitude, the equator, is called the 0° parallel. The latitude measured from the equator to the north is called the north latitude; The one to the south is called the southern latitude. There are 90° north and south latitudes. The North Pole is 90° north latitude.
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Latitude is a geographical concept, also known as latitude and longitude or latitude lines. It refers to a virtual line on the earth's surface from the pole to the equator, which is used to divide the latitude or latitude zone on the earth's surface. Here is an 800-word explanation of the definition of weft:
A line of latitude is a line on the surface of the earth, a virtual line perpendicular to the earth's axis. They extend from the poles of the Earth (North and South Poles) to the equator, circumnavigating the Earth. The latitude line is one of the units of division of the earth and is used to determine the latitude or latitude zone of the earth's surface.
The division of the weft zenma is based on the Earth's equator, which divides the earth's surface into an infinite number of equally spaced zones of latitude. The equator is the largest latitude of the Earth, located in the middle of the Earth, with a latitude of 0 degrees. The equator divides the earth into the northern and southern hemispheres.
North latitude and southern latitude are two directions relative to the equator, north latitude is the angle from the equator to the north, and southern latitude is the angle from the equator to the south.
The way the parallels are measured is expressed in angles, measured in degrees. The Earth's equator is 0 degrees of latitude, the North Pole is 90 degrees north latitude, and the South Pole is 90 degrees south latitude. In order to demarcate the Earth's surface more precisely, parallels passing beyond the equator are usually expressed in minutes and seconds.
The division of latitudes is very important for geolocation and navigation. Through the parallel, we can determine the latitude of any place on the planet. Latitude is the angle of a location on the earth's surface relative to the equator, and it helps us determine the north or south direction of the location.
The density of the weft is not the same, and the closer it is to the equator, the higher the density of the weft. Near the equator, the distance between the parallels is smaller, while the distance between the parallels gradually increases as they move north or south. This is because the Earth is an approximate ellipsoidal shape, not a perfect sphere.
The division and measurement of wefts are of great application value in many fields. They all play a vital role in navigation, aviation, meteorology, cartography, and geographical research. The presence and division of parallels allows us to better understand the distribution and characteristics of the Earth's surface and helps us better understand the Earth's natural and human environment.
In summary, the parallels are the virtual lines from the pole to the equator on the earth's surface that are used to divide the latitude or latitude zones on the earth's surface. They help us orient and navigate, and are of great importance for nautical, aeronautical, meteorological, and geographical research.
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Explanation of the weft.
1) [weft] Horizontal lines woven on the Kai calendar of weft weaving (2) [parallel] Where the plane parallel to the equator, the circle line that cuts through the earth and intersects with the earth's surface is called the weft Detailed explanation (1).Horizontal lines on weft or braids. (2).
A line along the Earth's surface that is assumed to be parallel to the equator as assumed in geography. See " Latitude ".
Word decomposition Explanation of weft Weft (weft) ě weaves cloth with a shuttle weaving horizontal yarn, the horizontal line of the knitted fabric, as opposed to "warp": weft. Weft.
Warp and weft. Geographically refers to the line on the ground that runs parallel to the equator: latitude.
East-West Cross Road: Wei Mo. Ancient names for planets:
Latitude star. Title: Ancient Qiwei (refers to the interpretation of the theological line in the Han Dynasty à made of silk, cotton, hemp, metal, etc., which is slender and can be arbitrarily twisted and turned
Silk thread. Cotton. Coil.
Wire rod. Cord. Geometrically, it refers to the figure formed by the arbitrary movement of a point
Straight line. Curve. Lines.
Something like a thread: light. Line of sight.
Clues (..)The clue of the matter or.
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A meridian is the arc of the Earth's surface that connects the north and south poles and is perpendicular to the equator. Also called meridian. Two warp threads facing each other form a warp coil.
The latitude line refers to the trajectory formed by the rotation of the earth at a point on the earth's surface. All the parallels are parallel to each other and perpendicular to the meridians, which point east-west. The weft is shaped as a circle.
Characteristics of the meridian: The meridian represents the north-south direction of the locality. Points on the same meridian have the same longitude.
That is, the great circle formed by intersecting the plane of the earth's axis with the ground is called a warp circle. All the meridian circles intersect at the north and south poles and are divided into two semicircles by the poles, called meridians or meridians. The meridian indicates the north-south direction; Orthogonal to all parallels.
Each meridian on Earth is roughly equal in length.
Characteristics of weft: 1. The weft is perpendicular to each other.
2. All the wefts are circles.
3. The length of the parallels with the same latitude is the same, and the length of the parallels with different latitudes is not the same The equator is the longest parallel, which is reduced to points towards the poles.
4. All the wefts are parallel to each other.
5. The parallels except the poles point to the east-west direction.
The latitude and longitude lines on the globe together form the graticule. With graticules and their latitude and longitude, the location of various points on the earth is easily determined. Two different locations on Earth can have the same latitude or longitude, but it is not possible to have both the same latitude and the same longitude.
Therefore, different places and different positions on the earth can be represented by corresponding latitude and longitude.
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The longitude and latitude lines are drawn on globes and maps in order to determine the position and direction on the earth, and they are parallel on the ground. The thread perpendicular to the warp thread is called the weft thread.
The weft is a circle of varying lengths. The longest parallel is the equator. Because the warp bucket group indicates the north-south direction, the meridian is also called the meridian.
Internationally, the meridian that passes through the original site of the Greenwich Observatory in the United Kingdom is called the 0° meridian, also known as the prime meridian. On Earth, the meridian line indicates the north-south direction, and the noisy latitude line indicates the east-west direction. Dividing line between the eastern and western hemispheres: 160° east longitude and 20° west longitude.
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